火星探测计划
天体生物学
有机质
火星人
撞击坑
碳纤维
环境化学
有机分子
热解
化学
地质学
环境科学
地球科学
有机化学
分子
材料科学
复合材料
物理
复合数
作者
J. L. Eigenbrode,Roger E. Summons,A. Steele,Caroline Freissinet,M. Millán,R. Navarro‐González,B. Sutter,A. C. McAdam,H. B. Franz,D. P. Glavin,P. D. Archer,P. R. Mahaffy,P. G. Conrad,J. A. Hurowitz,J. P. Grotzinger,Sanjeev Gupta,Doug Ming,D. Y. Sumner,Cyril Szopa,C. A. Malespin
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2018-06-07
卷期号:360 (6393): 1096-1101
被引量:492
标识
DOI:10.1126/science.aas9185
摘要
Measuring martian organics and methane The Curiosity rover has been sampling on Mars for the past 5 years (see the Perspective by ten Kate). Eigenbrode et al. used two instruments in the SAM (Sample Analysis at Mars) suite to catch traces of complex organics preserved in 3-billion-year-old sediments. Heating the sediments released an array of organics and volatiles reminiscent of organic-rich sedimentary rock found on Earth. Most methane on Earth is produced by biological sources, but numerous abiotic processes have been proposed to explain martian methane. Webster et al. report atmospheric measurements of methane covering 3 martian years and found that the background level varies with the local seasons. The seasonal variation provides an important clue for determining the origin of martian methane. Science , this issue p. 1096 , p. 1093 ; see also p. 1068
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