A quantitative method to infer lake area changes based on an extensive survey of lake surface sediment grain size across the Inner Mongolia Plateau, and its application to understanding the evolution of Lake Wulanhushao in northern China since 18.59 cal. kyr BP
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Published:2024-05
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ISSN:0031-0182
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Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
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