Causes of changing organic carbon content in Pleistocene sediments from beneath the Benguela Current upwelling system

Author(s): Robinson, Rebecca S.; Meyers, Philip A.; Murray, Richard W.
Author Affiliation(s): Primary:
University of Michigan, Department of Geological Sciences, Ann Arbor, MI, United States
Other:
Boston University, United States
Volume Title: AGU 1998 fall meeting
Source: Eos, Transactions, American Geophysical Union, 79(45 Suppl.), p.498; American Geophysical Union, 1998 fall meeting, San Francisco, CA, Dec. 6-10, 1998. Publisher: American Geophysical Union, Washington, DC, United States. ISSN: 0096-3941 CODEN: EOSTAJ
Note: In English
Year of Publication: 1998
Research Program: ODP Ocean Drilling Program
Key Words: 24 Surficial Geology, Quaternary Geology; Atlantic Ocean; Benguela Current; C-13/C-12; Cape Basin; Carbon; Cenozoic; Isotope ratios; Isotopes; Leg 175; N-15/N-14; Nitrogen; ODP Site 1082; ODP Site 1084; Ocean Drilling Program; Organic carbon; Paleo-oceanography; Paleocurrents; Pleistocene; Quaternary; Sedimentation; South Atlantic; Stable isotopes; Upwelling
Coordinates: S210539 S210539 E0114914 E0114914
S253049 S253049 E0130140 E0130140
Record ID: 2011097966
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