资源环境科技发展态势分析平台

Periodic changes in sediment composition are usually ascribed to insolation forcing controlled by Earth's orbital parameters. During the Cretaceous Thermal Maximum at 97-91Myr ago (Ma), a 37-50-kyr-long cycle that is generally believed to reflect obliquity forcing dominates the sediment record. Here, we use a numerical ocean model to show that a cycle of this length can be generated by marine biogeochemical processes without applying orbital forcing. According to our model, the restricted proto-North Atlantic and Tethys basins were poorly ventilated and oscillated between iron-rich and sulfidic (euxinic) states. The Panthalassa Basin was fertilized by dissolved iron originating from the proto-North Atlantic. Hence, it was less oxygenated while the proto-North Atlantic was in an iron-rich state and better oxygenated during euxinic periods in the proto-North Atlantic. This redox see-saw was strong enough to create significant changes in atmospheric p(CO2). We conclude that most of the variability in the mid-Cretaceous ocean-atmosphere system can be ascribed to the internal redox see-saw and its response to external orbital forcing.