| Chapter Five |
The origin
of life
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125
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Unfortunately,
however, clays can only favour an accumulation of pre-existing molecules,
not the in situ develoment of two-dimensional organic systems,
because their negative charges repel the negative charges of amino acids
and nucleic acids. This is why Wächtershäuser proposed that surface metabolism
developed on positively-charged minerals, and in particular on crystals
of iron pyrite (FeS2).
“Postchemical” evolution The
first scientific theories on the origin of life were proposed independently
by Alexander Oparin in 1924 and by J.B.S. Haldane in 1929. Oparin discovered
that a solution of proteins can spontaneously produce microscopic aggregates
– which he called coacervates – that are capable of a bland metabolism,
and proposed that the first cells came into being by the evolution of
primitive metabolic coacervates. Haldane, on the other hand, was highly
impressed by the replication properties of viruses, and attributed the
origin of life to the evolution of virus-like molecular replicators.
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