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| Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2014
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| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.832885 |
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| _version_ | 1867171824655138816 |
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| author | Hernandéz-Molina, Francisco Javier Stow, Dorrik A V Alvarez Zarikian, Carlos A Acton, Gary D Bahr, André Balestra, Barbara Ducassou, Emmanuelle Flood, Roger D Flores, José-Abel Furota, Satoshi Grunert, Patrick Hodell, David A Jiménez-Espejo, Francisco Jose Kim, Jin Kyoung Krissek, Lawrence A Kuroda, Junichiro Li, Bill Llave, Estefania Lofi, Johanna Lourens, Lucas Joost Miller, Max Nanayama, Futoshi Nishida, Naohisa Richter, Carl Roque, C Pereira, H Sanchez Goñi, Maria Fernanda Sierro, Francisco Javier Singh, Arun Deo Sloss, Craig Takashimizu, Yasuhiro Tzanova, Alexandrina Voelker, Antje H L Williams, Trevor J Xuan, Chuang |
| author_facet | Hernandéz-Molina, Francisco Javier Stow, Dorrik A V Alvarez Zarikian, Carlos A Acton, Gary D Bahr, André Balestra, Barbara Ducassou, Emmanuelle Flood, Roger D Flores, José-Abel Furota, Satoshi Grunert, Patrick Hodell, David A Jiménez-Espejo, Francisco Jose Kim, Jin Kyoung Krissek, Lawrence A Kuroda, Junichiro Li, Bill Llave, Estefania Lofi, Johanna Lourens, Lucas Joost Miller, Max Nanayama, Futoshi Nishida, Naohisa Richter, Carl Roque, C Pereira, H Sanchez Goñi, Maria Fernanda Sierro, Francisco Javier Singh, Arun Deo Sloss, Craig Takashimizu, Yasuhiro Tzanova, Alexandrina Voelker, Antje H L Williams, Trevor J Xuan, Chuang |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_832885 |
| institution | PANGAEA |
| language | en |
| publishDate | 2014 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Seismic multichannel reflection profiles from the Gulf of Cadiz, IODP Expedition 339 Hernandéz-Molina, Francisco Javier Stow, Dorrik A V Alvarez Zarikian, Carlos A Acton, Gary D Bahr, André Balestra, Barbara Ducassou, Emmanuelle Flood, Roger D Flores, José-Abel Furota, Satoshi Grunert, Patrick Hodell, David A Jiménez-Espejo, Francisco Jose Kim, Jin Kyoung Krissek, Lawrence A Kuroda, Junichiro Li, Bill Llave, Estefania Lofi, Johanna Lourens, Lucas Joost Miller, Max Nanayama, Futoshi Nishida, Naohisa Richter, Carl Roque, C Pereira, H Sanchez Goñi, Maria Fernanda Sierro, Francisco Javier Singh, Arun Deo Sloss, Craig Takashimizu, Yasuhiro Tzanova, Alexandrina Voelker, Antje H L Williams, Trevor J Xuan, Chuang Event label; Exp339; File format; File size; Gulf of Cádiz, Atlantic Ocean; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; Mediterranean Outflow; P74-45; PD00-833; Reference/source; Seismic reflection profile; SEISREFL; Uniform resource locator/link to graphic 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. |
| title | Seismic multichannel reflection profiles from the Gulf of Cadiz, IODP Expedition 339 |
| topic | Event label; Exp339; File format; File size; Gulf of Cádiz, Atlantic Ocean; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; Mediterranean Outflow; P74-45; PD00-833; Reference/source; Seismic reflection profile; SEISREFL; Uniform resource locator/link to graphic |
| url | https://doi.org/10.1594/PANGAEA.832885 |