Assessment of the probability of microbial contamination for sample return from Martian moons II: The fate of microbes on Martian moons
arXiv:1907.07576 · doi:10.1016/j.lssr.2019.07.006
Abstract
This paper presents a case study of microbe transportation in the Mars-satellites system. We examined the spatial distribution of potential impact-transported microbes on the Martian moons using impact physics by following a companion study (Fujita et al.). We used sterilization data from the precede studies. We considered that the microbes came mainly from the Zunil crater on Mars. We found that 70-80% of the microbes are likely to be dispersed all over the moon surface and are rapidly sterilized due to radiation except for those microbes within a thick ejecta deposit produced by meteoroids. The other 20-30% might be shielded from radiation by thick regolith layers that formed at collapsed layers in craters produced by Mars rock impacts. The total number of potentially surviving microbes at the thick ejecta deposits is estimated to be 3-4 orders of magnitude lower than at the Mars rock craters. The microbe concentration is irregular in the horizontal direction and is largely depth-dependent due to the radiation sterilization. The surviving fraction of transported microbes would be only 1 ppm on Phobos and 100 ppm on Deimos, suggesting that the transport processes and radiation severely affect microbe survival. The microbe sampling probability from the Martian moons was also investigated. We suggest that sample return missions from the Martian moons are classified into Unrestricted Earth-Return missions for 30 g samples and 10 cm depth sampling, even in our conservative scenario. We also conducted a full statistical analysis for sampling the regolith of Phobos to include the effects of uncertainties in input parameters on the sampling probability. The most likely probability of microbial contamination for return samples is estimated to be two orders of magnitude lower than the criterion defined by the planetary protection policy of the Committee on Space Research (COSPAR).
arXiv comment50 pages, 16 figures, 2 tables, The abstract was shortened to meet the arXiv words limit, accepted for publication in Life Sciences in Space Research, special issues on planetary protection
References in corpus (9)
- Seven temperate terrestrial planets around the nearby ultracool dwarf star TRAPPIST-1
- Temperate Earth-sized planets transiting a nearby ultracool dwarf star
- Warm Debris Disks Produced by Giant Impacts During Terrestrial Planet Formation
- Enhanced interplanetary panspermia in the TRAPPIST-1 system
- Effects of friction and plastic deformation in shock-comminuted damaged rocks on impact heating
- Hydrocode modeling of the spallation process during hypervelocity impacts: Implications for the ejection of Martian meteorites
- Dynamical transport of asteroid fragments from the nu6 resonance
- On the Impact Origin of Phobos and Deimos IV: Volatile Depletion
- Fast litho-panspermia in the habitable zone of the TRAPPIST-1 system
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- Mixing model of Phobos' bulk elemental composition for the determination of its origin: Multivariate analysis of MMX/MEGANE data
- Mars: new insights and unresolved questions