(Q105427106)

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Carbon isotopic disequilibrium in polar planktonic foraminifera and its impact on modern and Last Glacial Maximum reconstructions

scientific article published in February 2000

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Carbon isotopic disequilibrium in polar planktonic foraminifera and its impact on modern and Last Glacial Maximum reconstructions (English)

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J. Lynch-Stieglitz

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K. E. Kohfeld

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1

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R. F. Anderson

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2

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publication date

February 2000

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published in

Paleoceanography

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volume

15

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issue

1

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page(s)

53-64

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cites work

Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentration

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Vostok ice core provides 160,000-year record of atmospheric CO2

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Ocean chemistry during glacial time

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7 January 2021

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Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates

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Glacial-interglacial history of Antarctic Intermediate Water: Relative strengths of Antarctic versus Indian Ocean sources

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The influence of air-sea exchange on the isotopic composition of oceanic carbon: Observations and modeling

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The δ13C in benthic foraminiferal tests ofFontbotia wuellerstorfi(Schwager) Relative to the δ13C of dissolved inorganic carbon in Southern Ocean Deep Water: Implications for glacial ocean circulation models

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7 January 2021

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Deep-dwelling planktonic foraminifera of the northeastern Pacific Ocean reveal environmental control of oxygen and carbon isotopic disequilibria

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Particulate organic matter delta 13C variations across the Drake Passage.

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7 January 2021

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Variations in Atlantic surface ocean paleoceanography, 50°-80°N: A time-slice record of the last 30,000 years

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7 January 2021

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Isotopic evidence for reduced productivity in the glacial southern ocean

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7 January 2021

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Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes

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https://api.crossref.org/works/10.1029%2F1999PA900049

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7 January 2021

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An explanation of the effect of seawater carbonate concentration on foraminiferal oxygen isotopes

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10.1029/1999PA900049

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(Q105427106)

Carbon isotopic disequilibrium in polar planktonic foraminifera and its impact on modern and Last Glacial Maximum reconstructions

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