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Inproceedings Reference Biodiversity of the freshwater crabs of Benin: a genetic approach
Located in Library / RBINS Staff Publications 2024
Inproceedings Reference Biodiversity research and monitoring related capacities in Kisangani (DRC)
Located in Library / RBINS Staff Publications 2017
Proceedings Reference Biodiversity, Bushmeat and Monkeypox in the Democratic Republic of the Congo: another viral threat upon larger cities?
Located in Library / RBINS Staff Publications
Inproceedings Reference Biodiversity, reproduction and population structure of Sciuridae (Rodentia, Mammalia) from the Forest Reserves of Yoko, Masako and the locality of Uma (Eastern Province, DR Congo)
Located in Library / RBINS Staff Publications
Inproceedings Reference Bioerosional marks in the shells of two extinct sea turtle taxa from the Eocene of Belgium
Bioerosional marks are frequently recognized as indicators of the dynamic interactions between the organisms and their surrounding environments. In the fossil record, these structures are frequently manifest in the skeletal remains of vertebrates, being commonly associated to predation activity, scavenging, or post-mortem degradation processes. In the case of the turtles, their shells offer a distinctive substrate, exposed for the development of bioerosional processes throughout the organism life, unlike other vertebrate osseous structures. These bioerosions can indicate the type of habitat in which the turtles live, their behavioral patterns, and even their state of health. Sea turtles, as other marine vertebrates, have been extensively studied in the realms of the biology, evolution, and conservation. However, relatively scarce information is available regarding the pathologies and infectious diseases affecting their shells, especially when extinct taxa are analyzed. The aim of this study is to analyze the diverse types of bioerosional marks on the shells of two sea turtle individuals, attributable to taxa, from the Lutetian (middle Eocene) of Belgium. One of them corresponds to the shell of the holotype of Eochelone brabantica (IRSNB R 0001). Its carapace exhibits multiple erosive anomalies on several costal plates. The second specimen is a carapace of Puppigerus camperi (IRSNB R 0004). It displays different typologies of shell deviations, also of erosive character. The analyses of these specimens have been performed through both the detailed macroscopic examination and the study of the cross-sectional images provided by CT scanning in the case of Eochelone brabantica, and a 3D model obtained through a surface scanner for Puppigerus camperi. As a result, insights into the shell modifications of these two turtle individuals induced by various external agents have been provided, enhancing our understanding of the physical stressors affecting these organisms in ancient marine environments and the organisms responsible for these changes.
Located in Library / RBINS Staff Publications 2025
Article Reference Biogeography and phylogeography of non-marine Ostracoda (Crustacea). Crustacean conference
Located in Library / RBINS Staff Publications
Techreport Reference Biogeomorphological self-organization in sandy shelf seas. In: V. Van Lancker & T. Garlan (Eds.), MARID 2013, 4th International Conference on Marine and River Dune Dynamics. Bruges, Belgium. 15-17 April 2013 (pp. 53-57). Oostende, Belgium: VLIZ.
Located in Library / RBINS Staff Publications
Article Reference Biogeomorphology in the field: bedforms and species, a mystic relationship.
In: Van Lancker, V. and T. Garlan (Eds.), MARID 2013. Fourth International Conference on Marine and River Dune Dynamics, Bruges, Belgium, 15-17 April 2013, Royal Belgian Institute of Natural Sciences and SHOM. VLIZ Special Publication 65 – Flanders Marine Institute (VLIZ), Oostende, Belgium, 277-284.
Located in Library / RBINS Staff Publications
Inproceedings Reference Biotic and lithologic expressions of lower Paleogene hyperthermals in the Nile Basin, Egypt.
Located in Library / RBINS Staff Publications
Inproceedings Reference Biotic and lithologic expressions of lower Paleogene hyperthermals in the Nile Basin, Egypt.
Located in Library / RBINS Staff Publications