Orbital - millennial environment and hydrology changes of the central Okhotsk Sea over the last 136 kyr inferred by micropaleontological (radiolarian and benthic foraminifera), geochemical and lithological proxies and mechanisms responsible for them

Published: 26 August 2020| Version 1 | DOI: 10.17632/gbr7tprkyd.1
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Description

Supplementary data for MS submitted to Quaternary Science Review

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Foraminifera, Origin of Organic Matter, Radiolaria

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