997 resultados para 164-996C
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Fractionation of the noble gases should occur during formation of a Structure I gas hydrate from water and CH4 such that CH4 hydrate is greatly enriched in Xenon. Noble gas concentrations and fractionation factors (F[4He], F[22Ne], F[86Kr], and F[132Xe] as well as R/Ra) were determined for eight gas hydrate specimens collected on Leg 164 to evaluate this theoretical possibility and to assess whether sufficient quantities of Xe are hosted in oceanic CH4 hydrate to account for Xe "missing" from the atmosphere. The simplest explanation for our results is that samples contain mixtures of air and two end-member gases. One of the end-member gases is depleted in Ne, but significantly enriched in Kr and Xe, as anticipated if the source of this gas involves fractionation during Structure I gas hydrate formation. However, although oceanic CH4 hydrate may be greatly enriched in Xe, simple mass balance calculations indicate that oceanic CH4 hydrate probably represents only a minor reservoir of terrestrial Xe. Noble gas analyses may play an important role in understanding the dynamics of gas hydrate reservoirs, but significantly more work is needed than presented here.
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Site 996 is located above the Blake Diapir where numerous indications of vertical fluid migration and the presence of hydrate existed prior to Ocean Drilling Program (ODP) Leg 164. Direct sampling of hydrates and visual observations of hydrate-filled veins that could be traced 30-40 cm along cores suggest a connection between fluid migration and hydrate formation. The composition of pore water squeezed from sediment cores showed large variations due to melting of hydrate during core recovery and influence of saline water from the evaporitic diapir below. Analysis of water released during hydrate decomposition experiments showed that the recovered hydrates contained significant amounts of pore water. Solutions of the transport equations for deuterium (d2H) and chloride (Cl-) were used to determine maximum (d2H) and minimum (Cl-) in situ concentrations of these species. Minimum in situ concentrations of hydrate were estimated by combining these results with Cl- and d2H values measured on hydrate meltwaters and pore waters obtained by squeezing of sediments, by the means of a method based on analysis of distances in the two-dimensional Cl- d2H space. The computed Cl- and d2H distribution indicates that the minimum hydrate amount solutions are representative of the actual hydrate amount. The highest and mean hydrate concentrations estimates from our model are 31% and 10% of the pore space, respectively. These concentrations agree well with visual core observations, supporting the validity of the model assumptions. The minimum in situ Cl- concentrations were used to constrain the rates of upward fluid migration. Simulation of all available data gave a mean flow rate of 0.35 m/k.y. (range: 0.125-0.5 m/k.y.).
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Estrogen is known to stimulate the proliferation and basement membrane invasiveness of the MCF-7 human breast cancer cell line. We have compared the new steroidal antiestrogen ICI 164,384, the triphenylethylene 4-hydroxytamoxifen (OHT), and the benzothiophene LY 117018, for their effects on the proliferation and invasiveness of the MCF-7 cell line and its antiestrogen-resistant variant LY-2. While all three antiestrogens blocked the proliferative effects of 17β-estradiol on MCF-7 cells, OHT and LY 117018, but not ICI 164,384 stimulated their proliferation in the absence of estrogen. The proliferative effects of OHT and LY 117018 were blocked by ICI 164,384. Basement membrane invasiveness of MCF-7 cells was stimulated by 17β-estradiol and OHT, but not LY 117018 or ICI 164,384. Both ICI 164,384 and Ly 117018 were able to block the invasiveness induced by either 17β-estradiol or OHT. The LY-2 antiestrogen-resistant variant of the MCF-7 cell line showed increased basal proliferation, and responded only slightly to estrogen. ICI 164,384, but not OHT or LY 117018 antagonized the effects of 17β-estradiol, but did not reduce proliferation below control levels. The LY-2 line was not resistant to the antiestrogenic effects of LY 117018 or ICI 164,384 on invasiveness, and was stimulated by LY 117018 for this parameter. Thus, ICI 164,384 is a pure antiestrogen for MCF-7 cell proliferation and invasiveness, and may offer clinical advantage over nonsteroidal antiestrogens which can stimulate these activities in tumor models in vitro.
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Contenido: Dios en la filosofía (cont.) / Octavio N. Derisi -- El acto constitutivo del conocimiento y de la cognoscibilidad o verdad / Octavio N. Derisi -- Presupuestos necesarios para una recta formulación del concepto de ciencia práctica / Federico Mihura Seeber -- Filosofía tomista, educación y teología en Fray Alberto García Vieyra O.P. 1912-1985 / Alberto Caturelli -- Notas y comentarios -- Bibliografía
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O Senador Afonso Arinos (PFL-RJ), Presidente da Comissão de Sistematização da Assembleia Nacinal Constituinte (ANC), debate diversos assuntos polêmicos com o Presidente da ANC, Deputado Ulysses Guimarães (PMDB-SP) e lideranças partidárias. Ele é favorável ao adiamento da decisão dos temas polêmicos, para evitar um número exagerado de artigos na nova Constituição. O ator José Dumond pede a população que ocupe seu espaço na discussão da Constituinte. O Deputado Eduardo Moreira (PMDB-SC) defende emenda do Deputado Eduardo Jorge (PT-SP) que beneficia aposentados. No Plenário, o Senador Francisco Rollemberg (PMDB-SE) pede a transferência, para o Estado de Sergipe, de uma grande área pertencente ao Estado da Bahia. O Deputado João Machado Rollemberg (PFL-SE) apoia essa ideia, porque a região não está sendo assistida pelo Estado da Bahia. O Deputado Gil César (PMDB-MG) almeja a negociação da dívida externa, para que o Brasil continue tendo acesso aos capitais externos.
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Representatives from the family of Lemnaceae (duckweed) make ideal experimental material for research into a succession of phytophysiological processes with regard to growth rate and vegetative reproduction. They are also easy to maintain in sterile cultures. Lemnaceae belong to the higher flowering plants (flowers are rarely produced), however they are distinguished by a much simplified morphological and anatomical structure. As water plants they possess the advantage, that they can be cultivated in synthetic media under laboratory conditions controlled by the application of both a known light intensity and temperature. This paper describes experimental research of growth of Lemnaceae in different conditions. Some of the variables were mineral media, illumination and aeration.
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When flow returns to a temporary stream a certain number of plant and animal species establish themselves more or less rapidly on the stream-bed constituting the initial phase of evolution of the re-population. This phase is essentially characterised by the ”awakening” of animal species that passed the dry season in a dormant state and by the development of the first unicellular algae that constitute the periphyton. Then they are succeeded by more or less stable animal groups and the structural complexity increases. The authors of the present study aim to analyse the dynamics of community succession from the return of water to the biotope until its drying up. It is attempted to determine the influence of the duration of flow on this evolution. This work is based on the analysis of population diversity with reference to its two complementary aspects, species richness and equitability. The River Destel which was studied for this project is situated in the Gorge of Ollioules near the town of Toulon.
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Coccolithoviruses infect the marine coccolithophorid microalga Emiliania huxleyi. Here, we describe the genomes of four new coccolithoviruses isolated from UK coastal locations. Of particular interest, EhV-18 and EhV-145 encode serine palmitoyltransferase function via two distinct genes, whereas all other coccolithoviruses have SPT as a gene fusion of LCB1/LCB2 domains.
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With a relativistic Hartree-Fock-Slater calculation we determined the most stable configurations of the elements of the possibly quasistable island around Z = 164. It is found that the expected noble gas at Z = 168 should not occur, but instead the element Z = 164 should have the properties of a noble gas.