The DOI matches its Crossref record; 28 of the 28 references it cites were found in a registry or an index.
ENSO-like Forcing on Oceanic Primary Production During the Late Pleistocene
Abstract
Late Pleistocene changes in oceanic primary productivity along the equator in the Indian and Pacific oceans are revealed by quantitative changes in nanoplankton communities preserved in nine deep-sea cores. We show that variations in equatorial productivity are primarily caused by glacial-interglacial variability and by precession-controlled changes in the east-west thermocline slope of the Indo-Pacific. The precession-controlled variations in productivity are linked to processes similar to the Southern Oscillation phenomenon, and they precede changes in the oxygen isotopic ratio, which indicates that they are not the result of ice sheet fluctuations. The 30,000-year spectral peak in the tropical Indo-Pacific Ocean productivity records is also present in the Antarctica atmospheric CO 2 record, suggesting an important role for equatorial biological productivity in modifying atmospheric CO 2 .
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Cited by
Loukos, H., Monfray, P., Bopp, L., & Lehodey, P. (2003) · Fisheries Oceanography · doi:10.1046/j.1365-2419.2003.00241.x · Cited by 72
Metadata
- Authors
- Beaufort, L., de Garidel-Thoron, T., Mix, A. C., & Pisias, N. G.
- Venue
- Science
- Published
- 2001-09-28
- Volume
- 293
- Issue
- 5539
- Pages
- 2440-2444
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2062019088
- Cited by
- 305
- References
- 28
- FWCI
- 7.82
- Type
- journal article
- Language
- en
- Open access
- closed
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- Beaufort, L., de Garidel-Thoron, T., Mix, A. C., & Pisias, N. G. (2001). ENSO-like Forcing on Oceanic Primary Production During the Late Pleistocene. Science. https://doi.org/10.1126/science.293.5539.2440
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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.
