Eocene global warming events driven by ventilation of oceanic dissolved organic carbon

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doi: 10.1038/nature09826
Author(s): Sexton, Philip F.; Norris, Richard D.; Wilson, Paul A.; Palike, Heiko; Westerhold, Thomas; Röhl, Ursula; Bolton, Clara T.; Gibbs, Samantha
Author Affiliation(s): Primary:
Scripps Institution of Oceanography, La Jolla, CA, United States
Other:
University of Southampton, United Kingdom
University of Bremen, Germany
Volume Title: Nature (London)
Source: Nature (London), 471(7338), p.349-352. Publisher: Macmillan Journals, London, United Kingdom. ISSN: 0028-0836 CODEN: NATUAS
Note: In English. Supplemental information/data is available in the online version of this article. 30 refs.; illus.
Year of Publication: 2011
Research Program: ODP Ocean Drilling Program
Key Words: 12 Stratigraphy, Historical Geology and Paleoecology; Atlantic Ocean; C-13/C-12; Calcium carbonate; Carbon; Cenozoic; Climate change; Concentration; Demerara Rise; Eocene; Equatorial Atlantic; Foraminifera; Global change; Global warming; Invertebrata; Isotope ratios; Isotopes; Leg 198; Leg 207; Leg 208; Marine environment; Microfossils; North Atlantic; North Pacific; Northwest Atlantic; Northwest Pacific; O-18/O-16; ODP Site 1210; ODP Site 1258; ODP Site 1267; Ocean Drilling Program; Organic carbon; Oxygen; Pacific Ocean; Paleocene-Eocene Thermal Maximum; Paleoclimatology; Paleogene; Protista; Reconstruction; Shatsky Rise; South Atlantic; Stable isotopes; Tertiary; Walvis Ridge; West Atlantic; West Pacific
Coordinates: N321300 N321300 E1581600 E1581600
S280600 S280600 E0014300 E0014200
N092600 N092600 W0544400 W0544400
Record ID: 2011050307
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