Originally posted by Omnislash
Actually, you bring up a point I am interested in. I must admit my ignorance on this one, and thusly would appreciate input.
Formost, in a vast pimordial ocean, wouldn't the oxygen in the ocean (which would be vastly more than today, yes?) interact with the developing building blocks of life (amino acids, sugars, purines, etc.)?
I am also concerned ...[text shortened]... rt trying to promote my perspecite. Just a guy trying to learn. ๐
Best Regards,
Omnislash
Omnislash,
Always a pleasure discussing things with you so here goes (I may try and stick some references in, but mostly I write from memory)
Ocean oxygen concentration.
Surpisingly for many people, oxygen doesn't actually dissolve very well, CO2 dissolves far better (but still not very well). Current understanding is that the atmosphere was very reducing (a huge amount of energy from the earths creation still remained) and oxygen (as in di-oxygen, O2) did not exist in the atmosphere. This can be pretty much verified by the composition of rocks older than, say, 2 billion year old or so. Were there O2 in the water then yes, it would probably screw things up, but since there wasn't it's a moot point.
Diluting effects of the ocean volume.
Yes, nowadays that would represent a huge problem but since the atmosphere was such a strong reducing environment these problems were less than now. Lightning discharges in the atmosphere even today can split the triple bond between two nitrogen atoms. This nitrogen tends not to revert to N2, but is converted to NH3. Ammonia dissolves well in water becoming ammonium (NH4+). There would be some kind of equalibrium between the atmosphere and the ocean, probably quite strongly ocean based.
Synthesis vs. destruction.
A very very good point on two fronts.
1) The assumption of your statement is that the oceans are a homogenous environment. This is patently not the case. Amino acids (for example) formed would adhere to surfaces, such as rocks etc, where they would be afforded some protection against desctruction. It is on the surfaces of rocks / shallow pools that life is inferred to have evolved.
2) There would be differential breakdown of products based on their chemical stability. Some things will breakdown readily (simple hydrocarbons, etc), but other things are far more chemically stable and will remain for longer such as DNA or RNA (even if they initially were very short strands). If these molecules had the ability to reproduce in a high evergy environment (and we certainly know they have the ability to split apart DNA strands at certain temperatures, it's how th Polymerase Chain Reaction for DNA amplification works) and some are more stable than others, then the most stable configurations would come to predominate the ocean. Once the available resources had been used up then the variants that breakdown less readily will be there to reproduce when shorter 'lived' molecules breakdown. This was the first case of Natural Selection, based on the stability and reproductive 'fecundity' of simple, but relatively stable, molecules (probably RNA). From here, more and more complex situations arose, each one made the chemical replicator more successfull than it's competition.
Incompatability.
Again a chemical stability thing. Same answer as above really.