Phase relationship between carbonate and benthic δ18O in ODP Site 1089 is a direct test of the "coral reef hypothesis" for atmospheric CO2 variability

Author(s): Hodell, David A.; Charles, Christopher D.
Ocean Drilling Program, Leg 177, Shipboard Scientific Party
Author Affiliation(s): Primary:
University of Florida, Department of Geology, Gainesville, FL, United States
Other:
Scripps Institution of Oceanography, La Jolla, CA, United States
Volume Title: AGU 1999 spring meeting
Source: Eos, Transactions, American Geophysical Union, 80(17 Suppl.), p.198; American Geophysical Union 1999 spring meeting, Boston, MA, June 1-4, 1999. Publisher: American Geophysical Union, Washington, DC, United States. ISSN: 0096-3941 CODEN: EOSTAJ
Note: In English
Year of Publication: 1999
Research Program: ODP Ocean Drilling Program
Key Words: 02 Geochemistry; 24 Surficial Geology, Quaternary Geology; Atlantic Ocean; Atmosphere; Brunhes Chron; Cape Basin; Carbon dioxide; Carbonates; Cenozoic; Detritus; Glacial environment; Glaciation; Global; Interglacial environment; Isotope ratios; Isotopes; Leg 177; Lysoclines; Marine sediments; North Atlantic Deep Water; O-18/O-16; ODP Site 1089; Ocean Drilling Program; Ocean circulation; Oxygen; Paleo-oceanography; Quaternary; Sea-level changes; Sedimentation; Sedimentation rates; Sediments; South Atlantic; Stable isotopes; Upper Quaternary
Coordinates: S405611 S405611 E0095338 E0095338
Record ID: 2001065888
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