987 resultados para 3.420.684
Resumo:
Ce mémoire traite des Saturnales de Macrobe, haut fonctionnaire du 5ième siècle après J.C. et encyclopédiste latin. Malgré l’opinion reçue, selon laquelle les Saturnales dépendraient presque exclusivement d’un nombre très restreint de sources, souvent copiées mot à mot, on a reconnu depuis longtemps que Macrobe remanie de son propre chef l’une de ces sources, les Propos de Table de Plutarque, dans son septième livre. Ce mémoire démontre que ce modèle, tout comme les sources mineures, latines et grecques, avec lesquelles Macrobe le complète, lui était assez familier pour servir à l’articulation d’une vision propre; les Saturnales ne peuvent donc être cités comme preuve de la décadence de leur époque. Ce mémoire fournit une traduction et un commentaire des chapitres 7.1-3 des Saturnales, avec une explication de leurs rapports avec les Propos de Table 1.1 et 2.1 de Plutarque ainsi que des éléments propre à Macrobe, afin de reconstruire sa méthode de composition et de déterminer ses attentes par rapport à son lecteur de l’empire tardif. Le commentaire est précédé d’une introduction de l’auteur, de l’œuvre, et du septième livre.
Resumo:
The ice cover of the Arctic Ocean has been changing dramatically in the last decades and the consequences for the sea-ice associated ecosystem remain difficult to assess. Algal aggregates underneath sea ice have been described sporadically but the frequency and distribution of their occurrence is not well quantified. We used upward looking images obtained by a remotely operated vehicle (ROV) to derive estimates of ice algal aggregate biomass and to investigate their spatial distribution. During the IceArc expedition (ARK-XXVII/3) of RV Polarstern in late summer 2012, different types of algal aggregates were observed floating underneath various ice types in the Central Arctic basins. Our results show that the floe scale distribution of algal aggregates in late summer is very patchy and determined by the topography of the ice underside, with aggregates collecting in dome shaped structures and at the edges of pressure ridges. The buoyancy of the aggregates was also evident from analysis of the aggregate size distribution. Different approaches used to estimate aggregate biomass yield a wide range of results. This highlights that special care must be taken when upscaling observations and comparing results from surveys conducted using different methods or on different spatial scales.
Resumo:
The euphotic depth (Zeu) is a key parameter in modelling primary production (PP) using satellite ocean colour. However, evaluations of satellite Zeu products are scarce. The objective of this paper is to investigate existing approaches and sensors to estimate Zeu from satellite and to evaluate how different Zeu products might affect the estimation of PP in the Southern Ocean (SO). Euphotic depth was derived from MODIS and SeaWiFS products of (i) surface chlorophyll-a (Zeu-Chla) and (ii) inherent optical properties (Zeu-IOP). They were compared with in situ measurements of Zeu from different regions of the SO. Both approaches and sensors are robust to retrieve Zeu, although the best results were obtained using the IOP approach and SeaWiFS data, with an average percentage of error (E) of 25.43% and mean absolute error (MAE) of 0.10 m (log scale). Nevertheless, differences in the spatial distribution of Zeu-Chla and Zeu-IOP for both sensors were found as large as 30% over specific regions. These differences were also observed in PP. On average, PP based on Zeu-Chla was 8% higher than PP based on Zeu-IOP, but it was up to 30% higher south of 60°S. Satellite phytoplankton absorption coefficients (aph) derived by the Quasi-Analytical Algorithm at different wavelengths were also validated and the results showed that MODIS aph are generally more robust than SeaWiFS. Thus, MODIS aph should be preferred in PP models based on aph in the SO. Further, we reinforce the importance of investigating the spatial differences between satellite products, which might not be detected by the validation with in situ measurements due to the insufficient amount and uneven distribution of the data.