Fragm. lat. I 54 - Biblia (I Mcc 12,46 - 13,9; 13,25 - 45; 16,19 - 24; Capitulatio ad II Mcc)

Trägerband: 'Praed. 1791'; Vorbesitzer: Dominikanerkloster Frankfurt am Main

Fragm. lat. I 98 - Biblia (Is 43,9 - 21; 43,24 - 44,8; 45,24 - 46,10; 46,13 - 47,9)

Trägerband: Ms. Praed. 133; Vorbesitzer: Dominikanerkloster Frankfurt am Main

Opressão econômica e violência social: retratos do cotidiano em três parábolas da Fonte Q (Q 12,39-40; 42-46; 19,12-27)

Num ambiente como o da Galiléia do século I, onde o ensino era realizado nas comunidades religiosas, vilarejos e núcleos familiares de forma oral, o método de fixação de ensinos mediante a assimilação de símbolos do cotidiano era fundamental. Por conta disso, acreditamos que, dentre as fontes orais ou escritas preservadas e organizadas pelos Evangelhos Sinóticos, as parábolas de Jesus compõem o gênero literário mais original por terem sido preservadas na memória, com maior precisão pelos primeiros seguidores de Jesus. Muitos estudiosos empreenderam importantes trabalhos para pesquisar o lugar social das parábolas de Jesus, a maioria deles partindo dos próprios textos dispostos como estão nos Evangelhos. Neste trabalho, nos propomos trabalhar as parábolas de Jesus como ditos bem preservados pela oralidade a partir da teoria da Fonte Q, que é tratada como um dos estratos mais primitivos da tradição formativa dos Evangelhos Sinóticos e do movimento de Jesus. As parábolas do Ladrão (Q 12,39-40), Servo Infiel (Q 12,42-46) e do Dinheiro Confiado (Q 19,12-27) sempre foram vistas pela tradição eclesial como parábolas que tratam da necessária vigilância do cristão por conta da repentina parusia de Jesus. No entanto, nesse trabalho vamos além, pois acreditamos que essas parábolas tratam do contexto social da Galiléia do século I, onde são retratadas a opressão econômica e a violência social imposta aos pequenos proprietários e camponeses empobrecidos.(AU)

Multinational Performance and the Geography of FDI:evidence from 46 countries

The literature on multinationality and firm performance has generally disregarded the role of geography. However, the location of FDI assumes particular importance in terms of the link between multinationality at the firm level. The purpose of this paper is to consider the multinationality-performance relationship within the context of greater emphasis on the importance of location, but also emphasising the importance of the location decision. This paper draws on firm-level data covering over 16,000 multinationals from 46 countries over the period of 1997-2007 and allows for different effects upon the performance of the multinational firm depending on the level of development of the host economy. In our results, we find a clear positive relation between multinationality and firm performance. However, investment in developing countries is associated with larger effects on performance than in the case of investment in developed countries. We also find that the return to investing in developing countries is U-shaped. This indicates that multinationals are likely to face losses in the early stage of their investment in developing countries before the positive returns are realized. Overall, our results suggest that the net gains for multinationals from greater geographical diversification have not yet been fully explored. Geographical diversification into developing countries may be an important source of competitive advantages that deserves more serious consideration from business leaders and academics alike. © 2013 Springer-Verlag Berlin Heidelberg.

Medical School Donor Recognition Reception Photo 46

http://digitalcommons.fiu.edu/com_images/1051/thumbnail.jpg

Fragm. lat. VI 46 - Tropar

Trägerband: Inc. qu. 526; Vorbesitzer: Hinricus Sticz; Peter Heidenreich; Dominikanerkloster Frankfurt am Main

Data compilation on the biological response to ocean acidification: environmental and experimental context of data sets and related literature

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.

O ciclo Slopiewnie opus 46 bis de Karol Szymanowski: uma abordagem de estudo e performance

This text presents a discussion about the song cycle Slopiewnie Opus 46 bis of Karol Szymanowski, one of the most important Polish composers of the 20th century. Slopiewnie was composed on texts of Julian Tuwim, poet born in 1894 in Łódź, who used ancient roots to create new words and search for special sonorities. First, this text introduces a brief biographical sketch about Szymanowski, in order to contextualize Slopiewnie in relation to the composer’s works. Afterwards, the text provides an analysis of the songs and their texts, which may serve as a study tool for future perfomers. Interpretative suggestions are offered, based on the experience of learning these songs and on references. The text also presents the phonetic transcription of the poems, as well as a suggested translation to Portuguese, making it easier for Brazilian singers to learn the cycle’s text and prosody.

(Appendix B) Benthic foraminifera in Indian Ocean surface sediments

Multivariate analysis was performed on percentages of 46 species of unstained deep-sea benthic foraminifera from 131 core-top to near-core-top samples (322-5013 m) from across the Indian Ocean. Faunal data are combined with GEOSECS geochemical data to investigate any relationship between benthic foraminifera (assemblages and species) and deep-sea properties. In general, benthic foraminifera show a good correlation to surface productivity, organic carbon flux to the sea floor, deep-sea oxygenation and, to a lesser extent, to bottom temperature, without correlation with the water depths. The foraminiferal census data combined with geochemical data has enabled the division of the Indian Ocean into two faunal provinces. Province A occupies the northwestern Indian Ocean (Arabian Sea region) where surface primary production has a major maximum during the summer monsoon season and a secondary maximum during winter monsoon season that leads to high organic flux to the seafloor, making the deep-sea one of the most oxygen-deficient regions in the world ocean, with a pronounced oxygen minimum zone (OMZ). This province is dominated by benthic foraminifera characteristic of low oxygen and high organic food flux including Uvigerina peregrina, Robulus nicobarensis, Bolivinita pseudopunctata, Bolivinita sp., Bulimina aculeata, Bulimina alazanensis, Ehrenbergina carinata and Cassidulina carinata. Province B covers southern, southeastern and eastern parts of the Indian Ocean and is dominated by Nuttallides umbonifera, Epistominella exigua, Globocassidulina subglobosa, Uvigerina proboscidea, Cibicides wuellerstorfi, Cassidulina laevigata, Pullenia bulloides, Pullenia osloensis, Pyrgo murrhina, Oridorsalis umbonatus, Gyroidinoides (= Gyroidina) soldanii and Gyroidinoides cf. gemma suggesting well-oxygenated, cold deep water with low (oligotrophic) and pulsed food supply.

3.46 Ga Apex chert 'microfossils' reinterpreted as mineral artefacts produced during phyllosilicate exfoliation

We acknowledge the facilities, scientific and technical assistance of the Australian Microscopy & Microanalysis Research Facility at: Centre for Microscopy Characterisation and Analysis, The University of Western Australia; Electron Microscopy Unit, The University of New South Wales. These facilities are funded by the Universities, State and Commonwealth Governments. DW was funded by the European Commission and the Australian Research Council (FT140100321). This is ARC CCFS paper number XXX. We acknowledge Martin van Kranendonk, Owen Green, Cris Stoakes, Nicola McLoughlin, the late John Lindsay and the Geological Survey of Western Australia for fieldwork assistance, Thomas Becker for assistance with Raman microspectroscopy, Anthony Burgess from FEI for the preparation of one of the TEM wafers, and Russell Garwood, Tom Davies, Imran Rahman & Stephan Lautenschlager for training and advice on the SPIERS and AVIZO software suites. We thank Chris Fedo and an anonymous reviewer for comments that improved the manuscript.