THE ONSET OF LIFE IS A COROLLARY OF CONVECTION ON EARLY EARTH
The mounds are negative electrodes. The Earth is a giant photoelectric cell. The ocean is the electrolyte. The ferric iron is eddy-pumped to the ocean bottom. The iron sulfide/hydroxide bubbles inflate fitfully. Though the hydrothermal solution is trapped, there is some escape of electrons, from hydrogen and methane through the conducting layers of mackinawite (~FeS), drawn to reduce the ferric iron. Now activated, the hydrogen and methane take part in further extempore chemosynthesis. Nucleotides poison the mackinawite but spell the password to a coevolutionary future. The side chains of particular amino acids register to fitting nucleotide triplet clefts. The amino acids are polymerised to form alpha chains by invading protons, making short protopeptides. Some sequester [4Fe-4S] to become protoferredoxins. Peptides, the would-be outer bands of mackinawite, continually spall away from bound RNA (the penultimate layer), driven by the protonmotive force.
This circuitry offers a continuous supply of proticity and electricity at a voltage appropriate for the onset of life. Life may then decouple from the hydrothermal system and individuate. Contention ensues. The chirality war looms. Photosynthesis beckons.