Joseph A. Bonsor, J. Lockwood, J. Leite, Amy Scott-Murray, S. Maidment
{"title":"THE OSTEOLOGY OF THE HOLOTYPE OF THE BRITISH IGUANODONTIAN DINOSAUR MANTELLISAURUS ATHERFIELDENSIS","authors":"Joseph A. Bonsor, J. Lockwood, J. Leite, Amy Scott-Murray, S. Maidment","doi":"10.1080/02693445.2023.2234156","DOIUrl":"https://doi.org/10.1080/02693445.2023.2234156","url":null,"abstract":"ABSTRACT Iguanodontian dinosaurs are known from Middle Jurassic to Late Cretaceous deposits worldwide and are historically important because they include the first fossils to be identified as giant extinct reptiles that later became known as dinosaurs. Due to historical taxonomic practices and the fragmentary nature of many specimens, discoveries from the 19th century were referred to Iguanodon with little appraisal, resulting in the genus becoming something of a ‘wastebasket taxon’. Reinterpretations of holotype specimens are an important step in attempting to understand the evolutionary history of iguanodontian dinosaurs. Here, we redescribe the holotype of Mantellisaurus atherfieldensis, one of the most complete British dinosaur specimens, from the Barremian/Aptian of the Isle of Wight, UK, and assess its phylogenetic position. We find that Mantellisaurus atherfieldensis is a valid taxon distinct from the genus Iguanodon based on three autapomorphies of the premaxilla, maxilla, and scapula, and resolves as an early diverging hadrosauroid styracosternan, representing an important step in the evolutionary history of the ornithopods.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"45 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-01-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126673393","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
S. Maidment, Kimberley E. J. Chapelle, Joseph A. Bonsor, David J. Button, P. Barrett
{"title":"OSTEOLOGY AND RELATIONSHIPS OF CUMNORIA PRESTWICHII (ORNITHISCHIA: ORNITHOPODA) FROM THE LATE JURASSIC OF OXFORDSHIRE, UK","authors":"S. Maidment, Kimberley E. J. Chapelle, Joseph A. Bonsor, David J. Button, P. Barrett","doi":"10.1080/02693445.2022.2162669","DOIUrl":"https://doi.org/10.1080/02693445.2022.2162669","url":null,"abstract":"ABSTRACT The iguanodontian dinosaurs have a fossil record that extends from the Middle Jurassic to the end of the Cretaceous, by which time they had diversified to become the dominant herbivores of Laurasian ecosystems. They are historically important because fossils of British iguanodontians were among the first to be recognised as the gigantic reptiles that formed the basis for naming Dinosauria. However, the early stages of their evolution remain obscure because of a sparse fossil record, and taxonomic and systematic controversies among non-hadrosaurid iguanodontians abound. In order to shed light on the early stages of iguanodontian evolution, new discoveries and re-interpretations of historic specimens are crucial. Here, we redescribe the Late Jurassic early-branching iguanodontian Cumnoria prestwichii from the Kimmeridge Clay Formation of Oxfordshire, UK, and assess its phylogenetic position. We find that Cumnoria is distinct from the North American taxon Camptosaurus, with which it was previously synonymized, and is valid, possessing two autapomorphies of the pectoral girdle. We recover its phylogenetic position as a non-ankylopollexian iguanodontian. Cumnoria represents one of just four valid ornithopod taxa from the Jurassic of Europe.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"77 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125417257","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"BRITISH SILURIAN BEYRICHIACEA (OSTRACODA). PART 2","authors":"D. Siveter","doi":"10.1080/02693445.2022.2143626","DOIUrl":"https://doi.org/10.1080/02693445.2022.2143626","url":null,"abstract":"ABSTRACT In Part 2 those ostracods belonging to the Treposellidae, Beyrichiidae and Beyrichiacea Family Uncertain are described, and are referred to a total of 17 genera and 35 named species. The Treposellidae comprises six genera (one new) and seven species (four new). The Beyrichiidae comprises Beyrichiinae (five genera, one new; one new subgenus; and 19 species, five new) and Kloedeniinae (four genera; and six species). Beyrichiacea Family Uncertain comprises two genera (one new) and three species (one new). A total of seven other forms are referred to the Treposellidae, Beyrichiidae and Beyrichiacea Family Uncertain under open nomenclature or are simply recorded. The biostratigraphy of British Silurian Beyrichiacea and their palaeoecological and palaeobiogeographical context is also documented.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"66 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-05-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128753495","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"THE EARLY JURASSIC BIVALVIA FROM THE HETTANGIAN AND LOWER SINEMURIAN OF SOUTH-WEST BRITAIN. PART 4","authors":"P. Hodges","doi":"10.1080/02693445.2022.2133204","DOIUrl":"https://doi.org/10.1080/02693445.2022.2133204","url":null,"abstract":"ABSTRACT Part 4 concludes the descriptions of early Jurassic bivalves from the Hettangian and Lower Sinemurian stages of south-west Britain. Fifty-four species are assigned to the subclass Pteriomorphia, including the genera Grammatodon (Grammatodon), Grammatodon (Cosmetodon), Plagiostoma, Antiquilima, Pseudolimea, Ctenostreon, Otapiria, Oxytoma (Oxytoma), Palmoxytoma, Meleagrinella (Praemeleagrinella), Bositra, Terquemia, Placunopsis, Entolium (Entolium), Chlamys (Chlamys), Chlamys (Copeipecten) subgen. nov., Pseudopecten (Pseudopecten), Camptonectes (Gandalfus) subgen. nov., Eopecten, Harpax, Atreta, Liostrea, Gryphaea (Gryphaea), including G. (G.) lavernockensis sp. nov., Gryphaea (Bilobissa), Nanogyra, Parainoceramya, Semuridia, Anningella, Pteria, Cuneigervillia, Gervillella, Gervillia (Gervillia), Gervillia (Cultriopsis) and Pinna (Pinna). Semuridia and Anningella are placed in the new proposed family Anningellidae.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"13 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-01-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128416099","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"THE OSTEOLOGY OF DIMORPHODON MACRONYX, A NON-PTERODACTYLOID PTEROSAUR FROM THE LOWER JURASSIC OF DORSET, ENGLAND","authors":"Sarah Sangster","doi":"10.1080/02693445.2021.2037868","DOIUrl":"https://doi.org/10.1080/02693445.2021.2037868","url":null,"abstract":"ABSTRACT Dimorphodon macronyx (Buckland, 1829) is one of the earliest known Jurassic pterosaurs and the first English pterosaur to have been formally described; the original specimens from the London Natural History Museum have not been fully reviewed since Richard Owen’s monograph of 1870. This monograph provides a detailed, comparative osteological description and emended diagnosis of D. macronyx, based primarily on the four key London and British Geological Survey specimens, and supplemented by the other known skeletal material. Previously undescribed palatal bones uncovered in one of the Natural History Museum specimens (NHMUK 41212) in 2002 are also described and a tentative reconstruction of the palate presented. A short review of previous phylogenetic studies on the taxonomic status of D. macronyx is provided.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"6 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129523369","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"BRITISH SILURIAN STROMATOPOROIDS. FAUNAS, PALAEOBIOLOGY, AND PALAEOGEOGRAPHICAL SIGNIFICANCE","authors":"S. Kershaw, A. Christine, Da Silva, C. Sendino","doi":"10.1080/02693445.2021.2027157","DOIUrl":"https://doi.org/10.1080/02693445.2021.2027157","url":null,"abstract":"ABSTRACT Recommended reference to this publication: Kershaw, S., Da Silva, A.-C. & Sendino, C. 2021. British Silurian stromatoporoids. Fauna, palaeobiology, and palaeogeographical significance. Monograph of the Palaeontographical Society, London: 1-92; pls 1-22. (Publ. No. 660, part of Vol. 175 for 2021.) British Silurian stromatoporoids occur in carbonate rocks, mostly in the Wenlock Series, together with a small number in the Llandovery Series and very few in the Ludlow Series. Using field and museum material (408 samples) and literature, this study identifies 15 stromatoporoid genera, doubling the previously known generic diversity, so the British Isles holds the third highest genera-diversity Wenlock assemblage after Gotland/Estonia (23 genera) and the Siberian Platform (20 genera). Remarkably, nearly all samples come from the small (100 × 100 km) Much Wenlock Limestone Formation (MWLF) (Homerian Stage, uppermost Wenlock Series) in the Midland Platform of central England (Avalonia), surrounded, underlain, and overlain by siliciclastics. On the Midland Platform one sample is Llandovery age; 11 samples are Ludlow age (Aymestry Limestone). Other samples from the Isle of Man (Wenlock age, six samples) and south-west Scotland (Llandovery age, three samples) are in transported material, with associated corals and they indicate unpreserved carbonate platforms in northern Britain. A few Llandovery Series stromatoporoids are also reported from Ireland, both north and south of the Iapetus Suture; published reports of Wenlock stromatoporoids from Ireland are shown to be misidentified trace fossils. In the MWLF stromatoporoids (together with the more abundant rugose corals, tabulates, heliolitids, and some microbial carbonates) occur in small patch reefs and in bedded bioclastic grainstones, packstones, and nodular wackestones; stromatoporoids are more common in and near patch reefs. The MWLF stromatoporoid fauna has 15 confirmed low-level taxa: Labechia conferta (Lc), Lophiostroma schmidti (Ls), Ecclimadictyon macrotuberculatum (Em) and E. astrolaxum (Ea), Petridiostroma simplex (Ps) and P. linnarssoni (Pl), Actinostromella vaiverensis (Av), Araneosustroma fistulosum (Af), Densastroma pexisum (Dp), Plectostroma intertextum (Pi), Simplexodictyon yavorskyi (Sy), Eostromatopora impexa (Ei), ‘Stromatopora’ venukovi (‘S’v), Syringostromella borealis (Sb) and Parallelostroma typicum (Pt). No new taxa were found. The five most abundant taxa (Lc, Av, Dp, Px, and Sb) total 230 specimens, 64.2% of the MWLF assemblage, consistent with taxa proportions in other Palaeozoic stromatoporoid assemblages. The stromatoporoids have limited growth forms: Lc grew laminar frames, mostly in patch reefs; the other taxa range from laminar to high domical, maximum sizes around 40 cm basal diameter. They almost completely lack the complexities and diversities of form of their contemporaries in nearby large carbonate platforms of Baltica (Gotland/Estonia) and Laurentia (eastern USA","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"20 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-05-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124287551","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"THE BRITISH DEVONIAN CRINOIDEA. PART 2","authors":"S. Donovan, F. E. Fearnhead","doi":"10.1080/02693445.2020.1853380","DOIUrl":"https://doi.org/10.1080/02693445.2020.1853380","url":null,"abstract":"The Palaeontographical Society issues an annual volume of serially numbered publications; these may either be a single complete monograph or part of a continuing monograph.Publication 658, issued a...","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"4 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121412932","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Ostracoda from the Turonian of South-East England Part 2. Cytherocopina","authors":"I. Slipper","doi":"10.1080/02693445.2020.1782044","DOIUrl":"https://doi.org/10.1080/02693445.2020.1782044","url":null,"abstract":"ABSTRACT Part 2 is concerned with the Order Podocopida, Suborder Cytherocopina, Superfamily Cytheroidea. The stratigraphic occurrence has been determined by examining 2096 specimens, assigned to 74 species-group taxa arranged in 31 genera. Of these, 40 are referred to previously described taxa, nine species and six subspecies are here described as new, one nomen novum is erected, while 17 taxa are left in open nomenclature, 11 of which are compared to previously described taxa. The Lower Turonian shows a pattern of rapidly increasing richness from 20 to 36 species, followed by periods of stasis and gradually increasing standing richness in the Middle Turonian, rising up to a maximum of 76 species in the Upper Turonian. The platycopid signal hypothesis is rejected as an explanation for the high abundances of cytherellids in the Lower Turonian and isolated younger marls in favour of a more complex solution involving oxygenation, oligotrophy, water depth changes, and diagenetic alteration. Examples of evolutionary patterns are given to demonstrate four cases of loss of ornamentation and one of increase in ornamentation.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"30 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-02-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114637416","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"The Mammals of the Late Eocene – Early Oligocene Solent Group","authors":"J. Hooker","doi":"10.1080/02693445.2021.1928440","DOIUrl":"https://doi.org/10.1080/02693445.2021.1928440","url":null,"abstract":"ABSTRACT Part 1 begins a systematic account of the mammals from the British Solent Group. Their previous study is summarised. The stratigraphy is reviewed and lithostratigraphic logs are provided for the mammal-bearing localities. The new Fort Victoria Member replaces the previous restricted use Cliff End Member in the Headon Hill Formation. Seventeen species-group taxa of the placental euarchontan family Nyctitheriidae are described, with the new genera Actinyctia and Cheilonyctia and the new species Amphidozotherium gassoni, Actinyctia bulbodens, Cheilonyctia lawsoni, Scraeva yulei, Euronyctia curranti and E. plesiolambda. The occurrence of Saturninia mamertensis near the base of the Headon Hill Formation extends its range from the Bartonian to early Priabonian. The occurrence of Oligonyctia hoffmani in the Bembridge Limestone Formation and lower Hamstead Member extends its range from the early Rupelian to the late Priabonian. A phylogenetic analysis of European Bartonian–Rupelian Nyctitheriidae results in an expanded subfamily Amphidozotheriinae and a new subfamily Saturniniinae for Saturninia (s.s.), Cryptotopos and Oligonyctia. Cryptotopos communis and Euronyctia recta from the German Oligocene are transferred to the genus Paradoxonycteris, whilst Sigenyctia (type species S. oligocaena) is synonymised with the genus Euronyctia. Saturninia mamertensis and S. grandis are shown not to be members of this genus. Euronyctia curranti, E. plesiolambda and E. oligocaena form a stratigraphical morphocline, suggestive of an evolutionary sequence. A phylogenetic analysis of primitive eutherians confirms Nyctitheriidae as stem members of the superorder Euarchonta, supporting an earlier analysis. Aspects of evolution, faunal turnovers and diversity of locomotor adaptations during deposition of the Solent Group are discussed.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"187 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-01-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131490316","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"The Ammonoidea of the Upper Chalk. Part 2","authors":"W. Kennedy","doi":"10.1080/02693445.2020.1759932","DOIUrl":"https://doi.org/10.1080/02693445.2020.1759932","url":null,"abstract":"ABSTRACT A total of 40 species, assigned to 17 genera, belonging to the Suborder Ancyloceratina are described. One species is new. Sixteen are from the Upper Turonian, nine from the Lower Campanian, and 15 from the Upper Campanian. Eight types of aptychi are described.","PeriodicalId":134015,"journal":{"name":"Monographs of the Palaeontographical Society","volume":"53 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2020-01-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133243474","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}