Search results for "Waters"

showing 10 items of 281 documents

Petrography and high-resolution geochemical records of Lower Jurassic manganese-rich deposits from Monte Mangart, Julian Alps

2016

Deposits with unusually high Mn contents sampled at Monte Mangart in the Julian Alps include organic-rich marlstone and black shale with interbedded manganoan and siliceous limestone, which were deposited during the early Toarcian Oceanic Anoxic Event. Mn enrichment during that period has been related to global sea-level change coincident with increasing subsidence rate. The formation of Fe-Mn nodules, marking a hardground at the base of the Monte Mangart section, seems to be triggered by release of Mn from remote hydrothermal vents into a region of relatively elevated submarine topography where oxidizing conditions prevailed. However, very high Mn contents in carbonate phases above the har…

GeochemistrySettore GEO/07 - Petrologia E PetrografiaPaleontologyengineering.materialOceanographyCarbonate hardgroundsEarly Toarcian Mn-bearing deposits Anoxic Event Stable isotope stratigraphy Rare earth elementsAnoxic watersDiagenesisSettore GEO/08 - Geochimica E VulcanologiaPetrographyEarth scienceschemistry.chemical_compoundPaleontologychemistryMarlengineeringCarbonatePyriteEarly Toarcian Mn-bearing deposits Anoxic Event Stable isotope stratigraphy Rare earth elementsEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesHydrothermal vent
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Sediment features, macrozoobenthic assemblages and trophic relationships (δ13C and δ15N analysis) following a dystrophic event with anoxia and sulphi…

2007

Macrozoobenthic assemblages and stable carbon (delta C-13) and nitrogen (delta N-15) isotope values of various primary producers (macroalgae and angiosperms) and consumers (macroinvertebrate filter/suspension feeders, deposit feeders, detritivores/omnivores and carnivores and fishes) were studied in the Santa Giusta lagoon (Sardinia, Italy) before (spring) and after (autumn) a dystrophic event which occurred in the summer of 2004. A few days after the dystrophy, the physico-chemical characteristics of sediments and macrozoobenthic assemblages were also investigated. In the latter occasion, high total organic carbon (3.9%) and organic matter (15.9%) contents of surface sediments went togethe…

Geologic SedimentsFood ChainAnimal Ecology and PhysiologyOceans and Seasstable isotopesSulfidesAquatic ScienceBiologyOceanographyBenthosAnimalsSedimentary organic matterSeawaterOrganic matterAnaerobiosisIsotope analysisTrophic levelPopulation Densitychemistry.chemical_classificationCarbon IsotopesNitrogen IsotopesEcologyTemperatureDetritivoreBiodiversitypollution impactInvertebratesPollutionFood webOxygenItalychemistrymacrofaunabenthic communities food webs stable isotopes eutrophication transitional watersfood websorganic enrichmentFish killMarine Pollution Bulletin
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A new marker for sea surface temperature trend during the last centuries in temperate areas: Vermetid reef

2004

The presence of Vermetid reefs in temperate waters, their diffusion in the Mediterranean Sea, and the possibility of performing 14 C ages allowed the use of Vermetids as an indicator of sea level changes. We present new data on sea climate trend fluctuations that could be interpreted as Sea Surface Temperature (SST) variations, recorded on Vermetid (Dendropoma petraeum) reefs, by means of isotopic analysis. The isotopic records show positive values of the d 18 O relative to present-day values in the period between 1600 and 1850 AD; this deviation occurs in association with the climatic cooling event known as Little Ice Age (LIA). Subsequently, we can observe the warming trend that character…

Global and Planetary ChangeDendropoma petraeumgeographygeography.geographical_feature_categorybiologyDendropomaOceanographybiology.organism_classificationVermetid reefs Sea surface temperature trend Late Holocene Temperate watersSea surface temperatureOceanographyMediterranean seaTemperate climateReefGeologySea levelIsotope analysisGlobal and Planetary Change
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Authigenic phase formation and microbial activity control Zr, Hf, and rare earth element distributions in deep-sea brine sediments

2014

Abstract. Sediments collected from hypersaline and anoxic deep-sea basins in the eastern Mediterranean (Thetis, Kryos, Medee, and Tyro) were characterised in terms of their mineralogical composition, the distributions of rare earth elements (REE), Zr, and Hf and their content of microbial DNA. We identified two major mineralogical fractions: one fraction of detritic origin was composed of quartz, gypsum, and low-Mg calcite bioclasts (with 0 < Mg < 0.07%) and another fraction of authigenic origin constituted of halite, dolomite, high-Mg calcite (with a Mg content of up to 22%) and rare bischofite and showed a textural evidence of microbial assemblages. We found that in the Medee and Ty…

Gypsum010504 meteorology & atmospheric sciencesSettore AGR/13 - Chimica AgrariaGeochemistrylcsh:LifeMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesengineering.material010502 geochemistry & geophysics01 natural sciencesDeep seachemistry.chemical_compoundlcsh:QH540-549.5Settore CHIM/01 - Chimica AnaliticaQuartzEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesgeochemistryCalciteRare-earth elementlcsh:QE1-996.5AuthigenicAnoxic watersSettore GEO/08 - Geochimica E Vulcanologialcsh:Geologylcsh:QH501-531chemistryengineeringCarbonatelcsh:EcologyGeology
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Acqua Fitusa cave: An example of inactive water-table sulphuric acid cave in Central Sicily

2012

Description of the sulphuric acid cave in Sicily (see pdf attached)

HYPOGENE KARSTSPELEOGENESISMINERALOGYSettore GEO/04 - Geografia Fisica E GeomorfologiaGEOMORPHOLOGYgypsum hypogenic caves sulphuric acid cave thermal waters Sicily.
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Geochemical and sedimentological evidence of productivity cycles recorded in Toarcian black shales from the Belluno Basin, Southern Alps, northern It…

1999

ABSTRACT Organic-carbon-rich black shales cyclically alternating with bioturbated limestones and gray marlstones, which crop out in the Belluno Trough (Southern Alps, Italy), are expression of the early Toarcian anoxic event in the Tethys basin. Sedimentological and geochemical features such as well-developed lamination, common very small ( A negative 13C excursion at the middle part of the studied interval is correlative to maxima in TOC, V/Rb, and Ba/Rb values, identifying, within the Toarcian anoxic event, a stage of more intense bottom-water anoxia coupled with high surface fertility.

High surfacePaleontologyExcursionTrough (geology)GeologyStructural basinAnoxic watersGeologyNorthern italyJournal of Sedimentary Research
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Using unsteady-state water level data to estimate channel roughness and discharge hydrograph

2009

A novel methodology for simultaneous discharge and channel roughness estimation is developed and applied to data sets available at three experimental sites. The methodology is based on the synchronous measurement of water level data in two river sections far some kilometers from each other, as well as on the use of a diffusive flow routing solver and does not require any direct velocity measurement. The methodology is first analyzed for the simplest case of a channel with a large slope, where the kinematic assumption holds. A sensitivity and a model error analysis are carried out in this hypothesis in order to show the stability of the results with respect to the error in the input paramete…

HydrologyFlow meterDischargeDiffusive modelShallow watersHydrographSoil scienceStability (probability)Flow measurementDischarge estimationCalibrationErrors-in-variables modelsFlow routingStage (hydrology)GeologyFlow routingWater Science and TechnologyCommunication channel
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Data Mining Technique (Maximum Entropy Model) for Mapping Gully Erosion Susceptibility in the Gorganrood Watershed, Iran

2019

Soil erosion is a serious problem affecting most of the countries. This study was carried out in Gorganrood Watershed (Iran), which extends for 10,197 km2 and is severely affected by gully erosion. A gully headcut inven- tory map consisting of 307 gully headcut points was provided by Google Earth images, field surveys, and national reports. Gully conditioning factors including sig- nificant geo-environmental and morphometric variables were selected as predictors. Maximum entropy (ME) model was exploited to model gully susceptibility, whereas the area under the ROC curve (AUC) and draw- ing receiver operating characteristic (ROC) curves were employed to evaluate the performance of the model.…

HydrologyGully erosion Susceptibility Geographic information systems (GIS) Maximum entropy (ME) model Area under the ROC curve (AUC)WatershedReceiver operating characteristicPrinciple of maximum entropySettore GEO/04 - Geografia Fisica E GeomorfologiaGully erosionArea under the roc curveSettore GEO/05 - Geologia ApplicataGeology
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Linking sediment yield and caesium-137 spatial distribution at basin scale

1999

Abstract Identifying areas of the landscape that are most sensitive or susceptible to erosion stimulated the study of within-basin variability of the sediment delivery processes and the use of spatially distributed models coupled with Geographic Information Systems. The progress of sediment delivery distributed modelling is also dependent on the availability of measurements able to establish the link between eroded soil leaving an area and the patterns of erosion and deposition occurring along the hydraulic path from the considered area to the nearest stream reach. In this paper, the tracer technique using the radionuclide137Cs and its employment in sediment yield studies at basin scale are…

HydrologyUniversal Soil Loss EquationWatershedDistributed element modelErosionSedimentWEPPAquatic ScienceStructural basinGeologyDeposition (geology)
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The role of vegetation on gully erosion stabilization at a severely degraded landscape: A case study from Calhoun Experimental Critical Zone Observat…

2018

Abstract Gully erosion was evidence of land degradation in the southern Piedmont, site of the Calhoun Critical Zone Observatory (CCZO), during the cotton farming era. Understanding of the underlying gully erosion processes is essential to develop gully erosion models that could be useful in assessing the effectiveness of remedial and soil erosion control measures such as gully backfilling, revegetation, and terracing. Development and validation of process-based gully erosion models is difficult because observations of the formation and progression of gullies are limited. In this study, analytic formulations of the two dominant gullying processes, namely, plunge pool erosion and slab failure…

HydrologyWatershedLandscape evolution model010504 meteorology & atmospheric sciences04 agricultural and veterinary sciencesGully erosionVegetation01 natural sciences040103 agronomy & agricultureLand degradationErosion0401 agriculture forestry and fisheriesRevegetationPlunge poolGeology0105 earth and related environmental sciencesEarth-Surface ProcessesGeomorphology
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