Onset of Mediterranean outflow into the North Atlantic

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doi: 10.1126/science.1251306
Author(s): Hernández-Molina, F. Javier; Stow, Dorrik A. V.; Alvarez-Zarikian, Carlos A.; Acton, Gary; Bahr, Andre; Balestra, Barbara; Ducassou, Emmanuelle; Flood, Roger; Flores, José-Abel; Furota, Satoshi; Grunert, Patrick; Hodell, David; Jimenez-Espejo, Francisco; Kim, Jin Kyoung; Krissek, Lawrence; Kuroda, Junichiro; Li, Baohua; Llave, Estefania; Lofi, Johanna; Lourens, Lucas; Miller, Madeline; Nanayama, Futoshi; Nishida, Naohisa; Richter, Carl; Roque, Cristina; Pereira, Helder; Sanchez Goñi, Maria Fernanda; Sierro, Francisco J.; Singh, Arun Deo; Sloss, Craig; Takashimizu, Yasuhiro; Tzanova, Alexandrina; Voelker, Antje; Williams, Trevor; Xuan, Chuang
Author Affiliation(s): Primary:
University of London, Department of Earth Sciences, London, United Kingdom
Other:
Heriot-Watt University, United Kingdom
Texas A&M University, United States
Sam Houston State University, United States
University of Frankfurt, Germany
University of California, Santa Cruz, United States
Université de Bordeaux, France
Stony Brook University, United States
Universidad de Salamanca, Spain
Hokkaido University, Japan
University of Graz, Austria
University of Cambridge, United Kingdom
Japan Agency for Marine-Earth Science and Technology, Japan
Korea Institute of Ocean Science and Technology, South Korea
Ohio State University, United States
Nanjing Institute of Geology and Palaeontology, China
Instituto Geológico y Minero de EspanØa, Spain
Université Montpellier II, United Kingdom
Utrecht University, Netherlands
California Institute of Technology, United States
Geological Survey of Japan, Japan
University of Louisiana, United States
Instituto Portugues do Mar e da Atmosfera, Portugal
Escola Secundaria de Loule, Portugal
Banaras Hindu University, India
Queensland University of Technology, Australia
Niigata University, Japan
Brown University, United States
Lamont-Doherty Earth Observatory, United States
University of Southampton, United Kingdom
Volume Title: Science
Source: Science, 344(6189), p.1244-1250. Publisher: American Association for the Advancement of Science, Washington, DC, United States. ISSN: 0036-8075 CODEN: SCIEAS
Note: In English. 34 refs.; illus., incl. sect., strat. cols., sketch map
Summary: Sediments cored along the southwestern Iberian margin during Integrated Ocean Drilling Program Expedition 339 provide constraints on Mediterranean Outflow Water (MOW) circulation patterns from the Pliocene epoch to the present day. After the Strait of Gibraltar opened (5.33 million years ago), a limited volume of MOW entered the Atlantic. Depositional hiatuses indicate erosion by bottom currents related to higher volumes of MOW circulating into the North Atlantic, beginning in the late Pliocene. The hiatuses coincide with regional tectonic events and changes in global thermohaline circulation (THC). This suggests that MOW influenced Atlantic Meridional Overturning Circulation (AMOC), THC, and climatic shifts by contributing a component of warm, saline water to northern latitudes while in turn being influenced by plate tectonics.
Year of Publication: 2014
Research Program: IODP Integrated Ocean Drilling Program
Key Words: 12 Stratigraphy, Historical Geology and Paleoecology; Atlantic Ocean; Atlantic meridional overturning circulation; Cenozoic; Cores; Currents; Expedition 339; Holocene; IODP Site U1386; IODP Site U1387; IODP Site U1389; IODP Site U1390; IODP Site U1391; Integrated Ocean Drilling Program; Marine sediments; Mediterranean Outflow Water; Mediterranean Sea; Neogene; North Atlantic; Ocean circulation; Ocean currents; Paleo-oceanography; Pliocene; Quaternary; Sediments; Tertiary; Thermohaline circulation
Coordinates: N360000 N370000 W0060000 W0100000
Record ID: 2014060485
Copyright Information: GeoRef, Copyright 2017 American Geosciences Institute.