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Abundance of planktonic foraminifera from IODP Hole 339-U1386C

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B2FIND2026-03-21 收录
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https://b2find.eudat.eu/dataset/1daa5ade-662d-547f-9961-5424b8bc8e18
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The base of the Faro contouritic drift (IODP Site U1386) on the northern margin of the Gulf of Cádiz (Algarve margin) is characterized by two sequences of frequent gravity...
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