摘要
提出了一种假说:地球生物信息起源于海陆交界处的一种次生粘土矿物——蒙脱石〔(OH)4Al4Si8O20〕.在初始生物信息形成后,其数量经算术级数和几何级数增长,发展成为今天丰富的生物信息资源,文中还就相关问题进行了讨论.
A hypothesis was described in the paper as follows; biological information on the earth originated from the montmorillonite〔(OH)\-4Al\-4Si\-8O\-\{20\}〕 that was a kind of secondary clay mineral on the juncture of the sea and the land. After the emergence of elementary biological information, the biological information content increasd and evolved into rich biological information resources of today by way of arithmetic progression and geometric progression. Some problems were also disscussed in this paper.
出处
《甘肃科学学报》
2003年第4期34-39,共6页
Journal of Gansu Sciences
关键词
岩石风化
次生粘土矿物
蒙脱石
初始生物信息
类生命物体
类生命体
生命体
生物信息
rock efflorescence
secondary clay mineral
montmorillonite
elementary biological information
quasi-life substance
quasi-life body
organism
biological information.
