Rodríguez Vidal, JoaquínCáceres Puro, Luis MiguelRuiz Muñoz, FranciscoAbad de los Santos, ManuelFinlayson, CliveFinlayson, GeraldineMartínez Aguirre, AranchaFa, Darren A.2014-03-142014-03-142010http://hdl.handle.net/10272/7895During the period represented by the sandy infills of the eastern flank caves and the Catalan Sand formation, it was likely that Gibraltar was part of the mainland, including a broad coastal plain covered with transgressive wind-blown dunes. All aeolian formations originated on marine beaches, from 6 m a.s.l. to 100 m b.s.l., before being blown inland to accumulate as topographic dunes. CUff-front aeolian accumulations comprise echo dunes, climbing dunes and sand ramps. Aeolian deposition began immediately before the last interglacial marine highstand (MIS 6-5 transition) and continued during the subsequent fall in sea level until the end ofMIS 3spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Coastal dunePalaeoenvironmentEvolutionLate PleistoceneGibraltarjournal articleopen access