International audienceke sediment DNA to trace past landscape changes (plant DNA), agricultural activities(plant, mammal and bacteria DNA) as well as the human presence (human-specific bacteriaDNA). However, as all sedimentologists know, the sedimentation in a lake can vary temporallyand spatially depending of the variations of processes at the origin of the sedimentformation. Moreover, depending on the geological, topographical, climatic and ecologicalcontexts, the sedimentation can be very different from a lake to another. These lake sedimentscharacteristics might affect the aDNA archiving in a various ways including potentialbiases related to both, the taphonomic processes (DNA source, transfer and deposit) andthe analytical process. Con...