Temporal range: Late Jurassic, 154 Ma
Mateus et al. in Sander et al., 2006
Mateus et al. in Sander et al., 2006
Europasaurus is a basal macronarian sauropod, a form of quadrupedal herbivorous dinosaur. It lived during the Late Jurassic (middle Kimmeridgian, about 154 million years ago) of northern Germany, and has been identified as an example of insular dwarfism resulting from the isolation of a sauropod population on an island within the Lower Saxony basin.
Discovery and naming
Around 1995 multiple small sauropod bones were uncovered from an open quarry at Langenberg Mountain, near the city of Oker, Germany. The 203 m (666 ft) quarry exposes well-dated rocks from the Lower Saxony Basin that have been well-dated to 154 million years old (early Oxfordian to late Kimmeridgian). Throughout the next 10 years about 650 individual bones were recovered and stored in the Dinosaurier-Freilichtmuseum Münchehagen (DFMMh) located close to Hanover. The variety of sauropod bones are located within an area of 60–80 m (200–260 ft) squared, and include variously articulated individuals. The name for the locality is middle Kimmeridgian bed 93 reference 2. From these specimens, the holotype was selected, a disarticulated but associated individual.
The holotype includes multiple cranial bones (premaxilla, maxilla and quadratojugal), a partial braincase, multiple mandible bones (dentary, surangular and angular), large amounts of teeth, cervical vertebrae, sacral vertebrae and ribs from the neck and torso. This specimen is catalogued under the specimen number DFMMh Verein zur Förderung der Niedersächsischen Paläontologie 291 (DFMMh/FV 291). At least 10 other individuals were referred to the same taxon based on overlap in material. In a 2006 description, these individuals were named as the new genus related to Brachiosauridae, Europasaurus holgeri. The description and naming paper was authored by Martin P. Sander, Octávio Mateus, Thomas Laven and Nils Knötschke. The given etymology for the genus name is "reptile from Europe", and the specific name honours Holger Lüdtke, the discoverer of the sauropod fossils.
Europasaurus is a very small sauropod, measuring only 6.2 m (20 ft) as an adult. This length was estimated based off a partial femur, scaled to the size of a nearly complete Camarasaurus specimen. Younger individuals are known, from sizes of 3.7 m (12 ft) to the youngest juvenile at 1.75 m (5.7 ft). The titanosaur Magyarosaurus is similarly sized, being 900 kg (2,000 lb) compared to Europasaurus at approximately 800 kg (1,800 lb). Another small titanosaur, Neuquensaurus, is larger than either taxon, being up to 9 m (30 ft) long and weighing 3,200 kg (7,100 lb)
Aside from being a very small neosauropod, Europasaurus was thought to have multiple unique morphological features to distinguish it from close relatives by its original describers, Sander et al. (2006). The nasal process of the premaxilla was thought to curve anteriorly while projecting upwards (now known to be preservational), there is a notch on the upper surface of the centra of cervical vertebrae, the scapula has a prominent process on the posterior surface of its body, and the astragalus (an ankle bone) is twice as wide as tall.
When compared to Camarasaurus, Europasaurus has a different morphology of the postorbital where the posterior flange is not as short, a short contact between the nasal and frontal bones of the skull, the shape of its parietal (rectangular in Europasaurus), and the neural spines of its vertebrae in front of the pelvis are unsplit. Comparisons with Brachiosaurus (now named Giraffatitan) were also mentioned, and it was identified that Europasaurus has a shorter snout, a contact between the quadratojugal and squamosal, and a humerus (upper forelimb bone) that has flattened and aligned proximal and distal surfaces. There were finally quick comparisons to the potential brachiosaurid Lusotitan, which has a different ilium and astragalus shape, and Cetiosaurus humerocristatus (named Duriatitan), which has a deltopectoral crest that is less prominent and extends across less of the humerus.
Nearly all external skull bones have been preserved among Europasaurus specimens, except the prefrontals. Some additional bones are only represented by very fragmented and uninformative fossils, such as the lacrimals. Eight premaxillae are known, with a generally rectangular snout shape as found in Camarasaurus. The anterior projection of the premaxilla identified in Sander et al. (2006) was re-identified as a preservational artifact in Marpmann et al. (2014), similar to the anatomy found in Camarasaurus and Euhelopus to a lesser degree. The dorsal projection of the premaxilla, the one which contacts the nasal bone, begins as a postero-dorsal projection, before becoming straight vertical at the point of the subnarial foramen, until it reaches the nasal. This weak "step" is seen in Camarasaurus and Euhelopus, and is present more strongly in Abydosaurus, Giraffatitan and a possible skull of Brachiosaurus. These latter taxa also have a longer snout, with more distance from the first tooth until the nasal process of the premaxilla. As well, Europasaurus shares with the basal camarasauromorphs (brachiosaurids, Camarasaurus, Euhelopus and Malawisaurus) a similarly sized orbit and nasal fenestra, whereas the nasal opening is significantly reduced in derived titanosaurs (Rapetosaurus, Tapuiasaurus and Nemegtosaurus).
A single maxilla is present in the well-preserved material of Europasaurus, DFMMh/FV 291.17. This maxilla has a long body, with two elongate processes, a nasal and a posterior process. There is only a weak lacrimal process, like in most sauropods except Rapetosaurus. The nasal process is elongate and covers the anterior and ventral rim of the antorbital fenestra. This process extends about 120º from the horizontal tooth row. The base of the nasal process also forms the body of the lacrimal process, and at their divergence is the antorbital fenestra, similar in shape to those of Camarasaurus, Euhelopus, Abydosaurus and Giraffatitan, but about 1/2 taller proportionally. The pre-antorbital fenestra, a small opening in front of or beneath the antorbital opening, is well developed in taxa like Diplodocus and Tapuiasaurus, is nearly absent, like in Camarasaurus and Euhelopus. There were about 12-13 total teeth in the maxilla of Europasaurus, fewer than in more basal taxa (16 teeth in Jobaria and 14-25 in Atlasaurus), but falling within the range of variation in Brachiosauridae (15 in Brachiosaurus to 10 in Abydosaurus). All of the unworn teeth preserved display up to four small denticles on their mesial edges. A small amount of the posterior tooth crowns are slightly twisted (~15º), but much less than in brachiosaurids (30-45º).
Among the nasal bones of Europasaurus, several are known, but few are complete or undistorted. The nasals are overlapped posteriorly by the frontal bones, and towards the side, they articulate bluntly with the prefrontals. Unlike the nasals of Giraffatitan, those in Europasaurus project horizontally forwards, forming a small portion of the skull roof over the antorbital fenestrae. Four frontals are known from Europasaurus, three being from the left and one being from the right. Because of their disarticulation, it is likely that the frontals never fused during growth, unlike in Camarasaurus. The frontals form a portion of the skull roof, articulating with other bones such as the nasals, parietals, prefrontals and postorbitals, and they are longer antero-posteriorly than they are wide, a unique character among a eusauropodan. Like in diplodocoids (Amargasaurus, Dicraeosaurus and Diplodocus), as well as Camarasaurus, the frontals are excluded from the frontoparietal fenestra (or parietal fenestra when frontals are excluded). The frontals are also excluded from the supratemporal fenestra margin (a widespread character in sauropods more derived than Shunosaurus), and they only have a small, unornamented participation in the orbit. Several parietal bones are known in Europasaurus, which show a rectangular shape much wider than long. the parietals are also wide when viewed from the back of the skull, being slightly taller than the foramen magnum (spinal cord opening). The parietals contribute to about half the post-temporal fenestra (opening above the very back of the skull) border, with the other region enclosed by the squamosal bones and some braincase bones. Parietals also form part of the edge of the supratemporal fenestra, which is wider than long in Europasaurus, like in Giraffatitan, Camarasaurus and Spinophorosaurus. Besides the before mentioned fenestra, the parietals also have a "postparietal fenestra", something rarely seen outside of Dicraeosauridae. A triradiate postorbital bone is present in Europasaurus, which evolved as the fusion of the postfrontal and postosbital bone of more basal taxa. Between the anterior and ventrally projecting processes the postorbital forms the margin of the orbit, and between the posterior and ventral processes it borders the infratemporal fenestra.
Multiple jugals are known from Europasaurus, which are more similar in morphology to basal sauropodomorphs than other macronarians. It forms part of the border of the orbit, infratemporal fenestra and the bottom edge of the skull, but does not reach the antorbital fenestra. The posterior process of the jugal are very fragile and narrow, showing a bone scar from the articulation with the quadratojugal. There are two prominences projecting from the back of the jugal body, which diverge at 75º and form the bottom and front edges of the infratemporal fenestra. Like in Riojasaurus and Massospondylus, two non-sauropod sauropodomorphs, the jugal forms a large part of the orbit edge, from the back to the front bottom corner. This feature has been seen in embryos of titanosaurs, but no adult individuals. The quadratojugal bone is an elongate element that has two projecting arms, one anterior and one dorsal. Like in other sauropods, the anterior process is longer than the dorsal, but in Europasaurus the arms are more similar lengths. The horizontal process is parallel to the tooth row of Europasaurus, similar to in Camarasaurus but unlike in Giraffatitan and Abydosaurus. There is a prominent ventral flange on the anterior arm of the bone, which is a possibly synapomorphy of Brachiosauridae, although it is also found in some Camarasaurus individuals. The two quadratojugal processes diverge at a nearly right angle (90º), although the dorsal process curves as it follows the shape of the quadrate. Squamosals found from Europasaurus show the same approximate shape in lateral view as Camarasaurus, that of a question mark. The squamosals articulate with many skull bones, including those of the skull roof, those of the ventral skull, and those of the braincase. Like the postorbitals, the squamosals are triradiate, with a ventral, anterior and medial process.
There are thirteen preserved elements of the palate of Europasaurus, including the quadrate, pterygoid and ectopterygoid. The quadrates articulate with the palate and braincase bones, as well as the external skull bones. They are similar in shape to those of Giraffatitan and Camarasaurus, and have well developed articular surfaces. A single shaft is present for a majority of the quadrates length, with a pterygoid wing along the medial side. Pterygoids are the largest of the sauropod palate bones, and it has a triradiate shape, like the postorbitals. An anterior projection contacts the opposite pterygoid, while a lateral wing contacts the ectopterygoid, and a posterior wing supports the quadrate and basipterygoid (a bone that provides connection between the palate and the braincase). The ectopterygoid is a small palate bone, which articulates the central palate bones (pterygoid and palatine) with the maxilla. Ectopterygoids are 'L' shaped, with an anterior process attaching to the maxilla, and a dorsal process that meets the pterygoid.
The cervical vertebrae of Europasaurus are the best preserved and most represented of the vertebral column. However, not the entire neck is known, so the cervical number could be between Camarasaurus (12 vertebrae) and Rapetosaurus (17 vertebrae). Additionally, the multiple cervical vertebrae come from different-aged individuals, and the centrum length and internal structure are known to change throughout development. The adult cervical centra are elongated and opisthocoelous (anterior end is ball-shaped), with a notch in the top of the rear end of the centrum. This feature was described as characteristic of Europasaurus but is also known in Euhelopus and Giraffatitan. In the side of the centra of Europasaurus there is an excavation which opens into the internal pneumaticity of the vertebrae. Unlike in Giraffatitan and brachiosaurids, Europasaurus does not have thin ridges (laminae) dividing this opening. Europasaurus shares laminae features on the upper vertebrae with basal macronarians and brachiosaurids. Differing from the anterior and middle cervicals, the posterior cervical vertebrae are less elongate, and taller proportionally, like in other macronarians, with significant changes in the positions of articular surfaces.
Among macronarians, fossilized skin impressions are only known from Haestasaurus, Tehuelchesaurus and Saltasaurus. Both Tehuelchesaurus and Haestasaurus may be closely related to Europasaurus as basal macronarians, and the characteristics of all sauropod skin impressions are similar. Haestasaurus, the first dinosaur known from skin impressions, preserved integument over a portion of the arm around the elbow joint approximately 19.5 by 21.5 cm (7.7 by 8.5 in) in area. Dermal impressions are more widespread in the material of Tehuelchesaurus, where they are known from the areas of the forelimb, scapula and torso. There are no bony plates or nodules, to indicate armour, but there are several types of scales. The skin types of Tehuelchesaurus are overall more similar to those found in diplodocids and Haestasaurus than in the titanosaur embryos of Auca Mahuevo. As the shape and articulation of the preserved tubercles in these basal macronarians are similar in other taxa where skin is preserved, including specimens of Brontosaurus excelsus and intermediate diplodocoids, such dermal structures are probably widespread throughout Neosauropoda.
When it was first named, Europasaurus was considered to be a taxon within Macronaria that didn't fall within the family Brachiosauridae or the clade Titanosauromorpha. This indicated that the dwarfism of the taxon was a result of evolution, instead of being a characteristic of a group. Three matrices were analysed with the inclusion of Europasaurus, that of Wilson (2002) and Upchurch (1998) and Upchurch et al. (2004). All analyses resulted in similar phylogenetics, where Europasaurus placed more derived than Camarasaurus but outside a clade of Brachiosauridae and Titanosauromorpha (now named Titanosauriformes). The results of the favoured analysis of Sander et al. (2006) are shown below on the left:
During a description of the vertebrae of Europasaurus by Carballido & Sander (2013), another phylogenetic analysis was conducted (right column above). The cladistic matrix was expanded to include more sauropod taxa, such as Bellusaurus, Cedarosaurus and Tapuiasaurus. The taxon Brachiosaurus was also separated into true Brachiosaurus (B. altithorax) and Giraffatitan (B. brancai), based on Taylor (2009). Based on this newer and more expansive analysis, Europasaurus was found to be in a similar placement, as a basal camarasauromorph closer to titanosaurs than Camarasaurus. However, Euhelopus, Tehuelchesaurus, Tastavinsaurus and Galvesaurus were placed between Europasaurus and Brachiosauridae.
Placement as a brachiosaurid
In a 2012 analysis of the phylogeny of Titanosauriformes, D'Emic (2012) considered Europasaurus to belong to Brachiosauridae, instead of being basal to the earliest brachiosaurids. The phylogeny resolved the most true brachiosaurids to date, although several potential brachiosaurids were instead determined to belong to Somphospondyli (Paluxysaurus, Sauroposeidon and Qiaowanlong). However, D'Emic was tentative in considering Europasaurus to be a confirmed brachiosaurid. While there was strong support in the phylogeny for its placement, Europasaurus, one of few basal macronarians with a skull, lacks multiple bones that display characteristic features of the group, such as caudal vertebrae. The cladogram below on the left illustrates the phylogenetic results of D'Emic (2012), with Euhelopodidae and Titanosauria collapsed.
A later analysis on titanosauriformes agreed with D'Emic (2012) in the placement of Europasaurus. It formed a polytomy with Brachiosaurus and the "French Bothriospondylus" (named Vouivria) as the basalmost brachiosaurids. Next most derived in the clade was Lusotitan, with Giraffatitan, Abydosaurus, Cedarosaurus and Venenosaurus forming a more derived clade of brachiosaurids. The "twisted" teeth of Europasaurus were found to be one of the unique features of Brachiosauridae, which could mean a confident referral of isolated sauropod teeth to the clade.
A further phylogenetic analysis was performed on Brachiosauridae, based on that of D'Emic (2012). This phylogeny, conducted by D'Emic et al. (2016), resolved a very similar placement of Europasaurus within Brachiosauridae, although Sonorasaurus was placed in a clade with Giraffatitan, and Lusotitan was placed in a polytomy with Abydosaurus and Cedarosaurus. The remaining tree was the same as in D'Emic (2012), although Brachiosaurus was collapsed into a polytomy with more derived brachiosaurids. Another phylogeny, Mannion et al. (2017) found similar results to D'Emic (2012) and D'Emic et al. (2016). Europasaurus was the basalmost brachiosaurid, with the "French Bothriospondylus", or Vouivria, as the next most basal brachiosaurid. Brachiosaurus was placed outside of a poltomy of all other brachiosaurids, Giraffatitan, Abydosaurus, Sonorasaurus, Cedarosaurus and Venenosaurus. A 2017 phylogeny, that of Royo-Torres et al. (2017), resolved more complex relations within Brachiosauridae. Besides Europasaurus as the basalmost brachiosaurid, there were two subgroups within the clade, one containing Giraffatitan, Sonorasaurus and Lusotitan, and another including almost all other brachiosaurids, as well as Tastavinsaurus. This second clade would be termed Laurasiformes under the group's definition. Brachiosaurus was in a polytomy with the two subclades of Brachiosauridae. The phylogeny of Royo-Torres et al. (2017) can be seen above, in the right column.
It was identified that Europasaurus was a unique dwarf species, and not a juvenile of an existing taxon like Camarasaurus, by a histology analysis of multiple specimens of Europasaurus. The youngest specimen (DFMMh/FV 009) was shown by this analysis to lack signs of agins such as growth marks or laminar bone tissue, and is also the smallest specimen at 1.75 m (5.7 ft) in length. Such bone tissue is an indicator of rapid growth, so the specimen is probably a young juvenile. A larger specimen (DFMMh/FV 291.9) at 2 m (6.6 ft) shows large amounts of laminar tissue, with no growth marks present, so is likely a juvenile as well. The next smallest specimen (DFMMh/FV 001) has shows the presence of growth marks (specifically annuli), and at the length of 3.5 m (11 ft) is possibly a subadult. Further larger, DFMMh/FV 495 displays mature osteons as well as annuli, and is 3.7 m (12 ft). The second largest analysed specimen (DFMMh/FV 153) also shows growth marks, but they are more frequent. This specimen is 4.2 m (14 ft). A single partial femur represents the largest known Europasaurus individual, at a body length of 6.2 m (20 ft). Unlike all other specimens, this one (DFMMh/FV 415) shows the presence of lines of arrested growth, indicating it died after reaching full body size. The internal bone is also partially lamellar, which shows it had stopped growing recently.
These combinations of growth factors show that Europasaurus developed its small size because of a largely reduced growth rate, gaining size slower than larger taxa such as Camarasaurus. This slowing growth rate is the opposite of the general trend of sauropods and theropods, who reached greater sizes with increased growth rates. Some of the close relatives of Europasaurus represent the largest dinosaurs known, including Brachiosaurus and Sauroposeidon. Marpmann et al. (2014) proposed that the small size and reduced growth rate of Europasaurus was an effect of pedomorphism, where the adults of taxa retain juvenile characteristics, such as size.
It has been suggested that an ancestor of Europasaurus would have quickly decreased in body size after emigrating to an island that existed at the time, as the largest of the islands in the region around northern Germany was smaller than 200,000 km (120,000 mi) squared, which may not have been able to support a community of large sauropods. Alternately, a macronarian may have shrunken concurrently with a larger landmass, until achieving the size of Europasaurus. Previous studies on insular (island) dwarfism are largely restricted to the Maastrichtian of Haţeg Island in Romania, home to the dwarf titanosaur Magyarosaurus and the dwarf hadrosaur Telmatosaurus. Telmatosaurus is known to be from a small adult, and although it is very small, Magyarosaurus specimens of small sizes are known to be from adult to old individuals. Magyarosaurus dacus adults were a similar body size to Europasaurus, but the largest of the latter had longer femora than the largest of the former, while Magyarosaurus hungaricus was significantly larger than either taxon. The dwarfism in Europasaurus represents the only significant rapid body mass change in derived Sauropodomorpha, with the general trend of taxa being a growth in overall size in other groups.
The Langenberg locality in Germany, from the early Oxfordian to late Kimmeridgian, displays the variety of plant and animal life from an island ecosystem from the late Jurassic. During the Kimmeridgian the locality would have been marine, being located between the Rhenisch, Bohemian, and London-Brabant Massifs. This does not indicate that the taxa present were marine, as the animals and plants may have been deposited allochthonously (albeit only by a short distance) from the surrounding islands. The sediments to show that there was an occasional influx of fresh or brackish water, and the fossils preserved display that. There are large numbers of marine bivalve fossils, as well as echinoderms and microfossils present in the limestone of the quarry, although many of the animals and plants were terrestrial.
Many marine taxa are preserved at Langenberg, although they would not have co-existed often with Europasaurus. There are at least three turtle genera, Plesiochelys, Thalassemys and up to two unnamed taxa. Actinopterygian fish are abundant, being represented by Lepidotes, Macromesodon, Proscinetes, Coelodus, Macrosemius, Notagogus, Histionotus, Ionoscopus, Callopterus, Caturus, Sauropsis, Belonostomus, and Thrissops. Also present are at least five distinct morphologies of hybodont sharks, the neoselachians Palaeoscyllium, Synechodus and Asterodermus. Two marine crocodilians are known from Langenberg, Machimosaurus and Steneosaurus, which likely fed off turtles and fish, and the amphibious crocodilian Goniopholis has also been found.
Conifer cones and twigs can be identified as the araucarian Brachyphyllum, from the terrestrial fossils of the site. Deposited in the locality are many taxa, including a large accumulation of Europasaurus skeletons. Among all the terrestrial fossils, there is a very large amount of Europasaurus bones and individuals. At least 450 bones from Europasaurus were recovered from the Langenberg Quarry, with about 1/3 bearing tooth marks Of these tooth marks, the sizes and shapes match well with the teeth of fish, crocodilians or other scavengers, but no confirmed theropod marks. The high number of individuals present suggests that a herd of Europasaurus was crossing a tidal zone and drowned. While the dominant large-bodied animal present is Europasaurus, there is also material from a diplodocid sauropod, a stegosaurian, and multiple theropods. Three cervicals of the diplodocid are preserved, and from their size it is possible that the taxon was also a dwarf. The stegosaurian and variety of theropods only preserve teeth, with the exception of a few bones possibly from a taxon in Ceratosauridae. Isolated teeth show that there were at least four different types of theropods present at the locality, including the megalosaurid Torvosaurus sp. as well as an additional megalosaurid and indeterminate members of the Allosauridae and Ceratosauria; and there are also the oldest teeth known from Velociraptorinae.
Besides the dinosaurs, many small-bodied terrestrial vertebrates are also preserved in the Langenberg quarry. Such animals include a well-preserved three-dimensional pterosaur skeleton from Dsungaripteridae, and isolated remains from Ornithocheiroidea and Ctenochasmatidae; a paramacellodid lizard; and partial skeletons and skulls from a relative of Theriosuchus now named as the genus Knoetschkesuchus. Teeth from dryolestid mammals are also preserved, as well as a docodont, a taxon in Eobaataridae, a multituberculate with similarities to Proalbionbataar (now named Teutonodon).
Dinosaur footprints preserved at the Langenberg Quarry display a possible reason for the extinction of Europasaurus, and potentially other insular dwarfs present on the islands of the region. The footprints are located 5 m (16 ft) above the deposit of Europasaurus individuals, which shows that at least 35,000 years after that deposit there was a drop in sea level which allowed for a faunal overturn. The inhabiting theropods of the island, that coexisted with Europasaurus, would have been about 4 m (13 ft), but the theropods that arrived over the land bridge preserve footprints up to 54 cm (21 in), which indicates a body size between 7 and 8 m (23 and 26 ft) if reconstructed as an allosaurian. It was suggested by the describers of these tracks (Jens Lallensack and colleagues), that these theropod taxa likely made the specialized dwarf fauna extinct, and the bed from which the footprints originated (Langenberg bed 92) was probably the youngest boundary that Europasaurus lived.
- Sander, P.M.; Mateus, O.V.; Laven, T.; Knötschke, N. (2006). "Bone histology indicates insular dwarfism in a new Late Jurassic sauropod dinosaur". Nature. 441 (7094): 739–741. Bibcode:2006Natur.441..739M. doi:10.1038/nature04633. PMID 16760975.
- Sander, P.M.; Mateus, O.V.; Laven, T.; Knötschke, N. (2006). "Supplementary Information for: Bone histology indicates insular dwarfism in a new Late Jurassic sauropod dinosaur". Nature. 441: 739–741. Bibcode:2006Natur.441..739M. doi:10.1038/nature04633. PMID 16760975.
- Stein, K.; Csiki, Z.; Curry-Rogers, K.; Weishampel, D.B.; Redelstorff, R.; Carballido, J.L.; Sander, P.M. (2010). "Small body size and extreme cortical bone remodeling indicate phyletic dwarfism in Magyarosaurus dacus (Sauropoda: Titanosauria)". Proceedings of the National Academy of Sciences. 107 (20): 9258–9263. Bibcode:2010PNAS..107.9258S. doi:10.1073/pnas.1000781107. ISSN 0027-8424. PMC . PMID 20435913.
- Marpmann, J.S.; Carballido, J.L.; Sander, P.M.; Knötschke, N. (2014). "Cranial anatomy of the Late Jurassic dwarf sauropod Europasaurus holgeri (Dinosauria, Camarasauromorpha): Ontogenetic changes and size dimorphism". Journal of Systematic Palaeontology. 13 (3): 1–43. doi:10.1080/14772019.2013.875074.
- Carballido, J.L.; Sander, M.P. (2013). "Postcranial axial skeleton of Europasaurus holgeri (Dinosauria, Sauropoda) from the Upper Jurassic of Germany: implications for sauropod ontogeny and phylogenetic relationships of basal Macronaria" (PDF). Journal of Systematic Palaeontology. 12 (3): 335–387. doi:10.1080/14772019.2013.764935. ISSN 1477-2019.
- Upchurch, P.; Mannion, P.D.; Taylor, M.P. (2015). "The Anatomy and Phylogenetic Relationships of "Pelorosaurus" becklesii (Neosauropoda, Macronaria) from the Early Cretaceous of England". PLOS One. 10 (6): e0125819. doi:10.1371/journal.pone.0125819. ISSN 1932-6203. PMC . PMID 26039587.
- Giménez, O. del V. (2007). "Skin impressions of Tehuelchesaurus (Sauropoda) from the Upper Jurassic of Patagonia" (PDF). Revista del Museo Argentino de Ciencias Naturales. 9 (2): 119–124. doi:10.22179/revmacn.9.303.
- Wilson, J.A. (2002). "Sauropod dinosaur phylogeny: critique and cladistic analysis" (PDF). Zoological Journal of the Linnean Society. 136 (2): 217–276. doi:10.1046/j.1096-3642.2002.00029.x.
- Upchurch, P.M. (1998). "The phylogenetic relationships of sauropod dinosaurs". Zoological Journal of the Linnean Society. 124: 43–103. doi:10.1111/j.1096-3642.1998.tb00569.x.
- Upchurch, P.M.; Barrett, P.M.; Dodson, P. (2004). "Sauropoda". In Weishampel, D.B.; Dodson, P.; Osmólska, H. The Dinosauria (2 ed.). Berkeley: University of California Press. pp. 259–322. ISBN 978-0-520-94143-4.
- Taylor, M.P. (2009). "A re-evaluation of Brachiosaurus altithorax Riggs 1903 (Dinosauria, Sauropoda) and its generic separation from Giraffatitan brancai (Janensch 1914)". Journal of Vertebrate Paleontology. 29: 787–806. doi:10.1671/039.029.0309.
- D'Emic, M.D. (2012). "The early evolution of titanosauriform sauropod dinosaurs". Zoological Journal of the Linnean Society. 166 (3): 624–671. doi:10.1111/j.1096-3642.2012.00853.x.
- Mannion, P.D.; Upchurch, P.; Barnes, R.N.; Mateus, O. (2013). "Osteology of the Late Jurassic Portuguese sauropod dinosaur Lusotitan atalaiensis (Macronaria) and the evolutionary history of basal titanosauriforms". Zoological Journal of the Linnean Society. 168 (1): 98–206. doi:10.1111/zoj.12029. ISSN 0024-4082.
- D’Emic, M.D.; Foreman, B.Z.; Jud, N.A. (2016). "Anatomy, systematics, paleoenvironment, growth, and age of the sauropod dinosaur Sonorasaurus thompsoni from the Cretaceous of Arizona, USA". Journal of Paleontology. 90 (1): 102–132. doi:10.1017/jpa.2015.67. ISSN 0022-3360.
- Mannion, P.D.; Allain, R.; Moine, O. (2017). "The earliest known titanosauriform sauropod dinosaur and the evolution of Brachiosauridae". PeerJ. 5: e3217. doi:10.7717/peerj.3217. ISSN 2167-8359. PMC . PMID 28480136.
- Royo-Torres, R.; Fuentes, C.; Meijide, M.; Meijide-Fuentes, F.; Meijide-Fuentes, M. (2017). "A new Brachiosauridae Sauropod dinosaur from the lower Cretaceous of Europe (Soria Province, Spain)". Cretaceous Research. 80: 38–55. doi:10.1016/j.cretres.2017.08.012.
- Nopcsa, F. (1914). "Über das Vorkommen der Dinosaurier in Siebenbürgen". Ver. Zool. Bot. Ges. Wien. 54: 12–14.
- Weishampel, D.B.; Norman, D.B.; Grigorescu, D. (1993). "Telmatosaurus transsylvanicus from the Late Cretaceous of Romania: the most basal hadrosaurid dinosaur". Palaeontology. 36: 361–385.
- Benson, R.B.J.; Campione, N.E.; Carrano, M.T.; Mannion, P.D.; Sullivan, C.; Upchurch, P.; Evans, D.C. (2014). "Rates of Dinosaur Body Mass Evolution Indicate 170 Million Years of Sustained Ecological Innovation on the Avian Stem Lineage". PLoS Biology. 12 (5): e1001853. doi:10.1371/journal.pbio.1001853. PMC . PMID 24802911.
- Wings, O. (2015). "The Langenberg Quarry near Goslar: Unique window into a terrestrial Late Jurassic ecosystem in Northern Germany" (PDF). Abstracts of the 12th Symposium on Mesozoic Terrestrial Ecosystems: 99–100.
- Schwarz, D.; Raddatz, M.; Wings, O. (2017). "Knoetschkesuchus langenbergensis gen. nov. sp. nov., a new atoposaurid crocodyliform from the Upper Jurassic Langenberg Quarry (Lower Saxony, northwestern Germany), and its relationships to Theriosuchus". PLOS One. 12 (2): e0160617. Bibcode:2017PLoSO..1260617S. doi:10.1371/journal.pone.0160617.
- Wings, O. (2013). "Unique taphonomy of the dwarfed sauropod Europasaurus from Late Jurassic marine strata of the Langenberg Quarry (Lower Saxony, Northern Germany)" (PDF). Journal of Vertebrate Paleontology, Program and Abstracts. 73rd Annual Meeting of the Society of Vertebrate Paleontology. 2013: 239.
- Wings, O.; Sander, M.P. (2012). "The Late Jurassic Vertebrate Assemblage of the Langenberg Quarry, Oker, Northern Germany". 10th Annual Meeting of the European Association of Vertebrate Paleontologists. 20: 281–284.
- Marinheiro, J.; Mateus, O. (2011). "Occurrence of the marine turtle Thalassemys in the Kimmeridgian of Oker, Germany" (PDF). 71st Annual Meeting of the Society of Vertebrate Paleontology. Abstracts of the 71st Annual Meeting of the Society of Vertebrate Paleontology: 151.
- Mudroch, A.; Thies, D. (1996). "Knochenfischzähne (Osteichthyeso Actinopterygii) aus dem Oberjura (Kimmeridgium) des Langenbergs bei Oker (Norddeutschland)" (PDF). Geologica et Palaeontologica (in German). 30: 239–265.
- Thies, D. (1995). "Placoid scales (Chondrichthyes: Elasmobranchii) from the Late Jurassic (Kimmeridgian) of northern Germany". Journal of Vertebrate Paleontology. 15 (3): 463–481. doi:10.1080/02724634.1995.10011242.
- Karl, H.-V.; Gröning, E.; Brauckmann, C.; Schwarz, D.; Knötschke, N. (2006). "The Late Jurassic crocodiles of the Langenberg near Oker, Lower Saxony (Germany), and description of related materials (with remarks on the history of quarrying the "Langenberg Limestone" and "Obernkirchen Sandstone")". Clausthaler Geowissenschaften. 5: 59–77.
- Slodownik, M.; Wings, O. (2015). "Bite marks on Europasaurus bones from the Langenberg Quarry near Goslar (Lower Saxony, Germany)" (PDF). 13th Annual Meeting of the European Association of Vertebrate Palaeontologists Opole, Poland, Abstracts: 141.
- Gerke, O.; Wings, O. (2016). "Multivariate and Cladistic Analyses of Isolated Teeth Reveal Sympatry of Theropod Dinosaurs in the Late Jurassic of Northern Germany". PLOS One. 11 (7): e0158334. Bibcode:2016PLoSO..1158334G. doi:10.1371/journal.pone.0158334.
- Lubbe, T. van Der; Richter, U.; Knötschke, N. (2009). "Velociraptorine Dromaeosaurid Teeth from the Kimmeridgian (Late Jurassic) of Germany" (PDF). Acta Palaeontologica Polonica. 54 (3): 401–408. doi:10.4202/app.2008.0007.
- Martin, T.; Schultz, J.A.; Schwermann, A.H.; Wings, O. (2016). "First Jurassic mammals of Germany: Multituberculate teeth from Langenberg Quarry (Lower Saxony)" (PDF). Palaeontologia Polonica. 67: 171–179. doi:10.4202/pp.2016.67_171.
- Lallensack, J.N.; Sander, M.P.; Knötschke, N.; Wings, O. (2015). "Dinosaur tracks from the Langenberg Quarry (Late Jurassic, Germany) reconstructed with historical photogrammetry: Evidence for large theropods soon after insular dwarfism" (PDF). Palaeontologica Electronica. 18 (2): 1–34.
- Hall, B.K.; Hallgrímsson, B. (2011). Strickberger's Evolution. Jones & Bartlett Publishers. p. 446. ISBN 978-1-4496-4722-3.
- Brusatte, S.L. (2012). Dinosaur Paleobiology. John Wiley & Sons. p. 210. ISBN 978-0-470-65658-7.
- Bolecsek, C.; Wings, O. (2013). "Europasaurus holgeri – the dwarfed dinosaur from the Late Jurassic of Germany". VI Journadas Internacionales sobre Paleontología de Dinosaurios y su Entorno. Salas de los Infantes, Burgos. Libro du resúmenes: 46–47. ISBN 84-695-8567-3.
- Organ, C.L.; Brusatte, S.L.; Stein, K. (2009). "Sauropod dinosaurs evolved moderately sized genomes unrelated to body size". Proceedings of the Royal Society of London B: Biological Sciences. 276 (1677): 4303–4308. doi:10.1098/rspb.2009.1343. ISSN 0962-8452. PMC . PMID 19793755.
- Filippini, F.S.; Otero, A.; Gasparini, Z. (2016). "The phylogenetic relevance of the sacrum among macronarian sauropods: insights from a pelvis from the Upper Cretaceous of Patagonia, Argentina". Alcheringa. 41: xxx–xxx. doi:10.1080/03115518.2016.1180806. ISSN 0311-5518.