Synchronizing volcanic, sedimentary, and ice core records of Earth’s last magnetic polarity reversal-Reference-Cited by-同舟云学术

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Synchronizing volcanic, sedimentary, and ice core records of Earth’s last magnetic polarity reversal

Published:2019-08-02 Issue:8 Volume:5 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Singer Brad S.¹^ORCID,Jicha Brian R.¹^ORCID,Mochizuki Nobutatsu²^ORCID,Coe Robert S.³

Affiliation:

1. Department of Geoscience, University of Wisconsin-Madison, 1215 West Dayton Street, Madison, WI 53706, USA.

2. Priority Organization for Innovation and Excellence, Kumamoto University, Kumamoto 860-8555, Japan.

3. Earth Sciences Department, University of California, Santa Cruz, CA 95064, USA.

Abstract

Earth’s last magnetic field reversal was complex, with excursions at 795 and 784 ka before a final polarity flip at 773 ka.

Funder

National Science Foundation

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference63 articles.

1. Deciphering records of geomagnetic reversals;Valet J.-P.;Rev. Geophys.,2016

2. Complexity in Matuyama–Brunhes polarity transitions from North Atlantic IODP/ODP deep-sea sites;Channell J. E. T.;Earth Planet. Sci. Lett.,2017

3. Magnetic polarity reversals in the core;Glatzmaier G. A.;Treatise Geophysics,2015

4. An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677;Shackleton N. J.;Earth Environ. Sci. Trans. R. Soc. Edinb.,1990

5. Astronomical calibration of the Matuyama-Brunhes boundary: Consequences for magnetic remanence acquisition in marine carbonates and the Asian loess sequences;Tauxe L.;Earth Planet. Sci. Lett.,1996

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