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Multidisciplinary integrated field campaign to an acidic Martian Earth analogue with astrobiological interest: Rio Tinto

机译:涉及天文生物学兴趣的酸性火星地球类似物的多学科综合野战:Rio Tinto

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Recently reported results from latest Mars Orbiters and Rovers missions are transforming our opinion about the red planet. That dry and inhospitable planet reported in the past is becoming a wetter planet with high probabilities of water existence in the past. Nowadays, some results seem to indicate the presence of water beneath the Mars surface. But also mineralogy studies by NASA Opportunity Rover report iron oxides and hydroxides precipitates on Endurance Crater. Sedimentary deposits have been identified at Meridiani Planum. These deposits must have generated in a dune aqueous acidic and oxidizing environment. Similarities appear when we study Rio Tinto, and acidic river under the control of iron. The discovery of extremophiles on Earth widened the window of possibilities for life to develop in the Universe, and as a consequence on Mars and other planetary bodies with astrobiological interest. The compilation of data produced by the ongoing missions offers an interested view for life possibilities to exist: signs of an early wet Mars and rather recent volcanic activity as well as ground morphological characteristics that seem to be promoted by liquid water. The discovery of important accumulations of sulfates and the existence of iron minerals such as jarosite in rocks of sedimentary origin has allowed specific terrestrial models to come into focus. Río Tinto (Southwestern Spain, Iberian Pyritic Belt) is an extreme acidic environment, product of the chemolithotrophic activity of micro-organisms that thrive in the massive pyrite-rich deposits of the Iberian Pyritic Belt. Some particular protective environments should house the organic molecules and bacterial life forms in harsh environments such as Mars surface supporting microniches inside precipitated minerals or inside rocks. Terrestrial analogues could help us to afford the comprehension of habitability (on other planetary bodies). We are reporting here the multidisciplinary study of some endolithic niches inside salt deposits used by phototrophs for taking advantage of sheltering particular light wavelengths. These acidic salts deposits located in Río Tinto shelter life forms that are difficult to visualize by eye. This interdisciplinary field analogue campaign was conducted in the framework of the CAREX FP7 EC programme.
机译:最新的火星轨道和火星探测器任务最新报道的结果正在改变我们对红色星球的看法。过去报道的那个干燥而荒凉的星球正在变成一个潮湿的星球,过去有很高的水存在可能性。如今,一些结果似乎表明火星表面下存在水。但是,NASA机会漫游者的矿物学研究也报告了Endurance Crater上的铁氧化物和氢氧化物沉淀。在Meridiani Planum上已经发现了沉积物。这些沉积物一定是在沙丘水溶液的酸性和氧化环境中产生的。当我们研究力拓(Rio Tinto)和铁控制下的酸性河流时,会出现相似之处。地球上极端微生物的发现拓宽了生命在宇宙中发展的可能性之窗,结果是火星和其他具有天文生物学兴趣的行星体也因此发展。进行中的任务收集的数据为存在的生命可能性提供了有趣的观点:火星早湿的迹象和近期的火山活动以及液态水似乎促进了地面形态特征。在沉积起源的岩石中发现了重要的硫酸盐积累和铁矿物质(例如黄铁矿),这使特定的陆地模型成为人们关注的焦点。 RíoTinto(西班牙西南部,伊比利亚黄铁矿带)是一种极端酸性环境,是微生物在化石营养作用下生长的产物,该微生物在伊比利亚黄铁矿带的大量富含黄铁矿的矿床中壮成长。一些特殊的保护环境应容纳有机分子,并在恶劣的环境中形成细菌的生命形式,例如在沉淀的矿物质或岩石内部的火星表面支撑微生态位。地球类似物可以帮助我们理解(在其他行星体上)的宜居性。我们在这里报告了多学科研究,这些盐沉积内部的一些内生壁ni被光养生物利用,以利用掩盖特定光波长的优势。这些酸性盐沉积物位于RíoTinto,掩盖了难以用肉眼看到的生命形式。这项跨学科的现场模拟运动是在CAREX FP7 EC计划的框架内进行的。

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