ACE research vignette 039: The Ineffectiveness of Enterprise Policy : Is Policy Formulation to Blame?

This series of research vignettes is aimed at sharing current and interesting research findings from our team of international Entrepreneurship researchers. This vignette, written by Dr Norin Arshed, Professor Sara Carter and Professor Colin Mason examines whether the ineffectiveness of enterprise policy can be attributed to the formulation of the enterprise policy itself.

Teología, 1982, Tomo XIX nº 039 (número completo)

Matrimonio indisoluble en un mundo inestable: incertidumbres y certezas. Análisis de algunas opiniones vertidas en el planteo actual del problema de la pastoral de divorciados / Juan Carlos Meinville -- Apuntes bíblicos sobre la templanza / José María Arancibia -- “El hijo pródigo”: un auto-sacramental cuzqueño del siglo XVII / Francisco Jorge Veissmann -- Los seminarios y la formación de los eclesiásticos en el período de la confederación 1852-1861 / Néstor Tomás Auza -- Pedro y Pablo. Dos publicaciones recientes. Comentario bibliográfico / Jorge Mejía -- Notas bibliográficas -- Libros recibidos

Diário da Constituinte [gravação de vídeo] : [programa n. 039]

Relatores vão ao PRODASEN usar computadores com banco de dados da Constituição. José Jorge (PFL-PE), relator da Subcomissão do Poder Legislativo da Assembleia Nacional Constituinte (ANC), fala sobre a conclusão dos relatórios. Mário Lima (PMDB-BA), relator da Subcomissão dos Diretos dos Trabalhadores e Servidores Públicos, fala dos direitos de greve dos trabalhadores, estabilidade de emprego e jornada de trabalho. Ricardo Fiuza (PFL-PR) mostra um quadro organizacional que associa propostas semelhantes. Plínio Arruda (PT-SP) comenta sobre os direitos e deveres na nova Constituição. Siqueira Campos (PDC-GO), relator da Subcomissão dos Estados, fala da redivisão territorial do Brasil e do fortalecimento da federação com equilíbrio entre os Estados. Apresentado parecer na Subcomissão dos Negros, Populações Indígenas, Pessoas Deficientes e Minorias que trata das garantias das minorias. Benedita da Silva (PT-RJ) afirma que discriminação é crime, pede isonomia aos negros e povos indígenas. José Fogaça(PMDB-RS), relator da Subcomissão do Poder Executivo, diz que a Subcomissão entrou em consenso quanto a eleição direta e a existência do primeiro-ministro.

Resolución No. 039: Por la cual se acepta un desistimiento de un recurso de reposición

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Planktonic and benthic stables Isotopes, age model and carbon analysis of HUD91/039 from the northernmost Baffin Bay

A multiproxy study of palaeoceanographic and climatic changes in northernmost Baffin Bay shows that major environmental changes have occurred since the deglaciation of the area at about 12 500 cal. yr BP. The interpretation is based on sedimentology, benthic and planktonic foraminifera and their isotopic composition, as well as diatom assemblages in the sedimentary records at two core sites, one located in the deeper central part of northernmost Baffin Bay and one in a separate trough closer to the Greenland coast. A revised chronology for the two records is established on the basis of 15 previously published AMS 14C age determinations. A basal diamicton is overlain by laminated, fossil-free sediments. Our data from the early part of the fossiliferous record (12 300 - 11 300 cal. yr BP), which is also initially laminated, indicate extensive seasonal sea-ice cover and brine release. There is indication of a cooling event between 11 300 and 10 900 cal. yr BP, and maximum Atlantic Water influence occurred between 10 900 and 8200 cal. yr BP (no sediment recovery between 8200 and 7300 cal. yr BP). A gradual, but fluctuating, increase in sea-ice cover is seen after 7300 cal. yr BP. Sea-ice diatoms were particularly abundant in the central part of northernmost Baffin Bay, presumably due to the inflow of Polar waters from the Arctic Ocean, and less sea ice occurred at the near-coastal site, which was under continuous influence of the West Greenland Current. Our data from the deep, central part show a fluctuating degree of upwelling after c. 7300 cal. yr BP, culminating between 4000 and 3050 cal. yr BP. There was a gradual increase in the influence of cold bottom waters from the Arctic Ocean after about 3050 cal. yr BP, when agglutinated foraminifera became abundant. A superimposed short-term change in the sea-surface proxies is correlated with the Little Ice Age cooling.