Print Email Facebook Twitter Pronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperatures Title Pronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperatures Author Douglas, P.M.J. Affek, H.P. Ivany, L.C. Houben, A.J.P. Sijp, W.P. Sluijs, A. Schouten, S. Pagani, M. Publication year 2014 Abstract Paleoclimate studies suggest that increased global warmth during the Eocene epoch was greatly amplified at high latitudes, a state that climate models cannot fully reproduce. However, proxy estimates of Eocene near-Antarctic sea surface temperatures (SSTs) have produced widely divergent results at similar latitudes, with SSTs above 20 °C in the southwest Pacific contrasting with SSTs between 5 and 15 °C in the South Atlantic. Validation of this zonal temperature difference has been impeded by uncertainties inherent to the individual paleotemperature proxies applied at these sites. Here, we present multiproxy data from Seymour Island, near the Antarctic Peninsula, that provides well-constrained evidence for annual SSTs of 10-17 °C (1σ SD) during the middle and late Eocene. Comparison of the same paleotemperature proxy at Seymour Island and at the East Tasman Plateau indicate the presence of a large and consistent middle-to-late Eocene SST gradient of ~7 °C between these two sites located at similar paleolatitudes. Intermediate- complexity climate model simulations suggest that enhanced oceanic heat transport in the South Pacific, driven by deep-water formation in the Ross Sea, was largely responsible for the observed SST gradient. These results indicate that very warm SSTs, in excess of 18 °C, did not extend uniformly across the Eocene southern high latitudes, and suggest that thermohaline circulation may partially control the distribution of high-latitude ocean temperatures in greenhouse climates. The pronounced zonal SST heterogeneity evident in the Eocene cautions against inferring past meridional temperature gradients using spatially limited data within given latitudinal bands. Subject Earth / EnvironmentalPG - Petroleum GeosciencesELSS - Earth, Life and Social SciencesGeological Survey NetherlandsGeosciencesEnergy / Geological Survey NetherlandsClimate modelingClumped isotopesHigh-latitude climateOrganic geochemistryPaleooceanographyCalcium carbonateStrontiumAntarcticaBenthic foraminiferaEoceneGeochemistryLatitudeNonhumanPaleoclimatesea surface temperatureSedimentSimulationThermohaline circulation To reference this document use: http://resolver.tudelft.nl/uuid:163ff425-cac9-4304-b3c7-d5b8c0be3e1e DOI https://doi.org/10.1073/pnas.1321441111 TNO identifier 503267 Publisher National Academy of Sciences ISSN 1091-6490 Source Proceedings of the National Academy of Sciences of the United States of America, 111 (18), 6582-6587 Document type article Files To receive the publication files, please send an e-mail request to TNO Library.