945 resultados para 57-441


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Trägerband: Inc. qu. 862; 'Polem. 295' oder 'Ref. Luther 796'; Vorbesitzer: Dominikanerkloster Frankfurt am Main

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Trägerband: Inc. oct. 511; Vorbesitzer: Dominikanerkloster Frankfurt am Main

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Neste trabalho sobre A Influência das Mulheres Clânicas no Pensamento Profético do Pós-Exílio. Um Estudo de Isaías 57,1-21, propomos apresentar uma pesquisa para demonstrar fundamentalmente quem eram os três grupos de mulheres clânicas, que surgem no Isaías 57,3-9, a saber: hn+n>[o(agoureira),aEßnm. (adultério, significando adúltera - tp,a(nm.) e hnAz(prostituta). E daí desenvolver que influência tiveram na profecia, no período do pós-exílio. Para tal tarefa utilizamos dois métodos: o primeiro, um método diacrônico no qual o texto demonstrou uma visão muito negativa dessas mulheres, já que o pano de fundo onde estaria estabelecido o texto é de forte influência patriarcal. Mas, ao aplicarmos um segundo, o método sincrônico e intertextual, o resultado se mostrou diferente, pois o conjunto de textos onde está incluso, a saber: Isaías 56,1-12; 58,1-14 e 61,1-11, demonstram um programa inclusivo. Assim, no Isaías 56,3-4 - rkªNEh;-!B, (filho do estrangeiro) e syrIêSh; (os eunucos), são admitidos na comunidade; no Isaías 58, 1 bqoß[]y: tybeîl.W (e para casa de Jacó), essa casa representada por um grupo de homens é repreendida por causa do jejum; e no Isaías 61,5-6 ~yrIêz (estranhos) e rkênE ynEåb.W (e filhos de estrangeiro), serão os que alimentarão a comunidade. Devido a isto, surgiu uma hipótese de que uma visão negativa sobre elas não poderia ser aceita dentro de um projeto inclusivo. No entanto a questão deve ser respondida. Partirmos para fazer um mapeamento do modo de vida clânico no Gênesis, um conjunto de textos que fala principalmente da família/clã. Ao estudarmos algumas mães míticas: Eva, Sara, Agar, filhas de Ló e Tamar, e ao compará-las com as de Isaías 57,3-9, muitas das características se mostram semelhantes. Pudemos assim perceber que todas essas mulheres clânicas por possuírem conhecimentos do reino animal e vegetal, exerceram influência na vida e morte das famílias/clãs, assim elas tiveram que serem combatidas pelos grupos de homens ao longo do tempo. Ainda outra característica importante no Pós-Exílio, é a movimentação que as famìlias/clãs realizam, mas, essa ‗saìda é sempre carregada de abundância de fertilidade e resolução de conflito pela solidariedade. Devemos estar na profecia, já que ao cristalizar-se um texto ‗desfavorável contra um grupo de mulheres, na verdade se está denunciando uma violência contra elas.

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1 The L6 myocyte cell line expresses high affinity receptors for calcitonin gene-related peptide (CGRP) which are coupled to activation of adenylyl cyclase. The biochemical pharmacology of these receptors has been examined by radioligand binding or adenosine 3':5'-cyclic monophosphate (cyclic AMP) accumulation. 2 In intact cells at 37 degrees C, human and rat alpha- and beta-CGRP all activated adenylyl cyclase with EC50s of about 1.5 nM. A number of CGRP analogues containing up to five amino acid substitutions showed similar potencies. In membrane binding studies at 22 degrees C in 1 mM Mg2+, the above all bound to a single site with IC50s of 0.1-0.4 nM. 3 The fragment CGRP(8-37) acted as a competitive antagonist of CGRP stimulation of adenylyl cyclase with a calculated Kd of 5 nM. The Kd determined in membrane binding assays was lower (0.5 nM). 4 The N-terminal extended human alpha-CGRP analogue Tyro-CGRP activated adenylyl cyclase and inhibited [125I]-iodohistidyl-CGRP binding less potently than human alpha-CGRP (EC50 for cyclase = 12 nM, IC50 for binding = 4 nM). 5 The pharmacological profile of the L6 CGRP receptor suggests that it most closely resembles sites on skeletal muscle, cardiac myocytes and hepatocytes. The L6 cell line should be a stable homogeneous model system in which to study CGRP mechanisms and pharmacology."

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http://digitalcommons.fiu.edu/com_images/1062/thumbnail.jpg

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Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

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The exponential growth of studies on the biological response to ocean acidification over the last few decades has generated a large amount of data. To facilitate data comparison, a data compilation hosted at the data publisher PANGAEA was initiated in 2008 and is updated on a regular basis (doi:10.1594/PANGAEA.149999). By January 2015, a total of 581 data sets (over 4 000 000 data points) from 539 papers had been archived. Here we present the developments of this data compilation five years since its first description by Nisumaa et al. (2010). Most of study sites from which data archived are still in the Northern Hemisphere and the number of archived data from studies from the Southern Hemisphere and polar oceans are still relatively low. Data from 60 studies that investigated the response of a mix of organisms or natural communities were all added after 2010, indicating a welcomed shift from the study of individual organisms to communities and ecosystems. The initial imbalance of considerably more data archived on calcification and primary production than on other processes has improved. There is also a clear tendency towards more data archived from multifactorial studies after 2010. For easier and more effective access to ocean acidification data, the ocean acidification community is strongly encouraged to contribute to the data archiving effort, and help develop standard vocabularies describing the variables and define best practices for archiving ocean acidification data.