ABSTRACT: The understanding of the differences between living (L) and dead (D) benthic foraminiferal assemblages and all the factors that might lead their distribution should be a key to characterize the environmental and paleoenvironmental changes accurately. Population dynamics and dissimilarities of biological nature (the differences in turnover rate and seasonal alterations in standing stock) can cause significant divergences between the L and D foraminiferal assemblages. This study compares L and D foraminifera to evaluate the sediment quality of the Brazilian Saquarema Lagoon System (SLS) using biogeochemical proxies and predict how coastal ecosystems are responding to the combined effects of eutrophication and pollution pressure and areas where the paleoenvironmental studies can be performed. The SLS is a transitional environment where total organic carbon, proteins, and dissolved oxygen are the main factors controlling the distribution of foraminiferal assemblage. The high values of biopolymers (carbohydrates, lipids, and proteins) in SLS indicate a very impacted environment with long water residence time. The low values of species richness, Shannon-Weaver diversity, and evenness for both L and D foraminiferal assemblages are a consequence of fluctuating conditions in the SLS. Due to low salinities, agglutinated species and Quinqueloculina seminula can occur in the most confined areas, and Ammonia parkinsoniana, Cribroelphidium excavatum, Cribroelphidium poeyanum, and Elphidium gunteri characterized the area with the highest marine influence. Although in most of the SLS the taphonomic processes modified the original assemblage, in some regions the thanatocoenosis corresponds to the biocenosis. These areas can be considered the most suitable for future paleoenvironmental and paleoclimatic studies.

Surface coal mining causes an intense topographic and hydrologic change in the area with suppression of local vegetation, degrading the environment. One main problem presented by the rehabilitated soil refers to physical disruption of the soil, which delays the regrowth of plant species in the mining area. The objective of this study was to evaluate the influence of four grass species in the retrieval of the rehabilitated soil's physical properties at a recovered coal mine area in Candiota, Rio Grande do Sul State, southern Brazil. With the data an ANOVA was performed and treatments means were compared using Tukey test (p ≤0.05). The treatments were: T1-Hemarthria altissima; T2-Paspalum notatum; T3-Cynodon dactylon; T4-Urochloa brizantha; a rehabilitated soil without vegetation cover was used as control. Preserved soil samples after 78 months were collected in the 0.00-0.10 m and 0.10-0.20 m layers to determine bulk density, total porosity, macroporosity, microporosity and available water capacity. The process of rehabilitation of coal mined areas was slow due to the high degree of degradation that occurs during the extraction of coal and the topographic recovery of the area, adversely affecting the structural quality of the soils. The assessed grasses showed potential to reclaim these areas, since improvements were observed in the values of the soil attributes over time, especially in the 0.00-0.10 m layer. After 78 months of evaluation, U. brizantha showed the higher potential to recover the physical properties of the compacted rehabilitated mine soils.

La minería del carbón en superficie provoca un intenso cambio topográfico e hidrológico en la zona por la supresión de la vegetación local, degradando el ambiente. Un problema principal presentado por el suelo rehabilitado es la perturbación física del suelo, lo que retrasa el rebrote de las especies vegetales en el área minera. El objetivo de este estudio fue evaluar la influencia de cuatro especies de gramíneas en la recuperación de las propiedades físicas del suelo en un área minera de carbón rehabilitada en Candiota, Rio Grande do Sul, sur de Brasil. Con los datos se realizó un ANDEVA y las medias de los tratamientos se compararon con la prueba de Tukey (p≤ 0.05). Los tratamientos fueron: T1-Hemarthria altissima; T2- Paspalum notatum; T3-Cynodon dactylon; T4-Urochloa brizantha; un suelo rehabilitado sin cubierta vegetal se usó como testigo. Muestras de suelo protegido se recolectaron después de 78 meses en capas de 0.00-0.10 m and 0.10-0.20 m para determinar densidad aparente, porosidad total, macroporosidad, microporosidad y capacidad de agua disponible. El proceso de rehabilitación de las zonas de minas de carbón fue lento debido al grado alto de degradación producido durante la extracción de carbón y la recuperación topográfica de la zona, lo que afecta negativamente la calidad estructural de los suelos. Las gramíneas evaluadas mostraron potencial para recuperar estas áreas, ya que se observaron mejoras en los valores de los atributos del suelo en el tiempo, especialmente en la capa de 0.00 a 0.10 m. Después de 78 meses de evaluación, U. brizantha mostró el potencial mayor para recuperar las propiedades físicas de los suelos rehabilitados de las minas.

Este trabalho descreve a composição química e a atividade antimicrobiana dos óleos voláteis de Ocimum canum e Ocimum selloi, que ocorrem em Jequié/BA, nordeste do Brasil. As plantas foram colhidas no inverno de 2005 e verão de 2006 e os óleos extraídos por destilação a vapor foram posteriormente analisados por GC-MS. Um total de 30 e 31 compostos foi identificado a partir dos óleos de O. selloi e O. canum, respectivamente. Foi observado que o teor de óleo de O. canum apresentou variação durante as estações do ano, enquanto o óleo de O. selloi não. Metilchavicol e linalol foram os principais componentes químicos encontrados na parte aérea e folhas de O. canum. Esta descoberta permitiu caracterizar este espécime como um novo quimiotipo de O. canum. Com relação às partes aéreas de O. selloi, eugenol, 1,8-cineol, trans-cariofileno e linalol foram identificadas como os seus principais componentes. Todos os óleos extraídos das partes aéreas apresentaram atividade biológica contra cocos gram-positivo - Staphylococcus aureus ATCC 25923 - mas apenas aquele de O. canum apresentou atividade contra bacilo gram-negativo - Escherichia coli ATCC 25922.

This work describes the chemical composition and antimicrobial activity of the volatile oils of Ocimum canum and Ocimum selloi, both occurring in Jequié/BA, northeastern Brazil. The plants were collected in the winter/2005 andsummer/2006, the oils extracted by steam distillation and further analyzed by GC-MS. A total of 30 and 31 compounds was identified from the oils of O. selloi and O. canum, respectively. It was observed that the oil content of O. canum showed variation during the seasons, while the oils of O. selloi did not. Methylchavicol and linalool were the main chemical components found in the aerial parts and leaves of O. canum. This finding permitted to characterize this specimen as a new chemotype of O. canum. Regarding the aerial parts of O. selloi, eugenol, 1,8-cineole, transcaryophyllene and linalool were identified as their major components. All extracted oils from the aerial parts showed biological activity against gram-positive cocci - Staphylococcus aureus ATCC 25923 - but only the O. canum one showed activity against gram-negative bacilli - Escherichia coli ATCC 25922.

A distribuição de compostos aromáticos selecionados e a microbiologia foram avaliados em sedimentos superficiais do Manguezal de Suruí, Baía de Guanabara. Amostras foram coletadas em 23 pontos e determinados a granulometria, matéria orgânica, compostos aromáticos, atividade microbiológica, biopolímeros e a topografia. A concentração dos compostos aromáticos foi distribuída em manchas por todo o manguezal e sua concentração total mais elevada foi encontrada na área central do manguezal. A granulometria diferiu da maioria dos manguezais, uma vez que no Manguezal de Suruí existem chernies nas bordas e na frente dos manguezais e areia através da superfície inteira, impedindo o relacionamento entre granulometria e os hidrocarbonetos. Uma média de 10% p/p da matéria orgânica foi obtida e os biopolímeros apresentaram concentrações elevadas, especialmente na área central e fundo do Manguezal. Os biopolímeros se distribuíram em altas concentrações. A presença de finos sedimentos é fator importante na acumulação de hidrocarbonetos. Na concentração elevada de matéria orgânica e de biopolímeros, topografia com chernies e as raízes que protegem os manguezais, áreas mais calmas são criadas, com depósito do material transportado pela ação das ondas. Comparadas às distribuições globais, as concentrações das substâncias aromáticas neste manguezal podem ser classificadas de moderadas a elevadas, demonstrando que a área estudada está altamente impactada.

The distribution of selected aromatic compounds and microbiology were assessed in superficial sediments from Suruí Mangrove, Guanabara Bay. Samples were collected at 23 stations, and particle size, organic matter, aromatic compounds, microbiology activity, biopolymers, and topography were determined. The concentration of aromatic compounds was distributed in patches over the entire mangrove, and their highest total concentration was determinated in the mangrove's central area. Particle size differed from most mangroves in that Suruí Mangrove has chernies on the edges and in front of the mangrove, and sand across the whole surface, which hampers the relationship between particle size and hydrocarbons. An average @ 10% p/p of organic matter was obtained, and biopolymers presented high concentrations, especially in the central and back areas of the mangrove. The biopolymers were distributed in high concentrations. The presence of fine sediments is an important factor in hydrocarbon accumulation. With high concentration of organic matter and biopolymers, and the topography with chernies and roots protecting the mangrove, calmer areas are created with the deposition of material transported by wave action. Compared to global distributions, concentrations of aromatic compounds in Suruí Mangrove may be classified from moderate to high, showing that the studied area is highly impacted.