Search results for "Crust"

showing 10 items of 599 documents

Morphological determination of the phototrophic community composition of biological soil crusts in coastal sand dunes in northern Germany

2022

This dataset comprises the microbial community composition of biological soil crusts in north-German sand dunes. For this we obtained enrichment cultures of phototrophic microorganisms, by placing fragments of biocrusts of the same Petri dishes as used for sequencing, in Petri dishes with Bold Basal (1N BBM) agarized medium (Bischoff and Bold 1963). Cultures were grown under standard laboratory conditions: with a 12-hour alteration of light and dark phases and irradiation of 25 μmol photons m-2 s-1 at a temperature 20 ± 5 ºС. Microscopic study of these raw cultures began in the third week of cultivation. Morphological examinations were performed using Olympus BX53 light microscope with Noma…

Nostoc cf linckiaNodosilinea cf. epilithicaTetracystis cf. sarcinalisCylindrocystis cf crassaPtychostomum moravicumElliptochloris subsphaericaThin layer chromatographyAsterococcus spCylindrocystis cf. crassaCladonia phyllophoraChloroidium cf ellipsoideumChlorolobion sp.Hypnum cupressiforme var lacunosumHypogymnia physodesStichococcus cf. bacillarisEremochloris spCrustsParmelia sulcataStenomitos sp.algaeBracteacoccus sp.Chlorococcum spPtychostomum capillarewith Nomarski DIC opticsCladonia chlorophaeaCladonia foliaceaBiospheric SciencesMyrmecia cf irregularisField experimentNodosilinea cf epilithicaBacidina etayanaPolytrichum juniperinumCoccomyxa sp.Placynthiella uliginosaLeptolyngbya spPohlia nutansCladonia furcataPeltigera extenuataWatanabea cf. acidophilaGeosciencesChloroidium cf. ellipsoideumLongitude of eventWatanabea cf acidophilaParietochloris cf. alveolarisPtychostomum imbricatulumSiteLight microscope Olympus Ltd BX53 with Nomarski DIC opticsDicranum scopariumSyntrichia ruraliformisBX53Pseudochlorella spKlebsormidium cf flaccidumOlympus LtdCladonia novochlorophaeaDATE TIMECladonia cocciferaCladonia conistaNostoc cf. linckiaDiplosphaera chodatii16S rRNAOxyrrhynchium praelongumTetracystis cf sarcinalisChlorokybus atmophyticusNostoc sp.Interfilum cf. massjukiaeMicarea misellaCoelastrella spStenomitos spNostoc spEvent labelLecanora hageniiPolytrichum piliferumTetradesmus arenicolaElevation of eventPlanophila spChlorococcum sp.Campylopus introflexusCladonia ramulosaCephaloziella divaricataPseudochlorella sp.Nostoc cf. communeChlorolobion spNannochloris spCladonia rangiformisMacrochloris spNannochloris sp.Cladonia fimbriataEvernia prunastriCaloplaca cerinellaLecania cyrtellaLecanora persimilisCladonia subulataPseudoscleropodium purumStichococcus cf bacillarisLatitude of eventLight microscopeInterfilum terricolaCladonia glaucaCladonia portentosaPlanophila sp.Spongiochloris spCladonia reisediment analysisCladonia gracilisHypnum cupressiformeTolypothrix cf. byssoideaCeratodon purpureusEcologyCladonia uncialis ssp biuncialisPseudomuriella cf. aurantiacaCylindrocystis sp.Klebsormidium cf. subtileRacomitrium canescensMicrocoleus vaginatusCoccomyxa spCylindrocystis spLobochlamys sp.soil ecologyXanthoria parietinaCladonia ciliataHypnum cupressiforme var. lacunosumActinochloris terrestrisInterfilum cf massjukiaeNatural SciencesChlorella vulgarisMacrochloris sp.Coelastrella sp.Bracteacoccus spRacomitrium elongatumCladonia scabriusculaNostoc cf. edaphicumStichococcus allasLocationNostoc cf edaphicumKlebsormidium cf. flaccidumLophozia bicuspidataPseudomuriella cf aurantiacaKlebsormidium crenulatumduneNostoc cf communeLeptolyngbya sp.Ptilidium ciliatumCladonia macilentaMyrmecia cf. irregularisPtychostomum compactumLobochlamys spPleurozium schreberiCladonia arbusculaPhyscia tenellaBrachythecium albicansPeltigera hymeniaAmandinea punctataTimaviella sp.Scoliciosporum galluraeParietochloris cf alveolarisAsterococcus sp.Hennediella heimiiTimaviella spDATE/TIMECladonia humilisBryum capillareTolypothrix cf byssoideaKlebsormidium cf subtileEremochloris sp.Cladonia floerkeanaSpongiochloris sp.Cladonia uncialis ssp. biuncialisHypnum jutlandicum
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The nucleic acid binding protein PcCNBP is transcriptionally regulated during the immune response in red swamp crayfish Procambarus clarkii

2015

Cellular nucleic acid binding proteins (CNBPs) represent a highly conserved protein family among vertebrates; they harbour seven tandem zinc finger repeats CCHC type and have been described as transcriptional and translational regulators. To date, there is little characterization of CNBP in invertebrates since its structure and function have been analysed solely in Drosophila melanogaster. However, no CNBP has been investigated in other arthropod systems. In an effort to isolate immune-related genes in Procambarus clarkii, a partial mRNA coding a zinc finger containing protein was found to be up-regulated during the response to white spot syndrome virus (WSSV) infection. The red swamp crayf…

Nucleic acid binding proteins zinc finger containing proteins cloning gene expression crustaceans.Settore BIO/11 - Biologia Molecolare
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The structure of parasite component communities in brackish water fishes of the northeastern Baltic Sea

2001

We used nestedness analysis to seek non-random patterns in the structure of component communities of metazoan parasites collected from 31 sympatric fish species from the northeastern Bothnian Bay, the most oligohaline area of the Baltic Sea. Only 8 marine parasite species were found among the 63 species recorded, although some marine fish species reproduce in the bay and others occasionally visit the area. Marine parasite species can utilize both freshwater and marine fish species as intermediate or final hosts, and marine fish can harbour freshwater parasite species. This exchange of parasite species between marine and freshwater fish has probably resulted from ecological factors acting ov…

Oceans and SeasGeneralist and specialist speciesHost-Parasite InteractionsFish DiseasesCrustaceaHelminthsLeechesAnimalsParasitesSeawaterMolluscaEcosystembiologyEcologyFishesAquatic animalbiology.organism_classificationInfectious DiseasesMolluscaSympatric speciationFreshwater fishNestednessAnimal Science and ZoologyParasitologySpecies richnessHelminthiasis AnimalBayParasitology
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Gaining deeper insight into aroma perception: An integrative study of the oral processing of breads with different structures

2017

WOS:000394071900015; International audience; The objective of this study was to investigate for the first time the influence of bread structure, volatile compounds, and oral processing on aroma perception. 3 types of French baguette were created using the same raw ingredients but different bread-making processes; they consequently varied in their crumb and crust structures. We characterized the initial volatile profiles of two bread structural subtypes-namely bread crumb and bread crumb with crust-using proton transfer reaction-mass spectrometry (PTR-MS) headspace analysis. Three types of bread were characterized by thirty-nine ion fragments from m/z 45 to 139. We then conducted a study in …

Olfactory perceptionAdultMalecrumb[ SDV.AEN ] Life Sciences [q-bio]/Food and Nutrition[SDV]Life Sciences [q-bio]FlourcrustreleaseGas Chromatography-Mass SpectrometryBolusYoung Adult0404 agricultural biotechnologyHumansFood scienceProgressive profilingAromaFlavorTriticum2. Zero hungerprofileVolatile Organic CompoundssalivaChromatographybreakdownbiologyChemistrydigestive oral and skin physiologySensory analysesfood and beverages04 agricultural and veterinary sciencesBreadreaction-mass-spectrometrybiology.organism_classificationOlfactory Perception040401 food scienceFlavorTasteOdorantsimpactFemaleGas chromatography–mass spectrometryflavor compoundstexture[SDV.AEN]Life Sciences [q-bio]/Food and NutritionProton transfer reaction-mass spectrometry (PTR-MS)Food Science
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Dehydration of melt inclusions in olivine and implications for the origin of silica-undersaturated island-arc melts

2019

Highlights • New experiments with melt inclusions in olivine at 1200 °C and 300 MPa. • Coupled behavior H2O and SiO2 in inclusions during re-hydration and dehydration. • SiO2 mobility results from formation/destruction of metal vacant olivine. • SiO2-undersaturated arc melt inclusions may originate by dehydration. • New method to assess initial H2O in dehydrated inclusions. Abstract Primary subduction-related magmas build up modern continental crust and counterbalance massive recycling of crustal material into the deep mantle occurring at this tectonic setting. Melt inclusions in Mg-rich olivine are believed to be the best probes of primary subduction-related melts. However, unexpectedly, m…

Olivine010504 meteorology & atmospheric sciencesContinental crustCrustengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)law.inventionGeophysics13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologylawEarth and Planetary Sciences (miscellaneous)engineeringIsland arcCrystallization10. No inequalityPetrologyDissolutionGeology0105 earth and related environmental sciencesMelt inclusionsEarth and Planetary Science Letters
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Crystallization of late-stage MORB under varying water activities and redox conditions: Implications for the formation of highly evolved lavas and ox…

2018

Abstract In order to understand late magmatic processes that occur in the deep oceanic crust, we performed a phase-equilibria study in a representative late-stage system at a pressure of 200 MPa with a special focus on the role of water and oxygen fugacity. The starting composition for the experiments was evaluated based on a statistical approach using evolved fresh MORB glasses from the database PETDB highest in FeO and TiO2 (in average 17.92 wt% and 3.73 wt%, respectively), assumed to represent frozen liquids erupted at the seafloor generated by extensive differentiation of MORB. We conducted crystallization experiments in a range of temperatures from 850 to 1050 °C with water activities …

Olivine010504 meteorology & atmospheric sciencesGabbroGeochemistryGeologyLiquidusengineering.material010502 geochemistry & geophysics01 natural sciencesSeafloor spreadingGeochemistry and PetrologyMineral redox bufferOceanic crustengineeringPlagioclaseAmphiboleGeology0105 earth and related environmental sciencesLithos
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Detection of a Ca-rich lithology in the Earth's deep (>300 km) convecting mantle

2005

Earth's deep convecting upper mantle is believed to represent a rather homogenous geochemical reservoir of spinel or garnet lherzolite with primitive major element and moderately depleted trace element composition. Only where subduction occurs is this homogeneity disrupted by a suite of rocks ranging from eclogites/garnet pyroxenites (former oceanic crust) to residual harzburgites. In addition to these well documented peridotitic and metabasaltic rocks we have now discovered the presence of a chemically distinct reservoir in the deep convecting upper mantle. In situ structural analyses (micro X-ray diffraction and micro Raman spectroscopy) and three-dimensional trace element mapping (confoc…

OlivineSubductionTrace elementGeochemistryPyroxeneengineering.materialMantle (geology)GeophysicsSpace and Planetary ScienceGeochemistry and PetrologyLithosphereOceanic crustEarth and Planetary Sciences (miscellaneous)engineeringEclogiteGeologyEarth and Planetary Science Letters
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Ostracods of Mediterranean temporary inland waters (Greece, Southern Italy, and Malta)

2015

Ostracoda Temporary ponds Crustacea
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A survey of ovarian maturation in a population of Aristeus antennatus [Crustacea: Decapoda)

1995

Ovarian maturation Crustacea Decapoda Aristeus antennatus Mediterranean SeaSettore BIO/05 - Zoologia
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African, southern Indian and South American cratons were not part of the Rodinia supercontinent: evidence from field relationships and geochronology

2003

We discuss the question whether the late Mesoproterozoic and early Neoproterozoic rocks of eastern, central and southern Africa, Madagascar, southern India, Sri Lanka and South America have played any role in the formation and dispersal of the supercontinent Rodinia, believed to have existed between about 1000 and 750 Ma ago. First, there is little evidence for the production of significant volumes of ~1.4–1.0 Ga (Kibaran or Grenvillian age) continental crust in the Mozambique belt (MB) of East Africa, except, perhaps, in parts of northern Mozambique. This is also valid for most terranes related to West Gondwana, which are made up of basement rocks older than Mesoproterozoic, reworked in th…

PaleontologyGondwanaGeophysicsContinental collisionContinental crustRodiniaLaurentiaMetamorphismMozambique BeltSupercontinentSeismologyGeologyEarth-Surface ProcessesTectonophysics
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