Search results for "microbialite"

showing 10 items of 12 documents

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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COMMENT TO LEHRMANN ET AL. NEW SECTIONS AND OBSERVATIONS FROM THE NANPANJIANG BASIN, SOUTH CHINA

2016

In the study of Earth-surface environmental processes during the events associated with the Permian–Triassic boundary, a key issue is the nature of the latest Permian pre-extinction surface in shallow marine limestones in numerous sites, principally within the Tethyan realm. Sediments below this surface pre-date the extinction event, so that the limestones comprising these latest Permian facies contain diverse fossil remains of organisms that lived just before the extinction. At all reported sites, this surface is disconformably overlain by post-extinction sediments, which contain microbialites in many places, particularly in Tethys. The nature of the youngest pre-extinction surface remains…

010506 paleontologyPermianOutcropStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontology14. Life underwaterGeopetal sediemntComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesExtinction eventExtinctionPendent CementsMicrobialitePaleontologyOcean acidification13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSubaerial[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyErosional historyPALAIOS
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Integrative analysis of the mineralogical and chemical composition of modern microbialites from ten Mexican lakes: What do we learn about their forma…

2021

International audience; Interpreting the environmental conditions under which ancient microbialites formed relies upon comparisons with modern analogues. This is why we need a detailed reference framework relating the chemical and mineralogical compositions of modern microbialites to the physical and chemical parameters prevailing in the environments where they form. Here, we measured the chemical, including major and trace elements, and mineralogical composition of microbialites from ten Mexican lakes as well as the chemical composition of the surrounding waters. Saturation states of lakes with different mineral phases were systematically determined and correlations between solution and so…

(Mg-)calcite010504 meteorology & atmospheric sciencesREE+YDolomiteGeochemistryalkalinityengineering.material010502 geochemistry & geophysics01 natural sciencesaragonitechemistry.chemical_compoundmonohydrocalciteGeochemistry and Petrologyhydromagnesite0105 earth and related environmental sciencesCalciteAragoniteTrace elementmicrobialitesAuthigenic6. Clean waterDiagenesisMonohydrocalcitecrater lakechemistry13. Climate actionkerolite[SDE]Environmental SciencesengineeringCarbonate
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Smithian shoreline migrations and depositional settings in Timpoweap Canyon (Early Triassic, Utah, USA).

2014

AbstractIn Timpoweap Canyon near Hurricane (Utah, USA), spectacular outcrop conditions of Early Triassic rocks document the geometric relationships between a massive Smithian fenestral-microbial unit and underlying, lateral and overlying sedimentary units. This allows us to reconstruct the evolution of depositional environments and high-frequency relative sea-level fluctuations in the studied area. Depositional environments evolved from a coastal plain with continental deposits to peritidal settings with fenestral-microbial limestones, which are overlain by intertidal to shallow subtidal marine bioclastic limestones. This transgressive trend of a large-scale depositional sequence marks a lo…

010506 paleontologyOutcropEarly Triassicshoreline migrationsEarly Triassic010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentrelative sea levelPaleontology14. Life underwaterSea level0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyCanyongeographySW Utahgeography.geographical_feature_categoryTerrigenous sedimentSmithianmicrobialitesGeology15. Life on land13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologydepositional environments
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Microbial deposits in the aftermath of the end-Permian mass extinction: A diverging case from the Mineral Mountains (Utah, USA)

2015

40 pages; International audience; The Lower Triassic Mineral Mountains area (Utah, USA) preserves diversified Smithian and Spathian reefs and bioaccumulations that contain fenestral-microbialites and various benthic and pelagic organisms. Ecological and environmental changes during the Early Triassic are commonly assumed to be associated with numerous perturbations (productivity changes, acidifica-tion, redox changes, hypercapnia, eustatism and temperature changes) post-dating the Permian–Triassic mass extinction. New data acquired in the Mineral Mountains sediments provide evidence to decipher the relationships between depositional environments and the growth and distribution of microbial …

Microbially induced sedimentary structurereef evolutionStratigraphyEarly Triassic10125 Paleontological Institute and Museum[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphySedimentary depositional environmentDepositional environmentsPaleontologyUtah14. Life underwaterReef1907 GeologyPermian–Triassic extinction event[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyOncoliteExtinction eventRed bedsgeographySpathiangeography.geographical_feature_categoryEarly Triassic recoverySmithianmicrobialitesGeology[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences15. Life on land560 Fossils & prehistoric life[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy1913 Stratigraphy[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Genesis of the Lower Triassic bonebeds from Gogolin (S Poland): The impact of microbial mats on trapping of vertebrate remains

2017

Three bone-bearing horizons, consis ting of seven bone-bearing beds with fi sh and reptile remains, were recently discovered in the Uppermost Röt (Buntsandstein, Lower Tri assic) peritidal and shallow marine carbonates in the vi- cinity of Gogolin (S Poland). The aim of this study is to reco gnize the genesis and deposi tional environments of the bonebeds. Detailed fi eldwork, microfacies analysis, and SEM-EDS anal ysis reveal that the vertebrate remains occur to a great extent alongside evidence for former microbial activity. The reptile remains represent at least Dactylosaurus and Nothosaurus (Sauropterygia) genera, while the fi sh remains belong to the Chondrichthyes and Actinopterygii. …

Dactylosaurus010506 paleontologyIntertidal zonebonebed010502 geochemistry & geophysicsOceanography01 natural sciencesSedimentary depositional environmentPaleontologyNothosaurusstromatolitesMicrobial matEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesSabkhageographygeography.geographical_feature_categorybiologyEcologyActinopterygiimicrobialitesPaleontologybiology.organism_classificationtidal flatSauropterygiaLower TriassicGeologyPalaeogeography Palaeoclimatology Palaeoecology
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Structure and evolution of a Messinian mixed carbonate-siliciclastic platform: the role of evaporites (Sorbas Basin, South-east Spain).

2010

36 pages; International audience; The Sorbas Member is a late Messinian complex sedimentary systemthat formed immediately following deposition of the Messinian evaporites in the Sorbas Basin (South-east Spain). This work describes the sequence architecture and facies organization of a continuous kilometre long, alluvial fan to open platform transect near the village of Cariatiz in the north-east of the basin. The postevaporitic Cariatiz platform was a mixed carbonate-siliciclastic system composed of four intermediate-frequency, fifth-order depositional sequences (Depositional Sequences 1 to 4) arranged in an overall prograding trend. The intense fracturing and brecciation of these deposits …

010506 paleontologyEvaporiteStratigraphy[SDE.MCG]Environmental Sciences/Global Changeslate Messinian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentPaleontologyooidsooids.14. Life underwater0105 earth and related environmental sciencesmixed carbonate/siliciclastic platform[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryAlluvial fanmicrobialitesGeology[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics15. Life on landEvaporite collapse and deformation[ SDE.MCG ] Environmental Sciences/Global Changes[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesOoidSiliciclasticSedimentary rockProgradationGeology
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Dépôts carbonatés microbiens en domaine lacustre et fluviatile : fabriques et facteurs de contrôle

2020

The non-marine carbonates related to microbial activity display a large range of morphologies and compositions and accumulate in various settings (freshwater, alkaline, and saline lakes, fluvial environments, thermal and freshwater springs, …). The variety of non-marine microbial carbonates and their particularity led to propose numerous and complex terminologies and classifications, making their use complicated and restrictive for the interpretation of depositional settings. Mineralization of these carbonates results from the interaction between biotic factors (intrinsic) and environmental factors (extrinsic and external) at multi-scales. The first aim of this work was to characterize morp…

FabricControlling factorsEnvironnement fluviatileMicrobialite[SDU.OTHER] Sciences of the Universe [physics]/OtherFacteurs de contrôleTufaLacustrine setting[SDU.OTHER]Sciences of the Universe [physics]/OtherFluvial settingEnvironnement lacustreFabrique
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Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?

2012

International audience; Ocean acidification in modern oceans is linked to rapid increase in atmospheric CO 2 , raising concern about marine diversity, food security and ecosystem services. Proxy evidence for acidification during past crises may help predict future change, but three issues limit confidence of comparisons between modern and ancient ocean acidification, illustrated from the end-Permian extinction, 252 million years ago: (1) problems with evidence for ocean acidification preserved in sedimentary rocks, where proposed marine dissolution surfaces may be subaerial. Sedimentary evidence that the extinction was partly due to ocean acidification is therefore inconclusive; (2) Fossils…

010504 meteorology & atmospheric sciencesEffects of global warming on oceansocean acidification010502 geochemistry & geophysics01 natural sciencesEcosystem services14. Life underwaterPermian–Triassic extinction event0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyHigh rateend-Permian extinctionocean acidification; end-Permian extinction; microbialite; ocean buffer; stylolitestylolitelcsh:QE1-996.5fungiBiotaOcean acidificationlcsh:GeologyOceanographymicrobialite13. Climate actionSubaerialGeneral Earth and Planetary SciencesSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontologyocean bufferGeologygeographic locations
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Étude multi-isotopique de microbialites actuels au sein d'analogues Précambriens (lacs de cratères volcaniques alcalins)

2021

[SDU] Sciences of the Universe [physics]lacs alcalinsgéochimieMicrobialitesArchéenisotopes
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