996 resultados para 80-551


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Vorbesitzer: Leonhardstift Frankfurt am Main

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Offener Brief zugunsten einer armen Kranken in Königstein. Mit zahlreichen Unterschriften und Notizen

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143 Briefe zwschen Leo Löwenthal und Max Horkheimer, Mai - Dezember 1947; 1 Brief von Max Horkheimer an Else Brunswik, 29.08.1947; 6 Briefe zwischen Max Horkheimer und Samuel H. Flowerman; 4 Briefe zwischen Samuel H. Flowerman und Leo Löwenthal; 3 Briefe von Max Horkheimer an Paul Lazarsfeld; 1 Brief von Leo Löwenthal an Frederick Pollock, 08.08.1947; 1 Brief von Harvey J. Locke an Leo Löwenthal, 01.08.1947; 1 Brief von Max Horkheimer an Harvey J. Locke, 01.08.1947; 1 Brief von Max Horkheimer an Paul Massing, 23.07.1947; 7 Briefe zwischen John Slawson und Max Horkheimer; 1 Brief von dem American Jewish Committee an Leo Löwenthal, 01.10.1947;

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Vorbesitzer: Johannes Bartholomaei

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The effect of DNA cytosine methylation on H-ras promoter activity was assessed using a transient expression system employing the plasmid H-rasCAT (NaeI H-ras promoter linked to the chloramphenicol acetyltransferase (CAT) gene). This 551 bp promoter is 80% GC rich, enriched with 168 CpG dinucleotides, and contains six functional GC box elements which represent major DNA methylation target sites. Prokaryotic methyltransferases HhaI (CGm$\sp5$CG) and HpaII (Cm$\sp5$CGG) alone or in combination with a human placental methyltransferase (HP MTase) were used to introduce methyl groups at different CpG sites within the promoter. To test for functional promoter activity, the methylated plasmids were introduced into CV-1 cells and CAT activity assessed 48 h post-transfection. Methylation at specific HhaI and HpaII sites reduced CAT expression by 70%, whereas more extensive methylation at generalized CpG sites with HP MTase inactivated the promoter $>$95%. The inhibition of H-ras promoter activity was not attributable to methylation-induced differences in DNA uptake or stability in the cell, topological form of the plasmid, or methylation effects in nonpromoter regions. We also observed that DNA cytosine methylation of a 360 bp promoter fragment by HP MTase induced a local change in DNA conformation. Using three independent methodologies (nitrocellulose filter binding assays, gel mobility shifts, and Southwestern blots), we determined that this change in promoter conformation affected the interaction of nuclear proteins with cis-regulatory sequences residing in the promoter region. The results provide evidence to suggest that DNA methylation may regulate gene expression by inducing changes in local promoter conformation which in turn alters the interactions between DNA and protein factors required for transcription. The results provide supportive evidence for the hypothesis of Cedar and Riggs, who postulated that DNA methylation may regulate gene expression by altering the binding affinities of proteins for DNA. ^

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Cenozoic planktonic foraminiferal biostratigraphy at DSDP-IPOD Leg 80 sites documents the existence of regionwide stratigraphic gaps in the Paleocene and middle Miocene. Episodes of carbonate dissolution also occurred during the Paleocene at several sites, particularly at Site 549, where destruction of foraminiferal tests may obscure evidence of an unconformity. The middle Miocene hiatus is apparent at each site where Neogene sediments were continuously cored. Upper Miocene sediments at Site 550 (the only abyssal site) are characterized by moderate to extensive dissolution of planktonic foraminifers, but they contain abundant specimens of Bolboforma that mark this stratigraphic interval (von Daniels and Spiegler, 1974, doi:10.1007/BF02986990; Roegl, 1976, doi:10.2973/dsdp.proc.35.133.1976; Murray, 1979, doi:10.2973/dsdp.proc.48.116.1979; Müller et al., 1985, doi:10.2973/dsdp.proc.80.117.1985). Although foraminiferal evidence is not conclusive, nannofossils indicate a widespread Oligocene unconformity (Müller, 1985). Several oceanographic factors, not just simple sea-level change, probably interacted to produce these regional unconformities. There are also dramatic differences in the Cenozoic sedimentary record among Leg 80 sites, indicating that each has had a distinct geologic history. The thickness of the Cenozoic section varies from 100 m at Site 551 to 471 m at Site 548. The thickness of individual chronostratigraphic units also varies, as do the number and stratigraphic position of unconformities other than those mentioned. Differences in the stratigraphic record from site to site across the continental slope result from (1) location in separate half-graben structures, (2) varying location across the developing margin, and (3) difference in position relative to the seaward edge of the enclosing half-graben. Except for turbidites, deposition at Site 550 (abyssal) was largely independent of developments on the continental slope; but it was affected by oceanographic events widespread in the North Atlantic.

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En Argentina, el liberalismo y el conservadorismo, constituyen el trasfondo ideológico del sistema político de la generación de 1880. A partir de 1880 se consolidan las instituciones políticas y se definen los rasgos centrales de la sociedad argentina, la que sufrirá profundas transformaciones al influjo del crecimiento económico, demográfico y de las políticas de educación pública. La empresa política es protagonizada por los hombres del "80", quienes constituyen la primera "generación argentina" que concreta ese nuevo espíritu que surge en el "53": coexistencia de amplias libertades civiles y económicas junto a una estructura con rasgos centralizadores, con claro predominio del órgano ejecutivo como reaseguro contra las tendencias anárquicas.

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Three lower Barremian to middle/upper Cenomanian samples from DSDP Hole 549 and three lower Cenomanian to lower Maestrichtian samples from DSDP Hole 550B were investigated by organic geochemical and organic petrographic methods. The samples came from wells drilled in the area of the Goban Spur in the northeastern Atlantic; they represent gray to greenish gray carbonaceous mud or siltstones from the deeper parts of the Cretaceous sequences penetrated and light-colored chalks from the shallower ones. The total amount of organic carbon is below 1% in all samples; it is especially low in the Cenomanian to Maestrichtian chalks. Terrigenous organic matter predominates; only the Barremian sample shows a moderate number of marine phytoclasts. As indicated by several parameters, the maturity of the organic matter is low, corresponding to about 0.4% vitrinite reflectance.

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La finalidad de este trabajo prospectivo es determinar la eficacia del método KTPláser (Kalium-Titanyl-Phosphat) de 80 Watt para la vaporización y eliminación del adenoma prostático. Se analizan también los resultados que se obtienen al combinar el método KTP-láser de 80 watt con la RTUP de baja presión hidráulica. Para ello 225 pacientes con HBP sintomática fueron tratados entre Agosto del 2004 y Mayo del 2006 con el KTP-Láser o combinado con RUTP a baja presión. La resección adicional fue efectuada en aquellos pacientes con adenomas grandes o por tener el lóbulo medio acentuado. El efecto ablativo fue controlado al final de la operación por medio de TRUS (sonografía prostática transrectal). 225 pacientes tratados en 2 grupos, el grupo 1 (n:50) aquéllos con sólo tratamiento láser, sobre todo pequeños adenomas y el grupo 2 (n:175) con tratamiento combinado de KTP-láser y RTUP a baja presión en adenomas grandes. La flujometría máxima demuestra una mejoría del 44,5% en el grupo 1 entre antes y después del tratamiento, en el grupo 2 la diferecia es de 122,4%. Nuestro estudio pone de manifiesto, las ventajas de combinar ambos procedimientos quirúrgicos para obtener un mejor resultado en la ablación del adenoma prostático sobre todo en próstatas de gran tamaño.

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Fil: Castellan, Ángel.

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Fil: Pró, Diego F..

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Site 549 recovered a Lower Cretaceous succession which has been shown to include parts of the Barremian and Albian stages. Forty-four species of Ostracoda are illustrated and their stratigraphic distribution used to recognise three major facies units. An high diversity inner shelf facies earlier in the Barremian gives way to a low diversity, outer shelf facies, higher in the succession. The early Albian appears to indicate a return to an inner shelf fauna. The faunas recovered have been compared to similar faunas elsewhere in N. W. Europe.