Stable isotope record of DSDP Hole 81-552A in the northeastern Atlantic Ocean
Oxygen and carbon isotope ratios in benthic foraminifers have been determined at 10 cm intervals through the top 59 m of DSDP Hole 552A. This provides a glacial record of remarkable resolution for the late Pliocene and Pleistocene. The major glacial event which marked the onset of Pleistocene-like g...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1984
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.698993 https://doi.org/10.1594/PANGAEA.698993 |
Summary: | Oxygen and carbon isotope ratios in benthic foraminifers have been determined at 10 cm intervals through the top 59 m of DSDP Hole 552A. This provides a glacial record of remarkable resolution for the late Pliocene and Pleistocene. The major glacial event which marked the onset of Pleistocene-like glacial-interglacial alternations was at about 2.4 m.y. ago. These very high-resolution data do not support the notion of significant Northern Hemisphere glaciation between 3.2 and 2.4 m.y. ago. |
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