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Scientific Reports|February 23, 2012
The ineluctable requirement for the trans-iron elements molybdenum and/or tungsten in the origin of lifeBarbara Schoepp-Cothenet, Robert van Lis, Pascal Philippot, et al.Nature|August 21, 2024
Neoarchaean oxygen-based nitrogen cycle en route to the Great Oxidation EventAlice Pellerin, Christophe Thomazo, Magali Ader, et al.Science (New York, N.Y.)|September 18, 2007
Early Archaean microorganisms preferred elemental sulfur, not sulfatePascal Philippot, Mark Van Zuilen, Kevin Lepot, et al.Journal of Synchrotron Radiation|July 3, 2015
Optical design and multi-length-scale scanning spectro-microscopy possibilities at the Nanoscopium beamline of Synchrotron SoleilAndrea Somogyi, Kadda Medjoubi, Gil Baranton, et al.Geobiology|March 4, 2021
Anoxygenic photosynthesis linked to Neoarchean iron formations in Carajás (Brazil)Eric Siciliano Rego, Vincent Busigny, Stefan V Lalonde, et al.Geobiology|March 3, 2020
In Situ Fe and S isotope analyses in pyrite from the 3.2 Ga Mendon Formation (Barberton Greenstone Belt, South Africa): Evidence for early microbial iron reductionJohanna Marin-Carbonne, Vincent Busigny, Jennyfer Miot, et al.Nature Communications|June 10, 2018
Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation EventPascal Philippot, Janaína N Ávila, Bryan A Killingsworth, et al.Pageof 2