The Deccan Traps are a series of lava flows that occurred at the end of the Cretaceous period, spanning 145 million to 66 million years ago. Covering an area of about 1.5 million square kilometres near India's Western Ghats, roughly half the size of modern India, these volcanic eruptions released large amounts of sulphur and fluorine into the atmosphere, further cooling the Earth's climate and blocking out sunlight. This hindered plant growth, leading to starvation among many animals.
This study challenges the commonly held belief that the
“Our research demonstrates that climatic conditions were almost certainly unstable, with repeated volcanic winters that could have lasted decades, prior to the extinction of the dinosaurs,” explains Don Baker, co-author of the study. “This instability would have made life difficult for all plants and animals and set the stage for the dinosaur extinction event.”
The research findings have been published in Scientific Advances and can be accessed here.