Search results for "Silicic"

showing 10 items of 95 documents

Pre-Hirnantian (latest Ordovician) benthic community assemblages: controls and replacements in a siliciclastic-dominated platform of the eastern Anti…

2007

17 pages; International audience; Lower-middle Ashgill sedimentary strata from the Mediterranean region have recorded a key episode of temperate-to-cold water, carbonate productivity predating the onset of the Hirnantian glaciation. The latitudinal position of the Moroccan margin of North Gondwana during Ashgill should have been adequate for the recorded development of carbonate factories. However, carbonate productivity was neither homogeneous nor laterally persistent, as documented in the eastern Anti-Atlas. Whereas in the Erfoud area, the bryozoan-dominated limestones of the Ashgill Khabt-el-Hajar Formation indicate the intensive activity of carbonate factories, these were dramatically r…

010506 paleontologyNorthern Gondwana010502 geochemistry & geophysicsOceanographyCarbonate factory[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesUnconformitychemistry.chemical_compoundPaleontologyBenthic communities14. Life underwaterGlacial periodCoquinaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesLate OrdovicianPaleontologyGondwanaMoroccochemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrdovicianCarbonateSedimentary rockSiliciclasticGeology
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Unravelling extrinsic and intrinsic factors of the early Palaeozoic diversification of blastozoan echinoderms

2010

19 pages; International audience; The Subphylum Blastozoa represents more than one third of the early Palaeozoic echinoderm fauna. A comprehensive database including all records of blastozoans was built to provide quantitative analyses of palaeogeography and diversity patterns and processes, for the 10 classes currently included in this subphylum during the early Palaeozoic. The global pattern of taxonomic diversity shows two peaks during the Cambrian Series 3 and the Late Ordovician intervals. In Cambrian times, the high taxonomic diversity seems to be related with a high turnover rate and a high endemicity of blastozoan genera, whereas in Ordovician times, the rise in diversity is associa…

010506 paleontologyPaleozoicEvolutionBlastozoaEvolutionary fauna010502 geochemistry & geophysicsOceanography01 natural sciencesBlastozoaPaleontologyEcology Evolution Behavior and Systematics[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesEarth-Surface ProcessesExtinction eventDiversitybiologyCambrian Series 3EcologyEarly PalaeozoicPaleontology15. Life on landbiology.organism_classification13. Climate actionOrdovicianSiliciclastic[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalaeogeographyOriginationGeologyEchinodermataPalaeogeography, Palaeoclimatology, Palaeoecology
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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
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Paleoecological constraints on reef-coral morphologies in the Tortonian–early Messinian of the Lorca Basin, SE Spain

2004

Abstract Coral reefs represent one of the main carbonate factories that contributed to the control of the stratigraphic architecture of carbonate platforms, which had a widespread development during the late Miocene in the paleo-Mediterranean area. The late Miocene reef complexes of the Lorca Basin in southeastern Spain are composed of five mixed siliciclastic/carbonate units, middle Tortonian to early Messinian in age. The development of coral reefs probably ceased when the first evaporitic event occurred in the basin centre in the early Messinian. This study mainly focuses on the response of reef communities and the modifications of reef organisation to global and regional parameters. At …

010506 paleontologygeographygeography.geographical_feature_categorybiologyCarbonate platformCoralPoritesPaleontologyCoralline algaeCoral reefLate Miocene010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesPaleontologySiliciclastic14. Life underwaterReefEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Secondary structure and dynamics study of the intrinsically disordered silica-mineralizing peptide P5S3during silicic acid condensation and silica de…

2017

The silica forming repeat R5 of sil1 from Cylindrotheca fusiformis was the blueprint for the design of P5 S3 , a 50-residue peptide which can be produced in large amounts by recombinant bacterial expression. It contains 5 protein kinase A target sites and is highly cationic due to 10 lysine and 10 arginine residues. In the presence of supersaturated orthosilicic acid P5 S3 enhances silica-formation whereas it retards the dissolution of amorphous silica (SiO2 ) at globally undersaturated concentrations. The secondary structure of P5 S3 during these 2 processes was studied by circular dichroism (CD) spectroscopy, complemented by nuclear magnetic resonance (NMR) spectroscopy of the peptide in …

0301 basic medicineCircular dichroismProtein ConformationSilicic AcidPeptideMolecular Dynamics SimulationSodium Chloride010402 general chemistry01 natural sciencesBiochemistryArticle03 medical and health scienceschemistry.chemical_compoundStructural BiologyPolymer chemistryOrganic chemistrySilicic acidNuclear Magnetic Resonance BiomolecularMolecular BiologyDissolutionProtein secondary structurePolyproline helixchemistry.chemical_classificationNuclear magnetic resonance spectroscopySilicon Dioxide0104 chemical sciencesIntrinsically Disordered Proteins030104 developmental biologychemistryPolymerizationPeptidesProteins: Structure, Function, and Bioinformatics
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The Relevance of Mineral Mobilization and -Dissolution on the Reservoir Quality of Sandstones in CO2 Storage Sites

2014

Abstract Rotliegend siliciclastic formations are important reservoirs in central Europe. These sediments consist of pristine red coloured and bleached, high porous and permeable sandstones. To evaluate the relevance of distinct fluids and their fluid-rock alteration reactions on such bleaching processes laboratory static batch experiments under reservoir conditions were conducted. Thereby mineralogical, petrophysical and (hydro-, geo-) chemical rock features were investigated by different analytical methods before and after the experiments. The achieved results suggest that during such fluid-rock interactions a complex interplay between mineral detachment and mineral dissolution processes w…

AltmarkPetrophysicsGeochemistryMineralogySandstoneCo2 storageRotliegendCCSReservoir qualityMineral dissolutionPermeability (earth sciences)Energy(all)BleachingMineral detachmentCO2SiliciclasticAutoclave experimentsPorosityDissolutionGeologyEnergy Procedia
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Strength of pre-Roman amphorae: Comparison of the different types

2015

Abstract Given that amphorae were used for storage or for long and/or short distance transport, they must have been able to retain their content and, at the same time, be able to resist important load during transport. This paper concerns aspects of the techno-functionality of pre-Roman Iberian amphorae. The basic performance requirement concerned here is the mechanical strength (transverse rupture strength: TRS). Strength is related to the adequacy for storage or short and/or long distance transport that, up to now, is only assessed by typological identification or archaeological evidence. Experimental implementation on actual archaeological material has confirmed that strength increased w…

ArcheologyInelastic deformationArchaeologyTexture (geology)Archaeological evidenceShort distanceFlexural strengthMechanical loading Inelastic deformation Strength Iberian amphora Trade StorageMechanical strengthPerformance requirementGeotechnical engineeringSiliciclasticSettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.GeologyJournal of Archaeological Science: Reports
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Lithologic composition of the Earth's continental surfaces derived from a new digital map emphasizing riverine material transfer

2005

[1] A new digital map of the lithology of the continental surfaces is proposed in vector mode (n ≈ 8300, reaggregated at 0.5° × 0.5° resolution) for 15 rock types (plus water and ice) targeted to surficial Earth system analysis (chemical weathering, land erosion, carbon cycling, sediment formation, riverine fluxes, aquifer typology, coastal erosion). These types include acid (0.98% at global scale) and basic (5.75%) volcanics, acid (7.23%) and basic (0.20%) plutonics, Precambrian basement (11.52%) and metamorphic rocks (4.07%), consolidated siliciclastic rocks (16.28%), mixed sedimentary (7.75%), carbonates (10.40%), semi- to un-consolidated sedimentary rocks (10.05%), alluvial deposits (15…

Atmospheric ScienceGlobal and Planetary Changegeographygeography.geographical_feature_categoryEvaporiteLithologyGeochemistryVolcanic rockPrecambrianBasement (geology)Environmental ChemistryCarbonate rockSiliciclasticSedimentary rockGeomorphologyGeologyGeneral Environmental ScienceGlobal Biogeochemical Cycles
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Bioencapsulation of living bacteria (Escherichia coli) with poly(silicate) after transformation with silicatein-α gene

2007

Bioencapsulation is an intriguing way to immobilize biological materials, including cells, in silica, metal-oxides or hybrid sol-gel polymers. Until now only the sol-gel precursor technology was utilized to immobilize bacteria or yeast cells in silica. With the discovery of silicatein, an enzyme from demosponges that catalyzes the formation of poly(silicate), it became possible to synthesize poly(silicate) under physiological (ambient) conditions. Here we show that Escherichia coli can be transformed with the silicatein gene, its expression level in the presence of isopropyl beta-D-thiogalactopyranoside (IPTG) can be efficiently intensified by co-incubation with silicic acid. This effect co…

Bacterial capsuleMaterials scienceBiophysicsGene Expressionlac operonBioengineeringmedicine.disease_causelaw.inventionBiomaterialschemistry.chemical_compoundlawEscherichia colimedicineTransgenesSilicic acidEscherichia coliBacterial Capsuleschemistry.chemical_classificationMicrobial ViabilitybiologySilicatesSodiumbiology.organism_classificationCathepsinsYeastEnzymechemistryBiochemistryMechanics of MaterialsMicroscopy Electron ScanningCeramics and CompositesRecombinant DNABacteriaBiomaterials
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The origin and evolution of breakouts in a cooling-limited rhyolite lava flow

2018

Understanding lava flow processes is important for interpreting existing lavas and for hazard assessments. Although substantial progress has been made for basaltic lavas our understanding of silicic lava flows has seen limited recent advance. In particular, the formation of lava flow breakouts, which represent a characteristic process in cooling-limited basaltic lavas, but has not been described in established models of rhyolite emplacement. Using data from the 2011–2012 rhyolite eruption of Puyehue-Cordón Caulle, Chile, we develop the first conceptual framework to classify breakout types in silicic lavas, and to describe the processes involved in their progressive growth, inflation, and mo…

BasaltBreakout010504 meteorology & atmospheric sciencesLavaFront (oceanography)SilicicGeologyCrust010502 geochemistry & geophysics01 natural sciencesRhyoliteMagmaPetrologyGeology0105 earth and related environmental sciencesGSA Bulletin
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