I was talking more about things like the great oxidation (reduced atmosphere and iron in the water to a very little oxygen in the air and hydrogen sulfide in the water) and the proterozoic/phanaerozic transition (low-phosphate oceans with some hydrogen sulfide and low oxygen levels to oxic, high-phosphate very productive oceans and lots of atmospheric oxygen that supports an ozone layer).
The great oxidation is looking like it almost certainly was NOT due to the recent invention of oxygenic photosynthesis, but was instead a geochemical tipping point that came when the slowing geology of the earth and the steady oxidation of crustal sinks could no longer absorb all the biogenic oxygen and the very-small-compared-to-the-crust atmosphere whipped into a new state long after the oxygenic photosynthesizer drivers that ultimately caused it were in place, triggering massive biochemical shifts across the biosphere in a short time.
The proterozoic/phanerozoic transition is looking more and more like it could have been an interesting earth-system-scale flip that had something to do both with a major increase in exposed above-water landmass (coming from the growing continents and steadily thinning oceanic crust causing a sudden shift when the ocean level fell to a level that exposed large plains rather than just mountains) and an intrinsic bistability of ocean chemistry such that there are two stable states, one with low primary productivity/oxygen and one with high, that you can only flip between via some kind of shock. Multicellular animals as we know them may simply not be a viable strategy in the low-productivity low-oxygen state, and predators that can drive evolutionary arms races of the sort that probably drove the Cambiran explosion certainly are not. As such, the late emergence of multicellular heterotrophs on Earth (there is evidence for multicellular photosynthesizers for over a billion years, last I saw) is not necessarily due to them being HARD, but due to the need for the geosphere and the chemical environment to go through some phase transitions first, some driven by slow buildups of material over time and some possibly more stochastic. They show up remarkably fast after those phase transitions are complete.
EDIT: I don’t understand the assertion in the linked slides having to do with abiogenesis that genetic systems that were precursors to ours could’ve been more stable than ours. LUCA had our genetic system, full stop, and is certainly older than 3.7 gigayears at the VERY least, for all we know it could be back to 4.4 gigayears. Our genetic code also bears the imprint of an explosive period of waaaaay pre-LUCA evolution in which it was optimized to be literally one in a million in terms of resistance to mutational damage. What came before LUCA was unstable and fell into a stable state, not the other way around. Furthermore there could be other stable biochemistries, without the need to posit going directly here (though I will go out on a limb and say I suspect protein will be everywhere there is water as a solvent and that genetic polymers are likely to have phosphates, hah).
EDIT 2: Okay now I see what you are referring to about transitions in abiogenesis, treating it as a chemical event with some odds per unit volume per unit time. A reasonable analysis, better than most, but neglecting it as a self-reinforcing PROCESS rather than a singular event. There are other schools of thought, though. There are others who, treating living things as dissipative systems that are a channel through which to discharge persistent chemical disequilibrium and our core biochemistry as being able to do so at a remarkably low level of organization, see abiogenesis as a form of breakdown into the preferred state of a planet out of equliibrium and under chemical stress. The idea being that even though the breakdown is stochastic, it is still the preferred state you are pushing the system into via putting a stress on it. See Dr. Eric Smith for a discussion of the idea from one direction (there is a lot of diversity in ideas on this front):
That’s what they talk about on the abiogenesis slides, right?
I was talking more about things like the great oxidation (reduced atmosphere and iron in the water to a very little oxygen in the air and hydrogen sulfide in the water) and the proterozoic/phanaerozic transition (low-phosphate oceans with some hydrogen sulfide and low oxygen levels to oxic, high-phosphate very productive oceans and lots of atmospheric oxygen that supports an ozone layer).
The great oxidation is looking like it almost certainly was NOT due to the recent invention of oxygenic photosynthesis, but was instead a geochemical tipping point that came when the slowing geology of the earth and the steady oxidation of crustal sinks could no longer absorb all the biogenic oxygen and the very-small-compared-to-the-crust atmosphere whipped into a new state long after the oxygenic photosynthesizer drivers that ultimately caused it were in place, triggering massive biochemical shifts across the biosphere in a short time.
The proterozoic/phanerozoic transition is looking more and more like it could have been an interesting earth-system-scale flip that had something to do both with a major increase in exposed above-water landmass (coming from the growing continents and steadily thinning oceanic crust causing a sudden shift when the ocean level fell to a level that exposed large plains rather than just mountains) and an intrinsic bistability of ocean chemistry such that there are two stable states, one with low primary productivity/oxygen and one with high, that you can only flip between via some kind of shock. Multicellular animals as we know them may simply not be a viable strategy in the low-productivity low-oxygen state, and predators that can drive evolutionary arms races of the sort that probably drove the Cambiran explosion certainly are not. As such, the late emergence of multicellular heterotrophs on Earth (there is evidence for multicellular photosynthesizers for over a billion years, last I saw) is not necessarily due to them being HARD, but due to the need for the geosphere and the chemical environment to go through some phase transitions first, some driven by slow buildups of material over time and some possibly more stochastic. They show up remarkably fast after those phase transitions are complete.
EDIT: I don’t understand the assertion in the linked slides having to do with abiogenesis that genetic systems that were precursors to ours could’ve been more stable than ours. LUCA had our genetic system, full stop, and is certainly older than 3.7 gigayears at the VERY least, for all we know it could be back to 4.4 gigayears. Our genetic code also bears the imprint of an explosive period of waaaaay pre-LUCA evolution in which it was optimized to be literally one in a million in terms of resistance to mutational damage. What came before LUCA was unstable and fell into a stable state, not the other way around. Furthermore there could be other stable biochemistries, without the need to posit going directly here (though I will go out on a limb and say I suspect protein will be everywhere there is water as a solvent and that genetic polymers are likely to have phosphates, hah).
EDIT 2: Okay now I see what you are referring to about transitions in abiogenesis, treating it as a chemical event with some odds per unit volume per unit time. A reasonable analysis, better than most, but neglecting it as a self-reinforcing PROCESS rather than a singular event. There are other schools of thought, though. There are others who, treating living things as dissipative systems that are a channel through which to discharge persistent chemical disequilibrium and our core biochemistry as being able to do so at a remarkably low level of organization, see abiogenesis as a form of breakdown into the preferred state of a planet out of equliibrium and under chemical stress. The idea being that even though the breakdown is stochastic, it is still the preferred state you are pushing the system into via putting a stress on it. See Dr. Eric Smith for a discussion of the idea from one direction (there is a lot of diversity in ideas on this front):
https://www.youtube.com/watch?v=0cwvj0XBKlE
https://www.youtube.com/watch?v=7DfzoBvnM2g
EDITED VIDEOS, wrong but still relevant link earlier