Changes in Iron Oxidation Rate in Hydrothermal Plumes as a Potential Driver of Enhanced Hydrothermal Input to Near-ridge Sediments During Glacial Terminations

Jay T. Cullen, University of Victoria, School of Earth and Ocean Sciences, Victoria, BC, Canada and Laurence A Coogan, University of Victoria, Victoria, BC, Canada
Back to: Biogeochemical Processes Across Oxic-Anoxic Transitions I