Beckmann, Britta et al. (2007): Coniacian-Santonian climate evolution inferred from molecular markers of primary producers and ocean water oxygenation; results from the Demerara Rise (ODP Leg 207)

Leg/Site/Hole:
ODP 207
ODP 207 1261
Identifier:
2008-131989
georefid

Creator:
Beckmann, Britta
University of Cologne, Institute for Geology and Mineralogy, Cologne, Federal Republic of Germany
author

Hofmann, Peter
University of Calgary, Canada
author

Pedentchouk, Nikolai
Royal NIOZ, Netherlands
author

Schouten, Stefan
Newcastle University, United Kingdom
author

Sinninghe Damste, Jaap S.
author

Wagner, Thomas
author

Identification:
Coniacian-Santonian climate evolution inferred from molecular markers of primary producers and ocean water oxygenation; results from the Demerara Rise (ODP Leg 207)
2007
In: Farrimond, Paul (editor), The 23rd international meeting on Organic geochemistry; book of abstracts
[publisher varies], [location varies], International
23
247-248
English
Coverage:Geographic coordinates:
North:9.0300
West:-54.1900East: -54.1900
South:9.0300

Stratigraphy; Geochemistry of rocks, soils, and sediments; aliphatic hydrocarbons; alkanes; Atlantic Ocean; biomarkers; black shale; carbon; clastic rocks; Coniacian; Cretaceous; Demerara Rise; Equatorial Atlantic; experimental studies; geochemistry; hydrocarbons; laminations; Leg 207; Mesozoic; n-alkanes; North Atlantic; Northwest Atlantic; Ocean Drilling Program; ODP Site 1261; organic carbon; organic compounds; paleo-oceanography; paleoclimatology; paleoecology; planar bedding structures; productivity; Santonian; sedimentary rocks; sedimentary structures; Senonian; Upper Cretaceous; ventilation;

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