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• W2053512104 abstract "Research Article| February 01, 2015 Saline Indian Ocean waters invaded the South Atlantic thermocline during glacial termination II Paolo Scussolini; Paolo Scussolini 1Earth and Climate Group, Vrije Universiteit, Amsterdam 1081HV, Netherlands *Current address: IVM (Institute for Environmental Studies), Vrije Universiteit, Amsterdam 1081HV, Netherlands. Search for other works by this author on: GSW Google Scholar Gianluca Marino; Gianluca Marino 2Institut de Ciència i Tecnologia Ambientals, Univesitat Autònoma de Barcelona, Bellaterra 08193, Spain3Research School of Earth Sciences, The Australian National University, Canberra, ACT 2601, Australia Search for other works by this author on: GSW Google Scholar Geert-Jan A. Brummer; Geert-Jan A. Brummer 1Earth and Climate Group, Vrije Universiteit, Amsterdam 1081HV, Netherlands4Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, Den Burg NL-1790AB, Netherlands Search for other works by this author on: GSW Google Scholar Frank J.C. Peeters Frank J.C. Peeters 1Earth and Climate Group, Vrije Universiteit, Amsterdam 1081HV, Netherlands Search for other works by this author on: GSW Google Scholar Author and Article Information Paolo Scussolini *Current address: IVM (Institute for Environmental Studies), Vrije Universiteit, Amsterdam 1081HV, Netherlands. 1Earth and Climate Group, Vrije Universiteit, Amsterdam 1081HV, Netherlands Gianluca Marino 2Institut de Ciència i Tecnologia Ambientals, Univesitat Autònoma de Barcelona, Bellaterra 08193, Spain3Research School of Earth Sciences, The Australian National University, Canberra, ACT 2601, Australia Geert-Jan A. Brummer 1Earth and Climate Group, Vrije Universiteit, Amsterdam 1081HV, Netherlands4Department of Geology and Chemical Oceanography, NIOZ Royal Netherlands Institute for Sea Research, Den Burg NL-1790AB, Netherlands Frank J.C. Peeters 1Earth and Climate Group, Vrije Universiteit, Amsterdam 1081HV, Netherlands Publisher: Geological Society of America Received: 02 Sep 2014 Revision Received: 22 Nov 2014 Accepted: 25 Nov 2014 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2015 Geological Society of America Geology (2015) 43 (2): 139–142. https://doi.org/10.1130/G36238.1 Article history Received: 02 Sep 2014 Revision Received: 22 Nov 2014 Accepted: 25 Nov 2014 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Paolo Scussolini, Gianluca Marino, Geert-Jan A. Brummer, Frank J.C. Peeters; Saline Indian Ocean waters invaded the South Atlantic thermocline during glacial termination II. Geology 2015;; 43 (2): 139–142. doi: https://doi.org/10.1130/G36238.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Salty and warm Indian Ocean waters enter the South Atlantic via the Agulhas leakage, south of Africa. Model simulations and proxy evidence of Agulhas leakage strengthening during glacial terminations led to the hypothesis that it was an important modulator of the Atlantic Ocean circulation. Yet, the fate of the leakage salinity and temperature anomalies remains undocumented beyond the southern tip of Africa. Downstream of the leakage, new paleoceanographic evidence from the central Walvis Ridge (southeast Atlantic) shows that salinity increased at the thermocline, and less so at the surface, during glacial termination II. Thermocline salinity change coincided with higher frequency of Agulhas rings passage at the core location and with salinity maxima in the Agulhas leakage area, suggesting that leakage waters were incorporated in the Atlantic circulation through the thermocline. Hydrographic changes at the Walvis Ridge and in the leakage area display a distinct two-step structure, with a reversal at ca. 134 ka. This matched a wet interlude within the East Asia weak monsoon interval of termination II, and a short-lived North Atlantic warming. Such concurrence points to a Bølling-Allerød–like recovery of the Atlantic circulation amidst termination II, with a northward shift of the Intertropical Convergence Zone and Southern Hemisphere westerlies, and attendant curtailment of the interocean connection south of Africa. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2053512104 title "Saline Indian Ocean waters invaded the South Atlantic thermocline during glacial termination II" @default.
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