Apparatus architecture of Pseudofurnishius murcianus (Gondolellidae, Conodonta) and its implications for the evolution of the conodont skeleton
Conodonts are known primarily from their microscopic tooth‐like skeletal feeding elements that occur commonly in jumbled assemblages in marine rocks from the late Cambrian to the Triassic–Jurassic boundary interval. Interpreting their evolution requires a scheme of positional homology of these elements within the f...