@techreport{gilmore1933on1,
    author = "Gilmore, C. W",
    title = "On the dinosaurian fauna of the Iren Dabasu Formation",
    year = "1933",
    howpublished = "Bulletin of the American Museum of Natural History, v. 67, p. 23-78",
    note = "talkorigins\_source = {true}; raw\_reference = {Gilmore, C. W., 1933, On the dinosaurian fauna of the Iren Dabasu Formation: Bulletin of the American Museum of Natural History, v. 67, p. 23-78.}"
}

@article{openalexw1556338760,
    author = "Gilmore, Charles W. and Expeditions, Central Asiatic",
    title = "On the dinosaurian fauna of the Iren Dabasu Formation. Bulletin of the AMNH; v. 67, article 2",
    year = "1933",
    journal = "American Museum Novitates",
    url = "https://openalex.org/W1556338760",
    openalex = "W1556338760"
}

@article{openalexw7157510809,
    author = "Gilmore, Charles W. and Expeditions, Central Asiatic",
    title = "Dinosaurian fauna of the Iren Dabasu Formation",
    year = "1933",
    journal = "American Museum Novitates",
    abstract = "p. 23-78, 8 leaves of plates: ill., map; 25 cm.",
    url = "https://openalex.org/W7157510809",
    openalex = "W7157510809"
}

@article{smith1990osteology,
    author = "Smith, David and Galton, Peter",
    title = "Osteology of Archaeornithomimus asiaticus (Upper Cretaceous, Iren Dabasu Formation, People's Republic of China)",
    year = "1990",
    journal = "Journal of Vertebrate Paleontology",
    url = "https://doi.org/10.1080/02724634.1990.10011811",
    doi = "10.1080/02724634.1990.10011811",
    number = "2",
    openalex = "W2013213746",
    pages = "255-265",
    volume = "10",
    references = "doi101038277560a0, doi101086273307, doi101126science9231776, doi101139e72031, doi105281zenodo16246150, doi105281zenodo16651680, doi105479si03629236110i, openalexw2788234611, openalexw2980052577, openalexw3208547338"
}

@article{currie1993palaeontology,
    author = "Currie, P.J. and Eberth, D.A.",
    title = "Palaeontology, sedimentology and palaeoecology of the Iren Dabasu Formation (Upper Cretaceous), Inner Mongolia, People's Republic of China",
    year = "1993",
    journal = "Cretaceous Research",
    url = "https://doi.org/10.1006/cres.1993.1011",
    doi = "10.1006/cres.1993.1011",
    number = "2",
    openalex = "W2053963693",
    pages = "127-144",
    volume = "14"
}

@article{doi10108002724634199510011230,
    author = "Carpenter, Kenneth and Dilkes, David W. and Weishampel, David B.",
    title = "The Dinosaurs of the Niobrara Chalk Formation (Upper Cretaceous, Kansas)",
    year = "1995",
    journal = "Journal of Vertebrate Paleontology",
    abstract = {ABSTRACT The dinosaurian fauna of the Niobrara Chalk Formation constitutes the best known assemblage from the middle Santonian-early Campanian interval of the Late Cretaceous of North America. The fauna consists of both hadrosaurid ornithopods and nodosaurid ankylosaurs. The nodosaurid specimens from the Smoky Hill Chalk Member of the Niobrara Chalk Formation include the holotype of Hierosaurus sternbergii (here regarded as nomen dubium), material of "Hierosaurus" coleii (herein designated the type species of the new genus Niobrarasaurus) and two specimens that may belong to N. coleii, but are better interpreted as Nodosauridae incertae sedis. Claosaurus agilis, the sole hadrosaurid from the Niobrara Chalk Formation, constitutes a poorly known, but distinct species having a basal relationship among remaining hadrosaurids.},
    url = "https://doi.org/10.1080/02724634.1995.10011230",
    doi = "10.1080/02724634.1995.10011230",
    openalex = "W2072060069",
    references = "doi101007bf02988144, doi10108002724634199010011815, doi101086273307, doi101093nqs5vi146318i, doi101126science5123738, doi101130spe40p1, doi102475ajss339233418, doi105281zenodo1048846, doi105281zenodo16226902, doi105479si00963801361666197, openalexw1556338760, openalexw51761775"
}

@article{vanitterbeeck2005stratigraphy,
    author = "Van Itterbeeck, Jimmy and Horne, David J. and Bultynck, Pierre and Vandenberghe, Noël",
    title = "Stratigraphy and palaeoenvironment of the dinosaur-bearing Upper Cretaceous Iren Dabasu Formation, Inner Mongolia, People's Republic of China",
    year = "2005",
    journal = "Cretaceous Research",
    url = "https://doi.org/10.1016/j.cretres.2005.03.004",
    doi = "10.1016/j.cretres.2005.03.004",
    number = "4",
    openalex = "W2004815860",
    pages = "699-725",
    volume = "26",
    references = "crossref1996the, doi1010160012825277900551, doi101016003101828890096x, doi101017s0094837300006941, doi101111j136530911972tb00013x, doi101130001676061968791573scpcot20co2, doi1011300016760619931050129cop23co2, doi1011300016760620011131560sratio20co2, doi105860choice331556, openalexw1535663436"
}

@article{longrich2008a,
    author = "LONGRICH, NICK",
    title = "A NEW, LARGE ORNITHOMIMID FROM THE CRETACEOUS DINOSAUR PARK FORMATION OF ALBERTA, CANADA: IMPLICATIONS FOR THE STUDY OF DISSOCIATED DINOSAUR REMAINS",
    year = "2008",
    journal = "Palaeontology",
    abstract = "Only two ornithomimid genera, Ornithomimus and Struthiomimus, are currently known from the Upper Cretaceous of North America. However, a number of ornithomimid elements from Alberta’s Dinosaur Park Formation (Upper Campanian), cannot be assigned to either Ornithomimus or Struthiomimus. These bones, including a frontal, caudal vertebrae, and unguals of the manus and the pes, come from animals significantly larger than any previously known Judithian ornithomimid. The frontal exhibits several unusual features, including transverse expansion over the prefrontals, and extreme reduction of the supratemporal fossae. Caudal vertebrae are characterized by neural arches that are posteriorly shifted and transversely expanded. Manual unguals possess a highly concave articular surface, a flexor tubercle divided by a sulcus, and a broad claw. Pedal unguals display highly concave articular surfaces, and a ridge‐like flexor tubercle dividing a deep ventral fossa. Although it is difficult to know whether these elements represent a single taxon, this is currently the most parsimonious hypothesis. This study demonstrates how isolated dinosaur bones can extend our knowledge of dinosaur faunas.",
    url = "https://doi.org/10.1111/j.1475-4983.2008.00791.x",
    doi = "10.1111/j.1475-4983.2008.00791.x",
    number = "4",
    openalex = "W1984804423",
    pages = "983-997",
    volume = "51",
    references = "doi101017cbo9780511608377011, doi101139e72031, doi1016660022336020030770822mbatho20co2, doi102475ajss32313381, doi105860choice393984, doi105860choice434677, doi105860choice435902, openalexw3190253505, openalexw3215057009, openalexw337536883, openalexw607142922, smith1990osteology"
}

@incollection{crossref2009iren,
    title = "Iren Dabasu Formation",
    year = "2009",
    booktitle = "Geological Formation Names of China (1866–2000)",
    url = "https://doi.org/10.1007/978-3-540-93824-8\_3450",
    doi = "10.1007/978-3-540-93824-8\_3450",
    openalex = "W2477825070",
    pages = "488-488"
}

@article{doi10108002724630903412372,
    author = "Jin, Liyong and Jun, Chen and Shuqin, Zan and Butler, Richard J. and Godefroit, Pascal",
    title = "Cranial anatomy of the small ornithischian dinosaur Changchunsaurus parvus from the Quantou Formation (Cretaceous: Aptian–Cenomanian) of Jilin Province, northeastern China",
    year = "2010",
    journal = "Journal of Vertebrate Paleontology",
    abstract = "ABSTRACT The Quantou Formation of Jilin Province, People's Republic of China, has recently yielded an important new fauna of ‘middle’ Cretaceous vertebrates. This fauna includes the small-bodied cerapodan ornithischian dinosaur Changchunsaurus parvus, represented by excellent cranial and postcranial material. When initially described, Changchunsaurus was hypothesed to represent one of the most basal known ornithopods; however, similarities to ceratopsians were also noted, suggesting that Changchunsaurus may be crucial to elucidating the interrelationships of basal cerapodans, one of most problematic areas of ornithischian phylogeny. Here we present a detailed description of the craniodental anatomy of Changchunsaurus, rediagnose the taxon based upon three autapomorphies, and provide comparisons to other basal cerapodans, as a foundation for future studies of basal cerapodan relationships. Changchunsaurus shows strong similarities to the Chinese Early Cretaceous cerapodan Jeholosaurus, and it is likely that they are sister taxa.",
    url = "https://doi.org/10.1080/02724630903412372",
    doi = "10.1080/02724630903412372",
    openalex = "W2030740650",
    references = "doi10120600030082200635301ydanpc20co2"
}

@article{doi10108014772011003594870,
    author = "Agnolín, Federico L. and Ezcurra, Martín D. and Pais, Diego F. and Salisbury, Steven W.",
    title = "A reappraisal of the Cretaceous non-avian dinosaur faunas from Australia and New Zealand: evidence for their Gondwanan affinities",
    year = "2010",
    journal = "Journal of Systematic Palaeontology",
    abstract = "It has often been assumed that Australasian Cretaceous dinosaur faunas were for the most part endemic, but with some Laurasian affinities. In this regard, some Australasian dinosaurs have been considered Jurassic relicts, while others were thought to represent typical Laurasian forms or endemic taxa. Furthermore, it has been proposed that some dinosaurian lineages, namely oviraptorosaurians, dromaeosaurids, ornithomimosaurians and protoceratopsians, may have originated in Australia before dispersing to Asia during the Early Cretaceous. Here we provide a detailed review of Cretaceous non-avian dinosaurs from Australia and New Zealand, and compare them with taxa from other Gondwanan landmasses. Our results challenge the traditional view of Australian dinosaur faunas, with the majority of taxa displaying affinities that are concordant with current palaeobiogeographic models of Gondwanan terrestrial vertebrate faunal distribution. We reinterpret putative Australian ‘hypsilophodontids’ as basal ornithopods (some of them probably related to South American forms), and the recently described protoceratopsians are referred to Genasauria indet. and Ornithopoda indet. Among Theropoda, the Australian pigmy ‘Allosaurus’ is referred to the typical Gondwanan clade Abelisauroidea. Similarities are also observed between the enigmatic Australian theropod Rapator, Australovenator and the South American carcharodontosaurian Megaraptor. Timimus and putative oviraptorosaurians are referred to Dromaeosauridae. The present revision demonstrates that Australia's non-avian Cretaceous dinosaurian faunas were reminiscent of those found in other, roughly contemporaneous, Gondwanan landmasses, and are suggestive of faunal interchange with these regions via Antarctica.",
    url = "https://doi.org/10.1080/14772011003594870",
    doi = "10.1080/14772011003594870",
    openalex = "W2151988812",
    references = "chinsamy1998polar, crossref1998encyclopedia, deklerk2000a, doi101017s0016756804000330, doi10108002724634198510011859, doi10108002724634199510011230, doi101093oxfordjournalsafrafa101747, doi101098rspb20060443, doi101126science10246376, doi101126science11282807, doi101126science24248841403, doi101126science28454232137, doi105281zenodo16171435, doi105281zenodo16673433, doi105281zenodo16692311, doi105860choice331556, doi105860choice353642, doi107312kiel11918, openalexw1821824396, openalexw1879660213, openalexw2173200745, openalexw597685939, openalexw616953834"
}

@article{doi101080147720192013781067,
    author = "Choiniere, Jonah N. and Clark, James M. and Forster, Catherine A. and Norell, Mark A. and Eberth, David A. and Erickson, Gregory M. and Chu, Hongjun and Xu, Xing",
    title = "A juvenile specimen of a new coelurosaur (Dinosauria: Theropoda) from the Middle–Late Jurassic Shishugou Formation of Xinjiang, People's Republic of China",
    year = "2013",
    journal = "Journal of Systematic Palaeontology",
    abstract = "We describe the anatomy of a new coelurosaurian theropod Aorun zhaoi gen. et sp. nov., from the Middle–Late Jurassic of Xinjiang, China. Histological analysis of the holotype and only known specimen shows that the new taxon is represented by the skeleton of a juvenile individual aged no more than one year. A phylogenetic analysis of theropod relationships places Aorun as a basal member of the Coelurosauria. Although the sole use of a sub-adult ontogenetic exemplar is potentially problematic for phylogenetic reconstruction, we show that the phylogenetic position of Aorun as a member of Coelurosauria is robust to the exclusion of characters known to change during theropod ontogeny. Aorun is the seventh theropod taxon, and temporally oldest coelurosaur, known from the Shishugou Formation, which has one of the most taxonomically diverse Jurassic coelurosaurian theropod faunas in the world.http://zoobank.org/urn:lsid:zoobank.org:pub:5CC73577-9EB3-47AB-9983-1677B278EFFD",
    url = "https://doi.org/10.1080/14772019.2013.781067",
    doi = "10.1080/14772019.2013.781067",
    openalex = "W2144457175",
    references = "doi101017cbo9780511536045, doi101051jphystap019020010017801, doi101080027246342010520779, doi101080027246342011557116, doi10108025761900202212131807, doi101086273307, doi101111j109600311994tb00179x, doi101111j109600311999tb00278x, doi101111j10963642200700269x, doi101111j14209101201102427x, doi101111j155856461982tb05453x, doi1011270077774920100125, doi101144sp31516, doi101371journalpone0017932, doi105281zenodo16171435, openalexw1821824396, openalexw2611511275, openalexw2989049194, openalexw3206657856, xu2010a"
}

@article{doi101016jcretres201406003,
    author = "Romilio, Anthony and Salisbury, Steven W.",
    title = "Large dinosaurian tracks from the Upper Cretaceous (Cenomanian–Turonian) portion of the Winton Formation, Lark Quarry, central-western Queensland, Australia: 3D photogrammetric analysis renders the ‘stampede trigger’ scenario unlikely",
    year = "2014",
    journal = "Cretaceous Research",
    url = "https://doi.org/10.1016/j.cretres.2014.06.003",
    doi = "10.1016/j.cretres.2014.06.003",
    openalex = "W2060622248",
    references = "apesteguía2011tunasniyoj, doi101016jcretres200908003"
}

@article{doi1010800272463420161269539,
    author = "Salisbury, Steven W. and Romilio, Anthony and Herne, Matthew and Tucker, Ryan T. and Nair, Jay P.",
    title = "The Dinosaurian Ichnofauna of the Lower Cretaceous (Valanginian–Barremian) Broome Sandstone of the Walmadany Area (James Price Point), Dampier Peninsula, Western Australia",
    year = "2016",
    journal = "Journal of Vertebrate Paleontology",
    abstract = "Extensive and well-preserved tracksites in the coastally exposed Lower Cretaceous (Valanginian–Barremian) Broome Sandstone of the Dampier Peninsula provide almost the entire fossil record of dinosaurs from the western half of the Australian continent. Tracks near the town of Broome were described in the late 1960s as Megalosauropus broomensis and attributed to a medium-sized theropod trackmaker. Brief reports in the early 1990s suggested the occurrence of at least another nine types of tracks, referable to theropod, sauropod, ornithopod, and thyreophoran trackmakers, at scattered tracksites spread over more than 80 km of coastline north of Broome, potentially representing one of the world's most diverse dinosaurian ichnofaunas. More recently, it has been proposed that this number could be as high as 16 and that the sites are spread over more than 200 km. However, the only substantial research that has been published on these more recent discoveries is a preliminary study of the sauropod tracks and an account of the ways in which the heavy passage of sauropod trackmakers may have shaped the Dampier Peninsula's Early Cretaceous landscape. With the other types of dinosaurian tracks in the Broome Sandstone remaining undescribed, and the full extent and nature of the Dampier Peninsula's dinosaurian tracksites yet to be adequately addressed, the overall scientific significance of the ichnofauna has remained enigmatic. At the request of the area's Goolarabooloo Traditional Custodians, 400+ hours of ichnological survey work was undertaken from 2011 to 2016 on the 25 km stretch of coastline in the Yanijarri–Lurujarri section of the Dampier Peninsula, inclusive of the coastline at Walmadany (James Price Point). Forty-eight discrete dinosaurian tracksites were identified in this area, and thousands of tracks were examined and measured in situ and using three-dimensional photogrammetry. Tracksites were concentrated in three main areas along the coast: Yanijarri in the north, Walmadany in the middle, and Kardilakan–Jajal Buru in the south. Lithofacies analysis revealed 16 repeated facies types that occurred in three distinctive lithofacies associations, indicative of an environmental transgression between the distal fluvial to deltaic portions of a large braid plain, with migrating sand bodies and periodic sheet floods. The main dinosaurian track-bearing horizons seem to have been generated between periodic sheet floods that blanketed the preexisting sand bodies within the braid plain portion of a tidally influenced delta, with much of the original, gently undulating topography now preserved over large expanses of the present day intertidal reef system. Of the tracks examined, 150 could be identified and are assignable to a least eleven and possibly as many as 21 different track types: five different types of theropod tracks, at least six types of sauropod tracks, four types of ornithopod tracks, and six types of thyreophoran tracks. Eleven of these track types can formally be assigned or compared to existing or new ichnotaxa, whereas the remaining ten represent morphotypes that, although distinct, are currently too poorly represented to confidently assign to existing or new ichnotaxa. Among the ichnotaxa that we have recognized, only two (Megalosauropus broomensis and Wintonopus latomorum) belong to existing ichnotaxa, and two compare to existing ichnotaxa but display a suite of morphological features suggesting that they may be distinct in their own right and are therefore placed in open nomenclature. Six of the ichnotaxa that we have identified are new: one theropod ichnotaxon, Yangtzepus clarkei, ichnosp. nov.; one sauropod ichnotaxon, Oobardjidama foulkesi, ichnogen. et ichnosp. nov.; two ornithopod ichnotaxa, Wintonopus middletonae, ichnosp. nov., and Walmadanyichnus hunteri, ichnogen. et ichnosp. nov.; and two thyreophoran ichnotaxa, Garbina roeorum, ichnogen. et ichnosp. nov., and Luluichnus mueckei, ichnogen. et ichnosp. nov. The level of diversity of the main track types is comparable across areas where tracksites are concentrated: Kardilakan–Jajal Buru (12), Walmadany (11), and Yanijarri (10). The overall diversity of the dinosaurian ichnofauna of the Broome Sandstone in the Yanijarri–Lurujarri section of the Dampier Peninsula is unparalleled in Australia, and even globally. In addition to being the primary record of non-avian dinosaurs in the western half of Australia, this ichnofauna provides our only detailed glimpse of Australia's dinosaurian fauna during the first half of the Early Cretaceous. It indicates that the general composition of Australia's mid-Cretaceous dinosaurian fauna was already in place by the Valanginian–Barremian. Both sauropods and ornithopods were diverse and abundant, and thyreophorans were the only type of quadrupedal ornithischians. Important aspects of the fauna that are not seen in the Australian mid-Cretaceous body fossil record are the presence of stegosaurians, an overall higher diversity of thyreophorans and theropods, and the presence of large-bodied hadrosauroid-like ornithopods and very large-bodied sauropods. In many respects, these differences suggest a holdover from the Late Jurassic, when the majority of dinosaurian clades had a more cosmopolitan distribution prior to the fragmentation of Pangea. Although the record for the Lower Cretaceous of Gondwana is sparse, a similar mix of taxa occurs in the Barremian–lower Aptian La Amarga Formation of Argentina and the Berriasian–Hauterivian Kirkwood Formation of South Africa. The persistence of this fauna across the Jurassic-Cretaceous boundary in South America, Africa, and Australia might be characteristic of Gondwanan dinosaurian faunas more broadly. It suggests that the extinction event that affected Laurasian dinosaurian faunas across the Jurassic-Cretaceous boundary may not have been as extreme in Gondwana, and this difference may have foreshadowed the onset of Laurasian-Eurogondwanan provincialism. The disappearance of stegosaurians and the apparent drop in diversity of theropods by the mid-Cretaceous suggests that, similar to South America, Australia passed through a period of faunal turnover between the Valanginian and Aptian. SUPPLEMENTAL DATA—Supplemental materials are available for this article for free at www.tandfonline.com/UJVP Citation for this article: Salisbury, S. W., A. Romilio, M. C. Herne, R. T. Tucker, and J. P. Nair. 2017. The dinosaurian ichnofauna of the Lower Cretaceous (Valanginian–Barremian) Broome Sandstone of the Walmadany area (James Price Point), Dampier Peninsula, Western Australia. Society of Vertebrate Paleontology Memoir 16. Journal of Vertebrate Paleontology 36(6, Supplement). DOI: 10.1080/02724634.2016.1269539.",
    url = "https://doi.org/10.1080/02724634.2016.1269539",
    doi = "10.1080/02724634.2016.1269539",
    openalex = "W2602833024",
    references = "apesteguía2011tunasniyoj, deklerk2000a, doi101002mmng19994860020102, doi101007bf02988144, doi1010160012825277900551, doi1010160012825279900011, doi1010160012825285900017, doi101016002532279290061l, doi101016jcretres200908003, doi101016jcretres201304001, doi101016jcretres201307009, doi101016jgr201403014, doi101016jjafrearsci201205005, doi101016jsedgeo200610001, doi101016s001678780180047x, doi101017cbo9780511626487, doi101038srep06196, doi101038srep19165, doi101038srep34467, doi101046j14401738200300386x, doi10108000288306197010418211, doi10108002724634199810011086, doi10108008912960903503345, doi10108010420940109380189, doi10108010420940490428625, doi10108010420940601006859, doi10108011035890902924877, doi1010801477201920151059985, doi101093oxfordjournalsafrafa100309, doi101111j10963642201000620x, doi101111j10963642201000642x, doi101130g23452a1, doi101139e91009, doi101144pygs543185, doi101306212f83b92b2411d78648000102c1865d, doi101371journalpone0013120, doi101371journalpone0072579, doi101371journalpone0137709, doi1022179revmacn7344, doi1026879529, doi104095105049, doi104202app20080049, foster1995tridactyl, mateus2010a, nouri2011tetradactyl, openalexw1564145569, openalexw1592791648, openalexw2173200745, openalexw2618301958, openalexw2619609965, openalexw616953834"
}

@article{doi101038s41598017052726,
    author = "Chinzorig, Tsogtbaatar and Kobayashi, Yoshitsugu and Tsogtbaatar, Khishigjav and Currie, Philip J. and Watabe, Mahito and Барсболд, Ринчен",
    title = "First Ornithomimid (Theropoda, Ornithomimosauria) from the Upper Cretaceous Djadokhta Formation of Tögrögiin Shiree, Mongolia",
    year = "2017",
    journal = "Scientific Reports",
    abstract = "The Upper Cretaceous Djadokhta Formation has been intensively surveyed for its fossil vertebrate fauna for nearly a century. Amongst other theropods, dromaeosaurids and parvicursorines are common in the formation, but ornithomimosaurs are extremely rare. A new ornithomimosaur material was discovered from the Djadokhta Formation, represented by eolian deposits, of the Tögrögiin Shiree locality, Mongolia. This is only the third ornithomimosaur specimen reported from this formation, and includes the astragalus, the calcaneum, the third distal tarsal, and a complete pes. The new material is clearly belonged to Ornithomimidae by its arctometatarsalian foot condition and has the following unique characters; unevenly developed pair of concavities of the third distal tarsal, curved contacts between the proximal ends of second and fourth metatarsals, the elongate fourth digit, and a laterally inclined medial condyle on phalanx IV-1. These diagnostic characters of the Djadokhtan ornithomimosaur indicate that this is a new taxon. Our phylogenetic analysis supports three clades within derived ornithomimosaurs, and the new taxon is placed a member of the derived ornithomimosaurs. The present specimen is the first ornithomimid record from eolian Tögrögiin Shiree locality, and is indicative of their capability to adapt to arid environments.",
    url = "https://doi.org/10.1038/s41598-017-05272-6",
    doi = "10.1038/s41598-017-05272-6",
    openalex = "W2734949035",
    references = "doi1010160195667191900155, doi101038362623a0, doi10108002724634199510011574, doi101111j10960031200800217x, doi101139e72031, doi101525california97805202420980010001, doi102475ajss32313381, doi105281zenodo13315375, openalexw2751580477, openalexw3215057009"
}

@article{doi1010801477201920211978005,
    author = "Lockwood, Jeremy A. F. and Martill, David M. and Maidment, Susannah C. R.",
    title = "A new hadrosauriform dinosaur from the Wessex Formation, Wealden Group (Early Cretaceous), of the Isle of Wight, southern England",
    year = "2021",
    journal = "Journal of Systematic Palaeontology",
    abstract = "A new genus and species of non-hadrosaurid hadrosauriform dinosaur, Brighstoneus simmondsi gen. et sp. nov., is described from the Lower Cretaceous Wessex Formation of the Isle of Wight. The new taxon has two autapomorphies, a nasal having a modest nasal bulla with convex sides, and primary and accessory ridges on the lingual aspect of the maxillary crown. The dentary has at least 28 alveolar positions, which is the highest number recorded in an ornithopod with non-parallel sided alveoli, creating a character combination that is unique within Iguanodontia. The hadrosauriform fauna of the Barremian–Aptian Wealden Group on both the Isle of Wight and mainland England has been represented for almost a century by just two taxa, the robust Iguanodon bernissartensis and the more gracile Mantellisaurus atherfieldensis, with referred material often being fragmentary or based on unassociated elements. This discovery increases the known hadrosauriform diversity in England and, together with recent discoveries in Spain, suggests that their diversity in the upper Wealden of Europe was considerably wider than initially realized. This find also has important implications for the validity of the Mantellisaurus atherfieldensis hypodigm, and a reassessment of existing material is suggested.http://zoobank.org/urn:lsid:zoobank.org:pub:31F0D48F-C1DA-406E-A811-1F5937ED19F4",
    url = "https://doi.org/10.1080/14772019.2021.1978005",
    doi = "10.1080/14772019.2021.1978005",
    openalex = "W3211438913",
    references = "doi101111brv12666, doi101111zoj12193, doi101371journalpone0045712, gates2018a, tsogtbaatar2019a"
}

@article{carr2022a,
    author = "Carr, Thomas D.",
    title = "A reappraisal of tyrannosauroid fossils from the Iren Dabasu Formation (Coniacian–Campanian), Inner Mongolia, People’s Republic of China",
    year = "2022",
    journal = "Journal of Vertebrate Paleontology",
    url = "https://doi.org/10.1080/02724634.2023.2199817",
    doi = "10.1080/02724634.2023.2199817",
    number = "5",
    openalex = "W4378882686",
    volume = "42",
    references = "carr1999craniofacial, doi101007s11692022095731, doi101017cbo9780511608377011, doi101038063003a0, doi10108002724634200310010947, doi101098rspl18870117, doi101126science2562999, doi101139e93179, doi1012067481, doi105860choice393984, openalexw1535663436"
}

@article{doi103390d16090531,
    author = "Longrich, Nicholas R. and Ramírez-Velasco, Ángel Alejandro and Kirkland, Jim and Torres, Andrés and Serrano-Brañas, Claudia Inés",
    title = "Coahuilasaurus lipani, a New Kritosaurin Hadrosaurid from the Upper Campanian Cerro Del Pueblo Formation, Northern Mexico",
    year = "2024",
    journal = "Diversity",
    abstract = "The Late Cretaceous of Western North America (Laramidia) supported a diverse dinosaur fauna, with duckbilled dinosaurs (Hadrosauridae) being among the most speciose and abundant members of this assemblage. Historically, collecting and preservational biases have meant that dinosaurs from Mexico and the American Southwest are poorly known compared to those of the northern Great Plains. However, evidence increasingly suggests that distinct species and clades inhabited southern Laramidia. Here, a new kritosaurin hadrosaurid, represented by the anterior part of a skull, is reported from the late Campanian of the Cerro del Pueblo Formation, \textasciitilde 72.5 Ma, in Coahuila, Mexico. The Cerro del Pueblo Formation kritosaur was originally considered to represent the same species as a saurolophine from the Olmos Formation of Sabinas, but the Sabinas hadrosaur is now considered a distinct taxon. More recently, the Cerro del Pueblo Formation kritosaur has been referred to Kritosaurus navajovius. We show it represents a new species related to Gryposaurus. The new species is distinguished by its large size, the shape of the premaxillary nasal process, the strongly downturned dentary, and massive denticles on the premaxilla’s palatal surface, supporting recognition of a new taxon, Coahuilasaurus lipani. The dinosaur assemblage of the Cerro del Pueblo Formation shows higher diversity than the contemporaneous fauna of the Horseshoe Canyon Formation in Alberta. Furthermore, Kritosaurini, Lambeosaurini, and Parasaurolophini all persist into the latest Campanian in southern Laramidia after disappearing from northern Laramidia. These patterns suggest declining herbivore diversity seen at high latitudes may be a local, rather than global phenomenon, perhaps driven by cooling at high latitudes in the Late Campanian and Maastrichtian.",
    url = "https://doi.org/10.3390/d16090531",
    doi = "10.3390/d16090531",
    openalex = "W4402127568",
    references = "doi101016jjsames2020102610, doi107287peerjpreprints2554"
}

@article{wang2025a,
    author = "Wang, Shuo and Ding, Nuo and Tan, Qingwei and Yang, Rui and Zhang, Qiyue and Tan, Lin",
    title = "A new Urbacodon (Theropoda, Troodontidae) from the Upper Cretaceous Iren Dabasu Formation, China: Implications for troodontid phylogeny and tooth biology",
    year = "2025",
    journal = "Cladistics",
    abstract = "Tooth attachment and replacement play significant roles in the feeding ecology of polyphyodont vertebrates, yet these aspects have remained largely unexplored in non‐avialan paravians including troodontids. Here, we describe a new troodontid species, Urbacodon norelli sp.n., recovered from the Upper Cretaceous Iren Dabasu Formation of Inner Mongolia, China, based on an incomplete right dentary and 12 associated replacement teeth. Urbacodon norelli is distinguished from all other known troodontids, including its relative U. itemirensis from Uzbekistan, by several features: the presence of paired dentary symphyseal foramina, the presence of a relatively steep anterior margin of the dentary, the absence of a dentary chin, the presence of a common groove hosting the anterior 12 dentary teeth, and the presence of relatively larger dentary teeth. Phylogenetic analysis places both species of Urbacodon as sister taxa to Zanabazar junior, confirming their status as later‐diverging troodontids. Radiographs revealed an alternating tooth replacement pattern in U. norelli, with a maximum Zahnreihen‐spacing estimated to be 3. During tooth replacement, the anteriorly inclined interdental septa, which wedge between anterior dentary teeth, underwent frequent remodelling as the developing tooth moved upwards, particularly anterolabially. This rapid turnover left insufficient time for an interdental plate to form, resulting in the absence of such structures in this specimen. The frequent remodelling of periodontal tissues accompanying tooth replacement is likely to account for the absence of interdental plates. The discovery of this new troodontid expands our understanding of paravian theropods from the Upper Cretaceous Iren Dabasu Formation and provides valuable insights into troodontid tooth biology.",
    url = "https://doi.org/10.1111/cla.12592",
    doi = "10.1111/cla.12592",
    number = "1",
    openalex = "W4400734969",
    pages = "104-134",
    volume = "41",
    references = "crossref1998encyclopedia, doi101038nature05986, doi101038nature08322, doi101093bioinformatics178754, doi101093bioinformaticsbty633, doi101093sysbiosyp067, doi101093sysbiosys029, doi101111cla12524, doi101111j10960031200800217x, doi101186s12862024022332, doi105962bhltitle52196, sues1977dentaries"
}