Search results for "E7"

showing 10 items of 152 documents

The unique fossil assemblage from the Lode Quarry (Upper Devonian, Latvia)

2001

The unique fossil fauna from the Lode clay quarry, lower Frasnian, Latvia, includes a diverse ichthyofauna of at least 15 taxa of agnathans and gnathostomes, representing most of the major taxa of Devonian vertebrates. Six new fish taxa (five species and one genus) were discovered during the last ten years. Exceptionally well-preserved juvenile fishes (<i>Asterolepis ornata, Lodeacanthus gaujicus</i>) provide unique data on ontogenetic change. Diverse arthropods are recorded. Parasitic platyhelminth remains in juvenile fish bodies is their first discovery in the fossil record, and represents the oldest parasitic association ever found. A complete faunal and floral list for the L…

LodeEcologyAssemblage (archaeology)PaleontologyQE701-760GeologyDevonianFossil Record
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Clinicopathological and immunohistochemical analysis of 20 cases of Merkel cell carcinoma in search of prognostic markers.

2005

Aims:  To evaluate the clinicopathological and immunohistochemical characteristics of Merkel cell carcinoma (MCC) in an attempt to find new, potentially significant, prognostic markers. Methods and results:  Clinical data and follow-up, histopathological features (pattern, cell size, thickness, mitoses, vascular invasion, lymphocytic infiltration) and immunohistochemical detection [CK20, thyroid transcription factor (TTF-1), chromogranin A, synaptophysin, p53, Ki67, Fli-1, CD99, c-Kit] were evaluated in 20 cases of MCC. Fli-1 and CD99 were detected in 90% and 55% of cases, respectively. Tumour size > 30 mm, stage II, ‘absent’ lymphocytic infiltration, and the presence of > 50% of Ki67+ tumo…

MalePathologyThyroid Nuclear Factor 1Keratin-20Intermediate Filament ProteinsLymph nodeAged 80 and overbiologyMerkel cell carcinomaChromogranin ANuclear ProteinsGeneral MedicineMiddle AgedPrognosisImmunohistochemistryDNA-Binding ProteinsProto-Oncogene Proteins c-kitmedicine.anatomical_structureFemaleMerkel cellmedicine.medical_specialtyHistologyCD99Synaptophysin12E7 AntigenPathology and Forensic MedicineAntigens CDProto-Oncogene ProteinsCarcinomamedicineBiomarkers TumorChromograninsHumansSurvival analysisAgedNeoplasm StagingProto-Oncogene Protein c-fli-1Keratin 20medicine.diseaseSurvival AnalysisCarcinoma Merkel CellMicroscopy ElectronKi-67 AntigenMultivariate Analysisbiology.proteinTrans-ActivatorsChromogranin ANeoplasm Recurrence LocalTumor Suppressor Protein p53Cell Adhesion MoleculesFollow-Up StudiesTranscription FactorsHistopathology
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Inhibin-α, CD99, HEA125, PLAP, and chromogranin immunoreactivity in testicular neoplasms and the androgen insensitivity syndrome

2000

We investigated 115 testicular and 3 epididymal tumors and 6 cases of the complete androgen insensitivity syndrome (AIS) for the expression of inhibin-alpha, CD99, HEA125, PLAP, and chromogranin, using monoclonal antibodies and standard immunhistochemical techniques. Ihibin-alpha was detected in the neoplastic cells in 27 of 27 primary Leydig cell tumors (LCTs), 1 of 1 metastatic LCT, 6 of 20 Sertoli cell tumors (SCTs), 4 of 5 juvenile granulosa cell tumors (GCTs), and 2 of 5 unclassified sex cord-stromal tumors (USCSTs). Except for 2 choriocarcinomas, the choriocarcinomatous component of 1 mixed germ cell tumor, and a small focus of inhibin-positive syncytiotrophoblast in 1 embryonal carci…

Maleendocrine systemmedicine.medical_specialtyPathologyendocrine system diseasesCD9912E7 AntigenBiologyPathology and Forensic MedicineEmbryonal carcinomaTesticular NeoplasmsAntigens CDAntigens NeoplasmRete testisInternal medicineBiomarkers TumorChromograninsmedicineHumansInhibinsRhabdomyosarcomaGranulosa Cell TumorEpididymisLeydig cellProteinsChromogranin AAndrogen-Insensitivity Syndromemedicine.diseaseSertoli cellNeoplasm Proteinsmedicine.anatomical_structureEndocrinologyFluorescent Antibody Technique DirectAntigens Surfacebiology.proteinGerm cell tumorsPeptidesCell Adhesion MoleculesHuman Pathology
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Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)

2017

[EN]: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identified in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. And Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of …

MammalsMamíferosDuero basinDorcatheriumgeography.geographical_feature_categorybiologySteppePaleontologyDuero BasinYacimientos de Cuesta del ReyBiostratigraphyStructural basinMioceno mediobiology.organism_classificationQE701-760ArchaeologyUpper AragonianCuestaMiddle MioceneAragoniense superiorGeographymammals middle miocene upper aragonian duero basin cuesta del rey sitesCuesta del Rey sitesMammalCuenca del DueroSpanish Journal of Palaeontology
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Milnor-Witt Motives

2020

We develop the theory of Milnor-Witt motives and motivic cohomology. Compared to Voevodsky's theory of motives and his motivic cohomology, the first difference appears in our definition of Milnor-Witt finite correspondences, where our cycles come equipped with quadratic forms. This yields a weaker notion of transfers and a derived category of motives that is closer to the stable homotopy theory of schemes. We prove a cancellation theorem when tensoring with the Tate object, we compare the diagonal part of our Milnor-Witt motivic cohomology to Minor-Witt K-theory and we provide spectra representing various versions of motivic cohomology in the $\mathbb{A}^1$-derived category or the stable ho…

Mathematics - Algebraic GeometryMathematics::K-Theory and HomologyMathematics::Category Theory11E70 13D15 14F42 19E15 19G38 (Primary) 11E81 14A99 14C35 19D45 (Secondary)FOS: Mathematics[MATH.MATH-AG] Mathematics [math]/Algebraic Geometry [math.AG][MATH.MATH-AG]Mathematics [math]/Algebraic Geometry [math.AG]Algebraic Geometry (math.AG)Mathematics::Algebraic Topology
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Systematic and biostratigraphy of the genera Parasolenopleura, Badulesia, and Pardailhania in the Iberian Chains: a useful zonation for the Miaolingi…

2020

The trilobite species of three genera included in the Family Solenopleuridae: Parasolenopleura , Badulesia , and Pardailhania are revised. These genera have a great biostratigraphic interest due to their broad distribution in the Miaolingian Series (former middle Cambrian) of the Mediterranean Subprovince and because they constitute an evolutionary lineage, that facilitates an accurate regional correlation. Two of these genera ( Pardailhania and Badulesia ) have been used to define middle Cambrian zones in Spain (lower and middle Caesaraugustan, equivalent to the uppermost Wuliuan and the lower Drumian stages). Although, all authors have been using the same species to establish the Mediterr…

Mediterranean climateSeries (stratigraphy)biologyEstratigrafiaLineage (evolution)PaleontologyPaleontologiaBiostratigraphybiology.organism_classificationQE701-760TrilobitePaleontologyGeographytrilobites systematic biostratigraphy wuliuan-drumian (miaolingian) mediterranean region.Solenopleuridae
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Zonation by ammonites and foraminifers of the Vraconnian-Turonian interval: A comparison of the Boreal and Tethyan domains (NW Europe / Central Tunis…

2008

International audience; Since the end of the 19th century the interval comprising the uppermost Upper Albian, the Cenomamian, the Turonian and the basal Coniacian has been subdivided, first into ammonite zones, then, beginning in the middle of the 20th century, into zones of planktonic foraminifera. These two groups, one macrofossil, the other microfossil, are particularly effective for bio-chronostratigraphy thanks to their rapid rates of evolution. But differences in the faunal makeup between the Boreal domain (northwestern Europe) and the Tethyan domain (Mediterranean) have for a long time hindered precise correlation of the two domains. Today, in a time interval covering about 16 millio…

Mediterranean climateStratigraphyzones[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDE.MCG.CPE] Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeCretaceousForaminiferaPaleontologyzonationlcsh:Stratigraphy[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCenomanianTethyslcsh:QE701-760lcsh:QE640-699Ammoniteammonitesbiologylcsh:QE1-996.5PaleontologyMacrofossilGeologyVraconnianAlbianTuronianbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageCretaceouslcsh:GeologyBoreallcsh:Paleontologylanguage[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyforaminifersCenomanianGeologyCarnets de Géologie
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Middle Miocene foraminifera from Canals (Valencia, western Mediterranean). Biostratigraphic and palaeoenvironmental aspects

2020

The age and the palaeoenvironmental conditions of the tap marls outcroppings near the locality of Canals in the south of the Valencia Province (E Spain) are discussed. Based on the planktonic foraminifera assemblages, mainly the species Globorotalia praemenardii , these tap marls are dated as Serravallian in age (middle Miocene). The analysis of the foraminiferal assemblages suggests a relatively well-ventilated uppermiddle bathyal environment, with only a moderate oxygen deficiency throughout most of the studied section. The rather cool waters indicated by the planktonic foraminifera (e.g. Globigerina bulloides ) are compatible with the decreasing temperatures trend during the middle Mioce…

Mediterranean climatebiologyPaleontologyGlobigerina bulloidesbiology.organism_classificationQE701-760Bathyal zoneForaminiferaOceanographyforaminifera middle miocene biostratigraphy palaeoenvironment valencia spain.Benthic zoneMarlUpwellingGeologyRadiolariaSpanish Journal of Palaeontology
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Benthic foraminifera and environmental changes in the Quaternary of the western Mediterranean coast: the core of Xeraco, Valencia, Spain

2020

The evolution of the benthic foraminiferal assemblages from a 60 m core drilled in the Quaternary lagoon of Xeraco (Valencia, Spain) is studied. Two moments of warm climate, high sea-level and maximal marine influence in the lagoon have been identified. The first one at the base of the core, punctuated by highly frequent changes during the Upper Pleistocene, and the other one in the upper end of the series during the Holocene. The presence of a middle core section with low diversity and a nearly total absence of marine foraminifers is interpreted as a regressive interval of cold climate conditions linked to a glacial stage.

Mediterranean climatebiologyPleistocenePaleontologybiology.organism_classificationforaminifera quaternary palaeoenvironments xeraco valenciaQE701-760ForaminiferaPaleontologyOceanographyBenthic zoneStage (stratigraphy)Glacial periodQuaternaryGeologyHoloceneSpanish Journal of Palaeontology
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Pseudolillia Maubeuge, 1949 (Ammonitida, Hildoceratidae) in the Lower Jurassic (Toarcian) of the NE Spain

2017

In the present paper, 147 specimens assigned to the genus Pseudolillia Maubeuge, 1949 are studied. This is a considerably high number of samples in comparison with those known in other geographical areas where they have been cited, such as northern France, the Pyrenees, the Betic Range, Morocco, Portugal, Italy, Hungary and Bulgaria. The six taxa described, P. murvillensis, P. hispanica, P. emiliana, P. donovani, Pseudolillia ? n. sp. (en García-Gómez & Rivas, 1980), and Pseudolillia ? sp., come from 22 sites in the Cantabrian and Iberian Ranges and the Isle of Majorca. Their presence in expanded sections enabled us to situate the stratigraphic position of the genus between the upper part o…

Mediterranean climatebiologyRange (biology)Paleontologyupper toarcian grammoceratinae taxonomy palaeobiogeography iberian peninsulabiology.organism_classificationArchaeologyQE701-760PaleontologíaAmmonitidaPaleontologyGeographyTaxonAbundance (ecology)GenusHildoceratidaeChronozone
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