The Micro-Cauldron of Life?
May 30th, 2007 Placozoan
THE QUESTION of the origin of the first living organism has fascinated scientists for decades. Currently the RNA world hypothesis, which proposes RNA as the first self-reproducing molecule, is the most promising. One difficulty is that this hypothesis require a high concentration of simple organic molecules, which were probably present in low concentrations in the earliest oceans. Some suggest adsorption onto solid surfaces as one solution to this problem, now a new solution has been proposed.
There are some hypotheses that the earliest life evolved around hot springs in the ocean floor, which now harbor unusual eubacteria and archaea. These hot springs build up mineral mounds around them that are riddled with pores. Baaske and coworkers demonstrate that a simulated hydrothermal pore system under a thermal gradient (from hot spring to cold ocean) can concentrate small molecules including nucleotides up to 108 times, a hundred times higher than needed for intermolecular interaction.
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