Middle Eocene to late Oligocene calcareous nannofossils of ODP Hole 120-748B
A major deterioration in global climate occurred through the Eocene-Oligocene time interval, characterized by long-term cooling in both terrestrial and marine environments. During this long-term cooling trend, however, recent studies have documented several short-lived warming and cooling phases. In...
Main Authors: | , , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2008
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.773713 https://doi.org/10.1594/PANGAEA.773713 |