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Article Reference Sample basedwater quality monitoring of coastal seas: How significant is the information loss in patchy time series compared to continuous ones?
Located in Library / RBINS Staff Publications 2023
Article Reference A dynamic 2DH flocculation model for coastal domains
Located in Library / RBINS Staff Publications 2023
Article Reference Coastal wetland adaptability to sea level rise: The neglected role of semi-diurnal vs. diurnal tides
Located in Library / RBINS Staff Publications 2023
Article Reference Limits of calcium isotopes diagenesis in fossil bone and enamel
Diagenesis has been recognized for decades to significantly alter the trace elements biogenic signatures in fossil tooth enamel and bone that are routinely used for paleobiological and paleoenvironmental reconstructions. This signature is modified during diagenesis according to a complex continuum between two main processes, addition and substitution. For an additive-like, or early diagenesis, the trace elements biogenic profiles can be restored by leaching secondary minerals, but this technique is inefficient for a substitutive-like, or extensive diagenesis for which secondary trace elements are incorporated into the biogenic mineral. This scheme is however unclear for Ca, the major cation in tooth enamel and bone hydroxylapatite, whose stable isotope composition (δ44/42Ca) also conveys biological and environmental information. We present a suite of leaching experiments for monitoring δ44/42Ca values in artificial and natural fossil enamel and bone from different settings. The results show that enamel δ44/42Ca values are insensitive to an additive-like diagenesis that involves the formation of secondary Ca- carbonate mineral phases, while bone shows a consistent offset toward 44Ca-enriched values, that can be restored to the biogenic baseline by a leaching procedure. In the context of a substitutive-like diagenesis, bone exhibits constant δ44/42Ca values, insensitive to leaching, and shows a REE pattern symptomatic of extensive diagenesis. Such a REE pattern can be observed in fossil enamel for which δ44/42Ca values are still fluctuating and follow a trophic pattern. We conclude that Ca isotopes in fossil enamel are probably not prone to extensive diagenesis and argue that this immunity is due to the very low porosity of enamel that cannot accommodate enough secondary minerals to significantly modify the isotopic composition of the enamel Ca pool.
Located in Library / RBINS Staff Publications 2023
Article Reference SARS-CoV-2 Infection in Captive Hippos (Hippopotamus amphibius), Belgium
Located in Library / RBINS Staff Publications 2023 OA
Article Reference Subspecific rodent taxa as the relevant host taxonomic level for mammarenavirus host specificity
Located in Library / RBINS Staff Publications 2023 OA
Article Reference Les glaçures plombifères médiévales mosanes : recettes et expérimentations.
Located in Library / RBINS Staff Publications 2023
Article Reference Une épingle “des palafiittes » du Bronze final (Xième s. av. n.è.), de l’habitat de Pitet (commune de Braives, prov. De Hesbaye liégeoise, Belgique). Nouvel examen.
Located in Library / RBINS Staff Publications 2023
Article Reference Rome à la campagne : les décors en pierre de la villa de la Grande Boussue à Nouvelles (Mons, Belgique).
Located in Library / RBINS Staff Publications 2023
Article Reference La ville de Huy entre eaux et pierres.
Located in Library / RBINS Staff Publications 2023