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@ARTICLE{Lamentowicz:203174,
author = {Lamentowicz, M. and Gałka, M. and Lamentowicz, Ł. and
Obremska, M. and Kühl, N. and Lücke, A. and Jassey, V. E.
J.},
title = {{R}econstructing climate change and ombrotrophic bog
development during the last 4000years in northern {P}oland
using biotic proxies, stable isotopes and trait-based
approach},
journal = {Palaeogeography, palaeoclimatology, palaeoecology},
volume = {418},
issn = {0031-0182},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2015-05179},
pages = {261 - 277},
year = {2015},
abstract = {In this study, we present a record spanning the last 4000
years from a Baltic bog (Kusowskie Bagno) in northern
Poland. Using numerous biotic and abiotic proxies, such as
testate amoebae (depth to water table reconstructions),
stable carbon isotopes (13C), plant macrofossils (proxies
for local vegetation and mire surface wetness), pollen and
spores (proxies for regional vegetation and human impact),
we reconstructed and identified the regional hydro-climatic
signal of Kusowskie Bagno bog and compared it to other bog
records around the Baltic Sea. Our aims were to: 1) combine
the species traits of bryophytes and testate amoebae, and
more common proxies (isotopes, plant micro-and
macro-remains) to infer past peatland development, 2)
compare the hydro-climatic signal of Kusowskie Bagno bog to
existing records around the Baltic Sea. We found that
Kusowskie Bagno bog was very wet during the last 4000 years,
and even drainage and peat exploitation had not disturbed
its hydrology in northern part in the last 200 years. Carbon
isotopes and plant macrofossils were significantly related
to specific traits of testate amoebae, which in turn
reflected the water table changes over the last 4000 years.
Kusowskie Bagno recorded at least the following wet shifts:
AD 250, 550, 850, 1250 and 1700, while wet conditions
occurred during the Migration period at ca AD 550.
Furthermore, the testate amoeba-based quantitative wetness
reconstruction in Kusowskie Bagno bog resembles the pattern
observed in other sites around the Baltic, i.e., Estonia,
Finland, Ireland, northern Britain and the 7500-year record
from the Stążki bog, northern Poland. Our results provided
statistically validated evidence that interactions between
plant and microbe need to be more considered further to
reconstruct past hydrological. This is the first study of
past hydro-climatic changes in peatlands based upon a
trait-based approach.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000349804100019},
doi = {10.1016/j.palaeo.2014.11.015},
url = {https://juser.fz-juelich.de/record/203174},
}