Search results for "NK"

showing 10 items of 14343 documents

Thermal and structural modeling of the Scillato wedge-top basin source-to-sink system. Insights into the Sicilian fold-and-thrust belt evolution (Ita…

2019

AbstractTemperature-dependent clay mineral assemblages, vitrinite reflectance, and one-dimensional (1-D) thermal and three-dimensional (3-D) geological modeling of a Neogene wedge-top basin in the Sicilian fold-and-thrust belt and its pre-orogenic substratum allowed us to: (1) define the burial history of the sedimentary succession filling the wedge-top basin and its substratum, (2) reconstruct the wedge-top basin geometry, depocenter migration, and sediment provenance through time in the framework of a source-to-sink system, and (3) shed new light into the kinematic evolution of the Apennine-Maghrebian fold-and-thrust belt.The pre-orogenic substratum of the Scillato basin shows an increase…

010504 meteorology & atmospheric sciencesmixed layers illite-smectiteStratigraphyCenozoic deformation[SDU.STU]Sciences of the Universe [physics]/Earth SciencesReflectionStructural basin010502 geochemistry & geophysics01 natural sciencesWedge (geometry)Paleontologywedge-top basin; vitrinite reflectance; mixed layers illite-smectite; thermal modelling; source-to-sink systems; Sicilian fold-and-thrust beltSicilian fold-and-thrust beltThermalthermal modellingClay mineralSedimentologySource to sinkEurope faultsvitrinite reflectancesource-to-sink systems0105 earth and related environmental sciencesMesozoic sedimentary rocks tectonicsgeographygeography.geographical_feature_categoryFaultingGeologySedimentology15. Life on landwedge-top basinlanguage.human_languageStratigraphyFold and thrust beltlanguageThree dimensional computer graphicsSicilianGeologyTertiary
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Productivity modes in the Mediterranean Sea during Dansgaard–Oeschger (20,000–70,000 yr ago) oscillations

2013

The study of planktonic organisms during abrupt climatic variations of the last glacial period (Dansgaard-Oeschger oscillations, D-O) may reveal important insights on climatic, oceanographic and biological interactions. Here we present planktic foraminifera and coccolithophore data collected at the Ocean Drilling Program Site 963 (Sicily Channel), with a mean sampling resolution of respectively 43.5 and 98.9. yr, over the interval between 70,000 and 20,000. yr ago. The paleoenvironmental reconstruction suggests that three different scenarios can be seen across each D-O cycle: 1. oligotrophic surface water and a deep thermocline for the early Interstadials; 2. a Deep Chlorophyll Maximum and …

010506 paleontology010504 meteorology & atmospheric sciencesCoccolithophoreMediterraneanOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnMediterranean seaPaleoproductivity Dansgaard–Oeschger Mediterranean Planktonic Foraminifera CoccolithophoresCoccolithophores14. Life underwaterStadialGlacial periodSDG 14 - Life Below WaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesDeep chlorophyll maximumbiologyPaleontologybiology.organism_classificationOceanography13. Climate actionClimatologyPlanktonic ForaminiferaDansgaard-OeschgerThermoclineGeologyPaleoproductivityPalaeogeography, Palaeoclimatology, Palaeoecology
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Du Néolithique récent à l’âge du Bronze dans le Centre Nord de la France : les étapes de l’évolution chrono-culturelle

2011

Die seit 2001 im Rahmen eines PCR (Programme Collectif Régional) durchgeführte Gemeinschaftsarbeit über das Ende des Neolithikums und den Beginns der Bronzezeit im Zentrum Nordfrankreichs führt heute zu einer neuen Periodisierung der Zeit zwischen 3600 und 1800 v. Chr. in acht Etappen. Obwohl, insbesondere bezüglich der Transition zwischen dem Mittel-und dem Jungneolithikum einerseits und dem Jung-und dem Endneolithikum andererseits, auch weiterhin einige Lücken bestehen, erlaubt dieser präzisere Rahmen die Hauptetappen im Zentrum Nordfrankreichs mit denen der benachbarten Regionen zu synchronisieren, um eine dynamischere Vision der kulturellen Phänomene vorzuschlagen.

010506 paleontology060102 archaeologyCampaniformemedia_common.quotation_subjectNéolithiqueJungneolithikum ; Endneolithikum ; Frühbronzezeit ; Chronologie ; Zentrum Nordfrankreichs06 humanities and the artsArt01 natural sciences[SHS]Humanities and Social SciencesLate Neolithic ; central part of northern France ; Chronology ; Early Bronze Age ; Final NeolithicChronologie 14C AMSAge du BronzeBronze Age[ SHS ] Humanities and Social Sciences0601 history and archaeologyPharmacology (medical)[SHS] Humanities and Social SciencesBronze ancien ; Néolithique récent ; Néolithique final ; chronologie ; Centre Nord de la FranceHumanitiesNord de la FranceComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesmedia_common
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Wildcat scats: Taphonomy of the predator and its micromamal prey

2019

Small sized felids, such as wild and domestic cats, are one of the most common predators in the nature and in sites occupied by humans in archaeological and historical contexts. Wildcats have ingestion/ digestion traits highly destructive for their prey, i.e.: teeth to chew causing extreme breakage, and digestion along the entire digestive tract with low pH gastric juices causing extreme bone corrosion. Small sized cats are also well known to play with the prey and select skeletal parts to ingest. The present study is focused on the taphonomic analysis of micromammal remains recovered from scats produced by European wildcats (Felis silvestris silvestris) during several months and years. Exc…

010506 paleontologyArcheologyTaphonomy010504 meteorology & atmospheric sciencesZoologyMicromammals01 natural sciencesPredationFelis silvestris silvestris WildcatTaxonomic compositionAbundance (ecology)Taxonomic rankPredatorEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangebiologyFelisGeologybiology.organism_classificationCarnivoresTaphonomyFelidsDigestionMontes do Invernadeiro Natural Park (Galicia Spain)
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Environmental responses of past and recent agropastoral activities on south Greenlandic ecosystems through molecular biomarkers

2016

Paleoenvironmental studies previously performed on Lake Igaliku revealed two agropastoral phases in south Greenland: the Norse settlement from AD 986 to ca. AD 1450 and the recent installation of sheep farmers, since the 1920s. To improve the knowledge of the timing and magnitude of the Greenlandic agropastoral activities, a lipid inventory was realized and compared with biological and geochemical data. During the 12th century, a major increase in deoxycholic acid (DOC) and coprophilous fungal spores revealed a maximum of herbivores. Synchronously, a minimum of the n-C29/ n-C31 alkane ratio and tree and shrub pollen and a maximum of triterpenyl acetates showed a reduction in the tree and s…

010506 paleontologyArcheologysouth Greenlandved/biology.organism_classification_rank.specieslake sediments010502 geochemistry & geophysicsmedicine.disease_cause01 natural sciencesShrubmolecular biomarkersPollenGrazingmedicine[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentEcosystemRumex[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeHerbivoreEcologybiologyEcologyved/biologyPaleontology15. Life on landbiology.organism_classificationMolecular biomarkersagropastoral activities13. Climate actionPlant speciesNorseGeologyecosystem responses
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Terrestrial plants and marine algae from the Late Jurassic lithographic limestone of the Causse Méjean (Lozère, southern France)

2016

International audience; A new Late Jurassic flora was discovered in the fossiliferous lithographic limestone of the Causse Méjean, Lozère (southern France). It consists of the first Kimmeridgian/Tithonian plants from this area. Fossil plants are represented by megaremains preserved as impressions. This flora shows a co-occurrence of terrestrial plants and marine algae. The land plants include vegetative remains ascribed to bennettitaleans (Zamites Brongniart, 1828), conifers (Brachyphyllum Brongniart, 1828), and pteridosperms (Cycadopteris Zigno, 1853). Marine algae were ascribed to dasyclads (Goniolina D’Orbigny, 1850). Lithological and palaeontological features suggest preservation in a f…

010506 paleontologyFloraved/biology.organism_classification_rank.speciesLate JurassicContext (language use)010502 geochemistry & geophysics01 natural sciencesBennettitaleansBrachyphyllumPaleontologyAlgaeTerrestrial plant14. Life underwaterPteridospermsDasycladales0105 earth and related environmental sciencesZamites[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiologyved/biologyEcologyDasycladslcsh:QE1-996.5PtéridospermesGeologyVegetation15. Life on landbiology.organism_classificationConifèreslcsh:GeologyConifersHabitatJurassique terminalBennettitalesBassin des Causses.[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCausses basin.GeologyCausses basin
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The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years

2016

AbstractThe Mediterranean Sea is an ideal location to test the response of organisms to hydrological transformations driven by climate change. Here we review studies carried out on planktonic foraminifera and coccolithophores during the late Quaternary and attempt the comparison of data scattered in time and space. We highlight the prompt response of surface water ecosystems to both orbital- and suborbital-climatic variations.A markedly different spatial response was observed in calcareous plankton assemblages, possibly due to the influence of the North Atlantic climatic system in the western, central and northern areas and of the monsoon system in the easternmost and southern sites. Orbita…

010506 paleontologyQE1-996.5010504 meteorology & atmospheric sciencesGeologyForcing (mathematics)Environmental Science (miscellaneous)Plankton01 natural scienceslate quaternaryMediterranean seaOceanographyplanktonic foraminiferaClimatologyGeneral Earth and Planetary SciencesEcosystemUniquenessmediterranean seacoccolithophoresGeology0105 earth and related environmental sciencesOpen Geosciences
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An aeolian or a glaciolacustrine record? A case study from Mieļupīte, Middle Gauja Lowland, northeast Latvia

2017

Abstract In the Middle Gauja Lowland, northeast Latvia, dunes are distributed over a vast glaciolacustrine plain that formed during the retreat of the Fennoscandian ice sheet. Such a direct contact between aeolian and glaciolacustrine sediments can be used to infer depositional settings and decipher to what extent these sediments bear an aeolian component. Our proxies, although preliminary, reveal a limited range of variation in grain-size parameters, a significant presence of quartz grains with silica precipitation and matt-surface grains of various rounding degrees and massive structure combined with horizontal lamination. These are indicative of periglacial-aeolian depositional condition…

010506 paleontologyQE1-996.5Optically stimulated luminescenceEarth sciencequartz grainsGeologyBaltic states010502 geochemistry & geophysicsbaltic states01 natural sciencesduneice-dammed lakelinkuva ice-marginal zoneGeneral Earth and Planetary SciencesAeolian processesLinkuva ice-marginal zoneoptically stimulated luminescenceGeomorphologyGeology0105 earth and related environmental sciencesGeologos
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Integrated bio- and carbon-isotope stratigraphy of the Upper Cretaceous Gurpi Formation (Iran): A new reference for the eastern Tethys and its implic…

2018

29 pages; International audience; A high-resolution stratigraphic analysis of the Upper Cretaceous Gurpi Formation has been undertaken in the Shahneshin section (Zagros Basin, Iran). New results on calcareous nannofossils, planktic foraminifers, dinoflagellate cysts and high-resolution carbon and oxygen stable isotopes form the basis of a reference section for the eastern Tethys that spans the upper Coniacian to the late Danian. Carbon-isotope correlation to Gubbio, Italy and the NW German chalk allows for the identification of many isotopic events as well as for the definition of new events in the Campanian and Maastrichtian. Our results allow for a review of the accurate position of the C…

010506 paleontologyStructural basin010502 geochemistry & geophysics01 natural sciencesPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryStage (stratigraphy)Calcareous nannofossils14. Life underwater0105 earth and related environmental sciencesbiologyStable isotope ratioDinoflagellate cystsCarbon isotopesDinoflagellatePaleontologyPlanktic foraminiferaPlanktonbiology.organism_classificationZagrosCretaceousStratigraphy13. Climate actionIsotopes of carbonTethyan realm[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyConiacian–MaastrichtianGeologyCretaceous Research
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Biostratigraphy and isotope stratigraphy of upper Maastrichtian–Danian marine deposits of the Kopet-Dagh Basin, northeast Iran

2018

Abstract Biostratigraphy, using foraminifera and echinoids, plus high-resolution carbon isotope stratigraphy of the upper Maastrichtian–Danian interval in the western part of the Kopet-Dagh Basin in northeast Iran are outlined. Our study of shallow-marine carbonate platform deposits of the Kalat Formation, rich in larger benthic foraminifera (predominantly Clypeorbis mammillatus Schlumberger, Lepidorbitoides sp. and Siderolites calcitrapoides Lamarck), has allowed the definition of a C. mammillatus-S. calcitrapoides Assemblage Zone, of late Maastrichtian age. Clypeorbis mammillatus is here recorded for the first time from the Maastrichtian Kalat Formation and represents the most easterly fi…

010506 paleontologybiologyCarbonate platformMesozoic Cenozoic Clypeorbis mammillatus Kalat Formation Chehel Kaman Formation Planktonic foraminifera Isotope stratigraphy.PaleontologyBiozoneBiostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousForaminiferaPaleontologyStratigraphyEchinocorysCenozoicGeology0105 earth and related environmental sciences
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