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Inproceedings Reference Where and why: using a structural framework to contextualise and improve the understanding of processes leading to mineral occurrences
The societal development towards climate neutrality and the ambition for economic growth and well-being in Europe rely on mineral raw materials. Mineral occurrences can be seen as manifestations of specific geological processes that happened in the subsurface, or geomanifestations. Locating and better understanding mineral occurrences and deposits in Europe is crucial for future informed decision making on local resourcing. The GeoConnect³d project is developing a multi-scale structural framework in which geological maps and 3D models can be inserted and related to. In our novel approach, the structural framework reorganises geological information in terms of geological limits and geological units. Limits are defined as broadly planar structures that separate a given geological unit from its neighbouring units, e.g. faults (limits) that define a graben (unit), or an unconformity (limit) that defines a basin (unit). Geomanifestation data are then added to the structural framework model aiming to show where and how processes and structures may be linked. This approach was tested in Belgium, where a structural framework was created at different scales, from most detail at 1:250,000 to more generalised at 1:2,000,000. Mineral occurrence data from the Minerals4EU database were used to test the model. As an example, a spatial link between Pb-Zn deposits and structural framework elements is identifiable in the Herve-Vesdre and Landenne areas. Although the deposits are located within the Variscan orogenic front, deposition is post-Variscan and spatially associated with transverse NNW-SSE faults part of the Rhine graben network (Dejonghe, 1998). With a combination of database attributes and SKOS vocabulary, the information of deposition age and time of activity of faults displayed in the structural framework helps to quickly place these deposits in the context of the Lower Rhine embayment. Therefore, the structural framework can translate highly technical scientific knowledge by using an interactive tool that presents information in a more understandable way. We consider the outcomes of this test promising to fulfil one of the main goals of GeoConnect³d: preparing and disclosing geological information in a way it is more useful for stakeholders. We also consider this as the way forward towards pan-European integration and harmonisation of geological information, where the ultimate challenge is to correlate or otherwise link information from different geological domains and of different scales. This will be beneficial for the identification and better geological understanding of European mineral resources. This project has received funding from the European Union's Horizon 2020 research and innovation programme under grant agreement No 731166. Reference: Dejonghe, L., 1998. Zinc-lead deposits in Belgium. Ore Geology Reviews 12, 329-354.
Located in Library / RBINS Staff Publications 2020
Inproceedings Reference Interdisciplinary study of horticultural practices in late medieval Brussels
Over the last decades a series of sites attesting the presence of ancient crop fields and gardens were discovered in the historical center of Brussels. Well aerated crop field and garden soils with a high biological activity, are often not suitable for the preservation of organic plant remains. In most cases, their studies yielded only small quantities of more resistant seeds and fruits. The identification of the cultivated plants relied therefore mainly on phytolith analysis.Recently, a Holocene peat sequence was excavated in the lower part of the city in a quarter that is historically documented as a horticultural area (rue des Boiteux, BR295). Micromorphology showed that the upper layers of the peat sequence were drained during the late Middle Ages and subsequently converted into horticulture. In this poster the potential of studying these contexts will be discussed. Thanks to the prevailing wet conditions of the soil, higher densities of waterlogged macrobotanical remains could be analysed. Remains of divers cultivated plants and garden weeds were found, most probably partly from the local vegetation and local cultivated crops. The archaeobotanical and archaeozoological studies also shed light on manuring practices.
Located in Library / RBINS Staff Publications 2019
Article Reference A relative of the beluga and narwhal (Odontoceti, Monodontidae) from the Early Pliocene of the North Sea
Located in Library / RBINS Staff Publications
Article Reference Tusk-bearing beaked whales from the Miocene of Peru
Located in Library / RBINS Staff Publications
Article Reference A new pithanodelphinine dolphin from the Miocene of Peru and the origin of modern delphinidan families
Located in Library / RBINS Staff Publications
Article Reference A new genus and species of Pliocene dolphin (Cetacea: Odontoceti: Inioidea) from North Carolina, U.S.A.
Located in Library / RBINS Staff Publications
Article Reference New insights on the brain, tooth development, and feeding specializations of the sirenian Miosirenkocki(Trichechidae, Sirenia) as revealed by CT
Located in Library / RBINS Staff Publications
Article Reference Evolution of high-frequency hearing in odontocetes (Mammalia: Cetacea)
Located in Library / RBINS Staff Publications
Article Reference New material of Australophoca (Carnivora, Phocidae) from the late Miocene of Peru suggests sexual dimorphism in the smallest, early-branching monachine seal
Located in Library / RBINS Staff Publications 2017
Inproceedings Reference Characterization of a multiple burial context from Pachacamac, Peru: complementarity between bioarchaeology and molecular archaeology
Pachacamac is a major precolumbian site located on Peru’s Central Coast. Covering approximately 6 km2, the site was occupied for over a thousand years before the Spanish conquest in the early sixteenth century. In 2012, the Ychsma Project discovered a unique Late Intermediate period (AD 900–1470) multiple burial (“Cx4”) made of two funerary chambers with a vegetal roof structure, containing over 110 intact and fragmentary deceased together with numerous grave goods. More than 60% of the individuals are subadults whose sex cannot be assigned using osteological observation. Among the adults, 23 females and 20 males were identified, and the sex of the remaining four individuals couldn’t be assigned with certainty. We aim to fully understand the sociobiology of the Cx4 population, including biological sex, using a combined bioarchaeology and molecular archaeology approach. Despite significant human modern contamination and low amounts of endogenous ancient DNA, our results show that sex could be assigned genetically in >70% of the cases, including subadults. Sex identification of infants, children and adolescents is crucial to fully understand this complex context and its funerary recruitment, and to perform an integrated and holistic analysis of all associated data.
Located in Library / RBINS Staff Publications 2024