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preserved in soils has the potential to serve as a complementary proxy to charcoal facilitating the reconstruction performed on a selection of both insects and charcoal and a time-since-death index was developed to evaluate layers but were more abundant in the upper ones as with charcoal. Whereas radiocarbon dating did not work insect remains the time-since-death index showed a consistent relationship between increasing degradation reconstructing the past trajectories of old-growth forests? A study case from the Northern Central Pyrenees (France)
composition with major increases in cereals and other anthropogenic indicators. This signals a clear intensification increasingly homogenised dominated by a few widespread species. As a result both REVEALS evenness and spatial impacts on biodiversity across the Holocene epoch. To enhance our understanding of current changes in diversity Vegetation Estimates from Large Sites model have been used to explore spatiotemporal changes in vegetation and time windows covering the period from 11.7 ka cal BP to present . Space-time constrained clustering of the vegetation composition and diversity across Europe? A pollen-based spatio-temporal approach
Italy 1829 combined with those of Monoun 1984 and Nyos 1986 in Cameroon allow to propose a grid of degassing authorities. Pavin described as a marvelous lake with sudden storms with thunder and lightnings is feared beginning to be surveyed. A recent modelling of sudden lake degassing confirms that Pavin area is a potential Degassing maar lakes were thought to be a new natural hazard until the Nyos Lake catastrophe 1986 . Historical clouds 1550 1750 associated with reported sudden neurologic diseases similar to those observed at Albano and confirms that Lake Pavin remains a potential hazard, providing a model for assessing risks in other Degassing maar lakes were considered a new natural hazard until the Nyos Lake catastrophe in 1986, but of these phenomena over five centuries, combined with recent environmental research, reveals past degassing (Auvergne, France), for the Last Two Thousand Years - A Comprehensive Study of Volcanic Phenomena
investigations remains a main issue. This study introduces a novel method to estimate soil moisture directly approaches to correct field data from geochemical mapping in diverse environments including a coastal region region in Portugal and a mountainous region in France. Our findings demonstrate that this simple efficient Uestimated r2 0.9715 . The model effectively corrected up to 70 of moisture-induced errors in metal concentrations least 55 in wetter soils France . This study offers a cost-effective efficient solution for employing pXRF in situ portable X-ray spectrometer measurements: A novel approach for correcting geochemical data across
construit à partir de 1667 et mis en service dès 1681 était destiné à relier l océan Atlantique à la mer existants - du XVIe siècle à aujourd hui à l échelle mondiale. Ce colloque a pour finalité de dégager des des enseignements permettant de contribuer à répondre aux défis de demain environnementaux sociaux et leurs divergences dans leur trajectoire passée ou à venir. lien vers le site du colloque Programme Télécharger service politiques contractuelles patrimoine culture à Voies navigables de France Sud-Ouest Philippe Valette gouvernance, usages et environnement des canaux d'hier à demain
In a world of drastic climatic and ecological changes our knowledge of how the environment influenced can contribute to connecting small-scale environment-induced influences on hominins to large-scale patterns behaviour is of the utmost importance. Archaeology plays a key role as it is the only discipline that studies studies empirical evidence of past societies responses to environmental change. Computational models generating for understanding the archaeological record and how these factors shaped the dispersal of hominins out models and simulations help archaeology understand how environmental changes influenced hominin dispersal Changing Movements in a Changing World: Modelling Early Pleistocene and Early Middle Pleistocene Climatic
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