Magnetic analyses of ODP Hole 119-738B sediments
Magnetotactic bacteria intracellularly biomineralize magnetite of an ideal grain size for recording palaeomagnetic signals. However, bacterial magnetite has only been reported in a few pre-Quaternary records because progressive burial into anoxic diagenetic environments causes its dissolution. Deep-...
Main Authors: | , , , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2011
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.788624 https://doi.org/10.1594/PANGAEA.788624 |