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Article Reference Molecular composition and ultrastructure of Jurassic paravian feathers
The Middle-Late Jurassic fossil assemblage found in the Tiaojishan Formation of Liaoning Province in northeastern China has yielded unparalleled evidence on the early evolution of birds1–4. Most importantly, the identification of various feather-like integumental appendages in non-avian and stem avialan theropods has illuminated the diversity and distribution of plumage structures during their adaptive transition towards use in flight4. Epidermal traces in the Tiaojishan Formation are preserved as either faint impressions or phosphatised and carbonised residues4,5. The latter were long thought to be a product of keratin-degrading bacteria6. However, more recent interpretations have favoured fossilised melanosomes; that is, melanin-bearing cellular organelles responsible in part for the colouration of skin and its structural derivatives7. This landmark hypothesis has spawned an entirely new field of exploratory inference into dinosaurian colour5,7–11, behaviour5 and physiology12.
Located in Library / RBINS collections by external author(s)
Webpublished Reference 1001 décisions, gouvernance et gestion - 1001 besslissingen, beleid en politiek
Série de 10 vidéos des ministres publiées sur le channel Youtube "1001 for Biodiversity". Messages vidéos des ministres responsables de la biodiversité en Belgique à l'occasion de l'anniversaire des 20 ans de la ratification de la Convention sur la Diversité Biologique (CBD) par la Belgique et de la conférence 1001 décisions organisée le 20 mai 2016 à l'IRSNB par le Point focal national CDB. Chaque ministre livre un message sur sa politique en matière de biodiversité et un second message sur les actions qu'il met en oeuvre personnellement à l'inspiration du livret "366 gestes pour la biodiversité" publié par l'Institut royal des Sciences naturelles de Belgique.
Located in Library / RBINS Staff Publications 2017
Article Reference Revised lithostratigraphic scale of the Devonian of Belgium: An introduction and an homage to Pierre Bultynck
Located in Library / RBINS Staff Publications 2024
Article Reference Lower Devonian lithostratigraphy of Belgium
Located in Library / RBINS Staff Publications 2024
Article Reference Middle Devonian lithostratigraphy of Belgium
Located in Library / RBINS Staff Publications 2024
Article Reference Upper Devonian lithostratigraphy of Belgium
Located in Library / RBINS Staff Publications 2024
Book Reference Devonian lithostratigraphy of Belgium
Located in Library / RBINS Staff Publications 2024
Book Reference Environmental Impacts of Offshore Wind Farms in the Belgian Part of the North Sea: Marking a Decade of Monitoring, Research and Innovation.
Located in Library / RBINS Staff Publications 2019
Techreport Reference Radar registrations of bird migration validation through an interdisciplinary approach (RAVen project)
Located in Library / RBINS Staff Publications 2019
Article Reference The genus Charcotia Chevreux, 1906 in the Southern Ocean, with the description of a new species (Crustacea, Amphipoda, Lysianassoidea)
It is demonstrated here that Charcotia Chevreux, 1906 (Amphipoda) has priority over Charcotia Vayssière, 1906 (Gastropoda), and that Waldeckia Chevreux, 1906 has to be treated as an invalid objective junior synonym of Charcotia Chevreux, 1906. An analysis of a part of the mitochondrial COI gene of Charcotia indicates that Charcotia obesa sensu lato, consists of two genetically distant clades that fulfil the criteria of genetic species. Each genetic clade corresponds to a different morphotype. The first one has a low triangular protrusion on the dorsal border of urosomite 1, a strong tooth on epimeron 3, and the posterodistal corner of the basis of pereiopod 7 is regularly rounded. It agrees with the original description of Charcotia obesa Chevreux, 1906. The second one has a protrusion of urosomite 1 prolongated by a sharp and usually long denticle, a small tooth on epimeron 3, and the posterodistal corner of the basis of pereiopod 7 is bluntly angular. The second form is treated herein as a new species, Charcotia amundseni sp. nov., which is described in detail. While the bathymetric distribution of the two Antarctic Charcotia species overlaps (0–300 m for C. obesa and 7–1200 m for C. amundseni sp. nov.), C. obesa largely predominates at depths of less than 150 m, while Charcotia amundseni sp. nov. predominates at greater depths. Both species are widely distributed and presumably circum-Antarctic.
Located in Library / RBINS Staff Publications 2018