Gulf of Cádiz
The Gulf of Cádiz (in Spanish: Golfo de Cádiz) is the arm of the Atlantic Ocean between Cabo de Santa Maria (Cape of St. Mary), the southernmost point of Mainland Portugal and Cape Trafalgar (Cabo Trafalgar) at the western end of the Strait of Gibraltar. Two major rivers, the Guadalquivir and the Guadiana, as well as smaller rivers, like the Odiel, the Tinto, and the Guadalete, reach the ocean here.
The Gulf of Cádiz is located in the north-eastern Atlantic Ocean between 34°N and 37°15'N and 6°W to 9°45'W.[1] It is enclosed by the southern Iberian and northern Moroccan margins, west of Gibraltar Strait.[1]
Geology
The geological history of the Gulf of Cádiz is intimately related to plate tectonic interaction between Southern Eurasia and North Africa and is driven by two major mechanisms:[2]
- subduction associated with the westward emplacement of the Gibraltar Arc and formation of the Gulf of Cádiz accretionary wedge.[3] The current activity of the subduction is unclear, with some advocating ongoing active subduction.[2] Others suggest that subduction is inactive and that a new plate boundary has recently formed along a series of prominent WNW-ESE trending lineaments acting as a dextral strike-slip (transform) plate boundary.[4]
- oblique lithosphere collision between Iberia and Nubia. Oblique convergence between Africa (Nubia) and Iberia (Eurasia) occurs here at about 4mm/yr in a NW-SE direction.[5][6] Some have suggested this may also be causing active thrusting in the Gulf of Cadiz.[2][7]
It is now well established that the whole area is under compressive deformation and that mud volcanism and processes associated with the escape of hydrocarbon-rich fluids sustain a broad diversity of chemosynthetic assemblages.[1] The accretionary wedge formed by subduction represents an extensive area which encompasses over forty mud volcanoes (a type of cold seep), at depths ranging from 200 to 4000 m (confirmed by coring), and active methane seepage has been documented on several locations.[1][8]
Biota
The occurrence of chemosymbiotic biota in the extensive mud volcano fields of the Gulf of Cadiz was first reported in 2003.[1][8] There were found mainly pogonophoran worms, but also gastropods and bivalves, polychaetes, crustaceans and echinoderms. There were also recorded dead corals of genera Madrepora and Lophelia.[8] The chemosymbiotic bivalves collected from the mud volcanoes of the Gulf of Cadiz were reviewed in 2011.[1] There were reported the following species of chemosymbiotic bivalves of Solemyidae: Acharax gadirae, Solemya elarraichensis; Mytilidae: Bathymodiolus mauritanicus, Idas sp.; Lucinidae: Lucinoma asapheus; Thyasiridae: Thyasira vulcolutre, Spinaxinus sentosus; Vesicomyidae: Isorropodon perplexum, Isorropodon megadesmus, Callogonia cyrili, Christineconcha regab, Laubiericoncha chuni and Pliocardia sp.[1] There is high degree of endemism within chemosymbiotic bivalve assemblages.[1]
See also
References
- ↑ 1.0 1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 Oliver G., Rodrigues C & Cunha M. R. (2011). "Chemosymbiotic bivalves from the mud volcanoes of the Gulf of Cadiz, NE Atlantic, with descriptions of new species of Solemyidae, Lucinidae and Vesicomyidae". ZooKeys 113: 1-38. doi:10.3897/ZooKeys.113.1402.
- ↑ 2.0 2.1 2.2 2.3 Gutscher, M.-A., Dominguez, S., Westbrook, G., Le Roy, P., Rosas, F.M., Duarte, J.C., Terrinha, P., Miranda, J.M., Gailler, A., Sallares, V., and Bartolome, R., 2012. The Gibraltar subduction: A decade of new geophysical data. Tectonophysics (invited review paper) v. 574-575, p. 72-91, doi: 10.1016/j.tecto.2012.08.038.
- ↑ 3.0 3.1 Gutscher, M.-A., Malod, J., Rehault, J.-P., Contrucci, I., Klingelhoefer, F., Mendes-Victor, L., Spakman, W., 2002. Evidence for active subduction beneath Gibraltar. Geology 30, 1071–1074.
- ↑ 4.0 4.1 Zitellini, N., Gracia, E., Matias, L., Terrinha, P., Abreu, M.A., DeAlteriis, G., Henriet, J.P., Danobeitia, J.J., Masson, D., Mulder, T., Ramella, R., Somoza, L., Diez, S., 2009. The quest for NW Africa–SW Eurasia plate boundary west of Gibraltar. Earth and Planetary Science Letters 280, 13–50. http://dx.doi.org/10.1016/j.epsl.2008.12.005.
- ↑ 5.0 5.1 Stich, D., Serpelloni, E., Mancilla, F.d.L., Morales, J., 2006. Kinematics of the Iberia– Maghreb plate contact from seismic moment tensors and GPS observations. Tectonophysics 426, 295–317. http://dx.doi.org/10.1016/j.tecto.2006.08.004.
- ↑ 6.0 6.1 Koulali, A., Ouzar, D., Tahayt, A., King, R.W., Vernant, P., Reilinger, R.E., McClusky, S., Mourabit, T., Davila, J.M., Amraoui, N., 2011. New GPS constraints on active defor- mation along the Africa–Iberia plate boundary. Earth and Planetary Science Letters 308, 211–217. http://dx.doi.org/10.1016/j.epsl.2011.05.048.
- ↑ 7.0 7.1 Bartolome, R., Gracia, E., Stich, D., Martinez-Loriente, S., Klaeschen, D., Mancilla, F., Lo Iacona, C., Danobeitia, J.J., and Zitellini, N., 2012. Evidence for active strike-slip faulting along the Eurasia-Africa convergence zone: Implications for seismic hazard in the southwest Iberian margin. Geology, v. 40, p. 495–498; doi:10.1130/G33107.1
- ↑ 8.0 8.1 8.2 8.3 Pinheiro L. M., Ivanov M. K., Sautkin A., Akhamanov G., Magalhães V. H., Volkonskaya A., Monteiro J. H., Somoza L., Gardner J., Hamouni N. & Cunha M. R. (2003). "Mud volcanoes in the Gulf of Cadiz: results from the TTR-10 cruise". Marine Geology 195: 131-151. doi:10.1016/S0025-3227(02)00685-0.