Search results for " Cretaceo"

showing 10 items of 23 documents

Neocomian to early Aptian syn-rift evolution of the normal to oblique-rifted North Gabon Margin (Interior and N'Komi Basins).

2009

18 pages; International audience; The North Gabon coastal rift basins consist of a set of 130–150 long-segment asymmetrically tilted half grabens (Interior Basin) and 000–020 short-segment en échelon half grabens (N'Komi Basin) separated by 040–060 major transverse faults. Tectono-sedimentary analysis of field and subsurface data reveals the control exerted by extensional tectonism over continental sedimentation. During Berriasian to early Barremian times, uniform uniaxial 040–060 extension was responsible for the stretching of the brittle upper crust over a 100-km wide domain. During late Barremian–early Aptian times, the main locus of extension stepped westward resulting in severe end-rif…

010504 meteorology & atmospheric sciencesAptianStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesEarly CretaceousEnd-rift erosionStructural basin010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyEchelon formationGabon0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsRift segmentationRiftOblique riftingGeologyCrust[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsCretaceousGrabenTectonics[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysics[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyEconomic GeologyPrecambrian heritageNormal riftingGeology
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Geodynamic control on carbonate diagenesis: Petrographic and isotopic investigation of the Upper Jurassic formations of the Paris Basin (France).

2007

23 pages; International audience; The Oxfordian and Kimmeridgian carbonates of the eastern edge of the Paris Basin display poor reservoir properties (Φb15% and Kb0.1 md). The petrographic investigation and the resultant paragenetic sequence show that this is due to extensive precipitation of 2 types of almost synchronous blocky LMC (Low Magnesian Calcite) cements during mesogenesis (burial). Stable isotope investigation of these non-recrystallized cements, through both microdrilling sampling and in-situ SIMS (Secondary IonMass Spectrometry) analysis, shows that they originated from slightly buffered meteoric fluids (−3‰SMOW to −8‰SMOW) flowing through the Malm carbonate aquifers of the east…

010504 meteorology & atmospheric sciencesStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCarbonates010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyBasin evolution01 natural sciencesUnconformityDiagenesisPetrographyPaleontologychemistry.chemical_compoundUnconformities[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryLower Cretaceous0105 earth and related environmental sciencesStable isotopesgeographygeography.geographical_feature_categoryGeologyMassif[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesDenudationchemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMeteoric waterCarbonateGeology
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Report on the 4th International Meeting of the IUGS Lower Cretaceous ammonite working group, the "Kilian Group" (Dijon, France, 30th August 2010).

2011

8 pages; International audience; The 4th Kilian Group meeting (Dijon, France, 30th August 2010) focused on the Aptian and Albian Stages. For the Aptian, a two-fold division of the stage was adopted for the Mediterranean area with a boundary between the Dufrenoyia furcata and Epicheloniceras martini Zones. The main changes to the zonal scheme concern the Lower Aptian with: the introduction of a Deshayesites luppovi Subzone in the upper part of the Deshayesites oglanlensis Zone; the replacement of Deshayesites weissi by Deshayesites forbesi as new indexspecies of the second interval zone; the introduction of a Roloboceras hambrovi Subzone in the upper part of the D. forbesi Zone; and the subd…

010506 paleontologyKilian GroupAptian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyStage (stratigraphy)AmmonitesGroup (stratigraphy)Lower CretaceousAptianMortoniceras0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmonitebiologyDouvilleicerasPaleontologyAlbianbiology.organism_classificationCretaceouslanguage.human_language[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyStandard zonationDipoloceraslanguage[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Paleoclimate and extensional tectonics of short-lived lacustrine environments. Lower Cretaceous of the Panormide Southern Tethyan carbonate platform …

2017

Abstract Subaerial erosion and continental sedimentation interbedded with shallow-water carbonates are unequivocal stratigraphic records to evaluate paleoenvironmental and paleoclimate evolution of emerged landmass. Stratigraphic analysis of the Cretaceous Monte Gallo section of the Mesozoic Panormide carbonate platform, in the northern side of the Palermo Mountains (NW Sicily) records a peculiar continental-derived clays that interrupted the shallow-water carbonate sedimentation. These clays rest, with lenticular geometries, above the tectonically-enhanced subaerial erosional unconformity of the Barremian-Lower Aptian Requienid limestones and are covered by the Upper Cretaceous Rudistid li…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaAptianCarbonate platformStratigraphyGeology010502 geochemistry & geophysicsOceanography01 natural sciencesUnconformityCretaceouschemistry.chemical_compoundPaleontologyGeophysicsLacustrine clays Uplift Weathering Warm-humid paleoclimate Lower Cretaceous SicilychemistrySubaerialHalf-grabenCarbonateEconomic GeologyExtensional tectonicsGeology0105 earth and related environmental sciencesMarine and Petroleum Geology
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Distribution of late Maastrichtian pachydiscid and scaphitid ammonites in the Maastricht and Kunrade formations of the southeast Netherlands

2018

Abstract The pachydiscid Pachydiscus ( Pachydiscus ) gollevillensis (d'Orbigny, 1850), long held to be confined to the ‘Kunrade Limestone’ (nowadays Kunrade Formation) in the eastern part of southern Limburg (Kunrade–Benzenrade area, the Netherlands), is now recorded from the basal Nekum Member (Maastricht Formation) at the ENCI-HeidelbergCement Group quarry, Sint-Pietersberg (Maastricht). Here we review the stratigraphic distribution of pachydiscid and scaphitid ammonites in outcrops west of the River Maas (Maastricht Formation) and in the Kunrade–Benzenrade area (Kunrade Formation). The latter unit has been correlated with part of the Lanaye Member (Gulpen Formation) up to the basal Emael…

010506 paleontologybiologyDesmoceratoideaOutcropPaleontology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousType areaPaleontologyCephalopodaScaphitoideaPachydiscusDesmoceratoideaGroup (stratigraphy)HoploscaphitesMenuitesUpper CretaceousGeology0105 earth and related environmental sciencesCretaceous Research
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Carbonate slope re‐sedimentation in a tectonically‐active setting (Western Sicily Cretaceous Escarpment, Italy)

2020

Tectonic processes are widely considered as a mechanism causing carbonate platform margin instabilities leading to the emplacement of mass transport deposits and calciturbidites. However, only few examples establishing a clear link between tectonics and re-sedimentation processes are known from the lit- erature. The two-dimensional and three-dimensional wire-cut walls of hun- dreds of quarries extracting ornamental limestones (for example, Perlato di Sicilia) from the Western Sicily Cretaceous Escarpment in Italy expose a series of mass transport deposits. The depositional architecture, spatial facies distri- bution and sedimentary features of these deposits were studied in detail. Thin sec…

010506 paleontologygeographyPillow lavageography.geographical_feature_categoryCarbonate platformStratigraphyGeochemistryGeologyEscarpment010502 geochemistry & geophysics01 natural sciencesCretaceousSedimentary depositional environmentTectonicsFaciesGeneral Earth and Planetary SciencesSedimentary rockGeologyCarbonate slope Cretaceous mass transport deposits re-deposited facies tectonics0105 earth and related environmental sciencesGeneral Environmental ScienceSedimentology
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Flore turonienne des silex fossilifères de Châtellerault (Ouest de la France)

2018

International audience; Three new localities yielding fossiliferous flints are reported from the Châtellerault area (Vienne, western France). They include one archaeological site (La Grande Vallée) and two zones with alterite deposits (L’Aunas and Les Bariollières). Broken surfaces of flint nodules show co-occurrence of marine invertebrates such as bryozoans, echinoids (Micraster Agassiz, Orthopsis Cotteau), gastropods (Acteonella d’Orbigny), rudists, and sponges. The association of Acteonella, Micraster and Orthopsis confirms the Turonian age (Upper Cretaceous) of the fossil assemblage. The marine invertebrates co-occur with plant macroremains including fragments of conifer leafy axes such…

0106 biological sciences010506 paleontologyFloraAngiosperms[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryPlantes010603 evolutionary biology01 natural sciencesBrachyphyllumPaleontologyAssemblage (archaeology)Invertébrés marins14. Life underwaterCrétacé supérieur0105 earth and related environmental sciencesInvertebrateMarinebiologyGeneral EngineeringMarine invertebratesPlantes Conifères Angiospermes Invertébrés marins Silex Crétacé supérieur ViennePlants15. Life on landinvertebratesbiology.organism_classificationCretaceousConifèresConifersSilexVienne[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryRudistsAngiospermesUpper CretaceousMicrasterPlants Conifers Angiosperms Marine invertebrates Flints Upper Cretaceous VienneFlintsGeologyComptes Rendus Palevol
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Chilamnestocoris mixtus gen. et spec. nov., the first burrower bug (Hemiptera: Pentatomoidea: Cydnidae) in Upper Cretaceous Burmese amber

2018

Burrower bug fossilAmnestinaeMyanmar amberChilamnestocoris mixtus gen. et sp. nov.Upper CretaceousCydnidaeCretaceous Research
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FACIES HETEROGENEITY AND SEDIMENTARY PROCESSES ALONG A TECTONICALLY-CONTROLLED CARBONATE SLOPE: A CASE STUDY FROM THE CRETACEOUS OF WESTERN SICILY (I…

2020

Carbonate slope Cretaceous mass transport deposits re-deposited facies biostratigraphy rudists tectonicsSettore GEO/02 - Geologia Stratigrafica E Sedimentologica
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Preparation protocols for SEM visualization of charred fossil plants: the case of Weichselia reticulata pinnule anatomy

2021

The cosmopolite Mesozoic fern Weichselia reticulata presents many peculiarities in the anatomy of its stem as well as in the architecture of its leaves. Previous analyses of the ultrastructure of their pinnule laminas provided some insight on xeromorphic traits. In this work new protocols for the preparation of charred compression foliage specimens embedded in a limestone matrix for their observation under SEM are presented, which enhance the observation of different plant tissues. The preparation with HCl allows for the visualization of the whole lamina, from the upper to the lower epidermis, which had not been done to date. Additionally, collodion, latex, or wax coverings of the fossils b…

Epidermis (botany)Ultrastructurelower cretaceous las hoyas bernissart polypodiopsida leaf anatomy.PaleontologyAnatomyFernBiologybiology.organism_classificationQE701-760Vascular tissueSpanish Journal of Palaeontology
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