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Science 25 February 1994:
Vol. 263. no. 5150, pp. 1122 - 1125
DOI: 10.1126/science.263.5150.1122

Articles

A Molecular Organic Carbon Isotope Record of Miocene Climate Changes

M. Schoell 1, S. Schouten 2, J. S. Sinninghe Damsté 2, J. W. de Leeuw 2, and R. E. Summons 3

1 Chevron Petroleum Technology Company, P.O. Box 446, La Habra, CA 90633, USA.
2 Division of Marine Biogeochemistry, Netherlands Institute of Sea Research, P. O. Box 59, 1790 AB, Den Burg, Texel, Netherlands
3 Australian Geological Survey Organisation, GPO Box 378, Canberra ACT 2601, Australia

The difference in carbon-13 (13C) contents of hopane and sterane biomarkers in the Monterey formation (Naples Beach, California) parallels the Miocene inorganic record of the change in 18O (dgr18O), reflecting the Miocene evolution from a well-mixed to a highly stratified photic zone (upper 100 meters) in the Pacific. Steranes (dgr13C = 25.4 ± 0.7 per mil versus the Pee Dee belemnite standard) from shallow photic-zone organisms do not change isotopically throughout the Miocene. In contrast, sulfur-bound C35 hopanes (likely derived from bacterial plankton living at the base of the photic zone) have systematically decreasing 13C concentrations in Middle and Late Miocene samples (dgr13C = –29.5 to –31.5 per mil), consistent with the Middle Miocene formation of a carbon dioxide—rich cold water mass at the base of the photic zone.

Submitted on June 22, 1993
Accepted on November 23, 1993


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