0000000000247582

AUTHOR

Pieter T. Visscher

showing 5 related works from this author

Between a rock and a soft place: the role of viruses in lithification of modern microbial mats.

2021

10 pages; International audience; Stromatolites are geobiological systems formed by complex microbial communities, and fossilized stromatolites provide a record of some of the oldest life on Earth. Microbial mats are precursors of extant stromatolites; however, the mechanisms of transition from mat to stromatolite are controversial and are still not well understood. To fully recognize the profound impact that these ecosystems have had on the evolution of the biosphere requires an understanding of modern lithification mechanisms and how they relate to the geological record. We propose here viral mechanisms in carbonate precipitation, leading to stromatolite formation, whereby viruses directl…

Microbiology (medical)Geologic SedimentsBiogeochemical cycleviral lifestyleEarth sciencevirus–host interactionsGeologic recordMicrobiologyMESH: Host-Parasite InteractionsHost-Parasite InteractionsMESH: Viruses03 medical and health sciencesGeologic time scalebacteriophageVirologylytic/lysogenic cyclevirusesMicrobial matstromatoliteLithification030304 developmental biologyearly Earth0303 health sciencesBacteriabiology030306 microbiologyMESH: Virus Physiological PhenomenamicrobialitesBiosphereexopolymeric substances (EPS)MESH: Geologic Sedimentsbiology.organism_classificationEarly Earthmicrobial matMESH: BacteriaInfectious Diseases[SDV.MP]Life Sciences [q-bio]/Microbiology and ParasitologyStromatolite13. Climate actionCRISPRbiosignaturesVirus Physiological Phenomena
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Distribution, redox state and (bio)geochemical implications of arsenic in present day microbialites of Laguna Brava, Salar de Atacama

2018

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 …

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
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Formation of microbial organic carbonates during the Late Jurassic from the Northern Tethys (Amu Darya Basin, Uzbekistan): implications for Jurassic …

2020

23 pages; International audience; The Late Jurassic was a period of major global carbon cycle perturbations with episodes of anoxia leading to regional accumulation of organic matter in sediments worldwide. The Tubiegatan section (SW Gissar Mountains, Uzbekistan) located in the Northern Tethys, shows atypical organic-rich limestone and marl deposits (up to 6% of total organic carbon) marked by pronounced negative excursions of δ13Ccarb (amplitude of ca. 12‰) and δ13Corg (amplitude of ca. 4‰) recorded during the Middle Oxfordian (Transversarium Zone). A transdisciplinary approach including sedimentology, palynofacies characterization, mineralogy, organic and inorganic geochemistry was carrie…

microbial/laminated sediments52 anoxia010504 meteorology & atmospheric sciencesGeochemistryLate Jurassic02 engineering and technologyOceanography01 natural scienceschemistry.chemical_compoundAnoxia[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarl0202 electrical engineering electronic engineering information engineeringAmu Darya BasinOrganic matter14. Life underwaterMicrobial mat0105 earth and related environmental sciencesStable isotopesTotal organic carbonSabkhachemistry.chemical_classificationGlobal and Planetary Changegeographygeography.geographical_feature_category020206 networking & telecommunicationsorganic-rich carbonatesstable isotopes 5315. Life on landCretaceousPalynofacieschemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
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Oligo-Miocene lacustrine microbial and metazoan buildups from the Limagne Basin (French Massif Central)

2018

The Limagne Basin (French Massif Central) is an extensive continental lacustrine system accommodating microbial and metazoan buildups from Chattian to Aquitanian age. A description of these buildups and their associated biotic components in Grand Gandaillat and Crechy quarries provides insights into their spatio-temporal distribution patterns. Flats, cauliflowers, domes, cones and coalescent columnar morphologies have been identified with a main laminated mesofabric and laminated, columnar, filamentous and caddisfly-coated microfabrics. Two low-gradient margin models emerged based on the changes in the distribution, morphology and size of the microbial and metazoan-rich deposits through tim…

010504 meteorology & atmospheric sciencesGeochemistryCarbonatesVolcanismEcological successionStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesVolcanismMarlCycle ClimateEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryPaleontologyMassif15. Life on landTectonicTectonicsVolcanoSedimentary rockLacustrine/palustrine[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Geochemical evidence for arsenic cycling in living microbialites of a High Altitude Andean Lake (Laguna Diamante, Argentina)

2020

Arsenic is best known as an environmental toxin, but this element could also serve as a metabolic energy source to certain microorganisms. Moreover, As cycling may have driven microbial life on early Earth prior to oxygenation of the atmosphere. Still, little is known about the arsenic cycling processes occurring in the presence of microorganisms and the possible traces that could be preserved in the rock record. To advance our understanding of this we studied the geochemical proxies of microbial As metabolism in living microbialites from Laguna Diamante, a likely Precambrian ecosystem analogue (Catamarca, Argentina). In this study, we show that the coexistence of As(III) and As(V) strongly…

Carbonate010504 meteorology & atmospheric sciencesSynchrotron-based X-ray imagingchemistry.chemical_element010502 geochemistry & geophysicsGeologic record01 natural sciencesEarly lifechemistry.chemical_compoundPrecambrian[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryANDES LAKESGeochemistry and PetrologyExtremophileEcosystemArsenic cyclingArsenic0105 earth and related environmental sciencesEXTREMOPHILEEcologyMicrobialitesOtras Ciencias Naturales y ExactasGeologyARCHEAEEarly Earthchemistry13. Climate actionCarbonateCalciumARSENICCyclingCIENCIAS NATURALES Y EXACTASGeologyChemical Geology
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