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paleo studies. Furthermore, our knowledge of Holocene climate at high altitudes remains very limited (Jomelli et al., 2022). Monsoon proxies located at low altitudes show no direct links with glacier
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experimental methods are available and currently fully operational in the laboratory. Collaborative Environment: Centrifugal instabilities are not limited to magnetized plasma columns in the laboratory but also
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of the team are structured around 3 research aeras: • Research Area 1: On-line analytical methods via microfluidic devices for the quantification of air pollutants; • Research Area 2: Off-line analysis methods
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hand through individual sampling and genotyping, and on the other through eDNA analysis of river water, in order to test the relevance and limits of the eDNA approach for studying infraspecific genetic