Search results for "Easter"

showing 10 items of 348 documents

Cave bear occupation in Schwabenreith Cave, Austria, during the early last glacial: constraints from 230 Th/U‐dated speleothems

2019

The cave bear was a prominent member of the Upper Pleistocene fauna in Eurasia. While breakthroughs were recently achieved with respect to its phylogeny using ancient DNA techniques, it is still challenging to date cave bear fossils beyond the radiocarbon age range. Without an accurate and precise chronological framework, however, key questions regarding the palaeoecology cannot be addressed, such as the extent to which large climate swings during the last glacial affected the habitat and possibly even conditioned the final extinction of this mammal. Key to constraining the age of cave bear fossils older than the lower limit of radiocarbon dating is to date interlayered speleothems using 23…

/dk/atira/pure/subjectarea/asjc/1200/1201geographygeography.geographical_feature_categoryEastern AlpsbiologyPalaeontologyPaleontologySpeleothemTh/U datingbiology.organism_classificationArchaeologyArts and Humanities (miscellaneous)Cave/dk/atira/pure/sustainabledevelopmentgoals/climate_actionSDG 13 - Climate ActionEarth and Planetary Sciences (miscellaneous)Cave bearcave bear/dk/atira/pure/subjectarea/asjc/1900/1901/dk/atira/pure/subjectarea/asjc/1900/1911Glacial periodearly last glacialspeleothemGeologyJournal of Quaternary Science
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Seasonal Analysis of Surface Soil Moisture Dry-Downs in a Land-Atmosphere Hotspot as Seen by LSM and Satellite Products

2018

The soil drying process is a challenging framework to assess climatic, hydrologic and ecosystem processes. This work develops a seasonal analysis of temporal e-folding decay ( $\tau$ ) of surface soil moisture dry-downs using ORCHIDEE land surface model and SMOS observations over South Eastern South America (SESA). Results show that the soil drying process depends on both location and season, and that the modeled drying velocity is faster than the observed one, even when modeled data is sampled at the same frequency as the observations. Differences between observed and modeled data have been found both in the analysis of the regional overall $\tau$ and in the spatial patterns of $\tau$ esti…

010504 meteorology & atmospheric sciences0208 environmental biotechnology02 engineering and technologyAtmospheric sciences01 natural sciences020801 environmental engineeringHotspot (geology)Spatial ecologyEnvironmental scienceEcosystemWater contentSoil dryingSouth eastern0105 earth and related environmental sciencesIGARSS 2018 - 2018 IEEE International Geoscience and Remote Sensing Symposium
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Kinematics, deformation partitioning and late Variscan magmatism in the Agly massif, Eastern Pyrenees, France

2020

International audience; In order to constrain the finite deformation pattern of the Variscan basement of the Agly massif, a detailed structural analysis over the whole Agly massif was performed. Our investigation combined geological mapping, reappraisal of published and unpublished data completed with our own structural work. Results are provided in the form of new tectonic maps and series of regional cross-sections through the Agly massif. At variance from previous studies, we identified three deformation fabrics named D1, D2 and D3. The D1 deformation is only relictual and characterized by a broadly northwest-southeast striking and eastward dipping foliation without any clear mineral and …

010504 meteorology & atmospheric sciencesCrustal thinningPlutonGneiss domeMetamorphism[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesTranspressionLineationPetrologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesVariscan orogengeographygeography.geographical_feature_categorylcsh:QE1-996.5GeologyMassifPlutonismAgly Massiflcsh:GeologySinistral and dextral[SDU]Sciences of the Universe [physics]eastern pyreneesShear zoneGeology
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Analysing the effect of land use and vegetation cover on soil infiltration in three contrasting environments in northeast Spain

2017

Este estudio presenta el análisis conjunto de la información obtenida a partir de 195 ensayos de infiltración en el campo, que fueron realizados mediante dispositivos de doble anillo. Los experimentos se realizaron en 20 situaciones contrastadas de usos del suelo, los cuales se encuentran distribuidos en tres contextos geográficos (costa NE de Cataluña, monte bajo del sector central del valle del Ebro y montaña media de la vertiente Sur del Pirineo central). El objetivo de esta investigación es determinar los factores más importantes que explican la variabilidad de la infiltración: uso del suelo, tipo de cubierta vegetal, características del suelo y del substrato rocoso, humedad del suelo y…

010504 meteorology & atmospheric sciencesGeography Planning and DevelopmentSòls -- FiltracióLand coverEnvironmental Science (miscellaneous)infiltrationvegetation cover01 natural sciencesSòls Absorció i adsorcióSòl Ús delVegetation typeEarth and Planetary Sciences (miscellaneous)Water content0105 earth and related environmental sciencesGeography (General)geographygeography.geographical_feature_categorySoil percolationLand useBedrockland useHumidity04 agricultural and veterinary sciencesdouble ring testInfiltration (hydrology)Land useSoil water040103 agronomy & agricultureG1-9220401 agriculture forestry and fisheriesEnvironmental sciencenortheastern spainSòls -- HumitatSoil moisturePhysical geographysoil moistureCuadernos de Investigación Geográfica
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Phanerozoic geological evolution of Northern and Central Africa: An overview.

2005

61 pages; International audience; The principal paleogeographic characteristics of North and Central Africa during the Paleozoic were the permanency of large exposed lands over central Africa, surrounded by northerly and northwesterly dipping pediplanes episodically flooded by epicontinental seas related to the Paleotethys Ocean. The intra-continental Congo–Zaire Basin was also a long-lived feature, as well as the Somali Basin from Late Carboniferous times, in conjunction with the development of the Karoo basins of southern Africa. This configuration, in combination with eustatic sea-level fluctuations, had a strong influence on facies distributions. Significant transgressions occurred duri…

010504 meteorology & atmospheric sciencesPaleozoicPhanerozoicInversion (geology)Northeastern Africa010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesDevonianPaleontologyPassive margin[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg14. Life underwaterNorthern AfricaWestern Africa0105 earth and related environmental sciencesEarth-Surface Processes[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsgeographyNeotethysgeography.geographical_feature_categoryRiftCentral AfricaRiftingArabiaTectonicsInversionMagmatismGeologyOrogeny[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsCraton13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPaleogeographyOrdovicianPaleotethysGeology
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On the occurrence of strong vertical wind shear in the tropopause region: a 10-year ERA5 northern hemispheric study

2021

A climatology of the occurrence of strong wind shear in the upper troposphere–lower stratosphere (UTLS) is presented, which gives rise to defining a tropopause shear layer (TSL). Strong wind shear in the tropopause region is of interest because it can generate turbulence, which can lead to cross-tropopause mixing. The analysis is based on 10 years of daily northern hemispheric ECMWF ERA5 reanalysis data. The vertical extent of the region analyzed is limited to the altitudes from 1.5 km above the surface up to 25 km, to exclude the planetary boundary layer as well as strong wind shear in higher atmospheric layers like the mesosphere–lower thermosphere. A threshold value of St2=4×10-4s-2 of t…

010504 meteorology & atmospheric sciencesPlanetary boundary layerTropical Easterly JetJet stream010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesTroposphereMeteorology. ClimatologyWind shearWalker circulationQC851-999TropopauseStratosphereGeology0105 earth and related environmental sciences
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The north-eastern aeolian ‘European Sand Belt’ as potential record of environmental changes: A case study from Eastern Latvia and Southern Estonia

2016

Abstract The Latvian and Estonian inland dunes belong to the north-eastern part of the ‘European Sand Belt’ (ESB). These dunes are widely distributed over broad glaciolacustrine plains and Late Glacial alluvial deltas, considered to be potential sources for the aeolian material. Little is known about these aeolian sediments and their substratum; here we present a detailed sedimentary structural and textural characterisation together with a luminescence-based chronology. Through a comparison between grain-size, rounding of quartz grains and surface characteristics in medium/coarse (0.5–0.8 mm) sand, and the light mineral content, we found an alternation of aeolian and periglacial components.…

010506 paleontology010504 meteorology & atmospheric sciencesThermoluminescence datingEuropean Sand BeltGeochemistrySedimentGeologyOptically stimulated luminescence01 natural sciencesEastern LatviaSouthern EstoniaSedimentary featuresAeolian depositsAeolian processesSedimentary rockAlluviumAeolian landformGlacial periodGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesChronologyAeolian Research
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A 2500 year record of natural and anthropogenic soil erosion in South Greenland

2012

International audience; The environmental impact of the Norse landnám in Greenland has been studied extensively. But to date, no study has quantified the soil erosion that Norse agricultural practices are believed to have caused. To resolve this problem, a high resolution sedimentary record from Lake Igaliku in South Greenland is used to quantitatively reconstruct 2500 years of soil erosion driven by climate and historical land use. An accurate chronology allows for the estimation of detritic fluxes and their uncertainties. Land clearance and the introduction of grazing livestock by the Norse around 1010 AD caused an acceleration of soil erosion up to 8 mm/century in 1180 AD which is two-fo…

010506 paleontologyArcheology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesGreenland01 natural sciencesNatural (archaeology)Grazing[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentOvergrazing[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangeLand useEastern settlementLandnámAgricultureGeologyVegetation15. Life on land[ SDE.MCG ] Environmental Sciences/Global ChangesOceanographyDisturbance (ecology)13. Climate actionSoil erosionNorseLand degradationErosionPhysical geographyGeologyQuaternary Science Reviews
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A 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian Arctic

2016

A lake sediment record from the north-eastern European Russian Arctic was examined using palaeolimnological methods, including subfossil chironomid and diatom analysis. The objective of this study is to disentangle environmental history of the lake and climate variability during the past 2000 years. The sediment profile was divided into two main sections following changes in the lithology, separating the limno-telmatic phase between ~2000 and 1200 cal. yr BP and the lacustrine phase between ~1200 cal. yr BP and the present. Owing to the large proportion of semi-terrestrial chironomids and poor modern analogues, a reliable chironomid-based temperature reconstruction for the limno-telmatic p…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesta1171chironomidsClimate change01 natural sciencesdiatomsPrecipitation0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeSubfossilEcologybiologyPaleontologySedimentpalaeolimnologybiology.organism_classificationArctic RussiaEastern europeanclimate changequantitative reconstructionDiatomArctic13. Climate actionClimatologyPeriod (geology)ta1181Physical geographyGeologyThe Holocene
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Trilobites from the Red Fauna (latest Emsian, Devonian) of Hamar Laghdad, Morocco and their biodiversity

2018

36 pages; International audience; Trilobites are widespread in Early Devonian deposits of north Gondwana; some of the most emblematic ones were collected from the famous latest Emsian (Early Devonian) mudmound locality Hamar Laghdad in south-eastern Morocco. This locality is famous for its trilobites, especially for the conspicuous red-coloured remains of phacopid trilobites with often greenish eyes. Here, we present a taxonomic revision of the previously described trilobites from the so-called Red Fauna of Hamar Laghdad. We introduce the new taxa Harpes hamarlaghdadensis n. sp. and Morocops davidbrutoni n. sp. Phacopids dominate the trilobite assemblage from the Red Cliff at Hamar Laghdad …

010506 paleontologyFaunaBiodiversity10125 Paleontological Institute and Museum[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomy010502 geochemistry & geophysics01 natural sciencesTafilaltDevoniandiversitytaxonomyPaleontology[SDV.BID.SPT] Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyCliff14. Life underwaterEmsian0105 earth and related environmental sciencesgeography.geographical_feature_categorybiologyvariabilityPalaeontologyTrilobitaPaleontologybiology.organism_classificationTrilobite1911 PaleontologyGondwanaTaxonGeography560 Fossils & prehistoric lifeeastern Anti-Atlas[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyNeues Jahrbuch für Geologie und Paläontologie - Abhandlungen
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