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...
Main Authors: | , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2001
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.735232 https://doi.org/10.1594/PANGAEA.735232 |