1,742,408 research outputs found
The use of οἰκονομία for missions in Ephesians
Get PDFThe concern which prompted the letter and the author�s digression in Ephesians 3:2�12 represents a lacuna in Ephesians scholarship. Its function within the wider discourse remains uncertain. The term οἰκονομία is prominent in the discourse and has been interpreted as an administrative office or activity in the Pauline corpus. This article shows that the term has a missional nuance in Ephesians. It is used for the role of Christ in the execution of the plan of God (Eph 1:10) and the role of Paul in the implementation of the plan (Eph 3:2). The author of Ephesians acknowledges the role Paul played in the mission�s movement of the gospel itself, �I Paul the prisoner of Jesus Christ� (Eph 3:1, 7). He is identified as the person to whom �the stewardship of the grace of God has been given� (Eph 3:2). The οἰκονομία of the gospel is committed by Paul to the church, marking a new phase in the development of the mission of the church.Intradisciplinary and/or interdisciplinary implications: The article suggests that in Ephesians 3:10, which is a crux interpretum, that the missional nuance of the term οἰκονομία indicates in Ephesians 3:10 the role of the Church in the execution of the plan of God and the missio Dei is implied.Keywords: oikonomia; missions; Ephesians</p
Οικογένειες παιδιών με μαθησιακές και ψυχοκοινωνικές δυσκολίες και προαγωγή της κουλτούρας ένταξης στο σχολικό πλαίσιο: ανασταλτικοί παράγοντες και παράγοντες ώθησης Families of children with learning and psychosocial difficulties and school inclusion: Risk and promoting...
No full textΘεωρητικό Μέρος
Οικογένειες παιδιών με μαθησιακές και ψυχοκοινωνικές δυσκολίες και προαγωγή της κουλτούρας ένταξης στο σχολικό πλαίσιο: ανασταλτικοί παράγοντες και παράγοντες ώθησης
H. E. Κουρκούτας & R. Caldin (Italy)
Theoretical Issues
Families of children with learning and psychosocial difficulties and school inclusion: Risk and promoting factors
E. Kourkoutas & R. Caldin (Italy
Toward 959 nematode genomes
No full textThe sequencing of the complete genome of the nematode Caenorhabditis elegans was a landmark achievement and ushered in a new era of whole-organism, systems analyses of the biology of this powerful model organism. The success of the C. elegans genome sequencing project also inspired communities working on other organisms to approach genome sequencing of their species. The phylum Nematoda is rich and diverse and of interest to a wide range of research fields from basic biology through ecology and parasitic disease. For all these communities, it is now clear that access to genome scale data will be key to advancing understanding, and in the case of parasites, developing new ways to control or cure diseases. The advent of second-generation sequencing technologies, improvements in computing algorithms and infrastructure and growth in bioinformatics and genomics literacy is making the addition of genome sequencing to the research goals of any nematode research program a less daunting prospect. To inspire, promote and coordinate genomic sequencing across the diversity of the phylum, we have launched a community wiki and the 959 Nematode Genomes initiative (www.nematodegenomes.org/). Just as the deciphering of the developmental lineage of the 959 cells of the adult hermaphrodite C. elegans was the gateway to broad advances in biomedical science, we hope that a nematode phylogeny with (at least) 959 sequenced species will underpin further advances in understanding the origins of parasitism, the dynamics of genomic change and the adaptations that have made Nematoda one of the most successful animal phyla
Os isotope record of ODP Site 159-959
No full textThe known temporal relationship between the benthic foraminiferal d18O record and the marine Os isotope record is used to reinterpret the absolute chronology and paleoceanographic context of an episode of organic carbon burial on the West African margin Ocean Drilling Program (ODP) Site 959. Although organic-rich sediments require significant corrections for in situ decay of 187Re to 187Os, these results demonstrate the utility of the marine Os isotope record for chemostratigraphic correlation of organic-rich sediments that are devoid of age diagnostic microfossils with pelagic carbonate sequences. Revision of the ODP Site 959 chronology shifts the age assignment of an interval of biosiliceous, organic-rich sediment deposition from the Oligocene to the late Eocene and earliest Oligocene, likely culminating with the first major glaciation of the Oligocene (Oi1). We speculate that enhanced organic carbon burial over much of the West African margin may have contributed to drawdown of atmospheric carbon dioxide before and during the Oi1 event and suggest that Os isotope chemostratigraphy provides a valuable tool for further exploring this possibility
Dispelling the Myths Behind First-author Citation Counts
Get PDFWe conducted a full-scale evaluative citation analysis study of scholars in the XML research field to explore just how different from each other author rankings resulting from different citation counting methods actually are, and to demonstrate the capability of emerging data and tools on the Web in supporting more realistic citation counting methods. Our results contest some common arguments for the continued
use of first-author citation counts in the evaluation of scholars, such as high correlations between author rankings by first-author citation counts and other citation
counting methods, and high costs of using more realistic citation counting methods that are not well-supported by the ISI databases. It is argued that increasingly available digital full text research papers make it possible for citation analysis studies to go beyond what the ISI databases have directly supported and to employ more
sophisticated methods
Gilbert Family Home, 959 Penniman Avenue, Plymouth Mich.
No full textPrint made from negative of the home of local author, Helen Gilbert, 959 Penniman Avenue, taken October 1962
Osmium-isotope geochemistry of ODP Site 159-959
No full textAnalyses of Re, Os, and Ir concentrations, as well as Os-isotopic compositions, are reported for a suite of sediments from Ocean Drilling Program Site 959. These samples vary in age from late Neogene to Late Cretaceous, and represent a range in depositional oxidation-reduction conditions from suboxic in the Neogene to anoxic in the Late Cretaceous. Age assignments based on shipboard biostratigraphic data are used to calculate initial 187Os/186Os ratios of Neogene nannofossil/foraminifer oozes and Eocene to upper Oligocene laminated diatomites. These calculated initial ratios are in general agreement with published data constraining the Os-isotopic evolution of seawater through time, indicating that the Os-isotopic composition of these sediments is controlled largely by the Os isotopic composition of contemporaneous seawater. Results from analyses of Upper Cretaceous to lower Paleocene claystones do not exhibit elevated Ir concentrations and exhibit Re-Os systematics that are highly consistent with closed-system production of 187Os by in situ 187Re decay. Scatter in both the Cretaceous and Cenozoic data sets is likely the result of the influence of nonhydrogenous Os, carried by clastics, on the bulk sediment Os-isotopic composition, or post-depositional mobility of Re and/or Os
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