Quantifying the effect of the Drake Passage opening on the Eocene Ocean

• Published in: Paleoceanography and Paleoclimatology
• Main Authors: Toumoulin, A., Donnadieu, Y., Ladant, J.‐B., Batenburg, Sietske, Poblete, F., Dupont-Nivet, Guillaume
• Other Authors: Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), University of Michigan Ann Arbor, University of Michigan System, Géosciences Rennes (GR), Université de Rennes 1 (UR1), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Centre National de la Recherche Scientifique (CNRS), Universidad de Santiago de Chile Santiago (USACH)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2020
• Subjects: Antarctic‐Circumpolar Current; Southern Ocean; Neodymium; climate modeling; gateways; Eocene; [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography; Antarctic; The Antarctic; Drake Passage; Antarc*; NADW; North Atlantic Deep Water; North Atlantic
• Online Access: https://hal-insu.archives-ouvertes.fr/insu-02870316; https://hal-insu.archives-ouvertes.fr/insu-02870316/document; https://hal-insu.archives-ouvertes.fr/insu-02870316/file/2020PA003889.pdf; https://doi.org/10.1029/2020PA003889

International audience The opening of the Drake Passage (DP) during the Cenozoic is a tectonic event of paramount importance for the development of modern ocean characteristics. Notably, it has been suggested that it exerts a primary role in the onset of the Antarctic Circumpolar Current formation (ACC), in the cooling of high‐latitude South Atlantic waters and in the initiation of North Atlantic Deep Water (NADW) formation.Several model studies have aimed to assess the impacts of DP opening on climate, but most of them focused on surface climate and only few used realistic Eocene boundary conditions. Here, we revisit the impact of the DP opening on ocean circulation with the IPSL‐CM5A2 Earth System Model. Using appropriate middle Eocene (40 Ma) boundary conditions, we perform and analyze simulations with different depths of the DP (0 m, 100 m, 1000 m and 2500 m) and compare results to existing geochemical data. Our experiments show that DP opening has a strong effect on Eocene ocean structure and dynamics even for shallow depths. The DP opening notably allows the formation of a proto‐ACC and induces deep ocean cooling of 1.5°C to 2.5°C in most of the Southern Hemisphere. There is no NADW formation in our simulations regardless of the depth of the DP, suggesting that the DP on its own is not a primary control of deep‐water formation in the North Atlantic. This study elucidates how and to what extent the opening of the Drake Passage contributed to the establishment of the modern global thermohaline circulation.