Experimental evidence for rapid biotic and abiotic reduction of Fe (III) at low temperatures in salt marsh sediments: a possible mechanism for formation of modern sedimentary siderite concretions

Title
Experimental evidence for rapid biotic and abiotic reduction of Fe (III) at low temperatures in salt marsh sediments: a possible mechanism for formation of modern sedimentary siderite concretions
Authors
Keywords
-
Journal
SEDIMENTOLOGY
Volume 58, Issue 6, Pages 1514-1529
Publisher
Wiley
Online
2011-02-26
DOI
10.1111/j.1365-3091.2011.01224.x

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