(Q59099218)

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Silicon-isotope composition of diatoms as an indicator of past oceanic change

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Silicon-isotope composition of diatoms as an indicator of past oceanic change (English)

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C. L. De La Rocha

1

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M. A. Brzezinski

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2

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M. J. DeNiro

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3

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A. Shemesh

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4

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language of work or name

English

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publication date

October 1998

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published in

Nature

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volume

395

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issue

6703

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page(s)

680-683

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exact match

https://scigraph.springernature.com/pub.10.1038/27174

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cites work

Evidence for lower productivity in the Antarctic Ocean during the last glaciation

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Increased biological productivity and export production in the glacial Southern Ocean

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Purification, recovery, and laser-driven fluorination of silicon from dissolved and particulate silica for the measurement of natural stable isotope abundances

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Isotopic evidence for reduced productivity in the glacial southern ocean

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Meltwater input to the southern ocean during the last glacial maximum

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The silica balance in the world ocean: a reestimate.

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Contribution of Southern Ocean surface-water stratification to low atmospheric CO2 concentrations during the last glacial period

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Iron-limited diatom growth and Si:N uptake ratios in a coastal upwelling regime

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21 January 2018

Influence of iron availability on nutrient consumption ratio of diatoms in oceanic waters

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On Conditions for the Vernal Blooming of Phytoplankton

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Reconstruction of the Atlantic and Western Indian Ocean Sectors of the 18,000 B.P. Antarctic Ocean

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inferred from DOI database lookup

Origin of Diatom Ooze Belt in the Southern Ocean: Implications for Late Quaternary Paleoceanography

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DOI

10.1038/27174

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Dimensions Publication ID

1033506740

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(Q59099218)

Silicon-isotope composition of diatoms as an indicator of past oceanic change

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