Asynchronicity of deglacial permafrost thawing controlled by millennial-scale climate variability

Abstract Permafrost is a potentially important source of deglacial carbon release alongside deep-sea carbon outgassing. However, limited proxies have restricted our understanding in circumarctic regions and the last deglaciation. Tibetan Plateau (TP), the Earth’s largest low-latitude and alpine perm...

Full description

Saved in:
Bibliographic Details
Main Authors: Xinwei Yan, Xu Zhang, Bo Liu, Huw T. Mithan, John Hellstrom, Sophie Nuber, Russell Drysdale, Junjie Wu, Fangyuan Lin, Ning Zhao, Yuao Zhang, Wengang Kang, Jianbao Liu
Format: Article
Language:English
Published: Nature Portfolio 2025-01-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-024-55184-z
Tags: Add Tag
No Tags, Be the first to tag this record!