Quantitative study of a hippuritid rudist lithosome in a Santonian carbonate platform in the southern Central Pyrenees

The Santonian carbonate platform deposits of the Sant Corneli anticline in the southern Central Pyrenees contain distinctive lenticular to tabular lithosomes formed by congregations of slender hippuritid rudists. Here we make a quantitative study of one of the lithosomes in the Sant Pere de Vilanoveta Member, in the northern side of Sant Corneli. It is exposed over some 4 km, along a WNW–ESE section, and shows a remarkably persistent thickness up to a maximum of 5.15 m, though for the most part it is less than 3 m thick. In the lithosome, hippuritid shells are mostly preserved inclined about 30°–60° from the perpendicular with respect to bedding. The majority of inclined shells lean towards the southwestern to southeastern quadrants, the inferred principal downstream direction. Hippuritids are loosely clustered and supported in a fine bioclastic matrix. Percentage cover of hippuritids ranges from 19.8% at the base to 31.9% in the middle and top of the lithosome. The preliminary data on numerical densities (number of individuals per unit area) of hippuritids show some clustering around values of about 290–750 individuals per m2. The inclined orientation of hippuritid shells seems original and the result of active growth by the animals. The high numerical density of hippuritids at the base of the lithosome may indicate that the hippuritid congregation grew rapidly. The congregation appears to have reached an optimal level of density by the middle of the lithosome and to have maintained it through time during the development of the rudist congregation. The lithosome lacks relief and has no evidence of any rigid framework.