The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum
Abstract
Lithologic, faunal, seismic, and isotopic evidence from the Blake Nose (subtropical western North Atlantic) links a massive release of biogenic methane ∼55.5 million years ago to a warming of deep-ocean and high-latitude surface waters, a large perturbation in the combined ocean-atmosphere carbon cycle (the largest of the past 90 million years), a mass extinction event in benthic faunas, and a radiation of mammalian orders. The deposition of a mud clast interval and seismic evidence for slope disturbance are associated with intermediate water warming, massive carbon input to the global exogenic carbon cycle, pelagic carbonate dissolution, a decrease in dissolved oxygen, and a benthic foraminiferal extinction event. These events provide evidence to confirm the gas hydrate dissociation hypothesis and identify the Blake Nose as a site of methane release.
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Cites
Revised Carbonate-water isotopic temperature scale
EPSTEIN, S., BUCHSBAUM, R., LOWENSTAM, H. A., & UREY, H. C. (1953) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1953)64[1315:rcits]2.0.co;2 · Cited by 2,271
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
Dickens, G. R. (2003) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(03)00325-x · Cited by 429
Self-citationJiang, G., Kennedy, M. J., Christie-Blick, N., Wu, H., & Zhang, S. (2006) · Journal of Sedimentary Research · doi:10.2110/jsr.2006.086 · Cited by 228
Westerhold, T., Röhl, U., Laskar, J., Raffi, I., Bowles, J., Lourens, L. J., & Zachos, J. C. (2007) · Paleoceanography · doi:10.1029/2006pa001322 · Cited by 193
Stoll, H. M. (2005) · Paleoceanography · doi:10.1029/2004pa001046 · Cited by 59
Metadata
- Authors
- Katz, M. E., Pak, D. K., Dickens, G. R., & Miller, K. G.
- Venue
- Science
- Published
- 1999-11-19
- Volume
- 286
- Issue
- 5444
- Pages
- 1531-1533
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2025149153
- Cited by
- 379
- References
- 1
- FWCI
- 22.47
- Type
- journal article
- Language
- en
- Open access
- closed
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- Katz, M. E., Pak, D. K., Dickens, G. R., & Miller, K. G. (1999). The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum. Science. https://doi.org/10.1126/science.286.5444.1531
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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).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
