|Cast of an Ichthyornis dispar skeleton, Rocky Mountain Dinosaur Resource Center|
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Ichthyornithiformes Furbringer, 1888
Ichthyornithes is an extinct group of toothed avialans very closely related to the common ancestor of all modern birds. They are known from fossil remains found throughout the late Cretaceous period of North America, though only one species, Ichthyornis dispar, is represented by complete enough fossils to have been named. Ichthyornitheans became extinct at the Cretaceous–Paleogene boundary, along with enantiornitheans, all other non-avian dinosaurs, and many other animal and plant groups.
Origin and evolution
The earliest known ichthyornitheans appear in the fossil record about 95 million years ago, during the Cenomanian age of the Late Cretaceous. Based on fragmentary fossil remains, the two known species present in the Ashville Formation have not been given names, but overall were very similar to Ichthyornis dispar. I. dispar itself had a very long temporal range, and specimens referred to it or very similar species existed relatively unchanged (other than some fluctuations in average adult size) for nearly 10 million years, when species referable to I. dispar disappeared and were replaced by other, though still somewhat similar, species of ichthyornitheans. The fact that ichthyornitheans appear to have existed virtually unchanged in their general size and anatomy for nearly the entire duration of the late Cretaceous period suggests that their evolutionary pace was in relative stasis compared to other, contemporary species of closely related avialans, like the hesperornitheans. Both the ichthyornitheans and hesperornitheans were strongly linked to their ecosystem in the Western Interior Seaway that bisected North America for much of the Cretaceous. It may be that while the flightless, aquatic hesperornitheans were much more sensitive to changes in shoreline extent and sea level during that time, driving their evolution and adaptation into more specialized forms, the flying, tern-like ichthyornitheans were not as dependent on specific coastal or sea level conditions, and they were able to inhabit basically the same ecological niche for a very long period of time. The icthyornithean lineage finally became extinct in the Cretaceous–Paleogene extinction event that caused the extinction of many major land and marine animal groups at the end of the Mesozoic era. The last ichthyornithean fossils are found in the Hell Creek Formation very close (within 300,000 years at least) of the K-Pg boundary, dated to 66 million years old.
Ichthyornitheans were close to the ancestry of modern birds, the crown group Aves, but represents an independent lineage of toothed seabird-like animals. It was long believed that several similar Cretaceous species known from fragmentary remains, including Ambiortus, Apatornis, Iaceornis and Guildavis, were members of the Ichthyornithes in addition to the group's namesake, Ichthyornis. However, these seem to have been more closely related to modern birds than to Ichthyornis dispar. In Julia Clarke's 2004 review of Ichthyornis-like fossils, the former order Ichthyornithiformes and the family Ichthyornithidae were considered synonyms of the clade Ichthyornithes, which in that paper was defined according to phylogenetic taxonomy as all descendants of the most recent common ancestor of Ichthyornis dispar and modern birds.
Ichthyornis dispar, known from the Niobrara Formation of Kansas, is currently the only valid species of ichthyornithean that is well-supported enough by distinctive fossil evidence to have received a name. However, isolated remains of other ichthyornithean species have been identified. For example, three isolated shoulder bone specimens (RSM P2992.1, UCMP 187207, AMNH 22002) found in the Hell Creek Formation of Montana, Lance Formation of Wyoming, and Frenchman Formation of Saskatchewan have been identified as all belonging to a single species of Ichthyornis-like avialan that inhabited this region of North America at the very end of the Maastrichtian age, within 300,000 years of the Cretaceous-Paleogene extinction event 66 million years ago. Another unnamed species similar to Ichthyornis is known from isolated remains found in Campanian-age rocks from Alberta. Two more species also represented only by fossil shoulder bones are known from the Cenomanian-age Ashville Formation near Carrot River, Saskatchewan. Though originally thought to be species of Ichthyornis, they probably represent one or more new genera. Additional ichthyornithean remains have been described from Russia, suggesting that this group ranged across much of the northern hemisphere in the Cenomanian.
The cladogram below is the result of a 2014 analysis by Michael Lee and colleagues that expanded on data from an earlier study by O’Connor & Zhou in 2012, showing the relationship of Ichthyornis to other ornithurine stem-birds. The clade names are positioned based on their definitions.
- Clarke, J.A. (2004). "Morphology, phylogenetic taxonomy, and systematics of Ichthyornis and Apatornis (Avialae: Ornithurae)" (PDF). Bulletin of the American Museum of Natural History. 286: 1–179. doi:10.1206/0003-0090(2004)286<0001:MPTASO>2.0.CO;2. hdl:2246/454.
- Tokaryk, T.T.; Cumbaa, S.L.; Storer, J.E. (1997). "Early Late Cretaceous birds from Saskatchewan, Canada: the oldest diverse avifauna known from North America". Journal of Vertebrate Paleontology. 17 (1): 172–176. doi:10.1080/02724634.1997.10010961.
- Longrich, N.R.; Tokaryk, T.; Field, D.J. (13 September 2011). "Mass extinction of birds at the Cretaceous–Paleogene (K–Pg) boundary". Proceedings of the National Academy of Sciences. 108 (37): 15253–15257. doi:10.1073/pnas.1110395108. PMC 3174646. PMID 21914849.
- Nikita V. Zelenkov, Alexander O. Averianov & Evgeny V. Popov (2017) An Ichthyornis-like bird from the earliest Late Cretaceous (Cenomanian) of European Russia. Cretaceous Research, 75: 94-100.
- Lee, Michael SY; Cau, Andrea; Darren, Naish; Gareth J., Dyke (May 2014). "Morphological Clocks in Paleontology, and a Mid-Cretaceous Origin of Crown Aves". Systematic Biology. 63 (3): 442–449. doi:10.1093/sysbio/syt110. PMID 24449041.