Habitability: Where to look for life? Halophilic habitats: Earth analogs to study Mars habitability

被引:9
|
作者
Gomez, F. [1 ]
Rodriguez-Manfredi, J. A. [1 ]
Rodriguez, N. [1 ]
Fernandez-Sampedro, M. [1 ]
Caballero-Castrejon, F. J. [1 ]
Amils, R. [1 ,2 ]
机构
[1] Ctr Astrobiol INTA CSIC, Madrid 28850, Spain
[2] Univ Autonoma Madrid, Ctr Biol Mol, E-28049 Madrid, Spain
关键词
Endolithic micro environments; Astrobiology; MERIDIANI-PLANUM; ENVIRONMENT; ROCKS; IRON;
D O I
10.1016/j.pss.2011.12.021
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Oxidative stress, high radiation doses, low temperature and pressure are parameters which made Mars's surface adverse for life. Those conditions found on Mars surface are harsh conditions for life to deal with. Life, as we know it on Earth, needs several requirements for its establishment but, the only "sine qua nom" element is water. Extremophilic microorganisms widened the window of possibilities for life to develop in the universe, and as a consequence on Mars. Recently reported results in extreme environments indicate the possibility of presence of "oasys" for life in microniches due to water deliquescence in salts deposits. The compilation of data produced by the ongoing missions (Mars Global Surveyor, Mars Odyssey, Mars Express and Mars Exploration Rover Opportunity) offers a completely different view from that reported by Viking missions: signs of an early wet Mars and rather recent volcanic activity. The discovery of important accumulations of sulfates, and the existence of iron minerals like jarosite, goethite and hematite in rocks of sedimentary origin has allowed specific terrestrial models related with this type of mineralogy to come into focus. Rio Tinto (Southwestern Spain, Iberian Pyritic Belt) is an extreme acidic environment, product of the chemolithotrophic activity of microorganisms that thrive in the massive pyrite-rich deposits of the Iberian Pyritic Belt. The high concentration of ferric iron and sulfates, products of the metabolism of pyrite, generate a collection of minerals, mainly gypsum, jarosite, goethite and hematites, all of which have been detected in different regions of Mars. Some particular protective environments or elements could house organic molecules or the first bacterial life forms on Mars surface. Terrestrial analogs could help us to afford its comprehension. We are reporting here some preliminary studies about endolithic niches inside salt deposits used by phototrophs for taking advantage of sheltering particular light wavelengths. These acidic salts deposits located in Rio Tinto shelter life forms which are difficult to localize by eye. Techniques for its localization and study during space missions are needed to develop. Extreme environments are good scenarios where to test and train those techniques and where hypothetical astrobiological space missions could be simulated for increasing possibilities of micro niches identification. (C) 2011 Elsevier Ltd. All rights reserved.
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收藏
页码:48 / 55
页数:8
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