Last glacial–Holocene water structure in the southwestern Okhotsk Sea inferred from radiolarian assemblages
In order to reconstruct paleoceanographic conditions in the southwestern (SW) Okhotsk Sea, radiolarian assemblages were analyzed from 10 surface sediments and 5 sediment cores obtained from various water depths, ranging between 461 and 1348 m. We also measured geochemical components such as biogenic...
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Veröffentlicht in: | Marine micropaleontology 2008-05, Vol.67 (3), p.191-215 |
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Sprache: | eng |
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