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-Reference-Cited by-同舟云学术

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

Published:2011-02-24 Issue:6 Volume:58 Page:1514-1529
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:

Author:

MORTIMER ROBERT J. G.,GALSWORTHY AMANDA M. J.,BOTTRELL SIMON H.,WILMOT LUCY E.,NEWTON ROBERT J.

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-3091.2011.01224.x/fullpdf

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3. Coupling between sedimentary dynamics, early diagenetic processes, and biogeochemical cycling in the Amazon-Guianas mobile mud belt: coastal French Guiana;Aller;Mar. Geol.,2004

4. Early diagenetic mineralization and fossil preservation in modern carbonate concretions;Allison;Palaios,1994

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