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Inproceedings Reference Neogene and Quaternary fossil remains of beaked whales (Cetacea, Odontoceti, Ziphiidae) from deep-sea deposits off Crozet and Kerguelen Islands
Located in Library / RBINS Staff Publications 2019
Article Reference Neolithic pottery finds at the wetland site of Bazel-Kruibeke (Flanders, Belgium): evidence of long-distance forager-farmer contact during the late 6th and 5th millennium cal BC in the Rhine-Meuse-Scheldt area
Located in Library / RBINS Staff Publications
Article Reference Octet Stream Neolithic woodland management and land-use in south-eastern Europe: The anthracological evidence from Northern Greece and Bulgaria
Wood charcoal (anthracological) remains accumulated in archaeological deposits provide a valuable tool for reconstruction of past local vegetation and its use. They can offer evidence complementary to pollen analysis or be the main source on past vegetation change in areas where no pollen preservation is available. The current study assembles the anthracological evidence from 18 Neolithic sites situated in the zone spanning between the Lower Danube plain and the Aegean coast. This evidence is presented within the broader archaeological and paleoecological context of the region and in cal. years BC and/or BP. The data is interpreted in terms of land-use related to woodland management and exploitation of woodland resources during three chronological phases which could be distinguished within the Neolithic of south-eastern Europe: a) 6500-5800 cal. BC, b) 5800-5500 cal. BC, and c) 5500-4900 cal BC). The main vegetation type targeted by the Neolithic population were the thermophilous, mixed deciduous oak communities, which contained a rich and diverse undergrowth of light-demanding and fruit/nut bearing trees, shrubs and herbs. Those plant communities were the major source of fuel wood, forest pasture, fodder, gathered fruits, etc. The analyses indicate stability and sustainability of the firewood procurement and woodland management practices for the whole considered period and further suggest that the Neolithic land-use strategies favoured the rich and often fruit-bearing undergrowth of the oak forests and woodland.
Located in Library / RBINS Staff Publications 2018
Article Reference Neotype of Pseudagrion approximans Selys, 1876 designated to resolve a nomenclatorial confusion in the genus Aciagion Selys, 1891 (Odonata: Coenagrionidae)
Located in Library / RBINS Staff Publications
Article Reference Nest relocation and high mortality rate in a Neotropical social wasp: impact of an exceptionally rainy La Niña year / Migration et fort taux de mortalité chez une guêpe Néotropicale: conséquence de pluies exceptionnelles durant une année La Niña.
Located in Library / RBINS Staff Publications
Article Reference Nested clade analysis in non-marine ostracods with asexual reproduction
Located in Library / RBINS Staff Publications
Article Reference Nestedness in sessile and periphytic rotifer communities: A meta-analysis.
Located in Library / RBINS Staff Publications
Article Reference Net ecosystem production and carbon dioxide fluxes in the Scheldt estuarine plume
Located in Library / RBINS Staff Publications
Article Reference New amphisbaenian lizards from the Early Paleogene of Europe and their implications for the early evolution of modern amphisbaenians
Three new amphisbaenian lizard taxa are described from the Early Paleogene of Western Europe. Two new basal forms, Polyodontobaena belgica gen. et sp. nov. from the Early Paleocene of Hainin (Belgium) and Camptognathosaurus parisiensis gen. et sp. nov. from the Late Paleocene of Rivecourt-Patit Pâtis and Cernay-lès-Reims (France), are characterised by a dentary lacking a strong angle at the symphysis and bearing 10 to 12 massively built and conical teeth. These two taxa form the new family Polyodontobaenidae. A third new amphisbaenian, Blanosaurus primeocaenus gen. et sp. nov., is also described from the Early Eocene of Dormaal (Belgium), Condé-en-Brie and Prémontré (France) and represents the oldest modern amphisbaenian lizard of Europe, tentatively assigned to Blanidae. It is characterised by a reduction of tooth number and by the presence of a strong angle at the symphysis. Palaeobiogeographic considerations suggest a first hypothesis that the Eocene forms would have evolved from the Paleocene species.The second hypothesis would be that as for the lizard Scincoideus haininensis, primitive amphisbaenians were present in Europe from the Paleocene,whereasbeginning in the Early Eocene only modern forms with typical reduced dentition (fewer than 10 teeth) are present. The origin of these modern forms is very likely related with the dispersal of the first modern mammals.
Located in Library / RBINS Staff Publications
Article Reference New and interesting records of Diptera on glacial sand deposits in Silesia (NE Czech Republic). Part 2 – Brachycera except for Schizophora
Located in Library / RBINS Staff Publications 2021 OA