Search publications of the members of the Royal Belgian institute of natural Sciences
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Notice explicative de la carte géologique Troisvierges N°1 à 1:25000
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Wibrin-Houffalize 60/3-4.
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Notice explicative de la feuille Wibrin-Houffalize 60/3-4 (carte géologique de Wallonie à l'échelle de 1/25000).
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Note sur la présence de Berginnus tamarisci Wollaston, 1854 en Belgique (Insecta: Coleoptera: Mycetophagidae)
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CT-CEPH: Applying micro-CT imaging in the study of Belgian fossil nautilid cephalopods
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Sclerochronological evidence of pronounced seasonality from the late Pliocene of the southern North Sea Basin, and its implications
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Sclerochronological evidence of pronounced seasonality from the Pliocene of the southern North Sea Basin, and its implication
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Seasonal variability in a warming climate: Lessons from the Pliocene Warm Period and beyond.
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Review of Trictenotomid beetles (Coleoptera: Trictenotomidae) of India and Sri Lanka
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Shallow Suberitida (Porifera, Demospongiae) from Peru
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Megastomia crovatoi Nofroni, Renda & Vannozzi, 2022 (Gastropoda: Pyramidellidae) alive in Bozcaada Island (Aegean Sea - Turkey)
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Environmental and climatic inferences for Marine Isotope Stage 2 of southern Belgium (Meuse valley, Namur Province) based on rodent assemblages
- The environmental and climatic conditions of the Late Pleistocene of Southern Belgium are here determined for the final part of Marine Isotope Stage 3 (MIS 3) and for MIS 2 on the basis of a study of rodent assemblages. This paper provides a synthesis of several sets of environmental and climatic data from Late Pleistocene sites, all of which are located in southern Belgium. One has previously been published (Caverne Marie-Jeanne), and seven are unpublished (Cavernes de Goyet, Trou des Nutons, Trou du Frontal, Trou de Chaleux, Grotte la Chefalize, Trou du Chˆene, and Trou du Sureau). The habitat weighting and quantified ecology methods are applied to rodent material housed in the Royal Belgian Institute of Natural Sciences (RBINS, Brussels), and previous radiocarbon dates are updated, in order to reconstruct past environments. Among all the sites under analysis, the quantified ecology method shows that Trou de Chaleux corresponds to the coldest temperatures and lowest precipitation. Trou de Chaleux, with a chronology between ca. 15,964–14,014 cal yr B.P., could probably be placed in Greenland Stadial 2 (GS2) or Heinrich Event 1 (HE1). It has a rodent assemblage associated with a predominance of open dry and rocky formations, the most abundant species being the collared lemming and the narrow-headed vole. These data are found to coincide with previous studies carried out on the large-mammal, herpetofaunal, and avifaunal associations of the site, as well as on small-mammal associations from other sites in southern Belgium with similar chronology, such as Grotte Walou. Taken together, this indicates that these latest Pleistocene intervals in southern Belgium were characterized by harsh climatic and environmental conditions. In contrast, the other assemblages under study yielded much more heterogeneous results, frequently inconsistent with an attribution to the Pleistocene. This is likely to be a result of their admixture with Holocene material due to recent intrusions.
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Pleistocene hyperostotische visbotten van de stranden van Dishoek en De Banjaard,
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‘Vis en blik’ is nog geen ‘vis in blik’. Een greep uit het leven in de Stützpunkt Flugplatz aan de Zwinmonding
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A Tale of Five Fishes: First direct evidence of trade in Galilean salted fish on the Carmel coast in the early Islamic period
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(Sub-) fossiele faunavondsten en een inventarisatie van mollusken van het strand bij Dishoek afkomstig van één suppletie
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A behavioural framework for the evolution of feeding in predatory aquatic mammals
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Een midden-Romeinse rurale site in de Sigma zone ‘Wijmeers 2’ (gemeente Wichelen, Oost-Vlaanderen)
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Somewhere I belong: phylogeny and morphological evolution in a species-rich lineage of ectoparasitic flatworms infecting cichlid fishes
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A tardigrade in Dominican amber
- Tardigrades are a diverse group of charismatic microscopic invertebrates that are best known for their ability to survive extreme conditions. Despite their long evolutionary history and global distribution in both aquatic and terrestrial environments, the tardigrade fossil record is exceedingly sparse. Molecular clocks estimate that tardigrades diverged from other panarthropod lineages before the Cambrian, but only two definitive crown-group representatives have been described to date, both from Cretaceous fossil deposits in North America. Here, we report a third fossil tardigrade from Miocene age Dominican amber. Paradoryphoribius chronocaribbeus gen. et sp. nov. is the first unambiguous fossil representative of the diverse superfamily Isohypsibioidea, as well as the first tardigrade fossil described from the Cenozoic. We propose that the patchy tardigrade fossil record can be explained by the preferential preservation of these microinvertebrates as amber inclusions, coupled with the scarcity of fossiliferous amber deposits before the Cretaceous.
