Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event
Sindia Sosdian, Tali L. Babila, Rosanna Greenop, Gavin L. Foster, Caroline H. Lear
Abstract
Abstract The Miocene Climatic Optimum (MCO, 14–17 Ma) was ~3–4 °C warmer than present, similar to estimates for 2100. Coincident with the MCO is the Monterey positive carbon isotope (δ 13 C) excursion, with oceans more depleted in 12 C relative to 13 C than any time in the past 50 Myrs. The long-standing Monterey Hypothesis uses this excursion to invoke massive marine organic carbon burial and draw-down of atmospheric CO 2 as a cause for the subsequent Miocene Climate Transition and Antarctic glaciation. However, this hypothesis cannot explain the multi-Myr lag between the δ 13 C excursion and global cooling. We use planktic foraminiferal B/Ca, δ 11 B, δ 13 C, and Mg/Ca to reconstruct surface ocean carbonate chemistry and temperature. We propose that the MCO was associated with elevated oceanic dissolved inorganic carbon caused by volcanic degassing, global warming, and sea-level rise. A key negative feedback of this warm climate was the organic carbon burial on drowned continental shelves.