Seismic multichannel reflection profiles from the Gulf of Cadiz, IODP Expedition 339

  1. Hernandéz-Molina, Francisco Javier
  2. Stow, Dorrik A V
  3. Alvarez Zarikian, Carlos A
  4. Acton, Gary D
  5. Bahr, André
  6. Balestra, Barbara
  7. Ducassou, Emmanuelle
  8. Flood, Roger D
  9. Flores, José-Abel
  10. Furota, Satoshi
  11. Grunert, Patrick
  12. Hodell, David A
  13. Jiménez-Espejo, Francisco Jose
  14. Kim, Jin Kyoung
  15. Krissek, Lawrence A
  16. Kuroda, Junichiro
  17. Li, Bill
  18. Llave, Estefania
  19. Lofi, Johanna
  20. Lourens, Lucas Joost
  21. Miller, Max
  22. Nanayama, Futoshi
  23. Nishida, Naohisa
  24. Richter, Carl
  25. Roque, C
  26. Pereira, H
  27. Sanchez Goñi, Maria Fernanda
  28. Sierro, Francisco Javier
  29. Singh, Arun Deo
  30. Sloss, Craig
  31. Takashimizu, Yasuhiro
  32. Tzanova, Alexandrina
  33. Voelker, Antje H L
  34. Williams, Trevor
  35. Xuan, Chuang
  36. Erakutsi egile guztiak +

Argitaratzaile: PANGAEA

Argitalpen urtea: 2014

Mota: Dataset

DOI: 10.1594/PANGAEA.832885 lock_openSarbide irekia editor

Laburpena

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.