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Insights into a remote cryosphere: A multi-method approach to assess permafrost occurrence at the Qugaqie basin, western Nyainqêntanglha Range, Tibetan Plateau [期刊论文]
Cryosphere, 2021-01-01, 15 (1
Buckel J.;  Reinosch E.;  Hördt A.;  Zhang F.;  Riedel B.;  Gerke M.;  Schwalb A.;  Mäusbacher R.
View/Download:21/0
 
Climate variability in the past ∼19,000 yr in NE Tibetan Plateau inferred from biomarker and stable isotope records of Lake Donggi Cona [期刊论文]
Quaternary Science Reviews, 2017-01-01, 157
Saini J.;  Günther F.;  Aichner B.;  Mischke S.;  Herzschuh U.;  Zhang C.;  Mäusbacher R.;  Gleixner G.
View/Download:32/0
 
Sea level and climate change at the southern Cape coast, South Africa, during the past 4.2 kyr [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2016-01-01, 446
Wündsch M.;  Haberzettl T.;  Kirsten K.L.;  Kasper T.;  Zabel M.;  Dietze E.;  Baade J.;  Daut G.;  Meschner S.;  Meadows M.E.;  Mäusbacher R.
View/Download:28/0
 
Quaternary ecological responses and impacts of the Indian Ocean Summer Monsoon at Nam Co, Southern Tibetan Plateau [期刊论文]
Quaternary Science Reviews, 2015-01-01, 112
Günther F.;  Witt R.;  Schouten S.;  Mäusbacher R.;  Daut G.;  Zhu L.;  Xu B.;  Yao T.;  Gleixner G.
View/Download:30/0
 
Trace element variability in single ostracod valves as a proxy for hydrochemical change in Nam Co, central Tibet, during the Holocene [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2014-01-01, 399
Yang Q.;  Jochum K.P.;  Stoll B.;  Weis U.;  Börner N.;  Schwalb A.;  Frenzel P.;  Scholz D.;  Doberschütz S.;  Haberzettl T.;  Gleixner G.;  Mäusbacher R.;  Zhu L.;  Andreae M.O.
View/Download:39/0
 
Interplay between redox conditions and hydrological changes in sediments from Lake Nam Co (Tibetan Plateau) during the past 4000cal BP inferred from geochemical and micropaleontological analyses [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2013-01-01, 392
Kasper T.;  Frenzel P.;  Haberzettl T.;  Schwarz A.;  Daut G.;  Meschner S.;  Wang J.;  Zhu L.;  Mäusbacher R.
View/Download:28/0
 

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