Search results for "PELE"

showing 10 items of 139 documents

Investigation of marine and continental layers in a stalactite older than 1 million years (Custonaci, north-western sector of Sicily)

2012

Questo lavoro si basa sul ritrovamento, in una grotta carsica, a 100 metri di quota a Custonaci in provincia di Trapani, di una stalattite di notevole interesse paleo climatico, ricoperta da coralli marini, la cui sezione rivela la presenza di 3 Iatus che denotano una interruzione della deposizione di carbonato continentale presumibilmente in seguito a trasgressioni marine. Il carbonato, datato attraverso la metodologia 230Th/U MC-ICPMS (NeptunePlus), ha fornito una età più antica del limite temporale massimo di applicabilità del metodo ( 600 ka). I coralli, che ricoprono il livello continentale più giovane, analizzati usando il rapporto 87Sr/86Sr, hanno fornito una età di 1.1±0.2 Myrs. Al…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere[SDU.OCEAN] Sciences of the Universe [physics]/Ocean AtmosphereSettore GEO/04 - Geografia Fisica E GeomorfologiaSettore GEO/01 - Paleontologia E Paleoecologia[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentspeleothem with marine and continental layers coral overgrowth submerged cave.[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS
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2021

Abstract. Lignin oxidation products (LOPs) are widely used as vegetation proxies in climate archives, such as sediment and peat cores. The total LOP concentration, Σ 8, provides information on the abundance of vegetation, while the ratios C / V and S / V of the different LOP groups also provide information on the type of vegetation. Recently, LOP analysis has been successfully applied to speleothem archives. However, there are many open questions concerning the transport and microbial degradation of LOPs on their way from the soil into the cave system. These processes could potentially alter the original source-dependent LOP signals, in particular the C / V and S / V ratios, and thus compli…

geographygeography.geographical_feature_categoryPeat010504 meteorology & atmospheric sciencesSpeleothemSedimentSoil scienceVegetation15. Life on landPlant litter010502 geochemistry & geophysics01 natural sciencesCaveAbundance (ecology)Environmental scienceSoil horizonEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesBiogeosciences
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Abnormalities caused by chloroform and ether in the spermatogenesis of mammals [Chloroforma un ētera radītie traucējumi zīdītāju spermatogenezē]

1937

Teksts angļu valodā, kopsavilkums latviešu valodā.

Zoology experimentalAnimal experimentsPeles - eksperimentiDzīvnieku eksperimentiZīdītāju spermatogeneze - eksperimenti:NATURAL SCIENCES::Biology::Organism biology::Morphology [Research Subject Categories]Mammalian spermatogenesis - experimentsZooloģija eksperimentālā
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In-situ high spatial resolution LA-MC-ICPMS 230Th/U dating enables detection of small-scale age inversions in speleothems

2017

Abstract We present an in-situ method for Th and U isotope measurements by laser ablation multi-collector inductively coupled plasma mass spectrometry (LA-MC-ICPMS) to determine possible age inversions of stalagmites, using a 213 nm Nd:YAG laser connected to an MC-ICPMS. Due to the low ion beam intensity of 230 Th (20–120 counts per second, cps), we carefully optimized the operating parameters to get highest possible ion beam intensities, i.e., laser fluence (25 J cm −2 ), spot size (110 μm), pulse repetition rate (20 Hz), scan speed (4 μm s −1 ), integration time (1000 s), and He and Ar gas flow (∼0.9 L min −1 and ∼0.6 L min −1 respectively). A precision (2 relative standard error, 2RSE) o…

Time delay and integrationIon beamAnalytical chemistryMineralogy010502 geochemistry & geophysics01 natural scienceslaw.inventionGeochemistry and PetrologylawImage resolutionInductively coupled plasma mass spectrometry0105 earth and related environmental sciencesEarth-Surface ProcessesReproducibilityLaser ablationChemistry010401 analytical chemistrylcsh:QE1-996.5GeologySecular equilibriumGeotechnical Engineering and Engineering GeologyLaserSpeleothemLaser ablation0104 chemical scienceslcsh:Geology230Th/U datingGeophysicsMC-ICPMS
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Constraining speleothem oxygen isotope disequilibrium driven by rapid CO2 degassing and calcite precipitation: Insights from monitoring and modeling

2020

Abstract Oxygen isotopes are the most commonly applied speleothem proxy for reconstructing Quaternary changes in precipitation and/or temperature. These interpretations are either limited to qualitative wetting and drying trends or rely on theoretical, experimental and/or empirical equilibrium isotope fractionation factors for more quantitative constraints. These various fractionation factors have similar temperature sensitivities, but their absolute values differ, and cave calcite does not appear to generally precipitate in isotopic equilibrium with its drip water. Rapid CO2 degassing paired with calcite precipitation, both occurring under disequilibrium conditions, are a set of mechanisms…

Calcitegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesδ18OSpeleothemMineralogyStalagmite010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenchemistry.chemical_compoundIsotope fractionationchemistryCaveGeochemistry and PetrologyPaleoclimatologyEnvironmental science0105 earth and related environmental sciencesGeochimica et Cosmochimica Acta
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Persistent link between Caribbean precipitation and Atlantic Ocean circulation during the Last Glacial revealed by a speleothem record from Puerto Ri…

2020

The sensitivity of tropical Atlantic precipitation patterns to the mean position of the Intertropical Convergence Zone (ITCZ) at different time scales is well‐known. However, recent research suggests a more complex behavior of the northern hemispheric tropical rain belt related to the ITCZ in the western tropical Atlantic. Here we present a precisely dated speleothem multi‐proxy record from a well‐monitored cave in Puerto Rico, covering the period between 46.2 and 15.3 ka. The stable isotope and trace element records document a pronounced response of regional rainfall to abrupt climatic excursions in the North Atlantic across the Last Glacial such as Heinrich stadials and Dansgaard/Oeschger…

551.7Atmospheric Sciencegeographygeography.geographical_feature_categoryStable isotope ratio550.28Last GlacialspeleothemsOcean currentPaleontologySpeleothemstable isotopesprecipitation reconstructionOceanographyOceanographyHeinrich stadialsPrecipitationGlacial periodGeologyDansgaard/Oeschger cycles
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Effects of glaciation on karst hydrology and sedimentology during the Last Glacial Cycle: The case of Granito cave, Central Pyrenees (Spain)

2021

In Alpine regions, speleothem development on karst systems largely occurs during warm interglacial or interstadial phases due to their limited growth during cold stages. Still, recent attention has been given to the role of clastic sediments in caves, less dependent on temperature conditions. Yet, only a small number of caves worldwide preserve both speleothems and detrital deposits. Here we present an outstanding record of fine-grain laminated sediments and carbonate speleothems from the Granito cave (South Central Pyrenees, Spain) associated with seasonal to annual hydroclimatic pulses through the Last Glacial Cycle (LGC). Analysis of cave clastic facies together with new absolute dates o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistrySpeleothemHydrological responseStalagmite04 agricultural and veterinary sciences580 Plants (Botany)Upper Pleistocene01 natural sciencesCaveMoraineInterglacial040103 agronomy & agriculture0401 agriculture forestry and fisheriesGlacial periodCave sedimentsCentral PyreneesGeologyHolocenePhreaticGlacier dynamics0105 earth and related environmental sciencesEarth-Surface Processes
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New insights on the Carburangeli Cave speleogenesis: a flank margin cave in Northern Sicily (Italy)

2022

Flank margin caves form in coastal regions by mixing dissolution. Their development is controlled by the position of the freshsalt water mixing boundary, which in turn, is related to sea-level position. They are characterized by a typical cave pattern and cave-wall morphologies and represent good indicators of past sea levels. This contribution shows the results of recent studies conducted in the Carburangeli Cave, a small sub-horizontal cavity developed in Northern Sicily, close to Palermo. This cave was firstly known for paleontological and archaeological findings and for these reasons, along with its speleological and biological interest, a Nature Reserve has been instituted by the Sicil…

speleogenesiflank margin caveSettore GEO/04 - Geografia Fisica E GeomorfologiaKarst processeSicily
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2020

Abstract. A compilation of the published literature on dust content in terrestrial and marine sediment cores was synchronized with pollen data and speleothem growth phases on the Greenland Ice Core Chronology 2005 (GICC05) time axis. Aridity patterns for eight key areas of the global climate system have been reconstructed for the last 60 000 years. These records have different time resolutions and different dating methods, i.e. different types of stratigraphy. Nevertheless, all regions analysed in this study show humid conditions during early Marine Isotope Stage 3 (MIS3) and the early Holocene or deglaciation, but not always at the same time. Such discrepancies have been interpreted as reg…

Global and Planetary Changegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesStratigraphyNorthern HemispherePaleontologySpeleothemLast Glacial Maximum010502 geochemistry & geophysics01 natural sciencesAridIce core13. Climate actionPaleoclimatologyDeglaciationPhysical geographyHoloceneGeology0105 earth and related environmental sciencesClimate of the Past
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Climatic dependence of stable carbon and oxygen isotope signals recorded in speleothems: From soil water to speleothem calcite

2011

Abstract Understanding the relationship between stable isotope signals recorded in speleothems (δ 13 C and δ 18 O) and the isotopic composition of the carbonate species in the soil water is of great importance for their interpretation in terms of past climate variability. Here the evolution of the carbon isotope composition of soil water on its way down to the cave during dissolution of limestone is studied for both closed and open-closed conditions with respect to CO 2 . The water entering the cave flows as a thin film towards the drip site. CO 2 degasses from this film within approx. 10 s by molecular diffusion. Subsequently, chemical and isotopic equilibrium is established on a time scal…

CalciteHydrologygeographygeography.geographical_feature_categoryStable isotope ratioMineralogySpeleothemOxygen isotope ratio cycleIsotopes of oxygenchemistry.chemical_compoundIsotope fractionationchemistryGeochemistry and PetrologySoil waterCarbonateGeologyGeochimica et Cosmochimica Acta
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