V31B:
Triple Isotopes of Oxygen and Sulfur in Terrestrial Systems I


Submit an Abstract to this Session


Session ID#: 63635

Session Description:
Recent developments in high precision isotope analysis allow the resolution of systematic mass dependent variations in Δ17O, Δ33S and Δ36S of terrestrial materials. This caused a rapid growth of publications and emergence of labs with capabilities to produce high-quality triple isotope measurements providing novel insights into geological processes. We invite authors that work on theoretical and practical aspects of triple oxygen and multiple sulfur isotope geochemistry to contribute their abstracts to the session. The session is aimed to highlight research in the fields of atmospheric and surface geochemistry, early Earth processes, paleoclimate, mass spectrometry, water-rock interaction and other fields where triple and multiple isotope proxies proved to be a powerful tool.
Primary Convener:  David O Zakharov, University of Oregon, Earth Sciences, Eugene, OR, United States
Convener:  Justin Hayles, Rice University, Houston, United States
Primary Liaison:  David O Zakharov, University of Oregon, Earth Sciences, Eugene, OR, United States
Chairs:  David O Zakharov, University of Oregon, Earth Sciences, Eugene, OR, United States and Justin Hayles, Rice University, Houston, United States
OSPA Liaison:  Justin Hayles, Rice University, Houston, United States

Cross-Listed:
  • EP - Earth and Planetary Surface Processes
  • PP - Paleoceanography and Paleoclimatology

Abstracts Submitted to this Session:

David T Johnston, Harvard University, Earth and Planetary Sciences, Cambridge, United States, Jordon Hemingway, ETH Zurich, Geological Institute, Department of Earth and Planetary Sciences, Zurich, Switzerland and David Johnston, Harvard, Cambridge, MA, United States
Perinne Tyler1, Trevor R Ireland2, Peter Holden2, Axel Hofmann3, Li Liu2 and Robert Bolhar4, (1)Australian National University, Research School of Earth Sciences, Canberra, ACT, Australia, (2)Australian National University, Research School of Earth Sciences, Canberra, Australia, (3)University of Johannesburg, Department of Geology, Auckland Park, South Africa, (4)University of the Witwatersrand, School of Geosciences, Johannesburg, South Africa
Amaury Bouyon1, Pierre Cartigny1, Janaina Avila2, Eric Siciliano Rego3, Camille Rossignol4, Pascal Philippot5, Ricardo IF Trindade6 and Sergio RB Hühn7, (1)Institut de Physique du Globe de Paris, Paris, France, (2)Australian National University, Earth Science, Canberra, Australia, (3)University of California San Diego, La Jolla, United States, (4)Universidade de São Paulo, Geophysics, São Paulo, Brazil, (5)Institut de Physique du Globe de Paris, Sorbonne-Paris Cité, Université Paris Diderot, CNRS, Paris, France, (6)Universidade de São Paulo, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, São Paulo, Brazil, (7)Vale SA, Santa Luzia, Brazil
Andreas Pack, University of Göttingen, Göttingen, Germany
Sukanya Sengupta, Georg-August-Universitaet Goettingen, Geowissenschaftliches Zentrum, Goettingen, Germany; Dr., Göttingen, Germany and Andreas Pack, Prof. Dr., Georg August Universität Göttingen, Geowissenschaftliches Zentrum, Göttingen, Germany
Ilya Bindeman, University of Oregon, Department of Earth Sciences, Eugene, OR, United States
Weifu Guo, Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, United States and Chen Zhou, University of Science and Technology of China, Hefei, China; Woods Hole Oceanographic Institution, Woods Hole, United States