Search results for "Schist"

showing 10 items of 171 documents

Systemic schistosomiasis and large bowel perforation: An unexpected surgical urgency. Report of a case and literature review

2019

Key Clinical Message In the presence of suggestive clinical picture (high eosinophil count and multiple CT scan granuloma‐like lesions), schistosomiasis should be taken into account in case of suspected bowel perforation even if common risk factors are not identified through anamnesis.

Anamnesismedicine.medical_specialtyHigh eosinophil countmedicine.diagnostic_testbusiness.industryCase ReportSchistosomiasisComputed tomographyCase ReportsGeneral MedicineBowel perforation030204 cardiovascular system & hematologymedicine.disease03 medical and health sciences0302 clinical medicineEmergency surgery030220 oncology & carcinogenesiscolonic perforationMedicineRadiologyemergency surgerysystemic schistosomiasisbusinessClinical Case Reports
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Major palaeohydrographic changes in Alpine foreland during the Pliocene - Pleistocene

2008

International audience; The changing palaeogeographical pattern of Alpine deposits across the European forelands can be traced by identifying mineral assemblages and establishing the chronology of Pliocene-Pleistocene deposits in Alpine foreland. In the late Miocene, the upper courses of the Rhine and the Aar flowed east from the Swiss molasse plain towards the Danube. In the early Pliocene (Brunssumian, 5-3.2 Ma), these same rivers headed north-wards towards the Rhine Graben of Alsace. In the early Reuverian, these streams were captured south of the Rhine Graben by the Doubs. They ceased their northward flow and headed west to feed the Bresse Graben. This phase is dated to the Lower and Mi…

Archeologygeographygeography.geographical_feature_category[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory010504 meteorology & atmospheric sciencesPleistoceneSchistGeologyMassifLate Miocene010502 geochemistry & geophysics01 natural sciencesMolasseGrabenPaleontology13. Climate actionForeland basinEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesChronologyBoreas
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Four Remarkable Additions to the Biodiversity of Chinese Mosses

2022

Four species of moss genus Schistidium are reported for the first time from China. All of them have been found in the Xinjiang Uyghur Autonomous Region. Ecological and distributional details of the newly recorded species are provided and their local distribution is mapped. Photographs of the species are attached. Checklist of Schistidium species and identifying key are added. Considering the present records, Schistidium consists of 15 species in China.

AsiaEcologychecklist; identifying keyphytogeographydistribution mapsbryophytes; ChinaXinjiang Uyghur Autonomous RegionMusciPlant ScienceSchistidiumAsia; bryophytes; China; distribution maps; Musci; phytogeography; <i>Schistidium</i>; Xinjiang Uyghur Autonomous Region; checklist; identifying keyEcology Evolution Behavior and SystematicsPlants
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Schistosomes in the north: a unique finding from a prosobranch snail using molecular tools.

2009

article i nfo Samples of schistosome cercariae from three different snail species (Lymnaea stagnalis, Radix auricularia and Valvata (Tropidina) macrostoma) collected from lakes in Central Finland were analyzed using molecular techniques. Based on sequences of ITS region of rDNA, the parasite isolates from L. stagnalis and R. auricularia belong to Trichobilharzia szidati and T. franki, respectively. This confirms a wide distribution of these two species in Europe. On the other hand, the isolates from V. macrostoma represent a unique finding — they belong to yet unknown schistosome species falling into the bird schistosome clade. Therefore, identification of natural final hosts and morphologi…

AuriculariabiologyEcologyMolecular Sequence DataSnailsZoologyLymnaea stagnalisSnailSequence Analysis DNADNA Helminthbiology.organism_classificationInfectious Diseasesbiology.animalSchistosomatidaeDNA Ribosomal SpacerRadix auriculariaValvataParasite hostingHelminthsAnimalsParasitologyCladePhylogenyLymnaeaParasitology international
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Ubendian basement and its late Mesoproterozoic and early Neoproterozoic structural and metamorphic overprint in northeastern Zambia

2004

The Palaeoproterozoic basement in the Muyombe and Luwumbu River areas of northeastern Zambia comprises a WNW‐ESE (to E‐W) trending cordierite‐garnet‐sillimanite granulite unit with numerous enderbite bodies and an amphibolite-facies migmatite unit. Zircons from a biotite metatonalite intruding the granulites were dated at 1960.7±0.4 Ma, and this is time-equivalent with the Nyika granite in adjacent Malawi. Mesoproterozoic intrusions into this basement are represented by a nepheline syenite at Mivula Hill (zircon age: 1360.1±0.8 Ma) and the porphyritic Ntendele biotite metagranite (zircon age: 1329.1±0.6 Ma). The Ntendele granite attains plutonic dimensions north of Muyombe. The Mesoproteroz…

Basement (geology)geology.rock_typeSchistGeochemistryMetamorphismGeologyNepheline syeniteGranuliteMigmatiteGeologyEarth-Surface ProcessesGneissZirconJournal of African Earth Sciences
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The Extracellular Vesicles of the Helminth Pathogen, Fasciola hepatica : Biogenesis Pathways and Cargo Molecules Involved in Parasite Pathogenesis

2015

Extracellular vesicles (EVs) released by parasites have important roles in establishing and maintaining infection. Analysis of the soluble and vesicular secretions of adult Fasciola hepatica has established a definitive characterisation of the total secretome of this zoonotic parasite. Fasciola secretes at least two sub-populations of EVs that differ according to size, cargo molecules and site of release from the parasite. The larger EVs are released from the specialised cells that line the parasite gastrodermus and contain the zymogen of the 37 kDa cathepsin L peptidase that performs a digestive function. The smaller exosome-like vesicle population originate from multivesicular bodies with…

Biochemistry & Molecular BiologyBIOCHEMICAL-CHARACTERIZATIONHelminth proteinHOST FIBRINOLYTIC SYSTEMPopulationSTATISTICAL-MODELBINDING PROTEINBiochemistryExosomeAnalytical ChemistryproteomicsLIVER FLUKEFasciola hepaticaParasite hostingAnimalsexosomeeducationMolecular BiologyhelminthTRICHOMONAS-VAGINALISSyncytiumeducation.field_of_studyFasciolabiologyResearchGene Expression ProfilingGene Expression Regulation DevelopmentalHelminth ProteinsIN-VITROFasciola hepaticaExtracellular vesiclesbiology.organism_classificationCell biologysecretomeCATHEPSIN L1transcriptomeLEUCINE AMINOPEPTIDASEBiogenesisSCHISTOSOMA-MANSONIMolecular &amp; Cellular Proteomics
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Considerazioni su un caso di schistosomiasi urinaria.

2005

Urinary tract schistosomiasis is a parasitic disease caused by S. haematobium with a wide range of clinical manifestations related to the mucosal and submucosal granulomatous lesions of the bladder. It affects about 80 million people in Africa, Middle-East and India, while in Italy it is rarely seen among immigrants from endemic areas and returning travellers. The authors describe a case occurred in a 26 year old man, recently emigrated from a rural area of Ghana. He had the symptoms of a haemorrhagic cystitis. Cystoscopy and biopsy showed granulomatous lesions of bladder with calcified eggs. Microscopic examination of urine was positive for Schistosoma haematobium eggs. The therapy with Pr…

Bladder cancer Schistosomiasis Travelling disease
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Emergence of blueschists on Earth linked to secular changes in oceanic crust composition

2015

The oldest blueschists—metamorphic rocks formed during subduction—are of Neoproterozoic age1, and 0.7–0.8 billion years old. Yet, subduction of oceanic crust to mantle depths is thought to have occurred since the Hadean, over 4 billion years ago2. Blueschists typically form under cold geothermal gradients of less than 400 °C GPa−1, so their absence in the ancient rock record is typically attributed to hotter pre-Neoproterozoic mantle prohibiting such low-temperature metamorphism; however, modern analogues of Archaean subduction suggest that blueschist-facies metamorphic conditions are attainable at the slab surface3. Here we show that the absence of blueschists in the ancient geological rec…

Blueschist010504 meteorology & atmospheric sciencesSubductionContinental crustMetamorphic rockEarth science010502 geochemistry & geophysicsGeologic record01 natural sciencesOceanic crustAdakiteGeneral Earth and Planetary SciencesEarth (classical element)Geology0105 earth and related environmental sciences
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Early exhumation of high-pressure rocks in extrusion wedges: Cycladic blueschist unit in the eastern Aegean, Greece, and Turkey

2007

Structural, metamorphic, and geochronologic work shows that the Ampelos/Dilek nappe of the Cycladic blueschist unit in the eastern Aegean constitutes a wedge of high-pressure rocks extruded during early stages of orogeny. The extrusion wedge formed during the incipient collision of the Anatolian microcontinent with Eurasia when subduction and deep underthrusting ceased and the Ampelos/Dilek nappe was thrust southward over the greenschist-facies Menderes nappes along its lower tectonic contact, the Cycladic-Menderes thrust, effectively cutting out a ∼30- to 40-km-thick section of crust. The upper contact of the Ampelos/Dilek extrusion wedge is the top-to-the-NE Selcuk normal shear zone, alon…

Blueschist010504 meteorology & atmospheric sciencesSubductionMetamorphic rockCrustOrogeny010502 geochemistry & geophysics01 natural sciencesNappeGeophysicsGeochemistry and PetrologyShear zonePetrologySeismologyGeology0105 earth and related environmental sciencesMyloniteTectonics
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Timing of deformational events in the Río San Juan complex: implications for the tectonic controls on the exhumation of high-P rocks in the northern …

2013

An integrated structural, petrological and geochronological study was undertaken to constrain the tectonic history and controls on the exhumation of the high-P rocks of the Río San Juan complex in the northern Caribbean subduction–accretionary wedge. In the main structural units of the complex, microtextural analyses were performed to identify the fabrics formed at peak ofmetamorphismin eclogite-facies conditions and during the main retrogressive event toward the low-P amphibolite or blueschist/greenschist-facies conditions. U–Pb SHRIMP dating on zircon rims (71.3 ± 0.7 Ma) coupled with 40Ar–39Ar analyses on phengite (~70– 69 Ma) in felsic sills placed temporal constraints on the exhumation…

BlueschistAccretionary wedgeSubductionAccretionary complexGeochemistryMetamorphismGeologyHigh-pressure metamorphismSubductionAnatexisU–Pb and 40Ar/39Ar geochronologyGeochemistry and PetrologyCaribbean plateClosure temperatureGeologyZirconTerrane
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