Mastodonsaurus Temporal range: | |
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Skeleton of Mastodonsaurus giganteus in the Staatliches Museum für Naturkunde Stuttgart | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Order: | † Temnospondyli |
Suborder: | † Stereospondyli |
Clade: | † Capitosauria |
Family: | † Mastodonsauridae |
Genus: | † Mastodonsaurus Jaeger, 1828 |
Type species | |
†Mastodonsaurus jaegeriHoll, 1829 | |
Other species | |
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Synonyms | |
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Mastodonsaurus (meaning "teat tooth lizard") is an extinct genus of temnospondyl from the Middle Triassic of Europe. It belongs to a Triassic group of temnospondyls called Capitosauria, characterized by their large body size and presumably aquatic lifestyles. Mastodonsaurus remains one of the largest amphibians known, and may have exceeded 6 meters (20 feet) in length.
Like those of many other capitosaurs, the head of Mastodonsaurus was triangular, reaching about 1.5 metres (4.9 ft) in the largest specimens. [1] Narrow grooves on the surface of the skull bones called sulci show it had sensory organs that could detect vibrations and pressure under water, similar to the lateral lines on fish. The large, oval eye sockets are midway along the skull with the nostrils near the tip of the snout. Small ear holes (otic notches) are indented on either side of the back of the skull. The upper surface of the skull bones of Mastodonsaurus bore an intricate pattern of pits and ridges, a feature found in many temnospondyls. The function of this rugged ornamentation is not fully understood. As with other capitosaurs, Mastodonsaurus had a pineal foramen (opening) between the parietal bones behind the orbits on the roof of the skull, which would have contained a light-sensing parietal eye linked to the pineal gland to regulate the circadian sleep-wake cycle and hormone production related to body temperature for a cold-blooded (ectotherm) animal and to reproduction.
The sides of upper jaw are lined with a double row of small conical teeth, while the lower jaw has a single row of similar small teeth. The upper and lower arrangement of small, narrow teeth could function like a trap for small prey when Mastodonsaurus closed its mouth. The tip of the upper jaw has a set of larger teeth. Behind these teeth at the front end of the palate on the underside of the skull are sets of small teeth and multiple pairs of large fangs or tusks (about 8 in all). Two large tusks project up from the end of the lower jaw, fitting through openings on the palate and emerging out from the top of the skull in front of the nostrils when the jaw is closed. The tusk-like teeth on the palate and in the lower jaw could bite and hold bigger prey.
The exact number of vertebrae in the skeleton is still not known but recent research shows that Mastodonsaurus had about 28 trunk vertebrae and a relatively long tail, revised from the squat body shape and short tail assumed in earlier reconstructions. [2] [3] The total length of the largest individuals is about 4 to 6 metres (13 to 20 ft). [1] Isolated teeth up to 14 cm (6 in) long indicate that old individuals grew even larger.
The marked reduction of the limbs, the strong tail and sensory grooves on the head called sulci show that Mastodonsaurus was an aquatic animal that rarely, if ever, ventured on land. Mastodonsaurus may have been completely unable to leave the water, as large quantities of bones have been found that suggest individuals died en masse when pools dried up during times of drought. [4] It normally inhabited freshwater to brackish swamps, lakes, and river deltas. Fossil skull remains found in marine sediments suggest it also may have entered into saltier environments on occasion. [2] [5]
Its tail was likely thickened with a fleshy fin for propulsion. The stronger tail in combination with small limbs, a trunk section stiffened with long, broadened, overlapping ribs, and extra-heavy bones would indicate that Mastodonsaurus was an aquatic ambush predator that lurked on the bottom in wait for prey, making sudden, rapid attacks with its giant mouth and impaling tusks, propelled by its tail. [2] [6]
Mastodonsaurus fed mainly on fish, whose remains have been found in its fossilized coprolites. [4] The fossils of some smaller temnospondyls bear tooth marks made by Mastodonsaurus-like animals and there is evidence for cannibalism by adults on juveniles of Mastodonsaurus. It probably also ate land-living animals, such as small archosaurs that ventured into or along the edge of water. Bite marks on Mastodonsaurus bones show that the large terrestrial archosaur Batrachotomus actively preyed on the giant amphibians, entering the water or attacking individuals stranded in pools during droughts. [7]
Mastodonsaurus was once thought to be responsible for the footprints found in Triassic sandstones and described as Chirotherium , but later research found that the tracks belong to crocodile-like pseudosuchian reptiles like the aforementioned Batrachotomus or Ticinosuchus . [4] Based on the misattributed tracks and misidentified bones from other Triassic animals, early illustrations depicted the giant amphibians (often referred to as "Labyrinthodon" at the time) as big froglike creatures that supposedly crossed their legs as they walked since the outer fifth digit on the Chirotherium footprints resembled a thumb.
Most of the skeleton of Mastodonsaurus, apart from skulls and jaws, remained poorly known until recently. Both scientific and popular sources continued to describe Mastodonsaurus as having a squat, frog-like body and a short tail from the 19th century into the 20th century, including for the "Labyrinthodon" sculptures by Waterhouse Hawkins at the Crystal Palace outside London in 1854 and in a painting of Mastodonsaurus by the famous Czech paleoartist Zdeněk Burian in 1955. [8] [9] A life-size model put on display for the American Museum of Natural History Hall of Vertebrate Origins in 1996 also restored Mastodonsaurus with a short, broad body and a short tail, and so presumably able to crawl on land. [10]
A site discovered during road construction near the town of Kupferzell in southern Germany in 1977 provided researchers with important new fossils of Mastodonsaurus that included well preserved skulls and disarticulated bones from all parts of the body. Thousands of individual fossils were recovered during a three-month salvage operation before road work resumed, including, in addition to Mastodonsaurus, remains of the temnospondyl Gerrothorax and the archosaur Batrachotomus, as well as of many fishes. [11] Some of the bones showed evidence of being rolled and transported a long distance. Working from the rich Kupferzell finds, German paleontologist Rainer Schoch published a revised description of Mastodonsaurus in 1999 that revealed a longer body and an estimated longer tail, for a larger, more massive animal with a highly aquatic lifestyle. [1] Although no complete and fully articulated skeleton has been found to date, research since 1999 was incorporated into a composite skeletal reconstruction and a fleshed-out model displayed at the Staatliches Museum für Naturkunde Stuttgart in Germany that give Mastodonsaurus more crocodile-like proportions, with a lengthened tail for swimming, similar to some other capitosaurs. [3] [12] [2]
The growth stages of Mastodonsaurus are documented from numerous specimens found at Kupferzell, with skulls that range from 30 cm (12 in) up through 125 cm (50 in) long. Stereospondyls lacked a true larval stage of development and Mastodonsaurus followed a slow, conservative ontogenetic pattern with relatively minor changes as it grew so that small juveniles would have resembled adults. [6]
The German paleontologist Georg Friedrich von Jaeger gave the name Mastodonsaurus in 1828 to a single large conical fang with vertical striations and a worn off tip, found in the Triassic Lettenkeuper deposits near Gaildorf in Baden-Württemberg in southern Germany. [13] Jaeger assumed the big tooth (a snout fang about 10.4 cm (4.1 in) long as preserved) belonged to a giant reptile and that the indented missing tip was a distinctive natural feature that, when viewed from above, resembled a nipple or teat with a small hole in the middle, which he expressed in the name Mastodonsaurus or "teat tooth lizard" (from Greek mastos "breast, nipple" + odous (odon) "tooth" + sauros "lizard"): "Dieser Zahn ist nämlich besonders ausgezeichnet durch seine zitzenartige Spitze." [This tooth namely is especially distinguished by its teat-like tip.] He illustrated the tooth and its "teat-like" tip in a plate (Plate IV, figure 4). [14] [15] However, Jaeger did not provide a type species name for Mastodonsaurus.
Also in 1828, Jaeger identified part of the back of a large skull found in the same area as coming from an amphibian-like animal because of the double articulation of the occipital condyles. He gave the creature the genus-species name combination Salamandroides giganteus, meaning "gigantic salamander-like (animal)". The fossil was later identified as a specimen of Mastodonsaurus.
The name Mastodonsaurus has led to confusion over its intended meaning, and as pointed out by the British paleontologist Richard Owen, the name could be misinterpreted as a reference to the extinct proboscidean mastodon, supposedly to suggest gigantic size ("mastodon(-size) lizard"), the false meaning given in some sources. [16]
Owen noted that the teat-like appearance was not a real diagnostic feature and also objected to the term "saurus" for a "batrachian" (amphibian). He proposed what he thought was the more fitting replacement name Labyrinthodon or "labyrinth tooth" to refer to the complex maze-like appearance of the inner tooth structure when viewed in cross section. However, the rules of zoological nomenclature require that the earliest name established be used and Labyrinthodon is a junior synonym of Mastodonsaurus. The maze-like inner tooth structure in Mastodonsaurus is found in multiple types of extinct amphibians, and Richard Owen created the formal taxonomic category Labyrinthodontia (published in 1860) as a supposed order of "Reptilia" to unite them. However, the "order" turned out to contain multiple types of animals that not are not closely related and the category Labyrinthodontia no longer has recognized scientific status, although the general form "labyrinthodont" is still used as a descriptive term. [17]
After a complex nomenclatural history and recognition that the original Mastodonsaurus tooth and the Salamandroides giganteus skull section were from different individuals of the same kind of animal, most authors used the binomial combination Mastodonsaurus giganteus. A reexamination of the genus by Markus Moser and Rainer Schoch in 2007 restored M. jaegeri Holl from 1829 as the historically oldest type species for Mastodonsaurus, designating Jaeger's original tooth (SMNS 55911) as the lectotype of Mastodonsaurus jaegeri. A large number of species have been attributed to the genus over the years, but they determined only three of the species are valid: the type species M. jaegeri, the best known species, M. giganteus (which could be a senior synonym of M. jaegeri if the two species are not taxonomically distinct), both from Europe, and M. torvus from Russia. The species M. acuminatus was shown to be a junior synonym to M. giganteus, while the species M. tantus & M. maximus were both determined to be synonyms of M. torvus. [15]
The species M. andriani, M. indicus, M. laniarius, M. lavisi, M. meyeri, M. pachygnathus and M. silesiacus, when reexamined by Moser and Schoch, were not deemed assignable to the genus Mastodonsaurus due to the fragmentary nature of the type specimens and as such are considered nomen dubium . [15] Examination of the literature showed M. conicus to be a senior synonym of the genus M. ventricosus; however this species was never formally published and is thus considered a nomen nudum . [15]
In 1923, German paleontologist Emil Wepfer described the new species Mastodonsaurus cappelensis for fossils found near the town of Kappel in Baden-Württemberg in an older formation than remains of Mastodonsaurus giganteus. [18] Swedish paleontologist Gunnar Säve-Söderbergh erected the new genus Heptasaurus ("seven lizard" for seven skull openings) for the species in 1935. [19] In his review of Mastodonsaurus, Rainer Schoch (1999) recognized Heptasaurus as a genus that was distinct from Mastodonsaurus, with "smaller orbits and a markedly broader snout tip", and that was found in the Middle and Upper Buntsandstein Formation, earlier than fossils of Mastodonsaurus giganteus. [1]
This analysis was questioned by Damiani (2001), who used the original name Mastodonsaurus cappelensis for the species. [20] Moser and Schoch (2007) continued to accept the valid status of the genus Heptasaurus but noted that the species "could also be re-referred to Mastodonsaurus". [15] Rayfield, Barrett & Milner (2009) pointed out that the skull and size differences between Heptasaurus and Mastodonsaurus may not be important diagnostic features at a generic level. [21]
In more recent research, Schoch has restored the combination Mastodonsaurus cappelensis for the geologically older species, noting in 2008 that "present evidence indicates close ties with Mastodonsaurus giganteus, which is why this species is here referred to Mastodonsaurus". [22] [23] A revised description of Mastodonsaurus cappelensis by Schoch and others in 2023 indicated that the earlier species was 3 meters long and differed from M. giganteus in having a wider snout and differently shaped orbits, as well as a longer and more gracile humerus. The Mastodonsaurus lineage evolved larger tusks and stronger jaws over time to deal with more types of prey, becoming a dominant predator in lake-related ecosystems. [24]
The species Mastodonsaurus torvus was described in 1955 by Russian paleontologist Elena Dometevna Konzhukova (wife of paleontologist Ivan Yefremov) based on a lower jaw fragment (holotype PIN 415/1) and other bones unearthed near the village of Koltaevo in Bashkortostan in the Southern Urals in Middle Triassic beds that are part of the Bukobay Svita in Russia. [25] Additional fossils of very large mastodonsaurids have been discovered as well at Middle Triassic sites in the Orenburg Oblast in Russia and in northern Kazakhstan. In 1972, Russian paleontologist Leonid Petrovich Tatarinov found a complete skull (measuring 1.25 meters long) on an expedition to Koltaevo. The giant skull is on display at the Orlov Paleontological Museum (specimen PIN 2867/67) in Moscow in Russia and has been labeled Mastodonsaurus torvus, although some sources cite the specimen as Mastodonsaurus sp. instead. [26] [27] [28] [29] A full scientific description has not been published yet, but differences from Mastodonsaurus giganteus include smaller orbits positioned further back on the skull.
Researchers debate the generic classification of the Russian fossils, sometimes referring to them as "Mastodonsaurus" in quotes or with a question mark (?) to indicate that further study may justify a separate giant mastodonsaurid genus. [30] [21]
Temnospondyli or temnospondyls is a diverse ancient order of small to giant tetrapods—often considered primitive amphibians—that flourished worldwide during the Carboniferous, Permian and Triassic periods, with fossils being found on every continent. A few species continued into the Jurassic and Early Cretaceous periods, but all had gone extinct by the Late Cretaceous. During about 210 million years of evolutionary history, they adapted to a wide range of habitats, including freshwater, terrestrial, and even coastal marine environments. Their life history is well understood, with fossils known from the larval stage, metamorphosis and maturity. Most temnospondyls were semiaquatic, although some were almost fully terrestrial, returning to the water only to breed. These temnospondyls were some of the first vertebrates fully adapted to life on land. Although temnospondyls are amphibians, many had characteristics such as scales and large armour-like bony plates (osteoderms) that generally distinguish them from the modern soft-bodied lissamphibians.
Gerrothorax is an extinct genus of temnospondyl amphibian from the Triassic period of Greenland, Germany, Poland, Sweden, and possibly Thailand. It is known from a single species, G. pulcherrimus, although several other species such as G. pustuloglomeratus have been named in the past.
Batrachotomus is a genus of prehistoric archosaur. Fossils of this animal have been found in southern Germany and dated from the Ladinian stage of the Middle Triassic period, around 242 to 237 million years ago. Batrachotomus was described by palaeontologist David J. Gower 22 years after its discovery.
Cyclotosaurus is an extinct genus of temnospondyl within the family Mastodonsauridae. It was of great size for an amphibian, had an elongated skull up to 56 cm (22 in).
Uranocentrodon is an extinct genus of temnospondyls in the family Rhinesuchidae. Known from a 50 centimetres (20 in) skull, Uranocentrodon was a large predator with a length up to 3.75 metres (12.3 ft). Originally named Myriodon by van Hoepen in 1911, it was transferred to a new genus on account of the name being preoccupied in 1917. It has been synonymized with Rhinesuchus, but this has not been widely supported. It was also originally considered to be of Triassic age, but more recent analysis has placed its age as just below the Permian-Triassic boundary.
Sclerocephalus is an extinct genus of temnospondyl amphibian from the lowermost Permian of Germany and Czech Republic with four valid species, including the type species S. haeuseri. It is one of the most completely preserved and most abundant Palaeozoic tetrapods. Sclerocephalus was once thought to be closely related to eryopoid temnospondyls, but it is now thought to be more closely related to archegosauroids. It is the only genus in the family Sclerocephalidae.
Eocyclotosaurus is an extinct genus of mastodonsauroid temnospondyl from the Middle Triassic (Anisian). The name Eocyclotosaurus means "dawn round-eared lizard". It is characterized as a capitosauroid with a long and slender snout, closed otic fenestra, and small orbits. It measured over one metre and had a 22 cm skull.
Konzhukovia is an amphibian genus that belongs to an extinct family Konzhukoviidae of temnospondyls, the largest clade of basal tetrapods including about 198 genera, 292 species, and more than half of which were alive during the early Mesozoic period. The animal was a predator that lived about 260 million years ago, and could get up to about three meters in length. Specifically, Konzukovia lived during the Permian, between 252 and 270 million years ago according to the type of rock the fossil was found in. There are three species within this genus, K. vetusta, K. tarda, and K. sangabrielensis, the first two originating from Russia while the latest originating from Southern Brazil. The discovery of this specimen in Southern Brazil provided more evidence to support the idea that during this animals existence, there was a “biological corridor” because of the supercontinent Pangea, allowing these species to be found so far apart from each other. Konzhukovia belongs to the family Archegosauridae, a family consisted of large temnospondyls that most likely compare to modern day crocodiles. Since the discovery of the latest species, K. sangabrielensis, Pacheco proposes that there must be the creation of a new family, Konzhokoviidae, a monophyletic group in a sister-group relationship with Stereospondlyi in order to accommodate the three species. Konzhukovia skulls usually exhibit typical rhinesuchid features including an overall parabolic shape, small orbits located more posteriorly, and the pterygoids do not reach the vomer. These animals were long-snouted amphibians that had clear adaptations made for fish catching, as well as exemplifying aquatic features.
Mastodonsauridae is a family of capitosauroid temnospondyls. Fossils belonging to this family have been found in North America, Greenland, Europe, Asia, and Australia. The family Capitosauridae is synonymous with Mastodonsauridae.
The Mastodonsauroidea are an extinct superfamily of temnospondyl amphibians known from the Triassic. Fossils belonging to this superfamily have been found in North America, Greenland, Europe, Asia, and Australia. Ferganobatrachus from the Jurassic of Asia was initially assigned to this superfamily, but is now considered to be congeneric with the brachyopid Gobiops.
Bukobaja is an extinct genus of mastodonsaurid temnospondyl from the middle Triassic of Russia. It contains a single species, Bukobaja enigmatica. Bukobaja mainly occurs in the Bukobay Svita as part of the Ladinian?-age "Mastodonsaurus fauna", a section of Russian Triassic biostratigraphy characterized by "Mastodonsaurus" torvus. It was also present in the underlying Donguz Svita. Bukobaja appears to be a valid genus similar to, yet distinct from, Mastodonsaurus. Despite appearing to possess several unique features, Bukobaja is still known from very few remains. This has led to difficulties in determining its relations more precisely than "Mastodonsauridae incertae sedis". It has also been compared to trematosaurids.
Cryobatrachus is an extinct genus of temnospondyl amphibian from the Early Triassic of Antarctica. The type species is Cryobatrachus kitchingi. It is known from a partial skull and an imprint of the skull roof, both found in the Fremouw Formation of the Transantarctic Mountains at about 85° south latitude and described in 1974. Many small bone fragments have also been identified, although they cannot be attributed with certainty to C. kitchingi. Cryobatrachus has been classified in the family Lydekkerinidae, as it is similar in appearance to the genus Lydekkerina from South Africa.[a] Because only a small number of features distinguish it from other lydekkerinids, Cryobatrachus kitchingi has more recently been considered a nomen dubium, meaning that its distinction from other better-known species may be unwarranted.
Xenotosuchus is an extinct genus of mastodonsaurid temnospondyl within the family Mastodonsauridae known from the Triassic of South Africa. The genus is based on a skull originally described as Parotosuchus, an animal which it resembled in general build and habit.
Micropholis is an extinct genus of dissorophoid temnospondyl. Fossils have been found from the Lystrosaurus Assemblage Zone of the Karoo Basin in South Africa and are dated to the Induan. Fossils have also been found from the lower Fremouw of Antarctica.Micropholis is the only post-Permian dissorophoid and the only dissorophoid in what is presently the southern hemisphere and what would have been termed Gondwana during the amalgamation of Pangea.
Teraterpeton is an extinct genus of trilophosaurid archosauromorphs. It is known from a partial skeleton from the Late Triassic Wolfville Formation of Nova Scotia, described in 2003. It has many unique features seen in no other related form, including an elongated, toothless snout and large openings for the nostrils. Because of this, Teraterpeton was originally placed in its own family, Teraterpetidae, related to Trilophosaurus. Newer studies generally place it within Trilophosauridae.
Heptasaurus is an extinct genus of Triassic capitosaurian temnospondyl within the family Mastodonsauridae.
The Erfurt Formation, also known as the Lower Keuper, is a stratigraphic formation of the Keuper group and the Germanic Trias supergroup. It was deposited during the Ladinian stage of the Triassic period. It lies above the Upper Muschelkalk and below the Middle Keuper.
Jaxtasuchus is an extinct genus of armored doswelliid archosauriform reptile known from the Middle Triassic of the Erfurt Formation in Germany. The type species, Jaxtasuchus salomoni, was named in 2013 on the basis of several incomplete skeletons and other isolated remains. Like other doswelliids, members of the genus were heavily armored, with four longitudinal rows of bony plates called osteoderms covering the body. Jaxtasuchus is the first doswelliid known from Europe and is most closely related to Doswellia from the Late Triassic of the eastern United States. However, it was not as specialized as Doswellia, retaining several generalized archosauriform characteristics and having less armor. Jaxtasuchus fossils have been found in aquatic mudstones alongside fossils of temnospondyl amphibians, crustaceans, and mollusks, suggesting that Jaxtasuchus was semiaquatic like modern crocodilians.
Scapanops is an extinct genus of dissorophid temnospondyl amphibian known from the Early Permian Nocona Formation of north-central Texas, United States. It contains only the type species Scapanops neglecta, which was named by Rainer R. Schoch and Hans-Dieter Sues in 2013. Scapanops differs from other dissorophids in having a very small skull table, which means that its eye sockets are unusually close to the back of the skull. The eye sockets are also very large and spaced far apart. Scapanops was probably small-bodied with a proportionally large head and short trunk and tail. Like other dissorophids, it probably spent most of its life on land.
Manubrantlia was a genus of lapillopsid temnospondyls from the Early Triassic Panchet Formation of India. This genus is only known from a single holotype left jaw, given the designation ISI A 57. Despite the paucity of remains, the jaw is still identifiable as belonging to a relative of Lapillopsis. For example, all three of its coronoid bones possessed teeth, the articular bone is partially visible in lateral (outer) view, and its postsplenial does not contact the posterior meckelian foramen. However, the jaw also possesses certain unique features which justify the erection of a new genus separate from Lapillopsis. For example, the mandible is twice the size of any jaws referred to other lapillopsids. The most notable unique feature is an enlarged "pump-handle" shaped arcadian process at the back of the jaw. This structure is responsible for the generic name of this genus, as "Manubrantlia" translates from Latin to the English expression "pump-handle". The type and only known species of this genus is Manubrantlia khaki. The specific name refers to the greenish-brown mudstones of the Panchet Formation, with a color that had been described as "khaki" by the first British geologists who studied the formation.