Search publications of the members of the Royal Belgian institute of natural Sciences
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The integration of nature conservation into the marine spatial planning process.
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Monitoring and evaluation of spatially managed areas: A generic framework for implementation of ecosystem based marine management and its application.
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The role of structuring benthos for juvenile flatfish.
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Encounter competition partly explains the segregation of the sandy beach amphipods Bathyporeia pilosa and Bathyporeia sarsi. A mecocosm experiment.
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Hydrometeorological influences and multimodal suspended particle size distributions in the Belgian nearshore area (southern North Sea).
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Benthic habitat variations over tidal ridges, North Sea
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Fine-scale geomorphological mapping for the prediction of macrobenthic occurrences in shallow marine environments, Belgian part of the North Sea
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Very high SPM concentrations in the southern Bight of the North Sea detected from space.
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Recent anoxic cohesive sediment deposits in the Belgian near-shore area: sedimentological context and anthropogenic impact
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Flocculation in a eutrophic coastal turbidity maximum zone.
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Heterogeneous flocculation combining the biological and mineralogical populations in a marine and coastal environment: Literature study for a conceptual model.
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Optimalisatie van de efficiëntie van de baggerstortplaatsen - sedimentbeheer in de Noordzee. 9de Waterforum: de verdoken schakel in het waterbeleid. Sediment samen aanpakken biedt vele kansen.
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Dredged material disposal : Does it substantially affect the ecosystem?
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Sediment dynamics as a proxy for soft substrata habitat distributions, Belgian part of the North Sea.
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RV Belgica Cruise Report 2012/02
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The chronology of Lateglacial and Holocene fluvial dynamics in the Lower Scheldt basin (N-Belgium), and its relation with the archaeological record
- In light of tidal restoration and nature development projects, several alluvial areas in the Lower Scheldt Basin (LSB) have been subjected to geo-archaeological surveys and excavations. An analysis of 80 radiocarbon dates obtained in these studies shows several trends in the chronology of Lateglacial and Holocene fluvial activity in the LSB. Similar evolutions are observed in other lowland river basins in NW Europe, and can be related to both climatic changes, and from the 4 th millennium cal BP onwards, also to anthropogenic influences. In general a low energy aggradation regime dominates the built up of the alluvial area throughout most of the early and middle Holocene. In several areas of the LSB fluvial activity increases in the 1 st millennium BC, with the incision and following aggradation of local channels. From the Roman period onwards the aggradation of alluvial fines again dominates the fluvial regime, extending the area of overbank sedimentation. The comparison between these radiocarbon dating results and the observed archaeological record allows to draw conclusions concerning the interplay between landscape development and the presence and preservation of the archaeological record.
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RV Belgica Cruise Report 2012/12
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RV Belgica Cruise Report 2012/15
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RV Belgica Cruise Report 2012/18
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RV Belgica Cruise Report 2012/21
