Neodymium isotopes from fossil fish teeth and detrital sediment, and oxygen isotopes from benthic forams from ODP Hole 119-738 B
Ephemeral polar glaciations during the middle-to-late Eocene (48-34 Ma) have been proposed based on far-field ice volume proxy records and near-field glacigenic sediments, although the scale, timing, and duration of these events are poorly constrained. Here we confirm the existence of a transient co...
Main Authors: | , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2014
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.858177 https://doi.org/10.1594/PANGAEA.858177 |