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Metal-catalyzed degradation and racemization of amino acids in iron sulfate brines under simulated martian surface conditions
- Source :
- Icarus. May, 2010, Vol. 207 Issue 1, p124, 9 p.
- Publication Year :
- 2010
-
Abstract
- To link to full-text access for this article, visit this link: http://dx.doi.org/10.1016/j.icarus.2009.11.028 Byline: Adam P. Johnson (a), Lisa M. Pratt (b) Keywords: Exobiology; Photochemistry; Geological processes; Mars Abstract: Recent lines of evidence indicate that Mars may have been substantially warmer and wetter, raising questions about whether the planet's surface was once more conducive to the possibility of life. To better constrain the extent of preservation of ancient amino acid biosignatures, the effects of metal ions and UV radiation were investigated with respect to the rates of diagenesis of amino acids in metal-rich sulfate brines. Individual experimental results indicate that the oxidation rates of amino acids loosely followed trends characteristic of a radiolytic oxidation mechanism that is dependent on variations in side-chain constituents. Relative rates of racemization only show a limited dependence on the presence of metals; overall, rates of racemization in the presence of metals in solution are an order of magnitude slower than oxidation and both are several orders of magnitude faster than previously reported. This increase in rate constant is indicative of an extremely efficient catalytic enhancement of this destructive diagenetic pathway. These findings imply that chiral life-detection strategies should focus on specific geochemical environments that exhibit relatively slow rates of both degradation and racemization. Episodic liquid water during periods of increased water activity on the martian surface may have significant implications for the oxidation of organic matter through secondary diagenetic reactions and may act as a leveling mechanism for organic compounds. Author Affiliation: (a) Department of Molecular and Cellular Biochemistry, Indiana University, 1001 E. 10th Street, Bloomington, IN 47405, United States (b) Department of Geological Sciences, Indiana University, 1001 E. 10th Street, Bloomington, IN 47405, United States Article History: Received 6 April 2009; Revised 5 November 2009; Accepted 24 November 2009
Details
- Language :
- English
- ISSN :
- 00191035
- Volume :
- 207
- Issue :
- 1
- Database :
- Gale General OneFile
- Journal :
- Icarus
- Publication Type :
- Academic Journal
- Accession number :
- edsgcl.223228803