α-hydroxy acids and α-amino acids can form at hydrothermal temperatures
Hydrothermal vent temperatures would decompose organic compounds
Extreme thermophiles cannot protect against hydrolysis and degradation at high temperatures
Due to the accumulation of formamide in hydrothermal pores, prebiotic nucleobases can form
Around the origin of life, hydrogen cyanide (HCN) would not have been present in hydrothermal vents because they are too hot to have sufficient concentrations of HCN to form polymers
Alkaline hydrothermal vent conditions could have driven prebiotic chemistry and caused the divergence of bacteria and archaea
β-amino acids are more likely to be produced near hydrothermal vents rather than α-amino acids, when subjected to simulated primitive Earth conditions
Protein envelopes were constructed from amino acids under simulated primitive earth conditions and held at high temperatures
Consecutive stages in prebiological chemical evolution might have occurred in dry phases, instead of wet phases like those around hydrothermal vents
Protocell structures could have been rapidly produced in hydrothermal vents as soon as they formed in the Archean oceans