Baptornis Temporal range: Late Cretaceous, | |
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Illustration of a tarsometatarsus, 1880 | |
Scientific classification | |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | Saurischia |
Clade: | Theropoda |
Clade: | Avialae |
Clade: | † Hesperornithes |
Family: | † Baptornithidae AOU, 1910 |
Genus: | † Baptornis Marsh, 1877 |
Species: | †B. advenus |
Binomial name | |
†Baptornis advenus Marsh, 1877 [1] | |
Synonyms | |
Parascaniornis Lambrecht, 1933 |
Baptornis ("diving bird") is a genus of flightless, aquatic birds from the Late Cretaceous, some 87-80 million years ago (roughly mid-Coniacian to mid-Campanian faunal stages). The fossils of Baptornis advenus, the type species, were discovered in Kansas, which at its time was mostly covered by the Western Interior Seaway, a shallow shelf sea. It is now known to have also occurred in today's Sweden, where the Turgai Strait joined the ancient North Sea; possibly, it occurred in the entire Holarctic.
Othniel Charles Marsh discovered the first fossils of this bird in the 1870s. This was, alongside the Archaeopteryx , one of the first Mesozoic birds to become known to science.
More material evidence exists for the ecology of B. advenus than for any other member of the Hesperornithes, with the possible exception of Hesperornis regalis, but still much is left to conjecture. The loon-sized bird was of middle size among its relatives and had a markedly elongated neck. Presumably, it thus behaved in a manner similar to today's darters, hunting smaller, more mobile prey than its larger relatives. Unlike a darter however, it could not spear its prey, but instead held it with its beak like today's mergansers.
The waters which it inhabited were fairly shallow epicontinental or shelf seas. Remains found far off the prehistoric shore suggest that it either ventured far out and/or that it bred on islands. A considerable number of juvenile specimens are known. These tend to be from the northern part of its range - today's Canada and Alaska - though they have also been found in Kansas. This suggests that the birds were migratory like some penguins are today, moving polewards in summer to breed. The Cretaceous had a much warmer climate than today; the waters inhabited by Baptornis were subtropical to temperate.
While it was excellently adapted to swimming and diving, Baptornis is thought to have been clumsy on land, pushing itself along the rocks with its feet rather than actually walking. The natural position of the lower legs was flush against the body, with the feet stretched out sideways and thus it would have been unable to move upright without toppling over. As opposed to Hesperornis which almost certainly had to slide on its belly or galumph like an earless seal, Baptornis's lower leg was not as firmly placed along the body sides. Thus, it would have found it more easy to place its feet under its body with the toes pointing forwards and might have managed small hops or even an awkward waddle, body held low to the ground.
The only certain record of Hesperornithes' food found so far comes from Baptornis: Specimen UNSM 20030 was found associated with some coprolites. These are small round lumps - maybe a centimeter in diameter or so - and contain the remains of a small species of the sabre-toothed "herring" Enchodus , possibly E. parvus. Baptornis had powerful gastric juices and/or regurgitated most indigestible parts of its prey as a pellet like most living fish-eating birds do, because the Enchodus remains make up only a small fraction of the coprolites' mass, most of which was nondescript feces.
Baptornis was related to the bigger, better known Hesperornis . Both belonged to the Hesperornithes, a group of prehistoric birds which were uniquely adapted to diving and swimming, and had teeth. Otherwise, they were fairly similar to living birds rather than to more dinosaur-like forms such as Archaeopteryx or the Enantiornithes.
As Baptornis was quite peculiar among the Hesperornithes, the family Baptornithidae has been established for it. Presently this is considered monotypic by most. However, it was recently established [2] that the supposed "Cretaceous flamingo" Parascaniornis stensioi from the Late Cretaceous of Ivö Island in Sweden was not a flamingo and neither, as suggested by others, a gaviiform (loon) nor a procellariiform, but in fact belongs with Baptornis. As there is insufficient material for a proper comparison, it is not known whether it is also a junior synonym of B. advenus or a second species.
In 2004, it was announced that material of a second species were being prepared for description. This specimen was about twice as massive as the type of B. advenus. The bones had been found in the lower Pierre Shale of SW South Dakota. [3] James Martin and Amanda Cordes-Person named this species Baptornis varneri in 2007, but it was later reclassified as a species of the genus Brodavis and may not have been closely related to B. advenus. [4]
In addition, two other prehistoric diving birds of the Late Cretaceous are sometimes placed in the Baptornithidae:
Potamornis is in all probability a member of the Hesperornithes. However, it is unclear with which of these it is most closely allied; some place it in the Baptornithidae.
More interesting - or controversial - is the case of Neogaeornis . This bird, whose remains were found in Chile, might be a baptornithid also. Others consider it closely related to certain modern birds, either the Gaviiformes, or the Procellariiformes.
Gaviiformes is an order of aquatic birds containing the loons or divers and their closest extinct relatives. Modern gaviiformes are found in many parts of North America and northern Eurasia, though prehistoric species were more widespread.
Hesperornithes is an extinct and highly specialized group of aquatic avialans closely related to the ancestors of modern birds. They inhabited both marine and freshwater habitats in the Northern Hemisphere, and include genera such as Hesperornis, Parahesperornis, Baptornis, Enaliornis, and Potamornis, all strong-swimming, predatory divers. Many of the species most specialized for swimming were completely flightless. The largest known hesperornithean, Canadaga arctica, may have reached a maximum adult length of 2.2 metres (7.2 ft).
Ichthyornis is an extinct genus of toothy seabird-like ornithuran from the late Cretaceous period of North America. Its fossil remains are known from the chalks of Alberta, Alabama, Kansas, New Mexico, Saskatchewan, and Texas, in strata that were laid down in the Western Interior Seaway during the Turonian through Campanian ages, about 95–83.5 million years ago. Ichthyornis is a common component of the Niobrara Formation fauna, and numerous specimens have been found.
Hesperornis is a genus of cormorant-like bird that spanned the first half of the Campanian age of the Late Cretaceous period. One of the lesser-known discoveries of the paleontologist O. C. Marsh in the late 19th century Bone Wars, it was an early find in the history of avian paleontology. Locations for Hesperornis fossils include the Late Cretaceous marine limestones from Kansas and the marine shales from Canada. Nine species are recognised, eight of which have been recovered from rocks in North America and one from Russia.
Enchodus is an extinct genus of aulopiform ray-finned fish related to lancetfish and lizardfish. Species of Enchodus flourished during the Late Cretaceous, and survived the Cretaceous–Paleogene extinction event, persisting into the late Eocene.
Mosasaurus is the type genus of the mosasaurs, an extinct group of aquatic squamate reptiles. It lived from about 82 to 66 million years ago during the Campanian and Maastrichtian stages of the Late Cretaceous. The earliest fossils of Mosasaurus known to science were found as skulls in a chalk quarry near the Dutch city of Maastricht in the late 18th century, which were initially thought to have been the bones of crocodiles or whales. One skull discovered around 1780, which was seized by France during the French Revolutionary Wars for its scientific value, was famously nicknamed the "great animal of Maastricht". In 1808, naturalist Georges Cuvier concluded that it belonged to a giant marine lizard with similarities to monitor lizards but otherwise unlike any known living animal. This concept was revolutionary at the time and helped support the then-developing ideas of extinction. Cuvier did not designate a scientific name for the new animal, and this was done by William Daniel Conybeare in 1822 when he named it Mosasaurus in reference to its origin in fossil deposits near the Meuse River. The exact affinities of Mosasaurus as a squamate remain controversial, and scientists continue to debate whether its closest living relatives are monitor lizards or snakes.
Tylosaurus is a genus of mosasaur, a large, predatory marine reptile closely related to modern monitor lizards and to snakes, from the Late Cretaceous.
Iberomesornis is a monotypic genus of enantiornithine bird of the Cretaceous of Spain.
Odontornithes is an obsolete and disused taxonomic term proposed by Othniel Charles Marsh for birds possessing teeth, notably the genera Hesperornis and Ichthyornis from the Cretaceous deposits of Kansas.
Gansus is a genus of aquatic birds that lived during the Aptian age of the Early Cretaceous (Aptian-Albian) period in what are now Gansu and Liaoning provinces, western China. The rock layers from which their fossils have been recovered are dated to 120 million years ago. It was first described in 1984 on the basis of an isolated left leg. It is the oldest-known member of the Ornithurae, the group which includes modern birds (Neornithes) and extinct related groups, such as Ichthyornis and Hesperornithes.
Platecarpus is an extinct genus of aquatic lizards belonging to the mosasaur family, living around 84–81 million years ago during the middle Santonian to early Campanian, of the Late Cretaceous period. Fossils have been found in the United States and possible specimens in Belgium and Africa. A well-preserved specimen of Platecarpus shows that it fed on moderate-sized fish, and it has been hypothesized to have fed on squid, and ammonites as well. Like other mosasaurs, it was initially thought to have swum in an eel-like fashion, although another study suggests that it swam more like modern sharks. An exceptionally well-preserved specimen of P. tympaniticus known as LACM 128319 shows skin impressions, pigments around the nostrils, bronchial tubes, and the presence of a high-profile tail fluke, showing that it and other mosasaurs did not necessarily have an eel-like swimming method, but were more powerful, fast swimmers. It is held in the Natural History Museum of Los Angeles County. Isotopic analysis on teeth specimens has suggested that this genus and Clidastes may have entered freshwater occasionally, just like modern sea snakes.
Polarornis is a genus of prehistoric bird, possibly an anserimorph. It contains a single species Polarornis gregorii, known from incomplete remains of one individual found on Seymour Island, Antarctica, in rocks which are dated to the Late Cretaceous.
Neogaeornis is a controversial prehistoric genus of diving bird. The single known species, Neogaeornis wetzeli, was described from fossils found in the Campanian to Maastrichtian Quiriquina Formation of Chile. It lived about 70-67 million years ago. It remains known from the single tarsometatarsus described in 1929 by Lambrecht, and today housed in the Paläontologisches Institut und Museum in Kiel, Germany.
Scaniornis is a prehistoric bird genus. The only known species, Scaniornis lundgreni, lived in the MP 1–5.
Asiahesperornis is a prehistoric foot-propelled diving toothed flightless bird genus from the Late Cretaceous. The single known species is Asiahesperornis bazhanovi. It lived in what today is Kazakhstan, at its time the shores of the shallow Turgai Sea.
Parahesperornis is a genus of prehistoric flightless birds from the Late Cretaceous. Its range in space and time may have been extensive, but its remains are rather few and far between, at least compared with its contemporary relatives in Hesperornis. Remains are known from central North America, namely the former shallows of the Western Interior Seaway in Kansas. Found only in the upper Niobrara Chalk, these are from around the Coniacian-Santonian boundary, 85-82 million years ago (mya).
Limenavis is a prehistoric bird genus from the Late Cretaceous. It lived about 70 million years ago, around the Campanian-Maastrichtian boundary. Known from several broken bones, the remains of the only known species Limenavis patagonica were found in rocks of the "lower member" of the Allen Formation at Salitral Moreno, 20 km south of General Roca, Río Negro (Argentina). It is the closest relative, in the fossil record, of the modern birds.
Canadaga is a flightless bird genus from the Late Cretaceous. The single known species is Canadaga arctica. It lived in the shallow seas around what today is Bylot Island in Nunavut, Canada. Its fossils were found in rocks dated to the mid-Maastrichtian age, about 67 million years ago.
Ornithurae is a natural group which includes the common ancestor of Ichthyornis, Hesperornis, and all modern birds as well as all other descendants of that common ancestor.
Brodavis is a genus of freshwater hesperornithiform birds known from the Late Cretaceous of North America and Asia. It was first described and named by Larry D. Martin, Evgeny N. Kurochkin and Tim T. Tokaryk in 2012 and assigned to a new monogeneric family, Brodavidae. Four species were described and assigned to Brodavis.