Camarasaurus lewisi Temporal range: Late Jurassic, | |
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Sacrum of holotype BYU 9047 | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | Saurischia |
Clade: | † Sauropodomorpha |
Clade: | † Sauropoda |
Clade: | † Macronaria |
Family: | † Camarasauridae |
Genus: | † Camarasaurus |
Species: | †C. lewisi |
Binomial name | |
†Camarasaurus lewisi (Jensen, 1988) McIntosh, 1990 | |
Synonyms | |
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Camarasaurus lewisi is a species of sauropod dinosaur from the Upper Jurassic of the United States. It was named by James A. Jensen in 1988. C. lewisi was originally placed in its own genus, Cathetosaurus, but in 1996 it was reclassified as a species of Camarasaurus ; most researchers since have considered it to be one of the four valid species of Camarasaurus. Two unpublished studies have since argued that the genus Cathetosaurus should be reinstated, whereas two other studies have argued that C. lewisi may be a junior synonym of another species of Camarasaurus.
C. lewisi is the smallest species assigned to Camarasaurus; despite representing a very old individual, the holotype specimen is roughly 26% smaller than C. supremus, with a humerus 101.8 centimetres (40.1 in) long. [1] [2] The possible C. lewisi specimen SMA 0002 also represents a fully mature individual, but is exceptionally small, with a humerus only 70.5 centimetres (27.8 in) long. [3] It is possible that the size difference reflects sexual dimorphism. Frank Seebacher estimated the length of C. lewisi as 15.4 metres (51 ft) and mass as 11.7 tonnes, [4] whereas Gregory S. Paul estimated the length of C. lewisi as 13 metres (43 ft) and mass as 10 tonnes. [5]
C. lewisi was relatively long-necked compared to most specimens of Camarasaurus. [6]
In 1996, six traits were indicated distinguishing C. lewisi from other species. The bifurcated vertebrae of the neck and back have a narrow but deep cleft incising the tops of the neural spines, resulting in a V-shaped transverse profile instead of the U-shaped profile typical of Camarasaurus species. The bifurcation continues to the sacrum, instead of ending in the middle of the back as is typical of Camarasaurus. The first sacral vertebra is more strongly "sacralised" and the fifth, last, sacral vertebra is less strongly sacralised than typical in Camarasaurus. The costal plate of the sacrum is more strongly developed than typical of Camarasaurus, even compared to very old individuals of these. The ilium is rotated to the front and below, relative to the longitudinal axis of the sacrum. In the rear chevrons the rear facets make a steep angle of 60° with the horizontal plane while the front facets are placed horizontally. [2] However, several of these characteristics may reflect the old age of the specimen, rather than distinctive characteristics of the species. It would then be a "ontogimorph". [7] Mateus and Tschopp proposed three diagnostic characteristics for C. lewisi present in the holotype: the pelvis is rotated anteriorly, such that the pubis projects posteroventrally, and the ischium projects posteriorly (1), lateroventrally projecting spurs in the neural spines of the last dorsals (2); and posterior cervical and anterior dorsal diapophyses bearing an anterior projection lateral to the prezygapophyses (3). [8]
The pelvis of C. lewisi is rotated forward relative to the sacrum, such that the preacetabular process of the ilium is oriented to point 20° below the axis of the sacrum. Jensen regarded this as one of the most distinctive characteristics of the taxon, and both McIntosh et al. and Mateus and Tschopp included it in their list of diagnostic characteristics for the taxon. [9] [2] [8] However, the condition in other species of Camarasaurus is not entirely clear. [10] In 1921, Osborn and Mook reconstructed the pelvis of C. supremus without the rotation. The condition is unclear in C. grandis, due to the lack of articulated pelves, but the disarticulated ilium of one specimen appears it would not exhibit such a strongly rotated condition. Specimens of C. lentus exhibit a rotated pelvis, but the precise angle is difficult to confirm due to distortion of the bones and may be less than in C. lewisi. [2]
The holotype of C. lewisi lacks a skull, but based on the specimen SMA 0002, which may belong to the species, the skull possesses several diagnostic characteristics: frontals with anterior midline projection into the nasals (1); trapezoidal supraoccipital (more expanded dorsally than ventrally) (2); lateral spur on the dorsal part of the lacrimal (3); fenestrated pterygoid (4); and the large pineal foramen between the frontals (5). [8]
The specimen SMA 0002, which may belong to C. lewisi, has unusual proportions. [8] [11] It has an exceptionally large skull, which is roughly 58% the length of the femur, leading to it being described as "bobbleheaded". [8] [11] Nearly all sauropodomorphs have a skull less than 50% of the length of the femur, but several Camarasaurus specimens of varying species possess such "bobbleheaded" proportions, which may be due to individual variation or sexual dimorphism. [11] The limbs are shorter in proportion to the body, particularly due to especially short lower limb elements, such that it has been described as "dachshund reminiscent". [8] [11] The ribs are long, extending below knee level. [8] Due to the length of the ribs and the rotation of the pelvis, the taxon would have had an atypically large gut volume. [8]
The holotype specimen of C. lewisi was discovered in 1967 by Vivian and Daniel Jones in Pit 1 of the Dominguez/Jones Quarry, near the confluence of the Little Dominguez Creek and the Big Dominguez Creek. [2] They warned James A. Jensen, the preparator of the Brigham Young University who collected the find. The specimen was found in the Brushy Basin Member of the Morrison Formation, in Mesa County, Colorado. [9] Jensen named and described it as a new genus and species, Cathetosaurus lewisi, in 1988. The genus name means "perpendicular lizard" (from Ancient Greek : κάθετος, romanized: káthetos, lit. 'perpendicular'), in reference to Jensen's hypothesis that the animal was adept at rearing onto its hind legs. The specific name honors Jensen's mentor Arnold David Lewis, the preparator of the Harvard Museum of Natural History.
When Jensen first named C. lewisi, he assigned it to a new genus of camarasaurid, Cathetosaurus. [9] In 1996, John S. McIntosh and colleagues synonymized Cathetosaurus with Camarasaurus, noting that most of the differences proposed by Jensen pertained to the maturity of the specimen, but retained C. lewisi as a distinct species; [2] this assignment was followed by later reviews of sauropod taxonomy. [12] [13] In 2005, Takehito Ikejiri noted that C. lewisi did not clearly differ from C. grandis, with which it was contemporary, and therefore may be synonymous with it. [1] Two unpublished studies, presented at the 2013 and 2014 annual meetings of the Society of Vertebrate Paleontology by Octávio Mateus and Emanuel Tschopp, reevaluated the taxonomy of Camarasaurus and concluded that Cathetosaurus should be regarded as a separate genus from Camarasaurus after all, [8] [14] though subsequent papers by Tschopp have included C. lewisi within Camarasaurus without comment, [15] [16] or expressed uncertainty over whether C. lewisi belonged to Camarasaurus or Cathetosaurus. [17] In 2017, Cary Woodruff and John Foster argued that most of the putative distinguishing traits of C. lewisi were indicative of old age, suggesting that C. lewisi may be based on an old individual of another Camarasaurus species. [7] Most researchers consider C. lewisi to be one of the four valid species of Camarasaurus. [17]
The holotype and only definite specimen of C. lewisi is BYU 9047 [lower-alpha 1] , a mostly complete specimen representing an old individual. [9] It consists of a partial skeleton lacking the skull, the still present occiput probably not having been collected due its poor quality. [2] It contains the vertebral column from the first neck vertebra onwards to the forty-third tail vertebra; neck ribs; twenty dorsal ribs; twenty-six chevrons; the right forelimb; the left pelvis and the right ischium. [2] According to Michael P. Taylor, as of 2022, the holotype of C. lewisi was one of only nine described sauropod specimens to preserve all of the cervical vertebrae, though not all the vertebrae are well-preserved. [18]
An unpublished study by Octávio Mateus and Emanuel Tschopp referred a second specimen, SMA 0002, to the species, but subsequent study has regarded the specimen as belonging to an indeterminate species of Camarasaurus. [19] [20] [21] The precise affinities of SMA 0002 remain uncertain; it is the geologically oldest Camarasaurus specimen and, despite representing a mature individual, is much smaller than most adult Camarasaurus specimens and may represent a distinct small species. [21] [3] [22] Another unpublished study by Tschopp, Mateus, and colleagues found a third specimen, GMNH-PV 101, to form a clade with SMA 0002 and the C. lewisi holotype. [14] GMNH-PV 101 had originally been described as a specimen of Camarasaurus grandis . [23]
Apatosaurus is a genus of herbivorous sauropod dinosaur that lived in North America during the Late Jurassic period. Othniel Charles Marsh described and named the first-known species, A. ajax, in 1877, and a second species, A. louisae, was discovered and named by William H. Holland in 1916. Apatosaurus lived about 152 to 151 million years ago (mya), during the late Kimmeridgian to early Tithonian age, and are now known from fossils in the Morrison Formation of modern-day Colorado, Oklahoma, New Mexico, Wyoming, and Utah in the United States. Apatosaurus had an average length of 21–23 m (69–75 ft), and an average mass of 16.4–22.4 t. A few specimens indicate a maximum length of 11–30% greater than average and a mass of approximately 33 t.
Supersaurus is a genus of diplodocid sauropod dinosaur that lived in North America during the Late Jurassic period. The type species, S. vivianae, was first discovered by Vivian Jones of Delta, Colorado, in the middle Morrison Formation of Colorado in 1972. The fossil remains came from the Brushy Basin Member of the formation, dating between 153 to 145 million years ago. It is among the longest dinosaurs ever discovered, with the three known specimens reaching 33–40 meters (108–131 ft) in length, with the largest individual possibly exceeding 40 meters (130 ft) in size. Mass estimates for the WDC and BYU specimens tend to be around 35–44 metric tons in body mass. A potential second species, S. lourinhanensis (Dinheirosaurus), is known from Portugal and has been dated to a similar time.
Camarasaurus was a genus of quadrupedal, herbivorous dinosaurs and is the most common North American sauropod fossil. Its fossil remains have been found in the Morrison Formation, dating to the Late Jurassic epoch, between 155 and 145 million years ago.
Haplocanthosaurus is a genus of intermediate sauropod dinosaur. Two species, H. delfsi and H. priscus, are known from incomplete fossil skeletons. It lived during the late Jurassic period, 155 to 152 million years ago. The type species is H. priscus, and the referred species H. delfsi was discovered by a young college student named Edwin Delfs in Colorado, United States. Haplocanthosaurus specimens have been found in the very lowest layer of the Morrison Formation, along with Hesperosaurus mjosi, Brontosaurus yahnahpin, and Allosaurus jimmadseni.
Brontosaurus is a genus of herbivorous sauropod dinosaur that lived in present-day United States during the Late Jurassic period. It was described by American paleontologist Othniel Charles Marsh in 1879, the type species being dubbed B. excelsus, based on a partial skeleton lacking a skull found in Como Bluff, Wyoming. In subsequent years, two more species of Brontosaurus were named: B. parvus in 1902 and B. yahnahpin in 1994. Brontosaurus lived about 156 to 146 million years ago (mya) during the Kimmeridgian and Tithonian ages in the Morrison Formation of what is now Utah and Wyoming. For decades, the animal was thought to have been a taxonomic synonym of its close relative Apatosaurus, but a 2015 study by Emmanuel Tschopp and colleagues found it to be distinct. It has seen widespread representation in popular culture, being the archetypal "long-necked" dinosaur in general media.
Diplodocoidea is a superfamily of sauropod dinosaurs, which included some of the longest animals of all time, including slender giants like Supersaurus, Diplodocus, Apatosaurus, and Amphicoelias. Most had very long necks and long, whip-like tails; however, one family are the only known sauropods to have re-evolved a short neck, presumably an adaptation for feeding low to the ground. This adaptation was taken to the extreme in the highly specialized sauropod Brachytrachelopan. A study of snout shape and dental microwear in diplodocoids showed that the square snouts, large proportion of pits, and fine subparallel scratches in Apatosaurus, Diplodocus, Nigersaurus, and Rebbachisaurus suggest ground-height nonselective browsing; the narrow snouts of Dicraeosaurus, Suuwassea, and Tornieria and the coarse scratches and gouges on the teeth of Dicraeosaurus suggest mid-height selective browsing in those taxa. This taxon is also noteworthy because diplodocoid sauropods had the highest tooth replacement rates of any vertebrates, as exemplified by Nigersaurus, which had new teeth erupting every 30 days.
Dicraeosauridae is a family of diplodocoid sauropods who are the sister group to Diplodocidae. Dicraeosaurids are a part of the Flagellicaudata, along with Diplodocidae. Dicraeosauridae includes genera such as Amargasaurus, Suuwassea, Dicraeosaurus, and Brachytrachelopan. Specimens of this family have been found in North America, Asia, Africa, and South America. In 2023, a dicraeosaurid fossil was discovered in India for the first time. Their temporal range is from the Early or Middle Jurassic to the Early Cretaceous. Few dicraeosaurids survived into the Cretaceous, the youngest of which was Amargasaurus.
Dinheirosaurus is a genus of diplodocid sauropod dinosaur that is known from fossils uncovered in modern-day Portugal. It may represent a species of Supersaurus. The only species is Dinheirosaurus lourinhanensis, first described by José Bonaparte and Octávio Mateus in 1999 for vertebrae and some other material from the Lourinhã Formation. Although the precise age of the formation is not known, it can be dated around the early Tithonian of the Late Jurassic.
Dystrophaeus is an extinct genus of sauropod dinosaur. Its type and only species is Dystrophaeus viaemalae, named by Edward Drinker Cope in 1877. Its fossils were found in the Tidwell Member of the Morrison Formation of Utah. Due to the fragmentary condition of its only known specimen, the affinities of Dystrophaeus are uncertain, although excavations carried out at the discovery site since 1989 have uncovered more of the original specimen and hold the potential for an improved understanding of the taxon.
Camarasauridae is a family of sauropod dinosaurs. Among sauropods, camarasaurids are small to medium-sized, with relatively short necks. They are visually identifiable by a short skull with large nares, and broad, spatulate teeth filling a thick jaw. Based on cervical vertebrae and cervical rib biomechanics, camarasaurids most likely moved their necks in a vertical, rather than horizontal, sweeping motion, in contrast to most diplodocids.
Camarasaurus grandis is an extinct species of sauropod dinosaur in the genus that lived during the Jurassic in what is now the western United States. It is the geologically oldest of the four species of the genus Camarasaurus.
Camarasaurus supremus is a species of sauropod dinosaur that lived during the Jurassic period in what is now the western United States. It is the type species of Camarasaurus, which also includes the species Camarasaurus grandis, Camarasaurus lentus, and Camarasaurus lewisi. C. supremus was discovered by the paleontologist Edward Drinker Cope in 1877, at the outset of the Bone Wars, a period of scientific competition between Cope and his rival Othniel Marsh. C. supremus is the largest and geologically youngest species in its genus, and was contemporary with several other exceptionally large dinosaurs, such as Saurophaganax and Maraapunisaurus. Despite being the first discovered species of Camarasaurus, C. supremus is relatively rare and poorly known.
Apatosaurinae is a subfamily of diplodocid sauropods, an extinct group of large, quadrupedal dinosaurs, the other subfamily in Diplodocidae being Diplodocinae. Apatosaurines are distinguished by their more robust, stocky builds and shorter necks proportionally to the rest of their bodies. Several fairly complete specimens are known, giving a comprehensive view of apatosaurine anatomy.
Camarasaurus lentus is an extinct species of sauropod dinosaur that lived during the Jurassic period in what is now the western United States. It is one of the four valid species of the well-known genus Camarasaurus. C. lentus fossils have been found in Wyoming, Colorado, and Utah. It is the species of Camarasaurus found in Dinosaur National Monument and the middle layers of the Morrison Formation. Camarasaurus lentus is among the best-known sauropod species, with many specimens known. A juvenile specimen of C. lentus, CM 11338, is the most complete sauropod fossil ever discovered.
Amphicoelias is a genus of herbivorous sauropod dinosaur that lived approximately 150 million years ago during the Tithonian of what is now Colorado, United States. Amphicoelias was moderately sized at about 18 metres (59 ft) in length and 15 metric tons in body mass, shorter than its close relative Diplodocus. Its hindlimbs were very long and thin, and its forelimbs were proportionally longer than in relatives.
Brachiosaurus is a genus of sauropod dinosaur that lived in North America during the Late Jurassic, about 154 to 150 million years ago. It was first described by American paleontologist Elmer S. Riggs in 1903 from fossils found in the Colorado River valley in western Colorado, United States. Riggs named the dinosaur Brachiosaurus altithorax; the generic name is Greek for "arm lizard", in reference to its proportionately long arms, and the specific name means "deep chest". Brachiosaurus is estimated to have been between 18 and 22 meters long; body mass estimates of the subadult holotype specimen range from 28.3 to 46.9 metric tons. It had a disproportionately long neck, small skull, and large overall size, all of which are typical for sauropods. Atypically, Brachiosaurus had longer forelimbs than hindlimbs, which resulted in a steeply inclined trunk, and a proportionally shorter tail.
Kaatedocus is a genus of flagellicaudatan sauropod known from the middle Late Jurassic of northern Wyoming, United States. It is known from well-preserved skull and cervical vertebrae which were collected in the lower part of the Morrison Formation. The type and only species is Kaatedocus siberi, described in 2012 by Emanuel Tschopp and Octávio Mateus.
Galeamopus is a genus of herbivorous diplodocid sauropod dinosaurs. It contains two known species: Galeamopus hayi, known from the Late Jurassic lower Morrison Formation of Wyoming, United States, and Galeamopus pabsti, known from the Late Jurassic fossils from Wyoming and Colorado. The type species is known from one of the most well preserved diplodocid fossils, a nearly complete skeleton with associated skull.
Vallibonavenatrix is a genus of spinosaurid dinosaur from the Early Cretaceous (Barremian) Arcillas de Morella Formation of Castellón, Spain. The type and only species is Vallibonavenatrix cani, known from a partial skeleton.
Ardetosaurus is an extinct genus of diplodocid sauropod dinosaurs from the Late Jurassic (Kimmeridgian) Morrison Formation of northern Wyoming, United States. The genus contains a single species, Ardetosaurus viator. It was first described in 2024 on the basis of a partial articulated skeleton, including vertebrae from the neck, back, and tail, hip bones, and part of the left hindlimb. The genus is a member of the Diplodocinae, a subfamily of large long-necked dinosaurs with whiplike tails. Ardetosaurus represents one of many distinct sauropod taxa that coexisted in this formation.
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