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Sedimentary and carbonate preservation of ODP Sites 1262, 1263 and 1266

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https://b2find.eudat.eu/dataset/f8cd9deb-2187-56e5-a77d-5a5536dbca10
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Rapid carbon input into the ocean-atmosphere system caused a dramatic shoaling of the lysocline during the Paleocene-Eocene thermal maximum (PETM), a transient (~170 kyr) global...
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