Methylhopane biomarker hydrocarbons in Hamersley Province sediments provide evidence for Neoarchean aerobiosis

By J. Eigenbrode, K. Freeman, R. Summons. 2008

152 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Mechanics of Materials, Paleontology

View Paper: https://www.semanticscholar.org/paper/80dd16a794dc3321ff4f3fc11ad2944b79c89aa1

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In Environmental Chemistry

1. A. Kappler
2. K. Konhauser

In Paleontology

1. A. Kappler
2. E. Roden

Citations in the corpus

• Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770 Ma Isua Supracrustal Belt (West Greenland) (2013, background): “45 Ga based on geochemical and biomarker evidence (e.g., Brocks et al., 1999; Anbar et al., 2007; Kaufman et al., 2007; Eigenbrode et al., 2008; Waldbauer et al., 2009; Kendall et al., 2010; Czaja et al., 2012; Stüeken et al., 2012).”
• Microbiological processes in banded iron formation deposition (2013, background): “Bitumens from the 2 6 Ga Marra Mamba Iron Formation and the 2 5 Ga Mount McRae Shale of the Hamersley Group, Western Australia, for example yield abundant 2a-methylhopanes, derivatives of prominent lipids in cyanobacteria (methyl-bacteriohopanepolyols) that serve to improve cell membrane rigidity (B”