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This study examines paleoproductivity values determined from benthic foraminifera from the Late Oligocene (~26 Ma) until the Late Pliocene/Early Pleistocene (~2.5 Ma), and tests the hypothesis that paleoproductivity values prior to closure of the Central American Seaway are similar in both the Caribbean and equatorial Pacific and then diverge by the time of early shoaling events. Published data from the equatorial Eastern Pacific (DSDP Sites 503, 568, and 569), are examined in conjunction with new data from ODP Site 999 and previously published Caribbean data (DSDP Site 502). Identifications of deep-sea benthic foraminifera in previous studies of the Caribbean and equatorial Eastern Pacific were taxonomically standardized and examined for trends in

Neogene Changes in Caribbean Paleoproductivity and the Diversity and Paleobiogeography of Deep-sea Benthic Foraminifera