Resilience of deep aquifer microbial communities to seasonal hydrological fluctuations. [PDF]
Giroud S +4 more
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Eco-Friendly Extraction of Phlorotannins from Padina pavonica: Identification Related to Purification Methods Towards Innovative Cosmetic Applications. [PDF]
Nour M +8 more
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Genetic diversity and conservation implications for European Griffon Vultures (Gyps fulvus): Insights from mitochondrial D-loop HVR1. [PDF]
Mereu P +27 more
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Predicting fiber content in herbivore fecal samples using a multispecies NIRS model. [PDF]
Rossa M +12 more
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A multi-Omic resource for exploring microbial eukaryotes in the meromictic freshwater Lake Pavin. [PDF]
Courtine D +11 more
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Variscan subduction of an Ordovician granite : the Lévézou massif, French Massif Central
International Journal of Earth Sciences, 2015The Variscan Belt is usually interpreted as the result of an oceanic subduction followed by continental collision. The subducted ocean is represented by eclogitic lenses enclosed in amphibolite-facies rocks. This rock assemblage, called the Leptyno-Amphibolic Group (LAG), is considered as a suture unit that separates two different continental fragments
Lotout, Caroline +5 more
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The Merinchal antimoniferous district (French Massif Central)
Periodico di Mineralogia, 2013This article presents the Merinchal antimoniferous district (French Massif Central) from the historical and metallogenic points of view. This small district has been mined in the early 20th century. Subsequent characterization of mineralized indexes occurred afterwards in the 1960's and 1980's.
Thiery, Vincent, Cartannaz, Charles
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Forest restoration in the French Massif Central Mountains
2004La restauration de la forêt est plutôt un fait récent dans le massif central. Au XIXème siècle, pratiquement toute la surface de terre était occupée par l'agriculture. Avec la spécialisation de l'agriculture et son intensification, beaucoup de terres agricoles ont été abandonnées. Elles ont été soit plantées avec des espèces résineuses (e.g.
Balandier, Philippe +2 more
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Imaging a mantle plume beneath the French Massif Central
Earth and Planetary Science Letters, 1995Abstract Teleseismic tomography is now widely recognised as a very powerful tool for studying the velocity structure of the lithosphere-asthenosphere system on both local and regional scales. A prime objective is to identify velocity perturbations and to constrain their location and intensity. Here we use the arrival times of P-waves from teleseismic
Michel Granet +2 more
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