The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum
oleh: 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 |
|---|---|
| Diterbitkan: | Nature Portfolio 2022-05-01 |
Deskripsi
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.