Search results for "Ocean"

showing 10 items of 2919 documents

Influence of pre-existing microstructure on mechanical properties of marine ice during compression experiments

2014

AbstractMarine ice is an important component of ice shelves in Antarctica. It accretes in substantial amounts at weak points and below ice shelves. It is likely to exhibit peculiar rheological properties, which are crucial to understanding its potential role in stabilizing ice-shelf flow. Due to its location and consolidation processes, marine ice can present a variety of textures which are likely to influence its rheological properties. We present a new dataset of unconfined uniaxial compression experiments on folded marine ice samples that have been cut at various angles to the folds. Texture and fabric analyses are described ‘before’ and ‘after’ the deformation experiment. It is shown th…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesConsolidation (soil)MineralogyPressure ridge010502 geochemistry & geophysics01 natural sciencesIce shelfPhysics::GeophysicsCreepSea ice growth processesRheologyPerpendicularGeotechnical engineeringAstrophysics::Earth and Planetary AstrophysicsAnisotropyPhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Glaciology
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Improved constraints on open-system processes in fossil reef corals by combined Th/U, Pa/U and Ra/Th dating: A case study from Aqaba, Jordan

2019

Abstract Here we present 230Th/U, 231Pa/U as well as 226Ra/230Th isotope ratios from five fossil reef corals of Last Interglacial origin from the Gulf of Aqaba, Northern Red Sea. The results show clear evidence for open-system behaviour with strongly elevated δ234U values and U concentrations indicating post-depositional U addition. The combined application of all isotope systems enables us to better constrain the nature and timing of the open-system processes than only based on the 230Th/U data. Quantitative modelling of the diagenetic processes allowed us to reproduce the trends in the isotope ratios. Two of the five corals were probably affected by two separate phases of U addition with …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesCoralCoral reef010502 geochemistry & geophysics01 natural sciencesDiagenesisOceanographyGeochemistry and PetrologyInterglacialSeawaterStadialCoral growthReefGeology0105 earth and related environmental sciencesGeochimica et Cosmochimica Acta
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2015

Large volcanic eruptions are major geohazards, so identifying their frequency in the geologic record is critical for making predictions and hazard assessments. Following the discovery of a thick (18 cm) tephra layer in marine sediments from Integrated Ocean Drilling Program (IODP) Site U1396 between Montserrat and Guadeloupe in the Caribbean Sea, we document here how high-precision Pb isotopes, trace elements, and grain morphological analyses of the tephra can be used, together with volcanological models, to identify a large (Volcanic Explosivity Index ?6) Plinian eruption from Basse-Terre, Guadeloupe, at ca. 2.36 Ma. This previously unrecognized eruption is believed to be the largest docum…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesDrillingSedimentGeologyVolcanic explosivity index010502 geochemistry & geophysicsGeologic record01 natural sciencesPaleontologyDense-rock equivalentOceanographyVolcano13. Climate actionStage (stratigraphy)14. Life underwaterTephraGeology0105 earth and related environmental sciencesGeology
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NO EXCESSIVE CRUSTAL GROWTH IN THE CENTRAL ASIAN OROGENIC BELT: FURTHER EVIDENCE FROM FIELD RELATIONSHIPS AND ISOTOPIC DATA

2017

Abstract We provide new field observations and isotopic data for key areas of the Central Asian Orogenic Belt (CAOB), reiterating our previous assessment that no excessive crustal growth occurred during its ca. 800 Ma long orogenic evolution. Many Precambrian blocks (microcontinents) identified in the belt are exotic and are most likely derived from the northern margin of Gondwana, including the Tarim craton. Ocean opening in the Palaeo-Asian Ocean, arc formation and accretionary processes began in the latest Mesoproterozoic along the southern margin of the Siberian craton and continued into the Neoproterozoic, giving rise to tectono-metamorphic terranes distinct from the exotic microcontin…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEarth scienceContinental crustScienceQGeochemistryGeologyOrogenyCrust010502 geochemistry & geophysics01 natural sciencesCratonGondwanaGeophysicsOceanic crustIsland arcGeologyEarth-Surface Processes0105 earth and related environmental sciencesTerraneGeodinamika i Tektonofizika
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Late Holocene erosion of the Canopic promontory (Nile Delta, Egypt)

2017

International audience; The mouths of the Nile Delta are sensitive coastal areas, their geomorphology primarily being mediated by relative sea-level rise and sediment supply. To further document the Holocene evolution of the Nile's Canopic mouth, a core was taken from the southern shores of Abu Qir Bay, close to the ancient Canopic channel. Core bio-sedimentology and chronostratigraphy highlight four stages of marine incursion which are juxtaposed upon the general progradation trend of the Nile coast in this area. Compiled age-depth points from sediment cores taken in Abu Qir Bay underscore two phases of negative sediment budget at the Canopic mouth: (1) a first period, between 3.5 and 2 ka…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeoarchaeologySubmersion (coastal management)[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeology15. Life on land010502 geochemistry & geophysicsOceanography01 natural sciencesOceanography13. Climate actionGeochemistry and PetrologyRiver mouth14. Life underwaterProgradationChronostratigraphySedimentary budgetGeologySea levelHolocene0105 earth and related environmental sciencesMarine Geology
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El Niño in the Eocene greenhouse recorded by fossil bivalves and wood from Antarctica

2011

[1] Quasi-periodic variation in sea-surface temperature, precipitation, and sea-level pressure in the equatorial Pacific known as the El Nino – Southern Oscillation (ENSO) is an important mode of interannual variability in global climate. A collapse of the tropical Pacific onto a state resembling a so-called ‘permanent El Nino’, with a preferentially warmed eastern equatorial Pacific, flatter thermocline, and reduced interannual variability, in a warmer world is predicted by prevailing ENSO theory. If correct, future warming will be accompanied by a shift toward persistent conditions resembling El Nino years today, with major implications for global hydrological cycles and consequent impact…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGreenhouseDriftwood15. Life on land010502 geochemistry & geophysics16. Peace & justice01 natural sciencesGeophysicsOceanographyEl Niño13. Climate actionPeninsulaClimatologyGeneral Earth and Planetary SciencesEnvironmental scienceClimate modelPrecipitationThermocline0105 earth and related environmental sciencesTeleconnectionGeophysical Research Letters
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Enhanced volcanic hot-spot detection using MODIS IR data: results from the MIROVA system

2015

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMeteorologyGeologyOcean EngineeringHot spot (veterinary medicine)010502 geochemistry & geophysics01 natural sciencesVolcanoGeology0105 earth and related environmental sciencesWater Science and TechnologyRemote sensingGeological Society, London, Special Publications
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Dynamics of ice mass deformation: Linking processes to rheology, texture, and microstructure

2013

[1] Prediction of glacier and polar ice sheet dynamics is a major challenge, especially in view of changing climate. The flow behavior of an ice mass is fundamentally linked to processes at the grain and subgrain scale. However, our understanding of ice rheology and microstructure evolution based on conventional deformation experiments, where samples are analyzed before and after deformation, remains incomplete. To close this gap, we combine deformation experiments with in situ neutron diffraction textural and grain analysis that allows continuous monitoring of the evolution of rheology, texture, and microstructure. We prepared ice samples from deuterium water, as hydrogen in water ice has …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMineralogyGlacierSlip (materials science)Strain rateNeutron scattering010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsGeophysicsRheologyDeformation mechanism13. Climate actionGeochemistry and PetrologyHardening (metallurgy)CrystallitePhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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Reorganization of the North Atlantic Oscillation during early Holocene deglaciation

2016

Laurentide ice-sheet retreat continued into the mid-Holocene. Speleothem-based precipitation records suggest the cessation of melt led to the establishment of the present precipitation patterns associated with the North Atlantic Oscillation. The North Atlantic Oscillation is the dominant atmospheric pressure mode in the North Atlantic region and affects winter temperature and precipitation in the Mediterranean, northwest Europe, Greenland, and Asia1. The index1 that describes the sea-level pressure difference between Iceland and the Azores is correlated with a dipole precipitation pattern over northwest Europe and northwest Africa. How the North Atlantic Oscillation will develop as the Gree…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesNorth Atlantic Deep WaterGreenland ice sheet010502 geochemistry & geophysics01 natural sciencesOceanographyAtlantic Equatorial mode13. Climate actionNorth Atlantic oscillationClimatologyAtlantic multidecadal oscillationDeglaciationGeneral Earth and Planetary SciencesIce sheetGeology0105 earth and related environmental sciencesAzores HighNature Geoscience
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A mechanism for brief glacial episodes in the Mesozoic greenhouse

2011

[1] The Mesozoic, perhaps the longest period of warmth during the Phanerozoic Earth history, has been repeatedly affected by short-lived cold interludes lasting about one million years. While the origin of these cold snaps has been classically attributed to a temporary atmospheric CO2 drawdown, quantified mechanisms explaining these instabilities of the carbon cycle are still lacking. Based on a climate carbon cycle model, we show that the general demise of carbonate platforms accompanying these short-lived cold interludes is a powerful mechanism capable of generating a fast atmospheric CO2 decrease and a moderate sea level drop associated with ice sheet buildup. The temporary nature of the…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesPaleontology010502 geochemistry & geophysicsOceanography01 natural sciencesCarbon cyclePaleontologychemistry.chemical_compoundchemistry13. Climate actionPhanerozoicPaleoclimatologySnowball EarthCarbonateGlacial periodIce sheetGeologySea level0105 earth and related environmental sciencesPaleoceanography
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