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Reconstructing climate change and ombrotrophic bog development during the last 4000years in northern Poland using biotic proxies, stable isotopes and trait-based approach

Authors :
Mariusz Gałka
Norbert Kühl
Mariusz Lamentowicz
Vincent E. J. Jassey
Milena Obremska
Łukasz Lamentowicz
Andreas Lücke
Department of Biogeography and Paleoecology
Adam Mickiewicz University in Poznań (UAM)
Swiss Federal Institute for Forest, Snow and Landscape Research WSL
Source :
Palaeogeography, Palaeoclimatology, Palaeoecology, Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2015, 418, pp.261-277. ⟨10.1016/j.palaeo.2014.11.015⟩
Publication Year :
2015
Publisher :
Elsevier BV, 2015.

Abstract

article i nfo 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 reconstruc- tions), stable carbon isotopes ( 13 C), 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 re- gional 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 re- latedtospecifictraitsoftestateamoebae,whichinturnreflectedthewatertablechangesoverthelast4000years. Kusowskie Bagno recorded at least the following wet shifts: AD 250, 550, 850, 1250 and 1700, while wet condi- tions 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,northernBritainandthe7500-yearrecordfromthe Stązkibog,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.

Details

ISSN :
00310182
Volume :
418
Database :
OpenAIRE
Journal :
Palaeogeography, Palaeoclimatology, Palaeoecology
Accession number :
edsair.doi.dedup.....ec4f3168d8403208f50a4adc4bc00bc0
Full Text :
https://doi.org/10.1016/j.palaeo.2014.11.015