Sinninghe Damste, Jaap S. et al. (2010): A CO (sub 2) decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous oceanic anoxic event 2

Leg/Site/Hole:
ODP 210
ODP 210 1276
Identifier:
2010-074517
georefid

10.1016/j.epsl.2010.02.027
doi

Creator:
Sinninghe Damste, Jaap S.
Royal Netherlands Institute for Sea Research, Department of Marine Organic Biogeochemistry, Den Burg, Netherlands
author

van Bentum, Elisabeth C.
Utrecht University, Netherlands
author

Reichart, Gert-Jan
University of Frankfurt, Federal Republic of Germany
author

Pross, Joerg
author

Schouten, Stefan
author

Identification:
A CO (sub 2) decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous oceanic anoxic event 2
2010
Earth and Planetary Science Letters
Elsevier, Amsterdam, Netherlands
293
1-2
97-103
English
Serial
Coverage:Geographic coordinates:
North:45.2400
West:-44.4700East: -44.4700
South:45.2400

Stratigraphy; Atlantic Ocean; burial; C-13/C-12; carbon; carbon dioxide; Cenomanian; cooling; Cretaceous; greenhouse effect; isotope ratios; isotopes; latitude; Leg 210; Mesozoic; microfossils; Middle Cretaceous; Newfoundland Basin; North Atlantic; Northwest Atlantic; Ocean Drilling Program; oceanic anoxic events; ODP Site 1276; organic carbon; organic compounds; paleoclimatology; paleotemperature; palynomorphs; partial pressure; sea-surface temperature; stable isotopes; temperature; total organic carbon; Turonian; Upper Cretaceous;

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