Ichthyornithiformes
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Ichthyornithes is an extinct group of toothed
avialans Avialae ("bird wings") is a clade containing the only living dinosaurs, the birds. It is usually defined as all theropod dinosaurs more closely related to birds (Aves) than to deinonychosaurs, though alternative definitions are occasionally used ...
very closely related to the common ancestor of all modern
bird Birds are a group of warm-blooded vertebrates constituting the class Aves (), characterised by feathers, toothless beaked jaws, the laying of hard-shelled eggs, a high metabolic rate, a four-chambered heart, and a strong yet lightweigh ...
s. They are known from
fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...
remains found throughout the late
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of th ...
period of North America, though only two genera, '' Ichthyornis'' and ''
Janavis ''Janavis'' (from the Roman god Janus and the Latin ''avis'' for bird) is an extinct toothed bird, belonging to the Ichthyornithes, from the Late Cretaceous of Belgium. The genus has one named species, ''Janavis finalidens'' (from Latin ''finalis ...
'', are represented by complete enough fossils to have been named. Ichthyornitheans became extinct at the
Cretaceous–Paleogene boundary The Cretaceous–Paleogene (K–Pg) boundary, formerly known as the Cretaceous–Tertiary (K–T) boundary, is a geological signature, usually a thin band of rock containing much more iridium than other bands. The K–Pg boundary marks the end of ...
, along with
enantiornitheans The Enantiornithes, also known as enantiornithines or enantiornitheans in literature, are a group of extinct avialans ("birds" in the broad sense), the most abundant and diverse group known from the Mesozoic era. Almost all retained teeth and cl ...
, 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 The Cenomanian is, in the ICS' geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in the s ...
age of the
Late Cretaceous The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the ...
. Based on fragmentary fossil remains, the two known species present in the
Ashville Formation The Ashville Formation is a geological formation in Saskatchewan and Manitoba whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel, David B; et al. (2004). "Di ...
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 In ecology, a niche is the match of a species to a specific environmental condition. Three variants of ecological niche are described by It describes how an organism or population responds to the distribution of resources and competitors (for ...
for a very long period. 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. The study describing ''Protodontopteryx'' notes some "striking" similarities between the jaw structure of ichthyornitheans and Pelagornithidae, pelagornithids. The study still classifies pelagornithids as neognaths based on a few post-cranial features and recovers them in a polytomy with Galloanserae and Neoaves, but does note that this link is worth investigating and that the pelagornithid palate is not known. A study on an '' Ichthyornis'' endocast reveals that it had a relatively "primitive" brain compared to modern birds, similar to that of ''Archaeopteryx'' and other non-avian theropods. Conversely, it had a palate remarkably convergent with that of modern Neognathae, neognaths.


Classification

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 (biology), order Ichthyornithiformes and the Family (biology), 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.


Species

''Ichthyornis dispar'' from North America and ''Janavis finalidens'' from Belgium are currently the only valid species of ichthyornitheans well-supported enough by distinctive fossil evidence to have received scientific names. 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 The Cenomanian is, in the ICS' geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in the s ...
-age
Ashville Formation The Ashville Formation is a geological formation in Saskatchewan and Manitoba whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel, David B; et al. (2004). "Di ...
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.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.


Relationships

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 ornithurines. The clade names are positioned based on their definitions.


References

{{Taxonbar, from=Q2114071 Prehistoric ornithurans Cenomanian first appearances Maastrichtian extinctions Taxa named by Othniel Charles Marsh