Search results for "Universe"

showing 10 items of 2171 documents

Ammonite diversity and its palaeobiogeographical structure during the early Pliensbachian (Jurassic) in the western Tethys and adjacent areas.

2009

14 pages; International audience; The early Pliensbachian (Early Jurassic) is known as a time of marked provincialism in the marine realm, notably between the Mediterranean Tethys and North–West Europe. In order to test this observation quantitatively, we compiled 104 locality-level species lists from those areas based on a comprehensive revision of early Pliensbachian ammonites. With this dataset, we also explore the relationship between ammonite richness and biogeography at the scale of the sub-chronozone during the early Pliensbachian. Using various multivariate statistics and rarefaction techniques, we show that: (i) there is a sharp contrast between the NW European (NWE) and the Medite…

Mediterranean climateAmmoniteRange (biology)EcologyBiogeographyEarly JurassicBiodiversityPaleontologyPliensbachianBiodiversityOceanographylanguage.human_languagePaleontologyBiogeographyAmmoniteslanguageRarefaction (ecology)ChronozoneSpecies richnessEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesWestern Tethys[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
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African monsoon variability during the previous interglacial maximum.

2002

Little is known about centennial- to millennial-scale climate variability during interglacial times, other than the Holocene. We here present high-resolution evidence from anoxic (unbioturbated) sediments in the eastern Mediterranean Sea that demonstrates a sustained V800-yr climate disturbance in the monsoonal latitudes during the Eemian interglacial maximum (V125 ka BP). Results imply that before and after this event, the Intertropical Convergence Zone (ITCZ) penetrated sufficiently beyond the central Saharan watershed (V21n) during the summer monsoon to fuel flooding into the Mediterranean along the wider North African margin, through fossil river/wadi systems that to date have been cons…

Mediterranean climateEemianIntertropical Convergence ZoneSapropelMonsoonMediterranean BasinGeophysicsOceanographySpace and Planetary ScienceGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyInterglacialEarth and Planetary Sciences (miscellaneous)HoloceneGeologyComputingMilieux_MISCELLANEOUS
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Multiple recharge processes to heterogeneous Mediterranean coastal aquifers and implications on recharge rates evolution in time

2018

Abstract Climate change is nowadays widely considered to have major effects on groundwater resources. Climatic projections suggest a global increase in evaporation and higher frequency of strong rainfall events especially in Mediterranean context. Since evaporation is synonym of low recharge conditions whereas strong rainfall events are more favourable to recharge in heterogeneous subsurface contexts, a lack of knowledge remains then on the real ongoing and future drinking groundwater supply availability at aquifers scale. Due to low recharge potential and high inter-annual climate variability, this issue is strategic for the Mediterranean hydrosystems. This is especially the case for coast…

Mediterranean climateHydrologyIrrigationgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences0208 environmental biotechnologyClimate changeContext (language use)Aquifer02 engineering and technologyGroundwater recharge01 natural sciences6. Clean water020801 environmental engineering13. Climate actionEnvironmental science[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/HydrologySurface runoffGroundwaterComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesWater Science and Technology
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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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The end of the Messinian Salinity Crisis in the western Mediterranean: insights from the carbonate platforms of south-eastern Spain.

2010

International audience; How the Messinian Salinity Crisis (MSC) ended is still a matter of intense debate. The Terminal Carbonate Complex (TCC) is a late Messinian carbonate platform system that recorded western Mediterranean hydrological changes from the final stages of evaporite deposition till the advent of Lago-Mare fresh- to brackish water conditions at the very end of Messinian times. A multidisciplinary study has been carried out in three localities in south-eastern Spain to reconstruct the history of TCC platforms and elucidate their significance in the MSC. Overall, this study provides evidence that the TCC formed following a regional 4th order water level rise and fall concomitant…

Mediterranean climateWestern Mediterranean010506 paleontologyEvaporiteEnvironmental changeSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformStratigraphyEvaporite deformation and dissolutionMessinian Salinity Crisis010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentMessinian Salinity Crisis Western Mediterranean Carbonate platforms Evaporite deformation and dissolution Eustasy Return to marine conditionschemistry.chemical_compoundReturn to marine conditions14. Life underwaterCarbonate platformsEustasy0105 earth and related environmental sciencesBrackish waterGeologySettore GEO/01 - Paleontologia E PaleoecologiaWater levelOceanographychemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
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Characterization of the interannual and intraseasonal variability of West African vegetation between 1982 and 2002 by means of NOAA AVHRR NDVI data

2007

AbstractThe interannual and intraseasonal variability of West African vegetation over the period 1982–2002 is studied using the normalized difference vegetation index (NDVI) from the Advanced Very High Resolution Radiometer (AVHRR).The novel independent component analysis (ICA) technique is applied to extract the main modes of the interannual variability of the vegetation, among which two modes are worth describing. The first component (IC1) describes NDVI variability over the Sahel from August to October. A strong photosynthetic activity over the Sahel is related to above-normal convection and rainfall within the intertropical convergence zone (ITCZ) in summertime and is partly associated …

Mediterranean climateWet seasonAtmospheric Science010504 meteorology & atmospheric sciencesAdvanced very-high-resolution radiometerATMOSPHERIC DYNAMICS0211 other engineering and technologies02 engineering and technology01 natural sciencesNormalized Difference Vegetation IndexRAINY-SEASONPHENOLOGYEL-NINO[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentPrecipitation[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentINDEX021101 geological & geomatics engineering0105 earth and related environmental sciencesAIR-TEMPERATUREINDEPENDENT COMPONENT ANALYSISIntertropical Convergence Zone15. Life on landSea surface temperature13. Climate actionClimatologySEA-SURFACE TEMPERATUREPRECIPITATIONEnvironmental scienceOutgoing longwave radiationSAHEL RAINFALL
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Degassing vs. eruptive styles at Mt. Etna volcano (Sicily, Italy). Part I: Volatile stocking, gas fluxing, and the shift from low-energy to highly ex…

2018

International audience; Basaltic magmas can transport and release large amounts of volatiles into the atmosphere, especially in subduction zones, where slab-derived fluids enrich the mantle wedge. Depending on magma volatile content, basaltic volcanoes thus display a wide spectrum of eruptive styles, from common Strombolian-type activity to Plinian events. Mt. Etna, in Sicily, is a typical basaltic volcano where the volatile control on such a variable activity can be investigated. Based on a melt inclusion study in products from Strombolian or lava-fountain activity to Plinian eruptions, here we show that for the same initial volatile content, different eruptive styles reflect variable dega…

Melt inclusion010504 meteorology & atmospheric sciencesExplosive materialMantle wedgeGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMicroliteGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyBasaltic explosive volcanism0105 earth and related environmental sciencesMelt inclusionsBasaltgeographygeography.geographical_feature_categorySubductionMt. EtnaTotal volatilesChemical thermodynamicsGeologyTotal volatileStrombolian eruptionChemical thermodynamicVolcano13. Climate actionengineeringMelt inclusionsGeology
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Monsoon onset over Sudan-Sahel: Simulation by the regional scale model MM5.

2006

[1] The Mesoscale Model MM5 is used to study the regional features of the West African Monsoon onset. In order to increase the results, simulations are carried out for eight consecutive seasons (March to September) of the years 1994 to 2001. The results show that the model can reproduce the dynamical features of the monsoon in a reasonably good manner but the seasonal cycle seems enhanced. It is hypothesized that overestimated rainfall amounts could be related to a poor representation of the land surface characteristics. Nevertheless, the mean simulated monsoon onset dates are similar to those find in the CMAP data set. The onset is characterized by an apparent increase in zonal flow that c…

Mesoscale meteorologyThermal lowMonsoon[SDE.MCG] Environmental Sciences/Global Changes[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysics[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyZonal flowGeneral Earth and Planetary SciencesEnvironmental scienceMM5[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyScale modelSeasonal cycleComputingMilieux_MISCELLANEOUSDownscaling
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El Ciclo Ándico de Groeber en la cuenca Neuquina, una revisión y actualización.

2022

A state of the knowledge of the Andean cycle is presented, mainly based on our recent works, butalso on highlights of recent research of many colleagues. This synthesis allowed us to update thegeochronology of its different units. New absolute ages through U-Pb analysis in zircons by differentmethods complement those previously carried out and made possible to accurately limit the ageof these units. We have been able to define the boundary between the Tordillo and Vaca MuertaFormations very precisely between 147 and 146 Ma; the age of the Agrio Formation between 132 and126 Ma, and to present the first absolute ages of the Huitrín Formation. All these data are screenedthrough precise biostra…

Mesozoico[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyEstratigrafíaAndesGeocronologíaPaleontología
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Dust Production and Particle Acceleration in Supernova 1987A Revealed with ALMA

2013

Supernova (SN) explosions are crucial engines driving the evolution of galaxies by shock heating gas, increasing the metallicity, creating dust, and accelerating energetic particles. In 2012 we used the Atacama Large Millimeter/Submillimeter Array to observe SN 1987A, one of the best-observed supernovae since the invention of the telescope. We present spatially resolved images at 450um, 870um, 1.4mm, and 2.8mm, an important transition wavelength range. Longer wavelength emission is dominated by synchrotron radiation from shock-accelerated particles, shorter wavelengths by emission from the largest mass of dust measured in a supernova remnant (>0.2Msun). For the first time we show unambig…

MetallicityAstrophysics::High Energy Astrophysical PhenomenaFOS: Physical sciencesSynchrotron radiationAstrophysicsAstrophysics::Cosmology and Extragalactic AstrophysicsSubmillimeter ArrayEARLY UNIVERSEindividual (1987A) [supernovae]Magellanic CloudsAstrophysics::Solar and Stellar AstrophysicsEjectaSupernova remnantSolar and Stellar Astrophysics (astro-ph.SR)Astrophysics::Galaxy AstrophysicsQBHigh Energy Astrophysical Phenomena (astro-ph.HE)PhysicsISM [galaxies]supernova remnants [ISM]Astronomy and AstrophysicsOPTICAL-PROPERTIESHUBBLE-SPACE-TELESCOPEAstrophysics - Astrophysics of GalaxiesEVOLUTIONGalaxyParticle accelerationEJECTASupernovaPhysics and AstronomyAstrophysics - Solar and Stellar AstrophysicsSpace and Planetary ScienceAstrophysics of Galaxies (astro-ph.GA)REVERSE SHOCKREMNANTAstrophysics::Earth and Planetary AstrophysicsEMISSIONAstrophysics - High Energy Astrophysical PhenomenaMASSIVE STARSSN 1987A
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