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12 Sep 2025 Job Information Organisation/Company CNRS Department Laboratoire Jean-Alexandre Dieudonné Research Field Mathematics History » History of science Researcher Profile Leading Researcher
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20 Sep 2025 Job Information Organisation/Company CNRS Department Institut Montpelliérain Alexander Grothendieck Research Field Mathematics History » History of science Researcher Profile First Stage
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appendages using the (halo)archaea as a model. Studying the infection mechanisms of archaeal viruses can provide insight into the evolutionary history of viruses and help to understand adaptation to extreme
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Max Planck Institute for Human Cognitive and Brain Sciences, Leipzig | Leipzig, Sachsen | Germany | 6 days ago
, mathematics, electrical engineering etc.). Excellent programming skills (Python, Matlab) are required. The candidate will be embedded in the Neural Computation Group at the Max Planck Institute for Human
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performance and explore the use of an ultrasonic sensor for real-time monitoring. Experiment with ultrasonic sensors for real-time seal gap measurement. Combine experimental research and mathematical modelling
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on the analysis and interpretation of the GNSS observations as well as on the application of geological and glacial-geomorphological findings for the reconstruction of ice-load history in Antarctic regions
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efficient LAFP process simulations of large structures while still capturing the relevant thermal history with sufficient accuracy. Develop and implement an accurate and efficient optical model to calculate
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appendages using the (halo)archaea as a model. Studying the infection mechanisms of archaeal viruses can provide insight into the evolutionary history of viruses and help to understand adaptation to extreme
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working across the Cognitive Neuroscience Department and the Mental Health and Neuroscience Research Institute. The mapping of local differences in the brain’s cortical architecture has a long history. The
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modelling of the GIA process and elaborate on constraints regarding geological and glacial-geomorphological findings for the reconstruction of ice-load history in Antarctic regions as well as the geodynamic