确认微生物从太空进入

N. Wickramasinghe, M. Rycroft, D. Wickramasinghe, D. Wallis, R. Temple, G. Tokoro, A. Syroeshkin, T. Grebennikova, O. Tsygankov, Millington Road Cambridge Cb Hw Uk. Caesar Consultancy, Moscow Russian Federation Microbiology named Gamalei, Korolev Rocket
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引用次数: 3

摘要

俄罗斯研究人员(Grebennikova et al., 2018)在2013年至2017年期间多次在国际空间站(ISS)外表面发现微生物,这可能被解释为支持Hoyle-Wickramasinghe彗星泛种论的证据。国际空间站恢复的基因型与已知陆地细菌之间的同源性可以被视为跨越天文距离的生物圈内共同进化和基因转移(HGT)的证据。一方面,国际空间站400公里的轨道高度可能会被认为对地表微生物来说太高了。然而,有一种理论声称可以解释小粒子从对流层进入平流层下层和电离层的可能运输,这是由于涡旋运动和垂直流(飘带)的结果,这是电离层等离子体调制不稳定性发展的结果。需要更多的研究来正确评估这一建议。
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Confirmation of Microbial Ingress from Space
The discovery by Russian researchers (Grebennikova et al., 2018) of microorganisms on the exterior surface of the International Space Station (ISS) on several occasions between 2013 and 2017 may be interpreted as evidence supporting the Hoyle-Wickramasinghe theory of cometary panspermia. The homologies between the ISS-recovered genotypes and known terrestrial bacteria can be seen as evidence of co-evolution and gene transfers (HGT) within a biosphere that spans astronomical distances. On the one hand, the height of the ISS orbit at 400km can be argued as being too high for lofting surface microorganisms. However, there is a theory that purports to explain the possible transport of small particles from the troposphere into the lower stratosphere and ionosphere as a result of vortex motions as well as vertical flows (streamers), which are generated as a result of the development of the modulational instability in the ionospheric plasma. More research is needed to properly evaluate this proposal.
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