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molecules using site-specific conjugation strategies. - Development of DNA origami scaffolds to spatially organize and orient proteins for structural studies by single-particle Cryo-Electron Microscopy
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chemistry synthesis (organic and coordination chemistry) - intercalation and exfoliation chemistry - synthesis in supercritical media - structural and spectroscopic characterisation - magnetic and
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developmental) and integrative neuroscience, the laboratory is structured around four main teams: - Cognition-Behavior-Context - Social Behaviors and Collective Dynamics - Physiological and Psychosocial Stress
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complexes with nucleic acids; 2) Evaluation of the delivry complexes for inhalation by Aerosol technology; 4) Analysis of the structure-activity relationship of dendrimers for nucleic acid delivery via
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polymerization and electropolymerization. The structures will be confirmed, for example, by 1H and 13C NMR titration, FTIR, mass spectrometry, UV-vis and fluorescence spectroscopy, electrochemistry, size exclusion
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and associated with biological processes such as the circadian rhythm. The aim of the project is to understand at a molecular level the impact of these modifications on the structure and dynamics
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surface-chemistry trends across selected metals and their oxides. These data will support the construction of a machine-learning force field tailored to NHC–surface systems, enabling large-scale molecular
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from the advantages offered by the CNRS. Where to apply Website https://emploi.cnrs.fr/Candidat/Offre/UMR5280-FRABES-003/Candidater.aspx Requirements Research FieldEngineeringEducation LevelPhD
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techniques; Structural and functional characterization of interfaces and junctions, in particular through nanoscale analyses; Development, adaptation, and optimization of experimental methodologies
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Postdoctoral researcher (M/F). Modeling damage during earthquakes. Comparison with geophysical data.
(# ANR-22-CE01-0028) funded by the ANR. This two-year project (01/04/26 to 31/03/28) aims to explore the link between the dynamics of rupture on seismic faults and the structure of the damage zone