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Ecological development of Lake Donggi Cona, north-eastern Tibetan Plateau, since the late glacial on basis of organic geochemical proxies and non-pollen palynomorphs

Authors

Aichner,  B.
External Organizations;

Herzschuh,  U.
External Organizations;

/persons/resource/wilkes

Wilkes,  Heinz
4.3 Organic Geochemistry, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/schulzhm

Schulz,  Hans-Martin
4.3 Organic Geochemistry, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Wang,  Y.
External Organizations;

/persons/resource/birgit

Plessen,  Birgit
5.2 Climate Dynamics and Landscape Evolution, 5.0 Earth Surface Processes, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Mischke,  S.
External Organizations;

Diekmann,  B.
External Organizations;

Zhang,  C.
External Organizations;

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Citation

Aichner, B., Herzschuh, U., Wilkes, H., Schulz, H.-M., Wang, Y., Plessen, B., Mischke, S., Diekmann, B., Zhang, C. (2012): Ecological development of Lake Donggi Cona, north-eastern Tibetan Plateau, since the late glacial on basis of organic geochemical proxies and non-pollen palynomorphs. - Palaeogeography Palaeoclimatology Palaeoecology, 313-314, 140-149.
https://doi.org/10.1016/j.palaeo.2011.10.015


https://gfzpublic.gfz-potsdam.de/pubman/item/item_244117
Abstract
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