Millennial paleoclimate variations on the Central Tibetan Plateau during MIS4-MIS2 inferred from a sediment core based RPI chronology

Millennial paleoclimate variations on the Central Tibetan Plateau during MIS4-MIS2 inferred from a sediment core based RPI chronology

Abstract Lakes on the Tibetan Plateau, highly sensitive to environmental changes, play a key role in paleoclimatic studies. However, dating limitations often constrain investigations to periods before the Last Glacial Maximum (LGM). Relative paleointensity (RPI) of lake sediments offers a valuable m...

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Bibliographic Details
Main Authors: Yang Zhang, Junbo Wang, Shuangwen Yi, Siwei Yu, Jinlei Kai, Yao Gu, Qingfeng Ma, Jianting Ju, Liping Zhu
Format: Article
Language:English
Published: Nature Portfolio 2025-05-01
Series:Scientific Reports
Subjects:
Lacustrine sediments
Nam Co
Relative paleointensity
Age model
Environmental magnetic parameters
Tibetan Plateau
Online Access:https://doi.org/10.1038/s41598-025-03315-x
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https://doi.org/10.1038/s41598-025-03315-x

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