The DOI matches its Crossref record; 22 of the 22 references it cites were found in a registry or an index.
Pore Fluid Constraints on the Temperature and Oxygen Isotopic Composition of the Glacial Ocean
Abstract
Pore fluids from the upper 60 meters of sediment 3000 meters below the surface of the tropical Atlantic indicate that the oxygen isotopic composition (δ 18 O) of seawater at this site during the last glacial maximum was 0.8 ± 0.1 per mil higher than it is today. Combined with the δ 18 O change in benthic foraminifera from this region, the elevated ratio indicates that the temperature of deep water in the tropical Atlantic Ocean was 4°C colder during the last glacial maximum. Extrapolation from this site to a global average suggests that the ice volume contribution to the change in δ 18 O of foraminifera is 1.0 per mil, which partially reconciles the foraminiferal oxygen isotope record of tropical sea surface temperatures with estimates from Barbados corals and terrestrial climate proxies.
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Cites
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Cited by
Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present
Zachos, J., Pagani, M., Sloan, L., Thomas, E., & Billups, K. (2001) · Science · doi:10.1126/science.1059412 · Cited by 10,458
Clark, P. U., Dyke, A. S., Shakun, J. D., Carlson, A. E., Clark, J., Wohlfarth, B., Mitrovica, J. X., Hostetler, S. W., & McCabe, A. M. (2009) · Science · doi:10.1126/science.1172873 · Cited by 3,277
Sea level change through the last glacial cycle
Lambeck, K., & Chappell, J. (2001) · Science · doi:10.1126/science.1059549 · Cited by 1,619
Clark, P. U., Archer, D., Pollard, D., Blum, J. D., Rial, J. A., Brovkin, V., Mix, A. C., Pisias, N. G., & Roy, M. (2006) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2006.07.008 · Cited by 1,239
Shackleton, N. J. (2000) · Science · doi:10.1126/science.289.5486.1897 · Cited by 1,068
Metadata
- Authors
- Schrag, D. P., Hampt, G., & Murray, D. W.
- Venue
- Science
- Published
- 1996-06-28
- Volume
- 272
- Issue
- 5270
- Pages
- 1930-1932
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W1992470362
- Cited by
- 469
- References
- 22
- FWCI
- 12.77
- Type
- journal article
- Language
- en
- Open access
- closed
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- Schrag, D. P., Hampt, G., & Murray, D. W. (1996). Pore Fluid Constraints on the Temperature and Oxygen Isotopic Composition of the Glacial Ocean. Science. https://doi.org/10.1126/science.272.5270.1930
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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