Mosasauroids are conventionally conceived of as gigantic, obligatorily aquatic marine lizards (1000s of specimens from marine deposited rocks) with a cosmopolitan distribution in the Late Cretaceous (90–65 million years ago [mya]) oceans and seas of the world. Here we report on the fossilized remains of numerous individuals (small juveniles to large adults) of a new taxon, Pannoniasaurus inexpectatus gen. et sp. nov. from the Csehbánya Formation, Hungary (Santonian, Upper Cretaceous, 85.3–83.5 mya) that represent the first known mosasauroid that lived in freshwater environments. Previous to this find, only one specimen of a marine mosasauroid, cf. Plioplatecarpus sp., is known from non-marine rocks in Western Canada. Pannoniasaurus inexpectatus gen. et sp. nov. uniquely possesses a plesiomorphic pelvic anatomy, a non-mosasauroid but pontosaur-like tail osteology, possibly limbs like a terrestrial lizard, and a flattened, crocodile-like skull. Cladistic analysis reconstructs P. inexpectatus in a new clade of mosasauroids: (Pannoniasaurus (Tethysaurus (Yaguarasaurus, Russellosaurus))). P. inexpectatus is part of a mixed terrestrial and freshwater faunal assemblage that includes fishes, amphibians turtles, terrestrial lizards, crocodiles, pterosaurs, dinosaurs and birds.

Funding: MWC was supported by an NSERC Discovery Grant (#238458-01) and a University of Alberta, Chairs Research Allowance. Fieldwork and the work of LM and AŐ were supported by the OTKA T-39045, PD-73021, NF-84193 grants; the MTA-ELTE Lendület (Dinosaur Research Group, grant n.95102); the National Geographic Society; the Jurassic Foundation, and the Hantken Foundation. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

Copyright: © 2012 Makádi et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

It is worth mentioning that several similar sequences are exposed within the mine. In most of these cases the basal breccia (bonebed) is missing and the cycle starts with sandstone, or, if present, the basal breccia is thin (only a few centimeters, containing no, or only a few vertebrate remains). Moreover, the cycles sometimes end with paleosoils, which also might contain vertebrate remains, mostly dinosaur and crocodile teeth, and bone and turtle shell fragments [13] , [25] .

The sandstone bed covering the basal breccia also contains vertebrate fossils, but the bones are fewer in number and more poorly preserved. However, two incomplete associated skeletons of the nodosaurid ankylosaur Hungarosaurus tormai have been found in this bed. The overlying bed is a laminated, grayish siltstone of variable thickness (30 cm to 1.5 m) and contains plant debris and only a few bones, but this bed also yielded two partial associated skeletons of Hungarosaurus. The sequence is closed by a greyish siltstone of several meters thickness in which vertebrate remains are extremely rare [13] , [25] .

At Iharkút, vertebrate remains, including those of Pannoniasaurus inexpectatus gen. et sp. nov., were found throughout exposures of the Csehbánya Formation, but the SZ-6 site is without question the most important site. This outcrop is an approximately 2–3 m thick sequence of beds built up of coarse, pebbly sand and organic-rich silt and clay, which are interpreted as crevasse splay deposits ( Figure 2 ). The base of the sequence is clearly erosional as it forms noticeable erosional surfaces into the floodplain deposits. The bonebed at SZ-6 is a 10 to 50 cm thick, basal breccia composed of gray sand, siltstone, clay clasts, pebbles, and plant debris (also charcoal) that occasionally contains surprisingly complete bones, but more frequently yields fragmentary bones; the basal breccia is sometimes interrupted by finer sediments that settled out under calmer circumstances [13] . As a result of these alternating energy conditions of deposition, bones in different states of preservation can be found in the same bed. Nearly 80% of the vertebrate remains from Iharkút were discovered in the bonebed of this site [13] , [25] .

The bone-yielding Csehbánya Formation ( Figure 2 ) overlies the Nagytárkány Bauxite Formation and the Triassic Main Dolomite Formation. It is a floodplain and channel deposit built up of variegated clay, silt with interbedded grey and brown sand, sand and sandstone beds, as well as paleosoils. In some exposures of the open-pit mine area, the Csehbánya Formation is sometimes covered by the Eocene Iharkút Conglomerate Formation; in other locations it is covered by the Oligocene–Miocene Csatka Formation or sits immediately below Quaternary deposits [25] – [29] . Detailed palynological studies suggest a Santonian age for the Csehbánya Formation [28] , a date that is also supported by recent paleomagnetic data [13] , [25] .

In the Late Cretaceous the Iharkút area where P. inexpectatus lived was part of an alluvial floodplain system on an island landmass in the western Tethyan archipelago. Besides vertebrates and freshwater invertebrates, plant fossils were also unearthed and provide evidence that the area was covered by terrestrial vegetation [13] , [25] .

The Iharkút fossil vertebrate locality (referred to as Iharkút in memory of the village of Iharkút that was destroyed in order to create the mine) that yielded the numerous remains of Pannoniasaurus is located in an open-pit bauxite mine near Németbánya, Bakony Mountains, Western Hungary ( Figure 1 ). The mine exposes the base of the Csehbánya Formation (Santonian, Upper Cretaceous), an alluvial floodplain deposit that contains various vertebrate remains, as well as invertebrate and plant fossils. To date, the documented vertebrate fauna includes lepisosteid and pycnodontiform fishes [13] , albanerpetontid and anuran amphibians [14] , bothremydid turtles [15] , lizards [16] , alligatoroid, ziphosuchian and heterodont eusuchian crocodiles [13] , [17] , azhdarchid pterosaurs [18] , a rhabdodontid ornithopod [19] , the ceratopsian dinosaur Ajkaceratops [20] , the basal nodosaurid ankylosaur Hungarosaurus [21] , [22] , theropods [23] , and enantiornithine birds [24] .

Modern squamate reptiles are largely restricted to terrestrial environments with only a few species living in aquatic environments and an even smaller number, i.e., the marine iguana and sea snakes such as the acrochordids, true sea snakes and sea kraits, occupying facultative and obligatory niches in marine environments [1] . The adaptive radiation into aquatic environments by the long extinct squamate clade commonly known as mosasauroids (mosasaurs and aigialosaurs), resulted in the evolution of paddle-like limbs (hydropedality) [2] and modified hips (hydropelvia) [3] , [4] , a laterally compressed and downturned tail for swimming [5] , modifications to the middle-ear osteology [6] , [7] , and a progressive increase towards gigantism within different subclades [6] . It is therefore an excellent example of a major secondarily aquatic transition in vertebrate evolution, and the only one of its kind among squamates [8] . However, despite our broad understanding of the ∼30 million year time span of mosasauroid aquatic evolution, there has never been a clearly documented example of a mosasauroid group that unequivocally occupied freshwater habitats [6] , . Similar to almost all living cetaceans, all previously known mosasauroids are considered to have occupied marine habitats.

The electronic edition of this article conforms to the requirements of the amended International Code of Zoological Nomenclature, and hence the new names contained herein are available under that Code from the electronic edition of this article. This published work and the nomenclatural acts it contains have been registered in ZooBank, the online registration system for the ICZN. The ZooBank LSIDs (Life Science Identifiers) can be resolved and the associated information viewed through any standard web browser by appending the LSID to the prefix " http://zoobank.org/ ". The LSID for this publication is: urn:lsid:zoobank.org:pub:29161BAD-A892-46F0-AB28-1EE594A229A1. The electronic edition of this work was published in a journal with an ISSN, and has been archived and is available from the following digital repositories: PubMed Central, LOCKSS.

The data matrix, available online (See Appendix S3 ), was modified with the recoding of Tethysaurus (characters 1, 87, 88, 98, 105, 107 and 128) based on personal observation and the original description [33] and with the addition of new character data from Pannoniasaurus.

Phylogenetic analysis of thirty-two taxa and one hundred and thirty five characters was conducted using a taxon-character matrix from a recent cladistic analysis of mosasauroid squamates [4] . That character list and taxon-character matrix originates from a previous work [32] , with characters deleted/added/modified through later studies [2] , [3] . In order to make it easier for the reader to follow the changes made through that series of studied, the character list (See Appendix S2 ) was recompiled by quoting almost word-by-word from the original character list of Bell [32] and including all changes made by later studies [3] , [4] .

Therefore, as is the case for the Iharkút fauna, and staying with the vertebral example given above, if all of the presacral vertebrae assigned to Pannoniasaurus possess a common characteristic (in this case there are many) that is shared regardless of size class or presumed position in the vertebral column, then it is reasonable to conclude there is only a single morphotaxon present in the fauna. The case for only a single aigialosaur-grade mosasauroid morphotaxon being present in the Iharkút assemblage is reinforced by the application of this same methodology to the multiple specimens of the same skull, lower jaw, and appendicular skeletal elements regardless of size. In the final analysis, there simply is no evidence of more than one morphotaxon of mosasauroid, nor of any other large-sized squamate, at the locality. Similar methodologies have been used by other authors, e.g. Houssaye et al. [31] referred newly discovered cervical vertebrate to Pachyvaranus crassispondylus, though the species was originally described on the basis of dorsal vertebrae.

For example, the logic we have applied in identifying a single taxon of mosasauroid from the Iharkút assemblage is as follows: if in an assemblage of extant lizard vertebrae one finds that all the vertebrae show a similar diagnostic feature (e.g., in extant Varanus all vertebrae display a flared condyle), then it is reasonable to conclude that all of the lizards represented are morphologically Varanus (a morphospecies concept is being applied); it would therefore logically follow that if there is one vertebra that differs, then the application of a morphospecies concept and its criterion for inclusion/exclusion would be that there are at least two morphotaxa present, not one.

Though all remains (including the holotype) of Pannoniasaurus are isolated bones, the density of the specimens, the various size classes, the large number of similar elements from individual animals, and their unique characters, make it possible to link them together into a single taxon.

The holotype and referred specimens have been collected from the alluvial sediments of the Csehbánya Formation from various exposures at the Iharkút open-pit bauxite mine, Bakony Hills, Western Hungary since the discovery of the locality in 2000. A single vertebra has been collected in 1999 from the interdigitating Ajka Coal Formation at the waste dump of the coal mines next to the town of Ajka, 20 kms from Iharkút [13] , [28] , [29] . Currently more than one hundred bones of Pannoniasaurus (See Appendix S1 ), sourced from a large number of individuals of differing age classes, are known from the alluvial flood-plain [30] deposits that comprise the Csehbánya Formation. All specimens of Pannoniasaurus are housed in the Hungarian Natural History Museum (Magyar Természettudományi Múzeum: MTM), Budapest, Hungary.

The Tethysaurinae (Pannoniasaurus (Tethysaurus (Yaguarasaurus, Russellosaurus))) ( Figure 9B ) is reconstructed at the base of a clade that includes the aigialosaurs Carsosaurus, Komensaurus, and Haasiasaurus, and the clades that include conventional marine mosasaur-grade mosasauroids such as halisaurs, tylosaurs and plioplatecarpines. The concept of a monophyletic clade of aigialosaurs from within which a polyphyletic Mosasauridae arises (two major lineages of a grade of paddle-bearing marine mosasaurs) [11] , is supported here, and provides further support for the hypothesis of convergent aquatic adaptations in paddle-bearing mosasaurs [2−4] , .

Our analysis found three equally most parsimonious trees (length = 374, CI = 0.4679, RI = 0.7375, HI = 0.5508) that place Pannoniasaurus in a new clade, the Tethysaurinae. The three trees ( Figure 8 ) reconstruct Pannoniasaurus as the sister taxon to the clade that includes Tethysaurus nopcsai (Early Turonian), Yaguarasaurus columbianus (?Late Turonian) and Russellosaurus coheni (Middle Turonian). This clade was recognized previously as a monophyletic group [2] , [4] , but not in the sister group position found in this analysis ( Figure 9 ).

The proximal humeral epiphysis ( Figures 4T , 7K ), though partial, appears to be part of a much longer element, similar to the expected condition for a plesiopedal limb [4] . It is mediolaterally compressed and the deltopectoral crest is undivided. Similarly, an isolated right distal tip ( Figures 4U , 7L−N ) shows a well-fused diaphysis, with well-developed ent- and ectepicondyles and an ectepicondylar groove. The ilium ( Figures 4V , 7O−P ) is robust with a long posterior blade, a well-developed acetabular face, a well-developed ventral facet for the ischium and a spoon-shaped preacetabular process that overlapped the pubis. This process is similar to that seen in many extant lizards and the mosasauroids Aigialosaurus dalmaticus [3] and Tethysaurus nopcsai (LM, personal observation) and represents the plesiopelvic condition [3] , [4] .

second sacral vertebra (MTM Gyn/121.) in anterior (A), posterior (B), dorsal (C), ventral (D), and left lateral (E) views. Anterior caudal vertebra (MTM Gyn/104.) in anterior (F), and right lateral (G) views. Anterior caudal vertebra (MTM 2007.46.1.) in ventral view (H). Posterior caudal vertebra (MTM 2007.99.1.) in left lateral view (I). Left rib fragment (MTM 2007.89.1.) in lateral view (J). Proximal end of left humerus (MTM 2007.42.1.) in flexor view (K). Distal end of right humerus (MTM 2011.42.1.) in flexor (L), extensor (M) and distal (N) views. Left ilium (MTM 2007.40.1) in lateral (O) and medial (P) views. Scale bars represent 1 cm.

The vertebrae ( Figures 4N−R , 6A−P , 7A−I ) of Pannoniasaurus are similar in almost all respects (size, shape, size and shape of processes, and intracolumnar variation) to those of Tethysaurus [33] , and cannot be compared to either Russellosaurus [37] or Yaguarasaurus [38] , [41] as postcranial remains are almost entirely absent for both taxa. In all presacral vertebrae of Pannoniasaurus inexpectatus the condyles/cotyles are oval and oblique, and the vertebral condyles are flared ( = precondylar constriction) (most pronounced on juvenile cervicals), in contrast to all known mosasauroids [6] , [43] , but similar to varanids [46] . The cervicals ( Figures 4N , 6A−E ) have compressed centra similar to Tethysaurus and Halisaurus [33] , [45] , [47] , and bear small zygosphenes and zygantra. Large crests extend between the synapophyses and anterior edge of the cotyles and project ventrally below the ventral surface of the centrum as in Halisaurus [47] , [48] and Tethysaurus [33] , and are morphologically similar to the dorsally positioned pterosphenes of palaeophiid snakes [49] . Hypapophyseal peduncles have circular articulation surfaces in contrast to Tethysaurus [33] . Zygosphenes/zygantra are small on the anteriormost dorsals, similar to the cervicals. Further posteriorly on the dorsals ( Figures 4O , 6F−K ) the zygosphenes/zygantra become large and functional. Contrary to the condition in Tethysaurus, no vertebrae exhibit parazygosphenal and paracotylar foramina [33] . In contrast to derived mosasauroids, i.e., taxa within the grade of hydropelvic mosasaurs [6] , [43] , there appear to be two sacrals. The massive first sacral ( Figures 4P , 6L−P ) is short and broad. The posteroventrally projecting transverse processes are crescent-shaped in cross-section and share a broad platform with the prezygapophyses. The zygosphenes of the first sacral are the largest in the vertebral series. The second sacral ( Figures 4Q , 7A−E ) is similar to the first in general shape but its centrum and transverse processes are less robust, the latter being subcircular in cross-section. The distal end of the transverse process bears a facet for the articulation with the ilium. Zygosphenes/zygantra are present. The caudals ( Figures 4R , 7F−I ) are similar to those of Tethysaurus [33] and to pontosaurs [50] . The centra are elongate, being app. two times longer than wide (width/length ratio: 1.8–2.3) with the anterior caudals being slightly shorter compared to the posterior ones. The condyles/cotyles are circular, the posteriorly directed haemapophyses are large, the haemal arches are unfused, the prezygapophyses are elongate, while the postzygapophyses are small on the neural spines, and zygosphenes/zygantra are absent. The anterior caudals bear well-developed transverse processes. The neural spines are nearly two times the length of the centra and project posteriorly. The ribs ( Figures 4S , 7J ) have a shape typical of mosasaurs [6] , [43] and their heads heads are more oval than in Tethysaurus (LM, personal observation).

Premaxilla (MTM 2007.25.1.) in dorsal (A), ventral (B), and right lateral (C) views. Right maxilla (MTM 2007.29.1.) in lingual (D) and labial (E) views. Left postorbitofrontal (MTM 2007.28.1.) in dorsal (F), ventral (G), and medial (H) views. Left dentary (MTM 2007.37.1.) in lingual (I) and occlusal (J) views. Isolated teeth isolated teeth without and with base preserved (K). Left splenial (MTM 2011.41.1.) in medial (L) and posterior (M) views. Left coronoid (MTM 2007.23.1.) in lateral (N) and medial (O) views. Right angular (MTM 2007.36.1.) in lateral (P) and anterior (Q) views. Right surangular (MTM 2007.30.1.) in lateral (R) and medial (S) views. Right articular (MTM 2007.39.1.) in dorsal view. Scale bars represent 1 cm.

The generic name is derived from the ancient Roman province “Pannonia” in the Transdanubian part of Hungary and “saurus”, New Latin word from Greek ‘sauros’, meaning lizard; the specific epithet “inexpectatus”, meaning unexpected in Latin, refers to the unexpected occurrence of this mosasaur in freshwater environments.

Medium-sized (max. 6 meters) mosasauroid with following combination of characters: quadrate stapedial pit length/width ratio of 3∶1; saddle-shaped mandibular condyle of quadrate; quadrate shaft, distal to the conch and infrastapedial process, long and gracile; large infrastapedial process; long suprastapedial process with tip angled medially; dorsoventrally flattened, laterally wide, violin-shaped premaxilla in dorsal view; high dorsal process on coronoid; teeth with carinae and anastomosing longitudinal striae; hypapophyseal peduncles with circular articulation surface; large ventrolateral crests on cervicals; parazygosphenal and paracotylar foramina absent; well-developed precondylar constriction on precaudal vertebrae; ribs with oval heads.

2 isolated premaxillae; 3 maxillae; 2 postorbitofrontals; 2 quadrates; 3 dentaries; 3 splenials; 3 angulars; coronoid; 2 surangulars; articular; 91 isolated teeth; 20 cervical, 40 dorsal, 4 sacral, and 18 caudal vertebrae; 34 vertebral fragments; 3 ribs; 2 humeral fragments; 4 ilia (See Appendix S1 for inventory numbers). Since all remains are isolated bones, the basis for the referral of this material to Pannoniasaurus is explained above in the “Materials and Methods” section.

A: skull drawing shows known elements in grey. B: skeletal reconstruction showing preserved bones in white. C: premaxilla (MTM 2007.25.1.) in dorsal view. D: right maxilla (MTM 2007.29.1.) in lingual view. E: left postorbitofrontal (MTM 2007.28.1.) in dorsal view. F: right quadrate (MTM 2011.43.1.) in lateral view. G: left dentary (MTM 2007.37.1.) in lingual view. H: isolated teeth without and with base preserved. I: left splenial (MTM 2011.41.1.) in lingual view. J: right coronoid (MTM 2007.23.1.) in lingual view. K: left angular (MTM 2007.36.1.) in labial view. L: right surangular (MTM 2007.30.1.) in labial view. M: left articular (MTM 2007.39.1.) in dorsal view. N: mid-cervical vertebra (MTM V.01.149.) in lateral view. O: dorsal vertebra (MTM V.01.222.) in dorsal view. P: first sacral vertebra (MTM Gyn/122.) in dorsal view. Q: second sacral vertebra (MTM Gyn/121.) in dorsal view. R: anterior caudal vertebra (MTM Gyn/104.) in lateral view. S: rib fragment (MTM 2007.89.1.) in dorsolateral view. T: proximal end of left humerus (MTM 2007.42.1.) in flexor view. U: distal end of right humerus (MTM 2011.42.1.) in flexor view. V: left ilium (MTM 2007.40.1) in lateral view. All known elements of Pannoniasaurus are isolated bones from multiple individuals and many are known as multiple specimens but only one is figured. Vertebrae and ribs not figured in (B) symbolize that no complete series has been found. Scale bars represent 1 cm (A, C-V) and 1 meter (B).

Tethysaurus was chosen as type genus because it is the best-represented genus of the subfamily, known from multiple partial skeletons. Thus the subfamily name derives from the name of its type genus.

Medium-sized (max. 6 meters) mosasauroids exhibiting combination of primitive characters: predental rostrum absent; premaxilla-maxilla suture ends anterior to or level with the midline of the fourth maxillary tooth; nearly straight frontoparietal suture; quadrate alar concavity shallow; elongated stapedial pit (at least three times longer than wide); quadrate distal condyle saddle-shaped, upward deflection of quadrate distal condyle absent; mandibular glenoid formed mainly by articular; cervical synapophyses extend below ventral border of centrum; dorsoventrally compressed centra in precaudal vertebrae; two sacrals with large ribs/transverse processes subcircular/oval in cross-section; facet for ilium on tip of sacral transverse processes; very elongated (two times longer than wide) pontosaur-like caudal centra; anteroposteriorly narrow scapula; ilium with posterior iliac process with compressed dorsal end bearing longitudinal grooves and ridges, and spoon-shaped preacetabular process overlapping the pubis.

Discussion

Comments on the Pannoniasaurus Material, its Taphonomy and Geochemical Analysis Since the SZ-6 bonebed (Figure 2), which yielded most Pannoniasaurus remains, is depositionally a crevasse splay and was formed in a short time interval, likely as a result of a flood, non-weathered and unabraded vertebrate remains preserved in this bonebed originate from animals that might have died shortly before final burial [13], [25], [51]. Considering the tropical climate, bones lacking signs of weathering might not have been exposed or were temporarily buried before they were picked up by the flood and deposited in the bonebed. Bones lacking abrasion, as well as breakage angles, suggest rapid burial, showing that they were not transported very far, which indicates that the animals lived and died close to the place of accumulation [13]. It is important to note that a single vertebra of Pannoniasaurus (MTM V.2000.21.), as well as a variety of fish and crocodile teeth, were collected from the waste dump of the subterranean Ajka coal mine. The Ajka Coal Formation interdigitates with the Csehbánya Formation, the depositional environment of the latter was a floodplain, while the Ajka Coal Formation was formed in the accumulation basin of the same river system [30]. Both of these facies were formed in the same paleogeographic area, which itself might have been part of a larger, but isolated landmass, as suggested by endemic taxa such as Iharkutosuchus [17], Ajkaceratops [20], Hungarosaurus [21], [22], or Pannoniasaurus itself. Throughout the scientific study of the Csehbánya and Ajka Coal Formations (lasting back more than a century), these sediments are known to contain terrestrial plant and freshwater invertebrate fossils, the former yielding the continental vertebrate fauna discovered in 2000 [13], [29]. The Csehbánya Formation has never produced a single marine or brackish faunal or floral element. Besides lithological and sedimentological evidence, floral (i.e. leaf imprints and carbonized tree trunks) and faunal elements (i.e. freshwater invertebrates, freshwater and terrestrial vertebrates) also suggest that the environment of deposition was a freshwater river system. In the Ajka coal mines area, where the waste dump of the mine yielded the single Pannoniasaurus vertebra, only the upper part of the Ajka Coal Formation is known to contain marine invertebrates as transgression proceeded. The lower part of the formation contains freshwater molluscs and ostracods [25], [52]. The piece of rock that yielded the single vertebra is typical of the lower part of the formation, and contains abundant freshwater molluscs. Thus there is no evidence of Pannoniasaurus occurring outside freshwater environments. As with the other vertebrate remains found in the Iharkút assemblage, bones and teeth of Pannoniasaurus are known from multiple horizons of the Csehbánya Formation in the mine (though most of its remains were excavated from the SZ-6 bonebed). The single Pannoniasaurus vertebra from the Ajka Coal Formation, though compressed, is clearly not transported and indicates the presence of Pannoniasaurus also in that area. These facts demonstrate that Pannoniasaurus was abundant spatially and temporally within the Iharkút paleogeographic unit. The size of individual bones of Pannoniasaurus, when compared to those of various mosasaurs [6] and large bodied extant lizards, indicates that the total length of the largest specimens was about 6 meters, though most bones appear to refer to body lengths of approximately 3–4 meters; the smallest vertebrae suggest individuals with a total length of about 70 cm. Taphonomical studies of the vertebrate material of the locality suggest that there was no filter effect by size in the accumulation process [13], thus this size range of Pannoniasaurus remains seems to represent the population correctly. These evidences suggest that many individuals of various size and age classes of Pannoniasaurus were present in the area over a short time interval, suggesting that an entire population of Pannoniasaurus was living in these river systems as opposed to migrating into them for seasonal food opportunities or reproduction. A recent geochemical study [40] investigated the taphonomical and ecological differences among different vertebrates found at Iharkút. This study has proven that all the fossils belonging to different taxonomic groups from Iharkút have identical, generally high Rare Earth Element patterns as a result of early diagenetic maturation or recrystallization of the fossils, and identical Nd isotope compositions, which suggest a common diagenetic alteration history. Thus, the common presence of different taxa at the Iharkút site is unlikely to be related to reworking from different sedimentary units. Moreover, the δ18O PO4 values of Pannoniasaurus (and fish of the group Pycnodontiformes) are most compatible with a freshwater paleoenvironment, and are incompatible with these species having lived in Cretaceous seawater. δ18O CO3 values in all fossils from Iharkút were homogenized by diagenesis, thus ecological implications could be made only from the oxygen isotope composition of the phosphate. Finally, the 87Sr/86Sr ratios both of Pannoniasaurus and the Pycnodontiformes are inconsistent with a marine paleohabitat for these taxa. Thus the geochemical and isotopic data are most compatible with Pannoniasaurus having lived in a predominantly freshwater ecosystem [40]. Such evidence suggests strongly that Pannoniasaurus was not a seasonal migrant from marine waters into fresh, but rather that ecologically it was a permanent member of a freshwater fauna.

Ecological Implications Based on the Osteology of Pannoniasaurus The size of Pannoniasaurus makes it the largest known predator in the waters of this paleoenvironment [13]. Additionally, we consider the crocodile-like flattened skull (as indicated by the premaxilla and maxilla), to be a useful adaptation for water-level ambush hunting of terrestrial and shallow water prey. It is difficult to estimate how the unknown girdle and limb elements of Pannonisasaurus may have looked. As far as we know, Pannoniasaurus had a primitive vertebral column, a posteriorly oriented ilium and an elongated humerus with a distal epiphysis, all most similar to aigialosaurs [3], [43]. These suggest that P. inexpectatus had an overall aigialosaur-like postcranial morphology (including plesiopelvia and plesiopedia). However, Dallasaurus, for example, has an anteriorly oriented, hydropelvic ilium in combination with primitive-looking proximal limb elements [2]; thus, a flattened, derived distal limb morphology is not impossible for that taxon as noted by Caldwell and Palci [4]. Nevertheless, one must be careful when trying to reconstruct unknown portions of these animals. For Pannoniasaurus a primitive morphology of the complete limbs in correlation with the primitive axial skeleton and pelvis is more probable, but far from certain. It is possible that the retention of a robust sacrum, pelvis and possibly non-paddle-like limbs were used to help to propel the body forward from the bottom during prey-capture in shallow water, similar to extant crocodiles.

Previous Reports of Mosasauroids and Relatives from Freshwater Sediments The Pythonomorpha (dolichosaurs, aigialosaurs and mosasaurs) are conventionally characterized as ecologically marine lizards. A marine ecology is ascribed to them primarily because nearly 100% of their fossil occurrences are from rocks that are interpreted as having been deposited in a wide variety of marine environments (e.g., inland seaways, patch reef lagoons, a variety of nearshore and foreshore environments). The geological time range of the Pythonomorpha currently is recognized as beginning in the Barremian (Kaganaias sp. in Japan [10]) and terminating at the end of the Maastrichtian [6]. Though there is little doubt that the deep ancestry of pythonomorphs finds a common ancestor with an as yet unidentified sister group amongst terrestrial lizards and snakes [55], it is not known if their subsequent evolution took place in coastal environments and they adapted directly to marine and freshwater environments, or if they evolved on land, primarily adapting to freshwater and later inhabiting the seas. Though pythonomorph fossils have been recognized as coming from marine sediments since Cuvier [54], only recently have a few discoveries [9], [10], [13], [39], [40] raised the possibility of a freshwater ecology for a few taxa. The mosasaur Plioplatecarpus has been reported from freshwater sediments [9] from the Maastrichtian of Canada. It is not clear whether this report of a well-known marine genus demonstrates that some species of mosasaurs regularly exploited estuarine or freshwater environments, or if this specimen represents nothing more than a stochastic occurrence with no ecological implications whatsoever. The lack of similar finds suggests the latter. Goronyosaurus, an unusual mosasaur from Nigeria and Niger is thought to have possibly exploited estuarine environments based on its skull morphology, but none of its remains are known from freshwater sediments [56], [57]. As there is no corroborating evidence to suggest anything other than a marine ecology for Goronyosaurus, we take a conservative view and consider it to be a marine mosasaur. The recent publication [10] that reported Kaganaias, a long-bodied platynotan lizard from Lower Cretaceous freshwater sediments of Japan used the term mosasauroid loosely, as a collective term for dolichosaurs, pontosaurs, aigialosaurs, and mosasaurs. However, Kaganaias, as pointed out by the authors [10], is a primitive dolichosaur-like platynotan and might represent the first stages of aquatic adaptation among basal pythonomorphs. These finds mentioned above were not clear evidence of mosasauroids adapted to freshwater environments. However, a large number of remains of a new species of mosasauroid (described here as Pannoniasaurus), originating from multiple individuals were collected during several excavations at the Iharkút locality after its discovery in 2000. The first known specimen of Pannoniasaurus was the dorsal vertebra found on the waste dump of the Ajka coal mine in 1999, and more vertebrae were unearthed after the discovery of the Iharkút locality. However, these vertebrae were fragmentary and thus were first considered as belonging to large terrestrial varanoid lizards based on their characters such as precondylar constriction and oblique articulation of their centra [46]. Dorsal vertebrae of Pannoniasaurus strongly resemble varanoid vertebrae and terrestrial varanoids do occur in some Cretaceous localities (e.g. Estesia mongoliensis [58]). Thus, only after the discovery of more material (e.g. quadrates) was it recognized that these remains from Iharkút demonstrate the presence of a mosasauroid in the fauna. Later, other bones were identified in the material, and large-scale excavations at the locality continued, yielding more remains of Pannoniasaurus, and more evidence for the freshwater occurrence for multiple individuals of a basal mosasauroid [13], [39], [40,]. Pannoniasaurus became the first mosasauroid to be represented by multiple specimens from freshwater sediments. As a matter of fact, even if some pannoniasaurs were capable of moving back and forth from fluvial systems to the estuaries, or even further into marine environments, similar to extant La Plata dolphins but in contrast to exclusively riverine dolphin species (e.g. Amazon river dolphin) [12], it would not be a rejection of our hypothesis of Pannoniasaurus being the first mosasaur adapted to a freshwater environment.