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Survival of microbial life under shock compression: implications for Panspermia

机译:缓冲压缩下微生物生活的存活:对粉虱的影响

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An analysis is carried out of the survival fraction of micro-organisms exposed to extreme shock pressures. A variety of data sources are used in this analysis. The key findings are that survival depends on the behaviour of the cell wall. Below a critical shock pressure there is a relatively slow fall in survival fraction as shock pressures increase. Above the critical threshold survival starts to fall rapidly as shock pressure increases further. The critical shock pressures found here are in the range 2.4 to 20 Gpa, and vary not only from organism to organism, but also depend on the growth stage of given organisms, with starved (I.e., no growth) states favoured for survival. At the shock pressures typical of those involved in interplanetary transfer of rocky materials, the survival fractions are found to be small but finite. This lends credence to the idea of Panspermia, I.e. life may naturally migrate through space. Thus for example, Martian meteorites should not a prior be considered as sterile due to the shock processes they have undergone, but their lack of viable micro-organisms either reflects no such life being present at the source at the time of departure or the influence of other hazardous processes such as radiation in space or heating of surfaces during entry into a planetary atmosphere.
机译:将微生物的存活部分进行分析,暴露于极端震动压力。在该分析中使用各种数据源。关键发现是存活取决于细胞壁的行为。低于临界冲击压力,在震动压力增加时,存活率较差的较慢较慢。在临界阈值存活率上方开始迅速下降,因为冲击压力进一步增加。这里发现的临界休克压力在2.4至20GPa的范围内,不仅可以从生物体到生物体,而且取决于给定生物的生长阶段,饥饿(即没有生长)的生存。在诸如涉及岩石材料的行星际转移的人的震动压力下,发现存活级分是小但有限的。这将归功于Panspermia的想法,即生命可以自然地通过空间迁移。因此,例如,由于休克过程,Martian Meteorites不应该被认为是因为它们经历的休克过程而被认为是无菌的,但它们缺乏可行的微生物的缺乏反映在出发时不会在源处存在的寿命或影响其他危险过程,例如在进入行星气氛中的空间或表面加热的辐射或加热。

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