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Article Reference Brassicaceae seed oil identified as illuminant in Nilotic shells from a first millennium AD Coptic church in Bawit, Egypt
Burned greasy deposits were found inside shells of the large Nile bivalve Chambardia rubens, excavated in an eight- to tenth- century AD church of the Coptic monastery of Bawit, Egypt, and supposedly used as oil lamps. The residues were subjected to a combination of chromatographic residue analysis techniques. The rather high concentrations of unsaturated fatty acids, as analysed by gas chromatography (GC) in the methylated extract, suggest the presence of a vegetal oil. Analysis of the stable carbon isotopes (δ13C values) of the methyl esters also favoured plants over animals as the lipid source. In the search for biomarkers by GC coupled to mass spectrometry on a silylated extract, a range of diacids together with high concentrations of 13,14-dihydroxydocosanoate and 11,12- dihydroxyeicosanoate were found. These compounds are oxidation products of erucic acid and gondoic acid, which are abundantly present in seeds of Brassicaceae plants. Liquid chromatography coupled to mass spectrometry analysis showed low concentrations of unaltered triglycerides, but revealed sizeable amounts of triglycerides with at least one dihydroxylated acyl chain. The unusual preservation of dihydroxylated triglycerides and α,ω-dicarboxylic acids can be related to the dry preservation conditions. Analysis of the stereoisomers of the dihydroxylated fatty acids allows one to determine whether oxidation took place during burning of the fuel or afterwards. The results prove that the oil of rapeseed (Brassica napus L.) or radish (Raphanus sativus L.) was used as illuminant in early Islamic Egypt, and that not only ceramic lamps but also mollusk shells were used as fuel containers.
Located in Library / RBINS Staff Publications
Article Reference Brawn before brains in placental mammals after the end-Cretaceous extinction
Mammals are the most encephalized vertebrates, with the largest brains relative to body size. Placental mammals have particularly enlarged brains, with expanded neocortices for sensory integration, the origins of which are unclear. We used computed tomography scans of newly discovered Paleocene fossils to show that contrary to the convention that mammal brains have steadily enlarged over time, early placentals initially decreased their relative brain sizes because body mass increased at a faster rate. Later in the Eocene, multiple crown lineages independently acquired highly encephalized brains through marked growth in sensory regions. We argue that the placental radiation initially emphasized increases in body size as extinction survivors filled vacant niches. Brains eventually became larger as ecosystems saturated and competition intensified.
Located in Library / RBINS Staff Publications 2022 OA
Article Reference Brockphasma spinifemoralis gen. et spec. nov.: a new phasmid genus and new species of Neohiraseini (Phasmida: Necrosciinae) from Vietnam
Located in Library / RBINS Staff Publications
Article Reference Bruchidius imbricornis (Panzer, 1795), Bruchus occidentalis Lukjanovitch & Ter-Minassian, 1957 et Bruchus brachialis Fåhraeus, 1839 nouveaux pour la faune belge et données récentes de Bruchidius siliquastri Delobel, 2007 (Coleoptera: Chrysomelidae, Bruchi
Located in Library / RBINS Staff Publications 2021
Article Reference Bryocamptus (Bryocamptus) gauthieri (Roy, 1924): a Mediterranean edaphic specialist (Crustacea: Copepoda: Harpacticoida)
Located in Library / RBINS Staff Publications
Inproceedings Reference Building a Lithotectonic Framework for Belgium
Almost all geological subdisciplines depend, to varying extents, on regional geological knowledge. Stratigraphic terminology is typically well-defined, while other concepts rely on generally accepted definitions or hierarchical schemes, such as palaeontological, structural and magmatic terminologies. This is much less the case for the regional geological building blocks. Their nomenclature is usually composed of a reference to a geographical locality and a geological term. Examples from Belgium include the (Anglo-)Brabant Massif, Campine Basin, and Malmedy Graben. Despite wide recognition, such terms often lack precise definitions and may even present conflicting interpretations across different contexts and authors. Even when their meanings have drifted or become less precise, these terms continue to be utilized. Increased awareness has led to significant yet isolated initiatives aimed at improving the structure and definition of regional geological information [1-3], recently brought together through pan-European cooperation [4]. Lithotectonic unit appears to be the most effective concept for encompassing all geological features. A lithotectonic unit is characterized by its composition, structural elements, mutual relations, and/or geological history [5]. Following a geotemporal conceptual approach, lithotectonic units are defined and bounded by relative limits in time and space [6]. Lithotectonic limits are planar features corresponding to geological events which have formed and define these units. Examples of lithotectonic units include orogens, terranes, sedimentary basins, and grabens, while examples of lithotectonic limits include deformation fronts, faults, and unconformities. This approach facilitates the organization and formalization of relationships between units and limits through ontologies. The data model can be linked to established ontologies, such as the ICS Geological Time Scale Ontology [7], and allows future extensions, such as attribution to orogenic cycles [2]. The associated concepts can be linked to 2D and 3D visualizations, thereby adding an important layer of knowledge to geological maps and models. Primary objective of the newly established Lithotectonic Working Group, under the National Commission for Stratigraphy in Belgium, is to create a comprehensive lithotectonic framework, that systematically defines and describes the main geological units and limits of Belgium. This initiative aligns closely with emerging standards currently being developed and implemented at European level [4] and largely based on GeoSciML [8]. [1] Hintersberger et al. 2017, Jb Geol B-A 157:195-207. [2] Németh 2021, Miner Slovaca 2:81-90. [3] Le Bayon et al. 2022: https://doi.org/10.1051/bsgf/2022017. [4] GSEU 2022-2027: https://doi.org/10.3030/101075609. [5] INSPIRE 2015: https://inspire.ec.europa.eu/theme/ge. [6] Piessens et al. 2024: https://doi.org/10.31223/X5RT28. [7] Cox & Richard 2005: https://doi.org/10.1130/GES00022.1. [8] GeoSciML 2016: http://www.opengis.net/doc/geosciml/4.1.
Located in Library / RBINS Staff Publications 2025
Article Reference Bypassing the Suess-effect: Age determination of charcoal kiln remains using OSL dating
Located in Library / RBINS Staff Publications 2020
Article Reference Cabindachanos dartevellei gen. and sp. nov., a new chanid fish (Ostariophysi, Gonorynchiformes) from the marine Paleocene of Cabinda (Central Africa)
The osteology of Cabindachanos dartevellei gen. and sp. nov., a fossil fish from the marine Danian or early Selandian deposits of Landana (Cabinda Territory, Central Africa), is here studied in detail. This fish is known by only one partially preserved specimen that shows typical characters. The opercle is greatly hypertrophied. The preopercle has a very broad dorsal limb and a long narrower ventral limb. There is a wide plate-like suprapreopercle. The lower jaw is deep, with a well-marked coronoid process formed by the dentary. The articulation between the quadrate and the mandible is located before the orbit. The first supraneurals are enlarged. These characters indicate that C. dartevellei belongs to the family Chanidae (Teleostei, Gonorynchiformes). Cabindachanos dartevellei differs from all the other known fossil or recent chanid fishes by the gigantic development of its opercle and by the loss of the subopercle. The straight angle formed by the two limbs of the preopercle and the well-developed posterior median crest of the supraoccipital indicate that C. dartevellei belongs to the subfamily Chaninae and the tribe Chanini.
Located in Library / RBINS Staff Publications 2019
Article Reference Calcardea junnei Gingerich, 1987 from the late Paleocene of North America is not a heron, but resembles the early Eocene Indian taxon Vastanavis Mayr et al., 2007
We revisit the holotype of Calcardea junnei Gingerich, 1987 from the latest Paleocene (Clarkforkian) of the Willwood Formation (Wyoming, USA). The species is based on a partial skeleton and was originally assigned to the Ardeidae (herons). As we show, this classification cannot be upheld and Calcardea Gingerich, 1987 more closely resembles the taxon Vastanavis Mayr et al., 2007 (Vastanavidae), a parrot-like bird from the early Eocene of India. Even though C. junnei is a large bird, its long wings and short tarsometatarsus argue against a predominantly terrestrial way of living, and the morphology of the tarsometatarsus and pedal phalanges instead suggest strong grasping feet.We conclude that an assignment of Calcardea to the landbird clade (Telluraves) is better supported than its classification into the waterbird clade (Aequornithes), which includes Ardeidae and other ‘ciconiiform’ and ‘pelecaniform’ taxa. Calcardea junnei is one of the oldest known representatives of Telluraves and its morphology shows plesiomorphic features, which contributed to its previous misidentification as a heron. Calcardea exhibits a distinctive osteology and affords a glimpse of a previously unknown late Paleocene avian morphotype.
Located in Library / RBINS Staff Publications 2019
Incollection Reference Calcareous nannofossil events at the Eocene-Oligocene boundary.
Located in Library / RBINS Staff Publications