Evidence for glaciation predating MIS-6 in the eastern Nyainqêntanglha, southeastern Tibet
Southeastern Tibet is one of the most glaciated regions on the Tibetan Plateau both at present and during the Quaternary. Numerical dating of glacial deposits has allowed the establishment of a provisional chronology of Quaternary glacial fluctuations in this region, with the oldest glaciation (Guxiang Glaciation) occurring in marine oxygen isotope stage 6 (MIS-6). However, glaciations predating MIS-6 have been identified at many locations on the Tibetan Plateau and its surrounding mountains, posing the question: as a major glaciation center both at present and during the Quaternary, did a glaciation prior to MIS-6 ever occur in southeastern Tibet?
Zhou et al. (2021) provide evidence for a glacier advance in the Bodui Zangbo River ...















