Search results for "E7"

showing 10 items of 152 documents

Lower Bashkirian fusulinoideans from the upper part of the Tagnana Formation (Carboniferous, NW Algeria)

2021

The upper member of the Tagnana Formation of the Djebel Bechar Group (informally the Tagnana-3 or Tagnana Ill member) yielded fusulinoideans and other related foraminifera of the genera Pseudoendothyra (rare), Pseudostajfella (Semistaffella) (rare), Millerella, Pseudonovel/a, Plectostaffella, Eostaffella and Mediocris. The presence of Eostaffellina (rare) and Endostaffella is doubtful. The difference between Millerella and Eostaffella cannot be adequately defined by evolute versus involute coiling. Pseudonovella Kireeva, 1949 is redefined to include Seminovella Rauzer-Chernousova, 1951. The foraminifera are from two samples, one from close to the top and the other from near the base of the …

ForaminiferaPaleontologybiologyfusulinoideans taxonomy biostratigraphy carboniferous lower bashkirian tagnana formation algeriaCarboniferousGroup (stratigraphy)Paleontologybiology.organism_classificationQE701-760GeologySpanish Journal of Palaeontology
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Book Review. The Pleistocene of Untermassfeld near Meiningen (Thüringen, Germany).

2020

Around one million years ago (late Early Pleistocene), a major faunal turnover occurred in Europe, linked to the onset of increased climatic instability: the transition between Villafranchian and Galerian faunas. Few palaeontological sites in Europe documents this biological event, highlighting over all of them the site of Untermassfeld, near Meiningen (Thuringia, Germany), which provided an amazing fossil record, either in abundance, diversity, and good preservation.Previous results of the interdisciplinary research developed on Untermassfeld were published in three volumes of the monograph series of the Romisch-Germanischen Zentralmuseums, Mainz, released in 1997 and 2001, as well as in a…

Fossil RecordEarly PleistoceneGeographyPleistoceneVillafranchianPaleontologyExcavationArchaeologyQE701-760Spanish Journal of Palaeontology
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El registro fósil de vertebrados y patrimonio paleontológico más representativo de los pirineos occidentales

2019

Los Pirineos occidentales son un territorio con una notable diversidad geológica y un importante registro fósil, que constituye un gran archivo de paleobiodiversidad. En lo que respecta al registro fósil de vertebrados, los Pirineos occidentales (Región Vasco-Cantábrica, Cuenca de Pamplona y sector noroccidental de la Cuenca del Ebro) son relevantes tanto desde el punto de vista de los yacimientos paleontológicos como de las colecciones de fósiles procedentes de ellos. Varios yacimientos de vertebrados forman parte del Inventario de Lugares de Interés Geológico (LIG) con alto o muy alto interés paleontológico en la Comunidad Autónoma del País Vasco. Destacan los yacimientos de peces cretáci…

Fossil RecordPaleontologyStructural basinArchaeologyYACIMIENTOS Y COLECCIONES PALEONTOLÓGICASQE701-760PIRINEOS OCCIDENTALES//purl.org/becyt/ford/1 [https]CRETÁCICO-CENOZOICO//purl.org/becyt/ford/1.5 [https]GeographyGeodiversityVERTEBRADOS FÓSILES[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyComputingMilieux_MISCELLANEOUS
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FE DE ERRATAS / ERRATUM

2021

Please make the following correction in the previous issue. López-Martínez, N., Likius, A., Mackaye, H. T., Vignaud, P. & Brunet, M. 2007. A new Lagomorph from the Late Miocene of Chad (Central Africa). Revista Española de Paleontología, 22 (1), 1-20.

GeographyCentral africaPaleontologyLate MioceneArchaeologyQE701-760Spanish Journal of Palaeontology
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Non-marine invertebrate trace fossils from the Tertiary Calatayud- Teruel Basin, NE Spain. Reply

2021

We thank the comments of Dr Calzada. We think that this kind of discussions is very healthy to the Paleontology and it would be necessary to do it more frequently, so that thanks again for your example. It is true that some of the descriptions of ichnofossils in our work need further discussion and comments, but when we analysed several poorly-preserved specimens (such as the so-called Spongeliomorpha isp.) we preferred to make a quick introduction and describe them in open nomenclature. It was beyond the scope of our paper to make a revision of the ichnogenus with this kind of material, but we hope that Calzada's comments and our reply will improve some ideas concerning the ichnogenus Spon…

GeographyScope (project management)PaleontologyStructural basinTrace fossilArchaeologyOpen nomenclatureQE701-760Spanish Journal of Palaeontology
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Gliridae from the late Oligocene of the province of Teruel (Spain)

2020

The Calatayud-Teruel Basin is one of the richest areas of Spain, when fossil mammals are concerned. Around the village of Montalban many lower Oligocene fossil mammal localities are known and several upper Oligocene localities with rich micromammal faunas are present between the villages of Vivel del Rio Martin and Martin del Rio. Previous papers on these upper Oligocene localities were dedicated to the Cricetidae and to the zapodid  Plesiosminthus , in this work we describe the fauna of Gliridae, composed of the genera  Gliravus , Butseloglis ,  Peridyromys ,  Microdyromys and  Paraglis . Among these the latter genus is very poorly represented.  Microdyromys is of special importance becaus…

GeographybiologyGenusFaunaPaleontologyMammalStructural basinbiology.organism_classificationQE701-760ArchaeologyCricetidaeSpanish Journal of Palaeontology
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Conodont association of the Bashkirian-Moscovian boundary interval of the Donets Basin, Ukraine

2018

Ten sections spanning the Bashkirian-Moscovian boundary interval were studied in the Donets Basin. Six of them contain most representative conodont and foraminifer associations. In this paper we focused on three the most complete sections that include stratigraphically important conodont species, which belong to the Declinognathodus, Idiognathoides, Idiognathodus, Neognathodus, “Streptognathodus”, Mesogondolella and Diplognathodus genera. The majority of those species are widely distributed, which makes the correlation to other areas reliable. Two biotic events in conodont evolution were discovered in these sections. Two conodont lineages established here are considered as potential markers…

Global Boundary Stratotype Section and PointPaleontologybiologyStage (stratigraphy)PaleontologyBoundary (topology)Interval (graph theory)Structural basinConodontbiology.organism_classificationQE701-760GeologySpanish Journal of Palaeontology
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Hypoxia inducible factor-1 alpha expression is increased in infected positive HPV16 DNA oral squamous cell carcinoma and positively associated with H…

2011

Abstract Background There is increasing evidence for the role of High Risk (HR) Human PapillomaVirus (HPV) in the pathogenesis of Oral Squamous Cell Carcinoma (OSCC). The E6 and E7 oncogenes from HR HPVs are responsible for the deregulation of p53 and pRB proteins involved in cell cycle and apoptotic pathways. In cell lines experiments, the HPV E7 protein seems to be able to enhance Hypoxia Inducible Factor-1 alpha (HIF-1α) activity, normally involved in the response to hypoxia and able to enhance angiogenesis. Results We studied tumor specimens from 62 OSCC; a higher prevalence of tumors in TNM stage II and also in pT2 class between OSCC infected positive HPV16 DNA than non-infected ones w…

HPV16Cancer ResearchPathologymedicine.medical_specialtyHPVNecrosisAngiogenesisEpidemiologyAlpha (ethology)BiologyOral Squamous Cell Carcinomalcsh:RC254-282lcsh:Infectious and parasitic diseasesPathogenesisHypoxia-Inducible Factor 1-Alphachemistry.chemical_compoundmedicinelcsh:RC109-216E7Oral Squamous Cell Carcinoma Hif-1α HPV HPV16 E7virus diseasesHypoxia (medical)lcsh:Neoplasms. Tumors. Oncology. Including cancer and carcinogensfemale genital diseases and pregnancy complicationsstomatognathic diseasesInfectious DiseaseschemistryOncologyApoptosisCancer researchmedicine.symptomHif-1αDNAResearch ArticleInfectious agents and cancer
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Immunohistochemical Study as a Tool in Differential Diagnosis of Pediatric Malignant Rhabdoid Tumor

2010

Malignant rhabdoid tumors (MRTs) are aggressive childhood neoplasms, occurring mainly in the kidney and brain. We describe 2 unusual cases of extrarenal and noncranial location (liver and soft tissue with dissemination) mimicking hepatoblastoma, neuroblastoma or Ewing sarcoma. Both cases revealed a polyphenotypic profile, combined with cytokeratin, vimentin, and CD99 expression. INI1/BAF-47 showed negative protein nuclear expression in both cases, suggesting a diagnosis of MRT. An extensive immunohistochemical panel was performed to exclude pediatric tumors reminiscent of MRT. The genetic studies failed to detected MYCN amplification, 11q23 deletion, and EWS break-apart positivity. No alter…

HepatoblastomaPathologymedicine.medical_specialtySkin NeoplasmsHistologyDesmoplastic small-round-cell tumorChromosomal Proteins Non-HistoneCD9912E7 AntigenN-Myc Proto-Oncogene ProteinPathology and Forensic MedicineDiagnosis DifferentialNeoplasms Multiple PrimaryFatal OutcomeAntigens CDNeuroblastomaAntineoplastic Combined Chemotherapy ProtocolsmedicineHumansVimentinRhabdoid TumorChromosome AberrationsOncogene ProteinsN-Myc Proto-Oncogene Proteinbusiness.industryLiver NeoplasmsInfant NewbornInfantNuclear ProteinsWilms' tumorSMARCB1 Proteinmedicine.diseaseImmunohistochemistryDNA-Binding ProteinsMedical Laboratory TechnologyDrug Resistance NeoplasmKeratinsFemaleSarcomaRNA-Binding Protein EWSDifferential diagnosisbusinessCell Adhesion MoleculesTranscription FactorsApplied Immunohistochemistry & Molecular Morphology
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Mapping the geometry of the F(4) group.

2007

In this paper we present a construction of the compact form of the exceptional Lie group F4 by exponentiating the corresponding Lie algebra f4. We realize F4 as the automorphisms group of the exceptional Jordan algebra, whose elements are 3 x 3 hermitian matrices with octonionic entries. We use a parametrization which generalizes the Euler angles for SU(2) and is based on the fibration of F4 via a Spin(9) subgroup as a fiber. This technique allows us to determine an explicit expression for the Haar invariant measure on the F4 group manifold. Apart from shedding light on the structure of F4 and its coset manifold OP2=F4/Spin(9), the octonionic projective plane, these results are a prerequisi…

High Energy Physics - TheoryJordan algebraGroup (mathematics)General MathematicsGeneral Physics and AstronomyLie groupFOS: Physical sciencesGeometryMathematical Physics (math-ph)AutomorphismHigh Energy Physics - Theory (hep-th)22E70Lie algebraCoset22E46Projective planeSpecial unitary groupMathematical PhysicsMathematics22E46; 22E70
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