Microbial anaerobic Fe(II) oxidation – Ecology, mechanisms and environmental implications
Abstract
Iron is the most abundant redox-active metal in the Earth's crust. The one electron transfer between the two most common redox states, Fe(II) and Fe(III), plays a role in a huge range of environmental processes from mineral formation and dissolution to contaminant remediation and global biogeochemical cycling. It has been appreciated for more than a century that microorganisms can harness the energy of this Fe redox transformation for their...
Paper Details
Title
Microbial anaerobic Fe(II) oxidation – Ecology, mechanisms and environmental implications
Published Date
Oct 1, 2018
Journal
Volume
20
Issue
10
Pages
3462 - 3483
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Notes
History