Fig. 4


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Llopis Formation slope facies. (a-c) Sierra de Mariola: a: float from lower member, containing fragment of caprinid rudist, Offneria interrupta Paquier, 1905 (left valve; note diagnostic absence of canals in mid-ventral margin, arrowed, cf. Paquier, 1905, Pl. XI, Figs. 15–17); b: middle member, bioclastic grainstone in massive clinoform bed; c: middle member, floatstone with Chondrodonta (ch) and rudists (ru); d: Casetas del Mayor, distal slope facies in lower limestones of Llopis Formation., containing rounded rudist rubble in grainstone matrix. All scale bars = 10 mm.

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