Beilstein J. Org. Chem.2017,13, 620–624, doi:10.3762/bjoc.13.60
hydrothermalfields associated with volcanic landmasses. These are considered as alternative hypotheses and the accumulating weight of evidence for each site is described and analyzed.
Keywords: hydrothermalfields; hydrothermal vents; origin of life; polymerization by condensation; protocells; Introduction
volcanic land masses.
The water accumulates in hydrothermalfields that undergo cycles of evaporation and refilling.
During evaporation, dilute solutes in the water become concentrated films on mineral surfaces.
If the solutes can undergo chemical or physical interactions, they will do so in the
concentrated films.
The products will accumulate in the pools when water returns either in the form of precipitation or as fluctuations in water levels related to hot springs or geyser activity.
Conjecture: life originated in fresh water hydrothermalfields associated with volcanic land masses, then adapted to