Search results for "oceanography"

showing 10 items of 1567 documents

Geochemical implications for changing dust supply by the Indian Monsoon system to the Arabian Sea during the last glacial cycle

2004

Element concentrations of 43 elements as well as inorganic and organic carbon content of sediment core 70KL from the western Arabian Sea were measured with high (1 cm) sample resolution. Principal components of the sediment’s chemical composition were determined with the help of statistical principle component analysis. These components are representing the major environmental factors at the site. The most important processes controlling the observed variations are the changing lithogenic influx derived from the major wind systems of the region (i.e., the Arabian northwesterly winds, the northeast winter monsoon and the southwest summer monsoon), summer monsoon associated upwelling and biog…

Total organic carbonMonsoon of South AsiaOceanographyProductivity (ecology)UpwellingSediment550 - Earth sciencesGlacial periodMonsoonChemical compositionGeology
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Cenomanian–Turonian carbonate and organic-carbon isotope records, biostratigraphy and provenance of a key section in NE Sicily, Italy: Palaeoceanogra…

2008

In eastern Sicily, a series of highly organic-rich black shales occur as exotic blocks (~ 100 m across) floating in tectonized sediments (Argille Varicolori Unit containing olistoliths of Cretaceous-Palaeogene age). A 19-metre section, through one of these blocks near the town of Novara di Sicilia, includes cyclically bedded black shales, marlstones and claystones, which have been dated using planktonic foraminiferal and nannofossil biostratigraphy. On this basis, the section is assigned to the latest Cenomanian and clearly represents a manifestation of the Oceanic Anoxic Event characteristic of that interval. Total organic-carbon values range up to 23% and the relatively high hydrogen indi…

Total organic carbonProvenanceRange (biology)PaleontologyBiostratigraphyOceanographyCretaceousPaleontologychemistry.chemical_compoundchemistrySection (archaeology)CarbonateCenomanianEcology Evolution Behavior and SystematicsGeologySicily OAE Bonarelli Level Carbon-isotope stratigraphy TOC Biostratigraphy Palaeoceanography PalaeogeographyEarth-Surface Processes
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Origin and distribution of suspended organic matter as inferred from carbon isotope composition in a Mediterranean semi-enclosed marine system

1999

The origin and distribution of suspended organic matter, the trophic features and the stable carbon isotopic composition of particulate organic carbon (POC) were studied monthly in a Western Mediterranean semi-enclosed basin. Sampling stations were selected as a function of wind-exposure and the degree of vegetation cover and then compared with an adjacent unvegetated site. The predominant vegetation was seagrass (Posidonia oceanica and Cymodocea nodosa) and Caulerpa prolifera. Water samples were analyzed for total suspended matter (inorganic and organic fractions), photosynthetic pigments (chlorophyll-a and phaeopigments), dissolved organic carbon, particulate organic carbon and their isot…

Total organic carbonchemistry.chemical_classificationEcologybiologyCymodocea nodosachemistry.chemical_elementCaulerpa proliferabiology.organism_classificationOceanographyMediterranean seachemistryPosidonia oceanicaEnvironmental chemistryDissolved organic carbonGeneral Earth and Planetary SciencesEnvironmental scienceorganic matter sources carbon isotope ratio DOC POC MEDOrganic matterCarbonEcology Evolution Behavior and SystematicsGeneral Environmental Science
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Suspended particulate matter fluxes along with their associated metals, organic matter and carbonates in a coastal Mediterranean area affected by min…

2016

International audience; A study of suspended particulate matter (SPM) fluxes along with their associated metals, organic matter and carbonates, was conducted off the Mejerda River outlet in May 2011 and in March and July 2012 at depths of 10, 20 and 40 m using sediment traps. SPM fluxes are more significant near the Mejerda outlet, especially in winter, but dissipate further offshore. Normalization reveals that the Mejerda is a major source of Pb, Zn, Cd, Cu, Ni, and Co, all of which are the result of human activities. In contrast, Fe, Mn and N are of authigenic origin. The enrichment factor shows that Pb, Zn and especially Cd are the most highly polluting metals off the Mejerda outlet. Thi…

Tunisia010504 meteorology & atmospheric sciencesDrainage basinCarbonates010501 environmental sciencesAquatic ScienceOceanography01 natural sciencesMining[ SDE ] Environmental SciencesRiversMetals HeavyOrganic matter14. Life underwaterMejerda RiverHumic Substances0105 earth and related environmental scienceschemistry.chemical_classificationgeographyPrincipal Component Analysisgeography.geographical_feature_categoryMediterranean RegionCoastal pollutionHeavy metalsAuthigenicSuspended particulate matterParticulatesPollutionEnrichment factor6. Clean waterchemistryHeavy metals13. Climate actionMetalsEnvironmental chemistry[SDE]Environmental SciencesEnvironmental scienceMediterranean areaSubmarine pipelineParticulate MatterSeasonsEnrichment factorWater Pollutants ChemicalEnvironmental Monitoring
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Subglacial to proglacial depositional environments in an Ordovician glacial tunnel valley, Alnif, Morocco

2013

Abstract This paper presents the sedimentary analysis of an exceptional Ordovician glacial tunnel valley in the eastern part of the Anti-Atlas. The valley infill comprises two major glacial erosion surfaces (striated pavements) each overlain by a fining-upward glacial unit. These units are composed of five distinct facies associations, recording the evolution from subglacial to proglacial environments, and an additional sixth facies association, overtopping the tunnel valley infill, and associated with post-glacial environments. The tunnel valley infill also records a transitional environment between the subglacial and proglacial settings, which is compared with the Antarctic ice-sheet marg…

Tunnel valleyPaleontologyOceanographySedimentary depositional environmentPaleontologyFaciesOutwash plainInfillOrdovicianSedimentary rockGlacial periodGeomorphologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Does porewater or meltwater control tunnel valley genesis? Case studies from the Hirnantian of Morocco.

2015

18 pages; International audience; Several Ordovician tunnel valleys are exposed in the Moroccan Anti-Atlas Mountains, including the Alnif and the Foum Larjamme tunnel valleys, located 150 km away from each other. Sedimentological and deformational analyses of these two glacial troughs reveal that differing processes lead to their formations.The Alnif tunnel valley contains numerous deformation structures within sediments both below and above the main glacial erosion contact surface. Ball-structures and clastic dykes occur within preglacial sediments down to 35 m below glacial incisions while overlying glacial sediments contain fluted surfaces, clastic dykes, dewatering structures, folds and…

Tunnel valleyTunnel valleyMeltwaterIce streamGeochemistry[ SDU.STU.GL ] Sciences of the Universe [physics]/Earth Sciences/GlaciologyOrdovicianPaleontologySediment15. Life on landOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyPorewater pressureClastic rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyErosionSedimentary rockGlacial period[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/GlaciologyIce streamsMeltwaterGeomorphologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface Processes
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Environmental and depositional controls on laminated freshwater carbonates: An example from the Roman aqueduct of Patara, Turkey

2013

Carbonate deposits in aqueducts are a new high-resolution data source for environmental changes during the time of the Roman Empire, notably in the fields of palaeoclimate and spring hydrology. In order to distinguish environmental effects from those related to depositional setting, laminated carbonate deposits were compared along the entire length of an ancient aqueduct channel at Patara, Turkey. The carbonate deposits, up to 80mm in thickness, are composed of lamina couplets up to 1mm thick of alternating porous microspar and dense, columnar sparite. The former formed in the dry, warm season and the latter in the wet, cool season. The presence of biofilms seems to play a role in the devel…

Turkeyaqueductcarbon isotopeRoman eraδ18ORoman aqueductmicrostructureGeochemistryAqueductMuglaArchaeoseismologyPalaeoclimateOceanographybiofilmIsotopes of oxygenSedimentary depositional environmentcarbonatechemistry.chemical_compoundPaleontologyCalcareous sinterwater temperaturepaleoclimatelaminationstable isotopeoxygen isotopeCarbonate depositssinterPataraEcology Evolution Behavior and SystematicsStable isotopesdepositional environmentEarth-Surface ProcessesCalcareous sinterPaleontologyarchaeologyLamination (geology)chemistryCarbonateLayeringenvironmental effectGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Benthic foraminifera as indicators of relative sea-level fluctuations: Paleoenvironmental and paleoclimatic reconstruction of a Holocene marine succe…

2017

This study presents the results of an integrated stratigraphic analysis conducted on a marine gravity core (MSK-12 C4) recovered from the outer continental shelf (82 mwater depth) of western Calabria, ~2.6 km, NE of Capo Vaticano (Eastern Tyrrhenian margin). The gravity core MSK-12 C4 recovered a stratigraphic succession of 4.18 m beneath the seafloor representing the last ~11.1 ka. Sedimentological analysis, micropaleontological quantitative analysis on benthic foraminiferal assemblages, tephrostratigraphy, sequence stratigraphic analysis of high resolution reflection seismic data recorded in the core site area and AMS 14C absolute age determinations allowed reconstructing the marine recor…

Tyrrhenian Sea010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaHolocene climatic optimum010502 geochemistry & geophysics01 natural sciencesForaminiferaPaleontologyAbsolute datingSea levelHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesStable isotopesgeographyIntegrated stratigraphygeography.geographical_feature_categoryPaleoenvironmental and paleoclimatic reconstructionbiologyContinental shelfBenthic foraminiferaSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationStable isotopeSeafloor spreadingSettore GEO/08 - Geochimica E VulcanologiaOceanographyBenthic zoneLittle Ice AgeGeology
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Sea-level changes during the last 41,000 years in the outer shelf of the southern Tyrrhenian Sea: Evidence from benthic foraminifera and seismostrati…

2011

Abstract An integrated high resolution study based both on a seismostratigraphic approach and on a sedimentary core (VIB 10), collected in the outer shelf (127 m depth) from the southern Tyrrhenian Sea (Gulf of Termini, Sicily), provides new data about climatic, eustatic and paleoenvironmental changes during the last ∼41,000 years. The results based on the interpretation of a seismic profile, on benthic foraminifera assemblages and on δ18O records, allowed recognition of two drastic sea-level falls during the Last Glacial Maximum (LGM) and the Younger Dryas (YD). The short deglacial event, between LGM and YD, known as Bolling/Allerod, played an important role in the sea-level rise that prod…

Tyrrhenian Sea010506 paleontologySettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18O[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Holocene climatic optimumbenthic foraminifera[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesAllerød oscillationstable isotopes.ForaminiferaSea-level changeSea-level changes; Tyrrhenian Sea; benthic foraminifera; seismostratigraphic analysis; stable isotopes.14. Life underwaterYounger DryasSea levelComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyLast Glacial MaximumSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationOceanography13. Climate actionBenthic zoneseismostratigraphic analysiGeology
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Signals from the deep-sea: Genetic structure, morphometric analysis, and ecological implications of Cyclothone braueri (Pisces, Gonostomatidae) early…

2020

Abstract Cyclothone braueri (Stomiiformes, Gonostomatidae) is a widely distributed fish inhabiting the mesopelagic zone of marine tropical and temperate waters. Constituting one of the largest biomasses of the ocean, C. braueri is a key element in most of the ecological processes occurring in the twilight layer. We focused on the ecological processes linked to early life stages in relation to marine pelagic environmental drivers (temperature, salinity, food availability and geostrophic currents) considering different regions of the Central Mediterranean Sea. A multivariate morphometric analysis was carried out using six parameters with the aim of discerning different larval morphotypes, whi…

Tyrrhenian Sea0106 biological sciencesGenetic StructuresMesopelagic zoneAquatic ScienceOceanography010603 evolutionary biology01 natural sciencesLarvaeMediterranean seaGeneticsMediterranean SeaAnimalsCiliophoraStomiiformesbiologyEcologyMorphometry010604 marine biology & hydrobiologyFishesPelagic zoneGeneral MedicineFish populationRemote sensingIchthyoplanktonbiology.organism_classificationPollutionStrait of SicilyGenetic divergenceMultivariate analysisLarvaIchthyoplanktonGenetic structureMesopelagic zoneGonostomatidaeMarine Environmental Research
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