The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum
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H. Tanyaş | G. Dupont‐Nivet | Zhaojie Guo | C. Fioroni | A. Rohrmann | J. Frieling | M. Kaya | S. Altıner | Ezgi Vardar | M. Mamtimin | Guo Zhaojie