Abrupt sand-dune accumulation at the northeastern margin of the Tibetan Plateau challenges the wet MIS3a inferred from numerous lake-highstands View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2016-09

AUTHORS

Hao Long, Markus Fuchs, Linhai Yang, Hongyi Cheng

ABSTRACT

Over the Tibetan Plateau and adjacent regions, numerous (14)C-based lake records revealed a ubiquitous wet climatic period during 40-25 ka (late MIS 3), which is in contradiction with the global pattern of generally cold and dry climates. This paper focuses on OSL dating results of a large set of sand dunes and alluvial sediments (50 OSL ages) from the Qinwangchuan (QWC) Basin at the northeast edge of the Tibetan Plateau, with the aim to test the validity of the anomalous wet condition for the late MIS 3 interval, evidenced by numerous lake highstands. The abrupt sand dune accumulation as indication of increased aridity in the study area was OSL dated to ~40-13 ka. This dry climatic inference of the sand dune system from QWC apparently shows no wet MIS 3a event. Thus, the anomalous wet conditions revealed by high lake levels for the late MIS 3 phase may not be a universal phenomena across entire western China. More... »

PAGES

25820

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/srep25820

DOI

http://dx.doi.org/10.1038/srep25820

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1007264501

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/27172907


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This table displays all metadata directly associated to this object as RDF triples.

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