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Search publications of the members of the Royal Belgian institute of natural Sciences

Book Reference De abdij van Averbode, een verhaal van steen en marmer.
Article Reference Chapitre 3 – L’époque romaine.
In Dossogne M. (dir), Authom N., Collette O., Goemaere E., Guillaume A., Hanut F., Genvier S., Pigière F., Raepsaet-Charlier M.-T. et Yernaux C., 2021. Occupations protohistoriques et gallo-romaines à Péruwelz/Braffe. Les sites de “Couture de Clérivau”, “Grande Ramette” et “Gros Tilleul ». Publication sortie de presse en juin 2022
Booklet Reference Occupations protohistoriques et gallo-romaines à Péruwelz/Braffe. Les sites de “Couture de Clérivau”, “Grande Ramette” et “Gros Tilleul ».
Imprimé en 2022 Etudes et documents, Archéologie, 44, AWaP, 411 p. ISBN 978-2-39038-128-0
Article Reference Ath/Ghislanghien : vestiges protohistoriques dans le parc d’activité économique Orientis III.
Imprimé avril 2022
Article Reference Viroinval/Treignes : campagne de fouilles 2020 à la grotte Genvier.
Imprimé avril 2022, AWaP
Article Reference Geochemical and mineralogical characterisation of vitrified waste material discovered in large quantities on Roman salt production sites along the southern North Sea coast.
Article Reference Mortiers en pierre à Dinant et à Poilvache (Prov. Namur) : exemples mosans d’une production diffusée jusqu’au Danemark en passant par la zone de confluence de la Meuse et du Lek/Rhin ?
Article Reference Mons/Nouvelles : les décors en pierre de la villa de la Grande Boussue.
Inproceedings Reference A peculiar ornamental stone in the civitas Treverorum used in funeral monuments and the antique theatre of Dalheim (Grand-Duchy of Luxembourg).
Inproceedings Reference Red, grey and green marbles in the Civitates Tungrorum and Nerviorum: local and regional resources versus Mediterranean supplies.
Inproceedings Reference De la terre au métal : les approvisionnements d’un atelier du travail du cuivre et de ses alliages à Bruxelles au début du XVe siècle.
Inproceedings Reference Characterization, procurement and transformation of iron-rich raw material during Early Neolithic in Northwestern Europe
Unpublished Reference Etude de roche. Exposition « Autour de Sainte-Gertrude. Les dessous de la Grand Place de Nivelles révélés par l’archéologie »
Article Reference Toxic Peptides in Populations of Two Pergid Sawflies, Potential Biocontrol Agents of Brazilian Peppertree
Inproceedings Reference WATERHYPERNET: Automated in situ measurements of hyperspectral water reflectance for satellite validation ... and more.
Article Reference Fossil bog soils (`dwog horizons') and their relation to Holocene coastal changes in the Jade Weser region, southern North Sea, Germany
After the deceleration of the postglacial marine transgression, the German North Sea coast was subject to deposition of a complex pattern of subtidal to terrestrial facies. This study aims at reconstructing these facies changes in the `Land Wursten' region (Lower Saxony) by focussing on so-called dwog horizons (incipient soil horizons of the pre-engineered salt marshes). We explore their implications for relative sea-level reconstructions and their indication for early settlement activities. Archive drilling data (1960, provided by the `Landesamt für Bergbau, Energie und Geologie') were analysed to create five high-resolution stratigraphic cross sections. Three new drilling records were subjected to sedimentological and microfaunal investigations and interpreted to verify and calibrate the archive data. Two dwog horizons were found and 14C-AMS dated. We found basal salt marsh deposits inundated by a high-energy event and covered by tidal flat sediments. The thick tidal flat unit is again overlain by salt marsh deposits indicating the transition from a shallow marine to a terrestrial environment where dwogs were developed and covered by episodic marine incursions. The ages of the dwogs (1128–969 cal BC; cal AD 1426–1467) do not correlate with known layers of adjacent settlement sites and are critically discussed. However, we show that they correlate with phases of stagnant regional relative sea level (RSL) and can be used as RSL indicators. The combined archive and modern data provide valuable information for the RSL reconstruction and palaeoenvironmental changes. However, further research is recommended to accomplish more detailed information about coastal response during the Holocene sea-level changes and implications for settlement dynamics.
Article Reference Multiple dating approach (14C, 230Th/U and 36Cl) of tsunami-transported reef-top boulders on Bonaire (Leeward Antilles) – Current achievements and challenges
Article Reference Mega-tsunami conglomerates and flank collapses of ocean island volcanoes
Article Reference Chenier-type ridges in Giralia Bay (Exmouth Gulf, Western Australia) - Processes, chronostratigraphy, and significance for recording past tropical cyclones
Article Reference Migration of Barchan Dunes in Qatar–Controls of the Shamal, Teleconnections, Sea-Level Changes and Human Impact
Barchan dune fields are a dominant landscape feature in SE Qatar and a key element of the peninsula’s geodiversity. The migration of barchan dunes is mainly controlled by dune size, wind patterns, vegetation cover and human impact. We investigate the variability of dune migration in Qatar over a time period of 50 years using high-resolution satellite and aerial imagery. We then explore its relation to the regional Shamal wind system, teleconnection patterns, and limitations in sand supply associated with the transgression of the Arabian Gulf. Strong size-dependent differences in migration rates of individual dunes as well as significant decadal variability on a dune-field scale are detected, which are found to correlate with the intensity of the North Atlantic Oscillation (NAO) and the Indian Summer Monsoon (ISM), in particular during years of relatively strong (weak) summer Shamals. High uncertainties associated with the extrapolation of migration rates back into the Holocene, however, do not permit further examination of the timing of the loss of sand supply and the onset of the mid-Holocene relative sea-level (RSL) highstand. For the youngest phase considered in this study (2006–2015), human impact has likely accelerated dune migration under a weakening Shamal regime through sand mining and excessive vehicle traffic upwind of the core study area.
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