Physiology, Fe(II) oxidation, and Fe mineral formation by a marine planktonic cyanobacterium grown under ferruginous conditions-Reference-Cited by-同舟云学术

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Physiology, Fe(II) oxidation, and Fe mineral formation by a marine planktonic cyanobacterium grown under ferruginous conditions

Published:2015-10-08 Issue: Volume:3 Page:
ISSN:2296-6463
Container-title:Frontiers in Earth Science
language:
Short-container-title:Front. Earth Sci.

Author:

Swanner Elizabeth D.,Wu Wenfang,Hao Likai,Wüstner Marina Lisa,Obst Martin,Moran Dawn M.,McIlvin Matthew R.,Saito Mak A.,Kappler Andreas

Funder

National Science Foundation

Carl-Zeiss-Stiftung

Gordon and Betty Moore Foundation

Deutsche Forschungsgemeinschaft

European Research Council

Publisher

Frontiers Media SA

Subject

General Earth and Planetary Sciences

Reference153 articles.

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2. Stromatolite reef from the early Archaean era of Australia;Allwood;Nature,2006

3. A Whiff of oxygen before the great oxidation event?;Anbar;Science,2007

4. Ferric uptake regulation protein acts as a repressor, employing iron(II) as a cofactor to bind the operator of an iron transport operon in Escherichia coli;Bagg;Biochemistry,1987

5. Photochemical cycling of iron in the surface ocean mediated by microbal iron(III)-binding ligands;Barbeau;Nature,2001

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1. Cyanobacteria-ferrihydrite aggregates, BIF sedimentation and implications for Archaean- Palaeoproterozoic seawater geochemistry;South African Journal of Geology;2024-06-01

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