Search results for "Sedimentary"

showing 10 items of 455 documents

Mid-Holocene vegetation dynamics in the Tejo River estuary based on palaeobotanical records from Ponta da Passadeira (Barreiro-Setúbal, Portugal)

2014

This paper presents the results of pollen and charcoal analyses carried out in the sedimentary formation of Ponta da Passadeira, south of the Tejo River estuary, Portugal. The data provide information regarding the evolution of the coastline and ecosystem of the estuary during the mid and late Holocene. The study focuses on a group of upright woody fossilized tree remains that, together with those identified earlier by Garcia-Amorena et al. (2007), form part of the fossil forest of Ponta da Passadeira. Eight remains were identified as Pinus pinaster, four as Pinus pinea and one as Pinus sp. Two specimens of these species were dated to 6523 and 5805 cal. a BP. Pollen analysis was undertaken …

Archeologygeographygeography.geographical_feature_categorybiologyGeologyEstuaryVegetationmedicine.disease_causebiology.organism_classificationArchaeologylaw.inventionlawvisual_artPollenvisual_art.visual_art_mediummedicinePinus pinasterSedimentary rockRadiocarbon datingPhysical geographyCharcoalEcology Evolution Behavior and SystematicsHoloceneGeologyBoreas
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Milankovitch forcing of Early Jurassic wildfires

2019

The Early Jurassic was characterized by major climatic and environmental perturbations which can be seen preserved at high resolution on orbital timescales. The Early Jurassic is a period of overall global warmth, and therefore serves as a suitable modern-day analogue to understand changes in the Earth System. Presently, Earth’s climate is warming and the frequency of large wildfires appears to be increasing. Recent research has indicated that Quaternary deposits reveal that wildfires respond to orbital forcings; however, to date no study has been able to test whether wildfire activity corresponds to changes over Milankovitch timescales in the deep past. A high-resolution astrochronology ex…

AstrochronologyMilankovitch cyclesOrbital forcingSedimentary rockPhysical geographyVegetationForcing (mathematics)QuaternaryMonsoonGeology
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Observations of atmospheric chemical deposition to high Arctic snow

2017

Abstract. Rapidly rising temperatures and loss of snow and ice cover have demonstrated the unique vulnerability of the high Arctic to climate change. There are major uncertainties in modelling the chemical depositional and scavenging processes of Arctic snow. To that end, fresh snow samples collected on average every 4 days at Alert, Nunavut, from September 2014 to June 2015 were analyzed for black carbon, major ions, and metals, and their concentrations and fluxes were reported. Comparison with simultaneous measurements of atmospheric aerosol mass loadings yields effective deposition velocities that encompass all processes by which the atmospheric species are transferred to the snow. It is…

Atmospheric Science010504 meteorology & atmospheric sciencesClimate changeCarbon black010501 environmental sciencesAtmospheric sciencesSnow01 natural scienceslcsh:QC1-999AerosolSedimentary depositional environmentlcsh:ChemistryDeposition (aerosol physics)Arcticlcsh:QD1-99913. Climate actionClimatologyEnvironmental scienceScavenginghuman activitieslcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Lithologic composition of the Earth's continental surfaces derived from a new digital map emphasizing riverine material transfer

2005

[1] A new digital map of the lithology of the continental surfaces is proposed in vector mode (n ≈ 8300, reaggregated at 0.5° × 0.5° resolution) for 15 rock types (plus water and ice) targeted to surficial Earth system analysis (chemical weathering, land erosion, carbon cycling, sediment formation, riverine fluxes, aquifer typology, coastal erosion). These types include acid (0.98% at global scale) and basic (5.75%) volcanics, acid (7.23%) and basic (0.20%) plutonics, Precambrian basement (11.52%) and metamorphic rocks (4.07%), consolidated siliciclastic rocks (16.28%), mixed sedimentary (7.75%), carbonates (10.40%), semi- to un-consolidated sedimentary rocks (10.05%), alluvial deposits (15…

Atmospheric ScienceGlobal and Planetary Changegeographygeography.geographical_feature_categoryEvaporiteLithologyGeochemistryVolcanic rockPrecambrianBasement (geology)Environmental ChemistryCarbonate rockSiliciclasticSedimentary rockGeomorphologyGeologyGeneral Environmental ScienceGlobal Biogeochemical Cycles
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Worldwide distribution of continental rock lithology: Implications for the atmospheric/soil CO2uptake by continental weathering and alkalinity river …

2003

[1] The silicate rock weathering followed by the formation of carbonate rocks in the ocean, transfers CO2 from the atmosphere to the lithosphere. This CO2 uptake plays a major role in the regulation of atmospheric CO2 concentrations at the geologic timescale and is mainly controlled by the chemical properties of rocks. This leads us to develop the first world lithological map with a grid resolution of 1° × 1°. This paper analyzes the spatial distribution of the six main rock types by latitude, continents, and ocean drainage basins and for 49 large river basins. Coupling our digital map with the GEM-CO2 model, we have also calculated the amount of atmospheric/soil CO2 consumed by rock weathe…

Atmospheric ScienceGlobal and Planetary Changegeographygeography.geographical_feature_categorySoil production functionLithologyGeochemistryWeatheringVolcanic rockIgneous rockClastic rockEnvironmental ChemistryCarbonate rockSedimentary rockGeomorphologyGeologyGeneral Environmental ScienceGlobal Biogeochemical Cycles
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Mixing relationships and the effects of secondary alteration in the Wishstone and Watchtower Classes of Husband Hill, Gusev Crater, Mars

2006

[1] The Wishstone and Watchtower Class rocks on Husband Hill preserve evidence for a geochemical relationship consistent with two-component mixing between a high Al 2 O 3 , TiO 2 , CaO, Na 2 O, P 2 O 5 end-member and a second end-member enriched in the elements MgO, Zn, S, Br, and Cl. The first end-member appears to be reasonably well represented by rocks of the Wishstone Class, while the second end-member is consistent with a chemical component, not represented by any lithology encountered by Spirit. The Watchtower Class appears to be an intermediate in the mixture. The concentration of the redox sensitive elements Fe and Mn display no systematic variation between rock classes, and the Fe-…

Atmospheric ScienceLithologyAnalytical chemistrySoil ScienceMineralogyWeatheringAquatic ScienceOceanographychemistry.chemical_compoundImpact craterGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)SulfateDissolutionEarth-Surface ProcessesWater Science and TechnologyEcologyPaleontologyForestryPhosphateGeophysicschemistrySpace and Planetary ScienceSoil waterSedimentary rockGeologyJournal of Geophysical Research: Planets
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Crustal dynamics of Mount Vesuvius from 1998 to 2005: Effects on seismicity and fluid circulation

2008

[1] This paper presents the results of hydrogeochemical and seismological studies carried out at Mount Vesuvius during the period June 1998 to December 2005. Hydrogeochemical data show the occurrence of slowly varying long-term variations in the total dissolved salts and bicarbonate contents of the groundwaters, accompanied by a general decline in water temperatures. The temporal distributions of air temperature and rainfall in the Vesuvius area suggest that these variations do not depend on changes in the hydrological regime. The changes in the geochemical parameters are accompanied by slight variations in both the seismicity rate and energy release. A further relationship between seismic …

Atmospheric ScienceSoil Sciencehydrogeochemistry vesuviusAquiferAquatic ScienceInduced seismicityOceanographyGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryAtmospheric temperatureStress fieldGeophysicsVolcanoShear (geology)Space and Planetary ScienceSedimentary rockGroundwaterGeologySeismologyJournal of Geophysical Research
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Geochemical mapping of magmatic gas–water–rock interactions in the aquifer of Mount Etna volcano

2001

Abstract Systematic analysis of major and minor elements in groundwaters from springs and wells on the slopes of Mt. Etna in 1995–1998 provides a detailed geochemical mapping of the aquifer of the volcano and of the interactions between magmatic gas, water bodies and their host rocks. Strong spatial correlations between the largest anomalies in pCO2 (pH and alkalinity) K, Rb, Mg, Ca and Sr suggest a dominating control by magmatic gas (CO2) and consequent basalt leaching by acidified waters of the shallow (meteoric) Etnean aquifer. Most groundwaters displaying this magmatic-type interaction discharge within active faulted zones on the S–SW and E lower flanks of the volcanic pile, but also in…

Basalt[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAlkalinityGeochemistryMineralogyAquifer010502 geochemistry & geophysics01 natural sciencesSalinityGeophysicsVolcano13. Climate actionGeochemistry and PetrologySedimentary rock[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMud volcanoWater well
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Composition and provenance analysis of beach sands in an almost isolated sedimentary system – A field study of the Galápagos Archipelago

2021

The Galapagos Archipelago is the surface expression of an active hotspot or long-lived mantle plume. The Archipelago consists of a group of 13 main islands which are located in the eastern central Pacific Ocean about 1,000 km west of the northern edge of the South American continent, east of the East Pacific Rise and south of the Galapagos spreading center. Because of the large distance to the nearest continental land mass, Galapagos can be seen as an almost isolated sedimentary system. A provenance study conducted on samples collected from seventeen beaches on eleven islands, demonstrates that mineral grains and particles were derived from weathering of predominantly basaltic rocks and wer…

BasaltgeographyProvenancegeography.geographical_feature_categoryGeochemistryengineering.materialMantle plumePumiceHotspot (geology)ArchipelagoengineeringGeneral Earth and Planetary SciencesPlagioclaseSedimentary rockGeologyAmerican Journal of Science
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The Lefkada barrier and beachrock system (NW Greece) — Controls on coastal evolution and the significance of extreme wave events

2012

Abstract The Lefkada–Preveza coastal zone, NW Greece, is characterised by an active barrier system and related extensive beachrock sequences. Besides the gradual coastal processes of longshore drift and spit evolution, the presence of active tectonics and the occurrence of tsunamis have been documented in previous studies and are part of the coastal geomorphological system. In this paper, we present the results of detailed multi-proxy sedimentological and geomorphological investigations carried out along the northern part of the barrier system and in back-beach positions. Our findings suggest that extreme wave events contributed to coastal and environmental changes and involved temporary br…

BeachrockLongshore driftTectonicsOceanographyCoastal zoneLittoral zoneSedimentary rockGeomorphologyGeologyNatural (archaeology)Earth-Surface ProcessesGeomorphology
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