My review of the video:
A bit long, but a nice video.
I like his explanation at about 11:55 concerning what and why is is looking at particular chemical changes at different layers.
I think it could have benefited by having more of a up-to-date theoretical intro about what the current thinking on this transition is: something like:
- big (actually truly massive) eruptions (but spread out over a long period of time)
- changes in atmospheric chemistry which leads to changes in oceanic chemistry (over long periods of time)
- changes in water chemistry can have drastic effects on certain biological functions
- loss of parts of an ecosystem can lead to its collapse
- leading to a decrease in the amount of environmental energy/resources biology can collect
- smaller overall, less diverse species-ome, with many groups being lost completely (extinct), from which subsequent species evolve.
However, I think he gets to this later in the video.
I liked his technical details throughout.
I also liked his use of TOC (total organic carbon; the amount of carbon in the local biochemistry).
This is an important water condition, for water systems used to successfully rear particular organisms.
Within the geological record, TOC reflects what is going on in the ecosystem at time of deposition (how much oxygen is passing through the ecosystem). Greatly reduced at the time of the extinction.
The relationship of carbonates with pH is well known, to knowledgeable aquarists (both fresh and salt). CO
2 dissolves well in water where it can combine with water (H
2O), form an acid.
By changing the water pH, the ratio of dissolved and undissolved carbonate is shifted (more acidic favors greater dissolution).
Bubbling CO
2 into aquarium water (done to produce luxuriant plant growth), can change the pH.
Strong aeration can change the pH (by more rapidly blowing off CO
2).
Response to Question:
Your question amounts to a compare and contrast question between the current climate change situation and the period of the end Permian extinction.
One big obvious distinction is the length of time over which the changes are occurring.
An example of a quick (and very dramatic) change would be the giant
meteor impact at Chicxulub in Mexico, which (combined with subsequent environmental changes) probably killed all the dinosaurs with-in a year or two (many within a day).
Our current bout of
human induced climate change (assuming for argument, that this is the current reality (this means, argue this somewhere else)), might appear slow to the individual's human awareness of a single life (much as evolution does), but it is really rapid on the evolutionary time scale, over which large evolutionary changes can be seen.
Some are concerned that these changes (like with the dinosaurs) will be too fast for a rapid and smooth biological response to the changing environmental conditions.
This might then lead to lots of extinctions which could then be amplified through ecosystem collapse.
Some now claim that we are at the beginning of a new geological period of time, the Anthropocene, marked by things like atomic bomb radiation and plastics in sediments.
If changes in sea water chemistry were to get large enough and be maintained long enough, one should expect powerful impacts on the ocean ecosystems of the world.
This would also show up in the geological record, probably somewhat like in the Permian, a distinct transition (as seen from the distant future).
The
Permian occurred about when the
Siberian traps were being produced. These eruptions seem to have come in very large bursts of extruded volcanic mass (with a bunch of associated gasses coming out).
These eruptions were spread out over a much longer time period (and can be more easily distinguished geologically).
The eruptions continued for roughly two million years and spanned the
Permian–Triassic boundary, or P–T boundary, which occurred between
251 to 250 million years ago.
[1][2]
Large volumes of
basaltic lava covered a large expanse of Siberia in a
flood basalt event. Today, the area is covered by about 7 million km2 (3 million sq mi) of basaltic rock, with a volume of around 4 million km3 (1 million cu mi).
[3]
I would have liked to see direct geological evidence of burned coal fields (I have not heard of these before).
Seems like that should be findable in very specific areas (in and neighboring to the traps).
I'm not clear on the detailed relationships between the timing of the eruptions and the extinctions.
I am pretty sure there have been publications on this.
Also, what are the differences between land and sea extinctions?