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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},
}