【作者】Georg Miehe[a,∗]，Shabeh ul Hasson[b]，Bruno Glaser[c]，Steffen Mischke[d]，Jürgen Böhner[b]，Willem O. van der Knaap[e]，Jacqueline F.N. van Leeuwen[e]，La Duo[f]，Sabine Miehe[g]，Torsten Haberzettl[h]
【作者单位】[a]Philipps Universität Marburg, Faculty of Geography, Deutschhausstrasse 10, D-35032, Marburg, Germany;[b]Universität Hamburg, Institute of Geography, Cluster of Excellence “Climate, Climatic Change, and Society” (CLICCS), 805A Geomatikum, Bundesstraße 55, D-20146, Hamburg, Germany;[c]Martin Luther Universität Halle-Wittenberg, Institute of Agricultural and Nutritional Sciences, Soil Biogeochemistry, von-Seckendorff-Platz 3, D-06120, Halle (Saale), Germany;[d]University of Iceland, Institute of Earth Sciences, Sturlugata 7, 102, Reykjavik, Iceland;[e]Institute of Plant Sciences and Oeschger-Centre for Climate Change Research, Altenbergrain 21, CH 3013, Bern, Switzerland;[f]School of Science, Tibet University, Jiangsu Road No 10, Lhasa, Tibet Autonomous Region, China;[g]Am Kohlbach 10, D-79199, Kirchzarten, Germany;[h]Universität Greifswald, Institute for Geography and Geology, Physical Geography, Friedrich-Ludwig-Jahn-Str. 16, D-17489, Greifswald, Germany
【年份】2021
【卷号】Vol.256 No.0
【页码】106817
【ISSN】0277-3791
【关键词】Qinghai-Tibet-Plateau Palynology Ostracods Black carbon Climate modelling Last Glacial Maximum Holocene Anthropocene Neolithisation
【摘要】 The lithology, ostracods, palynomorphs and black carbon of a sediment core from a saline wetland in the southern Tibetan highlands is analyzed and climate modelling applied with respect to core questions in Quaternary research: Do meso-climatic eff...
