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Items where Author is "Mischke, Steffen"

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Number of items: 5.

Article

Article
Tian, F. , Herzschuh, U. , Dallmeyer, A. , Xu, Q. , Mischke, S. and Biskaborn, B. K. (2013)
Environmental variability in the monsoon–westerlies transition zone during the last 1200 years: lake sediment analyses from central Mongolia and supra–regional synthesis ,
Quaternary Science Reviews, 73 , pp. 31-47 .
doi:10.1016/j.quascirev.2013.05.005 , hdl:10013/epic.42367

Article
Opitz, S. , Ramisch, A. , Mischke, S. and Diekmann, B. (2013)
Holocene lake stages and thermokarst dynamics in a discontinuous permafrost affected region, north-eastern Tibetan Plateau. ,
Journal of Asian Earth Sciences, 76 , pp. 85-94 .
doi:10.1016/j.jseaes.2013.08.006 , hdl:10013/epic.42371

Article
Opitz, S. , Wünnemann, B. , Aichner, B. , Dietze, E. , Hartmann, K. , Herzschuh, U. , IJmker, J. , Lehmkuhl, F. , Li, S. , Mischke, S. , Plotzki, A. , Stauch, G. and Diekmann, B. (2012)
Late Glacial and Holocene development of Lake Donggi Cona, north-eastern Tibetan Plateau, inferred from sedimentological analysis ,
Palaeogeography Palaeoclimatology Palaeoecology, 337-33 , pp. 159-176 .
doi:10.1016/j.palaeo.2012.04.013 , hdl:10013/epic.39442

Article
Dietze, E. , Wünnemann, B. , Diekmann, B. , Aichner, B. , Hartmann, K. , Herzschuh, U. , IJmker, J. , Jin, H. , Kopsch, C. , Lehmkuhl, F. , Li, S. , Mischke, S. , Niessen, F. , Opitz, S. , Stauch, G. and Yang, S. (2010)
Basin Morphology and Seismic Stratigraphy of Lake Donggi Cona, north-eastern Tibetan Plateau, China ,
Quaternary International:, 218 , pp. 131-142 .
hdl:10013/epic.33916

Conference

Conference -Poster
Wang, Y. , Herzschuh, U. , Birks, H. J. B. , Mischke, S. , Böhner, J. , Lehmkuhl, F. , Diekmann, B. , Wünnemann, B. and Zhang, C. (2011)
Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the LGM extending the concept of pollen-source area to pollen-based climate reconstructions from large lakes ,
XVIII. INQUA Congress (21-27.07.2011, Bern Switzerland). .
hdl:10013/epic.37834

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