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首页> 外文期刊>Astrobiology >Ancient Sedimentary Structures in the < 3.7 Ga Gillespie Lake Member, Mars, That Resemble Macroscopic Morphology, Spatial Associations, and Temporal Succession in Terrestrial Microbialites
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Ancient Sedimentary Structures in the < 3.7 Ga Gillespie Lake Member, Mars, That Resemble Macroscopic Morphology, Spatial Associations, and Temporal Succession in Terrestrial Microbialites

机译:小于3.7 Ga的Gillespie湖成员火星中的古代沉积结构,类似于宏观形态,空间协会和陆生微生物岩的时间演替

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摘要

Sandstone beds of the <3.7 Ga Gillespie Lake Member on Mars have been interpreted as evidence of an ancient playa lake environment. On Earth, such environments have been sites of colonization by microbial mats from the early Archean to the present time. Terrestrial microbial mats in playa lake environments form microbialites known as microbially induced sedimentary structures (MISS). On Mars, three lithofacies of the Gillespie Lake Member sandstone display centimeter- to meter-scale structures similar in macroscopic morphology to terrestrial MISS that include "erosional remnants and pockets," "mat chips," "roll-ups," "desiccation cracks," and "gas domes." The microbially induced sedimentary-like structures identified in Curiosity rover mission images do not have a random distribution. Rather, they were found to be arranged in spatial associations and temporal successions that indicate they changed over time. On Earth, if such MISS occurred with this type of spatial association and temporal succession, they would be interpreted as having recorded the growth of a microbially dominated ecosystem that thrived in pools that later dried completely: erosional pockets, mat chips, and roll-ups resulted from water eroding an ancient microbial mat-covered sedimentary surface; during the course of subsequent water recess, channels would have cut deep into the microbial mats, leaving erosional remnants behind; desiccation cracks and gas domes would have occurred during a final period of subaerial exposure of the microbial mats. In this paper, the similarities of the macroscopic morphologies, spatial associations, and temporal succession of sedimentary structures on Mars to MISS preserved on Earth has led to the following hypothesis: The sedimentary structures in the <3.7 Ga Gillespie Lake Member on Mars are ancient MISS produced by interactions between microbial mats and their environment. Proposed here is a strategy for detecting, identifying, confirming, and differentiating possible MISS during current and future Mars missions. Key Words: Astrobiology-Life on Mars-Microbial mats-MISS-Biosignature-Curiosity rover. Astrobiology 15, 169-192.
机译:火星上<3.7 Ga Gillespie Lake Member的砂岩床被解释为古代普拉亚湖环境的证据。在地球上,从太古代开始到现在,这样的环境一直是微生物垫的定居点。普拉亚湖环境中的陆地微生物垫形成称为微生物诱导沉积结构(MISS)的微生物。在火星上,吉莱斯皮湖成员砂岩的三个岩相显示出厘米到米级的结构,其宏观形态与陆地MISS相似,包括“侵蚀性残留物和凹穴”,“垫屑”,“卷起”,“干燥裂缝, ”和“气体圆顶”。在“好奇号”漫游者任务图像中识别出的微生物诱导的沉积样结构没有随机分布。相反,发现它们以空间关联和时间顺序排列,表明它们随时间变化。在地球上,如果这种MISS发生在这种类型的空间关联和时间顺序上,那么它们将被解释为记录了一个以微生物为主导的生态系统的生长,该生态系统在后来完全干燥的水池中蓬勃发展:侵蚀袋,垫屑和卷起物由于水侵蚀了古老的微生物垫覆盖的沉积表面而导致的;在随后的水位下降过程中,通道将切入微生物垫的深处,留下侵蚀残留物;在微生物垫的空中暴露的最后阶段会发生干燥裂纹和气顶。在本文中,火星上的沉积物与地球上保存的MISS的宏观形态,空间联系和时间序列的相似性导致了以下假设:火星上<3.7 Ga Gillespie Lake Member的沉积结构是古老的MISS。由微生物垫与其环境之间的相互作用产生。本文提出了一种在当前和未来的火星任务期间检测,识别,确认和区分可能的MISS的策略。关键词:天体生物学,火星上的生命,微生物垫,MISS,生物特征,好奇号流浪者。天体生物学15,169-192。

著录项

  • 来源
    《Astrobiology》 |2015年第2期|169-192|共24页
  • 作者

    Noffke Nora;

  • 作者单位

    Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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