Search results for "Pal"

showing 10 items of 11479 documents

Black shale deposition during Toarcian super-greenhouse driven by sea level

2013

Abstract. One of the most elusive aspects of the Toarcian oceanic anoxic event (T-OAE) is the paradox between carbon isotopes that indicate intense global primary productivity and organic carbon burial at a global scale, and the delayed expression of anoxia in Europe. During the earliest Toarcian, no black shales were deposited in the European epicontinental seaways, and most organic carbon enrichment of the sediments postdated the end of the overarching positive trend in the carbon isotopes that characterises the T-OAE. In the present study, we have attempted to establish a sequence stratigraphic framework for Early Toarcian deposits recovered from a core drilled in the Paris Basin using a…

010504 meteorology & atmospheric sciencesStratigraphylcsh:Environmental protection[SDE.MCG]Environmental Sciences/Global ChangesGeochemistry010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyWater columnlcsh:Environmental pollution[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySequence stratigraphylcsh:TD169-171.8Earth ScienceSea levellcsh:Environmental sciences0105 earth and related environmental sciencesTotal organic carbonlcsh:GE1-350Global and Planetary ChangePaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryAnoxic waters[ SDE.MCG ] Environmental Sciences/Global ChangesIsotopes of carbon13. Climate action[SDU]Sciences of the Universe [physics][SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphylcsh:TD172-193.5Enhanced weatheringOil shaleGeology
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U-Pb Zircon Geochronology Of The Paleogene - Neogene Volcanism In The Nw Anatolia: Its Implications For The Late Mesozoic-Cenozoic Geodynamic Evoluti…

2017

The northern Aegean region was shaped by subduction, obduction, collision, and post-collisional extension processes. Two areas in this region, the Rhodope-Thrace-Biga Peninsula to the west and Armutlu-Almacik- Nallihan (the Central Sakarya) to the east, are characterized by extensive Eocene to Miocene post-collisional magmatic associations. We suggest that comparison of the Cenozoic magmatic events of these two regions may provide insights into the Late Mesozoic to Cenozoic tectonic evolution of the Aegean. With this aim, we present an improved Cenozoic stratigraphy of the Biga Peninsula derived from a new comprehensive set of U-Pb zircon age data obtained from the Eocene to Miocene volcani…

010504 meteorology & atmospheric sciencesSubduction010502 geochemistry & geophysicsNeogene01 natural sciencesCretaceousObductionPaleontologyGeophysicsSuture (geology)MesozoicGeomorphologyCenozoicPaleogeneGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Mid-Holocene tectonic geomorphology of northern Crete deduced from a coastal sedimentary archive near Rethymnon and a Late Bronze Age Santorini tsuna…

2019

Abstract The Late Bronze Age (LBA) tsunami and the A.D. 365 tsunami are supposed to have affected the northern coasts of Crete. However, near-coast sedimentary archives have been rarely investigated in this area, and sedimentary archives including palaeotsunami fingerprints are still unknown. The main objective of our research was to search for appropriate tsunami sediment traps in order to gain detailed insights into the Holocene palaeotsunami history of northern Crete. We found an excellent fine sediment archive near Pirgos, located to the west of Rethymnon. Based on a multi-electrode geoelectrical survey and an 11-m-deep sediment core, we analysed the event-geochronostratigraphical recor…

010504 meteorology & atmospheric sciencesSubductionBrackish waterSediment010502 geochemistry & geophysics01 natural scienceslaw.invention[SHS]Humanities and Social SciencesPaleontologyHabitat13. Climate actionlawBronze AgeSedimentary rock14. Life underwaterRadiocarbon datingGeologyHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface Processes
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Submarine morphology of the Comoros volcanic archipelago

2021

co-auteur étranger; International audience; A detailed morpho-bathymetric study of the Comoros archipelago, based on mostly unpublished bathymetric data, provides a first glimpse into the submarine section of these islands. It offers a complete view of the distribution of volcanic structures around the archipelago, allowing to discuss the origin and evolution of this volcanism. Numerous volcanic cones and erosional-depositional features have been recognized throughout the archipelago. The magmatic supply is focused below one or several volcanoes for each island, but is also controlled by lithospheric fractures evidenced by volcanic ridges, oriented along the supposed Lwandle-Somali plate bo…

010504 meteorology & atmospheric sciencesVolcanic ridges[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographySubmarine volcanismVolcanism010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyComoros archipelagoGeochemistry and PetrologyLithosphereComoros archipelago Mass slope instabilities Morpho-bathymetry Mounds Submarine volcanism Volcanic cones Volcanic ridges[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyVolcanic conesMass slope instabilitiesBathymetry14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMorpho-bathymetrySubmarineGeologyPlate tectonicsVolcanoArchipelagoMoundsVolcanic coneGeology
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Evolution of the neodymium isotopic signature of neritic seawater on a northwestern Pacific margin: new constrains on possible end-members for the co…

2013

11 pages; International audience; The Neodymium(Nd) isotope composition of fish remains has beenwidely used to track past changes in oceanic circulation. Although the number of published Nd isotope data for the Cretaceous has markedly increased in the last years, no consensus has been reached on the structure of the oceanic circulation and its evolution during the Late Cretaceous. Yet this period is characterised bymajor geodynamical and climatic changes andmarked by the disappearance of global oceanic anoxic events inwhich changes in oceanic circulation modesmay have played a significant role. In this study we present the first record of Nd isotopic composition of fish remains from contine…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousIsotopic signaturePaleontologyContinental marginJapanGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryoceanic circulation14. Life underwater[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesRadiogenic nuclide[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySeafloor spreadingCretaceous[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPeriod (geology)Seawaterneodymium isotopesGeology
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The Early-Cambrian Boho volcano of the El Graara massif, Morocco: Petrology, geodynamic setting and coeval sedimentation

2006

15 pages; International audience; A major volcanic episode is recorded across the Neoproterozoic-Cambrian transition in the Moroccan Anti-Atlas. Several volcanic cones are still preserved in the El Graara massif, laterally correlatable with volcanic flows dated as Early Cambrian (U/Pb date of 534 ± 10 Ma). Volcanic ashes and flows are interbedded with the uppermost part of the Adoudou dolostones, whereas the best-preserved volcano (the Boho Jbel) is onlapped by the overlying Lie-de-vin strata. Available petro-geochemical data from the Boho volcano suggest an alkaline magmatism probably derived from low-grade melting of a garnet–lherzolite mantle source, followed by fractional crystallizatio…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrySlope apron[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/Volcanology010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphySyenites01 natural sciencesDiagenesisLower CambrianBreccia[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyAlkaline basaltsPetrologySlope aponComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyBasaltgeographygeography.geographical_feature_categoryTerrigenous sedimentGeologyMassifDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesMoroccoVolcano13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphySubaerial[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyVolcanic coneGeology
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Occurrence of fossil organic matter in modern environments: optical, geochemical and isotopic evidence

2011

International audience; This study relates to the input and fate of fossil organic matter (FOM) in the modern environment, and focuses on two experimental watersheds overlying Jurassic marls: Le Laval and Le Brusquet (1 km(2) in area), located near Digne, Alpes-de-Haute-Provence, France. Considering that FOM delivery is mainly a result of different processes affecting sedimentary rocks [(bio)chemical and mechanical weathering], samples from different pools were collected: bedrocks, weathering profiles, soils and riverine particles. The samples were examined using complementary techniques: optical (palynofacies methods), geochemical (Rock-Eval 6 pyrolysis, C/N ratio), molecular (gas chromato…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesMineralogyWeatheringatmospheric carbon010502 geochemistry & geophysics01 natural sciencesstorageGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarlEnvironmental ChemistryOrganic matterglobal carbon balance0105 earth and related environmental scienceschemistry.chemical_classificationvariabilitysedimentary-rocks[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryerosionPollutionPalynofaciesALPES DE HAUTE PROVENCE[ SDE.MCG ] Environmental Sciences/Global Changesmarine-sedimentschemistry13. Climate actionSoil waterrock-eval pyrolysis[SDE]Environmental SciencesErosionSedimentary rockmodern soilshaute-provencePyrolysisGeology
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The first 40Ar-39Ar date from Oxfordian ammonite-calibrated volcanic layers (bentonites) as a tie-point for the Late Jurassic.

2013

AbstractEight volcanic ash layers, linked to large explosive events caused by subduction-related volcanism from the Vardar Ocean back-arc, interbedded with marine limestones and cherts, have been identified in the Rosso Ammonitico Veronese Formation (northeastern Italy). The thickest ash layer, attributed to the Gregoryceras transversarium ammonite Biozone (Oxfordian Stage), yields a precise and reliable 40Ar–39Ar date of 156.1 ± 0.89 Ma, which is in better agreement with GTS2004 boundaries than with the current GTS2012. This first biostratigraphically well-constrained Oxfordian date is proposed as a new radiometric tie-point to improve the Geologic Time Scale for the Late Jurassic, where a…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesgeochronologyBiozone010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesOxfordianPaleontologyGeologic time scale[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryStage (stratigraphy)0105 earth and related environmental sciencesAmmonitegeographygeography.geographical_feature_categorypalaeovolcanismbentoniteGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageJurassic Time Scale[ SDE.MCG ] Environmental Sciences/Global ChangesVolcano[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeochronologylanguageRadiometric datingGeologyVolcanic ash
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Tectonics of the Northern Bresse region (France) during the Alpine cycle

2003

International audience; Combining fieldwork and surface data, we have reconstructed the Cenozoic structural and tectonic evolution of the Northern Bresse. Analysis of drainage network geometry allowed to detect three major fault zones trending NE-SW, E-W and NW-SE, and smooth folds with NNE trending axes, all corroborated with shallow well data in the graben and fieldwork on edges. Cenozoic paleostress succession was determined through fault slip and calcite twin inversions, taking into account data of relative chronology. A N-S major compression, attributed to the Pyrenean orogenesis, has activated strike-slip faults trending NNE along the western edge and NE-SW in the graben. After a tran…

010504 meteorology & atmospheric sciences[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistorySketch map010502 geochemistry & geophysics01 natural sciences[SHS]Humanities and Social SciencesPaleontologyBresse grabenMicrotectonicsCompression (geology)0105 earth and related environmental sciencesEarth-Surface Processes[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and PrehistoryDeformation (mechanics)Alpine orogenesisGrabenTectonicsGeophysicsPaleostressesDrainage[SHS] Humanities and Social SciencesQuaternaryCenozoicGeologySeismologyChronology
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An improved understanding of the Alaska Coastal Current: the application of a bivalve growth-temperature model to reconstruct freshwater-influenced p…

2011

Shells of intertidal bivalve mollusks contain sub-seasonally to interannually resolved records of temperature and salinity variations in coastal settings. Such data are essential to understand changing land-sea interactions through time, specifically atmospheric (precipitation rate, glacial meltwater, river discharge) and oceanographic circulation patterns; however, independent temperature and salinity proxies are currently not available. We established a model for reconstructing daily water temperatures with an average standard error of ∼1.3 °C based on variations in the width of lunar daily growth increments of Saxidomus gigantea from southwestern Alaska, United States. Temperature explai…

010504 meteorology & atmospheric sciencesbiologyDischargeTemperature salinity diagramsPaleontologyIntertidal zone010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesSaxidomus giganteaSalinityOceanography13. Climate action[SDE]Environmental SciencesSeawater14. Life underwaterGlacial periodMeltwaterEcology Evolution Behavior and SystematicsGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences
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