Respuesta :
The first stage of the origin of life on earth was the formation of carbon and hydrogen-containing macromolecules.
An organic microsystem must leave its current stable state in the first stage of the succession due to a considerable change in the external conditions before transitioning to a new stable state via the unstable critical (bifurcation) point. The microsystem gains the original characteristics necessary for life to exist at the bifurcation point (self-maintaining heterogeneous structure, incessant fluctuations, rearrangement of molecules, exchange with the surroundings by matter and energy, etc.). Through balanced oscillations around the bifurcation point, its unstable state stabilizes somewhat during the second stage, giving rise to the paradoxical state of "stabilized instability."
The network of chemical processes undergoes a fundamental change in the third stage, as the contribution from free energy starts to outweigh that from entropy. The ability to focus free energy and information, enhanced resistance to outside stimuli, expeditious behavior, and persistent self-improvement are the essential characteristics of biological organization that emerge at this stage. Such successive transformations of biological matter took place in the fluid hydrothermal medium of the early Earth. New approaches are proposed for theoretical and experimental inquiry in the area of the beginning of life.
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