A new mechanism for the two-step δ 18 O signal at the Eocene-Oligocene boundary

• Published in: Climate of the Past
• Main Authors: A. S. von der Heydt, H. A. Dijkstra, M. Tigchelaar
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2011
• Subjects: Environmental pollution; TD172-193.5; Environmental protection; TD169-171.8; Environmental sciences; GE1-350; Antarctic; Southern Ocean; The Antarctic; Antarc*; Ice Sheet
• Online Access: https://doi.org/10.5194/cp-7-235-2011; https://doaj.org/article/65f0c0b848ac4b66bf19a0f8145138c5

The most marked step in the global climate transition from "Greenhouse" to "Icehouse" Earth occurred at the Eocene-Oligocene (E-O) boundary, 33.7 Ma. Evidence for climatic changes comes from many sources, including the marine benthic δ 18 O record, showing an increase by 1.2–1.5‰ at this time. This positive excursion is characterised by two steps, separated by a plateau. The increase in δ 18 O values has been attributed to rapid glaciation of the Antarctic continent, previously ice-free. Simultaneous changes in the δ 13 C record are suggestive of a greenhouse gas control on climate. Previous modelling studies show that a decline in p CO 2 beyond a certain threshold value may have initiated the growth of a Southern Hemispheric ice sheet. These studies were not able to conclusively explain the remarkable two-step profile in δ 18 O. Furthermore, they considered changes in the ocean circulation only regionally, or indirectly through the oceanic heat transport. The potential role of global changes in ocean circulation in the E-O transition has not been addressed yet. Here a new interpretation of the δ 18 O signal is presented, based on model simulations using a simple coupled 8-box-ocean, 4-box-atmosphere model with an added land ice component. The model was forced with a slowly decreasing atmospheric carbon dioxide concentration. It is argued that the first step in the δ 18 O record reflects a shift in meridional overturning circulation from a Southern Ocean to a bipolar source of deep-water formation, which is associated with a cooling of the deep sea. The second step in the δ 18 O profile occurs due to a rapid glaciation of the Antarctic continent. This new mechanism is a robust outcome of our model and is qualitatively in close agreement with proxy data.