Old Rocks
Diamond Member
Wrong.![]()
History of Atmospheric CO2 through geological time (past 550 million years: from Berner, Science, 1997). The parameter RCO2 is defined as the ratio of the mass of CO2in the atmosphere at some time in the past to that at present (with a pre-industrial value of 300 parts per million). The heavier line joining small squares represents the best estimate of past atmospheric CO2 levels based on geochemical modeling and updated to have the effect of land plants on weathering introduced 380 to 350 million years ago. The shaded area encloses the approximate range of error of the modeling based on sensitivity analysis. Vertical bars represent independent estimates of CO2 level based on the study of ancient soils.
The last time there was 4000 ppm of CO2 in the atmosphere, longterm, was about 350 million years ago. Quite a bit before the evolution of mammals. Even before the evolution of therapsids. At about 250 million years ago, there was a very large spike in CO2 and CH4, that was the P-T Extinction. Really, Billy Boob, look up things before making a fool of yourself.
And the temperature NEVER ran away...
End-Permian mass extinction the Great Dying Natural History Museum
Causes
A single supercontinent, Pangaea, stretched from pole to pole in the Permian Period. Thishuge landmass created extremely hot, dry conditions across most of the interior. By the Late Permian, global temperatures were thehighest they’d ever been.
The severe conditions meant vast numbers of land and marine species were at risk. And then something happened that tipped them over the edge - one of the biggest volcanic eruptions ever.
![early-volcano-118911-1.jpg](/proxy.php?image=http%3A%2F%2Fwww.nhm.ac.uk%2Fresources-rx%2Fimages%2F1008%2Fearly-volcano-118911-1.jpg&hash=3bcbb38dadecc6a0b5870b9530ab68b3)
Huge volcanic eruptions in Siberia are likely to have been a major trigger of the end-Permian extinction event.
Over the course of about 600,000 years huge volumes of viscous basalt lava poured out across Siberia, covering an area roughly 7 times the size of France.
Massive clouds of gases belched out. The sulphur dioxide caused acid rain and global cooling. But this was only short-term. The temperature increased as the eruptions injected carbon dioxide into the atmosphereand yet more escaped from coal deposits exposed in the surrounding area.
As the oceans warmed, frozen methanelocated in marine sediments may have melted. If so, the release of this potent greenhouse gas could have turned the planet’s temperature upeven more.
As well as being devastating for marine and land plants and animals, Late Permian environmental changes created anoxic conditions in the sea. This lack of oxygen caused additional widespread extinctions because it destroyed food chains.