Insolation driven biomagnetic response to the Holocene Warm Period in semi-arid East Asia-Reference-Cited by-同舟云学术

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Insolation driven biomagnetic response to the Holocene Warm Period in semi-arid East Asia

Published:2015-01-23 Issue:1 Volume:5 Page:
ISSN:2045-2322
Container-title:Scientific Reports
language:en
Short-container-title:Sci Rep

Author:

Liu Suzhen,Deng Chenglong,Xiao Jule,Li Jinhua,Paterson Greig A.,Chang Liao,Yi Liang,Qin Huafeng,Pan Yongxin,Zhu Rixiang

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/srep08001.pdf

Reference37 articles.

1. Kopp, R. E. & Kirschvink, J. L. The identification and biogeochemical interpretation of fossil magnetotactic bacteria. Earth-Sci. Rev. 86, 42–61, 10.1016/j.earscirev.2007.08.001 (2008).

2. Roberts, A. P. et al. Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron. Earth Planet. Sci. Lett. 310, 441–452, 10.1016/j.epsl.2011.08.011 (2011).

3. Larrasoaña, J. C. et al. Magnetotactic bacterial response to Antarctic dust supply during the Palaeocene-Eocene thermal maximum. Earth Planet. Sci. Lett. 333–334, 122–133, 10.1016/j.epsl.2012.04.003 (2012).

4. Kopp, R. E. et al. An Appalachian Amazon? Magnetofossil evidence for the development of a tropical river-like system in the mid-Atlantic United States during the Paleocene-Eocene thermal maximum. Paleoceanography 24, PA4211, 10.1029/2009PA001783 (2009).

5. Kopp, R. E. et al. Magnetofossil spike during the Paleocene-Eocene thermal maximum: Ferromagnetic resonance, rock magnetic and electron microscopy evidence from Ancora, New Jersey, United States. Paleoceanography 22, PA4103, 10.1029/2007PA001473 (2007).

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