And here I'm going to quote from an interview I did 10 years ago with Dr Dennis Bushnell, chief scientist at NASA's Langley Research Centre. It's all still true today.
He had been talking about the 'feedbacks' (melting permafrost, warming oceans, huge releases of methane and carbon dioxide). Because they cannot yet be fully incorporated into the computer models of climate, they lead to systematic underestimates of future warming. And then he cut to the chase.
"If you take all these feedbacks into account, the estimates are that by 2100, instead of two to six degrees Celsius rise (in average global temperature), it looks like a possibility of six to 12 degrees ...
"These temperature changes would change the ocean circulation patterns and end up with much of the oceans going anoxic — very low oxygen content — which would then promote bacteria which produce hydrogen sulphates. These would rise and take out the ozone layer, and also make it somewhat difficult to breathe. This is by 2100."
What Bushnell was referring to was 'Canfield oceans', now strongly suspected of being the cause of four out of the big five mass extinctions. Everybody knows about the huge asteroid that struck the Gulf of Mexico 65 million years ago and wiped out the dinosaurs.
Fewer people know that there is no trace of an asteroid strike associated with the other four 'great dyings', 444 million, 360 million, 251 million and 200 million years ago. So what happened then?
One common factor was that the planet was unusually hot at the time, but the real clue was that the deep oceans were anoxic. There was no oxygen down there, and therefore no life that used oxygen.
When the oceans are very warm, the 'overturning circulation' (like the Gulf Stream) that carries vast amounts of oxygen-rich surface water down into the depths simply stops, and the oceans stratify into an oxygenated surface layer and an anoxic deeper layer.
But there was still life down there: sulphate bacteria that normally hide in the silt, away from the oxygen that would destroy them. In an anoxic ocean, they come out and multiply — and eventually, if the conditions are right, they rise all the way to the surface and kill all the oxygen-based life in the sea.
Not only that, but hydrogen sulphide gas, a waste product of their metabolism, rises into the atmosphere, destroys the ozone layer, and drifts over the land where it also wipes out most life. However, there hasn't been a 'Canfield' event in the past 200 million years, and when those earlier mass extinctions happened the planet was a good deal hotter to begin with.
Food is the key issue: as warming turns whole regions into desert, mass starvation is imaginable, although actual extinction seems improbable. It's also still possible that we will react fast enough to stop well short of mass death.
The situation is quite grim. Bad news, of course, but when you find yourself in a high-stakes game you should know what the stakes are.
• Gwynne Dyer, is a London-based independent Canadian journalist, columnist and military historian.
