Pseudofurnishius (Conodonta) in the Triassic of the Betic Cordilleras, SE Spain
Scripta Geologica , Volume 16 p. 1- 23
The stratigraphical position and the fossil content of several Triassic carbonate beds in the Betic Cordilleras are described. Three different conodont faunas have been found: one with Pseudofurnishius murcianus as the dominant species, a second in which Pseudofurnishius murcianus occurs together with Tardogondolella mungoensis mungoensis and a third in which Pseudofurnishius huddlei sp. nov. is the characteristic species.
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van den Boogaard, M, & Simon, O.J. (1973). Pseudofurnishius (Conodonta) in the Triassic of the Betic Cordilleras, SE Spain. Scripta Geologica, 16, 1–23.