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Tirez Lake as a Terrestrial Analog of Europa

机译:提兹湖作为欧罗巴的陆地类似物

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Tirez Lake (La Mancha, central Spain) is proposed as a terrestrial analogue of Europa's ocean. The proposal is based on the comparison of the hydrogeochemistry of Tirez Lake with the geochemical features of the alteration mineralogy of meteoritic precursors and with Galileo's Near Infrared Mapping Spectrometer data on Europa's surface. To validate the astrobiological potential of Tfrez Lake as an analog of Europa/ different hydrogeochemical, mineral/ and microbial analyses were performed. Experimental and theoretical modeling helped to understand the crystallization pathways that may occur in Europa's crust. Calculations about the oxidation state of the hypothetical Europan ocean were estimated to support the sulfate-rich neutral liquid model as the origin of Europa's observed hydrated minerals and to facilitate their comparison with Tirez's hydrogeochemistry. Hydrogeochemical and mineralogical analyses showed that Tirez waters corresponded to Mg-Na-SO4-Cl brines with epsomite, hexahydrite, and halite as end members. A preliminary microbial ecology characterization identified two different microbial domains: a photosynthetically sustained community represented by planktonic/benthonic forms and microbial mat communities, and a subsurficial anaerobic realm in which chemolithotrophy predominates. Fluorescence in situ hybridization has been used to characterize the prokaryotic diversity of the system. The subsurficial community seemed to be dominated by sulfate-reducing bacteria and methanogens. Frozen Tirez brines were analyzed by Fourier-transform infrared techniques providing spectra similar to those reported previously using pure components and to the Galileo spectral data. Calorimetric measurements of Tirez brines showed pathways and phase metastability for magnesium sulfate and sodium chloride crystallization that may aid in understanding the processes involved in the formation of Europa's icy crust. The use of fluorescence hybridization techniques for microbial detection and characterization in hypersaline environments makes this methodology strongly advisable for future Europa astrobiological missions.
机译:提尔兹湖(西班牙中部拉曼恰)被提议作为欧罗巴海洋的陆地类似物。该提议是基于对Tirez Lake的水文地球化学与陨石前兆蚀变矿物学的地球化学特征以及欧罗巴表面上Galileo的近红外测绘光谱仪数据的比较而得出的。为了验证Tfrez湖作为欧罗巴类似物的天文生物学潜力/进行了不同的水文地球化学,矿物/微生物分析。实验和理论建模有助于了解欧罗巴地壳可能发生的结晶途径。估计有关假设的欧罗潘海域氧化态的计算可支持富含硫酸盐的中性液体模型,作为欧罗巴观测到的水合矿物的起源,并有助于将其与提尔兹的水文地球化学进行比较。水文地球化学和矿物学分析表明,提尔兹水对应于镁盐,钠盐,亚硫酸盐,卤水和六水石盐的卤水。初步的微生物生态学特征鉴定了两个不同的微生物域:以浮游/膨松形式和微生物垫群落为代表的光合持续群落,以及以化石营养为主导的地下亚厌氧域。荧光原位杂交已被用来表征系统的原核多样性。地下生活的社区似乎以减少硫酸盐的细菌和产甲烷菌为主。冷冻的Tirez盐水通过傅里叶变换红外技术进行了分析,其光谱与以前使用纯组分报告的光谱和伽利略光谱数据相似。提尔兹盐水的量热法测量表明,硫酸镁和氯化钠结晶的途径和相亚稳性可能有助于理解欧罗巴结冰壳形成过程。荧光杂交技术在高盐环境中用于微生物检测和表征的用途,使该方法对于未来的欧罗巴天文生物学任务非常可取。

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