Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron-Reference-Cited by-同舟云学术

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Magnetotactic bacterial abundance in pelagic marine environments is limited by organic carbon flux and availability of dissolved iron

Published:2011-10 Issue:3-4 Volume:310 Page:441-452
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Roberts Andrew P.,Florindo Fabio,Villa Giuliana,Chang Liao,Jovane Luigi,Bohaty Steven M.,Larrasoaña Juan C.,Heslop David,Fitz Gerald John D.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference77 articles.

1. Biochemical vs. detrital mechanism of remanence acquisition in marine carbonates: a lesson from the K-T boundary interval;Abrajevitch;Earth Planet. Sci. Lett.,2009

2. Iron fertilisation and biogeochemical cycles in the sub-Arctic northwest Pacific during the late Pliocene intensification of northern hemisphere glaciation;Bailey;Earth Planet. Sci. Lett.,2011

3. Magnetosome formation in prokaryotes;Bazylinski;Nat. Rev. Microbiol.,2004

4. Fe3O4 and Fe3S4 in a bacterium;Bazylinski;Nature,1993

5. Modes of biomineralization of magnetite by microbes;Bazylinski;Geomicrobiol. J.,2007

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