Mars analog minerals’ spectral reflectance characteristics under Martian surface conditions

Icarus ◽  
2018 ◽  
Vol 306 ◽  
pp. 50-73
Author(s):  
J.T. Poitras ◽  
E.A. Cloutis ◽  
M.R. Salvatore ◽  
S.A. Mertzman ◽  
D.M. Applin ◽  
...  
2021 ◽  
pp. 105377
Author(s):  
Nathalie Turenne ◽  
Alexis Parkinson ◽  
Daniel M. Applin ◽  
Paul Mann ◽  
Edward A. Cloutis ◽  
...  

Icarus ◽  
2011 ◽  
Vol 211 (2) ◽  
pp. 1162-1178 ◽  
Author(s):  
A.P. Johnson ◽  
L.M. Pratt ◽  
T. Vishnivetskaya ◽  
S. Pfiffner ◽  
R.A. Bryan ◽  
...  

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Deborah Maus ◽  
Jacob Heinz ◽  
Janosch Schirmack ◽  
Alessandro Airo ◽  
Samuel P. Kounaves ◽  
...  

AbstractThe current understanding of the Martian surface indicates that briny environments at the near-surface are temporarily possible, e.g. in the case of the presumably deliquescence-driven Recurring Slope Lineae (RSL). However, whether such dynamic environments are habitable for terrestrial organisms remains poorly understood. This hypothesis was tested by developing a Closed Deliquescence System (CDS) consisting of a mixture of desiccated Martian Regolith Analog (MRA) substrate, salts, and microbial cells, which over the course of days became wetted through deliquescence. The methane produced via metabolic activity for three methanogenic archaea: Methanosarcina mazei, M. barkeri and M. soligelidi, was measured after exposing them to three different MRA substrates using either NaCl or NaClO4 as a hygroscopic salt. Our experiments showed that (1) M. soligelidi rapidly produced methane at 4 °C, (2) M. barkeri produced methane at 28 °C though not at 4 °C, (3) M. mazei was not metabolically reactivated through deliquescence, (4) none of the species produced methane in the presence of perchlorate, and (5) all species were metabolically most active in the phyllosilicate-containing MRA. These results emphasize the importance of the substrate, microbial species, salt, and temperature used in the experiments. Furthermore, we show here for the first time that water provided by deliquescence alone is sufficient to rehydrate methanogenic archaea and to reactivate their metabolism under conditions roughly analogous to the near-subsurface Martian environment.


2008 ◽  
Vol 74 (16) ◽  
pp. 5159-5167 ◽  
Author(s):  
Patricia Fajardo-Cavazos ◽  
Andrew C. Schuerger ◽  
Wayne L. Nicholson

ABSTRACTMost planetary protection research has concentrated on characterizing viable bioloads on spacecraft surfaces, developing techniques for bioload reduction prior to launch, and studying the effects of simulated martian environments on microbial survival. Little research has examined the persistence of biogenic signature molecules on spacecraft materials under simulated martian surface conditions. This study examined how endogenous adenosine-5′-triphosphate (ATP) would persist on aluminum coupons under simulated martian conditions of 7.1 mbar, full-spectrum simulated martian radiation calibrated to 4 W m−2of UV-C (200 to 280 nm), −10°C, and a Mars gas mix of CO2(95.54%), N2(2.7%), Ar (1.6%), O2(0.13%), and H2O (0.03%). Cell or spore viabilities ofAcinetobacter radioresistens, Bacillus pumilus, andB. subtiliswere measured in minutes to hours, while high levels of endogenous ATP were recovered after exposures of up to 21 days. The dominant factor responsible for temporal reductions in viability and loss of ATP was the simulated Mars surface radiation; low pressure, low temperature, and the Mars gas composition exhibited only slight effects. The normal burst of endogenous ATP detected during spore germination inB. pumilusandB. subtiliswas reduced by 1 or 2 orders of magnitude following, respectively, 8- or 30-min exposures to simulated martian conditions. The results support the conclusion that endogenous ATP will persist for time periods that are likely to extend beyond the nominal lengths of most surface missions on Mars, and planetary protection protocols prior to launch may require additional rigor to further reduce the presence and abundance of biosignature molecules on spacecraft surfaces.


2016 ◽  
Vol 9 (6) ◽  
pp. 425-428 ◽  
Author(s):  
M. Massé ◽  
S. J. Conway ◽  
J. Gargani ◽  
M. R. Patel ◽  
K. Pasquon ◽  
...  

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Carolina Gil-Lozano ◽  
Alberto G. Fairén ◽  
Victoria Muñoz-Iglesias ◽  
Maite Fernández-Sampedro ◽  
Olga Prieto-Ballesteros ◽  
...  

Abstract The presence of organic matter in lacustrine mudstone sediments at Gale crater was revealed by the Mars Science Laboratory Curiosity rover, which also identified smectite clay minerals. Analogue experiments on phyllosilicates formed under low temperature aqueous conditons have illustrated that these are excellent reservoirs to host organic compounds against the harsh surface conditions of Mars. Here, we evaluate whether the capacity of smectites to preserve organic compounds can be influenced by a short exposure to different diagenetic fluids. We analyzed the stability of glycine embedded within nontronite samples previously exposed to either acidic or alkaline fluids (hereafter referred to as “treated nontronites”) under Mars-like surface conditions. Analyses performed using multiple techniques showed higher photodegradation of glycine in the acid-treated nontronite, triggered by decarboxylation and deamination processes. In constrast, our experiments showed that glycine molecules were preferably incorporated by ion exchange in the interlayer region of the alkali-treated nontronite, conferring them a better protection against the external conditions. Our results demonstrate that smectite previously exposed to fluids with different pH values influences how glycine is adsorbed into their interlayer regions, affecting their potential for preservation of organic compounds under contemporary Mars surface conditions.


2005 ◽  
Vol 4 (1) ◽  
pp. 93-96 ◽  
Author(s):  
N.B. Gontareva

Life has probably existed on Earth for about 3.5 billion years and ever since people could wonder, they have tried to understand its origins. It is thought that organisms as complex as bacteria emerged within 0.5–1 billion years. Organic molecules, such as amino acids, organic acids and sugars have been observed in material from extraterrestrial sources in the solar system. But, to confirm the possibility of nucleic acid bases also being synthesized under these conditions, we have replicated the synthesis of monophosphates as dry pellets (5′-monophosphates, the predominant reaction products) under simulated Martian conditions. Our research task was to find out whether the main organic substances were able to survive in the absence of water. This reaction must proceed under solvent-free conditions and incident short ultraviolet radiation (UVC) in a vacuum. After 5 months of reaction time monophosphates could be identified in detectable quantities. These experiments utilized basalt and limonite as protectors and successfully shielded the products from decomposition by UVC. Our team has obtained more results concerning prebiotic synthesis of polypeptides and nucleotides in the presence of meteorite dust; these are the same kind of experiment, but using different extraterrestrial material.


Icarus ◽  
2008 ◽  
Vol 195 (1) ◽  
pp. 140-168 ◽  
Author(s):  
E.A. Cloutis ◽  
M.A. Craig ◽  
R.V. Kruzelecky ◽  
W.R. Jamroz ◽  
A. Scott ◽  
...  

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