978 resultados para Adaptação marginal dentária
Resumo:
Terrigenous components were separated from the bulk sediment of Core A7 from the Okinawa Trough and Core A37 from the Ryukru Trench and grain-size distributions of these sub-samples were analyzed. Based upon an analysis of the grain-size data of the two sedimentary sequences, grain-size populations are identified to be sensitive to sedimentary environmental changes. The modal values and size ranges of the two main grain-size populations in Core A7 are evidently different from those of Core A37, indicating the spatial variability of sediment sources and transport processes between the two places. The downcore variations in the content of the environmentally sensitive grain-size populations reveal that during the accumulation of sedimentary material the environment remained relatively stable at the site where Core A7 was collected, except for the apparent events for the formation of two turbidite layers and a volcanic ash layer. However, the sedimentary sequence of Core A37 shows six sedimentary cycles, indicating a highly variable sedimentary environment at this location.
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The characteristics and distribution patterns of detrital minerals (0.063 similar to 0.125 mm) in marine sediments provide a significant indicator for the identification of the origin of sediment. The detrital mineral composition of 219 surface sediment samples was analysed to identify the distribution of sediments within the western Philippine Sea. The area can be divided into three mineral provinces: ( 1) province east of the Philippine Trench, the detrital minerals in this province are mainly composed of calcareous or siliceous organisms, with the addition of volcanogenic minerals from an adjacent island arc; (II) middle mineral province, clastic minerals including feldspar, quartz and colorless volcanic glass, sourced from seamounts with intermediate-acid volcanic rock, or erupting intermediate-acid volcano; (III) province west of the Palau-Kyushii Ridge, the matter provenance within this province is complex; the small quantity of feldspar and quartz may be sourced from seamounts or erupting volcano with intermediate - acid composition, with a component of volcanic scoria sourced from a volcano erupting on the Palau-Kyushu Ridge. it is suggested that, ( I) Biogenic debris of the study area is closely related to water depth, with the amount of biogenic debris controlled by carbonate lysocline. (2) Volcaniclastic matter derived from the adjacent island are can be entrained by oceanic currents and transported towards the abyssal basin over a short distance. The weathering products of volcanic rocks of the submarine plateau ( e. g. I Benham Plateau) and adjacent ridges provide an important source of detrital sedimentation, and the influence scope of them is constrained by the intensity of submarine weathering. (3) Terrigenous sediments from the continent of Asia and the adjacent Philippine island arc have little influence on the sedimentation of this study area, and the felsic mineral component is probably sourced from volcanic seamounts of intermediate-acid composition.
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2010
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Peso da parte aérea, Nossa Senhora das Dores; Peso de raízes, Nossa Senhora das Dores; Teor de matéria seca de raíz, Nossa Senhora das Dores; Teor de amido, Nossa Senhora das Dores; Peso da parte aérea, Lagarto; Peso de raízes, Lagarto; Teor de matéria seca de raíz, Lagarto; Teor de amido, lagarto; Altura da planta, Lagarto; Altura da 1º ramificação, Lagarto; peso da parte aérea, Umbaúba; Peso de raíz, Umbaúba; Teor de matéria seca de raíz, Umbaúba; Teor de amido, Umbaúba; Altura da planta, Umbaúba; Altura da 1º ramificação, Umbaúba; comprimento de raíz, Umbaúba; Ensaio de variedades e híbridos de mandioca; Avaliação de cultivares de mandioca no período 2004/2006; Peso da parte aérea, Nossa Senhora das Dores; peso de raízes, Nossa Senhora das Dores; Índice de colheita, Nossa Senhora das Dores; Teor de matéria seca de raíz, Nossa Senhora das Dores; Teor de amido, Nossa Senhora das Dores
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2008
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2006
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2005
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2005
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2005
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2005
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2005
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2005
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2005
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2005
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2005