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| The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum | 192 |
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| The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum | 14 | 0 | 14 | 14 | 3 | 9 | 12 |
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| s43247-022-00451-4.pdf | 111 |
