Ampelosaurus

*Ampelosaurus atacis*

***Ampelosaurus*** (/ˌæmpɨlɵˈsɔrəs/ AM-pi-lo-SAWR-əs; meaning "vine lizard") is a titanosaurian sauropod dinosaur hailing from the Late Cretaceous Period of what is now Europe. Its type species is *A. atacis*, named by Le Loeuff in 1995. A possible unnamed species has given *Ampelosaurus* an age reaching to the latest Cretaceous, from about 70 to 66 million years ago.

Like most sauropods, it would have had a long neck and tail but it also carried armor in the form of osteoderms. Over 500 bones have been assigned to *Ampelosaurus* and all but the braincase (assigned to *A. sp*.) has been assigned to *A. atacis*. They are assigned to the same species because all the differences in the limb proportions have been linked to individual variation. *A. atacis* is known from a few, well-preserved teeth and some cranial material. A right scapula was discovered associated with a coracoid. The blade of the scapula, contrary to most titanosaurs, is triangular. The blade narrows at one end instead of showing an expansion like most other genera. *A. atacis* is also known from a pubis about 75 centimetres (30 in) long and an ilium. Aside from that, it is known from a partial forelimb, and many femora.

Titanosaurians were a flourishing group of sauropod dinosaurs during Cretaceous times. The Spanish locality from the latest Cretaceous of “Lo Hueco” yielded a relatively well preserved, titanosaurian braincase, which shares a number of unique features with *A. atacis* from France. However, it appeared to differ from A. atacis in some traits also. The specimen has been provisionally identified as *Ampelosaurus* sp.. *A. sp*. is most likely a mature titanosaurian since the bones of the braincase have largely fused together.

*Ampelosaurus* lived alongside many other animals. Over 8500 specimens have been found alongside it, including gastropods, bivalves, crocodiles, other sauropods, plants and invertebrates in the Villalba de la Sierra, Gres de Saint-Chinian, Marnes Rouges Inférieures and Gres de Labarre formations. Recent attention has made *Ampelosaurus* one of the most well-known dinosaurs known from France.

## Description

Like most sauropods, *Ampelosaurus* would have had a long neck and tail, but it also carried armor in the form of osteoderms 25 to 28 centimetres (9.8 to 11.0 in) long. The four osteoderms found have three different morphologies, they are plate, bulb, and spine-shaped. This dinosaur would have stretched up to about 15-16 metres (50-53 ft) from snout to tail. *Ampelosaurus atacis* is known from many unattached bones and teeth. It is one of the best-known dinosaurs from France. It is considered to be a dwarf sauropod by Coria et al. (2005) because it has a smaller size in comparison with its ancestors.

### Skeleton

*Ampelosaurus* is one of the most completely known titanosaurian sauropod from Europe. Since 1989, over 500 bones discovered at the Upper Cretaceous Bellevue locality of southern France have been assigned to *A. atacis*. An abundant amount of well-preserved elements have been uncovered at Bellevue. In the original description, only a tooth and some vertebrae were examined. In 2005, a complete description was made by Le Loueff of all known material, allowing *Ampelosaurus* to be much better understood. All the material has been assigned to the species, and even though there are some differences in limb proportions, it has all been linked to individual variation.

*A. atacis* is known from a few, well-preserved teeth and some cranial material, a tooth of which was described in its original description. The teeth differentiate *Ampelosaurus* from *Magyarosaurus* and *Lirainosaurus*, both of which are also from Europe. The teeth are different from the two later genera as *Ampelosaurus* has teeth that are roughly cylindrical in the top with thin expansions at the bottom. They are 21 millimetres (0.83 in) high and about 6 millimetres (0.24 in) wide. Those expansions give its teeth a slight constriction between the root and the crown. The teeth are also quite different from the peg-like teeth of titanosaurids. The teeth, have a general morphology similar to titanosaurians *Antarctosaurus* and a braincase from Dongargaon. Another skull was described from southern France, but showed some differences, meaning there could have been at least two different titanosaurians in France during the Late Cretaceous.

The scapula was found attached to a coracoid. In the longer direction, the bone is 72 centimetres (28 in) long. The blade of the scapula, contrary to titanosaurs, is triangular, larger closer to the base. The blade narrows distally instead of showing an expansion. Differing from *Magyarosaurus* and *Saltasaurus*, the scapula does not have the dorsal crest at the base of the scapular blade. The shape of the coracoid is quadrangular, and the coracoid has a thickened cranial margin.

*Ampelosaurus* is also known from a pubis, about 75 centimetres (30 in) long. It has a strong distal expansion, that is similar to a titanosaur from Brazil, and a large foramen. Contrary to the South American titanosaurs, the ilium does not have an expansion on the side. The ischium, known from a shaft, is unexpanded distally and very well developed. It is also very flat. An incomplete radius is also known. It lacks the proximal and distal ends, and possesses a very prominent ridge along it. The largest and best-preserved specimens are both ulnas. The right ulna has a total length of 395 millimetres (15.6 in). The right ulna is small and slender, is missing an olecranon, and has a well-marked ridge. The left ulna is larger, with a length of 725 millimetres (28.5 in). The ulna has a deep radial fossa.

About 27 femora are known from Bellevue, making them the most common bone, most of them more-or-less complete. They are very flat craniocaudally but otherwise, lack any unusual features. In a study of its bone physiology, it was found that the maximum known femur length was 1,100 millimetres (43 in), which is much larger than previously known (802 millimetres (31.6 in)). That means, that the ancestors *Ampelosaurus* were slightly smaller than itself. 18 humeri are also known, but none of them approach the size of the largest femur. The humeri do not have a free medullary cavity. The humeri are robust, about 63 centimetres (25 in) long, with very expanded distal and proximal ends.

Three different types of osteoderms have been recovered at Bellevue. Two with large spines have been uncovered. At the base of each spine, which is about 12 centimetres (4.7 in) tall, are two large foramina. The internal faces are all concavo-convex and have a ridge opposite the spine. In side view, they have two sections, a low half that progressively thickens, and a spine.

#### Vertebrae

The holotype specimen of *A. atacis* is a group of three connected dorsal vertebrae. Vertebrae are uncommon from Bellevue and most of the vertebrae are poorly preserved. The vertebrae are opisthocoelous, with centra that lengthen toward the rear. Neural spines have been preserved on the vertebrae, and they face toward the rear. Two dorsal vertebrae were preserved with a complete, but very crushed neural arch, a neural spine with a characteristic shape: it is very widened distally and narrows downwards. The vertebrae also have an internal structure that is spongy, with very large cells. The caudal vertebrae are all strongly procoelous and are compressed on the sides. The neural spines of the caudal vertebrae are very narrow and very tall and point toward the rear. The middle caudal vertebrae are more compressed on the sides that the others. Also, the centrum of middle caudal vertebrae is longer proportionally. Two sacral vertebrae were known from Bellevue. They are poorly preserved, and are thought to belong to a juvenile. A complete sacrum was also found in 2002.

### Distinguishing anatomical features

This set of characters was identified by Le Loeuff in his description of *Ampelosaurus* to distinguish it from all other genera: teeth that weakly spatulate; a laterally widening distal extremity of neural spines on the dorsal vertebrae; neural arch of the dorsal vertebrae inclining strongly towards the rear; the lack of a distal expansion on the scapular blade; the presence of a light, ventral crest on top of the scapula; the presence of plate, bulb, and spine shaped osteoderms;[1] and, in 2005, Le Loeuff added that the constriction of the neural spine on the dorsal and cervical vertebrae was also probably a characteristic of *Ampelosaurus*.

### *Ampelosaurus* sp.

A fossil braincase from Lo Hueco was tentatively assigned to an unnamed species of *Ampelosaurus*, *A. sp*., in a 2013 article in the journal PLoS ONE. The braincase was found to share many features with A. atacis, such as a back of the skull that is flat. The braincase, MCCM-HUE-8741, is small in size overall, with a front-to-back length of 100.8 millimetres (3.97 in), and the maximum width of the left half being 64.3 millimetres (2.53 in). Parts of the bottom half of the braincase are missing. Even though section are missing, the specimen does not appear to have been deformed much, as the left and right halves are not very different.

Two frontals are preserved. They are each 57.3 millimetres (2.26 in) long and 64.3 millimetres (2.53 in) wide. The upper surface of each frontal is not smooth. One crest runs along the each frontal, and the together the two crests make up the orbital roof. Both parietals have also been found. The connection between them is marked by a ω-shaped crest. Viewed from the side, the parietal has two extensions. These extensions are not fully preserved, but they would have been on the border of the upper temporal fenestrae in their middle. Each parietal was preserved as 79.6 millimetres (3.13 in) wide. The basioccipital of the specimen from Lo Hueco is unique as it has an occipital condyle that is much wider than tall. The occipital condyle has an irregular surface that was probably caused by the loss of the original cartilaginous covering. The complete braincase was especially low in the skull, and was oriented to the side. The occipital condyle is 28.6 millimetres (1.13 in) wide and 15.8 millimetres (0.62 in) tall. The braincase floor is made by the parabasisphenoid. The prootic is a tall but not long bone. The basisphenoid is mostly on the side of it, along with the laterosphenoid, the parietal, and the otoccipital. The length of the prootic from the front to the back is around 10.6 millimetres (0.42 in).

#### Neuroanatomy

Compared with the *Giraffatitan*, the inner ear of *A. sp*. shows a more basal morphology. That feature is possibly related to a restricted range of possible movements that involve head-turning.

Like in *Jainosaurus* and most other non-avian archosaurs, the hindbrain and midbrain of A. sp. is relatively poorly preserved in the endocast. In contrast with TMM 40435 and a few other taxa such as cf. *Cetiosaurus oxoniensis* and *Giraffititan*, no characteristic "nub" of the cerebellum can be seen. As in TMM 40435 and many other archosaurs, the back of the brain is especially narrow in A. sp.

The cerebral region of the brain is separated from the rest of the brain by a distinct compression caused in the endocranial cavity. The rearmost part of the cerebral region of the braincase has a top with a small expansion. This is different from *Jainosaurus*. However, relatively much larger expansions are known in the diplodocoid sauropods *Dicraeosaurus* and *Diplodocus*. In MCCM-HUE-8741, the small opening in the skull roof middle is responsible for a swelling on the endocast that is suggestive of a pineal system. It is in the exact position where the pineal gland is expected to have been, between the forebrain and the midbrain.

The semicircular canals are contracted, and they are highly curved. The semicircular system of MCCM-HUE-8741 shows also a basal morphology, because the semicircular canals do not attach to each other.

## Discovery and naming

*Ampelosaurus* was originally found near the commune of Campagne-sur-Aude in the Aude département of France. It was recovered in the lower levels of the Marnes Rouges Inférieures Formation, which belong to the early Maastrichtian epoch of the Late Cretaceous Period, ~ 70 million years ago. These sediments represent an ancient floodplain with numerous river channels. French paleontologist Jean Le Loeuff first described and named this dinosaur in 1995. *Ampelosaurus* is derived from the Greek αμπελους, "the vineyard" and the Latin saurus, "reptile". Therefore, *Ampelosaurus* means "vineyard lizard" after the Blanquette de Limoux vineyard. The vineyard is located on the south side of the region *Ampelosaurus* was found in. The specific name is based on the Latin ajax, the "Aude river".

The first remains were found in a bonebed discovered in 1989, which produced numerous ribs and vertebrae from the back and tail, as well as many limb bones, but no skull material aside from one tooth. Four osteoderms of different sizes and shapes were also recovered from this bonebed. This material comes from several different individuals. Since 1989, more material has been uncovered in the same region of France, including a relatively complete skeleton with some elements of the skull and lower jaw.

Later, in 2001, the Campagne-sur-Aude site was explored again, this time by Gerard Chauvet, Jean-Luc Le Douarec, Colette Rives and Yvonne Vidoux. After 13 years of searching, they had uncovered a mostly complete skeleton that contained much more material, including bones unknown from the holotype. The material all went to the Musee des Dinosaures, and together took about 10 years to assemble.

The *A. sp*. was discovered in 2007. It was found in the course of the construction of a high-speed rail track connecting Madrid with Valencia, in a fossil site that many animals were found in, in the Villalba de la Sierra Formation. The site was at a locality named “Lo Hueco,” near the village of Fuentes, Castile-La Mancha, Spain. Over the course of several months, a large-scale emergency excavation by over 60 paleontologists and 100 manual workers allowed thousands of specimens of plants, invertebrates, and vertebrates of late Campanian-early Maastrichtian age to be saved, including *A. sp*.

## Classification

Characteristics of the tail vertebrae and the presence of osteoderms indicate that *Ampelosaurus* belongs to Lithostrotia, a group of derived titanosaurians which also includes *Alamosaurus* and *Saltasaurus*. Many other paleontologists have classified *Ampelosaurus* as belonging to Titanosauria, Saltasauridae, and Titanosauridae. *Ampelosaurus* may have an uncertain classification, but it is clearly a titanosaur, with many features found in titanosaurs.

More recently, *Ampelosaurus* has been put in a clade with other French and Spanish titanosaurs from the late Campanian to Maastrichtian, which was named Lirainosaurinae by Díez Díaz *et al.* in 2018. *Ampelosaurus* nested as sister taxon to *Atsinganosaurus* also from France, and the entire clade was placed in between the taxa commonly classified as Saltasauridae and taxa normally in either Aeolosaurini or Lognkosauria.

## Paleobiology

### Growth

*Ampelosaurus* seems to have grown in a way similar to more basal sauropods. After a certain point in its development, the microscopic material of the bone became very different from more basal Sauropoda. *Ampelosaurus* grew more slowly once the bone microstructure became unique among sauropods. Although Diplodocoidea and basal Macronaria also show an increase in bone growth and a decrease in growth rate around the presumed onset of sexual maturity, it is much more gradual than *Ampelosaurus*. The process of growing, which in other sauropods started around sexual maturity, was clearly delayed in *Ampelosaurus*. The period of growth after sexual maturity seems to be shortened in *Ampelosaurus* and is dominated by slow bone building instead of fast growth. Growth marks are generally rare in sauropods or appearing only late in ontogeny, if at all. The lack of growth marks is suggestive of fast and continuous growth in sauropods, which supports the hypothesis that they achieved large body size through because of fast growth. *Ampelosaurus* does not show growth marks on any bone sample. This is unusual to be found with the apparently reduced growth rate and high level of bone growth seen in it, as those features are often associated with the occurrence of growth marks.

### Histology

EFS, a system found on the surface of bones, is thought to show a growth plateau which indicates that maximum body size and skeletal maturity is reached in an individual. *Ampelosaurus* has not been known to have EFS, found on most non-titanosaurian sauropods. *Magyarosaurus*, a closely related titanosaur, *Lirainosaurus*, a titanosaur related to saltasaurids, *Alamosaurus*, a saltasaurid, and *Phuwiangosaurus*, a very basal titanosaur, were also found to have lacked EFS. However, the basal macronarian *Europasaurus* has been shown to have had EFS, so it was likely just titanosaurians that did not have them. The outer edge of the bones, were EFS would have been found, was well-preserved, and still lacked any fossilized proof of them being present for *Ampelosaurus*. However, in the PLoS ONE study that found the lack of EFS, the larger specimens were not tested, so *Ampelosaurus* might have had EFS. This is characteristic of titanosaurs, as diplodocoids and basal macronarians seem to have EFS. A majority of all *Ampelosaurus* specimens have been found with secondary osteons placed densely in the inner regions of bones, and lightly in outer regions. The osteon orientation found in *Ampelosaurus* of osteons not only facing across the bone is not typical of Neosauropoda. Also, there is no medullary cavity in any bones of *Ampelosaurus*. *Ampelosaurus* seems to have had many ontogenetic stages in its life based on its bone histology.

## Paleoecology

*Ampelosaurus atacis* is only known with certainty at the base of the Marnes de la Maurine Member of the Marnes Rouges Inférieures Formation in the Upper Aude Valley in southwestern France (Aude department). *Ampelosaurus* was also reported in other localities in France and Spain (notably Massecaps and Lo Hueco) but these specimens were found to belong to different titanosaurs. The age of the Marnes Rouges Inférieures Formation, which is divided in four members, extends from the late Campanian, 75 million years ago (for the Marnes Rouges de Campagne Member dated by palynology), to the end of the early Maastrichtian, 70 million years ago (for the Poudingue Fleuri Member). Magnetostratigraphic studies indicate an age of 71.5 million years (top of chron C32n.1n) for the localities of the basal part of the Marnes de la Maurine Member (including the Bellevue locality), which corresponds to the early Maastrichtian. At that time Europe was an archipelago made up of islands of varying sizes and changing geography over time. *Ampelosaurus* roamed the vast plains of the Ibero-Armorican Island, an emergent landmass made up of much of the present day France and Iberian Peninsula. The sediments of the Marnes Rouges Inférieures Formation consist of mudstones, sandstones, conglomerates, and siltstones, of fluvial and alluvial origin.

Fauna associated with *Ampelosaurus atacis* included another yet unnamed titanosaur, the ornithopod *Rhabdodon priscus* (represented by teeth, jaws, and postcranial bones), an indeterminate nodosaurid ankylosaur (known only by dermal scutes), an indeterminate Dromaeosauridae ( represented by teeth), the giant ground bird *Gargantuavis philoinos*, an undetermined pterosaur, the turtles *Foxemys mechinorum* (known by an incomplete skull and shell elements) and a new yet unnamed compsemydid (one skull and an isolated costal plate), an undescribed allodaposuchid eusuchian (represented by many elements including a complete skull showing similarities with *Musturzabalsuchus* and *Allodaposuchus subjuniperus*), and fisches (a lepisosteid and the coelacanth *Axelrodichthys megadromos*). Dinosaurs eggshells and nests are also present in the Marnes de la Maurine Member. They are represented by the oospecies *Cairanoolithus roussetensis*, *C. dughii*, and *Megaloolithus siruguei* in the lower part, *M. siruguei* and *Montanoolithus labadousensis* in the middle part, *M. siruguei* and *M. mamillare* in the upper part. *Fusioolithus baghensis* is recorded in the Poudingue Fleuri Member. *Megaloolithus* and *Fusioolithus* are titanosaur eggs. The oogenera *Cairanoolithus* and *Montanoolithus* are referred respectively to nodosaurids and dromaeosaurids. A few invertebrate and plant remains are also known. The macroflora, notably found at Bellevue, is represented by leaves of palm trees and cycads, as well as fragments of angiosperm wood from trees 10 to 15 m high.

### Biogeography

Titanosaurians were a flourishing group of sauropod dinosaurs during Cretaceous times. Fossils of titanosaurians have been found on all continents and their remains are abundant in a number of Late Cretaceous sites. Titanosaurian sauropods were among the most common dinosaurs in the ibero-Armorican island during the Campanian-Maastrichtian times. In this island a shift in the dinosaur fauna known as the Maastrichtian Dinosaur Turnover is observed in which a late Campanian-early Maastrichtian pre-turnover dinosaur fauna was replaced by an early-late Maastrichtian post-turnover assemblage. Concerning the titanosaurs the pre-turnover assemblage included small-sized species such as *Atsinganosaurus* and *Garrigatitan* (latest-middle Campanian to early-late Campanian in age) from southeastern France (Bouches-du-Rhône department) and *Lirainosaurus* (latest Campanian in age, 72 to 73.5 Ma) from north-central Spain (Burgos province, Treviño enclave), and moderate-sized forms such as *Lohuecotitan* (late Campanian-early Maastrichtian) from central Spain (Cuenca province) and *Ampelosaurus* (early Maastrichtian 71.5 Ma) from southwestern France (Aude department). The post-turnover assemblage is dominated by larger forms such as *Abditosaurus* (mid-early Maastrichtian, 70.5 Ma) from northeastern Spain (Lleida province). The latter is closely related to Gondwanan titanosaurs and does not show reduced growth rate or reduced body size, two common traits found in pre-turnover titanosaurs assemblages. It belongs to a distinct immigrant clade of large titanosaurs that reached the Ibero–Armorican island during the early Maastrichtian, being a member of the post-turnover titanosaurian assemblage of this island. This dispersal event from the southern landmasses, probably Africa, took place probably during the called KMa2 regressive event (which occurred about 70.6 million years ago during the Lower Maastrichtian), a eustatic event that affected the central Tethyan margin and northern Africa.

## JPInstitute.com Description

Ampelosaurus is the best-known long-necked (sauropod) European dinosaur.

Found in France in 1989, this giant plant eater is from the same family as Argentinosaurus. It was probably related to dinosaurs that traveled from South America when that continent was still connected to Africa. Like the huge African sauropods, such as Paralititan, it shares many characteristics with its South American ancestors.

A number Ampelosaurus skeletons have been found. This genus differs significantly enough from other European titanosaurs to show that these sauropods had a chance to evolve and diversify after they made the journey from South America through Africa to Europe. Like other titanosaurs, Ampelosaurus also had dermal scutes.

## Appearance in other media

### *Jurassic Park*

* Ampelosaurus appeared in the Jurassic World toys.

## Links

http://web.archive.org/web/20031006001704/http://www.jpinstitute.com/dinopedia/dinocards/dc\_ampel.html#

## References

1. ↑ Template:Cite book
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3. ↑ Template:Cite journal
4. ↑ 4.0 4.1 Cite error: Invalid `<ref>` tag; no text was provided for refs named `LeLoeuff1995`
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8. ↑ Template:Cite journal
9. ↑ 9.0 9.1 9.2 9.3 Cite error: Invalid `<ref>` tag; no text was provided for refs named `klein2012`
10. ↑ Template:Cite journal
11. ↑ 11.0 11.1 11.2 Template:Cite journal
12. ↑ Template:Cite journal
13. ↑ Cite error: Invalid `<ref>` tag; no text was provided for refs named `Vila&al2023`
14. ↑ 14.0 14.1 14.2 14.3 Cite error: Invalid `<ref>` tag; no text was provided for refs named `LeLoeuff2005`
15. ↑ Template:Cite thesis
16. ↑ Template:Cite journal
17. ↑ Template:Cite journal
18. ↑ Template:Cite journal
19. ↑ Template:Cite journal
20. ↑ Template:Cite journal
21. ↑ Template:Cite journal
22. ↑ Template:Cite journal
23. ↑ Template:Cite journal
24. ↑ Template:Cite journal
25. ↑ Template:Cite journal
26. ↑ Template:Cite journal
27. ↑ Template:Cite journal
28. ↑ Template:Cite journal
29. ↑ Cite error: Invalid `<ref>` tag; no text was provided for refs named `Vila&al2022`