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| The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum | 172 |
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| The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum | 19 | 14 | 0 | 14 | 14 | 3 | 1 |
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| s43247-022-00451-4.pdf | 83 |
