Search results for "Oceanography"

showing 10 items of 1567 documents

Use of stable isotopes to investigate dispersal of waste from fish farm as a function of hydrodynamics.

2006

Stable isotopes were used to examine differential effects of fish farm waste on the water column and sediments. To achieve this objective, we chose 3 marine fish farms located along the coast of Sicily (Mediterranean Sea) as point-source disturbances, and a control area. The hypothesis that carbon and nitrogen isotope composition of particulate (POM) and sedimentary (SOM) organic matter varied with increasing distance (from cages to 1000 m) was tested at 3 levels of hydrodynam- ics: low (mean velocity of current (MVC) ~12 cm s -1 ), intermediate (MVC ~22 cm s -1 ), and high (MVC ~40 cm s -1 ). Different isotopic signals from allochthonous (fish waste) over natural (phytoplankton, terrigenou…

chemistry.chemical_classificationSettore BIO/07 - EcologiaEcologybusiness.industryTerrigenous sedimentStable isotope ratioFish farmingstable isotope aquaculture sedimentsAquatic ScienceIsotopes of nitrogenOceanographyWater columnMediterranean seachemistryAquacultureEnvironmental scienceOrganic matterFish farming Impact Water column Sediment Stable isotopes Hydrodynamics MediterraneanbusinessEcology Evolution Behavior and Systematics
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Role of peat organic matter on isotopic composition of most abundant benthic organisms in intertidal habitats of SW Iceland

2008

The transfer of peat organic matter (OM) from tidal pools of upper littoral to downstream rocky shores and its potential incorporation into marine biota were investigated using the stable isotope approach. Samplings were carried out in September 2004 in two SW Icelandic sites (Osar and Hvassahraun), where we selected (1) areas with shores where grass gently declined towards rocks and, on reaching the sea line, formed small tidal peat pools and (2) areas where grass and rocky shores were not contiguous, rather the grass lower limits were several hundreds of meters back from the shore. In both grass and no grass areas, in the intertidal zone, all benthic organisms and all potential OM sources…

chemistry.chemical_classificationSettore BIO/07 - EcologiaPeatEcologyEcologyIntertidal zoneFucus vesiculosusBiotaAquatic ScienceBiologybiology.organism_classificationRocky shoreOceanographyBenthic organism · Intertidal environment · Grass-pool · Peat · Stable isotope · Iceland · North AtlanticchemistryBenthic zoneLittoral zoneOrganic matterEcology Evolution Behavior and Systematics
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Sources of organic matter for inter-tidal consumers in Ascophyllum-shores (Sw Iceland): a multi stable isotope approach.

2007

Stable isotopes were used to examine the origin of organic matter in Icelandic Ascophyllum-based habitats, the role of different organic matters in filling intertidal food webs and the food preferences of the most abundant suspension feeders, grazers and predators. We selected three intertidal sites on the SW coast of Iceland where we sampled in early September 2004, organic matter sources (POM, SOM and most abundant primary producers, A. nodosum and F. vesciculosus) and the most abundant macrofauna species (barnacles, mussels, gastropods, sponge and crabs). Even though the primary production (Ascophyllum-based) was the same at the three study sites, the isotopic composition of common-among…

chemistry.chemical_classificationSettore BIO/07 - EcologiaPrimary producersbiologyEcologyStable isotope ratioIntertidal zoneAquatic ScienceIntertidal ecologyOceanographybiology.organism_classificationFood webchemistryHabitatBenthic organism Intertidal environment Stable isotope Iceland North AtlanticEnvironmental scienceOrganic matterAscophyllum
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Meiofauna and benthic microbial biomass in a semi-enclosed mediterranean marine system (Stagnone di Marsala, Italy)

2004

Microbial and meiofaunal dynamics and their relationships with the biochemical composition of the sedimentary organic matter were investigated in a semi-enclosed marine system (Marsala lagoon, Western Sicily, Mediterranean Sea). Sediment samples were collected on a monthly basis from March 1996 to February 1997 in four stations located along a N–S transect characterized by different hydrodynamic regimes. Total sedimentary organic matter concentration ranged from 5.681.11 to 156.2812.63 mg g1, while the biopolymeric fraction of organic carbon (BPC, measured as sum of the lipids, carbohydrates and proteins) accounted for only a small fraction (24%) of total organic matter. Total meiofaunal de…

chemistry.chemical_classificationTotal organic carbonMediterranean climateSettore BIO/07 - EcologiaEcologyMeiobenthosMeiofaunaBenthic microbial communityMediterranean lagoonSedimentOceanographyMediterranean seachemistryBenthic zoneSedimentary organic matterGeneral Earth and Planetary SciencesSedimentary organic matterEnvironmental scienceOrganic matterEcology Evolution Behavior and SystematicsGeneral Environmental Science
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Orbitally induced limestone/marlstone rhythms in the Albian—Cenomanian Cismon section (Venetian region, northern Italy): Sedimentology, calcareous an…

1996

Abstract A multidisciplinary study of the upper Albian—Cenomanian portion of the Cismon section (Venetian region, northern Italy) was undertaken in order to characterize the cyclic alternations of carbonate-rich and carbonate-poor layers and to investigate their possible origin and cyclic patterns. Limestone semicouplets are characterized by abundant radiolarians and micarbs (micron-sized calcitic fragments), common planktonic foraminifera, strong bioturbation, good oxygenation as expressed by the Mn* and V/(V+Ni) parameters, high Si/Al ratio, low K/Al, in the absence of pyrite and organic matter. The marlstone semicouplets are, on the contrary, frequently laminated, rich in pyrite and orga…

chemistry.chemical_classificationbiologyTerrigenous sedimentGeochemistryPaleontologyBiogenic silicaOceanographybiology.organism_classificationAnoxic watersForaminiferaPaleontologychemistryIsotope geochemistryMarlSedimentary rockOrganic matterEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Speciation of trialkyltin(IV) cations in natural fluids

2004

The hydrolysis of (CH(3))(3)Sn(+), (C(2)H(5))(3)Sn(+) and (C(3)H(7))(3)Sn(+) has been studied in a Synthetic Seawater (SSW) ionic medium simulating the major composition of natural seawater, at different salinities (5 less than or equal to S less than or equal to 45), and at t = 25 degreesC. Interactions with anionic components of SSW, considered as single sea salt, are determined by means of a complex formation model. By potentiometric measurements (ISE-H(+) and ISE-F(-) electrodes), the model has been extended to also consider interactions of organotins with carbonate and fluoride ions, which are other important components of seawater. Literature and new values of hydrolysis constants in …

chemistry.chemical_classificationfood.ingredientChemistryHydrolysisSea saltmedia_common.quotation_subjectInorganic chemistryIonic bondingArtificial seawaterSalt (chemistry)General ChemistryOceanographytrialkyltin(IV)SpeciationHydrolysisfoodIonic strengthEnvironmental ChemistrySeawaterIonic strength Protonation protonation constantsHydrolysis; trialkyltin(IV); Natural FluidsNatural FluidsWater Science and Technologymedia_commonMarine Chemistry
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Iodine containing species in the remote marine boundary layer: A link to oceanic phytoplankton

2011

[1] Iodine containing species have been measured in the particle phase (PM2.5) and the gas phase during a ship campaign between January and February 2007 in the South Atlantic marine boundary layer (MBL). Methyl iodide (CH3I) in the gas phase and soluble iodine species, i.e. iodide, iodate and an unidentified organic iodine species (UOI), in PM2.5 were measured. Temporal variations of gaseous and particulate iodine species were investigated. The exposure of the sampled air masses to phytoplankton along the back-trajectories was studied using a lagrangian transport model and satellite observations of oceanic chlorophyll-a concentration. Significant correlations were found between the concent…

chemistry.chemical_classificationfungiIodidechemistry.chemical_elementPelagic zoneParticulatesIodinechemistry.chemical_compoundGeophysicsOceanographychemistryChlorophyllEnvironmental chemistryPhytoplanktonGeneral Earth and Planetary SciencesEnvironmental scienceIodateMethyl iodideGeophysical Research Letters
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Thymine content of sea water as a measure of biosynthetic potential

1977

A hydrolysis procedure along with a high-pressure liquid chromatographic procedure is given enabling simple and reliable thymine determinations in the nanogram range in different fractions of sea-water samples taken from three different locations in the Northern Adriatic Sea. The levels corresponded to 1–3 μg DNA per liter. From total polyanionic thymine, which had been precipitated as the cetyltrimethylammonium salt, the highest percentage was linked to the particulate fraction, with a definite subsurface minimum at 10 to 15 m. There was a corresponding maximum of a high molecular “non-particulate” thymine-containing fraction at the corresponding depth. From the bottom at 30 m upwards to a…

chemistry.chemical_classificationgeographyRiver deltageography.geographical_feature_categoryEcologyEcologyAnalytical chemistryFront (oceanography)Salt (chemistry)Fraction (chemistry)Aquatic ScienceParticulatesBiologyThymineHydrolysischemistry.chemical_compoundchemistrySeawaterEcology Evolution Behavior and SystematicsMarine Biology
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Riverine impacts on benthic biodiversity and functional traits: A comparison of two sub-Arctic fjords

2020

Abstract Climate change is leading to increases in freshwater discharge to coastal environments with implications for benthic community structure and functioning. Freshwater inputs create strong environmental gradients, which potentially affect the community structure of benthic infauna. In turn, changes in functional trait composition have the potential to affect the processing of terrestrially-derived nutrients and organic matter along the freshwater to marine continuum. We investigated the effects of riverine inputs on benthic community structure, functional traits, taxonomic and functional diversity, and utilization of terrestrial organic matter in two contrasting northern Norwegian fjo…

chemistry.chemical_classificationgeographygeography.geographical_feature_categoryEcologyCommunity structureBiodiversityClimate changeFjordVDP::Matematikk og Naturvitenskap: 400Aquatic ScienceOceanographyNutrientchemistryBenthic zoneMacrobenthosVDP::Matematikk og Naturvitenskap: 400::Basale biofag: 470Environmental scienceOrganic matterVDP::Landbruks- og Fiskerifag: 900::Fiskerifag: 920VDP::Mathematics and natural science: 400
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Variability in inorganic and organic nitrogen uptake associated with riverine nutrient input in the Gulf of Riga, Baltic Sea

2001

Concentrations and rates of uptake of dissolved organic nitrogen (DON, free amino acids, and urea) and inorganic nitrogen (DIN, nitrate, and ammonium) were measured along two transects in the Gulf of Riga, a sub-basin of the Baltic Sea, during May and July 1996. Concentrations of total dissolved nitrogen (TDN) were 23±3 μg-at N 1−1 in the northern region (mouth) and 41±5 μg-at N 1−1 in the southern region (head) of the Gulf. Rates of nitrogen uptake, determined with15N-labeled substrates, reflected differences in TDN concentration between the regions. In May, uptake of DIN+DON measured 0.17 and 0.43 μg-at N 1−1 h−1 in the northern and southern parts of the Gulf, respectively. In July, DIN+D…

chemistry.chemical_elementAquatic SciencePlanktonNitrogenchemistry.chemical_compoundNutrientOceanographychemistryNitrateEnvironmental chemistryPhytoplanktonUreaEnvironmental ChemistryEnvironmental scienceAmmoniumTransectGeneral Environmental Science
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