The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
Phase relationships between millennial‐scale events 64,000–24,000 years ago
Open accessAbstract
A core recovered on the Iberian margin off southern Portugal can be correlated with Greenland ice cores using oxygen isotope variability in planktonic foraminifera which closely matches the ice core records of temperature over Greenland. Our age model identifies the base of every interstadial between 64,000 and 24,000 years ago and uses the Greenland Ice Core Project (GRIP) timescale. The oxygen isotope signal in benthic foraminifera (on this GRIP‐based timescale) is quite different from the planktonic record and resembles the temperature record over Antarctica when this is synchronized with Greenland using the record of methane in the atmospheric air in the polar ice cores. We interpret the benthic record as indicating significant fluctuations in ice volume during millennial events, and we suggest that Antarctic temperature changed as a function of ice volume.
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Citations
Cites
Asynchrony of Antarctic and Greenland climate change during the last glacial period
Blunier, T., Chappellaz, J., Schwander, J., Dällenbach, A., Stauffer, B., Stocker, T. F., Raynaud, D., Jouzel, J., Clausen, H. B., Hammer, C. U., et al. (1998) · Nature · doi:10.1038/29447 · Cited by 772
Cited by
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
High-resolution record of Northern Hemisphere climate extending into the last interglacial period
North Greenland Ice Core Project members (2004) · Nature · doi:10.1038/nature02805 · Cited by 3,170
Sea-level fluctuations during the last glacial cycle
Siddall, M., Rohling, E. J., Almogi-Labin, A., Hemleben, C., Meischner, D., Schmelzer, I., & Smeed, D. A. (2003) · Nature · doi:10.1038/nature01690 · Cited by 1,626
One-to-one coupling of glacial climate variability in Greenland and Antarctica
Members, E. C. (2006) · Nature · doi:10.1038/nature05301 · Cited by 1,305
An Assessment of Earth's Climate Sensitivity Using Multiple Lines of Evidence
Sherwood, S. C., Webb, M. J., Annan, J. D., Armour, K. C., Forster, P. M., Hargreaves, J. C., Hegerl, G., Klein, S. A., Marvel, K. D., Rohling, E. J., et al. (2020) · Reviews of Geophysics · doi:10.1029/2019rg000678 · Cited by 1,254
Metadata
- Authors
- Shackleton, N. J., Hall, M. A., & Vincent, E.
- Venue
- Paleoceanography
- Publisher
- American Geophysical Union (AGU)
- Published
- 2000-12
- Volume
- 15
- Issue
- 6
- Pages
- 565-569
- ISSN
- 0883-8305 (ISSN-L)
- 1944-9186
- OpenAlex
- W1976521143
- Cited by
- 637
- References
- 1
- FWCI
- 10.85
- Type
- journal article
- Language
- en
- Open access
- bronze
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- Shackleton, N. J., Hall, M. A., & Vincent, E. (2000). Phase relationships between millennial‐scale events 64,000–24,000 years ago. Paleoceanography. https://doi.org/10.1029/2000pa000513
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
