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ot Organizmlarda hayotiy jarayonlarni taʼminlashda ishtirok etishi faraz qilingan ozuqa moddasi.

ot Tirik mavjudotlar Yerda anorganik materiyadan paydo boʻlganligini inkor etuvchi qarash, nazariya.

process of formation of organic compounds by living organisms. A theory of B. denies a concept of origin of life on the Earth as a result of generation of living things from a lifeless matter. A basic idea of B. lays in opposing of the living things from the lifeless substance and idea of eternity of life.

organizmlar hayotiy faoliyati natijasida vujudga kelgan kimyoviy birikma (lekin aynan shu vaqtning oʻzida ularning jismi tarkibida boʻlmasligi ham mumkin).

asosan qirilib ketgan hayvonlar (zoogen), oʻsimliklar (fitogen) va ularning hayotiy faoliyati mahsulotlaridan tarkib topgan togʻ jinslari.

rocks composed basically of oddments of extinct fauna (zoogenical), flora (phytogenical) and products of their vital functions.

a chemical compound formed as a result of living functions of organisms (but it is not necessarily contained in composition of their bodies at present time).

tirik organizmlar tarkibiga shaksiz kiradigan kimyoviy elementlar.

tirik modda tomonidan vujudga keltirilib, u bilan bogʻliq boʻlgan jarayonlar (mas. biogen aylanish).

chemical elements which are essentially contained in composition of living organisms.

processes generated by a living matter and related to it. (e.g., biogenic cycle).

ot Abiogenezga aloqador, u bilan bogʻliq.

ot Hayotning anorganik moddalar bora-bora murakkablashib borishi oqibatida yuzaga kelganini taʼkidlovchi nazariya.

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.