Differential proxy responses to late Allerød and early Younger Dryas climatic change recorded in varved sediments of the Trzechowskie palaeolake in Northern Poland
Research was funded by the National Science Centre grants No. NN306085037, NN306034040 and partly funded by No. 2015/17/B/ST10/03430. This study is a contribution to the Virtual Institute of Integrated Climate and Landscape Evolution (ICLEA) of the Helmholtz Association (http://www.iclea.de/en/home/) and Science and Research Funds for 2015-2016, allocated to a co-financed international project (No. 3500/ICLEA/15/2016/0). It is a contribution to the climate initiative REKLIM Topic 8 ‘Abrupt climate change derived from proxy data’ of the Helmholtz Association. We thank Sebastian Tyszkowski for invaluable help during the field work.
Department of Environmental Resources and Geohazards, Institute of Geography, Polish Academy of Sciences, Warszawa, Poland; GFZ German Research Centre for Geosciences, Section 5.2 – Climate Dynamics and Landscape Evolution, Telegrafenberg C, Potsdam, Germany; Department of Geoecology and Climatology, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Warszawa, Poland; Institute of Archaeology, Nicolaus Copernicus University in Toruń, Poland; Institute of Geology, Adam Mickiewicz University, Poznań, Poland; Institute Geoecology and Geoinformation, Department of Geology and Quaternary Paleogeography, Adam Mickiewicz University, Poznań, Poland; GADAM Centre of Excellence, Department of Radioisotopes, Institute of Physics – CSE, Silesian University of Technology, Gliwice, Poland; Senckenberg Research Institute and Natural History Museum, BIK-F, TSP6 Evolution and Climate, Senckenberganlage 25, Frankfurt a.M., Germany; Heidelberg University, Institute of Earth Sciences, Im Neuenheimer Feld 234, Heidelberg, Germany; Department of Ecology, University of Silesia, Katowice, Poland
Recommended Citation:
Słowiński M.,Zawiska I.,Ott F.,et al. Differential proxy responses to late Allerød and early Younger Dryas climatic change recorded in varved sediments of the Trzechowskie palaeolake in Northern Poland[J]. Quaternary Science Reviews,2017-01-01,158