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paleurafrica origin of the european modern faunas through palaeogene central africa collections menu the project partners & sponsors the team members collaborators laboratories labo rbins labo rmca labo ughent labo unamur labo duke lemur center labo ohio university expeditions democratic republic of congo 2014 india 2015 india 2016 democratic republic of congo 2016 results publications posted on july 2018 plesiadapid mammals from the latest paleocene of france offer new insights on the evolution of plesiadapis during the paleocene-eocene transition plesiadapidae are among the most successful mammal families of the paleocene, but in north america they disappear abruptly around the paleocene-eocene boundary. in contrast, in europe, they survive a few million years into the eocene, although only as the genus platychoerops . the latest paleocene deposits of petit-patis (paris basin, france) have produced three new plesiadapid species, one of each genus known in europe: plesiadapis ploegi , sp. nov., platychoerops boyeri , sp. nov., and chiromyoides mauberti , sp. nov. each of these new species is represented by the very characteristic upper incisor, thus ascertaining their concomitant presence and in particular the spatial and temporal coexistence of plesiadapis and platychoerops . plesiadapis ploegi , sp. nov., is morphologically intermediate between plesiadapis tricuspidens and platychoerops russelli , with a tricuspid i1 typical of plesiadapis and a semimolariform p4 closer to platychoerops . its relatively high morphological variability is illustrated. platychoerops boyeri , sp. nov., has the simple derived i1 of all platychoerops and a p4 slightly more molariform than that of ples. ploegi . phylogeny of plesiadapids, including the three new species and their dentition. skeleton of plesiadapis chiromyoides mauberti , sp. nov., is closest to chiromyoides campanicus , but it is smaller and has a particular i1 with multiple posterocones. the systematic position of ‘ platychoerops ’ georgei is discussed; this taxon is considered a chimera, and its type i1 belongs to either chiromyoides or plesiadapis . cladistic analysis highlights the paraphyly or polyphyly of all genera of plesiadapidae. finally, there is some indication of morphological convergences between european and north american plesiadapids, which may be the result of similar environmental changes on both continents just before the paleocene-eocene boundary. this study was published in journal of vertebrate paleontology (de bast et al, 2018). go to top posted on july 2018 a fossil gekkotan (squamata) from the late oligocene nsungwe formation, rukwa rift basin, tanzania we describe the first record of a fossil gekkotan from the late oligocene nsungwe formation in the rukwa rift basin, tanzania. the specimen consists of an almost complete maxilla containing 23 tooth positions, with 10 teeth still in place. typical gekkotan features include the tall facial process along with a posteriorly sloping angle, and the presence of unicuspid, pleurodont teeth with large resorption pits. limited preservation does not allow for a more specific systematic assignment, which is why we refer the specimen to gekkota incertae sedis. the material represents the second record of a paleogene gekkotan from africa and the first one from the central part of the continent. this study was published in journal of herpetology (müller et al, 2018). specimen photograph and locality map. (a) rrbp 13002, gekkotan right maxilla in lateral view and (b) in medial view (scale bar = 1 mm); (c) map showing the nsungwe formation within the rukwa rift basin (tanzania) and the collection locality, including its relative position within tanzania go to top posted on june 2018 morphological diversification of ampullariid gastropods (nsungwe formation, late oligocene, rukwa rift basin, tanzania) is coincident with onset of east african rifting a new freshwater gastropod fauna is described from the late oligocene nsungwe formation of the rukwa rift basin, tanzania. six new species of ampullariids are established including five species of lanistes ( l. microovum , l. nsungwensis , l. rukwaensis , l. songwellipticus and l. songweovum ) and one species of carnevalea ( c. santiapillaii ). these taxa occupy a morphospace region comparable to nearly half of extant lanistes , a common and widespread genus in africa and madagascar. palaeoecological evidence indicates that nsungwe ampullariids inhabited fluvial, pond and paludal environments. among these species are the oldest high-spired and fluvially adapated lanistes taxa. we suggest that nsungwe lanistes rapidly diversified in concert with habitat heterogeneity associated with the initiation of rifting along the western branch of the east african rift system (ears). taxonomy, evolution and the biogeographical affinities of nsungwe formation freshwater gastropods contributes significantly to expanding the undersampled palaeogene invertebrate fossil record of continental africa. this study was published in the journal papers in palaeontology (epa et al, 2018). depressed lanistes morphotypes. a–d, l. nsungwensis sp. nov.; e, l. carinatus (olivier, 1804), ansp 367298-11; f–q, l. rukwaensis sp. nov. scale bars represent 10 mm. go to top posted on june 2018 geology, biostratigraphy and carbon isotope chemostratigraphy of the palaeogene fossil-bearing dakhla sections, southwestern moroccan sahara new palaeogene vertebrate localities were recently reported in the southern dakhla area (southwestern morocco). the eocene sediment strata crops out on cliffs along the atlantic ocean coast. vertebrate remains come from five conglomeratic sandstone beds and are principally represented by isolated teeth belonging to micromammals, selachians and bony fishes, a proboscidean assigned to ? numidotherium sp. and many remains of archaeocete whales (basilosauridae). from fieldwork five lithostratigraphic sections were described, essentially based on the lithological characteristic of sediments. carbon isotope values (‰ vpdb) of the porto rico and el argoub sections, compared to δ13c curves around the eocene–oligocene transition at odp site 1218 (erhardt, pälike & paytan, 2013) and reference δ13c composite curve (cramer et al. 2009; modified by vandenberghe, hilgen & speijer, 2012). eot – eocene–oligocene transition; u1–u5 – lithological units defined in the text; b1, b2, c1, c2 – fossil-bearing levels despite the lateral variations of facies, correlations between these five sections were possible on the basis of fossil-bearing beds (a1, b1, b2, c1 and c2) and five lithological units were identified. the lower part of the section consists of rhythmically bedded, chert-rich marine siltstones and marls with thin black phosphorite with organic matter at the base. the overlying units include coarse-grained to microconglomeratic sandstones interbedded with silts, indicating deposition in a shallow-marine environment with fluvial influence. the natural remanence magnetization of a total of 50 samples was measured; the intensity of most of the samples is too weak however, before or after the first step of demagnetization. the palaeomagnetic data from the samples are very unstable, except for eight from three similar sandstone levels which show a normal polarity. matched with biostratigraphic data on rodents, primates, the selachian, sirenian and cetacean faunas, the new carbon isotope chemostratigraphy on organics (1) refines the age of the uppermost c2 fossil-bearing bed to earliest oligocene time and (2) confirms the priabonian age of the b1 to c1 levels. this study was published in the journal geological magazine (benammi et al, 2017). go to top posted on june 2018 the first hyaenodont from the late oligocene nsungwe formation of tanzania: paleoecological insights into the paleogene-neogene carnivore transition throughout the paleogene, most terrestrial carnivore niches in afro-arabia were occupied by hyaenodo

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Domain: paleurafrica.be
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