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蒂雷斯湖作为木卫二的地球类似物。

Tírez lake as a terrestrial analog of Europa.

作者信息

Prieto-Ballesteros Olga, Rodríguez Nuria, Kargel Jeffrey S, Kessler Carola González, Amils Ricardo, Remolar David Fernández

机构信息

Centro de Astrobiología (CSIC-INTA), Torrejón de Ardoz, Spain.

出版信息

Astrobiology. 2003 Winter;3(4):863-77. doi: 10.1089/153110703322736141.

Abstract

Tírez 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 Tírez 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 Tírez 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 Tírez's hydrogeochemistry. Hydrogeochemical and mineralogical analyses showed that Tírez waters corresponded to Mg-Na-SO(4)-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 Tírez 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 Tírez 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.

摘要

蒂雷斯湖(位于西班牙中部的拉曼恰)被提议作为木卫二海洋的陆地模拟物。这一提议基于对蒂雷斯湖水文地球化学与陨石前身蚀变矿物学的地球化学特征以及伽利略号近红外测绘光谱仪关于木卫二表面数据的比较。为了验证蒂雷斯湖作为木卫二模拟物的天体生物学潜力,进行了不同的水文地球化学、矿物学和微生物分析。实验和理论建模有助于理解木卫二地壳中可能发生的结晶途径。对假想的木卫二海洋氧化态的计算旨在支持富含硫酸盐的中性液体模型作为木卫二观测到的水合矿物的起源,并便于将其与蒂雷斯湖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,蒂雷斯湖的水相当于以泻利盐、六水泻盐和石盐为端元的镁 - 钠 - 硫酸根 - 氯卤水。初步的微生物生态学特征鉴定出两个不同的微生物域:一个以浮游/底栖形式和微生物垫群落为代表的光合维持群落,以及一个以化学无机营养为主导的地下厌氧区域。荧光原位杂交已被用于表征该系统的原核生物多样性。地下群落似乎以硫酸盐还原菌和产甲烷菌为主。通过傅里叶变换红外技术对冷冻的蒂雷斯湖卤水进行分析,得到的光谱与之前使用纯组分报告的光谱以及伽利略号光谱数据相似。对蒂雷斯湖卤水的量热测量显示了硫酸镁和氯化钠结晶的途径和相亚稳性,这可能有助于理解木卫二冰壳形成过程中涉及的过程。在高盐环境中使用荧光杂交技术进行微生物检测和表征,使得这种方法非常适合未来的木卫二天体生物学任务。

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