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Lava tubes and basaltic caves as astrobiological targets on Earth and Mars: A review

机译:熔岩管和玄武岩洞穴作为地球和火星上的天体生物学目标:回顾

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Lava tubes and basaltic caves are common features in volcanic terrains on Earth. Lava tubes and cave-like features have also been identified on Mars based on orbital imagery and remote-sensing data. Caves are unique environments where both secondary mineral precipitation and microbial growth are enhanced by stable physico-chemical conditions. Thus, they represent excellent locations where traces of microbial life, or biosignatures, are formed and preserved in minerals. By analogy with terrestrial caves, caves on Mars may contain a record of secondary mineralization that would inform us on past aqueous activity. They may also represent the best locations to search for biosignatures. The study of caves on Earth can be used to test hypotheses and better understand biogeochemical processes, and the signatures that these processes leave in mineral deposits. Caves may also serve as test beds for the development of exploration strategies and novel technologies for future missions to Mars. Here we review recent evidence for the presence of caves or lava tubes on Mars, as well as the geomicrobiology of lava tubes and basaltic caves on Earth. We also propose future lines of investigation, including exploration strategies and relevant technologies.
机译:熔岩管和玄武岩洞穴是地球上火山地形的常见特征。在火星上还根据轨道影像和遥感数据确定了熔岩管和类似洞穴的特征。洞穴是独特的环境,通过稳定的物理化学条件,矿物质的次生沉淀和微生物的生长均得到增强。因此,它们代表了在矿物质中形成并保存微生物生命或生物特征痕迹的绝佳位置。类似于陆地洞穴,火星上的洞穴可能包含次生矿化记录,这将使我们了解过去的水活动。它们也可能代表搜索生物特征的最佳位置。对地球上洞穴的研究可以用来检验假设并更好地理解生物地球化学过程,以及这些过程留在矿床中的特征。洞穴还可以作为开发勘探策略和为未来的火星任务提供新技术的试验台。在这里,我们回顾了火星上存在洞穴或熔岩管的最新证据,以及地球上熔岩管和玄武岩洞穴的地球微生物学。我们还提出了未来的研究方向,包括勘探策略和相关技术。

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