Seymouria

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Seymouria
Temporal range: Early Permian
Seymouria1.jpg
A fossil of Seymouria baylorensis displayed at the National Museum of Natural History
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Order:† Seymouriamorpha
Family:† Seymouriidae
Genus:† Seymouria
Broili, 1904
Species
  • †S. baylorensis Broili, 1904 (type)
  • †S. sanjuanensis Vaughn, 1966
  • †S. grandis Olson, 1979
Synonyms
  • Conodectes favosus Cope, 1896
  • Desmospondylus anomalus Williston, 1910

Seymouria is an extinct genus of seymouriamorph from the Early Permian of North America and Europe. [1] Although they were amphibians (in a biological sense), Seymouria were well-adapted to life on land, with many reptilian features—so many, in fact, that Seymouria was first thought to be a primitive reptile. [2] [3] It is primarily known from two species, Seymouria baylorensis [4] and Seymouria sanjuanensis. [5] The type species, S. baylorensis, is more robust and specialized, though its fossils have only been found in Texas. [6] On the other hand, Seymouria sanjuanensis is more abundant and widespread. This smaller species is known from multiple well-preserved fossils, including a block of six skeletons found in the Cutler Formation of New Mexico, [7] and a pair of fully grown skeletons from the Tambach Formation of Germany, which were fossilized lying next to each other. [8]

For the first half of the 20th century, Seymouria was considered one of the oldest and most "primitive" known reptiles. [2] [3] Paleontologists noted how the general body shape resembled that of early reptiles such as captorhinids, and that certain adaptations of the limbs, hip, and skull were also similar to that of early reptiles, rather than any species of modern or extinct amphibians known at the time. The strongly-built limbs and backbone also supported the idea that Seymouria was primarily terrestrial, spending very little time in the water. [9] However, in the 1950s, fossilized tadpoles were discovered in Discosauriscus , which was a close relative of Seymouria in the group Seymouriamorpha. This shows that seymouriamorphs (including Seymouria) had a larval stage which lived in the water, therefore making Seymouria not a true reptile, but rather an amphibian which was closely related to reptiles. [10] Though no longer considered the most primitive reptile, Seymouria is still an important transitional fossil documenting the acquisition of reptile-like skeletal features prior to the evolution of the amniotic egg, which characterizes amniotes (reptiles, mammals, and birds). [1]

History

Early history as a putative reptile

Outdated depiction of Seymouria as a primitive egg-laying terrestrial reptile, from a series of paintings by F.L. Jaques illustrating the "progressive" stages of evolution from fish to man for the American Museum of Natural History in the 1930s The dinosaur book - the ruling reptiles and their relatives (1945) (20768758508).jpg
Outdated depiction of Seymouria as a primitive egg-laying terrestrial reptile, from a series of paintings by F.L. Jaques illustrating the "progressive" stages of evolution from fish to man for the American Museum of Natural History in the 1930s

Fossils of Seymouria were first found near the town of Seymour, in Baylor County, Texas (hence the name of the type species, Seymouria baylorensis, referring to both the town and county). The earliest fossils of the species to be collected were a cluster of individuals acquired by C.H. Sternberg in 1882. However, these fossils would not be properly prepared and identified as Seymouria until 1930. [12]

Various paleontologists from around the world recovered their own Seymouria baylorensis fossils in the late 19th century and early 20th century. Seymouria was formally named and described in 1904 based on a pair of incomplete skulls, one of which was associated with a few pectoral and vertebral elements. These fossils were described by German paleontologist Ferdinand Broili, and are now stored in Munich. [4] American paleontologist S.W. Williston later described a nearly complete skeleton in 1911, and noted that "Desmospondylus anomalus", a taxon he had recently named from fragmentary limbs and vertebrae, likely represented juvenile or even embryonic individuals of Seymouria. [2]

Likewise, English paleontologist D.M.S. Watson noted in 1918 that Conodectes, a dubious genera named by Edward Drinker Cope back in 1896, was likely synonymous with Seymouria. [3] Robert Broom (1922) argued that the genus should be referred to as Conodectes since that name was published first, [13] but Alfred Romer (1928) objected, noting that the name Seymouria was too popular within the scientific community to be replaced. [9] During this time, Seymouria was generally seen as a very early reptile, part of an evolutionary grade known as "cotylosaurs", which also included many other stout-bodied Permian reptiles or reptile-like tetrapods.

Proposed amphibian affinities

Many paleontologists were uncertain about Seymouria's allegiance with the reptiles, noting many similarities with the embolomeres, which were unquestionably "labyrinthodont" amphibians. This combination of features from reptiles (i.e. other "cotylosaurs") and amphibians (i.e. embolomeres) was evidence that Seymouria was central to the evolutionary transition between the two groups. Regardless, not enough was known about its biology to conclude which group it was truly part of. Broom (1922) [13] and Russian paleontologist Peter Sushkin (1925) [14] supported a placement among the Amphibia, but most studies around this time tentatively considered it an extremely "primitive" reptile; these included a comprehensive redescription of material referred to the species, published by Theodore E. White in 1939. [12]

However, indirect evidence that Seymouria was not biologically reptilian started to emerge by the 1940s. Around this time, several newly described genera were linked to Seymouria as part of the group Seymouriamorpha. Some seymouriamorphs, such as Kotlassia , had evidence of aquatic habits, and even Seymouria itself had occasionally been argued to possess lateral lines, sensory structures only usable underwater. [12] Watson (1942) [15] and Romer (1947) [16] each reversed their stance on Seymouria's classification, placing it among the amphibians rather than the reptiles. Perhaps the most damning evidence came in 1952, when Czech paleontologist Zdeněk Špinar reported gills preserved in juvenile fossils of the seymouriamorph Discosauriscus . This unequivocally proved that seymouriamorphs had an aquatic larval stage, and thus were amphibians, biologically speaking. [10] Nevertheless, the numerous similarities between Seymouria and reptiles supported the idea that seymouriamorphs were close to the ancestry of amniotes.

Additional species and fossils

A replica of the Cutler Formation block containing six Seymouria sanjuanensis skeletons, described by Berman, Reisz, & Eberth (1987) Seymouria in Canada.jpg
A replica of the Cutler Formation block containing six Seymouria sanjuanensis skeletons, described by Berman, Reisz, & Eberth (1987)

In 1966, Peter Paul Vaughn described an assortment of Seymouria skulls from the Organ Rock Shale of Utah. These remains represented a new species, Seymouria sanjuanensis. [5] Fossils of this species are now understood to be more abundant and widespread than those of Seymouria baylorensis. Several more species were later named by Paul E. Olson, although their validity has been more questionable than that of S. sanjuanensis. For example, Seymouria agilis (Olson, 1980), known from a nearly complete skeleton from the Chickasha Formation of Oklahoma, was reassigned by Michel Laurin and Robert R. Reisz to the parareptile Macroleter in 2001. [17] Seymouria grandis, described a year earlier from a braincase found in Texas, has not been re-referred to any other tetrapod, but it remains poorly known. Langston (1963) reported a femur indistinguishable from that of S. baylorensis in Permian sediments at Prince Edward Island on the Eastern coast of Canada. [18] Seymouria-like skeletal remains are also known from the Richards Spur Quarry in Oklahoma, as first described by Sullivan & Reisz (1999). [19]

A cast of the "Tambach lovers" Seymouria sanjuanensis specimen first described by Berman et al. (2000) Seymouria Tambach Lovers.jpg
A cast of the "Tambach lovers" Seymouria sanjuanensis specimen first described by Berman et al. (2000)

A block of sediment containing six S. sanjuanensis skeletons was found in the Cutler Formation of New Mexico, as described by Berman, Reisz, & Eberth (1987). [7] In 1993, Berman & Martens reported the first Seymouria remains outside of North America, when they described S. sanjuanensis fossils from the Tambach Formation of Germany. [18] The Tambach Formation has produced S. sanjuanensis fossils of a similar quality to those of the Cutler Formation. For example, in 2000 Berman and his colleagues described the "Tambach Lovers", two complete and fully articulated skeletons of S. sanjuanensis fossilized lying next to each other (though it cannot be determined whether they were a couple killed during courtship). [8] The Tambach Formation has also produced the developmentally youngest known fossils of Seymouria, assisting comparisons to Discosauriscus, which is known primarily from juveniles. [20]

Description

Life restoration and size comparison of Seymouria baylorensis Seymouria NT small.jpg
Life restoration and size comparison of Seymouria baylorensis

Seymouria individuals were robustly-built animals, with a large head, short neck, stocky limbs, and broad feet. [2] [16] Even the largest specimens were fairly small, only about 2 ft (60 cm) long. The skull was boxy and roughly triangular when seen from above, but it was lower and longer than that of most other seymouriamorphs. The vertebrae had broad, swollen neural arches (the portion above the spinal cord). As a whole the body shape was similar to that of contemporary reptiles and reptile-like tetrapods such as captorhinids, diadectomorphs, and parareptiles. Collectively these types of animals have been referred to as "cotylosaurs" in the past, although they do not form a clade (a natural, relations-based grouping).

Skull

Diagrams of skulls from S. baylorensis and S. sanjuanensis. Seymouria skull diagrams.png
Diagrams of skulls from S. baylorensis and S. sanjuanensis.

The skull was composed of many smaller plate-like bones. The configuration of skull bones present in Seymouria was very similar to that of far more ancient tetrapods and tetrapod relatives. For example, it retains an intertemporal bone, which is the plesiomorphic ("primitive") condition present in animals like Ventastega and embolomeres. [16] The skull bones were heavily textured, as was typical for ancient amphibians and captorhinid reptiles. In addition, the rear part of the skull had a large incision stretching along its side. This incision is termed an otic notch, and a similar incision in the same general area is common to most Paleozoic amphibians ("labyrinthodonts", as they are sometimes called), but unknown in amniotes. The lower edge of the otic notch was formed by the squamosal bone, while the upper edge was formed by downturned flanges of the supratemporal and tabular bones (known as otic flanges). The tabular also has a second downturned flange visible from the rear of the skull; this flange (known as an occipital flange) connected to the braincase and partially obscured the space between the braincase and the side of the skull. The development of the otic and occipital flanges is greater in Seymouria (particularly S. baylorensis) than in any other seymouriamorph. [6]

The sensory apparatus of the skull also deserves mention for an array of unique features. The orbits (eye sockets) were about midway down the length of the skull, although they were a bit closer to the snout in juveniles. They were more rhomboidal than the circular orbits of other seymouriamorphs, with an acute front edge. [12] Several authors have noted that a few specimens of Seymouria possessed indistinct grooves present in bones surrounding the orbits and in front of the otic notch. These grooves were likely remnants of a lateral line system, a web of pressure-sensing organs useful for aquatic animals, including the presumed larval stage of Seymouria. [12] [16] [5] Many specimens do not retain any remnant of their lateral lines, [7] [6] not even juveniles. [20] Near the middle of the parietal bones was a small hole known as a pineal foramen, which held a sensory organ known as a parietal eye. The pineal foramen is smaller in Seymouria than in other seymouriamorphs. [8]

The stapes, a rod-like bone which lies between the braincase and the wall of the skull, was tapered. It connected the braincase to the upper edge of the otic notch, and likely served as a conduit of vibrations received by a tympanum (eardrum) which presumably lay within the otic notch. In this way it could transmit sound from the outside world to the brain. The configuration of the stapes is intermediate between non-amniote tetrapods and amniotes. On the one hand, its connection to the otic notch is unusual, since true reptiles and other amniotes have lost an otic notch, forcing the tympanum and stapes to shift downwards towards the quadrate bone of the jaw joint. On the other hand, the thin, sensitive structure of Seymouria's stapes is a specialization over most non-amniote tetrapods, which have a thick stapes better suited for reinforcing the skull rather than hearing. [9] The inner ear of Seymouria baylorensis retains a cochlear recess located behind (rather than below) the vestibule, and its anterior semicircular canal was likely encompassed by a cartilaginous (rather than bony) supraoccipital. These features are more primitive than those of true reptiles and synapsids. [21]

The palate (roof of the mouth) had some similarities with both amniote and non-amniote tetrapods. On the one hand, it retained a few isolated large fangs with maze-like internal enamel folding, as is characteristic for "labyrinthodont" amphibians. On the other hand, the vomer bones at the front of the mouth were fairly narrow, and the adjacent choanae (holes leading from the nasal cavity to the mouth) were large and close together, as in amniotes. The palate is generally solid bone, with only vestigial interpteryoid vacuities (a pair of holes adjacent to the midline) separated by a long and thin cultriform process (the front blade of the base of the braincase). Apart from the fangs, the palate is also covered with small denticles radiating out from the rear part of the pterygoid bones. [22] Seymouria has a few amniote-like characteristics of the palate, such as the presence of a prong-like outer rear branch of the pterygoid (formally known as a transverse flange) as well as an epipterygoid bone which is separate from the pterygoid. However, these characteristics have been observed in various non-amniote tetrapods, so they do not signify its status as an amniote. [6]

The lower jaw retained a few plesiomorphic characteristics. For example, the inner edge of the mandible possessed three coronoid bones. [12] The mandible also retained at least one large hole along its inner edge known as a meckelian fenestra, although this feature was only confirmed during a 2005 re-investigation of one of the Cutler Formation specimens. [22] Neither of these traits are the standard in amniotes. The braincase had a mosaic of features in common with various tetrapodomorphs. The system of grooves and nerve openings on the side of the braincase were unusually similar to those of the fish Megalichthys, and the cartilaginous base is another plesiomorphic feature. However, the internal carotid arteries perforate the braincase near the rear of the bone complex, a derived feature similar to amniotes. [12]

Postcranial skeleton

A skeletal illustration of Williston (1911)'s Seymouria baylorensis specimen. Note that the fourth finger of the hand is too long and too many caudal ribs are illustrated. Primitive Cotylosaur Seymouria. Wellcome M0006645.jpg
A skeletal illustration of Williston (1911)'s Seymouria baylorensis specimen. Note that the fourth finger of the hand is too long and too many caudal ribs are illustrated.

The vertebral column is fairly short, with a total of 24 vertebrae between the hip and skull. [8] The vertebrae are gastrocentrous, meaning that each vertebra has a larger, somewhat spool-shaped component known as a pleurocentrum, and a smaller, wedge-shaped (or crescent-shaped from the front) component known as an intercentrum. The neural arches, which lie above the pleurocentra, are swollen into broad structures with table-like zygapophyses (joint plates) about three times as wide as the pleurocentrum itself. Some vertebrae have neural spines which are partially subdivided down the middle, while others are oval-shaped in horizontal cross-section. The ribs of the dorsal vertebrae extend horizontally and attach to the vertebrae at two places: the intercentrum and the side of the neural arch. [12] The neck is practically absent, only a few vertebrae long. The first neck vertebra, the atlas, had a small intercentrum as well as a reduced pleurocentrum which was only present in mature individuals. Although the atlantal pleurocentrum (when present) was wedged between the intercentrum of the atlas and intercentrum of the succeeding axis vertebra (as in amniotes), the low bone development in this area of the neck contrasts with the characteristic atlas-axis complex of amniotes. [23] In addition, later studies found that the atlas intercentrum was divided into a left and right portion, more like that of amphibian-grade tetrapods. [7] Unlike almost all other Paleozoic tetrapods (amniote or otherwise), Seymouria completely lacks any bony remnants of scales or scutes, not even the thin, circular belly scales of other seymouriamorphs. [6] [8]

The pectoral (shoulder) girdle has several reptile-like features. For example, the scapula and coracoid (bony plates which lie above and below the shoulder socket, respectively) are separate bones, rather than one large shoulder blade. Likewise, the interclavicle was flat and mushroom-shaped, with a long and thin "stem". The humerus (forearm bone) was shaped like a boxy and slightly twisted L, with large areas for muscle attachment. This form, which has been described as "tetrahedral", is plesiomorphic for tetrapods and contrasts with the slender hourglass-shaped humerus of amniotes. On the other hand, the lower part of the humerus also has a reptile-like adaptation: a hole known as an entepicondylar foramen. The radius was narrowest at mid-length. The ulna is similar, but longer due to the possession of a pronounced olecranon process, as is common in terrestrial tetrapods but rare in amphibious or aquatic ones. The carpus (wrist) has ten bones, and the hand has five stout fingers. The carpal bones are fully developed and closely contact each other, another indication of terrestriality. The phalanges (finger bones) decrease in size towards the tip of the fingers, where they each end in a tiny, rounded segment, without a claw. The phalangeal formula (number of phalanges per finger, from thumb to little finger) is 2-3-4-4-3. [8]

Two sacral (hip) vertebrae were present, though only the first one possessed a large, robust rib which contacted the ilium (upper blade of the hip). [12] [8] Some studies have argued that there was only one sacral vertebra, with the supposed second sacral actually being the first caudal due to having a shorter, more curved rib than the first sacral. [7] Each ilium is low and teardrop-shaped when seen from the side, while the underside of the hip as a whole is formed by a single robust puboischiadic plate, which is rectangular when seen from below. Both the hip and shoulder sockets were directed at 45 degrees below the horizontal. The femur is equally stout as the humerus, and the tibia and fibula are robust, hourglass-shaped bones similar to the radius and ulna. [12] The tarsus (ankle) incorporates 11 bones, intermediate between earlier tetrapods (which have 12) and amniotes (which have 8 or fewer). The five-toed feet are quite similar to the hands, with phalangeal formula 2-3-4-5-3. [8]

There were only about 20 caudal (tail) vertebrae at most. Past the base of the tail, the caudals start to acquire bony spines along their underside, known as chevrons. These begin to appear in the vicinity of the third to sixth caudal, depending on the specimen. Ribs are only present within the first five or six caudals; they are long at the base of the tail but diminish soon afterwards and typically disappear around the same area the chevrons appear. [8]

Differences between species

Seymouria baylorensis and Seymouria sanjuanensis can be distinguished from each other based on several differences in the shape and connections between the different bones of the skull. For example, the downturned flange of bone above the otic notch (sometimes termed the "tabular horn" or "otic process") is much more well-developed in S. baylorensis than in S. sanjuanensis. In the former species, it acquires a triangular shape (when seen from the side) as it extends downwards more extensively towards the rear of the skull. [8] In S. sanjuanensis, the postfrontal bone contacts the parietal bone by means of an obtuse, wedge-like suture, while the connection between the two bones is completely straight in S. baylorensis.

Life restoration of two Seymouria sanjuanensis individuals, based on the "Tambach lovers" Bromacker2 copy.jpg
Life restoration of two Seymouria sanjuanensis individuals, based on the "Tambach lovers"

Some authors have argued that the postparietals of S. baylorensis were smaller than those of S. sanjuanensis, but some specimens of S. sanjuanensis (for example, the "Tambach lovers") also had small postparietals. In addition, the "Tambach lovers" have a quadratojugal bone which is more similar to that of S. baylorensis rather than S. sanjuanensis. The combination of features from both species in these specimens may indicate that the two species are part of a continuous lineage, rather than two divergent evolutionary paths. Likewise, some differences relating to the proportions of the rear of the skull may be considered to be an artifact of the fact that most S. sanjuanensis specimens were not fully grown prior to the discovery of the "Tambach lovers", which were adult members of the species. [8]

Nevertheless, several traits are still clearly differentiated between the two species. The lacrimal bone, in front of the eyes, only occupies the front edge of the orbit in S. baylorensis. Conversely, specimens of S. sanjuanensis have a branch of the lacrimal which extends a small distance under the orbit. In S. sanjuanensis, much of the rear edge of the orbit is formed by the chevron-shaped postorbital bone, which is more rectangular in S. baylorensis. The shape of the lacrimal and postorbital of S. sanjuanensis closely corresponds to the condition in other seymouriamorphs, while the condition in S. baylorensis is more unique and derived. [8]

The tooth-bearing maxilla bone, which forms the side of the snout, is also distinctively unique in S. baylorensis. In S. sanjuanensis, the maxilla was low, with many sharp, closely spaced teeth extending along its length. This condition is similar to other seymouriamorphs. However, S. baylorensis has a taller snout, and its teeth are generally much larger, less numerous, and less homogenous in size. [8] The palate is generally similar between the two species, although the ectopterygoids are more triangular in S. baylorensis and rectangular in S. sanjuanensis. [22]

Paleobiology

Lifestyle

A Seymouria model at the Milwaukee Public Museum Milwaukee Public Museum May 2023 07 (Third Planet--Seymouria).jpg
A Seymouria model at the Milwaukee Public Museum

Romer (1928) was among the first authors to discuss the biological implications of Seymouria's skeleton. He argued that the robust limbs and wide-set body supported the idea that it was a strong, terrestrial animal with a sprawling gait. However, he also noted that Permian trackways generally support the idea that terrestrial tetrapods from this time period were not belly-draggers, but instead were strong enough to keep their bodies off of the ground. As with other paleontologists around the time, Romer assumed that Seymouria had a reptilian (or amniote) mode of reproduction, with eggs laid on dry land and protected from the elements by an amnion membrane. [9]

White (1939) elaborated on biological implications. He noted that the presence of an otic notch reduces jaw strength by lowering the amount of surface area jaw muscles can attach to within the cranium. In addition, the skull would have been more fragile due to the presence of such a large incision. As a whole, he found it unlikely that Seymouria was capable of tackling large, active prey. Nevertheless, the sites for muscle attachment on the palate were more well-developed than those of contemporaneous amphibians. White extrapolated that Seymouria was a mostly carnivorous generalist and omnivore, feeding on invertebrates, small fish, and perhaps even some plant material. It may have even been cannibalistic according to his reckoning. [12]

White also drew attention to the unusual swollen vertebrae, which would have facilitated lateral (side-to-side) movement but prohibit any torsion (twisting) of the backbone. This would have been beneficial, since Seymouria had low-slung limbs and a wide, top-heavy body that would have otherwise been vulnerable to torsion when it was walking. This may also explain the presence of this trait in captorhinids, diadectomorphs, and other "cotylosaurs". Perhaps swollen vertebrae were an interim strategy to prevent torsion, which would later be supplanted by strong hip muscles in later reptiles. The rather undeveloped hip muscles of Seymouria are in line with this hypothesis. Nevertheless, these vertebrae were inefficient at defending against torsion at any speed faster than a brisk walk, so Seymouria was probably not a quick-moving animal. [12]

Although White considered Seymoria to be quite competent on land, he also discussed a few other lifestyles. He supposed that Seymouria was also a good swimmer, since he (erroneously) estimated that the animal had a deep and powerful tail similar to that of modern crocodilians. However, he also noted that it would have been vulnerable to semiaquatic or aquatic predators, and that Seymouria fossils were more common in terrestrial deposits as a result of its habitat preferences. Berman et al. (2000) supported this hypothesis, as the Tambach Formation preserved Seymouria fossils while also completely lacking aquatic animals. They also pointed out the well-developed wrist and ankle bones of the "Tambach lovers" as supportive of terrestrial affinities. Despite the strong musculature of the forelimbs, Romer (1928) [9] and White (1939) [12] found little evidence for burrowing adaptations in Seymouria.

Sexual dimorphism

Some authors have argued in favor of sexual dimorphism existing in Seymouria, but others are unconvinced by this hypothesis. White (1939) argued that some specimens of Seymouria baylorensis had chevrons (bony spines on the underside of the tail vertebrae) which first appeared on the third tail vertebra, while other specimens had them first appear on the sixth. He postulated that the later appearance of the chevrons in some specimens was indicative that they were males in need of more space to store their internal genitalia. This type of sexual differentiation has been reported in both turtles and crocodilians. Based on this, he also supported the idea that Seymouria females gave birth to large-yolked eggs on land, as with turtles and crocodilians. [12] Vaughn (1966) later found a correlation between chevron acquisition and certain skull proportions in Seymouria sanjuanensis, and proposed that they too were examples of sexual dimorphism. [5]

However, Berman, Reisz, & Elberth (1987) criticized the methodologies of White (1939) and Vaughn (1966). They argued that White's observations were probably unrelated to the sex of the animals. This was supported by the fact that some of the Cutler Formation specimens had chevrons which first appeared on their fifth tail vertebra. Although it was possible that genital size was variable among males to the extent of impacting the skeleton, the more likely explanation was that the differences White had observed were caused by individual skeletal variation, evolutionary divergence, or some other factor unrelated to sexual dimorphism. Likewise, they agreed that skull proportions supported Vaughn (1966)'s proposal that dimorphism was present in Seymouria fossils, though they disagreed with how he linked it to sex using a fossil which was considered "female" under White's criteria. [7] The discovery of fossilized larval seymouriamorphs has shown that Seymouria likely had an aquatic larval stage, debunking earlier hypotheses that Seymouria laid eggs on land. [10]

Histology and development

Histological evidence from specimens found in Richards Spurs, Oklahoma has provided additional information on Seymouria's biology. A femur was found to have an internal structure characterized by a lamellar matrix pierced by numerous plexiform canals. Rest lines of slow growth are indistinct and closely spaced, but there is no evidence that growth ceased at any time during bone development. Like most lissamphibians, the medullary cavity is open and has a small amount of spongiosa bone. The development of spongiosa bone is slightly higher that of Acheloma (a terrestrial amphibian), but is much less extensive than aquatic amphibians such as Rhinesuchus and Trimerorhachis . Seymouria's vertebrae are more robust in shape compared to Discosauriscus, and have a low amount of cartilage despite a high amount of porosity. Seymouria are inferred to have undergone metamorphosis very early in life, likely due to environmental stresses from fluctuating wet and dry seasons. [24]

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<span class="mw-page-title-main">Diadectidae</span> Extinct family of tetrapods

Diadectidae is an extinct family of early tetrapods that lived in what is now North America and Europe during the Late Carboniferous and Early Permian, and in Asia during the Late Permian. They were the first herbivorous tetrapods, and also the first fully terrestrial animals to attain large sizes. Footprints indicate that diadectids walked with an erect posture. They were the first to exploit plant material in terrestrial food chains, making their appearance an important stage in both vertebrate evolution and the development of terrestrial ecosystems.

<span class="mw-page-title-main">Diadectomorpha</span> Extinct clade of tetrapods

Diadectomorpha is a clade of large tetrapods that lived in Euramerica during the Carboniferous and Early Permian periods and in Asia during Late Permian (Wuchiapingian), They have typically been classified as advanced reptiliomorphs positioned close to, but outside of the clade Amniota, though some recent research has recovered them as the sister group to the traditional Synapsida within Amniota, based on inner ear anatomy and cladistic analyses. They include both large carnivorous and even larger herbivorous forms, some semi-aquatic and others fully terrestrial. The diadectomorphs seem to have originated during late Mississippian times, although they only became common after the Carboniferous rainforest collapse and flourished during the Late Pennsylvanian and Early Permian periods.

<i>Cacops</i> Extinct genus of amphibians

Cacops, is a genus of dissorophid temnospondyls from the Kungurian stage of the early Permian of the United States. Cacops is one of the few olsoniforms whose ontogeny is known. Cacops fossils were almost exclusively known from the Cacops Bone Bed of the Lower Permian Arroyo Formation of Texas for much of the 20th century. New material collected from the Dolese Brothers Quarry, near Richards Spur, Oklahoma in the past few decades has been recovered, painting a clearer picture of what the animal looked and acted like.

<span class="mw-page-title-main">Temnospondyli</span> Ancestors of modern amphibians adapted to life on land

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 armour-like bony plates that distinguish them from the modern soft-bodied lissamphibians.

<span class="mw-page-title-main">Captorhinidae</span> Extinct family of tetrapods

Captorhinidae is an extinct family of tetrapods, typically considered primitive reptiles, known from the late Carboniferous to the Late Permian. They had a cosmopolitan distribution across Pangea.

<i>Westlothiana</i> Extinct genus of tetrapods

Westlothiana is a genus of reptile-like tetrapod that lived about 338 million years ago during the latest part of the Viséan age of the Carboniferous. Members of the genus bore a superficial resemblance to modern-day lizards. The genus is known from a single species, Westlothiana lizziae. The type specimen was discovered in the East Kirkton Limestone at the East Kirkton Quarry, West Lothian, Scotland in 1984. This specimen was nicknamed "Lizzie the lizard" by fossil hunter Stan Wood, and this name was quickly adopted by other paleontologists and the press. When the specimen was formally named in 1990, it was given the specific name "lizziae" in homage to this nickname. However, despite its similar body shape, Westlothiana is not considered a true lizard. Westlothiana's anatomy contained a mixture of both "labyrinthodont" and reptilian features, and was originally regarded as the oldest known reptile or amniote. However, updated studies have shown that this identification is not entirely accurate. Instead of being one of the first amniotes, Westlothiana was rather a close relative of Amniota. As a result, most paleontologists since the original description place the genus within the group Reptiliomorpha, among other amniote relatives such as diadectomorphs and seymouriamorphs. Later analyses usually place the genus as the earliest diverging member of Lepospondyli, a collection of unusual tetrapods which may be close to amniotes or lissamphibians, or potentially both at the same time.

<span class="mw-page-title-main">Seymouriamorpha</span> Extinct order of tetrapodomorphs

Seymouriamorpha were a small but widespread group of limbed vertebrates (tetrapods). They have long been considered stem-amniotes (reptiliomorphs), and most paleontologists still accept this point of view, but some analyses suggest that seymouriamorphs are stem-tetrapods. Many seymouriamorphs were terrestrial or semi-aquatic. However, aquatic larvae bearing external gills and grooves from the lateral line system have been found, making them unquestionably amphibians. Though as they matured, they became more terrestrial and reptile-like. They ranged from 30 cm long lizard-sized creatures to the 1.5 m long Enosuchus. If seymouriamorphs are reptiliomorphs, they were the distant relatives of amniotes. Seymouriamorphs form into three main groups, Kotlassiidae, Discosauriscidae, and Seymouriidae, a group that includes the best known genus, Seymouria. The last seymouriamorph became extinct by the end of the Permian.

<i>Platyhystrix</i> Genus of amphibians (fossil)

Platyhystrix is an extinct temnospondyl amphibian with a distinctive sail along its back, similar to the unrelated synapsids, Dimetrodon and Edaphosaurus. It lived during the boundary between the latest Carboniferous and earliest Permian periods throughout what is now known as the Four Corners, Texas, and Kansas about 300 million years ago.

<span class="mw-page-title-main">Parareptilia</span> Subclass of reptiles

Parareptilia ("near-reptiles") is a subclass or clade of basal sauropsids/reptiles, typically considered the sister taxon to Eureptilia. Parareptiles first arose near the end of the Carboniferous period and achieved their highest diversity during the Permian period. Several ecological innovations were first accomplished by parareptiles among reptiles. These include the first reptiles to return to marine ecosystems (mesosaurs), the first bipedal reptiles, the first reptiles with advanced hearing systems, and the first large herbivorous reptiles. The only parareptiles to survive into the Triassic period were the procolophonoids, a group of small generalists, omnivores, and herbivores. The largest family of procolophonoids, the procolophonids, rediversified in the Triassic, but subsequently declined and became extinct by the end of the period.

<span class="mw-page-title-main">Embolomeri</span> Extinct order of tetrapods

Embolomeri is an order of tetrapods or stem-tetrapods, possibly members of Reptiliomorpha. Embolomeres first evolved in the Early Carboniferous (Mississippian) Period and were the largest and most successful predatory tetrapods of the Late Carboniferous (Pennsylvanian) Period. They were specialized semiaquatic predators with long bodies for eel-like undulatory swimming. Embolomeres are characterized by their vertebral centra, which are formed by two cylindrical segments, the pleurocentrum at the rear and intercentrum at the front. These segments are equal in size. Most other tetrapods have pleurocentra and intercentra which are drastically different in size and shape.

<i>Limnoscelis</i> Genus of diadectomorphs

Limnoscelis was a genus of large diadectomorph tetrapods from the Late Carboniferous to early Permian of western North America. It includes two species: the type species Limnoscelis paludis from New Mexico, and Limnoscelis dynatis from Colorado, both of which are thought to have lived concurrently. No specimens of Limnoscelis are known from outside of North America. Limnoscelis was carnivorous, and likely semiaquatic, though it may have spent a significant portion of its life on land. Limnoscelis had a combination of derived amphibian and primitive reptilian features, and its placement relative to Amniota has significant implications regarding the origins of the first amniotes.

<i>Kotlassia</i> Genus of reptile-like amphibians

Kotlassia extinct genus of kotlassiine seymouriamorph from the Late Permian of Russia. The type, and currently only, species is K. prima.

<i>Microleter</i> Extinct genus of reptiles

Microleter is an extinct genus of basal procolophonomorph parareptiles which lived in Oklahoma during the Early Permian period. The type and only known species is Microleter mckinzieorum. Microleter is one of several parareptile taxa described from the Richards Spur fissure fills, and can be characterized from its high tooth count, lacrimal/narial contact, short postfrontal, and slit-like temporal emargination edged by the postorbital, jugal, squamosal, and quadratojugal. Contrary to Australothyris, which had a similar phylogenetic position as a basal procolophonomorph, Microleter suggests that early parareptile evolution occurred in Laurasia and that multiple lineages developed openings or emarginations in the temporal region.

<span class="mw-page-title-main">Tambach Formation</span> Early Permian-age geologic formation in Germany

The Tambach Formation is an Early Permian-age geologic formation in central Germany. It consists of red to brown-colored sedimentary rocks such as conglomerate, sandstone, and mudstone, and is the oldest portion of the Upper Rotliegend within the Thuringian Forest Basin.

<span class="mw-page-title-main">Organ Rock Formation</span>

The Organ Rock Formation or Organ Rock Shale is a formation within the late Pennsylvanian to early Permian Cutler Group and is deposited across southeastern Utah, northwestern New Mexico, and northeastern Arizona. This formation notably outcrops around Canyonlands National Park, Natural Bridges National Monument, and Monument Valley of northeast Arizona, southern Utah. The age of the Organ Rock is constrained to the latter half of the Cisuralian epoch by age dates from overlying and underlying formations. Important early terrestrial vertebrate fossils have been recovered from this formation in northern Arizona, southern Utah, and northern New Mexico. These include the iconic Permian terrestrial fauna: Seymouria, Diadectes, Ophiacodon, and Dimetrodon. The fossil assemblage present suggests arid environmental conditions. This is corroborated with paleoclimate data indicative of global drying throughout the early Permian.

This list of fossil amphibians described in 2020 is a list of new taxa of fossil amphibians that were described during the year 2020, as well as other significant discoveries and events related to amphibian paleontology that occurred in 2020.

References

  1. 1 2 Laurin, Michel (January 1, 1996). "Seymouria". Tree of Life Web Project . Paris: Muséum National d'Histoire Naturelle . Retrieved February 24, 2018.
  2. 1 2 3 4 Williston, S.W. (1911). "Restoration of Seymouria baylorensis Broili, an American Cotylosaur". The Journal of Geology. 19 (3): 232–237. Bibcode:1911JG.....19..232W. doi:10.1086/621840. S2CID   140644621.
  3. 1 2 3 Watson, D.M.S. (1918). "On Seymouria, the most primitive known reptile". Proceedings of the Zoological Society of London. 88 (3–4): 267–301. doi:10.1111/j.1096-3642.1918.tb02098.x.
  4. 1 2 Broili, Ferdinand (1904). "Permische Stegocephalen und Reptilien aus Texas". Palaeontographica. 51: 1–48.
  5. 1 2 3 4 Vaughn, Peter Paul (May 1966). "Seymouria from the Lower Permian of Southeastern Utah, and Possible Sexual Dimorphism in That Genus". Journal of Paleontology. 40 (3): 603–612. JSTOR   1301745.
  6. 1 2 3 4 5 Laurin, Michel (13 July 1996). "A Redescription of the Cranial Anatomy of Seymouria baylorensis, the best known Seymouriamorph (Vertebrata: Seymouriamorpha)" (PDF). PaleoBios. 17 (1): 1–16.
  7. 1 2 3 4 5 6 7 Berman, David S.; Reisz, Robert R.; Eberth, David A. (1987). "Seymouria sanjuanensis (Amphibia, Batrachosauria) from the Lower Permian Cutler Formation of north-central New Mexico and the occurrence of sexual dimorphism in that genus questioned". Canadian Journal of Earth Sciences. 24 (9): 1769–1784. Bibcode:1987CaJES..24.1769B. doi:10.1139/e87-169.
  8. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 Berman, David S.; Henrici, Amy C.; Sumida, Stuart S.; Martens, Thomas (2000). "Redescription of Seymouria sanjuanensis (Seymouriamorpha) from the Lower Permian of Germany based on complete, mature specimens with a discussion of paleoecology of the Bromacker locality assemblage". Journal of Vertebrate Paleontology. 20 (2): 253–268. doi:10.1671/0272-4634(2000)020[0253:ROSSSF]2.0.CO;2. JSTOR   4524091. S2CID   130445307.
  9. 1 2 3 4 5 Romer, Alfred S. (1928). "A Skeletal Model of the Primitive Reptile Seymouria, and the Phylogenetic Position of that type". The Journal of Geology. 36 (3): 248–260. Bibcode:1928JG.....36..248R. doi:10.1086/623510. JSTOR   30060526. S2CID   129513686.
  10. 1 2 3 Bratislava, Jozef Klembara (1995-03-01). "The external gills and ornamentation of skull roof bones of the Lower Permian tetrapod Discosauriscus (Kuhn 1933) with remarks to its ontogeny". Paläontologische Zeitschrift. 69 (1): 265–281. doi:10.1007/BF02985990. S2CID   87658588.
  11. ↑ Gregory, William King (1931) "Students in Nature's Training School" in American Museum of Natural History Hall of Human Evolution guide book https://archive.org/details/scienceguide7692amer/page/n394/mode/1up?view=theater
  12. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 White, T.E. (1939). "Osteology of Seymouria baylorensis Broili". Bulletin of the Museum of Comparative Zoology. 85 (5): 323–409.
  13. 1 2 Broom, R. (1922). "On the Persistence of the Mesopterygoid in certain Reptilian Skulls". Proceedings of the Zoological Society of London. 1922:pt.1-2 [pp.1-481] (2): 455–460. doi:10.1111/j.1096-3642.1922.tb02151.x.
  14. ↑ Sushkin, Peter P. (18 December 1925). "On the representatives of the Seymouriamorpha, supposed primitive Reptiles, from the Upper Permian of Russia, and on their phylogenetic relations". Occasional Papers of the Boston Society of Natural History. 5: 179–181.
  15. ↑ Watson, D. M. S. (1942). "On Permian and Triassic Tetrapods". Geological Magazine. 79 (2): 81–116. Bibcode:1942GeoM...79...81W. doi:10.1017/S0016756800073593. ISSN   1469-5081. S2CID   131417438.
  16. 1 2 3 4 Romer, Alfred Sherwood (1947). "Review of the Labyrinthodontia". Bulletin of the Museum of Comparative Zoology at Harvard College. 99 (1): 7–368.
  17. ↑ Laurin, Michel; Reisz, Robert R. (September 2001). "The reptile Macroleter: First vertebrate evidence for correlation of Upper Permian continental strata of North America and Russia" (PDF). Geological Society of America Bulletin . 113 (9): 1229–1233. Bibcode:2001GSAB..113.1229R. doi:10.1130/0016-7606(2001)113<1229:trmfve>2.0.co;2. Archived from the original (PDF) on March 11, 2012.
  18. 1 2 Berman, David S.; Martens, Thomas (25 February 1993). "First occurrence of Seymouria (Amphibia: Batrachosauria) in the Lower Permian Rotliegend of central Germany". Annals of the Carnegie Museum. 62 (1): 63–79. doi: 10.5962/p.226648 . S2CID   91262105 – via Biostor.
  19. ↑ Sullivan, Corwin; Reisz, Robert R. (1999). "First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma". Canadian Journal of Earth Sciences. 36 (8): 1257–1266. doi:10.1139/e99-035.
  20. 1 2 Klembara, Jozef; Berman, David S.; Henrici, Amy C.; Cernansky, Andrej; Werneberg, Ralf; Martens, Thomas (30 March 2007). "First description of skull of Lower Permian Seymouria sanjuanensis (Seymouriamorpha: Seymouriidae) at an early juvenile growth stage". Annals of Carnegie Museum. 76 (1): 53–72. doi:10.2992/0097-4463(2007)76[53:FDOSOL]2.0.CO;2. S2CID   86217084.
  21. ↑ Klembara, Jozef; Hain, Miroslav; Ruta, Marcello; Berman, David S.; Pierce, Stephanie E.; Henrici, Amy C. (2019). "Inner ear morphology of diadectomorphs and seymouriamorphs (Tetrapoda) uncovered by high-resolution x-ray microcomputed tomography, and the origin of the amniote crown group". Palaeontology. 63: 131–154. doi: 10.1111/pala.12448 . ISSN   1475-4983.
  22. 1 2 3 Klembara, Jozef; Berman, David S.; Henrici, Amy C.; Cernansky, Andrej (30 December 2005). "New structures and reconstructions of the skull of the Seymouriamorph Seymouria sanjuanensis Vaughn". Annals of Carnegie Museum. 74 (4): 217–225. doi:10.2992/0097-4463(2005)74[217:NSAROT]2.0.CO;2. S2CID   85794721.
  23. ↑ Sumida, Stuart S.; Lombard, Eric; Berman, David S. (29 May 1992). "Morphology of the atlas-axis complex of the late Palaeozoic tetrapod suborders Diadectomorpha and Seymouriamorpha". Philosophical Transactions of the Royal Society B: Biological Sciences. 336 (1227): 259–273. Bibcode:1992RSPTB.336..259S. doi:10.1098/rstb.1992.0060.
  24. ↑ Bazzana, Kayla D.; Gee, Bryan M.; Bevitt, Joseph J.; Reisz, Robert R. (2020-03-10). "Postcranial anatomy and histology of Seymouria, and the terrestriality of seymouriamorphs". PeerJ. 8: e8698. doi: 10.7717/peerj.8698 . ISSN   2167-8359. PMC   7069408 . PMID   32195050.
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