Search publications of the members of the Royal Belgian institute of natural Sciences
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Royseux: a palaeobiodiversity hotspot in the Late Viséan (Carboniferous) of Belgium
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Geological context of the Mesolithic Heid de Fer and Ourlaine sites at Becco (Liège province, Belgium)
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Les ressources du sous-sol du bassin du Hoyoux jusqu'aux portes de la ville d'Andenne. Un riche passé industriel qui se conjugue au présent
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Aperçu géologique du bassin du Hoyoux
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Les Brachiopodes
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Les gastéropodes et rostroconches
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Patchiness of Distribution of Mangrove Insects Suggests the Need to Protect Multiple Sites
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Species Turnover in the Mangroves of the South-China Sea: a Comparison of the Predatory Fly Communities of Tropical Singapore with Subtropical Hong Kong
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Sclerochronological evidence of pronounced seasonality from the late Pliocene of the southern North Sea Basin, and its wider implications
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Revisiting the chondrichthyan egg capsules inventory from the Pennsylvanian (Carboniferous) of Belgium: new data and perspectives
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Applying micro-CT imaging in the study of historically and newly collected specimens of Belosaepia (Sepiida, Coleoidea, Cephalopoda) from the Early Eocene (Ypresian) of Belgium
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Cone Penetration Test characterization of middle and upper Miocene lithostratigraphic units near Antwerp International Airport
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The fossil bivalve Angulus benedeni benedeni: a potential seasonally resolved stable isotope-based climate archive to investigate Pliocene temperatures in the southern North Sea basin
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Using self–organizing maps and machine learning models to assess mollusc community structure in relation to physicochemical variables in a West Africa river–estuary system
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Have birds ever mattered? An evaluation of the contribution of avian species to the archaeozoological record of Belgium (Iron Age to recent times)
- This preliminary study aims to document general trends in the representation of bird remains in anthropogenic contexts from Belgian archaeological sites. A large dataset is analysed, consisting of 186 faunal assemblages from 79 different sites. The contexts included vary in terms of their taphonomic nature (refuse layers, latrines, pits, etc.) and date, ranging from the Iron Age to the modern period. The characteristics of the study area and the dataset as a whole are described, with a focus on identification rates, past and present avian taxonomic diversity, and relative abundance of bird remains compared with domestic mammal remains. The impact of recovery methods (sieving or hand collecting) on these various aspects is also evaluated. A taxonomic analysis describes the diversity and abundance of the different groups of species that are encountered and shows which habitats were preferentially exploited for the hunting of wild birds. The study shows that there is significant taxonomic diversity across the dataset. However, this diversity is not necessarily present in each separate archaeological context, as the number of remains identified by taxon is generally low. Some species or groups of species are ubiquitous and dominant, in particular domestic fowl. Although this analysis is broad and exploratory, it is believed that it will serve as a sound methodological basis for future, more detailed studies focusing on the role that birds played in past human societies during specific chronological periods
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NATUURSTEEN in het STADHUIS van KLUNDERT
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GEN-EX – Metagenomics of Extreme-Wave Events
- Extreme-wave events (tsunamis, storm surge and waves) pose significant hazards to coastal communities worldwide. Onshore deposits from these events significantly enhance our understanding of their long-term frequency-magnitude patterns, which are usually not covered by historical and instrumental documentation. Such perspectives are crucial for successful coastal hazard assessments and consequential efforts to mitigate against the loss of life and assets. Methods enabling reliable and consistent differentiation between the sedimentary evidence for tsunamis and storms remain elusive as deposits from both processes share a number of sedimentary criteria. Microfossil approaches (foraminifera, ostracods, diatoms) have yielded promising progress towards conclusive identification (PILARCZYK et al., 2014), however dissolution and bacterial degradation of carbonate tests often prevent microfossil identification. To address this issue in a pioneering project kicked-off in late 2017, we aim at using high-throughput, metagenomic sequencing techniques to identify marine organisms in onshore sand layers from their DNA remains and to unravel cryptic diversities. We focus on foraminifera, single-celled protists, which show depth-related zonation in subtidal environments and have already been traced successfully in palaeo-tsunami deposits by their ancient DNA (SZCZUCIŃSKI et al., 2016), and compare classic and molecular methods for their identification. Three objectives will be followed to reach this goal: 1. Quantify the relationship between water depth and the distribution of different species of foraminifera using both classic assemblage methods and metagenomic approaches. 2. Assess the potential for identifying key indicator species in extreme-wave deposits in different climate settings based on both assemblage approaches and metagenomic high-throughput sequencing techniques; 3. Establish how metagenomic approaches contribute to consistent and reliable differentiation between the sedimentary evidence for storms and tsunamis in coastal settings. The three key field areas, which share an abundance of published, well-dated evidence for both storms and tsunamis, comprise the Shetland Islands, south central Japan, and southern Chile. The Shetland Islands have a temperate oceanic climate, and near-shore lakes and coastal peat lowlands feature sand sheets deposited by the submarine Storegga landslide around 8 ka years ago and a younger tsunami dated to 1.5 ka (e.g. BONDEVIK et al., 2005). Extreme-wave deposits from south central Japan, underlying a subtropical climate, are available through the ongoing BELSPO BRAIN-be-funded QuakeRecNankai project, focusing on records of past earthquakes and tsunamis along the Nankai Trough (GARRETT et al., 2016). At temperate-humid Chaihuin, southern Chile, deposits of the 1960 Chile tsunami and several older events have been documented (HOCKING & GARRETT, 2016) and sampled for identification of foraminiferal assemblages based on DNA remains. REFERENCES BONDEVIK, S., MANGERUD, J., DAWSON, S., DAWSON, A. & LOHNE, Ø. 2005. Evidence for three North Sea tsunamis at the Shetland Islands between 8000 and 1500 years ago. — Quaternary Science Reviews, 24: 1757–1775. GARRETT, E., FUJIWARA, O., GARRETT, P., HEYVAERT, V.M.A., SHISHIKURA, M., YOKOYAMA, Y., HUBERT-FERRARI, A., BRÜCKNER, H., NAKAMURA, A., DE BATIST, M. & THE QUAKERECNANKAI TEAM. 2016. A systematic review of geological evidence for Holocene earthquakes and tsunamis along the Nankai-Suruga Trough, Japan. — Earth-Science Reviews, 159: 337–357. HOCKING, E. & GARRETT, E. 2016. Geological records of recent and historical ruptures of the Chilean subduction zone: a latitudinal transect of earthquake deformation and tsunami inundation. — Geophysical Research Abstracts, 18: EGU2016-938. PILARCZYK, J.E., DURA, T., HORTON, B.P., ENGELHART, S.E., KEMP, A.C. & SAWAI, Y. 2016. Microfossils from coastal environments as indicators of paleo-earthquakes, tsunamis and storms. — Palaeogeography, Palaeoclimatology, Palaeoecology, 413: 144–157. SZCZUCIŃSKI, W., PAWŁOWSKA, J., LEJZEROWICZ, F., NISHIMURA, Y., KOKOCIŃSKI, M., MAJEWSKI, W., NAKAMURA, Y. & PAWLOWSKI, J. 2016. Ancient sedimentary DNA reveals past tsunami deposits. — Marine Geology, 381: 29–33.
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Un Malachide nouveau pour la faune de Belgique, Hypebaeus albifrons (Fabricius, 1775) (Coleoptera, Melyridae, Malachiinae)
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Micropalaeontological dating of the Prémontré mammal fauna (MP10, Prémontré Sands, EECO, early late Ypresian, Paris Basin)
- At their type locality the Prémontré Sands contain fairly well-diversified organic-walled microfossil assemblages attributable to the lower part of dinoflagellate cyst Zone D9 and indicating a transition from an estuarine to a lagoonal depositional regime, up-section as well as laterally. Identical assemblages have been recorded in the inner to mid-neritic Merelbeke Clay Member in Belgium, allowing the Prémontré Sands to be positioned within lower NP13 and early Chron C22r. The deposition of the MP10 Prémontré mammal fauna is estimated to postdate the onset of both NP13 and Chron C22r, which are nearly coincident, by about 200 to 300 kyr. The biostratigraphic dating refers this deposit to the early late Ypresian and to the final phase of the Early Eocene Climatic Optimum (EECO) at about 50.4 to 50.3 million years ago. The Prémontré Sands, as well as their distal equivalent the Merelbeke Clay Member, were deposited following a major sea-level rise, the highest of the late Ypresian in the southern North Sea Basin s.l. (including the Paris Basin). They are separated from the overlying “Glauconie grossière” (zone NP14; middle part of zone D9) by a hiatus of approximately 2.5 myr.
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MaRVEN- Environmental Impacts of Noise, Vibrations and Electromagnetic Emission from Marine Renewable Energy
- The construction and operation of marine renewable energy developments (MREDs) will lead to, among other things, the emission of electromagnetic fields (EMF), underwater sound, and vibrations into the marine environment. Knowledge on these pressures and associated effects has been increasing over the past decade. Yet, many open questions with regard to the potential for MRED to impact on marine life remain. These information gaps pose challenges to the planning and deployment of MREDs. To address this, the European Union (EU) Commission, Directorate-General for Research and Innovation commissioned a study of the environmental effects of noise, vibrations and electromagnetic emissions from MREDs (Marine Renewable Energy, Vibration, Electromagnetic fields and Noise - MaRVEN). MaRVEN provides a review of the available literature related to environmental impacts of marine renewable energy devices and an in-depth analysis of studies on the environmental effects of noise, vibrations and electromagnetic emissions during installation and operation of wind, wave and tidal energy devices. The current norms and standards related to noise, vibrations and EMF were reviewed. On-site measurements and field experiments to fill priority knowledge gaps and to validate and build on the results obtained in reviews were undertaken. Finally, we outline a programme for further research and development with justified priorities.
