Ok .. so I still agree that Seager's Earth-example-centric hypothesis, seems to have a problem around this point.In the 45-75km altitude range the H₂SO₄ concentration is 73-98%.
H₂SO₄ is produced in the Venusian atmosphere via the following reactions.
CO₂ → CO + O (photo-disassociation of CO₂ by photons.)
SO₂ + O → SO₃
2SO₃ + 4H₂O → 2H₂SO₄. H₂O
Furthermore H₂SO₄ is hygroscopic and its concentration is a function of the amount of H₂O absorbed.
Even at 70% concentration H₂SO₄ is highly corrosive to most organic matter so rather than reactivating the bacterium inside the spore it would seem more likely to destroy it.
So, {'achem' .. throat clearing sound here}; let me wave my magic speculation wand (and wickedly, deliberately, shift the goalposts in order to get my way ) and invoke surface Abiogenesis, followed by an organism evolving over time and adapting to increasing concentrations of sulphuric acid, (and escaping water), and then becoming an airborne spore.
(Ie: @FrumiousBandersnatch's idea has now been changed from panspermia to naturally Venusian evolved).
From: 'Acidophile', it appears that some of our earthly ones have adapted ways of keeping their cytoplasm at a neutral pH, even when immersed in an acidic environment. Others have acidic cytoplasm, and special proteins that contain H+ ions.
So, our Venusian organic chemistry is basically now acidic (with variations in concentrations, thereof):
Will that work as a substitute hypothesis?.. other acidophiles, such as Acetobacter aceti, have an acidified cytoplasm which forces nearly all proteins in the genome to evolve acid stability. For this reason, Acetobacter aceti has become a valuable resource for understanding the mechanisms by which proteins can attain acid stability.
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