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Survival of microbial life under shock compression: implications for Panspermia

机译:休克压缩下微生物生命的生存:对紫精的影响

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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:对暴露于极端冲击压力下的微生物的存活率进行了分析。在此分析中使用了各种数据源。关键发现是存活取决于细胞壁的行为。在临界冲击压力以下,随着冲击压力的增加,生存率会相对缓慢下降。高于临界阈值时,随着冲击压力的进一步增加,生存率开始迅速下降。此处发现的临界冲击压力在2.4至20 Gpa的范围内,不仅因生物而异,还取决于给定生物的生长阶段,其中饥饿(即无生长)状态有利于生存。在岩石材料的行星际转移所涉及的典型冲击压力下,发现生存分数很小但很有限。这使Panspermia的想法可信,即生活可能会自然地在太空中迁移。因此,例如,火星陨石由于经历了冲击过程,因此不应被认为是无菌的,但由于它们缺乏生存的微生物,或者反映出出发时没有这种生命存在,也没有受到影响。其他有害过程,例如进入行星大气期间的空间辐射或表面加热。

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