2012
DOI: 10.4000/quaternaire.6252
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Late-middle Pleistocene, late Pleistocene and Holocene palaeo-sea-level records at Agadir and the Atlantic Atlas coastal reach, Morocco: an updated overview

Abstract: Out of the Late Holocene sea-level highstand at ca. 2.7 ka, seven Late Pleistocene and Late-Middle Pleistocene palaeo-sealevels (PSL) are today recorded along the coast of the Atlantic Atlas of Morocco: 1) as near-shore dunes (NSD) deposits, records of two MIS 2 and MIS 3 PSL near 0 m a.s.l. or just below, at 28 and ca. 40 ka; 2) records of three MIS 5a, 5c and 5e PSL between zero and + 8 m a.s.l.; 3) records of two MIS 7 and MIS 9 PSL above + 10 m a.s.l. and near + 20 m a.s.l.. All datable records are placed … Show more

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Cited by 8 publications
(2 citation statements)
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“…5b) that show high-energy-deposited-sediments occurring at the same time as E1 and E2, suggesting a regional forcing causing these marine transgressions. These on-shore deposits were reported in the form of fine sediments layers at the estuaries of Tahaddart (35.5° N) 10,72 and Loukkos (35.15° N) 4 and at the Moulay-Bousalham (34°N) and Oualidia (32°N) lagoons 38,39,54 , and marine gastropods shells deposited at Moulay Douraïne (31° N) 73 . Biogeographic evidence from the NW African coast (28 -19° N) suggests a transgression event taking place around 3.5 kyrs BP 74 , also recorded by wetlands on the Atlantic coast of Spain in addition to another one around 2.8 kyrs BP [75][76][77] .…”
Section: Holocene Climate Variability and Coastal Responses In Northw...mentioning
confidence: 88%
“…5b) that show high-energy-deposited-sediments occurring at the same time as E1 and E2, suggesting a regional forcing causing these marine transgressions. These on-shore deposits were reported in the form of fine sediments layers at the estuaries of Tahaddart (35.5° N) 10,72 and Loukkos (35.15° N) 4 and at the Moulay-Bousalham (34°N) and Oualidia (32°N) lagoons 38,39,54 , and marine gastropods shells deposited at Moulay Douraïne (31° N) 73 . Biogeographic evidence from the NW African coast (28 -19° N) suggests a transgression event taking place around 3.5 kyrs BP 74 , also recorded by wetlands on the Atlantic coast of Spain in addition to another one around 2.8 kyrs BP [75][76][77] .…”
Section: Holocene Climate Variability and Coastal Responses In Northw...mentioning
confidence: 88%
“…Primary lands are heavily folded, tectonized and leveled off (Combe, 1963). Between the first cordon and a line of dead cliffs, there is a gutter or furrow, a depression more or less parallel to the rib line, commonly called « Oulja » (Figure 2) (Guilcher and Joly, 1954;Weisrock, 1980;Weisrock and Fontugne, 1991).…”
Section: Geological and Hydrogeological Frameworkmentioning
confidence: 99%