Tethydraco Temporal range: Late Cretaceous, | |
---|---|
Holotype humerus | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Order: | † Pterosauria |
Suborder: | † Pterodactyloidea |
Clade: | † Ornithocheiroidea |
Genus: | † Tethydraco Longrich et al., 2018 |
Type species | |
†Tethydraco regalis Longrich et al., 2018 |
Tethydraco is a genus of pterodactyloid pterosaur that lived during the Late Cretaceous period (Maastrichtian stage) of what is now the area of present Morocco, about 66 million years ago. Tethydraco was originally assigned to the family Pteranodontidae. Some researchers argued that subsequently described material suggests that it may have been an azhdarchid, and possibly synonymous with Phosphatodraco , though this has been disputed. The type and only species is T. regalis. [1]
Since 2015, a group of paleontologists has been acquiring pterosaur fossils from commercial Moroccan fossil traders, who obtain these from workers in the phosphate mines on the Khouribga plateau, which is located within the Ouled Abdoun Basin. The purpose of this project is to determine pterosaur diversity in the latest Cretaceous. From this stage, no Konservat-Lagerstätten are known, sites combining a large variety of species with exceptional preservation. It is in such sites that the vast majority of pterosaur fossils and taxa have been discovered. The latest Cretaceous had only produced some partial skeletons of Azhdarchidae. Researchers usually have concluded from this fact that other pterosaur groups had already gone extinct. However, an alternative explanation could be that the poor fossil record caused a distorted image of the true situation through undersampling. To test this hypothesis, an effort was made to collect all pterosaurs bones brought to light by the massive and systematic commercial exploitation of the Khourigba phosphate layers. It transpired that indeed some finds could not be determined as azhdarchids and likely represented other groups. Four of the findings were described as new species in 2018, including Tethydraco. [1]
In 2018, Nicholas R. Longrich, David M. Martill and Brian Andres described and named the type species Tethydraco regalis. The generic name combines a reference to the Tethys, the ocean in the Late Cretaceous separating Africa from Europe and Asia, with a Latin draco, "dragon". The specific name means "royal" in Latin. [1]
The holotype, FSAC-OB 1, was found in the middle Couche III, itself the lowest phosphate layer complex at Sidi Daoui, dating from the late Maastrichtian. It consists of a left humerus. The bone is relatively crushed. Other specimens have been referred to the species. FSAC-OB 199 is an ulna. FSAC-OB 200 is another ulna. FSAC-OB 201 is a thighbone. FSAC-OB 202 consists of a thighbone with shinbone. The describing authors admitted that a connection between the holotype and the referred specimens is hard to prove, in view of the lack of overlapping material. However, the wide ulnae fit the exceptional distal width of the humerus. The thighbones were, more tentatively, referred because they seemed to be pteranodontid. [1]
Tethydraco had a wingspan of 5 meters (16 ft) and a body mass of 15 kg (33 lb). [1] [2]
The describing authors indicated some traits in which Tethydraco could be distinguished from known pteranodontids. In the humerus, the deltopectoral crest is placed rather proximally, closer to the torso of the animal, its closest border being positioned just proximal to the beginning of the opposite crest, the crista ulnaris. Distally, away from the torso, the humerus has a broad triangular expansion. The bone ridge running to the outer joint condyle has a distinct process pointing to above, when the wing is in a stretched position. The ridge leading to the inner condyle is enlarged and extends towards the torso over a long distance. The ulna is relatively short and wide while its proximal end, towards the humerus, is massively expanded. [1]
Tethydraco was placed in the family Pteranodontidae; it would have been the youngest known member of that family, since its fossil remains dated back 66 million years ago. Its existence was seen as proof that pterosaur diversity in the Maastrichtian was higher than previously assumed. Apparent pterosaur decline would have been an illusion caused by the Signor–Lipps effect, groups seeming to disappear earlier than a mass extinction because their youngest fossils by chance have been found at somewhat older layers than the extinction event. [1]
Below is a cladogram showing the results of a phylogenetic analysis first presented by Andres and colleagues in 2014, and updated with additional data by Longrich and colleagues in 2018. In this analysis, they found Tethydraco to be the sister taxon of the two species of Pteranodon (P. longiceps and P. sternbergi ); all three of them forming the family Pteranodontidae, which is found as the sister taxon of the family Nyctosauridae. [3] [1]
In 2020, a wing from the same deposit was assigned to the genus; however, the morphology suggested that Tethydraco was an azhdarchid, rather than a pteranodontid as originally proposed, and possibly represented the wing-elements of Phosphatodraco . [4] In 2022, researchers who described Epapatelo noted that the humerus of Epapatelo shares similarity with that of Tethydraco and other non-Nyctosaurus pteranodontoids, and recovered Tethydraco as a pteranodontian closely related to Pteranodon . [5]
Tethydraco was discovered in the Ouled Abdoun Basin in Morocco. This basin is divided into layers called "Couches", and Tethydraco was discovered in Couche III. It coexisted with the pterosaurs Alcione , Barbaridactylus , Simurghia and Phosphatodraco and the abelisaurid dinosaur Chenanisaurus . [1] [6]
Azhdarchidae is a family of pterosaurs known primarily from the Late Cretaceous Period, though an isolated vertebra apparently from an azhdarchid is known from the Early Cretaceous as well. Azhdarchids are mainly known for including some of the largest flying animals discovered, but smaller cat-size members have also been found. Originally considered a sub-family of Pteranodontidae, Nesov (1984) named the Azhdarchinae to include the pterosaurs Azhdarcho, Quetzalcoatlus, and Titanopteryx. They were among the last known surviving members of the pterosaurs, and were a rather successful group with a worldwide distribution. Previously it was thought that by the end of the Cretaceous, most pterosaur families except for the Azhdarchidae disappeared from the fossil record, but recent studies indicate a wealth of pterosaurian fauna, including pteranodontids, nyctosaurids, tapejarids and several indeterminate forms.
Nyctosaurus is a genus of nyctosaurid pterosaur from the Late Cretaceous period of what is now the Niobrara Formation of the mid-western United States, which, during the time Nyctosaurus was alive, was covered in an extensive shallow sea. Some remains belonging to a possible Nyctosaurus species called "N." lamegoi have been found in Brazil, though it likely belongs to a different genus Simurghia. The genus Nyctosaurus has had numerous species referred to it, though how many of these may actually be valid requires further study. At least one species possessed an extraordinarily large antler-like cranial crest.
Arambourgiania is a genus of azhdarchid pterosaur that lived during the Maastrichtian age of the Late Cretaceous, in what is now Jordan. Additional fossil remains from the United States and Morocco have also been found, but their assignment to Arambourgiania is only tentative. The original specimen was discovered in the 1940s by a railway worker near Russeifa, Jordan. After examination by paleontologist Camille Arambourg, a new species was named in 1959, Titanopteryx philadelphiae. The generic name means "titan wing", as the fossil was initially misidentified as a huge wing metacarpal, while the specific name refers to the ancient name of Amman, Philadelphia. The genus "Titanopteryx" would later be problematic, as it had already been taken by a fly. Because of this, paleontologist Lev Nessov in 1989 named a new genus, Arambourgiania, in honor of Arambourg. The new species was now known as Arambourgiania philadelphiae.
The Pteranodontidae are a family of large pterosaurs from the Late Cretaceous of North America and possibly other continents including Europe and Africa. The family was named in 1876 by Othniel Charles Marsh. Pteranodontids had a distinctive, elongated crest jutting from the rear of the head. The spectacularly-crested Nyctosaurus is sometimes included in this family, though usually placed in its own family, the Nyctosauridae.
Montanazhdarcho is a genus of azhdarchoid pterosaur from the Late Cretaceous period of what is now the state of Montana, United States. Montanazhdarcho is known from only one species, M. minor.
Phosphatodraco is a genus of azhdarchid pterosaur that lived during the Late Cretaceous of what is now Morocco. In 2000, a pterosaur specimen consisting of five cervical (neck) vertebrae was discovered in the Ouled Abdoun Phosphatic Basin. The specimen was made the holotype of the new genus and species Phosphatodraco mauritanicus in 2003; the genus name means "dragon from the phosphates", and the specific name refers to the region of Mauretania. Phosphatodraco was the first Late Cretaceous pterosaur known from North Africa, and the second pterosaur genus described from Morocco. It is one of the only known azhdarchids preserving a relatively complete neck, and was one of the last known pterosaurs. Additional cervical vertebrae have since been assigned to the genus, and it has been suggested that fossils of the pterosaur Tethydraco represent wing elements of Phosphatodraco.
Cretornis is a pterosaur genus from the late Cretaceous period of what is now the Jizera Formation in the Czech Republic, dating to about 92 million years ago. It only contains a single species, Cretornis hlavaci.
Elanodactylus is a genus of ctenochasmatid pterodactyloid pterosaur from the Early Cretaceous period of what is now the Yixian Formation of Liaoning, China.
Volgadraco is a genus of pteranodontian pterosaur from the Upper Cretaceous of European Russia.
Nyctosauridae is a family of specialized soaring pterosaurs of the late Cretaceous Period of North America, Africa, and possibly other continents including South America. It was named in 1889 by Henry Alleyne Nicholson and Richard Lydekker.
Pteranodontia is an extinct group of ornithocheiroid pterodactyloid pterosaurs. It lived during the Late Cretaceous of North America, South America, Europe and Africa. They were some of the most advanced pterosaurs, and possessed highly specialized cranial crests that may have served as sexual attraction, with males having a much larger crest.
Eupterodactyloidea is an extinct group of pterodactyloid pterosaurs that existed from the latest Late Jurassic to the latest Late Cretaceous periods. Eupterodactyloids have been found on all continents except Antarctica.
Alamodactylus is an extinct genus of pteranodontian pterosaur known from the Late Cretaceous of Texas, southern United States. It contains a single species, Alamodactylus byrdi.
Radiodactylus is an extinct genus of non-azhdarchid azhdarchoid pterosaur known from the Early Cretaceous period of what is now Texas, southern United States. It contains a single species, Radiodactylus langstoni.
The Oulad Abdoun Basin is a phosphate sedimentary basin located in Morocco, near the city of Khouribga. It is the largest in Morocco, comprising 44% of Morocco's phosphate reserves, and at least 26.8 billion tons of phosphate. It is also known as an important site for vertebrate fossils, with deposits ranging from the Late Cretaceous (Cenomanian-Turonian) to the Eocene epoch (Ypresian), a period of about 25 million years.
Alcione is a genus of pterosaur from the Ouled Abdoun Basin of Morocco, dating back to the Maastrichtian stage of the Late Cretaceous period. Only one species, A. elainus, is known. This pterosaur lived in a marine environment alongside several other pterosaurs, including Simurghia and Barbaridactylus.
Barbaridactylus is a nyctosaurid pterosaur from the Ouled Abdoun Basin of Morocco, a basin that dates back to the Maastrichtian stage of the Late Cretaceous. It was published in 2018 by paleontologists Nicholas R. Longrich, David M. Martill, and Brian Andres. In the same publication, two other pterosaurs from the same basin were described: Alcione and Simurghia. The type and only species is B. grandis.
Simurghia is a genus of pterosaur from the Ouled Abdoun Basin of Morocco, a basin that dates to the Maastrichtian stage of the Late Cretaceous period, about 66 million years ago. It was published in 2018 by paleontologists Nicholas R. Longrich, David M. Martill, and Brian Andres, along with two other pterosaurs from the same basin: Alcione and Barbaridactylus. The type species is S. robusta. A possible second species, S. ("Nyctosaurus") lamegoi, is known from the Campanian-Maastrichtian age strata of Brazil.
Apatorhamphus is an extinct genus of azhdarchoid pterosaur from the Kem Kem Group of Morocco. It might have been part of the Chaoyangopteridae. It is only known from a few snout fragments and it likely had a wingspan of between 3–7 metres (9.8–23.0 ft)
Thalassotitan is an extinct genus of large mosasaurs that lived during the late Maastrichtian of the Cretaceous period in what is now Morocco, around 67 to 66 million years ago. The only known species is T. atrox, described in 2022 from fossils discovered in the Ouled Abdoun Basin, initially identified as coming from other genera such as Mosasaurus or Prognathodon. Hypothetical Thalassotitan specimens may have been found in other corners of the world, although researchers also note the possibility that they come from distinct, related taxa. It is considered to be close to the genera Prognathodon and Gnathomortis, together forming the tribe Prognathodontini. The prognathodontines are separated from other mosasaurs based on their massive jaws and robust teeth.