1000 ppm starts affecting performance from co2 poisoning.
Average for the last decade was ~2.25ppm/y
1000ppm by 2100 is probably not going to happen, but considering the significant lag behind the effects, it's starting to look more and more likely that we will hit 1000ppm at some high point, perhaps in the 22nd century, before it starts going down again.
Regarding the poisoning comment, that's not very accurate. It's true, there is reduced performance at high CO2 levels, but 1000 is probably the lowest bound for the most sensitive people and the effects aren't really noticeable until high teens. You can still function indefinitely at those levels.
"With no force on earth capable of preventing the oceans from continuing to warm and acidify for centuries to come, Veron had no illusions about the future."
I feel you're missing the point of the article. The reality is that the reef effectively has a terminal illness and there's little anyone can do now.
Stage 5. Acceptance.
Totally understand that - but the article is written from the point of view that its already dead, which it of course is not, which will cause people to ignore the article. If I was diagnosed with a terminal illness today, I would not write to everyone I know saying I was dead, I would say I was dying.
I guess I'm happy to grant the author a little artistic license to make his point.
I can understand that you might think other people would be misled by the rhetorical structure... but I encourage you to not get upset at imagined misunderstandings on behalf of others. (Not that it's wrong, it's just makes your life a little less happy)
The problem is, global warming is largely an issue _because_ of the "misunderstandings on behalf of others", so in this case, it is a real issue.
Rage, rage against the dying of the light.
For context: Many shelled organisms (cnidarians - corals, brittlestars, sea urchins; molluscs - shellfish) build shells from CaCO3, either as the polymorphs calcite or aragonite. Other options for shell material are silica (SiO2; e.g. some radiolaria, siliceous sponges) or chitin (C8H13O5N; e.g. shells of crustaceans). Animals make their skeletons from hydroxy apatite Ca5(PO4)3(OH).
The unknown for coral is the rate of change of temperature.
[1] https://www.sciencedaily.com/releases/2012/04/120401160101.h...