Protosqualus | |
---|---|
Drawing of a Protosqualus argentinensis tooth | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Chondrichthyes |
Subclass: | Elasmobranchii |
Subdivision: | Selachimorpha |
Order: | Squaliformes |
Family: | Squalidae |
Genus: | † Protosqualus Cappetta, 1977 |
Type species | |
†Protosqualus sigei [3] Cappetta, 1977 | |
Other species | |
|
Protosqualus ("Primitive Squalus") was a genus of dogfish shark that existed during the Cretaceous. Fossils have been found in Europe (mainly in France, Russia, Germany, Lithuania, The United Kingdom and Ukraine), East Asia (mainly in Japan), [5] Antarctica, [6] Australia, [7] India and South America. [8] [9] The type species is Protosqualus sigei, which was found around an Albian aged deposit in France. [10] There are 6 species which can be differentiated by distinct features in their teeth. Some species show some level of heterodonty, for example Protosqualus barringtonensis shows a rather high level of heterodonty within its teeth. The oldest specimens are from the Speeton Clay Formation. [11] Protosqualus teeth are quite common in the Grey Chalk deposit of England. [12] The genus went extinct at the end of the Cretaceous during the Cretaceous–Paleogene extinction event, with the last species in the genus being Protosqualus argentinensis from southern Argentina as well as possibly being from earlier deposits in India.
The type specimen of Protosqualus was found in a deposit that had been known to contain shark teeth since the 1930's. The type specimen was finally named in 1977 by paleontologist and ichthyologist, Henri Cappetta. The deposit is the Mortoniceras inflatum ammonoid zone. The name Protosqualus literally means "Primitive Squalus" in reference to how it is an ancient genus related to the extant genus, Squalus. The type species, P.sigei, derives its species name from paleontologist, B.Siegé. [10]
Protosqualus, like most fossil sharks, is known from mostly dental remains. [13] Protosqualus had an undulated ventral margin of the dental crown that was distal to the apron. Unlike modern members of the genus Squalus, Protosqualus had dental crowns which did not have a great degree of labiolingual compression. [14] The holotype of P. sigei featured a tooth with small gaps between them, each with a clearly defined slanted tip. Its front ledge was well-developed and slightly raised, culminating in a rounded shape firmly attached at the base of the crown. The back of the tooth appeared flat, with a slight depression near the ledge. The root was low and thick, angled slightly in relation to the crown, and exhibited minor protrusions on both its front and rear sides. The bottom of the tooth was flat and gently curved, with the holes on the sides either separated or, less commonly, connected by a groove. [10] The teeth of P. pachyrhiza were more bulky. [15] Protosqualus glickmani had a broad cusp. [16] Protosqualus argentinensis had defined serrated cutting edges and was probably the largest member of the genus. [14] Protosqualus barringtonensis may have shown some sexual dimorphism in the teeth, however all teeth show a short cusp. [17] P.albertsi had a broad, labial protuberance. [15]
Protosqualus is a member of the Squalidae within the Squaliformes group. Today, only two extant genera of squalids exist. Squalids tend to note have the teeth in their lower jaw not being any larger than the teeth seen in the upper jaw. [18] Below is a cladogram showing where Squalidae sits in the Squaliform clade. [19]
In 2001, Adnet & Cappetta found the following position for Protosqualus. [20] Here, it is shown to be closer to the extant dogfishes called Spurdogs.
Protosqualus lived alongside other chondrichthyans as well as other types of fish. It also lived alongside mosasaurs and plesiosaurs. [21] Fossils of Protosqualus have been found in the Speeton Clay Formation, Omagari Formation, Hunstanton Formation, Jiesia Formation, Lopez de Bertodano Formation, Burim Formation, Ferriby Formation, Karai Formation, [22] Labguva Formation, Hibernian Greensand Formation and Calafate Formation among a few others. The Calafate Formation likely had estuaries and shallow seas. [23] [24]
The Hexanchiformes are a primitive order of sharks, numbering just seven extant species in two families. Fossil sharks that were apparently very similar to modern sevengill species are known from Jurassic specimens.
The Squaliformes are an order of sharks that includes about 126 species in seven families.
Squalidae, more commonly known as dogfish, dog sharks, or spiny dogfish, are one of several families of sharks categorized under Squaliformes, making it the second largest order of sharks, numbering 119 species across 7 families. Having earned their name after a group of fishermen reportedly observed the species chasing down smaller fish in dog-like packs, dogfish have slender, streamlined bodies, usually more compact in comparison to other species, and a pointed snout. Dogfish likewise have two dorsal fins, each with smooth spines, but no anal fin, and their skin is generally rough to the touch. As the species reaches adulthood, males usually measure a maximum of 100 cm, while females typically measure 125 cm long. The species therefore exhibits female-dominant sexual dimorphism.
Squalicorax, commonly known as the crow shark, is a genus of extinct lamniform shark known to have lived during the Cretaceous period. The genus had a global distribution in the Late Cretaceous epoch. Multiple species within this genus are considered to be wastebasket taxon due to morphological similarities in the teeth.
The spiny dogfish, spurdog, mud shark, or piked dogfish is one of the best known species of the Squalidae (dogfish) family of sharks, which is part of the Squaliformes order.
Squalus is a genus of dogfish sharks in the family Squalidae. Commonly known as spurdogs, these sharks are characterized by smooth dorsal fin spines, teeth in upper and lower jaws similar in size, caudal peduncle with lateral keels; upper precaudal pit usually present, and caudal fin without subterminal notch. In spurdogs, the hyomandibula is oriented at a right angle to the neurocranium, while in other sharks, the hyomandibula runs more parallel to the body. This led some to think that the upper jaw of Squalus would not be as protractile as the jaws of other sharks. However, a study that compared different jaw suspension types in sharks showed that this is not the case and that Squalus is quite capable of protruding its upper jaw during feeding.
The mandarin dogfish is a dogfish, a member of the family Squalidae in the order Squaliformes. It is found at depths of 140–650 metres (460–2,130 ft) off southern Japan, Taiwan, and Indonesia. Populations off Australia and New Zealand were formerly included in this species, but in 2007 these were assigned to a new species, the southern mandarin dogfish. It is not clear which of these species is involved in other populations from the tropical West Pacific.
The rasptooth dogfish is a dogfish, found on the Kyushu–Palau Ridge in the northwest Pacific Ocean at depths of 360 m. Its maximum length is unknown. This species was originally described as Centroscyllium sheikoi, and subsequently allocated to the newly named genus Miroscyllium based on anatomical features not shared with other Centroscyllium. More recent molecular data suggest this species belongs to the genus Etmopterus, but as of June 2014 Miroscyllium sheikoi remains the valid name recognized by FishBase, the Catalog of Fishes World Register of Marine Species, and the IUCN
The viper dogfish or viper shark is a rare species of dogfish shark in the family Etmopteridae, and the only extant member of its genus. It has been found in the Pacific Ocean off southern Japan, the Bonin Islands, Pacific Ocean off northern Taitung County and the Northwestern Hawaiian Islands. This species inhabits upper continental slopes and seamounts. It may migrate vertically, shifting between bottom waters 270–360 m (890–1,180 ft) deep during the day and upper waters less than 150 m (490 ft) deep at night. A slender, black shark reaching 54 cm (21 in) in length, the viper dogfish can be recognized by its narrow, triangular jaws and well-spaced, fang-like teeth. It also has two spined dorsal fins, dermal denticles with faceted crowns, and numerous light-emitting photophores concentrated on its ventral surface.
The shortspine spurdog is a dogfish, a member of the family Squalidae, found on continental shelves off Japan in temperate waters, from the surface to 950 m. Its length is up to 75 cm.
Hybodontiformes, commonly called hybodonts, are an extinct group of shark-like cartilaginous fish (chondrichthyans) which existed from the late Devonian to the Late Cretaceous. Hybodonts share a close common ancestry with modern sharks and rays (Neoselachii) as part of the clade Euselachii. They are distinguished from other chondrichthyans by their distinctive fin spines and cephalic spines present on the heads of males. An ecologically diverse group, they were abundant in marine and freshwater environments during the late Paleozoic and early Mesozoic, but were rare in open marine environments by the end of the Jurassic, having been largely replaced by modern sharks, though they were still common in freshwater and marginal marine habitats. They survived until the end of the Cretaceous, before going extinct.
Meristodonoides is an extinct genus of hybodont. The type species is M. rajkovichi, which was originally a species in the genus Hybodus. The species, along with other Hybodus species such as H. butleri and H. montanensis, was reassigned to Meristodonoides by Charlie J. Underwood and Stephen L. Cumbaa in 2010. The species is primarily known from remains from the Cretaceous of North America, spanning from the Aptian/Albian to Maastrichtian, making it one of the last surviving hybodont genera, though records of the genus likely extend as far back as the Late Jurassic, based on an undescribed skeleton from the Tithonian of England, and fragmentary teeth from the Kimmeridgian of Poland, England and Switzerland. Other remains of the genus are known from the Coniacian of England, the Aptian-Albian of France, and the Campanian of European Russia. The morphology of the teeth suggests an adaptation to tearing prey. Fossils from the Western Interior Seaway suggest that it preferred nearshore marine environments, being absent from deeper-water areas, with it likely also being able to tolerate brackish and freshwater conditions.
Cretalamna is a genus of extinct otodontid shark that lived from the latest Early Cretaceous to Eocene epoch. It is considered by many to be the ancestor of the largest sharks to have ever lived, such as Otodus angustidens, Otodus chubutensis, and Otodus megalodon.
Sclerorhynchoidei is an extinct suborder of rajiform rays that had long rostra with large denticles similar to sawfishes and sawsharks. This feature was convergently evolved, recently proposed as 'pristification', and their closest living relatives are actually skates. While they are often called "sawfishes", sawskates is a more accurate common name proposed in 2021 for sclerorhynchoids, which has been subsequently used by other researchers.
Plicatoscyllium is an extinct genus of orectolobiform shark known from deposits of Late Cretaceous age in France, Jordan, the Netherlands, Syria and the United States. Remains tentatively referrable to the genus from Cenozoic deposits have been discovered in Saudi Arabia.
Paraisurus is an extinct genus of mackerel sharks that lived during the Cretaceous. It contains four valid species, which have been found in Europe, Asia, North America, and Australia. A fifth species, P. amudarjensis, is now considered a synonym of P. compressus. While this genus is mostly known from isolated teeth, an associated dentition of P. compressus was found in the Weno Formation of Texas. It went extinct around the Albian-Cenomanian boundary, as a supposed Coniacian occurrence of "P. sp." is likely a misidentified pseudoscapanorhynchid.
Xiphodolamia is a rare extinct genus of mackerel shark which lived during the Eocene epoch. It is only known from isolated teeth, but has been found in Europe, Africa, and Asia. It is assumed to be pelagic, occurring more frequently in deeper water deposits, most notably the London Clay and Eocene deposits in Denmark. It is distinguished by its rectangular root and twisted blade, unique among mackerel sharks. It is unclear what niche this specialized dentition helped exploit.
Angoumeius is an extinct genus of squaliform shark from the Eocene epoch of the Paleogene period. It is named for its type locality, Angoumé, France. It is known from a single species, A. paradoxus. It is known from many isolated teeth from the Lutetian stage. The inferred dentition is highly unusual for so its familial placement and relationship with other genera remains uncertain. It may be close to Kitefin or Sleeper sharks.
Galeocorax is an extinct genus of mackerel sharks that lived during the Late Cretaceous. It contains a single valid species, G. jaekeli, that has been found in Europe and North America.
Protocentrophorus is a genus of was a genus of dogfish shark that existed during the Cretaceous. Fossils have been found in the Tauragė County of Lithuania and British Columbia in Canada. Known from teeth, they were originally assigned to the genus Centrophorus.
{{cite journal}}
: Cite journal requires |journal=
(help)