997 resultados para 205


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veröffentlicht in: Schopenhauer, Arthur : Arthur Schopenhauers sämtliche Werke - München : Piper - Bd. 14 : Der Briefwechsel Arthur Schopenhauers ; 1 (1799 - 1849), Nr. 270

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Frankfurter Latern, Devrient, Paris, Mathilde Heine, Anlage (nicht enthalten): Gedicht aus Heinrich Heines Nachlaß, "Brendelche Schnud", Dr. Heine, Dresden, Nizza

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Vorbesitzer: Michelangelo Gualandi

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p63, a p53 family member, is a transcription factor that has complex roles in cancer. This study focuses on the role of the ∆Np63α isoform in bladder cancer (BC). Epithelial – mesenchymal transition (EMT) is a physiological process that plays an important part in metastasis and drug resistance. At the molecular level, EMT is characterized by the loss of the epithelial marker E-cadherin, and the acquisition of the transcriptional repressors of E-cadherin (ZEB1, ZEB2, TWIST, SNAI1 and SNAI2). Recent publications highlight the role of microRNAs belonging to the miR-200 family and miR-205 in preventing EMT through suppression of ZEB1 and ZEB2. p53, the homologue of p63, is implicated in regulating EMT by modulating the expression of miR-200c; however, the mechanisms underlying miR-205 control remain unclear. Here we show that ∆Np63α regulates the transcription of miR-205 and controls EMT in human BC cells. We observed a strong correlation between the expression of ∆Np63α, miR-205 and E-cadherin in a panel of BC cell lines (n=28) and also in bladder primary tumors from a cohort of patients (n=98). A remarkably inverse correlation is observed between ∆Np63α and ZEB1/2 in cell lines. Stable knockdown (KD) ∆Np63α in UC6, an “epithelial” BC cell line, decreased the expression of miR-205 and induced ZEB1/2 expression, the effects that were reversed by expression of exogenous miR-205. Moreover, overexpressing ∆Np63α in UC3, a “messenchymal” BC cell line, brought about opposite results, an increase in miR-205 expression and a reduction in ZEB1/2 expression. Modulation of ∆Np63α expression resulted in a parallel change in the expression of miR-205 and miR-205 “host” gene (miR-205HG). Nuclear run-on and chromatin immunoprecipitation experiments demonstrated that ∆Np63α regulates the transcription of miR-205 through controlling the recruitment of RNA Polymerase II to the promoter of miR-205HG. Interestingly, high miR-205 expression correlated with poor clinical outcome in BC patients, consistent with our recent publication highlighting the enrichment of ∆Np63 in a lethal subset of muscle invasive BC. In summary, our data present the important roles of ∆Np63α in preventing EMT mediated by miR-205. Our study also identifies miR-205 as a potential molecular marker to predict clinical outcome in BC patients.

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http://lib.dr.iastate.edu/carver_narratives/1030/thumbnail.jpg

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Pore fluid and sediment chemical and isotopic data were obtained for samples from Ocean Drilling Program (ODP) Leg 205 Sites 1253, 1254, and 1255 in the Costa Rica subduction zone. The chemical and isotopic data reported here were generated in our shore-based laboratories to complement shipboard inorganic geochemical data. Li isotopic analyses were carried out by L.-H. Chan at Louisiana State University (USA). The data reported herein include fluoride, bromide, rubidium, cesium, and barium concentrations; Li and Sr isotopic compositions in pore fluids; and Rb, Cs, and Ba concentrations in representative bulk sediments. The data also include new pore fluid fluoride and bromide concentrations from corresponding ODP Leg 170 Sites 1039, 1040, and 1043. O.M. Saether's Site 1039 and 1040 fluoride concentration data are shown for comparison. Basal sediment fluoride concentrations and Li and Sr isotope ratios at both Sites 1253 and 1039 show reversals that approach modern seawater values. Br/Cl ratios are, however, conservative throughout the sediment section at Sites 1039 and 1253. The observed sharp F and Br concentration maxima, Rb and K concentration minima, the most radiogenic 87Sr/86Sr ratios, and highest 7Li values along the décollement and fracture zone (Sites 1040, 1043, 1254, and 1255) strengthen the evidence obtained during Leg 170 that a deeply sourced fluid, originating from fluid-rock reactions at ~150°C and corresponding to between 10 and 15 km depth, is transporting solutes to the ocean.

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We determined the C and N concentrations and isotopic compositions of sediments in the prism sampled during Ocean Drilling Program Legs 170 and 205 offshore Costa Rica, with the goals of evaluating sediment sources and extents of diagenesis and identifying any effects of infiltrating fluids on the sedimentary C and N. The sediments from Leg 170 Site 1040 contain 0.85-1.96 wt% total organic carbon (TOC) with Vienna Peedee belemnite (VPDB) d13CVPDB from -26.3 per mil to -22.5 per mil, and 832-2221 ppm total nitrogen (TN) with d15Nair from +3.5 per mil to +6.6 per mil. Sediment TN concentrations and d15N values show dramatic downhole increases within the uppermost 130 m of the section and more gradual downhole decreases from 130 meters below seafloor (mbsf) to the base of the décollement at ~370 mbsf. Concentrations and isotopic compositions of TOC are relatively uniform within the entire section, showing some minor perturbation within the décollement zone. In the uppermost 100 m, upsection increases in TN concentrations at constant TOC concentrations produce significant increases in atomic TOC/TN ratios from ~8 to ~18. Carbonate (calcite) contents in the wedge sediments are generally low (<4 wt%), but the d13C and Vienna standard mean ocean water (VSMOW) d18OVSMOW values vary significantly from -26.1 per mil to +4.1 per mil and from +30.0 per mil to +35.3 per mil, respectively. Concentrations and isotopic compositions of TOC and TN for sediments from Leg 205 Sites 1254 and 1255 overlap well with C-N data for sediments from the same depth intervals obtained during Leg 170 at Site 1040.

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Fil: Ercoli, César Adrián. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.