[QUOTE=CalMeacham]
It depends. For years scientists believed that life first formed in early shallow seas, with a primive atmosphere without free oxygen and with plentiful UV light. But more recently, with what’s been leatrned of thermal vents, there’s been speculation that life began near such vents, and may be continuing today.
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That is debatable. So-called archaebacteria have a wide range of morphology and intercellular mechanisms, and many have substantial similarities to more complex eukaryotic organisms, leaving many molecular biologists to conclude that at least some archaea are degenerate forms of eukayote predecessors. Archaea aren’t just found in deep ocean vents and the like; you can also find them up at the surface in extreme environments that are antipathetic to “normal” life, such as in natural or artificial acidic tailings, or sulphurous geological vents, and they can also be found in more habitable conditions like oceans or marshes where energy is sufficient that they can successfully compete with other organisms. It is possible that some form of what we would today classify as Archaea were the first “complex” life, but the most likely hypothesis (but by no means evidentially factual) is that the first organisms developed from crystalline templates and then became self-replicating by some kind of adaptive recombination process.
As for biogenesis occurring today, it could certainly be happening. However, there are at least two and perhaps more major strikes against protolife developing independently. The first is competition; life is all about using energy gradients for respiration and replication, and a more developed, better adapted organism will tend to push out a newer, less adapted one. Given that life already exists in unimaginable multitude in every nook and cranny, it would be difficult for neolife to get a toehold.
The other problem is oxygen; the primordial atmosphere of Earth was full of relatively gentle, mostly nonvalent complete hydrocarbons like methane and ethane. These are fairly easy to “crack” for energy, but as long as you leave them alone that don’t go nipping away at your trailing ions. However, the modern atmosphere is 21% oxygen, an extremely reactive element which readily and sometimes spontaneously causes violently energetic redox reactions. Imagine, there you are, a new organism casually trying to pry a hydrogen away from a molecule of methane, and all of a sudden comes some free oxygen bully, grabbing your hydrogen and zapping you with a hot photon for your trouble. It’s just not worth it, really. Oxygen is a very dangerous toxin to simple life that has yet to build protective boundaries, and would probably prevent the formation of simple organisms from basic amino acids.
There may be other factors, including the relative transparency of air to UV (which kills simple organisms quickly when exposed), the lack of occasional but strong mutagenic sources, et cetera. It is also quite possible, as the o.p. notes, that biologists wouldn’t even recognize the process if they observe it, especially since it would probably look like random contamination to a valid experiment unless you were specifically looking for it.
The big question is, do the conditions and processes that led to the origin of life on Earth occur elsewhere, to what extent, and how linearizable are those processes, i.e. can we reasonably expect them to be naturally replicated elsewhere? Setting aside Star Trek fans and SETI advocates, this is really the interesting and probably (at this point) unanswerable question in the metaphysics of biology; are we really all alone out here?
Stranger