Search results for "rog"

showing 10 items of 22807 documents

Ammonoids and quantitative biochronology - A unitary association perspective

2015

Ammonoid evolutionary changes have long been recognized to be excellent time markers. They are the major macrofossil group to date and correlate Paleozoic and Mesozoic marine strata. Originations and extinctions of ammonoid species are commonly used to define GSSPs and build high resolution biozonations. Biochronology is now an advanced field with the recent development of computerized, quantitative methods yielding robust biochronological schemes. It has been demonstrated that such quantitative biochronological methods are very efficient to resolve (often complex) biostratigraphic contradictions and produce accurate and high resolution biozonations, thus enabling precise dating and correla…

010506 paleontologyAssociation (object-oriented programming)High resolutionGeometry10125 Paleontological Institute and MuseumBiostratigraphy010502 geochemistry & geophysics01 natural sciencesUnitary statePaleontology560 Fossils & prehistoric lifeBiochronology14. Life underwater[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyComputingMilieux_MISCELLANEOUS[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences
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Sr isotope variations in the Upper Triassic succession at Pizzo Mondello, Sicily: Constraints on the timing of the Cimmerian Orogeny

2018

Abstract The Late Triassic Cimmerian Orogeny was a result of the final closure of the Palaeotethys Ocean and the accretion of Gondwana-derived (Cimmerian) continents to southern Eurasia. Determining the timing of the Cimmerian Orogeny is crucial to our understanding of the large-scale climate changes driven by the uplift of the Cimmerian Mountains. Here we present stratigraphic variations in 87Sr/86Sr values of Upper Triassic pelagic limestone from the Pizzo Mondello section, Sicily, Italy, that constrain the timing of uplift of the Cimmerian Mountains. The 87Sr/86Sr values remain relatively constant in the lower part of the section, decreasing slightly in the Tuvalian (upper Carnian) and L…

010506 paleontologyCarnian; Cimmerian Mountains; Climate change; Limestone; Norian; Tethys; Oceanography; Ecology Evolution Behavior and Systematics; Earth-Surface Processes; PaleontologyEvolutionCimmerian MountainsClimate changeWeatheringEcological succession010502 geochemistry & geophysicsNorianOceanography01 natural sciencesPaleontologyBehavior and SystematicsClimate changeTethysEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesCarnianRadiogenic nuclideEcologyPaleontologyOrogenyTethys OceanLimestoneErosionAccretion (geology)Geology
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Structure and evolution of a Messinian mixed carbonate-siliciclastic platform: the role of evaporites (Sorbas Basin, South-east Spain).

2010

36 pages; International audience; The Sorbas Member is a late Messinian complex sedimentary systemthat formed immediately following deposition of the Messinian evaporites in the Sorbas Basin (South-east Spain). This work describes the sequence architecture and facies organization of a continuous kilometre long, alluvial fan to open platform transect near the village of Cariatiz in the north-east of the basin. The postevaporitic Cariatiz platform was a mixed carbonate-siliciclastic system composed of four intermediate-frequency, fifth-order depositional sequences (Depositional Sequences 1 to 4) arranged in an overall prograding trend. The intense fracturing and brecciation of these deposits …

010506 paleontologyEvaporiteStratigraphy[SDE.MCG]Environmental Sciences/Global Changeslate Messinian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentPaleontologyooidsooids.14. Life underwater0105 earth and related environmental sciencesmixed carbonate/siliciclastic platform[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryAlluvial fanmicrobialitesGeology[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics15. Life on landEvaporite collapse and deformation[ SDE.MCG ] Environmental Sciences/Global Changes[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesOoidSiliciclasticSedimentary rockProgradationGeology
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Coarsely crystalline cryogenic cave carbonate – a new archive to estimate the Last Glacial minimum permafrost depth in Central Europe

2012

Abstract. Cryogenic cave carbonate (CCC) represents a specific type of speleothem whose precipitation is triggered by freezing of mineralized karst water. Coarsely crystalline CCC, which formed during slow freezing of water in cave pools, has been reported from 20 Central European caves located in Germany, the Czech Republic, Slovakia and Poland. All these caves are situated in an area which was glacier-free during the Weichselian. Whereas the formation of usual types of speleothems in caves of this region usually ceased during the glacials, coarsely crystalline CCC precipitation was restricted to glacial periods. Since this carbonate type represents a novel, useful paleoclimate proxy, data…

010506 paleontologyGroundwater flowStratigraphylcsh:Environmental protectionGeochemistryAquifer010502 geochemistry & geophysicsPermafrost01 natural scienceslcsh:Environmental pollutionLatent heatlcsh:TD169-171.8Glacial periodGeomorphologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary ChangegeographyHydrogeologygeography.geographical_feature_categoryPaleontology13. Climate actionlcsh:TD172-193.5QuaternaryGroundwaterGeologyClimate of the Past
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Tectonic evolution of the northern Austral-Magallanes basin in the Southern Patagonian Andes from provenance analysis

2019

We studied the northern tip of the Austral-Magallanes basin in the Southern Patagonian Andes, between the Buenos Aires Lake and the Mayer River at 46°35′ SL and 48°35′ SL, respectively. Proposed objectives were: i) to differentiate Mesozoic-Cenozoic tectonostratigraphic units and, ii) to characterize the different deformational events that took place in the area linked to a variable regional geodynamic context. Sandstones provenance analysis was performed on the Aptian - Albian compressive retroarc deposits and Cenozoic foreland deposits. Studied samples were classified using tectonic discrimination diagrams which show: i) for Cretaceous rocks a dominant sediment source from a recycled orog…

010506 paleontologyProvenanceAptian010502 geochemistry & geophysics01 natural sciencesUnconformityCiencias de la Tierra y relacionadas con el Medio Ambiente//purl.org/becyt/ford/1 [https]//purl.org/becyt/ford/1.5 [https]PaleontologyGeologíaForeland basin0105 earth and related environmental sciencesEarth-Surface ProcessesRiftTECTONOSTRATIGRAPHIC UNITSGEODYNAMICSGeologySOUTHERN PATAGONIAN ANDESCretaceousBack-arc basinPROVENANCE ANALYSISCenomanianSEDIMENTARY PETROGRAPHYGeologyCIENCIAS NATURALES Y EXACTAS
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Electron Paramagnetic Resonance and petrographic analysis for dating Mesolithic and Neolithic pottery from Al Khiday (Sudan)

2016

Abstract Electron Paramagnetic Resonance (EPR) dating, like luminescence techniques, is based on the time-dependent accumulation of trapped charges at mineral defect centres. However, Fe(III) ions prevent the common Continuous Wave (CW-EPR) approach for dating pottery, which always contains iron. The Pulsed method (ED-EPR) allowed this limitation to be overcome, with recording of radiation-induced defect signals, as shown by increased signal intensity after artificial irradiation of samples. The method was applied to studying Mesolithic and Neolithic pottery from Al Khiday (Central Sudan), characterized by quartz-rich tempers and coming from dated contexts. As the occurrence of a natural ED…

010506 paleontologyRadiation060102 archaeologyAl Khiday; EPR dating; Prehistoric pottery; Quartz; Radiation; InstrumentationMineralogy06 humanities and the artsQuartz01 natural sciencesEPR datinglaw.inventionPetrographylawPrehistoric pottery0601 history and archaeologyPotterySignal intensityElectron paramagnetic resonanceAl KhidayQuartzInstrumentationGeologyMesolithic0105 earth and related environmental sciences
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Spongy-like porosity in peritidal carbonates: An interaction of cyclic sea-level oscillations, fresh water supply and sediment texture

2016

Abstract This paper focuses upon the analysis of a complex paleokarstic system recorded within uppermost Triassic peritidal cycles in northwestern Sicily. Besides documenting spectacular karstification at the Triassic/Jurassic boundary, it provides an example of stratabound ‘spongy’ or ‘swiss-cheese’ dissolution. On the base of field observations, microfacies analysis, transmitted-light and cathodoluminescence petrography and stable-isotope analyses we put forward an original model for the formation of this peculiar stratabound dissolution. It implies a complex interaction of several controlling factors at the interface between the marine and meteoric diagenetic realms during the relative c…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformStratigraphyGeochemistrySedimentGeology010502 geochemistry & geophysics01 natural sciencesCarbonate platform Diagenesis Stratabound dissolution Spongy-like pattern Triassic SicilyDiagenesisPetrographyPaleontologySubaerialDissolutionPhreaticSea levelGeology0105 earth and related environmental sciences
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Palaeoenvironmental interpretation of the Pliocene fan-delta system of the Vera Basin (SE Spain): Fossil assemblages, ichnology and taphonomy

2020

Abstract The marine fossil assemblages of the Pliocene of south Spain constitute the record of the marine fauna that colonised the western part of the Mediterranean after the Messinian Salinity Crisis. This work focuses on the analysis of lithofacies and fossil assemblages including trace fossils, invertebrates, and vertebrates with special attention to taphonomic features, for interpreting palaeoenvironmental conditions in the Vera Basin (SE Spain). The sedimentary sequences of the northern region of the Vera Basin display diverse stratigraphical, sedimentological, and palaeontological features that correspond to the evolution of a fan-delta in a narrow basin. The Vera Basin was characteri…

010506 paleontologyTaphonomyStratigraphyPaleontologyTrace fossilStructural basin010502 geochemistry & geophysics01 natural sciencesPaleontologyIchnologyFaciesMarlSedimentary rockProgradationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesPalaeoworld
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Quartz OSL dating of late quaternary Chinese and Serbian loess: A cross Eurasian comparison of dust mass accumulation rates

2019

© 2018 Elsevier Ltd and INQUA. Reconstructing dust Mass Accumulation Rate (MAR) from loess deposits is critical to understanding past atmospheric mineral dust activity and requires accurate independent age models from loess deposits across Europe and Asia. Previous correlations of loess in Europe and China have tended to focus on multi-millennial timescales, with no detailed examination of dust MAR at the two ends of the Eurasian loess belt on shorter, sub-orbital scales. Here we present a detailed quartz optically stimulated luminescence (OSL) chronology from the Serbian Titel Loess Plateau (Veliki Surduk loess core) and the Chinese Loess Plateau (Lingtai section). The luminescence ages pa…

010506 paleontologyTitel loess plateau010504 meteorology & atmospheric sciencesOptically stimulated luminescenceOSL datingGeochemistryLoessDustMars Exploration ProgramMineral dust01 natural sciencesMARLoessChinese Loess PlateauGlacial periodQuaternary[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]QuartzGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesChronology
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Facies variations in response to Holocene sea-level and climate change on Bora Bora, French Polynesia: Unravelling the role of synsedimentary siderit…

2017

International audience; Five mixed carbonate-siliciclastic sedimentary facies were identified in the barrier-reef lagoon of Bora Bora using microfacies and statistical analyses of 70 sediment samples taken at high resolution from two vibrocores. Fades and fades successions were interpreted with respect to Holocene sea-level and climate changes. The windward lagoon core is characterized by sideritic marly wackestones and foraminifera-sideritic wackestones, deposited around 7700 years BP (years before present) during the early-mid Holocene transgression. At that time, extensive weathering and erosion of iron-bearing minerals from the volcanic island, due to a wetter climate, were expressed in…

010506 paleontology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaSideritechemistry.chemical_compoundGeochemistry and Petrology14. Life underwaterLithificationReefComputingMilieux_MISCELLANEOUSHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyGeologybiology.organism_classification6. Clean waterOceanographychemistry13. Climate action[SDE]Environmental SciencesSiliciclasticProgradationGeologyMarine transgression
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