Like other members of its genus, Iapetognathus fluctivagus had ramiform (branching) array of elements (apparatus). It is believed that the ramiform apparatus in Iapetognathus fluctivagus evolved from the coniform (cone-like) apparatus of Iapetonudus ibexensis.[3]
^Iapetonudus (N. gen.) and Iapetognathus Landing, unusual Earliest Ordovician multielement conodont taxa and their utility for biostratigraphy. Robert S. Nicoll, J.F. Miller, G.S. Nowlan, J.E. Repetski, and Raymond L. Ethington, Brigham Young University Geology Studies, 1999, volume 44, pages 27–101
^Designation of holotypes for new species of Iapetonudus Nicoll, Miller, Nowlan, Repetski and Ethington and Iapetognathus Landing. Journal of Micropalaeontology, 1999, volume 18, page 124, doi:10.1144/jm.18.2.124
^Roger A. Cooper; Godfrey S. Nowlan; S. Henry Williams (2001). "Global Stratotype Section and Point for base of the Ordovician System" (PDF). Episodes. 24 (1): 19–28. doi:10.18814/epiiugs/2001/v24i1/005.
Iapetonudus is an extinct genus of conodonts. Like other members of its genus, Iapetognathus fluctivagus had ramiform (branching) array of elements (apparatus)...
Iapetognathus fluctivagus evolved from the coniform (cone-like) apparatus of Iapetonudus ibexensis. It can be readily distinguished from other conodonts existing...
Iapetognathus fluctivagus evolved from the coniform (cone-like) apparatus of Iapetonudus ibexensis. It can be readily distinguished from other conodonts existing...