lpetrich
Contributor
I'd earlier posted on how The end-Permian mass extinction was very fast by geological standards. The Permian–Triassic extinction event was the biggest mass extinction ever, at least in the Phanerozoic.
Finally, We Know What Killed Sea Life in The Deadliest Mass Extinction in History noting Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction | Science
Global warming.
Around the end-Permian mass extinctions were some big volcanic eruptions in Siberia, eruptions that made big sheets of "flood basalt" volcanic rock, the Siberian Traps, a Large Igneous Province. The Earth has several other flood-basalt LIP's, like at the Columbia River in western North American, and also the Deccan Traps of India. The Moon's "seas" are also flood-basalt LIP's.
The authors of that paper simulated the effects of the carbon dioxide emitted by those volcanoes, and they found an increase in the average temperature of 11 C / 20 F. This both speeded up the metabolism of marine animals and reduced the solubility of oxygen in the oceans. Many of these animals suffocated. Comparison to the oxygen needs of similar present-day organisms reveled a good match, though an imperfect one.
Our Planet's Largest Mass Extinction Had Warning Signs - And They're Happening Again noting Pre–mass extinction decline of latest Permian ammonoids | Geology | GeoScienceWorld
From the first article,
Finally, We Know What Killed Sea Life in The Deadliest Mass Extinction in History noting Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction | Science
Global warming.
Around the end-Permian mass extinctions were some big volcanic eruptions in Siberia, eruptions that made big sheets of "flood basalt" volcanic rock, the Siberian Traps, a Large Igneous Province. The Earth has several other flood-basalt LIP's, like at the Columbia River in western North American, and also the Deccan Traps of India. The Moon's "seas" are also flood-basalt LIP's.
The authors of that paper simulated the effects of the carbon dioxide emitted by those volcanoes, and they found an increase in the average temperature of 11 C / 20 F. This both speeded up the metabolism of marine animals and reduced the solubility of oxygen in the oceans. Many of these animals suffocated. Comparison to the oxygen needs of similar present-day organisms reveled a good match, though an imperfect one.
Our Planet's Largest Mass Extinction Had Warning Signs - And They're Happening Again noting Pre–mass extinction decline of latest Permian ammonoids | Geology | GeoScienceWorld
From the first article,
Brachiopods were shrinking and radiolarians were in decline, and there is some evidence that that may be happening today, like Atlantic menhaden fish shrinking by 15%. However, overfishing can also cause size decline.By examining previously unresearched fossils in Iran, they have now found warning signs as early as 700,000 years before the event occurred.
They found that several species of ammonoids - marine molluscs also known as ammonites - were killed off around that time, and the species that survived grew increasingly smaller and less complex.
There were other signs, too - and they are shockingly familiar.
"There is much evidence of severe global warming, ocean acidification, and a lack of oxygen," said lead author Wolfgang Kießling of the FAU.
"What separates us from the events of the past is the extent of these phenomena. For example, today's increase in temperature is significantly lower than 250 million years ago."