Article | Open

A Sauropod Tooth from the Santonian of Hungary and the European Late Cretaceous ‘Sauropod Hiatus’

  • Scientific Reports 7, Article number: 3261 (2017)
  • doi:10.1038/s41598-017-03602-2
  • Download Citation
Published online:


The lack of sauropod body fossils from the 20 My-long mid-Cenomanian to the late Campanian interval of the Late Cretaceous in Europe is referred to as the ‘sauropod hiatus’, with only a few footprints reported from the Apulian microplate (i.e. the southern part of the European archipelago). Here we describe a single tooth from the Santonian continental beds of Iharkút, Hungary, that represents the first European body fossil evidence of a sauropod from this critical time interval. The mosaic of derived and plesiomorphic features documented by the tooth crown morphology points to a basal titanosauriform affinity suggesting the occurrence of a clade of sauropods in the Upper Cretaceous of Europe that is quite different from the previously known Campano-Maastrichtian titanosaurs. Along with the footprints coming from shallow marine sediments, this tooth further strengthens the view that the extreme rarity of sauropod remains from this period of Europe is the result of sampling bias related to the dominance of coastal over inland sediments, in the latter of which sauropod fossils usually occur. This is also in line with the hypothesis that sauropods preferred inland habitats to swampy environments.


Sauropod dinosaurs were important elements of different Late Cretaceous continental vertebrate communities in Europe. Their record comes, however, mainly from upper Campanian to upper Maastrichtian sediments, and only a very few isolated and fragmentary remains are known from older Upper Cretaceous deposits1,2,3. Almost all of these sporadic remains, both skeletal elements and footprints, have been discovered in Cenomanian localities4,5,6,7,8,9,10,11,12,13 with some of these even possibly reworked from older, Albian sediments. Accordingly, the late Cenomanian to late Campanian time period, an approximately 20 My long interval14, was long thought to represent a hiatus in the European sauropod record8, 15. The discovery of some Turonian-Coniacian sauropod footprints in Croatia1, 16 and a trackway of a probable small sauropod from the Santonian of Italy1, 17, however, seem to challenge this view, and suggest a sampling bias instead18, mainly due to the “rarity of inland sediments and dominance of coastal deposits” (Mannion and Upchurch1 2011:529) in the European Upper Cretaceous.

Here we report a sauropod dinosaur tooth from the Santonian of Iharkút, Hungary, an unexpected discovery that represents the first body fossil of the clade known from this poorly sampled period of the sauropod fossil record in the European Cretaceous.

Material and Methods

The isolated tooth (MTM PAL 2017.1.1.) described here was collected in the Iharkút vertebrate locality (western Hungary) and is housed in the Vertebrate Paleontological Collection of the Hungarian Natural History Museum, Budapest. The specimen was prepared mechanically in the lab of the Hungarian Natural History Museum and the fragmentary margins of the tooth were fixed by cyanoacrylic glue.

The description of the tooth follows the dental terminology proposed by Smith and Dodson19. Quantitative shape descriptors such as Slenderness Index (SI: ratio of crown height to maximum mesiodistal width)20 and Compression Index (CI: ratio of the maximum labiolingual width to the maximum mesiodistal width of the crown)2 were also calculated.

Locality and geological setting

The Iharkút vertebrate locality is in an open-pit bauxite mine near the villages of Németbánya and Bakonyjákó (Bakony Mountains, western Hungary, N47°13′52″, E17°39′01″; Fig. 1A). The oldest rock unit at the locality is the Upper Triassic Main Dolomite Formation, the karstified sinkholes of which were filled up by Cretaceous (pre-Santonian) bauxites (Nagytárkány Bauxite Formation), formerly mined here. The bauxite and the karstified paleosurface is covered by alluvial floodplain deposits of the Santonian Csehbánya Formation consisting of alternating coarse basal breccia, sandstone, siltstone and paleosol beds deposited in a continental environment21. Bones at the site are accumulated in bonebeds, among which the most productive one (SZ-6 site, Fig. 1B,C), a greyish, coarse basal breccia layer, produced most of the vertebrate remains including the tooth described in this study. Systematic excavations at the locality resulted in more than 50.000 specimens, represented by isolated and associated bones and teeth of fishes, amphibians, turtles, mosasaurs and other lizards, pterosaurs, crocodyliforms, and dinosaurs, including birds3, 22.

Figure 1
Figure 1

The Santonian Iharkút vertebrate locality (Hungary), and the geological background of site SZ-6. (A) Location map of the Iharkút vertebrate locality. (Maps were created by AŐ with Corel Draw 12, (B), Aerial photo of the Iharkút open-pit, showing the position of site SZ-6. (Photo was taken by Péter Somogyi-Tóth) (C), Stratigraphic section of the Csehbánya Formation exposed in the open-pit with site SZ-6 highlighted by green (modified after Botfalvai et al.)21.


Crown morphology

The tooth (MTM PAL 2017.1.1.; Fig. 2) has most of the crown preserved. Apically and basally, however, it is broken, thus the tip and the base of the crown, as well as the root, are missing. The crown is apicobasally elongate (preserved apicobasal height: 10.2 mm) and mesiodistally narrow (4.8 mm) with a minimum SI value of 2.12 (Fig. 2). This gives a minimum log10 value of 0.326 for SI that falls just outside of or on the edge of the SI cluster for Macronaria23 indicating a relatively wide crown. The mesial and distal margins of the tooth extend parallel to each other before converging apically. Apically, the crown bends labially at first and then seems to incline backwards lingually near its very tip. The lingual surface of the crown (Fig. 2B) does not have a central longitudinal ridge, but is divided into three parts: the basal third is mesiodistally flat with a very shallow depression centrally bordered by shallow, low and rounded mesial and distal buttresses; the central third, albeit placed in the same plane, becomes slightly concave and is still bordered by subtly raised mesial and distal shoulders (‘rounded edge’ in Fig. 2B,E), while the apical third of the lingual surface, gently bending labially, is also slightly concave.

Figure 2
Figure 2

Basal titanosauriform tooth (MTM PAL 2017.1.1.) from the Santonian of Iharkút, Hungary. (A) apical, (B) lingual, (C) labial, (D) mesial, (E) distal, (F) oblique distolingual, and (G) basal views. Abbreviations: bap, broken apex of the crown; cla, convex labial surface; cli, slightly concave lingual surface; pc, pulp cavity; re, rounded edge; sc, scratch.

The labial surface is strongly convex (Fig. 2A,D,E), resulting in a D-shaped transverse cross-section at mid-crown, with a CI of 0.79. The same D-shaped cross-section is still present at the base of the crown (Fig. 2G). Apically, the crown becomes more spatulate, labiolingually pinched, than in its basal part. Here, the labial surface also curves mildly labially, mirroring the more marked labial bend of the lingual surface. No distinct grooves or ridges are present on any side of the crown. It is also void of marked carinae, presenting only the two parallel, lingually shifted, low and rounded edges that separate the mesial and distal sides from the lingual surface (Fig. 2B,F). Most of the enamel surface appears to be worn all around the crown; as such, the surface of the crown is smooth and unwrinkled, although covered by feeding-related scratches and pits (see below).

The pulp cavity, filled with pyrite and calcite, can be observed both basally and apically. Whereas its basal section is subcircular in cross-section, apically the pulp cavity becomes strongly labiolingually compressed.

Tooth wear

The crown does not show well-distinguished wear facets with exposed dentine, or they may not be preserved due to the missing crown apex (Fig. 3). It seems, nevertheless, that the entire crown was more or less uniformly eroded during life, resulting in hundreds of shorter or longer scratches that are mainly parallel or sub-parallel with the long axis of the crown (Fig. 3A–C). Accordingly, a high orientational consistency is characteristic, with very rare crosswise oriented scratches occurring mainly apically. Scratches are the best developed and longest (over 5–7 mm) along the mesiolabial and distolabial margins of the crown (Fig. 3A,C). Some scratches on the mesial and distal sides are slightly oblique, starting basally from the mesial or distal margin and ending apically on the labial surface. Although scratches are dominant, shallow, apicobasally elongate and triangular pits are also present (Fig. 3F), mainly in the apical third of the crown. A ‘meteor shower’ pattern of short scratches and pits, similar to that reported on the titanosaur teeth from Lo Hueco, Spain24, can be observed on the lingual surface of the crown.

Figure 3
Figure 3

Wear pattern of the basal titanosauriform tooth (MTM PAL 2017.1.1.) from the Santonian of Iharkút, Hungary. (A–C) Details of the worn surface of labial (D) side. (E) Lingual view of the tooth crown; (F) ‘meteor shower’ pattern of short scratches and pits on the lingual surface of the crown. Abbreviations: msc, ‘meteor shower’ pattern of short scratches; pi, pit; sc, scratch.

Since the tooth crown shows a uniformly eroded pattern, it cannot be ruled out that it is a digested tooth etched by gut acid25 resulting in an unwrinkled, enamel-less surface but still leaving the deeper scratches and pits preserved on the dentine surface.


Since this tooth represents the only indication of sauropod dinosaurs in Iharkút up to now, it raises the question whether this specimen might have been reworked from older deposits, as teeth are known to survive relatively long-distance transport and reworking without significant damage26. Nonetheless, there are several arguments against this scenario that support the autochthony of the tooth at the site: 1) the tooth has exactly the same dark brownish colour (due to the disperse early diagenetic pyrite present in almost all bones) and general textural pattern as that of the other vertebrate remains from the site; 2) the pulp cavity is lined with a crust of early diagenetic pyrite, in a pattern that is characteristic for many teeth and bones from Iharkút, especially those that have extensive internal cavities, such as theropod and pterosaur bones27;3) the tooth is completely void of any signs of abrasion that would have eventually resulted from the interaction between sediment particles and tooth during reworking, 4) the tooth surface is pristine, well-preserved and shows ornamentation as well as features generated only by tooth-food contact. Taken together, these taphonomic features indicate that, similarly to the other teeth and bones preserved in site Sz-6 from Iharkút, the primary depositional setting of MTM PAL 2017.1.1. is represented by the bone-yielding beds of this site.

Identification and comparisons

Teeth of almost all dentulous vertebrate taxa discovered at Iharkút (from fish to enantiornithine birds) are known from the locality, and MTM PAL 2017.1.1. differs markedly from all of these (see Supplementary information 1), suggesting that it represents a vertebrate taxon not previously identified in the local assemblage. Furthermore, the general shape, morphology and detailed features of the tooth differentiate it from those of most major Late Cretaceous continental vertebrate clades (see Supplementary Information), although it shows remarkable (and somewhat surprising) resemblances to sauropod teeth.

Among sauropods, the tooth MTM PAL 2017.1.1. can be referred to eusauropods based on the possession of a concave lingual surface and a D-shaped crown cross-section28, 29. The wrinkled enamel texture characteristic of sauropod teeth28 cannot be observed on this tooth, most probably as the result of extensive wear or perhaps of gut acid etching. This condition suggests that the specimen was a functional tooth with prolonged tooth-food contact. However, well distinguished wear facets (such as interlocking V-shaped, high- or low-angled planar facets)30 are not present on the preserved part of the crown, making the assessment of tooth-tooth occlusion details impossible. The specimen displays a mosaic of basal and advanced dental features within Eusauropoda. It retains the lingual concavity and a D-shaped cross section, but the tooth crown is narrow and not markedly expanded relative to the root, the labial grooves are absent, and no denticulate mesial and distal margins are present.

The tooth differs from the peg-like teeth of diplodocoids, such as Diplodocus31, 32, and the spatulated, mesiodistally wide teeth of non-titanosauriform eusauropods (e.g., Camarasaurus)33, although the crown curvature in mesial/distal view and the lingual concavity are similar to those seen in Mamenchisaurus34. MTM PAL 2017.1.1. is similar to a brachiosaurine tooth from the Lower Cretaceous of Galve, Spain35 in having a D-shaped cross-section, concave lingual surface, and parallel, non-carinated mesial and distal margins, although the details of the crown curvature differ slightly. The general form and cross-section of the crown is reminiscent of the premaxillary teeth of the Early Cretaceous North American brachiosaurid Abydosaurus23 as well. Some similarities can also be pointed out with the teeth of somphospondylan Euhelopus36,37,38, and those of some indeterminate basal titanosauriforms from the Lower Cretaceous of Japan39 that also have parallel-sided crowns with concave lingual surface and relatively low SI values. Nevertheless, they differ from MTM PAL 2017.1.1. in their simple lingual apical curvature, as well as in the presence of a midline ridge within the lingual concavity and of basal lingual buttresses. On the other hand, the tooth markedly differs from the subcylindrical or cylindrical teeth of derived lithostrotian titanosaurs such as Rapetosaurus40 or Nemegtosaurus41, 42 in having a much lower SI value and a morphologically more complex crown. Indeed, according to the character list of Mannion et al.43, the Hungarian tooth does not represent a lithostrotian, since it lacks synapomorphies of this clade such as the high-angled planar wear facets (C105) and the cylindrical tooth crown (C109) with a convex lingual surface (C110). The only lithostrotian character present in MTM PAL 2017.1.1. is the absence of an apicobasally orientated lingual ridge (C111).

New discoveries of European latest Cretaceous titanosaurs document an increasing diversity with at least six different taxa (Ampelosaurus, Lirainosaurus, Atsinganosaurus, Lohuecotitan, Magyarosaurus, and Paludititan), among which the first three genera preserve teeth as well24, 44, and further isolated, indeterminate titanosaur tooth morphotypes are also reported from different localities from Spain24, southern France2, 45 and western Romania (pers. observ.). Isolated titanosaur teeth from the Haţeg Basin, Romania, possibly referable to either Magyarosaurus or Paludititan, are very simple, cylindrical and peg-like, with a mildly convex lingual surface and a high SI value (~5) making these markedly different from the Iharkút tooth. The single known tooth referred to Ampelosaurus, and found in a bonebed from southern France2, 46, 47, is labiolingually flattened, mesiodistally expanded with mesially and distally positioned longitudinal grooves, again, being clearly distinct from MTM PAL 2017.1.1. Whereas the French taxon Atsinganosaurus has gracile, spatulate teeth with a cylindrical crown and mesial and distal ridges extending from the apex to the middle of the crown, the teeth of Lirainosaurus from northern Spain are simple cylindrical with a circular cross section2, 48 - both of these morphologies are also very different from that of the Iharkút specimen. Besides these three Iberoarmorican taxa, Díez Díaz and colleagues24 described two additional morphotypes from the Spanish locality of Lo Hueco. Among them, ‘morphotype B’ is more similar to the Iharkút tooth in having mesiodistally parallel sided crown and shallow ridge-like margins mesially and distally; however, crown curvature and cross section are different. Finally, the ‘Massecaps’ titanosaur tooth morphotype reported by Díez Díaz et al.2 from southern France and described as ‘robust spatulate’ has a flat lingual surface, without the complex morphology shown by the Iharkút specimen, and lacks the labial bend of the crown in mesial/distal view.

Interestingly, MTM PAL 2017.1.1. bears some resemblance to the isolated and indeterminate sauropod teeth reported from the mid-Lower Cretaceous of western France49, especially in the labial bend of the crown at mid-height, followed by a lingual leaning of the tip. Although the teeth figured by Néraudeau et al.49 are markedly different from the Iharkút specimen in their overall shape, with a more leaf-like contour and asymmetrical, distally deflected apical part, these as well as another unpublished tooth apparently originating from the same site appear to have a similar lingual morphology with a concave basal half flanked by rounded and lingually projecting edges and a more convex apical half. Unfortunately, the affinities of these isolated teeth from western France remain poorly understood, and thus are not useful in shedding light on the affinities of the Hungarian specimen either. Finally, MTM PAL 2017.1.1. is somewhat reminiscent of the dental teeth of the ‘mid’-Cretaceous (Cenomanian-Turonian) basal somphospondylan Sarmientosaurus from South America50. Although details of the morphology are different, the teeth of Sarmientosaurus also show moderate SI values (regarded as intermediate between the broad teeth of basal macronarians and the cylindrical, pencil-like teeth of derived titanosaurs), a D-shaped cross-section of the crown, and more particularly the labially leaning crown at mid-height, below a lingually recurved apical part.

To sum up, specimen MTM PAL 2017.1.1. is certainly a tooth composed of an extensive pulp cavity and dentine covered by heavily worn enamel that shows a number of parallel, elongate scratches along the entire crown. Its morphology, being an elongate non-carinated, spatula-like and pointed tooth, is most closely reminiscent of those of certain sauropods. The mosaic of derived and plesiomorphic characters displayed by the Iharkút tooth clearly suggests a neosauropod affinity. It markedly differs from the peg-like diplodocoid and chisel-like derived titanosaurian teeth (including most titanosaur morphotypes reported previously from the uppermost Cretaceous of Europe), instead being more similar to some brachiosaurid teeth or to those of the basal somphospondylan titanosauriform Euhelopus38 and Sarmientosaurus50. Thus, we suggest a non-titanosaur titanosauriform affinity for this specimen, pending discovery of further material that might reveal its more precise taxonomic status.

Status of the European “sauropod hiatus”

Despite being a single piece of evidence, the sauropod tooth from the Santonian of Hungary is of great importance for at least two reasons. First, this specimen is the first sauropod body fossil from a 20 My long hiatus in the fossil record of this clade in Europe, extending from the mid-Cenomanian to the late Campanian interval. Second, the mosaic of derived and plesiomorphic features documented by the crown morphology points to a basal titanosauriform affinity and suggests the occurrence of a clade of sauropods in the Upper Cretaceous of Europe that is markedly different from that encompassing the previously known Campano-Maastrichtian titanosaurs.

Similarly to the ‘sauropod hiatus’ hypothesis proposed by Lucas and Hunt51 to account for the absence of sauropod fossils for the largest part of the mid to Late Cretaceous interval in North America, Le Loeuff 8 and Le Loeuff and Buffetaut15 suggested that the fossil record supports the absence of sauropods from the Cenomanian to late Campanian continental vertebrate record of Europe. This assertion was based on the fact that until the end of the 1990’s not even a single bone or footprint, certainly referable to this group, was known from the, admittedly few, European vertebrate localities representing this time period. The discovery of tracks identified as belonging to small sauropods from the Santonian of southern Italy17, 52 and trackways of larger sauropods16 (probably titanosaurs)1 from the upper Turonian–lower Coniacian of Dalmatia, Croatia, however, indicates that sauropods were present in the Cenomanian to Coniacian continental ecosystems of Europe as well1, 3. The sauropod tooth from Iharkút further strengthens this view, filling in the previously hypothesized Late Cretaceous gap in the sauropod fossil record, and shows that instead of their disappearance, the absence of sauropod fossils in European Late Cretaceous assemblages is probably in part the by-product of sampling bias.

Mannion and Upchurch53 (2011:534) convincingly demonstrated “the abundance of titanosaurs during the Early and latest Cretaceous and their apparent absence during the mid-Cretaceous” in Europe, and pointed out a positive correlation between the abundance (or lack) of sauropod remains and the amount of terrestrial sediment deposition during the Cretaceous. The Iharkút sauropod tooth came from the deposits of a flash flood event that was formed on a low-lying alluvial floodplain developed not far from swampy/deltaic environments that existed under humid conditions21. Accordingly, this landscape was probably more similar to a ‘coastal’ environment than to the much drier and open inland habitats likely preferred by the titanosaur sauropods29, 53. The fact that this tooth represents the only fossil of a sauropod discovered so far among more than 50.000 bones and teeth of the Iharkút assemblage fits well into this environmental scenario, but also confirms that sauropods existed in pre-Campanian times within the European archipelago. In addition, the Santonian sauropod fossil evidence from southern Italy and from Iharkút reveals their presence in both the southern17 and northern21 parts of the Apulian microplate, and suggests their more widespread existence in this region.

The basal titanosauriform affinity of the Iharkút tooth, as assessed based on its mosaic features, might further suggest that the Santonian-aged Iharkút sauropod apparently represented a lineage different from, and more basal than, that of the known European Campano-Maastrichtian sauropods2, 24, 44, 45, 48, 54, 55. If this suggested affinity is upheld by future discoveries, the presence of the Iharkút titanosauriform expands the apparently cryptic sauropod diversity in Europe during the Late Cretaceous, from where only lithostrotian titanosaurs3, 44, 56,57,58 have been reported before. It further supports the endemic and relictual nature of these latest Cretaceous European assemblages, highlighted by the presence of a basal titanosauriform sauropod clade that most probably went extinct by Santonian times in most other landmasses59.

However, the uncertain taxonomic status of the specimen does not allow a more precise clarification of its affinities and relationships. As such, it also remains unknown whether this form represents an immigrant from Gondwana or Asia, as suggested for some Late Cretaceous European titanosaurs1, 8, 15, or it is a relict form that survived in a geographically limited refugium within the European Cretaceous archipelago, a biogeographical phenomenon already pointed out in the case of many other latest Cretaceous continental vertebrates3, 60, 61. Certain morphological similarities with the Hauterivian-Barremian aged sauropod teeth from Charentes, western France might support the second scenario, while possible affinities with the ‘mid’-Cretaceous Argentinian Sarmientosaurus would rather argue for a southern immigrant. Hopefully further material of the enigmatic Iharkút sauropod will be discovered and will help clarifying this problematic aspect of the Late Cretaceous European biogeography as well.

Additional Information

Publisher's note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.


  1. 1.

    Mannion, P. D. & Upchurch, P. A re-evaluation of the ‘mid-Cretaceous sauropod hiatus’ and the impact of uneven sampling of the fossil record on patterns of regional dinosaur extinction. Palaeogeo., Palaeoclim., Palaeoecol 299, 529–540 (2011).

  2. 2.

    Díez Díaz, V., Tortosa, T. & Le Loeuff, J. Sauropod diversity in the Latest Cretaceous of south-western Europe: The lessons of odontology. Ann. Paleont. 99(2), 119–129 (2013).

  3. 3.

    Csiki-Sava, Z., Buffetaut, E., Ősi, A., Pereda-Suberbiola, X. & Brusatte, S. L. Island life in the Cretaceous - faunal composition, biogeography, evolution, and extinction of land-living vertebrates on the Late Cretaceous European archipelago. Zookeys 469, 1–161 (2015).

  4. 4.

    Seeley, H. G. On Macrurosaurus semnus (Seeley), a long tailed animal with procoelous vertebrae from the Cambridge Upper Greensand, preserved in the Woodwardian Museum of the Univ. Cambridge. J. Geol. Soc. London 32, 440–444 (1876).

  5. 5.

    Lydekker, R. Note on a new Wealden iguanodont and other dinosaurs. Q. J. Geol. Soc. London 44, 46–61 (1888).

  6. 6.

    Huene, F. von. Die Besonderheit der Titanosaurier: Centralbl. Miner. Geol. Palaont Stuttgart, Abhandlungen, Abt. A, 493–499 (1929).

  7. 7.

    Buffetaut, E. Archosaurian reptiles with Gondwanan affinities in the Upper Cretaceous of Europe. Terra Nova 1, 69–74 (1989).

  8. 8.

    Le Loeuff, J. European titanosaurids. Rev. Paléobiol. 7, 105–117 (1993).

  9. 9.

    Mezga, A. & Bajraktarevic, Z. Cenomanian dinosaur tracks on the islet of Fenoliga in southern Istria, Croatia. Cret. Res. 20, 735–746 (1999).

  10. 10.

    Nicosia, U. et al. Dinosaur tracks as paleogeographic constraints: new scenarios for the Cretaceous geography of the Periadriatic region. Ichnos 14, 69–90 (2007).

  11. 11.

    Vullo, R., Néraudeau, D. & Lenglet, T. Dinosaur teeth from the Cenomanian of Charentes, western France: evidence for a mixed Laurasian-Gondwanan assemblage. J. Vert. Paleont. 27, 931–943 (2007).

  12. 12.

    Santos V. F. Dinosaur tracksites in Portugal: the Jurassic-Cretaceous record. I Encontro Internacional sobre Paleobiologia dos Dinossáurios, pp 7–16 (1998).

  13. 13.

    Antunes, M. T. & Mateus, O. Dinosaurs of Portugal. C.R. Palevol 2, 77–95 (2003).

  14. 14.

    Cohen, K. M., Finney, S. C., Gibbard, P. L. & Fan, J.-X. The ICS International Chronostratigraphic Chart. Episodes 36, 199–204 (2013).

  15. 15.

    Le Loeuff, J. & Buffetaut, E. The evolution of Late Cretaceous non-marine vertebrate fauna in Europe. In: 6th Symposium of Mesozoic Terrestrial Ecosystems and Biotas (eds Sun, A. & Wang, Y.) 181–184 (China Ocean Press, Beijing, 1995).

  16. 16.

    Mezga, A., Meyer, C. A., Tesovic, B. C., Bajraktarevic, Z. & Gusic, I. The first record of dinosaurs in the Dalmatian part (Croatia) of the Adriatic–Dinaric carbonate platform (ADCP). Cret. Res. 27, 735–742 (2006).

  17. 17.

    Nicosia, U. et al. The Late Cretaceous dinosaur tracksite near Altamura (Bari, southern Italy). I—Geological framework. Geol. Rom. 35, 231–236 (1999).

  18. 18.

    Wilson, J. A. & Upchurch, P. A revision of Titanosaurus (Dinosauria Sauropoda), the first ‘Gondwanan’ dinosaur genus. J. Syst. Palaeont. 1, 125–160 (2003).

  19. 19.

    Smith, J. B. & Dodson, P. A proposal for a standard terminology of anatomical notation and orientation in fossil vertebrate dentitions. J. Vert. Paleontol. 23, 1–12 (2003).

  20. 20.

    Upchurch, P. The phylogenetic relationships of sauropod dinosaurs. Zool. J. Linn. Soc. London 124, 43–103 (1998).

  21. 21.

    Botfalvai, G., Haas, J., Mindszenty, A. & Ősi, A. Facies Architecture and Paleoenvironmental implications of the Upper Cretaceous (Santonian) Csehbánya Formation at the Iharkút vertebrate locality (Bakony Mountains, northwestern Hungary). Palaeogeo., Palaeoclim., Palaeoecol 441, 659–678 (2016).

  22. 22.

    Ősi, A. et al. The Late Cretaceous continental vertebrate fauna from Iharkút, western Hungary: a review. In: Bernissart Dinosaurs and Early Cretaceous Terrestrial Ecosystems (ed. Godefroit, P.) 533–568 (Indiana University Press, 2012).

  23. 23.

    Chure, D., Britt, B. B., Whitlock, J. A. & Wilson, J. A. First complete sauropod dinosaur skull from the Cretaceous of the Americas and the evolution of sauropod dentition. Die. Naturwissenschaften 97, 379–391 (2010).

  24. 24.

    Díez Díaz, V., Ortega, F. & Sanz, J. L. Titanosaurian teeth from the Late Cretaceous of “Lo Hueco” (Cuenca, Spain). Cret. Res. 51, 285–291 (2014).

  25. 25.

    Fisher, D. C. Crocodilian scatology, microvertebrate concentrations, and enamel-less teeth. Paleobiology 7, 262–275 (1981).

  26. 26.

    Argast, S., Farlow, J. D., Gabet, R. M. & Brinkman, D. L. Transport-induced abrasion of fossil reptilian teeth: Implications for the existence of Tertiary dinosaurs in the Hell Creek Formation, Montana. Geology 15, 927–930 (1987).

  27. 27.

    Ősi, A., Apesteguía, S. & Kowalewski, M. Non-avian theropod dinosaurs from the early Late Cretaceous of Central Europe. Cretaceous Research 31, 304–320 (2010).

  28. 28.

    Wilson, J. A. & Sereno, P. Early evolution and higher-level phylogeny of the sauropod dinosaurs. Mem. Soc. Vert. Paleontol. 5, 1–68 (1998).

  29. 29.

    Upchurch, P., Barrett, P. M. & Dodson, P. Sauropoda. In: The Dinosauria, second ed. (eds Weishampel, D. B., Dodson, P. & Osmólska, H.) 259–322 (University of California Press, Berkeley, 2004).

  30. 30.

    Wilson, J. A. Sauropod dinosaur phylogeny: critique and cladistic analysis. Zool. J. Linn. Soc. 136, 217–276 (2002).

  31. 31.

    Hatcher, J. B. Diplodocus Marsh, its osteology, taxonomy and probable habits, with a restoration of the skeleton. Mem. Carnegie Mus. 1, 1–64 (1901).

  32. 32.

    Upchurch, P. & Barrett, P. M. The evolution of sauropod feeding mechanisms. In: Evolution of Herbivory in Terrestrial Vertebrates: Perspectives from the Fossil Record (ed. Sues, H.-D.) 79–122 (Cambridge University Press, Cambridge, 2000).

  33. 33.

    Madsen, J. H. Jr., McIntosh, J. S. & Berman, D. S. Skull and atlas-axis complex of the Upper Jurassic sauropod Camarasaurus Cope (Reptilia: Saurischia). Bull. Carnegie Mus. Nat. Hist. 31, 1–115 (1995).

  34. 34.

    Ouyang, H. & Ye, Y. The First Mamenchisaurian Skeleton with Complete Skull: Mamenchisaurus youngi. Sichuan Science and Technology Press, Chengdu, 111 p (2002).

  35. 35.

    Sanz, J. L. A sauropod dinosaur tooth from the Lower Cretaceous of Galve (Province of Teruel, Spain). Géobios 15, 943–949 (1982).

  36. 36.

    Wiman, C. Die Kreide-dinosaurier aus Shantung. Palaeontol. Sin. (Ser. C) 6, 1–67 (1929).

  37. 37.

    Barrett, P. M. & Wang, X. -L. Basal titanosauriform (Dinosauria, Sauropoda) teeth from the Lower Cretaceous Yixian Formation of Liaoning Province, China. Palaeoworld, doi:10.1016/j.palwor.2007.07.001 (2007).

  38. 38.

    Wilson, J. A. & Upchurch, P. Redescription and reassessment of the phylogenetic affinities of Euhelopus zdanskyi (Dinosauria: Sauropoda) from the Early Cretaceous of China. J. Syst. Palaeont. 7, 199–239 (2009).

  39. 39.

    Barrett, P. M., Hasegawa, Y., Manabe, M., Isaji, S. & Matsuoka, H. Sauropod dinosaurs from the Lower Cretaceous of eastern Asia: taxonomic and biogeographical implications. Palaeontology 45, 1197–1217 (2002).

  40. 40.

    Curry Rogers, K. & Forster, C. A. The skull of Rapetosaurus krausei (Sauropoda: Titanosauria) from the Late Cretaceous of Madagascar. J. Vert. Paleontol. 24, 121–144 (2004).

  41. 41.

    Nowinski, A. Nemegtosaurus mongoliensis n. gen., n. sp. (Sauropoda) from the uppermost Cretaceous of Mongolia. Palaeontol. Pol. 25, 57–81 (1971).

  42. 42.

    Wilson, J. A. Redescription of the Mongolian sauropod Nemegtosaurus mongoliensis Nowiński (Dinosauria: Saurischia) and comments on Late Cretaceous sauropod diversity. J. Syst. Palaeont. 3, 283–318 (2005).

  43. 43.

    Mannion, P. D., Upchurch, P., Barnes, R. N. & Mateus, O. Osteology of the Late Jurassic Portuguese sauropod dinosaur Lusotitan atalaiensis (Macronaria) and the evolutionary history of basal titanosauriforms. Zool J Linnean Soc 168, 98–206 (2013).

  44. 44.

    Díez Díaz, V. et al. A new titanosaur (Dinosauria, Sauropoda) from the Upper Cretaceous of Lo Hueco (Cuenca, Spain). Cret. Res. 68, 49–60, doi:10.1016/j.cretres.2016.08.001 (2016).

  45. 45.

    Díez Díaz, V., Garcia, G., Knoll, F., Suberbiola, X. P. & Valentin, X. New cranial remains of titanosaurian sauropod dinosaurs from the Late Cretaceous of Fox-Amphoux-Métisson (Var, SE France). Proc. Geol. Ass. 123, 626–637 (2012).

  46. 46.

    Le Loeuff, J. Ampelosaurus atacis (nov. gen., nov. sp.), un nouveau Titanosauridae (Dinosauria, Sauropoda) du Crétacé supérieur de la Haute Vallée de l’Aude (France). Compt. Rend. Acad. Sci., Paris 321, 693–699 (1995).

  47. 47.

    Le Loeuff, J. Osteology of Ampelosaurus atacis (Titanosauria) from Southern France. In: Thunder-Lizards. The Sauropodomorph Dinosaurs (eds Tidwell, V. & Carpenter, K.) 115-137 (Indiana University Press, Bloomington, 2005).

  48. 48.

    Díez Díaz, V., Pereda Suberbiola, X. & Sanz, J. L. Juvenile and adult teeth of the titanosaurian dinosaur Lirainosaurus (Sauropoda) from the Late Cretaceous of Iberia. Geobios 45, 265–274 (2012).

  49. 49.

    Néraudeau, D. et al. The Hauterivian-Barremian lignitic bone bed of Angeac (Charente, south-west France): stratigraphical, palaeobiological and palaeogeographical implications. Cret. Res. 37, 1–14 (2012).

  50. 50.

    Martínez, R. D. F. et al. A basal lithostrotian titanosaur (Dinosauria: Sauropoda) with a complete skull: implications for the evolution and paleobiology of Titanosauria. PLoS ONE 11(4), e0151661, doi:10.1371/journal.pone.0151661 (2016).

  51. 51.

    Lucas, S. G. & Hunt, A. P. Alamosaurus and the sauropod hiatus in the Cretaceous of the North American Western Interior. Geol. Soc. America Special Paper 238, 75–85 (1989).

  52. 52.

    Dal Sasso, C. Dinosaurs of Italy. Compt. Rend. Palevol 2, 45–66 (2003).

  53. 53.

    Mannion, P. D. & Upchurch, P. A quantitative analysis of environmental associations in sauropod dinosaurs. Paleobiology 36, 253–282 (2010).

  54. 54.

    Díez Díaz, V., Pereda Suberbiola, X. & Sanz, J. L. Appendicular skeleton and dermal armour of the Late Cretaceous titanosaur Lirainosaurus astibiae (Dinosauria: Sauropoda) from Spain. Palaeont. Elect. 16(2), 19A, 1–18 (2013).

  55. 55.

    Díez Díaz, V., Peredea Suberbiola, X. & Sanz, J. L. The axial skeleton of the titanosaur Lirainosaurus astibiae (Dinosauria: Sauropoda) from the latest Cretaceous of Spain. Cret. Res. 43, 145–160 (2013).

  56. 56.

    Díez Díaz, V., Garcia, G., Pereda Suberbiola, X., Valentin, X. & Sanz, J. L. Phylogenetic relationships of the titanosaurian dinosaurs from the Late Cretaceous of the Ibero-Armorican Island. In: (Editors), Fernández-Baldor, F. T. & Huerta, P. VI Jornadas Internacionales sobre Paleontología de Dinosaurios y su Entorno. Colectivo Arqueológico y Paleontológico de Salas, C.A.S., Salas de los Infantes, Burgos, pp 63–64. (2013).

  57. 57.

    Gorscak, E. & O’Connor, P. M. Time-calibrated models support congruency between Cretaceous continental rifting and titanosaurian evolutionary history. Biology Letters 12, 20151047, doi:10.1098/rsbl.2015.1047 (2016).

  58. 58.

    García, G., Amico, S., Fournier, F., Thouand, E. & Valentin, X. A new titanosaur genus (Dinosauria, Sauropoda) from the Late Cretaceous of southern France and its paleobiogeographic implications. Bull. Soc. Géol. France 181, 269–277 (2010).

  59. 59.

    D’Emic, M. D. The early evolution of titanosauriform sauropod dinosaurs. Zool. J. Linn. Soc. 166, 624–671 (2012).

  60. 60.

    Benton, M. J. et al. Dinosaurs and the island rule: The dwarfed dinosaurs from Haţeg Island. Palaeogeo., Palaeoclim., Palaeoecol. 293, 438–454 (2010).

  61. 61.

    Weishampel, D. B., Csiki, Z., Benton, M. J., Grigorescu, D. & Codrea, V. Palaeobiogeographic relationships of the Haţeg biota — between isolation and innovation. Palaeogeo., Palaeoclim., Palaeoecol. 293, 419–437 (2010).

Download references


We are grateful to the two anonymous reviewers for their constructive comments that greatly improved the previous version of the manuscript. We thank the 2000–2016 field crew for their assistance in the fieldwork. We are especially grateful to the Bakony Bauxite Mining Company and the Geovolán Zrt. for their logistic help. We thank Réka Kalmár and Márton Szabó (Hungarian Natural History Museum, Budapest) for their technical assistance. Field and laboratory work was supported by the MTA–ELTE Lendület Dinosaur Research Group (Grant no. 95102), Hungarian Scientific Research Fund (OTKA T–38045, PD 73021, NF 84193, K 116665), National Geographic Society (Grant No. 7228–02, 7508–03), Bolyai Fellowship, Hungarian Natural History Museum, Eötvös Loránd University, the Jurassic Foundation and the Hungarian Dinosaur Foundation. EP is funded by Bijzonders Onderzoeksfonds (BOF) – Universiteit Gent (grant nr. 01P12815).

Author information


  1. Eötvös University, Department of Paleontology, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary

    • Attila Ősi
  2. Hungarian Natural History Museum, Baross u 13., Budapest, 1088, Hungary

    • Attila Ősi
  3. Department of Geology, Faculty of Geology and Geophysics, University of Bucharest, 1 N. Bălcescu Blvd, 010041, Bucharest, Romania

    • Zoltán Csiki-Sava
  4. Department of Biology, Evolutionary Morphology of Vertebrates, Ghent University, K. L. Ledeganckstraat 35, 9000, Gent, Belgium

    • Edina Prondvai


  1. Search for Attila Ősi in:

  2. Search for Zoltán Csiki-Sava in:

  3. Search for Edina Prondvai in:


A.Ő., Z.Cs.-S., and E.P. contributed to all discussions throughout and wrote the main manuscript text, and A.Ő. prepared Figures 1–3 and Supplementary information 1.

Competing Interests

The authors declare that they have no competing interests.

Corresponding author

Correspondence to Attila Ősi.

Supplementary information


By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.

Creative Commons BY

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit