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Phytosaurs are the most basal group of crurotarsan archosaurs. Superficially resembling crocodiles in habit and probably also in their ecological requirements, they form an important component of terrestrial vertebrate communities in the Late Triassic. The phytosaurs from the Stubensandstein deposits (Norian) of southwestern Germany are among the first representatives to become known of the group. However, our poor knowledge of European Norian phytosaurs is well exemplified by many morphological details of the cranium that in the course of this study were found to be hitherto unknown, or to be at variance with the literature. Virtually all phytosaur specimens from these deposits were examined to established their taxonomic status. The specimens comprise four valid species, which are referred to the genera Nicrosaurus FRAAS, 1866 and Mystriosuchus FRAAS, 1896. Both genera and all species are redefined on the basis of shared derived characters. The aim of this thesis is to redescribe the cranial anatomy of each taxon, a prerequisite to determine the variability and to test the validity of cranial characters that have been utilised to establish phylogenetic relationships among phytosaurs. A comprehensive skull osteology and a study of the variation in cranial characters of Nicrosaurus kapffi (MEYER, 1860) forms the main part of the thesis. The complete upper dentition is described in order to determine the positional variation of dental characters. Nicrosaurus kapffi is characterised by two features of its prenarial crest. Two morphs are recognised among the specimens based mainly on different skull width. The distinction is congruent with the distribution of other dimorphic features of the postorbital part of the skull and details of the crested rostrum, many of which are currently employed in phytosaur taxonomy. The intraspecific variation is interpreted as sexual dimorphism. The study demonstrates also that other characters are actually variable at species level and can provide only limited taxonomic and phylogenetic information. These include, most importantly, a reduction of the suborbital opening, a partly persisting parietal foramen, and, varying individually, the configuration of a number of dermal skull bones. The slender-snouted and gracile specimens previously referred to Belodon plieningeri MEYER, 1844 actually represent a species of Nicrosaurus, here referred to as Nicrosaurus species B. A hitherto undescribed skull provides important missing information on the temporal region in this taxon. Nicrosaurus species B is more derived than Nicrosaurus kapf in having, among more uncertain characters, a more elongated squamosal with a pointed squamosal tip and a narrower supratemporal fenestra. Nicrosaurus species B shows the same two intraspecific morphotypes regarding skull width, but, additionally, a significant variation of the shorter prenarial crest can be observed. Additional cranial data is provided to characterise the highly derived Mystriosuchus planirostris (MEYER, 1863), the type species of the genus. Previous suggestions that a particular skull represents a different species of Mystriosuchus are confirmed. The occipital aspect of this skull is redescribed, and a new reconstruction of the braincase is presented. The hitherto unnamed species is distinguished by numerous cranial characters, including details of the temporal region, an orbitosphenoid, a supernumerary bone in the occipital region, and possibly a premaxillary crest. A phylogenetic analysis of 22 phytosaur taxa based on 49 characters using PAUP was conducted. As a preliminary result, the Paleorhininae were found not to be monophyletic as previously suggested, but to represent the paraphyletic stem-group of all other phytosaurs (Phytosauridae). Secondly, Mystriosuchus is not closely related to any non-phytosaurid phytosaur, but the most derived Phytosauridae forming a Glade with Pseudopalatus pristinus and Arribasuchus buceros

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.

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