Search results for "Stratigraphy"

showing 10 items of 904 documents

Northern Hemisphere atmospheric pattern enhancing Eastern Mediterranean Transient-type events during the past 1000 years

2021

High-resolution climate model simulations for the last millennium were used to elucidate the main winter Northern Hemisphere atmospheric pattern during enhanced Eastern Mediterranean Transient (EMT-type) events, a situation in which an additional overturning cell is detected in the Mediterranean at the Aegean Sea. The differential upward heat flux between the Aegean Basin and the Gulf of Lion was taken as a proxy of EMT-type events and correlated with winter mean geopotential height at 500 mbar in the Northern Hemisphere (20–90∘ N and 100∘ W–80∘ E). Correlations revealed a pattern similar to the East Atlantic/Western Russian (EA/WR) mode as the main driver of EMT-type events, with the past …

Mediterranean climate010506 paleontologyAlkenoneEUROPEGULF010504 meteorology & atmospheric sciencesDEEPStratigraphyCIRCULATIONGeopotential heightStructural basinEnvironmental protection01 natural sciencesEnvironmental pollutionREGIONAL CLIMATE PALAEOSIMULATIONVARIABILITYEastern Mediterranean TransientTD169-171.8GE1-350SOLAR[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereGlobal and Planetary ChangeSEANorthern HemispherePaleontologyClimate model simulationsEnvironmental sciencesMODELSea surface temperatureEastern mediterraneanTD172-193.513. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyClimate modelSTRAITGeology
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Ages and stratigraphical architecture of late Miocene deposits in the Lorca Basin (Betics, SE Spain): New insights for the salinity crisis in margina…

2020

International audience; Unlike most Neogene basins of the Betic Cordillera where the Salinity Crisis is dated to the Messinian, a contradictory Tortonian dating was proposed for evaporites of the Lorca Basin. As a consequence, complex structural models have been proposed in the literature to explain this discrepancy in the timing of evaporites. In order to integrate the Lorca Basin into the geological context of the western Mediterranean domain during the Late Miocene, new sedimentological and stratigraphical studies coupled with new dating were performed, which allow us to propose a Messinian age for both diatomite-bearing deposits and evaporites of the Lorca Basin. These new ages challeng…

Mediterranean climate010506 paleontologyEvaporiteStratigraphyStructural basinLate Mioceneengineering.material010502 geochemistry & geophysicsNeogene01 natural sciencesUnconformityBase-level fluctuationsPaleontologyMessinian0105 earth and related environmental sciencesTortonianBrackish waterGeologySalinity crisisBeticss Lorca BasinSpain[SDU]Sciences of the Universe [physics]Lorca Basin[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBase-level fluctuationengineeringHaliteGeology
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2018

Abstract. The 4.2 ka BP event is defined as a phase of environmental stress characterized by severe and prolonged drought of global extent. The event is recorded from the North Atlantic through Europe to Asia and has led scientists to evoke a 300-year global mega-drought. For the Mediterranean and the Near East, this abrupt climate episode radically altered precipitation, with an estimated 30 %–50 % drop in rainfall in the eastern basin. While many studies have highlighted similar trends in the northern Mediterranean (from Spain to Turkey and the northern Levant), data from northern Africa and the central-southern Levant are more nuanced, suggesting a weaker imprint of this climate shift on…

Mediterranean climate010506 paleontologyGlobal and Planetary ChangeClimate patternDead seaMiddle East010504 meteorology & atmospheric sciencesStratigraphyClimate shiftPaleontology15. Life on landStructural basin01 natural sciencesAridGeography13. Climate actionPhysical geographyPrecipitation0105 earth and related environmental sciencesClimate of the Past
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The Albian (Vraconnian)-Cenomanian boundary at the western Tethyan margins (Central Tunisia and southeastern France).

2008

AbstractThrough the description and interpretation of the position of macro- and microfossils in several sections of the Albian-Cenomanian boundary in SE France and Central Tunisia, a comparison is made between the north and south margins of the Tethyan Ocean by using the occurrences of marker bioevents. For the planktonic foraminifera, the criterions applicable for the accurate determination of Thalmanninella globotruncanoides (Sigal) – the marker species for the base of the Cenomanian stage – are discussed. The species Th. globotruncanoides and the intermediate forms with its ancestor Th. caroni (Ion) are illustrated. For the ammonites, two subjects are new. Firstly, the species Stoliczka…

Mediterranean climate010506 paleontologyPlanktonic foraminiferaTunisiaStoliczkaiaSouth France010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesForaminiferaPaleontologyStage (stratigraphy)Ammonites14. Life underwater0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologybiologyUtaturicerasGeologyVraconnianbiology.organism_classificationAlbian-Cenomanian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyCenomanian[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Reconstruction of the paleoenvironmental changes around the Miocene-Pliocene boundary along a W-E transect across the Mediterranean

2006

Abstract In order to reconstruct the environmental changes at the end of the Messinian salinity crisis, a multidisciplinary study has been carried out with a high sampling resolution of the late Messinian–early Zanclean (Zone MPl 1) sediments along a West–East Mediterranean transect. The studied examples comprise sections from southern Spain (Vera/Almanzora), Balearic Basin (ODP Site 975), Tyrrhenian Basin (ODP Site 974), Sicily (Eraclea Minoa), Zakynthos (Kalamaki), Corfu (Aghios Stefanos), Crete (Aghios Vlasis). Previously analyzed sections from the Levantine Basin (Cyprus and ODP Sites 968 and 969) are used for comparison. The sections have been correlated using planktonic foraminiferal …

Mediterranean climate010506 paleontologySettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18OStratigraphy[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesMediterranean areaPlanktonic foraminiferMiocene–Pliocene transitionPaleontologyStratotype14. Life underwaterSedimentologyTransect0105 earth and related environmental sciencesSettore GEO/06 - Mineralogiaδ13CbiologyGeologySedimentologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationStable isotope6. Clean waterSettore GEO/08 - Geochimica E VulcanologiaAmmonia tepida13. Climate actionFaciesGeology
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Atopidae (Trilobita) in the upper Marianian (Cambrian Series 2, Stage 4) of Iberia

2020

AbstractNew atopid trilobites are described from the early Cambrian Cumbres beds and Herrerías shale of northern Huelva Province (Andalusia, Spain) and are dated as middle–late Marianian (Cambrian Series 2, Stage 4). New specimens ofAtops calanusRichter and Richter, 1941 are described and the Laurentian speciesPseudatops reticulatus(Walcott, 1890b) is recognized for the first time in the Mediterranean subprovince. The associated trilobite assemblage studied herein suggests an age close to the base of Cambrian Stage 4.

Mediterranean climate010506 paleontologybiologyPseudatopsPaleontologyCambrian Stage 4010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesAtopsTrilobitePaleontologyStage (stratigraphy)CalanusCambrian Series 2Geology0105 earth and related environmental sciencesJournal of Paleontology
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Paleoenvironments and human adaptations during the Last Glacial Maximum in the Iberian Peninsula: A review

2021

Abstract The Iberian Peninsula is considered one of the most well-suited regions in Europe to develop studies on the relationship between environmental changes and human adaptations across the Late Pleistocene. Due to its southwesternmost cul-de-sac position and eco-geographical diversity, Paleolithic Iberia was the stage of cyclical cultural/technological changes, linked to fluctuations in climate and environments, human demographics, and the size, extension, and type of social exchange networks. Such dynamics are particularly evident during the Last Glacial Maximum (LGM) timeframe, with a series of innovations emerging in the archaeological record, marking the transitions between the trad…

Mediterranean climate010506 paleontologygeographygeography.geographical_feature_categoryPleistoceneArchaeological recordLast Glacial Maximum010502 geochemistry & geophysicsSolutrean01 natural sciencesPeninsulaStage (stratigraphy)Physical geographyMagdalenian0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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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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Paleoclimatic control of biogeographic and sedimentary events in Tethyan and peri-Tethyan areas during the Oxfordian (Late Jurassic)

2005

International audience; The paleobiogeographical distribution of Oxfordian ammonites and coral reefs in northern and Central Europe, the Mediterranean area, North and East Africa, and the Middle East and Central Asia is compared with the distribution in time and space of the most important lithofacies. Interest in the Oxfordian is focused on changes in facies and in biogeographical patterns that can be interpreted as the results of climatic events. Paleotemperature trends inferred from oxygen isotopes and paleoclimatic simulations are tested against fossil and facies data. A Late Callovian–Early Oxfordian crisis in carbonate production is indicated by the widespread absence of Lower Oxfordi…

Mediterranean climate010506 paleontologyδ18OHiatus010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyPaleobiogeography01 natural sciencesIsotopes of oxygenOxfordianchemistry.chemical_compoundPaleontologyAmmonites14. Life underwaterTethysPaleoclimates[SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categoryPaleontologyCoral reefchemistry13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesCoralsCarbonateSedimentary rock[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology[ SDU.STU.AG ] Sciences of the Universe [physics]/Earth Sciences/Applied geology
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Effects of afforestation with four unmixed plant species on the soil–water interactions in a semiarid Mediterranean region (Sicily, Italy)

2012

Purpose An assessment of the effect of plant cover on the properties of four afforested soils in central Sicily was performed with the aim of discriminating among them after 60 years of afforestation. Materials and methods Chemical and biochemical soil analyses were coupled to fast field cycling (FFC) NMR relaxation investigations in order to monitor surface interactions of water in water-saturated soils. Results and discussion The traditional soil analyses revealed that the most stable soil properties such as soil texture and pH are not affected by 60 years of afforestation. Soils developed under eucalyptus trees showed larger amounts of hydrophilic organic matter as compared to the soils …

Mediterranean climateAgroforestryStratigraphymedia_common.quotation_subjectSettore AGR/13 - Chimica AgrariaSoil biochemical propertieDesertificationAfforestationSoil waterPlant speciesWater molecular dynamicsAfforestationEnvironmental sciencePlant coverDesertificationFFC-NMREarth-Surface Processesmedia_commonJournal of Soils and Sediments
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