An interesting paleoclimate study that changes the way we should possibly think about the dinosaur demise, with a warning of where we are going today.
>>Professor MacLeod’s team analysed the chemical composition of sand-grain-sized fragments of fish fossils embedded in the sedimentary layers below and above the Cretaceous-Paleogene boundary, signifying the 50,000 years preceding and 300,000 years after the collision.
When fish build minerals in their teeth, bones and scales, the temperature of the surrounding water dictates how much of a specific type or isotope of oxygen, called oxygen-18, is laid down.
In the El Kef fish fossils, he and his team found the signature of a rapid, intense rise in temperature from around 20 to 25 degrees Celsius, which was sustained for 100,000 years before dropping back to pre-collision levels.
And because of polar amplification, which tends to produce bigger climate swings near the poles than the equator, it’s likely the polar regions warmed even more than the 5 degrees calculated at El Kef, Professor MacLeod said.
You might have been taught that when the asteroid that killed the dinosaurs smashed into the Earth, fine particles were blasted into the atmosphere, blocking the sun and causing global cooling.
Even though this may have been the case in some parts, particularly close to the impact site, any local effects would have soon been swamped by overall global warming, said Andrew Glikson, a palaeoclimatologist at the Australian National University, who was not involved with the study.<<
http://www.abc.net.au/news/science/2018-05-25/dinosaur-killing-asteroid-impact-global-warming-fossils-el-kef/9796244