Pérez López, Alberto2019-06-032019-06-031992http://hdl.handle.net/10272/16338In Majanillos Formation (middle -upper Ladinian age) of the Subbetic Zone, the bioturbate textures are related with deep ramp facies. F/ieTlialassinoides trace fossil is placed in the middle levels of the formation corresponding to lagoon facies (low energy). And the Diplocaaterion, Rhizocorallium and Chondrites trace fossils are related with the shallower facies of a restricted stonespaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/TriassicMuschelkalkSubbeticTrace fossiljournal articleopen access