V027:
Redox From the Surface to the Core over Earth History





Session ID#: 23695

Session Description:
Oxidation/reduction (redox) processes control the geochemical and geophysical evolution of Earth's core, mantle, crust, oceans, and atmosphere. The high activity of oxygen at Earth’s surface is unique among rocky planets in our solar system and is a signature of life, while the reduced nature of the interior plays a key role in volcanism and the formation of minerals like diamonds and sulfides. Redox processes have also impacted Earth differentiation and mobility of elements over deep time. This session aims to bring together a wide range of disciplines and their intersections, from the deep Earth to the biosphere. We are particularly interested in studies that promote a broad view of redox systematics and interactions between surface and interior. We invite submissions from approaches including experiments, modeling, and observations of redox processes in sediments, intrusive and extrusive volcanic rocks, exhumed metamorphic terranes, and inaccessible phase assemblages of Earth’s mantle and core.
Primary Convener:  Maryjo N Brounce, California Institute of Technology, Pasadena, CA, United States
Conveners:  Alicia M Cruz-Uribe, University of Maine, School of Earth and Climate Sciences, Orono, ME, United States, Suzanne Birner, Stanford University, Stanford, CA, United States and Susannah Dorfman, Michigan State University, East Lansing, MI, United States
Co-Organized with:
Volcanology, Geochemistry and Petrology, Study of Earth's Deep Interior, Mineral and Rock Physics, and Tectonophysics

Cross-Listed:
  • DI - Study of the Earth's Deep Interior
  • MR - Mineral and Rock Physics
  • PP - Paleoceanography and Paleoclimatology
Index Terms:

3640 Igneous petrology [MINERALOGY AND PETROLOGY]
3660 Metamorphic petrology [MINERALOGY AND PETROLOGY]
5225 Early environment of Earth [PLANETARY SCIENCES: ASTROBIOLOGY]
8439 Physics and chemistry of magma bodies [VOLCANOLOGY]

Abstracts Submitted to this Session:

Allison T Greaney1, Roberta L Rudnick1, Stephen J Romaniello2, Aleisha Johnson2, Richard M Gaschnig3 and Ariel D Anbar2, (1)University of California Santa Barbara, Department of Earth Sciences, Santa Barbara, CA, United States, (2)Arizona State University, Tempe, AZ, United States, (3)University of Massachusetts Lowell, Lowell, MA, United States
James Eguchi and Rajdeep Dasgupta, Rice University, Department of Earth, Environmental, and Planetary Sciences, Houston, TX, United States
Avishek Rudra and Marc M Hirschmann, Univ Minnesota, Minneapolis, MN, United States
Ming Tang1, Monica Erdman2, Graham Eldridge3 and Cin-Ty Lee2, (1)Rice University, Houston, TX, United States, (2)Rice Univ, Houston, TX, United States, (3)Rice University, Houston, United States
William F McDonough, University of Maryland College Park, Department of Geology, College Park, MD, United States, Meng Guo, University of Maryland College Park, Geology, College Park, MD, United States and Scott Alan Wipperfurth, University of Maryland College Park, College Park, MD, United States
Dalton Shane Hardisty1, Tristan J Horner1, Scott D Wankel1, Zunli Lu2, Timothy Lyons3 and Sune Nielsen4, (1)Woods Hole Oceanographic Institution, Woods Hole, MA, United States, (2)Syracuse University, Syracuse, NY, United States, (3)University of California Riverside, Chino, CA, United States, (4)Woods Hole Oceanographic Institute, Woods Hole, MA, United States
Marek Locmelis, Missouri University of Science and Technology, Department of Geosciences and Geological and Petroleum Engineering, Rolla, MO, United States, Ricardo D Arevalo Jr, NASA Goddard Space Flight Center, Greenbelt, MD, United States, Igor S Puchtel, University of Maryland, Department of Geology, College Park, MD, United States and Marco L Fiorentini, The University of Western Australia, Centre for Exploration Targeting and ARC Centre of Excellence for Core to Crust Fluid Systems, School of Earth Sciences, Crawley, Australia
Kenneth James Peterman1, Seth Bryson1, Sarah Rilling-Hall2 and Michael Barton1, (1)Ohio State University Main Campus, Columbus, OH, United States, (2)Shell Exploration and Production Company, Houston, TX, United States
Suzanne Birner1,2, Fred A Davis3, Elizabeth Cottrell1, Jessica M Warren4 and Katherine A Kelley5, (1)National Museum of Natural History, Smithsonian Institution, Department of Mineral Sciences, Washington, DC, United States, (2)Stanford University, Department of Geological Sciences, Stanford, CA, United States, (3)University of Minnesota Duluth, Duluth, MN, United States, (4)University of Delaware, Newark, DE, United States, (5)Graduate School of Oceanography, University of Rhode Island, Narragansett, RI, United States
Kayla Iacovino, Arizona State University, Tempe, AZ, United States and Christy B. Till, Arizona State University, School of Earth & Space Exploration, Tempe, AZ, United States
Catherine A McCammon1, Valerio Cerantola2, Elena Bykova3, Ilya Kupenko4, Maxim Bykov5, Alexander I Chumakov2, Rudolf Rüffer2 and Leonid S Dubrovinsky5, (1)University of Bayreuth, Bayreuth, Germany, (2)ESRF European Synchrotron Radiation Facility, Grenoble, France, (3)DESY Deutsches Elektronen Synchrotron, Hamburg, Germany, (4)University of Muenster, Institute for Mineralogy, Muenster, Germany, (5)Bayerisches Geoinstitut, Universitaet Bayreuth, Bayreuth, Germany
Fred A Davis, University of Minnesota Duluth, Duluth, MN, United States, Kellie T Wall, Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States and Elizabeth Cottrell, National Museum of Natural History, Smithsonian Institution, Department of Mineral Sciences, Washington, DC, United States
Daniel R Hummer1, Joshua J Golden2, Grethe Hystad3, Robert T Downs2, Ahmed Eleish4, Chao Liu5, Jolyon Ralph6, Shaunna Morrison5, Michael Meyer5 and Robert M Hazen3, (1)Southern Illinois University Carbondale, Department of Geology, Carbondale, IL, United States, (2)University of Arizona, Department of Geosciences, Tucson, AZ, United States, (3)Carnegie Inst, Washington, DC, United States, (4)Rensselaer Polytechnic Institute, Troy, NY, United States, (5)Carnegie Institution for Science Washington, Geophysical Laboratory, Washington, DC, United States, (6)mindat.org, Surray, United Kingdom
Souvik Das, University of Texas at Arlington, Earth and Environmental Sciences, Arlington, TX, United States and Asish R Basu, University of Texas at Arlington, Arlington, TX, United States
Asish R Basu, University of Texas at Arlington, Earth & Environmental Sciences, Arlington, TX, United States and Souvik Das, Physical Research Laboratory, Ahmedabad, India
Kanani K M Lee1, Tingting Gu2, Neala Creasy1, Mingming Li3, Catherine A McCammon4 and Jennifer Girard5, (1)Yale University, Department of Geology and Geophysics, New Haven, CT, United States, (2)Center for High Pressure Science & Technology Advanced Research, Shanghai, China, (3)University of Colorado at Boulder, Department of Physics, Boulder, CO, United States, (4)University of Bayreuth, Bayerisches Geoinstitut, Bayreuth, Germany, (5)Yale University, New Haven, CT, United States