Basiuk V A, Navarro-Gonzalez R
Laboratorio de Química de Plasmas y Estudios Planetarios, Instituto de Ciencias Nucleares, Universidad Nacional Autónoma de México, México.
Orig Life Evol Biosph. 1995 Oct;25(5):457-93. doi: 10.1007/BF01581996.
In the present review we analyze the available literature on the distribution of dust in the Universe, methods of its observation and determination of the chemical composition, and the roles for terrestrial prebiotic chemistry. The most plausible natural sources of dust on the Earth in the prebiotic era are sedimentation of interplanetary dust, meteoritic and cometary impacts, volcanic eruptions, and soil microparticulates; the interplanetary medium being among the most powerful supplier of the dust matter. Two fundamental roles of dust particles for the origins of life are considered: (1) catalytic formation of prebiotic compounds; and (2) delivery of organic matter to the Earth by space dust particles. Due to the fact that there is only approximate information on the chemical composition and properties of interstellar, circumstellar, and major part of interplanetary dust, even the simulating experiments are difficult to perform. Until these gaps are filled, it seems reasonable to focus efforts of the scientists dealing with dust-driven catalytic formation of prebiotically important compounds on the volcanic and meteoritic/cometary impact environments.
在本综述中,我们分析了关于宇宙中尘埃分布、其观测方法和化学成分测定以及对地球前生物化学作用的现有文献。前生物时代地球上最可能的尘埃自然来源是行星际尘埃的沉降、陨石和彗星撞击、火山喷发以及土壤微粒;行星际介质是尘埃物质最强大的供应源之一。尘埃颗粒对生命起源的两个基本作用被考虑在内:(1)前生物化合物的催化形成;(2)太空尘埃颗粒将有机物质输送到地球。由于关于星际、恒星周围和大部分行星际尘埃的化学成分和性质只有近似信息,甚至模拟实验都难以进行。在这些空白被填补之前,将致力于研究尘埃驱动的前生物重要化合物催化形成的科学家的精力集中在火山和陨石/彗星撞击环境上似乎是合理的。