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Article Reference Two odd ones: Mediterranean ballast stones and Italian maritime connections in the medieval Bruges’ harbor system.
Excavations in the Bruges’ Medieval outer ports of Hoeke and Monnikerede, located along the Zwin tidal inlet, revealed numerous rounded cobbles of exotic geological provenance among which were two specimens of remarkable mineralogical composition. An interdisciplinary study combining archeological, geological, petrographic-geochemical, and historical research has demonstrated their Mediterranean, i.e., Italian, provenance. A first stone is identified as Carrara marble originating from the alluvial fans of the Apuan Alps, deposited along the Versilian coast near the Renaissance towns of Lucca, Pisa, and Genoa. The second cobble is determined as a bioclastic calcarenite limestone from the Apulian shores. Both finds are interpreted as part of the non-saleable ballast once put in the holds of Italian carracks and galleys that touched the Flemish ports during the late thirteenth to fifteenth centuries. As such, both seemingly ordinary objects constitute a rare material and lithological testimony of an important late Medieval commercial network between the Mediterranean and North Sea coasts. Furthermore, the very rare occurrence of these Mediterranean cobbles compared to thousands of Scando-Baltic and Anglo-Scottish ballast stones in the whole of the Bruges outer harbor area can be related to differences in maritime traffic frequency and sheer commercial volumes. Also, the nature of the ballast itself and the ballasting procedures are important, the whole making Mediterranean ballast stones considerably less detectable in the Bruges’ harbors than their North-European equivalents.
Located in Library / RBINS Staff Publications 2022
Article Reference Type material of South-American land snails (Mollusca: Gastropoda) of Wladyslaw Emanuel Lubomirski collection deposited in the Museum and Institute of zoology, Warsaw, Poland
Located in Library / RBINS Staff Publications 2022
Article Reference TYPE-MAASTRICHTIAN GASTROPOD FAUNAS SHOW RAPID ECOSYSTEM RECOVERY FOLLOWING THE CRETACEOUS–PALAEOGENE BOUNDARY CATASTROPHE
The study of the global mass extinction event at the Cretaceous–Palaeogene (K/Pg) boundary can aid in understanding patterns of selective extinction, and survival and dynamics of ecosystem recovery. Outcrops in the Maastrichtian type area (south-east Netherlands, north-east Belgium) comprise a stratigraphically expanded K/Pg boundary succession that offers a unique opportunity to study marine ecosystem recovery within the first few thousand years following the mass extinction event. A quantitative analysis was performed on systematically sampled macrofossils of the topmost Maastrichtian and lowermost Danian strata at the former Ankerpoort-Curfs quarry (Geulhem), which represent ‘snapshots’ of the latest Cretaceous and earliest Palaeogene marine ecosystems, respectively. Molluscs in particular are diverse and abundant in the studied succession. Regional ecosystem changes across the K/Pg boundary are relatively minor, showing a decline in suspension feeders, accompanied by an ecological shift to endobenthic molluscs. The earliest Paleocene gastropod assemblage retains many ‘Maastrichtian’ features and documents a fauna that temporarily survived into the Danian. The shallow, oligotrophic carbonate platform in this area was inhabited by taxa that were adapted to low nutrient levels and resistant to starvation. As a result, the local taxa were less affected by the short-lived detrimental conditions related to K/Pg boundary perturbations, such as darkness, cooling, starvation and ocean acidification. This resulted in relatively high survival rates, which enabled rapid recolonization and recovery of marine faunas in the Maastrichtian type area
Located in Library / RBINS Staff Publications 2019
Article Reference Typologie générale des pierres à aiguiser : description des types et caractérisation des aménagements.
Located in Library / RBINS Staff Publications 2019
Article Reference Ultraconserved elements-based phylogenomic systematics of the snake superfamily Elapoidea, with the description of a new Afro-Asian family
The highly diverse snake superfamily Elapoidea is considered to be a classic example of ancient, rapid radiation. Such radiations are challenging to fully resolve phylogenetically, with the highly diverse Elapoidea a case in point. Previous attempts at inferring a phylogeny of elapoids produced highly incongruent estimates of their evolutionary relationships, often with very low statistical support. We sought to resolve this situation by sequencing over 4,500 ultraconserved element loci from multiple representatives of every elapoid family/subfamily level taxon and inferring their phylogenetic relationships with multiple methods. Concatenation and multispecies coalescent based species trees yielded largely congruent and well-supported topologies. Hypotheses of a hard polytomy were not retained for any deep branches. Our phylogenies recovered Cyclocoridae and Elapidae as diverging early within Elapoidea. The Afro-Malagasy radiation of elapoid snakes, classified as multiple subfamilies of an inclusive Lamprophiidae by some earlier authors, was found to be monophyletic in all analyses. The genus Micrelaps was consistently recovered as sister to Lamprophiidae. We establish a new family, Micrelapidae fam. nov., for Micrelaps and assign Brachyophis to this family based on cranial osteological synapomorphy. We estimate that Elapoidea originated in the early Eocene and rapidly diversified into all the major lineages during this epoch. Ecological opportunities presented by the post-Cretaceous-Paleogene mass extinction event may have promoted the explosive radiation of elapoid snakes.
Located in Library / RBINS Staff Publications 2023
Article Reference Un acarien qui saute et qui se met en boule
Located in Library / RBINS Staff Publications
Article Reference Un fossé circulaire de l’âge du Bronze moyen au lieu-dit Champ de la Bruyère
Located in Library / RBINS Staff Publications
Article Reference Uncertainties associated with in situ high-frequency long-term observations of suspended particulate matter concentration using optical and accoustic sensors
Located in Library / RBINS Staff Publications 2019
Article Reference Uncertainty assessment applied to marine subsurface datasets
A recently released voxel model quantifying aggregate resources of the Belgian part of the North Sea includes lithological properties of all Quaternary sediments and modelling-related uncertainty. As the underlying borehole data come from various sources and cover a long time-span, data-related uncertainties should be accounted for as well. Applying a tiered data-uncertainty assessment to a composite lithology dataset with uniform, standardized lithological descriptions and rigorously completed metadata fields, uncertainties were qualified and quantified for positioning, sampling and vintage. The uncertainty on horizontal positioning combines navigational errors, on-board and off-deck offsets and underwater drift. Sampling-gear uncertainty evaluates the suitability of each instrument in terms of its efficiency of sediment yield per lithological class. Vintage uncertainty provides a likelihood of temporal change since the moment of sampling, using the mobility of fine-scale bedforms as an indicator. For each uncertainty component, quality flags from 1 (very uncertain) to 5 (very certain) were defined and converted into corresponding uncertainty percentages meeting the input requirements of the voxel model. Obviously, an uncertainty-based data selection procedure, aimed at improving the confidence of data products, reduces data density. Whether or not this density reduction is detrimental to the spatial coverage of data products, will depend on their intended use. At the very least, demonstrable reductions in spatial coverage will help to highlight the need for future data acquisition and to optimize survey plans. By opening up our subsurface model with associated data uncertainties in a public decision support application, policy makers and other end users are better able to visualize overall confidence and identify areas with insufficient coverage meeting their needs. Having to work with a borehole dataset that is increasingly limited with depth below the seabed, engineering geologists and geospatial analysts in particular will profit from a better visualization of datarelated uncertainty.
Located in Library / RBINS Staff Publications 2020
Article Reference Uncertainty estimation for operational ocean forecast products—a multi-model ensemble for the North Sea and the Baltic Sea
Multi-model ensembles for sea surface temperature (SST), sea surface salinity (SSS), sea surface currents (SSC), and water transports have been developed for the North Sea and the Baltic Sea using outputs from several operational ocean forecasting models provided by different institutes. The individual models differ in model code, resolution, boundary conditions, atmospheric forcing, and data assimilation. The ensembles are produced on a daily basis. Daily statistics are calculated for each parameter giving information about the spread of the forecasts with standard deviation, ensemble mean and median, and coefficient of variation. High forecast uncertainty, i.e., for SSS and SSC, was found in the Skagerrak, Kattegat (Transition Area between North Sea and Baltic Sea), and the Norwegian Channel. Based on the data collected, longer-term statistical analyses have been done, such as a comparison with satellite data for SST and evaluation of the deviation between forecasts in temporal and spatial scale. Regions of high forecast uncertainty for SSS and SSC have been detected in the Transition Area and the Norwegian Channel where a large spread between the models might evolve due to differences in simulating the frontal structures and their movements. A distinct seasonal pattern could be distinguished for SST with high uncertainty between the forecasts during summer. Forecasts with relatively high deviation from the multi-model ensemble (MME) products or the other individual forecasts were detected for each region and each parameter. The comparison with satellite data showed that the error of the MME products is lowest compared to those of the ensemble members.
Located in Library / RBINS Staff Publications