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Simulating Precambrian banded iron formation diagenesis

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TLDR
In this article, the authors show that electron transfer from organic carbon to Fe(III) minerals during temperature/pressure diagenesis can drive the production of key BIF minerals.
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This article is published in Chemical Geology.The article was published on 2013-12-20 and is currently open access. It has received 92 citations till now. The article focuses on the topics: Ferrihydrite & Hematite.

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Atmospheric Evolution on Inhabited and Lifeless Worlds

TL;DR: In this article, the authors present a survey of the current understanding of the atmospheric evolution and climate on Earth, on other rocky planets within our Solar System, and on planets far beyond.

Iron and Carbon Isotope Evidence for Microbial Iron Respiration Throughout the Archean

TL;DR: In this article, the authors reported the results of a study of the early Archean BIFs from the Hamersley Basin, Australia and the early Isua Supracrustal Belt (ISB), Greenland.
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Biogenic Fe(III) minerals: From formation to diagenesis and preservation in the rock record

TL;DR: In this article, the role of Fe(II)-oxidizing bacteria in the deposition of ancient banded iron formations (BIF) is discussed, with the main challenge of separating biogenic from abiogenic processes over deep time.
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Experimental diagenesis of organo-mineral structures formed by microaerophilic Fe(II)-oxidizing bacteria

TL;DR: It is suggested that iron minerals might play a role in maintaining the structural and chemical integrity of stalks under diagenetic conditions and provide spectroscopic signatures for the search of ancient life in the rock record.
References
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The iron oxides: structure, properties, reactions, occurrences and uses.

TL;DR: In this article, the authors introduce the concept of iron oxides and their properties, including surface chemistry and Colloidal stability, as well as their properties in terms of surface area and porosity.
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Evidence for life on Earth before 3,800 million years ago.

TL;DR: In this article, ion-microprobe measurements of the carbon-isotope composition of carbonaceous inclusions within grains of apatite (basic calcium phosphate) from the oldest known sediment sequences a approx. 3,800 Myr-old banded iron formation from the Isua supracrustal belt, West Greenland and a similar formation from Akilia island that is possibly older than 3,850 Myr.
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2-Methylhopanoids as biomarkers for cyanobacterial oxygenic photosynthesis

TL;DR: It is shown that 2-methylbacteriohopanepolyols occur in a high proportion of cultured cyanob bacteria and cyanobacterial mats and are abundant in organic-rich sediments as old as 2,500 Myr, which may help constrain the age of the oldest cyanobacteria and the advent of oxygenic photosynthesis.
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Geobacter metallireducens gen. nov. sp. nov., a microorganism capable of coupling the complete oxidation of organic compounds to the reduction of iron and other metals.

TL;DR: Profiles of the phospholipid ester-linked fatty acids indicated that both the anaerobic desaturase and the branched pathways for fatty acid biosynthesis were operative, and the 16S rRNA sequence indicated that this organism belongs in the delta proteobacteria.
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A Whiff of Oxygen Before the Great Oxidation Event

TL;DR: In this article, high-resolution chemostratigraphy reveals an episode of enrichment of the redox-sensitive transition metals molybdenum and rhenium in the late Archean Mount McRae Shale in Western Australia.
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