Cabarzia

Last updated

Cabarzia
Temporal range: Asselian–Sakmarian
Cabarzia fossil illustration.png
Illustration of the holotype fossil
Scientific classification Red Pencil Icon.png
Kingdom: Animalia
Phylum: Chordata
Family: Varanopidae
Subfamily: Mycterosaurinae
Genus: Cabarzia
Spindler, Werneberg, & Schneider, 2019
Type species
Cabarzia trostheidei
Spindler, Werneberg, & Schneider, 2019

Cabarzia is an extinct genus of varanopid from the Early Permian of Germany. It contains only a single species, Cabarzia trostheidei, which is based on a well-preserved skeleton found in red beds of the Goldlauter Formation. Cabarzia shared many similarities with Mesenosaurus romeri (a varanopid from Russia), although it did retain some differences, such as more curved claws, a wide ulnare, and muscle scars on its sacral ribs. With long, slender hindlimbs, a narrow body, an elongated tail, and short, thick forelimbs, Cabarzia was likely capable of running bipedally to escape from predators, a behavior shared by some modern lizards. It is the oldest animal known to have adaptations for bipedal locomotion, predating Eudibamus , a bipedal bolosaurid parareptile from the slightly younger Tambach Formation. [1]

Contents

Discovery

Cabarzia is known from a single articulated skeleton, missing only the head, neck, and portions of the shoulder, tail, and left limbs. This holotype specimen, NML-G2017/001, was discovered in 1989 by Frank Trostheide, a fossil collector prospecting at the Cabarz Quarry in the Thuringian Forest of Germany. This quarry preserves a large portion of the Goldlauter Formation, which is a sequence of Early Permian red beds, lake sediments, and volcanic layers slightly older than the nearby Artinskian or Kungurian-age red beds of the Tambach Formation. [1]

Preliminary study of the specimen tentatively considered it an araeoscelidian diapsid reptile, but a 2019 study by Frederik Spindler, Ralf Werneburg, and Jörg W. Schneider reasoned against that assignment after comparing the postcranial anatomy of small Permian amniotes such as basal synapsids, parareptiles, and eureptiles. They argued that it was likely a varanopid closely related to Mesenosaurus , part of the subfamily Mesenosaurinae which they had named the previous year. The specimen was assigned the name Cabarzia trostheidei in honor of both the locale of its collection and its collector. [1]

Description

The dorsal vertebrae have long centra and widely spaced zygapophyses, giving them an hourglass shape when seen from above. Their neural spines are low, rectangular and blade-like. Cabarzia's vertebrae were relatively simple by varanopid standards, with no distinct lateral excavations or mammillary processes. Mesenosaurus also lacks these characteristics. The seemingly holocephalous (single-headed) ribs, which were already short to begin with, diminished further towards the hip. There were likely only two sacral vertebrae, based on the number of sacral ribs. All of the sacral ribs apparently flared out to the same extent as they contacted the pelvis, like Mesenosaurus, although Cabarzia additionally possessed knob-like scars on the upper surface of its sacral ribs. The caudal (tail) vertebrae were fairly elongated, with thick, hook-shaped caudal ribs proportionally similar to those of Apsisaurus . Preserved portions of the shoulder girdle indicate that Cabarzia had a thin scapula with a convex front edge. The pelvis included an ilium with a long and low dorsal blade and a pubis with a small tubercule. [1]

The forelimb is short and robust relative to the long and slender hindlimb. The humerus in particular is thick, with a large entepicondyle. Cabarzia's entepicondylar foramen was located near the elbow, a far position only otherwise seen in Mesenosaurus among basal synapsids. The radius was relatively short (only slightly longer than the humerus) and was straight, unlike the twisted radius of Mesenosaurus. Most of Cabarzia's carpals (wrist bones) were proportionally similar to those of Mesenosaurus, with a broad intermedium and fairly large proximal carpals and centrale/centralia. However, it also differs due to its characteristically wide ulnare and the retention of two centralia. A tiny pisiform bone is also preserved, much smaller than that of varanodontines. On the other hand, the relative metacarpal proportions of Cabarzia are close to varanodontines. [1]

The femur is neither particularly robust nor slender, but it does have a thin and angular internal trochanter. Like other varanopids (and diapsids), the tibia and fibula were each relatively long, more than 80% the length of the femur. The ratio of the tibia to the longest toe in the foot (the fourth toe) is 3:4, like Mesenosaurus. The astragalus was large and simple, and the calcaneum abutted it along a slightly concave edge surrounding a narrow hole. The fourth distal tarsal is large and unfused to the fifth distal tarsal. As in Mesenosaurus, the elongated fourth metatarsal had a proximal projection which contacted the short fifth metatarsal. The position of the fossil suggests Cabarzia had a fifth toe which was angled relative to the rest of the foot. One of the most clear differences between Cabarzia and Mesenosaurus was the fact that Mesenosaurus had long but rather straight unguals while those of Cabarzia were shorter, deeper, and sharply curved, a characteristic also known in the hands of Tambacarnifex . [1]

Paleobiology

Fused neural spines and well-ossified joints indicate that the holotype specimen of Cabarzia was an adult animal. The curved claws of Cabarzia and Tambacarnifex were likely adapted for predation, in contrast to the more straight claws of Mesenosaurus and Varanops which may have been more useful for digging. The broad ulnare is an adaptation also seen in aquatic animals, although there is no other evidence for aquatic habits in Cabarzia. [1]

Cabarzia's proportions (short forelimbs, thin body, long hindlimbs and tail) are similar to those of modern lizards capable of bipedalism. They also match the Tambach bolosaurid Eudibamus , although the 'sprawling" ankle and foot of Cabarzia are not as specialized for bipedal habits. This may indicate that Cabarzia did not engage in active bipedalism (slow, methodical walking on the hindlimbs) but rather passive bipedalism (a shift into a bipedal posture when running at high speeds, due to the center of weight being behind the hindlimbs). The advantage of passive bipedalism is not fully understood, even in living reptiles, though it may be involved with increased coordination or assistance in the capture of flying insects. Other "mesenosaurines" (such as Mesenosaurus) shared Cabarzia's adaptations for bipedalism, and may have had increased hip musculature to habituate to the lifestyle further. Information on "mesenosaurine" foot proportions afforded by the description of Cabarzia indicates that they are good candidates for the trackmakers of Dromopus , a common Permian reptile footprint ichnogenus which has traditionally been assumed to have been created by araeoscelidian diapsids. Although no known Dromopus fossils seem to correspond to bipedal animals, this is likely due to bipedalism in "mesenosaurines" being restricted to rare circumstances where they are forced to escape predators. As Cabarzia is the oldest known "mesenosaurine" and predates the previously oldest known bipedal animal (Eudibamus) in Thuringian stratigraphy, Cabarzia can be considered the oldest animal known to have practiced bipedalism. [1]

Related Research Articles

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

Marasuchus is a genus of basal dinosauriform archosaur which is possibly synonymous with Lagosuchus. Both genera lived during the Late Triassic in what is now La Rioja Province, Argentina. Marasuchus contains a single species, Marasuchus lilloensis.

<i>Petrolacosaurus</i> Genus of tetrapods

Petrolacosaurus is an extinct genus of diapsid reptile from the late Carboniferous period. It was a small, 40-centimetre (16 in) long reptile, and the earliest known reptile with two temporal fenestrae. This means that it was at the base of Diapsida, the largest and most successful radiation of reptiles that would eventually include all modern reptile groups, as well as dinosaurs and other famous extinct reptiles such as plesiosaurs, ichthyosaurs, and pterosaurs. However, Petrolacosaurus itself was part of Araeoscelida, a short-lived early branch of the diapsid family tree which went extinct in the mid-Permian.

<i>Seymouria</i> Extinct genus of reptile-like amphibians

Seymouria is an extinct genus of Seymouriamorph from the Early Permian of North America and Europe. Although they were amphibians, 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. It is primarily known from two species, Seymouria baylorensis and Seymouria sanjuanensis. The type species, S. baylorensis, is more robust and specialized, though its fossils have only been found in Texas. 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, and a pair of fully grown skeletons from the Tambach Formation of Germany, which were fossilized lying next to each other.

Varanopidae Extinct family of synapsids

Varanopidae is an extinct family of amniotes that resembled monitor lizards and may have filled a similar niche, hence the name. Typically, they are considered synapsids that evolved from an Archaeothyris-like synapsid in the Late Carboniferous. However, some recent studies have recovered them being taxonomically closer to diapsid reptiles. A varanopid from the latest Middle Permian Pristerognathus Assemblage Zone is the youngest known varanopid and the last member of the "pelycosaur" group of synapsids.

Parareptilia Subclass of reptiles

Parareptilia 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 and continued to be successful until their demise in the Triassic-Jurassic mass extinction.

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

Utatsusaurus hataii is the earliest-known ichthyopterygian which lived in the Early Triassic period. It was nearly 3 metres (9.8 ft) long with a slender body. The first specimen was found in Utatsu-cho, Miyagi Prefecture, Japan. It is the only described species in the genus Utatsusaurus and the only member of the family Utatsusauridae. The name Utatsusaurus was given after the city. The fossils have been found from the Early Triassic Osawa Formation of Miyagi Prefecture, Japan and British Columbia, Canada.

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

Mecistotrachelos is an extinct genus of gliding reptile believed to be an archosauromorph, distantly related to crocodylians and dinosaurs. The type and only known species is M. apeoros. This specific name translates to "soaring longest neck", in reference to its gliding habits and long neck. This superficially lizard-like animal was able to spread its lengthened ribs and glide on wing-like membranes. Mecistotrachelos had a much longer neck than other gliding reptiles of the Triassic such as Icarosaurus and Kuehneosaurus. It was probably an arboreal insectivore.

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

Acerosodontosaurus is an extinct genus of neodiapsid reptiles that lived during the Upper Permian of Madagascar. The only species of Acerosodontosaurus, A. piveteaui, is known from a natural mold of a single partial skeleton including a crushed skull and part of the body and limbs. The fossil was discovered in marine deposits of the Lower Sakamena Formation. In conjunction with several skeletal characteristics, this may indicate that Acerosodontosaurus individuals were at least partially aquatic.

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

Eunotosaurus is an extinct genus of reptile, possibly a close relative of turtles, from the late Middle Permian Karoo Supergroup of South Africa. The Eunotosaurus resided in the swamps of southern Africa. It is often considered as a possible "missing link" between turtles and their prehistoric ancestors. Its ribs were wide and flat, forming broad plates similar to a primitive turtle shell, and the vertebrae were nearly identical to those of some turtles. It is possible that these turtle-like features evolved independently of the same features in turtles, though some studies suggest Eunotosaurus is a genuine, primitive turtle relative. Other anatomical studies and phylogenetic analysis suggest that Eunotosaurus is a parareptile and not a basal turtle.

<i>Aerosaurus</i> Extinct family of mammals

Aerosaurus is an extinct genus within Varanopidae, a family of non-mammalian synapsids. It lived between 252-299 million years ago during the Early Permian in North America. The name comes from Latin aes (aeris) “copper” and Greek sauros “lizard,” for El Cobre Canyon in northern New Mexico, where the type fossil was found and the site of former copper mines. Aerosaurus was a small to medium-bodied carnivorous synapsid characterized by its recurved teeth, triangular lateral temporal fenestra, and extended teeth row. Two species are recognized: A. greenleeorum (1937) and A. wellesi (1981).

Eosimops is an extinct genus of pylaecephalid dicynodonts. They were small synapsids superficially resembling modern mammals. Eosimops is known from several skull specimens, as well as one complete skeleton. Eosimops lived during the Middle Permian of South Africa.

<i>Mesenosaurus</i> Extinct genus of synapsids

Mesenosaurus is an extinct genus of amniote. It belongs to the family Varanopidae. This genus includes two species: the type species Mesenosaurus romeri from the middle Permian Mezen River Basin of northern Russia, and Mesenosaurus efremovi from the early Permian (Artinskian) Richards Spur locality. M. romeri’s stratigraphic range is the middle to late Guadalupian while M. efremovi’s stratigraphic range is the Cisuralian.

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

Heleosarus scholtzi is an extinct species of basal synapsids, known as pelycosaurs, in the family of Varanopidae during the middle Permian. At first H. scholtzi was mistakenly classified as a diapsid. Members of this family were carnivorous and had dermal armor, and somewhat resembled monitor lizards. This family was the most geologically long lived, widespread, and diverse group of early amniotes. To date only two fossils have been found in the rocks of South Africa. One of these fossils is an aggregation of five individuals.

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

Orovenator is an extinct genus of diapsid from Lower Permian deposits of Oklahoma, United States. It is known from two partial skulls from the Richards Spur locality in Oklahoma. The holotype OMNH 74606 consists of a partial skull preserving snout and mandible, and the referred specimen, OMNH 74607, a partial skull preserving the skull roof, vertebrae and palatal elements. It was first named by Robert R. Reisz, Sean P. Modesto and Diane M. Scott in 2011 and the type species is Orovenator mayorum. The generic name means "mountain", oro, in Greek in reference to the Richards Spur locality, which was mountainous during the Permian period and "hunter", venator, in Latin. The specific name honours Bill and Julie May. Orovenator is the oldest and most basal neodiapsid to date.

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

Cosesaurus is a genus of archosauromorph reptiles likely belonging to the family Tanystropheidae. It is known from fossil imprints of a single small skeleton, MGB V1, which was found in Muschelkalk outcrops near the municipalities of Mont-ral and Alcover in Spain. These outcrops are dated to the Ladinian age of the middle Triassic about 242 to 237 million years ago. The specimen is stored at the Museu Martorell, which is now part of the Museu de Ciències Naturals de Barcelona. The poor preservation and likely juvenile nature of the specimen has led to the anatomy of Cosesaurus being misidentified by several different sources. For example, Paul Ellenberger claimed that it was an ancestor to birds in the 1970s, while David Peters claimed that it was a pterosaur ancestor in 2000. Both of these claims contrast with mainstream scientific theories on the origins of either group, and other paleontologists who study the specimen are unable to find the features which Ellenberger or Peters reported to be present. The Ellenberger and Peters hypotheses are thus considered fringe theories with questionable scientific soundness due to their low reproducibility. Mainstream hypotheses for the relations of Cosesaurus generally agree that it is a "protorosaur", specifically a tanystropheid closely related to long-necked reptiles such as Macrocnemus, Tanytrachelos, Tanystropheus, or Langobardisaurus.

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.

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

Erpetonyx is an extinct genus of bolosaurian parareptile from the Gzhelian stage of the Carboniferous period, with a single known species: Erpetonyx arsenaultorum. It is known from a single articulated and mostly complete specimen from Prince Edward Island in Canada. Phylogenetics has predicted that parareptiles first evolved in the Carboniferous, parallel to eureptiles. However, Hylonomus, the oldest eureptile known from fossil evidence, lived millions of years before parareptiles appeared in the fossil record. The discovery of Erpetonyx helped to shorten this gap between parareptile and eureptile fossils, as Erpetonyx lived in the Late Carboniferous and is one of the oldest known parareptiles. However, it was not closely related to ancestral parareptiles, so its discovery also indicated that the initial diversification of parareptiles occurred earlier in the Carboniferous. Erpetonyx was a small reptile, with the entire skeleton about 20 to 25 centimeters in length. It was likely carnivorous, and could be characterized by a variety of skeletal features, including a relatively elongated body and large claws with powerful tendon attachment points.

Pectodens is an extinct genus of archosauromorph reptile which lived during the Middle Triassic in China. The type and only species of the genus is P. zhenyuensis, named by Chun Li and colleagues in 2017. It may be a member of the Protorosauria; an unusual combination of traits similar and dissimilar to other members causes Pectodens to elude exact classification.

Ascendonanus is an extinct genus of varanopid amniote from the Early Permian of Germany. It is the earliest specialized arboreal (tree-living) vertebrate currently known and resembled a small lizard, although it was related to mammals. The fossils of Ascendonanus are of special scientific importance because they include remains of skin, scales, scutes, bony ossicles, and body outlines, indicating that some of the oldest relatives of mammals had a scaly "reptilian-type" appearance. The animal was about 40 cm long, with strongly curved claws, short limbs, a slender, elongated trunk, and a long tail. It would have preyed on insects and other small arthropods.

Dendromaia is an extinct genus of varanopid from the Carboniferous of Nova Scotia. It contains a single species, Dendromaia unamakiensis. Dendromaia is the oldest known varanopid, likely the oldest known synapsid, and the only member of the family Varanopidae to be discovered in Nova Scotia. Known from a large partial skeleton preserved with its tail wrapped around a much smaller partial skeleton, Dendromaia may also represent the oldest known occurrence of parental care in the fossil record. While the larger skeleton possessed certain mycterosaurine-like features, the smaller skeleton resembled basal varanopids such as Archaeovenator and Pyozia, creating uncertainty over whether characteristics at the base of Varanopidae have legitimate phylogenetic significance or instead reflect the immaturity of basal varanopid specimens.

References

  1. 1 2 3 4 5 6 7 8 Spindler, Frederik; Werneburg, Ralf; Schneider, Jörg W. (2019-06-01). "A new mesenosaurine from the lower Permian of Germany and the postcrania of Mesenosaurus: implications for early amniote comparative osteology". PalZ. 93 (2): 303–344. doi:10.1007/s12542-018-0439-z. ISSN   1867-6812. S2CID   91871872.