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Inproceedings Reference BopCo, a barcoding facility for organisms and tissues of policy concern, and its role in the identification of vector species
Located in Library / RBINS Staff Publications 2022 OA
Article Reference The Diest Formation: a review of insights from the last decades
Located in Library / RBINS Staff Publications 2020
Article Reference Devonian and Carboniferous dendroid graptolites from Belgium and their significance for the taxonomy of the Dendroidea
Located in Library / RBINS Staff Publications 2020
Article Reference Shell chemistry of the Boreal Campanian bivalve Rastellum diluvianum (Linnaeus, 1767) reveals temperature seasonality, growth rates and life cycle of an extinct Cretaceous oyster.
Located in Library / RBINS Staff Publications 2020
Article Reference Osteology and relationships of Luxembourgichthys (“Pholidophorus”) friedeni gen. nov. (Teleostei, “Pholidophoriformes”) from the Lower Jurassic of Belgium and the Grand Duchy of Luxembourg.
The osteology of Luxembourgichthys friedeni (Delsate, 1999) gen. nov. from the marine Toarcian (Grandcourt Formation, Lower Jurassic) of Belgium and the Grand Duchy of Luxembourg is studied in detail. This fossil teleost fish was initially assigned to Pholidophorus, a genus that recently received an emended diagnosis (Arratia, 2013). The cranial characters of L. friedeni considerably differ from those that now define Pholidophorus and the Pholidophoridae, excluding its attribution to both this genus and this family. In L. friedeni the posttemporal fossa is completely located on the lateral face of the braincase and not on the rear of the skull as usual. Such a position is unique among “Pholidophoriformes” and justifies the peculiar generic status of this taxon. L. friedeni possesses three specialized characters (a beryciform foramen piercing the anterior ceratohyal, arcocentra associated to the chordacentra and ovoid scales devoid of the peg-and-socket system) suggesting it occupies a position crownward of most “pholidophoriforms”, closer to Jurassic and younger teleosts with cycloid scales.
Located in Library / RBINS Staff Publications 2017
Inproceedings Reference Investigating the Gill-Oxygen Limitation Theory (GOLT) in the context of gill parasite diversification
Located in Library / RBINS Staff Publications 2023
Article Reference Anthisnes/Anthisnes : alimentation d’origine animale et coq de combat, l’apport des restes fauniques du Moyen Âge et de l’Epoque moderne
Located in Library / RBINS Staff Publications 2016
Article Reference Huy - Saint-Victor: utilisation des animaux sur un site d’habitat et d’artisanat du Haut Moyen Âge
Located in Library / RBINS Staff Publications 2016
Book Reference Les prélèvements des restes bioarchéologiques: manuel de terrain
Located in Library / RBINS Staff Publications 2016
Article Reference Lanice conchilega structures carbon flows in soft-bottom intertidal areas
Biogenic reefs constructed by the tube-building ecosystem engineer Lanice conchilega (Terrebilidae, Polychaeta) have profound structuring impacts on the benthic environment in that they alter the biogeochemical and physical properties of the sediment. This study provides new insights into the functioning and effects on food webs of L. conchilega reefs in intertidal sediments using linear inverse models to quantify the carbon flows in the food webs in the presence and absence of the tubeworm. The inverse food web models were based on an empirical dataset from 2 study sites, which provided biomass and stable isotope data, and information on general physiological constraints from the literature. Results of the model showed that the carbon input into reef food webs (mean ± SE; 191 ± 50 mmol C m−2 d−1) is ca. 40 times higher compared to bare sand areas (5 ± 2 mmol C m−2 d−1) and is mainly derived from organic matter (OM) in the water column. Most of the OM input towards these reefs is consumed by suspension-feeding macrofauna, particularly L. conchilega; however, the worm is not an important source of carbon for other macrofaunal organisms. The ratio of OM input to primary production indicates that the OM needs to be produced in an area at least 15 times larger than the reef area, demonstrating significant OM ‘focussing’ within the reef food web. The reef structures created by L. conchilega act as a trap for OM, resulting in an overall higher macrofaunal biomass and much more diverse food webs than in the absence of the tubeworm.
Located in Library / RBINS Staff Publications 2016