(Q59067848)

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Chlorin accumulation rate as a proxy for Quaternary marine primary productivity

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Chlorin accumulation rate as a proxy for Quaternary marine primary productivity (English)

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A. Rosell-Melé

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Ralf Tiedemann

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R. Tiedemann

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4

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P. G. Harris

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1

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M. Zhao

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2

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M. Sarnthein

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J. R. Maxwell

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English

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publication date

September 1996

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Nature

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383

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6595

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63-65

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https://scigraph.springernature.com/pub.10.1038/383063a0

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Younger Dryas-Style Cooling Events at Glacial Terminations I-VI at ODP Site 658: Associated benthic δ13C anomalies constrain meltwater hypothesis

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Molecular record of secular sea surface temperature changes on 100-year timescales for glacial terminations I, II and IV

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Comparison of two U37K-sea surface temperature records for the last climatic cycle at ODP Site 658 from the sub-tropical Northeast Atlantic

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Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years

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Importance of continental margins in the marine biogeochemical cycling of carbon and nitrogen

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Astronomical solutions for paleoclimate studies over the last 3 million years

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7 January 2021

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Molecular stratigraphy of cores off northwest Africa: Sea surface temperature history over the last 80 Ka

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10.1038/383063A0

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1039102073

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(Q59067848)

Chlorin accumulation rate as a proxy for Quaternary marine primary productivity

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