Search results for "Palaeogeography"

showing 10 items of 38 documents

Land use change, soil erosion and alluvial dynamic in the lower Doubs Valley over the 1st millenium AD (Neublans, Jura, France)

2003

International audience; Geochemical and particle size analyses, surface scanning magnetic susceptibility, microscopic charcoal counting and pollen analysis, have been carried out on two cores from the lower Doubs valley in order to reconstruct the land use history. The interpretation of anthropogenic pollen indicators and micro-charcoal deposits is discussed in relation to the lithological variation of sedimentary accumulation and evolution of the settlement. The environmental changes which occurred during the 1st and the 6th century AD reflect the impact of human activities on the landscape in the immediate surroundings of the site. Multiproxy indicators indicate that soil erosion as a con…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencespalaeogeographymedicine.disease_cause01 natural sciences[ SHS.ENVIR ] Humanities and Social Sciences/Environmental studies[SHS.ENVIR] Humanities and Social Sciences/Environmental studiesPollenmedicineLand use land-use change and forestryCharcoalpalynologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesHydrologyLand useSurface scanningsedimentology15. Life on landerosionPerturbation (geology)1st millenium ADvisual_art[SHS.ENVIR]Humanities and Social Sciences/Environmental studiesvisual_art.visual_art_mediumAlluviumSedimentary rockPhysical geographyFranceGeologyfire
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Unravelling extrinsic and intrinsic factors of the early Palaeozoic diversification of blastozoan echinoderms

2010

19 pages; International audience; The Subphylum Blastozoa represents more than one third of the early Palaeozoic echinoderm fauna. A comprehensive database including all records of blastozoans was built to provide quantitative analyses of palaeogeography and diversity patterns and processes, for the 10 classes currently included in this subphylum during the early Palaeozoic. The global pattern of taxonomic diversity shows two peaks during the Cambrian Series 3 and the Late Ordovician intervals. In Cambrian times, the high taxonomic diversity seems to be related with a high turnover rate and a high endemicity of blastozoan genera, whereas in Ordovician times, the rise in diversity is associa…

010506 paleontologyPaleozoicEvolutionBlastozoaEvolutionary fauna010502 geochemistry & geophysicsOceanography01 natural sciencesBlastozoaPaleontologyEcology Evolution Behavior and Systematics[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesEarth-Surface ProcessesExtinction eventDiversitybiologyCambrian Series 3EcologyEarly PalaeozoicPaleontology15. Life on landbiology.organism_classification13. Climate actionOrdovicianSiliciclastic[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalaeogeographyOriginationGeologyEchinodermataPalaeogeography, Palaeoclimatology, Palaeoecology
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The space-time relationship of taxonomic diversity and morphological disparity in the Middle Jurassic ammonite radiation.

2007

14 pages; International audience; The Middle Jurassic ammonite radiation (from the late Aalenian to the end of the mid-Bathonian) is traced using combined analyses of morphological disparity and taxonomic diversity. The global signals of disparity and diversity are compared. These signals are then broken down by paleogeographical provinces to detect any heterogeneity in the radiation. An examination of the global signals reveals three biodiversity crises (discordances between signals) where morphological disparity grows while taxonomic diversity declines. The subdivision of the signals indicates the radiation was heterogeneous between provinces: the global signal is an aggregate of signals …

010506 paleontologyTaxonomic diversitymedia_common.quotation_subjectBiodiversity[SDV.BID]Life Sciences [q-bio]/BiodiversityJurassic010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyAmmonitesPalaeogeographyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesSubdivisionmedia_common[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmonite[ SDV.BID ] Life Sciences [q-bio]/Biodiversitybusiness.industrySpace timePaleontologylanguage.human_languagePaleogeographylanguagebusiness[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyDiversity (politics)Morphological disparity
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Landscape reconstruction and major flood events of the River Main (Hesse, Germany) in the environs of the Roman fort at Groβkrotzenburg

2020

Abstract Detailed geoarchaeological studies were conducted at the Groβkrotzenburg floodplain (Southern Hesse, Germany) in order to reconstruct the fluvial palaeogeography and search for Roman harbour installations. Another objective was to reconstruct the local flood history based on stratigraphic and geochronological data. Prospection based on electrical resistivity tomography, vibracoring and direct push electrical conductivity logging were carried out to detect and analyze subsurface stratigraphies. Altogether, 6 sediment cores, up to 7 m long, were drilled along transects along and perpendicular to the present course of the River Main. Based on sedimentological and geochemical data, we …

010506 paleontologygeographygeography.geographical_feature_categoryFloodplainFlood mythWater flowBedrockFluvial010502 geochemistry & geophysics01 natural sciencesAlluvial plainSedimentary rockPhysical geographyPalaeogeographyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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Seismites resulting from high-frequency, high-magnitude earthquakes in Latvia caused by Late Glacial glacio-isostatic uplift

2016

Abstract Geologically extremely rapid changes in altitude by glacial rebound of the Earth crust after retreat of the Scandinavian Ice Sheet at the end of the last Weichselian glaciation influenced the palaeogeography of northern Europe. The uplift of the Earth crust apparently was not gradual, but shock-wise, as the uplift was accompanied by frequent, high-magnitude earthquakes. This can be deduced from strongly deformed layers which are interpreted as seismites. Such seismites have been described from several countries around the Baltic Sea, including Sweden, Germany and Poland. Now similarly deformed layers that must also be interpreted as seismites, have been discovered also in Latvia, a…

010506 paleontologygeographygeography.geographical_feature_categorySoft-sediment deformation structures (SSDS) SeismitesGeography Planning and DevelopmentMagnitude (mathematics)PaleontologyPost-glacial rebound010502 geochemistry & geophysics01 natural sciencesLatviaQE701-760PaleontologyTectonic upliftAltitudeEarthquake recurrence timeGlacio-isostatic reboundGlacial periodIce sheetWeichselian glaciationPalaeogeographySeismologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Palaeogeography
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Integrated geophysical surveys in the tarragona cathedral

2009

An integrated geophysical survey has been conducted at the Tarragona’s Cathedral (Catalonia, NE Spain) with the aim to detect the existence of archaeological remains of the Roman’s temple devoted to August. Many hypotheses have been proposed about its possible location, the last ones regarding the inner part of the Cathedral, which is one of the most famous temple of Spain (12th century) evolving from Romanesque to Gothic styles. A project including electrical resistivity tomography (ERT), ground probing radar (GPR) and frequency domain electromagnetics (FDEM) has been planned over one year and conducted during a week of intensive field survey. From all the methods applied, both ERT and GPR…

3D ERT 2D ERT GPR archaelogical surveysElectromagneticsGeophysical survey (archaeology)Settore GEO/11 - Geofisica ApplicataGround-penetrating radarElectrical resistivity tomographyStratigraphy (archaeology)Economic geologyPalaeogeographyGeologySeismologyEnvironmental geology
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Estratigrafía y petrología del subsuelo precuaternario del sector SW de la depresión de Barcelona (Cadenas Costeras Catalanas, NE de Iberia)

2008

Juan.Usera@uv.es Las numerosas obras de Ingeniería Civil que se han realizado en los últimos años en la depresión de Barcelona (ampliación del aeropuerto, ampliación del metro y AVE fundamentalmente) han permitido recabar mucha información sobre el subsuelo de esta área. En este trabajo se caracterizan las distintas unidades de subsuelo precuaternarias que aparecen en los numerosos sondeos realizados recientemente en la zona SW de la depresión de Barcelona. Se ha identificado un sustrato triásico formado por areniscas del Buntsandstein y dos unidades de edad Miocena, una basal de carácter continental y otra superior depositada en un ambiente marino. Todas estas unidades fueron fracturadas d…

:CIENCIAS DE LA TIERRA Y DEL ESPACIO::Geología::Geología regional [UNESCO]Barcelona plainCadenas Costeras CatalanaUNESCO::CIENCIAS DE LA TIERRA Y DEL ESPACIO::Geología::Geología regionalDepresión de BarcelonaMiocenoGeology Stratigraphic--MiocenePaleogeografiaGeology--Spain--CataloniaMioceneGeologia--CatalunyaCadenas Costeras CatalanasPaleogeografíaEstratigrafia--MiocèDepresión de Barcelona; Mioceno; Paleogeografía; Cadenas Costeras CatalanasPaleogeography:Enginyeria civil::Geologia [Àrees temàtiques de la UPC]PalaeogeographyCatalan Coastal Ranges
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The Jura glaciers: palaeogeography in the Würmian circum-Alpine zone

2008

Since the first studies on the glacial formations of the Jura mountains there have been two concepts concerning type of glaciation and ice origin during the Wurmian glaciation. Some authors believed that the Jura was totally inundated by ice of Alpine origin, while others believed that the Jura had its own glaciers, originating from a single ice-cap. Several recent studies on both the NW and SE slopes of the range define the problem more accurately. This paper presents a synthesis of the new results from mapping the moraine systems and studying the stratigraphic relationships between Alpine and Jura tills. It is concluded that even the highest level of Alpine glaciers could not lead to a pe…

ArcheologyPaleontologygeographygeography.geographical_feature_categoryMoraineAlpine climateGeologyGlacierGlacial periodGeomorphologyPalaeogeographyEcology Evolution Behavior and SystematicsGeologyBoreas
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Archaeological excavation confirms the geophysical anomalies recorded at the cathedral of tarragona - A comparative study

2011

An integrated geophysical survey was conducted in September 2007 at the Cathedral of Tarragona to search for archaeological remains of the Roman temple dedicated to the Emperor Augustus. Many hypotheses about its location have been put forward, the most recent ones suggesting it could be inside the present cathedral. A project including Electrical resistivity tomography (ERT) and Ground probing radar (GPR) was planned for a year and conducted during a week of intensive field survey. Both ERT and GPR provided detailed information about subsoil structures. Different ERT techniques and arrays were used, ranging from standard Wenner-Schlumberger 2D sections to full 3D electrical imaging using t…

BasementGeophysical survey (archaeology)Settore GEO/11 - Geofisica ApplicataGround-penetrating radarExcavationGeophysicsElectrical resistivity tomographyEconomic geologyStratigraphy (archaeology)ArchaeologyPalaeogeographyArchaeogeophysics ERT MYG array GPR TarragonaGeology
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Mineralogical variability of Callovo-Oxfordian clays from the Paris Basin and the Subalpine Basin.

2006

High-resolution clay mineralogical data at the Middle/Upper Jurassic boundary from the French Subalpine Basin, the Jura Mountains and the Paris Basin (ANDRA boreholes) from Callovo-Oxfordian clayey deposits allow spatial and temporal terrigenous flux evolution to be considered over a period of 6 to 7 Myr. Recorded diachronisms of major mineralogical changes and complex clays distribution at the Paris Basin scale result to combined palaeogeographic/eustatic variations and climate input. In the French Subalpine Basin, mineralogical homogeneity confirms the burial diagenesis influence, but other terrigenous supplies must be involved in contrast to the Paris Basin domains. Volcanogenic clays (b…

Bentonites010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesCallovian[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/VolcanologyBiostratigraphyStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesOxfordianPaleontologyPalaeovolcanismParis Basin[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgPhanerozoic[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesGlobal and Planetary ChangeTerrigenous sedimentDiagenesisClay minerals[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate actionClastic rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary SciencesSedimentary rockFrancePalaeogeographyGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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