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本文引用的文献

1
Identification of carotenoids in ancient salt from Death Valley, Saline Valley, and Searles Lake, California, using laser Raman spectroscopy.使用激光拉曼光谱法鉴定加利福尼亚州死亡谷、盐谷和瑟尔斯湖的古盐中的类胡萝卜素。
Astrobiology. 2013 Nov;13(11):1065-80. doi: 10.1089/ast.2012.0952.
2
The miniaturized Raman system and detection of traces of life in halite from the Atacama Desert: some considerations for the search for life signatures on Mars.小型化拉曼系统与对来自阿塔卡马沙漠盐矿中生命痕迹的探测:对在火星上寻找生命特征的一些思考。
Astrobiology. 2012 Dec;12(12):1095-9. doi: 10.1089/ast.2012.0879. Epub 2012 Nov 14.
3
Extremely halophilic archaea and the issue of long-term microbial survival.极端嗜盐古菌与微生物长期生存问题
Rev Environ Sci Biotechnol. 2006 Aug;5(2-3):203-218. doi: 10.1007/s11157-006-0007-y.
4
Investigation of biomolecules trapped in fluid inclusions inside halite crystals by Raman spectroscopy.利用拉曼光谱研究盐晶体中流体包裹体中捕获的生物分子。
Spectrochim Acta A Mol Biomol Spectrosc. 2011 Dec;83(1):288-96. doi: 10.1016/j.saa.2011.08.032. Epub 2011 Aug 26.
5
Microbial colonization of halite from the hyper-arid Atacama Desert studied by Raman spectroscopy.利用拉曼光谱研究来自极干旱阿塔卡马沙漠的盐矿中的微生物定殖。
Philos Trans A Math Phys Eng Sci. 2010 Jul 13;368(1922):3205-21. doi: 10.1098/rsta.2010.0059.
6
Molecular analysis of the microbial communities of Mars analog lakes in Western Australia.对澳大利亚西部火星模拟湖微生物群落的分子分析。
Astrobiology. 2009 Dec;9(10):919-30. doi: 10.1089/ast.2008.0293.
7
Halophilic Archaea cultured from ancient halite, Death Valley, California.从加利福尼亚州死亡谷的古代岩盐中培养的嗜盐古菌。
Environ Microbiol. 2010 Feb;12(2):440-54. doi: 10.1111/j.1462-2920.2009.02086.x. Epub 2009 Oct 16.
8
Microscopic identification of prokaryotes in modern and ancient halite, Saline Valley and Death Valley, California.加利福尼亚州盐碱谷和死亡谷现代与古代岩盐中 prokaryotes 的微观鉴定
Astrobiology. 2009 Jun;9(5):467-82. doi: 10.1089/ast.2008.0282.
9
Fluorescence microscopy as a tool for in situ life detection.荧光显微镜作为一种用于原位生命检测的工具。
Astrobiology. 2008 Aug;8(4):859-74. doi: 10.1089/ast.2007.0043.
10
"Hairy blobs:" microbial suspects preserved in modern and ancient extremely acid lake evaporites.“毛团”:保存在现代和古代极酸性湖泊蒸发岩中的可疑微生物
Astrobiology. 2008 Aug;8(4):807-21. doi: 10.1089/ast.2006.0034.

来自西澳大利亚马奇湖盐卤中的包裹体中的嗜酸嗜盐微生物。

Acidophilic halophilic microorganisms in fluid inclusions in halite from Lake Magic, Western Australia.

机构信息

1 Department of Earth and Atmospheric Sciences, Central Michigan University , Mt. Pleasant, Michigan.

出版信息

Astrobiology. 2013 Sep;13(9):850-60. doi: 10.1089/ast.2012.0956. Epub 2013 Aug 24.

DOI:10.1089/ast.2012.0956
PMID:23971647
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3778947/
Abstract

Lake Magic is one of the most extreme of hundreds of ephemeral acid-saline lakes in southern Western Australia. It has pH as low as 1.7, salinity as high as 32% total dissolved solids, temperatures ranging from 0°C to 50°C, and an unusually complex aqueous composition. Optical petrography, UV-vis petrography, and laser Raman spectrometry were used to detect microorganisms and organic compounds within primary fluid inclusions in modern bedded halite from Lake Magic. Rare prokaryotes appear as 1-3 μm, bright cocci that fluoresce green with UV-vis illumination. Dimpled, 5-7 μm yellow spherules that fluoresce blue with UV-vis illumination are interpreted as Dunaliella algae. Yellow-orange beta-carotene crystals, globules, and coatings are characterized by orange-red fluorescence and three distinct Raman peaks. Because acid saline lakes are good Mars analogues, the documentation of prokaryotes, eukaryotes, and organic compounds preserved in the halite here has implications for the search for life on Mars. Missions to Mars should incorporate such in situ optical and chemical examination of martian evaporites for possible microorganisms and/or organic compounds in fluid inclusions.

摘要

玛琪湖是澳大利亚西南部数百个瞬间性酸盐湖中最极端的一个。它的 pH 值低至 1.7,盐度高达 32%总溶解固体,温度范围从 0°C 到 50°C,水的组成非常复杂。使用光学岩相学、紫外可见岩相学和激光拉曼光谱法来检测现代玛琪湖床状盐中初生流体包裹体中的微生物和有机化合物。罕见的原核生物呈 1-3μm 的亮球菌,在紫外可见光照下发出绿色荧光。用紫外可见光照亮的有麻点的 5-7μm 的黄色小球被解释为杜氏盐藻。黄色橙色的β-胡萝卜素晶体、小球和涂层的特征是橙红色荧光和三个明显的拉曼峰。由于酸性盐湖是火星的良好模拟物,因此这里的盐中保存的原核生物、真核生物和有机化合物的记录对在火星上寻找生命具有重要意义。火星任务应该包括对火星蒸发岩进行这种原位光学和化学检查,以寻找可能存在于流体包裹体中的微生物和/或有机化合物。