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Alexander Ivanovich Oparin |
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Around
the same time, a British-Indian biologist J. B. S. Haldane (John
Burdon Sanderson Haldane) had concluded the primordial soup
hypothesis as follows:
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The early Earth had a chemically reducing atmosphere.
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This atmosphere exposed to energy in various forms led to the
production of simple organic compounds like monomers.
>>
These compounds accumulated in a “soup” that may have concentrated
at various locations like shorelines, oceanic vents.
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By further transformation, more complex organic polymers and
ultimately life would developed in the soup.
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J. B. S. Haldane |
Haldane
also suggested that our Earth's prebiotic oceans were very different
from what the oceans are now; that prebiotic oceans would have formed
a “hot dilute soup” in which organic compounds could have formed.
This idea was called “Biopoiesis” which means the process of
living matter evolving from self-replicating but non-living
molecules.
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