Éditeur(s) : HAL CCSD
Résumé : International audience
The Imiter silver mine is a world-class deposit located in the Easternpart of the Anti-Atlas (Morocco). The deposit is hosted by Cryogenianblack shales and Ediacaran volcanics, and unconformablyoverlain byPaleozoic sedimentary rocks. The paragenetic sequence for the ganguemineral is composedby amacroscopically white quartz (Qz1) associatedwith the deposition of galena and scarce silver mineralsas matrixof hydraulic breccias, followed by a grey quartz (Qz2) associated withthe main silver deposition event and a first generation of scarcedolomite(Dol1). A third episode is characterized by massive pink dolomite precipitation(Dol2) with minor quartz (Qz3) and base metals. Finally, asurficial event affects the mineralisation and is responsible for a secondaryore enrichment.Microthermometry study coupled with Raman analyses reveals thatfluid inclusions are CaCl2-dominated. The general trend is a decreaseof temperature from Qz1 (250°C) to Dol1 (80°C) then Dol 2 (probablybelow 70°C) depositions. Fluid salinity increases from Qz1 (6.3 to 19.0wt % NaCleq) to Dol1 (27.2 % wt NaCleq), and decreases with the precipitationof Dol2 associated with quartz 3 (15 %wt NaCleq). The 18Oisotopic composition of fluids in equilibrium with quartz and dolomitesuggestsamagmatic,metamorphic and/or basinal origin for the fluid atthe origin of Qz1, and that meteoric / surficial basinal brinesmay be atthe origin of Dol2.The proposed model to explain the ore forming processes in Imiter is amixing of Ca-brines, probably providing chloride complexes, with a hotNaCl fluid of lower salinity, leading to the precipitation of silver.Theresults favour the important role of calcic brines, whose origin remainsmatter to debate in such a giant depositand for whom age of emplacementis strongly discussed.
24 ème Réunion des sciences de la Terre 2014
Pau, France

insu-01080858
https://hal-insu.archives-ouvertes.fr/insu-01080858

Éditeur(s) : HAL CCSD Nature Publishing Group
Résumé : International audience
Activation of cell signaling by reactive chemicals and pollutants is an important issue for human health. It has been shown that lipophilic nitro-benzoxadiazole (NBD) compounds rapidly move across the plasma membrane and enhance Epidermal Growth Factor Receptor (EGFR) tyrosine phosphorylation in cancer cells. Unlike ligand-dependent activation, the mechanism of this induction relies on the generation of hydrogen peroxide, which is involved in the activation of the catalytic site of the receptor and the inactivation of protein tyrosine phosphatase PTP-1B. Production of H2O2 during redox transformation of NBD compounds is associated with the transition of a monomeric form of Cu/Zn superoxide dismutase 1 (SOD1) to stable dimers. The highly stable and functionally active SOD1 dimer, in the absence of adequate activities in downstream reactions, promotes the disproportionate production and accumulation of intracellular hydrogen peroxide shortly after exposure to NBD compounds. The intrinsic fluorescence of small compounds was used to demonstrate their binding to SOD1. Our data indicate that H2O2 and concomitantly generated electrophilic intermediates behave as independent entities, but all contribute to the biological reactivity of NBD compounds. This study opens a promising path to identify new biomarkers of oxidative/electrophilic stress in the progression of cancer and other diseases
ISSN: 2045-2322

hal-01279094
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01279094
DOI : 10.1038/srep21088
PUBMED : 26883293