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Brontosaurus
Temporal range: Late Jurassic (Kimmeridgian to Tithonian), 156.3–146.8 Ma
Holotype specimen of B. excelsus (YPM 1980), Peabody Museum of Natural History, as remounted in 2020
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Dinosauria
Clade: Saurischia
Clade: Sauropodomorpha
Clade: Sauropoda
Superfamily: Diplodocoidea
Family: Diplodocidae
Subfamily: Apatosaurinae
Genus: Brontosaurus
Marsh, 1879
Type species
Brontosaurus excelsus
Marsh, 1879
Other species
  • Brontosaurus parvus
    (Peterson & Gilmore, 1902)
  • Brontosaurus yahnahpin
    (Filla & Redman, 1994)
Synonyms
  • Elosaurus Peterson & Gilmore, 1902
  • Eobrontosaurus Bakker, 1998
Synonyms of B. excelsus
  • Brontosaurus amplus
    Marsh, 1881
  • Apatosaurus excelsus
    (Marsh, 1879) Riggs, 1903
  • Apatosaurus amplus
    (Marsh, 1881) Riggs, 1903
  • Atlantosaurus excelsus
    (Marsh, 1879) Steel, 1970
  • Atlantosaurus amplus
    (Marsh, 1881) Steel, 1970
Synonyms of B. parvus
  • Elosaurus parvus
    Peterson & Gilmore, 1902
  • Apatosaurus parvus
    (Peterson & Gilmore, 1902) Upchurch et al., 2004
Synonyms of B. yahnahpin
  • Apatosaurus yahnahpin
    Filla & Redman, 1994
  • Eobrontosaurus yahnahpin
    (Filla & Redman, 1994) Bakker, 1998

Brontosaurus (/ˌbrɒntəˈsɔːrəs/;[1][2] meaning "thunder lizard" from the Greek words βροντή, brontē "thunder" and σαῦρος, sauros "lizard") 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.

The anatomy of Brontosaurus is well known, with fossils demonstrating that it was large, long-necked, and quadrupedal with a long tail terminating in a whip-like structure. The cervical vertebrae are notably extremely robust and heavily-built, in contrast to its lightly built relatives Diplodocus and Barosaurus. The forelimbs were short and stout whereas the hindlimbs were elongated and thick, supported respectively by a heavily built shoulder girdle and pelvis. Several size estimates have been made, with the largest species B. excelsus reaching up to 21–23 m (69–75 ft) from head to tail and weighing in at 15–20 t (17–22 short tons), whereas the smaller B. parvus only got up to 19 m (62 ft) long. Juvenile specimens of Brontosaurus are known, with younger individuals growing rapidly to adult size in as little as 15 years.

Brontosaurus has been classified within the family Diplodocidae, which was a group of sauropods that had shorter necks and longer tails compared to other families like brachiosaurs and mamenchisaurs. Diplodocids first evolved in the Middle Jurassic but peaked in diversity during the Late Jurassic with forms like Brontosaurus before becoming extinct in the Early Cretaceous. Brontosaurus is a genus in the subfamily Apatosaurinae, which includes only it and Apatosaurus, which are distinguished by their firm builds and thick necks. Although Apatosaurinae was named in 1929, the group was not used validly until an extensive 2015 paper, which found Brontosaurus to be valid. However, the status of Brontosaurus is still uncertain, with some paleontologists still considering it a synonym of Apatosaurus.

Being from the Morrison Formation, Brontosaurus coexisted with a menagerie of other taxa such as the sauropods Diplodocus, Barosaurus, and Brachiosaurus; herbivorous ornithischians Stegosaurus, Dryosaurus, and Nanosaurus; as well as the carnivorous theropods Allosaurus, Marshosaurus and Ceratosaurus. This formation was a hotspot of sauropod biodiversity, with over 16 recognized genera, which resulted in niche partitioning between different sauropods.

History of discovery

[edit]
An 1896 diagram of the B. excelsus holotype skeleton by O.C. Marsh. The head is based on material now assigned to Brachiosaurus sp.

The discovery of a large and fairly complete sauropod skeleton was announced in 1879 by Othniel Charles Marsh, a professor of paleontology at Yale University. The specimen was collected from Morrison Formation rocks at Como Bluff, Wyoming by William Harlow Reed. He identified it as belonging to an entirely new genus and species, which he named Brontosaurus excelsus,[3] meaning "thunder lizard", from the Greek brontē/βροντη meaning "thunder" and sauros/σαυρος meaning "lizard",[4] and from the Latin excelsus, "noble" or "high".[5] By this time, the Morrison Formation had become the center of the Bone Wars, a fossil-collecting rivalry between Marsh and another early paleontologist, Edward Drinker Cope. Because of this, the publications and descriptions of taxa by Marsh and Cope were rushed at the time.[6] Brontosaurus excelsus' type specimen (YPM 1980) was one of the most complete sauropod skeletons known at the time, preserving many of the characteristic but fragile cervical vertebrae.[7] Marsh believed that Brontosaurus was a member of the Atlantosauridae, a clade of sauropod dinosaurs he named in 1877 that also included Atlantosaurus and Apatosaurus.[7] A year later in 1880, another partial postcranial Brontosaurus skeleton was collected near Como Bluff by Reed,[8][9] including well-preserved limb elements.[10] Marsh named this second skeleton Brontosaurus amplus ("large thunder lizard") in 1881,[9] but it was considered a synonym of B. excelsus in 2015.[10]

In August 1883, Marshall P. Felch collected a disarticulated partial skull (USNM V 5730) of a sauropod further south in the Felch Quarry at Garden Park, Colorado and sent the specimen to Yale.[11][12] Marsh referred the skull to B. excelsus,[11][13] later featuring it in a skeletal reconstruction of the B. excelsus type specimen in 1891[13] and the illustration was featured again in Marsh's landmark publication, The Dinosaurs of North America, in 1896.[7] At the Yale Peabody Museum, the skeleton of Brontosaurus excelsus was mounted in 1931 with a skull based on the Marsh reconstruction of the Felch Quarry skull.[14] While at the time most museums were using Camarasaurus casts for skulls, the Peabody Museum sculpted a completely different skull based on Marsh's recon.[14][11] Marsh's skull was inaccurate for several other reasons: it included forward-pointing nasals, something truly different to any other dinosaur, and fenestrae differing from the drawing and other skulls. The mandible was based on a Camarasaurus'.[14] In 1998, the Felch Quarry skull that Marsh included in his 1896 skeletal restoration was suggested to belong to Brachiosaurus instead[11] and this was supported in 2020 with a redescription of the brachiosaurid material found at the Felch Quarry.[12]

Second Dinosaur Rush and skull issue

[edit]
Obsolete mount of an apatosaurine referred to B. excelsus (specimen AMNH 460) with sculpted skull, completed in 1905, American Museum of Natural History

During a Carnegie Museum expedition to Wyoming in 1901, William Harlow Reed collected another Brontosaurus skeleton, a partial postcranial skeleton of a young juvenile (CM 566), including partial limbs. However, this individual was found intermingled with a fairly complete skeleton of an adult (UW 15556).[15] The adult skeleton specifically was very well-preserved, bearing many cervical (neck) and caudal (tail) vertebrae, and is the most complete definite specimen of the species.[10] The skeletons were granted a new genus and species name, Elosaurus parvus ("little field lizard"), by Olof A. Peterson and Charles Gilmore in 1902.[15] Both of the specimens came from the Brushy Basin Member of the Morrison Formation. The species was later transferred to Apatosaurus by several authors.[16][17] In 2008, a nearly complete postcranial skeleton of an apatosaurine was collected in Utah by crews working for Brigham Young University (BYU 1252-18531) where some of the remains are currently on display.[10] The skeleton is undescribed, but many of the features of the skeleton are shared with A. parvus.[10] The species was placed in Brontosaurus Tschopp et al. in 2015 during their comprehensive study of Diplodocidae.[18][10]

Infographic explaining the history of Brontosaurus and Apatosaurus according to Tschopp et al. 2015

In the 1903 edition of Geological Series of the Field Columbian Museum, Elmer Riggs argued that Brontosaurus was not different enough from Apatosaurus to warrant a separate genus, so he created the new combination Apatosaurus excelsus for it. Riggs stated that "In view of these facts the two genera may be regarded as synonymous. As the term 'Apatosaurus' has priority, 'Brontosaurus' will be regarded as a synonym".[19] Nonetheless, before the mounting of the American Museum of Natural History specimen, Henry Fairfield Osborn chose to label the skeleton "Brontosaurus", though he was a strong opponent of Marsh and his taxa.[14][20] In 1905, the American Museum of Natural History (AMNH) unveiled the first-ever mounted skeleton of a sauropod, a composite specimen (mainly made of bones from AMNH 460) that they referred to as Brontosaurus excelsus. The AMNH specimen was very complete, only missing the feet, from the specimen AMNH 592 were added to the mount, lower leg and shoulder bones, added from AMNH 222, and tail bones, added from AMNH 339.[21] To finish the mount, the rest of the tail was fashioned to appear as Marsh believed it should, which meant it had too few vertebrae. In addition, a sculpted model of what the museum felt the skull of this massive creature might have looked like was placed on the skeleton. This was not a delicate skull like that of Diplodocus, which would later turn out to be more accurate, but was based on "the biggest, thickest, strongest skull bones, lower jaws, and tooth crowns from three different quarries".[22][19][23][24] These skulls were likely those of Camarasaurus, the only other sauropod of which good skull material was known at the time. The mount construction was overseen by Adam Hermann, who failed to find Brontosaurus skulls. Hermann was forced to sculpt a stand-in skull by hand. Henry Fairfield Osborn noted in a publication that the skull was "largely conjectural and based on that of Morosaurus" (now Camarasaurus).[14]

In 1909, an Apatosaurus skull was found, during the first expedition to what would become the Carnegie Quarry at Dinosaur National Monument, led by Earl Douglass. The skull was found a few meters away from a skeleton (specimen CM 3018) identified as the new species Apatosaurus louisae. The skull was designated CM 11162 and was very similar to the skull of Diplodocus. It was accepted as belonging to the Apatosaurus specimen by Douglass and Carnegie Museum director William J. Holland, although other scientists, most notably Osborn, rejected this identification. Holland defended his view in 1914 in an address to the Paleontological Society of America, yet he left the Carnegie Museum mount headless. While some thought Holland was attempting to avoid conflict with Osborn, others suspected that Holland was waiting until an articulated skull and neck were found to confirm the association of the skull and skeleton.[14] After Holland's death in 1934, a cast of a Camarasaurus skull was placed on the mount by museum staff.[20]

Skull correction, resurgent discoveries, and reassessment

[edit]
The sculpted "Brontosaurus" skull of the Yale Peabody Museum mount, which was based on fossils Camarasaurus and Brachiosaurus

No apatosaurine skull was mentioned in the literature until the 1970s when John Stanton McIntosh and David Berman redescribed the skulls of Diplodocus and Apatosaurus in 1975.[24] They found that though he never published his opinion, Holland was almost certainly correct in that Apatosaurus and Brontosaurus had a Diplodocus-like skull.[24] According to them, many skulls long thought to belong to Diplodocus might instead be those of Apatosaurus.[24] They reassigned multiple skulls to Apatosaurus based on associated and closely associated vertebrae.[24] Though they supported Holland, Apatosaurus was falsely theorized to possibly have possessed a Camarasaurus-like skull, based on a disarticulated Camarasaurus-like tooth found at the precise site where an Apatosaurus specimen was found years before.[24] However, this tooth does not come from Apatosaurus.[25] On October 20, 1979, after the publications by McIntosh and Berman, the first skull of an Apatosaurus was mounted on a skeleton in a museum, that of the Carnegie.[20] In 1995, the American Museum of Natural History followed suit, and unveiled their remounted skeleton (now labelled Apatosaurus excelsus) with a corrected tail and a new skull cast from A. louisae.[21] In 1998, Robert T. Bakker referred a skull and mandible of an apatosaurine from Como Bluff to Brontosaurus excelsus (TATE 099-01), though the skull is still undescribed.[26] In 2011, the first specimen of Apatosaurus where a skull was found articulated with its cervical vertebrae was described. This specimen, CMC VP 7180, was found to differ in both skull and neck features from A. louisae, and the specimen was found to have a majority of features related to those of A. ajax.[27]

The Peabody Museum mount with new skull but in its original pose before its 2020 remounting

Another specimen of an Apatosaurine now referred to Brontosaurus was discovered in 1993 by the Tate Geological Museum, also from the Morrison Formation of central Wyoming. The specimen consisted of a partial postcranial skeleton, including a complete manus and multiple vertebrae, and was described by James Filla and Pat Redman a year later.[26] Filla and Redman named the specimen Apatosaurus yahnahpin ("yahnahpin-wearing deceptive lizard"), but Robert T. Bakker gave it the genus name Eobrontosaurus in 1998.[26] Bakker believed that Eobrontosaurus was the direct predecessor to Brontosaurus,[26] although Tschopp et al.'s phylogenetic analysis placed B. yahnahpin as the basalmost species of Brontosaurus.[10]

Almost all 20th-century paleontologists agreed with Riggs that all Apatosaurus and Brontosaurus species should be classified in a single genus. According to the rules of the ICZN, which governs the scientific names of animals, the name Apatosaurus, having been published first, had priority; Brontosaurus was considered a junior synonym and was therefore discarded from formal use.[28][29][30][31] Despite this, at least one paleontologist—Robert T. Bakker—argued in the 1990s that A. ajax and A. excelsus are sufficiently distinct that the latter continues to merit a separate genus.[26] In 2015, an extensive study of diplodocid relationships by Emanuel Tschopp, Octavio Mateus, and Roger Benson concluded that Brontosaurus was indeed a valid genus of sauropod distinct from Apatosaurus. The scientists developed a statistical method to more objectively assess differences between fossil genera and species and concluded that Brontosaurus could be "resurrected" as a valid name. They assigned two former Apatosaurus species, A. parvus, and A. yahnahpin, to Brontosaurus, as well as the type species B. excelsus.[10] The publication was met with some criticism from other paleontologists, including Michael D'Emic,[32] Donald Prothero, who criticized the mass media reaction to this study as superficial and premature,[33] and many others below. Some paleontologists, such as John and ReBecca Foster, continue to consider Brontosaurus as a synonym of Apatosaurus.[34][35]

Description

[edit]
Comparison of three specimens and a human: Oklahoma specimen of Apatosaurus ajax (orange), A. louisae (red), and Brontosaurus parvus (green)

Brontosaurus was a large, long-necked, quadrupedal animal with a long, whip-like tail, and forelimbs that were slightly shorter than its hindlimbs. The largest species, B. excelsus, measured up to 21–23 m (69–75 ft) long from head to tail and weighed up to 15–20 t (17–22 short tons); other species were smaller, measuring 19 m (62 ft) long and weighing 14 t (15 short tons).[36][37][38]

Skull and vertebrae

[edit]

Although the skull of Brontosaurus has not been found, it was probably similar to the skull of the closely related Apatosaurus. Several skulls of Apatosaurus have been found, all of which are very small in proportion to the body. Their snouts were squared off and low, in contrast to those of macronarians.[39] Jaws of Apatosaurus and other diplodocids were lined with spatulate (chisel-like) teeth which were adapted for herbivory.[25][27]

A cervical (top) and dorsal vertebra (bottom) of B. excelsus

Like those of other diplodocids, the vertebrae of the neck were deeply bifurcated on the dorsal side; that is, they carried paired spines, resulting in a wide and deep neck.[40] The spine and tail consisted of 15 cervicals, ten dorsals, five sacrals, and about 82 caudals, based on Apatosaurus. The number of caudal vertebrae has been noted to vary, even within a species. Vertebrae in the neck, torso, and sacrum of sauropods bore large pneumatic foramina on their lateral sides.[9] These are used to lighten the bones which aided in keeping the animal lighter. Within the vertebrae as well, smooth bone walls in addition to diverticula would make pockets of air to keep the bones light.[41] Similar structures are observable in birds and large mammals.[42] The cervical vertebrae were stouter than those of other diplodocids, as in Apatosaurus. On the lateral sides of the cervicals, apatosaurines had well-developed and thick parapophyses (extensions on the lateral sides of the vertebrae that attached to cervical ribs) which would point ventrally under the centrum. These parapophyses in conjunction with dense diapophyses and cervical ribs were strong anchors for neck muscles, which could sustain extreme force.[43] The cervicals were also more boxy than in other sauropods due to their truncated zygapophyses and tall build.[44][10] These vertebrae are triangular in anterior view, whereas they most often are rounded or square in genera like Camarasaurus. Despite its pneumaticy, the neck of Brontosaurus is thought to have been double the mass of that of other diplodocids due to the former's sturdiness.[43] Brontosaurus differs from Apatosaurus in that the base of the posterior dorsal vertebrae's neural spines are longer than they are wide. The cervicals of species within Brontosaurus also vary, such as the lack of tubercules on the neural spines of B. excelsus and the lateral expansion of unbifurcated neural spines in B. parvus.[10]

Its dorsal vertebrae had short centra with large fossae (shallow excavations) on their lateral sides, though not as extensively as the cervicals'.[45] Neural canals, which contain the spinal cord of the vertebral column, are ovate and large in the dorsals. The diapophyses protrude outward and curve downward in a hook-shape. Neural spines are thick in anterior-posterior view with a bifurcate top.[10] The neural spines of the dorsals would increase in height further towards the tail, creating an arched back. Apatosaurine neural spines compose more than half the height of the vertebrae. Medial surfaces of neural spines are gently rounded in B. yahnahpin, whereas in other B. spp. they are not.[10] The dorsal ribs are not fused or tightly attached to their vertebrae, instead being loosely articulated.[22] Ten dorsal ribs are on either side of the body.[19] Expanded excavations within the sacrum are present making it into a hollow cylinder-shape. Sacral neural spines are fused together into a thin plate. The posteriormost caudal vertebra was lightly fused to the sacral vertebrae, becoming part of the plate. Internally, the neural canal was enlarged.[46][47][19] The shape of the tail was typical of diplodocids, being comparatively slender, due to the vertebral spines rapidly decreasing in height the farther they are from the hips. As in other diplodocids, the last portion of the tail of Brontosaurus possessed a whip-like structure.[22] The tail also bears an extensive air-sac system to lighten its weight, as observed in specimens of B. parvus.[48][49]

Limbs

[edit]
Restoration of B. excelsus

Several scapulae are known from Brontosaurus, all of which are long and thin with relatively elongated shafts.[46] One of the traits that distinguishes Brontosaurus and Apatosaurus is the presence of a depression on the posterior face of the scapula, which the latter lacks. The scapula of Brontosaurus also has a rounded extension off of its edge, a characteristic unique to Brontosaurus among Apatosaurinae.[10] The coracoid anatomy is closely akin to that of Apatosaurus, with a quadratic outline in dorsal view. Sterna have been preserved in some specimens of Brontosaurus, which display an oval outline.[9] The hip bones include robust ilia and the fused pubes and ischia. The limb bones were also very robust,[50] with the humerus resembling that of Camarasaurus, and those of B. excelsus being nearly identical to those of Apatosaurus ajax. The humerus had a thin bone shaft and larger transverse ends. Its anterior end bears a large deltopectoral crest, which was on the extremities of the bone.[51]

Left front limb of B. yahnahpin, Morrison Natural History Museum

Charles Gilmore in 1936 noted that previous reconstructions erroneously proposed that the radius and ulna could cross, when in life they would have remained parallel.[22] Brontosaurus had a single large claw on each forelimb which faced towards the body, whereas the rest of the phalanges lacked unguals.[52] Even by 1936, it was recognized that no sauropod had more than one hand claw preserved, and this one claw is now accepted as the maximum number throughout the entire group.[22][53] The metacarpals are elongated and thinner than the phalanges, bearing boxy articular ends on its proximal and distal faces.[7] The single front claw bone is slightly curved and squarely shortened on the front end. The phalangeal formula is 2-1-1-1-1, meaning the innermost finger (phalanx) on the forelimb has two bones and the next has one. The single manual claw bone (ungual) is slightly curved and squarely truncated on the anterior end. Proportions of the manus bones vary within Apatosaurinae as well, with B. yahnahpin's ratio of longest metacarpal to radius length around 0.40 or greater compared to a lower value in Apatosaurus louisae.[10] The femora of Brontosaurus are very stout and represent some of the most robust femora of any member of Sauropoda. The tibia and fibula bones are different from the slender bones of Diplodocus but are nearly indistinguishable from those of Camarasaurus. The fibula is longer and slenderer than the tibia. The foot of Brontosaurus has three claws on the innermost digits; the digit formula is 3-4-5-3-2. The first metatarsal is the stoutest, a feature shared among diplodocids.[22] B. excelsus's astragalus differs from other species in that it lacks a laterally directed ventral shelf.[10]

Classification

[edit]

Brontosaurus is a member of the family Diplodocidae, a clade of gigantic sauropod dinosaurs. The family includes some of the longest and largest creatures ever to walk the earth, including Diplodocus, Supersaurus, and Barosaurus. Diplodocids first evolved during the Middle Jurassic in what is now Georgia, spreading to North America during the Late Jurassic.[54] Brontosaurus is classified in the subfamily Apatosaurinae, which also includes Apatosaurus and possibly one or more unnamed genera.[10] Othniel Charles Marsh described Brontosaurus as being allied to Atlantosaurus, within the now defunct group Atlantosauridae.[19][55] In 1878, Marsh raised his family to the rank of suborder, including Apatosaurus, Brontosaurus, Atlantosaurus, Morosaurus (=Camarasaurus), and Diplodocus. He classified this group within Sauropoda. In 1903, Elmer S. Riggs mentioned that the name Sauropoda would be a junior synonym of earlier names, and grouped Apatosaurus within Opisthocoelia.[19] Most authors still use Sauropoda as the group name.[17]

Originally named by its discoverer Othniel Charles Marsh in 1879, Brontosaurus had long been considered a junior synonym of Apatosaurus; its type species, Brontosaurus excelsus, was reclassified as A. excelsus in 1903. However, an extensive study published in 2015 by a joint British-Portuguese research team concluded that Brontosaurus was a valid genus of sauropod distinct from Apatosaurus.[10][56][57] Nevertheless, not all paleontologists agree with this division.[58][33] The same study classified two additional species that had once been considered Apatosaurus and Eobrontosaurus as Brontosaurus parvus and Brontosaurus yahnahpin respectively.[10]

Cladogram of the Diplodocidae after Tschopp, Mateus, and Benson (2015):[10]

Diplodocidae

Species

[edit]
  • Brontosaurus excelsus, the type species of Brontosaurus, was first named by Marsh in 1879. Many specimens have been assigned to the species, such as FMNH P25112, the skeleton mounted at the Field Museum of Natural History, which has since been found to represent an unknown species of apatosaurine. Brontosaurus amplus, is a junior synonym of B. excelsus. B. excelsus therefore only includes its type specimen and the type specimen of B. amplus.[10][17] The largest of these specimens is estimated to have weighed up to 15 tonnes and measured up to 22 m (72 ft) long from head to tail.[36] The known definitive B. excelsus fossils have been reported from Reed's Quarries 10 and 11 of the Morrison Formation Brushy Basin member in Albany County, Wyoming, dated to the late Kimmeridgian age,[10][31] about 152 million years ago.
  • Brontosaurus parvus, first described as Elosaurus in 1902 by Peterson and Gilmore, was reassigned to Apatosaurus in 1994, and to Brontosaurus in 2015. Specimens assigned to this species include the holotype, CM 566 (a partial skeleton of a juvenile found in Sheep Creek Quarry 4 in Albany County, WY), BYU 1252-18531 (a nearly complete skeleton found in Utah and mounted at Brigham Young University), and the partial skeleton UW 15556. It dates to the middle Kimmeridgian.[17] Adult specimens are estimated to have weighed up to 14 tonnes and measured up to 22 m (72 ft) long from head to tail.[36]
  • Brontosaurus yahnahpin is the oldest species, known from a single site from the lower Morrison Formation, Bertha Quarry, in Albany County, Wyoming, dating to about 155 million years ago.[59][60] It grew up to 21 m (69 ft) long.[61] It was described by James Filla and Patrick Redman in 1994 as a species of Apatosaurus (A. yahnahpin).[62] The specific name is derived from Lakota mah-koo yah-nah-pin, "breast necklace", a reference to the pairs of sternal ribs that resemble the hair pipes traditionally worn by the tribe. The holotype specimen is TATE-001, a relatively complete postcranial skeleton found in the lower Morrison Formation of Wyoming. More fragmentary remains have also been referred to the species. A re-evaluation by Robert T. Bakker in 1998 found it to be more primitive, so Bakker coined the new generic name Eobrontosaurus, derived from Greek eos, "dawn", and Brontosaurus.[26]
Skeleton of the AMNH apatosaurine (possibly B. excelsus, specimen AMNH 460) as remounted in 1995

The cladogram below is the result of an analysis by Tschopp, Mateus, and Benson (2015). The authors analyzed most diplodocid type specimens separately to deduce which specimen belonged to which species and genus.[10]

Apatosaurinae

YPM 1840 ("Atlantosaurus" immanis type)

NSMT-PV 20375

AMNH 460

Apatosaurus
Apatosaurus ajax

YPM 1860 (Apatosaurus ajax type)

Apatosaurus louisae

CM 3018 (Apatosaurus louisae type)

YPM 1861 (Apatosaurus laticollis type)

Brontosaurus
Brontosaurus excelsus

YPM 1980 (Brontosaurus excelsus type)

YPM 1981 (Brontosaurus amplus type)

AMNH 5764 (Amphicoelias altus type)

FMNH P25112

Brontosaurus yahnahpin

Tate-001 (Eobrontosaurus yahnahpin type)

Brontosaurus parvus

CM 566 (Elosaurus parvus type)

UM 15556

BYU 1252-18531

Paleobiology

[edit]
Restoration of a B. excelsus group

When Brontosaurus was described in 1879, the widespread notion in the scientific community was that sauropods were semi-aquatic, lethargic reptiles that were inactive.[63][3][7] In Othniel Marsh's publication The Dinosaurs of North America, he described the dinosaur as "more or less amphibious, and its food was probably aquatic plants or other succulent vegetation".[7] This is unsupported by fossil evidence. Instead, sauropods were active and had adaptations for dwelling on land.[28] Marsh also noted the animal's supposed lack of intellect based on the small braincase of the Felch Quarry skull and slender neural cord. Recent research has found signs of intelligence in dinosaurs, akin to modern birds, though sauropods had relatively small brains.[64]

Various uses for the single claw on the forelimb of sauropods have been proposed. One suggestion is that they were used for defense, but their shape and size make this unlikely. It was also possible they were for foraging, but the most probable use for the claw was grasping objects such as tree trunks when rearing.[53]

Trackways of sauropods like Brontosaurus show that the average range for them was around 20–40 km (10–25 mi) per day, and they could potentially reach a top speed of 20–30 km/h (12–19 mph).[65] The slow locomotion of sauropods may be due to the minimal muscling or recoil after strides.[66] A possible bipedal trackway of a juvenile Apatosaurus is known, but it is disputed if it was possible for the sauropod.[67]

Diet and energy requirements

[edit]

Being a diplodocid sauropod, Brontosaurus was herbivorous and fed on ferns, cycadeoids, seed ferns, and horsetails, eating at ground height as a nonselective browser.[39] The replacement method and physiology of Apatosaurus's teeth is unique, with the entire tooth row being replaced at once and up to 60% more often than Diplodocus. The teeth of Apatosaurus are thick, lack denticles, and are strongly cylindrical in cross-section whereas they are long, slender, and elliptical in cross-section in Diplodocus. These characteristics imply that Apatosaurus, and likely Brontosaurus, consumed tougher vegetation than Diplodocus.[25] Diplodocids in general also have shorter necks than the long-necked, vertically inclined macronarians. This would result in niche partitioning, the various taxa thus avoiding direct competition with each other due to feeding on different plants and at different heights.[68] Hypotheses of the food requirements of Brontosaurus have been made, though predicting this is difficult due to the lack of modern analogues.[69] Endotherms (mammals) and ectotherms (reptiles) require a specific amount of nutrition to survive which correlates with their metabolism as well as body size. Estimations of the dietary necessities of Brontosaurus were made in 2010, with a guess of 2•10^4 to 50•10^4 kilojoules needed daily. This led to hypotheses on the distributions of Brontosaurus to meet this requirement, though they varied on whether it was an ectotherm or endotherm. If Brontosaurus was an endotherm, fewer adult individuals could be sustained than if it were an ectotherm, which could have tens of animals per square kilometer.[70][71] Due to this, it has been theorized that Brontosaurus and other sauropods living within the arid environment of the Morrison Formation participated in migrations between feeding sites.[69] James Farlow (1987) calculates that a Brontosaurus-sized dinosaur about 35 t (34 long tons; 39 short tons) would have possessed 5.7 t (5.6 long tons; 6.3 short tons) of fermentation contents.[72] Assuming Apatosaurus had an avian respiratory system and a reptilian resting-metabolism, Frank Paladino et al. (1997) estimate the animal would have needed to consume only about 262 liters (58 imp gal; 69 U.S. gal) of water per day.[73]

Posture

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Cast of B. parvus specimen UWGM 15556 at Tellus Science Museum

Historically, sauropods like Brontosaurus were believed to have been too massive to support their weight on dry land, so theoretically, they must have lived partly submerged in water, perhaps in swamps. Recent findings do not support this, and sauropods are thought to have been fully terrestrial animals.[74] Diplodocids like Brontosaurus are often portrayed with their necks held high up in the air, allowing them to browse on tall trees. Though some studies have suggested that diplodocid necks were less flexible than previously believed,[75] other studies have found that all tetrapods appear to hold their necks at the maximum possible vertical extension when in a normal, alert posture, and argue that the same would hold true for sauropods barring any unknown, unique characteristics that set the soft tissue anatomy of their necks apart from that of other animals.[76]

Physiology

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Pneumatic fossa in a caudal vertebra of the B. excelsus holotype

James Spotila et al. (1991) suggest that the large body size of Brontosaurus and other sauropods would have made them unable to maintain high metabolic rates, as they would not be able to release enough heat. However, temperatures in the Jurassic were 3 degrees Celsius higher than present.[77] Furthermore, they assumed that the animals had a reptilian respiratory system. Matt Wedel found that an avian system would have allowed them to dump more heat.[78] Some scientists have also argued that the heart would have had trouble sustaining sufficient blood pressure to oxygenate the brain.[74]

Given the large body mass and long neck of sauropods like Brontosaurus, physiologists have encountered problems determining how these animals breathed. Beginning with the assumption that, like crocodilians, Brontosaurus did not have a diaphragm, the dead-space volume (the amount of unused air remaining in the mouth, trachea, and air tubes after each breath) has been estimated at 0.184 m3 (184 L) for a 30 t (30 long tons; 33 short tons) specimen. Paladino calculates its tidal volume (the amount of air moved in or out during a single breath) at 0.904 m3 (904 L) with an avian respiratory system, 0.225 m3 (225 L) if mammalian, and 0.019 m3 (19 L) if reptilian.[73]

Based on this, its respiratory system would likely have consisted of parabronchi, with multiple pulmonary air sacs as in avian lungs, and a flow-through lung. An avian respiratory system would need a lung volume of about 0.60 m3 (600 L) compared with a mammalian requirement of 2.95 m3 (2,950 L), which would exceed the space available. The overall thoracic volume of the same-sized Apatosaurus has been estimated at 1.7 m3 (1,700 L), allowing for a 0.50 m3 (500 L), four-chambered heart and a 0.90 m3 (900 L) lung capacity. That would allow about 0.30 m3 (300 L) for the necessary tissue.[73] Evidence for the avian system in Brontosaurus and other sauropods is also present in the pneumaticity of the vertebrae. Though this plays a role in reducing the weight of the animal, Wedel (2003) states they are also likely connected to air sacs, as in birds.[78]

Juveniles

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Reconstructed skeleton of a juvenile B. parvus (type specimen CM 566), Carnegie Museum of Natural History

A 1999 microscopic study of Apatosaurus and Brontosaurus bones concluded the animals grew rapidly when young and reached near-adult sizes in about 10 years.[79][80] In 2008, a study on the growth rates of sauropods was published by biologists Thomas Lehman and Holly Woodward. They said that by using growth lines and length-to-mass ratios, Apatosaurus would have grown to 25 t (25 long tons; 28 short tons) in 15 years, with growth peaking at 5,000 kg (11,000 lb) in a single year. An alternative method, using limb length and body mass, found Brontosaurus and Apatosaurus grew 520 kg (1,150 lb) per year, and reached their full mass before it was about 70 years old.[81] These estimates have been called unreliable because the calculation methods are not sound; old growth lines would have been obliterated by bone remodeling.[82] One of the first identified growth factors of Apatosaurus was the number of sacral vertebrae, which increased to five by the time of the creature's maturity. This was first noted in 1903 and again in 1936.[22][19]

Juvenile Brontosaurus material is known based on the type specimen of B. parvus. The material of this specimen, CM 566, includes vertebrae from various regions, one pelvic bone, and some bones of the hindlimb.[17] When describing B. parvus, Peterson and Gilmore noted that the neural spines were sutured, the sacral vertebrae were unfused, and the coracoid was missing. All of these features are signs of immaturity in other archosaurs, showing that sauropods had these traits too.[15] Peterson and Gilmore also theorized that sauropods never stopped growing, which supposedly helped in attaining their massive size, a concept unsupported by fossils.[83]

Tail

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The estimated tail length of Brontosaurus is approximately 56% of the total body length, with the tail sometimes hypothesized to be capable of functioning like a very long, tapering bullwhip.[84] An article that appeared in the November 1997 issue of Discover magazine reported research into the mechanics of diplodocid tails by Nathan Myhrvold, a computer scientist at Microsoft. Myhrvold carried out a computer simulation of the tail, which in diplodocids like Brontosaurus was a very long, tapering structure resembling a [bullwhip. This computer modeling suggested that sauropods were capable of producing a whip-like cracking sound of over 200 decibels, comparable to the volume of a cannon.[85] There is some circumstantial evidence supporting this as well: a number of diplodocids have been found with fused or damaged tail vertebrae, which may be a symptom of cracking their tails: these are particularly common between the 18th and the 25th caudal vertebra, a region the authors consider a transitional zone between the stiff muscular base and the flexible whiplike section.[86]

However, Rega (2012) notes that Camarasaurus while lacking a tailwhip, displays a similar level of caudal co-ossification and that Mamenchisaurus while having the same pattern of vertebral metrics, lacks a tailwhip and does not display fusion in any "transitional region". Also, the crush fractures which would be expected if the tail was used as a whip have never been found in diplodocids.[87] More recently, Baron (2020) has considered the use of the tail as a bullwhip unlikely because of the potentially catastrophic muscle and skeletal damage such speeds could cause on the large and heavy tail. Instead, he proposes that the tails might have been used as a tactile organ to keep in touch with the individuals behind and to the sides of the animal in a group, which could have augmented cohesion and allowed communication among individuals while limiting more energetically demanding activities like stopping to search for dispersed individuals, turning to visually check on others behind, or communicating vocally.[84]

Neck combat

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Cervical vertebra of Brontosaurus excelsus.
A cervical vertebra of B. excelsus, showing its robusticity

The cervical vertebrae of Brontosaurus and Apatosaurus are robust, which has led to speculation on the use of these structures. These structures had expensive energy requirements, so the reason for their evolution must have been important to the animal. Notable features include dense cervical ribs and diapophyses, ribs that are angled ventrally, and an overall subtriangular cross-section. These traits are in contrast to the more fragile cervicals of diplodocines.[88] Cervical ribs acted as anchors for the longus colli ventralis and flexer colli lateralis muscles, which are used in the downward motion of the neck. Stronger muscles for ventral motions allowed more force to be exerted downward. The cervical ribs formed a "V"-shape, which could be used to shelter the softer underlying tissues of the neck from damage. Ventral sides of the cervical ribs were capped by round, protruding processes. These have been suggested to have been attachment points for bosses or keratinous spikes. A preprint by Wedel et al (2015) thought that due to the combination of these traits, Brontosaurus would use its neck for combat between individuals through the use of striking necks.[43][89] Behavior like this has been observed in other animals like giraffes and large tortoises.[90][91]

Paleoecology

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Allosaurus mounted as if feeding on a Brontosaurus carcass, AMNH

The Morrison Formation is a sequence of shallow marine and alluvial sediments which, according to radiometric dating, ranges between 156.3 million years old (Mya) at its base,[92] and 146.8 Mya at the top,[93] which places it in the late Oxfordian, Kimmeridgian, and early Tithonian stages of the Late Jurassic period. This formation is interpreted as a semi-arid environment with distinct wet and dry seasons. The Morrison Basin, where dinosaurs lived, stretched from New Mexico to Alberta and Saskatchewan and was formed when the precursors to the Front Range of the Rocky Mountains started pushing up to the west. The deposits from their east-facing drainage basins were carried by streams and rivers and deposited in swampy lowlands, lakes, river channels, and floodplains.[94] This formation is similar in age to the Lourinhã Formation in Portugal and the Tendaguru Formation in Tanzania.[95]

Brontosaurus may have been a more solitary animal than other Morrison Formation dinosaurs.[96] As a genus, Brontosaurus existed for a long interval, and was found in most levels of the Morrison. B. excelsus fossils have been reported from only the Brushy Basin Member, dating to the late Kimmeridgian age, about 151 Mya.[60] Older Brontosaurus remains have also been identified from the middle Kimmeridgian, and are assigned to B. parvus.[17] Fossils of these animals have been found in Nine Mile Quarry and Bone Cabin Quarry in Wyoming and at sites in Colorado, Oklahoma, and Utah, present in stratigraphic zones 2–6 according to John Foster's model.[97]

The Morrison Formation records an environment and time dominated by gigantic sauropod dinosaurs.[97] Dinosaurs known from the Morrison include the theropods Ceratosaurus, Ornitholestes, and Allosaurus, the sauropods Apatosaurus, Brachiosaurus, Camarasaurus, and Diplodocus, and the ornithischians Camptosaurus, Dryosaurus, and Stegosaurus.[98] Other vertebrates that shared this paleoenvironment included ray-finned fishes, frogs, salamanders, turtles, sphenodonts, lizards, terrestrial and aquatic crocodylomorphs, and several species of pterosaurs. Shells of bivalves and aquatic snails, are also common. The flora of the period has been revealed by fossils of green algae, mosses, horsetails, cycads, ginkgoes, and several families of conifers. Vegetation varied from river-lining forests of tree ferns and ferns (gallery forests), to fern savannas with occasional trees such as the Araucaria-like conifer Brachyphyllum.[99]

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Outdated 1897 restoration by Charles R. Knight of B. excelsus submerged in water, and Diplodocus dragging its tail

The length of time taken for Riggs's 1903 reclassification of Brontosaurus as Apatosaurus to be brought to public notice, as well as Osborn's insistence that the Brontosaurus name be retained despite Riggs's paper, meant that Brontosaurus became one of the most famous dinosaurs. Brontosaurus has often been depicted in cinema, beginning with Winsor McCay's 1914 classic Gertie the Dinosaur, one of the first animated films.[100] McCay based his unidentified dinosaur on the apatosaurine skeleton in the American Museum of Natural History.[101] The 1925 silent film The Lost World featured a battle between a Brontosaurus and an Allosaurus, using special effects by Willis O'Brien.[102] The 1933 film King Kong featured a Brontosaurus chasing Carl Denham, Jack Driscoll and the terrified sailors on Skull Island. In 1938 the assembling of a Brontosaurus skeleton was a major plot point in the Katharine Hepburn and Cary Grant film Bringing Up Baby. These, and other early uses of the animal as a major representative of the group, helped cement Brontosaurus as a quintessential dinosaur in the public consciousness.[103]

Sinclair Oil Corporation has long been a fixture of American roads (and briefly in other countries) with its green dinosaur logo and mascot, a Brontosaurus. While Sinclair's early advertising included a number of different dinosaurs, eventually only Brontosaurus was used as the official logo, due to its popular appeal.[104]

Gertie the Dinosaur (1914)

As late as 1989, the U.S. Postal Service faced controversy when it issued four "dinosaur" stamps: Tyrannosaurus, Stegosaurus, Pteranodon, and Brontosaurus. The use of the term Brontosaurus in place of Apatosaurus led to complaints of "fostering scientific illiteracy."[105] The Postal Service defended itself (in Postal Bulletin 21742)[106] by saying, "Although now recognized by the scientific community as Apatosaurus, the name Brontosaurus was used for the stamp because it is more familiar to the general population." Indeed, the Postal Service even implicitly rebuked the somewhat inconsistent complaints by adding that "[s]imilarly, the term 'dinosaur' has been used generically to describe all the animals [i.e., all four of the animals represented in the given stamp set], even though the Pteranodon was a flying reptile [rather than a true 'dinosaur']," a distinction left unmentioned in the numerous correspondence regarding the Brontosaurus/Apatosaurus issue.[107] Palaeontologist Stephen Jay Gould supported this position. In the essay from which the title of the 1991 collection Bully for Brontosaurus is taken, Gould wrote: "Touché and right on; no one bitched about Pteranodon, and that's a real error."[103] His position, however, was not one suggesting the exclusive use of the popular name; he echoed Riggs' original argument that Brontosaurus is a synonym for Apatosaurus. Nevertheless, he noted that the former has developed and continues to maintain an independent existence in the popular imagination.[103]

The more vociferous denunciations of the usage have elicited sharply defensive statements from those who would not wish to see the name be struck from official usage.[103] Tschopp's study[10] has generated a very high number of responses from many, often opposed, groupsof editorial,[108] news staff,[56][109] and personal blog nature (both related[110][111] and not[112]), from both[113] sides of the debate, from related[18] and unrelated contexts, and from all over the world.[114]

Since Wedel et al's 2015 preprint,[43] various reconstructions of Brontosaurus individuals engaging in intraspecific combat based on their study have been made. The art typically depicts the neck-battling hypothesis stipulated by their research. Many of these works are published online under the hashtag "#BrontoSmash".[115][116]

References

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from Grokipedia
Brontosaurus is a of large herbivorous sauropod dinosaurs in the family that lived during the epoch, approximately 156 to 145 million years ago, in what is now western . These quadrupedal giants were characterized by their exceptionally long necks and whip-like tails, with forelimbs slightly shorter than their hindlimbs, allowing them to browse vegetation efficiently. Adults typically measured 21 to 23 meters (69 to 75 feet) in length and weighed 15 to 20 metric tons, making them among the largest land animals of their time. The was first established by paleontologist in 1879 based on fossils from the in , initially named Brontosaurus excelsus. For over a century, it was synonymized with Apatosaurus due to perceived similarities, but a comprehensive 2015 phylogenetic study analyzing 81 specimens and 477 morphological traits revived Brontosaurus as a distinct , identifying three : B. excelsus (the ), B. parvus, and B. yahnahpin. This reinstatement highlighted subtle differences in neck vertebrae and other skeletal features that set Brontosaurus apart from its close relatives. Brontosaurus inhabited the expansive , a depositional basin spanning rivers, floodplains, lakes, and subtropical woodlands dominated by ferns, cycads, , ginkgoes, and tree ferns. As herbivores, they likely fed on low- to mid-level vegetation such as horsetails and conifer needles. Their fossils indicate they lived amid a diverse that included other sauropods like and , as well as predators such as .

Discovery and research history

Initial discoveries during the Bone Wars

The "," also known as the Second Dinosaur Rush, was a period of intense rivalry between paleontologists and spanning from 1877 to 1892, during which the two former collaborators competed fiercely to unearth and name new species in . This competition, fueled by personal animosity, financial backing from wealthy patrons, and access to federal resources like the U.S. Geological Survey, led to the rapid discovery of over 130 new species but often at the expense of thorough preparation and analysis of specimens. Marsh, a professor at , and Cope employed teams of collectors, bribed workers at rival sites, and rushed publications to claim priority, transforming into a high-stakes race amid the expanding frontiers of post-Civil War America. In August 1879, amid this escalating feud at the prolific fossil site of Como Bluff, Wyoming, Marsh's team uncovered the specimen YPM 1980, a nearly complete postcranial of what would become the iconic sauropod Brontosaurus excelsus. The bones were excavated from Reed's Quarry 10 in the Brushy Basin Member of the , a richly fossiliferous layer to approximately 156–145 million years ago that yielded numerous sauropod remains during the . This discovery, one of the most complete sauropod s known at the time, consisted primarily of vertebrae, ribs, limb bones, and other elements from a subadult individual, measuring about 20 meters in length and highlighting the dinosaur's enormous scale. The find at Como Bluff, a key battleground in the rivalry, allowed Marsh to outpace Cope in documenting giant herbivores, further intensifying their competition. Marsh formally described and named the specimen Brontosaurus excelsus in December 1879, emphasizing its postcranial features in a preliminary that captured the public's imagination. The name derives from words brontē (thunder) and sauros (lizard), evoking the creature's massive size and presumed earth-shaking gait, while the species excelsus means "lofty" or "noble" in Latin, alluding to its elevated neck and stature. In his description, Marsh highlighted the animal's exceptionally long neck composed of 15 , a relatively small head inferred from the robust but diminutive braincase impressions, and a barrel-shaped torso supported by pillar-like limbs, portraying it as a gigantic adapted for high . These traits positioned Brontosaurus as a "thunder lizard" emblematic of giants, though the hasty naming typical of the meant the initial account focused on skeletal outline rather than exhaustive anatomical detail. Notably absent from the holotype and early finds was a skull, a common issue with sauropod discoveries due to the fragile nature of these bones and their tendency to disarticulate post-mortem. Without direct cranial material, and subsequent reconstructors relied on generic sauropod skull models, often drawing from more complete specimens like those of , to visualize Brontosaurus; this led to early depictions featuring a deep, boxy with chisel-like teeth suited for cropping . Such approximations, while innovative for the era, underscored the limitations of Bone Wars-era paleontology, where speed often trumped precision in assembling the first public images of these colossal reptiles.

Naming, skull controversy, and invalidation

formally named the genus Brontosaurus in 1879, designating the Brontosaurus excelsus based on an incomplete postcranial skeleton (Yale Peabody Museum specimen YPM 1980) collected from the in Como Bluff, ; this lacked a skull, most of the hind limbs, and several other elements. The naming occurred amid the intense rivalry of the , though a more detailed description of the material appeared in subsequent publications by Marsh. Because the type specimen did not include a , Marsh reconstructed one for Brontosaurus in 1883 using elements resembling those of Camarasaurus, a shorter and more robust macronarian sauropod, despite the actual affinities of Brontosaurus lying with the diplodocoids. This erroneous assignment influenced early skeletal mounts, including the Yale Peabody Museum's composite reconstruction of B. excelsus, which incorporated a Camarasaurus-like and was displayed publicly starting in the early . In 1903, paleontologist Elmer S. Riggs reassessed Marsh's specimens at the Field Columbian Museum and determined that Brontosaurus excelsus exhibited no significant morphological differences from Apatosaurus ajax, a Marsh had named two years earlier in 1877; Riggs thus declared Brontosaurus a junior synonym of Apatosaurus under principles of nomenclatural priority, recommending the latter name for the genus. Riggs's analysis emphasized overlaps in vertebral and limb structure, solidifying the synonymy in scientific literature. The invalidation of Brontosaurus had limited immediate effect on public perception, as the name had already captured widespread imagination through illustrations and mounts; incorrect -style skulls remained standard on (labeled as Brontosaurus) displays in major museums, including Yale's, until the 1970s when more accurate diplodocid skulls from specimens like those of were adopted based on new .

Revival through cladistic analysis and recent assessments

In 2015, Emanuel Tschopp and colleagues published a landmark peer-reviewed study in PeerJ that revived Brontosaurus as a valid through rigorous cladistic analysis. The research involved a specimen-level phylogenetic examination of 81 sauropod specimens, primarily from the family, scored across 477 discrete morphological characters derived from axial and features. This quantitative approach, using parsimony analysis, consistently recovered Brontosaurus as monophyletic and distinct from Apatosaurus in 100% of most parsimonious trees, with strong bootstrap support (over 80%) for the separation within . The distinction was grounded in vertebral morphology, with Brontosaurus exhibiting higher neural spines in the dorsal vertebrae that project prominently above the postzygapophyses, more elongated cervical vertebrae (elongation indices exceeding 4.5 in mid-cervicals for some specimens), and unique caudal features including heart-shaped anterior centra with acute ventral ridges and anteroposteriorly expanded transverse processes—contrasting with the lower, less projecting neural spines, moderately elongated cervicals (indices 3.3–4.4), and sub-circular caudal centra in Apatosaurus. These differences were quantified through character states and supported by morphometric comparisons of holotype and referred specimens, such as YPM 1980 (B. excelsus) versus YPM 1860 (A. ajax). Subsequent validations have reinforced this taxonomic separation using advanced morphometric and imaging techniques. For instance, a 2022 phylogenetic analysis of apatosaurine cranial material expanded the original Tschopp et al. matrix, confirming generic boundaries while assigning a disputed to Apatosaurus sp. based on shared derived traits, thus upholding the 2015 framework without challenging Brontosaurus validity. Recent assessments, including CT-based examinations of pneumaticity and vertebral structure in sauropods, have further highlighted consistent morphological disparities in the . A 2025 comprehensive review of explicitly recognizes Brontosaurus as valid, listing species such as B. excelsus, B. parvus, and B. yahnahpin separately from . However, as of November 2025, debates persist among paleontologists, with some arguing that the morphological differences provide only equivocal support for the generic separation due to ontogenetic and individual variability. Ongoing debates center on species-level boundaries within Brontosaurus—particularly whether B. yahnahpin warrants separation from B. excelsus—and broader implications for diplodocid taxonomy, including potential revisions to genera like Supersaurus based on similar specimen-level variability and ontogenetic effects observed in the 2015 dataset. While the generic split is widely adopted in recent phylogenies, some analyses suggest overlap in juvenile morphologies that could influence synonymy decisions for related taxa.

Physical characteristics

Size, overall morphology, and distinguishing features

Brontosaurus was a large quadrupedal sauropod characterized by an elongated , with adult individuals estimated to reach lengths of 21–22 meters (69–72 feet) from head to tail. Shoulder for these animals has been estimated at up to 4.5 meters (15 feet), based on the proportions of well-preserved specimens such as the YPM 1980 of B. excelsus. Body mass estimates derived from volumetric models of specimens like YPM 1980 suggest adults weighed 15–17 metric tons, reflecting a robust yet relatively gracile build compared to closely related taxa. The overall morphology of Brontosaurus featured a comprising 15 , a barrel-shaped supported by 10 dorsal vertebrae, and a whip-like with approximately 80 caudal vertebrae, enabling a quadrupedal stance with pillar-like limbs that provided stability for its massive frame. This configuration contributed to its distinctive among diplodocid sauropods, with the elongated allowing for elevated while the deep, rounded ribcage housed extensive digestive organs. Several features distinguished Brontosaurus from its close relative , including a more gracile overall build, taller neural arches in the vertebrae, and a relatively longer neck, which together imparted a slenderer appearance despite similar overall dimensions. In comparison to , Brontosaurus exhibited less extreme elongation of the neck and tail, resulting in a more robust body profile with higher neural arches and shorter . Hypotheses of sexual dimorphism in Brontosaurus stem from observed size variations among fossil specimens, such as differences in limb robustness and vertebral proportions, though these remain unconfirmed due to limited sample sizes and the challenges of identifying sex in sauropod remains.

Skull, neck, and vertebrae

The skull of Brontosaurus was small relative to its massive body size, exhibiting a lightweight, elongate structure similar to that of Diplodocus, with large nares positioned dorsally on a relatively boxy cranium. The dentition consisted of peg-like, spatulate teeth concentrated at the front of the jaws, well-suited for cropping and stripping low vegetation such as ferns and cycads. No complete Brontosaurus skull has been found in direct association with diagnostic postcranial remains, but referred specimens, including partial crania from the Morrison Formation, confirm these features and refute earlier reconstructions that erroneously depicted a deeper, more robust skull akin to Camarasaurus. This skull morphology was definitively established in the through re-examination of apatosaurine specimens and updated museum mounts, such as those at the Yale Peabody Museum, which replaced outdated Camarasaurus-inspired heads with Diplodocus-like ones based on associated jaw fragments and . The of Brontosaurus comprised 15 elongated , each reaching up to 1 meter in length in adult individuals, contributing to a total neck span of approximately 8–9 meters. These vertebrae featured prominent pneumatic foramina on their lateral and ventral surfaces, evidencing invasion by that lightened the structure while maintaining robustness. Longitudinal flanges along the lateroventral margins of mid- and posterior cervical centra enhanced structural integrity, and overall flexibility was constrained, primarily allowing motion in the horizontal plane to facilitate efficient . The vertebral column included 10 dorsal vertebrae with notably tall, bifid neural spines—longer than wide at their bases—that formed a subtle, sail-like dorsal ridge along the back, distinguishing Brontosaurus from the chunkier spines of Apatosaurus. The five sacral vertebrae were fused into a robust synsacrum for weight support, while the approximately 80 caudal vertebrae tapered progressively, with anterior ones bearing procoelous centra and later ones featuring chevrons that indicate a muscular tail base for balance and propulsion. Pneumatic features, including foramina and internal camellae, were variably present in the presacral vertebrae, reflecting the extensive air sac system typical of sauropods.

Limbs, posture, and locomotion

The forelimbs of Brontosaurus were robust and adapted for weight-bearing support, featuring a humerus that was shorter than the femur, with a length ratio typically less than 0.7. The scapula and coracoid formed a strong shoulder girdle, providing stability for the animal's massive body mass, while the manus consisted of five digits arranged in a semi-circular pattern, with a prominent claw on the pollex (thumb) that likely aided in anchoring and preventing slippage during movement. In contrast, the hind limbs were longer and more columnar, with a pillar-like femur and tibia designed to bear the majority of the body weight, estimated to support 60–70% of the total load due to the posterior position of the center of mass in diplodocids. The pes had four functional digits, reflecting adaptations for efficient ground contact and propulsion in a quadrupedal stance. Brontosaurus maintained a fully quadrupedal posture, with its long held in a nearly horizontal orientation or slightly downward-sloping in its osteological neutral pose, allowing the head to reach low- to mid-level vegetation without excessive muscular strain. Biomechanical models from the and 2000s, incorporating zygapophyseal articulations and constraints, suggest the anterior was flexed ventrally at approximately 35° relative to the horizontal, while the overall body axis remained level, supported by the upright columnar limbs. The tail was likely held elevated off the ground, as evidenced by the absence of drag marks in associated trackways, preventing interference with locomotion and aiding balance. Locomotion in Brontosaurus was characterized by a slow, quadrupedal gait, inferred from trackway evidence showing narrow-gauge impressions consistent with diplodocid morphology. Speed estimates derived from stride lengths and limb proportions in sauropod trackways indicate walking velocities of 3–5 km/h, with no indications of bipedal capability or rapid movement, reflecting the biomechanical limitations of its gigantic size and graviportal limb design. This amble-like gait prioritized stability over speed, enabling efficient traversal of floodplain environments.

Classification

Phylogenetic relationships within Sauropoda

Brontosaurus belongs to the clade , a diverse group of long-necked, herbivorous dinosaurs that dominated terrestrial ecosystems during the era. More specifically, it is nested within , the advanced sauropods that emerged in the and are defined by features such as cylindrical teeth and an external mandibular . bifurcated into two primary lineages: , which includes robust forms like and titanosaurs with boxy skulls and pillar-like limbs, and , characterized by more slender builds and specialized feeding adaptations. Brontosaurus falls within , sharing diagnostic traits with this group, including an exceptionally elongated tail that could function as a whip-like structure for balance or defense, and narrow, pencil-shaped teeth with fine, planar wear facets suited for cropping vegetation rather than grinding. Within , Brontosaurus is assigned to the family , a radiation of gigantic sauropods known from , , and . A landmark specimen-level cladistic analysis incorporating over 200 morphological characters from 81 diplodocid specimens resolved Brontosaurus as a distinct genus in the , positioned as the sister taxon to . This relationship is bolstered by several apatosaurine synapomorphies, such as that extend well beyond the vertebral centrum, the absence of paired pneumatic fossae on the ventral surfaces of anterior , and the anterior divergence of posterior centrodiapophyseal and postzygodiapophyseal laminae in the vertebrae. thus forms one of the two main subclades of , with the other being Diplodocinae (encompassing genera like and ). As a derived diplodocid, it evolved from basal diplodocoid ancestors that appeared earlier in the , such as the Asian taxon Lingwulong shenqi, which documents an early diversification and dispersal of the group across . The phylogenetic framework has been influential, but the of remains debated in subsequent research, with some analyses proposing alternative configurations that place closer to apatosaurines, potentially expanding or redefining the subfamily boundaries. As of 2025, while the 2015 revision is widely accepted, some analyses continue to debate the distinctness of certain species.

Recognized species and synonyms

The genus Brontosaurus is currently recognized as comprising three valid , based on a comprehensive phylogenetic analysis of diplodocid specimens that separated it from the closely related genus . The is B. excelsus, originally described by in 1879, with its specimen YPM 1980 collected from the in ; this is characterized by a robust build and an estimated length of 21 meters. Brontosaurus yahnahpin, named in 1994 as a species of Apatosaurus and formally assigned to the genus in 2015, is based on the TATE-001 (a relatively complete postcranial ) from the in ; it exhibits a more gracile morphology compared to the . Brontosaurus parvus, revived in 2015 from the former genus Elosaurus (originally described in 1902), has its CM 566 from the in and is noted for its smaller overall size, though its specific validity has faced debate among paleontologists in the 2020s due to overlapping morphological traits with other apatosaurines; referred specimens include UW 15556. Several historical names have been considered synonyms or invalid within Brontosaurus. Additionally, some specimens previously allocated to Apatosaurus louisae have been partially re-examined and reassigned to Brontosaurus based on vertebral and limb differences, though the core of A. louisae remains distinct within . These taxonomic adjustments stem from the 2015 revision, which emphasized specimen-level comparisons to resolve long-standing synonymies in diplodocids.
SpeciesYear DescribedHolotype SpecimenLocation (Formation)Key Features
B. excelsus1879YPM 1980 (Morrison)Robust build, ~21 m length
B. yahnahpin1994 (assigned 2015)TATE-001 (Morrison)Gracile morphology, oldest species
B. parvus1902 (revived 2015)CM 566 (Morrison)Smaller size, debated status

Paleobiology

Diet, feeding mechanisms, and metabolic requirements

Brontosaurus was an exclusively herbivorous sauropod, primarily consuming low-growing vegetation such as ferns, cycads, , horsetails, and other pre-angiosperm available in its environment. As a low browser within the family, it targeted ground-level plants and mid-height foliage up to approximately 5 meters, achieved through lateral sweeps of its long, flexible rather than vertical elevation for high , a strategy more characteristic of brachiosaurids like . This feeding height was constrained by its horizontal neck posture and lack of evidence for upright rearing, allowing efficient access to a broad envelope of softer, more accessible plant matter without the need for extensive vertical reach. The feeding apparatus of Brontosaurus featured peg-like, pencil-shaped teeth at the front of a small, lightweight , suited for nipping, stripping, or shearing branches and leaves rather than grinding or mastication. Its bite force was notably weak, estimated at less than 500 N based on biomechanical models of related diplodocids such as (posterior bite force ~324 N), reflecting a reliance on bulk ingestion over mechanical processing, with food likely swallowed whole and digested via aided by symbiotic microbes. Gastroliths, or stomach stones, have been proposed to assist in within a gastric mill, similar to modern birds, but direct evidence associating polished pebbles with Brontosaurus skeletons remains inconclusive and rare, suggesting digestion primarily occurred through prolonged retention times rather than mechanical grinding. Metabolically, Brontosaurus exhibited physiological adaptations suited to its enormous size, with ongoing debates centering on ectothermy, endothermy, or as the primary mode of . Models from the , incorporating growth rates and bone histology, support an intermediate metabolism that maintained body temperatures around 30°C through , where low surface-to-volume ratios minimized heat loss while efficient respiratory systems, possibly including , facilitated and cooling. To sustain this, Brontosaurus required an estimated daily intake of 200–300 kg of , scaled allometrically from its body mass of 15–20 tons, enabling sufficient acquisition despite the low nutritional quality of its diet.

Growth, ontogeny, and sexual dimorphism

Brontosaurus hatchlings are estimated to have been approximately 1 meter in length and weighed around 35 kg upon hatching, based on comparative analyses of sauropod egg sizes and early growth models for closely related diplodocids like . development proceeded rapidly, with histological examination of long bones revealing lines of arrested growth (LAGs) that indicate seasonal pauses in a predominantly continuous growth pattern typical of sauropods. These LAGs, observed in diplodocid femora and humeri, document accelerated juvenile growth phases, allowing individuals to reach subadult proportions by 10–15 years of age. Early growth rates in Brontosaurus were substantial, with models estimating 180–400 kg per year during the initial exponential phase, slowing after skeletal maturity as secondary remodeling dominated the bone microstructure. Bone histology from 2008 studies of diplodocid long bones supports this trajectory, showing fibrolamellar tissue deposition that reflects high metabolic rates in youth, transitioning to lamellar bone in later ontogeny. Full adult size, exceeding 20 meters in length and 15 metric tons in mass, was likely attained by 20–30 years, as inferred from growth curve modeling calibrated against LAG counts in related taxa like Apatosaurus. Juvenile Brontosaurus exhibited distinct morphological features adapted to early life stages, including relatively longer and more gracile limbs suggestive of greater cursoriality compared to the pillar-like adult posture, and proportionally shorter necks that elongated markedly during growth. Bone beds containing multiple juvenile and subadult diplodocid specimens, such as those from the , imply gregarious herding behavior, potentially providing protection from predators during vulnerable early . Sexual dimorphism in Brontosaurus remains unconfirmed due to the scarcity of well-preserved associated skeletons and the challenges in identifying sex-specific osteological traits in sauropods. Some variation in pelvic girdle size has been noted in diplodocid specimens, hinting at possible sexual differences, but no definitive indicators—such as robusticity disparities or chevron modifications—have been consistently identified across populations.

Sensory systems, behavior, and hypothesized interactions

The sensory systems of Brontosaurus, inferred primarily from cranial endocasts and braincase morphology in related diplodocid sauropods like Apatosaurus, indicate a reliance on basic visual and vestibular capabilities with limited olfactory processing. The optic nerve foramina in the laterosphenoid bone are notably large and circular, suggesting a capacity for decent vision adapted to detecting movement or broad environmental cues in open habitats. The brain itself was small relative to body size—approximately walnut-sized in adults, with a modest cerebrum and elongated olfactory tracts connected to relatively small bulbs—implying restricted olfaction compared to predatory theropods, though sufficient for locating vegetation or mates. Hearing likely emphasized low-frequency sound detection, potentially facilitated by thin tympanic membranes and a well-developed vestibular apparatus with slender semicircular canals for balance, as seen in basal sauropods; this would have aided in perceiving distant rumbles from conspecifics or seismic vibrations. Overall, these traits reflect a sensory suite tuned for a large, herbivorous lifestyle rather than complex predation or navigation. Behavioral inferences for Brontosaurus derive from trackway evidence and comparisons with other diplodocoids, pointing to a largely solitary existence punctuated by small-group formations. Multiple sauropod trackways from formations, including those attributable to diplodocids, show parallel paths of similarly sized individuals traveling together, suggesting occasional gregariousness in subadult or mixed-age groups for or migration, though no large herds are indicated. Vocalizations are hypothesized to have consisted of low-frequency rumbles, produced via laryngeal structures similar to those in modern crocodilians, potentially used for long-distance communication during mating seasons to attract partners without alerting predators. No direct evidence exists for complex social hierarchies, but the animal's size and energy demands likely favored loose associations over persistent herds. Hypothesized interactions among Brontosaurus individuals or with predators remain speculative, drawn from skeletal robustness and biomechanical models. Intraspecific encounters may have involved low-intensity neck swinging or butting, leveraging the robust vertebrae and muscular necks observed in Apatosaurus specimens to establish dominance during mating rivalries, though without evidence of sexual dimorphism or healed injuries to confirm combat frequency. Defensive strategies against contemporaneous predators like Allosaurus probably relied on sheer body size as a deterrent, supplemented by tail whips; multibody simulations indicate that the whip-like tail could generate subsonic strikes capable of inflicting blunt trauma or deterring attacks on flanks, without reaching supersonic speeds. Trackways provide indirect support for group travel as a protective measure, but direct evidence of interactions is absent, emphasizing passive deterrence over active aggression.

Paleoecology

Geological formations and temporal range

Brontosaurus fossils are known exclusively from the Upper Jurassic Morrison Formation, a major sedimentary unit spanning the late Kimmeridgian to early Tithonian stages, approximately 156 to 145 million years ago. This formation consists of a sequence of sandstones, mudstones, and limestones deposited across a vast area of western North America, representing one of the most productive sources of Late Jurassic vertebrate fossils. The majority of Brontosaurus specimens have been recovered from sites in Wyoming, including the historic Como Bluff locality, where the type specimen of B. excelsus was discovered in Reed's Quarry 10, and Sheep Creek, the source of B. yahnahpin. Additional important quarries include the Bone Cabin Quarry near Como Bluff, which yielded partial Brontosaurus remains, as well as localities in Utah, such as those near Dinosaur National Monument, and scattered sites in Montana and Colorado. Stratigraphically, these fossils occur primarily in the Brushy Basin Member, with some in the underlying Salt Wash Member, reflecting deposition in varying fluvial settings within the formation. The temporal range of Brontosaurus itself spans from approximately 152 million years ago, encompassing the earliest B. parvus-like forms in lower stratigraphic zones, to around 145 million years ago for the latest B. excelsus specimens in upper zones, with no evidence of the genus persisting into the . Preservation of these fossils typically occurred in fluvial channel and overbank deposits, characterized by fine-grained sandstones and mudstones that indicate episodic river flooding interspersed with periodic droughts, as evidenced by development and evaporitic minerals.

Habitat, environment, and paleoclimate

Brontosaurus inhabited the semi-arid floodplains of western North America during the , characterized by a mosaic of riverine corridors, seasonal lakes, wetlands, and conifer-dominated woodlands. These environments formed part of the expansive Morrison Basin, where fluvial and lacustrine deposits indicate periodic flooding from streams originating in western uplands, interspersed with expansive dry plains. Vegetation was structured with low-lying ferns and horsetails dominating understories in wetter riparian zones, while taller gymnosperms such as , cycads, and ginkgos formed multi-layered canopies in forested areas, supporting the dietary needs of large herbivores like Brontosaurus. The paleoclimate was warm and temperate, with mean annual temperatures estimated at 20–25°C, influenced by a subtropical high-pressure system that promoted high rates and . Winters were mild at around 5°C, while summers reached up to 36°C, approximately 5°C warmer than modern equivalents in the region. occurred in monsoonal patterns, totaling 600–900 mm annually, with wet seasons driven by summer storms and prolonged dry periods marked by . Evidence from paleosols, including vertisols and gleysols, reveals wetting-drying cycles consistent with this , while oxygen ratios in pedogenic carbonates indicate elevated stress in soils. Adaptations to this fluctuating environment are inferred from oxygen isotope variations in sauropod teeth from the , such as those of , which show intra-tooth fluctuations suggesting seasonal movement across habitats. These isotopic signatures, reflecting shifts in water sources between lowland floodplains and higher-elevation uplands, imply migrations of at least 300 km to access reliable water during dry periods. Such mobility would have been facilitated by the dinosaur's large size and gregarious behavior, allowing traversal of the semi-arid landscape.

Contemporaneous taxa and ecological role

Brontosaurus coexisted with a diverse array of dinosaurs in the of western North America, including theropod predators such as and , which likely targeted juveniles and smaller individuals of herbivorous taxa. Other contemporaneous sauropods included , , , and , while ornithischians such as and filled roles as mid-sized herbivores. The preserves fossils from approximately 37 valid genera, making it one of the richest terrestrial ecosystems known. As a , Brontosaurus functioned as a primary and dominant browser in the , consuming large quantities of low- to mid-height such as ferns, cycads, and in a semi-arid environment. Niche partitioning among sauropods likely minimized competition, with Brontosaurus and related diplodocoids adapted for mid-level browsing on softer foliage, contrasting with the higher-reaching capabilities of taxa like for branch stripping or for tougher, woody plants. This specialization, evidenced by cranial and dental adaptations, supported high sauropod diversity despite resource limitations. Trophic interactions involved predation pressure from large theropods like , which preyed on juvenile sauropods, while adults may have faced minimal threats due to their size. Competition for browse occurred among sauropods, such as between Brontosaurus and for accessible mid-canopy vegetation. Bonebeds in the , including those with disarticulated sauropod remains, provide evidence of mass mortality events likely triggered by seasonal droughts, where herds congregated at shrinking water sources and perished en masse.

Cultural impact

Representation in scientific nomenclature and literature

The case of Brontosaurus has long served as a textbook example of the International Code of Zoological Nomenclature (ICZN) principle of priority in sauropod taxonomy, illustrating conflicts between nomenclatural stability and morphological evidence. Synonymized with the earlier-named Apatosaurus in 1903, its 2015 reinstatement based on quantitative phylogenetic analysis reignited discussions on the role of specimen-level data in taxonomy. This has influenced educational materials and debates on ethical issues in paleontology, stemming from the "Bone Wars" rivalry that led to rushed namings and taxonomic instability. In popular scientific literature, Brontosaurus featured prominently in early works like Othniel Charles Marsh's 1880s monographs as an icon of sauropod . During its synonymized period, it was reclassified under in texts such as Edwin H. Colbert's 1961 Dinosaurs: Their Discovery and Their World, emphasizing . Following the 2015 revival, it has appeared in studies on diplodocid diversity, including examinations of neck morphology and biomechanics that treat it distinctly from . As of 2025, the genus is referenced in thousands of scholarly works per , reflecting its ongoing significance in sauropod research and education. Brontosaurus has been a prominent fixture in museum exhibits since the early 20th century, often serving as an iconic representation of prehistoric giants. The first permanent mount of a sauropod dinosaur, labeled as Brontosaurus, was unveiled at the American Museum of Natural History (AMNH) in New York in 1905, constructed from multiple specimens including parts borrowed from Yale's collection; this composite skeleton, measuring over 66 feet long, featured an incorrect Camarasaurus skull that influenced public perceptions for decades. At the Yale Peabody Museum of Natural History, the original Brontosaurus excelsus holotype (YPM 1980), collected in the late 1870s, was fully mounted and displayed starting in 1931 as the hall's centerpiece, with its skull replaced in 1981 to reflect a more accurate Diplodocus-like morphology. Sinclair Oil Corporation contributed to these displays by debuting a life-sized Brontosaurus model at the 1933–1934 Chicago World's Fair, designed by sculptor Louis Paul Jonas and based on AMNH specimens, which later toured as promotional exhibits and reinforced the dinosaur's image in public venues. Following the 2015 taxonomic revival of the Brontosaurus genus, museums like Yale updated labels on their mounts, with the Peabody hosting a renaming ceremony for its skeleton and remounting it in a more dynamic pose in 2024 to enhance visitor engagement. In film and media, Brontosaurus appeared in early postcards and illustrations from the 1900s, capturing the AMNH mount and popularizing its image as a towering, long-necked behemoth. The 1933 film King Kong depicted a herd of aggressive, amphibious Brontosauruses on Skull Island, including a scene where one lifts and devours a sailor, blending horror with adventure in a way that cemented the dinosaur's fearsome reputation in cinema. Later, the 1969 film The Valley of Gwangi featured stop-motion sauropods resembling Brontosaurus amid a lost world of dinosaurs, showcasing Ray Harryhausen's effects in a Western-fantasy setting where cowboys encounter prehistoric creatures. In Steven Spielberg's 1993 Jurassic Park, the long-necked sauropod is scientifically named Apatosaurus but widely recognized and referred to as Brontosaurus in popular discourse, with scenes of herds grazing evoking the classic imagery despite the taxonomic distinction. Cartoons and animations further amplified this, notably through Sinclair Oil's green Apatosaurus logo—introduced in 1930 and trademarked in 1932—which evolved from Brontosaurus depictions and appeared in advertisements, fueling children's fascination with dinosaurs. Beyond screens, Brontosaurus symbolizes enormity and in broader , appearing in merchandise like toys, stamps, and books that emphasize its massive scale—up to 72 feet long and 15 tons in weight—as a for lost worlds. The revival of the genus name generated widespread media attention, including coverage highlighting its resurrection after over a century of invalidation, which spurred documentaries and articles revisiting its cultural legacy. This resurgence boosted public interest, leading to renewed exhibits and discussions in outlets like , where it was framed as a "prehistoric giant revived in name." A persistent misconception in public memory stems from the erroneous skulls on early mounts, such as the boxy head placed on the AMNH and Yale Brontosaurus skeletons in the early , which portrayed it with a short, blunt rather than its actual slender, horse-like features; despite corrections by the , this outdated image endures in illustrations, , and merchandise, shaping generations' view of the .

References

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