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地球上和火星上的趋磁细菌。

Magnetotactic bacteria on Earth and on Mars.

作者信息

McKay Christopher P, Friedmann E Imre, Frankel Richard B, Bazylinski Dennis A

机构信息

Space Science Division, NASA Ames Research Center, Moffett Field, California 94035, USA.

出版信息

Astrobiology. 2003 Summer;3(2):263-70. doi: 10.1089/153110703769016361.

Abstract

Continued interest in the possibility of evidence for life in the ALH84001 Martian meteorite has focused on the magnetite crystals. This review is structured around three related questions: is the magnetite in ALH84001 of biological or non-biological origin, or a mixture of both? does magnetite on Earth provide insight to the plausibility of biogenic magnetite on Mars? could magnetotaxis have developed on Mars? There are credible arguments for both the biological and non-biological origin of the magnetite in ALH84001, and we suggest that more studies of ALH84001, extensive laboratory simulations of non-biological magnetite formation, as well as further studies of magnetotactic bacteria on Earth will be required to further address this question. Magnetite grains produced by bacteria could provide one of the few inorganic traces of past bacterial life on Mars that could be recovered from surface soils and sediments. If there was biogenic magnetite on Mars in sufficient abundance to leave fossil remains in the volcanic rocks of ALH84001, then it is likely that better-preserved magnetite will be found in sedimentary deposits on Mars. Deposits in ancient lakebeds could contain well-preserved chains of magnetite clearly indicating a biogenic origin.

摘要

对ALH84001火星陨石中存在生命证据可能性的持续关注集中在磁铁矿晶体上。本综述围绕三个相关问题展开:ALH84001中的磁铁矿是生物起源、非生物起源还是两者的混合物?地球上的磁铁矿能否为火星上生物成因磁铁矿的合理性提供见解?趋磁现象是否可能在火星上发展?关于ALH84001中磁铁矿的生物起源和非生物起源都有可信的论据,我们认为需要对ALH84001进行更多研究、对非生物磁铁矿形成进行广泛的实验室模拟,以及对地球上的趋磁细菌进行进一步研究,以进一步解决这个问题。细菌产生的磁铁矿颗粒可能是火星过去细菌生命留下的少数无机痕迹之一,这些痕迹可以从地表土壤和沉积物中找到。如果火星上存在足够丰富的生物成因磁铁矿,从而在ALH84001的火山岩中留下化石遗迹,那么很可能在火星的沉积矿床中会发现保存得更好的磁铁矿。古代湖床中的沉积物可能含有保存完好的磁铁矿链,清楚地表明其生物成因。

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