Page 64 - The Final Appeal to Mankind
P. 64

«The Final Appeal to Mankind» by Nicolai Levashov

            appear, which, upon amassing organic substance, begin dividing on their own. Now
            eight identical cells are created, then sixteen, thirty-two, sixty-four, and so on. As a

            result, the growth rate of monocellular organisms unfolds in geometrical progression.

            For purposes of definition we will call organisms which synthesize organic substances
            through photosynthesis “vegetable organisms.” The growth rate of the amount of
            the simplest of these  —  phytoplankton  —  is defined by a biological efficiency
            factor  (BEF).  This  refers  to  that  portion  of  sunlight  per  square  unit  of  the
            organism’s surface, which is absorbed and utilized for the synthesis of organic

            substances.

            For  phytoplankton  the  BEF  is  2-3  %.  The  absorption  of  sunlight  is  a  necessary
            condition for photosynthesis. However, sunlight does not penetrate more than 300 feet
            below the surface of the primeval ocean. Therefore, phytoplankton only actively grows
            close to the ocean’s surface, gradually producing a solid carpet of growth. (A given
            area  of  ocean  surface  exposed  to  sunlight  can  support  only  a  limited  amount  of

            phytoplankton).  The  motion  of  water  at  the  surface  transports  some  of  the
            phytoplankton to the lower depths, where the sunlight either does not penetrate or is
            insufficient to support the life of monocellular plants. They cannot move on their own
            and depend completely on the circulation of the water. Most of the phytoplankton die
            because of the above conditions, creating a large mass of organic substance during the
            disintegration process. Yet, some of the organisms that were able to adapt to the new
            conditions  accumulated  organic  substances  from  the  environment  rather  than

            synthesizing them from the surrounding sea water. When, however, they were able to
            return to the sunlit surface of the ocean, these organisms again began to synthesize
            organic substances. Such organisms have survived to the present day.

            The  best-known  representative  of  monocellular  organisms  with  dual  means  of
            obtaining organic substance is the Green Euglena (F Fi ig g. .   2 24 4).


































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