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Article Reference Biofluorescence of the Crocodile Skinks, genus Tribolonotus: first report in Scincidae
Biofluorescence, the phenomenon where organisms absorb short wavelengths of light and re-emit longer wavelengths, has been documented in various reptile and amphibian groups. This study reports the first observation of UV-induced biofluorescence in the genus Tribolonotus (crocodile skinks), marking the first such report for the family Scincidae. Specimens of Tribolonotus novaeguineae, T. brongersmai, and T. gracilis were examined under UV light, revealing distinct fluorescence patterns. The fluorescence is primarily bone-induced, linked to the presence of osteoderms, although some skin-based fluorescence was also observed, particularly around the eyes. The study suggests potential ecological roles for this fluorescence, such as intraspecific signaling or predator-prey interactions, and highlights the need for further research to understand the functional significance of biofluorescence in these skinks.
Located in Library / RBINS Staff Publications 2024
Article Reference Biofluorescence in Morelia, Malayopython and Python: first reports for the Pythonidae
Ultraviolet (UV) induced biofluorescence in snakes has been underexplored compared to lizards. This study reports for the first time UV fluorescence in several Pythonidae species, including Morelia viridis, Malayopython reticulatus, and Python regius. Specimens were examined under both white and UV light, revealing that UV fluorescence in these snakes is likely skin-based, induced by chemical compounds rather than bone-based as seen in other reptiles. Notably, Morelia viridis and M. azurea exhibited a golden mustard yellow fluorescence, while Malayopython reticulatus displayed a complex pattern with intense yellow fluorescence. The study also found that UV fluorescence is absent in ethanol-preserved specimens, suggesting the degradation of fluorescent compounds during preservation. These findings contribute to the understanding of UV fluorescence in snakes and highlight the need for further research on its functional significance and the specific molecules involved.
Located in Library / RBINS Staff Publications 2024
Article Reference Description of a new species of the genus Anomophysis Quentin & Villiers, 1981 from Wetar Island (Contribution to the knowledge of Indonesian Prioninae-2) (Coleoptera, Cerambycidae, Prioninae)
Located in Library / RBINS Staff Publications 2024
Article Reference Illustrated and commented checklist of the longhorn beetles of Kuzikus Wildlife Reserve in the Kalahari, Namibia (Coleoptera: Cerambycidae)
Located in Library / RBINS Staff Publications 2023
Article Reference Calicnemis latreillei Laporte, 1832 (Coleoptera, Scarabaeidae, Dynastinae), a new host for the Tachinid fly Microphthalma europaea Egger, 1860
Located in Library / RBINS Staff Publications 2024
Article Reference A redescription of the Neotropical lanternfly Coptopola cincticrus Stål, 1869 (Fulgoridae: Poiocerinae: Poiocerini)
Located in Library / RBINS Staff Publications 2024
Article Reference Endocranial anatomy and phylogenetic position of the crocodylian Eosuchus lerichei from the late Paleocene of northwestern Europe and potential adaptations for transoceanic dispersal in gavialoids
Eosuchus lerichei is a gavialoid crocodylian from late Paleocene marine deposits of northwestern Europe, known from a skull and lower jaws, as well as postcrania. Its sister taxon relationship with the approximately contemporaneous species Eosuchus minor from the east coast of the USA has been explained through transoceanic dispersal, indicating a capability for salt excretion that is absent in extant gavialoids. However, there is currently no anatomical evidence to support marine adaptation in extinct gavialoids. Furthermore, the placement of Eosuchus within Gavialoidea is labile, with some analyses supporting affinities with the Late Cretaceous to early Paleogene “thoracosaurs.” Here we present novel data on the internal and external anatomy of the skull of E. lerichei that enables a revised diagnosis, with 6 autapormorphies identified for the genus and 10 features that enable differentiation of the species from Eosuchus minor. Our phylogenetic analyses recover Eosuchus as an early diverging gavialid gavialoid that is not part of the “thoracosaur” group. In addition to thickened semi-circular canal walls of the endosseous labyrinth and paratympanic sinus reduction, we identify potential osteological correlates for salt glands in the internal surface of the prefrontal and lacrimal bones of E. lerichei. These salt glands potentially provide anatomical evidence for the capability of transoceanic dispersal within Eosuchus, and we also identify them in the Late Cretaceous “thoracosaur” Portugalosuchus. Given that the earliest diverging and stratigraphically oldest gavialoids either have evidence for a nasal salt gland and/or have been recovered from marine deposits, this suggests the capacity for salt excretion might be ancestral for Gavialoidea. Mapping osteological and geological evidence for marine adaptation onto a phylogeny indicates that there was probably more than one independent loss/reduction in the capacity for salt excretion in gavialoids.
Located in Library / RBINS Staff Publications 2024 OA
Article Reference Timing of intercontinental faunal migrations: Anguimorph lizards from the earliest Eocene (MP 7) of Dormaal, Belgium
Here we report on anguimorph lizards from the earliest Eocene (MP 7) of the Dormaal locality in Belgium, from the time of the warmest global climate of the past 66 million years. Several clades can be identified in this site: Glyptosauridae, Varanidae, and Palaeovaranidae. Our study focuses on glyptosaurid specimens previously reported from the site, some of which had been provisionally described as a new species,?Placosaurus ragei, and some assigned to an unnamed Placosauriops-like ‘melanosaurine’. Our study presents data on new material, including an almost complete glyptosaurine frontal that has enabled us to assign much of the previously described material to a single genus and species. The specimens that had been assigned to both ?P ragei and the ‘melanosaurine’ share apomorphies (flat osteoderms and chevron-shaped osteoderms) with Gaultia, a glyptosaurid previously known from the earliest Eocene of Wyoming, USA. The Dormaal material represents the first record of this genus outside North America. In fact, the only potential evidence of the occurrence of ‘Melanosaurinae’ in Dormaal might be a single isolated vertebra described here. Here we also describe previously unfigured material of Saniwa and palaeovaranids from Dormaal. The presence of previously reported helodermatids cannot be supported in this Belgian site.
Located in Library / RBINS Staff Publications 2024 OA
Inproceedings Reference PerissOrigin : phylogénie et diversification des premiers périssodactyles
Les premiers vrais périssodactyles sont reconnus presque simultanément dès le tout début de l’Eocène en Europe de l'Ouest, en Asie et en Amérique du Nord, et semblent pourtant déjà appartenir à des familles distinctes (Smith et al. 2015 ; Bai et al. 2018). Cette apparente diversité pose donc question sur l’origine paléobiogéographique et phylogénétique de ces groupes, qui reste très débattue. En effet, le plus proche parent des périssodactyles reste encore incertain, bien que deux groupes-frères potentiels semblent aujourd’hui majoritairement acceptés : les périssodactyles pourraient soit être proches de certains Phenacodontidae nord-américains (Halliday et al. 2017), ou plutôt groupe-frère des Anthracobunia du sous-continent indien (Rose et al. 2019). Le projet PerissOrigin a pour but de mieux comprendre les premières dichotomies des périssodactyles anciens ainsi que leur origine paléobiogéographique. Grâce à l'une des plus complètes collections de moulages de périssodactyles anciens et à des spécimens inédits, une nouvelle matrice de caractères morphologiques a été compilée, comprenant actuellement une centaine de caractères cranio-dentaires pour 80 terminaux. Certains taxons européens ont pu être réévalués, et une nouvelle phylogénie des premiers périssodactyles sera présentée. Plusieurs méthodes et paramètres d'analyse phylogénétique (choix de l'extra-groupe, parcimonie ordonnée/non ordonnée, choix des caractères, polymorphisme, pondération...) seront comparés et leur impact sera discuté. Cette nouvelle phylogénie nous permet de définir quelques synapomorphies des grands groupes de périssodactyles et d'aborder une première discussion paléobiogéographique. Nous discuterons enfin des problèmes non résolus dans la phylogénie des périssodactyles. Le projet "PERISSORIGIN - Origin and early radiation of perissodactyls based on precious fossil collections" est financé par le programme de recherche BRAIN-be 2.0 de BELSPO.
Located in Library / RBINS Staff Publications 2024 OA
Inproceedings Reference Les lézard anguimorphes de l’Eocène inférieur (MP7) de Dormaal, Belgique
Depuis quelques années, les lézards de l’Eocène basal de Dormaal (niveau-repère MP7), Belgique sont en cours de révision. Après le varanidé Saniwa orsmaelensis (Augé et al., 2022), les geckos (Čerňanský et al., 2022) et les lézards Iguania (Čerňanský et al., 2023), le restant des Anguimorpha vient de faire l’objet d’une étude approfondie (Čerňanský et al., in press). Cette dernière met en évidence la présence d’au moins trois familles sur ce site : les Glyptosauridae, les Varanidae et les Palaeovaranidae. Les Glyptosauridae (contenant les glyptosaurinés et les mélanosaurinés) étaient identifiés dans la littérature au travers de ?Placosaurus ragei et d’un mélanosaure. Le matériel original de ?P. ragei est un dentaire isolé ainsi qu’un pariétal. Or, la taxonomie actuelle des espèces du genre Placosaurus est uniquement basée sur la morphologie du frontal. La mise en évidence d’un frontal de glyptosaure à Dormaal permet donc de discuter l’identification de ?P. ragei et d’attribuer ces éléments au genre Gaultia, un glyptosaure de l’Eocène inférieur du Wyoming, USA, représentant la première occurrence de ce genre en-dehors de l’Amérique du Nord. Une nouvelle combinaison, Gaultia ragei est donc proposée. La présence de mélanosaures (groupe paraphylétique) n’est pas formellement confirmée. Une vertèbre isolée pourrait appartenir à ce clade mais comme la morphologie des vertèbres de Gaultia est inconnue, des doutes subsistent. Nous décrivons également de nouveaux spécimens attribuables à Saniwa orsmaelensis ainsi qu’à un Palaeovaranidae. Ces taxons mettent à nouveau en évidence les migrations qui ont eu lieu durant le Maximum Thermique Paléocène-Eocène (PETM), climat le plus chaud des 66 derniers millions d'années. Ce travail fut possible grâce au financement SYNTHESYS BE-TAF-8234 de la Commission Européenne (A.Č.), à la bourse 1/0191/21 de l’Agence des Bourses Scientifiques du Ministère de l’Education de Slovaquie et de l’Académie des Sciences de Slovaquie (A.Č.) et
Located in Library / RBINS Staff Publications 2024 OA