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anorganik tabiiy moddalarning asta-sekin murakkablashuvi hamda tiriklikning asosiy xususiyatlariga xos boʻlgan va, dastavval, ular yashashining zaruriy sharti boʻlgan modda almashish xususiyatiga ega biopolimerlar (nuklein kislotalar, oqsillar va b.) paydo boʻlishi yoʻli bilan hayotning kelib chiqish jarayoni (faraziy).

process (assumed) of origin of life with gradual evolution of matters into more complicated forms of inorganic nature and originating of biopolymers (nucleon acids, protein, etc.) which are characterized by the basic properties of living things and, first and foremost, by capacities to metabolism, as an indispensable condition of their existence.

tirik materiyaning deyarli taʼsirisiz vujudga kelgan landshaft. A.l. ga shartli ravishda (hayot Yer yuzining hamma joyida u yoki bu tarzda namoyon boʻlgani sababli) Antarktidaning markaziy qismi, Grenlandiya muz qalqoni, Himolayning eng baland choʻqqilari, lava koʻllari kiritiladi. A.l. tirik organizmlar taʼsirida shakllangan biogen landshaft bilan taqqoslanadi.

landscape formed without significant influence of living matter. It is conditionally agreed (as all earth surface is pierced to some extent by evidences of life) to rank among A.l. the landscapes of a central part of the Antarctic Continent, the Greenland ice board, the highest peaks of the Himalayas, lava lakes, etc. A.l. is contrasted with biogenic landscapes formed under the influence of living organisms.