Fragm. lat. II 94 - Bibelkommentar (Is 38,13 - 17; 47,1 - 48,11; 50,1 - 51,13; 57,8 - 58,5)

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

Fragm. lat. II 57 - Sermones de tempore (Dom. I et II adv.)

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

A INFLUÊNCIA DAS MULHERES CLÂNICAS NO PENSAMENTO PROFÉTICO DO PÓS-EXÍLIO. UM ESTUDO DE ISAÍAS 57,1-21.

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.

Medical School Donor Recognition Reception Photo 57

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

(Table 1) Concentrations and isotopic ratios of sulfur and carbon in acid conglomerates from DSDP Hole 57-439

The sulfur content of one rhyolite and four dacite conglomerates was found to be low - from 9 to 97 ppm - similar to that of Quaternary andesites and basalts of the Japanese Islands. However, the d34S values of these samples are unexpectedly high - +23 to +35 per mill - relative to troilite from the Canon Diablo meteorite. The sulfide/sulfate ratios vary among the five samples from 0 to 13. No significant isotope fractionation seems to exist between sulfate and sulfide sulfurs. Carbon in these samples is predominantly in the form of carbonate (and probably CO2). It ranges in concentration from 128 to 721 ppm and in d13C from -2.5 to -20.7 per mill relative to PDB.

Mineralogy and geochemistry of volcanic ash at Japan Trench from DSDP Legs 87 and 57

Volcanogenic sediments were obtained from Site 584, located on the midslope of the Japan Trench. Occurrences of volcanic ash in the diatomaceous mudstones increase within sediments dated 6-3 Ma. The frequency pattern and the sediment accumulation rate obtained at Site 584 are similar to those of Site 440 and to those of Sites 438 and 439, located on the upper slope basin. Explosive volcanism increased during the Pliocene and late Miocene in relation to the intrusion of Tertiary granites and uplift of the Tohoku Arc (northeastern Japan Arc). Hygromagmaphile element concentration shows that the glass does not belong to a unique series, and a comparison with Nankai Trough data distinguishes at least two different evolutionary lines.

Hs. Rothschild 8° 57 - 35 Briefe der Freiin Louise von Rothschild und ihrer Tochter Hannah Louise von Rothschild an den Buchhändler Moritz Abendroth aus den Jahren 1875 - 1889

Vorbesitzer: Moritz Abendroth; Fräulein Abendroth; Freiherrlich Carl von Rothschild'sche öffentliche Bibliothek; alte Signatur: Hs. in Oktav 57; Hs in 8° 57

Iron Transformation Pathways and Redox Micro-Environments in Seafloor Sulfide-Mineral Deposits: Spatially Resolved Fe XAS and delta Fe-57/54 Observations

Hydrothermal sulfide chimneys located along the global system of oceanic spreading centers are habitats for microbial life during active venting. Hydrothermally extinct, or inactive, sulfide deposits also host microbial communities at globally distributed sites. The main goal of this study is to describe Fe transformation pathways, through precipitation and oxidation-reduction (redox) reactions, and examine transformation products for signatures of biological activity using Fe mineralogy and stable isotope approaches. The study includes active and inactive sulfides from the East Pacific Rise 9 degrees 50'N vent field. First, the mineralogy of Fe(III)-bearing precipitates is investigated using microprobe X-ray absorption spectroscopy (RXAS) and X-ray diffraction (mu XRD). Second, laser-ablation (LA) and micro-drilling (MD) are used to obtain spatially-resolved Fe stable isotope analysis by multicollector-inductively coupled plasma-mass spectrometry (MC-ICP-MS). Eight Fe -bearing minerals representing three mineralogical classes are present in the samples: oxyhydroxides, secondary phyllosilicates, and sulfides. For Fe oxyhydroxides within chimney walls and layers of Si-rich material, enrichments in both heavy and light Fe isotopes relative to pyrite are observed, yielding a range of delta Fe-57 values up to 6 parts per thousand. Overall, several pathways for Fe transformation are observed. Pathway 1 is characterized by precipitation of primary sulfide minerals from Fe(II)aq-rich fluids in zones of mixing between vent fluids and seawater. Pathway 2 is also consistent with zones of mixing but involves precipitation of sulfide minerals from Fe(II)aq generated by Fe(III) reduction. Pathway 3 is direct oxidation of Fe(II) aq from hydrothermal fluids to form Fe(III) precipitates. Finally, Pathway 4 involves oxidative alteration of pre-existing sulfide minerals to form Fe(III). The Fe mineralogy and isotope data do not support or refute a unique biological role in sulfide alteration. The findings reveal a dynamic range of Fe transformation pathways consistent with a continuum of micro-environments having variable redox conditions. These micro-environments likely support redox cycling of Fe and S and are consistent with culture-dependent and -independent assessments of microbial physiology and genetic diversity of hydrothermal sulfide deposits.