TRACE 2007 - Abstracts
Abstracts submitted till 12.04.2007.
Invited talks
Some aspects of
dendrochronology in the Baltics
Alar Läänelaid
Institute of Geography,
University of Tartu, Tartu, Estonia, e-mail:
alar.laanelaid@ut.ee
There are lots of common features in dendrochronology in the
three Baltic states – Estonia, Latvia and Lithuania: the same
tree species used (Scots pine Pinus sylvestris, Norway
spruce Picea abies, English oak Quercus robur),
similar climate, and many common research topics. The tradition
is strongest in Lithuania, where a tree-ring laboratory was
established in early 1960-ies. Chronology development of pine,
spruce and oak is carried out in all three states. At present
the dated pine chronologies extend back to the 12th century in
Estonia (with a gap) and Latvia and to the 11th century in
Lithuania. Spruce chronologies have minor extension because of
less findings and dating difficulties. Dated oak chronologies
exist in Estonia (AD 1264-1600) and in Lithuania (AD 1202-1418).
Prospective development directions of dendrochronology are more
alike in Estonia and Latvia: prolonging the chronologies,
dendrochronological dating for various tasks, dendroclimatology
and -ecology. A common prospective research topic for Latvia and
Lithuania is dendroprovenancing (historical timber trade from
the Baltics). In Lithuania the prospective directions include
genetical investigations of trees, stable isotopes, studies of
diurnal and seasonal growth, and investigation of introduced
tree species (e.g. Larix, Pseudotsuga). Several of
these research topics like dendroprovenancing, genetical studies
etc. require international co-operation within the Baltics and
with other countries. |
Reconstructing
Summer North Atlantic Oscillation (SNAO) variability over the
last centuries
Hans Linderholm1,
Chris Folland2, David Fereday2, Jim
Hurrell3, Sarah Ineson2, Jeff Knight2
and Adam Scaife2
1Earth
Sciences Centre, Göteborg University, Göteborg, Sweden, e-mail:
hansl@gvc.gu.se
2Hadley
Centre, Met Office, Exeter, UK
3National
Centre for Atmospheric Research, Boulder, Colorado, USA
Eigenvector analysis carried
out over the annual cycle in the North Atlantic and Arctic
region on seasonal NCEP mean sea level pressure data gives a set
of dipole patterns including the familiar winter North Atlantic
Oscillation. In summer, the scale of the EOF is smaller and its
southern node stretches from near UK to Scandinavia rather than
the Azores – Spain region seen in winter. Here, we use a new
daily data set of pressure at mean sea level, EMSLP, created
over 1850-2003. Its domain is limited to 70oN at its
northern-most latitude. An EOF analysis over 1881-2003 in summer
recreates mainly the southern part of the full summer EOF node
seen in NCEP data. Here we concentrate on July and August or
“high summer” as the temporal variation of pressure patterns at
this time is more similar than in June.
Regressions of the SNAO
pattern (chosen to be the daily EOF pattern) with surface
temperature and rainfall in high summer, show a strong influence
of the southern node of the SNAO for a region stretching from
the UK to Scandinavia. When the southern node has higher
pressure (positive SNAO), warmth and dryness is seen. Also, the
SNAO shows up strongly in cloudiness data. The SNAO varies
strongly interannually but also interdecadally, particularly in
the twentieth century. Relatively low SNAO values over 1920-1960
were followed by a sharp rise in the 1960s to 1970s with a
relatively high level maintained until the 1990s. This period
had several extreme UK summer droughts. Regression analysis of
the SNAO with sea surface temperature (SST) suggests that its
interdecadal variations can be related to the Atlantic
multidecadal oscillation (AMO), a periodic warming and cooling
of the North Atlantic that has been associated with variations
in the thermohaline circulation. Because the SNAO strongly
affects temperature and rainfall in Scotland and Scandinavia,
paleoclimate data based on tree rings have been used to
reconstruct an index of the SNAO back to the eighteenth century
with some skill, mainly on decadal time scales. The likely skill
of the reconstructions and the evolution of SNAO over the last
centuries is discussed. |
up
Talks
Representative Mean
Growth Behaviour of Forest Stands – Methodical Aspects from
Dendrochronology and Forest Mensuration
Dr. Wolfgang Beck
Federal research Centre for
Forestry and Forest Products, Institute for Forest Ecology and
Forest Inventory, Eberswalde, Germany
e-mail:
wbeck@bfh-inst7.fh-eberswalde.de
Building up tree ring index
chronologies requires the calculation of a mean index value at
each time step which represents the typical stand wide growth
reaction and which enhances the common climate signal of the
chronology. Mostly TUKEY’s biweight robust mean is used
therefore. This method calculates a mean close to the median
which includes this part of series which is close to the centre
of the distribution and excludes the tail. Inclusion is done by
a weighing function, values above a threshold are excluded. This
procedure is applied time step by time step, but the crucial
point is, that at each time step other series are included or
excluded. So, the contributing weight of a single series may
vary over time considerably.
The attempt proposed here acts
on the assumption that each sample tree with its increment cores
has to be seen as a representative of the whole stand. The
growth courses of all single sample trees reflect the common
system wide behaviour of the whole tree stand. Each single
sample tree has the same weight to contribute to the system’s
behaviour at each time step.
The procedure proposed here
consists in the following steps:
-
Reconstruction of the
diameter growth course from ring width series; determination
of a diameter at the beginning of the course if pith is
failed when core was taken; standardisation of the growth
course to DBH without bark
-
Transformation of the
absolute diameter series to relative series within a range
between 0 and 1.
-
Calculation of the mean
relative diameter growth course; evaluation of similarity or
dissimilarity of the single growth courses; exclusion of
single series from chronology if their growth dynamics
diverge from common mean growth course over time profoundly.
-
Calculation of the mean
basal area weighted diameter without bark of all included
sample trees.
-
Back-transformation of the
mean relative diameter growth series into a mean absolute
diameter growth course by multiplication with mean diameter.
-
Back-transformation of
mean diameter growth series into mean ring width series.
-
Calculation of mean tree
ring index series by prewhitening (AR(1)-modelling) and
elimination of persisting trend portions by spline
approximation
This procedure is seen to be
better qualified to express the mean common chronology signal,
because all included single series contribute in the same size
at all time steps of the series.
Additionally, calculated mean diameter growth trend and its
transformation to time series of mean basal area increment can
be used for a detailed growth behaviour analysis. Results of
analysis of climate effects on tree growth using mean tree ring
index chronologies can also be transformed till to mean diameter
growth course, because all calculation steps can be tracked
back. Both, mean tree ring index chronology and mean diameter
growth course are branches of a consistent system. |
Wood anatomical
analysis of fire-scarred chestnut in southern Switzerland
Erica Bigio, Holger
Gärtner & Marco Conedera
Swiss Federal Research
Institute WSL, Zürcherstrasse 111, Birmensdorf, Switzerland
e-mail:
ericabigio@hotmail.com
In April of 1997, a medium to
high intensity surface fire burned in a chestnut coppice in
southern Switzerland, leaving many trees scarred at the stem
base by the passing fire. The aim of the research is to use wood
anatomical methods to identify features within the cell
structures related to heat and fire injury. For this, focus is
set on analyzing trees where the fire had partially killed the
cambium, creating a fire scar, along with trees where the
cambium may have been affected by a sub-lethal level of heat.
Cross-sectional samples of adjacent fire-scarred and non-scarred
shoots were taken from the same stool, along with samples of
reference trees from outside of the burned area. Samples were
sanded and analyzed for macroscropic changes in growth preceding
and following the event year of 1997. Thin sections were made
of the 1997 growth ring from the fire-scarred cross sections on
the opposite side from the open scar face, from the uphill and
downhill sides of the intact cross sections, and also from the
reference trees.
First results show that the cell structures in the 1997 ring,
which were visually compared among all three sets of samples,
but did not show obvious differences in growth away from scar
region. However, at the outermost borders of the scar region, in
the immediate vicinity of the killed cambium, surviving cambium
initials kept on producing fibers and even vessels without
beginning to overgrow the wound. After producing several cell
layers, a portion of this area stops developing and is then
covered by cell layers starting to overgrow the wound. The onset
of the overgrowth is variable, often even starts in 1998.
Ongoing analysis will concentrate on the scar region as well as
further analyzing cell structures using an image analysis
program. |
Influence of tree
and stand index thresholds on the number of pointer years
Szymon Bijak
Department of Dendrometry and
Forest Productivity, Faculty of Forestry, Warsaw Agriculture
University, Nowoursynowska 159 bud. 34, 02-787 Warszawa, Poland
e-mail:
Szymon.Bijak@wl.sggw.pl
Determination of the pointer
years is very important task in dendrochronological analysis.
However, there are so many different procedures of that process
that any comparisons and cross-analyses are difficult. There are
also specific criteria to assess if the year is pointer or not.
Moreover, literature review, revealing the vast range of applied
values, gives no clue which of them to utilise.
We applied the ‘normalisation
in the moving window’ method to determine pointer years for the
period of 1953-2002 in two sets of spruce and oak tree-rings
data. Different tree and stand index thresholds were used, which
allowed determining formulae describing relationships between
index values and number of pointer years, and between both
indices. We derived minimum values of the thresholds necessary
to obtain single pointer year or number of pointer years equal
to 5, 10 and 20% of the total number of years in analysed
period. Results from the ‘normalisation’ method were then
compared to the output of subjective visual analysis of the
tree-ring series.
For both of analysed sets, it
turned out that, no matter which pointer year level we applied,
tree index remains constant when stand index equals less then
0,5. This stands on the contrary to the results of visual
examination, which gave constantly decreasing curve. |
Dendroecology of
neolithic timber using dendrotypology, growth-patterns and
stand-dynamics
Niels Bleichner
Römisch-Germanisches
Zentralmuseum Mainz, Ernst-Ludwig Platz 2, 55116 Mainz, Germany
e-mail:
bleicher@holzanalyse.de
A large number of
archaeological samples from upper-swabian neolithic timber have
been analysed dendrochronologically. In order to reconstruct
human activities in the landscape a threefold approach was used:
First the samples were classified into ecological groups using
dendrotypology. Analysis of stand-dynamics allowed to interpret
these groups in terms of what kind of stands they came from and
what kind of disturbance-regimes governed these stands. Lastly
it was tried to find analogies for the different kinds of
patterns observable in the samples both on the level of
tree-ring series and anatomy. In doing so different categories
of patterns were defined for the palaeoecological approach.
Among these are ring patterns, growth patterns, complex patterns
and stand-dynamic patterns.
These analyses allowed to
reconstruct cyclic human activities in and around the Federsee-basin
of the time around 3300 BC and 2890 BC. Hitherto unknown systems
of prehistoric forest-use were detected. The dating of the
settlements gave the opportunity also to reconstruct the rhythms
of settlement-dynamics as well as succession-phases on former
economic areas. These results can be directly compared with
local pollen-diagrams. Thus dendrochronology can be used to help
interpreting pollen-data leading to a more comprehensive
understanding of processes in the landscape and their traces in
our proxies. |
ENSO and NAO
impacts on Pinus pinaster Ait. growth in Spanish forest
Stella Bogino1,2;
Felipe Bravo1
1
Departamento de Producción
Vegetal y Recursos Forestales. Universidad de Valladolid, Avda.
de Madrid 44. 34004 Palencia. Spain. TE. 34 979108427
sbogino@pvs.uva.es
2Departamento
de Ciencias Agropecuarias. Facultad de Ingeniería y Ciencias
Económico-Sociales.
Universidad Nacional de San Luis. Argentina.
The impact of NAO and ENSO on
radial growth of maritime pine (Pinus pinaster Ait.) had
been analysed in Spaniard woodlands using dendroclimatological
techniques. Nine residual chronologies across the natural
distribution area of the species were built. Statistic indexes
that describe the chronologies suggested a strong association
between growth of maritime pine and causal environmental
factors. Growth response to NAO and ENSO atmospheric indexes
were calculated to the common period 1948 – 2005. Results showed
a positive significant correlation along all the sampling sites
with ENSO index, whereas NAO index effect changed from positive
to negative according to the sampling site. Although there was
not a common response to NAO index along all the analysed places
the results were consistent with previous meteorological studies
made in Spain that consider: that NAO index has a clear
relationship with climatic conditions in Europe but this general
association could not be applied to the Iberian Peninsula where
the topography and the Mediterranean sea might strongly affect
NAO behaviour. Even though future ENSO behaviour is still
unknown these results emphasise both the impact of this
atmospheric index on ecosystems locate too far away from centre
pressures that control it and its importance as the major factor
that control climatic conditions in the world. |
The
dendrochronology of archeological oak found in old town of
Klaipeda
Mindaugas
Brazauskas
Klaipeda University, Tilzes
13, Klaipeda, Lithuania
e-mail:
vmbrazauskai@takas.lt
Dendrochronological dating of
archaeological oak founds in Klaipeda have several aspects of
interest and investigation. First one is oriented in straight
interest of archaeological dating method, in dating of
archaeological cultural layers and structures.
Second one is exceptional
research based on dendrochronological questions and dendro
provenance. There we have mainly oak dating problems with master
chronologies and dendro provenance. At the moment all
archaeological oak samples are divided into two groups. The
first one consists of oak timber used in archaeological
structures as building material. Mainly there is oak timber of
local provenance. The second groups are the parts of barrels
distributed in cultural layers of Klaipeda from 15th
until 19th. The oak planks from barrels more
indicates not local origin and been observed as objects for
dendro provenance studies.
The compiled dendro scales
from Klaipeda are open for dendrochronologists have interest in. |
Life at the edge:
resolving the climatological sensitivity of sub alpine snow gum
Matthew Brookhouse
The Australian National
University, 48 Linneaus Way, 0200 Canberra, Australia
e-mail:
matthew.brookhouse@anu.edu.au
Dendroclimatological studies
usually investigate the relationship between tree ring
characteristics and the two climate parameters – precipitation
and temperature. While these are the climate factors of most
interest to humans, they may not be the most important in
determining inter-annual variation in tree growth and, hence,
tree ring formation. We examined the climate sensitivity of
tree-ring width chronologies from Eucalyptus pauciflora
Sieb. ex Spreng from three elevation classes. Based upon the
principle that climate sensitivity increases with proximity to
the limits of tree growth, we hypothesised that the sensitivity
of E. pauciflora tree-ring series would increase with
elevation. Consistent with our hypothesis we found an increase
in chronology statistics with elevation. We also found that ring
width in each chronology correlated negatively with mean maximum
air temperature during the preceding winter positively with
maximum air temperature during the growing season. However, we
did not observe an increase in sensitivity to temperature with
increasing elevation. A highly significant positive correlation
between each chronology and net radiation during summer appears
to explain the response to summer temperature and precipitation.
Rotated principal components analysis revealed greater
sensitivity to inter-annual variation in net radiation at higher
elevation. These results appear to have significant implications
for dendroclimatological studies of eucalypts. |
Application of
multivariate cross-dating to historical timbers with less than
50 tree rings
C.T. Bues, B. Günther,
J. König
Dresden University of
Technology, Institute for Forest Utilization and Forest
Technology, Chair for Forest Utilization, Pienner Straße 19,
D-01737 Tharandt, Germany
e-mail:
bues@forst-tu.dresden.de
During 2004 TRACE conference a
new dating method for wood samples from spruce trees with less
than 50 tree rings were presented. The so called “multivariate
dating method” uses 10 different tree ring characteristics
derived from X-ray images applying X-ray-densitometry. In a
parallel running cross-correlation over a special developed
standard chronology for spruce wood now true dating results can
be achieved for small wood samples using a new TRA-software.
In the meantime the multivariate dating method was carried out
for different cases to date historical spruce samples with e.g.
24, 32 or 35 tree-rings. Interesting examples from the practice
of the master builder of the cathedral Meißen, Mr. G. Donath (on
roof framings of the cathedral and the castle “Albrechtsburg” at
Meißen) and in addition the results of smaller Spruce samples
from the Cistercian monastery "Altzella" at Nossen will be
presented. The conditions for a successful application of the
new dating method will be described. It will be demonstrated,
how different the dating results can be, using the traditional
univariate dating method - only based on tree-ring width - in
comparison to the multivariate dating method using the 10
different tree-ring parameters. It will be shown that the new
method brings reliable results. First approaches will be
discussed to bring the multivariate method to a level, were the
dating of single samples with less than 50 tree rings can also
be realized. |
Eight centuries of
Pyrenees summer temperatures from tree-ring density
Ulf Büntgen1,
David C. Frank1, Håkan Grudd2, and Jan
Esper1
1Swiss Federal Research
Institute WSL, Dendro Sciences Unit, Zürcherstrasse 111, 8903
Birmensdorf, Switzerland
2 Dept. of Physical Geography
and Quaternary Geology, University of Stockholm, Sweden and
Abisko Scientific Research Station, The Royal Swedish Academy of
Science
e-mail:
buentgen@wsl.ch
May-September maximum
temperatures of the Spanish Pyrenees are reconstructed for AD
1260-2005 using 261 density measurement series from a
combination of living and dry-dead timberline trees. Application
of the regional curve standardization method for tree-ring
detrending allowed the preservation of low frequency temperature
variability. The new record correlates at 0.53 (0.68 in the
higher frequency domain) with temperatures over 1944-2005
calibration period. Reconstructed warm summers in the 14-15th
and 20th century are separated by a prolonged cooling from
~1450-1850. Six of the ten warmest decades fall within the 20th
century, with the remaining four between 1360-1440.
Comparison with new
density-based summer temperature reconstructions from the Swiss
Alps (Valais; AD 755-2004) and northern Sweden (Torneträsk; AD
500-2003) shows decadal to longer-term similarity between the
Pyrenees and Alps, but no coherence with northern Sweden.
Spatial field analyses using proxy and instrumental data support
the regional differentiation of the three records. While 20th
century warmth is evident in the Alps and Pyrenees, recent
temperatures in Scandinavia are relatively cold in comparison to
earlier warmth centered ~1000, 1400, and 1750. Cold periods
during the second half of the 15th century, between ~1600-1700,
and ~1820 are coherent between these regional-scale
reconstructions and records representing larger areas of the
Northern Hemisphere. However, while coldest summers in the Alps
and Pyrenees are in-phase with the Maunder and Dalton solar
minima, lowest temperatures in Scandinavia occur at the onset of
the 20th century. |
Blue Intensity in
Pinus sylvestris: application, validation and climatic
sensitivity of a new palaeoclimate proxy for tree ring research
Rochelle Campbell
Swansea University, School of
Society and Environment, Geography Department, Singleton Park,
SA2 8PP Swansea, United Kingdom
e-mail:
371431@swansea.ac.uk
Minimum blue intensity
measurements of resin-extracted Pinus sylvestris samples,
are shown to provide a robust and reliable surrogate for maximum
latewood density. Blue intensity data from fifteen trees, are
reported relative to a standard blue-scale in a manner similar
to grey-scale calibration in X-ray densitometry. The resulting
time series are highly correlated with X-ray densitometry data
generated from the same samples and preserve a high level of
signal strength. The sensitivity to summer climate variables is
similar to that identified in the relative density record,
demonstrating that minimum blue intensity can also be used for
the study of climate change. |
Archaeological site
of Dolmen de la Font dels Coms (Llavorsí, Pallars Sobirà,
Spain). Charcoal analysis for human impact and dendroecological
interpretation
Mireia Celma Martínez
Prehistory Department-Archaeobotany
Laboratory, Universitat Autònoma de Barcelona, Edifici B Campus
de la UAB, P.C.: 08913 Bellaterra (Cerdanyola del Vallés, Spain)
e-mail:
mireia_celma@hotmail.com
Dolmen de la Font dels Coms
is located at the top of Vall de Baiasca at 1850 m
altitude. The site was
dug in 2003-04 and showed a repeated ocupation from prehistoric
to roman times. Dolmenic construction was reused between third
century BC to first century AC as an iron kiln.
This historical high-altitude
iron kiln constitutes the site as a perfect example for studying
human explotaition of raw materials. Analysis of charcoal
samples are a conjunction
between human raw material selection and ecological growth
conditions. The object of analysis is determine species (used as
combustible) and to obtain different data collection from
anatomical features for growth-stress interpretation and attempt
to extrapolate it to human activities.
Thanks to Parc Natural de
l’Alt Pirineu (Alt Urgell-Pallars Sobirà, Catalonia, Spain),
Ecomuseu de les Valls d’Àneu (Esterri d’Àneu, Catalonia,
Spain) and Prehistory Department of Universitat Autònoma de
Barcelona (Catalonia, Spain). |
El Niño Southern
Oscillation Signal in World Highest Elevation Tree-Ring
Chronologies from the Altiplano Plateau at 4,600 m a.s.l.
D.A. Christie1,
A. Lara1, J.A. Barichivich1, R. Villalba2,
M.S. Morales2 & E.A. Cuq1
1Laboratorio
de Dendrocronología, Facultad de Ciencias Forestales,
Universidad Austral de Chile, Valdivia, Chile
2Departamento
de Dendrocronología e Historia Ambiental, IANIGLA, Mendoza,
Argentina.
e-mail:
duncan@sendadarwin.cl
El Niño-Southern Oscillation
(ENSO) is the largest source of inter-annual variability
operating in the earth's climate system, and is associated with
extreme weather conditions having large social, ecological and
economic impacts.
Several tree-rings records
have been utilized to reconstruct past ENSO variability but none
of them comes from South America. On the Altiplano plateau in
the central Andes are located the world highest elevation forest
composed by Polylepis tarapacana trees 4,000-5,000 m
a.s.l. We use two tree-ring chronologies in order to analyze the
regional climate and ENSO influences on P. tarapacana
growth at the east and west Andean slopes on the Altiplano.
P. tarapacana
growth has a strong common signal and a complex relation with
summer temperature and precipitation. Ring-width has an inverse
relation with temperature respect to precipitation. Temperature
has a positive and negative influence on ring-width during
current and previous summer, respectively. Tree-growth is
positively correlated with spring-summer tropical Pacific SSTs,
with a spatial pattern resembling to ENSO wedge. In general the
El Niño (La Niña) events are well recorded in the chronologies,
determining above (below) mean anomalies on tree-growth. P.
tarapacana chronologies offer a good opportunity to future
multi-proxy ENSO reconstructions. |
Intra-annual
variations of wood density of Picea abies [L.] Karst. at
different altitudes of the Black Forest. Typified density
profiles and the influence of weather conditions on wood density
Detlef Drosihn,
Philipp Duncker and Heinrich Spiecker
Institute for Forest Growth,
Albert-Ludwigs-Universität Freiburg. Tennenbacherstr. 4; D-79106
Freiburg i. Br./Germany
e-mail:
dedrosi@arcor.de
The following study is an
investigation about intra-annual wood density variations of
Norway spruce (Picea abies) measured at three sites of
different altitudes in the Black Forest/Germany, with an
elevation from 400 to 1.200 metres above sea level. The
objective of the study is to recognize certain weather
conditions in the variation of the wood density.
Every site is represented by
two trees and their stem discs in 1.3 metres height. The
variation of wood density is recorded by a method named
High-Frequency-Densitometry which makes use of the dielectric
characteristics of wood.
From the available data a
typified intra-annual wood density profile can be produced which
characterizes all sites likewise and besides it allows the
statistic comparison with the data of individual years that
differ significantly.
The investigation refers to
the year 2001 which was unusually warm and wet and the year 2003
which was unusually warm and dry when compared to the long term
average.
Sections of the typified wood
density profile of both years differ significantly but only in
the lowlands.
Since forest growth does not
take place in a linear way it is also necessary to develop a
time scale for an intra-annual wood density profile to be able
to assign wood density variations to exactly dated weather
conditions. By making use of chronological radial growth data
which were measured using dendrometres at the same three sites
and which are shown as diagrams, some reference points of time
can be applied to the wood density diagrams. By doing so short
term weather conditions can be understood in the wood density
profile of every site. It shows that drought makes the density
rising, precipitations however make it drop.
The result of the evaluation
shows that form and dimensions of the wood density-variation is
caused by the weather conditions at the different altitudes.
Apart from that, the variation of the wood density occurs
predominantly in the late wood section of the year ring. The
level of wood density increases from the highlands to the
lowlands.
Furthermore, the analysis of
the phenomena of air temperature and precipitation shows that a
change of wood density of trees at the highest site is stronger
linked up with important changes of air temperature than with
events of precipitation. This applies for the early wood section
as well as for the late wood section.
At the medium elevation site
the wood density is also influenced mainly by the weather
phenomena of air temperature but the growing influence of
precipitation is more pronounced by decreasing tree ring widths
during long lasting periods of drought.
The trees in the lowland-site
show a significant stronger reaction on precipitation than on
air temperature for the late wood section. |
Dendroecological
studies on subfossil pine and oak from „Totes Moor“ near
Hannover (Lower Saxony, Germany)
Eckstein, J;
Leuschner, HH; Bauerochse, A
Albrecht-von-Haller Institute,
Dep. of Palynology and Climate Dynamics, Untere Karspuele 2,
D-37073 Göttingen, Germany
e-mail:
Jan.Eckstein@biologie.uni-goettingen.de
Most of the raised bogs in
Germany are situated in the Lower Saxony part of the North
German Lowlands, in a landscape that was moulded during the ice
age. In many of these peatlands, remains of subfossil pine
(Pinus sylvestris) forests can be found. In the past these pine
forests hardly received any attention and dendrochronological
investigations were focussed on bog oaks. However the fact that
peatlands with pine are known as common stages of mire
ecosystems provides the chance to use dendroecological
reconstructions of peatlands to gain a better understanding of
climate influence on bog ecosystems.
In the framework of an ongoing
project, subfossil pine from peat extraction areas in Lower
Saxony are investigated at Göttingen University. One of the main
study sites ,“Totes Moor”, is situated about 25 km north-west of
Hannover. First results of dendroecologigal investigation in
this area are reported.
So far 309 specimens of bog
pines were studied. One hundred seventy fife of these specimens
represents 13 groups of different ages providing 13 floating
chronologies, the longest with more than 400 years. Only one
chronology of 19 bog pines was crossdated with the Lower Saxony
bog oak master chronology to the period 4783-4559 B.C.
The 60 studied bog oaks from
“Totes Moor” cover a period from 6200 to 4550 B.C. with only one
minor gap.
Both bog pines and oaks show a
pattern of clearly alternating populations with periods of
increased germination and/or dying off. Synchronous changes in
growth pattern and population dynamics indicate that
contemporary “stress-events“ occurred in former wetland woods
which are most likely linked to striking environmental changes.
In the case of the datable pines from “Totes Moor”, changes in
growth pattern and population dynamics synchronize surprisingly
well with those seen in oaks. |
Long-term drought
severity variations in Morocco
Jan Esper1,
David Frank1, Ulf Büntgen1, Anne Verstege1,
Jürg Luterbacher2, Elena Xoplaki2
1
Swiss Federal Research Institute WSL, 8903 Birmensdorf,
Switzerland
2
Institute of Geography, University of Bern, 3012 Bern,
Switzerland
e-mail:
esper@wsl.ch
Cedrus atlantica
ring width data are used to reconstruct long-term changes in the
Palmer Drought Severity Index (PDSI) in Morocco, North Africa,
over the past 953 years. The reconstruction captures the dry
conditions since the 1980s well and places this extreme event in
a long-term context. PDSI values were above average for most of
the 1450-1980 period letting the recent drought appear
exceptional. Our results, however, also indicate that this
pluvial second half of the last millennium was preceded by
generally drier conditions back to 1049. These long-term changes
from initially drier then pluvial and recent dry conditions are
similar to PDSI trends reported from western N-America, and we
suggest that they are related to long-term temperature changes,
potentially teleconnected with ENSO variability and forced by
solar irradiance changes. |
Effects of various
site ecological features on radial growth pattern in North
Rhine-Westphalia
S. Fischer, B.
Neuwirth, J. Löffler & M. Winiger
Institute of Geography,
University of Bonn, Meckenheimer Allee 166, 53115 Bonn, Germany
e-mail:
fischer@giub.uni-bonn.de
Dendroecological network
analyses are appropriate and often used approaches to
investigate climate/growth relations and their spatial
variabilities in larger regions. Although tree-ring sites in
midlatitudinal areas will be included more and more in such
networks there is a shortage of data leading to a lack of
knowledge concerning the complexity of climate/growth response
for lowlands and low mountain regions.
The present study, which is
included in a running PhD project, supplements the
dendroecological network. Therefore tree samples were taken in
North Rhine-Westphalia and in surrounding regions including
both, lowlands and low mountain ranges. An already existent
network of oaks will be completed with data of other important
tree species like
Fagus sylvatica, Quercus robur, Quercus
petraea, Picea abies,
Pinus sylvestris and Acer pseudoplatanus L. to a
multi species data set.
More than 60
dendrochronological sites, which are situated in heights ranging
from 100 to 750 m a. s. l. and in different expositions and
inclinations, represent a great diversity of site ecological
attributes. Detailed information like soil type or vegetation
type have been elevated for special forest ecological test areas
in the framework of the biomonitoring of the LÖBF.
To investigate climate/growth
relations single year analyses (according to Cropper) and time
series analyses (linear correlations) have been made, separated
in interannual and decadal variations. As a basis for these
investigations a grouping of sites with similar growth behaviour
(anomalies) will take place.
The talk presents the groups
basing on similar growth anomalies, their dendroecological
interpretations taking into consideration the biomonitoring data
and the corresponding climate/growth relations. Finally all the
results will be combined to generate growth patterns in North
Rhine-Westphalia responding to homogeneous effects of site
ecological features. |
Growth variations
of oaks under different climatic and environmental conditions in
low mountain ranges (Germany)
D. Friedrichs, B.
Neuwirth, J. Löffler, M. Winiger
Department of Geography,
University of Bonn, Germany
e-mail:
d.friedrichs@geographie.uni-bonn.de
Tree-ring growth is influenced
by different climatic and environmental factors. At the boundary
of a species range, the most limiting climate element determines
tree-growth, whereas the influence on tree-growth in low
mountain ranges is more complex. To investigate the important
elements on tree-growth, ecological studies can be carried out
using site analysis, transects or network analysis. By utilising
the same statistical procedures for all sites in a network
analysis, e.g. climate-growth relationships, of different sites
can be compared. In several transect and network analyses groups
are calculated on the base of tree-growth in order to detect
sites with similar growth patterns. These groupings are often
used to identify ecologically separated units, e.g. elevation
zones (Wilson and Hopfmueller, 2001).
In this study a newly
established tree-ring network is presented. Groupings of 52 oak
sites are calculated, using two grouping methods: i) the
hierarchical cluster analysis and ii) the principal component
analysis. The results of these groupings are compared, looking
for similarities and differences. In addition, the hierarchical
cluster analysis was applied, in order to group the sites in
three different time periods. Calculating different time
periods, we investigate the temporal stability of the groups.
Finally, the spatial distribution of the groups within the
research area is described and suggestions for the ecological
reasons of this distribution are discussed.
Wilson, RJS., Hopfmueller, M.,
2001.
Dendrochronological investigations of Norway spruce along an
elevational transect in the Bavarian Forest, Germany.
Dendrochronologia 19, 67-79. |
Traumatic rows of
resin ducts - A valuable parameter for dating events in
Geomorphology?
Holger Gärtner1
& Ingo Heinrich2
1
Swiss Federal Research
Institute WSL, Dendro Sciences Unit, 8903 Birmensdorf,
Switzerland, e-mail:
holger.gaertner@wsl.ch
2
Research Center Jülich, ICG-V,
Wilhelm-Johnen-Straße, 52425 Jülich, Germany
Dating geomorphic processes
based on the analysis of growth anomalies occurring in disturbed
trees is an established method in Geomorphology. The most common
anomaly related to mechanical stresses is the onset of reaction
wood and resulting eccentricities in the annual rings of
affected trees. These stresses can also cause abrupt growth
suppression depending on their intensity. These growth anomalies
are related to various stresses and they have frequently been
used to reconstruct processes such as debris flows, rock fall,
landslides, avalanches or creeping slopes. Although the presence
of these growth anomalies has often been used, their timing of
formation is a field of special interest rarely addressed in
Dendrogeomorphology.
This is in particular true for
traumatic resin ducts for which it is still not known when and
to what extend they occur within the annual rings of a naturally
grown tree. Reliable dendro-publications always regard traumatic
resin ducts as indicators for mechanical, insect-related or
other environmental disturbances describing them as late effects
to environmental stresses, not as immediate reactions.
Various experiments focussing
on the effects of insects or fungi and combinations of both on
the development of traumatic resin ducts have been conducted in
the last decades. However, there is still no proof for their
immediate formation in the annual tree ring after wounding in
naturally grown conifers. Additionally, only sparse information
exists on their spatial distribution around the wound or within
the respective annual ring of a mature conifer.
For the study presented,
wounding experiments have been conducted (i) before the
beginning of the vegetation period and (ii) after the end of the
vegetation period on two naturally grown conifer species,
European Larch (Larix decidua Mill.) and Norway spruce (Picea
abies (L.) Karst.).
The experiments revealed that
traumatic resin ducts show a high variability regarding their
timing and spatial spread within tree rings. Spruce trees did
not show immediate occurrences of traumatic resin ducts after
wounding. Depending on their distance to the wound a delay of up
to 10 months referred to the time of treatment was observed.
Wounded larch trees did show immediate occurrence of traumatic
resin ducts only in direct vicinity to the wound. Farther from
the wound, their formation was delayed more and more and their
occurrence was shifted towards the latewood of the respective
ring.
In conclusion, traumatic rows
of resin ducts cannot be used for accurately dating mechanical
disturbances, especially not when working with cores, and
therefore, they should be treated carefully only as what they
are, stress responses, more or less delayed in time, to various
forms of environmental impacts. |
Seasonal dynamics
of wood formation in Norway spruce during 2002-2004
Joþica Grièar1*,
Primoþ Oven2, Tom Levaniè1
1Slovenian
Forestry Institute, Veèna pot 2, SI-1000 Ljubljana, Slovenia
2University
of Ljubljana, Biotechnical Faculty, Department of Wood Science
and Technology,
Roþna dolina, Cesta VIII/34,
SI-1000 Ljubljana, Slovenia
*e-mail:
jozica.gricar@gozdis.si
Radial growth of tree species
is sensitive to environmental conditions determining onset, rate
and cessation of individual phases of xylogenesis. Seasonal
dynamics of cambial activity and cell differentiation of tree
species differs among years and sites. Length of the growing
period and rate of the cambial cell divisions determine widths
of the xylem increments. We studied the seasonal dynamics of
wood formation in Norway spruce (Picea abies Karst.)
in Slovenia during 2002-2004. Experiments using pinning
technique were performed on 5 adult Norway spruce trees growing
at Alpine site Pokljuka (Pok-elevation 1250 m) and 5 trees at
lowland plantation Sorsko polje (SorP-elevation 350 m) at weekly
intervals. The xylem increment was determined by investigation
of permanent transverse sections stained with safranin and astra
blue using a light microscope and an image analysis system.
Since the xylem increment realized by the time of wounding could
be interpreted as a number of cells or as measured widths, we
used both approaches and then compared the results. Number of
cells reflects the cambial productivity; meanwhile measured
widths include also the information on the extent of the radial
expansion of newly formed tracheids. However, in cases of
crushed or compressed developing tissues, measured values are
not reliable. We used Gompertz function for description of the
radial growth of the trees at each site in 2002-2004. The
pinning method uses the ability of the cambium and its youngest
derivatives to respond to a minute mechanical injury without
affecting the physiological integrity of a tree. Pin insertion
into the cambium causes minute wound reactions, which define the
increment reached from the time of pinning. The cambial activity
occurred from end-April till July-August in trees at SorP and
from second part of May till mid-August in trees at Pok. Greater
differences in the onset of the cambial activity among years
were observed in trees at Pok and just the opposite in trees at
SorP in the case of cessation of the cell divisions. The
duration of the cambial activity among years varied from 77-119
weeks at SorP and 70-84 weeks at Pok. The period of the maximal
cell production was estimated to 140-162 day of the year at SorP
and 162-180 day of the year at Pok. The differences in the
widths of the xylem growth rings among years were greatest at
SorP (37-62 cells or 1.06-1.73 mm) comparing to Pok (36-45 cells
or 1.26-1.42 mm). Comparison of the Gompertz function
coefficients between the number of cells and the measured widths
of the xylem increment revealed stiffer curves in the case of
the measurements which could be explained by higher contribution
of the wider early wood tracheids formed in the first part of
the growing season to the final widths of the xylem growth rings
than the narrower late wood cells. |
Dendrogeomorphological analysis of a landslide area near Buck’s
Mills, England
Roman Gut1, 2,
Holger Gärtner2 & Vanessa Winchester3
1
Institute of Geography – University of Zürich
2
Swiss Federal Research Institute WSL
3
Laboratory of Dendrogeomorphology, University of Oxford
e-mail:
r_gut@cevi.ch
Dendrogeomorphology allows
dendrochronological techniques to be applied for the
reconstruction of slope movements. The activity of slow mass
movements along the coast of Southeast England was reconstructed
by analyzing eccentricities and abrupt growth changes in 42 oak
trees (Quercus petraea). Leaning trees at the study site
near Buck’s Mills (Devon, UK) indicate unstable ground
conditions. Growth anomalies, such as eccentric growth between
two opposing radii, can therefore be used to date event years.
To further analyze the growth characteristics, a local reference
chronology was built, dating back to AD 1882. A geomorphological
map provided an overview of the study area and enabled the
interpretation of the slope movements according to the location
of the samples with the dated event years. In total, a large
number of certain (62) and possible (108) event years were
identified in the 43 sample pairs. Furthermore, results show
that the slope is not moving as a solid block, but in separate
units. These units show individual movement patterns, which are
linked in some cases.
The study area could be
divided in six sub-areas showing stable as well as unstable
zones at various times. Recurrent movements at the upper part of
the slope over the years impose pressure upon a bulge downslope.
Two sudden movements of a rocky slab just underneath the bulge
could be dated to the years 1924 and 1943. The area on the
uphill side of the bulge is still in state of flux. Therefore,
the bulge marks a potential starting zone for a bigger
landslide. The technique used enabled to reconstruct the
landslide activity along on the North Devon coast at a high
temporal and spatial resolution. |
Stable isotopes C,
H and O in tree rings as a tool for climate reconstruction
Sùawomira Paweùczyk1,
Anna Pazdur1, Tatjana Boettger2, Marika
Haupt 2, Marek Kràpiec3, Elýbieta
Kràpiec-Szychowska3
1Department
of Radioisotopes, Institute of Physics, Silesian University of
Technology, Krzywoustego 2, 44-100 Gliwice
2UFZ-Umweltforschungszentrum
Leipzig-Halle GmbH, Sektion Hydrogeologie, AG Paläoklimatologie;
Theodor-Lieser-Strasse 4, 06120 Halle/Saale, Germany
3Dendrochronological
Laboratory, AGH University of Science and Technology,
Mickiewicza 30, 30-059 Cracow
For the reconstruction of past
climatic changes can be used tree rings widths, maximum late
wood density and other parameters as stable isotopic composition
in tree rings.
Investigations of stable
isotopic C, H, and O composition in
a-cellulose extracted from tree rings of pines
(Pinus sylvestris L.) growing in the ecologically clean
Suwaùki Region (54°06 'N, 22°57'E),
North Eastern part of Poland were undertaken.
Climatically, the Suwaùki
region substantially differs from other regions of Poland. It is
the coldest part of Poland apart from mountains.
Isotope records (d13C,
d18O,
d2H)
cover the period 1600-2003. Those measurements constituted a
part of more complex investigations of stable isotopic
composition in tree rings for last 400 years in the frame of
European project ISONET.
Meteorological data used for
the investigation was obtained from the meteorological
observatory in Suwaùki (54°07’N,
22°58’E).
The meteorological data set starting from 1931.
Relations between
d13C,
d18O,
d2H
in tree ring
a-cellulose
and meteorological data (temperature
and precipitation) demonstrate that precipitation influences the
stable isotopic carbon, oxygen and hydrogen ratios to a lower
extend than temperature. July-August is the period with the
stronger influence on stable isotope composition of carbon,
oxygen and hydrogen, and therefore
d13C,
d18O,
d2H
can be regarded
as indicators of summer climate change. In case of correlation
coefficients due to temperature the highest correlation
coefficient exists for hydrogen (r=0.57, n=73, p<0.001). For the
combined periods (several months) higher correlation
coefficients than for one month have been obtained.
On the basis of
d13C,
d18O,
d2H
values in tree ring
a-cellulose
and relations between
isotopic composition
and meteorological data
reconstructions of the temperature for the period 1600-1930 were
performed. For those reconstructions inverse calibration and
classical calibration were used. |
Stable isotopes in
tree rings: climate and human activity in the last 400 years,
Poland
Anna Pazdur 1,
Slawomira Pawelczyk1, Natalia Piotrowska1,
Andrzej Rakowski1, Malgorzata Szczepanek 1,
Tatjana Boettger 2, Marika Haupt 2,
Stanislaw Halas3, Marek Krapiec 4,
Elýbieta Szychowska – Krapiec4 and Nakamura Toshio5
1Department
of Radioisotopes, Silesian University of Technology, Gliwice,
Poland
2UFZ-Umweltforschungszentrum
Leipzig-Halle GmbH, AG Palaeoklimatologie, Germany
3
Mass Spectrometry Laboratory,
Maria Curie-Sklodowska University, Lublin, Poland
4
Dendrochronological
Laboratory, AGH University of Science and Technology, Cracow,
Poland
5Nagoya University, Centre for Chronological
Research, Nagoya, Japan
The light stable isotopes
composition (δ2H, δ13C and δ18O
values) in the annual tree rings (especially in pine and oak
from moderate climate zone) are sensitive indicators of climate
change (temperature, precipitation and sunshine) and also the
anthropogenic influence. Δ14C in tree rings of the
last 150 years records the significant Suess effect, reflected
also in δ13C of the annual tree rings of pine
collected from the east-northern part of Poland.
The studies of climate change
by stable isotope analysis were continued as the investigation
of alpha cellulose extracted from the annual tree rings of pine
collected from east-northern part of Poland and alpha-cellulose
extracted from the annual tree rings and the late wood of oak
collected from the southern part of Poland (Niepolomice Forest)
within ISONET Project.
Both regions vary in the
climate condition - the influence of oceanic climate is
significant in the northern region, and the continental climate
in the southern region. The significant correlations between δ2H,
δ13C and δ18O, widths tree rings and
meteorological data were found. The correlation coefficients
between δ2H, δ13C and δ18O and
temperature, precipitation and sunshine were calculated on the
basis of accessible meteorological data for sampling sites.
The measurements of 14C
concentration was carried out in the whole wood from 2.5-years
samples of pine (1860-2003) by LSC technique and independently
with annual resolution in the alpha cellulose extracted from
tree rings of pine (1960-2003) by AMS technique.
The records of δ13C
in alpha cellulose from the tree rings of pine from the northern
and southern part of Poland and the data of δ13C in
the alpha cellulose from late wood of oak from the southern part
of Poland over last 400 years are presented on the background of
change of the climate indicators and Δ14C in
atmosphere in the NH1 zone.
The magnitude regional Suess
effect in Poland was estimated over the last several tens years
period and then correlated with the comparative effect in Nagoya
(central Japan, Arequipa (southern Peru) and the global changes
of Δ14C in the NH1 zone. |
500 years summer
temperature variability in Eastern Carpathians inferred from
stone pine (Pinus cembra) tree ring width
Ionel Popa, Olivier
Bouriaud
Forest Research and Management
Institute, Research Station for Norway Spruce Silviculture,
Campulung Moldovenesc – Romania
e-mail:
popa.ionel@suceava.astral.ro
The forest ecosystems from
Carpathians region have a high dendrochronological potential but
are still few studies about the climate-growth relationships,
dendrochronological series or dendroclimatological
reconstruction from Romanian territory (Schweingruber , 1985;
Popa, 2004, 2006). The aim of this paper is to present the first
long term temperature reconstruction for Eastern Carpathians.
The study area is located in the Eastern Carpathians in Rodna
Mountain National Park (47°32’N, 24°55’E), in a mixed timberline
forest of stone pine (Pinus cembra) and Norway spruce (Picea
abies), at 1750 m a.s.l.
In order to reconstruct the
temperature dynamics in the last millennium we have compiled the
longest tree rings chronology from Carpathians using samples
from dead and living trees of stone pine (Pinus cembra). The
LINTAB equipment and TSAP software were used for measuring the
annual rings width with a precision of 0.01 mm, as well as for
cross-dating the growth series by graphical comparison in a
logarithmic scale. The results were checked for missing ring and
dating error using the COFECHA software. The final dataset
comprise 212 individual series from 129 trees (106 series from
dead trees and 106 series from living trees). The growth series
were standardized in order to eliminate the non-climatic signals
and to maximize the climatic information from the individual
series. To preserve the low frequencies in the tree ring
chronologies the Regional curve standardization method (RCS) was
used. The tree ring index was calculated as differences between
individual growth series and regional growth curve. Instrumental
climatic data for the study area are available only for the
period 1961-2001 from Iezer Pietrosu weather station (47°36’N,
24°39’E 1785 m a.s.l.). In order to extend the instrumental data
we use the temperature data from 0.5°x0.5° resolution CRU2.1
grid data-basis (Mitchell and Jones 2005). Both, grid and
instrumental monthly temperature data were normalized to the
reference period 1961-1990.
For temperature reconstruction
was used the standard chronology obtained after RCS
standardization. To avoid the loss of amplitude as result of
regression we applied the scaling method of the mean chronology
to the grid temperature anomalies (Esper et al. 2005).
The correlation analysis
indicates a high and significant response to early summer
temperature from current year (June-July). Also a positive
reaction of tree growth is observed to the prior late autumn
temperature (October – November). High temperature during the
winter induces a negative response to cembra pine in the next
growth year.
Periods with lower temperature
are 1520-1620, 1660-1690, and 1725-1840 with a minimum in 1820
decade. High temperatures are reconstructed for 1700-1725 and
mostly after 1840 with a clear increase in last 15 years. |
Tree ring width and
basic density of wood in different forest type
Eva Přemyslovská,
Jarmila Ðlezingerová, Libuðe Gandelová
Mendel Agriculture and
Forestry University, Department of Wood Science, Zemědělská 3,
Brno 61300, Czech Republic
e-mail:
premyslo@mendelu.cz
The aim of this work is to
determinate an average tree ring width and basic density of
Norway spruce (Picea abies /L./Karst.) growing in
different vegetation forest zones. Norway spruce is the most
important commercial specie in Czech republic and its portion of
forest stands is 53 %. The typological system of forest stands
consists of horizontal (edaphic categories) and vertical
(vegetation zones) zonation. There are statistically significant
differences between the values of basic density and tree ring
width according to vegetation zones and edaphic categories,
however , statistically significant differences between the
values of tree ring width can be observed only for 4th-
6th vegetation zones. Differences between values of
basic density and tree ring width according to edaphic
categories are statistically highly significant especially for 5th
and 6th vegetation zones. We can observe close
relation between tree ring width and basic density, with
increasing basic density tree ring width decrease. In summary,
results of this study provide evidence of the influence of
growth conditions to wood formation.
The work on this project was
supported by 6215648902 grant. |
Temporal Stability
of Climate-Isotope Relationships in Tree Rings of Oak and Pine
(Ticino,
Switzerland)
C.E. Reynolds-Henne1,
R.T.W. Siegwolf1, K. Treydte2, J. Esper2,
S. Henne3, M. Saurer1
1
Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
2
Federal Research Institute WSL, 8903 Birmensdorf, Switzerland
3
Empa, Swiss Federal
Laboratories for Materials Testing and Research, 8600 Dübendorf,
Switzerland
e-mail:
Christina.Reynolds@psi.ch
Reconstructions of climate
based on stable isotopes in tree rings rely on the assumption
that the relationship between climate and tree rings is stable
over time. However, studies of tree ring growth have shown
age-dependent trends thought to result from either physiological
changes or changes in the climate-growth relationship. Isotope
ratios in tree rings are affected by climate through
photosynthesis (d13C) or
uptake and use of water (d18O).
This study tested the consistency of the relationship between
climate (temperature and precipitation amount) and tree ring
cellulose d13C
and d8O
for oak (Quercus petraea) and pine (Pinus sylvestris)
for the period 1660-2000, south of the main crest of the Swiss
Alps. The comparison between tree rings and climate was made
possible by long-term temperature and precipitation datasets
based on monthly instrumental and proxy documentary data.
Overall five generalizations concerning climate-isotope
relationships were identified, namely: (1) isotopic signals in
tree rings reflect conditions of current growing season, (2)
long-term temporal stability is observed for the
d13C
pine and temperature relationship only, (3) other correlations
between tree rings and climate are mostly unstable and show
step-wise shifts in correlation sign and intensity, over time,
(4) the climate signal is oak is strongest in the 20th
century for both isotopes and (5) tree ring
d13C
responds to local climatic conditions while
d18O
reflects larger-scale atmospheric circulation processes. These
results provide a cautionary note for the calibration of long
tree ring series with 20th century relationships, at
least for trees located at ecologically non-extreme sites. |
Building of the oak
standard chronology for the Czech Republic
Michal Rybníèek1,
Tomáð Kyncl2, Vladimír Gryc1, Eva
Přemyslovská1, Hanuð Vavrèík1
1Mendel
University of Agriculture and Forestry Brno,
Faculty of Forestry and Wood
Technology, Department of Wood Science, Zemědělská 3, 613 00
Brno, Czech Republic,
michalryb@email.cz
2DendroLab
Brno, Eliáðova 37, 616 00 Brno, Czech Republic
The main aim of this work was
to make up a standard oak chronology covering the area of the
Czech Republic. The standard oak chronology, which was given the
name CZGES 2005, is based on 194 average tree-ring series and
covers the period 545 BC – 289 BC, 26 BC – 271 AD and 462 AD to
2004 AD. The new standard chronology has filled a gap in the
network of the European standard oak chronologies to which it
bears a considerable resemblance. Currently, the standard
chronology enables dating of a vast majority of the oak wood
found during the archaeological excavation and exploration works
carried out in the historic buildings in the Czech Republic.
In addition to the aim stated
above, the study was focused on the comparison between the
detrended and undetrended standard chronologies. The differences
established between the detrended and undetrended standard
chronology have shown only too clearly how important it is to
develop the detrended standard chronologies.
Finally, this study was
concerned with stating the amount of the sapwood rings in the
recent oaks. Surveying the number of the sapwood rings in the
recent oaks, no significant differences were identified between
the amount of the sapwood rings in the samples taken from the
altitude 200 and 500 metres above the sea level. The overall
results show that in South Moravia the amount of the sapwood
rings in oak ranges from 5 to 21.
Acknowledgement
The project was prepared
within a research plan of LDF MZLU in Brno, MSM 6215648902. |
Growth responses to
NAO along a Central European West-East Transect
Johannes Schultz,
Burkhard Neuwirth, Jörg Löffler, Matthias Winiger
Institute of Geography,
University of Bonn; Meckenheimer Allee 166, 53115 Bonn, Germany
E-mail:
schultz@giub.uni-bonn.de
During the last decade,
tree-ring widths has become an important and often used proxy
for reconstructing large scale circulation conditions over the
North Atlantic and Central Europe. These circulation conditions
can be expressed by the North Atlantic Oscillation (NAO) and
corresponding indices (NAOI). To improve the reconstruction of
these indices and recognizing that tree growth in Central Europe
is forced by changing influences of climate factor like
temperature and precipitation, a better understanding of the NAO
as forcing factor for radial growth is necessary, especially in
low mountain ranges.
Therefore, the present study
investigates the growth responses to NAO along a Central
European multi-species transect from the Ardennes (Belgium) to
the Ore Mountains (Czech
Republic).
The dendrochronological dataset consist of more than 400
dominant trees. All trees are older than 120 years and were
sampled in 28 sites which represent the ecological and species
specific spectrum of closed forests in the west-eastern
transect. All tree ring-series were detrended in two ways, by
calculating ratios between the raw series and their 5-year
moving average and secondly by calculating ratios between the
raw series and their 150-year splines. The resulting interannual
and decadal growth anomalies were compared with three
differently calculated indices of the NAO, representing the
normalised surface pressure differences in the North Atlantic.
The three used NAOI and their
various influences on tree-ring growth are compared. Basing on
this, the modifications of the growth responses to NAO along the
Central European west-east transect are discussed in
consideration of the ecological gradients along this transect. |
Application of
electrospray ionization mass spectrometry in analysis of ancient
wood components
Barbara Sensuùa1,
Anna Pazdur1, Peter Derrick2
1
Department of Radioisotopes, Institute of Physics, Silesian
University of Technology,
Krzywoustego 2, 44-100 Gliwice, Poland
2
Department of Chemistry, The
University of Warwick, CV47AL, Coventry, UK
We presents the first results
of study of glucose, enzymatic hydrolyzed from α- cellulose of
tree rings, by using quadrupole ion trap mass spectrometer. The
samples of ancient wood were collected from bell-supports of the
free-standing Baroque belfry, situated nearby the Cistercian
Abbey in Jedrzejow (Poland). In this research we investigate
dynamics of enzyme reaction and we suspected interannual
volatility in glucose concentration. The dendrological research
and isotope ratios investigation was a part of ISONET project.
It is well known, that
α-cellulose, extracted from tree rings, is a source of
information for climatic reconstruction time scale. The
information is contained in the chemical composition of wood,
especially the isotope ratios, of the cellulose (δ2H,
δ13C, δ 18O). The large molecular size and
insolubility of carbohydrate polymers such as cellulose make it
difficult to define chemically with precision. Hydrolysis is the
principal mechanism by which enzymes degrade cellulose polymers.
In this research the biodegradability of cellulose-based
products was studied using a fungal
Trichoderma reesei. Mass
spectrometry analysis gave a chance to obtain more structural
information on saccharides enzymatic hydrolyzed. The mass
spectra of glucose were acquired by ESI-MS/MS in positive ion
mode. The differences and annual volatility in abundant glucose
ions has not been explained yet.
Firstly, we made mass
spectrometry analysis of glucose hydrolyzed from α-cellulose
extracted from ancient wood -
Quercus robur L. (1631-1642 and 1726-1737AD).
Secondly, we try to find out correlation between the annual
fluctuation of glucose and the other saccharides concentration
with the number of observed sunspots, isotope ratios and width
of tree rings. Finally, the highest correlation was observed
between interannual volatility of saccharides concentration and
tree-ring width index (RWI).
This project was
supported by Marie Curie Fellowship Scheme and British Council
Young Scientists Program and ISONET project. |
Tree ring analysis
in a damaged pine stand
Robert Tomusiak
Faculty of Forestry, Warsaw
Agricultural University, Nowoursynowska 159/34, 02-776 Warsaw,
Poland
e-mail:
rtomusiak@wl.sggw.pl
One of the applications of dendrochronological
methods is assessment of the influence of insect gradations on
tree growth.
The objective of this paper was to examine
hypothesis that Rhyacionia buoliana causes decrease in
tree ring widths on breast height.
The attempt of verification of that hypothesis
was carried out on the basis of material gathered in the Scotch
Pine stand growing close to Warsaw. In this stand a lot of trees
have visible sings of the damage caused by
Rhyacionia buoliana.
Tree ring chronologies were elaborated for four
groups of trees: damaged and undamaged from 1st and 3rd
Kraft bio-social classes.
Tree ring analysis and comparison of the
chronologies from different groups of trees did not reveal any
explicit influence of Rhyacionia buoliana on radial
growth of trees, except for higher value of coefficient of
variation of tree ring widths in damaged trees from 3rd
Kraft class. |
Signal strength and
climate calibration of a European tree-ring isotope network
Kerstin Treydte
Swiss Federal Research Institute
WSL, Zürcherstrasse 111, 8903 Birmensdorf, Switzerland
e-mail:
treydte@wsl.ch
We present the first European
network of
d13C and
d18O in tree rings, containing 23
sites from Finland to Morocco. Common climate signals are found
over broad climatic-ecological ranges and in temperate regions
with positive correlations to summer maximum temperatures and
negative correlations to summer precipitation and Palmer Drought
Severity Indices (PDSI) with no obvious species-specific
differences. Since PDSI integrates temperature and
precipitation, it seems to be most appropriate for climate
reconstruction at least in the higher frequencies. Averaged
'European'
¥13C and
¥18O chronologies share high common
variance in the year-to-year variations. Long-term variations,
however, differ and might be biased by age trends and/or plant
physiological response to increasing atmospheric
pCO2. Spatial correlation tests using a combined
¥13C-¥18O
chronology indicate that central European climate variability is
well captured, whereas Scandinavia and the Mediterranean region
currently are underrepresented. Future studies will therefore
focus on the regionalization of the climate signals. |
A tree-ring derived
fire weather reconstruction and climatology for northern
California and Oregon
Valerie Trouet,
Alan H. Taylor, C.N. Skinner, and A.M. Carleton
Swiss Federal Research
Institute WSL, Zürcherstrasse 111, 8903 Birmensdorf, Switzerland
e-mail:
trouet@wsl.ch
Wildland forest fires pose a
significant threat to life and property in the North American
Mediterranean climate region of northern California and southern
Oregon. Fire managers rely on fire weather indices (e.g.,
Haines index) to estimate fire risk and fire severity. A better
understanding of the relation between synoptic-scale circulation
patterns and surface fire weather conditions can contribute to
refining the functional link between fire activity and climate
variability.
This study aims at
reconstructing interannual Haines index variability for northern
California and southern Oregon. The Haines Index combines a
stability and a moisture component as a measure of wildfire
growth potential and wildfire severity. We used variation in
annual tree ring widths to reconstruct annual variation in
annual Haines Index values. Four regional ITRDB tree-ring
chronologies were selected in a stepwise linear regression
procedure for the calibration period 1961-1996. The tree ring
model was verified based a leave-one-out scheme and the Haines
Index was reconstructed over the full length of the tree ring
chronologies (1637-1996).
The reconstructed Haines Index
time series was then compared to independent, regional,
fire-scar derived records of fire frequency and fire extent
(1700-1900) and to independently reconstructed indices of
atmospheric circulation patterns (SOI, PDOI). Understanding the
low-frequency (inter-annual to inter-decadal) variability in
fire weather conditions can contribute to the development of
longer-term and more precise forecasting schemes for fire risk. |
Recent treeline
dynamics in northernmost Sweden (Torneträsk): a
multidisciplinary landscape approach
Rik Van Bogaert
Ghent University, Krijgslaan
281 S8, 9000 Gent, Belgium
e-mail:
Rik.VanBogaert@UGent.be
This project aspires to
contribute to the gap-filling at the landscape scale in northern
treeline research. A multidisciplinary assessment will be
handled. As in the present author’s opinion the treeline is
controlled by both environmental and plant performance factors,
disciplines such as geomorphology, ecology and climatology need
to be geographically interrelated. The project aims to explore
recent dynamics of the mountain birch treeline (Betula
pubescens Ehrh. spp. tortuosa (Ledeb.) Nyman) at the
Torneträsk area in northernmost Sweden. However, apart from
detection, also characterization and causation of treeline
dynamics will be sought for. This is urgently needed since this
is essential to refine vegetation models, using at present only
parameters from disciplines such as biogeography and
biochemistry. Dendrochronology and remote sensing provide major
tools in assessing the treeline issue. Dendro-climatology will
reveal the sensitivity of mountain birch to the late twentieth
century warming episode, whereas dendro-ecology and
–geomorphology may clarify the importance of treeline rise
inhibitors such as herbivory and geomorphologic events. |
Dendrochronological
investigation on historical English oak (Quercus robur
L.) in Lithuania and Latvia: problems and potential
Adomas Vitas1
, Mâris Zunde2
1Vytautas
Magnus University Faculty of Nature Sciences Environmental
Research Centre Group of Dendroclimatology and radiometrics, Þ.E.
Þilibero 2, LT-46324 Kaunas, Lithuania,
e-mail:
a.vitas@gmf.vdu.lt
2Institute
of Latvian History at the University of Latvia, Akadçmijas
laukums 1, LV-1050 Rîga, Latvia,
e-mail:
zunde@lanet.lv
Although the study of oak tree
rings has been widely used to obtain long-term millennial
chronologies in Europe, dendrochronological study of oak in the
Baltic States has so far produced very limited results.
Subfossil oak wood has been found in both countries in the past,
and in some cases also at the present day, in bogs and sandy
riverbank deposits, but the number of wood samples obtained is
very small.
In Lithuania, the findspots of
subfossil oak wood are located mainly in the northern part of
the country. Seven samples have been radiocarbon-dated,
indicating that some of the oak trunks discovered here date from
the period 3300–6100 BC.
The findspots of historical
oak wood in the area of present-day Latvia are very widely
dispersed. The oak trunks found at these sites cover the period
approximately from 4000 or 5000 BC up to the first half of the
14th century AD. These have not been dendro-dated so far, mainly
because there has not been sufficient interest or funding.
Dendro-dating has so far been
undertaken on extensive collection of wood samples from the
gravel pit at Smurgainiai (western Belarus). As a result, 10
floating chronologies have been obtained, covering periods of
84–902 years within the time interval from 5300–5000 BC up to
about 1325 AD (A. Vitas, Eurodendro 2004). These chronologies
might be used for absolute dating of historical oak trunks found
in the Baltic area.
Of course, the main sources of
archaeological and historical samples of English oak in the
territory of the Baltic States are historic structures and
buildings. Unfortunately, there is also very little oak wood
preserved in standing structures from the Historical Era. In
large measure, this can be explained in terms of the rapid
reduction of oak forest during the 2nd millennium AD.
In the past, a considerable quantity of oak timber was also
exported to Western Europe. A proportion of the structural
timbers of oak recovered in the course of earlier archaeological
excavation were not dendro-dated. However, although oak wood
from the Historical Era is very rarely preserved, we now have
the first successful dendro-dating results. So far, oak
structural timbers from Vilnius Lower Castle have been dated and
chronology covering
1202 - 1418 AD was compiled
(R. Pukienë, Eurodendro 2005), and dating work is currently in
progress on structural timbers from buildings in Klaipëda Old
Town.
The chances are promising that
the study of oak wood from buildings will permit us to compile
chronologies by extending the series based on living oaks. Since
the stocks of historical oak wood are gradually being lost,
there is a pressing need for dendrochronological study of this
material. |
Detecting annual
growth rythms
from oxygen and
carbon isotopes
in tropical
mountain rain forest trees in southern Ecuador
Peter von
Schnakenburg1, Achim Bräuning1, Gerd Helle2
1
Institute for Geography,
University of Erlangen, e-mail:
pvons@web.de
2
Forschungszentrum Jülich
Dendroclimatologic
investigations in temperate climate zones are commonly based on
the tree-ring parameters ring width and maximum latewood
density. While dendroclimatology contributed significantly to
our knowledge of past climate variability in higher latitudes,
only sparse information has been gained by dendroecological
studies in tropical region so far. Due to the lack of pronounced
climatic seasonality trees in the inner tropics usally do not
form distinct tree rings and this often hampers tree-ring
analyses using ring width. To derive information about past
climate variability in the humid tropics, we applied a
combination of different methodological approaches.
The location of our study site
is in the leeward position of the eastern Andean mountain range
in the Podocarpus National Park in southern Ecuador. Former
investigations in this project showed that some tree species
react on seasonal climate changes by forming visible density
variations and growth boundaries. For this study we used the
conifer Prumnopitys montana (Podocarpaceae) that shows
visible density variations and potentially reaches high ages of
several centuries.
High-frequency densitometry
and the analyses of stable carbon and oxygen isotopes are used
to gain information about growth rhythms and climate variability
in the past. The calibration of the tree-ring data is
accomplished with meteorological data from a nearby weather
station and oxygen isotope measurements of rainfall.
The seasonal change in the
prevailing wind direction causes a change of the dominant
moisture source, which should be reflected by intra-annual
variations of the δ18O-signal in the wood. On the
other hand the δ18O-signal is influenced by the
amount of rainfall (the higher the rainfall the more the δ18O-signal
is diluted). In contrast, the intra-annual variations of δ13C
reflect the seasonality of water availability. By using the δ13C-signal
it ought to be possible to verify whether changes in δ18O
depend on drought stress or on alterations of the atmospheric
circulation.
High-frequency densitometric
analysis are able to detect even small wood density variations
which help to identify indistinct growth boundaries. A
calibration of the density curves with the isotope signals shall
finally enable a reconstruction of the past climate variability. |
The reconstruction
of spring precipitation variation from tree rings since AD 1550
from Northwestern Yunnan, China
Fan Zexin and Achim
Bräuning
Insitute of Geography, University
of Erlangen-Nürnberg, Kochstrasse 4/4, D-91054 Erlangen, Germany
e-mail:
fanzexin@yahoo.com.cn
Tree rings play an important
role in understanding past climatic change on the Tibetan
Plateau. Here we developed four ring-width chronologies of
three species (Picea likiangensis, Tsuga dumosa,
Abies ernestii) on the Baima snow mountain, NW Yunnan,
China. Although the chronologies from difference species,
significant correlations exist among all the chronologies (mean
r=0.44), and the first principal component of the four
chronologies accounts for 58% variance over their common period
1550-2005. Correlation analyses showed that January, March and
May precipitation have positive affecting on radial growth,
which indicated that the growth is generally limited by spring
moisture availability. Dry spring occurred during AD: AD
1590-1610, 1620-1660, 1700-1715, 1733-1743, 1790-1825,
1910-1925, 1960-1990; Excessive spring precipitation occurred
during: AD1612-1623, 1687-1699, 1716-1732, 1744-1756, 1778-1790,
1825-1850, 1926-1960. |
up
Posters
The impact of
micro-site conditions on ring-width variations of the alpine
dwarf shrub Empetrum hermaphroditum
Annette Bär 1,2,
Jörg Löffler 1, Achim Bräuning 3
1
Department of Geography, University of Bonn, Germany
2
Department of Biology and Environmental Sciences, University of
Oldenburg, Germany
3
Department of Geography, University of Erlangen-Nuremberg,
Germany
e-mail:
baer@giub.uni-bonn.de
Ring-width chronologies of the
alpine dwarf shrub crowberry (Empetrum hermaphroditum) were
analysed focussing on micro-topographic differences between the
ridge, south-facing, and north-facing slope located in the
Norwegian Mountains. We expected effects on ring-width formation
since micro-topography is regarded to induce micro-climatic
differences in high mountains e.g. temperature and snow melt
variations. In addition, the prostrate growth of E.
hermaphroditum may reflect these differences which are more
pronounced near the surface.
Continuous time-series
analysis reveals the major impact of temperature during the
growing season (June to August) which is present in all
micro-site chronologies. Pointer year analysis confirms the
prominent low temperature signal for negative pointer years,
whereas positive pointer years do not necessarily occur
simultaneously with high temperature. As a consequence, in
summery warm years with additional low precipitation positive
pointer years are only found at the ridge and north-facing
slope, but not at south-facing slopes where highest temperatures
occur.
The study of vessel formation led to a more detailed view on the
interaction of temperature and precipitation. An approx. 25 day
delay in the growing season at the north-facing slope, owing to
late snow melt does not have significantly impact on the
percentage of vessel area compared to the ridge. While
temperature controls the rate of vessel formation at the
beginning, precipitation is more important in the middle of the
growing season, especially at ridges without melt water supply.
|
Tree-ring analyses
at a sporadic permafrost site below timberline, Bever Valley,
Switzerland
Alexander Bast1,2,
Holger Gärtner1, Isabelle Roer1 & Christof
Kneisel2
1
Swiss Federal Research
Institute WSL, Dendro Sciences Unit, 8903 Birmensdorf,
Switzerland
2
University of Würzburg,
Department of Physical Geography, 97074 Würzburg, Germany
e-mail:
a.bast@uni-wuerzburg.de
The study presented focuses on
tree growth analysis at a north facing slope extending from 1800
to 1900 m a.s.l. in the Bever Valley (Bever, Switzerland), a
tributary of the main valley Upper Engadine. BTS (bottom
temperature of winter snow cover) and geoelectric measurements
point to the existence of permafrost lenses at this site, which
was also confirmed by one core drilling experiment in 2006.The
slope is covered with a dense forest stand consisting of larch (Larix
decidua Mill.) and Swiss stone pine (Pinus cembra ssp.
sibirica). The trees do not show any morphological
differences (e.g., dwarfing) to trees adjacent to the slope, not
even to trees growing on the opposite south facing slope, where
definitely no permafrost is present.
The aim of the study was (i)
to investigate the possibility of detecting the presence of
permafrost by analyzing ring-width variations in larch related
to a local reference chronology established on the south facing
slope across from the study site, and (ii) if so, to determine
the spread of isolated permafrost lenses across the slope
combined with geophysical soundings. On the permafrost site, 88
dominant larch trees (av. age: 210 years) were cored in 5
horizontal transects and the position of each sampled tree was
documented in a detailed map of the slope. In addition, 18 trees
from the south facing slope were used to establish the reference
chronology.
Results show a distinct growth
suppression in the reference chronology from 1879 to 1890, where
average ring width is reduced by 30% compared to the average of
40 years before and after this time period. This period of
reduced growth also occurs in the chronologies of 44 trees (P 1)
taken from the permafrost site, which do show growth development
comparable to the reference. The remaining 44 trees (P 2) from
this site do show a strong growth suppression (up to 80%)
starting in the period 1879 to1985 but they do not recover after
1890. Annual growth of 24 trees of P 2 remains reduced until the
1960`s, then annual ring width increases again up to the level
which is common for the site. The remaining 20 trees of P 2 show
reduced growth until the 1990`s, when a weak growth release
started, not reaching the level of common growth.
First comparisons of single trees showing the enduring growth
reduction do correspond with locations of permafrost lenses
detected by geophysical soundings along a vertical transect
across the slope. According to the results of the tree ring
analyses it can be assumed that the permafrost lenses at this
site developed around 1879, because all trees do show a
comparable higher growth level for more than hundred years
before this suppression occurred. However, ongoing analysis is
directed to answer the question, if these 20 trees do all
definitely show the presence of permafrost or just low soil
temperatures restricting root growth. |
An easy technique
to collect wood and bark samples for anatomical studies
A. Boura and D. De
Franceschi
Muséum National d'Histoire
Naturelle. Département Histoire de la Terre. UMR 5143
Paléobiodiversité et Paléoenvironnement. Case Postale 38
Laboratoire de Paléobotanique. 57, rue Cuvier 75231 PARIS cedex
5.
email :
boura@mnhn.fr
Trees, and thus wood, are
major components of the biosphere. Wood constitutes a huge
source of information regarding several domains like systematic,
ecology or adaptative evolution. Despite its significance, wood
is not often sampled extensively; most probably due to
logistical reasons (harvesting or carrying problems). Moreover
the material used for studies is often limited to the
collections available at the moment, thus limiting the
opportunity to use it, especially in systematic or ecological
study.
This works aims to make a
review of the different techniques which already exist to
collect wood, from the Pressler increment borer, to the new
Trephor, draw up a specific methodology to sample wood and
finally describe a new cheap and easy method to sample wood, and
its handing.
This method only requires the
use of a punch, a clearing rod and a hammer. The punch is a
tool, initially designed to make holes on quite soft materials
such as leather or rubber, but which has proved to be useful to
core several trees, from softwood to hardwood, from temperate to
tropical species.
This sampling method has
several assets. The diameter of the tool, and thus of the core
varies from 1 mm to a few cm and can be adjust regarding to the
specific use of the wood sample. It is cheap and easy to find.
It is light and not bulky. In addition to this, its handing is
relatively easy and it allows taking a more or less big sample
containing the outermost stem tissues (bark, phloem, cambial
zone) and a more or less big part of the most recently formed
wood.
The sections prepared from the
obtained samples are perfectly usable for anatomy. The samples
can be collected as complements for herbarium samples (for
systematics) as well as for particular dendroecological studies
on tree diameter growth under to climate, soil and forest
structure and dynamic influences on individual trees. |
The anatomy of
invasion: A dendrochronological investigation of a woody weed,
Senna siamea (Lam.) HS Irwin & Barneby, in Australia’s
far north
Matthew Brookhouse
The Australian National
University, 48 Linneaus Way, 0200 Canberra, Australia
e-mail:
matthew.brookhouse@anu.edu.au
Senna siamea,
a tree species native to south-east Asia, is currently invading
the remote rainforests of Cape York. Its spread towards the
riverine forests in the Mungkan-Kandju National Park is of
particular concern. Due to its speed, scale and patchiness the
invasion has proven difficult to document. Thus, little is known
about the process of invasion by this woody species.
Dendrochronology has the capacity to provide data on tree age
and radial growth rates that can significantly improve
understanding of the dynamics of plant invasions. However, the
potential of S. siamea for dendrochronology is untested.
Thus, the question of whether the species forms annual tree
rings remains unanswered. Highly seasonal rainfall in Cape York
suggests that it is possible the species forms annual rings.
Given the limits of our knowledge of S. siamea and its
potential for dendrochronology in Cape York, we propose a
two-stage study of the species. The first stage will involve
analysis of intra-annual variation in radial growth and wood
anatomy. The second component involves the spatial and
dendrochronological analysis of tree age and growth data from
tree ring samples. |
Last millennium
multi-proxy record from a raised bog in northern Poland
Anna Cedro1,
Mariusz Lamentowicz2, Ùukasz Lamentowicz2,
Graýyna Miotk-Szpiganowicz2, Edward Mitchell3,
Jacek Pawlyta4
1University
of Szczecin, Poland
2Adam
Mickiewicz University in Poznañ, Poland
3WSL,
Swiss Federal Institute for Forest, Snow and Landscape Research,
Lausanne, Switzerland
4
Silesian University of Technology, Poland
e-mail:
Anna.Cedro@univ.szczecin.pl
Stàýki peatland is in the
initial phase of the palaeoenvironmental studies.
Reconstructions are based on analyses of: dendrochronology,
testate amoebae, palynological, plant macrofossils and stable
isotopes. Aims of the research were: reconstruction of the last
millennium environmental changes, reconstruction of local and
regional climatic changes, and an attempt to recognize between
signal of human impact and climatic change
Monolith sampled from the
central part of the mire was dated with two methods C-14 and
Pb-210. The sampling of 22 trees was carried out with Pressler
increment borers. High resolution approach applied to the peat
material and dendro samples allows to obtain precise
palaeoenvironmental reconstruction from northern Poland. We
hypothesize that proxies used in the study will give us the
opportunity to recognize the climatic and human signal in the
peat and trees archive.
Also tree rings from the Scots pines growing on the surface were
studies to describe the magnitude of human impact during the
last 100 years. The chronology (ST) based on 13 individual
patterns, cover the period of 143 years (1862-2004), it was used
to dendroclimatological research: signature years and response
function analysis. No distinct relationships between the ring
widths and the climatic conditions were observed. The
determining factor of cambial activity of Scots pine growing on
bog was human impact and connecting with it changes of
ground-water level. |
Collars, shepherds
and dendrochronology. Traditional activities end at Parc
Nacional d’Aigüestortes i Estany de Sant Maurici (Vall de Boí,
Alta Ribagorça, Spain)
Mireia Celma
Martínez
Prehistory Department-Archaeobotany
Laboratory, Universitat Autònoma de Barcelona, Edifici B Campus
de la UAB, P.C.: 08913 Bellaterra (Cerdanyola del Vallés,
Spain)
e-mail :
mireia_celma@hotmail.com
National Park of Aigüestortes
and Estany de Sant Maurici, in the Catalan Pyrenees, was a
territory interpreted exclusively as a natural landscape before
2004. Three years ago, archaeologists from Universitat Autònoma
de Barcelona started a new social study focused in the
explanation of interaction between societies and natural
high-lands.
During prospection field work
it was detected a repeated injury in P.uncinata population, long
cuts in bark made by human and related with pastoral activities.
This raw material was used for production of collars for
flocks-herds by shepherds of nineteenth and twentieth centuries.
Resulting objects of this local production were studied and
related to injuries detected in some areas of National Park. The
object is to record last practices of shepherds from high-lands,
a lost knowledge that is just still alive in trees. An extensive
dendrochronological study of these bark injuries could show a
large chronology for understanding the beginning and end of
traditional practices in the Catalan Pyrenees.
Thanks to National Park of Aigüestortes and Estany de Sant
Maurici (Alta Ribagorça, Catalonia, Spain), Ecomuseu de
les Valls d’Àneu (Esterri d’Àneu, Catalonia, Spain),
Ecology Department of Universitat de Barcelona (Catalonia,
Spain) and Prehistory Department of Universitat Autònoma de
Barcelona (Catalonia, Spain). |
A junipers woodland
story: spatial and temporal patterns in a mixed stand of
Juniperus thurifera, Quercus ilex and Pinus sylvestris
Lucía de Soto1,
José Miguel Olano1, Vicente Rozas2
1
Departamento de Ciencias
Agroforestales, E.U.I. Agrarias de Soria, Universidad de
Valladolid, c/ Los Pajaritos s/n, 42003 Soria, Spain.
e-mail:
luciadesoto@gmail.com;
jmolano@agro.uva.es
2
Departamento de Ecología, CIFA de Lourizán, Apdo. 127, 36080
Pontevedra, Spain. e-mail: vrozas.cifal@siam-cma.org
Introduction:
Thuriferous juniper woodlands
(Juniperus thurifera L.) develop on continental
Mediterranean environment over a narrow distribution and are
included as a priority habitat in UE Habitat Directive
(Directive 92/43/EEC). They are usually open forest systems or
coppice forests historically subjected to intense human
management. Thuriferous juniper is the dominant species, but
usually coexists with other trees, particularly oaks and pines.
Recent structure could be explained either as a result
environmental growth constrains for the other tree species or as
a consequence of traditional management.
Our questions are: (1) if
stressful growing conditions favour juniper dominance, which are
the growth pattern of the different tree species in a juniper
woodland?, (2) if the structure is influenced by management,
which factors determine their past and current structure?, and
(3) analysing the results of both hypothesis, what can we infer
about the future dynamics in this woodland?
Methods:
The selected stand was located
in Cabrejas del Pinar, north-central Spain, at 1300 m above sea
level, on poorly developed soils under limiting climatic
conditions. All the individuals found in a square plot of 1.44
ha were labelled, mapped, cored and measured. Individuals were
divided into two cathegories: trees (DBH > 5 cm) and saplings (DBH
< 5 cm). Standard dendrochronological techniques of tree-ring
dating and ring-width measuring were performed to compare tree
growth and to detect releases. Ripley’s K statistic was
used to analyse spatial distributions. Historical information on
cattle numbers was used to reconstruct management changes in the
past.
Results:
In the middle of XIX century
most of J. thurifera trees in the study plot have been
recruited and showed low radial growth rates and an abrupt
growth suppression in 1880, moreover other recruitment pulse
took place in the last five decades. Scots pines (P.
sylvestris L.) and holm oaks (Quercus ilex L.) showed
higher growth rates and established more recently, since 70’s.
J. thurifera
trees tend to be located together in clumps including both
genders, but separated from clumps of conspecific saplings.
Q. ilex saplings and trees tend to be associated to J.
thurifera, while P. sylvestris showed a random
spatial pattern.
Discussions:
The low growth rates of J. thurifera in comparison to
those of P. sylvestris and Q. ilex may reject the
hypothesis to a differential effect of environmental stress.
Results suggest that pines and holm oaks perform well in this
stand. Cattle density controls junipers, pines and holm oaks
radial growth and recruitment. Traditional management
abandonment has allowed other species entrance into the juniper
woodlands, with juniper facilitation as a nurse plant. If
grazing pressure is maintained in higher level than present one,
juniper woodlands will preserve theirs actual structure and
composition. However, if grazing keeps on low levels, holm oaks
and pines will increase the dominance in the stand and relegate
junipers to a supporting role. |
Inter species
comparison of tree ring
d13C
and
d18O
from subalpine sites in High Asia
J. Grießinger1,2,
A. Bräuning1 & G.H. Schleser2
1
Friedrich-Alexander-Universität Erlangen-Nürnberg, Institut für
Geographie, Kochstrasse 4/4, D-91058 Erlangen, Germany
2
Forschungszentrum Jülich GmbH, Institut für Chemie und Dynamik
der Geosphäre, ICG-V Sedimentäre Systeme, Leo-Brandt Strasse,
D-52425 Jülich, Germany
e-mail:
jgriess@geographie.uni-erlangen.de
In this study, we present the
relationship between climatic factors and annual isotope values
(d13C;
d18O)
in cellulose from tree rings of spruce (Picea balfouriana)
and juniper trees (Juniperus tibetica). The subalpine
investigation site is situated in the south western part of the
Tibetan Plateau, where the annual climate is mainly influenced
by a clear shift between summer and winter. During summer, the
influence of the Indian and East Asian monsoonal systems becomes
predominant, resulting in high summer temperatures and high
precipitation amounts caused by strong convective systems.
During winter months, the climate of the investigation area is
controlled by prevailing westerly winds, bringing cold and dry
air masses to the southwest of the Tibetan Plateau. As the
high-elevation site is characterized by steep slopes and soils
with limited water storage, access to groundwater is almost
excluded. Therefore, our site selection emphasizes two important
influencing factors for the stable carbon and oxygen isotope
fixation in tree rings. Water uptake by the roots should clearly
record the
d18O-signal
of precipitation, modified by the isotopic enrichment effect of
leaf water. The
d13C-values
in tree rings should tape atmospheric conditions during carbon
fixation controlled by evapotranspiration conditions at leaf
level.
First results indicate for both tree species highly significant
negative correlations with precipitation amounts during the
summer months. Results of the oxygen ratios of tree rings
underline therefore their strong potential to reconstruct past
climate variabilities. In contrast, characteristic differences
occur within the carbon isotope variations, where juniper trees
show only weak signal strength. |
The relation
between the microscopic structure and the wood density of
Fagus sylvatica L.
Vladimír Gryc, Hanuð
Vavrèík, Michal Rybníèek, Eva Přemyslovská
Mendel
Universtiy of Agriculture and Forestry Brno, Faculty of Forestry
and Wood Technology, Department of Wood Science, Zemědělská 3,
613 00 Brno, Czech Republic.
e-mail:
gryc@mendelu.cz
The European beech (Fagus
sylvatica L.) is one of the most important commercially used
hard wood species both in the Czech Republic and other countries
in Central Europe. In 2005, its proportion amounted to 6.6 % of
the total area of the Bohemian and Moravian forests. The aim of
this study was to compare the structure of the juvenile and
mature beech wood in relation to the wood density (moisture
content 12 %). The comparative analysis between the juvenile and
mature wood examined the diameter of vessels, the width and
height of pith rays, and the number of vessels and pith rays per
1 mm2. The results show that the average vessel
diameter, as well as the width and height of the pith rays reach
statistically lower values in the juvenile wood than in the
mature wood. On the other hand, no significant difference
between the two woods has been found in terms of the frequency
of vessels per 1 mm2. Having said that, the
difference in the frequency of rays per 1mm2 between
the juvenile and mature wood is far from negligible; the
juvenile wood has three times as many pith rays as the mature
wood. The density of the juvenile wood is higher (r12
= 726,07 kg/m3) than the density of the mature wood (r12
= 701,50 kg/m3).
The project was financially supported by the research invention
of Forest Faculty of the Mendel University in Brno, MSM
6215648902. |
A predictive GIS
model to locate tree-rings in the Los Tuxtlas forests (Veracruz,
Mexico)
Genaro Gutiérrez-Garcia,
Martin Ricker
Estación de Biología Tropical
“Los Tuxtlas”, Universidad Nacional Autónoma de México (UNAM),
Apartado Postal 94, San Andrés Tuxtla, Veracruz 95701, México.
e-mail:
genaro.gutierrez@gmail.com
Tree-ring research has been mainly focused on tree species of
temperate and semiarid zones. In contrast, relatively few
tree-ring chronologies have been determined in the tropics.
Recent dendrochronological work reports the presence of annual
rings in several tropical areas with short drought periods or
long-lasting inundations. Due to its high tree species
diversity and elevational range of 0-1,700 m above sea level the
1,500 km2 Los Tuxtlas Biosphere Reserve is a suitable area to
search for previously unreported tree species with
dendrochronological potential, from lowland rainforest to pine
and cloud forest. The main object of the present study was to
develop a predictive model based on a Geographic Information
System (GIS) to identify areas where trees can be expected to
form annual rings. The layers used in the model were climate,
insolation, soil type, soil texture, slope, slope position,
aspect, and vegetation (all nine in digital raster format). We
used the GIS to identify areas with short drought periods, steep
slopes, and nutrient deficient soils, and low insolation sites.
The predictive model indicates that18.12% of the area can be
expected to present annual rings. The corresponding field work
for verification will follow next. |
Hydrogen Isotopes
in a 400-Year Pinus uncinata Chronology from NE Spain
Sarah Hangartner, Marc
Filot, Markus Leuenberger
University of Bern, Climate
and Environmental Physics, Sidlerstrasse 6, 3012 Bern,
Switzerland
e-mail:
shangart@climate.unibe.ch
We measured annual hydrogen
isotope ratios in α-cellulose of mountain pine (Pinus
uncinata) growing in a subalpine forest in eastern
Pre-Pyrenees (Massís del Pedraforca). The online equilibration
method described in [1] was applied to measure the D/H ratio of
the non--exchangeable hydrogen. We compared the δD chronology to
the 400-year Pedraforca δ18O chronology [2]. Although
both hydrogen and oxygen originate from source water and share a
common pathway until the evaporative enrichment in the leaves,
the correlation between the chronologies is poor. Sporadic years
show extreme signals in both hydrogen and oxygen datasets. The
variability of the hydrogen serie tends to increase since 1950.
References:
[1] M. Filot et al.
Rapid online
equilibration method to determine the D/H ratios of
non-exchangeable hydrogen in cellulose. Rapid Commun. Mass
Spectrom. 2006, 20, 3337-3344.
[2] M. Filot. Isotopes in tree-rings: Development and
application of a rapid preparative online equilibration method
for the determination of D/H ration of nonexchangeable hydrogen
in tree-ring cellulose. PhD thesis, University of Bern,
Switzerland, December 21, 2006, 104 pp. |
Growth rings in
selected tropical Meliaceae species
Ingo Heinrich1
& Hans Beeckman2
1
Research Center Jülich, ICG-V,
Wilhelm-Johnen-Straße, 52425 Jülich, Germany,
i.heinrich@fz-juelich.de
2
Royal Museum for Central Africa, Leuvense Steenweg 13, 3080
Tervuren, Belgium
Tree-ring proxy data from the
tropics are valuable but sought after sources for climate
reconstructions and modelling to better prepare for the
catastrophic impacts of droughts and floodings caused by
long-term climate fluctuations such as ENSO. Although tree rings
in tropical trees are often difficult to identify, the tropics
still offer a vast pool of potentially valuable tree species for
future dendrochronological investigations. However, the
challenge remains to find the most useful species. A very
efficient approach is to analyse xylarium samples in order to
shortlist a number of potentially useful species for
dendrochronology instead of conducting arduous and expensive
field work in remote places often without any warranty of
success.
The current study concentrated
on the Meliaceae as it is among the most promising tropical
plant families for tree-ring studies. Most of its species are
deciduous to semi-deciduous trees and shrubs and often display
distinct ring boundaries. Several genera of the Meliaceae (Cedrela,
Swietenia and Toona) have already been used
successfully in tree-ring research, however, little is known
about the remaining 500 species, some of them likely with good
potential for new dendro-studies in the tropics.
Hence, wood anatomical analyses were conducted on selected
Meliaceae samples filed at the Tervuren xylarium. The analyses
concentrated on wood structures visible in cross-sections, that
is, the presence of parenchyma bands, distinct changes in vessel
and/or fibre sizes, ring widths, incidents and forms of possible
false or missing ring structures and any other obvious
structural anomalies. Additional attributes collected in
Tervuren were origins of the sample, geographical and ecological
site descriptions and size/age of the trees sampled. The poster
presents first results forming the basis for further tropical
tree-ring research. |
Tree-ring study of
the island formation and riparian forest along a gravel-bed
river in the Polish Carpathians
Ryszard J. Kaczka1,
Bartùomiej Wyýga2, Joanna Zawiejska3
1Faculty
of Earth Sciences, University of Silesia, Sosnowiec, Poland
2Institute
of Nature Conservation, Polish Academy of Sciences, Kraków,
Poland
3Institute
of Geography, Pedagogical University, Kraków, Poland
e-mail:
kaczka@wnoz.us.edu.pl
The Biaùka River draining the
Northern Carpathians, southern Poland, is one of the last
relatively undisturbed, gravel-bed rivers in Central Europe. Its
riparian zone and the floodplain are subject to human
activities, mainly wood harvesting and farming. However, the
character of both the island vegetation and the river channel
remain typical of the formerly widespread, semi-natural, braided
rivers in the Carpathians. The study aims at reconstructing
spatial and temporal dynamics of the island development in such
a gravel-bed river.
The research was conducted in
a 5 km long section of the lowest river course, where the active
channel is widest and islands and bars are most common.
Twenty-six established islands, their entire population in the
section, and the associated pioneer islands were analysed.
Standard dendrochronological techniques were employed to
determine age structure of trees growing on the islands and in
the riparian forest. The age of the oldest specimens was
considered to represent a minimal age of the island, and age
structure of the vegetation as a proxy of its spatial
development. The tree-ring dates were verified by more general
information gathered from an analysis of maps and aerial photos.
Willow and alder predominate on most of the islands, whereas
spruce and pine grow on older islands and in the riparian
forest.
So-defined minimal age of
islands is related to the occurrence of major floods that
effectively change the pattern of a braided channel. On the
Biaùka River, the last such floods occurred in 1997 and 2001.
Although a signal of previous floods is less apparent in
tree-ring dating, a comparison of the age of the islands and the
riparian forest reveals significant differences in the factors
controlling development of both elements of the riverine
landscape. When the first is related to the occurrence of
floods, the second is more independent of a natural dynamics and
largely determined by human activity.
Though preliminary results indicate different scenarios of the
island initiation and development, which are registered in the
tree-ring proxy, a common pattern exists – the oldest trees grow
in the central, best protected part of the islands. The decrease
in tree age from the island centre is more pronounced in the
upstream than in the downstream direction. Centrally growing
trees play an important role in the island development as they
trap wood and mineral sediment on the upstream island margin,
hence stimulating growth of islands in the upstream direction.
That pattern of island formation seems typical of mountain
European rivers, from which large wood pieces are typically
removed and where the resultant lack of key-member fallen trees
prevents initiation of bar and island formation in their
hydraulic shadow. |
Dendrochronological
method in use of dating three mansions from South Estonia
Ragnar Kapaun
University of Tartu, Faculty
of Biology and Geography, Institute of Geography, Kirde 1a-19,
Elva, Estonia
e-mail:
rk@ut.ee
Estonia is considered
relatively rich for its architectural heritage, which in some
parts can be found very genuine. Although we have plenty of well
preserved and restored old buildings, many of them are still in
bad condition. With every forgotten place we loose a piece of
our history. To prevent that from happening, we have to take
care of dilapidated heritage. The least to be done is to explore
deeply and preserve all the reasonable material.
And this is where
dendrochronology has to take part in this extremely important
process.
This thesis reflects author’s
progress in the field of dendrochronology, with the main aim to
date three old buildings using dendrochronological methods. All
the buildings are situated in southern part of Estonia: Rootsi
dairy farm and Suure-Kambja mansion are in Tartu County and
Toolamaa manor in the Põlva County.
The results were definitely
interesting. Toolamaa mansion was expected to date to the end of
17th or the beginning of 18th century. Dendrochronological
analysis showed that the wooden part of the house was probably
built in 1836 or 1837. So, about one century later than guessed.
The mansion of Suure-Kambja showed also significant outcome. As
the assumed building time was in the end of 18th or the
beginning of 19th century, dendrochronological dating indicates
to the exact year 1728, awhile after the Great Northern War. The
building time of the mansion was budged back in time about half
a century. The Rootsi dairy farm resulted with two different
dates from different parts of the house. It can be interpreted
so that the roof of the building was built in 1835 and evidently
in the same year the ceiling beams had been also put into the
stone-walled building. Shortly after 1897, in the very end of
19th century some renewing works were carried out, in which some
of the timber was replaced.
As mentioned, it is important
to continue practicing dendrochronological researches in
Estonia. As this work confirmed the area of Estonia can be
considered dendrochronologically homogeneous, the work will
continue. It is necessary to extend the local tree-ring network
and optimize tree-ring chronologies along with taking part in
the process of preserving the national cultural heritage. These
are the present main goals of dendrochronology in Estonia.
|
Dune movements and
tree rings: Czolpinska dune, Slowinski National Park, Poland
Marcin Koprowski1; V. Winchester2 ; A.
Zielski 3;
1Laboratory of Dendrochronology. Institute of Ecology and Environment
Protection, Nicolaus Copernicus University, Gagarina 9, 87-100
Torun, Poland.
koper@biol.uni.torun.pl
2Oxford
University Centre for the Environment, School of Geography,
Oxford OX1 3QY, U.K.
3Faculty
of Geology, Geophysics and Environmental Protection, University
of Science and Technology, al. Mickiewicza 30, 30-059 Kraków,
Poland.
One implication of climate
warming is that dunes in many parts of the world will start to
grow and studies are needed to investigate whether trees,
affected by encroaching sand, may be used as indicators of dune
dynamics. Our study on the famous, mobile Czolpinska dunes in
the Slowinski National park, Poland
(54°43'30.32"N
17°15'36.79"E) had two main aims: to establish how tree rings of
Scots Pine (Pinus sylvestris L.)
are affected by dune movements and to estimate rates of
movement.
The forest at the base of our site, locally named ‘the VIP Dune’
supplied a reference chronology showing tree growth unaffected
by sand for comparison with semi-buried trees on a transect up
the dune slope.
We
analyzed tree-ring widths from the semi-buried stems
using classical ring-width measurement, statistics and skeleton
plotting techniques
to provide (i) dates for initiation of tree suppression and (ii)
dates for reaction wood and eccentricity. The horizontal
distance from a buried tree to the dune base divided by the
number of years since the tree was first suppressed, or began to
form eccentric rings or compression wood, supplies a maximum
estimate for the rate of sand advance. The estimate is a maximum
because, as we found, tree reactions to invading sand may
frequently be delayed, with the length of delay possibly
dependent on whether dune movement is fast or slow; in which
case a tree may have time to adapt and, initially at least, show
no visible reaction at all. However, other factors including
genetic susceptibility and disease may also control growth
reactions, thus reducing the accuracy of annual estimates.
Despite these caveats, our preliminary findings are that
Czolpinska dune movements have decreased from previously
measured rates of between 3.5 m and 10 m/yr, to a maximum
between 2 and 3 m/yr since 2000. We hope to return in the
following years to check our results by re-measuring sand height
on a number of marked trees growing where the dune base met the
forest floor in July 2006. |
Influence of
climate on formation of radial growth
Pinus
Sylvestris
L. in
forest
and forest-steppe
zones of Ukraine
Koval I.M.
Research Institute of Forestry
and Forest Melioration, Pushkinska 86, 61024 Kharkiv, Ukraine
e-mail:
koval@uriffm.org.ua
Response of pine to climatic
fluctuation in different native zones of Ukraine presents
significant interest.
Objects of our research were
pine pure stands of medium ago located in different zones of
Ukraine with slight anthropogenic influence.
We have revealed common
pointer years of radial growth in forest and forest-steppe zones
for 1946-2001. Years of minimal of growth are
1952, 1956, 1963, 1976, 1979
that characterize small precipitation during vegetation and
severe winters. During years of maximum of growth:
1965, 1970, 1978, 1985, 1993
and 1997
was recorded high precipitation during vegetation period.
We have detected that in
Polissja radial growth limits temperature of could period (from
previous December to current March) in contrast to steppe where
influence droughts in period of vegetation on radial increment
was observed. Common influence minimal precipitation and winter
low temperature strengthen depression of growth. In last twenty
years in investigated stands we didn’t reveal decrease of radial
growth.
Soil also influences on
response of forests to fluctuation of climate. Positive mean
correlation between tree ring indexes and hydrothermic
coefficients О3,
that represents ratio of warmth and humidity during current year
and three previous years and with О1,
that characterizes ratio of warmth and humidity for current
year. In this case different reaction of trees growing on soil
with different moisture was discovered. |
Comparison of
densitometrical and histological methods to the identification
of early- and latewood boundary in tree-rings of spruce (Picea
abies [ L.]
Karst.)
J. König, B. Günther,
C.T. Bues, S. Marschallek
Technische Universität
Dresden, Institute for Forest Utilization and Forest Technology,
Chair for Forest Utilization, Pienner Straße 19, D-01737
Tharandt, Germany
e-mail:
koenig@forst-tu.dresden.de
The detailed demarcation of
early wood against late wood takes place in general using the
histological method for conifer woods after MORK. Therefore,
microsections were made and the coloured wood cells regarding
the cell wall thickness and cell lumen width were measured. To
implement multivariate cross correlation (KOENIG et al. 2004) a
reproducible early and late wood demarcation is necessary.
The base for the
densitometrical method of classification is the ratio between
the intra-annual minimum and maximum wood density values. 297
different tree ring sequences with approx. 39.000 wood cells of
spruce (Picea abies [L.] Karst.) from upper elevations
sites of the Erzgebirge Mountains (Oberwiesenthal, Abt. 368 a1,
1070 m a.s.l., Saxony,) were subjected to densitometric and
histological analysis.
It was shown that with the x-ray densitometric method all wood
cells were classifiable in early and late wood zones. On the
other hand, sometimes the late wood cells of thin and bright
tree rings could not be classified after MORK to late wood zones
because of the thin-walled wood cells. The late wood zones
calculated with both methods were compared with one another for
significant differences. As a result, the more practicable
densitometrical research method does not differ significantly
from the histological method after MORK. |
Dendrochronological
dating of churches from southern Poland
Marek Kràpiec,
Elýbieta Szychowska-Kràpiec, Andrzej Zielski
AGH – University of Science
and Technology; Department of Geology, Geophysics and
Environmental Protection
e-mail:
mkrapiec@geol.agh.edu.pl
In Poland, in many cases
problems arise at precise dating of old churches, because
written sources often do not specify the time of their building,
repairs, or reconstruction. The analyses presented were aimed at
determination of the absolute age of timbers from the roof
structures of historic churches from the Úwiætokrzyskie
voivodeship in S Poland. The research was carried out in 11
churches, from which altogether over 200 wood samples, mainly of
coniferous tree species, were taken. Scots pine (Pinus
sylvestris L.) was predominating and wood of fir (Abies
alba M.) was occasionally encountered. The dating was made
on the basis of regional standards for Scots pine, constructed
by A. Zielski (1106-1991) and E. Szychowska-Kràpiec (1622-1996),
and for fir – by E. Szychowska-Kràpiec (1106-1997).
The oldest examined object
turned out to be the church in Wiúlica, funded by the king of
Poland Kasimir the Great in the 3rd quarter of the 14th c.
Dendrochronologically analysed elements of the roof structure
came from fir trees cut down in 1365AD.
The other analysed churches
are younger objects; two of them, in Zborówek (1443 AD) and in
Czerwony Chotel (1449 AD), represent the middle of the 15th c.
In both cases the roof structures of the churches retained wood
from that time. The church in Chroberz turned out to be of
similar age; dendrochronological dating of wood from the
structure indicates 1437 AD, although the source data point out
the construction of the church in 1550 AD.
In the cases of younger
objects, dated to 16th, 17th, and 18th c., certain differences
between the data from archival sources and the
dendrochronological dating of wood from the roof structures also
appeared. According to the source data, the church in Nowy
Korczyn dates back to the middle of the 17th c., however, the
analysis did not reveal such old wood. The wood sampled from the
structure represents trees cut down in 1776 AD, which may point
out repairing of the roof. Similar is the case of the church in
Dobrowoda, built in the mid-16th c., though wooden elements of
the roof structure were dendrochronologically dated only to the
first half of the 18th c. (1734 AD). Lower divergence issued at
dating of the church in Maùogoszcz, according to the archive
materials built in the 1590s, whereas dated wooden elements came
from pine trees cut down in 1660 AD.
In the cases of the four
remaining churches, out of 11 ones examined, i.e. the 16th and
17th c. churches from Krzciæcice, Imielno, Szaniec, and Kossowo,
the results of the dendrochronological dating were in agreement
with the archive materials.
The research performed
resulted in construction of a local pine chronology, containing
520 rings and covering the period 1257-1776. It also permitted
to verify, precise, and specify data concerning history of
construction of some sacral objects in the Úwiætokrzyskie
voivodeship. |
The influence of
oil-shale underground mining on the growth of trees in Kohtla
mining area in northeastern Estonia
Kristel Kund, Vivian
Uibo
University of Tartu, Institute
of Geography, Estonia
e-mail:
Krkund@ut.ee
Oil-shale in northeastern
Estonia is mined in Ida-Virumaa area on the territory that
extends from Kiviõli in the west to Narva River in the east and
from Jõhvi in the north to Väike-Pungerja in the south.
Oil-shale mining causes numerous negative changes in the
environment: hollow gaps beneath the ground may collapse, the
groundwater level changes, waste water from the mines is being
pumped into the rivers, the micro-relief of the ground changes.
Although the main mining method used in underground mines was
chamber mining, in some areas longwall mining by combine
transporters was applied.
As the face advances the cavity behind the
line of hydraulic supports (called goaf) is allowed to collapse.
This collapsing reflects on the land surface, causing lowering
of it by 0.5 –
1.3 m.
As the ground sinks, the
forest growing on it sinks as well. Presumptively the changes in
the surface relief affect the radial growth of the trees growing
on it.
Tree-ring data has been
collected in three different subsided plots of Kohtla oil-shale
longwall mining, where mining has been conducted in different
years. These data has been compared with tree growth at two
control plots with similar environmental conditions. One
research plot consists of three circles, with the radius of ten
meters. Within the circles increment cores were gathered from
all the trees. The main tree species in the sample plots were
Norway spruce and Silver birch. Samples were gathered from 583
trees.
The aim of this research was
to find out how the radial growth (tree-ring widths) of trees
has changed since mining. One way to detect the assumed
influence of the mining is to compare the growth of the trees in
mining areas with that of the trees from the control areas.
Another option is to compare the radial growth of trees before
and after mining in the same tree samples.
Earlier studies on one
particular research plot have shown that after surface subsiding
the radial growth of spruces has mainly increased and the growth
of pines has decreased. The radial growth of trees is also
influenced by the age of the tree, position in the relief, tree
condition class, weather, inclination of trees, site conditions
and many other factors. To obtain more objective results about
the influence of surface deformation to tree growth, our further
studies contain different research plots and control plots.
|
Contribution to
chronology of conifers in northern and eastern Carpathians
(Slovakia and Transcarpathian Ukraine)
Kyncl T., Kyncl,
J., Fedaka P., Lukáè L.
DendroLab Brno, Eliáðova 37,
616 00 Brno, Czech Republic
e-mail:
kyncl@dendrochronologie.cz
The aim of the presented
research is the construction of master chronologies of conifer
species for northern Carpathian Mts. (Slovakia and Eastern
Ukraine). According to our preliminar survey, most of historical
wooden constructions in this region are made of fir, spruce and
larch. Now the fir chronologies have been compiled; and we have
started with the construction of larch chronology.
Fir chronology
On the basis of the
correlations among chronologies of living trees, we have
established two regions with specific chronologies. Chronologies
from western and central Slovakia (west of Preðov) show high
teleconnection to chronologies for Moravia (Kyncl J., Kyncl T.
1996) and eastern Austria (Liebert et al. 1998). Chronologies
from eastern Slovakia and transcarpathian Ukraine have specific
signal and are similar only to chronologies for southern Poland
(Szychowska-Krapiec E. 1998).
The chronology for western
Slovakia (ABSLO-we) has now the time span of 1125-1999. The most
of the series used in this chronology were taken from historical
buildings in Levoèa, Banska Ðtiavnica and Spiðské Podhradie.
For the dating of historical
wood, the construction of chronology for eastern part of
Carpathian Mts. (ABSLO-ea) is more important than the western
one. The samples have been taken from living trees and from
historical buildings, especially from wooden churches from
Eastern Slovakia and Transcarpathian Ukraine. The chronologies
for living trees were constructed for years 1724-2005. The
samples were collected from Èergov-Mts, Bukovské-vrchy-Mts
(forest Stuþica), south foothills of Gorgany-Mts and forest
massif Chorna-Gora (total of ca 200 trees). The historical
samples have been taken from wooden churches of Archangel
Michael from Nová-Sedlica, St. Nicholas in the village
Chernogolova and St. Ann in the village Bukivcevo. This material
can be crossdated with south-Poland chronology and sumarized to
chronology with time span of 1627-1793.
Larch chronology
The larch wood has high
frequency especially in constructions from Spið region. In some
specific regions (esp. Levoèa), more the 50% of beams are made
of larch wood. The closest larch chronologies from Eastern Alps
(cca 450 km westwards) are not suitable for cross-dating because
of low similarity with our material. In recent period, material
from historical objects is been collected and the first floating
chronologies are been developed.
References:
Kyncl J., Kyncl T., 1996:
Dating of historical fir (Abies alba) wood in Bohemia and
Moravia. Dendrochronologie 14: 237-240.
Liebert S., Grabner M., Wimmer
R., 1998: A 1000year fir chronology for East-Austria. In.:
Proceedings of Europpean dendrochronology workshop
„Eurodendro-98“, Kaunas: 18-23.
Szychowska-Krapiec E., 2000:
Poznoholocenki standard dendrochronologiczny dla jodly Abies
alba z obszaru poludniownej Polski.
Kwartalnik AGH, Geologie 26(2):
173-299. |
Subfossil pine woodland
and trackways in Campemoor (NW Germany)
Hanns Hubert Leuschner1,
A. Bauerochse2, B. Leuschner3 & U.
Sass-Klaassen4
1Dep.
Palynology
and Climate Dynamics, Univ. Goettingen, Germany. hleusch@gwdg.de
2Lower
Saxony State Service for Cultural Heritage,Hannover, Germany.
bauerochse@nld.niedersachsen.de
3DELAG,
Goettingen, Germany. delag_dendro@yahoo.de
4Centre
for Ecosystem Studies, Wageningen University, The Netherlands.
ute.sass-klaassenf@wur.nl.
Most of the raised
bogs in Germany are situated in the Lower Saxony part of the
North German Lowlands, in a landscape that was moulded during
the ice age. In many of these peatlands within the peat, at the
base of the raised bog peat, a subfossil wood layer of pine (Pinus
sylvestris) exists. At the Campemoor (located in the Duemmer
Geestniederung, one of the most important early settlement areas
in Northwest-Germany) these layers have been palynologically and
dendroecologically investigated. The dendroecological
correlation of the frequency, germination and dying-off of these
trees with those of the subfossil oak trunks from Lower Saxony
shows the change of the ecological conditions in a large time
scale. As a result of these investigations the transition from a
drier to a more humid climate period that initiated the raised
bog growth happened in two phases at the beginning of the 3rd
millennium, interrupted by a drier period between 2825 – 2770
BC. Afterwards large areas of former settlement sites within
today´s Campemoor became inaccessible and were covered by raised
bogs.
The study has to be seen in
the frame of the long-term research focus on subfossil bog
trees. The Dendrochronological laboratory at Göttingen
University holds the worldwide biggest archive of subfossil bog
oaks. This dataset comprises c. 3000 samples from NW Germany
covering the period from 6000 BC to AD 1000. Synchronous changes
in growth pattern and population dynamics of subfossil bog oaks
from different locations in NW Europe (Ireland, The Netherlands,
Germany) indicate that contemporary „stress-events“ occurred in
former wetland woods. The striking common variability in the
medium and long frequency domains of the tree-ring records
support the assumption that changes in past climate play a key
role as a trigger of environmental changes in these wetland
woods. The ongoing studies on subfossil pine from NW-German
peatlands indicate “stress-events”, most likely linked to
striking environmental changes, around 4.700 BC (Jan Eckstein,
TRACE 2007) and 2.900 BC which exactly synchronize with those in
oaks. The fact that peatlands with pine are known as common
stages of mire ecosystems provides the chance to use
dendroecological reconstructions of peatlands to get a better
understanding of climate influence on bog ecosystems. Moreover,
this 7.000-year long monitoring system has the potential to
serve as an unique source of information for recent mire
restoration projects.
References:
Leuschner,H.H., Sass-Klaassen, U., Jansma, E., Baillie, M.G.L.,
& Spurk, M. 2002: Subfossil European bog oaks: population
dynamics and long-term growth depressions as indicators of
changes in the Holocene hydro-regime and climate.
The Holocene
12 (6), 695-706.
Bauerochse A, Leuschner B, Leuschner HH (2006)
Moorhölzer und Archäologie – umweltgeschichtliche und
siedlungsarchäologische Befunde. Berichte zur Denkmalpflege in
Niedersachsen 26:40– 45
Leuschner, H.H., Bauerochse, A., Metzler, A.
2007: Environmental change,
bog history and human impact around 2900 b.c. in NW Germany – preliminary results from a dendroecological
study of a sub-fossil pine woodland at
Campemoor, Dummer Basin.
Veget Hist Archaeobot (2007) 16:183–195
|
Light rings in
larches: searching the causes
Alar Läänelaid
Institute of Geography,
University of Tartu
e-mail:
alar.laanelaid@ut.ee
Tree ring series of larches (Larix
spp.) growing in Estonia often contain special tree rings
which are characterized by three features:
1) Light rings with a very
narrow latewood band,
2) The ring width is several
times smaller than that of the neighboring rings,
3) They often locate in groups
of 2 to 4 alternately with normal rings.
Dendroclimatological analysis
of European larches growing in Tartu has shown that there is
significant correlation of residual chronology of ring widths
with monthly temperatures of previous April (positive),
previous June and July (both negative), previous October
(positive), current January, March, and May (all positive).
Precipitation sums have significant correlation with larch
chronology in previous July and August and in current January
(all positive). This correlation can explain the width
fluctuations of tree rings, but not the structural peculiarity -
extremely narrow latewood. The reason of the light rings can be
rather extreme weather events – extreme winter colds, late
spring frosts or severe droughts in summer.
It is also possible that the
light rings were caused by any insect damage of two-year
cyclicity. The two-year cyclic ring-width pattern of larches
with light rings is very similar to that of spruces and firs
growing in British Columbia (Zhang & Alfaro 2002). Alas, the
specific cycles in tree-ring series of spruces and firs in
British Columbia are attributed to spruce budworm
Choristoneura biennis, who does not habit larches in
northern Europe. The well-known insect pests on larches in
Estonia include Coleophora laricella, Pristiphora
wesmaeli, P. erichsonii and P. laricis,
probably also Coleophora sibiricella, Zeiraphera
griseana etc., but none of them is known by biennial life
cyclicity. A butterfly Coleophora laricella can
eat the foliage of larches in Estonia, while Pristiphora
wesmaeli has caused dying the tops of the crowns and even
dying the trees in larch cultures in 1958-1960 (Voolma, person.
commun.). Today we do not know the actual causes of the cyclic
light rings occurring in larch trunks in Estonia. Investigations
are continuing to find out the reasons and explain the feature.
|
Comparison of Scots
pine (Pinus sylvestris L.) growth response to climate in
dry and calcareous fen sites in Engure Lake are (Latvia)
Iluta Lûce & D.Elferts
University of Latvia, Faculty
of Biology, Kronvalda bulv. 4, LV-1586 Rîga, Latvia
e-mail:
iluta@lanet.lv
The past history of
environmental change as a climatic signal recorded on tree rings
is well known for regions in Europe for pines growing in dry
conditions, but little knowledge has accrued regarding pine
growth on mires, especially on calcareous fens.
These areas support mostly low
stunted pines, but which can have a surprisingly old age. The
aim of the study was to determine the effect of climatic
factors on the radial growth of Scots pine Pinus sylvestris
L. on a dry soil site in relation to a nearby calcareous
fen.
The study was conducted in
the Lake Engure
Nature Park. It is a unique European wetland (the Ramsar
site since 1995) and one of the most important nature
protection sites in Latvia. Trees in the dry soil site and
calcareous fen in Latvia were sampled by coring (two cores per
tree) in the years 2005 and 2006. Tree ring widths were measured
using Lignovision, measurement quality was checked with COFECHA
and chronologies established using ARSTAN. Correlation analysis
was performed to determine the relationship between climatic
factors (mean monthly, autumn, winter, spring, summer
temperature and precipitation sum) and chronologies. Regression
analysis was conducted to determine the proportion of tree-ring
width variation explained by the climatic factors. For
regression analysis predictors were chosen using response
function analysis using the program DendroClim 2002.
Acknowledgment:
This study was partly supported by European Social Fund. |
The influence of
meandering river activity on the alders form-growth recorded in
their tree rings
Ireneusz Malik
University of Silesia,
Department of Quaternary Paleogeography and Paleoecology,
Sosnowiec 41 – 200, ul.
Bedzinska 60, Poland
e-mail:
irekgeo@wp.pl
Roots exposure and different
growth-forms of riparian black alders have been observed along
laterally unstable concave and convex banks and in relatively
stable straight reaches of the Mala Panew River, which drains
one of the largest seminatural forest complex in southern
Poland. The Mala Panew is a meandering river that flows for 20
km through a closed forest. The bottom of the valley is covered
by sands of different grain sizes and river migrate laterally
about 0,5 m/year.
Black alders growing on undercutting banks are
mostly leaned and their stems are bended, usually they have
exposed root systems. Clumps of alders growing on the concave
banks numbered several stems, the stems are 1/3 less in diameter
than alders growing near straight or convex banks. The clumps
growing on banks forced by erosion are protruding in the middle
of the river channel. Alders producing clumps with expended root
system because it predispose the plant to obtain stability in
opposite to individual stems. Numerous alders growing on the
straight banks reaches have exposed roots system and strongly
bended stems to take shape of hook. The stem hooks are formed
due long-term sediments erosion around their root systems. As
result of this process stem gradually bending under the own
weight in conditions of laterally stable channel. The alders
growing at a distance of 5-15 meters from convex banks often
have similar shapes to trees observed on the straight and
concave bank. The similarity is caused by progressive lateral
erosion and line of trees withdraw from recent bank.
In general alders growing on
river banks produce thinner rings than alders growing in same
distance from present river channel After tilting eccentric
growth in alders stems occur, in hook-shape stems at first
eccentric growth produce and after several years concentric tree
rings are formed. The preliminary investigations suggests that
shape of trunks is not only related to fluvial dynamics.
Especially it is not clear why in stable reaches trunks of hook
shape are more frequent than only slightly bended and why tilted
trees are generally rare. The question which arise is to which
extent light accessibility control tree curvature, how it is
related to channel width and finally what fluvial processes are
recorded in tree rings pattern. |
Differential effect
of drought on Pinus nigra Arn. radial growth in mesic and
xeric sites from southeastern Spain
Darío Martín-Benito1,
Paolo Cherubini2, Miren del Río1, Isabel
Cañellas1.
1
Departamento Sistemas y Recursos Forestales. CIFOR-INIA. Crta.
La Coruña km 7.5 28040 Madrid, Spain
2
Swiss Federal Institute for Forest, Snow and Landscape Research
WSL, CH-8903 Birmensdorf, Switzerland.
Email:
dmartin@inia.es
The response of Pinus nigra
Arn. radial growth to drought in the Cazorla Mountain Range (southeastern
Spain) was investigated through tree-ring records. Two mesic and
two xeric stands were selected on the basis of location, slope,
and distance to a water current. For each tree, three ring
compartments (total ring, earlywood, and latewood widths) were
measured.
In general, there seemed to be
no differences between the radial growth of trees from mesic and
xeric sites as measured from total tree-ring width. Whereas,
there were differences in earlywood and latewood widths.
Earlywood widths were greater in xeric sites, where latewood
were narrower. Higher abundance of soil water seemed to balance
the widths of earlywood and latewood in mesic sites. Mesic site
stands showed lower mean sensitivity, lower expressed population
signals (EPS), and lower between-tree signals (Rbar).
Climatic signal in the three
tree-ring compartments was investigated by means of response
function analysis. Radial growth in trees from both types of
sites was positively influenced by moist and warm previous-year
autumns and cool current-year springs. While current-year autumn
temperature positively affected trees in mesic sites, spring
precipitation was only significantly correlated with growth of
trees from xeric sites. This later fact indicated that in xeric
sites water might be a limiting resource for growth, while in
mesic sites this limitation might be lower. Thus, the higher
relative abundance of wider latewood in tree-rings from mesic
sites. This is further supported by the greater negative
influence of temperatures of previous-year summers and
current-year springs in xeric sites that might decrease the
availability of water in the soil through evapotranspiration.
Through a superposed epoch
analysis (SEA), the differential growth of tree-rings was
assessed during ten drought episodes between 1942 and 1999. All
three tree-ring compartments showed reduced growth during these
periods, with latewood being the most affected, and earlywood
the least. Trees growing in xeric sites experienced greater
tree-ring reductions during droughts than those in mesic sites.
These differences continued during the year following droughts,
when trees in mesic stands almost recovered normal growth. Two
years after the droughts, trees achieved a growth greater than
that before the drought. This second year after drought, trees
in xeric sites grew faster compared to mesic sites.
Trees in mesic sites seemed to
experience less stress and recover faster from drought, while
trees from xeric sites grew to a higher potential when water in
the soil was not limiting. |
Radial growth characteristics of Scots
pine at seacoast wooded dunes on Kolka Horn
Roberts Matisons &
Guntis Brûmelis
University of Latvia, Faculty
of Biology, Kronvalda bulv. 4, LV-1586 Rîga, Latvia
e-mail:
robism@inbox.lv
Seacoast wooded dunes are
protected habitats in the EU (92/43/EEC 2180). These habitats
are characterized as highly dynamic structures with rapidly
changing environmental factors. There have been few
dendroecological studies that have focused on tree radial growth
in these habitats.
The aim of our studies was to
obtain more information about factors affecting Scots pine
radial growth in seacoast wooded dune habitats. We hypothesized
that partial burial by sand is a factor affecting stem response
above and below the burial margin. We estimated radial growth of
sand buried and unburied trees in relation to response to
climatic factors. Correlations were determined between buried
and unburied tree radial increment, as well as pointer year
occurrence and intensity.
The research site was located
in Latvia, on the Kolka Horn. Samples were collected from trees,
which were washed off a bluff in a storm in January 2005, The
burial depth could be estimated by sand debris on the stem.
These trees were all located on the beach. Control samples were
collected from trees growing up to 200 meters deeper in coasts,
where burial was absent.
Two or three tree cores were
collected 30 cm above stem base from all trees; additional
samples were collected from buried trees at a 1.3 m height above
stem base (above burial level). All samples were collected with
a Pressler increment corer.
Response to climate was different in buried trees, compared to
unburied trees. |
Growth/drought
responses in tree rings of cultured apple trees
Burkhard Neuwirth1,
Stefanie Johann1 & Christa Lankes2
1
Department of Geography, University of Bonn, Bonn, Germany,
Meckenheimer Allee 166, D-53115 Bonn
2
Department of Horticultural Sciences, University of Bonn, Bonn,
Germany
e-mail:
b.neuwirth@giub.uni-bonn.de
Tree-ring width is an
appropriate parameter for analysing growth responses to climate
events especially in areas with extreme climate. In general,
tree-ring growth in these areas is influenced by a single
climatic forcing factor. Due to the temperate, humid climate in
Central Europe, tree-ring growth is forced by changing
influences of climatic and non-climatic factors. Analysing
pointer years in dendroecological networks recent studies test
the suitability of tree-ring widths for climate-growth analyses
in low mountain ranges and lowlands. These studies lead to a
better understanding of spatially high resoluted tree-ring
growth in Central Europe and their climatic forcings.
Taking these aspects into
account, we investigate in the recent study the stability of
various apple trees (Malus domestica) under changing
climate conditions: The study is located in the area of Bonn
(West Germany). The analysis is focused on the influences of the
record year 2003 on radial growth.
Therefore, six sorts of
cultured apple trees (Boskoop, Cox Orange, Elstar, Roter Elstar,
Golden Delicious, and Jonagold) from two locations with
different site ecological settings were analyzed. In total, 444
radii from stem disks of 111 apple trees were measured using
Lintab V. Four radii were averaged for every tree and designed
as TMC (tree mean curve). Since trees are only 15 to 19 years
old, mean increments of the period 2000 to 2005 were calculated
for each TMC and compared sortwise and sitewise. Further,
residuals from these years against the mean increment of this
time period were used to detect sort related growth responses
affected by the drought 2003.
The poster illustrates the
results of this dendroecological study and compares them with
results from horticultural investigations and crop analyses.
Thus, this study documents the suitability of dendroecological
studies for investigations on cultured fruit trees. |
Calendar-dated
Holocene snow avalanche events in the Central Eastern Alps
Kurt Nicolussi1,
Matthias Kaufmann1, Roland Luzian2, Peter
Pindur2, Andrea Thurner1, David Zrostvz1
1Institute
of Geography, University of Innsbruck, Innrain 52, A-6020
Innsbruck, Austria
2BFW,
Rennweg 1, A-6020 Innsbruck, Austria
e-mail:
Kurt.Nicolussi@uibk.ac.at
The knowledge on Alpine snow
avalanche activity in the past is usually limited to the last
few centuries. It is mainly based on historical observations and
sources. With sub-fossil logs found in a peat bog, the so-called
Schwarzensteinmoor, we could establish a record of Holocene snow
avalanche events. The peat bog is located in the timberline
ecotone of the Zillertal Alps, central Eastern Alps. Dating of
the sub-fossil samples is based on the eastern Alpine tree-ring
chronology that covers continuously the last approx. 9100 years.
Some 180 logs from the Schwarzensteinmoor date between c. 9000
to 700 BP. Many of the samples (n=55) still had a fully
developed and usually wide terminal ring indicating a sudden
death of the trees caused by snow avalanches. We have found 21
forest destroying avalanche events dated by samples with
terminal rings. The oldest event so far happened in winter
6255/54 BC. Furthermore we also analysed the logs and tree-ring
series, respectively, from Schwarzensteinmoor to find scars,
compression wood and abrupt growth reductions as indicators for
forest damaging snow avalanches. |
Dating of wooden
shelters in Polish High Tatras - tree rings records of the
pasturing history in Carpathians
Magdalena Opala,
Ryszard J. Kaczka
Faculty of Earth Science,
University of Silesia, Poland
e-mail:
magdaopala@hotmail.com
The Tatra Mts., known as the
highest range of the Carpathians arc, is also one of the main
regions of the arc where pasturing on meadows located above
timberline, has been developed since 16th century.
This aspect of human activity played a major role in changing
the mountain environment of the Carpathians for several
centuries. In many locations new openings for pastures were
established and the tree-line was driven back as a result. This
happened independently to climate dynamics. Recently wooden
shelters, the highest located architecture objects in Tatras,
appear to be the only remains of former pasturing.
We attempt the systematic
dating of shelters, the first project of its kind in the Tatras
and within entire the Carpathian Mts. Lately the
studies on the highest preserved remote shepherds’ architecture
has a special importance. Despite the fact that in 1978 High
Tatra’s wooden shelters were accepted as monuments of cultural
heritage, the number of them has decreased four times in last
century, mainly as a result of the lack of the proper
maintenance.
In total, 26 objects from 10
glades (from elevations 1000-1900 m a.s.l.) located in the
Polish High Tatras were investigated. Standard techniques for
the sampling and dating of historical buildings were used.
Approximately 10 samples were extracted from each shelter,
thought the number of core samples varied from 3 to 17, due to
differing range of timber preservation. Only wood of Norway
spruce (Picea abies K.) has been used for construction
hence the 400 years long chronology of that conifer was employed
to cross-date historical wood. From all 310 historical samples
57% have been successfully dated. The poor number of rings per
sample and the condition of wood were the main problem of
satisfying cross-dating. Results of dendrochronological dating
have shown that preserved shelters are older than that was
evaluated by the previous ethnological investigations. The
oldest timbers were dated back to XVIII century (maximal age
1756). This is concurrent with the second period of intensive
farming in Tatras. Though obtained dates are limited to the
period of last 250 years and vary within each building, the
general age structure reveals a significant relation to
particular stages of expansion and restraint in human activity
in the High Tatra. Further analyses of connections with climate
dynamics and history can be provided for better understanding of
natural and anthropogenic changes of alpine environment in the
Carpathians. |
Carbon isotopic
composition in tree-rings: a temperature record and a tool for
biomonitoring CO2 level
Sùawomira Paweùczyk1,
Anna Pazdur1, Tatjana Boettger2, Marika
Haupt2, Marek Kràpiec3, Elýbieta
Kràpiec-Szychowska3
1Department
of Radioisotopes, Institute of Physics, Silesian University of
Technology, Krzywoustego 2, 44-100 Gliwice, Poland
2UFZ-Umweltforschungszentrum
Leipzig-Halle GmbH, Sektion Hydrogeologie, AG Paläoklimatologie;
Theodor-Lieser-Strasse 4, 06120 Halle/Saale, Germany
3Dendrochronological
Laboratory, AGH University of Science and Technology,
Mickiewicza 30, 30-059 Cracow, Poland
e-mail:
Slawomira.Pawelczyk@polsl.pl
Tree rings can be used as
archives of climatic and environmental data. For the
reconstruction of past climatic and environmental changes there
can be used tree rings widths, maximum late wood density and
other parameters as stable isotopic composition in tree rings.
Investigations of stable
isotopic C, H, and O composition in
a-cellulose extracted
from tree rings of pines (Pinus sylvestris L.) growing in
the ecologically clean Suwaùki region, North Eastern part of
Poland were undertaken. Presented isotope records cover the
period 1900-2003. Those measurements constituted a part of more
complex investigations of stable isotopic composition in tree
rings for this region for last 400 years in the frame of
European project ISONET.
Values of
d13C,
d18O
and d2H
observed in the tree ring
a-cellulose
are compared to meteorological data (temperature,
precipitation). On the basis of those investigations
d13C,
d18O,
d2H
can be regarded as an indicator of
summer climate change. Relations between
isotopic
and meteorological data (temperature and
precipitation) demonstrate that precipitation influences the
stable isotopic carbon, oxygen and hydrogen ratios to a lower
extend than temperature. In case of correlation coefficients due
to temperature the highest correlation coefficient exists for
hydrogen (r=0.57, n=73, p<0.001) from among the three
investigated isotopes.
Carbon isotopes are widely
used as indicators in the study of atmospheric CO2
variability in space and time. After removing individual
components of
d13C
originating from climatic factors (temperature and
precipitation) CO2 emission was estimated, but only
in terms of quality. |
Tree ring
investigation of alder posts from the foundations of the Vilnius
royal palace
Rûtilë Pukienë
Vytautas Magnus University
Faculty of Natural Sciences ERC Dendroclimatology and
Radiometrics Group
Þ.E.Þilibero 6, Kaunas,
LT-46324 Kaunas,
Lithuania;
e-mail:
r.pukiene@gmf.vdu.lt
The cultural layer of the
Vilnius Lower Castle territory has been accumulating at least
since the end of the 13th century. It is rich with
remnants of different wooden constructions. For centuries the
main tree species used in wooden constructions (houses,
pavements, wooden frameworks under masonry constructions, etc.)
was pine (Pinus sylvestris L.). But there was a period in
the territory development when black alder (Alnus glutinosa
Gaertn.) timbers were used in large amounts. Investigation of
wooden frameworks from under building basements has revealed
that alder timbers were used for some phases of the Royal
Palace, the palace premises and the wall north of the palace
construction.
Four groups of alder logs from
different constructions were dendrochronologicaly analysed. All
logs were with bark. Less than 60 years old trees were used for
posts and frameworks in C basement in SE wing of the palace and
for posts under the wall north of the palace. Together with
younger than 50 years old trees, alders of 70-100 years old were
used for W basement in NE wing of the Palace and the third
premise. The oldest tree had 106 annual rings.
Relative cross-dating of ring
width series of alder logs has demonstrated that W basement of
the Palace and the third premise were built almost contemporary.
The trees for W basement were felled in winter of relative 91/92
year – May of 92 year. The trees for the third premise
foundation were felled in the autumn – winter of relative 92 /
93 year. A floating 106 years long alder chronology, relatively
dated -13 to 92, was constructed using tree ring series of these
two groups.
The alder logs for the
foundation of the wall north of the palace were felled two years
later than the logs for C basement in SE wing of the Palace.
Cross-dated ring width series of these two groups were the basis
to build a 54 years long chronology. The chronology shows the
best agreement with the former 106 years long chronology in a
relative position 8 to 63. |
Reconstruction of
geomorphic processes using anatomical variations of exposed
roots (Fagus sylvatica)
Sahling, I.
1,
Gärtner, H.
2 & K.-H.
Schmidt1
1
Martin-Luther-University
Halle-Wittenberg, Institute of Geosciences,
Von-Seckendorff-Platz 4, 06120 Halle, Germany; E-mail:
ingo.sahling@geo.uni-halle.de ;
karl-heinz.schmidt@geo.uni-halle.de
2
Swiss Federal Research Institute
WSL, Züricherstrasse 111, 8903 Birmensdorf, Switzerland; E-Mail:
holger.gaertner@wsl.ch
The theses presented focuses
on the determination and verification of wood anatomical changes
in annual growth rings of beech (Fagus sylvatica L.)
roots due to exposure. Further, the new findings are applied to
date and reconstruct the initial phase of massive block
displacements (opening of tension cracks) along the
Wellenkalk-cuesta scarp (Wellenkalk-Schichtstufe) in the
southern Thuringia Basin, Germany.
For the first time
determination of specific anatomical features related to
exposure in roots of hardwoods, 21 roots of 10 Fagus
sylvatica L. trees and -as a control- 13 roots of 5 Pinus
sylvestris L. trees were artificially exposed in two test
areas: Area 1 within the vegetation period 2003 and area 2
before the beginning of the vegetation period 2004. 154 samples
were taken in December 2004 (area 1) and November 2005 (area 2)
for further wood anatomical analysis.
Microscopic analysis confirmed
that all roots did show distinct wood anatomical changes related
to exposure and these changes occurred simultaneously in beech
and pine roots. Amongst other changes described in detail in the
results chapter, the persistent size reduction of vessels of
more than 35% in roots of beech was determined as the specific
anatomical feature indicating the first time of exposure.
Moreover, sudden exposure resulting in an immediate vessel size
reduction can be differentiated from continuously exposed roots,
where vessel sizes decrease continuously over longer time
periods.
For the application of these
results, 180 discs of 50 roots (33 trees) were sampled and
detailed geomorphic mappings were conducted at 19 sites showing
tension cracks along the cuesta scarp. In addition, cores were
taken from the stems of these trees for complementary
dendrogeomorphological analysis and 74 trees were cored to
establish three local reference chronologies as a control.
As a result, (i) the initial
phases of block displacements at the different sites were
determined by dating the year of tension crack opening and (ii)
antecedent movements prior to the openings were reconstructed by
analyzing growth reactions in the stems of the adjacent trees.
Finally, comparing the
reconstructed phases of the geomorphic processes with
precipitation data available for the region, showed a definite
relation between the opening of tension cracks and extreme
precipitation events. |
Suess effect in Poland, Central Europe,on
the basis of radiocarbon investigations in tree rings
Barbara Sensuùa, Anna
Pazdur
Silesian University of
Technology, Institute of Physics, Department of Radioisotopes,
GADAM Centre of Excellence, Krzywoustego 2, 44-100 Gliwice,
Poland
e-mail:
Barbara.Sensula@polsl.pl
This is a summary of the
research results on Suess effect in Poland (Central Europe).
The volatility of radiocarbon
concentration in tree rings is an useful tool for the analysis
of climate and antrophogenic changes over the last 150 years.
Dendrological research gives a chance to detect these changes
with a high resolution.
The tree ring samples were
collected from an industrial area (Ruda Slaska, Cracow, Chorzow)
and the ecologically clean regions (Augustow and Niepolomice
Forest). In this research, we used wholewood and alpha
cellulose. Radiocarbon measurements were performed using the
liquid scintilation counter (LSC) in the Gliwice Radiocarbon
Laboratory, Poland and accelerator mass spectrometer (AMS) in
Nagoya University, Japan.
Since about 1955, nuclear
tests have added considerable amounts of 14C to the atmosphere.
Increasing of mining and combustion of fossil fuels like coal,
petroleum, natural gas in the industrial area caused emission of
carbon dioxide to the atmosphere and changes of carbon isotopic
composition in the atmosphere and other carbon reservoirs. First
investigation of contemporary tree samples by Suess showed that
their radiocarbon activity was lower than in samples from the
middle of the 19th century. The Suess effect has a global
character that is the consequence of air masses mixing in the
atmosphere and it is reflected in annual tree rings. |
Reaction of larch
trees from eastern taimyr to climatic changes caused by major
volcanic eruptions during the last 2 millenniums by tree-ring
and isotope data
Olga V. Sidorova,
1Tatjana Boettger, Eugene A. Vaganov, Mukhtar M.
Naurzbaev
V.N. Sukachev Institute of
Forest SB RAS, Russia
1UFZ
- Helmholtz Center for Environmental Research, Germany
E-mail:
ovsidorova@forest.akadem.ru
We analyzed reaction of larch
trees (Larix gmelinii Rupr) growing in the Eastern Taymir
[72N-102E] to extreme climatic changes after major volcanic
eruptions in the relevant periods based on dendrochronological
and isotope (d13C,
d18O)
data.
The annually isotope data sets
for wood cellulose of always four individually analyzed trees
for the Eastern Taimyr were obtained at the first time for the
special periods A.D. 516-560, 1243-1286 and 1614-1654. The
chosen time periods correspond to historically known major
(global) volcanic eruptions events. All four analyzed trees for
each period have a good agreement and synchronism between each
other for both isotopic characteristics (R=0.7; p<0.05). We
revealed that the
d13C
and the d18O
of cellulose as well as tree-ring width clear fixed reaction of
trees on thermal regime for all investigated periods. However
stable isotopes give us supplementary information about moisture
regime which fixed in
d18O
of cellulose for the periods from AD 516-560 and AD 1614-1654.
We established that period from AD 516-560 shows differences
with other periods in isotope ratios as for carbon as well as
for oxygen up to 0.5 ‰. For all analyzed time periods were
revealed high statistical relationships between
d13C
and d18O
of cellulose (up to 0.6-0.7). Comparison analysis between all
periods shows highest correlation relationships between
June-July air temperature reconstruction and isotopic data (d13C,
d18O)
for the period from the AD 516-560 (R=0.62; p<0.05 and R=0.42;
p<0.05 correspondingly). |
Sapwood Estimates
of Common Oak (Quercus robur L.) in Estonia
Kristina Sohar and
Alar Läänelaid
Institute of Geography,
University of Tartu, Estonia
e-mail:
kriss8@ut.ee
Common oak (Quercus robur
L.) is one of the most investigated woods in dendrochronology in
Europe. However, oak is a problematic object to date, as its
sapwood is often removed by woodworking and decay in
archaeological samples. Oak sapwood rings may also be
uncountable because of woodworm damage (Hillam et al.
1987). Number of sapwood rings is necessary for precise dating,
as the last sapwood ring indicates the felling date. Thus the
number of sapwood rings in living trees is examined to estimate
the missing sapwood rings on dating objects. This method has
been widely used in Europe. However, so far no such studies have
been implemented in Estonia, except K. Sohar (2006).
In this research a total of 75
oak samples from Estonia was examined. The statistical analysis
gave 3-22 sapwood rings (if sapwood was distinguished from
heartwood by absence of tyloses in earlywood vessels) and 6-21
sapwood rings (if sapwood was distinguished by colour), both
within 95% confidence limits. Comparing these results with
earlier studies, the general European trend of decreasing
sapwood ring number towards the East (Hillam et al. 1987)
was confirmed.
There was no good correlation
found between the number of sapwood rings and heartwood
characteristics studied to estimate missing sapwood. The largest
amount of variability of sapwood number is described by average
ring width of heartwood - 30%, if sapwood was distinguished by
colour; and 17%, if sapwood was distinguished by the absence of
tyloses.
The results of this research
will help to improve the precision of dating Estonian oak
objects. Further researches of sapwood of common oak should be
expanded also to Latvia and Lithuania. The investigation is
needed to explain the distribution of historical Estonian oak
timber in Europe.
References:
Hillam, J., Morgan, R. A.,
Tyers, I., 1987. Sapwood Estimates and the Dating of Short Ring
Sequences. In: R. G. W. Ward (Editor), Applications of tree-ring
studies: current research in dendrochronology and related
subjects. British Archaeological Reports International Series,
Oxford, pp.165-185.
Sohar, K., 2006. Eesti
hariliku tamme (Quercus robur L.) maltspuidu varieeruvus
ja kasutamise võimalused dendrokronoloogias. BSc Thesis,
Institute of Geography, University of Tartu, pp. 40. |
Fluorescence
microscopy utilization for lignin detection in wooden cell wall
in spruce
Hanuð Vavrèík1,
Vladimír Gryc1, Michal Rybníèek1
1
Mendel
University of Agriculture and Forestry Brno, Faculty of Forestry
and Wood Technology, Department of Wood Science, Zemědělská 3,
613 00 Brno, Czech Republic
e-mail:
vavrcik@mendelu.cz
A method of lignin detection
in cell walls of xylem of differentiating tree-ring in Norway
spruce was developed. This method is based on autofluorescence
of lignin as determined by reflected fluorescent microscopy.
Autofluorescence of lignin was observed at 340–380 nm wavelength
of excitation radiation as blue fluorescent light and at 510–560
nm wavelength of excitation radiation as red fluorescent light.
There was no emission of the fluorescent light observed at
450–490 nm wavelength. Software for image analysis was used to
combine (logical sum) the fluorescent picture with the common
light picture.
This method is also useful for
observation of microscopic wood structure of non microscopic
piece of wood, i.e. making of microscopic slices of wood sample
is not required.
The project was financially
supported by the research plan of LDF MZLU in Brno, MSM
6215648902. |
Linking tree-rings
and ecosystem research
Pascale Weber
Swiss Federal Institute for
Forest, Snow and Landscape Research, WSL, CH-8903 Birmensdorf,
Switzerland
e-mail:
pascale.weber@wsl.ch
Tree-rings have been widely
used as proxies for reconstructing climate, stand dynamics,
forest fires and insect calamities. However, not many studies
have dealt with tree-rings as proxies for ecosystem research
with regard to patterns and processes of nutrient cycling and
interactions between trees and soil. Trees integrate information
from their local up to their global environment. Consequently,
they also contain information about soil formation and soil
biological and physico-chemical properties of the forest
ecosystem, which they belong to. However, relationships between
soil processes and radial growth in trees have rarely been
studied so far. The aim of this contribution is to highlight the
potential of linking tree-rings and ecosystem research from a
general point of view. More specific, potential research
questions in this new field are illustrated by two case studies,
one on Scots pine forests in Scotland and the other one on beech
forests in Switzerland. |
Changing climate
sensitivity in northern forests – problem, challenge or not
important?
Martin Wilmking,
Yongxiang Zhang, Jayendra Singh, Glenn Juday, Rosanne D’Arrigo
Institute for Botany and
Landscape Ecology, University Greifswald, Grimmer Strasse 88,
17487 Greifswald, Germany
e-mail:
wilmking@uni-greifswald.de
Dendroclimatological research
is often based on the assumption that the relationship between
tree growth and climate is not variable over time. This
assumption, however, has been challenged recently. Here, we
explore how climate sensitivity of trees growing in northern
forests of Alaska, Canada, Russia and high altitude forest of
Asia has changed over time and what effects this might have for
climatic reconstruction. In our study, most trees have increased
their climate sensitivity in the latter part of the 20th
century, and in several cases former positive relationships with
climate variables have become negative or vice versa.
Common drivers of this change
in sensitivity include stress related features, threshold
effects, or simply methodological issues of analysis. |
Dendroclimatology
in Scotland: the potential for a 1000-year climate
reconstruction
Ewan Woodley
University of Wales Swansea,
Singleton Park, SA2 8PP Swansea, United Kingdom
e-mail:
292870@swan.ac.uk
Ring-width, density and stable
isotope data from tree rings have been utilised in a number of
Scottish climatic reconstructions. However, past land-use
practices and the local maritime climate severely limit the
preservation of suitable sample material in situ making
construction of long (multi-centennial to millennial length)
tree-ring chronologies a challenging task. Pinus sylvestris
L. from ancient pinewoods in north-west Scotland may represent
an archive of climate sensitive material, yet this approach is
reliant on the location and sampling of suitable standing
deadwood, submerged wood or building timbers for chronological
extension beyond the range of living specimens. This poster
presents preliminary results from an initial field campaign to
assess the dendroclimatic potential of this region. |
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