Perpetual Student said:
Is there something specific that he is missing?
Let's start with details.
JW said:
prebiotic earth is therefore taken to have been quite warm,
HOW warm? A difference of a half-dozen degrees is the difference between certain protiens functioning and others collapsing into inert squiggles of matter.
Meaning WHAT, precisely?
What is the % of water vapor in the atmosphere? This can have serious implications for biochemistry.
HOW stormy? How strong were those storms? Lightning may have played a roll in abiogenesis (either adding energy or removing it), and vague hand-waving around doesn't help anyone.
and exposed to solar UV radiation due to the absence of an ozone layer.
Meaning what, exactly?
It is taken that this prebiotic environment included a complex mixture of organic chemicals, commonly known as the primordial soup.
WHAT mix of chemicals? How difuse was it? Was it homogenous or heterogenous? WHERE was it--in the oceans, at the beaches, at oceanic vents, at ponds on land, in rivers?
All these assumptions are fairly standard.
While this is true, it's similar to saying "The Earth is warm" is a fairly standard assumption. It is--until you get into details.
Also note that nothing is discussed about redox state, something that biogeochemists typically get very long-winded about. This is a major error--certain chemical reactions, which (far as I've read) are important for the rise of life, won't take place in conditions with oxygen levels that are too high. Was there NO atmospheric free oxygen, or just very little? That's a major question. Back to the volcanism thing, volcanism is not some minor issue you can wave away as a standard assumption--biogeochemists dealing with the Cambrian Explosion get into very serious and complex verbal battles over just how much of a roll volcanism plays in providing nutrients for life (some argue that techtonic activity put enough ions into the oceans to allow for shell formation, while others argue that that idea is insane, to give you the 1:500,000 view of that particular argument). And what KIND of volcanism was it? Was it oceanic rifting, which produces hydrothermal vents in the ocean? Was it cauldara-type volcanism, which destroyes pretty much everything around it?
The issue is that in order to understand the chemistry, you need to understand the environment that chemistry is happening in. Some biochemical reactions won't take place if things are too acidic (was there a lot of CO2 in the atmosphere, which would mean a lot of carbonic acid in the oceans? Or was that CO2 taken up by chemical weathering of mountain ranges?) or too basic (how much CaCO3 was deposited? how much chemical weathering was going on?). Some reactions, as I stated earlier, need a lot of oxygen, or little, or none at all. Some need more saline aquious environments, some need less.
A good analogy is a novel: JW is attempting to argue about the characters, without acknowledging the plot, the setting, or the theme. And it's not just him that's doing it--he's just an easy target because he's here. Geologists tend to try to talk about the setting without discussing the characters, plot, or theme. Biologists try to talk about the plot without the setting, theme or characters. Paleontologists try to talk about the theme without the setting, plot, or characters. And I think I've stretched this analogy as far as it will go.
