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Pterosaur
Temporal range: Late TriassicLate Cretaceous, 228–66 Ma
Six pterosaurs (clockwise from top left): Pteranodon, Dimorphodon, Pterodactylus, Tupandactylus, Anurognathus, and Rhamphorhynchus
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauria
Clade: Avemetatarsalia
Clade: Ornithodira
Clade: Pterosauromorpha
Order: Pterosauria
Kaup, 1834
Subgroups[1][2]
Distribution of pterosaur fossil locations. Colored species or genera names correspond to their taxonomic group.[a]
Synonyms

Ornithosauria Seeley, 1870

Pterosaurs[b][c] are an extinct clade of flying reptiles in the order Pterosauria. They existed during most of the Mesozoic: from the Late Triassic to the end of the Cretaceous (228 million to 66 million years ago).[8] 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.[9]

Traditionally, pterosaurs were divided into two major types. Basal pterosaurs (also called non-pterodactyloid pterosaurs or 'rhamphorhynchoids') were smaller animals, up to two meter wingspan, with fully toothed jaws and, typically, long tails. Their wide wing membranes probably included and connected the hindlimbs. On the ground, they would have had an awkward sprawling posture due to short metacarpals, but the anatomy of their joints and strong claws would have made them effective climbers, and some may have lived in trees. Basal pterosaurs were insectivores, piscivores or predators of small land vertebrates. Later pterosaurs (pterodactyloids) evolved many sizes, shapes, and lifestyles. Pterodactyloids had narrower wings with free hindlimbs, highly reduced tails, and long necks with large heads. On the ground, they walked well on all four limbs due to long metacarpals with an upright posture, standing plantigrade on the hind feet and folding the wing finger upward to walk on the metacarpals with the three smaller fingers of the hand pointing to the rear. They could take off from the ground, and fossil trackways show that at least some species were able to run, wade, and/or swim.[10] Their jaws had horny beaks, and some groups lacked teeth. Some groups developed elaborate head crests with sexual dimorphism. Since 2010 it is understood that many species, the basal Monofenestrata, were intermediate in build, combining an advanced long skull with long tails.

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 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.[11] 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 a wide range of adult sizes, from the very small anurognathids to the largest known flying creatures, including Quetzalcoatlus and Hatzegopteryx,[12][13][14] 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 the descendants of the last common ancestor of the Saurischia and Ornithischia, which excludes the pterosaurs.[15] 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.[16] However, technically, pterodactyl may refer to members of the genus Pterodactylus, and more broadly to members of the suborder Pterodactyloidea of the pterosaurs.[17]

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.[18]

Anatomy

[edit]
Life reconstruction of Pterodactylus

The anatomy of pterosaurs 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.[19] Pterosaur skeletons often show considerable fusion. In 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.

Size

[edit]
Wide variation in Late Cretaceous pterosaur size, compared to birds and a human

Pterosaurs were highly diverse in size, and some were the largest flying organisms in earth's history.[20][21] Early pterosaurs of the Triassic and Jurassic periods were typically small animals with wingspans only up to 2 metres (6.6 ft), while most Cretaceous pterosaurs were larger.[20][22][23] Some isolated specimens indicate exceptions to this rule, and the divisions of size across time may be a partial result of an incomplete fossil record.[24][25][26] Anurognathids may have been the smallest pterosaurs, with wingspans of as small as 0.4 metres (1.3 ft), though the age of these individuals remains uncertain.[27][28] The largest pterosaurs were members of Azhdarchidae such as Hatzegopteryx and Quetzalcoatlus, which could attain estimated wingspans of 10–11 metres (33–36 ft) and weights of 150–250 kilograms (330–550 lb).[29][30]

Skull

[edit]
Skull of an early pterosaur, Seazzadactylus

Pterosaurs have large skulls compared to other flying vertebrates, the birds and bats. Later pterosaurs had very elongated skulls, sometimes longer than the whole torso. Many bones were fused in adults.[31] The skulls were pierced by multiple large holes: the bony nostrils, eye sockets, the antorbital fenestrae in the snout side and two temporal fenestrae on each rear side. Monofenestratan pterosaurs fused the nasal and antorbital fenestra into a single large nasantorbital fenestra.[32][31] The back of the head was at first vertical in orientation, but rotated to nearly horizontal later in evolution of some groups.[33] The paired lower jaws were fused at the front into an elongated mandibular symphysis. The lower jaws of the earliest pterosaurs were pierced at the rear by a mandibular fenestra, but this was lost in later species.[34]

Skull of Thalassodromeus (front on left), showing extensive crest, nasantorbital fenestra, and toothless beak

The snout or the back of the skull often sported an upward projecting crest, sometimes of enormous size. The lower jaws could likewise feature a downward projecting keel. These crests could be expanded in size and shape with soft tissues.[35] Some crests entirely lacked a bone core, with their presence only known from exceptionally well preserved specimens.[36][37][38]

Early pterosaurs were heterodont, with multiple tooth types. Later pterosaurs were homodont, having a single tooth form, often elongated and conical, throughout the skull. The teeth were replaced continuously throughout life. Between species, the dentition varied considerably. Fish eaters often had longer teeth in an expansion of the jaw tips. Filter feeders could have a sieve of up to a thousand teeth. Some later pterosaur groups were entirely toothless, featuring a horny beak similar to that of birds.[34][32] Most species had some keratinized beak tissue, though never in the same snout section as the teeth.[37]

Neck and torso

[edit]
Skull and torso of Anhanguera, showing long neck and compact torso

The vertebral column of pterosaurs had up to seventy vertebrae. Later pterosaurs have unique structures at the sides of the vertebrae, called exapophyses,[39] and the concave fronts may possess a midline prong, the hypapophysis.[40] Pterosaur necks were typically long, deep, and straight, and in pterodactyloids was longer than the torso.[41][42][43] The number of neck vertebrae is always seven, or nine if one includes two trunk vertebrae.[41] Pterodactyloids have lost all neck ribs.[40] The neck was deep and well-muscled.[42][43]

Pterosaur torso showing the fused front of the torso (notarium), shoulder girdle connected to it and the large breastbone, and the fused pelvic region

The torso was short and compact. Up to seven front back vertebrae and ribs can be fused into a rigid structure known as a notarium.[41][44]

The shoulder girdle was strong and well-muscled, with the upper shoulder blade and connected lower coracoid fused in later species into a single scapulocoracoid. The top of this structure fitted to the notarium, while the lower end connected to the breastbone, forming a rigid closed loop, better to withstand the forces of flapping flight.[45][46] The shoulder joint was saddle-shaped allowing considerable movement to the wing.[46] It faced obliquely sideways and upwards.[47]

The breastbone was wide with a shallow keel, via sternal ribs attached to the dorsal ribs.[48] Behind it, belly ribs (gastralia) covered the entire belly.[47] To the front, a long pointy structure termed the cristospina jutted obliquely upwards. The thorax was deepest at the rear of the breastbone.[49] There were no (inter)clavicles.[47]

The pelvis of pterosaurs was of moderate size compared to the body as a whole. Often the three pelvic bones were fused.[50] The sacrum had up to ten sacral vertebrae, sometimes connected by a bar in a similar fashion to the notarium.[44] 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.[43] Then, in side view narrow, pubic bone fused with 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.[51] It was directed obliquely upwards, preventing a perfectly vertical position of the leg.[50] The front of the pubic bones articulated with a unique structure, the paired prepubic bones. Together these formed 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.[51]

Wings

[edit]

Wing membranes

[edit]
Various configurations proposed for the wings of pterosaurs

The primary wing membranes attached to the extremely long fourth fingers, probably extending to the ankles. The profile of the trailing edge is uncertain.[52] The membranes were not leathery flaps composed of skin but highly complex dynamic structures suited to serve an active flight style.[53] They were strengthened by closely spaced fibers called actinofibrils,[54] in three distinct layers in the wing, in a crisscross pattern superimposed on one another. They had a stiffening or strengthening function.[55] Also a thin layer of muscle, fibrous tissue, and a unique, complex circulatory system of looping blood vessels was present.[36] This combination may have allowed the animal to adjust the wing slackness and camber to control lift.[53]

Two pterosaurs (Scaphognathus and Balaenognathus) in dorsal view, with wing parts labeled

(bp: brachiopatagium, cp: cruropatagium, pp: propatagium)

The wing membrane is divided into three parts.[56] 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") stretched from the fourth finger to the hindlimb. Finally, a membrane that stretched between the legs, possibly incorporated the tail, called the uropatagium.[56] It might only have connected the legs, rendering it a cruropatagium. Early pterosaurs perhaps had a broader uro/cruropatagium stretching between their long fifth toes; pterodactyloids, lacking such toes, only had membranes running along the legs.[57] Fossils of the rhamphorhynchoid Sordes,[58] the anurognathid Jeholopterus,[59] suggest that the wing membrane did attach to the hindlimbs.[60] However, pterosaur limb proportions show that there was considerable variation in wing-plans.[61]

Wing bones

[edit]
Skeletal reconstruction of Maaradactylus, showing outstretched wings

The arm bones supported and extended the wing. The humerus or upper arm bone is short but powerful.[62] It has a large deltopectoral crest, to which the major flight muscles are attached.[62] The humerus is hollow or pneumatised inside, reinforced by bone struts.[49] The long bones of the lower arm, the ulna and radius, are much longer than the humerus.[63] A bone unique to pterosaurs, the pteroid, supported the propatagium between the wrist and shoulder.[64] The pterosaur wrist consists of two inner and four outer carpals. Two inner and three outer carpals are fused together into "syncarpals". The remaining outer carpal bears a deep concave fovea within which the pteroid articulates, according to Wilkinson.[65]

In derived pterodactyloids metacarpals I-III are small and do not connect to the carpus, instead hanging in contact with the fourth metacarpal.[51] In that case the fourth metacarpal has been enormously elongated, typically equalling or exceeding the length of the long bones of the lower arm.[50] The fifth metacarpal had been lost.[62] The first to third fingers are much smaller than the fourth, the "wingfinger", and contain two, three and four phalanges respectively.[51] The smaller fingers are clawed. The wingfinger accounts for about half or more of the total wing length.[51] It normally consists of four phalanges. Their relative lengths vary among species, allowing to distinguish related forms.[51] The fourth phalanx is usually the shortest. It lacks a claw and has been lost completely by nyctosaurids. It is curved to behind, resulting in a rounded wing tip, which reduces induced drag. The wingfinger is also bent somewhat downwards.[50] Standing, pterosaurs rested on their metacarpals, with the outer wing folded to behind. The "anterior" sides of the metacarpals were then rotated to the rear. This would point the smaller fingers obliquely to behind. According to Bennett, this would imply that 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.[43][66]

Hindlimbs

[edit]
Diagram of hindlimb and uropatagium anatomy of early pterosaur Sordes (A), and in context of entire skeleton in related genus Rhamphorhynchus (B)

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.[67] The thighbone was rather straight, with the head making only a small angle with the shaft.[51] This implies that the legs were not held vertically below the body but were somewhat sprawling.[67] The shinbone was often fused with the upper ankle bones into a tibiotarsus that was longer than the thighbone.[67] It could attain a vertical position when walking.[67] The calf bone tended to be slender, especially at its lower end that in advanced forms did not reach the ankle, sometimes reducing total length to a third. Typically, it was fused to the shinbone.[51] The ankle was a simple, "mesotarsal", hinge.[67] The, rather long and slender,[68] metatarsus was always splayed to some degree.[69] The foot was plantigrade, meaning that during the walking cycle the sole of the metatarsus was pressed onto the soil.[68]

The first to fourth toes were long. They had two, three, four and five phalanges respectively.[67] Often the third toe was longest; sometimes the fourth. Flat joints indicate a limited mobility. These toes were clawed but the claws were smaller than the hand claws.[69] There was a clear difference between early pterosaurs and advanced species regarding 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.[68] It bore a long, and often curved, mobile clawless fifth toe consisting of two phalanges.[69] It's thought that these toes support the uropatagium (or cruropatagium). 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 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.[68] In more advanced pterosaurs, the fifth metatarsal was much reduced and the fifth toe, if present, little more than a stub.[70]

Tail

[edit]

The tail, a continuation of the vertebral column, was slender, incapable of powering the hindlimb.[43] Early species had long tails of up to fifty vertebrae, stiffened by elongated zygapophyses and chevrons.[48] They acted as rudders, ending at the rear in a vertical vane.[47] In pterodactyloids, the tails were short and flexible,[47] with as few as ten vertebrae.[44]

Pycnofibers

[edit]
Diagram showing complex branched filaments in Tupandactylus, with a reconstruction at right showing thick pelt of pycnofibres

All pterosaurs had hair-like filaments known as pycnofibers on the head and torso.[71] Pycnofibres were unique structures similar to mammalian hair, an example of convergent evolution,[58] and pterosaur pelts might have been comparable in density those of mammals[71] Skin patches show small round non-overlapping scales on the soles of the hands and feet, but these were absent from the rest of the body.[72][73][74] The pycnofibers show that pterosaurs were warm-blooded, providing insulation to prevent heat-loss.[71]

Remains of two small Jurassic-age pterosaurs from Inner Mongolia, China, demonstrated that some pterosaurs had a wide array of pycnofiber shapes and structures, as opposed to the homogeneous structures that had previously documented. Some of these had frayed ends, very similar in structure to certain feather types known from birds or other dinosaurs.[75] A well preserved fossil of Tupandactylus was found to have pigment cells with similar forms to those seen in modern birds, more complex in organization than those previously known from other pterosaurs. This specimen also suggest the presence of Stage IIIa feathers, further indication of more complex filament structures in pterosaurs. Supporting a model of common ancestry with the filaments of birds, the authors termed these structures as pterosaur feathers rather than pycnofibres.[76] This common origin had been suggested before, but remains controversial.[38][55][71]

History of discovery

[edit]

First finds

[edit]
Engraving of the original Pterodactylus antiquus specimen by Egid Verhelst II, 1784

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,[77] became much sought after by rich collectors.[78] In 1784, Italian naturalist Cosimo Alessandro Collini was the first scientist to describe a pterosaur fossil.[79] 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.[80] The discovery of pterosaurs would thus play an important role in the progress of modern paleontology and geology.[81] Scientific opinion at the time 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.[82] 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.[83]

Newman's marsupial pterosaurs

In 1800, Johann Hermann first suggested that it represented a flying creature in a letter to Georges Cuvier. Cuvier agreed in 1801, understanding it was an extinct flying reptile.[84] In 1809, he coined the name Ptéro-Dactyle, "wing-finger".[85] This was in 1815 Latinised to Pterodactylus.[86] At first most species were assigned to this genus and ultimately "pterodactyl" was popularly and incorrectly applied to all members of Pterosauria.[16] Today, paleontologists limit the term to the genus Pterodactylus or members of the Pterodactyloidea.[17]

In 1812 and 1817, Samuel Thomas von Soemmerring redescribed the original specimen and an additional one.[87] 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.[88] In 1843, Edward Newman thought pterosaurs were flying marsupials.[89] Ironically, as 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.[90]

Expanding research

[edit]
Historical reconstruction of Dimorphodon as a biped by Seeley

In 1828, Mary Anning found in England the first pterosaur genus outside Germany,[91] named as Dimorphodon by Richard Owen, also the first non-pterodactyloid pterosaur known.[92] Later in the century, the Early Cretaceous Cambridge Greensand produced thousands of pterosaur fossils, that however, were of poor quality, consisting mostly of strongly eroded fragments.[93] Nevertheless, based on these, numerous genera and species would be named.[81] Many were described by Harry Govier Seeley, at the time the main English expert on the subject, who also wrote the first pterosaur book, Ornithosauria,[94] and in 1901 the first popular book,[81] Dragons of the Air. Seeley thought that pterosaurs were warm-blooded and dynamic creatures, closely related to birds.[95] Earlier, the evolutionist St. George Jackson Mivart had suggested pterosaurs were the direct ancestors of birds.[96] Owen opposed the views of both men, seeing pterosaurs as cold-blooded "true" reptiles.[97]

In the US, Othniel Charles Marsh in 1870 discovered Pteranodon in the Niobrara Chalk, then the largest known pterosaur,[97] the first toothless one and the first from America.[98] These layers too rendered thousands of fossils,[98] also including relatively complete skeletons that were three-dimensionally preserved instead of being strongly compressed as with the Solnhofen specimens. This led to a much better understanding of many anatomical details,[98] such as the hollow nature of the bones.

Early reconstruction of Rhamphorhynchus

Meanwhile, finds from the Solnhofen had continued, accounting for the majority of complete high-quality specimens discovered.[99] They allowed to identify most new basal taxa, such as Rhamphorhynchus, Scaphognathus and Dorygnathus.[99] This material gave birth to a German school of pterosaur research, which saw flying reptiles as the warm-blooded, furry and active Mesozoic counterparts of modern bats and birds.[100] In 1882, Marsh and Karl Alfred Zittel published studies about the wing membranes of specimens of Rhamphorhynchus.[101][102] German studies continued well into the 1930s, describing new species such as Anurognathus. In 1927, Ferdinand Broili discovered hair follicles in pterosaur skin,[103] and paleoneurologist Tilly Edinger determined that the brains of pterosaurs more resembled those of birds than modern cold-blooded reptiles.[104]

In contrast, English and American paleontologists by the middle of the twentieth century largely lost interest in pterosaurs. They saw them as failed evolutionary experiments, cold-blooded and scaly, that hardly could fly, the larger species only able to glide, being forced to climb trees or throw themselves from cliffs to achieve a take-off. In 1914, for the first-time pterosaur aerodynamics were quantitatively analysed, by Ernest Hanbury Hankin and David Meredith Seares Watson, but they interpreted Pteranodon as a pure glider.[105] Little research was done on the group during the 1940s and 1950s.[81]

Pterosaur renaissance

[edit]
This drawing of Zhejiangopterus by John Conway exemplifies the "new look" of pterosaurs

The situation for dinosaurs was comparable. From the 1960s onwards, a dinosaur renaissance took place, a quick increase in the number of studies and critical ideas, influenced by the discovery of additional fossils of Deinonychus, whose spectacular traits refuted what had become entrenched orthodoxy. In 1970, likewise the description of the furry pterosaur Sordes began what Robert Bakker named a renaissance of pterosaurs.[106] Kevin Padian especially propagated the new views, publishing a series of studies depicting pterosaurs as warm-blooded, active and running animals.[107][108][109] This coincided with a revival of the German school through the work of Peter Wellnhofer, who in 1970s laid the foundations of modern pterosaur science.[77] In 1978, he published the first pterosaur textbook,[110] the Handbuch der Paläoherptologie, Teil 19: Pterosauria,[111] and in 1991 the second ever popular science pterosaur book,[110] the Encyclopedia of Pterosaurs.[112]

This development accelerated through the exploitation of two new Lagerstätten.[110] During the 1970s, the Early Cretaceous Santana Formation in Brazil began to produce chalk nodules that, though often limited in size and the completeness of the fossils they contained, perfectly preserved three-dimensional pterosaur skeletal parts.[110] German and Dutch institutes bought such nodules from fossil poachers and prepared them in Europe, allowing their scientists to describe many new species and revealing a whole new fauna. Soon, Brazilian researchers, among them Alexander Kellner, intercepted the trade and named even more species.

Specimen of Sinopterus, one of many excellent pterosaurs fossils from Liaoning, China

Even more productive was the Early Cretaceous Chinese Jehol Biota of Liaoning that since the 1990s has brought forth hundreds of exquisitely preserved two-dimensional fossils, often showing soft tissue remains. Chinese researchers such as Lü Junchang have again named many new taxa. As discoveries also increased in other parts of the world, a sudden surge in the total of named genera took place. By 2009, when they had increased to about ninety, this growth showed no sign of levelling-off.[113] In 2013, M.P. Witton indicated that the number of discovered pterosaur species had risen to 130.[114] Over ninety percent of known taxa has been named during the "renaissance". Many of these were from groups the existence of which had been unknown.[110] Advances in computing power enabled researchers to determine their complex relationships through the quantitative method of cladistics. New and old fossils yielded much more information when subjected to modern ultraviolet light or roentgen photography, or CAT-scans.[115] Insights from other fields of biology were applied to the data obtained.[115] All this resulted in a substantial progress in pterosaur research, rendering older accounts in popular science books completely outdated.

In 2017 a fossil from a 170-million-year-old pterosaur, later named as the species Dearc sgiathanach in 2022, was discovered on the Isle of Skye in Scotland. The National Museum of Scotland claims that it is the largest of its kind ever discovered from the Jurassic period, and it has been described as the world's best-preserved skeleton of a pterosaur.[116]

Evolution and extinction

[edit]

Origins

[edit]
Life restoration of Scleromochlus, an archosauromorph theorized to be related to pterosaurs.

Because pterosaur anatomy has been so heavily modified for flight, and immediate transitional fossil predecessors have not so far been described, the ancestry of pterosaurs is not fully understood.[117] The oldest known pterosaurs were already fully adapted to a flying lifestyle. Since Seeley, it was recognised that pterosaurs were likely to have had their origin in the "archosaurs", what today would be called the Archosauromorpha. In the 1980s, early cladistic analyses found that they were Avemetatarsalians (archosaurs closer to dinosaurs than to crocodilians). As this would make them also rather close relatives of the dinosaurs, these results were seen by Kevin Padian as confirming his interpretation of pterosaurs as bipedal warm-blooded animals. Because these early analyses were based on a limited number of taxa and characters, their results were inherently uncertain.[118]

Several influential researchers who rejected Padian's conclusions offered alternative hypotheses. David Unwin proposed an ancestry among the basal Archosauromorpha, specifically long-necked forms ("protorosaurs") such as tanystropheids. A placement among basal archosauriforms like Euparkeria was also suggested.[119] Basal archosauromorps such as these seemed to be good candidates for close pterosaur relatives due to their long-limbed anatomy; especially notable is Sharovipteryx, which possessed skin membranes on its hindlimbs likely used for gliding.[118] A 1999 study by Michael Benton reinforced that pterosaurs were avemetatarsalians closely related to Scleromochlus, and named the group Ornithodira to encompass pterosaurs and dinosaurs.[120] In 1996, research S. Christopher Bennett published an analysis finding pterosaurs to be protorosaurs or closely related to them after removing characteristics of the hindlimb from his analysis, to test the possibility of locomotion-based convergent evolution between pterosaurs and dinosaurs.[121] A 2007 reply by Dave Hone and Michael Benton could not reproduce this result, finding pterosaurs to be closely related to dinosaurs even without hindlimb characters. They concluded that, although more basal pterosauromorphs are needed to clarify their relationships, current evidence indicates that pterosaurs are avemetatarsalians, as either the sister group of Scleromochlus or a branch between the latter and Lagosuchus.[122]

Life restoration of Lagerpeton. Lagerpetids share many anatomical and neuroanatomical similarities with pterosaurs and may be close relatives

A 2011 archosaur-focused phylogenetic analysis by Sterling Nesbitt benefited from far more data and found strong support for pterosaurs being avemetatarsalians, though Scleromochlus was not included due to its poor preservation.[123] A 2016 archosauromorph-focused study by Martin Ezcurra included various proposed pterosaur relatives, yet also found pterosaurs to be closer to dinosaurs and unrelated to more basal taxa.[124] Working from his 1996 analysis, Bennett published a 2020 study on Scleromochlus which argued that both Scleromochlus and pterosaurs were non-archosaur archosauromorphs, albeit not particularly closely related to each other.[125] By contrast, a later 2020 study proposed that lagerpetid archosaurs were the sister clade to pterosauria.[126] This was based on newly described fossil skulls and forelimbs showing various anatomical similarities with pterosaurs and reconstructions of lagerpetid brains and sensory systems based on CT scans also showing neuroanatomical similarities with pterosaurs.[127][128] The results of the latter study were subsequently supported by an independent analysis of early pterosauromorph interrelationships.[129]

A related problem is the origin of pterosaur flight.[130] Like with birds, hypotheses can be ordered into two main varieties: "ground up" or "tree down". Climbing a tree would cause height and gravity to provide both the energy and a strong selection pressure for incipient flight, as a fall could kill a climbing animal. Rupert Wild in 1983 proposed a hypothetical "propterosaurus": a lizard-like arboreal animal developing a membrane between its limbs, first to safely parachute and then, gradually elongating the fourth finger, to glide.[131] However, subsequent cladistic results did not fit this model well. Neither protorosaurs nor ornithodirans are biologically equivalent to lizards. Furthermore, the transition between gliding and flapping flight is not well-understood. More recent studies on basal pterosaur hindlimb morphology seem to vindicate a connection to Scleromochlus. Like this archosaur, basal pterosaur lineages have plantigrade hindlimbs that show adaptations for saltation.[132]

At least one study found that the early Triassic ichnofossil Prorotodactylus is anatomically similar to that of early pterosaurs.[126]

Extinction

[edit]
Azhdarchid pterosaurs such as Arambourgiana thrived at the end of the Cretaceous

It was once assumed that competition with early bird species resulted in the extinction of many of the pterosaurs.[133] It was thought that by the end of the Cretaceous, only very large species of pterosaurs were present. The smaller species were presumed to have become extinct, their niche filled by birds.[134] However, pterosaur decline (if actually occurring) seems unrelated to bird diversity, as ecological overlap between the two groups appears to be minimal.[135] In fact, at least some avian niches were reclaimed by pterosaurs prior to the Cretaceous–Paleogene extinction event.[136] It seems that this K-Pg extinction event at the end of the Cretaceous, which wiped out all non-avian dinosaurs and many other animals, was the direct cause of the extinction of the pterosaurs.

Small-sized pterosaur species apparently were present in the Csehbánya Formation, indicating a higher diversity of Late Cretaceous pterosaurs than previously accounted for.[137] The recent findings of a small cat-sized adult azhdarchid further indicate that small pterosaurs from the Late Cretaceous might actually have simply been rarely preserved in the fossil record, helped by the fact that there is a strong bias against terrestrial small sized vertebrates such as juvenile dinosaurs, and that their diversity might actually have been much larger than previously thought.[138]

A 2021 study showcases that niches previously occupied by small pterosaurs were increasingly occupied by the juvenile stages of larger species in the Late Cretaceous. Rather than being outcompeted by birds, pterosaurs essentially specialized a trend already occurring in previous eras of the Mesozoic.[139]

Classification and phylogeny

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Fossil of Eudimorphodon, one of the most primitive pterosaurs

In phylogenetic taxonomy, the clade Pterosauria has usually been defined as node-based and anchored to several extensively studied taxa as well as those thought to be primitive. One 2003 study defined Pterosauria as "The most recent common ancestor of the Anurognathidae, Preondactylus and Quetzalcoatlus and all their descendants."[140] However, these types of definition would inevitably leave any related species that are slightly more primitive out of the Pterosauria. To remedy this, a new definition was proposed that would anchor the name not to any particular species but to an anatomical feature, the presence of an enlarged fourth finger that supports a wing membrane.[141] This apomorphy-based definition was adopted by the PhyloCode in 2020 as "[T]he clade characterized by the apomorphy fourth manual digit hypertrophied to support a wing membrane, as inherited by Pterodactylus (originally Ornithocephalus) antiquus (Sömmerring 1812)".[142] A broader clade, Pterosauromorpha, has been defined as all ornithodirans more closely related to pterosaurs than to dinosaurs.[143]

The internal classification of pterosaurs has historically been difficult, because there were many gaps in the fossil record. Starting from the 21st century, new discoveries are now filling in these gaps and giving a better picture of the evolution of pterosaurs. Traditionally, they were organized into two suborders: the Rhamphorhynchoidea, a "primitive" group of long-tailed pterosaurs, and the Pterodactyloidea, "advanced" pterosaurs with short tails.[119] However, this traditional division has been largely abandoned. Rhamphorhynchoidea is a paraphyletic (unnatural) group, since the pterodactyloids evolved directly from them and not from a common ancestor, so, with the increasing use of cladistics, it has fallen out of favor among most scientists.[114][144]

Within pterosaurs, several smaller clades have been named. The clade Novialoidea was named by paleontologist Alexander Wilhelm Armin Kellner in 2003 as a node-based taxon consisting of the last common ancestor of Campylognathoides, Quetzalcoatlus and all its descendants. This name was derived from Latin novus "new", and ala, "wing", in reference to the wing synapomorphies that the members of the clade possess.[145]

Paleontologist David Unwin in 2003 had named the group Lonchognatha in the same issue of the journal that published Novialoidea (Geological Society of London, Special Publications 217) and defined it as Eudimorphodon ranzii, Rhamphorhynchus muensteri, their most recent common ancestor and all its descendants (as a node-based taxon).[146] Under Unwin's and Kellner's phylogenetic analyses (where Eudimorphodon and Campylognathoides form a group that is basal to both Rhamphorhynchus and Quetzalcoatlus), Novialoidea is materially identical to Lonchognatha. However, other analyses find Lonchognatha to be a separate concept (Andres et al., 2010),[147] or synonymous with the Pterosauria (Andres, 2010).[148]

The precise relationships between pterosaurs is still unsettled. Many studies of pterosaur relationships in the past have included limited data and were highly contradictory. However, newer studies using larger data sets are beginning to make things clearer. The cladogram (family tree) below follows a phylogenetic analysis presented by Longrich, Martill and Andres in 2018, with clade names after Andres et al. (2014).[1][136]

Pterosauria

The position of the clade Anurognathidae (Anurognathus, Jeholopterus, Vesperopterylus) is debated.[149] 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.

Paleobiology

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Flight

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Diagrams showing breathing motion (top two) and internal air sac system (bottom two)

The mechanics of pterosaur flight are not completely understood or modeled at this time.[150][151][needs update]

Katsufumi Sato, a Japanese scientist, did calculations using modern birds and concluded that it was impossible for a pterosaur to stay aloft.[150] In the book Posture, Locomotion, and Paleoecology of Pterosaurs it is theorized that they were able to fly due to the oxygen-rich, dense atmosphere of the Late Cretaceous period.[152] However, both Sato and the authors of Posture, Locomotion, and Paleoecology of Pterosaurs based their research on the now-outdated theories of pterosaurs being seabird-like, and the size limit does not apply to terrestrial pterosaurs, such as azhdarchids and tapejarids. Furthermore, Darren Naish concluded that atmospheric differences between the present and the Mesozoic were not needed for the giant size of pterosaurs.[153]

Skeletal reconstruction of a quadrupedally launching Pteranodon longiceps

Another issue that has been difficult to understand is how they took off. Earlier suggestions were that pterosaurs were largely cold-blooded gliding animals, deriving warmth from the environment like modern lizards, rather than burning calories. In this case, it was unclear how the larger ones of enormous size, with an inefficient cold-blooded metabolism, could manage a bird-like takeoff strategy, using only the hind limbs to generate thrust for getting airborne. Later research shows them instead as being warm-blooded and having powerful flight muscles, and using the flight muscles for walking as quadrupeds.[154] Mark Witton of the University of Portsmouth and Mike Habib of Johns Hopkins University suggested that pterosaurs used a vaulting mechanism to obtain flight.[155] The tremendous power of their winged forelimbs would enable them to take off with ease.[154] Once aloft, pterosaurs could reach speeds of up to 120 km/h (75 mph) and travel thousands of kilometres.[155]

In 1985, the Smithsonian Institution commissioned aeronautical engineer Paul MacCready to build a half-scale working model of Quetzalcoatlus northropi. The replica was launched with a ground-based winch. It flew several times in 1986 and was filmed as part of the Smithsonian's IMAX film On the Wing.[156][157]

Large-headed species are thought to have forwardly swept their wings in order to better balance.[158]

Air sacs and respiration

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A 2009 study showed that pterosaurs 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. The presence of a subcutaneous air sac system in at least some pterodactyloids would have further reduced the density of the living animal.[159] Like modern crocodilians, pterosaurs appeared to have had a hepatic piston, seeing as their shoulder-pectoral girdles were too inflexible to move the sternum as in birds, and they possessed strong gastralia.[160] Thus, their respiratory system had characteristics comparable to both modern archosaur clades.

Nervous system

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Brain endocast of Allkaruen

An X-ray study of pterosaur brain cavities revealed that the animals (Rhamphorhynchus muensteri and Anhanguera santanae) had massive flocculi. The flocculus is a brain region that integrates signals from joints, muscles, skin and balance organs.[19] The pterosaurs' flocculi occupied 7.5% of the animals' total brain mass, more than in any other vertebrate. Birds have unusually large flocculi compared with other animals, but these only occupy between 1 and 2% of total brain mass.[19]

The flocculus sends out neural signals that produce small, automatic movements in the eye muscles. These keep the image on an animal's retina steady. Pterosaurs may have had such a large flocculus because of their large wing size, which would mean that there was a great deal more sensory information to process.[19] The low relative mass of the flocculi in birds is also a result of birds having a much larger brain overall; though this has been considered an indication that pterosaurs lived in a structurally simpler environment or had less complex behaviour compared to birds,[161] recent studies of crocodilians and other reptiles show that it is common for sauropsids to achieve high intelligence levels with small brains.[162] Studies on the endocast of Allkaruen show that brain evolution in pterodactyloids was a modular process.[163]

Terrestrial locomotion

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The fossil trackways show that pterosaurs like Hatzegopteryx were quadrupeds, and some rather efficient terrestrial predators.

Pterosaurs' hip sockets are oriented facing slightly upwards, and the head of the femur (thigh bone) is only moderately inward facing, suggesting that pterosaurs had an erect stance. It would have been possible to lift the thigh into a horizontal position during flight, as gliding lizards do.

There was considerable debate whether pterosaurs ambulated as quadrupeds or as bipeds. In the 1980s, paleontologist Kevin Padian suggested that smaller pterosaurs with longer hindlimbs, such as Dimorphodon, might have walked or even run bipedally, in addition to flying, like road runners.[109] However, a large number of pterosaur trackways were later found with a distinctive four-toed hind foot and three-toed front foot; these are the unmistakable prints of pterosaurs walking on all fours.[164][165]

The probable azhdarchid trace fossil Haenamichnus uhangriensis.

Fossil footprints show that pterosaurs stood with the entire foot in contact with the ground (plantigrade), in a manner similar to many mammals like humans and bears. Footprints from azhdarchids and several unidentified species show that pterosaurs walked with an erect posture with their four limbs held almost vertically beneath the body, an energy-efficient stance used by most modern birds and mammals, rather than the sprawled limbs of modern reptiles.[166][154] Indeed, erect-limbs may be omnipresent in pterosaurs.[132]

Though traditionally depicted as ungainly and awkward when on the ground, the anatomy of some pterosaurs (particularly pterodactyloids) suggests that they were competent walkers and runners.[167] Early pterosaurs have long been considered particularly cumbersome locomotors due to the presence of large cruropatagia, but they too appear to have been generally efficient on the ground.[132]

Fossil pterosaur footprints, Pterosaur Beach (France).

The forelimb bones of azhdarchids and ornithocheirids were unusually long compared to other pterosaurs, and, in azhdarchids, the bones of the arm and hand (metacarpals) were particularly elongated. Furthermore, as a whole, azhdarchid front limbs were proportioned similarly to fast-running ungulate mammals. Their hind limbs, on the other hand, were not built for speed, but they were long compared with most pterosaurs, and allowed for a long stride length. While azhdarchid pterosaurs probably could not run, they would have been relatively fast and energy efficient.[166]

The relative size of the hands and feet in pterosaurs (by comparison with modern animals such as birds) may indicate the type of lifestyle pterosaurs led on the ground. Azhdarchid pterosaurs had relatively small feet compared to their body size and leg length, with foot length only about 25–30% the length of the lower leg. This suggests that azhdarchids were better adapted to walking on dry, relatively solid ground. Pteranodon had slightly larger feet (47% the length of the tibia), while filter-feeding pterosaurs like the ctenochasmatoids had very large feet (69% of tibial length in Pterodactylus, 84% in Pterodaustro), adapted to walking in soft muddy soil, similar to modern wading birds.[166] Though clearly forelimb-based launchers, basal pterosaurs have hindlimbs well adapted for hopping, suggesting a connection with archosaurs such as Scleromochlus.[132]

Swimming

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Tracks made by ctenochasmatoids indicate that these pterosaurs swam using their hindlimbs. In general, these have large hindfeet and long torsos, indicating that they were probably more adapted for swimming than other pterosaurs.[168] Pteranodontians conversely have several speciations in their humeri interpreted to have been suggestive of a water-based version of the typical quadrupedal launch, and several like boreopterids must have foraged while swimming, as they seem incapable of frigatebird-like aerial hawking.[168] These adaptations are also seen in terrestrial pterosaurs like azhdarchids, which presumably still needed to launch from water in case they found themselves in it. The nyctosaurid Alcione may display adaptations for wing-propelled diving like modern gannets and tropicbirds.[136]

Diet and feeding habits

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Modern interpretations of the diet of Dimorphodon have challenged traditional ideas of all pterosaurs being piscivorous

Traditionally, almost all pterosaurs were seen as surface-feeding piscivores or fish-eaters, a view that still dominates popular science. Today, many pterosaurs groups are thought to have been terrestrial carnivores, omnivores or insectivores.

Early-on it was recognised that the small Anurognathidae were nocturnal, aerial insectivores. With highly flexible joints on the wing finger, a broad, triangular wing shape, large eyes and short tail, these pterosaurs were likely analogous to nightjars or extant insectivorous bats, being capable of high manoeuvrability at relatively low speeds.[169]

Ctenochasmatoid pterosaurs such as Lusognathus may have had specialised niches in freshwater ecosystems

Interpretations of the habits of basal groups have changed profoundly. Dimorphodon, envisioned as a puffin analogue in the past, is indicated by its jaw structure, gait, and poor flight capabilities, as a terrestrial/semiarboreal predator of small mammals, squamates, and large insects.[170] Its robust dentition caused Campylognathoides to be seen as a generalist or a terrestrial predator of small vertebrates, but the highly robust humerus and high-aspect wing morphology, suggest it may have been capable of grabbing prey on the wing;[171] a later study indicates it was teuthophagous based on squid findings within its gut.[172] The small insectivorous Carniadactylus and the larger Eudimorphodon were highly aerial animals and fast, agile flyers with long robust wings. Eudimorphodon has been found with fish remains in its stomach, but its dentition suggests an opportunistic diet. Slender-winged Austriadactylus and Caviramus were likely terrestrial/semiarboreal generalists. Caviramus likely had a strong bite force, indicating an adaptation towards hard food items that might have been chewed in view of the tooth wear.[173]

Many pteranodontoid pterosaurs such as Haliskia likely fed on fish at sea

Some Rhamphorhynchidae, such as Rhamphorhynchus itself or Dorygnathus, were fish-eaters with long, slender wings, needle-like dentition and long, thin jaws. Sericipterus, Scaphognathus and Harpactognathus had more robust jaws and teeth (which were ziphodont, dagger-shaped, in Sericipterus), and shorter, broader wings. These were either terrestrial/aerial predators of vertebrates[174] or corvid-like generalists.[175] Wukongopteridae like Darwinopterus were first considered aerial predators. Lacking a robust jaw structure or powerful flying muscles, they are now seen as arboreal or semiterrestrial insectivores. Darwinopterus robustidens, in particular, seems to have been a beetle specialist.[176]

Among pterodactyloids, a greater variation in diet is present. Pteranodontia contained many piscivorous taxa, such as the Ornithocheirae, Boreopteridae, Pteranodontidae and Nyctosauridae. Niche partitioning caused ornithocheirans and the later nyctosaurids to be aerial dip-feeders like today's frigatebirds (with the exception of the plunge-diving adapted Alcione elainus), while boreopterids were freshwater diving animals similar to cormorants, and pteranodonts pelagic plunge-divers akin to boobies and gannets. An analysis of Lonchodraco found clusters of foramina at the tip of its beak; birds with similarly numerous foramina have sensitive beaks used to feel for food, so Lonchodraco may have used its beak to feel for fish or invertebrates in shallow water.[177] The istiodactylids were likely primarily scavengers.[178] Archaeopterodactyloidea obtained food in coastal or freshwater habitats. Germanodactylus and Pterodactylus were piscivores, while the Ctenochasmatidae were suspension feeders, using their numerous fine teeth to filter small organisms from shallow water. Pterodaustro was adapted for flamingo-like filter-feeding.[179]

Azhdarchoid pterosaurs such as Kariridraco fed on terrestrial prey

In contrast, Azhdarchoidea mostly were terrestrial pterosaurs. Tapejaridae were arboreal omnivores, likely supplementing seeds and fruits with small insects and vertebrates.[168][180] Gut contents consisting of phytoliths from various plants in a specimen of the tapejarid Sinopterus constitute the first evidence of herbivory in a pterosaur.[181] Dsungaripteridae were specialist molluscivores, using their powerful jaws to crush the shells of molluscs and crustaceans. Thalassodromidae were likely terrestrial carnivores. Thalassodromeus itself was named after a fishing method known as "skim-feeding", later understood to be biomechanically impossible. Perhaps it pursued relatively large prey, in view of its reinforced jaw joints and relatively high bite force.[182] Azhdarchidae are now understood to be terrestrial predators akin to ground hornbills or some storks, eating any prey item they could swallow whole.[183] Hatzegopteryx was a robustly built predator of relatively large prey, including medium-sized dinosaurs.[184][185] Alanqa may have been a specialist molluscivore.[186]

A 2021 study reconstructed the adductor musculature of skulls from pterodactyloids, estimating the bite force and potential dietary habits of nine selected species.[187] The study corroborated the view of pteranodontids, nyctosaurids and anhanuerids as piscivores based on them being relatively weak but fast biters, and suggest that Tropeognathus mesembrinus was specialised in consuming relatively large prey compared to Anhanguera. Dsungaripterus was corroborated as a durophage, with Thalassodromeus proposed to share this feeding habit based on high estimated bite force quotients (BFQ) and absolute bite force values.[187] Tapejara wellnhoferi was corroborated as a specialised consumer of hard plant material with a relatively high BFQ and high mechanical advantage, and Caupedactylus ybaka and Tupuxuara leonardii were proposed to be ground-feeding generalists with intermediate bite force values and less specialised jaws.[187]

Natural predators

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Theropod dinosaur Irritator shown feeding on a pterosaur

Pterosaurs are known to have been eaten by theropods. In the 1 July 2004 edition of Nature, paleontologist Éric Buffetaut discusses an Early Cretaceous fossil of three cervical vertebrae of a pterosaur with the broken tooth of a spinosaur, most likely Irritator, embedded in it. The vertebrae are known not to have been eaten and exposed to digestion, as the joints are still articulated.[188] Fossils of Pteranodon have been found with tooth marks from sharks such as Squalicorax,[189] and a fossil with tooth marks from the Toolebuc formation has been interpreted as being attacked or scavenged by an ichthyosaur (most likely Platypterygius).

Reproduction and life history

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Fossil pterodactyloid juvenile from the Solnhofen Limestone

While very little is known about pterosaur reproduction, it is believed that, similar to all dinosaurs, all pterosaurs reproduced by laying eggs, though such findings are very rare. The first known pterosaur eggs were found in the quarries of Liaoning, the same place that yielded feathered dinosaurs, and in Loma del Pterodaustro (Lagarcito Formation, Argentina). The eggs from Liaoning were squashed flat with no signs of cracking, so evidently the eggs had leathery shells, as in modern lizards.[190] The egg from the Lagarcito Formation was laid by a Pterodaustro,[191][192] a pterosaur known by abundant material.[193] This was supported by the description of an additional pterosaur egg belonging to the genus Darwinopterus, described in 2011, which also had a leathery shell and, also like modern reptiles but unlike birds, was fairly small compared to the size of the mother.[194] In 2014 five unflattened eggs from the species Hamipterus tianshanensis were found in an Early Cretaceous deposit in northwest China. Examination of the shells by scanning electron microscopy showed the presence of a thin calcareous eggshell layer with a membrane underneath.[195] A study of pterosaur eggshell structure and chemistry published in 2007 indicated that it is likely pterosaurs buried their eggs, like modern crocodiles and turtles. Egg-burying would have been beneficial to the early evolution of pterosaurs, as it allows for more weight-reducing adaptations, but this method of reproduction would also have put limits on the variety of environments pterosaurs could live in and may have disadvantaged them when they began to face ecological competition from birds.[196]

A Darwinopterus specimen showcases that at least some pterosaurs had a pair of functional ovaries, as opposed to the single functional ovary in birds, dismissing the reduction of functional ovaries as a requirement for powered flight.[197]

Growth series of Rhamphorhynchus specimens showing changes throughout life

Wing membranes preserved in pterosaur embryos are well developed, suggesting that pterosaurs were ready to fly soon after birth.[198] However, tomography scans of fossilised Hamipterus eggs suggests that the young pterosaurs had well-developed thigh bones for walking, but weak chests for flight.[199] It is unknown if this holds true for other pterosaurs. Fossils of pterosaurs only a few days to a week old (called "flaplings") have been found, representing several pterosaur families, including pterodactylids, rhamphorhinchids, ctenochasmatids and azhdarchids.[119] All preserved bones that show a relatively high degree of hardening (ossification) for their age, and wing proportions similar to adults. In fact, many pterosaur flaplings have been considered adults and placed in separate species in the past. Additionally, flaplings are normally found in the same sediments as adults and juveniles of the same species, such as the Pterodactylus and Rhamphorhynchus flaplings found in the Solnhofen limestone of Germany, and Pterodaustro flaplings from Argentina. All are found in deep aquatic environment far from shore.[200]

Some pterosaurs may have reproduced in colonies similar to those of modern seabirds

For the majority of pterosaur species, it is not known whether they practiced any form of parental care, but their ability to fly as soon as they emerged from the egg and the numerous flaplings found in environments far from nests and alongside adults has led most researchers, including Christopher Bennett and David Unwin, to conclude that the young were dependent on their parents for a relatively short period of time, during a period of rapid growth while the wings grew long enough to fly, and then left the nest to fend for themselves, possibly within days of hatching.[119][201] Alternatively, they may have used stored yolk products for nourishment during their first few days of life, as in modern reptiles, rather than depend on parents for food.[200] Fossilised Hamipterus nests were shown preserving many male and female pterosaurs together with their eggs in a manner to a similar to that of modern seabird colonies.[195][202] Due to how underdeveloped the chests of the hatchlings were for flying, it was suggested that Hamipterus may have practiced some form of parental care.[199] However, this study has since been criticised.[203] Most evidence currently leans towards pterosaur hatchlings being superprecocial, similar to that of megapode birds, which fly after hatching without the need of parental care. A further study compares evidence for superprecociality and "late term flight" and overwhelmingly suggests that most if not all pterosaurs were capable of flight soon after hatching.[204] A later study suggested that while smaller-bodied pterosaurs were most likely superprecocial or precocial, owing to the consistent or decreasing wing aspect ratio during growth, certain large-bodied pterosaurs, such as Pteranodon showed possible evidence of their young being altricial, due to the fast rate the limb bones closest to the body grew compared to any other element of their skeleton after hatching. Other factors mentioned were the limits of soft shelled eggs and the size of the pelvic opening of large female pterosaurs.[205][206]

Growth rates of pterosaurs once they hatched varied across different groups. In earlier, long-tailed pterosaurs ("rhamphorhynchoids"), such as Rhamphorhynchus, the average growth rate during the first year of life was 130% to 173%, slightly faster than the growth rate of alligators. Growth in these species slowed after sexual maturity, and it would have taken more than three years for Rhamphorhynchus to attain maximum size.[201] In contrast, the later pterodactyloid pterosaurs, such as Pteranodon, grew to adult size within the first year of life. Additionally, pterodactyloids had determinate growth, meaning that the animals reached a fixed maximum adult size and stopped growing.[200]

A 2021 study indicates that pterosaur juveniles of larger species increasingly took the roles previously occupied by adult small pterosaurs.[139]

Daily activity patterns

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Comparisons between the scleral rings of pterosaurs and modern birds and reptiles have been used to infer daily activity patterns of pterosaurs. The pterosaur genera Pterodactylus, Scaphognathus, and Tupuxuara have been inferred to be diurnal, Ctenochasma, Pterodaustro, and Rhamphorhynchus have been inferred to be nocturnal, and Tapejara has been inferred to be cathemeral, being active throughout the day for short intervals. As a result, the possibly fish-eating Ctenochasma and Rhamphorhynchus may have had similar activity patterns to modern nocturnal seabirds, and the filter-feeding Pterodaustro may have had similar activity patterns to modern anseriform birds that feed at night. The differences between activity patterns of the Solnhofen pterosaurs Ctenochasma, Rhamphorhynchus, Scaphognathus, and Pterodactylus may also indicate niche partitioning between these genera.[207]

Cultural significance

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Quetzalcoatlus models in South Bank, created by Mark Witton for the Royal Society's 350th anniversary

Pterosaurs have been a staple of popular culture for as long as their cousins the dinosaurs, though they are usually not featured as prominently in films, literature or other art. While the depiction of dinosaurs in popular media has changed radically in response to advances in paleontology, a mainly outdated picture of pterosaurs has persisted since the mid-20th century.[208]

Scene from When Dinosaurs Ruled the Earth depicting an outsized Rhamphorhynchus

The vague generic term "pterodactyl" is often used for these creatures. The animals depicted in fiction and pop culture frequently represent either Pteranodon or (non-pterodactyloid) Rhamphorhynchus, or a fictionalized hybrid of the two.[208] Many children's toys and cartoons feature "pterodactyls" with Pteranodon-like crests and long, Rhamphorhynchus-like tails and teeth, a combination that never existed in nature. However, at least one pterosaur did have both the Pteranodon-like crest and teeth: Ludodactylus, whose name means "toy finger" for its resemblance to old, inaccurate children's toys.[209] Pterosaurs have sometimes been incorrectly identified as (the ancestors of) birds, though birds are theropod dinosaurs and not descendants of pterosaurs.

Pterosaurs were used in fiction in Sir Arthur Conan Doyle's 1912 novel The Lost World and its 1925 film adaptation. They appeared in a number of films and television programs since, including the 1933 film King Kong, and 1966's One Million Years B.C. In the latter, animator Ray Harryhausen had to add inaccurate bat-like wing fingers to his stop motion models in order to keep the membranes from falling apart, though this particular error was common in art even before the film was made. Rodan, a fictional giant monster (or kaiju) which first appeared in the 1956 film Rodan, is portrayed as an enormous irradiated species of Pteranodon.[210][211] Rodan has appeared in multiple Japanese Godzilla films released during the 1960s, 1970s, 1990s, and 2000s, and also appeared in the 2019 American-produced film Godzilla: King of the Monsters.[211][212][213]

Versperopterylus is one of the only pterosaurs with grasping feet, despite popular depictions of them on many pterosaurs

The Fell Beasts of J.R.R. Tolkien's Lord of the Rings are often understood as "pterosaur-like", although Tolkien himself did deny they were actual pterosaurs.

After the 1960s, pterosaurs remained mostly absent from notable American film appearances until 2001's Jurassic Park III. Paleontologist Dave Hone noted that the pterosaurs in this film had not been significantly updated to reflect modern research. Errors persisting were teeth while toothless Pteranodon was intended to be depicted, nesting behavior that was known to be inaccurate by 2001, and leathery wings, rather than the taut membranes of muscle fiber required for pterosaur flight.[208] Petrie from The Land Before Time (1988), is a notable example from an animated film.[214]

In most media appearances, pterosaurs are depicted as piscivores, not reflecting their full dietary variation. They are also often shown as aerial predators similar to birds of prey, grasping human victims with talons on their feet. However, only the small anurognathid Vesperopterylus and small wukongopterid Kunpengopterus[215] are known to possess prehensile feet and hands respectively; all other known pterosaurs have flat, plantigrade feet with no opposable toes, and the feet are generally proportionally small, at least in the case of the Pteranodontia.[16]

See also

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Explanatory notes

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References

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Sources

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  • Berry, Mark F. (2005). The Dinosaur Filmography. McFarland & Company. ISBN 978-0-7864-2453-5.
  • Wellnhofer, Peter (1991). The Illustrated Encyclopedia of Pterosaurs: An Illustrated Natural History of the Flying Reptiles of the Mesozoic Era. Crescent Books. ISBN 978-0-517-03701-0.
  • Witton, Mark (2013). Pterosaurs: Natural History, Evolution, Anatomy. Princeton University Press. ISBN 978-0-691-15061-1.
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Pterosaurs are an extinct of flying reptiles that represent the first vertebrates known to have evolved powered, flapping flight. Their wings consisted of a thin of skin, muscle, and other tissues stretched between an elongated fourth finger and the body, supported by lightweight, . These archosaurian reptiles, closely related to but distinct from dinosaurs, dominated skies for over 150 million years, from the Period approximately 210 million years ago until their extinction at the end of the Period 66 million years ago. Pterosaurs exhibited remarkable diversity in size and form, with more than 200 described species ranging from small, sparrow-sized forms with wingspans of about 40 centimeters to gigantic species like Quetzalcoatlus, which boasted wingspans of up to 11–12 meters and stood as tall as a giraffe. Early pterosaurs, such as those from the Triassic, were generally smaller and more generalized, while later Jurassic and Cretaceous forms included specialized groups like the short-tailed Pterodactyloidea, which featured crests, elongated skulls, and adaptations for diverse diets including insects, fish, and possibly small vertebrates. Their skeletons show evidence of warm-blooded physiology, with air-filled bones reducing weight and large brain cavities suggesting advanced sensory capabilities for aerial navigation and hunting. Although often mistakenly called "flying dinosaurs," pterosaurs were not dinosaurs but fellow ornithodirans along with dinosaurs and birds, all sharing a common ancestor from the early ; crocodilians are more distantly related as fellow archosaurs. They coexisted with dinosaurs throughout much of the but occupied distinct ecological niches, primarily as aerial predators and rather than terrestrial herbivores or carnivores. Flight in pterosaurs likely evolved from ancestors, enabling them to exploit three-dimensional environments in ways no other reptiles had before, with some large species capable of soaring long distances like modern albatrosses. Pterosaurs vanished during the Cretaceous–Paleogene mass event, triggered by an asteroid impact and associated environmental catastrophes, which also eliminated non-avian dinosaurs. Their extinction highlights their vulnerability as large-bodied flyers in a rapidly changing world, though smaller, bird-like dinosaurs survived as the ancestors of modern birds. Fossil discoveries, from iconic sites like the in , continue to reveal details about their locomotion, —evidenced by rare finds of eggs and embryos—and global distribution across all continents.

Anatomy

Size and general morphology

Pterosaurs displayed remarkable variation in body size, ranging from diminutive early forms to some of the largest flying animals ever known. The smallest recognized pterosaur is Nemicolopterus crypticus, an azhdarchoid with an estimated wingspan of 0.25 m. In contrast, gigantic azhdarchids such as Quetzalcoatlus northropi and Hatzegopteryx thambema achieved wingspans exceeding 10 m, with estimates for Q. northropi around 10–11 m and for H. thambema up to 12 m. Body mass estimates for pterosaurs span from a few grams in hatchlings of the smallest to approximately kg in the largest adults, reflecting adaptations for flight across diverse ecological niches. These masses are derived from three-dimensional skeletal models scaled with reconstructions, accounting for pterosaur-specific traits like extensive pneumatization. Scaling relationships between mass (M) and (W) follow allometric equations of the form M = k W2.5, where k is a constant calibrated to pterosaur and proportions, yielding M ≈ 0.52 W2.55 for pterodactyloids and slightly steeper exponents for basal forms. Such relations highlight how increased size correlated with enhanced skeletal robusticity to support flight loads. The general of pterosaurs was optimized for aerial locomotion, featuring a quadrupedal stance on the ground with forelimbs modified into . The fourth metacarpal was disproportionately elongated, forming the primary support for the membrane (), while the first three fingers retained claws for terrestrial use. Hindlimbs were reduced in size relative to the forelimbs, typically comprising less than 20% of total limb length, and adapted for bipedal or quadrupedal walking rather than . The skeleton consisted of lightweight, with exceptionally thin walls—often pneumatized by invading the medullary cavities—reducing overall density to levels comparable to modern birds. Size variations underscored evolutionary trends, with small-bodied Jurassic pterosaurs like Pterodactylus antiquus ( 0.5–1 m, ~50–200 g) representing early diversity, while larger Cretaceous forms such as Anhanguera sanctanae ( 4–5 m, ~10–20 kg) exemplified the shift toward in later clades. This progression from compact builds in basal taxa to more elongated, lightweight frames in advanced pterodactyloids facilitated exploitation of varied habitats, from forests to open skies.

Skull and dentition

Pterosaur skulls displayed remarkable diversity in form, reflecting adaptations to varied ecological niches. Basal forms and "rhamphorhynchoids" typically featured broader with numerous small teeth, as exemplified by muensteri, which had a relatively short, wide suited for capturing small aquatic or aerial prey. In contrast, pterodactyloids evolved longer, narrower , prominently seen in longiceps, where the elongated, slender likely facilitated skimming or probing behaviors in marine environments. This shift in rostrum morphology contributed to increased cranial disparity over time, with pterodactyloids occupying a broader morphospace than their precursors. Cranial crests varied from modest bony projections to elaborate, soft-tissue augmented structures, such as the towering, fan-like crest of Tupandactylus imperator, which may have functioned primarily in visual display for intraspecific signaling or mate attraction. Biomechanical analyses and CT-based reconstructions of skulls, including those of Dimorphodon macronyx, indicate that some crests generated aerodynamic lift during flight or aided by increasing surface area for heat dissipation, though display remains the most widely supported role across taxa. Dentition in most pterosaurs consisted of conical, recurved teeth arranged in multiple rows along the jaws, optimized for grasping elusive prey like or without requiring strong crushing forces. Wear patterns on these teeth, observed in specimens such as Coloborhynchus robustus, reveal rapid replacement cycles, with resorption pits and successive tooth generations indicating turnover rates potentially every few months to maintain sharpness amid frequent use. However, derived pterodactyloids like azhdarchids (e.g., Azhdarcho lancicollis) and pteranodontids (e.g., ) were edentulous, featuring elongated, toothless beaks akin to modern shorebirds, which emerged prominently from the onward and dominated assemblages. Sensory adaptations were pronounced in pterosaur crania, with large orbits—often comprising a significant portion of skull length—indicating acute for detecting prey or obstacles during flight, as reconstructed from taxa like Anhanguera santanae. Nasal openings and associated cavities suggest olfaction contributed to foraging, though evidence from endocasts points to vision as the dominant sense. Braincase analyses via CT scans reveal relatively expanded cerebral regions compared to other reptiles, with encephalization quotients estimated at 0.2–0.5 relative to avian benchmarks, supporting coordinated sensory processing for aerial lifestyles; for instance, Rhamphorhynchus endocasts show enlarged olfactory bulbs and floccular lobes for integrating visual and vestibular inputs.

Axial skeleton

The axial skeleton of pterosaurs, comprising the vertebral column, , and associated elements, was adapted for lightweight construction and enhanced flexibility, particularly in the , while providing rigidity in the to support flight. The vertebral column typically consisted of seven , with the and axis often fused, enabling significant neck elongation and flexibility for feeding and aerial maneuvering; this count remained consistent across most taxa, though early forms like those in the Rhamphorhynchidae exhibited slightly more (up to eight or nine) through subtle variations in fusion. In contrast, the thoracic and sacral regions featured extensive fusion in adults: the notarium formed by the coalescence of two to eight dorsal vertebrae (sometimes including the last cervical), beginning with of neural spines and progressing to full integration of and transverse processes, which stiffened the mid-body for aerodynamic stability during flight. The , comprising fused sacral vertebrae (typically three to five) along with adjacent caudals and pelvic elements, further reinforced the , with fusion developing ontogenetically to accommodate increasing body size and flight demands. The and contributed to both respiratory efficiency and muscle support. Thoracic bore uncinate processes—elongated, overlapping projections that enhanced rib mobility and formed part of a skeletal for costal ventilation, facilitating the expansion and contraction of the in coordination with diverticula. The was typically broad and keeled ventrally, providing a robust attachment site for the large flight muscles, such as the pectoralis complex, while its thin, pneumatized structure minimized mass; in some basal taxa, sternal connected it to the vertebral column for added stability. , or ventral abdominal , were present in certain non-pterodactyloid forms, forming a flexible that supported the belly wall and aided in respiration by allowing ventral expansion, though they were reduced or absent in more derived pterodactyloids. Tail morphology varied markedly between major pterosaur clades, reflecting evolutionary adaptations to locomotion and balance. In rhamphorhynchoids (basal pterosaurs), the tail was long and stiffened by elongated chevrons and osteoderms, often comprising up to 50% of total body length and terminating in a vane-like structure that may have functioned as a for during flight or . Pterodactyloids, in contrast, evolved short, reduced tails with few caudal vertebrae (typically 20 or fewer), freeing up mass for larger heads and wings while relying less on tail-based control. This reduction correlated with shifts toward quadrupedal and more maneuverable . Pneumatization was a hallmark of the pterosaur , with extensive air-filled cavities invading the vertebrae, , and via diverticula from the pulmonary system, substantially reducing skeletal density. In cervical and dorsal vertebrae, pneumatic foramina—often multiple per side on the centrum and neural arch—allowed ingress of these diverticula, resulting in air space proportions of 68–72% in well-preserved specimens, particularly higher in neural arches (up to 77%) than . This pneumatization, more pronounced in mid-cervical than posterior regions and varying by (e.g., abundant in anhanguerids), lightened the without compromising strength, contributing to overall weight reduction estimated at significant levels for flight-capable forms, while also linking the axial elements to the respiratory apparatus.

Pectoral girdle and forelimbs

The pectoral girdle of pterosaurs is characterized by a robust fusion of the and bones, forming a synostosis that provides structural support for the flight apparatus. This fusion creates a large, saddle-shaped at the , which accommodates the humeral head and allows for a limited optimized for elevation and depression during flight. In many taxa, the features an acrocoracoid process that acts as a for the supracoracoideus muscle, facilitating the upstroke of the . The , a thin and often pneumatic plate of bone, integrates with the scapulocoracoid via an anterior cristospine, anchoring major flight muscles such as the pectoralis and enhancing chest rigidity. Clavicles are present but reduced in basal pterosaurs, occasionally forming a V-shaped structure similar to a in some specimens, though they are absent or unossified in derived pterodactyloids. The forelimbs are highly modified for flight, with the serving as a robust proximal element that can constitute up to 50% of the total length in some , featuring a prominent deltopectoral crest for muscle attachment and stress distribution during takeoff. Distally, the and are slender and subequal in length, approximately matching the humerus, while the carpus includes syncarpal elements and a unique pteroid bone—a slender, rod-like structure articulating at the and extending anteriorly toward the to brace the of the . The manus exhibits unequal digit lengths, with digits I-III short and clawed for terrestrial support, contrasting sharply with the hyper-elongated manual digit IV, whose metacarpal is 30-65% of humeral length and whose phalanges extend 8-10 times the metacarpal's length, resulting in a total manual IV-to-humerus ratio exceeding 5 in flying forms to span the efficiently. These proportions, adapted for tensile stress during launch, feature hollow yet reinforced s to minimize weight while maximizing strength. Wing membrane attachments to the involve specialized soft tissues, including layers of actinofibrils—parallel collagenous fibers 0.1-0.5 mm in diameter—that reinforce the propatagium (anterior membrane from shoulder to pteroid) and uropatagium (tailward extension). The primary brachiopatagium spans from the ankle to the elongated fourth finger, with actinofibrils oriented spanwise to resist narrowing under tension and distribute aerodynamic loads, as evidenced by exceptionally preserved fossils showing fiber impressions aligned perpendicular to the trailing edge. This fibrous network enhances membrane stiffness without adding significant mass, enabling controlled deformation during flight maneuvers.

Pelvic girdle and hindlimbs

The pelvic girdle of pterosaurs consisted of fused ilium, pubis, and bones forming a relatively elongated structure compared to the body, with the three elements typically co-ossifying in adults to create a rigid incorporating 3–10 sacral vertebrae depending on the . A prominent preacetabular process extended anteriorly from the ilium, varying in length across clades—short in dimorphodontids (about 40% of iliac length) but longer in rhamphorhynchids (50–60%) and ornithocheiroids (often exceeding 90% with dorsal deflection)—serving as a key attachment site for retractor muscles such as the caudofemoralis. The pubis and fused along their medial margins to form a broad, imperforate ischiopubic plate, which remained partially open ventrally in juveniles or certain lineages like ornithocheiroids, facilitating abdominal expansion during respiration. The was imperforate, with a small supraacetabular crest and laterally facing orientation that supported an erect posture conducive to bipedal stance, though posterior deflection of the pubis in advanced forms like ornithocheiroids optimized leverage for leg extensors. Hindlimb elements were robust yet proportionally reduced relative to the elongated forelimbs adapted for flight, emphasizing their secondary role in locomotion and takeoff. The femur was notably shorter than the humerus, with length ratios typically ranging from 0.6 to 0.8 across taxa such as rhamphorhynchoids and pterodactyloids, reflecting diminished propulsive demands compared to the wing-supporting humerus; for instance, in Pteranodon, the femur measured about 62% of humeral length. The tibia and fibula were elongated, often fused distally into a tibiotarsus-like structure, with tibia-to-femur ratios of 1.1–1.5 enabling strides suited to terrestrial support rather than speed. Pedal digits were generally reduced in number and size, with five toes present but the fifth vestigial and the others bearing sharp claws for grasping; the ankle joint incorporated astragalus and calcaneum fusions, sometimes associated with soft tissue extensions like interdigital membranes for stability. Bone robusticity indices, calculated as midshaft second moment of area, were lower in hindlimbs than forelimbs (e.g., femoral bending strength often 40–60% of humeral values), indicating adaptation for weight-bearing rather than high-impact forces. Foot morphology supported versatile terrestrial behaviors, with pes impressions in trackways revealing a semi-erect posture and claws adapted for substrate grasping or perching in arboreal contexts. Some taxa, particularly early pterodactyloids like ctenochasmatoids, exhibited enlarged feet (up to 69% of tibial length) with hooked unguals suggesting perching capabilities, though not strictly anisodactyl like modern birds; instead, the hallux was opposable in limited ranges for clinging. Fossil trackways, such as those from the Crayssac site in , consistently document a quadrupedal with manus prints positioned anterior to pes tracks, spaced up to three interpedal widths from the midline, confirming coordinated use of all limbs for walking and implying a narrow-based, semi-erect stance. In contrast to the dominant forelimb-driven flight apparatus, hindlimbs facilitated ground support and brief bipedal bursts. Biomechanical models of takeoff highlight the s' role in initiating launch, particularly in quadrupedal sequences where they provided initial before forelimbs dominated. In simulations of ornithocheiroids with 5 m wingspans, hindlimb extensors generated moment arms peaking at 0.14–0.16 m during the crouch-to-push phase, contributing an estimated 20–30% of total propulsive force in combined limb models, with robusticity supporting this without fracture risk. This integration allowed efficient energy transfer from ground to air, differing markedly from the primary aerodynamic functions of the pectoral girdle and forelimbs.

Soft tissues

Pterosaurs possessed a variety of structures preserved in exceptional fossil sites known as Lagerstätten, such as the and the , providing insights into their integument and physiology beyond the skeleton. One prominent feature was pycnofibers, filament-like integumentary structures covering the body, head, and sometimes wings. These ranged from simple, unbranched filaments about 1-2 mm long and 0.05-0.1 mm thick, observed in taxa like , to more complex, branched forms in anurognathids such as pilosus, where distal branching created a fuzzy, feather-like appearance. In well-preserved specimens from the , pycnofibers formed a dense covering, estimated at up to 100-200 filaments per square millimeter on the torso, suggesting a role in through insulation and possibly display for intraspecific signaling, analogous to functions in avian feathers. The flight membranes, or patagia, were critical soft structures composed of skin reinforced by parallel actinofibrils—thin, collagenous fibers about 0.1-0.5 mm in diameter arranged perpendicular to the . The main membrane, or chiropatagium, extended from the elongated fourth finger to the ankles, while the uropatagium spanned from the hindlimbs to the tail base, and the propatagium stretched from the neck or shoulder to the , forming a forward sail. These s had a thickness of approximately 0.1-0.5 mm in smaller pterosaurs, increasing slightly in larger forms, with actinofibrils providing structural support to maintain camber and resist tension during flight without restricting flexibility. Preservation in Solnhofen specimens reveals that the membranes were vascularized and likely keratinized on the surface, contributing to aerodynamic efficiency. Internal soft tissues are less commonly preserved but include impressions of muscle fibers and possible adipose structures. In Rhamphorhynchus muensteri from the , faint outlines of flight muscle fibers and potential pads along the indicate a robust supporting powered flight. Recent analyses of the pterosaur Dearc sgiathanach from the Isle of Skye reveal detailed wing bone articulations that imply soft tissue attachments, though direct membrane preservation is absent; such fossils highlight the challenges and rarities in soft tissue recovery. These impressions suggest pterosaurs had well-developed musculature and possibly energy-storage fats, aiding endurance in aerial lifestyles. Evidence for coloration comes from melanosome preservation in soft tissues, particularly in head crests. In the tapejarid Tupandactylus imperator, eumelanosomes and phaeomelanosomes indicate reddish-brown hues with potential iridescent effects from associated iridophores, while darker body regions suggest for . These pigments likely served signaling functions, such as recognition or display, with varied shapes (spherical to elongate) implying genetic control over color patterns similar to modern birds. Such findings underscore the complexity of pterosaur integuments, blending insulation, , and visual communication.

History of discovery

Initial discoveries

The first pterosaur fossil was discovered in 1784 near in , , by Italian naturalist Cosimo Alessandro Collini, who served as superintendent of the natural history collections at the . Collini described the incomplete , later as Pterodactylus antiquus, in a detailed memoir, interpreting it as an unusual aquatic vertebrate with webbed feet and a possibly bird-like form, but he refrained from assigning it to any known group. The specimen, preserved in the fine-grained , featured a long fourth finger supporting wing membranes, though Collini did not recognize its aerial adaptations. In 1801, French anatomist Georges Cuvier re-examined Collini's description and a cast of the fossil, correctly identifying it as a flying reptile with bat-like wings, distinct from birds due to its reptilian skeletal features. Cuvier formalized the name "Ptero-dactyle" in his 1809 publication Annales du Muséum d'Histoire Naturelle, emphasizing its toothed jaws and elongated finger as evidence of a novel reptilian order capable of flight. This naming spurred further interest, leading to additional discoveries in the Solnhofen Limestone during the 1820s, including specimens of long-tailed pterosaurs that Georg August Goldfuss described in 1831 as Ornithocephalus münsteri (later recognized as Rhamphorhynchus muensteri). Early interpretations sparked debates over pterosaurs' affinities, with some naturalists like Collini viewing them as bird-like or aquatic creatures, while Cuvier firmly placed them among reptiles based on vertebral and limb comparisons to and crocodiles. By the 1840s, British paleontologist reinforced this reptilian classification in his analyses of and new finds, arguing against avian links by highlighting the absence of feathers and the presence of sauropsid skeletal traits in publications such as his 1842 Report on British Fossil Reptiles. Owen's work, including descriptions of British specimens like Dimorphodon macronyx (first noted in 1828 from ), contributed to the British Museum's early acquisitions, where illustrations depicted these fossils as winged with sprawling limbs.

19th and early 20th century research

The mid-19th century marked a significant expansion in pterosaur research, driven primarily by the exceptional preservation of fossils from the in , , which yielded hundreds of specimens and led to the naming of numerous species, many initially classified under the . Paleontologists such as Hermann von Meyer described several new taxa from these deposits, including Ctenochasma in 1851 and in 1846, contributing to a proliferation of over 100 pterosaur species names by the early , though most are now regarded as synonyms of a handful of valid genera. This "Solnhofen boom" facilitated detailed anatomical studies and established pterosaurs as a distinct group of reptiles, separate from birds and bats. In 1870, British paleontologist Harry Govier Seeley proposed the subclass Ornithosauria to encompass all known pterosaurs, emphasizing their unique osteology based on fossils from the Cambridge Greensand and other British sites, which highlighted differences from traditional reptilian classifications. Concurrently, research expanded globally beyond ; in the , American paleontologist discovered the first North American pterosaur remains during expeditions to the Smoky Hill Chalk of , initially naming a partial wing oweni in honor of rival , though he later established the genus in 1876 for these edentulous forms with wingspans up to 7 meters. The Owen-Marsh rivalry, part of the broader "," spurred competitive naming and collection efforts, accelerating taxonomic descriptions of pterosaurs. Early interpretations often misconstrued pterosaur locomotion and capabilities; 19th-century reconstructions frequently depicted them as awkward quadrupeds incapable of sustained flight, with elongated fingers and toes suggesting a sprawling gait rather than bipedal or aerial prowess. This view persisted into the early 20th century, when some scholars, influenced by the animal's presumed heavy build, proposed they were primarily gliders rather than active fliers, a notion challenged by biomechanical analyses in the 1910s that began modeling their wings as efficient lift-generating structures. Institutional advancements bolstered this era's progress: the American Museum of Natural History (AMNH) amassed extensive collections from Kansas quarries in the 1890s–1910s, while the British Museum of Natural History (BMNH, now Natural History Museum) curated European specimens; Reginald Hooley's 1925 monograph on Isle of Wight pterosaurs, including the large ornithocheirid Istiodactylus, synthesized anatomical data and refined understandings of cranial and postcranial morphology.

Modern renaissance and recent finds

The modern study of pterosaurs experienced a significant resurgence beginning in the , driven by detailed monographic works that synthesized and expanded upon earlier fragmentary evidence. S. Christopher Bennett's extensive research during the 1980s and 1990s, including his 2001 study on the of and subsequent papers on its and growth, provided comprehensive anatomical revisions and highlighted the diversity of forms, revitalizing interest in pterosaur and . Parallel to this, major fossil discoveries from the in northeastern , which gained prominence in the , revealed exceptionally preserved pterosaurs with structures. These finds included specimens of dsungaripterids and anurognathids exhibiting pycnofibers—filamentous integumentary structures akin to those preserved in the theropod dinosaur —indicating a feathered or fuzzy body covering in some pterosaurs. Excavations in the Yixian and Jiufotang Formations yielded over a dozen new genera by the early , such as Beipiaopterus and Nurhachius, expanding understanding of pterosaur diversity in Asia during the Aptian-Albian stages. A contemporaneous boom in Brazilian pterosaur discoveries, starting in the 1970s from the Araripe Basin's Santana and Romualdo Formations, further fueled this renaissance. These lagerstätten produced hundreds of three-dimensional specimens, including tapejarids like Tapejara and azhdarchoids like Anhanguera, revealing adaptations for and crested head structures; by the , over 20 new species had been described, establishing as a key source for pterosaur material. Advancements in imaging technologies during the and transformed pterosaur research by enabling non-destructive analysis of internal structures. Computed tomography (CT) scanning and allowed detailed reconstruction of cranial cavities, pneumatic bones, and flight musculature, as demonstrated in studies of Solnhofen specimens revealing braincase morphology and vascularization. In Romania's Basin, 2010s excavations uncovered azhdarchid remains with preserved soft tissue impressions, including wing membrane outlines and neck skin textures in taxa like , providing insights into integumentary diversity beyond skeletal data. Post-2020 discoveries have continued to address longstanding gaps in the pterosaur record, particularly for forms. In , the nearly complete skeleton of sgiathanach from Scotland's Lealt Shale Formation was described, representing the oldest known large-bodied pterosaur with a exceeding 2.5 meters and offering the first three-dimensional view of early rhamphorhynchoid . This find, analyzed via CT scans, illuminated the earlier of gigantism in pterosaurs. Further enhancing Jurassic diversity, a 2023 study of postcranial elements from of Skye documented multiple morphotypes, including limb bones indicative of at least three distinct pterosaur lineages coexisting in the stage and challenging prior underestimates of richness. In 2024, a partial pterodactyloid wing from the Kimmeridgian-Tithonian of , , was identified as one of the largest specimens with an estimated 3-meter wingspan, highlighting the presence of advanced pterodactyloids in . In 2025, discoveries from included Bakiribu waridza, the first filter-feeding archaeopterodactyloid pterosaur from the Santana Group's , preserved in regurgitalite and exhibiting features linking European and tropical forms, as well as Galgadraco zephyrius, a small species from that connects Brazilian and Romanian pterosaur faunas. Additionally, a redescription of a giant muensteri specimen with a 1.8-meter from the challenged assumptions about size limits in pterosaurs. Behavioral and ecological insights have also advanced through recent ontogenetic studies. A 2021 analysis of and juvenile proportions demonstrated that young pterosaurs were capable of powered flight from birth, occupying distinct aerial niches from adults and suggesting precocial development in multiple lineages. That same year, the darwinopterid Kunpengopterus antipollicatus from the revealed arboreal adaptations, including the earliest opposed for grasping branches, indicating tree-dwelling habits in early pterosaurs. These findings have improved understanding of pterosaur life histories and filled gaps in juvenile morphology.

Evolutionary history

Origins and early diversification

Pterosaurs originated in the , approximately 228 million years ago during the stage, evolving from archosauromorph reptiles within the Ornithodira. Phylogenetic analyses position them as the to , a family of small, reptiles known from the Middle to , sharing synapomorphies including elongated hindlimbs, a reduced , and neuroanatomical adaptations for enhanced that prefigure pterosaur flight-related traits. Ezcurra et al. (2020) demonstrated this close relationship through comprehensive morphological comparisons, bridging a significant evolutionary gap between non-volant precursors and the first flying vertebrates. Further insights into transitional forms come from taylori, a diminutive reptile from the Sandstone Formation in . Micro-CT scans revealed previously unrecognized features, such as a lightweight skull and elongated limbs, placing as a basal member of and closely allied to lagerpetids and pterosaurs. Foffa et al. (2022) revised its diagnosis, highlighting its role in illuminating the early radiation of flight-capable archosauromorphs from dinosauromorph-like ancestors. The earliest definitive pterosaurs appeared by the late to stages, exemplified by buffarinii from the Calcari della Furlo Formation in , which preserves a small body size (wingspan ~45 cm) and primitive skeletal features including a long, stiffened tail. This taxon, redescribed by Dalla Vecchia (2013), lacks advanced flight specializations seen in later forms, indicating an initial phase of experimentation with powered flight. By the , more derived taxa like ranzii from the Dolomia di Forni Formation in and exhibited basal traits such as multicusped teeth suited for grasping small prey and elongated fourth digits supporting patagial membranes, suggesting diets focused on or . Wild (1978) originally described , noting its ~1 m wingspan and robust dentition as hallmarks of early pterosaur morphology. Early diversification accelerated in the , with around 10 genera documented across and , including Raeticodactylus filisurensis from the Kössen Formation in , a basal non-pterodactyloid with a prominent cranial crest and indicating piscivory. Dalla Vecchia (2009) described Raeticodactylus as potentially transitional, its bridging precursory forms and more specialized pterosaurs. These taxa adapted primarily to coastal and marginal marine environments, as evidenced by their preservation in lagoonal and shallow marine deposits like black shales of the Alpine region, implying an initial tied to aquatic habitats for foraging and nesting. Fossil records from the subsequent Rhaetian stage remain sparse, creating a gap in understanding the transition to diversity, though limited finds suggest continuity in coastal adaptations. Recent analyses, such as those by Foffa et al. (2025), interpret the predominance of marine-influenced sediments for early pterosaur fossils as evidence for aquatic-influenced origins, potentially facilitating the of flight through access to abundant protein-rich prey in intertidal zones.

Mesozoic radiation and diversity

During the Period (approximately 201–145 Ma), pterosaurs underwent significant diversification following their origins, with non-pterodactyloid forms dominating early stages and pterodactyloids emerging prominently in the . The record, previously sparse, has been enriched by recent discoveries such as Dearc sgiathanach from the Isle of Skye, , indicating a broader taxonomic and morphological diversity than previously recognized, including larger individuals with wingspans exceeding 2.5 m. This expansion included the rise of marine-adapted forms, with the in preserving an exceptional array of species, including and early pterodactyloids like , reflecting peak diversity in coastal and lagoonal environments during the . Overall, Jurassic pterosaur diversification occurred in multi-wave pulses, driven by ecological opportunities in island archipelagos and shallow seas, leading to increased disparity in wing morphology and body sizes. The transition to the Period (145–66 Ma) marked a major radiation of pterodactyloid clades, with a sharp diversity decline at the Jurassic- boundary followed by rapid recovery and expansion, particularly among advanced pterodactyloids. Giant azhdarchids, such as and with wingspans up to 10–12 m, dominated late-stage skies, adapting to terrestrial foraging in floodplains and uplands. In , tapejarids exhibited high diversity, with forms like Tapejara and showcasing ornate crests and specialized feeding structures, contributing to regional in and ; recent discoveries as of 2025, such as Galgadraco zephyrius from , further highlight unexpected biogeographic links with Laurasian forms. Niche partitioning with contemporaneous birds and early bats allowed pterosaurs to occupy larger-bodied aerial roles, with birds filling smaller insectivorous niches and bats emphasizing , minimizing direct competition. Global distribution patterns revealed distinct Laurasian and Gondwanan faunas, influenced by continental configurations and sea-level fluctuations; Laurasian assemblages featured diverse ornithocheiroids in and , while Gondwanan records highlighted azhdarchoids and tapejarids in and . Recent finds, including postcranial elements from Skye, have elevated the known pterosaur generic diversity to approximately 130, underscoring underestimated early radiations. Ecologically, pterosaurs shifted from predominantly insectivorous diets in the to piscivory, carnivory, and even filter-feeding in the , exemplified by ctenochasmatids with elongated, comb-like teeth. Body size trends generally followed , with mean wingspans increasing over time, though exceptions persisted in smaller, specialized forms that avoided competition with larger congeners through ontogenetic niche partitioning.

Extinction

Pterosaurs underwent an abrupt extinction at the Cretaceous-Paleogene (K-Pg) boundary approximately 66 million years ago, coinciding with the disappearance of non-avian dinosaurs and many other groups from the fossil record. No pterosaur fossils have been documented in strata above the boundary worldwide, indicating a complete and instantaneous clade-level extinction rather than a prolonged decline. The latest known pterosaur remains occur in late Maastrichtian deposits, such as the Hell Creek Formation of North America, where isolated azhdarchid cervical vertebrae—similar in morphology to those of Quetzalcoatlus—represent the final North American records just prior to the boundary. In North Africa, the Ouled Abdoun phosphate deposits yield a diverse assemblage including Tethydraco regalis (Pteranodontidae), Alcione elainus and Barbaridactylus grandis (Nyctosauridae), and azhdarchids like Phosphatodraco mauritanicus, demonstrating sustained taxonomic richness up to ~1 million years before the K-Pg event. The extinction is primarily linked to the Chicxulub asteroid impact off the , which unleashed a cascade of global disruptions including an "" from atmospheric soot, , and wildfires that collapsed food webs and primary productivity. Deccan Traps volcanism in , with massive eruptions releasing climate-altering gases over millennia leading to the boundary, likely exacerbated environmental stress through greenhouse warming and , compounding the impact's effects. Pterosaurs' ecological vulnerabilities amplified their susceptibility: most species were large-bodied (wingspans often exceeding 5 meters), with inferred low reproductive rates and determinate growth patterns that limited population recovery compared to the small, high-fecundity early birds that survived. Prior to the K-Pg crisis, pterosaurs experienced competitive pressures from avian radiation, particularly in small-bodied flying niches, leading to toward and reduced overlap in dietary and locomotor guilds. A 2021 study accounting for sampling biases in the record found evidence of niche partitioning, with pterosaurs dominating larger aerial and terrestrial foraging roles while birds increasingly occupied insectivorous and small-prey domains, though full competitive replacement remains debated. Unlike resilient reptile clades such as crocodilians or turtles that produced Lazarus taxa through refugia or reduced metabolic demands, pterosaurs show no such post-boundary reappearances, underscoring their total eradication without ecological rebound.

Systematics

Classification

Pterosauria, erected by in 1842, represents a monophyletic defined as the of , Preondactylus buffarinii, and northropi and all its descendants. This group occupies a basal position within Ornithodira as the sister taxon to , collectively forming part of the larger inside Archosauria. Subgroups such as Novialoidea (encompassing advanced non-pterodactyloid forms) and Caelidracones (a clade of derived pterosaurs including many pterodactyloids) have been proposed in recent taxonomic frameworks to refine interrelationships among early and transitional taxa. Pterosaurs are traditionally classified into two primary groups: the paraphyletic "," comprising basal forms characterized by long tails, elongated skulls, and multiple teeth, and the monophyletic , which includes advanced, short-tailed taxa with reduced tails, larger heads relative to body size, and specialized wing structures. Within , four major clades are widely recognized: Ornithocheiroidea (basal pterodactyloids with robust, toothed jaws and often crested snouts), Ctenochasmatoidea (filter-feeders with elongated, finely toothed rostra), Dsungaripteroidea (forms with specialized dentition for hard prey and varied cranial features), and (terrestrial stalkers with long necks, toothless jaws, and reduced hindlimbs; often placed as a subclade). These clades reflect increasing specialization from early origins to diversity. Representative genera illustrate the morphological diversity across these groups. Basal rhamphorhynchoids include (small size, multicusped teeth, and a moderately long tail from Late Triassic ) and (upturned snout, long tail with a distal vane for stability, and piscivorous dentition from Late Jurassic ). Dimorphodon features a robust skull with two tooth morphologies (sharp frontals for grasping, coarser posteriors for crushing) and short wings suited for agile flight. Anurognathus is notable for its short tail, large orbits indicating nocturnal habits, and short, broad jaws with reduced teeth for insectivory. Transitional forms like Campylognathoides exhibit elongated rostra and intermediate tail lengths bridging basal and advanced designs. Among pterodactyloids, (the , small-bodied with a short tail, large eyes, and an elongated fourth finger supporting the wing membrane from ) exemplifies early members of the group. Germanodactylus displays a deep, robust and strong for tearing prey. In Ornithocheiroidea, is distinguished by its toothless , prominent crest (larger in males), and wingspan up to 7 meters for soaring over oceans; Anhanguera has a kite-shaped premaxillary crest and interlocking teeth for catching . features an extreme, sail-like cranial crest potentially for display or aerodynamics. Ctenochasmatoids include Ctenochasma, with over 1,000 slender teeth forming a rake-like filter for straining small aquatic prey from soft sediment. Dsungaripteroids and azhdarchoids highlight late-stage adaptations: Tapejara bears a colorful, semicircular crest combining table and extensions, likely for visual signaling; (a dsungaripterid) possesses upturned tips and knobby, crushing teeth suited for hard-shelled prey. Azhdarchoids encompass (the largest known, with a 10-12 meter , long neck, and toothless jaws for terrestrial foraging) and (massive up to 2.5 meters long with a sharp, spear-like rostrum for predation on small vertebrates). These genera, spanning to , underscore the clade's . Pterosaur nomenclature has been fraught with issues since the , when over 100 invalid genera were erected based on fragmentary or poorly preserved specimens, leading to widespread synonymy and taxonomic instability. Recent revisions have addressed these challenges; for instance, a 2024 analysis re-evaluated Pterodactylus antiquus and Diopecephalus kochi, confirming them as distinct taxa, with D. kochi as the most basal pterodactyloid, and refining species boundaries within the genus. In , systematic reviews of proposed new clades like Anhangueroidea and emendations to stabilize names under both ICZN and , resolving conflicts in anhanguerid taxonomy. In , a phylogenetic study of further refined relationships within this diverse clade, highlighting the evolution of giant forms. These updates continue to streamline the over 280 named genera, with approximately 200 currently considered valid (as of ).

Phylogeny

Phylogenetic analyses of pterosaurs rely on cladistic methods that employ large character matrices to infer evolutionary relationships. These matrices typically include over 200 discrete morphological traits, such as variations in length, finger elongation for support, cranial fenestration, and vertebral morphology, scored across dozens to hundreds of taxa. Parsimony-based approaches, often implemented in software like TNT, search for the most efficient trees that minimize evolutionary changes, using techniques such as tree bisection-reconnection swapping to explore vast solution spaces. Recent analyses incorporate supertrees combining multiple datasets to resolve finer relationships, with matrices exceeding 200 taxa and 270 characters, including 158 cranial features alone. Consensus phylogenies from these analyses depict a basal grade of early pterosaurs, with as the most stemward taxon, followed stepwise by and . More derived non-pterodactyloids include Campylognathoididae, marking a split toward the clade comprising Rhamphorhynchidae and , defined by shared traits like elongated rostra and specialized wing membranes. emerges as a robust monophyletic group, supported by high bootstrap values often exceeding 90% in parsimony analyses, uniting short-tailed forms with advanced and reduced pedal digits. Within , major subclades such as Archaeopterodactyloidea, , and form successive branches, reflecting progressive adaptations in flight and feeding. Debates persist regarding the position of transitional taxa like wukongopterids, which exhibit a of basal non-pterodactyloid traits (e.g., long tails) and derived features (e.g., elongated skulls akin to pterodactyloids), often placing them as stemward to in cladograms. Their exact affinity varies across analyses, with some recovering them in polytomies near Darwinopterus, highlighting during the transition from long- to short-tailed forms. In the 2020s, updates incorporating new taxa such as sgiathanach—a Middle Jurassic specimen showing intermediate morphologies like extended —have refined these trees, nesting it within Pterodactylomorpha and supporting earlier divergence of monofenestratans, though without direct Ezcurra-led revisions to ingroup topology. Time-calibrated phylogenetic trees, generated via Bayesian tip-dating in MrBayes, reveal pterosaur diversification dynamics spanning the to . These models incorporate stratigraphic ages and fossil constraints to estimate branch lengths, showing initial evolutionary rate increases in the followed by diversification peaks, with net rates surging during the around the (~183–174 Ma), coinciding with global warming and habitat expansion. Subsequent waves occurred in the and , but rates declined toward the end-Cretaceous, underscoring a multi-phase macroevolutionary pattern without a single radiation event.

Paleobiology

Flight capabilities

Pterosaurs employed a quadrupedal launch for takeoff, utilizing all four limbs to generate , with the forelimbs—powered by large flight muscles—contributing the majority of the propulsive force, estimated at 60-80% of total power output. This approach allowed even large to achieve sufficient initial velocity, unlike the bipedal launches more feasible for smaller pterosaurs under 1 kg body mass. The lift required to overcome body weight during this phase follows the aerodynamic equation L=12ρv2SCLL = \frac{1}{2} \rho v^2 S C_L where LL is lift, ρ\rho is air density, vv is velocity, SS is wing area, and CLC_L is the lift coefficient, highlighting the role of wing acceleration in early flight stages. Pterosaur flight combined gliding and flapping, with wing aspect ratios typically ranging from 6 to 10 enabling efficient soaring in many taxa, particularly those with long, narrow wings suited to thermal or slope upcurrents. A 2009 study on soaring seabirds extrapolated to pterosaurs suggested that dynamic soaring—exploiting wind shear—was viable for large forms up to 41 kg, though giants like azhdarchids may have relied on intermittent flapping for sustained travel. Recent computational fluid dynamics simulations in the 2020s have refined these models, confirming low-speed gliding efficiencies but emphasizing flapping bursts for takeoff and maneuvering in variable winds. Energy demands for pterosaur flight were supported by metabolic rates elevated relative to those of modern reptiles, indicative of partial endothermy adapted for aerial activity. loadings averaged 10-20 kg/m² across , balancing lift generation with structural limits and allowing flight speeds of 15-30 m/s in larger forms. For azhdarchids, biomechanical models estimate single-flight of 100-500 km using soaring, with overall efficiency improving 50% over 150 million years through evolutionary increases in size and . Key adaptations enhanced these capabilities, including cambered wing membranes that increased lift coefficients for low-speed flight and slotted or upturned tips that reduced induced drag and improved maneuverability during turns or landings. These features, combined with pneumatic structure to minimize , optimized pterosaurs for diverse aerial niches from short bursts to long-distance migration.

Respiratory and metabolic systems

Pterosaurs exhibited a highly efficient analogous to that of birds, characterized by extensive postcranial (PSP) that indicates the presence of multiple invading the . Fossil evidence from early pterosaurs, such as and Austriadactylus, reveals PSP in , dorsal vertebrae, ribs, and sternal elements, supporting the existence of cervical, anterior thoracic, and abdominal . These diverticula extended from the lungs, lightening the while facilitating . The configuration of pneumatic foramina and skeletal architecture in pterosaurs suggests a unidirectional through the lungs, similar to modern birds, where inhaled air passes through the lungs in a continuous loop rather than tidal bidirectional flow. This system, inferred from the patterned invasion of diverticula into , would have minimized dead space and maximized oxygen extraction, essential for the aerobic demands of powered flight. Micro-CT scans of anhanguerid pterosaurs, such as Coloborhynchus, confirm extensive vertebral pneumatization occupying 68-72% of volume, with higher air space proportions in neural arches, further evidencing the broad extent of these sacs. This respiratory apparatus supported high metabolic rates indicative of endothermy. Bone histology in taxa like and Pterodaustro shows fibrolamellar bone tissue with rapid deposition rates comparable to those of modern endotherms, implying sustained high growth and oxygen delivery needs. Estimated tidal volumes, modeled from skeletal and soft-tissue proxies, range from 20-50 ml/kg body mass, enabling efficient ventilation that could supply the elevated oxygen requirements for . Isotopic analyses provide direct evidence of elevated body temperatures. Isotopic analyses of pterosaur remains provide evidence of elevated body temperatures consistent with endothermy, higher than those of co-occurring ectothermic reptiles like crocodilians. Carbon isotope (δ¹³C) compositions in bone collagen further suggest metabolically active tissues with rates exceeding those of extant reptiles, though variable across lineages. Pycnofibers, filamentous integumentary structures preserved in several pterosaurs, likely aided insulation to maintain these thermal regimes.

Locomotion on land and in water

Pterosaurs primarily utilized quadrupedal locomotion on land, with the forelimbs serving as the main load-bearing elements due to the anterior position of their center of gravity and the elongated wings attached to the fourth finger. This gait involved a form of knuckle-walking, where the digits of the manus were flexed ventrally to support weight, analogous to that seen in apes but adapted to the pterosaur's lateral hand orientation. Fossil trackways, such as those from the Upper Cretaceous Hwasun Seoyuri site in Korea and the Late Jurassic Wierzbica deposits in Poland, preserve impressions of both manus and pes prints, indicating symmetrical gaits with the forelimbs bearing more weight, as evidenced by deeper manus impressions. Estimated walking speeds from these trackways range from 0.25 to 1 m/s, reflecting deliberate, energy-efficient progression rather than rapid movement. In smaller taxa, such as early non-pterodactyloids, bipedal locomotion may have been possible or even habitual, facilitated by relatively longer hindlimbs and a more posterior center of gravity compared to larger pterodactyloids. However, the overall reduction in hindlimb length relative to forelimbs in most pterosaurs resulted in a waddling gait, limiting agility and increasing energy expenditure for terrestrial travel—potentially several times higher than in comparably sized birds due to the mechanical inefficiency of their sprawling posture and heavy wing loading. Evidence from skeletal remains suggests that some pterosaurs, particularly juveniles, possessed adaptations for , such as opposed thumbs and curved claws, indicating an arboreal component to their terrestrial habits that may have aided in accessing elevated resting or feeding sites. A discovery of the darwinopteran Kunpengopterus antipollicatus revealed the oldest known opposed thumb in pterosaurs, supporting arboreal capabilities through principal coordinate analyses of anatomical traits. In aquatic environments, certain pterosaurs exhibited adaptations for , particularly piscivorous forms like those in , which possessed enlarged, paddle-like feet with elongated metatarsals and interdigital webbing to facilitate propulsion through water. Swim trackways, characterized by elongate scrape marks from paddling feet and occasional paired depressions, document this behavior in shallow marine or lacustrine settings, as seen in deposits of western . The uropatagium, a membranous structure spanning the hindlimbs, likely acted as a stabilizer during , enhancing maneuverability similar to a . Buoyancy models based on three-dimensional reconstructions show that piscivorous pterosaurs, such as and , floated high in water with their bodies and necks held horizontally, immersing only the ventral quarter to third of the ; however, this posture positioned the external nares near or below the waterline, posing drowning risks during extended aquatic activity. These models imply that while capable of short-distance for , prolonged submersion or rough waters would have been challenging, favoring rapid aerial escapes over sustained surface dwelling.

Sensory and nervous systems

Pterosaur brains, as revealed by endocasts derived from computed tomographic (CT) scans of braincases, exhibit a mosaic of reptilian and avian-like features adapted for aerial lifestyles. The was notably expanded relative to basal reptiles, displacing the optic lobes ventrolaterally and contributing to a pronounced flexure in the axis, a condition intermediate between non-pterodactyloid and pterodactyloid forms. The , a cerebellar lobe associated with balance and gaze stabilization during flight, was disproportionately large, comprising approximately 7.5% of total volume in species like Rhamphorhynchus muensteri and Anhanguera santanae, exceeding the 1-2% typical in birds. Optic lobes, indicative of visual processing, were enlarged but secondary in size to the flocculus, positioned beneath the cerebral hemispheres in derived taxa, suggesting enhanced for navigation and prey detection. Encephalization quotients (EQs), a measure of relative adjusted for body mass, ranged from 0.3 to 0.5 across pterosaurs, lower than avian values (typically >1) but higher than most reptiles, reflecting moderate cognitive demands for flight control and sensory integration. A 2016 CT analysis of the early pterodactyloid Allkaruen koi from the of revealed a bird-like with an extremely enlarged (40-50% larger than in contemporaries) and ventrally displaced optic lobes, marking an evolutionary transition toward more avian for aerial agility. Sensory systems emphasized vision as the primary modality, with enlarged optic lobes supporting high-resolution sight, potentially including for in select taxa like Anhanguera, facilitated by a downturned head posture that aligned binocular fields with the horizon or prey. Olfactory bulbs varied in size, moderately developed in many pterosaurs for general chemosensory roles, though smaller in azhdarchids, indicating smell was secondary to vision but retained for cues. Claims of echolocation remain unproven, lacking anatomical or evidence such as specialized laryngeal structures seen in bats. Neural wiring adaptations included impressions of in endocasts, with the (CN X) exiting the braincase alongside glossopharyngeal and accessory nerves in a shared , supporting autonomic functions like respiration during flight. Spinal cord canals were highly enlarged relative to body size, particularly in the cervical and regions, enabling short neural circuits for rapid motor responses and enhanced agility in locomotion and maneuvering. These features underscore pterosaurs' reliance on integrated sensory-motor systems for powered flight and environmental navigation.

Diet and feeding ecology

Pterosaurs were predominantly carnivorous, with diets centered on animal prey across various taxa. Piscivory was widespread among many groups, particularly those with elongated suited for capturing , as evidenced by contents containing scales and bones in species like . A specialized form of piscivory involved filter-feeding, most notably in Pterodaustro guinazui from the of , which possessed over 1,000 bristle-like teeth in its lower jaw for straining small aquatic crustaceans and algae from water, analogous to modern . Insectivory characterized smaller-bodied pterosaurs such as anurognathids, whose short, wide jaws and large eyes suggest aerial hawking of flying in low-light conditions, supported by dental microwear textures indicating soft-bodied consumption. Evidence for pterosaurivory, or predation on other pterosaurs, comes from coprolites and associations, including a specimen where putative fecal material near a contained fragments interpretable as conspecific remains, indicating occasional or intraspecific predation. Although carnivory dominated, recent discoveries provide direct evidence for herbivory in at least some pterosaurs. In 2025, analysis of gastric contents in the tapejarid atavismus from the of revealed phytoliths—microscopic silica bodies—alongside gastroliths, marking the first unequivocal proof of consumption in pterosaurs and challenging prior assumptions of exclusive faunivory. Gastroliths, polished stones likely aiding digestion of tough material, have also been reported in other taxa such as Pterodaustro, further supporting occasional or opportunistic herbivory in select lineages. Pterosaur foraging strategies varied by ecology and morphology, including skim-feeding where ornithocheiroids like dipped their long jaws into water to scoop near the surface, and aerial hawking for intercepting airborne prey. Biomechanical models using finite element analysis estimate bite forces in smaller pterosaurs, such as , at 10–50 N, sufficient for grasping soft prey like or but inadequate for crushing hard-shelled items. Niche partitioning among pterosaurs minimized , with juveniles of larger species filling gaps in small-insect that adults overlooked, as indicated by ontogenetic studies showing capability and distinct size-based prey selection. Piscivorous pterosaurs likely competed with marine reptiles like ichthyosaurs for mid-sized resources in coastal environments, though isotopic data suggest some dietary separation through prey size or preferences.

Reproduction and ontogeny

Pterosaurs were oviparous reptiles that laid eggs with pliable, parchment-like shells composed of calcite fibers, which absorbed water during incubation and could increase in mass by 150–200%. These shells differed from the more rigid structures of some archosaurs but shared similarities with those of lepidosaurs, allowing flexibility during embryonic development. Fossil evidence confirms , with no indications of or other reproductive modes.00525-9) The first three-dimensionally preserved pterosaur eggs were discovered in 2014 from the in northeastern , associated with skeletons of the pterosaur Darwinopterus linglongtaensis.00525-9) These eggs measured approximately 16 cm in length and 3 cm in width, with elongated, ovoid shapes and a 1:1 size ratio relative to the small adult females that laid them, suggesting that egg size was constrained by maternal body dimensions.00525-9) The finds included multiple eggs clustered near adults, hinting at possible nesting behaviors, and revealed in cranial crests, where females lacked prominent crests while males had larger ones, potentially linked to reproductive display or mate selection.00525-9) Further insights came from a 2017 discovery of over 300 eggs of Hamipterus tianshanensis in the Lower Cretaceous Shirkentawu Formation, also in , representing the largest known accumulation of pterosaur eggs. Sixteen eggs contained three-dimensional embryos in mid- to late-stage development, showing early of the flight apparatus, including the fourth manual digit. The eggs, measuring 2–3 cm in diameter, indicate that hatchlings had wingspans of about 10–20% of adult size—for example, around 0.29 m for Pterodaustro compared to 3 m in adults—enabling super-precocial independence shortly after hatching. This egg cache, found in a sedimentary context suggesting substrate burial for incubation, supports possible colonial nesting, though direct evidence remains limited. Ontogenetic growth in pterosaurs was rapid, characterized by fibrolamellar bone tissue in limb shafts, indicative of high metabolic rates and fast skeletal deposition similar to birds and dinosaurs. Juveniles reached skeletal maturity in 1–3 years, with an initial fast-growth phase lasting 2–3 years followed by slower deposition, as seen in taxa like Pteranodon and Sinopterus. Bone histology reveals determinate growth, with extensive fusion of elements by adulthood, and sexual dimorphism often expressed in crest development during late ontogeny.00525-9) Evidence for parental care is minimal and largely inferential, derived from egg accumulations near adult remains, which may indicate protective behaviors or communal nesting in some species. However, the precocial nature of hatchlings, with functional flight capabilities at emergence, suggests limited post-hatching investment, though larger Cretaceous pterosaurs like Pteranodon may have exhibited enhanced care to support extended juvenile dependence.

Predation and daily rhythms

Pterosaurs faced predation from various vertebrates, with direct fossil evidence primarily consisting of bite marks on bones and rare associated remains. Crocodylomorphs, such as basal crocodylians, left identifiable tooth punctures on pterosaur skeletons, as seen in a Campanian-aged cervical of a juvenile Cryodrakon boreas from , , featuring a 4 mm-wide conical puncture consistent with crocodilian and lacking signs of healing, suggesting scavenging or a fatal attack. Theropod dinosaurs, including dromaeosaurids, also preyed on pterosaurs, evidenced by a azhdarchid wing with embedded velociraptorine teeth and associated bite traces indicating active predation. Although direct evidence is sparse, post-Cretaceous analogs from modern avian predators suggest that early birds like enantiornithines could have opportunistically targeted smaller pterosaurs, mirroring how raptors exploit flying reptiles today. Coprolites and gut contents rarely preserve pterosaur remains, but reviews of food webs document instances of pterosaur bones and wings in theropod digestive traces, underscoring their role as occasional prey. To counter these threats, pterosaurs employed behavioral and structural defenses suited to their aerial lifestyle. Rapid flight allowed escape from ground-based predators like crocodylomorphs, enabling pterosaurs to evade attacks during landing or roosting. Pycnofibers—filamentous integumentary structures covering much of the body—likely aided by providing coloration patterns that blended with forest or coastal environments, similar to in modern birds, potentially reducing visibility to visually hunting predators. beds, such as the exceptional assemblage of over 50 Caiuajara dobrusa individuals from the of , indicate gregarious , where groups may have offered collective vigilance and reduced individual predation risk through social foraging or nesting. Analysis of scleral rings—bony supports around the eye—reveals diverse daily activity patterns among pterosaurs, inferred from eye morphology that correlates with light sensitivity. Most pterosaurs, including basal forms like , exhibited diurnal habits, with relatively small scleral ring openings indicating adaptation to daytime vision for aerial and . However, some piscivorous taxa, such as certain pterodactyloids, show larger ring diameters suggestive of cathemeral (day-and-night active) or crepuscular patterns, allowing exploitation of low-light conditions for prey while avoiding peak diurnal predators. Stable isotope ratios in pterosaur bones and teeth further imply migratory behaviors in select , with variations in carbon and oxygen signatures indicating seasonal movements between coastal breeding grounds and inland foraging areas, potentially to evade localized predation pressures or access resources. Recent studies on fossils from the of China, including bite traces on dsungaripterid remains, reinforce these patterns by showing predation hotspots that may have driven adaptive rhythms and migrations.

Cultural depictions

In scientific illustration and paleoart

The earliest scientific illustrations of pterosaurs emerged in the late 18th century, with Cosimo Alessandro Collini's 1784 copper engraving of the holotype specimen of Pterodactylus antiquus (then unnamed) depicting it as an enigmatic aquatic creature with elongated, fin-like forelimbs rather than wings. By the early , reinterpreted the same fossil in 1801 as a flying reptile, naming it Ptero-dactyle and influencing subsequent bat-like depictions that emphasized leathery wings stretched between elongated finger IV and the body, often portraying pterosaurs as awkward, bat-mimicking gliders incapable of powered flight. These 1800s illustrations, such as those in Richard Owen's works, reinforced a view of pterosaurs as dimorphic reptiles with sprawling limbs, shaping early restorations in monographs like those of Harry Govier Seeley. In the 1920s, paleoart shifted toward glider poses, with artists like illustrating pterosaurs such as in passive soaring configurations over oceans, reflecting biomechanical assumptions of limited terrestrial mobility and reliance on wind currents for flight rather than active flapping. These depictions, featured in museum murals and publications like William Diller Matthew's texts, highlighted elongated wings as sails but underestimated muscle attachments, perpetuating the image of pterosaurs as fragile aerialists. From the 1970s onward, evolved to portray pterosaurs as dynamic flyers capable of powered flight, inspired by S. Christopher Bennett's anatomical analyses that emphasized robust shoulder girdles and muscle scars for sustained flapping. Bennett's reconstructions in papers and monographs depicted species like in active launch poses, influencing artists to show agile, bird-like aerial maneuvers over the earlier glider stereotypes. In the 2020s, paleoartist Mark Witton has advanced this tradition by integrating fossil evidence of soft tissues, such as pycnofibers—filamentous structures akin to proto-feathers—into vivid illustrations of taxa like and Pterodaustro, rendering them with fuzzy body coverings and textured wing membranes for more ecologically realistic scenes. Witton's works, often accompanying peer-reviewed studies, draw on recent specimens to emphasize pycnofiber distributions varying by body region, enhancing depictions of insulation and sensory roles. Pterosaur restorations have played a pivotal role in scientific monographs, serving as visual hypotheses to test anatomical interpretations and often igniting debates over posture, particularly the quadrupedal versus bipedal stances for and flight launches. For instance, early 20th-century illustrations favored bipedal upright poses, but trackway evidence and biomechanical models from the 1980s onward, as in Kevin Padian's analyses, supported quadrupedal with forelimbs positioned under the body, leading to revised restorations showing pterosaurs as proficient walkers rather than sprawlers. These debates, visualized in comparative diagrams within journals like Palaeontology, have refined to balance flight-ready with ground-based agility, avoiding earlier caricatures of clumsiness. The finely laminated slabs from have profoundly shaped accurate wing art by preserving rare soft-tissue impressions, including aktinofibrils—fine fibers reinforcing the —and vascular patterns that reveal the membrane's extent from ankle to elongated finger IV. Specimens like the crassirostris holotype, with its documented wing web and pycnofibers, have guided reconstructions to depict taut, multilayered membranes capable of precise control, as analyzed through techniques like reflectance transformation imaging. This fossil evidence counters speculative broad-wing models, promoting detailed illustrations in modern monographs that highlight regional variations in membrane thickness and flexibility. Pterosaurs have appeared in popular media since the early , often portrayed as menacing flying creatures akin to dragons in . In Arthur Conan Doyle's 1912 novel The Lost World, pterosaurs are depicted as inhabitants of a hidden prehistoric plateau, inspiring subsequent adaptations that emphasized their dramatic, bat-winged forms. The 1925 adaptation, directed by Harry O. Hoyt, featured groundbreaking stop-motion animation by Willis O'Brien, including models with elongated finger-supported membranes resembling bat wings rather than accurate anatomical structures. Iconic portrayals in late-20th-century media brought pterosaurs to wider audiences, blending scientific inspiration with cinematic spectacle. In Steven Spielberg's (2001), a flock of launches a terrifying attack from an aviary on Isla Sorna, showcasing their role as agile aerial predators with wingspans up to 10 meters, though the film's designs exaggerated their aggression and omitted pycnofibers. The BBC's (1999) series offered more realistic depictions in its fourth episode, "Giant of the Skies," where an migrates across oceans, highlighting powered flight capabilities and behaviors informed by contemporary , such as soaring on thermals. Additionally, the genus , named in 1975 after the Mesoamerican deity Quetzalcoatl—the god symbolizing wind and creation in —has evoked dragon-like imagery, linking the pterosaur to ancient cultural motifs of flying serpents despite no direct prehistoric connection. In modern media, pterosaurs feature prominently in interactive entertainment and updated documentaries, reflecting evolving scientific understanding. Video games like (2015) include tamable and as versatile flying mounts for exploration and combat, with customizable variants emphasizing their utility in survival scenarios. Recent documentaries incorporate discoveries like the 2022 description of Dearc sgiathanach, a well-preserved pterosaur from approximately 170 million years ago, to illustrate early flight evolution, as seen in specials updating aerial life. Similarly, the July 2025 discovery of Eotephradactylus mcintireae, North America's oldest known pterosaur from 209 million years ago, has been featured in media such as and , highlighting early diversification in the . Persistent misconceptions portray pterosaurs as "flying dinosaurs" or scaly reptiles, ignoring their distinct lineage and coverage in pycnofibers—fuzzy, fur-like filaments akin to proto-feathers—leading to inaccurate "furry dinosaur" depictions in some media. Pterosaurs also serve as cultural symbols, particularly in regions rich with their fossils. In , home to diverse Cretaceous pterosaur genera like Tapejara and Anhanguera, these creatures inspire national pride through museum exhibits and educational programs, though not formal emblems. Merchandise trends, including toys and apparel from franchises like , capitalize on their iconic silhouettes, boosting public fascination with prehistoric flight.

References

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