99-478: Ornithocheirus (from Ancient Greek "ὄρνις", meaning bird , and "χεῖρ", meaning hand ) is a pterosaur genus known from fragmentary fossil remains uncovered from sediments in the United Kingdom and possibly Morocco . Several species have been referred to the genus, most of which are now considered as dubious species, or members of different genera, and the genus is now often considered to include only
198-433: A type species . When Seeley published his conclusions in his 1870 book The Ornithosauria , this provoked a reaction by the leading British paleontologist of his day, Sir Richard Owen . Owen was not an evolutionist and he therefore considered the name Ornithocheirus to be inappropriate; he also thought it was possible to distinguish two main types within the material, based on differences in snout form and tooth position —
297-435: A Russian-language overview of Pterosauria designated the species Lonchodectes compressirostris , which was identified as Pterodactylus compressirostris in the overview, as the type species of Ornithocheirus , which was then followed by Kuhn in 1967, and Wellnhofer in 1978, yet those authors weren't aware that back in 1881, Seeley made already made the species P. simus as the type species of Ornithocheirus , in which defined
396-401: A body mass of 20 kg (44 lb). A topology made by Andres and Myers in 2013 placed Ornithocheirus within the family Ornithocheiridae in a more derived position than Tropeognathus , but in a more basal position than Coloborhynchus , and the family itself is placed within the more inclusive clade Ornithocheirae . In 2019, Pêgas et al. found Ornithocheirus to be in a basal member of
495-402: A cusp covering the rear belly, between the pelvis and the belly ribs. The vertical mobility of this element suggests a function in breathing, compensating the relative rigidity of the chest cavity. The hindlimbs of pterosaurs were strongly built, yet relative to their wingspans smaller than those of birds. They were long in comparison to the torso length. The thighbone was rather straight, with
594-458: A few millimetres thin transversely. The bony crest base would typically be extended by keratinous or other soft tissue. Since the 1990s, new discoveries and a more thorough study of old specimens have shown that crests are far more widespread among pterosaurs than previously assumed. That they were extended by or composed completely of keratin, which does not fossilize easily, had misled earlier research. For Pterorhynchus and Pterodactylus ,
693-411: A flying creature in a letter to Georges Cuvier . Cuvier agreed in 1801, understanding it was an extinct flying reptile. In 1809, he coined the name Ptéro-Dactyle , "wing-finger". This was in 1815 Latinised to Pterodactylus . At first most species were assigned to this genus and ultimately "pterodactyl" was popularly and incorrectly applied to all members of Pterosauria. Today, paleontologists limit
792-534: A junior synonym of O. simus . Misassigned species: Cimoliornis diomedeus , Cretornis hlavatschi , and Palaeornis clifti , originally misidentified as birds, were once referred to Ornithocheirus in the past, but recent papers have found them to be distinct; Cimoliornis may be closer to azhdarchoidea, Cretornis is a valid genus of azhdarchid, and Palaeornis was shown to be a lonchodectid in 2009. O. buenzeli (Bunzel 1871, often misspelled and incorrectly attributed as O. bunzeli , Seeley 1881), cited in
891-445: A limited mobility. These toes were clawed but the claws were smaller than the hand claws. The rare conditions that allowed for the fossilisation of pterosaur remains, sometimes also preserved soft tissues. Modern synchrotron or ultraviolet light photography has revealed many traces not visible to the naked eye. These are often imprecisely called "impressions" but mostly consist of petrifications , natural casts and transformations of
990-516: A membrane that stretched between the legs, possibly connecting to or incorporating the tail, called the uropatagium ; the extent of this membrane is not certain, as studies on Sordes seem to suggest that it simply connected the legs but did not involve the tail (rendering it a cruropatagium ). A common interpretation is that non-pterodactyloid pterosaurs had a broader uro/cruropatagium stretched between their long fifth toes, with pterodactyloids, lacking such toes, only having membranes running along
1089-402: A more developed "keeled" crest compared to Ornithocheirus . Another feature that made Ornithocheirus unique and unlike its relatives, was that its teeth of were mostly vertical, rather than set at an outward-pointing angle. It was believed in the past that Ornithocheirus was one of the largest pterosaurs to have existed, with a wingspan possibly measuring 40 feet (12.2 m) wide. However, this
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#17327730708371188-425: A new fossil of Tupandactylus cf. imperator was found to have melanosomes in forms that signal an earlier-than-anticipated development of patterns found in extant feathers. The new specimen suggested that pterosaur integumentary melanosomes exhibited a more complex organization than those previously known from other pterosaurs. This indicates the presence of a unique form of melanosomes within pterosaur integument at
1287-415: A new separate species called L. daviesii . The genus Amblydectes (meaning "blunt biter") also consisted of three species: A. platystomus , A. crassidens and A. eurygnathus . Hooley's classification however, was rarely applied later in the century, and therefore paleontologists weren't aware of it, and kept subsuming all the poorly preserved and confusing material under the name Ornithocheirus . In 1964,
1386-411: A rotation could be caused by an abduction of the thighbone, meaning that the legs would be spread. This would also turn the feet into a vertical position. They then could act as rudders to control yaw. Some specimens show membranes between the toes, allowing them to function as flight control surfaces. The uropatagium or cruropatagium would control pitch. When walking the toes could flex upwards to lift
1485-449: A supraneural plate that, however, would not contact the notarium. The tails of pterosaurs were always rather slender. This means that the caudofemoralis retractor muscle which in most basal Archosauria provides the main propulsive force for the hindlimb, was relatively unimportant. The tail vertebrae were amphicoelous, the vertebral bodies on both ends being concave. Early species had long tails, containing up to fifty caudal vertebrae,
1584-464: A thousand bristle-like teeth. Dsungaripteridae covered their teeth with jawbone tissue for a crushing function. If teeth were present, they were placed in separate tooth sockets. Replacement teeth were generated behind, not below, the older teeth. The public image of pterosaurs is defined by their elaborate head crests. This was influenced by the distinctive backward-pointing crest of the well-known Pteranodon . The main positions of such crests are
1683-416: A unique, complex circulatory system of looping blood vessels. The combination of actinofibrils and muscle layers may have allowed the animal to adjust the wing slackness and camber . As shown by cavities in the wing bones of larger species and soft tissue preserved in at least one specimen, some pterosaurs extended their system of respiratory air sacs into the wing membrane. The pterosaur wing membrane
1782-408: A weight of up to 250 kilograms (550 pounds) for the largest species. Compared to the other vertebrate flying groups, the birds and bats, pterosaur skulls were typically quite large. Most pterosaur skulls had elongated jaws. Their skull bones tend to be fused in adult individuals. Early pterosaurs often had heterodont teeth, varying in build, and some still had teeth in the palate. In later groups
1881-453: A wide range of adult sizes , from the very small anurognathids to the largest known flying creatures, including Quetzalcoatlus and Hatzegopteryx , which reached wingspans of at least nine metres. The combination of endothermy , a good oxygen supply and strong muscles made pterosaurs powerful and capable flyers. Pterosaurs are often referred to by popular media or the general public as "flying dinosaurs", but dinosaurs are defined as
1980-482: A wingspan no less than 25 centimetres (10 inches). The most sizeable forms represent the largest known animals ever to fly, with wingspans of up to 10–11 metres (33–36 feet). Standing, such giants could reach the height of a modern giraffe . Traditionally, it was assumed that pterosaurs were extremely light relative to their size. Later, it was understood that this would imply unrealistically low densities of their soft tissues. Some modern estimates therefore extrapolate
2079-402: Is a highly exaggerated number, as the animal's wingspan likely measured 15 to 20 feet (4.5 to 6.1 m) wide, which would make it a medium-sized pterosaur. A related species called Tropeognathus had a wingspan measuring about 27 feet (8.2 m) wide, making it the largest toothed pterosaur known. In 2022, Gregory S. Paul estimated that Ornithocheirus had a wingspan of 5 m (16 ft) and
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#17327730708372178-555: Is common in warm-blooded animals who need insulation to prevent excessive heat-loss. Pycnofibers were flexible, short filaments, about five to seven millimetres long and rather simple in structure with a hollow central canal. Pterosaur pelts might have been comparable in density to many Mesozoic mammals. Pterosaur filaments could share a common origin with feathers, as speculated in 2002 by Czerkas and Ji. In 2009, Kellner concluded that pycnofibers were structured similarly to theropod proto-feathers . Others were unconvinced, considering
2277-422: Is curved to behind, resulting in a rounded wing tip, which reduces induced drag . The wingfinger is also bent somewhat downwards. When standing, pterosaurs probably rested on their metacarpals, with the outer wing folded to behind. In this position, the "anterior" sides of the metacarpals were rotated to the rear. This would point the smaller fingers obliquely to behind. According to Bennett, this would imply that
2376-421: Is divided into three basic units. The first, called the propatagium ("fore membrane"), was the forward-most part of the wing and attached between the wrist and shoulder, creating the "leading edge" during flight. The brachiopatagium ("arm membrane") was the primary component of the wing, stretching from the highly elongated fourth finger of the hand to the hindlimbs. Finally, at least some pterosaur groups had
2475-418: Is short but powerfully built. It sports a large deltopectoral crest, to which the major flight muscles are attached. Despite the considerable forces exerted on it, the humerus is hollow or pneumatised inside, reinforced by bone struts. The long bones of the lower arm, the ulna and radius , are much longer than the humerus. They were probably incapable of pronation . A bone unique to pterosaurs, known as
2574-673: The Cambridge Greensand of England , dating to the beginning of the Albian stage of the early Cretaceous period, about 110 million years ago. Additional fossils from the Santana Formation of Brazil are sometimes classified as species of Ornithocheirus , but have also been placed in their own genera, most notably Tropeognathus . During the 19th century, in England many fragmentary pterosaur fossils were found in
2673-467: The Cambridge Greensand , a layer from the early Cretaceous, that had originated as a sandy seabed. Decomposing pterosaur cadavers, floating on the sea surface, had gradually lost individual bones that sank to the bottom of the sea. Water currents then moved the bones around, eroding and polishing them, until they were at last covered by more sand and fossilised. Even the largest of these remains were damaged and difficult to interpret. They had been assigned to
2772-800: The Ornithocheirus material and the validity of the several names based on it, for it might be possible that it could by more detailed studies be established that the Brazilian pterosaurs were actually junior synonyms of the European types. Several European researchers concluded that this was indeed the case. Unwin revived Coloborhynchus and Michael Fastnacht Criorhynchus , each author ascribing Brazilian species to these genera. However, in 2000 Unwin stated that Criorhynchus could not be valid. Referring to Seeley's designation of 1881 he considered Ornithocheirus simus , holotype CAMSM B.54428, to be
2871-831: The order Pterosauria . They existed during most of the Mesozoic : from the Late Triassic to the end of the Cretaceous (228 to 66 million years ago). Pterosaurs are the earliest vertebrates known to have evolved powered flight . Their wings were formed by a membrane of skin, muscle, and other tissues stretching from the ankles to a dramatically lengthened fourth finger. There were two major types of pterosaurs. Basal pterosaurs (also called 'non-pterodactyloid pterosaurs' or ' rhamphorhynchoids ') were smaller animals with fully toothed jaws and, typically, long tails. Their wide wing membranes probably included and connected
2970-477: The patagium , and the presence of both aktinofibrils and filaments on Jeholopterus ningchengensis and Sordes pilosus . The various forms of filament structure present on the anurognathids in the 2018 study would also require a form of decomposition that would cause the different 'filament' forms seen. They therefore conclude that the most parsimonious interpretation of the structures is that they are filamentous protofeathers. But Liliana D'Alba points out that
3069-427: The thorax . It was probably covered by thick muscle layers. The upper bone, the shoulder blade , was a straight bar. It was connected to a lower bone, the coracoid that is relatively long in pterosaurs. In advanced species, their combined whole, the scapulocoracoid, was almost vertically oriented. The shoulder blade in that case fitted into a recess in the side of the notarium, while the coracoid likewise connected to
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3168-552: The type species , Ornithocheirus simus . Species have been referred to Ornithocheirus from the mid- Cretaceous period of North America , Europe and South America , but O. simus is known mostly from the United Kingdom , though a specimen referred to O. cf. simus is also known from Morocco . Because O. simus was originally named based on poorly preserved fossil material, the genus Ornithocheirus has suffered enduring problems of zoological nomenclature . Fossil remains of Ornithocheirus have been recovered mainly from
3267-417: The "bat model" depicted pterosaurs as warm-blooded and furred, it would turn out to be more correct in certain aspects than Cuvier's "reptile model" in the long run. In 1834, Johann Jakob Kaup coined the term Pterosauria. Ornithocheirus buenzeli " Ornithocheirus " buenzeli (often mis-spelled O. bunzeli ) is a pterosaur species known from parts of a humerus (upper arm bone) and part of
3366-428: The 1990s, pterosaur finds and histological and ultraviolet examination of pterosaur specimens have provided incontrovertible proof: pterosaurs had pycnofiber coats. Sordes pilosus (which translates as "hairy demon") and Jeholopterus ninchengensis show pycnofibers on the head and body. The presence of pycnofibers strongly indicates that pterosaurs were endothermic (warm-blooded). They aided thermoregulation, as
3465-428: The ankle, sometimes reducing total length to a third. Typically, it was fused to the shinbone. The ankle was a simple, "mesotarsal", hinge. The, rather long and slender, metatarsus was always splayed to some degree. The foot was plantigrade, meaning that during the walking cycle the sole of the metatarsus was pressed onto the soil. There was a clear difference between early pterosaurs and advanced species regarding
3564-484: The ankles. The exact curvature of the trailing edge, however, is still equivocal. While historically thought of as simple leathery structures composed of skin, research has since shown that the wing membranes of pterosaurs were highly complex dynamic structures suited to an active style of flight. The outer wings (from the tip to the elbow) were strengthened by closely spaced fibers called actinofibrils . The actinofibrils themselves consisted of three distinct layers in
3663-427: The anterior surface of the distal syncarpal. The medial carpal bears a deep concave fovea that opens anteriorly, ventrally and somewhat medially, within which the pteroid articulates, according to Wilkinson. In derived pterodactyloids like pteranodontians and azhdarchoids , metacarpals I-III are small and do not connect to the carpus, instead hanging in contact with the fourth metacarpal. With these derived species,
3762-421: The best fossils consisted of jaw fragments. In 1874, he created two new genera: Coloborhynchus and Criorhynchus . Coloborhynchus (meaning "maimed beak") which comprised a new type species called Coloborhynchus clavirostris , as well as two other species reassigned from Ornithocheirus : C. sedgwickii and C. cuvieri . Criorhynchus (meaning "ram beak") consisted entirely of former Ornithocheirus species:
3861-413: The breastbone. This way, both sides together made for a rigid closed loop, able to withstand considerable forces. A peculiarity was that the breastbone connections of the coracoids often were asymmetrical, with one coracoid attached in front of the other. In advanced species the shoulder joint had moved from the shoulder blade to the coracoid. The joint was saddle-shaped and allowed considerable movement to
3960-447: The broad ischium into an ischiopubic blade. Sometimes, the blades of both sides were also fused, closing the pelvis from below and forming the pelvic canal. The hip joint was not perforated and allowed considerable mobility to the leg. It was directed obliquely upwards, preventing a perfectly vertical position of the leg. The front of the pubic bones articulated with a unique structure, the paired prepubic bones. Together these formed
4059-474: The clade Anurognathidae ( Anurognathus , Jeholopterus , Vesperopterylus ) is debated. Anurognathids were highly specialized. Small flyers with shortened jaws and a wide gape, some had large eyes suggesting nocturnal or crepuscular habits, mouth bristles, and feet adapted for clinging. Parallel adaptations are seen in birds and bats that prey on insects in flight. Pterosaurs had a wide range of sizes, though they were generally large. The smallest species had
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4158-876: The clade Ornithocheirae, reclassifying all other snout-crested pterosaurs in the family Anhangueridae . Their cladogram is shown on the right. Topology 1: Andres & Myers (2013). Liaoningopterus gui Anhanguera araripensis Anhanguera blittersdorffi Anhanguera piscator Anhanguera santanae Tropeognathus mesembrinus Ornithocheirus simus Coloborhynchus clavirostris Coloborhynchus wadleighi Topology 2: Pêgas et al. (2019). Ornithocheirus simus Targaryendraconidae Cimoliopteridae Hamipterus tianshanensis Iberodactylus andreui Tropeognathus mesembrinus Coloborhynchinae Anhanguerinae [REDACTED] [REDACTED] [REDACTED] Pterosaur Ornithosauria Seeley , 1870 Pterosaurs are an extinct clade of flying reptiles in
4257-445: The clades Ornithocheiroidea ( Istiodactylus , Ornithocheirus , Pteranodon ), Ctenochasmatoidea ( Ctenochasma , Pterodactylus ), Dsungaripteroidea ( Germanodactylus , Dsungaripterus ), and Azhdarchoidea ( Tapejara , Tupuxuara , Quetzalcoatlus ). The two groups overlapped in time, but the earliest pterosaurs in the fossil record are basal pterosaurs, and the latest pterosaurs are pterodactyloids. The position of
4356-502: The descendants of the last common ancestor of the Saurischia and Ornithischia , which excludes the pterosaurs. Pterosaurs are nonetheless more closely related to birds and other dinosaurs than to crocodiles or any other living reptile, though they are not bird ancestors. Pterosaurs are also colloquially referred to as pterodactyls , particularly in fiction and journalism. However, technically, pterodactyl may refer to members of
4455-431: The description of the preserved integumentary structures on the two anurognathid specimens is still based upon gross morphology. She also points out that Pterorhynchus was described to have feathers to support the claim that feathers had a common origin with Ornithodirans but was argued against by several authors. The only method to assure if it was homologous to feathers is to use a scanning electron microscope. In 2022,
4554-544: The difference with the "quills" found on many of the bird-like maniraptoran specimens too fundamental. A 2018 study of the remains of two small Jurassic -age pterosaurs from Inner Mongolia , China , found that pterosaurs had a wide array of pycnofiber shapes and structures, as opposed to the homogeneous structures that had generally been assumed to cover them. Some of these had frayed ends, very similar in structure to four different feather types known from birds or other dinosaurs but almost never known from pterosaurs prior to
4653-846: The direct ancestors of birds, and assumed the hand of the genus to represent a transitional stage in the evolution towards the bird hand. To distinguish the best pieces in the collection, and partly because they had already been described as species by other scientists. Between the years 1869 and 1870, Seeley each gave them a separate species name: O. simus , O. woodwardi , O. oxyrhinus , O. carteri , O. platyrhinus , O. sedgwickii , O. crassidens , O. capito , O. eurygnathus , O. reedi , O. cuvieri , O. scaphorhynchus , O. brachyrhinus , O. colorhinus , O. dentatus , O. denticulatus , O. enchorhynchus , O. xyphorhynchus , O. fittoni , O. nasutus , O. polyodon , O. tenuirostris , O. machaerorhynchus , O. platystomus , O. microdon , O. oweni and O. huxleyi , thus 27 in total. As yet Seeley did not designate
4752-410: The down feathers found on both avian and some non-avian dinosaurs , suggesting that early feathers evolved in the common ancestor of pterosaurs and dinosaurs, possibly as insulation. They were warm-blooded (endothermic), active animals. The respiratory system had efficient unidirectional "flow-through" breathing using air sacs , which hollowed out their bones to an extreme extent. Pterosaurs spanned
4851-404: The extent of their wing membranes and it is possible that, like these groups, different species of pterosaur had different wing designs. Indeed, analysis of pterosaur limb proportions shows that there was considerable variation, possibly reflecting a variety of wing-plans. The bony elements of the arm formed a mechanism to support and extend the wing. Near the body, the humerus or upper arm bone
4950-676: The feather-specific melanosome signaling found in extant birds are possibly homologous with those found in pterosaurs. Pterosaur fossils are very rare, due to their light bone construction. Complete skeletons can generally only be found in geological layers with exceptional preservation conditions, the so-called Lagerstätten . The pieces from one such Lagerstätte , the Late Jurassic Solnhofen Limestone in Bavaria , became much sought after by rich collectors. In 1784, Italian naturalist Cosimo Alessandro Collini
5049-432: The fifth toes as hooks. Another hypothesis held that they stretched the brachiopatagia, but in articulated fossils the fifth digits are always flexed towards the tail. Later it became popular to assume that these toes extended an uropatagium or cruropatagium between them. As the fifth toes were on the outside of the feet, such a configuration would only have been possible if these rotated their fronts outwards in flight. Such
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#17327730708375148-450: The forces caused by flapping the wings. The notarium included three to seven vertebrae, depending on the species involved but also on individual age. These vertebrae could be connected by tendons or a fusion of their neural spines into a "supraneural plate". Their ribs also would be tightly fused into the notarium. In general, the ribs are double headed. The sacrum consisted of three to ten sacral vertebrae. They too, could be connected via
5247-400: The forelimb digits besides the wingfinger have been lost altogether. The wingfinger accounts for about half or more of the total wing length. It normally consists of four phalanges. Their relative lengths tend to vary among species, which has often been used to distinguish related forms. The fourth phalanx is usually the shortest. It lacks a claw and has been lost completely by nyctosaurids. It
5346-417: The form of the fifth digit. Originally, the fifth metatarsal was robust and not very shortened. It was connected to the ankle in a higher position than the other metatarsals. It bore a long, and often curved, mobile clawless fifth toe consisting of two phalanges. The function of this element has been enigmatic. It used to be thought that the animals slept upside-down like bats, hanging from branches and using
5445-415: The fourth metacarpal has been enormously elongated, typically equalling or exceeding the length of the long bones of the lower arm. The fifth metacarpal had been lost. In all species, the first to third fingers are much smaller than the fourth, the "wingfinger", and contain two, three and four phalanges respectively. The smaller fingers are clawed, with the ungual size varying among species. In nyctosaurids
5544-473: The front of the snout, as an outgrowth of the premaxillae, or the rear of the skull as an extension of the parietal bones in which case it is called a "supraoccipital crest". Front and rear crests can be present simultaneously and might be fused into a single larger structure, the most expansive of which is shown by the Tapejaridae . Nyctosaurus sported a bizarre antler-like crest. The crests were only
5643-429: The genus Pterodactylus , and more broadly to members of the suborder Pterodactyloidea of the pterosaurs. Pterosaurs had a variety of lifestyles. Traditionally seen as fish-eaters, the group is now understood to have also included hunters of land animals, insectivores, fruit eaters and even predators of other pterosaurs. They reproduced by eggs , some fossils of which have been discovered. The anatomy of pterosaurs
5742-652: The genus Pterodactylus , as was common for any pterosaur species described in the early and middle 19th century. Young researcher Harry Govier Seeley was commissioned to bring order to the pterosaur collection of the Sedgwick Museum in Cambridge . He soon concluded that it was best to create a new genus for the Cambridge Greensand material that he named Ornithocheirus (meaning "bird hand"), as he in this period still considered pterosaurs to be
5841-683: The ground, they walked well on all four limbs with an upright posture, standing plantigrade on the hind feet and folding the wing finger upward to walk on the three-fingered "hand". They could take off from the ground, and fossil trackways show that at least some species were able to run, wade, and/or swim. Their jaws had horny beaks, and some groups lacked teeth. Some groups developed elaborate head crests with sexual dimorphism . Pterosaurs sported coats of hair-like filaments known as pycnofibers , which covered their bodies and parts of their wings. Pycnofibers grew in several forms, from simple filaments to branching down feathers . These may be homologous to
5940-464: The head and torso. The term "pycnofiber", meaning "dense filament", was coined by palaeontologist Alexander Kellner and colleagues in 2009. Pycnofibers were unique structures similar to, but not homologous (sharing a common origin) with, mammalian hair, an example of convergent evolution . A fuzzy integument was first reported from a specimen of Scaphognathus crassirostris in 1831 by Georg August Goldfuss , but had been widely doubted. Since
6039-412: The head making only a small angle with the shaft. This implies that the legs were not held vertically below the body but were somewhat sprawling. The shinbone was often fused with the upper ankle bones into a tibiotarsus that was longer than the thighbone. It could attain a vertical position when walking. The calf bone tended to be slender, especially at its lower end that in advanced forms did not reach
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#17327730708376138-478: The hind legs. On the ground, they would have had an awkward sprawling posture, but the anatomy of their joints and strong claws would have made them effective climbers, and some may have even lived in trees. Basal pterosaurs were insectivores or predators of small vertebrates. Later pterosaurs ( pterodactyloids ) evolved many sizes, shapes, and lifestyles. Pterodactyloids had narrower wings with free hind limbs, highly reduced tails, and long necks with large heads. On
6237-401: The jaw joint was in a more forward position. The front lower jaw bones, the dentaries or ossa dentalia , were at the tip tightly fused into a central symphysis. This made the lower jaws function as a single connected whole, the mandible . The symphysis was often very thin transversely and long, accounting for a considerable part of the jaw length, up to 60%. If a crest was present on the snout,
6336-480: The legs. There has been considerable argument among paleontologists about whether the main wing membranes (brachiopatagia) attached to the hindlimbs, and if so, where. Fossils of the rhamphorhynchoid Sordes , the anurognathid Jeholopterus , and a pterodactyloid from the Santana Formation seem to demonstrate that the wing membrane did attach to the hindlimbs, at least in some species. However, modern bats and flying squirrels show considerable variation in
6435-402: The membrane from the ground. In Pterodactyloidea, the fifth metatarsal was much reduced and the fifth toe, if present, little more than a stub. This suggests that their membranes were split, increasing flight maneuverability. The first to fourth toes were long. They had two, three, four and five phalanges respectively. Often the third toe was longest; sometimes the fourth. Flat joints indicate
6534-421: The middle ones stiffened by elongated articulation processes, the zygapophyses , and chevrons . Such tails acted as rudders, sometimes ending at the rear in a vertical diamond-shaped or oval vane. In pterodactyloids, the tails were much reduced and never stiffened, with some species counting as few as ten vertebrae. The shoulder girdle was a strong structure that transferred the forces of flapping flight to
6633-575: The neck is typically longer than the torso. This length is not caused by an increase of the number of vertebrae, which is invariably seven. Some researchers include two transitional "cervicodorsals" which brings the number to nine. Instead, the vertebrae themselves became more elongated, up to eight times longer than wide. Nevertheless, the cervicals were wider than high, implying a better vertical than horizontal neck mobility. Pterodactyloids have lost all neck ribs. Pterosaur necks were probably rather thick and well-muscled, especially vertically. The torso
6732-524: The new combination of O. simus . From the seventies onwards many new pterosaur fossils were found in Brazil in deposits slightly older than the Cambridge Greensand, 110 million years old. Unlike the English material, these new finds included some of the best preserved large pterosaur skeletons and several new genera names were given to them, such as Anhanguera . This situation caused a renewed interest in
6831-458: The original material. They may include horn crests, beaks or claw sheaths as well as the various flight membranes. Exceptionally, muscles were preserved. Skin patches show small round non-overlapping scales on the soles of the feet, the ankles and the ends of the metatarsals . They covered pads cushioning the impact of walking. Scales are unknown from other parts of the body. Most or all pterosaurs had hair -like filaments known as pycnofibers on
6930-456: The past as evidence of Late Cretaceous ornithocheirids, has since been re-identified as a likely azhdarchid as well. The type species, Ornithocheirus simus , is only known from fragmentary jaw tips. It bore a distinctive convex "keeled" crest on its snout similar to its relatives. Ornithocheirus had relatively narrow jaw tips compared to the related Coloborhynchus and Tropeognathus , which had prominently-expanded rosettes of teeth, as well as
7029-405: The pteroid bone, which may itself be a modified distal carpal. The proximal carpals are fused together into a "syncarpal" in mature specimens, while three of the distal carpals fuse to form a distal syncarpal. The remaining distal carpal, referred to here as the medial carpal, but which has also been termed the distal lateral, or pre-axial carpal, articulates on a vertically elongate biconvex facet on
7128-402: The pteroid in articulation with the proximal syncarpal, suggesting that the pteroid articulated with the 'saddle' of the radiale (proximal syncarpal) and that both the pteroid and preaxial carpal were migrated centralia. The pterosaur wrist consists of two inner (proximal, at the side of the long bones of the arm) and four outer (distal, at the side of the hand) carpals (wrist bones), excluding
7227-441: The pteroid pointed forward, extending the forward membrane and allowing it to function as an adjustable flap . This view was contradicted in a 2007 paper by Chris Bennett, who showed that the pteroid did not articulate as previously thought and could not have pointed forward, but rather was directed inward toward the body as traditionally interpreted. Specimens of Changchengopterus pani and Darwinopterus linglongtaensis show
7326-488: The pteroid, connected to the wrist and helped to support the forward membrane (the propatagium) between the wrist and shoulder. Evidence of webbing between the three free fingers of the pterosaur forelimb suggests that this forward membrane may have been more extensive than the simple pteroid-to-shoulder connection traditionally depicted in life restorations. The position of the pteroid bone itself has been controversial. Some scientists, notably Matthew Wilkinson, have argued that
7425-586: The skull, the sutures between elements disappeared. In some later pterosaurs, the backbone over the shoulders fused into a structure known as a notarium , which served to stiffen the torso during flight, and provide a stable support for the shoulder blade . Likewise, the sacral vertebrae could form a single synsacrum while the pelvic bones fused also. Basal pterosaurs include the clades Dimorphodontidae ( Dimorphodon ), Campylognathididae ( Eudimorphodon , Campyognathoides ), and Rhamphorhynchidae ( Rhamphorhynchus , Scaphognathus ). Pterodactyloids include
7524-423: The species O. umbrosus and O. harpyia into Ornithocheirus , which were formerly species given to the genus Pteranodon by Edward Drinker Cope back in 1872. In 1914 Reginald Walter Hooley made a new attempt to structure the large number of species. Hooley synonymized Owen's Criorhynchus to Ornithocheirus , in which he also sunk Coloborhynchus into that genus, meaning that the only generic name he kept
7623-400: The study, suggesting homology. A response to this study was published in 2020, where it was suggested that the structures seen on the anurognathids were actually a result of the decomposition of aktinofibrils: a type of fibre used to strengthen and stiffen the wing. However, in a response to this, the authors of the 2018 paper point to the fact that the presence of the structures extend past
7722-405: The symphysis could feature a matching mandible crest, jutting out to below. Toothed species also bore teeth in their dentaries. The mandible opened and closed in a simple vertical or "orthal" up-and-down movement. The vertebral column of pterosaurs numbered between thirty-four and seventy vertebrae . The vertebrae in front of the tail were "procoelous": the cotyle (front of the vertebral body )
7821-405: The teeth mostly became conical. Front teeth were often longer, forming a "prey grab" in transversely expanded jaw tips, but size and position were very variable among species. With the derived Pterodactyloidea , the skulls became even more elongated, sometimes surpassing the combined neck and torso in length. This was caused by a stretching and fusion of the front snout bone, the premaxilla , with
7920-480: The term to the genus Pterodactylus or members of the Pterodactyloidea . In 1812 and 1817, Samuel Thomas von Soemmerring redescribed the original specimen and an additional one. He saw them as affiliated to birds and bats. Although he was mistaken in this, his "bat model" would be influential during the 19th century. In 1843, Edward Newman thought pterosaurs were flying marsupials . Ironically, as
8019-453: The time, distinct from previously known contemporary integumentary structures and more similar to those reported from mammalian hair and avian feathers. The feather fossils obtained from this specimen also suggest the presence of Stage IIIa feathers, a new discovery that indicates more complex feather structures were present in pterosaurs. The study describing this specimen further clarifies the timeline of avian feather evolution and suggests that
8118-422: The true extent of these crests has only been uncovered using ultraviolet photography. While fossil crests used to be restricted to the more advanced Pterodactyloidea, Pterorhynchus and Austriadactylus show that even some early pterosaurs possessed them. Like the upper jaws, the paired lower jaws of pterosaurs were very elongated. In advanced forms, they tended to be shorter than the upper cranium because
8217-699: The type species, Criorhynchus simus , and furthermore such as C. eurygnathus , C. capito , C. platystomus , C. crassidens and C. reedi . Seeley did not accept Owen's position. In 1881 he designated O. simus the type species of Ornithocheirus and named a new separate species called O. bunzeli . In 1888, Edwin Tulley Newton reassigned several existing species names into Ornithocheirus , which created new combinations: O. clavirostris , O. daviesii , O. sagittirostris , O. validus , O. giganteus , O. clifti , O. diomedeus , O. nobilis , O. curtus , O. macrorhinus and O. hlavaci . He also reassigned
8316-424: The type species. This also made it possible to revive Lonchodectes , using as type the former O. compressirostris , which then became L. compressirostris . As a result, though over forty species have been named in the genus Ornithocheirus over the years, only O. simus is currently considered valid by all pterosaur researchers. The species Tropeognathus mesembrinus , which was named by Peter Wellnhofer in 1987,
8415-416: The upper jawbone, the maxilla . Unlike most archosaurs , the nasal and antorbital openings of pterodactyloid pterosaurs merged into a single large opening, called the nasoantorbital fenestra . This feature likely evolved to lighten the skull for flight. In contrast, the bones behind the eye socket contracted and rotated, strongly inclining the rear skull and bringing the jaw joint forward. The braincase
8514-416: The wing, forming a crisscross pattern when superimposed on one another. The function of the actinofibrils is unknown, as is the exact material from which they were made. Depending on their exact composition (keratin, muscle, elastic structures, etc.), they may have been stiffening or strengthening agents in the outer part of the wing. The wing membranes also contained a thin layer of muscle, fibrous tissue, and
8613-402: The wing. It faced sideways and somewhat upwards. The breastbone, formed by fused paired sterna , was wide. It had only a shallow keel. Via sternal ribs, it was at its sides attached to the dorsal ribs. At its rear, a row of belly ribs or gastralia was present, covering the entire belly. To the front, a long point, the cristospina , jutted obliquely upwards. The rear edge of the breastbone
8712-475: The wingfinger, able to describe the largest arc of any wing element, up to 175°, was not folded by flexion but by an extreme extension. The wing was automatically folded when the elbow was bowed. A laser-simulated fluorescence scan on Pterodactylus also identified a membranous "fairing" (area conjunctioning the wing with the body at the neck), as opposed to the feathered or fur-composed "fairing" seen in birds and bats respectively. The pelvis of pterosaurs
8811-438: Was Ornithocheirus . To allow for a greater differentiation, Hooley created two new genera, again based on jaw form: Lonchodectes and Amblydectes . The genus Lonchodectes (meaning "lance biter") consisted of the former species Pterodactylus compressirostris , and Pterodactylus giganteus , which were reassigned as Lonchodectes compressirostris , the type species, and Lonchodectes giganteus , in addition, Hooley also named
8910-411: Was assigned to Ornithocheirus by David Unwin in 2003, making Tropeognathus a junior synonym. In 1989 however, Alexander Kellner considered it as an Anhanguera mesembrinus , then as a Coloborhynchus mesembrinus by André Veldmeijer in 1998 and as a Criorhynchus mesembrinus by Michael Fastnacht in 2001. Even earlier, in 2001, Unwin had referred the "Tropeognathus" material to O. simus in which
9009-401: Was concave and into it fitted a convex extension at the rear of the preceding vertebra, the condyle . Advanced pterosaurs are unique in possessing special processes projecting adjacent to their condyle and cotyle, the exapophyses , and the cotyle also may possess a small prong on its midline called a hypapophysis. The necks of pterosaurs were relatively long and straight. In pterodactyloids,
9108-454: Was followed by Veldmeijer; however, Veldmeijer rejected O. simus as the type species in favor of O. compressirostris (alternately Lonchodectes ), and he used the names Criorhynchus simus and Criorhynchus mesembrinus instead. In 2013, Rodrigues and Kellner found Ornithocheirus to be monotypic, containing only O. simus , and placed most other species in other genera, or declared them nomina dubia . They also considered O. platyrhinus
9207-451: Was highly modified from their reptilian ancestors by the adaptation to flight. Pterosaur bones were hollow and air-filled, like those of birds . This provided a higher muscle attachment surface for a given skeletal weight. The bone walls were often paper-thin. They had a large and keeled breastbone for flight muscles and an enlarged brain able to coordinate complex flying behaviour. Pterosaur skeletons often show considerable fusion. In
9306-407: Was of moderate size compared to the body as a whole. Often the three pelvic bones were fused. The ilium was long and low, its front and rear blades projecting horizontally beyond the edges of the lower pelvic bones. Despite this length, the rod-like form of these processes indicates that the hindlimb muscles attached to them were limited in strength. The, in side view narrow, pubic bone fused with
9405-643: Was relatively large for reptiles. In some cases, fossilized keratinous beak tissue has been preserved, though in toothed forms, the beak is small and restricted to the jaw tips and does not involve the teeth. Some advanced beaked forms were toothless, such as the Pteranodontidae and Azhdarchidae , and had larger, more extensive, and more bird-like beaks. Some groups had specialised tooth forms. The Istiodactylidae had recurved teeth for eating meat. Ctenochasmatidae used combs of numerous needle-like teeth for filter feeding; Pterodaustro could have over
9504-403: Was relatively short and egg-shaped. The vertebrae in the back of pterosaurs originally might have numbered eighteen. With advanced species a growing number of these tended to be incorporated into the sacrum . Such species also often show a fusion of the front dorsal vertebrae into a rigid whole which is called the notarium after a comparable structure in birds. This was an adaptation to withstand
9603-482: Was that if such creatures were still alive, only the sea was a credible habitat; Collini suggested it might be a swimming animal that used its long front limbs as paddles. A few scientists continued to support the aquatic interpretation even until 1830, when German zoologist Johann Georg Wagler suggested that Pterodactylus used its wings as flippers and was affiliated with Ichthyosauria and Plesiosauria . In 1800, Johann Hermann first suggested that it represented
9702-456: Was the deepest point of the thorax. Clavicles or interclavicles were completely absent. Pterosaur wings were formed by bones and membranes of skin and other tissues. The primary membranes attached to the extremely long fourth finger of each arm and extended along the sides of the body. Where they ended has been very controversial but since the 1990s a dozen specimens with preserved soft tissue have been found that seem to show they attached to
9801-400: Was the first scientist to describe a pterosaur fossil. At that time the concepts of evolution and extinction were imperfectly developed. The bizarre build of the pterosaur was shocking, as it could not clearly be assigned to any existing animal group. The discovery of pterosaurs would thus play an important role in the progress of modern paleontology and geology. Scientific opinion at the time
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