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Life on Mars: Evidence from Martian MeteoritesNew 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.
Document ID
20090038980
Acquisition Source
Johnson Space Center
Document Type
Preprint (Draft being sent to journal)
Authors
McKay, David S.
(NASA Johnson Space Center Houston, TX, United States)
Thomas-Keptra, Katie L.
(Jacobs Technologies Engineering Science Contract Group Houston, TX, United States)
Clemett, Simon J.
(Jacobs Technologies Engineering Science Contract Group Houston, TX, United States)
Gibson, Everett K., Jr.
(NASA Johnson Space Center Houston, TX, United States)
Spencer, Lauren
(NASA Johnson Space Center Houston, TX, United States)
Wentworth, Susan J.
(Jacobs Technologies Engineering Science Contract Group Houston, TX, United States)
Date Acquired
August 24, 2013
Publication Date
January 1, 2009
Subject Category
Life Sciences (General)
Report/Patent Number
JSC-CN-19247
Distribution Limits
Public
Copyright
Public Use Permitted.
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