Search results for "E64"

showing 10 items of 39 documents

Socio-Ecological Contingencies with Climate Changes over the Prehistory in the Mediterranean Iberia

2020

International audience; We conducted palynological, sedimentological, and chronological analyses of a coastal sediment sequence to investigate landscape evolution and agropastoral practices in the Nao Cap region (Spain, Western Mediterranean) since the Holocene. The results allowed for a reconstruction of vegetation, fire, and erosion dynamics in the area, implicating the role of fire in vegetation turnover at 5300 (mesophilous forests replaced by sclerophyllous scrubs) and at 3200 calibrated before present (cal. BP) (more xerophytics). Cereal cultivation was apparent from the beginning of the record, during the Mid-Neolithic period. From 5300 to 3800 cal. BP, long-lasting soil erosion was …

Mediterranean climate010506 paleontologypaleoenvironment010504 meteorology & atmospheric sciences[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistoryrapid climate changesSclerophyll4.2 kyr BP eventClimate changelcsh:GN281-28901 natural sciencesPrehistoryHolocene; paleoenvironment; archaeology; rapid climate changes; 4.2 kyr BP eventlcsh:StratigraphyBronze AgeEarth and Planetary Sciences (miscellaneous)Littoral zone[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/GeomorphologyHolocene0105 earth and related environmental sciencesEarth-Surface Processeslcsh:QE640-699[SDV.EE]Life Sciences [q-bio]/Ecology environmentHolocenearchaeologyChalcolithic15. Life on landGeography13. Climate actionlcsh:Human evolutionPhysical geographyQuaternary
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Zonation by ammonites and foraminifers of the Vraconnian-Turonian interval: A comparison of the Boreal and Tethyan domains (NW Europe / Central Tunis…

2008

International audience; Since the end of the 19th century the interval comprising the uppermost Upper Albian, the Cenomamian, the Turonian and the basal Coniacian has been subdivided, first into ammonite zones, then, beginning in the middle of the 20th century, into zones of planktonic foraminifera. These two groups, one macrofossil, the other microfossil, are particularly effective for bio-chronostratigraphy thanks to their rapid rates of evolution. But differences in the faunal makeup between the Boreal domain (northwestern Europe) and the Tethyan domain (Mediterranean) have for a long time hindered precise correlation of the two domains. Today, in a time interval covering about 16 millio…

Mediterranean climateStratigraphyzones[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDE.MCG.CPE] Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeCretaceousForaminiferaPaleontologyzonationlcsh:Stratigraphy[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCenomanianTethyslcsh:QE701-760lcsh:QE640-699Ammoniteammonitesbiologylcsh:QE1-996.5PaleontologyMacrofossilGeologyVraconnianAlbianTuronianbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageCretaceouslcsh:GeologyBoreallcsh:Paleontologylanguage[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyforaminifersCenomanianGeologyCarnets de Géologie
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On a new robust workflow for the statistical and spatial analysis of fracture data collected with scanlines (or the importance of stationarity)

2020

Abstract. We present an innovative workflow for the statistical analysis of fracture data collected along scanlines, composed of two major stages, each one with alternative options. A prerequisite in our analysis is the assessment of stationarity of the dataset, which is motivated by statistical and geological considerations. Calculating statistics on non-stationary data can be statistically meaningless, and moreover the normalization and/or sub-setting approach that we discuss here can greatly improve our understanding of geological deformation processes. Our methodology is based on performing non-parametric statistical tests, which allow detecting important features of the spatial distrib…

Normalization (statistics)statistical and spatial analysis of fracture dataComputer scienceStratigraphylcsh:QE1-996.5PaleontologySoil ScienceGeologyFunction (mathematics)computer.software_genrelcsh:GeologyGeophysicsWorkflowlcsh:StratigraphyGeochemistry and PetrologyFracture (geology)Statistical analysisData miningSpatial analysiscomputerlcsh:QE640-699Earth-Surface ProcessesSolid Earth
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Investigating the effects of intersection flow localization in equivalent-continuum-based upscaling of flow in discrete fracture networks

2021

Abstract. Predicting effective permeabilities of fractured rock masses is a crucial component of reservoir modeling. Its often realized with the discrete fracture network (DFN) method, whereby single-phase incompressible fluid flow is modeled in discrete representations of individual fractures in a network. Depending on the overall number of fractures, this can result in high computational costs. Equivalent continuum models (ECMs) provide an alternative approach by subdividing the fracture network into a grid of continuous medium cells, over which hydraulic properties are averaged for fluid flow simulations. While continuum methods have the advantage of lower computational costs and the pos…

QE1-996.5Darcy's lawDiscretizationStratigraphyPaleontologySoil ScienceGeologyMechanicsStokes flowPipe flowQE640-699Permeability (earth sciences)GeophysicsFlow (mathematics)Geochemistry and PetrologyFracture (geology)Fluid dynamicsGeologyEarth-Surface Processes
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Litter contribution to soil organic carbon in the processes of agriculture abandon

2015

The mechanisms of litter decomposition, translocation and stabilization into soil layers are fundamental processes in the functioning of the ecosystem, as they regulate the cycle of soil organic matter (SOM) and CO2 emission into the atmosphere. In this study the contribution of litters of different stages of Mediterranean secondary succession on carbon sequestration was investigated, analyzing the role of earthworms in the translocation of SOM into the soil profile. For this purpose the δ13C difference between meadow C4-C soil and C3-C litter was used in a field experiment. Four undisturbed litters of different stages of succession (45, 70, 100 and 120 since agriculture abandon) were colle…

Secondary successionSettore AGR/05 - Assestamento Forestale E SelvicolturaStratigraphySoil biologySoil ScienceCarbon sequestrationlcsh:StratigraphyGeochemistry and PetrologySoil Science; Earth-Surface Processes; Geochemistry and Petrology; Geology; Geophysics; Paleontology; StratigraphyGeophysiclcsh:QE640-699Earth-Surface ProcessesEcologySoil organic matterlcsh:QE1-996.5PaleontologyGeologySoil carbonPlant litterSettore AGR/02 - Agronomia E Coltivazioni Erbaceelcsh:GeologyGeophysicsAgronomyEarth-Surface ProcesseSoil waterEnvironmental scienceSoil horizon
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Grassland fire effect on soil organic carbon reservoirs in a semiarid environment

2013

Abstract. The aim of this work was to investigate the effect of an experimental fire used for grassland management on soil organic carbon (SOC) stocks. The study was carried out on Hyparrhenia hirta (L.) Stapf (Hh) grassland and Ampelodesmos mauritanicus (Desf.) T. Durand & Schinz (Am) grasslands located in the north of Sicily. Soil samples were collected at 0–5 cm before and after the experimental fire, and SOC was measured. During the grassland fire, soil surface temperature was monitored. Biomass of both grasses was analysed in order to determine dry weight and its chemical composition. The results showed that SOC varied significantly with vegetation type, while it is not affecte…

Settore AGR/05 - Assestamento Forestale E SelvicolturaSoil testStratigraphySoil ScienceAmpelodesmosSoil sciencecomplex mixturesGrasslandlcsh:StratigraphyGeochemistry and PetrologyVegetation typeotorhinolaryngologic diseasesGrassland managementnatural sciencesgrassland firesoil organic carbon mediterranean environmentlcsh:QE640-699Earth-Surface ProcessesgeographyBiomass (ecology)geography.geographical_feature_categorybiologylcsh:QE1-996.5food and beveragesPaleontologyGeologySoil carbonMineralization (soil science)biology.organism_classificationSettore AGR/02 - Agronomia E Coltivazioni Erbaceelcsh:Geologysoil organic carbonsemiarid environmentGeophysicsAgronomyLitterEnvironmental scienceSolid Earth
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Short-term changes in soil Munsell colour value, organic matter content and soil water repellency after a spring grassland fire in Lithuania

2014

Abstract. Fire is a natural phenomenon with important implications on soil properties. The degree of this impact depends upon fire severity, the ecosystem affected, topography of the burned area and post-fire meteorological conditions. The study of fire effects on soil properties is fundamental to understand the impacts of this disturbance on ecosystems. The aim of this work was to study the short-term effects immediately after the fire (IAF), 2, 5, 7 and 9 months after a low-severity spring boreal grassland fire on soil colour value (assessed with the Munsell colour chart), soil organic matter content (SOM) and soil water repellency (SWR) in Lithuania. Four days after the fire a 400 m2 plo…

Soil testStratigraphywaterSoil ScienceGrasslandSoillcsh:StratigraphyGeochemistry and PetrologySoil Science; Earth-Surface Processes; Geochemistry and Petrology; Geology; Geophysics; Paleontology; StratigraphyOrganic matterEcosystemGeophysicEarth-Surface Processeslcsh:QE640-699chemistry.chemical_classificationHydrologygeographygeography.geographical_feature_categorySoil organic matterlcsh:QE1-996.5PaleontologySampling (statistics)GeologyLithuaniaFireSettore AGR/02 - Agronomia E Coltivazioni Erbaceelcsh:GeologyGeophysicschemistryBorealEarth-Surface ProcesseSoil waterEnvironmental scienceOrganic matter
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Managing soil nitrate with cover crops and buffer strips in Sicilian vineyards

2013

When soil nitrate levels are low, plants suffer nitrogen (N) deficiency but when the levels are excessive, soil nitrates can pollute surface and subsurface waters. Strategies to reduce the nitrate pollution are necessary to reach a sustainable use of resources such as soil, water and plant. Buffer strips and cover crops can contribute to the management of soil nitrates, but little is known of their effectiveness in semiarid vineyards plantations. The research was carried out in the south coast of Sicily (Italy) to evaluate nitrate trends in a vineyard managed both conventionally and using two different cover crops (Triticum durum and Vicia sativa cover crop). A 10 m-wide buffer strip was se…

StratigraphySoil ScienceBuffer stripengineering.materialLolium perenneVineyardSoil managementchemistry.chemical_compoundNitratelcsh:StratigraphyGeochemistry and PetrologyStratigraphy; Paleontology; Geophysics; Geology; Geochemistry and Petrology; Earth-Surface Processes; Soil ScienceCover cropGeophysicEarth-Surface Processeslcsh:QE640-699biologylcsh:QE1-996.5PaleontologyGeologybiology.organism_classificationlcsh:GeologyGeophysicsAgronomychemistryEarth-Surface ProcesseengineeringEnvironmental scienceFertilizerGroundwaterSolid Earth
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Support for a Vraconnian Stage between the Albian sensu stricto and the Cenomanian (Cretaceous System)

2008

The geological scale for the middle Cretaceous currently used throughout the world was proposed by Alcide d'Orbigny in the XIXth century between the years 1842 and 1847 and establishes the succession of stages as Albian, Cenomanian and Turonian. In 1868 Renevier proposed that a supplemental chronostratigraphic division be intercalated between the Albian and the Cenomanian: the Vraconnian stage. This term was not generally accepted and after a period when it was referred to by Breistroffer (1936) as a substage constituting the upper part of the Albian, as an equivalent of the Stoliczkaia dispar ammonite Zone, its abandonment was "recommended" by the Conference on the Lower Cretaceous held in…

Stratigraphysequence stratigraphyzones[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyCretaceousForaminiferaPaleontologyzonationlcsh:StratigraphyStage (stratigraphy)Sequence stratigraphyTethysCenomanianlcsh:QE701-760lcsh:QE640-699[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmoniteammonitesbiologylcsh:QE1-996.5foraminiferaPaleontologyGeologyVraconnianTuronianAlbianbiology.organism_classificationlanguage.human_languageCretaceouslcsh:Geologylcsh:Paleontology[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphylanguagePeriod (geology)foraminifers[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyCenomanianVraconnian stageGeologyMarine transgression
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Spatial models for monitoring the spatio-temporal evolution of ashes after fire-a case study of a burnt grassland in Lithuania

2013

Ash thickness is a key variable in the protection of soil against erosion agents after planned and unplanned fires. Ash thickness measurements were conducted along two transects (flat and sloping areas) following a grided experimental design. In order to interpolate data with accuracy and identify the techniques with the least bias, several interpolation methods were tested in the grided plot. Overall, the fire had a low severity. However, the fire significantly reduced the ground cover, especially on sloping areas, owing to the higher fire severity and/or less biomass previous to the fire. Ash thickness depended on fire severity and was thin where fire severity was higher and thicker in lo…

Water erosionStratigraphySoil Sciencemacromolecular substancescomplex mixturesGrasslandlcsh:StratigraphyGeochemistry and PetrologyTransectlcsh:QE640-699Earth-Surface ProcessesHydrologyBiomass (ecology)geographygeography.geographical_feature_categoryEcologylcsh:QE1-996.5technology industry and agriculturePaleontologyGeologyrespiratory systemmusculoskeletal systemlcsh:GeologyGeophysicsErosionEnvironmental scienceSpatial variability
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