Sexton, Philip F. et al. (2011): Eocene global warming events driven by ventilation of oceanic dissolved organic carbon

Leg/Site/Hole:
ODP 198
ODP 207
ODP 208
ODP 198 1210
ODP 207 1258
ODP 208 1267
Identifier:
2011-050307
georefid
10.1038/nature09826
doi
Creator:
Sexton, Philip F.
Scripps Institution of Oceanography, La Jolla, CA, United States
author
Norris, Richard D.
University of Southampton, United Kingdom
author
Wilson, Paul A.
University of Bremen, Germany
author
Palike, Heiko
author
Westerhold, Thomas
author
Roehl, Ursula
author
Bolton, Clara T.
author
Gibbs, Samantha
author
Identification:
Eocene global warming events driven by ventilation of oceanic dissolved organic carbon
2011
Nature (London)
Macmillan Journals, London, United Kingdom
471
7338
349-352
English
Serial
Coverage:Geographic coordinates:
North:32.1300
West:-54.4400East: 158.1600
South:-28.0600
Stratigraphy; 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; Ocean Drilling Program; ODP Site 1210; ODP Site 1258; ODP Site 1267; 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;
.