Search results for "Lithification"

showing 10 items of 17 documents

Facies variations in response to Holocene sea-level and climate change on Bora Bora, French Polynesia: Unravelling the role of synsedimentary siderit…

2017

International audience; Five mixed carbonate-siliciclastic sedimentary facies were identified in the barrier-reef lagoon of Bora Bora using microfacies and statistical analyses of 70 sediment samples taken at high resolution from two vibrocores. Fades and fades successions were interpreted with respect to Holocene sea-level and climate changes. The windward lagoon core is characterized by sideritic marly wackestones and foraminifera-sideritic wackestones, deposited around 7700 years BP (years before present) during the early-mid Holocene transgression. At that time, extensive weathering and erosion of iron-bearing minerals from the volcanic island, due to a wetter climate, were expressed in…

010506 paleontology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaSideritechemistry.chemical_compoundGeochemistry and Petrology14. Life underwaterLithificationReefComputingMilieux_MISCELLANEOUSHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyGeologybiology.organism_classification6. Clean waterOceanographychemistry13. Climate action[SDE]Environmental SciencesSiliciclasticProgradationGeologyMarine transgression
researchProduct

The “chimney forest” of the deep Montenegrin margin, south-eastern Adriatic Sea

2015

A spectacular field of columnar carbonates has been discovered on the Montenegrin margin in the southern Adriatic Sea at a depth of about 450 m. The site exposes many columnar carbonates protruding from the substrate or abated on the bottom. Such carbonates attain maximum visible lengths of ca. 60 cm with diameters up to 20 cm; display an annular growth, and are either hollow or plugged by indurated sediment. Petrographic and geochemical analyses document the pervasive presence of dolomite, and delta C-13 values as low as -30%(0) VPDB. These 'chimneys' are therefore interpreted as former conduits related to hydrocarbon expulsion in this sector of the Adriatic basin. However, available data …

Adriatic SeaSessile fauna010504 meteorology & atmospheric sciencesHydrocarbonStratigraphyDolomite010502 geochemistry & geophysicsOceanography01 natural scienceslaw.inventionSedimentary depositional environmentchemistry.chemical_compoundPaleontologylawChimney14. Life underwaterGlacial periodRadiocarbon datingCarbonate chimneys[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentLithificationComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereSedimentGeology15. Life on landGeophysicschemistryROVCoralsCarbonateEconomic GeologyGeology
researchProduct

Microbially-induced Fe and Mn oxides in condensed pelagic sediments (Middle -Upper Jurassic, Western Sicily)

2011

Abstract This article presents a petrographic comparison of the Rosso Ammonitico facies of Western Sicily and the original Rosso Ammonitico Veronese of Northern Italy based on a total of 27 sections. The Rosso Ammonitico has been the subject of numerous controversies that range from bathyal to shallow-water platform sedimentation. Therefore it seemed interesting to verify if the term Rosso Ammonitico has the same geologic connotation from region to region. The Middle-Upper Jurassic Rosso Ammonitico of Western Sicily is a condensed succession formed during a period of extensional synsedimentary tectonics related to the spreading of the Ionian Ocean. Slope-to-basin or pelagic carbonate deposi…

CalcitebiologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStratigraphyGeologySaccocomaPelagic sedimentbiology.organism_classificationDiagenesisFe–Mn oxides Red pigmentation Microbial mediation DiagenesisPetrographychemistry.chemical_compoundPaleontologychemistryCarbonateLithificationGeologyOncolite
researchProduct

Deep-water stromatolites andFrutexites Maslov from the early and Middle Jurassic of S-Germany and Austria

1993

Despite extensive discussions during the last 20 years stromatolites are still used by many geologists as unequivocal indicators of very shallow-water conditions. We investigated four stratigraphic units from the Lower and Middle Jurassic of southern Germany (Posidonien-Schiefer, Amaltheen-Ton) and of the Northern Calcareous Alps (Adneter Kalk, Klauskalk), which were formerly interpreted as shallow marine sediments by some authors due to the occurrence of stromatolites. Our interpretations of the macro-, micro- and ultrafacies of these sediments are not compatible with shallow-water settings. We therefore propose a deep-marine, aphotic origin of these stromatolites. Former interpretations o…

Calcitegeographygeography.geographical_feature_categoryStratigraphyAragonitePaleontologyGeologyengineering.materialSedimentary depositional environmentchemistry.chemical_compoundPaleontologychemistryAphotic zoneengineeringSedimentary rockReefLithificationGeologyCarbonate compensation depthFacies
researchProduct

Microstructure-specific carbon isotopic signatures of organic matter from ∼3.5 Ga cherts of the Pilbara Craton support a biologic origin.

2016

21 pages; International audience; The ∼3.5 Ga Dresser Formation from the North Pole Dome of the Pilbara Craton (Western Australia) contains some of the oldest evidence for life on Earth. Here, we present a detailed study of microstructure-specific carbon isotopic composition of organic matter (OM) preserved in Dresser Formation bedded cherts and hydrothermal chert vein using in situ Secondary-Ion Mass Spectrometry (SIMS). The OM in these rocks occurs mainly as clots that, together with minor fine OM layers and laminae, are considered primary textures formed prior to host rock lithification. Other than rare OM-rich stylolites, no evidence was found for later OM migration beyond the micromete…

Carbon isotope ratio010504 meteorology & atmospheric sciencesMetamorphic rockPilbara CratonMineralogy010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesMicrofossilsPilbara cratonGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryDresser FormationOrganic matterLithificationAnkerite0105 earth and related environmental scienceschemistry.chemical_classificationδ13CGeology15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrychemistry13. Climate actionStylolite[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrganic matterVein (geology)SIMSGeology
researchProduct

Seepage carbonate mounds in Cenozoic sedimentary sequences from the Las Minas Basin, SE Spain

2016

Abstract A number of carbonate mounds composed of indurate, strongly folded and/or brecciated calcite and dolomite beds occur interstratified in Cenozoic sedimentary sequences from the Las Minas Basin. Part of the fabric of the rock forming the carbonate mounds is composed of laminated to banded dolostone similar to the host rock but showing contrasted lithification. Moreover, the carbonate deposits of the mounds display aggrading neomorphism of dolomite, partial replacement of dolomite by calcite, calcite cementation, and extensive silicification, locally resulting in box-work fabric. Eight main lithofacies were distinguished in the carbonate mound deposits. In some lithofacies, chert is p…

DolostoneCalcite010506 paleontologyStratigraphySE SpainDolomiteGeochemistryPetrologíaGeologyartesian groundwaterNeomorphism010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundchemistryCarbonate moundCarbonate rockCarbonateSedimentary rockseepage chertLithificationGeologycenozoic0105 earth and related environmental sciences
researchProduct

Review of the relationship between aggregates geology and Los Angeles and micro-Deval tests

2021

Rock aggregates constitute the enormous volume of inert construction material used around the globe. The petrologic description as igneous, sedimentary, and metamorphic types establishes the intrinsic formation pattern of the parent rock. The engineering properties of these rocks vary due to the differences in the transformation process (e.g. hydrothermal deposits) and weathering effect. The two most common mechanical tests used to investigate the performance of aggregates are the Los Angeles (LA) and micro-Deval (MD) tests. This study reviewed the geological parameters (including mineralogy, grain and crystal size, grain shape, and porosity) and the relationship to Los Angeles and micro-De…

Grain and crystal sizeMetamorphic rock0211 other engineering and technologiesMineralogyWeathering02 engineering and technology010502 geochemistry & geophysicsFeldspar01 natural sciences:Teknologi: 500 [VDP]Pore spaceParent rockGrain shapeQuartzLithification021101 geological & geomatics engineering0105 earth and related environmental sciencesMineralsGeologyGeotechnical Engineering and Engineering GeologyGrain sizeVDP::Teknologi: 500visual_artvisual_art.visual_art_mediumSedimentary rockLos Angeles testMicro-Deval testGeology
researchProduct

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
researchProduct

Controls of mud mound formation: The Early Devonian Kess-Kess carbonates of the Hamar Laghdad, Antiatlas, Morocco

1992

The origin and development of Early Devonian (late Pragian to late Zlichovian; predominantly uppermost Zlichovian as indicated by conodont faunas) mud mounds of the Hamar Laghdad area in the eastern Antiatlas, Morocco, are controlled by extrinsic and intrinsic factors. Extrinsic factors include the existence of a paleohigh (Lochkovian volcaniclastics), unidirectional currents and repeated storm events as well as sea level fluctuations. Intrinsic, biologically induced factors are the preferred growth of organisms on the top and the flanks of the mounds because of more favourable ecological conditions, and a rapid synsedimentary lithification of the steep mound flanks by interskeletal cementa…

OrthoconePaleontologybiologyFaciesGeneral Earth and Planetary SciencesSedimentologyConodontbiology.organism_classificationCrinoidLithificationDevonianSea levelGeologyGeologische Rundschau
researchProduct

Structures de déformation induites par surpressions de fluide dans les environnements sous-glaciaires et marin profonds : implications paléoenvironne…

2014

Soft-sediment deformation structures (SSDs) occur in unconsolidated sediments, during or shortly after deposition. SSDs are abundant in subglacial and deep-marine environments because of the development of fluid overpressure. Case studies of these two sedimentary environments were used (1) to reconstruct palaeoenvironments from SSDS, and (2) to define the impacts of SSDS on glacial morphologies and (3) petrophysical properties.(1) Analyses of strain regimes, deformation mechanisms, and chronologies in SSDs served to improve palaeoenvironmental reconstructions. These structures were used as proxys to estimate variations of ice flow velocities, ice thickness, meltwater production, and positio…

Reconstructions paléoenvironnementalesEnvironnement marin profondFluid pressureDeep-water environment[SDU.STU]Sciences of the Universe [physics]/Earth SciencesEnvironnement sous-glaciaireVallées tunnels[ SDU.STU ] Sciences of the Universe [physics]/Earth SciencesPalaeoenvironmental reconstructionsPropriétés réservoirsPression de fluide[SDU.STU] Sciences of the Universe [physics]/Earth SciencesSubglacial environmentTunnel valleysReservoir propertiesStructures de déformation pré-lithificationSoft-sediment deformation structures
researchProduct