Ground-truthing the boron isotope-paleo-pH proxy in planktonic foraminifera shells: Partial dissolution and shell size effects (Q58389644)

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scholarly article by Bärbel Hönisch & N. Gary Hemming published 3 November 2004 in Paleoceanography

Language	Label	Description	Also known as
English	Ground-truthing the boron isotope-paleo-pH proxy in planktonic foraminifera shells: Partial dissolution and shell size effects	scholarly article by Bärbel Hönisch & N. Gary Hemming published 3 November 2004 in Paleoceanography

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scholarly article

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Ground-truthing the boron isotope-paleo-pH proxy in planktonic foraminifera shells: Partial dissolution and shell size effects (English)

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Bärbel Hönisch

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Bärbel Hönisch

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author name string

N. Gary Hemming

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publication date

3 November 2004

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Paleoceanography

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19

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4

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Population dynamics of the planktic foraminifer Globigerinoides sacculifer (Brady) from the central Red Sea

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Boron isotopic composition and concentration in modern marine carbonates

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The influence of symbiont photosynthesis on the boron isotopic composition of foraminifera shells

1 reference

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Assessing scleractinian corals as recorders for paleo-pH: Empirical calibration and vital effects

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A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolution

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Reconstructing past ocean pH-depth profiles

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Atmospheric carbon dioxide concentrations over the past 60 million years

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Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

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Vital effects in foraminifera do not compromise the use of δ11B as a paleo-pH indicator: Evidence from modeling

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Evidence for a higher pH in the glacial ocean from boron isotopes in foraminifera

1 reference

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Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: changes in deep ocean circulation and chemical inventories

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Microsensor studies of photosynthesis and respiration in the symbiotic foraminifer Orbulina universa

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Oceanic pH control on the boron isotopic composition of foraminifera: Evidence from culture experiments

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Changes in pH in the eastern equatorial Pacific across stage 5-6 boundary based on boron isotopes in foraminifera

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A comparative study of the northwest Africa and eastern equatorial Pacific upwelling zones as sources of CO2during glacial periods based on boron isotope paleo-pH estimation

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Identifiers

10.1029/2004PA001026

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