Search results for "Tithonia"

showing 4 items of 4 documents

Tithonia oxfordiana, a new irregular echinoid associated with Jurassic seep deposits in south-east France

2011

The infaunal irregular echinoid, Tithonia oxfordiana, is described and compared to congeneric species previously described from Upper Jurassic and lowermost Cretaceous strata. This new species characterizes a monospecific echinoid assemblage, which occurs only in some places where deep-marine middle Oxfordian deposits are exposed in south-east France. Specimens are closely packed and clearly concentrated at the top of small carbonate chemoherms; a close connection of the echinoids with the emission of reduced chemicals, which were oxidized by chemoautotrophic bacteria, is highly probable. Based on general test shape and plate architecture, T. oxfordiana probably was a deposit feeder on chem…

Chemosynthesis010506 paleontologybiologyPaleontologyTithonia010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousPaleontologychemistry.chemical_compoundPetroleum seepchemistrySouth eastPaleoecologyCarbonateTaxonomy (biology)Ecology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesPalaeontology
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Importance des variations latérales discrètes dans les apports détritiques, observées dans des faciès de rampe sédimentaire riches en matière organiq…

2017

17 pages; International audience; We studied a potential petroleum source rock deposited in a clastic-dominated ramp environment: the Argiles de Châtillon Formation (Kimmeridgian-Tithonian, Boulonnais area, northern France). The formation was deposited along a proximal-distal gradient on this ramp affected by synsedimentary fault movements. A sedimentological, mineralogical and geochemical study was conducted to decipher the distribution patterns of sedimentary parameters along such a depth increase over the ramp. It comes out that smectite distribution unexpectedly mimics the lateral depth evolution despite the good floatability of the mineral. It is also observed that the Argiles de Châti…

Kimméridgien-Tithonien010504 meteorology & atmospheric sciencesSulfideBoulonnaisGeochemistryMineralogy[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesKimmeridgian-TithonianSedimentary depositional environment[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrygéochimieOrganic matterroches mères d'hydrocarbureComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesgeochemistryorganic matterchemistry.chemical_classificationminéraux argileuxlcsh:QE1-996.5Geology15. Life on landSedimentationlcsh:Geologyclay mineralschemistrySource rockClastic rockmatière organique[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphypetroleum source rocksSedimentary rock[SDU.OTHER]Sciences of the Universe [physics]/OtherClay mineralsGeology
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Seismogenic rotational slumps and translational glides in pelagic deep-water carbonates. Upper Tithonian-Berriasian of Southern Tethyan margin (W Sic…

2017

Abstract Soft-sediment deformation structures (SSDSs), which reflect sediment mobilization processes, are helpful to identify punctual events of paleoenvironmental stresses. In the upper Tithonian-Berriasian calpionellid pelagic limestone of the Lattimusa Fm. outcropping in the Barracu section (W Sicily), paleoenvironmental restoration reveals the occurrence of a deep-water flat basin, characterised by undeformed planar bedding, laterally passing to a gentle slope where the deformed horizons alternate with undeformed beds. Here, two types of gravity slides have been differentiated on the basis of different kinds of SSDSs, brittle deformation, involved lithofacies, geometry and morphology. T…

SSDSUpper Tithonian-erriasian pelagic carbonateDikeSettore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciencesBeddingCarbonate platformStratigraphyW Sicily010502 geochemistry & geophysics01 natural sciencesTranslational glidePaleontologyContinental marginMarlExtensional tectonics0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryRotational slumpGeologySlump scars and listric normal faultSeafloor spreadingTectonicsSeismologyGeologySedimentary Geology
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A facies distribution model controlled by a tectonically inherited sea bottom topography in the carbonate rimmed shelf of the Upper Tithonian–Valangi…

2016

The Upper Tithonian–Valanginian shallow-water carbonates outcropping in the Palermo Mts (NW Sicily) consist of several facies associations reflecting different depositional environments of a carbonate rimmed shelf, pertaining to the Southern Tethyan continental margin. The reconstructed depositional model, based on the sedimentological features, cyclic facies arrangement and biota distribution, shows that a wide protected lagoon, dominated by algae, molluscs and scattered patch reefs, was bordered landward by a tidal flat, where stromatolitic algal mats were cyclically subaerial exposed, and seaward by a marine sand belt and reef complex. Oolitic packstone-grainstone lithofacies, cyclically…

Upper Tithonian–Valanginian carbonate platform010506 paleontologygeographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformStratigraphyDepositional modelContinental marginTectonically-inherited sea bottom topographyGeology010502 geochemistry & geophysics01 natural sciencesSedimentary depositional environmentPaleontologyContinental marginPassive marginSubaerialFaciesExtensional tectonicsReefGeology0105 earth and related environmental sciencesSedimentary Geology
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