{"refrec":{"BRefID":233966,"RR":"<b>Taverne, L.; Van Simaeys, S.; Steurbaut, E.</b> (2006). <i>Belgocaranx luypaertsi</i> gen. and sp. nov., a new skeleton-based Carangid Fish from the Boom Clay (Rupelian, Early Oligocene) at Kallo (N. Belgium). <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 76</i>: 119-130","BEntID":225650,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 76</i>: 119-130","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Taverne, L.; Van Simaeys, S.; Steurbaut, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Taverne, L. <i>et al.</i>","Englishabstract":"A three dimensionally preserved carangid skull from a concretion level at the top of the Boom Clay (Rupelian, Oligocene) in the Vrasenedok (Kallo, Belgium) is described and assigned to a new genus and species: <i>Belgocaranx luypaertsi</i> (Teleostei, Perciformes). Geometric and biostratigraphic calibration with outcrop and borehole sections close to the Vrasenedok allows the concretion level to be positioned within the upper middle part of the Boom Clay Formation, respectively around septaria-level S110 according to the dinoflagellate cyst correlation and around septaria-level S150 according to geometric extrapolation. The discovery of this fish skull illustrates a specific step in the evolution of carangid fishes, allowing estimation of the nature and rate of their evolution during the last 50 million years.","AbstractOtherLang":"Un crâne de carangidé conservé en trois dimensions et provenant d'un niveau à concrétions au sommet de l'Argile de Boom (Rupélien, Oligocène) dans le Vrasenedok (Kallo, Belgique) est décrit et assigné à un nouveau genre et une nouvelle espèce: <i>Belgocaranx luypaertsi</i> (Teleostei, Perciformes). Un étalonnage géométrique et biostratigraphique avec des affleurements et des sondages proches du Vrasenedok a permis de situer ce niveau à concrétions au sommet de la partie moyenne de l'Argile de Boom, respectivement aux environs du niveau à septaria S110, d'après une corrélation avec les kystes de dinoflagellés, et aux environs du niveau à septaria S150, selon l'extrapolation géométrique. La découverte de ce crâne de poisson illustre une étape spécifique dans l'évolution des carangidés, permettant d'estimer la nature et le taux de leur évolution durant les 50 derniers millions d'années.","BibLvlCode":"AS","StandardTitle":"<i>Belgocaranx luypaertsi</i> gen. and sp. nov., a new skeleton-based Carangid Fish from the Boom Clay (Rupelian, Early Oligocene) at Kallo (N. 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