It
has long been suspected that the progenitor of life on planet earth most likely
came from the sea. It has been proposed
that the possible origins of life could have been in shallow pools or under
more extreme conditions such as within deep-sea vents or proximal to active volcanoes.
The
current domains of life consist of bacteria –prokaryotes, the archaea -found in
deep sea vents and the eukaryotes that comprise all the animal and plant life
on the planet. It has also been proposed
that the archaea and the bacteria preceded the more complex eukaryotic cell
type.
William
F. Martin, an evolutionary biologist, from Heinrich Heine University in
Düsseldorf, Germany, focused his research efforts on finding the progenitor of
archaea and bacteria. To do this, the
known genetic structure of members of the archaea and bacteria domains were
extensively examined. This involved the examination
of some six million genes representing thousands of microbes.
From
these data, Martin and his colleagues were able to construct evolutionary
family trees and were able to deduce that 355 gene families originated from
single cell bacteria-like organism. That
organism is referred to as the Last Universal Common Ancestor (LUCA). Furthermore, it is believed that LUCA lived
some four billion years ago when the young earth was barely 500 million years
old.
If
this conclusion is correct, it clearly proposes that life began very early in
the evolution of the planet earth and that the evolution of life was a much
longer process than previously envisioned.
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