The installation sermon of the very Rev. Dr. Joseph Herman Hertz : Chief rabbi of the United Hebrew Congregations of the British Empire ; Monday, April 14th, 5673-1913 ; at the Great Synagogue London

Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

Members of "The Samoan Expeditionary Force" who made the supreme sacrifice in the Great War, 1914-1918

[by Stephen John Smith, late 5th (Wellington) Regiment, secretary Samoa administration in military occupation, 1915-1918]

A retrospective cohort study of the duration of hepatitis B vaccine immunity and associated factors in pediatric dialysis patients

Dialysis patients are at high risk for hepatitis B infection, which is a serious but preventable disease. Prevention strategies include the administration of the hepatitis B vaccine. Dialysis patients have been noted to have a poor immune response to the vaccine and lose immunity more rapidly. The long term immunogenicity of the hepatitis B vaccine has not been well defined in pediatric dialysis patients especially if administered during infancy as a routine childhood immunization.^ Purpose. The aim of this study was to determine the median duration of hepatitis B immunity and to study the effect of vaccination timing and other cofactors on the duration of hepatitis B immunity in pediatric dialysis patients.^ Methods. Duration of hepatitis B immunity was determined by Kaplan-Meier survival analysis. Comparison of stratified survival analysis was performed using log-rank analysis. Multivariate analysis by Cox regression was used to estimate hazard ratios for the effect of timing of vaccine administration and other covariates on the duration of hepatitis B immunity.^ Results. 193 patients (163 incident patients) had complete data available for analysis. Mean age was 11.2±5.8 years and mean ESRD duration was 59.3±97.8 months. Kaplan-Meier analysis showed that the total median overall duration of immunity (since the time of the primary vaccine series) was 112.7 months (95% CI: 96.6, 124.4), whereas the median overall duration of immunity for incident patients was 106.3 months (95% CI: 93.93, 124.44). Incident patients had a median dialysis duration of hepatitis B immunity equal to 37.1 months (95% CI: 24.16, 72.26). Multivariate adjusted analysis showed that there was a significant difference between patients based on the timing of hepatitis B vaccination administration (p<0.001). Patients immunized after the start of dialysis had a hazard ratio of 6.13 (2.87, 13.08) for loss of hepatitis B immunity compared to patients immunized as infants (p<0.001).^ Conclusion. This study confirms that patients immunized after dialysis onset have an overall shorter duration of hepatitis B immunity as measured by hepatitis B antibody titers and after the start of dialysis, protective antibody titer levels in pediatric dialysis patients wane rapidly compared to healthy children.^

The antiapoptotic effect of overexpression c -erBb2 in breast cancer

Overexpression of the receptor tyrosine kinase p185ErbB2 confers taxol resistance in breast cancers and activation of p34Cdc2 is required for taxol-induced apoptosis and cytotoxicity. Here, we investigated the underlying mechanisms and found that overexpression of p185 ErbB2 inhibits taxol-induced apoptosis through two branches to inhibit activation of p34Cdc2. ^ Overexpression of p185ErbB2 in MDA-MB-435 cells by transfection transcriptionally upregulated p21Cip1, which associates with p34Cdc2, inhibits taxol-mediated p34Cdc2 activation, delays cell entrance to G2/M phase, and thereby inhibits taxol-induced apoptosis. In p21Cip1 antisense-transfected MDA-MB-435 cells or in p21−/− MEF cells, p185ErbB2 was unable to inhibit taxol-induced apoptosis. Therefore, p21Cip1 participates in the regulation of a G2/M checkpoint that contributes to resistance to taxol-induced apoptosis in p185ErbB2-overexpressing breast cancer cells. ^ Direct phosphorylation on Tyrosine-15 of p34Cdc2 by p185 ErbB2 receptor tyrosine kinase inhibits p34Cdc2 activation. The wild-type p185ErbB2 but not the kinase-defective mutant, when overexpressed in breast cancer cells, can phosphorylate p34Cdc2 on tyrosine (Tyr)15, an inhibitory phosphorylation site of p34 Cdc2. The kinase domain of the ErbB2 receptor was sufficient for binding to p34Cdc2 and directly phosphorylating the recombinant Cdc2. Phosphospecific Cdc2-Tyr15 immunoblot analyses, immunocomplex kinase assays, and phospho-amino acid analyses revealed that p185ErbB2 specifically phosphorylates Cdc2 on Tyr15. Phosphorylation of Cdc2-Tyr15 by ErbB2 is modulated during cell cycle and corresponded with delayed cell entry into G2/M phase. The kinase-defective p185ErbB2, which incapable of phosphorylating Cdc2-Tyr15, failed to inhibit taxol-induced activation and apoptosis, whereas the wild-type and the constitutive-active p185ErbB2 did. Increased Cdc2-Tyr15 phosphorylation was found in Erb132-overexpressing tumors from breast cancer patients. Thus, direct phosphorylation of Cdc2-Tyr15 by p185 ErbB2 RTK in breast cancer cells inhibits taxol-induced p34 Cdc2 activation and apoptosis, thereby conferring taxol resistance. ^

Appendix A. Whole-rock major, trace and rare earth element analyses of the Ulubey volcanics, Appendix B. Analytical standards and detection limits for analyses

Collisional and post-collisional volcanic rocks in the Ulubey (Ordu) area at the western edge of the Eastern Pontide Tertiary Volcanic Province (EPTVP) in NE Turkey are divided into four suites; Middle Eocene (49.4-44.6 Ma) aged Andesite-Trachyandesite (AT), Trachyandesite-Trachydacite-Rhyolite (TTR), Trachydacite-Dacite (TD) suites, and Middle Miocene (15.1 Ma) aged Trachybasalt (TB) suite. Local stratigraphy in the Ulubey area starts with shallow marine environment sediments of the Paleocene-Eocene time and then continues extensively with sub-aerial andesitic to rhyolitic and rare basaltic volcanism during Eocene and Miocene time, respectively. Petrographically, the volcanic rocks are composed primarily of andesites/trachyandesites, with minor trachydacites/rhyolites, basalts/trachybasalts and pyroclastics, and show porphyric, hyalo-microlitic porphyric and rarely glomeroporphyric, intersertal, intergranular, fluidal and sieve textures. The Ulubey (Ordu) volcanic rocks indicate magma evolution from tholeiitic-alkaline to calc-alkaline with medium-K contents. Primitive mantle normalized trace element and chondrite normalized rare earth element (REE) patterns show that the volcanic rocks have moderate light rare earth element (LREE)/heavy rare earth element (HREE) ratios relative to E-Type MORB and depletion in Nb, Ta and Ti. High Th/Yb ratios indicate parental magma(s) derived from an enriched source formed by mixing of slab and asthenospheric melts previously modified by fluids and sediments from a subduction zone. All of the volcanic rocks share similar incompatible element ratios (e.g., La/Sm, Zr/Nb, La/Nb) and chondrite-normalized REE patterns, indicating that the basic to acidic rocks originated from the same source. The volcanic rocks were produced by the slab dehydration-induced melting of an existing metasomatized mantle source, and the fluids from the slab dehydration introduced significant large ion lithophile element (LILE) and LREE to the source, masking its inherent HFSE-enriched characteristics. The initial 87Sr/86Sr (0.7044-0.7050) and eNd (-0.3 to +3.4) ratios of the volcanics suggest that they originated from an enriched lithospheric mantle source with low Sm/Nd ratios. Integration of the geochemical, petrological and isotopical with regional and local geological data suggest that the Tertiary volcanic rocks from the Ulubey (Ordu) area were derived from an enriched mantle, which had been previously metasomatized by fluids derived from subducted slab during Eocene to Miocene in collisional and post-collisional extension-related geodynamic setting following Late Mesozoic continental collision between the Eurasian plate and the Tauride-Anatolide platform.

Irven M. Resnick (Ed.), A companion to Albert the Great. Theology, Philosophy and the sciences, Leiden- Boston, Brill, 2013, ISBN 978-90-04-23407-9, 833 págs.

Fil: Costarelli Brandi, Hugo Emilio. Universidad Nacional de Cuyo

Stable oxygen isotope record of Globigerinoides ruber of ODP Site 133-820 off the Great Barriere Reef

Oxygen-isotope ratio measurements are presented for the planktonic species Globigerinoides ruber collected from shallow-water, upper-slope sediments from Holes 820A and 820B in 280 m of water, on the seaward edge of the Great Barrier Reef. Correlation of the Site 820 isotope curve with deep-sea reference curves of the Pacific Ocean (Core V28-238, Hole 677A, Hole 607A) permits the definition of isotope stages 1 to 19 in the top 145 m of Holes 820A and 820B. However, paleontological data indicate that stages 4 and 7 might be missing and that two hiatuses occur at a depth of 8.05 to 12.1 and 34.55 to 35.8 mbsf. Using deep-sea Hole 677A as a reference for ice-volume variations, we determine the difference in isotopic signature between it and Site 820. We propose that this difference is a regional signal representing a progressive 4°C increase in surface-water temperature at Site 820. The proposed temperature change was initiated at about 400 k.y. and corresponds to a change from high-to-low frequency variations in Pleistocene isotope signals. We postulate that these changes may have catalyzed the growth of the Great Barrier Reef. The shift also coincides with changes in seismic character and some physical and chemical sediment characteristics.