GSTDTAP  > 气候变化
DOI10.1029/2018GL081335
Indigenous Organic-Oxidized Fluid Interactions in the Tissint Mars Meteorite
Jaramillo, Elizabeth A.1,2; Royle, Samuel H.3; Claire, Mark W.4,5,6; Kounaves, Samuel P.1,3; Sephton, Mark A.3
2019-03-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2019
卷号46期号:6页码:3090-3098
文章类型Article
语种英语
国家USA; England; Scotland
英文摘要

The observed fall and rapid recovery of the Tissint Mars meteorite has provided minimally contaminated samples of the Martian surface. We report analyses of Tissint for organic compounds by pyrolysis-gas chromatography-mass spectrometry and for soluble salts by ion chromatography. Pyrolysis-gas chromatography-mass spectrometry analysis shows the presence of organic compounds similar to those in the Mars EETA79001 and Nakhla meteorites. The organic profile is dominated by aromatic hydrocarbons, including oxygen and nitrogen-containing aromatics, and sulfur-containing species including thiophenes. The soluble salts in Tissint are dominated by sulfate and various oxidation states of chlorine, including perchlorate. The organic compounds and salts in the soils from the Tissint recovery strewn field differ significantly from those found in Tissint suggesting minimal terrestrial contamination. Our results support the hypothesis that the soluble inorganic components of Tissint are most likely a result of indigenous fluid inclusion, thus providing a glimpse into the composition of early Martian fluids.


Plain Language Summary Meteorites that come from Mars usually become contaminated after landing on Earth. One Mars meteorite, named Tissint, was seen falling in the dry Moroccan desert, and many of its pieces were collected within months. We analyzed the meteorite and the local soil for organic compounds and soluble salts. We found differences between the Tissint meteorite and the local soil that suggest that Tissint is uncontaminated. The analyses also showed that the soluble salts in Tissint most likely came from Martian fluids that were similar to terrestrial seawater.


英文关键词Mars meteorite organics salts fluids
领域气候变化
收录类别SCI-E
WOS记录号WOS:000464650400009
WOS关键词MARTIAN METEORITE ; GALE CRATER ; MATTER ; SEARCH ; ORIGIN ; WATER ; SOIL ; PERCHLORATE ; PYROLYSIS ; COMPONENT
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/181756
专题气候变化
作者单位1.Tufts Univ, Dept Chem, Medford, MA 02155 USA;
2.CALTECH, Jet Prop Lab, Pasadena, CA USA;
3.Imperial Coll London, Dept Earth Sci & Engn, London, England;
4.Univ St Andrews, Sch Earth & Environm Sci, St Andrews, Fife, Scotland;
5.Univ St Andrews, Ctr Exoplanet Sci, St Andrews, Fife, Scotland;
6.Blue Marble Space Inst Sci, Seattle, WA USA
推荐引用方式
GB/T 7714
Jaramillo, Elizabeth A.,Royle, Samuel H.,Claire, Mark W.,et al. Indigenous Organic-Oxidized Fluid Interactions in the Tissint Mars Meteorite[J]. GEOPHYSICAL RESEARCH LETTERS,2019,46(6):3090-3098.
APA Jaramillo, Elizabeth A.,Royle, Samuel H.,Claire, Mark W.,Kounaves, Samuel P.,&Sephton, Mark A..(2019).Indigenous Organic-Oxidized Fluid Interactions in the Tissint Mars Meteorite.GEOPHYSICAL RESEARCH LETTERS,46(6),3090-3098.
MLA Jaramillo, Elizabeth A.,et al."Indigenous Organic-Oxidized Fluid Interactions in the Tissint Mars Meteorite".GEOPHYSICAL RESEARCH LETTERS 46.6(2019):3090-3098.
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