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Article Reference Ammonite extinction and nautilid survival at the end of the Cretaceous
Located in Library / RBINS Staff Publications
Article Reference Ammonites from the Dababiya Quarry Corehole: Taxonomic notes and age assessment
We describe a small collection of ammonites from the Dababiya Quarry corehole. It is almost entirely composed of heteromorph ammonites, in particular of scaphitids and baculitids. The presence of Indoscaphites pavana (Forbes 1848),which is for the first time reported from Egypt, points to a late to possibly latest Maastrichtian age for the interval DBD 80.36–DBD 99.11 of the Dababiya Quarry core. This is corroborated by preliminary data on planktonic foraminifera.
Located in Library / RBINS Staff Publications
Inproceedings Reference Ammonites on the brink of extinction
Keynote of session Cretaceous II, presented by Neil Landman on 09/09/2014 of 9th ISCPP Zurich, Switzerland.
Located in Library / RBINS Staff Publications
Inproceedings Reference Ammonoids and anoxia from the Belgian Frasnian: the Carrière de Lompret section
Located in Library / RBINS Staff Publications 2018
Article Reference Amphibians and squamate reptiles from the late Pleistocene of the “Caverne Marie-Jeanne” (Hastière-Lavaux, Namur, Belgium): Systematics, paleobiogeography, and paleoclimatic and paleoenvironmental reconstructions
Archeological sites usually provide important information about the past distribution ofsmall vertebrate fauna, and by extension about past terrestrial environments and climatein which human activities took place. In this context, Belgium has an interesting location innorthwestern Europe between the fully studied zooarcheological records of Germany andEngland. We present here the revision of the late Pleistocene (Marine Isotope Stages 3 and 2)collection of the “Caverne Marie-Jeanne” (Hastière-Lavaux, Namur), studied by Jean-ClaudeRage in the 1970s and the revision of the whole “indeterminate” small vertebrate materialsfrom the “Caverne Marie-Jeanne” stored in the Royal Belgian Institute of Natural Sciences(RBINS) Quaternary collections in search of more herpetofaunal remains. It is now by farthe largest late Pleistocene collection at RBINS with more than 20,500 recognized bonesof amphibians and reptiles and covering the last 60,000 years. The faunal list comprisestwo urodeles (Lissotriton gr. L. vulgaris and Salamandra salamandra), four anurans (Bufo gr.B. bufo-spinosus, Epidalea calamita, Rana temporaria and Rana cf. R. arvalis), three lizards(Lacerta cf. L. agilis, Zootoca vivipara and Anguis gr. A. fragilis), and three snakes (Natrix gr.N. natrix, Coronella austriaca, and Vipera berus). This study represents the first fossil record in Belgium for L. gr. L. vulgaris, R. arvalis, Z. vivipara, N. gr. N. natrix and C. austriaca. As awhole, this assemblage suggests a patchy humid landscape under colder and dryer climaticconditions in comparison with present ones. This study also underlines the necessity of aprimary separation in larger taxonomical categories by the specialist itself.
Located in Library / RBINS Staff Publications 2019
Article Reference Amphidromus setzeri, a new species (Gastropoda: Camaenidae) from Vietnam
Located in Library / RBINS Staff Publications 2016
Article Reference Amphidromus thachi, a new species (Gastropoda: Camaenidae) from Vietnam
Located in Library / RBINS collections by external author(s)
Article Reference An Amphibious Whale from the Middle Eocene of Peru Reveals Eatly South Pacific Dispersal of Quadrupedal Cetaceans.
Located in Library / RBINS Staff Publications 2019
Article Reference An annotated checklist of the Scatopsidae (Diptera) of the Botanic Garden Jean Massart at the outskirts of Brussels (Belgium)
Located in Library / RBINS Staff Publications 2023 OA
Article Reference An expanded lower Eocene shelf sequence from the eastern Aquitaine Basin, SW France: stratigraphy and δ18O / δ13C excursions
The early Eocene is characterized by a succession of orbitally-controlled global stable carbon isotope excursions, with some being linked to climatic and related biotic perturbations. The impact of these isotopic excursions has been primarily studied in deep-sea sections under comparably stable conditions. In order to investigate the impact of global post-PETM isotopic signals on shallow marine settings, the Ypresian neritic ʻBlue Marls’ of the Corbières (SW France) were investigated. High-resolution records of microfossil biota and stable carbon and oxygen isotopes pinpoint biostratigraphic, paleoecologic and geochemic constraints. Calcareous nannofossil biostratigraphy positions the sequence in the upper part of zone NP11, possibly ranging into basal NP12, which is conformable with larger benthic foraminifera data indicating shallow benthic zone SBZ8. This implies a time span of about 0.4 Myr and high overall sedimentation rates of about ~ 32 cm/kyr for the section. A shallowing upward trend from outer neritic to coastal settings is observed in the development of the lithostratigraphy and the microfossil assemblage. The assemblages can be subdivided in seven larger biofacies and four ostracod assemblage zones. The lower third of the section is characterized by strongly fluctuating and partly high plankton/benthos-ratios for neritic settings. A final pronounced peak in plankton occurrence is associated with strong decrease of benthic biota, suggesting anoxic conditions in the outer neritic environment. Several local negative δ13C- and δ18O-excursions can be identified in the section. The upper, most pronounced and consistent negative δ13C excursion is tentatively linked to global carbon isotope excursion K (ETM3) based on the biostratigraphic constraints.
Located in Library / RBINS Staff Publications