Late Quaternary planktonic foraminifera of ODP Hole 175-1087A

Planktonic foraminiferal assemblages from the upper Pleistocene part of Hole 1087A (0 to 12.1 meters below seafloor) are investigated to assess the role of global and local climate changes on surface circulation in the southern Benguela region. The benthic stable isotope record indicates that the st...

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Bibliographic Details
Main Authors: Giraudeau, Jacques, Pierre, Catherine, Herve, Laurence
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2001
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.735232
https://doi.org/10.1594/PANGAEA.735232