Campylognathoides ("curved jaw") is a genus of pterosaur, discovered in the Württemberg Lias deposits of Germany; this first specimen consisted however only of wing fragments. Further better preserved specimens were found in the Holzmaden shale: basing on these specimens Felix Plieninger erected a new genus.


In 1858 Friedrich August Quenstedt named a new species of PterodactylusP. liasicus. It was based on a fossil, holotype GPIT 9533, consisting of some wing bones, found on the Wittberg near Metzingen in layers dating from the early Toarcian, about 180 million years old. The specific name referred to the Lias. Quenstedt thought he had identified long metacarpals in the wing, concluding that the new species was therefore not belonging to more basal genera, like the long-tailed Rhamphorhynchus. In 1893 commercial fossil collector Bernhard Hauff sr. discovered a skeleton of a large pterosaur near Holzmaden. In 1894 Felix Plieninger based a new genus on this specimen: Campylognathus. The genus name is derived from Greek kampylos, "bent", and gnathos, "jaw", in reference to the bent lower jaw. The type species is Campylognathus zitteli. The specific name honours Alfred Von Zittel. The holotype is SMNS 9787. In 1897 Hauff prepared another specimen that eventually in 1903 was acquired by the Carnegie Museum of Natural History at Pittsburgh. This fossil, CM 11424, is due to its completeness the best source of information about the genus. In 1901 Plieninger for the first time studied P. liasicus and discovered that Quenstedt had mistaken the, in reality short, metacarpal, for a coracoid, meaning it was a basal pterosaur. In 1906 Plieninger referred P. liasicus and the Pittsburgh specimen to Campylognathus, though not yet establishing the specific status of each of the three exemplars. In 1907 however, Plieninger recognised a second species of CampylognathusC. liasicus, to which CM 11424 was referred also. Norwegian entomologist Embrik Strand discovered in the 1920s that the name Campylognathus had previously been used for the African bug Campylognathus nigrensis, a genus of the Heteroptera named in 1890. As the name was thus preoccupied, he renamed the pterosaur Campylognathoides in 1928. During the twentieth century new finds have brought the number of known specimens to about a dozen.


Compared to its contemporary from the same layers Dorygnathus, the snout on this genus is relatively short, though the skull is still in general elongated, be it much lighter built. The large eye sockets, placed low in the skull above a narrowjugal, have caused some researchers to speculate that Campylognathoides had especially acute vision, or possibly even a nocturnal lifestyle. The back of the skull is relatively high and flat, with a sudden downturn just in front of the eyes. The snout ends in a slender point curving a bit upwards at its very end. A large part of the snout is occupied by long bonynares. Below them a small triangular skull opening, the fenestra antorbitalis is present. Reflecting the more shallow snout, the teeth of Campylognathoides are also short and not at all laniaries or fang-like as in the markedly heterodont Dorygnathus. They are conical and recurved but have a broad base with the point bevelled off from the inside forming a sharp and strong cutting surface. In the upper jaw there are four rather widely spaced teeth in thepraemaxilla gradually increasing in size from the front to the back; the fourth pair of teeth is the largest. Behind them are ten smaller teeth in the maxilla, gradually decreasing posteriorely. In the lower jaw there are twelve to fourteen teeth present in C. liasicus, sixteen to nineteen in C. zitteli. The largest total number is thus 66. According to a study by Kevin Padian there are eight cervical vertebrae, fourteen dorsals, four or five sacrals and up to 38 caudal vertebrae. The tail base is flexible with about six short vertebrae; behind them the caudals elongate and are stiffened by very long extensions allowing the tail to function as a rudder. The sternum of Campylognathoides was a rather large rectangular plate of bone with a short forward-facing crest called a cristospina. The upper arm is short but robust with a square deltopectoral crest. The lower arm too is short but wing length is considerable due to the hand, which has short metacarpals but a very long wing finger for a basal pterosaur, of which the second phalanx is the largest. The pteroid is short and robust. The pelvis is not very well known. A fossil collector found a well preserved Campylognathoides hip in a Braunschweig shale quarry in 1986. This pelvis, BSP 1985 I 87, proved to be scientifically significant because the hip socket was according to Peter Wellnhofer in an upward lateral position, preventing the animal from being able to orient its legs erectly like in dinosaurs, birds and mammals. This would prove that Campylognathoides was not well able to walk on its hind legs but must have walked quadrupedally. This gait posture has been confirmed in other rhamphorhynchoids as well. However, Padian in 2009 concluded the opposite, stating that an erected position was necessary to place the feet on the ground and that, though a quadrupedal gait was possible, a bipedal way of locomotion was a precondition for a fast gait. This subject remains highly controversial. The leg is rather short and the feet are small. The fifth toe, often interpreted as carrying a membrane between the legs, is exceptionally short for a basal pterosaur.


Plieninger in his later publications assigned Campylognathus to the "Rhamphorhynchoidea". As this suborder is a paraphyleticassemblage of not specially related basal pterosaurs, this classification merely states the negative fact that it was not apterodactyloid. A positive determination was first attempted by Baron Franz Nopcsa who in 1928 assigned the genus to the subfamily Rhamphorhynchinae within the family Rhamphorhynchidae. After a period in which very little work was done on pterosaur systematics, in 1967 Oskar Kuhn placed Campylognathoides in its own subfamily within the Rhamphorhynchidae, the Campylognathoidinae. However, in 1974 Peter Wellnhofer concluded that it was placed in a more basal position in the phylogenetic tree, below the Rhamphorhynchidae. In the early twenty-first century this was confirmed by the first extensive exact cladistic analyses. In 2003 both David Unwin and Alexander Kellner introduced a clade Campylognathoididae; within Unwin's terminology this clade is the sister clade of the Breviquartossa within the Lonchognatha; applying Kellner's terminology it is the most basal offshoot within the Novialoidea. There is no material difference between the two positions. According to the analyses Campylognathoides would be closely related to Eudimorphodon, to which it is similar in skull, sternum and humerus form. This was confirmed by Padian in 2009, though Padian also pointed out several basal features present in Eudimorphodon but lacking in Campylognathoides. In 2010 an analysis was published by Brian Andres showing that Eudimorphodon together with Austriadactylus formed a very basal clade, leaving Campylognathoides as the only known member of the Campylognathoididae. Other recent phylogenetic analyses confirm these results, and suggest that Campylognathoides is more derived than all Triassic-aged pterosaurs, as well as the Early Jurassic Dimorphodon and ParapsicephalusCampylognathoides is the basalmost member of the Novialoideawhich is defined as a node-based taxon consisting of the last common ancestor of CampylognathoidesQuetzalcoatlus and all its descendants.


Traditionally a piscivore lifestyle is attributed to Campylognathoides, as to most pterosaurs; in this case supported by the provenance of the finds from marine sediments and the very long wings. Padian however, has suggested that, in view of the stout short teeth, ideal for delivering a piercing bite, the form might well have been a predator of small terrestrial animals instead. The niche of specialised fish eater would then have been filled by Dorygnathus which is five times as common in the layers. The area of the fossil sites was in the early Jurassic located to the northwest of a large island, the Massif of Bohemia, situated in a shallow gulf of the Tethys Sea.