998 resultados para 103-638B


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About 80 species of spores and pollen grains were recorded during detailed palynological investigations of selected Lower Cretaceous sections from Holes 638B and 638C and the bottom of Hole 641C. Most of them are long-ranging taxa with worldwide distribution. However, on the Iberian margin and in the southern European basins, Trilobosporites canadensis, Trilobosporites bernissartensis, Parvisaccites amplus, Foveosporites subtriangularis, and Ephedripites multicostatus seem to be index species of the Valanginian to late Aptian interval. Clavatipollenites was not recovered in the Barremian marginal marine sediments.

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The dinoflagellate cyst assemblages in 42 samples collected from Sites 638 and 639 were analyzed. All samples from Site 639 are barren; relatively poor assemblages occur in samples from Site 638. The distribution of 61 dinoflagellate cyst taxa identified in samples from Holes 638B and 638C are tabulated. The assemblages from Site 638 are comparable to those of Tethyian stratotypes and from neighboring areas, which permits age determinations and correlations between Holes 638B and 638C. The interval from Cores 103-638C-14R to 103-638C-1R is late Berriasian through Valanginian in age. In Hole 638B, the interval from Core 103-638B-43R to Section 103-638B-23R-2 is dated as early Valanginian through middle Barremian. Sections 103-638B-21R-2 and 103-638B-21R-1 are late Aptian in age. Taxonomic remarks are made about some species; a new dinoflagellate cyst Heterosphaeridiuml galiciae is described.

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Samples of Lower to middle Cretaceous rocks from ODP Sites 638, 640, and 641, drilled on the Galicia continental margin in the northeast Atlantic, have been investigated by organic geochemical methods (i.e., organic carbon determination, Rock-Eval pyrolysis, kerogen microscopy, gas chromatography, and gas chromatography/mass spectrometry) to define the Organofacies types and the depositional environments of these sediments. The results of this study fit well into the general picture drawn for the depositional history of the organic matter in Cretaceous organic-carbon-rich sediments in the North Atlantic from previous DSDP investigations. During the Valanginian to Albian, terrigenous organic carbon dominated the organic matter deposited on the Galicia continental margin. Cyclic changes in total organic carbon content were probably controlled by climatic-triggered changes in the supply of terrigenous organic matter from the nearby continent. A drastic change in depositional environment must have occurred near the Cenomanian/Turonian boundary. The preservation of large amounts of marine organic carbon in these sediments was probably caused by anoxic deep-water conditions during that time, rather than high productivity. All of the primary organic matter of the sediment samples investigated is thermally immature, as indicated by very low vitrinite reflectance values.

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The composition of 31 samples of Lower Cretaceous (Valanginian to Aptian) sandstone from ODP Sites 638 through 641 was analyzed using the Gazzi-Dickinson point-counting method. The results show that the source of the Valanginian to Hauterivian sand was a continental block, dominated by granitic and/or high-grade-metamorphic rocks. Although these petrologic results do not allow discrimination between various potential continental block provinces, they suggest, in conjunction with seismic profiles and regional considerations, that the source was the Galicia margin or western Iberia. In contrast, the Barremian and Aptian sand is dominated by carbonate grains that were derived from a carbonate platform, probably on Galicia Bank.

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Organic-carbon-rich 'black shales' and adjacent organic-carbon-poor rocks from three different Cretaceous settings encountered during ODP Leg 103 have been studied by organic geochemical methods. Rock-Eval analysis, carbon isotope data, and lipid biomarkers show organic matter to contain varying proportions of marine and continental materials. In Hauterivian-Barremian organic-carbon-rich marlstone turbidites, large amounts of land-derived organic matter are found. Aptian-Albian black-colored shales are interspersed within green claystones, from which they differ by containing more marine organic matter. An abbreviated layer of black shale from the Cenomanian/Turonian boundary is dominated by well-preserved marine organic matter. Downslope transport and rapid reburial within a predominantly oxygenated deep-water setting created most of these examples of black shales, except for the Cenomanian-Turonian deposits in which deep-water anoxia may have been involved.

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Early Cretaceous dinoflagellate cysts were reinvestigated from nine deep-sea sites of the North and Central Atlantic. In general the zonation scheme developed for the western Central Atlantic (Habib, 1977; Habib and Drugg, 1983 ) can also be applied to the eastern Central Atlantic. Comparison with the probabilistic zonation of Gradstein et al. (1992) show, however, that the first occurrences of the important marker species Druggidium apicopaucicure, Druggidium deflandrei, Druggidium rhabdoreticulatum and Odontochitina operculata appear to occur slightly later in the eastern Central Atlantic in respect to nannofossils and benthic foraminifers. Muderongia neocomica has a shorter stratigraphic range in the eastern Central Atlantic than in the western Central Atlantic.

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Os autores fazem uma revisão de 103 casos de endocardites infecciosas, dos quais 52 apresentaram manifestações neurológicas. Dos 52 que não tiveram problemas neurológicos, 39 faleceram 175%), enquanto que dos 51 que não tiveram alterações do sistema nervoso, apenas 18 evoluíram para o óbito 135,3%). A endocardite infecciosa com manifestações neurológicas, na presente série, foi dominante no sexo masculino. Os grupos etários mais envolvidos foram as crianças, adolescentes e adultos jovens. Houve outro pico importante em pacientes acima de 50 anos. Os critérios para o diagnóstico de endocardite infecciosa utilizados no presente estudo, foram os clássicos, acrescidos de outros considerados de extrema utilidade, à medida que a experiência foi sendo acumulada, acompanhando paralelamente as modificações dos padrões etiológicos, assim como as alterações dos espectros clínicos da doença, conseqüentes a muitos fatores aqui discutidos. Os principais distúrbios neurológicos observados foram as manifestações meningeias, 25/52 148,1%), alterações do comportamento, 20/52 (38,4%), fenômenos motores (paralisias e paresias), 20/52 (38,4%). Alterações do nível de consciência (torpor ou coma), ao lado de outras menos comuns, como cefaléia 16/52 (26,9%), convulsões, 10/52 (19,2%), afasia 7/52 (13,5%) e manchas de Roth, 7/53 (13,5%). As manifestações neurológicas frequentemente foram múltiplas em um mesmo paciente. Nas formas de endocardite, foram em muitos casos praticamente as alterações que abriram e dominaram a cena clínica. As mais comuns foram: síndrome meningeia, síndrome vascular e encefalopatia tóxica. Foi difícil, em conseqüência de múltiplas manifestações neurológicas num mesmo paciente, estabelecer critérios entre a lesão neurológica e o prognóstico, embora o coma profundo, as convulsões, os distúrbios motores acentuados, a meningite e as alterações do comportamento, isoladamente ou em associação, façam com que o mesmo seja bem mais sério. O germe mais encontrado em nossa série foi oStaphylococcus aureus, relacionado com formas agudas da infecção endocárdica, aliado a processos destrutivos valvulares e a sérias alterações neurológicas tais como meningite, encefalite, infartos, hemorragias e abcessos cerebrais. Os principais achados neurológicos referentes à patologia, no estudo de 15 casos, são apresentados ao lado de conclusões tiradas de reflexões sobre o material analisado e da experiência vivida. Uma revisão da literatura é feita desde os trabalhos iniciais sobre a doença até os dias de hoje, ficando evidenciada a importância do tema pelas grandes contribuições apresentadas pelos diferentes autores.