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Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
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“In sharp contrast, modern rates of atmospheric C emission (~9 Pg/year) are probably the highest of the Cenozoic Era (the last 65 Ma), likely surpassing even those of the Paleocene-Eocene thermal maximum ( 68 ).”
From The Anthropocene is functionally and stratigraphically distinct from the Holocene (2016) · cites this paper as [68]
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Metadata
- Authors
- Cui, Y., Kump, L. R., Ridgwell, A. J., Charles, A. J., Junium, C. K., Diefendorf, A. F., Freeman, K. H., Urban, N. M., & Harding, I. C.
- Affiliations
- Pennsylvania State University (US)
- University of Bristol (GB)
- National Oceanography Centre (GB)
- Northwestern University (US)
- Corresponding author
- Cui, Ying
- ORCID
- Venue
- Nature Geoscience
- Published
- 2011-06-05
- Volume
- 4
- Issue
- 7
- Pages
- 481-485
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2002859026
- Cited by
- 265
- References
- 43
- Citations by year
- 2026: 4 · 2025: 13 · 2024: 27 · 2023: 15 · 2022: 12 · 2021: 13 · 2020: 20 · 2019: 25 · 2018: 20 · 2017: 17 · 2016: 20 · 2015: 19 · 2014: 11 · 2013: 27 · 2012: 16
- FWCI
- 13.13
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature Geoscience (publishedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- Bristol Research (University of Bristol) (submittedVersion)
- Funders
- Natural Environment Research Council (NE/F001622/1, NE/C515904/1)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Keywords
- Paleocene-Eocene Thermal Maximum, carbon isotope excursion, Earth system models
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