黄铁矿
石炭纪
地质学
沉积岩
二叠纪
地球化学
自然发生
矿物学
古生物学
天体生物学
生物
构造盆地
作者
Michael J. Russell,A. J. Hall,Dugald Turner
出处
期刊:Terra Nova
[Wiley]
日期:1989-05-01
卷期号:1 (3): 238-241
被引量:132
标识
DOI:10.1111/j.1365-3121.1989.tb00364.x
摘要
ABSTRACT Iron monosulphide globules and tubes grown in the laboratory have similar morphologies to the fossil pyrite botryoids and chimneys found in the Silvermines exhalative sedimentary ore‐body of Carboniferous age in Ireland. We envisage analogous fine structures growing at hot springs (100–200°C) in the earliest oceans as having provided the culture chambers and flow reactors for life to originate by phosphorylation and growth of organic molecules on the iron sulphide surfaces. Such sulphide structures grown in the laboratory could be used in origin‐of‐life experiments.
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