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The Middle Bathonian to Middle Oxfordian interval in the Eastern External Subbetic (Betic Cordillera, SE Spain) is characterized by Ammonitico Rosso facies including various stratigraphic breaks. Five hardground-bounded units are recognized in relation to hiatuses in the ammonite record at the following stratigraphic boundaries: Hg1 (Lower–Middle Bathonian), Hg2 (Middle–Upper Bathonian), Hg3 (Lower–Middle...
Taphonomic analysis of cephalopod assemblages, together with analyses of ichnologic and sedimentologic features, are useful tools in the interpretation of the history of unconformities in Jurassic pelagic swells. The External Subbetic presents a complex evolution during the Middle Bathonian–Middle Oxfordian interval that includes hardgrounds and condensed levels rich in ammonoids. Bathonian and Callovian...
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