Towards determination of the source and magnitude of atmospheric pCO2 change across the early Paleogene hyperthermals

The early Paleogene greenhouse climate is punctuated by a series of extreme global warming events known as hyperthermals that are associated with massive additions of carbon to the ocean-atmosphere system. However, no existing proxies have suitable resolution to capture the change in atmospheric carbon dioxide (pCO2) across these events. Here, we reconstruct a nearly continuous record of pCO2 during the early Paleogene based on changes in...