(Q58309737)

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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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scholarly article

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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 (English)

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Andreas Mackensen

object named as

A. Mackensen

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author name string

H. -W. Hubberten

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T. Bickert

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G. Fischer

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D. K. Fütterer

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publication date

October 1993

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Paleoceanography

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8

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5

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587-610

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1 reference

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Carbon Isotope Fractionation in the System CO2(gas)—CO2(aqueous)—HCO3−(aqueous)

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A response by benthic Foraminifera to the deposition of phytodetritus in the deep sea

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A deep hydrological front between intermediate and deep-wafpr , masses in the glacial Indian Ocean

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West Atlantic abyssal circulation during the past 120,000 years

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Glacial to interglacial changes in ocean chemistry

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Responses by Benthic Organisms to Inputs of Organic Material to the Ocean Floor: A Review [and Discussion}

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Upper-level circulation in the South Atlantic Ocean

1 reference

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Temperature Dependence of Carbon Isotope Composition in Marine Plankton and Sediments

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Paleocirculation of the deep north atlantic: 150,000-year record of benthic foraminifera and oxygen-18

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1 reference

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based on heuristic

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Identifiers

10.1029/93PA01291

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