This work is mainly based on the collection of Neogene (Miocene-Pliocene) odontocetes (toothed whales) from the area of Antwerp (northern Belgium, southern margin of the North Sea Basin) preserved at the Institut royal des Sciences naturelles de Belgique (IRSNB). The systematic revision of members of the long-snouted dolphin family Eurhinodelphinidae leads to the description/re-description of five species in the genera Eurhinodelphis (E. cocheteuxi and E. longirostris), Schizodelphis (S. morckhoviensis), and Xiphiacetus n. gen. (X. cristatus and X. bossi). Furthermore, the systematic status of several eurhinodelphinid species from other localities in the world is revised. A cladistic analysis with the parsimony criterion is undertaken to highlight the phylogenetic relationships of several eurhinodelphinid taxa with other fossil and extant odontocetes. Eurhinodelphinids are more closely related to the beaked whales; the latter are distinctly separated from the sperm whales. A second analysis, with a likelihood criterion, reaches nearly identical results. Then a separate parsimony analysis investigates the relationships within the family Eurhinodelphinidae; the results suggest sister-group relationships between Schizodelphis + Xiphiacetus and Ziphiodelphis + (Mycteriacetus + Argyrocetus) and a more stemward position for Eurhinodelphis. After that, anatomical, palaeogeographic, and phylogenetic data allow several suggestions about the ecological features of the eurhinodelphinids. The extinction of this family, before the end of the Miocene, is commented, related to the changes in the biodiversity of other odontocete groups and to a contemporary major sea level drop. Members of the family Platanistidae, subfamily Pomatodelphininae, are recorded for the first time in the Miocene of the North Sea, on the basis of several long-snouted specimens. The review of the large collection of Neogene beaked whales (Ziphiidae) from the IRSNB diagnoses eleven species in seven genera: Aporotus recurvirostris, A. dicyrtus, Beneziphius brevirostris n. gen. n. sp., Cetorhynchus atavus, Choneziphius planirostris, C. macrops, Mesoplodon longirostris, Ziphirostrum marginatum, Z. turniense, Z. recurvus, and Archaeoziphius microglenoideus n. gen. n. sp. The latter is dated with dinoflagellates from the Middle Miocene; it constitutes the oldest beaked whale known by diagnostic cranial material. A parsimony analysis indicates sister-group relationships between Ziphirostrum + Beneziphius and Choneziphius + (Tusciziphius + Ziphius). A functional anatomy chapter deals with the pachy-osteosclerotic structure of the rostrum in several beaked whale species from Antwerp; several functional hypotheses (including deep diving and intraspecific fights) are confronted to data on extant taxa and to the evolutionary history of the family. Finally, the review of the Miocene short-snouted dolphin species Protophocaena minima leads to the first European record of members of the family Pontoporiidae.

Les archosaures sont un clade de vertébrés comprenant les oiseaux, les crocodiliens, ainsi que de nombreux groupes fossiles. Ce groupe fait depuis plusieurs décennies l'objet d'un important débat parmi les paléontologues quant à l'évolution du thermométabolisme au sein de ses différentes lignées. L'hypothèse classique considère que seuls les oiseaux modernes sont endothermes, tandis que tous les autres archosaures sont ectothermes. L'histologie osseuse permet d'étudier plusieurs traits relatifs au thermométabolisme impossibles à mesurer sur des spécimens fossiles ; c'est pourquoi nous avons utilisé des caractères mesurés sur des coupes histologiques d'os longs.Nous nous sommes consacrés dans une première partie à une revue détaillée de la mesure du signal phylogénétique pour des caractères ostéohistologiques dans deux clades de vertébrés, ce qui nous a permis de mieux définir l'approche à suivre dans la construction de nos modèles prédictifs.Après une étude préliminaire consacrée à l'élaboration d'un modèle prédictif du taux de croissance osseuse, nous avons construit un modèle global capable de prédire directement le taux métabolique de nos spécimens fossiles. Nos résultats montrent que la majorité des archosaures de notre échantillonnage étaient endothermes. Cela implique que le dernier ancêtre commun des archosaures était probablement endotherme, et que les crocodiliens sont donc devenus secondairement ectothermes, probablement en réponse aux contraintes du milieu aquatique. Des études plus spécifiques sur la lignée des pseudosuchiens devraient permettre de déterminer à quel niveau de l'arbre phylogénétique s'est effectué le retour à cet état ectotherme. / Archosaurs are a clade of vertebrates that includes birds, crocodiles, and numerous fossil groups. This clade has been a matter of debate among paleontologists for decades concerning the evolution of thermometabolism in its different lineages. The classical hypothesis considers that only modern birds are true endotherms, whereas all other archosaurs are ectotherms. Bone histology allows to study several traits linked to bone growth rate and thermometabolism, otherwise impossible to estimate on fossil specimens; for this reason, we used characters measured on long bone histological sections.In the first section, we extensively reviewed the measure of phylogenetic signal for osteohistological features in two clades of vertebrates, which was then used to define the methodology for building our predictive models.After a preliminary study during which we built a predictive model for bone growth rate, we built a global model to predict the metabolic rate of our fossil specimens, using both histological features and phylogenetic information for each specimen. Our results show that a majority of archosaurs in our sample were endotherms. This implies that the last common ancestor of archosaurs was likely an endotherm, and that modern crocodiles became secondarily ectothermic, probably in response to their aquatic environment. More specific studies on pseudosuchians should allow to precisely identify the level of the phylogenetic tree at which the ectothermic state was acquired, as well as adaptive constraints behind this acquisition.

This work is mainly based on the collection of Neogene (Miocene-Pliocene) odontocetes (toothed whales) from the area of Antwerp (northern Belgium, southern margin of the North Sea Basin) preserved at the Institut royal des Sciences naturelles de Belgique (IRSNB). <p> The systematic revision of members of the long-snouted dolphin family Eurhinodelphinidae leads to the description/re-description of five species in the genera Eurhinodelphis (E. cocheteuxi and E. longirostris), Schizodelphis (S. morckhoviensis), and Xiphiacetus n. gen. (X. cristatus and X. bossi). Furthermore, the systematic status of several eurhinodelphinid species from other localities in the world is revised. A cladistic analysis with the parsimony criterion is undertaken to highlight the phylogenetic relationships of several eurhinodelphinid taxa with other fossil and extant odontocetes. Eurhinodelphinids are more closely related to the beaked whales; the latter are distinctly separated from the sperm whales. A second analysis, with a likelihood criterion, reaches nearly identical results. Then a separate parsimony analysis investigates the relationships within the family Eurhinodelphinidae; the results suggest sister-group relationships between Schizodelphis + Xiphiacetus and Ziphiodelphis + (Mycteriacetus + Argyrocetus) and a more stemward position for Eurhinodelphis. After that, anatomical, palaeogeographic, and phylogenetic data allow several suggestions about the ecological features of the eurhinodelphinids. The extinction of this family, before the end of the Miocene, is commented, related to the changes in the biodiversity of other odontocete groups and to a contemporary major sea level drop. <p>\ / Doctorat en sciences, Spécialisation biologie animale / info:eu-repo/semantics/nonPublished