Isotopic links between atmospheric chemistry and the deep sulphur cycle on Mars

Heather B. Franz (), Sang-Tae Kim, James Farquhar, James M. D. Day, Rita C. Economos, Kevin D. McKeegan, Axel K. Schmitt, Anthony J. Irving, Joost Hoek and James Dottin
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Heather B. Franz: Center for Research and Exploration in Space Science and Technology, NASA Goddard Space Flight Center
Sang-Tae Kim: School of Geography and Earth Sciences, McMaster University, Hamilton, Ontario L8S 4K1, Canada
James Farquhar: University of Maryland, College Park
James M. D. Day: Scripps Institution of Oceanography, University of California San Diego
Rita C. Economos: University of California
Kevin D. McKeegan: University of California
Axel K. Schmitt: University of California
Anthony J. Irving: University of Washington
Joost Hoek: University of Maryland, College Park
James Dottin: University of Maryland, College Park

Nature, 2014, vol. 508, issue 7496, 364-368

Abstract: Isotopic analyses of 40 Martian meteorites indicate that assimilation of sulphur into Martian magmas was a common occurrence throughout much of the planet’s history and that the atmospheric imprint of photochemical processing preserved in Martian meteoritic sulphide and sulphate is distinct from that observed in terrestrial analogues.

Date: 2014
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DOI: 10.1038/nature13175

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