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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
- 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.
- Subjects :
- 010506 paleontology
geography
geography.geographical_feature_category
Peat
010504 meteorology & atmospheric sciences
Ecology
[SDE.MCG]Environmental Sciences/Global Changes
Paleontology
Ombrotrophic
Climate change
Macrofossil
Vegetation
15. Life on land
Oceanography
01 natural sciences
13. Climate action
Mire
14. Life underwater
Testate amoebae
Bog
ComputingMilieux_MISCELLANEOUS
Ecology, Evolution, Behavior and Systematics
Geology
0105 earth and related environmental sciences
Earth-Surface Processes
Subjects
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