Abstract
Late Oligocene to late Pliocene vertical water-mass stratification along depth traverses in the northern Indian Ocean is depicted in this paper by benthic foraminifer index faunas. During most of this time, benthic faunas indicate well-oxygenated, bottom-water conditions at all depths except under the southern Indian upwelling and in the Pliocene in the southern Arabian Sea. -from Author
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CITATION STYLE
Boersma, A. (1990). Late Oligocene to Late Pliocene benthic foraminifers from depth traverses in the central Indian Ocean. Proc., Scientific Results, ODP, Leg 115, Mascarene Plateau, 315–379. https://doi.org/10.2973/odp.proc.sr.115.146.1990
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