Alexander Ivanovich Oparin |
Around
the same time, a British-Indian biologist J. B. S. Haldane (John
Burdon Sanderson Haldane) had concluded the primordial soup
hypothesis as follows:
>>
The early Earth had a chemically reducing atmosphere.
>>
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.
>>
By further transformation, more complex organic polymers and
ultimately life would developed in the soup.
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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