Abstract
Isotope analyses have been performed on planktonic and benthic foraminifers from levels widely spaced in time (2 to 4 my) at Hole 400A and Site 401. In addition, isotope analyses of bulk carbonates from 250 levels from Holes 400A, 402A, and Sites 401, 403 and 406 are interpreted in terms of paleoceanographic changes. Their evolution is compared with the thermal evolution that can be deduced from foraminiferal analyses. -Authors
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CITATION STYLE
Letolle, R., Vergnaud Grazzini, C., & Pierre, C. (1979). Oxygen and carbon isotopes from bulk carbonates and foraminiferal shells at DSDP sites 400, 401, 402, 403 and 406. Initial Reports of the Deep Sea Drilling Project, Leg 48, Brest, France to Aberdeen, Scotland, 1976, (Scripps Institution of Oceanography; UK Distributors, IPOD Committee, NERC, Swindon), 741–756. https://doi.org/10.2973/dsdp.proc.48.132.1979
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