Search results for "SAPR"

showing 10 items of 142 documents

Calcareous Nannofossil and Planktonic Foraminifera Biostratigraphy of selected Piacenzian-Gelasian Laminites from Southern Italy

2011

Here we present the biostratigraphic and chronostratigraphic framework of a number of selected diatomaceous laminated intervals from the Crotone Basin (Calabria, Southern Italy). These layers, which we consider correlative to the Eastern Mediterranean Sapropel Layers, range in age from the early Piacenzian to the Gelasian, and show surprising thicknesses, suggesting that they were probably laid down in a landlocked, overfed basin. Specifically, a thick laminite from the surroundings of Cropani (Catanzaro) can be ascribed to nannofossil biozone MNN 16a and planktonic foraminifera biozone MPL 4b (lower Piacenzian) according to the Mediterranean calcareous plankton biostratigraphic zonations. …

Mediterranean climateCalcareous NannofossilPiacenzianbiologyBiostratigraphyGeologyBiozonePlio-PleistoceneSapropelCalcareous Nannofossil; Planktonic Foraminifera; Biostratigraphy; Southern Italy; Plio-PleistoceneBiostratigraphyStructural basinbiology.organism_classificationForaminiferaPaleontologyPlio-PleistoceneGeneral Earth and Planetary SciencesPlanktonic ForaminiferaSouthern ItalyGeologyItalian Journal of Geosciences
researchProduct

African monsoon variability during the previous interglacial maximum.

2002

Little is known about centennial- to millennial-scale climate variability during interglacial times, other than the Holocene. We here present high-resolution evidence from anoxic (unbioturbated) sediments in the eastern Mediterranean Sea that demonstrates a sustained V800-yr climate disturbance in the monsoonal latitudes during the Eemian interglacial maximum (V125 ka BP). Results imply that before and after this event, the Intertropical Convergence Zone (ITCZ) penetrated sufficiently beyond the central Saharan watershed (V21n) during the summer monsoon to fuel flooding into the Mediterranean along the wider North African margin, through fossil river/wadi systems that to date have been cons…

Mediterranean climateEemianIntertropical Convergence ZoneSapropelMonsoonMediterranean BasinGeophysicsOceanographySpace and Planetary ScienceGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyInterglacialEarth and Planetary Sciences (miscellaneous)HoloceneGeologyComputingMilieux_MISCELLANEOUS
researchProduct

Pliocene sapropels in the northern Adriatic area: chronology and paleoenvironmental significance

1997

Abstract A detailed stratigraphic and paleoenvironmental study was carried out ona marine section from the Marecchia Valley in the Northern Apennines. The section consists predominantly of deep-water hemipelagic clays intercalated with 15 thick, laminated sapropels (M1–M15). Based on biostratigraphic (calcareous nannoplankton and planktonic foraminifera) and magnetostratigraphic results, the Marecchia Valley section is interpreted as being middle to late Pliocene in age, extending from the upper part of the Gauss Chron to the lower part of the Matuyama Chron. The high resolution stratigraphy allows us to correlate, for the first time, these northern Italian sapropels with sapropels previous…

Mediterranean climatePliocenebiologyStratigraphyPaleontologySapropelOceanographybiology.organism_classificationMediterranean region; Paleoclimatology; Pliocene; StratigraphyForaminiferaBottom waterPaleontologyStratigraphyBenthic zonePaleoclimatologyMediterranean regionPaleoclimatologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesChronologyPalaeogeography, Palaeoclimatology, Palaeoecology
researchProduct

Surface and deep water conditions in the Sicily channel (central Mediterranean) at the time of sapropel S5 deposition

2011

New centennial-scale data of benthic foraminifera assemblages and of stable isotopes of foraminifera shells from the Sicily Channel, representative of surface and bottom waters, over the interval between about 140 and 110 kyr BP, are presented. During this period anoxia developed on the eastern Mediterranean basin and sapropel S5 deposited. Although anoxic sediments have not been deposited in the Sicily Channel, this area is strategic to study the character of intermediate waters, whose chemical-physical properties strongly precondition the eastern Mediterranean deep water formation. So far, no data from these water masses have been obtained, apart from the isotopic composition of shells of…

Mediterranean climateWater massbiologyPleistoceneSicily ChannelBenthic foraminiferaPaleontologySapropelLate QuaternaryOceanographybiology.organism_classificationLast InterglacialForaminiferaMediterranean seaOceanographyStable IsotopeBenthic zoneSapropel S5Surface waterEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesStable isotopes
researchProduct

A high-resolution record of the last deglaciation in the Sicily Channel based on foraminifera and calcareous nannofossil quantitative distribution

2003

Abstract Relative abundance fluctuations in planktic foraminiferal and calcareous nannofossil assemblages are reported on the basis of a high-resolution study of ODP Leg 160 Hole 963D, drilled in the Sicily Strait, near Capo Rossello (southern Sicily). With its 8 m of undisturbed sediments, the core covers the interval from 1.5 to 23 kyr, allowing a 50–100-yr sampling resolution. All the short warm and cold events and sub-events recorded in this time interval in the GRIP Greenland ice core and at several Mediterranean sites were recognized. On this basis, a total number of nine ecozones based on planktic foraminifera and seven ecozones based on calcareous nannofossils were identified. A sho…

Mediterranean climatebiologySouthern MediterraneanPaleontologyplanktic foraminiferaSapropelOceanographybiology.organism_classificationpaleoecologyForaminiferaPaleontologyOceanographyIce corecalcareous nannofossilPaleoecologyDeglaciationecozoneSedimentary rockEcology Evolution Behavior and SystematicsHoloceneGeologylate QuaternaryEarth-Surface Processes
researchProduct

Macrofungi in Mediterranean maquis along seashore and altitudinal transects

2014

In semi-arid Mediterranean environments, fungal activity is fundamental for buffering biotic and abiotic stress to the plant and for sustaining a vegetation cover. Despite the important role that fungi play in habitats stability, mycological data from Mediterranean ecosystems are scarce and fragmentary. We investigated fungal diversity in several areas characterized by Mediterranean maquis, from continental Italy, Sicily, and Greece in order to contribute to the analysis of distribution, ecology, and diversity of macrofungi in evergreen sclerophyllous shrublands at different elevation and distance from the seashore across the Mediterranean Basin. Several fungal taxa that are remarkable due …

Mediterranean climategeographygeography.geographical_feature_categoryEcologySclerophyllSettore BIO/02 - Botanica SistematicaPlant ScienceBiologyEvergreenMediterranean BasinShrublandTaxonEctomycorrhizal specieswood-inhabiting fungiHabitatmacromycetesBotanyMediterranean ecosystemsmolecular analysisEctomycorrhizal species macromycetes Mediterranean ecosystems molecular analysis saprotrophs wood-inhabiting fungi.TransectsaprotrophsEcology Evolution Behavior and Systematics
researchProduct

Wood-inhabiting fungal communities : Opportunities for integration of empirical and theoretical community ecology

2022

Publisher Copyright: © 2021 The Author The interest in studying wood-inhabiting fungal communities has grown in recent years. This interest has mainly been motivated by the important roles of wood-inhabiting fungi in ecosystem functioning (e.g. nutrient cycling) and conservation biology (e.g. their sensitivity to forest management). In this paper, I argue that another important, but yet largely unexplored motivation for studying wood-inhabiting fungal communities, is their potential to advance fundamental community ecology. One major advantage of wood-inhabiting fungi as model systems is that they are organized as spatially well-defined metacommunities, thus conforming to the assumptions of…

Metacommunity systemAssembly processFungal communityWood decaying communityHabitat patchSaproxylic communityResource-tracking communityeliöyhteisötsienetlahopuutAssembly rulelahottajasienet4111 Agronomy
researchProduct

The hemagglutinin of Staphylococcus saprophyticus binds to a protein receptor on sheep erythrocytes.

1997

Staphylococcus saprophyticus, an important cause of urinary tract infections, produces two major surface proteins, the S. saprophyticus surface-associated protein (Ssp) and the hemagglutinin, which mediates fibronectin binding and also functions as the major adhesion of the organism. The hemagglutinating and fibronectin binding functions probably reside on different parts of the molecule. To identify a receptor on eukaryotic cells, binding and inhibition studies with acidic and neutral glycosphingolipids, carbohydrates, and proteins of sheep erythrocyte membranes were conducted. S. saprophyticus did not bind to any glycosphingolipid and no inhibition was observed when hemagglutination assay…

Microbiology (medical)HemagglutinationStaphylococcusImmunologyBiologyBacterial AdhesionGlycosphingolipidsMicrobiologyImmunology and AllergyAnimalsHumanschemistry.chemical_classificationStaphylococcus saprophyticusSheepHemagglutinationErythrocyte MembraneMembrane ProteinsGeneral MedicineBlood ProteinsHemagglutininLigand (biochemistry)biology.organism_classificationMolecular WeightBiochemistryMembrane proteinchemistryFibronectin bindingGalactose oxidaseGlycoproteinMedical microbiology and immunology
researchProduct

Expression of Staphylococcus saprophyticus surface properties is modulated by composition of the atmosphere.

1995

Expression of two major surface proteins of Staphylococcus saprophyticus, the haemagglutinin and the Staphylococcus saprophyticus surface-associated protein (Ssp), requires carefully defined culture conditions. The Ssp is produced when bacteria are grown on agar, whereas expression of the haemagglutinin requires growth in broth. We sought to identify the environmental signals that are responsible for this modulation. Varying the pH, the osmolarity of the growth medium or the temperature did not influence expression of the proteins. In contrast, growth in an anaerobic atmosphere increased haemagglutination titres and fibronectin binding (both mediated by the haemagglutinin) but suppressed pr…

Microbiology (medical)food.ingredientStaphylococcusImmunologyBiologyMicrobiologychemistry.chemical_compoundfoodBacterial ProteinsImmunology and AllergyAgarAdhesins Bacterialchemistry.chemical_classificationGrowth mediumStaphylococcus saprophyticusOsmotic concentrationGeneral MedicineHemagglutininbiology.organism_classificationFibronectinsMolecular WeightHemagglutininsFibronectin bindingchemistryBiochemistryGlycoproteinCarrier ProteinsBacteriaBacterial Outer Membrane ProteinsMedical microbiology and immunology
researchProduct

Dematiaceous Hyphomycetes from Quercus suber litter

2011

Microfungi Saprotroph Litter
researchProduct