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Article Reference Where do adaptive shifts occur during invasion? A multidisciplinary approach to unravelling cold adaptation in a tropical ant species invading the Mediterranean area
Evolution may improve the invasiveness of populations, but it often remains unclear whether key adaptation events occur after introduction into the recipient habitat (i.e. post-introduction adaptation scenario), or before introduction within the native range (i.e. prior-adaptation scenario) or at a primary site of invasion (i.e. bridgehead scenario). We used a multidisciplinary approach to determine which of these three scenarios underlies the invasion of the tropical ant Wasmannia auropunctata in a Mediterranean region (i.e. Israel). Species distribution models (SDM), phylogeographical analyses at a broad geographical scale and laboratory experiments on appropriate native and invasive populations indicated that Israeli populations followed an invasion scenario in which adaptation to cold occurred at the southern limit of the native range before dispersal to Israel. We discuss the usefulness of combining SDM, genetic and experimental approaches for unambiguous determination of eco-evolutionary invasion scenarios.
Located in Library / RBINS Staff Publications
Article Reference Terrestrial mammals as biostratigraphic indicators in upper Paleocene-lower Eocene marine deposits of the southern North Sea Basin
Teeth of terrestrial mammals found in shallow marine deposits of the late Paleocene and early Eocene in the southern North Sea Basin (Belgium, northern France and southeastern England) have been used as biostratigraphic indicators. Analyses indicate that the age of the continental Walbeck mammal fauna (Germany) is close to that of the Upper Selandian Heers Formation of Belgium (NP4-5). The MP6 referencelevel of Cernay (France) is probably correlated with the lower part of NP9 (late Thanetian). The MP7 – MP8 + 9 intermediate faunas of Meudon and Pourcy could be partly equivalent in age to Biochron NP10. The MP8 + 9 reference-level of Avenay corresponds to the upper part of the London Clay and Kortrijk Formations, which are of late middle Ypresian age (lower NP12), or to the lower part of the Wittering and Tielt Formations, which are dated early late Ypresian (middle NP12). The MP10 Grauves and Prémontré faunas (France) are correlated with the NP13 Upper Wittering Formation. The taphonomy of terrestrial mammals discovered in marine deposits indicates several origins of the material such as reworking, action of predators or fluvial transport.
Located in Library / RBINS Staff Publications
Article Reference The in situ Glyptostroboxylon forest of Hoegaarden (Belgium) at the Initial Eocene Thermal Maximum (55 Ma)
Located in Library / RBINS Staff Publications
Article Reference Paleocene-Eocene carbon isoltope excursion in organic carbon and pedogenic carbonate: direct comparision in a continental stratigraphic section
Located in Library / RBINS Staff Publications
Article Reference Les mammifères de l'Ypresien moyen du Bassin de Paris (niveau-repère MP8-9) sont-ils présents dès la limite Paléocène/Eocène de Dormaal (niveau-repère MP7, Belgique)?
Located in Library / RBINS Staff Publications
Article Reference Anatomy and phylogeny of the gavialoid crocodylian Eosuchus lerichei from the Paleocene of Europe
Located in Library / RBINS Staff Publications
Article Reference A new scincomorph lizard from the Paleocene of Belgium and the origin of the Scincoidea in Europe
Located in Library / RBINS Staff Publications
Article Reference Rapid Asia–Europe–North America geographic dispersal of earliest Eocene primate Teilhardina during the Paleocene–Eocene Thermal Maximum
Located in Library / RBINS Staff Publications
Article Reference High-resolution carbon isotope stratigraphy and mammalian faunal change at the Paleocene-Eocene boundary in the Honeycombs area of the Southern Bighorn Basin, Wyoming.
Located in Library / RBINS Staff Publications
Article Reference A mitochondrial phylogeographic scenario for the most widespread African rodent species , Mastomys natalensis
In order to evaluate the contribution of geological, environmental, and climatic changes to the spatial distri- bution of genetic variation of Mastomys natalensis, we analysed cytochrome b sequences from the whole dis- tribution area of the species to infer its phylogeographic structure and historical demography. Six well-supported phylogroups, differentiated during the Pleistocene, were evidenced. No significant correlation between genetic and geographic distances was found at the continental scale, and the geographic distributions of the observed phylogroups have resulted from extensive periods of isolation caused by the presence of putative geographic and ecological barriers. The diversification events were probably influenced by habitat contraction/expansion cycles that may have complemented topographic barriers to induce genetic drift and lineage sorting. According to our results, we propose a scenario where climate-driven processes may have played a primary role in the differ- entiation among phylogroups.
Located in Library / RBINS Staff Publications