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

被引:102
作者
Lamentowicz, M. [1 ,2 ]
Galka, M. [2 ]
Lamentowicz, L. [3 ]
Obremska, M. [4 ]
Kuehl, N. [5 ]
Luecke, A. [6 ]
Jassey, V. E. J. [1 ,2 ,7 ,8 ]
机构
[1] Adam Mickiewicz Univ, Fac Geog & Geol Sci, Lab Wetland Ecol & Monitoring, PL-61680 Poznan, Poland
[2] Adam Mickiewicz Univ, Dept Biogeog & Paleoecol, PL-61680 Poznan, Poland
[3] Adam Mickiewicz Univ, Fac Biol, PL-61614 Poznan, Poland
[4] Polish Acad Sci, Inst Geol Sci, PL-00818 Warsaw, Poland
[5] Univ Bonn, Steinmann Inst Geol Mineral & Paleontol, D-53115 Bonn, Germany
[6] Forschungszentrum Julich, IBG Agrosphere 3, Inst Bio & Geosci, D-52425 Julich, Germany
[7] Ecole Polytech Fed Lausanne, Ecol Syst Lab ECOS, Sch Architecture Civil & Environm Engn ENAC, CH-1015 Lausanne, Switzerland
[8] Swiss Fed Inst Forest Snow & Landscape Res WSL, CH-1015 Lausanne, Switzerland
关键词
Multi-proxy; High-resolution; Peatland; Trait-based paleoecology; LAND-USE CHANGE; TESTATE-AMEBAS; LATE-HOLOCENE; MULTI-PROXY; RAISED BOG; BALTIC BOG; PEAT BOG; PALEOENVIRONMENTAL CHANGES; ERIOPHORUM-VAGINATUM; AUTOGENIC SUCCESSION;
D O I
10.1016/j.palaeo.2014.11.015
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
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 (C-13), 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 hydroclimatic 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 Stazki 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. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:261 / 277
页数:17
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