%0 Journal Article
%T Periodic changes in the Cretaceous ocean and climate caused by marine redox see-saw
%J -
%D 2019
%R https://doi.org/10.1038/s41561-019-0359-x
%X Periodic changes in sediment composition are usually ascribed to insolation forcing controlled by Earth¡¯s orbital parameters. During the Cretaceous Thermal Maximum at 97¨C91£¿Myr ago (Ma), a 37¨C50-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 \(p_{\mathrm {CO}_2}\). We conclude that most of the variability in the mid-Cretaceous ocean¨Catmosphere system can be ascribed to the internal redox see-saw and its response to external orbital forcing
%U https://www.nature.com/articles/s41561-019-0359-x