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.
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RBINS Staff Publications 2019
Climate change not only alters ocean physics and chemistry but also affects the biota. Larval dispersal patterns from spawning to nursery grounds and larval survival are driven by hydrodynamic processes and shaped by (a)biotic environmental factors. Therefore, it is important to understand the impacts of increased temperature rise and changes in wind speed and direction on larval drift and survival. We apply a particle-tracking model coupled to a 3D-hydrodynamic model of the English Channel and the North Sea to study the dispersal dynamics of the exploited flatfish (common) sole (Solea solea). We first assess model robustness and interannual variability of larval transport over the period 1995-2011. Then, using a subset of representative years (2003-2011), we investigate the impact of climate change on larval dispersal, connectivity patterns and recruitment at the nursery grounds. The impacts of five scenarios inspired by the 2040 projections of the Intergovernmental Panel on Climate Change are discussed and compared with interannual variability. The results suggest that 33% of the year-to-year recruitment variability is explained at a regional scale and that a 9-year period is sufficient to capture interannual variability in dispersal dynamics. In the scenario involving a temperature increase, early spawning and a wind change, the model predicts that (i) dispersal distance (+70%) and pelagic larval duration (+22%) will increase in response to the reduced temperature (–9%) experienced by early hatched larvae, (ii) larval recruitment at the nursery grounds will increase in some areas (36%) and decrease in others (-58%), and (iii) connectivity will show contrasting changes between areas. At the regional scale, our model predicts considerable changes in larval recruitment (+9%) and connectivity (retention -4% and seeding +37%) due to global change. All of these factors affect the distribution and productivity of sole and therefore the functioning of the demersal ecosystem and fisheries management.
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RBINS Staff Publications 2018