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Inproceedings Reference Foraminiferal Biofacies Analysis of the Boom Clay Formation in the Rupel area (Oligocene, Belgium) and Correlation with the Mainz Basin (Germany).
Located in Library / RBINS Staff Publications
Article Reference Foraminiferen und Ostrakoden im Ostfriesischen Wattenmeer – Ein Beitrag zur Meeresspiegelrekonstruktion.
Located in Library / RBINS Staff Publications 2019
Article Reference Forecasting fish distribution along stream networks: brown trout (Salmo trutta) in Europe
Aim Species inhabiting fresh waters are severely affected by climate change and other anthropogenic stressors. Effective management and conservation plans require advances in the accuracy and reliability of species distribution forecasts. Here, we forecast distribution shifts of Salmo trutta based on environmental predictors and examine the effect of using different statistical techniques and varying geographical extents on the performance and extrapolation of the models obtained. Location Watercourses of Ebro, Elbe and Danube river basins (c. 1,041,000 km2; Mediterranean and temperate climates, Europe). Methods The occurrence of S. trutta and variables of climate, land cover and stream topography were assigned to stream reaches. Data obtained were used to build correlative species distribution models (SDMs) and forecasts for future decades (2020s, 2050s and 2080s) under the A1b emissions scenario, using four statistical techniques (generalised linear models, generalised additive models, random forest, and multivariate adaptive regression). Results The SDMs showed an excellent performance. Climate was a better predictor than stream topography, while land cover characteristics were not necessary to improve performance. Forecasts predict the distribution of S. trutta to become increasingly restricted over time. The geographical extent of data had a weak impact on model performance and gain/loss values, but better species response curves were generated using data from all three basins collectively. By 2080, 64% of the stream reaches sampled will be unsuitable habitats for S. trutta, with Elbe basin being the most affected, and virtually no new habitats will be gained in any basin. Main conclusions More reliable predictions are obtained when the geographical data used for modelling approximate the environmental range where the species is present. Future research incorporating both correlative and mechanistic approaches may increase robustness and accuracy of predictions.
Located in Library / RBINS Staff Publications
Misc Reference Forest arthropod biodiversity from root tips to treetop
Located in Library / RBINS Staff Publications
Article Reference Foreword for the thematic volume of the PalEurAfrica project international symposium Evolution and paleoenvironment of early modern vertebrates during the Paleogene
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Located in Library / RBINS Staff Publications 2021
Article Reference Foreword. In: SCHÖN, I., P. VAN DIJK & K. MARTENS (Eds.), Lost Sex
Located in Library / RBINS Staff Publications
Article Reference Formation of the Zeebrugge Coastal Turbidity Maximum: The role of uncertainty in near-bed exchange processes.
Located in Library / RBINS Staff Publications 2020
Article Reference Fossil and Modern Ostracoda from Ancient Lakes. In: J.A. HOLMES & A. CHIVAS (eds.), The Ostracoda: Applications in Quaternary Research
Located in Library / RBINS Staff Publications
Article Reference Fossil bear bones in the Belgian Upper Palaeolithic: the possibility of a proto-bear ceremonialism
Located in Library / RBINS Staff Publications
Article Reference Fossil bog soils (`dwog horizons') and their relation to Holocene coastal changes in the Jade Weser region, southern North Sea, Germany
After the deceleration of the postglacial marine transgression, the German North Sea coast was subject to deposition of a complex pattern of subtidal to terrestrial facies. This study aims at reconstructing these facies changes in the `Land Wursten' region (Lower Saxony) by focussing on so-called dwog horizons (incipient soil horizons of the pre-engineered salt marshes). We explore their implications for relative sea-level reconstructions and their indication for early settlement activities. Archive drilling data (1960, provided by the `Landesamt für Bergbau, Energie und Geologie') were analysed to create five high-resolution stratigraphic cross sections. Three new drilling records were subjected to sedimentological and microfaunal investigations and interpreted to verify and calibrate the archive data. Two dwog horizons were found and 14C-AMS dated. We found basal salt marsh deposits inundated by a high-energy event and covered by tidal flat sediments. The thick tidal flat unit is again overlain by salt marsh deposits indicating the transition from a shallow marine to a terrestrial environment where dwogs were developed and covered by episodic marine incursions. The ages of the dwogs (1128–969 cal BC; cal AD 1426–1467) do not correlate with known layers of adjacent settlement sites and are critically discussed. However, we show that they correlate with phases of stagnant regional relative sea level (RSL) and can be used as RSL indicators. The combined archive and modern data provide valuable information for the RSL reconstruction and palaeoenvironmental changes. However, further research is recommended to accomplish more detailed information about coastal response during the Holocene sea-level changes and implications for settlement dynamics.
Located in Library / RBINS Staff Publications 2018