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

Sanyal, A., Hemming, N. G., Broecker, W. S., Lea, David W., Spero, Howard J., Hanson, Gilbert N.·1996·Paleoceanography

Abstract

Culture experiments were carried out with the species Orbulina universa at four different p H values (7.70±0.05, 8.15±0.05, 8.60±0.05, and 9.00±0.10) in order to establish the p H‐dependence of boron isotope fractionation between seawater and foraminifera. A clear relationship between the boron isotopic composition of the foraminifera and the p H of the seawater culture solutions was found, showing heavier boron isotopic composition at higher p H. This finding supports the viability of boron isotopes as a paleo‐p H tool. It is important to note that Orbulina universa cultured in natural seawater, as well as those obtained from coretop samples, have a significantly lighter boron isotopic ratio than Globigerinoides sacculifer from coretop samples, suggesting that at least for this species, a vital effect is active.

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Metadata

Authors
Sanyal, A., Hemming, N. G., Broecker, W. S., Lea, D. W., Spero, H. J., & Hanson, G. N.
Venue
Paleoceanography
Published
1996-10
Volume
11
Issue
5
Pages
513-517
ISSN
  • 0883-8305 (ISSN-L)
  • 1944-9186
OpenAlex
W2109836886
Cited by
224
References
0
FWCI
3.05
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Oceanic p H control on the boron isotopic composition of foraminifera: Evidence from culture experiments. https://app.cochat.ai/papers/10.1029/96pa01858
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Sanyal, A., Hemming, N. G., Broecker, W. S., Lea, D. W., Spero, H. J., & Hanson, G. N. (1996). Oceanic p H control on the boron isotopic composition of foraminifera: Evidence from culture experiments. Paleoceanography. https://doi.org/10.1029/96pa01858

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