998 resultados para B-191


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Contient : 1 « Relation d'Italie et Allemagne du sieur Bergeron » ; 2 ; « Voiage d'Italie et d'Espaigne ès années 1611 et 1612 ». La relation du voyage d'Italie commence par : « L'imperfection de la nature de l'homme est telle que la pluspart... Nous partismes de Paris le mardy 18 d'octobre 1611 et allasmes coucher à Fontainebleau... » et finit par : « ... reservant le reste de nostre voyage de Provence, Languedoc, Espagne, puis de rechef Guienne, etc. à un second traicté que nous esperons Dieu aydant en faire, etc. Fin du voyage d'Italie » ; La relation du voyage en Espagne commence par : « Pour reprendre nostre voyage, que nous avions laissé au fleuve du Var, qui faict aujourd'huy la separation de l'Italie et de la France, estans partis de Nice le 17 febvrier 1612... » et finit par : «... Le mardy 24 avril » 1612, « nous vinmes coucher à Estampes, et le lendemain à Paris, etc. Estampes, ancienne ville de Beausse... fut erigée en duché par le roy François Ier, etc. Fin du voyage »

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Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

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New efforts at biological control of Miconia calvescens (Melastomataceae) is a serious invader in the tropical Pacific, including the Hawaiian and Tahitian Islands, and currently poses a major threat to native biodiversity in the Wet Tropics of Australia. The species is fleshy-fruited, small-seeded and shade tolerant, and thus has the potential to be dispersed widely and recruit in relatively intact rainforest habitats, displacing native species. Understanding and predicting the rate of spread is critical for the design and implementation of effective management actions. We used an individual-based model incorporating a dispersal function derived from dispersal curves for similar berry-fruited native species, and life-history parameters of fecundity and mortality to predict the spatial structure of a Miconia population after a 30 year time period. We compared the modelled population spatial structure to that of an actual infestation in the rainforests of north Queensland. Our goal was to assess how well the model predicts actual dispersion and to identify potential barriers and conduits to seed movement and seedling establishment. The model overpredicts overall population size and the spatial extent of the actual infestation, predicting individuals to occur at a maximum 1,750 m from the source compared with the maximum distance of any detected individual in the actual infestation of 1,191 m. We identify several characteristic features of managed invasive populations that make comparisons between modelled outcomes and actual infestations difficult. Our results suggest that the model’s ability to predict both spatial structure and spread of the population will be improved by incorporating a spatially explicit element, with dispersal and recruitment probabilities that reflect the relative suitability of different parts of the landscape for these processes. Mikania micrantha H.B.K. (Asteraceae) in Papua New Guinea and Fiji.

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High-resolution spectra for 24 SMC and Galactic B-type supergiants have been analysed to estimate the contributions of both macroturbulence and rotation to the broadening of their metal lines. Two different methodologies are considered, viz. goodness-of-fit comparisons between observed and theoretical line profiles and identifying zeros in the Fourier transforms of the observed profiles. The advantages and limitations of the two methods are briefly discussed with the latter techniques being adopted for estimating projected rotational velocities ( v sin i) but the former being used to estimate macroturbulent velocities. The projected rotational velocity estimates range from approximately 20 to 60 kms(-1), apart from one SMC supergiant, Sk 191, with a v sin i similar or equal to 90 km s(-1). Apart from Sk 191, the distribution of projected rotational velocities as a function of spectral type are similar in both our Galactic and SMC samples with larger values being found at earlier spectral types. There is marginal evidence for the projected rotational velocities in the SMC being higher than those in the Galactic targets but any differences are only of the order of 5 - 10 km s(-1), whilst evolutionary models predict differences in this effective temperature range of typically 20 to 70 km s(-1). The combined sample is consistent with a linear variation of projected rotational velocity with effective temperature, which would imply rotational velocities for supergiants of 70 kms(-1) at an effective temperature of 28 000 K ( approximately B0 spectral type) decreasing to 32 km s(-1) at 12 000 K (B8 spectral type). For all targets, the macroturbulent broadening would appear to be consistent with a Gaussian distribution ( although other distributions cannot be discounted) with an 1/e half-width varying from approximately 20 km s(-1) at B8 to 60 km s(-1) at B0 spectral types.

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Two young African Canadian girls are the subject of this undated cabinet card photograph by John B. Cook, of Toronto. The address listed on the company stamp, which appears in gold lettering at the bottom of the card, is 191 and 193 Yonge [St.] Toronto. The original photo was over-exposed and faded, so image adjustments have been made for clarification purposes. This photograph was in the possession of Iris Sloman Bell, of St. Catharines, Ontario. It is possible these two girls are relatives of the Sloman and Bell families. Relatives of the Sloman - Bell families include former American slaves who settled in Canada.John B. Cook is listed as being a photographer -- and a hotelier -- in Toronto from 1879-1898. Source: Phillips, Glen C. The Ontario photographers list (1851-1900). Sarnia: Iron Gate Publishing Co., 1990.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)