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Science 5 June 1998:
Vol. 280. no. 5369, pp. 1580 - 1582
DOI: 10.1126/science.280.5369.1580

Reports

Atmosphere-Surface Interactions on Mars: Delta 17O Measurements of Carbonate from ALH 84001 

James Farquhar, Mark H. Thiemens, Teresa Jackson

Oxygen isotope measurements of carbonate from martian meteorite ALH 84001 (delta 18O = 18.3 ± 0.4 per mil, delta 17O = 10.3 ± 0.2 per mil, and Delta 17O = 0.8 ± 0.05 per mil) are fractionated with respect to those of silicate minerals. These measurements support the existence of two oxygen isotope reservoirs (the atmosphere and the silicate planet) on Mars at the time of carbonate growth. The cause of the atmospheric oxygen isotope anomaly may be exchange between CO2 and O(1D) produced by the photodecomposition of ozone. Atmospheric oxygen isotope compositions may be transferred to carbonate minerals by CO2-H2O exchange and mineral growth. A sink of 17O-depleted oxygen, as required by mass balance, may exist in the planetary regolith.

Department of Chemistry, University of California San Diego, 92093-0356, USA. E-mail: jfarquha{at}ucsd.edu (J.F.), mht{at}ucsd.edu (M.H.T.), tjackson{at}ucsd.edu (T.J.)


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