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Science 22 June 1984:
Vol. 224. no. 4655, pp. 1334 - 1336
DOI: 10.1126/science.224.4655.1334

Articles

Paleoceanographic Events and Deep-Sea Ostracodes

RICHARD H. BENSON 1, RALPH E. CHAPMAN 1, and LINDA T. DECK 1

1 Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560

Eight recognized or theorized paleoceanographic events during the past 70 million years were tested against changes in the global deep-sea benthic ostracode fauna. Two events, the sudden Cretaceous-Tertiary boundary event at 66 million years ago and the more gradual 40-million-year event (formation of the psychrosphere), show up most dramatically. Before the 40-million-year event, ostracodes freely radiated into the deeper water regions but were provincial. The development of thermal stratification isolated these deep-water taxa, mostly the survivors of the Cretaceous-Tertiary boundary event, which adapted to a new, free-flowing but more frigid ecosystem and spread rapidly throughout the world.

Submitted on December 30, 1983
Accepted on April 18, 1984


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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