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Title: The deep sea oxygen isotopic record: Significance for tertiary global ice volume history, with emphasis on the latest Miocene/early Pliocene

Thesis/Dissertation ·
OSTI ID:7266142

Planktonic and benthic isotopic records as well as carbonate sedimentation records extending from 6.1 to 4.1 Ma for eastern South Atlantic Holes 526A and 525B are presented. These data suggest ice volume variations about a constant mean sufficient to drive sea level between 10 m and 75 m below present. Isotopic records at the deeper (2500 m) site have been enriched by up to 0.5% by dissolution. Carbonate accumulation rates at both sites quadrupled at 4.6 Ma primarily because of increased production and, secondarily, decreased dissolution. The second part presents a Cenozoic-long composite {delta}{sup 18}O curve for tropical shallow-dwelling planktonic foraminifers and the benthic foraminifer Cibicides at 2-4 km depths. Surface {delta}{sup 18}O gradients between various low-and-mid latitude sites reflect: (1) widespread SST stability through the Cenozoic and (2) significant change in Tasman Sea SST through the Tertiary. Assuming average SST for tropical non-upwelling areas was constant, the planktonic composite suggest that global ice volume for the last 40 my has not been significantly less than today. Residual benthic {delta}{sup 18}O reflect relatively warm and saline deep water until the early Miocene after which time deep water progressively cooled. The third part presents {delta}{sup 18}O for Recent Orbulina universa from 44 core-tops distributed through the Atlantic and Indian Oceans. The purpose was to test the hypothesis that Orbulina calcifies at constant temperature and so records only ice volume changes. Orbulina commonly calcifies at intermediate depths over a wide range of temperatures salinities, and densities. These physical factors are not the primary controls on the spatial and vertical distribution of Orbulina.

Research Organization:
Brown Univ., Providence, RI (USA)
OSTI ID:
7266142
Resource Relation:
Other Information: Thesis (Ph. D.)
Country of Publication:
United States
Language:
English