A paleosol record of the evolution of Cr redox cycling and evidence for an increase in atmospheric oxygen during the Neoproterozoic.

Autor: Colwyn DA; Department of Geology and Geophysics, Yale University, New Haven, CT, USA., Sheldon ND; Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI, USA., Maynard JB; Department of Geology, University of Cincinnati, Cincinnati, OH, USA., Gaines R; Geology Department, Pomona College, Claremont, CA, USA., Hofmann A; Department of Geology, University of Johannesburg, Johannesburg, South Africa., Wang X; Department of Geology and Geophysics, Yale University, New Haven, CT, USA.; Department of Marine Sciences, University of South Alabama, Mobile, AL, USA.; Dauphin Island Sea Lab, Dauphin Island, AL, USA., Gueguen B; Department of Geology and Geophysics, Yale University, New Haven, CT, USA.; Institut Universitaire Européen de la Mer, CNRS UMS 3113, Université de Brest, Plouzané, France., Asael D; Department of Geology and Geophysics, Yale University, New Haven, CT, USA., Reinhard CT; School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA., Planavsky NJ; Department of Geology and Geophysics, Yale University, New Haven, CT, USA.

Publikováno v: Geobiology [Geobiology] 2019 Nov; Vol. 17 (6), pp. 579-593. Date of Electronic Publication: 2019 Aug 22.