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Planktonic foraminiferal assemblages in sediment core KC01B

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PANGAEA2024-03-11 收录
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https://doi.pangaea.de/10.1594/PANGAEA.856737
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Planktonic foraminiferal assemblages were studied at high-resolution in core KC01B from the Ionian Sea. Quantitative analysis allowed us to distinguish the main climatic features and associated paleoceanographic changes, that occurred between Marine Isotopic Stages (MIS) 13 and 9 (~500-300 ka).
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