6533b824fe1ef96bd1280a8f

RESEARCH PRODUCT

Distribution, redox state and (bio)geochemical implications of arsenic in present day microbialites of Laguna Brava, Salar de Atacama

Manuel ContrerasEmmanuelle GérardPascal PhilippotPieter T. VisscherPieter T. VisscherAntoine BergamaschiAlexander E. S. Van DriesscheMaria Sancho-tomásMaria Eugenia FariasAndrea SomogyiKadda Medjoubi

subject

0301 basic medicineBiogeochemical cycleMicroorganism030106 microbiologyOtras Ciencias de la Tierra y relacionadas con el Medio Ambientechemistry.chemical_elementSynchrotron-based X-ray imagingArsenicCiencias de la Tierra y relacionadas con el Medio AmbienteSYNCHROTRON-BASED X-RAY IMAGING03 medical and health sciencesStromatolitesMICROBIAL MATSGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMicrobial matsBiosignatureTrace metalMicrobial matBiosignatureArsenicComputingMilieux_MISCELLANEOUSBIOGEOCHEMICAL CYCLESGeologySorptionHypersaline lakeBiogeochemical cyclesBIOSIGNATURE030104 developmental biologychemistrySTROMATOLITES13. Climate actionEnvironmental chemistryARSENICGeologyCIENCIAS NATURALES Y EXACTAS

description

Understanding how microorganisms adapted to the high arsenic concentration present on early Earth requires understanding of the processes involved in the arsenic biogeochemical cycle operating in living microbial mats. To this end, we investigated a living microbial mat from Laguna Brava (Salar de Atacama, Chile), a hypersaline lake with high arsenic concentration, using an array of conventional geochemical techniques, such as X-ray diffraction, SEM-EDX and Confocal Laser Scanning Microscopy (CLSM), combined with state-of-the-art high resolution scanning imaging techniques, including X-ray micro-fluorescence (μXRF) and X-ray Absorption Near Edge Structure (XANES) mapping. This experimental approach allowed us to unravel the relationship between the microbial mat activity, mineral occurrence, arsenic speciation, distribution of major and trace elements and their relationship with the mineralogy and the exopolymeric substances (EPS). We show that As was not linked to Ca or Si, and only moderately related to Fe, resulting from sorption onto an iron (oxy)hydroxide mineral. In addition, we were able to identify organic-rich globules containing significant As but no other trace metal(loid)s, and determine the co-existence of As(III) and As(V). These observations strongly support the occurrence of microbially-mediated arsenic cycling in these microbial mats. Fil: Sancho Tomás, María. Institut de Physique Du Globe de Paris; Fil: Somogyi, Andréa. Soleil Synchrotron; Fil: Medjoubi, Kadda. Soleil Synchrotron; Fil: Bergamaschi, Antoine. Soleil Synchrotron; Fil: Visscher, Pieter T.. University of Connecticut; Estados Unidos. Université Bourgogne Franche-comté; Fil: Van Driessche, Alexander E.S.. Institut Des Sciences de la Terre, Grenoble; Fil: Gérard, Emmanuelle. Institut de Physique Du Globe de Paris; Fil: Farias, Maria Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Planta Piloto de Procesos Industriales Microbiológicos; Argentina Fil: Contreras, Manuel. Centro Ecologia Aplicada; Chile Fil: Philippot, Pascal. Institut de Physique Du Globe de Paris;

10.1016/j.chemgeo.2018.04.029https://hal.archives-ouvertes.fr/hal-02351114