Diplodocus (,
,
or
)
is a
genus of
diplodocid sauropod dinosaur whose
fossils were first discovered in 1877 by
S. W. Williston. The generic name, coined by
Othniel Charles Marsh in 1878, is a
Neo-Latin term derived from
Greek (
diploos) "double" and (dokos) "beam",
in reference to its double-beamed
chevron bones located in the underside of the tail. These bones were initially believed to be unique to
Diplodocus; however, they have since then been discovered in other members of the
diplodocid family and in non-diplodocid sauropods such as
Mamenchisaurus.
It lived in what is now western North America at the end of the
Jurassic Period.
Diplodocus is one of the more common dinosaur fossils found in the Upper
Morrison Formation, a sequence of shallow marine and alluvial sediments deposited about 150 to 147
million years ago, in what is now termed the
Kimmeridgian and
Tithonian stages. The Morrison Formation records an environment and time dominated by gigantic sauropod dinosaurs such as
Camarasaurus,
Barosaurus,
Apatosaurus and
Brachiosaurus.
Diplodocus is among the most easily identifiable dinosaurs, with its classic dinosaur shape, long neck and tail and four sturdy legs. For many years, it was the longest dinosaur known. Its great size may have been a deterrent to the predators
Allosaurus and
Ceratosaurus: their remains have been found in the same
strata, which suggests they coexisted with
Diplodocus.
Description
One of the best-known sauropods,
Diplodocus was a very large long-necked
quadrupedal animal, with a long, whip-like tail. Its forelimbs were slightly shorter than its hind limbs, resulting in a largely horizontal posture. The long-necked, long-tailed animal with four sturdy legs has been mechanically compared with a suspension bridge.
[Lambert D. (1993)The Ultimate Dinosaur Book ISBN 0-86438-417-3] In fact,
Diplodocus is the longest dinosaur known from a complete skeleton.
The partial remains of
D. hallorum have increased the estimated length, though not as much as previously thought; when first described in 1991, discoverer David Gillete calculated it may have been up to 54 m (177.05 ft) long, making it the longest known dinosaur (excluding those known from especially poor remains, such as
Amphicoelias). Some weight estimates ranged as high as 113 (rather only 50)
tonnes (125 US
short tons). This review was based on recent findings that show that the giant tail vertebrae were actually placed further forward on the tail than Gillete originally calculated. The study shows that the complete
Diplodocus skeleton at the
Carnegie Museum of Natural History in
Pittsburgh, Pennsylvania on which estimates of
Seismosaurus were based had its 13th tail vertebra come from another dinosaur, throwing size estimates for
Seismosaurus off by up to 30%. While dinosaurs such as
Supersaurus were probably longer, fossil remains of these animals are only fragmentary.
The skull of
Diplodocus was very small, compared with the
size of the animal, which could reach up to ,
of which over was neck.
Diplodocus had small, 'peg'-like teeth that pointed forward and were only present in the
anterior sections of the jaws.
Its braincase was small. The neck was composed of at least fifteen
vertebrae and is now believed to have been generally held parallel to the ground and unable to have been elevated much past horizontal. Modern mass estimates have tended to be in the 10 to 16
tonne (11–17.6
ton) range: 10 tonnes (11 tons);
[Dodson, P., Behrensmeyer, A.K., Bakker, R.T., and McIntosh, J.S. (1980). Taphonomy and paleoecology of the dinosaur beds of the Jurassic Morrison Formation. Paleobiology 6:208–232.] 11.5 tonnes (12.7 tons);
[Paul, G.S. (1994). Big sauropods - really, really big sauropods. The Dinosaur Report, The Dinosaur Society Fall:12–13.] 12.7 tonnes (14 tons);
[Foster, J.R. (2003). Paleoecological Analysis of the Vertebrate Fauna of the Morrison Formation (Upper Jurassic), Rocky Mountain Region, U.S.A. New Mexico Museum of Natural History and Science:Albuquerque, New Mexico. Bulletin 23.] and 16 tonnes (17.6 tons).
[Coe, M.J., Dilcher, D.L., Farlow, J.O., Jarzen, D.M., and Russell, D.A. (1987). Dinosaurs and land plants. In: Friis, E.M., Chaloner, W.G., and Crane, P.R. (eds.). The Origins of Angiosperms and Their Biological Consequences. Cambridge University Press:New York, 225–258. ISBN 0521323576.]Diplodocus had an extremely long tail, composed of about 80
caudal vertebrae,
which is almost double the number some of the earlier sauropods had in their tails (such as
Shunosaurus with 43), and far more than contemporaneous
macronarians had (such as
Camarasaurus with 53). There has been speculation as to whether it may have had a defensive or noisemaking (by cracking it like a
coachwhip) function. The tail may have served as a counterbalance for the neck. The middle part of the tail had 'double beams' (oddly shaped bones on the underside, which gave
Diplodocus its name). They may have provided support for the vertebrae, or perhaps prevented the blood vessels from being crushed if the animal's heavy tail pressed against the ground. These 'double beams' are also seen in some related dinosaurs.
Like other sauropods, the manus (front "feet") of
Diplodocus were highly modified, with the finger and hand bones arranged into a vertical column,
horseshoe-shaped in cross section.
Diplodocus lacked claws on all but one digit of the front limb, and this claw was unusually large relative to other sauropods, flattened from side to side, and detached from the bones of the hand. The function of this unusually specialized claw is unknown.
[Bonnan, M. F. (2003). "The evolution of manus shape in sauropod dinosaurs: implications for functional morphology, forelimb orientation, and phylogeny." Journal of Vertebrate Paleontology, 23: 595-613.]Discovery and species
Several species of
Diplodocus were described between 1878 and 1924. The first
skeleton was found at
Como Bluff,
Wyoming by
Benjamin Mudge and
Samuel Wendell Williston in 1878, and was named
Diplodocus longus ('long double-beam'), by
paleontologist Othniel Charles Marsh in 1878.
Diplodocus remains have since been found in the
Morrison Formation of the western
U.S. States of
Colorado,
Utah,
Montana and
Wyoming.
Fossils of this animal are common, except for the
skull, which is often missing from otherwise complete skeletons. Although not the type species,
D. carnegii is the most completely known and most famous due to the large number of casts of its skeleton in museums around the world.
The two Morrison Formation sauropod genera
Diplodocus and
Barosaurus had very similar limb bones. In the past, many isolated limb bones were automatically attributed to
Diplodocus but may, in fact, have belonged to
Barosaurus. Fossil remains of
Diplodocus have been recovered from stratigraphic zone 5 of the
Morrison Formation.
[Foster, J. (2007). "Appendix." Jurassic West: The Dinosaurs of the Morrison Formation and Their World. Indiana University Press. pp. 327-329.]Valid species

Restoration of Diplodocus carnegii

Diplodocus hallorum (formerly known as Seismosaurus)
- D. longus, the type species, is known from two skulls and a caudal series from the Morrison Formation of Colorado and Utah.
- D. hayi, known from a partial skeleton discovered by William H. Utterback in 1902 near Sheridan, Wyoming, was described in 1924.
- D. hallorum, first described in 1991 by Gillette as Seismosaurus halli from a partial skeleton comprising vertebrae, pelvis and ribs. George Olshevsky later attempted to emend the name as S. hallorum, citing incorrect grammar on the part of the original authors, a recommendation that has been followed by others, including Carpenter (2006).
[Carpenter, K. (2006). "Biggest of the big: a critical re-evaluation of the mega-sauropod Amphicoelias fragillimus." In Foster, J.R. and Lucas, S.G., eds., 2006, Paleontology and Geology of the Upper Jurassic Morrison Formation. New Mexico Museum of Natural History and Science Bulletin 36: 131-138.[https://scientists.dmns.org/sites/kencarpenter/PDFs%20of%20publications/Amphicoelias.pdf]] In 2004, a presentation at the annual conference of the Geological Society of America made a case for Seismosaurus being a junior synonym of Diplodocus. This was followed by a much more detailed publication in 2006, which not only renamed the species Diplodocus hallorum, but also speculated that it could prove to be the same as D. longus. The position that D. hallorum should be regarded as a specimen of D. longus was also taken by the authors of a redescription of Supersaurus, refuting a previous hypothesis that Seismosaurus and Supersaurus were the same.
Nomina dubia (doubtful species)
- D. lacustris is a nomen dubium, named by Marsh in 1884, from remains of a smaller animal from Morrison, Colorado.
These remains are now believed to have been from an immature animal, rather than from a separate species.[Upchurch, P., Barrett, P.M., and Dodson, P. (2004). "Sauropoda." In D. B. Weishampel, P. Dodson, and H. Osmólska (eds.), The Dinosauria (2nd edition). University of California Press, Berkeley 259–322.]
Paleobiology
Due to a wealth of skeletal remains,
Diplodocus is one of the best-studied dinosaurs. Many aspects of its lifestyle have been subjects of various theories over the years.
Habitat
Marsh and then
Hatcher assumed the animal was aquatic, because of the position of its nasal openings at the apex of the cranium. Similar aquatic behavior was commonly depicted for other large sauropods such as
Brachiosaurus and
Apatosaurus. However, a 1951 study by Kenneth A. Kermack indicates that sauropods probably could not have breathed through their nostrils when the rest of the body was submerged, as the water pressure on the chest wall would be too great.
Since the 1970s, general consensus has the sauropods as firmly terrestrial animals, browsing on trees. However, a more recent theory suggests a likely
riparian habitat for
Diplodocus.
Posture

An outmoded depiction of Diplodocus by Oliver P. Hay (1910), with sprawled limbs
The depiction of
Diplodocus posture has changed considerably over the years. For instance, a classic 1908 reconstruction by Oliver P. Hay depicts two
Diplodocus with splayed lizard-like limbs on the banks of a river. Hay argued that
Diplodocus had a sprawling, lizard-like gait with widely splayed legs, and was supported by Gustav Tornier. However, this hypothesis was contested by W. J. Holland, who demonstrated that a sprawling
Diplodocus would have needed a trench to pull its belly through. Finds of sauropod footprints in the 1930s eventually put Hay's theory to rest.

A classic depiction of Diplodocus by Mary Woodward (1905), with neck high up in the air and tail on the ground. This tail posture is believed to be incorrect
Later,
diplodocids were often portrayed with their necks held high up in the air, allowing them to graze from tall trees. Studies using computer models have shown that neutral posture of the neck was horizontal, rather than vertical, and scientists such as Kent Stephens have used this to argue that sauropods including
Diplodocus did not raise their heads much above shoulder level.
However, subsequent studies demonstrated that all
tetrapods appear to hold their necks at the maximum possible vertical extension when in a normal, alert posture, and argued that the same would hold true for sauropods barring any unknown, unique characteristics that set the soft tissue anatomy of their necks apart from other animals. One of the sauropod models in this study was
Diplodocus, which they found would have held its neck at about a 45 degree angle with the head pointed downwards in a resting posture.
As with the related genus
Barosaurus, the very long neck of
Diplodocus is the source of much controversy among scientists. A 1992
Columbia University study of Diplodocid neck structure indicated that the longest necks would have required a 1.6 ton heart — a tenth of the animal's body weight. The study proposed that animals like these would have had rudimentary auxiliary 'hearts' in their necks, whose only purpose was to pump blood up to the next 'heart'.

A depiction of two Diplodocus longus with horizontal necks, flexible whip tails, keratinous spines and nostrils low on the snouts.
While the long neck has traditionally been interpreted as a feeding adaptation, a recent study suggests that the oversized neck of
Diplodocus and its relatives may have been primarily a sexual display, with any other feeding benefits coming second.
Diet
Diplodocus has highly unusual teeth compared to other sauropods. The crowns are long and slender, elliptical in cross-section, while the apex forms a blunt triangular point.
[ Upchurch, P. & Barrett, P.M. (2000). Chapter 4: The evolution of sauropod feeding mechanism. IN: Evolution of Herbivory in Terrestrial Vertebrates ISBN 0-521-59449-9] The most prominent wear facet is on the apex, though unlike all other wear patterns observed within sauropods,
Diplodocus wear patterns are on the labial (cheek) side of both the upper and lower teeth.
What this means is
Diplodocus and other diplodocids had a radically different feeding mechanism than other sauropods. Unilateral branch-stripping is the most likely feeding behavior of
Diplodocus, as it explains the unusual wear patterns of the teeth (coming from tooth-food contact). In unilateral branch stripping, one tooth row would have been used to strip foliage from the stem, while the other would act as a guide and stabilizer. With the elongated preorbital (in front of the eyes) region of the skull, longer portions of stems could be stripped in a single action.
Also the palinal (backwards) motion of the lower jaws could have contributed two significant roles to feeding behaviour: 1) an increased gape, and 2) allowed fine adjustments of the relative positions of the tooth rows, creating a smooth stripping action.
With a laterally and dorsoventrally flexible neck, and the possibility of using its tail and rearing up on its hind limbs (tripodal ability),
Diplodocus would have had the ability to browse at many levels (low, medium, and high), up to approximately 10 metres (33 ft) from the ground. The neck's range of movement would have also allowed the head to graze below the level of the body, leading some scientists to speculate on whether
Diplodocus grazed on submerged water plants, from riverbanks. This concept of the feeding posture is supported by the relative lengths of front and hind limbs. Furthermore, its peglike teeth may have been used for eating soft water plants.
Other anatomical aspects

a) skull, b) classic rendering of the head with nostrils on top, c) Bakker's theory of a trunk, d) modern depiction with nostrils low on the snout and a possible resonating chamber
The head of
Diplodocus has been widely depicted with the nostrils on top due to the position of the nasal openings at the apex of the skull. There has been speculation over whether such a configuration meant that
Diplodocus may have had a trunk. A recent study surmised there was no paleoneuroanatomical evidence for a trunk. It noted that the
facial nerve in an animal with a trunk, such as an elephant, is large as it innervates the trunk. The evidence suggests that the facial nerve is very small in
Diplodocus. Studies by Lawrence Witmer (2001) indicated that, while the nasal openings were high on the head, the actual, fleshy nostrils were situated much lower down on the snout.
Recent discoveries have suggested that
Diplodocus and other diplodocids may have had narrow, pointed
keratinous spines lining their back, much like those on an
iguana. This radically different look has been incorporated into recent reconstructions, notably
Walking with Dinosaurs. It is unknown exactly how many diplodocids had this trait, and whether it was present in other sauropods.
Reproduction and growth
While there is no evidence for
Diplodocus nesting habits, other
sauropods such as the
titanosaurian
Saltasaurus have been associated with nesting sites. The titanosaurian nesting sites indicate that may have laid their eggs communally over a large area in many shallow pits, each covered with vegetation. It is possible that
Diplodocus may have done the same. The documentary
Walking with Dinosaurs portrayed a mother
Diplodocus using an
ovipositor to lay eggs, but it was pure speculation on the part of the documentary.
Following a number of
bone histology studies,
Diplodocus, along with other sauropods, grew at a very fast rate, reaching
sexual maturity at just over a decade, though continuing to grow throughout their lives. Previous thinking held that sauropods would keep growing slowly throughout their lifetime, taking decades to reach maturity.
Classification
Diplodocus is both the
type genus of, and gives its name to
Diplodocidae, the family to which it belongs.
[Marsh, O.C. 1884. Principal characters of American Jurassic dinosaurs. Part VII. On the Diplodocidae, a new family of the Sauropoda. American Journal of Science 3: 160–168.] Members of this family, while still massive, are of a markedly more slender build when compared with other sauropods, such as the
titanosaurs and
brachiosaurs. All are characterised by long necks and tails and a horizontal posture, with forelimbs shorter than hindlimbs. Diplodocids flourished in the Late Jurassic of North America and possibly Africa
and appear to have been replaced ecologically by titanosaurs during the
Cretaceous.
A subfamily,
Diplodocinae, was erected to include
Diplodocus and its closest relatives, including
Barosaurus. More distantly related is the contemporaneous
Apatosaurus, which is still considered a diplodocid although not a diplodocine, as it is a member of the subfamily Apatosaurinae.
[Taylor, M.P. & Naish, D. 2005. The phylogenetic taxonomy of Diplodocoidea (Dinosauria: Sauropoda). PaleoBios 25(2): 1–7. (download )][Harris, J.D. 2006. The significance of Suuwassea emiliae (Dinosauria: Sauropoda) for flagellicaudatan intrarelationships and evolution. Journal of Systematic Palaeontology 4(2): 185–198.] The
Portuguese Dinheirosaurus and the African
Tornieria have also been identified as close relatives of
Diplodocus by some authors.
[Bonaparte, J.F. & Mateus, O. 1999. A new diplodocid, Dinheirosaurus lourinhanensis gen. et sp. nov., from the Late Jurassic beds of Portugal. Revista del Museo Argentino de Ciencias Naturales. 5(2):13–29. (download )][Rauhut, O.W.M., Remes, K., Fechner, R., Cladera, G., & Puerta, P. 2005. Discovery of a short-necked sauropod dinosaur from the Late Jurassic period of Patagonia. Nature 435: 670–672.]The
Diplodocoidea comprises the diplodocids, as well as
dicraeosaurids,
rebbachisaurids,
Suuwassea,
Amphicoelias and possibly
Haplocanthosaurus,
[Wilson, J. A., 2002, "Sauropod dinosaur phylogeny: critique and cladistica analysis". Zoological Journal of the Linnean Society 136: 217–276.] and/or the
nemegtosaurids.
This
clade is the sister group to,
Camarasaurus,
brachiosaurids and titanosaurians; the Macronaria.
Together they comprise Neosauropoda; the largest, most diverse and successful group of
sauropodomorph dinosaurs.
In popular culture
Diplodocus has been a famous and much-depicted dinosaur as it has been on display in more places than any other
sauropod dinosaur.
["Diplodocus." In: Dodson, Peter & Britt, Brooks & Carpenter, Kenneth & Forster, Catherine A. & Gillette, David D. & Norell, Mark A. & Olshevsky, George & Parrish, J. Michael & Weishampel, David B. The Age of Dinosaurs. Publications International, LTD. p. 58-59. ISBN 0-7853-0443-6.] Much of this has probably been due to its wealth of skeletal remains and former status as the longest dinosaur. However, the donation of many mounted skeletal casts by industrialist
Andrew Carnegie to potentates around the world at the beginning of the twentieth century
did much to familiarize it to people worldwide. Casts of
Diplodocus skeletons are still displayed in many museums worldwide, including an unusual
D. hayi in the
Houston Museum of Natural Science, and
D. carnegii in a number of institutions.
This includes donations by Carnegie or his trust to:

Holland's Diplodocus replica in the Paris Musée d'histoire naturelle, much as it was in 1908.
- The Museum for Paleontology and Geology in Bologna, Italy (replica, unveiled in 1909). Skulls from this cast (i.e., 'second-generation') are on display in museums in Milan and Naples.
- The Museo de Paleontología in Mexico City (replica, unveiled in 1929)
This project, along with its association with 'big science',
philanthropism and
capitalism, drew much public attention in Europe. The German satirical weekly
Kladderadatsch devoted a poem to the dinosaur:
[...] Auch ein viel älterer Herr noch muß
Den Wanderburschen spielen
Er ist genannt Diplodocus‚ und zählt zu den Fossilen
Herr Carnegie verpackt ihn froh
In riesengroße Archen
Und schickt als Geschenk ihn so
An mehrere Monarchen [...]
(Translation: [...] But even a much older gent • Sees itself forced to wander • Goes by the name Diplodocus • And belongs among the fossils • Mr. Carnegie packs him joyfully • In giant arcs • And sends him as gift this way • To multiple monarchs [...])
A further
D. carnegii is on display at the
Field Museum of Natural History in
Chicago. Additionally,
D. longus is displayed the
Senckenberg Museum in
Frankfurt (a skeleton made up of several specimens, donated in
1907 by the
American Museum of Natural History), Germany. A mounted and more complete skeleton of
D. longus is at the Smithsonian
National Museum of Natural History in
Washington, D.C., while a mounted skeleton of
D. hallorum (formerly
Seismosaurus), which may be the same as
D. longus, can be found at the
New Mexico Museum of Natural History and Science.
Diplodocus has been a frequent subject in dinosaur films, both factual and fictional, beginning with
Winsor McKay's 1914 classic
Gertie the Dinosaur. It was featured in the second episode of the award-winning BBC television series
Walking with Dinosaurs. The episode "Time of the Titans" follows the life of a simulated
Diplodocus 152 million years ago. The animated feature
Fantasia features many sauropods in the
Rite of Spring sequence, some narrower-headed ones of which may be
Diplodocus. In literature,
James A. Michener's book
Centennial has a chapter devoted to
Diplodocus, narrating the life and death of one individual.
Diplodocus is a commonly seen figure in dinosaur
toy and
scale model lines. It has had two figures in the
Carnegie Collection.