Iridoy, PeruZudaire, SaioaAzaguirre, MaddiDorronsoro, AneOlano, GalderBeriain, EnekoUsarbarrena, ArianeElorza, Javier2013-12-162013-12-162010http://hdl.handle.net/10272/7509The Sopelana sea-cliff exposes marl-limestone couplets from the Upper Maastrichtian (MS1 and MS2 sections) and the Lower Eocene (EI section), in the deep Basque Arc domain. The high-resolution analysis (% CaCO3) of the MS1 couplets confirms a complex behaviour with strong compositional contrast vs. a more regular MS2 couplets. This may be due to a drastic environmental change (long humid and rainy alternating to drier periods) towards dominant humid and rainy periods, with a minor seasonal nature and high sedimentation rate (72 cm/20 ky). The deep, cold, oxygenated marine water produces a change of coloration (grey to purple) during the sedimentation, in the Upper Maastrichtian couplets before diagenesis activity. It is the beginning of the Cretaceous oceanic red beds (CORB´s)spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/ColourMarl-limestone coupletsLate MaastrichtianEarly EoceneBasque Arcjournal articleopen access