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...

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Bibliographic Details
Main Authors: Scher, Howie D, Bohaty, Steven M, Smith, Brian W, Munn, Colin B
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2014
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.858177
https://doi.org/10.1594/PANGAEA.858177