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Book Reference A new approach to the evolution of the so-called surface peat in the western coastal plain of Belgium
Located in Library / RBINS Staff Publications
Incollection Reference A new basal hadrosauroid dinosaur from the Late Cretaceous of Kazakhstan
Located in Library / RBINS Staff Publications
Article Reference A new deep sea coralline sponge from Turks & Caicos Islands: Willardia caicosensis gen. et sp. nov. (Demospongiae: Hadromerida). In: Ph. Willenz (Ed.) Recent Advances in Sponge Biodiversity Inventory and Documentation.
Located in Library / RBINS Staff Publications
Article Reference A new genus and species of Cicada from Vietnam: Cochloeopsaltria duffelsi gen. et. sp. nov. (Hemiptera: Cicadomorpha: Cicadidae)
Located in Library / RBINS Staff Publications 2017
Book Reference A new microvertebrate fauna from the Middle Hettangian. (Early Jurassic) of Fontenoille. (Province of Luxembourg, south Belgium)
Deze samenvatting is niet beschikbaar in het Nederlands. Abstract A new microvertebrate fauna from the Middle Hettangian (early Jurassic) of Fontenoille (Province of Luxembourg, south Belgium). A Lower Jurassic horizon from Fontenoille yielding fossil fish remains can be dated to the Middle Hettangian Liasicus zone on the basis of the early belemnite Schwegleria and the ammonite Alsatites laqueus francus. Hybodontiform sharks are represented by Hybodus reticulatus Lissodus sp., Polyacrodus sp, and Neoselachians by Synechodus paludinensis nov. sp. and Synechodus streitzi, nov. sp. Earlier reports of a scyliorhinid are not confirmed: teeth of similar morphology to scyliorhinids seem to be juvenile variants of S. paludinensis. Chimaeriform remains include Squaloraja sp., the earliest occurrence of the genus. The Actinopterygian fauna is introduced, comprising a palaeonisciform cf. Ptycholepis, a possible late perleidiform cf. Platysiagum, the dapediid semionotiforms Dapedium and cf. Tetragonolepis, the pycnodontiform Eomesodon, halecomorphs cf. Furidae or Ophiopsidae, pholidophoriforms and/or Leptolepididae, and actinistians. Lepidosaur remains are also present. Résumé Une nouvelle faune de microvertébrés de l'Hettangien moyen (Jurassique inférieur) de Fontenoille (Province de Luxembourg, Belgique méridionale). Le gisement hettangien de Fontenoille a fourni les bélemnites précoces Schwegleria et l'ammonite Alsatites laqueus francus, permettant de l'attribuer à la zone à Liasicus de l'Hettangien moyen. Les Hybodontiformes sont représentés par Hybodus cf. reticulatus, Lissodus sp, Polyacrodus sp, les Néosélaciens Synechodus paludinensis nov. sp. et Synechodus streitzi nov. sp. ; les Scyliorhinidae originellement signalés ne sont pas confirmés, mais on considère la morphologie scyliorhinide comme une variante juvénile possible de l'espèce S. paludinensis. Les chimères sont également présentes avec Squaloraja sp, l'occurrence la plus ancienne du genre. La faune d'Actinoptérygiens est brièvement présentée, comprenant un palaeonisciforme cf. Ptycholepis, un possible perléidiforme tardif cf. Platysiagum, des sémionotiformes Dapediidae Dapedium et cf. Tetragonolepis, le pycnodontiforme Eomesodon, des Halecomorphi cf. Furidae ou Ophiopsidae, des pholidophoriformes et/ou des Leptolepididae, ainsi qu' un Actinistia. On relève également la présence d'un reptile lépidosaure.
Located in Library / RBINS Staff Publications
Article Reference A new Pentatomidae for the fauna of Namibia: Kundelungua meridionalis (Heteroptera, Pentatomidae, Podopinae)
Located in Library / RBINS Staff Publications
Article Reference A new species of Archaeoryctes from the Middle Paleocene of China and the phylogenetic diversification of Didymoconidae
Didymoconidae are an enigmatic group of Asian endemic insectivorous mammals. We describe the new didymoconid species Archaeoryctes wangi sp. nov. from the Upper Member of the Wanghudun Formation (Middle Paleocene). This new species from the Qianshan Basin (Anhui Province, China) forms an interesting geographical intermediate between A. notialis from South China and A. borealis and A. euryalis from the Mongolian Plateau. To better understand the origin and evolutionary diversification of Didymoconidae, we performed a cladistic and stratocladistic study of the Didymoconidae and various outgroups. This study of dental material did not resolve the higher level affinities of Didymoconidae, but confirms the validity of the family and its distinctiveness from the morphologically similar Sarcodontidae. Moreover, our results corroborate the current didymoconid classification with the distinction of three subfamilies: “Ardynictinae”, Kennatheriinae and Didymoconinae; “Ardynictinae” are a paraphyletic stemgroup for the two other subfamilies. Our results suggest three distinct didymoconid radiations: (1) primitive ardynictines appeared in South China from the start of the Nongshanian; their evolution continues on the Mongolian Plateau with (2) the radiation of more evolved ardynictines and kennatheriines at the start of the Middle Eocene Arshantan and (3) the origin of didymoconines at the start of the Late Eocene Ergilian.
Located in Library / RBINS Staff Publications
Article Reference A new species of Bardunia Stal, 1863 extends the distribution of the genus to the Philippines (Hemiptera: Fulgoromorpha: Issidae)
Located in Library / RBINS Staff Publications 2018
Article Reference A new species of Drapetis Meigen from calcareous grassland in southern Netherlands (Diptera, Hybotidae, Tachydromiinae)
Located in Library / RBINS Staff Publications 2020
Article Reference A new species of Kriptobaatar (Multituberculata): the first Late Cretaceous mammal from Inner Mongolia (P.R. China)
Multituberculates are the best represented mammals of the Late Cretaceous in Asia and most of them are from Outer Mongolia. The djadochtatherioidean multituberculate Kr)ptobaut~im- andihuensis n. sp. is described on the basis of two skulls froin the Upper Cretaccous localiiy of Bayan Mandaliu (Inner Mongolia, People's Republic of China). The main characters that differentiate it from tlie type species K. dashzevegi Kielan-Jaworowska, 1970 are: the base of the zygomatic arch situated at the level of tlie anterior root of the P4 and the narrow anterior extent of the orbit, the "V" shape of the palatoinaxillary suture between the tlvo major palatine fonmina, the high and thick part of the dentary under the mandibular diastema. the long and low part of the dentary iinder the mandibular notch, the anteroposteriorly short coronoid process. the presence of 5 cusps on the middle row of Ml and on the labial row of ml, the long p4. the Iiigh ratio p4:ml length, and the robust il. The presence of this species in lnner Mongolia extends the palacogeographical distribution area of the djadochtatherioideans to the soutliern part of the Gobi Basin. Neveiiheless, morphological differences between K. tnandahitensis from lnner Mongolia and K. dushzevegi from Outer Mongolia suggest a palaeogeographical isolation within the Djadochtatherioidea group during the Campanian.
Located in Library / RBINS Staff Publications