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• W2138293889 abstract "Research Article| February 01, 2012 Abrupt changes in high-latitude nutrient supply to the Atlantic during the last glacial cycle K.R. Hendry; K.R. Hendry 1Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Massachusetts 02543, USA2School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3AT, UK Search for other works by this author on: GSW Google Scholar L.F. Robinson; L.F. Robinson 1Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Massachusetts 02543, USA3Department of Earth Sciences, University of Bristol, Queen's Road, Bristol BS8 1RJ, UK Search for other works by this author on: GSW Google Scholar M.P. Meredith; M.P. Meredith 4British Antarctic Survey, High Cross, Cambridge CB3 0ET, UK Search for other works by this author on: GSW Google Scholar S. Mulitza; S. Mulitza 5Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, D-28359 Bremen, Germany Search for other works by this author on: GSW Google Scholar C.M. Chiessi; C.M. Chiessi 6School of Arts, Sciences and Humanities, University of São Paulo, Rua Arlindo Bettio 1000, 03828-000 São Paulo, Brazil Search for other works by this author on: GSW Google Scholar H. Arz H. Arz 7Leibniz Institute for Baltic Sea Research Warnemünde (IOW) and Ernst-Moritz-Arndt-University Greifswald (EMAU), Seestraße 15, D-18119 Rostock-Warnemünde, Germany Search for other works by this author on: GSW Google Scholar Geology (2012) 40 (2): 123–126. https://doi.org/10.1130/G32779.1 Article history received: 26 Aug 2011 accepted: 12 Sep 2011 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation K.R. Hendry, L.F. Robinson, M.P. Meredith, S. Mulitza, C.M. Chiessi, H. Arz; Abrupt changes in high-latitude nutrient supply to the Atlantic during the last glacial cycle. Geology 2012;; 40 (2): 123–126. doi: https://doi.org/10.1130/G32779.1 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 The supply of nutrients to the low-latitude thermocline is largely controlled by intermediate-depth waters formed at the surface in the high southern latitudes. Silicic acid is an essential macronutrient for diatoms, which are responsible for a significant portion of marine carbon export production. Changes in ocean circulation, such as those observed during the last deglaciation, would influence the nutrient composition of the thermocline and, therefore, the relative abundance of diatoms in the low latitudes. Here we present the first record of the silicic acid content of the Atlantic over the last glacial cycle. Our results show that at intermediate depths of the South Atlantic, the silicic acid concentration was the same at the Last Glacial Maximum (LGM) as it is today, overprinted by high silicic acid pulses that coincided with abrupt changes in ocean and atmospheric circulation during Heinrich Stadials and the Younger Dryas. We suggest these pulses were caused by changes in intermediate water formation resulting from shifts in the subpolar hydrological cycle, with fundamental implications for the nutrient supply to the Atlantic. 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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• W2138293889 title "Abrupt changes in high-latitude nutrient supply to the Atlantic during the last glacial cycle" @default.
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