Search results for "96"

showing 10 items of 2333 documents

The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems

2018

Stable isotope records from speleothems provide information on past climate changes, most particularly information that can be used to reconstruct past changes in precipitation and atmospheric circulation. These records are increasingly being used to provide “out-of-sample” evaluations of isotope-enabled climate models. SISAL (Speleothem Isotope Synthesis and Analysis) is an international working group of the Past Global Changes (PAGES) project. The working group aims to provide a comprehensive compilation of speleothem isotope records for climate reconstruction and model evaluation. The SISAL database contains data for individual speleothems, grouped by cave system. Stable isotopes of oxyg…

010506 paleontologyClimate Research010504 meteorology & atmospheric sciencesClimate changeSpeleothemF800010502 geochemistry & geophysicscomputer.software_genre01 natural sciencesKlimatforskningCavePaleoclimatologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350geographygeography.geographical_feature_categoryDatabaseStable isotope ratiospeleothemsPALEOCLIMATOLOGIAlcsh:QE1-996.5lcsh:GeologyMetadata13. Climate actionGeneral Earth and Planetary SciencesEnvironmental scienceClimate modelcomputerChronologyEarth System Science Data
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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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Ocre, hematites y óxido de hierro: el problema terminológico = Ochre, Hematite and Iron Oxid: The Terminological Issue

2016

Los óxidos de hierro son prácticamente omnipresentes al analizar contextos, no solo referentes al arte rupestre, sino también en relación con toda una serie de actividades que podríamos considerar cotidianas en ambientes prehistóricos. Sin embargo, su estudio sistemático no ha comenzado hasta tiempos muy recientes. Fruto de ello, podría decirse que una parte de la literatura arqueológica no especializada en el campo de la pigmentología muestra, en ocasiones, cierta inexactitud terminológica. Con este documento pretendemos, a través de un análisis tanto de su funcionamiento, como de las propiedades geoquímicas y mineralógicas del ocre, la hematites y los propios óxidos de hierro, exponer la …

010506 paleontologyHistorylcsh:Prehistoric archaeology01 natural sciencesTerminologyPrehistoryocreterminologyIron oxide0601 history and archaeologylcsh:CC1-960terminología0105 earth and related environmental sciences060102 archaeologyochre06 humanities and the artsArchaeologylcsh:Auxiliary sciences of historylcsh:Clcsh:ArchaeologyHematitespigments.Rock artlcsh:GN700-890pigmentos =Hematiteóxido de hierroEspacio Tiempo y Forma. Serie I, Prehistoria y Arqueología
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Introduction. Leave no stone unturned: Perspectives on ground stone artefact research

2016

Ground stone tools served in many physical and social contexts through millennia, reflecting a wide variety of functions. Although ground stone tool studies were neglected for much of early archaeology, the last few decades witnessed a notable international uptick in the way archaeologists confront this multifaceted topic. Today, with the advance of archaeology as a discipline, research into ground stone artefacts is moving into a new phase that integrates high resolution documentation with new methodological, analytical techniques, and technological approaches. These open new vistas for an array of studies and wide-ranging interpretive endeavours related to understanding ground stone tool …

010506 paleontologyHistorymedia_common.quotation_subjectGlobeHigh resolution01 natural sciencesVisual artsground stone toolsPresentationDocumentationmedicine0601 history and archaeologyanthropologylcsh:CC1-960food production0105 earth and related environmental sciencesmedia_commonAGSTR060102 archaeologyGround stonearchaeology06 humanities and the artsArchaeologyVariety (cybernetics)medicine.anatomical_structurelcsh:ArchaeologyJournal of Lithic Studies
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Fossiliferous Holocene tufa of Mende (Lozère, southern France): implication for the Atlantic vegetation of the Causses Basin

2016

International audience; Tufas bearing plant macroremains are uncommon in the Causses Basin (southern France). Here, we report anew fossiliferous tufa deposits at Mende, in Lozère. This palaeontological site is the first Quaternary tufa from thenorthern part of the Causses Basin that yields such an abundance of plant macroremains. The radiocarbon dating showsthat these Holocene deposits are related to the Atlantic period. Geomorphology and mineralogy show that theplant-bearing deposit is a calcareous tufa only composed by calcite, deposited near to an outlet of cool water, linked tothe karstic hydrological system of the Causse de Mende. The flora exposed in this article is dominated by angio…

010506 paleontologyLeavesAngiosperms010504 meteorology & atmospheric sciencesTilia cordataStructural basin01 natural sciencesTufslaw.inventionFeuillesPaleontologyLozèrelawRadiocarbon datingCausses BasinHolocene0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categoryBassin des CaussesHolocenebiologylcsh:QE1-996.5GeologyVegetationTufasbiology.organism_classificationKarstlcsh:GeologyTufaAngiospermesQuaternary[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyHolocène
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The Borschovo section of the Gauja and Amata regional stages (Leningrad Region, Russia): sedimentology and biostratigraphy

2018

The results of the detailed sedimentological study and bed-by-bed collecting of fossils from the Borschovo section exposing the upper Givetian–lower Frasnian boundary beds are discussed. The succession consists of sandstones alternating with argillaceous and clayey packages that contain vertebrate and plant remains in the upper part. The grain size, sedimentary structures and cross-bed orientation considerably differ in the Oredezh Beds and the Staritsa Beds. Fine- to coarse-grained cross-stratified sandstones of the Oredezh Beds most probably are fluvial deposits, whereas the sandstones of the Staritsa Beds yielding tidal structures that show variable directions of the cross-bedding were a…

010506 paleontologyMiddle–Upper Devonianbiologylcsh:QE1-996.5Biostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural scienceslcsh:GeologyPaleontologyAmataSection (archaeology)sedimentary environmentGeneral Earth and Planetary Sciencessiliciclastic depositsSedimentologyvertebrate assemblage.Geology0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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Stage boundaries, global stratigraphy, and the time scale: towards a simplification

2004

International audience; This paper examines four facets of stratigraphic terminology and usage considered faulty and proposes corrective measures. The four perfectible areas are: (1) The system of dual nomenclature requiring discrete terminologies for the superpositional and temporal aspects of rock units. (2) The premise that a GSSP establishes the base of a stage as being coincident with the top of the preceding stage rather than simply defining it as the boundary between stages. (3) The rejection of supplementary (auxiliary) sections that would broaden the knowledge of a GSSP and enlarge the area in which it is easily usable. (4) The current dual system of nomenclature for Precambrian an…

010506 paleontologyPrecambrian-Cambrian boundaryComputer scienceStratigraphyPhanerozoiccomputer.software_genre[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCampanian-Maastrichtian boundaryBoundary (real estate)Terminologylcsh:StratigraphyStage (stratigraphy)Stages010503 geologyStratigraphy (archaeology)lcsh:QE701-7600105 earth and related environmental scienceslcsh:QE640-699GSSPChronostratigraphybusiness.industryScale (chemistry)Plio-Quaternarylcsh:QE1-996.5PaleontologyGeologyTerminologyPlio- QuaternaryCretaceous- Palaeogene boundaryDual (category theory)Global Boundary Stratotype Section and Pointlcsh:GeologyCretaceous-Palaeogene boundarylcsh:Paleontology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPremise[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyArtificial intelligencebusinessPrecambriancomputerNatural language processing
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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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Problems in the identity of "Crioceras" barremense Kilian, 1895 (Ancyloceratida, Late Barremian), and their proposed resolution

2010

17 pages; The study of "Crioceras" barremense KILIAN was undertaken as a part of the revision of the Hemihoplitidae. This species was considered "classic" and has been used as the index of an Upper Barremian subzone; this usage raises a number of problems. The type specimen from Tyrol was a fragment described and illustrated by UHLIG as Crioceras sp. ind. aff. roemeri. This specimen could not be retrieved, and a topotype could not be collected. Our study revealed that there is both a biostratigraphic hiatus and important differences between conceptions of this species: (1) that ascribed UHLIG's type specimen (Upper Barremian, Tyrol), (2) KILIAN's concept of the specimen he found and named "…

010506 paleontologyStratigraphyHiatusAmmonitinae[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesLower limitPaleontologylcsh:StratigraphyGenusmedicinelcsh:QE701-760Gassendiceras[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesConfusionTaxonomylcsh:QE640-699Upper Barremianbiologylcsh:QE1-996.5PaleontologybiozonationGeologyAlpinum Subzonebiology.organism_classificationlcsh:GeologyBiohorizonlcsh:Paleontology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyAlpinum Subzone / BiohorizonGassendiceratinae[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyType specimen[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyVandenheckei Biozonemedicine.symptomsoutheastern France[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCarnets de Géologie
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