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Geobiology|January 9, 2010
Coupling hydrocarbon degradation to anaerobic respiration and mineral diagenesis: theoretical constraintsT C Onstott, S M Hinton, B J Silver, et al.Geobiology|April 20, 2010
Subsurface characterization of methane production and oxidation from a New Hampshire wetlandJ K Shoemaker, D P SchragGeobiology|April 11, 2015
Ecologically and geologically relevant isotope signatures of C, N, and S: okenone producing purple sulfur bacteria Part ID A Smith, A Steele, R Bowden, et al.Geobiology|September 25, 2026
Coralline Algal Beds as Carbonate Factories: From Local Production to Global SignificanceNadine Schubert, Tainá L Gaspar, Marcial Cosme de Esteban, et al.Geobiology|September 11, 2026
Adaptation of Microbialite-Associated Prokaryotic Communities to Natural and Experimental Anoxic ConditionsJeanne Caumartin, Karim Benzerara, Ana Gutiérrez-Preciado, et al.Geobiology|October 17, 2026
Impact Crater Hydrothermal Systems Support Rapid Microbial Enrichment and Diverse Metabolic PotentialSabrina M C Hardy, Emily J Aguilar-Pine, Sean Gulick, et al.Geobiology|September 3, 2026
Thallium Isotopes Across the Smithian-Spathian Boundary: Evidence for Anoxia Throughout Most of the Early TriassicSean M Newby, Jeremy D Owens, Seth A Young, et al.Geobiology|September 19, 2019
On the biogenicity of Fe-oxyhydroxide filaments in silicified low-temperature hydrothermal deposits: Implications for the identification of Fe-oxidizing bacteria in the rock recordKaren C Johannessen, Nicola McLoughlin, Per Erik Vullum, et al.Geobiology|August 23, 2019
A paleosol record of the evolution of Cr redox cycling and evidence for an increase in atmospheric oxygen during the NeoproterozoicDavid Auerbach Colwyn, Nathan D Sheldon, J Barry Maynard, et al.Geobiology|January 20, 2022
Coccolith Sr/Ca is a robust temperature and growth rate indicator that withstands dynamic microbial interactionsOr Eliason, Einat SegevPageof 77