Origin of life on earth
How did life originate
· The only serious
hypothesis entertained by scientists is that life evolved spontaneously by
a process of chemosynthesis.
· This idea of spontaneous
generation from nonliving matter was first postulated by the Russian scientist A.J.
Oparin and the English scientist J.B.S. Haldane.
· According to this
hypothesis over a long period of time inorganic chemicals on the surface of the
earth were transformed into simple organic chemicals in shallow pools of water.
These organic chemicals in turn aggregated into more complex units. Long polymers
of amino acids and nucleotides could have been part of these complex
microscopic structures. Ability to replicate themselves and catalyze various
chemical reactions would have made these structures the most primitive living
things.
· Because RNA could store and
transmit hereditary information and also catalyze some chemical reactions
scientists believe that RNA rather than DNA might have been the genetic
material of the earliest organisms.
· There is evidence that simple
organic compounds could have been produced from inorganic matter without
the activities of living things. Alcohols, sugars. amino acids and nitrogen
bases have been extracted from the interior of meteorites.
· Experimental evidence for
the origin of organic compounds from inorganic substances was demonstrated by
S. Miller in 1953. He allowed steam to interact with reducing chemicals such as
methane, hydrogen and ammonia in a closed container.
· Earlier earth conditions:
There was no free molecular oxygen and the atmosphere was anaerobic. The surface of the
earth was reducing
because of the presence of such reducing substances as hydrogen sulphide,
methane and ammonia. Temperature in the prebiotic environment was very high,
perhaps about 500°C. There was abundant water vapour and high pressure.
· Later conditions on
earth: During the course of evolution of life
chlorophyll a evolved in some organisms. Only at this stage light energy from
the sun was used to split water and release free oxygen as waste product. Over
long periods oxygen accumulated and transformed the atmosphere into an oxidising
one. Oxygen could then be used in respiration to release more energy and this
was partly responsible for the evolution of structurally more complex
organisms.
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