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Article Reference Contribution of Asia to the evolution and paleobiogeography of the earliest modern mammals
The mammals, inconspicuous during the dinosaur period, saw an increase in their size and number of species after the extinction of these giants sixty-five million years ago. This was the beginning of the Age of Mammals. But it was only at the beginning of the Eocene fifty-five million years ago during an extremely fast and intense global warming called PETM (Paleocene Eocene Thermal Maximum) when their diversity exploded. New groups then suddenly appeared on the three northern continents via intercontinental land bridges across which they made important dispersals. These new groups, called “modern mammals”, consist of rodents, lagomorphs, perissodactyls, artiodactyls, cetaceans, primates, carnivorans and bats. Although these eight groups represent 83 % of the extant mammal species diversity, their ancestors are still unknown. A short overview of the knowledge and recent progress on this research is here presented on the basis of Belgian studies and expeditions, especially in India and China.
Located in Library / RBINS Staff Publications
Article Reference Conserving large populations of lions – the argument for fences has holes
Packer et al. reported that fenced lion populations attain densities closer to carrying capacity than unfenced populations. However, fenced populations are often maintained above carrying capacity, and most are small. Many more lions are conserved per dollar invested in unfenced ecosystems, which avoid the ecological and economic costs of fencing.
Located in Library / RBINS Staff Publications
Article Reference Stratigraphic and paleoenvironmental analysis of the Rupelian-Chattian transition in the type region: evidence from dinoflagellate cysts, foraminifera and calcareous nannofossils.
Located in Library / RBINS Staff Publications
Article Reference Danian/Selandian boundary stratigraphy, paleoenvironment and Ostracoda from Sidi Nasseur, Tunisia.
Located in Library / RBINS Staff Publications
Article Reference Paleoenvironmental change at the Danian-Selandian transition in Tunisia: planktic fioraminifera, calcareous nannofossil and organic-walled dinoflagellate cyst records
Located in Library / RBINS Staff Publications
Article Reference Danian/Selandian boundary criteria and North Sea Basin-Tethys correlations based on calcareous nannofossil and foraminiferal trends in SW France.
Located in Library / RBINS Staff Publications
Article Reference In search of the latest Danian Event in a paleobathymetric transect off Kasserine Island (North-Central Tunisia).
Located in Library / RBINS Staff Publications
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
Inbook Reference Palynology, paleoenvironments and organic carbon isotope evolution in lagoonal Paleocene/Eocene boundary settings in North Belgium.
Located in Library / RBINS Staff Publications
Inbook Reference The Eocene/Oligocene Boundary in the North Sea Area: A Sequence Stratigraphic Approach
Located in Library / RBINS Staff Publications