The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum

The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum

The Eurasian Epicontinental Sea sequestered 720–1300 Gt of organic carbon during the Palaeocene-Eocene Thermal Maximum, according to a palaeogeographic reconstruction and multi-proxy data from a sedimentary sequence in the Tarim Basin, China.

Bibliographic Details
Main Authors: Mustafa Y. Kaya, Guillaume Dupont-Nivet, Joost Frieling, Chiara Fioroni, Alexander Rohrmann, Sevinç Özkan Altıner, Ezgi Vardar, Hakan Tanyaş, Mehmut Mamtimin, Guo Zhaojie
Format: Article
Language:English
Published: Nature Portfolio 2022-05-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-022-00451-4

Internet

https://doi.org/10.1038/s43247-022-00451-4

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