The DOI matches its Crossref record; 8 of the 8 references it cites were found in a registry or an index.
Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations
Abstract
Cultured planktonic foraminifera, Orbulina universa (symbiotic) and Globigerina bulloides (nonsymbiotic), are used to reexamine temperature:δ 18 O relationships at 15°–25°C. Relationships for both species can be described by linear equations. Equations for O. universa grown under low light (LL) and high light (HL) share a slope of −4.80 (0.21‰ °C−1) with a HL‐LL offset of −0.33‰ due to symbiont photosynthetic activity. The effect of [CO 32−] on O. universa is −0.002‰ µmol−1 kg−1 and is insensitive to temperature. For G. bulloides, ontogenetic effects produce size‐related trends in temperature:δ 18 O, whereby larger shells are enriched in 18 O relative to smaller specimens. The O. universa temperature:δ 18 O relationships are more accurate than previously published equations for describing plankton tow data. Our equations do not explain planktonic core top data with the same precision but provide a good fit to benthic Cibicidoides data below 10°C. Temperature:δ 18 O relationships for G. bulloides provide good agreement with field data for this species from the northeast Pacific.
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Cites
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O'Brien, C. L., Robinson, S. A., Pancost, R. D., Sinninghe Damsté, J. S., Schouten, S., Lunt, D. J., Alsenz, H., Bornemann, A., Bottini, C., Brassell, S. C., et al. (2017) · Earth-Science Reviews · doi:10.1016/j.earscirev.2017.07.012 · Cited by 586
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Metadata
- Authors
- Bemis, B. E., Spero, H. J., Bijma, J., & Lea, D. W.
- Venue
- Paleoceanography
- Publisher
- American Geophysical Union (AGU)
- Published
- 1998-04
- Volume
- 13
- Issue
- 2
- Pages
- 150-160
- ISSN
- 0883-8305 (ISSN-L)
- 1944-9186
- OpenAlex
- W1968988439
- Cited by
- 1,108
- References
- 8
- FWCI
- 11.09
- Type
- journal article
- Language
- en
- Open access
- closed
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- Bemis, B. E., Spero, H. J., Bijma, J., & Lea, D. W. (1998). Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations. Paleoceanography. https://doi.org/10.1029/98pa00070
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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