Search results for " Formation"

showing 10 items of 1920 documents

Influence of microporosity distribution on the mechanical behavior of oolithic carbonate rocks.

2015

Abstract The mechanical behavior of oolithic carbonate rocks was investigated for selected rocks with two different microstructural attributes: uniform (UP) and rimmed (RP) distribution of microporosity within ooids. These oolithic carbonate rocks are from the Oolithe Blanche formation, a deep saline aquifer in the Paris Basin, and a possible target for CO2 sequestration and geothermal production. Samples of similar physical properties (porosity, grain diameter, cement content) but different microporosity textures were deformed under triaxial configuration, in water saturated conditions, at 28 MPa of confining pressure, 5 MPa of pore pressure and at a temperature of 55 °C. During the experi…

010504 meteorology & atmospheric sciences[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographyMineralogy010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesTortuosityPore water pressureBrittlenessRock mechanicsMicroporosityParis BasinComputers in Earth SciencesOolithe Blanche formationSafety Risk Reliability and QualityPorosity0105 earth and related environmental sciences[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/PetrographyCarbonate rockGeotechnical Engineering and Engineering GeologyOverburden pressurePermeability (earth sciences)Rock mechanics[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonate rockGeology
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GRB 050904 at redshift 6.3: observations of the oldest cosmic explosion after the Big Bang

2005

We present optical and near-infrared observations of the afterglow of the gamma-ray burst GRB 050904. We derive a photometric redshift z = 6.3, estimated from the presence of the Lyman break falling between the I and J filters. This is by far the most distant GRB known to date. Its isotropic-equivalent energy is 3.4x10^53 erg in the rest-frame 110-1100 keV energy band. Despite the high redshift, both the prompt and the afterglow emission are not peculiar with respect to other GRBs. We find a break in the J-band light curve at t_b = 2.6 +- 1.0 d (observer frame). If we assume this is the jet break, we derive a beaming-corrected energy E_gamma = (4-12)x10^51 erg. This limit shows that GRB 050…

010504 meteorology & atmospheric sciencesgamma rays: burstsAstrophysics::High Energy Astrophysical PhenomenaFOS: Physical sciencesAstrophysicsAstrophysics::Cosmology and Extragalactic AstrophysicsJet (particle physics)Astrophysics01 natural sciences[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]gamma rays: individual: GRB 0509040103 physical sciences010303 astronomy & astrophysics0105 earth and related environmental sciencesPhotometric redshiftPhysicsCOSMIC cancer database[SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]Star formationAstrophysics (astro-ph)Astronomy and Astrophysicsearly UniverseLight curveRedshiftAfterglowSpace and Planetary Sciencecosmology: observationsGamma-ray burst
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The global bio-events at the Cenomanian-Turonian transition in the reduced Bahloul Formation of Bou Ghanem (central Tunisia).

2010

In central Tunisia, the thickness of the Bahloul Formation varies generally between 20 to 40 m such as for example, respectively, at wadi Smara near Kalaat Senan and at wadi Bahloul near Maktar. The thickness is also of several tens metres at Koudiat el Azreg near Jerissa and at Tajerouine. In these sites where the thickness of the Bahloul Formation is dilated, in addition to five geochemical events (d13C), nine bio-events were defined near the Cenomanian-Turonian transition, successively in ascending order: 1. LO Rotalipora cushmani, 2. Heterohelix bio-event, 3. FO Pseudaspidoceras pseudonodosoides, 4. LO P. pseudonodosoides, 5. LO Thalmanninella multiloculata, 6. “filaments” bio-event, Ce…

010506 paleontologyBahloul Formationfood.ingredientTunisia010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyfoodStratotypeStage (stratigraphy)Cenomanian-Turonian boundaryCenomanianWadi0105 earth and related environmental sciencesgeographyLaminated faciesgeography.geographical_feature_categoryPaleontologyTuronianWatinocerasCretaceous[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBio-eventsCenomanianGeology
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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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ISOTOPIC TEMPERATURES FROM THE EARLY AND MID-PLIOCENE OF THE US MIDDLE ATLANTIC COASTAL PLAIN, AND THEIR IMPLICATIONS FOR THE CAUSE OF REGIONAL MARIN…

2017

Mean seasonal extreme temperatures on the seafloor calculated from the shell d 18 Oofthescallop Placopecten clintonius from the basal part of the early Pliocene Sunken Meadow Member (Yorktown Formation) in Virginia are very similar to those from the same horizon at the latitude of Cape Hatteras in North Carolina ( ~ 210 km to the south). The lowest and highest temperatures calculated from each shell (using d 18 O seawater ¼þ 0.7 % )givemean values for winter and summer of 8.4 6 1.1 8 C( 6 1 r ) and 18.2 6 0.6 8 CinVirginia,and8.6 6 0.4 8 Cand16.5 6 1.1 8 C in North Carolina (respective median temperatures: 13.3 8 C and 12.6 8 C). Patterns of ontogenetic variation in d 18 O, d 13 C and micro…

010506 paleontologygeographygeography.geographical_feature_categoryδ13CYorktown Formationδ18OCoastal plainPaleontologyOceanic climate010502 geochemistry & geophysics01 natural sciencesGulf StreamOceanographySclerochronologyPaleoclimatologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciences
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À l’aube des villes antiques : vocabulaire de la cité et formes urbaines. – Introduction

2020

How to envisage research on the ancient city? What are the most appropriate instruments to analyse it? What are the relationships between the emergence of the city as an independent community and the urbanization as archaeology can restore it? Without claiming to resolve these difficult questions, the contributions gathered here show that urbanization and the definitions of the ancient city used by contemporary historians and archaeologists are far from being precisely determined; they can even vary according to the authors, disciplines, periods and contexts. As a consequence, there is no town, but towns; no city, but cities. The issue of a definition is also the evaluation of theories, in …

010506 paleontologyurbanisation[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory060102 archaeology[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistorymethodology06 humanities and the arts01 natural sciencesméthodologieformation des citéstowncities’ formation[SHS.HIST] Humanities and Social Sciences/History11. Sustainabilityville0601 history and archaeology[SHS.HIST]Humanities and Social Sciences/Historyvocabulaire0105 earth and related environmental sciencesvocabulary
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Isotopic seawater temperatures in the Albian Gault Clay of the Boulonnais (Paris Basin): Palaeoenvironmental implications

2016

13 pages; International audience; Oxygen isotopes were measured on several types of fossil hardparts from the Gault Clay Formation including benthic and planktonic foraminifera, belemnite guards, and fish small-teeth. Belemnites δ18O values indicate low temperatures (13.5–19.3 °C) with an increase from the Middle to Late Albian. Foraminifera provide variable δ18O values, some too low to be relevant in terms of temperature (until 42 °C). These low values probably result from a diagenetic alteration of the foraminiferal tests even though SEM observations revealed well-preserved microstructures. However, higher foraminiferal δ18O values recorded in some levels indicate temperatures in the rang…

010506 paleontologyδ18OGault Clay FormationForaminifera010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenForaminiferaPaleontologyPalaeotemperatureBelemnites guardsParis BasinFish teeth14. Life underwaterComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesbiologyfungiSelachian teethPaleontologyGeologyPelagic zoneAlbianbiology.organism_classificationDiagenesisSea surface temperature13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOxygen isotopes[ SDU.STU.HY ] Sciences of the Universe [physics]/Earth Sciences/HydrologyBelemnitesGeology
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Middle Jurassic tracks of sauropod dinosaurs in a deep karst cave in France.

2019

14 pages; International audience; Although the deep galleries of natural underground cavities are difficult to access and are sometimes dangerous, they have the potential to preserve trace fossils. Here, we report on the first occurrence of sauropod dinosaur tracks inside a karstic cave. Three trackways are preserved on the roof of the Castelbouc cave 500 m under the surface of the Causse Méjean plateau, southern France. The tracks are Bathonian in age (ca. 168–166 Ma), a crucial but still poorly known time interval in sauropod evolution. The three trackways yield sauropod tracks that are up to 1.25 m long and are therefore amongst the largest known dinosaur footprints worldwide. The trackm…

0106 biological sciences010506 paleontologyBAGA FORMATIONTrace fossilSOUTHERN FRANCE010603 evolutionary biology01 natural sciencesNatural (archaeology)Sedimentary depositional environmentPaleontology0105 earth and related environmental sciencesBASINgeographygeography.geographical_feature_categoryPaleontologyTrackwayKarstEVOLUTIONMOUNTAINSGRANDS-CAUSSES[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyFOOTPRINTSPENINSULAGeologyICHNOFAUNABORNHOLM
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Shape, size, and quantity of ingested external abrasives influence dental microwear texture formation in guinea pigs

2020

Food processing wears down teeth, thus affecting tooth functionality and evolutionary success. Other than intrinsic silica phytoliths, extrinsic mineral dust/grit adhering to plants causes tooth wear in mammalian herbivores. Dental microwear texture analysis (DMTA) is widely applied to infer diet from microscopic dental wear traces. The relationship between external abrasives and dental microwear texture (DMT) formation remains elusive. Feeding experiments with sheep have shown negligible effects of dust-laden grass and browse, suggesting that intrinsic properties of plants are more important. Here, we explore the effect of clay- to sand-sized mineral abrasives (quartz, volcanic ash, loess,…

0106 biological sciences10253 Department of Small AnimalsGuinea PigsDental WearMineral dustdiet reconstruction010603 evolutionary biology01 natural sciencesTexture (geology)Texture formation010104 statistics & probabilitychemistry.chemical_compoundstomatognathic systemAnimalsHerbivoryParticle Size0101 mathematicsQuartzgrit2. Zero hunger1000 MultidisciplinaryMultidisciplinary630 AgricultureMetallurgyPlantsBiological SciencesAnimal FeedSilicateDietTooth AbrasionchemistryTooth weartooth wear570 Life sciences; biologyParticle sizedustfeeding experimentProceedings of the National Academy of Sciences
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Carbon, iron and sulphur cycling in the sediments of a Mediterranean lagoon (Ghar El Melh, Tunisia)

2019

Coastal lagoon sediments are important for the biogeochemical carbon cycle at the land-ocean transition, as they form hotspots for organic carbon burial, as well as potential sites for authigenic carbonate formation. Here, we employ an early diagenetic model to quantify the coupled redox cycling of carbon, iron and sulphur in the sediments of the shallow Ghar El Melh (GEM) lagoon (Tunisia). The model simulated depth profiles show a good correspondence with available pore water data (dissolved inorganic carbon, NH 4 + , total alkalinity, Ca 2+ , Fe 2+ and SO 4 2− ) and solid phase data (organic matter, pyrite, calcium carbonate and iron (oxyhydr)oxides). This indicates that the model is abl…

0106 biological sciencesBiogeochemical cycle010504 meteorology & atmospheric scienceschemistry.chemical_elementAquatic ScienceOceanography01 natural sciencesCarbon cyclechemistry.chemical_compoundMarine sedimentsAuthigenic carbonate formationDissolved organic carbonOrganic matter14. Life underwaterBiologyEarly diagenesis0105 earth and related environmental scienceschemistry.chemical_classificationTotal organic carbon010604 marine biology & hydrobiologyAuthigenicPyrite formationchemistry13. Climate actionEnvironmental chemistry[SDE]Environmental SciencesEnvironmental scienceCarbonateCarbonSciences exactes et naturelles
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