Paleomagnetic and stable carbon isotope record of ODP Hole 119-738C

Distinct magnetic properties of marine sediments that record the Palaeocene-Eocene thermal maximum (PETM) have been suggested to be due to a bacterial magnetofossil signal that is linked to enhanced weathering conditions during the PETM. We document the dominance of bacterial magnetite in deep-sea s...

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Bibliographic Details
Main Authors: Larrasoaña, Juan C, Roberts, Andrew P, Chang, Liao, Schellenberg, Stephen A, Fitz Gerald, John D, Norris, Richard D, Zachos, James C
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2012
Subjects:
119-738C
DRILL
Drilling/drill rig
Indian Ocean
Joides Resolution
Leg119
Ocean Drilling Program
ODP
Antarc*
Antarctic
Southern Ocean
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.792713
https://doi.org/10.1594/PANGAEA.792713

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