Edwards, Christopher S. and Ehlmann, Bethany L. (2015) Carbon sequestration on Mars. Geology, 43 (10). pp. 863-866. ISSN 1943-2682. http://resolver.caltech.edu/CaltechAUTHORS:20150827-175842753
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On Earth, carbon sequestration in geologic units plays an important role in the carbon cycle, scrubbing CO_2 from the atmosphere for long-term storage. While carbonate is identified in low abundances within the dust and soils of Mars, at <1 wt% in select meteorites, and in limited outcrops, no massive carbonate rock reservoir on Mars has been identified to date. Here, we investigate the largest exposed carbonate-bearing rock unit, the Nili Fossae plains, combining spectral, thermophysical, and morphological analyses to evaluate the timing and carbon sequestration potential of rocks on Mars. We find that the olivine-enriched (∼20%–25%) basalts have been altered, by low-temperature in situ carbonation processes, to at most ∼20% Fe-Mg carbonate, thus limiting carbon sequestration in the Nili Fossae region to ∼0.25–12 mbar of CO_2 during the late Noachian–early Hesperian, before or concurrent with valley network formation. While this is large compared to modern-day CO_2 reservoirs, the lack of additional, comparably sized post–late Noachian carbonate-bearing deposits on Mars indicates ineffective carbon sequestration in rock units over the past ∼3.7 b.y. This implies a thin atmosphere (≲500 mbar) during valley network formation, extensive post-Noachian atmospheric loss to space, or diffuse, deep sequestration by a yet-to-be understood process. In stark contrast to Earth’s biologically mediated crust:atmosphere carbon reservoir ratio of ∼10^4–10^5, Mars’ ratio is a mere ∼10–10^3, even if buried pre-Noachian crust holds multiple bars.
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|Additional Information:||© 2015 Geological Society of America. Manuscript received 18 May 2015; Revised manuscript received 23 July 2015; Manuscript accepted 24 July 2015. We thank R.E. Arvidson for providing the CRISM DISORT processed image, A.D. Rogers for the Syrtis-type TES spectra, and S. Piqueux for helpful discussions. T.D. Glotch, P.D. Niles, and an anonymous reviewer provided helpful formal reviews. A Mars Exploration Program Future Landing Sites grant administered by the Jet Propulsion Laboratory provided partial support for Edwards and Ehlmann to conduct this analysis.|
|Official Citation:||Christopher S. Edwards and Bethany L. Ehlmann Carbon sequestration on Mars Geology, October 2015, v. 43, p. 863-866, first published on August 21, 2015, doi:10.1130/G36983.1|
|Usage Policy:||No commercial reproduction, distribution, display or performance rights in this work are provided.|
|Deposited By:||Gail Peretsman Clement|
|Deposited On:||28 Aug 2015 01:21|
|Last Modified:||15 Oct 2015 22:53|
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