Asterotrygon Temporal range: Early Eocene, | |
---|---|
Holotype specimen of Asterotrygon maloneyi (FMNH PF 15166). | |
Scientific classification | |
Kingdom: | |
Phylum: | |
Class: | |
Subclass: | |
Order: | |
Suborder: | |
Genus: | †Asterotrygon |
Species | |
|
Asterotrygon is an extinct genus of stingray from the Eocene Green River Formation in Wyoming. Several complete skeletons representing juveniles, adults, males and females have been uncovered from the late early Eocene Fossil Butte Member of the formation. The type and only species, A. maloneyi, was named in 2004 on the basis of these fossils. Another stingray, Heliobatis , is also known from the formation. Asterotrygon is a primitive stingray closely related to the living family Urolophidae whose ancestors likely originated in the Indo-Pacific. It lived in Fossil Lake, a body of water that existed in a subtropical mountainous region for only about 2 million years.
Asterotrygon had a typical stingray shape with a flat, rounded disk formed from the head and pectoral fins and a long, narrow tail with sharp stingers. It ranged in size from 7.97 centimetres (3.14 in) in the smallest juvenile (the specimen SMMP 83.25) to 65 centimetres (26 in) in the largest adult (FMNH 15166). The shape of the disk is rounder than those of other extinct stingrays such as Heliobatis, which are more diamond-shaped. The upper surface of the disk is covered in small dermal denticles, each with a small hook. Unlike Heliobatis and modern stingrays, it has a small dorsal fin in front of its stingers. While most stingrays have a cartilaginous rod extending from the stinger to the tip of the tail, Asterotrygon retains separate vertebrae throughout the tail's entire length. The tail is also somewhat thicker at its base than those of other stingrays. Small fin-like tail folds are present at the tip of the tail. The puboischiadic girdle, an element to which the pelvic fins attach, is primitively narrow and arch-shaped. Like other stingrays, Asterotrygon lacks thoracic ribs but possesses cartilage around the spine called thoracolumbar synarcual cartilage. [1]
Several details of the neurocranium link Asterotrygon with modern stingrays. Like other stingrays, the hyomandibulae, which allow the jaw to extend outward, are completely separated from the lower jaw. In other cartilaginous fish, the hyomandibulae and lower jaw are fused by the hyomandibular-Meckelian ligament. Despite this loss, Asterotrygon still retains some calcified cartilage in the space where the ligament once was. The postorbital processes behind the eye sockets are broad, flat, and shelf-like. [1]
Before the description of Asterotrygon, Heliobatis was the only known stingray in the Green River Formation. American paleontologist Othniel Charles Marsh named Heliobatis radians in 1877, and Xiphotrygon acutidens and Palaeodasybatis discus were subsequently named from the formation in 1879 and 1947, respectively. These stingrays were later synonymized with Heliobatis. [1]
In 1980, a Green River fossil called AMNH P 11557 was described that included a female stingray and two smaller individuals thought to be aborted fetuses. A second specimen called FMNH PF 15166 included a female and a fetus that was still in an embryo within the animal. The genus Asterotrygon was erected in 2004 along with the type species A. maloneyi, and FMNH PF 15166 was designated the holotype specimen. AMNH P 11557 and many other complete fossils were also referred to A. maloneyi. Hundreds of fossils of Heliobatis have been found, while Asterotrygon is represented by a few dozen specimens. Asterotrygon means "star stingray" from the Greek asteros ("star") and trygon ("stingray") after the star-like shape of the base of each denticle. The type species A. maloneyi was named after Thomas and Hilda Maloney, who donated the paratype specimen AMNH P 11557 to the American Museum of Natural History. [1]
Although Asterotrygon is not the earliest stingray (they were present as early as the Early Cretaceous, it is one of the most well-preserved of the early forms. Most earlier stingrays are known only from small teeth, dermal denticles, or stingers, but not entire bodies. [1]
Asterotrygon is classified as basal stingray within Myliobatoidei. Only Hexatrygon , the living Sixgill stingray, is more basal. Despite living alongside each other, Asterotrygon and Heliobatis are not closely related. Neither are classified in any living family of stingrays, although a 2004 phylogenetic analysis found Heliobatis to be closely related to a clade including river stingrays and whiptail stingrays. Asterotrygon is more closely related to Urolophidae, the stingarees, and Plesiobatis , the Deepwater stingray. Both types are from the Indo-Pacific. Below is a cladogram showing the phylogenetic relationships of Asterotrygon from Carvalho et al. (2004): [1]
Batoidea |
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Asterotrygon is closely related to Pacific stingrays. Its ancestors probably originated in the western Pacific or Indo-Pacific. In contrast, the contemporaneous Heliobatis probably evolved from stingrays that were already present in the Americas. Because the two genera are not closely related, their ancestors probably colonized the Green River Formation lakes in two separate but closely timed events. Neither Asterotrygon nor Heliobatis are known outside the Green River Formation, so they probably evolved within the lakes. [1]
Asterotrygon and other organisms from the Green River Formation lived in subtropical lakes in a mountainous region. These lakes existed for a very long time, some up to 15 million years. The oldest modern lakes have existed for only a few million years, and the vast majority only a few thousand. Three major lakes are known: Fossil Lake, Lake Gosiute, and Lake Uinta. Although it was the shortest-lived, Fossil Lake preserved the most fossils, including all stingray fossils. Fossil Lake is one of two areas that preserve complete stingray fossils; the other, the Monte Bolca Formation in Italy, preserves stingrays that lived in a marine lagoon behind a coral reef. Monte Bolca preserves a greater diversity of rays, including guitarfishes and electric rays. More rays may have lived in Monte Bolca because it was a marine environment; today, most stingrays live in the ocean and only a few live in fresh water. [1]
Fossil Lake was a freshwater lake in a semitropical environment. The modern Gulf Coast and southern Atlantic regions of the United States have been used as modern analogues to the environment. Asterotrygon is found in two types of deposits. One group of fossil localities is called F-1 or the "18-inch layer" and includes limestone that was deposited in the middle of fossil lake over a few hundred years. These sediments were thought to have formed in a deep area where the lake bottom was anoxic. The F-2 layer is thicker, up to 4 metres (13 ft), and was deposited over a longer period of time, possibly several thousand years. F-2 limestone was deposited closer to the north and southeastern shorelines of the lake where the water was richer in dissolved oxygen and organic material. [1]
Stingrays are a group of sea rays, a type of cartilaginous fish. They are classified in the suborder Myliobatoidei of the order Myliobatiformes and consist of eight families: Hexatrygonidae, Plesiobatidae, Urolophidae (stingarees), Urotrygonidae, Dasyatidae, Potamotrygonidae, Gymnuridae and Myliobatidae . There are about 220 known stingray species organized into 29 genera.
Monte Bolca is a lagerstätte near Verona, Italy that was one of the first fossil sites with high quality preservation known to Europeans, and is still an important source of fossils from the Eocene.
The Green River Formation is an Eocene geologic formation that records the sedimentation in a group of intermountain lakes in three basins along the present-day Green River in Colorado, Wyoming, and Utah. The sediments are deposited in very fine layers, a dark layer during the growing season and a light-hue inorganic layer in the dry season. Each pair of layers is called a varve and represents one year. The sediments of the Green River Formation present a continuous record of six million years. The mean thickness of a varve here is 0.18 mm, with a minimum thickness of 0.014 mm and maximum of 9.8 mm.
Fossil Butte National Monument is a United States National Monument managed by the National Park Service, located 15 miles (24 km) west of Kemmerer, Wyoming, United States. It centers on an assemblage of Eocene Epoch animal and plant fossils associated with Fossil Lake—the smallest lake of the three great lakes which were then present in what are now Wyoming, Utah, and Colorado. The other two lakes were Lake Gosiute and Lake Uinta. Fossil Butte National Monument was established as a national monument on October 23, 1972.
The deepwater stingray or giant stingaree is a species of stingray and the sole member of the family Plesiobatidae. It is widely distributed in the Indo-Pacific, typically over fine sediments on the upper continental slope at depths of 275–680 m (900–2,230 ft). This species reaches 2.7 m (8.9 ft) in length and 1.5 m (4.9 ft) in width. It has an oval pectoral fin disc with a long, flexible, broad-angled snout. Most of the entire latter half of its tail supports a distinctively long, slender, leaf-shaped caudal fin. Its coloration is dark above and white below, and its skin is almost completely covered by tiny dermal denticles.
Heliobatis is an extinct genus of stingray in the Myliobatiformes family Dasyatidae. At present the genus contains the single species Heliobatis radians.
Mene rhombea is an extinct perciform fish belonging to the family Menidae. During the Middle Eocene, about 48 to 40 mya, these fishes lived in the Tethys Ocean, a large tropical sea in the area corresponding to the current Mediterranean. This ocean was extended between the continents of Gondwana and Laurasia. At this time, where Monte Bolca is today, M. rhombea, and its relative, M. oblonga, lived in a tropical lagoon.
Edestus is an extinct genus of eugeneodontid holocephalian fish known from the Late Carboniferous (Pennsylvanian) of the United Kingdom, Russia, and the United States. Most remains consist of isolated curved blades or "whorls" that are studded with teeth, that in life were situated within the midline of the upper and lower jaws. Edestus is a Greek name derived from the word edeste, in reference to the aberrant quality and size of the species' teeth. The largest species, E. heinrichi, has been conservatively estimated to reach greater than 6.7 m (22 ft) in length, around the size of the largest known great white shark, possibly making it the largest marine predator to have ever existed up to that point.
Urolophus is a genus of round rays mostly native to the western Pacific Ocean and the Indian Ocean, though one species occurs in the Pacific waters of the Mexican coast. Müller and Henle erected Urolophus in an 1837 issue of Bericht Akademie der Wissenschaften zu Berlin. The name is derived from the Greek oura, meaning "tail", and lophos, meaning "crest". In Urolophus, the outer rims of the nostrils are not enlarged into lobes, but may form a small knob at the back.
The Chesterfield Island stingaree or Deforge's stingaree is a little-known species of stingray in the family Urolophidae, endemic to the continental slope off the Chesterfield Islands. Reaching 34 cm (13 in) long, it has a rounded, diamond-shaped pectoral fin disc colored plain brown above and pale below, with a short head. There is a narrow, skirt-shaped curtain of skin between its nostrils. Its tail is relatively long and terminates in a leaf-shaped caudal fin; there are no dorsal fin or lateral skin folds. This species has been listed under Least Concern by the International Union for Conservation of Nature (IUCN), as there is little fishing activity within its range.
The patchwork stingaree is a little-known species of stingray in the family Urolophidae, with a disjunct distribution off northwestern and northeastern Australia. It usually inhabits the outer continental shelf, at a depth of 60–320 m (200–1,050 ft). This species has a diamond-shaped pectoral fin disc much wider than long, and a short, flattened tail with a prominent dorsal fin and leaf-like caudal fin. There is a skirt-shaped curtain of skin between its nostrils. Its dorsal colour pattern resembles a mosaic of dark brown rings with light-coloured centers, separated by fine reticulated lines. The International Union for Conservation of Nature (IUCN) has listed the patchwork stingaree under Least Concern, as it is subject to minimal fishing pressure.
The Coral Sea stingaree is a little-known species of stingray in the family Urolophidae, found at a depth of 171–310 m (561–1,017 ft) around the edge of the continental shelf off northern Queensland. Growing to a length of 48 cm (19 in), this species has a diamond-shaped pectoral fin disc with a protruding snout and a skirt-shaped flap of skin between the nostrils. Its tail bears a low dorsal fin before the stinging spine and terminates in a short leaf-shaped caudal fin. Its upper surface is grayish or brownish, sometimes with tiny dark spots. The Coral Sea stingaree may represent two closely similar species, one large and one small. There is very little fishing activity within its range, and thus it has been listed under Least Concern by the International Union for Conservation of Nature (IUCN).
Priscacara, is a genus of extinct temperate bass described from Early to Middle Eocene fossils. It is characterized by a sunfish-like body and its stout dorsal and anal spines. The genus is best known from the Green River Formation of Wyoming, Utah and Colorado. Mass deaths of Priscacara suggest it formed schools.
The Tumbes round stingray is a little-known species of round ray, family Urolophidae, known only from two immature male specimens collected from estuarine waters at depths of 1–2 m, and a third specimen collected in 2006 near mangroves. Its range appears to be limited to coastal waters off Tumbes in northern Peru, where it is found partially buried in sand or mud. The larger of the original two specimens measured 40.4 cm long and the smaller 15.7 cm.
Asiatosuchus is an extinct genus of crocodyloid crocodilians that lived in Eurasia during the Paleogene. Many Paleogene crocodilians from Europe and Asia have been attributed to Asiatosuchus since the genus was named in 1940. These species have a generalized crocodilian morphology typified by flat, triangular skulls. The feature that traditionally united these species under the genus Asiatosuchus is a broad connection or symphysis between the two halves of the lower jaw. Recent studies of the evolutionary relationships of early crocodilians along with closer examinations of the morphology of fossil specimens suggest that only the first named species of Asiatosuchus, A. grangeri from the Eocene of Mongolia, belongs in the genus. Most species are now regarded as nomina dubia or "dubious names", meaning that their type specimens lack the unique anatomical features necessary to justify their classification as distinct species. Other species such as "A." germanicus and "A." depressifrons are still considered valid species, but they do not form an evolutionary grouping with A. grangeri that would warrant them being placed together in the genus Asiatosuchus.
Bahndwivici is an extinct genus of lizard known from a nearly complete and articulated skeleton discovered in rocks of the Green River Formation of Wyoming, United States. The skeleton is very similar to that of the modern Chinese crocodile lizard, Shinisaurus.
Afairiguana avius is an extinct iguanid lizard known from a nearly complete and articulated skeleton discovered in rocks of the Early Eocene-aged Green River Formation of Wyoming, United States. As of the initial description, the skeleton represents the oldest complete iguanian from the Western Hemisphere, and is the oldest representative of the extant iguanid family of anoles, Polychrotidae.
Ornithoprion is a genus of extinct cartilaginous fish in the family Caseodontidae. The only species, O. hertwigi, lived during the Moscovian stage of the Pennsylvanian, between 315.2 to 307 million years ago, and is known from black shale deposits in what is now the Midwestern United States. The discovery and description of Ornithoprion, performed primarily via radiography, helped clarify the skull anatomy of eugeneodonts; a group which includes O. hertwigi and which were previously known primarily from isolated teeth. The genus name, which is derived from the ancient Greek órnith- meaning 'bird' and príōn meaning 'saw', was inspired by the animal's vaguely bird-like skull and the saw-like appearance of the lower teeth. The species name honors Oscar Hertwig.
Calciavis is an extinct genus of bird from the Eocene of Wyoming. It is a lithornithid, a member of a lineage of flying palaeognaths, distantly related to modern ratites. Like many other fossils from the Green River Formation, its are exceptionally well preserved, bearing impressions of skin and feathers.
Lessiniabatis is an extinct genus of highly unusual stingray from the Early Eocene of Italy. It contains a single species, L. aenigmatica. It is known from three specimens, one nearly complete, from the famous Monte Bolca lagerstätte.