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Where to search for martian biota?

机译:在哪里寻找火星生物田?

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Martian Salt. Terrestrial halite containing negative crystals which entrapped drops of viscous fluid yielded viable bacteria. The fluid has a Br/Mg ratio which chemist W.T. Holser characterized as a `Permian bittern.' All relevant salt on Mars should be inspected for negative crystals and possible ancient bacterial tenants. Martian Water. Moist soil in the regolith, cooled hydrothermal fluids, sediments of recurrent oceanic water, and related to inferred strand lines, even limited water in future SNC-type meteorites, upper atmosphere liquid water or water vapor, and North Polar liquid water or ice--all liquid water in any form, wherever, should be collected for microbiological analysis. Vent Fauna. Living or fossil thermophiles as trace fossils, or fauna metallicized in relation to sulphide ores. Iron Bacteria. Limonitized magnetite ore (USSR) in thin section showed structures attributed to iron bacteria. Biogenic magnetite, produced by both aerobic and anaerobic bacteria and its significance. Carbonaceous chondrites (non martian) (Ivuna and Orgueil) yielded apparent life forms that could not be attributed to contamination during the given study. Are they extraterrestrial?
机译:火星盐。含有负晶体的陆地宿骨,粘稠粘性流体滴产生可行的细菌。该流体具有BR / MG比的化学家W.T. HOLSER作为“二叠钟卤脏”。应检查所有相关盐是否应检查阴性晶体和可能的古代细菌租户。火星水。潮湿的土壤中的潮湿土壤,冷却水热流体,复发性海水沉积物,以及推断链线,甚至有限的水在未来的SNC型陨石,高大气液体水或水蒸气,以及北极液体水或冰 - 任何形式的所有液态都应该收集用于微生物学分析。发泄动物。生物或化石热料作为痕量化石,或与硫化物矿石相关的动物群。铁菌。薄膜中的灰度化磁铁矿矿石(USSR)显示归因于铁菌的结构。生物磁铁矿,由好氧和厌氧细菌产生及其意义。碳质填充(非火星)(Ivuna和Orgueil)产生明显的生命形式,不能归因于在给定的研究期间的污染。他们是外星人吗?

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