Search publications of the members of the Royal Belgian institute of natural Sciences
- The massive Mousny Quartz Occurrence (High-Ardenne slate belt, Belgium), a late-orogenic dilatational jog?
- Characteristics of the pegmatite-hosted Sn and Nb-Ta mineralisation of the Gatumba area, Rwanda: Preliminary results
- The added value of CO2 geological storage in developing countries: a case study for Kazakhstan
- Converting abandoned coal mines into pumped-storage hydroelectric power stations
- Implications of increasing subsurface concentrations of CO2 since 1966 as evidenced from measurements in caves on the monitoring programs for the detection of leakage from geological storage sites for CO2
- Natural CO2 releases of geogenic origin: Cross-border comparison (Belgium-Germany) for selected emission locations
- The Neeroeteren Formation as a viable CO2 storage option in Belgium
- Storage as bottleneck for the commercial introduction of CCS
- Critical Thinking about Critical Resources
- About canals and qanats: long-term human impact on Late Quaternary alluvial landscapes
- Changes in precipitation as inferred from a Holocene speleothem from the Hotton cave (Hotton, Marche–en-Famenne, Belgium)
- Petrography, geochemistry and stable isotope geochemistry of a banded columnar calcite deposit sampled at 1000 meters depth in the Wépion core drilling, Wépion, Belgium, implications for the origin of the calcite
- Kwaliteitsdocumentatie en definiëring van referentieobjecten voor de Databank Ondergrond Vlaanderen (VLA 10-2.1)
- Harpacticoid copepod colonization of coral fragments in a tropical reef lagoon (Zanzibar, Tanzania)
- Colonization experiments were conducted in a tropical lagoon (Zanzibar Island, off the coast of Tanzania) to investigate the temporal dynamics and mode of colonization of the harpacticoid copepods community on dead coral fragments. There was fast colonization of the coral fragments attaining a substantial diversity after only two days. The ability to colonize dead coral fragments is thought to be related to the morphology and life style of different harpacticoid species. Phytal taxa (e.g. Tisbidae) were fast colonizers, reaching high abundances during the initial colonization phase. Sediment-associated and eurytopic taxa (e.g. Ameiridae, Miraciidae and Ectinosomatidae) showed lower colonization rates and became the dominant group during the later colonization phase. Most species are able to colonize the coral fragments through the water column. However, colonization along the substrate surface is also considered to be an important colonization mode, especially for sediment-associated taxa, which showed lower colonization rates when migration through the sediment was hindered.
- Distribution patterns of subsurface copepods and the impact of environmental parameters
- On the brink - investigating biodiversity in endangered crater lakes of the Amber Mountains National Park (Madagascar)
- Updating the zooplankton species list for the Belgian part of the North Sea
- Community structure of harpacticoid copepods in intertidal and shallow-water habitats of Cat Ba archipelago (Vietnam, South China Sea)
- The assemblage structure of harpacticoid copepods inhabiting the soft sediments of littoral and sublittoral areas of Cat Ba archipelago (South China Sea) is analysed. Three basic types of harpacticoid taxocenes were observed in the upper sublittoral. Main dominant species of taxocenes were Amphiascoides sp., Stenhelia latioperculata, Paramphiascella sp., Phyllopodopsyllus sp., Tisbe sp.1 and Amphiascoides sp. In addition, the main characteristics of harpacticoid species composition in littoral rock pools are described. A comparative analysis of shallow-water harpacticoid communities from different biotopes of the tropical region is presented, and shows that harpacticoid diversity and abundance are lowest in muddy sediments. Highest diversity and abundance are found in washed sands and silty sands with detritus. In general, the structure of muddy bottom communities is the most homogeneous throughout the tropics. Mangrove forests have no significant influence on harpacticoid taxocene structure. Harpacticoid associations of washed sands and silty sands with detritus demonstrate greater diversity and are region-specific.
- High-resolution X-ray CT for 3D petrography of ferruginous sandstone for an investigation of building stone decay
- Early diversification of seeds and seed-like structures