Amphicoelias

AmphicoeliasAmphicoelias altus
Pronounced	AM-fa-SEE-lee-us
Diet	Herbivore (Plant eater)
Name Means	"Both Concave"
Length	76 feet (23 m) / 200 feet (60 m)
Time	Late Jurassic - 155 million years ago
Location	SW United States

Amphicoelias (/ˌæmfᵻˈsiːliəs/, meaning "biconcave", from the Greek αμφι, amphi: "on both sides", and κοιλος, koilos: "hollow, concave") is a genus of herbivorous sauropod dinosaurthat includes what may be the largest dinosaur ever discovered, A. fragillimus. Based on surviving descriptions of a single fossil bone, A. fragillimus may have been the longest known vertebrate at 40–60 meters (131–196 ft) in length, and may have had a mass of up to 122 metric tons (135 short tons), rivaling the heaviest animal known, the Blue Whale. However, because the only fossil remains were lost at some point after being studied and described in the 1870s, evidence survives only in drawings and field notes.

However, A 2021 study found A. altus is not dubious, and thus, the genus is preserved.

Description

Restoration of A. altus

Henry Fairfield Osborn and Charles Craig Mook note close similarity between Amphicoelias and Diplodocus, but are differentiated from longer forelimbs, a long and slender femur with a round cross-section (though this has also been seen in some Diplodocus. They were of similar size. Amphicoelias vertebrae are incomplete, but anatomy is discernible. Centra are compressed in the middle of all dimensions, having a large lateral pleurocoel inside the large lateral fossa. The neural arch is tall, with a prominent lamina from the posterior centrum to the prezygapophyses. Behind the latter sits the diapophyes, which slightly project up and out, which is surrounded shallow fossae and a large lamina that reaches to the neural spine, which is thin. A pair of ridges sit along each edge, with the distal wider than the main spine; it is approximately subequal in length and width. Osborn and Mook (1921) referred a partial forelimb that is more robust than but overall resembles Diplodocus. The distal of the scapula is incomplete, but has a scapular blade expansion smaller than Camarasaurus but larger than Apatosaurus. The preserved element is 161 centimeters (63 inches) long, thicker than Diplodocus but not as thick as Camarasaurus. The coracoid is more similar to the former, being round and long rather than tall, also being thicker. The foramen is large and centered on the short axis. The ulna, more elongate than any Diplodocus, has prominent articular faces for the humerus and radius, tapering to the incomplete distal. The pubis is fragmentary, and all that is known is that it is long, thick and has a small surface where the ilium articulates. The femur is slender, with only the right known of the holotype; it is 1.524 meters (5 feet) long. This is slightly longer than Camarasaurus supremus, but less robust, being somewhat round in the cross section and 22 centimeters (8.7 inches) wide. Its shaft curves towards the hip articulation, straightening at the prominent articular condyles. A partial left feur was found in the American Museum of Natural History's collections, assigning it to the holotype (though it was not mentioned by Cope). Most of the upper segment is lost, but the shaft and end are similar to Cope's femur, possibly being of the same individual. A 2021 study found A. altus is not likely dubious, and thus, the genus is preserved.

The type species of Amphicoelias, A. altus, was named by paleontologist Edward Drinker Cope in December 1877 (though not published until 1878) for an incomplete skeleton consisting of two vertebrae, a pubis (hip bone), and a femur (upper leg bone). In 1921, Osborn and Mook assigned additional bones to A. altus--a scapula (shoulder blade), a coracoid (shoulder bone), an ulna (lower arm bone), and a tooth. Henry Fairfield Osborn and C.C. Mook noted the overall close similarity between Amphicoelias and Diplodocus, as well as a few key differences, such as proportionally longer forelimbs in Amphicoelias than in Diplodocus. The femur of Amphicoelias is unusually long, slender, and round in cross section; while this roundness was once thought to be another distinguishing characteristic of Amphicoelias, it has since been found in some specimens of Diplodocus as well. A. altus was also similar in size to Diplodocus, estimated to be about 25m (82 ft) long.

Cope also named a second species, A. fragillimus, in the same paper. However, all subsequent researchers have considered A. fragillimus to be a synonym of A. altus. Even by 1881 however, it was recognized that A. altus could not be distinguished from other genera, as the features described by Cope were misinterpreted and are widespread. In 1921, Osborn and Mook assigned additional bones to A. altus—a scapula (shoulder blade), a coracoid (shoulder bone), an ulna (lower arm bone), and a tooth. Henry Fairfield Osborn and Charles Craig Mook noted the overall close similarity between Amphicoelias and Diplodocus, as well as a few key differences, such as proportionally longer forelimbs in Amphicoelias than in Diplodocus. The dentition of Amphicoelias is homodont. Its teeth are shaped like long slender cylindrical rods, are spaced apart and project forward towards the front of the mouth. The femur of Amphicoelias is unusually long, slender, and round in cross section; while this roundness was once thought to be another distinguishing characteristic of Amphicoelias, it has since been found in some specimens of Diplodocus as well.

A. altus was also similar in size to Diplodocus, estimated to be about 25 meters (82 feet) long. While most scientists have used these details to distinguish Amphicoelias and Diplodocus as separate genera, at least one has suggested that Amphicoelias is probably the senior synonym of Diplodocus.

History

E.D. Cope's original sketch of Amphicoelias altus as an "amphibious lizard", c. 1897

Many fossils were discovered by Oramel William Licas (1877) in rocky outcrops close to Canyon City, with some named Laelaps trihedrodon, Camarasaurus supremus and Caulodon by Edward Drinker Cope, and assumed to be of the Cretaceous since other Laelaps occur there. Of these, some dorsal vertebrae, a pubis and a femur was found by Aaron Rply in Quarry XII. Cope received these on October 21, 1877, concluding they were sauropod in origin and named them A. altus in December 1877. He found it was related to Camarasaurus since they were both solid limbed, pneumatized vertebral behemoths. He then sold his collection to the American Museum of Natural History. Before he died, he worked with Charles R. Knight to create paleoart, based on his field notes. Based on Knight's reconstructions, he considered Amphicoelias and Brontosaurus synonyms with Camarasaurus supremus. It was then assigned AMNH 5764, and assigned more material. Osborn and Mook (1921) referred a forelimb to the holotype since it was found in the same strata not far from the type locality and differs from Camarasaurus. Due to uncertainty on this, Emanuel Tschopp et al. (2015) rejected the tooth, scapula and coracoid referred to AMNH 5764, but accepted the ulna.

1897 restoration of aquatic A. altus, by Charles R. Knight, based on Cope's original.

Cope lists amphicoelous vertebrae as a reason to erect amphicoeliidae, which was found to be intermediate and poorly-defined by Othniel Charles Marsh (1881); he used two mildly-concave articular faces to differentiate it, which was later found to be widespread in related sauropods. Thus, it was merged with diplodocidae.

In 1884 Cope's description of A. fragillimus has been met with skepticism, with some researchers noting that there were typographical errors in his measurements. For example, the measurement units are given in (obviously incorrect) centimeters rather than millimeters. Carpenter argued that there is every reason to take Cope at his word, noting that the paleontologist's reputation was at stake. The discovery took place during the Bone Wars, and Cope's rival Marsh, who was "ever ready to humiliate" Cope, never called the claims into question. Marsh was known to have employed spies to monitor Cope's discoveries, and may have even had confirmation of the enormous size of the Amphicoelias fragillimus bones. Paleontologists Henry Fairfield Osborn and C.C. Mook in 1921, as well as John S. McIntosh in 1998, also accepted Cope's data without question in published reviews.

Previously assigned species

Illustration of an outdated Amphicoelias altus skeletal mount

Edward Drinker Cope described his finds in two 1878 issues of the American Naturalist, and assigned them to the new genus Amphicoelias. He placed it in a unique family, Amphicoeliidae, though this is now considered a nomen oblitum (forgotten name). The genus is usually assigned to the family Diplodocidae, though some modern analyses have found it at the base of the larger group Diplodocoidea or as a diplodocid incertae sedis (uncertain placement). The first named species in the genus, Amphicoelias altus (holotype specimen AMHD 5764), was discovered by Cope in 1877. But while it is only represented by a partial skeleton, there are enough diagnostic characteristics to provisionally define the genus. A. altus is known from better remains, but is smaller than A. fragillimus. Cope also named a second species in 1878: Amphicoelias latus.

The third named Amphicoelias species, A. fragillimus, was known only from a single, incomplete 1.5 m tall neural arch (the part of a vertebra with spines and processes), either last or second to last in the series of back vertebrae, D (dorsal) 10 or D9. Based only on an illustration published in 1878, this vertebra would have measured 2.7 metres (8.9 ft) tall in life. However, it has been argued that the scale bar in the published description contained a typographical error, and the fossil vertebra was in fact only 1.38 metres (4.5 ft) tall. In addition to this vertebra, Cope's field notes contain an entry for an "[i]mmense distal end of femur”, located only a few tens of meters away from the giant vertebra. It is likely that this undescribed leg bone belonged to the same individual animal as the neural spine.

Three skeletons informally assigned to "A. brontodiplodocus" in 2010, now labelled as diplodocids in Lee Kong Chian Natural History Museum, Singapore

In 2010, a monograph was made available, but not formally published, by Henry Galiano and Raimund Albersdorfer in which they referred a fourth species to Amphicoelias, as "A. brontodiplodocus" based on several complete specimens found in the Dana Quarry of Big Horn Basin, Wyoming and held in a private collection. The specific name referred to their hypothesis based on these specimens that nearly all Morrison diplodocid species are either growth stages or represent sexual dimorphism among members of the genus Amphicoelias, but this analysis has been met with skepticism and the publication itself has been disclaimed by its lead author, explaining that it is "obviously a drafted manuscript complete with typos, etc., and not a final paper. In fact, no printing or distribution has been attempted".

Osborn and Mook, in 1921, provisionally synonymized the three species, sinking A. latus into Camarasaurus supremus, and suggesting also that A. fragillimus is just a very large individual of A. altus, a position which most subsequent studies, including McIntosh 1998, Foster (2007), and Woodruff and Foster (2015) have agreed with. Carpenter (2006) disagreed about the synonymy of A. altus and A. fragillimus, however, citing numerous differences in the construction of the vertebra also noted by Cope, and suggested these differences are enough to warrant a separate species or even a separate genus for A. fragillimus. However, he went on to caution that the validity of A. fragillimus as a separate species is nearly impossible to determine without the original specimen to study. Although Amphicoelias latus is clearly not Amphicoelias, it is probably synonymous with Camarasaurus grandis rather than C. supremus because it was found lower in the Morrison Formation and the deeply concave articular faces on the caudal vertebrae are more consistent with C. grandis.

The crumbling giant

Illustration of Amphicoelias fragillimus fossils, 1884

The gigantic bones attributed to A. fragillimus have often been ignored in summaries of the largest dinosaurs partly because, according to various subsequent reports, the whereabouts of both the vertebra and the femur are unknown, and all attempts to locate them have failed. Carpenter, in 2006, presented a possible scenario for the disappearance of the A. fragillimus specimens. As Cope noted in his description, the neural arch bone material was very fragile, and techniques to harden and preserve fossil bone had not yet been invented (Cope's rival, paleontologist O.C. Marsh, was the first to use such chemicals, in the early 1880s). Carpenter observed that the fossil bones known from the A. fragillimus quarry would have been preserved in deeply weathered mudstone, which tends to crumble easily and fragment into small, irregular cubes. Therefore, the bone may have crumbled badly and been discarded by Cope soon after he illustrated it in rear view for his paper (Carpenter suggested that this may explain why Cope drew the vertebra in only one view, rather than from multiple angles as he did for his other discoveries).

In 1994, an attempt was made to relocate the original quarry where A. fragillimus and other species had been found, using ground-penetrating radar in an attempt to image bones still buried in the ground. This attempt failed because the fossilized mudstone bones were the same density as the surrounding rock, making it impossible to differentiate the two. A study of the local topography also showed that the fossil-bearing rock strata was severely eroded, and probably was so at the time Lucas made his discovery of A. fragillimus, indicating that a majority of the skeleton was gone by the time the vertebra and femur were recovered.

Carpenter (2006) also noted that, due to the extraordinary size and mysterious disappearance of the fossil, Cope's description of A. fragillimus has been met with skepticism, with some people assuming that there were typographical errors in his measurements. Carpenter argued that there is every reason to take Cope at his word, noting that the paleontologist's reputation was at stake. The discovery took place during the Bone Wars, and Cope's rival Marsh, who was "ever ready to humiliate" Cope, never called the claims into question. Marsh was known to have employed spies to monitor Cope's discoveries, and may have even had confirmation of the enormous size of the Amphicoelias fragillimus bones. Paleontologists Henry Fairfield Osborn and C.C. Mook in 1921, as well as John S. McIntosh in 1998, also accepted Cope's data without question in published reviews.

However, studies in 2019 show this species did not belong to his diplodocid, but was from a rebbachisaurid. As such, it was given the name Maraapunisaurus.

Size

Original illustration of E.D. Cope's Amphicoelias fragillimus specimen

Size comparison of selected giant sauropod dinosaurs, Amphicoelias in red

Producing an estimate of the complete size of A. fragillimus requires scaling the bones of better known species of diplodocid (a family of extremely long and slender sauropods) in the assumption that their relative proportions were similar. In his original paper, Cope did this by speculating on the size of a hypothetical A. fragillimus femur (upper leg bone). Cope noticed that in other sauropod dinosaurs, specifically A. altus and Camarasaurus supremus, the femora were always twice as tall as the tallest dorsal vertebra, and estimated the size of an A. fragillimus femur to be 12 ft (3.7 m) tall. In 1994, using the related Diplodocus as a reference, Gregory S. Paul estimated a femur length of 3.1-4 m (10-13 ft) for A. fragillimus. The 2006 re-evaluation of A. fragillimus by Ken Carpenter also used Diplodocus as a scale guide, finding a femur height of 4.3-4.6 m (14-15 ft). Carpenter went on to estimate the complete size of A. fragillimus, though he cautioned that relative proportions in diplodocids could vary from species to species. Assuming the same proportions as the well-known Diplodocus, Carpenter presented an estimated total length of 58 m (190 ft), which he noted fell within the range presented by Paul in 1994 (40-60 m, or 131-196 ft). Carpenter pointed out that even the lowest length estimates for A. fragillimus were higher than those for other giant sauropods, such as the diplodocid Supersaurus (32.5 m, 107 ft), the brachiosaurid Sauroposeidon (34 m, 111 ft), and the titanosaur Argentinosaurus (30 m, 98 ft). Carpenter presented more speculative, specific proportions for A. fragillimus (again, based on a scaled-up Diplodocus), including a neck length of 16.75 m (55 ft), a body length of 9.25 m (30 ft), and a tail length of 32 m (105 ft). He estimated the total forelimb height at 5.75 m (19 ft) and hind limb height at 7.5 m (25 ft), and the overall height (at the highest point on the back) at 9.25 m (30 ft). By comparison the blue whale, which is on average the longest living creature, reaches 30-33 m (98-110 ft) in length.

While A. fragillimus was relatively thin, its enormous size still made it very massive. Weight is much more difficult to determine than length in sauropods, as the more complex equations needed are prone to greater margins of error based on smaller variations in the overall proportions of the animal. Carpenter used Paul's 1994 estimate of the mass of Diplodocus carnegii (11.5 tons) to speculate that A. fragillimus could have weighed up to 122.4 metric tons. The heaviest blue whale on record weighed about 195 tons, and the heaviest dinosaur known from reasonably good remains, the Argentinosaurus, weighed 80-100 tons, although if the size estimates can be validated, it would still be lighter than Bruhathkayosaurus, which is estimated to weigh 139 tons.

Classification

In 2007, John Foster suggested that the differences usually cited to differentiate Amphicoelias altus from the more well known Diplodocus are not significant and may be due to individual variation. Foster argued that Amphicoelias is probably the senior synonym of Diplodocus, and that if further research bears this out, the familiar name Diplodocus would need to be abandoned in favor of Amphicoelias, as was the case with Brontosaurus and its senior synonym Apatosaurus. In 2015, Woodruff and Foster reiterated this conclusion, stating that there is only one species of Amphicoelias and that it could be referred to Diplodocus as Diplodocus altus. They considered the name Amphicoelias to be a nomen oblitum. It has also been hypothesized that Amphicoelias should be considered an apatosaurine, and therefore should be placed in the subfamily Apatosaurinae.

The following cladogram of the Diplodocidae after Tschopp, Mateus, and Benson (2015) instead shows A. altus outside Diplodocinae.

Skeletal mount of potentially closely related Brontosaurus excelsus holotype YPM 1980

Diplodocidae	Amphicoelias  Apatosaurinae  Unnamed Apatosaurus ajax Apatosaurus louisae Brontosaurus excelsus Brontosaurus yahnahpin Brontosaurus parvus  Diplodocinae  Unnamed Tornieria Supersaurus lourinhanensis Supersaurus vivianae Leinkupal Galeamopus Diplodocus carnegii Diplodocus hallorum Kaatedocus Barosaurus

A 2021 analysis reassured that Amphicoelias was distinct, noting a much higher sauropod diversity in the Morrison than historically expected.

Paleobiology

In his 2006 re-evaluation, Carpenter examined the paleobiology of giant sauropods, including Amphicoelias, and addresses the question of why this group attained such a huge size. He pointed out that gigantic sizes were reached early in sauropod evolution, with very large sized species present as early as the late Triassic Period, and concluded that whatever evolutionary pressure caused large size was present from the early origins of the group. Carpenter cited several studies of giant mammalian herbivores, such as elephants and rhinoceros, which showed that larger size in plant-eating animals leads to greater efficiency in digesting food. Since larger animals have longer digestive systems, food is kept in digestion for significantly longer periods of time, allowing large animals to survive on lower-quality food sources. This is especially true of animals with a large number of 'fermentation chambers' along the intestine which allow microbes to accumulate and ferment plant material, aiding digestion. Throughout their evolutionary history, sauropod dinosaurs were found primarily in semi-arid, seasonally dry environments, with a corresponding seasonal drop in the quality of food during the dry season. The environment of Amphicoelias was essentially a savanna, similar to the arid environments in which modern giant herbivores are found, supporting the idea that poor-quality food in an arid environment promotes the evolution of giant herbivores. Carpenter argued that other benefits of large size, such as relative immunity from predators, lower energy expenditure, and longer life span, are probably secondary advantages.

Paleoenvironment restoration of a young diplodocid feeding on ferns

The Morrison Formation environment in which Amphicoelias lived would have resembled a modern savanna, though since grass did not appear until the Late Cretaceous, ferns were probably the dominant plant and main food source for Amphicoelias. Though Engelmann et al. (2004) dismissed ferns as a sauropod food source due to their relatively low caloric content, Carpenter argued that the sauropod digestive system, well adapted to handle low-quality food, allows for the consumption of ferns as a large part of the sauropod diet. Carpenter also noted that the occasional presence of large petrified logs indicate the presence of 20–30 m (66–98 ft) tall trees, which would seem to conflict with the savanna comparison. However, the trees are rare, and since tall trees require more water than the savanna environment could generally provide, they probably existed in narrow tracts or "gallery forests" along rivers and gulleys where water could accumulate. Carpenter speculated that giant herbivores like Amphicoelias may have used the shade of the gallery forests to stay cool during the day, and done most of their feeding on the open savanna at night.

Dinosaur Earth Description

Amphicoelias was the first long necked dinosaur that people got to see as it looked in life. In 1897 Professor Cope, who discovered this dinosaur, worked with famous dinosaur artist Charles Knight to help him create a drawing of a giant sauropod as it looked when it was alive. It was published in a magazine and people all over the world got their first look at a real Jurassic giant. Unfortunately for Professor Cope, many modern scientists think that this dinosaur is the same as Diplodocus and that the name should be changed. In fact, of more than 20 dinosaurs that Professor Cope named, only three of those names are still used today. There is one thing that very few people know about Amphicoelias. It may have been the largest animal to ever walk the Earth. One of the bones that Cope discovered was truly gigantic. However, it was only a single bone, and no other material from that individual dinosaur was ever found. To make things worse, the bone was somehow lost and all that exists is a single sketch that Cope made of the bone. If Cope's drawing is accurate, and there really is no reason to believe it isn't, the bone would have belonged to a dinosaur that was close to 200 feet long!

Gallery