Ornithocheiromorpha
Ornithocheiromorpha is a group of pterosaurs within the suborder Pterodactyloidea. Fossil remains of this group date back from the Early to Late Cretaceous periods, around 140 to 94 million years ago. Ornithocheiromorphs were discovered worldwide, except Antarctica, though most genera were recovered in Europe, Asia and South America. They were the most diverse and successful pterosaurs during the Early Cretaceous, but throughout the Late Cretaceous they were replaced by better adapted and more advanced pterosaur species such the pteranodontids and azhdarchoids. The most diverse families of the group, the Ornithocheiridae and Anhangueridae, survived until the early Late Cretaceous with Ferrodraco, Ornithocheirus, Cimoliopterus, Lonchodectes and Lonchodraco being some of the last remaining. The Ornithocheiromorpha was defined in 2014 by Andres and colleagues, and they made Ornithocheiromorpha the most inclusive clade containing Ornithocheirus, but not Pteranodon.
Ornithocheiromorphs are considered to be some of the largest animals to have ever flown. Members of this group are also regarded to have some of the largest pterosaur wingspans, such as the one estimated for the huge Tropeognathus, though still not as large as those estimated for the azhdarchids, which may have reached up to. When ornithocheiromorphs first appeared, they were initially scavengers, consisting in a more terrestrial setting, but their success had made them the top predators of the skies, as well as the most common type of fish-eating pterosaur throughout the early Late Cretaceous. Some paleontologists also consider ornithocheiromorphs an earlier step of evolution to the pteranodontids, this is due to the similar flying techniques and flight locomotions, as well as their diet, which mainly consisted of fish, and therefore also hunted very similarly. Ornithocheiromorphs also flew like soaring birds, keeping their wings stretched and rarely flapping. The pteranodontids Pteranodon and Geosternbergia are also found to have had this flight technique, resulting in a much more effective way of hunting over the surface of the water, and therefore had more success than the more primitive scavenging istiodactylids.
History of research
Early discoveries
The first specimens of ornithocheiromorphs were unearthed at a chalk pit near Burham in Kent, England. In 1846, British paleontologist James Scott Bowerbank named and described the remains found as Pterodactylus giganteus, as it was common at that time to assign any new described pterosaur species to Pterodactylus. In the same chalk pit as P. giganteus, two other pterosaur species were discovered. The first was named in 1851 by Bowerbank as Pterodactylus cuvieri, in honor of the prominent German naturalist and zoologist Georges Cuvier, while the second was described in the same year by British paleontologist Sir Richard Owen as Pterodactylus compressirostris.In 1861, further pterosaur specimens were found in the UK, and were given the new species Pterodactylus simus by Owen. British paleontologist Harry Govier Seeley then created the new genus Ornithocheirus for the new species in the same year, the generic name translating as "bird hand" is due to the notion of the time that pterosaurs were the ancestors of modern birds.
In 1869, Seeley reassigned Pterodactylus cuvieri into Ptenodactylus cuvieri, but in 1870, Seeley had realized that the generic name Ptenodactylus had been considered a nomen nudum, and therefore reassigned the species into Ornithocheirus cuvieri. Between 1869 and 1870, Seeley reassigned various species of pterosaurs, including P. cuvieri into newly named species of Ornithocheirus, therefore 27 in total.
Richard Owen wasn't pleased when Seeley published his conclusions in his 1870 book The Ornithosauria, and he therefore considered the name Ornithocheirus to be inappropriate. In 1874, Owen created two new genera, Coloborhynchus, meaning "maimed beak" and Criorhynchus, meaning "ram beak".
While Coloborhynchus consisted in a totally new type species, C. clavirostris, as well as two other species reassigned from Ornithocheirus, Criorhynchus consisted entirely of former Ornithocheirus species, including the type species, O. simus, which was later reassigned by Owen as Criorhynchus simus, as well as 5 other species. In the same year, Owen also reassigned O. cuvieri into Coloborhynchus cuvieri. Seeley later disagreed and didn't accept Owen's position, and he therefore assigned Ornithocheirus simus as the type species of Ornithocheirus in 1881. Seeley had also named a new separate species called O. bunzeli in the same year.
In 1914, English paleontologist Reginald Walter Hooley kept the name Ornithocheirus, but created two new genera: Lonchodectes, meaning "lance biter", and Amblydectes, meaning "blunt biter". This classification was rarely applied at the time, though. The species Pterodactylus compressirostris was formerly transferred to Ornithocheirus in 1870 by Seeley, but it became the type species of Lonchodectes in Hooley's 1914 review of Ornithocheirus. Confusingly, this species was also long regarded, incorrectly, as the type species of Ornithocheirus.
of Pterodactylus cuvieri, now known as Cimoliopterus
In 2013, Brazilian paleontologists Taissa Rodrigues & Alexander Kellner made a deeper analysis on the species Pterodactylus cuvieri. In the analysis, they stated that it needed a separate genus, and assigning it to Ornithocheirus was inappropriate, therefore, they created the new genus called Cimoliopterus, with the new resulting combination Cimoliopterus cuvieri, though its type species still remains as P. cuvieri. The generic name Cimoliopterus combines Κιμωλία, Kimolia, in reference to the white clay of the island Kimolos, and the Latinised Greek word πτερόν, pteron, which means "wing". In the same year, Rodrigues & Kellner also reviewed the species Pterodactylus giganteus, and reassigned it to Lonchodectes, resulting in a Lonchodectes giganteus. Both paleontologists later concluded that the genus Lonchodectes and its type species L. compressirostris were nomina dubia, and therefore L. giganteus needed a new separate genus. Rodrigues & Kellner created the new genus Lonchodraco, and reassigned L. giganteus from Lonchodectes into the new genus, resulting in a new combination called Lonchodraco giganteus. The generic name combines Greek λόγχη, lonchē, with Latin draco, meaning "dragon".
In 1887, Seeley had described new fossil remains from the Isle of Wight, an island off the coast of southern England. He thought it belonged to some kind of bird-like creature, which he named it Ornithodesmus cluniculus. John Whitaker Hulke suggested later that year that Ornithodesmus was a pterosaur, finding it similar to fossils that he had seen before, but Seeley disagreed. Seeley also reported another specimen found on the same site, which was then acquired in the British Museum in 1882. The specimen had been assigned to Ornithocheirus nobilis by Richard Lydekker in 1888, but Seeley considered it another species of Ornithodesmus, which he now considered a species of pterosaur instead of a bird. In 1901, Seeley named the new species as O. latidens, which means "wide tooth".
Reginald Hooley later described two more specimens of O. latidens in 1913, which were collected in 1904 from the sea after a rockfall near Atherfield Point on the Isle of Wight. The first of the specimens was collected, and consisted of a skull, neck and trunk vertebrae, a shoulder blade, an ischium, and parts of the forelimbs. The second specimen was collected in just one block, and it includes parts of the forelimbs and pectoral girdle. These two specimens represent the most complete remains of Cretaceous pterosaurs found in England. Hooley also discussed O. latidens in detail, which led Ornithodesmus to be placed within its own family, Ornithodesmidae. But then his article ended with a discussion wherein it was noted that the palaeontologist Charles William Andrews had expressed doubts as to whether O. latidens belonged in the genus Ornithodesmus, as the vertebrae of the specimen that genus was based on differed markedly from those of Hooley's specimen. The American palaeontologist Samuel W. Williston subsequently reviewed Hooley's article, disagreeing with some of his conclusions about the anatomy and classification of the animal. After Hooley's monograph, little was written about the animal for the rest of the 20th century, and no similar pterosaurs were found for decades.
In 1993 however, the British palaeontologists Stafford C. Howse and Andrew C. Milner concluded that the holotype sacrum and only specimen of O. cluniculus didn't belong to a pterosaur, but instead to a maniraptoran theropod dinosaur. They also pointed out that no detailed attempts had been made to compare the sacrum of O. cluniculus with those of pterosaurs, and that O. latidens had in effect been treated as the type species of the genus Ornithodesmus. Now as a definite species of pterosaur, "O." latidens thus required a new genus name. Howse, Milner, and David Martill in 2001, moved "O." latidens to a new genus called Istiodactylus. The generic name means "sail finger", which refers to the wings of large pterosaurs. After moving "O." latidens into Istiodactylus, they had also named a new family called Istiodactylidae, with Istiodactylus'' as the only member.
Discoveries outside Europe
Other important ornithocheiromorph discoveries include the ornithocheirids Tropeognathus and Anhanguera from the Romualdo Formation in Brazil. Tropeognathus was described with its type species, T. mesembrinus in 1987 by German paleontologist Peter Wellnhofer. The generic name is derived from Greek τρόπις, tropis, meaning "keel", and γνάθος, gnathos, meaning "jaw". The specific name is derived from Koine mesembrinos, "of the noontide", simplified as "southern", in reference to the provenance from the Southern hemisphere. The description then led to an enormous taxonomic confusion. In 1989, Brazilian paleontologist Alexander Kellner considered it an Anhanguera mesembrinus, then a Coloborhynchus mesembrinus by Veldmeijer in 1998, and then a Criorhynchus mesembrinus in 2001 by German paleontologist Michael Fastnacht. T. mesembrinus was then considered a junior synonym of Ornithocheirus simus by British paleontologist David Unwin in 2001, but he then proposed an Ornithocheirus mesembrinus in 2003. In 2013 however, Taissa Rodrigues and Alexander Kellner concluded that Tropeognathus would be valid again, and containing only T. mesembrinus, the type species.The discovery of Anhanguera in 1985 made some authors assign several species of Ornithocheirus to the new genus, this is due to the similarities of Anhanguera and Ornithocheirus. One of which was Ornithocheirus cuvieri, formerly known as Pterodactylus cuvieri, was renamed by David Unwin in 2001 as Anhanguera cuvieri, though in 2013 it has been considered a synonym of Cimoliopterus. Other species of Anhanguera include A. piscator, which is known from a nearly-complete skeleton, and was once proposed to belong to the genus Coloborhynchus, but it has recently been placed back into Anhanguera by Andres and Myers. Another species which is also known from a complete skeleton is A. spielbergi, which was also originally considered as a species of Coloborhynchus in 2003, though in 2018, it has been reassigned to the genus Maaradactylus, specifically to its own species, M. spielbergi.
A discovery in Asia, specifically northwestern China, was reported in 2006. The lake sediments allowed an exceptional preservation of fossils, and therefore paleontologists Qiu Zhanxiang and Wang Banyue started official excavations. Part of the findings consisted of dense concentrations of pterosaur bones, associated with soft tissues and eggs. The site represented a nesting colony that storm floods had covered with mud. Dozens of individuals could be secured to run into the many hundreds. In 2014, a new species was named and described: Hamipterus tianshanensis. It was named by Wang Xiaolin, Alexander Kellner, Jiang Shunxing, Wang Qiang, Ma Yingxia, Yahefujiang Paidoula, Cheng Xin, Taissa Rodrigues, Meng Xi, Zhang Jialiang, Li Ning, and Zhou Zhonghe. The generic name Hamipterus combines that of the Hami region, with the word pteron, meaning "wing", and the specific name refers to the provenance from the Tian Shan, a mountain range. These findings represented an impressively large concentration of pterosaur fossils, and together with the Pterodaustro'' nesting colonies in Argentina, both are regarded as the most diverse fossil concentrations of pterosaurs ever known.
Description
Size
Ornithocheiromorphs were large pterosaurs, with wingspans normally ranging between. Istiodactylus for example, had a wingspan ranging from, with the most complete known skull estimated to have been about in length, based on a long-lost fragment of its jaw reported in 2012. Though its jaws measured only, which was less than 80 percent of the skull's length. Ornithocheirids were typically larger than others of the group and were more successful within the food chain rather than other ornithocheiromorphs, one reason is because of their large size, Ornithocheirus itself had a wingspan measuring. Other ornithocheirids were also regarded with similar wingspans, though the largest is probably Tropeognathus mesembrinus, with a wingspan exceeding, and as the maximum estimate. Another genus which was impresively large is Coloborhynchus, with a total skull length that could have been up to, leading to an estimated wingspan of. However, this species may belong to a different genus. One of the smaller genera includes the boreopterid Boreopterus, which is estimated to have a wingspan of around, but some paleontologists consider it a synonym of Zhenyuanopterus, in this case measuring around in length.Skull and crests
Most ornithocheirids bore distinctive convex "keeled" crests on their snout and underside of their mandible, this was well developed in several genera such as Tropeognathus. The similar Anhanguera possessed jaws that were tapered in width, but expanded into a broad, spoon-shaped rosette at the tip. The jaws are distinguished from its relatives by several differences in the crest and teeth: unlike its close relatives Coloborhynchus and Ornithocheirus, the crest on the upper jaw of Anhanguera didn't begin at the tip of the snout, therefore, it was set farther back on the skull. Several ornithocheiromorphs such as the basal Lonchodectes, had long jaws similar to the ornithocheirids, but were mostly thinner and more elongated. Lonchodectes had many short teeth, and its jaws were compressed vertically. Comparisons between ornithocheirids such as Ornithocheirus led to a conclusion that it had a relatively narrower premaxilla compared to related genera like Coloborhynchus and Anhanguera.Some basal anhanguerians like Cearadactylus had its first preparations with many serious mistakes: the front of the snout and the lower jaws were confused leading to a reconstruction in which the anterior part of the head was upside down. Some of the teeth were extensively restored and enlarged until the wider front of the jaws showed very large and robust teeth projecting outwards. With this arrangement, the maxilla was kinked, and its interlocking teeth suggested that Cearadactylus had a piscivourous diet, allowing the animal to keep hold of slippery fish. Cearadactylus was somewhat similar to ornithocheirids like Coloborhynchus, but it lacked the "keeled" crest on its snout, and therefore it was suggested to be a more basal form of ornithocheiromorph pterosaur. Another smaller genus similar to Cearadactylus is Guidraco. Its holotype skull has a length of, which makes it smaller than other genera. The skull is very elongated however, and a hollow profile is seen, but not very pointed, as the upper edge and the line of the jaw run nearly parallel over most of their length.
Even though most ornithocheiromorphs didn't have a cranial crest like the closely related pteranodontids, there were some exceptions, this included Caulkicephalus and Ludodactylus. While Ludodactylus is suggested to be a more basal member of the group, Caulkicephalus is more similar to ornithocheirids. This is due to its rounded snout, very similar to that of Ornithocheirus and therefore it was placed within Ornithocheiridae. Caulkicephalus was also a large pterosaur, with wingspan estimates of around.
Wings
Most pterosaurs of this group had extensive wing-membranes, which were distended by a long wing-finger and would have been covered in hair-like pycnofibres. Like the modern-day albatross, ornithocheiromorphs also had a high aspect ratio and low wing loadings, though this is typically in the larger and more advanced genera. Wing remains of the istiodactylid Nurhachius have been compared to those of modern soaring birds, which fly with little flapping, and may have been ideal for low-energy soaring, which is necessary when searching for carrion or fish. The wings of istiodactylids also seem to have been shorter compared to the fish-eating ornithocheirids, and unlike them, which were more suited for taking off and landing, istiodactylids may have preferred a more terrestrial setting. This is also seen in many inland soaring birds, which have a lower aspect ratio compared those that soar over the ocean. Huge genera such as Tropeognathus and Ornithocheirus are considered to have flown similar to modern-day albatrosses, which consisted on travelling very long distances and rarely flapping. This technique is mostly seen in later pterosaur locomotion, such as the related and mentioned pteranodontids, though not so common in the larger azhdarchids such as Hatzegopteryx and Quetzalcoatlus.Shoulder girdle
Ornithocheiromorphs had shoulder girdles of strong structure, which transferred the forces of a rarely flapping flight to the thorax.The shoulder girdle was probably covered by thick muscle layers, with the upper bone resulting in some kind of straight bar. The shoulder blade was connected to a lower bone called the coracoid, which is relatively long in most ornithocheiromorphs. In the more advanced species, the shoulder is combined whole, with the scapulocoracoid, being almost vertically oriented, meaning that it fitted into a recess in the side of the notarium, while the coracoid likewise connected to the breastbone. Some species also had the shoulder joint moved from the shoulder blade to the coracoid. The breastbone is somewhat wide, and was formed by fused paired sterna. At its rear, a row of belly ribs or gastralia was present, covering the entire belly. To the front of the breastbone, a long point called the cristospina, jutted obliquely upwards, and the rear edge of the breastbone was the deepest point of the thorax. The absence of clavicles or interclavicles had made paleontologists wonder if pterosaurs evolved in different ways than other archosaurs.
Vertebrae
The vertebral column of ornithocheiromorphs was heavily pneumatized by an extensive system of air sacs, leaving prominent pneumatic foraminae. The neck of ornithocheiromorphs was typically relatively long and robust, being longer than the torso in some derived clades. The neural spines of ornithocheiromorph cervical vertebrae were generally tall and spikelike. In some genera such as Tropeognathus and Istiodactylus, up to six dorsal vertebrae are fused into a notarium. In some genera such as Anhanguera, four to seven sacral vertebrae are fused into a synsacrum. The tail is not well-known in ornithocheiromorphs, however. Zhenyuanopterus, which is known for having 13 caudal vertebrae, formed one of the longest tails of any pterodactyloid. Anhanguera, another well-known genus, had a shorter tail, with broad caudal vertebrae that bore a "duplex" cross-section similar to Pteranodon.Pelvic structure
The pelvis of ornithocheiromorphs was of moderate size compared to the body as a whole, similar to other ornithocheiroids. The three pelvic bones were often fused, as seen in many species such as Anhanguera santanae, the ilium was long and low, and its front and rear blades projected horizontally beyond the edges of the lower pelvic bones. Despite the structure length, the processes of these rod-like forms indicate that the hindlimb muscles attached to them were limited in strength. The pubic bone was fused with the broad ischium into an ischiopubic blade, resulting in a narrow build. Sometimes, the blades of both sides were fused, closing the pelvis from below and forming the pelvic canal. The front of the pubic bones was also articulated with a unique structure, resulting in a pair of prepubic bones within. This formed a cusp covering the rear belly, and was located between the pelvis and the belly ribs. The hip joint of ornithocheiromorphs was not perforated and allowed considerable mobility to the leg, and suggests that it was vertical, as therefore had a function in breathing, compensating the relative rigidity of the chest cavity.Hindlimbs
The hindlimbs of ornithocheiromorphs were strongly built, yet relative to their wingspans, smaller than those of birds in terms of hindlimb-to-wingspan ratio. The hindlimbs were long in comparison to the torso length, and the thighbone was rather straight, with the head making only a small angle with the shaft. This implied the legs not being held vertically below the body, but were somewhat sprawling within. A tibiotarsus is mostly seen in many ornithocheiromorphs, this consisted on the shinbone being fused with the upper ankle bones, resulting in a longer structure than the thighbone, which could attain a vertical position when walking. Most of the toes of ornithocheiromorphs were long, though compared to earlier forms of pterosaurs, they were less robust, and were also connected to the ankle in a higher position than the other metatarsals. Often curved, the mobile clawless fifth toe consisted of two phalanges, this is seen some specimens, which showed membranes between the toes, and was concluded that this allowed them to function as flight control surfaces.Classification
Several studies show that ornithocheiromorphs were less derived than the toothless pteranodontids such as Pteranodon, and based on the different evolutionary changes, they therefore need to be grouped in a different clade than Pteranodon, though still within Pteranodontoidea. Early and controversial morphological comparisons of ornithocheiromorphs were made in 1913 by Hooley, with Istiodactylus as the sole member of Istiodactylidae. In the comparisons, different species were assigned within Ornithocheiridae, such as Coloborhynchus, but the data recovered from several ornithocheiromorphs in that time was limited, so specific placements were scarce. During the first phylogenetic analyses of Istiodactylus, it was considered to be some sort of rhamphorhynchid pterosaur, similar to Scaphognathus or maybe even the earlier Dimorphodon, but later studies show that it was closer related to the short-tailed pterodactyloids. With the discoveries of Tropeognathus and Anhanguera in the 1980s, it made more sense to group Istiodactylus with Ornithocheiridae, due to their very similar aspects. This also added to the reassigning of other istiodactylids and other similar toothed pterosaurs within Ornithocheiridae, which then led to debates between two schools of pterosaur classification. In 2003, David Unwin considered Istiodactylidae to group with the toothless Pteranodontidae, though still within Ornithocheiroidea, but Alexander Kellner grouped it with the toothed Ornithocheiridae instead, resulting in a more understandable change of evolution between the two toothed families.Studies on Lonchodectes and its family, Lonchodectidae, has since been classified to many different clades, including Ctenochasmatoidea and Azhdarchoidea. More recent reclassifications show that Lonchodectidae was instead a closer relative of the ornithocheirids, but was given a basal placement because of uncertain fossil structures and other features seen uniquely in Lonchodectes. The genus Prejanopterus was formerly considered a lonchodectid, but its placement is very uncertain, and some authors just consider it a basal archaeopterodactyloid. Another genus, Lonchodraco, is also in a dubious placement, Rodrigues & Kellner made a family called Lonchodraconidae containing only Lonchodraco, but it was then reclassified to Lonchodectidae along with Lonchodectes, and therefore synonymizing the two families.
Brian Andres and colleagues found the families Istiodactylidae, Ornithocheiridae and Anhangueridae to form a group in 2014, which he called Lanceodontia, and consists of the more advanced ornithocheiromorphs. The clade however, excludes the more poorly known family Lonchodectidae, even though members of the family had previously been seen as some of the most derived forms of toothed pterosaurs. In their analysis, they also included the family Boreopteridae within the clade Anhangueria, though placed in a more basal position, while also containing the genus Guidraco. In 2018 however, Nicholas Longrich and colleagues found Boreopteridae outside Anhangueria as the sister taxon of the family Lonchodectidae, both groups placed as basal members of the more inclusive group Lanceodontia.
Phylogeny
Below is a cladogram showing the results of a phylogenetic analysis presented by Longrich et al.. In the analysis, they placed the former istiodactylid Hongshanopterus as a basal member, and also found Guidraco as the sister taxon of the more derived Ludodactylus, meaning that Guidraco is placed in a more derived position, which contradicts the earlier analysis by Andres et al. in 2014. Longrich et al. also included the ornithocheirid Siroccopteryx in their analysis, more precisely as the sister taxon of Coloborhynchus.in flight
In 2019, new species of ornithocheiromorphs were found, and the former species Ornithocheirus wiedenrothi was renamed as Targaryendraco wiedenrothi. The discovery of Iberodactylus in Spain also made paleontologists reclassify the genus Hamipterus in a newly named family called Hamipteridae. The former ornithocheirid Cimoliopterus was also reclassified as well, and it is currently grouped with Aetodactylus and Camposipterus in the newly named clade Targaryendraconia, specificaly to its own family, the Cimoliopteridae. The former istiodactylid Haopterus was reclassified due to the discovery of Mimodactylus, and it's placed as the sister taxon of it in a new family called Mimodactylidae.
The cladogram below is a topology recovered by Pentland et al. in 2019. In the analysis, they found a different set than the previous analysis by Longrich et al. ; they recovered Lonchodectes outside Lanceodontia, while also replacing the name Boreopteridae to Boreopterinae. Pentland et al. also included the genera Ferrodraco and Mythunga in their analysis, where they placed them within the subfamily Ornithocheirinae as sister taxa.
and Mythunga, and holotype mandible of the targaryendraconian Aussiedraco
Paleobiology
Diet and feeding
Ornithocheiromorphs were originally regarded as piscivorous creatures, feeding mainly on small and mid-sized fish. Some paleontologists even suggested details on how these pterosaurs caught fish, some of which included dipping their beaks close to the water for prey. Hooley for example, found that the beak of the well known Istiodactylus was similar to those of birds such as herons, storks, and skimmers, and suggested that Istiodactylus probably fed on fish, this was mainly based on his 1913 jaw reconstruction of the animal. In 1991, Peter Wellnhofer compared the jaw endings of Istiodactylus with those of a duck, but he then noticed that it wasn't a "duck-billed pterosaur" or anything similar, even though it was popularly called that way. Other diet suggestions for Istiodactylus were mostly based on the broad snout remains, as well as the very distinctive teeth; leading to the thought of a more terrestrial life and hunting methods, which is far different from the lifestyle of later genera such as the huge Tropeognathus. This conclusion was later followed by Howse and colleagues suggesting that the strong, yet bizarre teeth of Istiodactylus were more suited for scavenging carcasses rather than catching fish, this led the idea of a different feeding technique, which consisted in bitting and twisting the skull to remove large chunks out of the carcass, very different from the initial suggestions of how early ornithocheiromorphs fed. Witton in 2012 found that the teeth of Istiodactylus were unlike the recurved and enlarged teeth seen in the more derived ornithocheirids such as Ornithocheirus, he instead pointed out that it was more "razor-edged" and better suited for carrion rather than fish.Another ornithocheiromorph that possesed similar features to Istiodactylus is Liaoxipterus, which is known from a skull with several unique traits, including numerous peg-like teeth. The shape of its teeth indicated that Liaoxipterus was a possible insectivore, though this conclusion isn't considered entirely accurate. Liaoxipterus was also smaller in size compared to Istiodactylus and other ornithocheiromorphs, this is perhaps an indication that the more primitive members of this group were smaller compared to more derived and advanced families such as the lonchodectids, ornithocheirids and targaryendraconians. This can also be seen in the size comparison between ornithocheirids and istiodactylids, with the wingspan of Tropeognathus for example, measuring almost double that of Istiodactylus.
stealing prey from a Lonchodectes, both were derived members of this group and possible fish hunters
Ornithocheirids like Tropeognathus and Coloborhynchus are considered to be fish-eaters, and had longer and sharper teeth compared to the more rounded teeth of Istiodactylus'', though this is still sometimes disputed. Another difference that can be seen in more primitive ornithocheiromorphs their eyes being proportionally smaller compared to the assumed predatory and more advanced ornithocheirids, this again adds to the fact that the more primitive groups were most likely scavengers, and later got more successful within the food chain, leading the later, more advanced groups to be the dominant fish hunters during the early Late Cretaceous.
Teeth enamels
A 2017 study confirmed that most ornithocheirids were fish-eaters, though in a deeper analysis, paleontologists found carbon isotopes within several teeth, and later compared the enamel values of the ornithocheirid teeth between the aquatic and terrestrial consumers near the fossil site. Pterosaur enamels from the Twin Mountains Formation were shown with lower enamel values in comparison to the aquatic consumers that lived near, suggesting a more terrestrial diet, this is mostly due to the similarly low enamel values found in carnivorous theropods such as Acrocanthosaurus, which mainly had a terrestrial diet. The enamels found in the Paw Paw Formation however, were described with higher values, in comparison to the nearby terrestrial consumers. Analyzing these enamel remains, paleontologists found out that the values seen were more comparable to the aquatic consumer values rather the terrestrial ones. These analyses are considered a very useful reference to the evolutionary changes between the earlier and later species of ornithocheirids, as well as other ornithocheiromorphs. The diet changes were also taken into account, with earlier genera such as Coloborhynchus having a varied diet, preying partially on fish, while also hunting on land. The later genera such as Uktenadactylus however, fed almost entirely on fish, and rarely hunted on land. This can be demonstrated with the age difference between the Twin Mountains Formation and the Paw Paw Formation. The enamel remains found in the Twin Mountains Formation dated back to the earlier Aptian stage, while the remains found in the Paw Paw Formation dated back to the later Albian stage, resulting in a slight diet transition between more primitive and more derived genera.Respiration
Pterosaur studies in 2009 showed that several pterosaurs, including ornithocheiromorphs, had a lung-and-air-sac system and a precisely controlled skeletal breathing pump, which supports a flow-through pulmonary ventilation model in pterosaurs, analogous to that of birds. This breathing method is also seen is carnivorous dinosaurs such as Aerosteon, but there are currently no studies showing its relationships with pterosaurs. A air sac system is present in at least some species of pterodactyloids, and this technique would have given a further reduced density to the living animal when breathing. Similar to modern crocodilians, many ornithocheiromorph genera appeared to have had some kind of hepatic piston, regarding their shoulder-pectoral girdles, which were suggested to be too inflexible to move the sternum. This can also be seen in modern-day birds, which similarly possess strong gastralia, and therefore paleontologists erect the idea that their respiratory system had characteristics comparable to primitive archosaurs.Locomotion and flight
Ornithocheiromorphs, like other pterosaurs, are considered to have been skilled fliers as well as swift at moving on the ground. Footprints from several species show that most pterosaurs did not sprawl their limbs to a large degree, as in modern reptiles, but rather held the limbs relatively erect when walking, like dinosaurs. While footprints are yet to be known, it is likely that ornithocheiromorphs also walked erect. Compared to other earlier pterosaurs such as rhamphorhynchids, ornithocheiromorphs had unusually uneven limb proportions, with the forelimbs resulting in a much longer scale compared to the hind limbs. Their close relatives, the pteranodontids, were also found with similar features, though they more likely flew like modern-day albatrosses rather than anything else. Paleontologists also suggest that they most likely spend long stretches of time sea fishing, travelling very long distances without flapping while at the same time flying close the surface of the water with exploited wind speed, and without the necesity of thermals. This would likely have required them to use unique modes of locomotion compared to other pterosaurs, this can already be seen in earlier evolutions such as Istiodactylus and Nurhachius, with powerful musculature attachments and well-developed pectoral and upper arm bones. It is also possible that ornithocheiromorphs ran bipedally, or that they used a hopping gait. Many pterosaur researchers like Mike Habib have noted that the limb proportions of some ornithocheiromorphs such as Anhanguera are consistent with hopping, though the scavenging istiodactylids are probably still the best examples of pterosaurs with a more terrestrial setting.Paleoecology
Ornithocheiromorphs were present since the Early Cretaceous, and evolved throughout the rest of the period. Studies on the ornithocheirids Tropeognathus and Anhanguera, suggested that ornithocheiromorphs also expanded their distribution, while also evolving specialized features. The significant adaptions of the ornithocheiromorphs had also made them the top pterosaurs in almost every formation by the early Late Cretaceous, including the ones they were rare in, such as the Blesa Formation in Spain, where only Iberodactylus has been found.Even though the ornithocheiromorphs were discovered worldwide, most of them were concentrated in specific places. One specific fossil site containing an impressive number of pterosaurs is the Romualdo Formation, a diverse Lagerstätte in the larger geologic group called the Santana Group, which is located in the Araripe Basin of northeastern Brazil, and dates back 111-108 million years ago during the Albian stage of the Early Cretaceous. The formation includes many species of Anhanguera, several fossil remains of basal ornithocheiromorphs, including Brasileodactylus, Cearadactylus and Unwindia, as well as the ornithocheirids Tropeognathus, Coloborhynchus, Maaradactylus, Araripesaurus and Barbosania. These pterosaur genera were just some of the many recovered from the site, which also include the thalassodromids Tupuxuara and Thalassodromeus, as well as the tapejarid Tapejara, the basal pteranodontoid Santanadactylus and the dubious Araripedactylus. Some other creatures from the formation include the theropods Irritator, Mirischia and Santanaraptor, and the crocodylomorph Araripesuchus. The formation also includes several turtle remains, with some specimens referring to Santanachelys, Cearachelys and Araripemys. A few fish remains were also found within the Romualdo Formation, some of which were referred to Brannerion, Rhinobatos, Rhacolepis, Tharrhias and Tribodus. The Santana Group also consists of another Lagerstätte called the Crato Formation, which is not as diverse as the Romualdo Formation, but its fossil remains are still considered important. This fossil site underlies the Romualdo Formation, and dates back around 115-113 million years ago during the Aptian stage, meaning that its fossil content is of older age. Similarly, the Crato Formation also contained several species of pterosaurs, including the basal lanceodontians Ludodactylus and Brasileodactylus, as well as the ornithocheirid Arthurdactylus. Other pterosaur genera include the tapejarids Tupandactylus and Aymberedactylus, as well as the chaoyangopterid Lacusovagus. The formation also contains other creatures such as the enantiornithine Cratoavis, the neosuchian Susisuchus, and several species of fish, including Belonostomus, Calamopleurus, Cladocyclus, Dastilbe and Lepidotes. These fish genera were suggested to be prey for the pterosaurs that lived in the formation, but fossil remains are limited, so the subject is still controversial.
Another important fossil site is the Wessex Formation in the Isle of Wight, near the coast of England, which dates back 140-125 million years ago. The formation doesn't contain many fossil remains of pterosaurs compared to the Romualdo Formation, but it is still a very important site. Fossil remains of the istiodactylid Istiodactylus, the ornithocheirid Caulkicephalus, and the tapejarid Wightia were found. The formation is also known for several theropods, including the spinosaurid Baryonyx, the tyrannosauroid Eotyrannus, the dromaeosaurid Ornithodesmus, the compsognathid Aristosuchus as well as the allosauroid Neovenator. Differents types of herbivorous dinosaurs like Iguanodon, Polacanthus, Ornithopsis, Mantellisaurus and Hypsilophodon were also found within the fossil site. Some other animals from the formation include the neosuchian Bernissartia, sea turtles such as Helochelydra and Brodiechelys, the cartilaginous fish Hybodus, ray-finned fishes such as Belonostomus, Caturus, Lepidotes and Scheenstia, as well as the mammals Eobaatar, Loxaulax and Yaverlestes.
on a diagram showing the known material, and based on the related Tropeognathus mesembrinus
A few fossils reported from the Toolebuc Formation and Winton Formation are believed to be from some of the most derived ornithocheiromorphs, due to the age of the fossil remains, which dated back to the Albian and Cenomanian stages of the Cretaceous, and some are even believed to belong to the Turonian stage. The Toolebuc Formation includes several remains of ornithocheiromorphs which are now referred to the genera Aussiedraco and Mythunga. The formation also includes several herbivorous dinosaurs such as the ornithopod Muttaburrasaurus and the ankylosaur Kunbarrasaurus. Fossil remains of marine animals were also uncovered within the fossil site, and some specimens of which belong to the ichthyosaur Platypterygius, the pliosaurid Kronosaurus and the elasmosaurid Eromangasaurus. Turtle remains from turtles that were proposed to be prey for pterosaurs were also found within the Toolebuc Formation, this included the genera Bouliachelys, Cratochelone and Notochelone. The Winton Formation consisted on a more terrestrial environment, containing several sauropod dinosaurs like Austrosaurus, Diamantinasaurus, Savannasaurus and Wintonotitan as well as large carnivorous dinosaurs such as Australovenator and crocodylomorphs like Isisfordia. The formation's only pterosaur is the derived ornithocheirid Ferrodraco, which is also considered as one of the last ornithocheiromorphs, and a close relative of Mythunga. Although these two Australian formations contain some of the most derived members of this group, some specimens from the Chalk Formation in Kent, England probably had a similar or younger age. These fossils dated back around 94 million years ago, and belonged to the lonchodectid Lonchodraco, and the former ornithocheirid Cimoliopterus, which is now reclassified as a targaryendraconian.
Lonchodraco, formerly known as Pterodactylus giganteus, lived throughout the late Cenomanian and early Turonian stages, and Cimoliopterus is also considered to be from the same time. Lonchodraco, along with Lonchodectes'', are both classified as basal members of Ornithocheiromorpha, due to complex taxonomy issues, despite their young ages.