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Manganese mineralogy and diagenesis in the sedimentary rock record

  • Published:2016-01 Issue: Volume:173 Page:210-231
  • ISSN:0016-7037
  • Container-title:Geochimica et Cosmochimica Acta
  • language:en
  • Short-container-title:Geochimica et Cosmochimica Acta

Author:

Johnson Jena E.,Webb Samuel M.,Ma Chi,Fischer Woodward W.

Funder

David and Lucile Packard Foundation

NSF-GRFP

DGE

Lewis and Clark Foundation

Agouron Institute

NSF

EAR

DMR

U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences

DOE Office of Biological and Environmental Research

National Institutes of Health

National Institute of General Medical Sciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference115 articles.

1. Miscibility and compatibility of braunite, Mn2+ Mn6 3+ O8/SiO4, in the system Mn–Si–O at 1 atm in air;Abs-Wurmbach;Contrib. Mineral. Petrol.,1980

2. Bioturbation and manganese cycling in hemipelagic sediments;Aller;Philos. Trans. R. Soc. Lond. Ser. Math. Phys. Sci.,1990

3. The photochemistry of manganese and the origin of banded iron formations;Anbar;Geochim. Cosmochim. Acta,1992

4. Mn(II) oxidation is catalyzed by heme peroxidases in “Aurantimonas manganoxydans” strain SI85-9A1 and Erythrobacter sp. strain SD-21;Anderson;Appl. Environ. Microbiol.,2009

5. Why did nature choose manganese to make oxygen?;Armstrong;Philos. Trans. R. Soc. B Biol. Sci.,2008
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