Search results for "water"

showing 10 items of 9348 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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Record of latest Barremian-Cenomanian environmental change in tectonically controlled depressions from the Jura-Burgundy threshold (Jura Mountains, e…

2019

Abstract The area of the western Jura Mountains constitutes the former Jura-Burgundy threshold between the Tethys Ocean and the epicontinental Paris Basin Sea. During the Barremian, the area was covered by a shallow-water Urgonian carbonate platform. Tectonic processes influenced the architecture of the Urgonian platform and were notably responsible for the formation of fault-related depressions on top of the Urgonian series, which were subsequently transformed into incised valleys and then to marine depocenters. Their sedimentary infills are mostly represented by the Perte-du-Rhone Formation and record stepwise environmental change on the innermost platform, which was strongly influenced b…

010506 paleontologyCarbonate platformPaleontologyStructural basin010502 geochemistry & geophysicsOceanographyTethys Ocean01 natural sciencesCretaceousPaleontology13. Climate actionMarlSedimentary rock14. Life underwaterCenomanianEcology Evolution Behavior and SystematicsGeologySea level0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Community replacement of neritic carbonate organisms during the late Valanginian platform demise: a new record from the Provence Platform.

2012

24 pages; International audience; The Valanginian is marked by amajor platform demise inducing a hiatus in the northern Tethyan neritic carbonate record from the top of the lower Valanginian to the lower Hauterivian. New biostratigraphic and chemostratigraphic data from the Ollioules section (Provence Platform, southern France) are presented here, demonstrating that a large part of the upper Valanginian is preserved in an inner platform environment. The thick, upper Valanginian, aggrading carbonate succession is observed in an aborted rift domain, implying relatively low subsidence. In this context, a relatively long-term sea-level rise was required to sustain a keep-up style of carbonate p…

010506 paleontologyCarbonate platformPlatform demiseContext (language use)010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural scienceschemistry.chemical_compoundPaleontology14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesRiftOllioules sectionTerrigenous sedimentCarbon isotopePaleontologySubsidencePhosphoruschemistryNeritic communitiesClastic rockValanginian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeologyMarine transgression
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Drowning of a carbonate platform as a precursor stage of the Early Toarcian global anoxic event (Southern Provence sub-Basin, South-east France)

2011

The Toarcian Oceanic Anoxic Event is well-known as coinciding with a carbonate crisis, coupled with organic matter accumulation and perturbation of the carbon cycle expressed by carbon-isotope excursions. In this palaeoenvironmental setting, the present research attempts to better constrain the palaeoenvironmental conditions leading to the drowning of a carbonate platform during Late Pliensbachian to Early Toarcian times. This study is based on the integrated sedimentological, diagenetic and geochemical (stable isotopes and Rock-Eval pyrolysis) analysis of several stratigraphic successions located in the Southern Provence sub-Basin (South-east France). Eodiagenetic ferroan calcite cements b…

010506 paleontologyCarbonate platformStratigraphyGeology15. Life on land010502 geochemistry & geophysicsCarbonate hardgrounds01 natural sciencesAnoxic watersCarbon cycleDiagenesisSedimentary depositional environmentPaleontologychemistry.chemical_compoundchemistry13. Climate actionCarbonateSedimentary rock14. Life underwaterGeology0105 earth and related environmental sciencesSedimentology
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Detailed record of the mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion in two hemipelagic sections (France and Switzerland): A plate …

2007

14 pages; International audience; The Oxfordian (Late Jurassic) was a time of widespread change in Jurassic marine (carbonate) sedimentation patterns. A marked positive excursion in δ13C is dated as Middle Oxfordian in age. In this study we investigate if changes in carbonate sedimentation coincided with altered carbon cycling and climate. We use C-isotope records as a proxy for the evolution of the carbon cycle and compare δ13C-trends with the evolution of sedimentation in a segment of the opening Tethys seaway. One of the studied sections is located in the Subalpine basin of France (Trescléoux and Oze), the other in the Swiss Jura mountains (Liesberg). Carbon-isotope stratigraphy of carbo…

010506 paleontologyClimate[SDE.MCG]Environmental Sciences/Global ChangesCarbon stable isotopes010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeCarbon cycleOxfordianchemistry.chemical_compoundPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterTethysEcology Evolution Behavior and SystematicsSea level[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesEarth-Surface ProcessesTotal organic carbon[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGlobal warmingExcursionPaleontologyCarbon cycle[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryPlate tectonics[ SDE.MCG ] Environmental Sciences/Global ChangeschemistryPalaeo-oceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
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Dental microwear texture analysis on extant and extinct sharks : Ante- or post-mortem tooth wear?

2020

Sharks are apex-predators that play an important role in past and present aquatic food webs. However, their diet - especially in extinct species - is often not well constrained. Dental microwear texture analysis (DMTA) has been successfully applied to reconstruct diet and feeding behaviours of different aquatic and terrestrial vertebrates. However, unlike in mammals, food-to-tooth contact in sharks is rather limited because only larger prey is manipulated before swallowing. Together with a fast tooth replacement rate, this reduces wear on individual teeth. Here, we present an explorative study of dental microwear texture on extant and extinct sharks to test whether ante-mortem wear is relat…

010506 paleontologyDental WearZoologyExtinct specieschemical and pharmacologic phenomenaShark teeth010502 geochemistry & geophysicsOceanography01 natural sciencesTexture (geology)DMTAZoologiPredationExtant taxonstomatognathic system14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyTumbling experimentPaleontologyGeologybiology.organism_classificationstomatognathic diseasesHabitatTooth wearCarcharhinusGeologiAlterationhuman activitiesZoologyGeologyElasmobranchii
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The relationships between soft-sediment deformation structures and synsedimentary extensional tectonics in Upper Triassic deep-water carbonate succes…

2016

Abstract We describe soft-sediment deformation structures into the Upper Triassic cherty limestone outcropping in the Pizzo Lupo section (Central Sicily, Italy), pertaining to the deep-water palaeodomain of the Southern Tethyan margin. In the study section, mainly consisting of thin-bedded mudstone/marl alternations with bedded chert intercalations, some lithofacies have been separated on the basis of the abundance of the calcium carbonate/clay content and the overall textural features. The deformational structures, displaying different deformational styles as folded and faulted beds, disturbed layers, clastic dikes, and slumps occur mainly in the deformed horizons that involve marl-dominat…

010506 paleontologyDikegeographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStratigraphyGeology010502 geochemistry & geophysics01 natural sciencesSeafloor spreadingSoft-sediment deformation structuresSoft-sediment deformation structures Synsedimentary tectonics Upper Triassic deep-water carbonates Central SicilyPaleontologyContinental marginClastic rockMarlExtensional tectonicsSedimentary rockGeology0105 earth and related environmental sciencesSedimentary Geology
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The biostratigraphical and palaeogeographical framework of the earliest diversification of tetrapods (Late Devonian)

2007

International audience; The earliest diversification of tetrapods is dated as Late Devonian based on 10 localities worldwide that have yielded bone remains. At least 18 different species are known from these localities. Their ages span the "middle"-late Frasnian to latest Famennian time interval, with three localities in the Frasnian, one at the F/F transition (though this one is not securely dated) and six in the Famennian. These localities encompass a wide variety of environments, from true marine conditions of the nearshore neritic province, to fluvial or lacustrine conditions. However, it does not seem possible to characterize a freshwater assemblage in the Upper Old Red Sandstone based…

010506 paleontologyDiversification (finance)GeologyOcean Engineering010502 geochemistry & geophysics01 natural sciencesDevonianPaleontologyTetrapod (structure)Late Devonian extinction14. Life underwater[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology0105 earth and related environmental sciencesWater Science and Technology
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A low seasonality scenario in the Mediterranean Sea during the Calabrian (Early Pleistocene) inferred from fossil Arctica islandica shells

2017

Understanding past seasonal temperature variability in the ocean is essential to evaluate the effects of future climate change on marine ecosystems. Here, we estimate seasonal water temperature amplitudes from stable oxygen isotope (δ18Oshell) values of fossil shells of Arctica islandica (assuming δ18Owater= + 0.9 ± 0.1‰ V-SMOW). Specimens were collected from three Pleistocene successions (Emilian and Sicilian substages of the Calabrian) in Central and Southern Italy (i.e., Rome, Lecce and Sicily). Biostratigraphic analyses from Rome Quarry deposits indicate an age between 1.6 and 1.2 Ma, whereas Sicily and Lecce successions are slightly more recent (between 1.1 and 0.62 Ma). Prior to …

010506 paleontologyEarly PleistoceneStable oxygen isotope010504 meteorology & atmospheric sciencesPleistoceneengineering.materialOceanography01 natural sciencesPaleontologyMediterranean seaSclerochronologySclerochronology14. Life underwaterGlacial periodArctica islandicaSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyAragonitePaleontologybiology.organism_classificationEcology Evolution Behavior and Systematiclanguage.human_languagePaleotemperature reconstructionOceanography13. Climate actionEarth-Surface ProcesseengineeringlanguageSicilianGeology
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Marine Early Triassic Actinopterygii from Elko County (Nevada, USA): implications for the Smithian equatorial vertebrate eclipse

2017

AbstractThe Early Triassic vertebrate record from low paleolatitudes is spotty, which led to the notion of an ‘equatorial vertebrate eclipse’ during the Smithian. Here we present articulated ray-finned fishes (Actinopterygii), collected from the marine Lower Triassic Thaynes Group at three new localities in Elko County (Nevada, USA), which were deposited within the equatorial zone. From the Smithian of the Winecup Ranch, we describe two partial skulls of the predatory actinopterygianBirgeria(Birgeriidae), attributed toB.americananew species andBirgeriasp.Birgeria americanan. sp. is distinguished from other species by a less reduced operculogular series. With an estimated total length of 1.7…

010506 paleontologyEarly Triassic10125 Paleontological Institute and MuseumStructural basin010502 geochemistry & geophysics01 natural sciencesSaurichthysPaleontologyGroup (stratigraphy)biology.animal14. Life underwaterBirgeria[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyEcologyActinopterygiiPaleontologyVertebratebiology.organism_classification1911 Paleontology560 Fossils & prehistoric lifeRidge[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyJournal of Paleontology
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