According to a new study it was likely a period of ocean anoxia and climate volatility related to the hottest interval of the last 541 million years. This interval, known as the Cenomanian/Turonian transition, experienced the highest carbon dioxide concentrations during the Cretaceous, as well as disturbances in nutrients like sulfur and iron in the oceans. This transition is associated with a shift in top predators, creating the unique and somewhat short-lived oceanic food webs of the Late Cretaceous, according to Valentin Fischer of the Université de Liège in Belgium and his colleagues.
Fischer and the team combined data on the phylogenetic relationships of hundreds of marine reptile lineages to analyze how extinctions were distributed in the tree of life. Then, they used the largest sample of 2D and 3D data on marine reptiles ever assembled to analyze the effect of these extinctions on the predatory capabilities of Cretaceous marine reptiles.
“Our analyses showed that the Cenomanian-Turonian transition is associated with elevated rates of extinction and that these extinctions disproportionally targeted some groups of large and fast predators in a stepwise manner,” Fischer said.
For example, skull shapes of predators were significantly different before and after the transition, “notably resulting in distinct bite force,” he said.
