Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

The Paleocene–Eocene boundary (∼55.8 million years ago) is marked by an abrupt negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease interpreted as the Paleocene–Eocene thermal maximum. Biogenic magnetite (Fe[subscript 3]O[subscript 4]) in the form of giant (micron-s...

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Bibliographic Details
Main Authors: Wang, Huapei, Wang, Jun, Chen-Wiegart, Yu-chen Karen, Kent, Dennis V.
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: National Academy of Sciences (U.S.) 2016
Online Access:http://hdl.handle.net/1721.1/102263
https://orcid.org/0000-0003-1676-3494

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http://hdl.handle.net/1721.1/102263
https://orcid.org/0000-0003-1676-3494

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