10 September 2009 Life on Mars: new evidence from martian meteorites
Author Affiliations +
Abstract
New data on Martian meteorite 84001 as well as new experimental studies show that thermal or shock decomposition of carbonate, the leading alternative non-biologic explanation for the unusual nanophase magnetite found in this meteorite, cannot explain the chemistry of the actual martian magnetites. This leaves the biogenic explanation as the only remaining viable hypothesis for the origin of these unique magnetites. Additional data from two other martian meteorites show a suite of biomorphs which are nearly identical between meteorites recovered from two widely different terrestrial environments (Egyptian Nile bottomlands and Antarctic ice sheets). This similarity argues against terrestrial processes as the cause of these biomorphs and supports an origin on Mars for these features.
© (2009) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
David S. McKay, David S. McKay, Kathy L. Thomas-Keprta, Kathy L. Thomas-Keprta, Simon J. Clemett, Simon J. Clemett, Everett K. Gibson, Everett K. Gibson, Lauren Spencer, Lauren Spencer, Susan J. Wentworth, Susan J. Wentworth, } "Life on Mars: new evidence from martian meteorites", Proc. SPIE 7441, Instruments and Methods for Astrobiology and Planetary Missions XII, 744102 (10 September 2009); doi: 10.1117/12.832317; https://doi.org/10.1117/12.832317
PROCEEDINGS
20 PAGES


SHARE
RELATED CONTENT

Iron microbial mats in modern and phanerozoic environments
Proceedings of SPIE (August 27 2008)
Oxides of Mars
Proceedings of SPIE (February 04 2002)
Atlas of bacteriomorphs in carbonaceous chondrites
Proceedings of SPIE (February 09 2004)

Back to Top