Search results for "Global changes"

showing 10 items of 533 documents

An experimental manipulation of life-history trajectories and resistance to oxidative stress

2006

Optimal investment into life-history traits depends on the environmental conditions that organisms are likely to experience during their life. Evolutionary theory tells us that optimal investment in reproduction versus maintenance is likely to shape the pattern of age-associated decline in performance, also known as aging. The currency that is traded against different vital functions is, however, still debated. Here, we took advantage of a phenotypic manipulation of individual quality in early life to explore (1) long-term consequences on life-history trajectories, and (2) the possible physiological mechanism underlying the life-history adjustments. We manipulated phenotypic quality of a co…

Male0106 biological sciencesSenescenceAgingsenescenceOffspringmedia_common.quotation_subject[SDE.MCG]Environmental Sciences/Global ChangesLongevityZoologyfree radicalsBiology010603 evolutionary biology01 natural sciences[ SDV.EE ] Life Sciences [q-bio]/Ecology environment03 medical and health sciencesGeneticsAnimalsEcology Evolution Behavior and Systematics030304 developmental biologymedia_common[SDV.EE]Life Sciences [q-bio]/Ecology environment0303 health sciences[ SDE.BE ] Environmental Sciences/Biodiversity and EcologyEcologyLongevitysenescence.biology.organism_classificationFecundityBiological Evolution[SDE.ES]Environmental Sciences/Environmental and SocietyBrooddisposable-soma theory of agingOxidative Stress[ SDE.MCG ] Environmental Sciences/Global ChangesFertilityPhenotypeAging/physiology; Animals; Evolution; Female; Fertility/physiology; Finches/physiology; Longevity; Male; Oxidative Stress/physiology; PhenotypeAge at first reproductionFemaleFinchesReproductive valueReproduction[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeneral Agricultural and Biological Sciencesresistance to oxidative stressTaeniopygia[ SDE.ES ] Environmental Sciences/Environmental and Societylife-table response experiment
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The beaker phenomenon and the Genomic transformations of Northwest Europe

2018

Bell Beaker pottery spread across western and central Europe beginning around 2750 BCE before disappearing between 2200–1800 BCE. The mechanism of its expansion is a topic of long-standing debate, with support for both cultural diffusion and human migration. We present new genome-wide ancient DNA data from 170 Neolithic, Copper Age and Bronze Age Europeans, including 100 Beaker-associated individuals. In contrast to the Corded Ware Complex, which has previously been identified as arriving in central Europe following migration from the east, we observe limited genetic affinity between Iberian and central European Beaker Complex-associated individuals, and thus exclude migration as a signific…

Male0301 basic medicineSteppeADNNéolithiqueBell BeakerArqueologiaBell Beaker culturegenome wide ancient DNA0302 clinical medicineArchéologiePhenomenonddc:5500601 history and archaeologySuisseHistory Ancient0303 health scienceseducation.field_of_studygeography.geographical_feature_categoryMultidisciplinary060102 archaeology[SDE.IE]Environmental Sciences/Environmental EngineeringHuman migrationPréhistoireNeolithic periodGene PoolGenomics[SHS.GEO]Humanities and Social Sciences/Geography06 humanities and the artsbell BeakerEuropeGeographyArchaeologyCeràmicaEthnologyMégalithisme1000ArchaeogeneticsCampaniformePotteryHuman Migration[SDE.MCG]Environmental Sciences/Global ChangesPopulationAncient historyArticle03 medical and health sciencesSpatio-Temporal Analysispopular geneticsBronze AgeBeakerCultural EvolutionNeolíticgenomicsHumansDNA Ancienteducation030304 developmental biologyChromosomes Human YGenome Humanbusiness.industryNorthwest Europebell Beaker; genome wide ancient DNA; EuropeChalcolithic[SDE.ES]Environmental Sciences/Environmental and SocietyAncient DNAGenetics Population030104 developmental biologyHaplotypesPeriod (geology)GenomicPottery[SDE.BE]Environmental Sciences/Biodiversity and Ecologybusiness030217 neurology & neurosurgery
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Late Pleistocene (MIS 3-4) climate inferred from micromammal communities and δ18O of rodents from Les Pradelles, France.

2013

The middle Paleolithic stratigraphic sequence of Les Pradelles (Charente, France) spans from the end of Marine Isotope Stage (MIS) 4 until the middle of MIS 3. Micromammal remains are present in all the stratigraphic levels, offering a rare opportunity to address the questions of both environmental and climatic fluctuations throughout this period. Climate modes were studied through the taphonomy, biodiversity and oxygen isotope compositions of phosphate (δ18O p ) from 66 samples of rodent tooth enamel. The δ18O p values from the lower sedimentary levels provide summer mean air temperatures of 19 ± 2°C (level 2/1) and of 16 ± 2°C (levels 2A, 2B and 4A). Within the middle of sequence (level 4…

Marine isotope stage010506 paleontologyTaphonomy010504 meteorology & atmospheric sciencesPleistoceneClimate[SDE.MCG]Environmental Sciences/Global ChangesPhosphate01 natural sciencesArts and Humanities (miscellaneous)[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMiddle PaleolithicSmall mammalsDicrostonyx torquatusSequence stratigraphyMicrotus0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRodentbiologyEcology15. Life on landbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryLes PradellesOxygen isotopePleistocene[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate actionPaleoecologyGeneral Earth and Planetary Sciences[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Bayesian calibration of the nitrous oxide emission module of an agro-ecosystem model

2008

1. NitroEurope Open Science Conference on Reactive Nitrogen and the European Greenhouse Gas Balance ; Ghent (Belgique) - (2008-02-20 - 2008-02-21) / Conférence; Nitrous oxide (N2O) is the main biogenic greenhouse gas contributing to the global warming potential (GWP) of agro-ecosystems. Evaluating the impact of agriculture on climate therefore requires a capacity to predict N2O emissions in relation to environmental conditions and crop management. Biophysical models simulating the dynamics of carbon and nitrogen in agro-ecosystems have a unique potential to explore these relationships, but are fraught with high uncertainties in their parameters due to their variations over time and space. H…

Mean squared error[SDE.MCG]Environmental Sciences/Global ChangesBayesian probabilityparameter uncertainty010501 environmental sciencesAtmospheric sciences7. Clean energy01 natural sciencesEcology and Environment[ SDV.EE ] Life Sciences [q-bio]/Ecology environmentsymbols.namesake[STAT.AP] Statistics [stat]/Applications [stat.AP]Ecosystem modelgreenhouse gasesMarkov Chain Monte Carlo0105 earth and related environmental sciences2. Zero hunger[SDV.EE]Life Sciences [q-bio]/Ecology environment[STAT.AP]Statistics [stat]/Applications [stat.AP]EcologyMarkov chainnitrous oxideEcology[ STAT.AP ] Statistics [stat]/Applications [stat.AP]Global warmingMarkov chain Monte Carlo04 agricultural and veterinary sciences15. Life on land[ SDE.MCG ] Environmental Sciences/Global Changes[SDV.EE] Life Sciences [q-bio]/Ecology environment[SDE.MCG] Environmental Sciences/Global ChangesAgriculture and Soil Science13. Climate actionGreenhouse gas040103 agronomy & agriculturesymbols0401 agriculture forestry and fisheriesEnvironmental scienceProbability distributionAnimal Science and ZoologyCERES-EGCAgronomy and Crop Sciencebayesian calibration
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The late Hauterivian Faraoni "Oceanic Anoxic Event" at Río Argos (southern Spain): an assessment on the level of oxygen depletion.

2013

14 pages; International audience; An integrated study of multiple geochemical proxies (TOC, δ13Ccarb, trace metallic elements, iron speciation) on the late Hauterivian Faraoni Oceanic Anoxic Event has been performed along the hemi-pelagic section of Río Argos (south-eastern Spain) in order to better constrain the environmental perturbations linked to this event in the Subbetic domain. In the studied section, the TOC is relatively low (b0.5 wt.%) except for one sample at the base of the Faraoni horizon, where it reaches 1.5 wt.%. The δ13Ccarb signal is characterized by a minor long-term increase, primarily attributed to an enhanced organic matter burial. However, both organic and isotopic si…

Mediterranean climate010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesIron cycle010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesLate HauterivianCarbon cyclePaleontologyIron cycleGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryFaraoni EventOrganic matter0105 earth and related environmental scienceschemistry.chemical_classificationHorizon (archaeology)GeologyCarbon cycle[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryAnoxic watersOAEDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangeschemistryProductivity (ecology)Oxygen concentration variations[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeology
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Holocene climate variability of the Western Mediterranean: Surface water dynamics inferred from calcareous plankton assemblages

2020

A high-resolution study (centennial scale) has been performed on the calcareous plankton assemblage of the Holocene portion of the Ocean Drilling Program Site 976 (Alboran Sea) with the aim to identify the main changes in the surface water dynamic. The dataset also provided a seasonal foraminiferal sea surface water temperatures (SSTs), estimated using the modern analog technique SIMMAX 28, and it was compared with available geochemical and pollen data at the site. Three main climate shifts were identified as (1) the increase in abundance of Syracosphaera spp. and Turborotalita quinqueloba marks the early Holocene humid phase, during maximum summer insolation and enhanced river runoff. It i…

Mediterranean climate010506 paleontologyArcheology010504 meteorology & atmospheric sciencesPaleoclimate[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistorymillennial–centennial-scale climate variability[SDE.MCG]Environmental Sciences/Global ChangesPhysical Geography; GeologyForaminifera01 natural sciencesForaminiferaPaleoclimatologyCoccolithophorescoccolithophore14. Life underwaterComputingMilieux_MISCELLANEOUSHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeEcologybiologyHoloceneMillennial-centennial-scale climate variabilityPaleontologyDrilling15. Life on landPlanktonbiology.organism_classificationAlboran SeaOceanography13. Climate actionMillennial-centennial scale climate variability[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologySurface waterCalcareousGeologyPaleoproductivity
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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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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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Occurrence of CTX-M Producing Escherichia coli in Soils, Cattle, and Farm Environment in France (Burgundy Region).

2012

Article en open access; International audience; CTX-M [a major type of extended-spectrum beta-lactamase (ESBU] producing Escherichia coli are increasingly involved in human infections worldwide. The aim of this study was to investigate potential reservoirs for such strains: soils, cattle, and farm environment. The prevalence of bla(CTX-M) genes was determined directly from soil DNA extracts obtained from 120 sites in Burgundy (France) using real-time PCR. bla(CTX-M) targets were found in 20% of the DNA extracts tested. Samples of cattle feces (n = 271) were collected from 182 farms in Burgundy. Thirteen ESBL-producing isolates were obtained from 12 farms and further characterized for the pr…

Microbiology (medical)Veterinary medicinesolBiodiversité et Ecologie[SDE.MCG]Environmental Sciences/Global ChangesPEDOLOGIElcsh:QR1-502extended-spectrum beta-lactamasefarm environmentbourgogneBiologymedicine.disease_causePastureMicrobiologyextended spectrum beta-lactamaselcsh:MicrobiologyMicrobiologysoilBiodiversity and Ecology03 medical and health sciencesbiologie du solGenotypeLong term survivalmedicineEscherichia coliCTX-MMilieux et Changements globauxEscherichia coliFeces030304 developmental biologyOriginal Researchbactérie2. Zero hunger0303 health sciencesgeographygeography.geographical_feature_category030306 microbiologyadnSoil dnabiochemical phenomena metabolism and nutritionbacterial infections and mycosesManureextended-spectrumbeta-lactamasecattlePEDOLOGIE;extended-spectrumbeta-lactamaseSoil water[SDE.BE]Environmental Sciences/Biodiversity and EcologyBurgundyFrontiers in microbiology
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Les modèles climatiques régionaux : outils de décomposition des échelles spatio-temporelles.

2011

11 pages; National audience; Les modèles climatiques régionaux sont des outils de désagrégation des champs géophysiques, résolvant les équations de la thermodynamique atmosphérique dans le but de simuler à des échelles fines des champs surfaciques tels que la pluviométrie. Prenant à la fois en compte les échelles larges imposées aux bornes du domaine et les échelles plus fines à l'intérieur du domaine (topographie, occupation du sol, types de sol, ...), ces outils sont particulièrement pertinents pour séparer le signal forcé du bruit stochastique inhérent au système climatique. Une méthodologie est ici proposée pour distinguer les différentes échelles spatio-temporelles de la variabilité cl…

Modèle climatique[ SDE.MCG ] Environmental Sciences/Global Changes[SDE.MCG] Environmental Sciences/Global Changes[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyPluviométrie[SDE.MCG]Environmental Sciences/Global ChangesAfrique australeSimulation d'ensemble[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyrégionalReproductibilité
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