A ictiofauna de poças rochosas de maré: padrões de distribuição associados ao espaço e ambiente

Em estudos com comunidades biológicas, a busca por padrões de ocorrência e distribuição das espécies vêm ganhando espaço em pesquisas realizadas nas últimas décadas. O conhecimento da estrutura das comunidades e suas relações, associados às interações desses organismos com o meio ambiente, fornecem subsídios necessários para a manutenção dessas comunidades, bem como informações relevantes em planos de conservação e manejo. Sendo assim, o objetivo desta pesquisa foi avaliar o efeito do ambiente e do espaço na estruturação da assembleia de peixes de poças rochosas de maré, descrevendo o padrão de ocupação das espécies nesse ambiente, testando a hipótese de que o espaço possui maior efeito na estruturação da ictiofauna. Foram amostradas 80 poças rochosas ao longo da Zona Costeira Amazônica, sendo 40 no período de maior precipitação e 40 no período de estiagem de 2011. Estas poças estão localizadas em cinco praias do litoral paraense e foram mensuradas quanto ao volume, a distância da margem e as variáveis físico-químicas da água, como pH, temperatura e salinidade. Foram coligidos 1.311 peixes, sendo 633 indivíduos na chuva e 648 na estiagem. Os indivíduos estão distribuídos em nove ordens, 14 famílias e 21 espécies, sendo a Ordem Perciformes a ordem mais abundante, com B. soporator e L. jocu sendo as espécies mais representativas. Os resultados obtidos na rotina BioEnv evidenciaram que as variáveis abióticas pH, temperatura e volume são responsáveis pela estruturação da comunidade. O cálculo da diversidade β evidenciou uma ampla variação de dados, abrangendo desde a substituição total das espécies até comunidades idênticas entre si, quanto à ocorrência e abundância. A DCA evidenciou que o período pluviométrico não é determinante na distribuição das espécies, uma vez que não há diferença na composição entre os dois períodos. O efeito do espaço e do ambiente sobre a comunidade foi pequeno, uma vez que a maior parte da variação não foi explicada utilizando-se todas as variáveis ambientais, como em uma segunda análise, em que só foram utilizadas as variáveis definidas pela rotina BioEnv. Seguindo o mesmo padrão, a pRDA apenas para as variáveis mais correlacionadas evidenciou que: 6% respondem ao ambiente, 4% ao espaço, 2% ao ambiente e espaço e 88% são outros fatores. Os resultados obtidos nessas análises comprovam que os fatores abióticos mensurados, bem como a distância entre as amostras, não são determinantes na composição e distribuição da ictiofauna em poças rochosas, refutando assim a hipótese de que o espaço possui efeito na estruturação da ictiofauna, uma vez que as condições ambientais sofrem constantes perturbações ocasionadas pelo movimento de marés. Sendo assim, as espécies que ocupam esse ambiente se mostram adaptadas, e por isso, não teriam sua distribuição afetada pela variação dos parâmetros ambientais nessa escala de estudo, respondendo somente ao efeito do espaço.

Condições oceanográficas, ocupação territorial e problemas ambientais na praia do Atalaia (nordeste do Pará, Brasil)

A conservação e gestão da zona costeira da região amazônica merecem atenção especial, devido à riqueza de seus recursos naturais. O presente estudo visa avaliar os impactos dos eventos naturais e atividades humanas na praia de Atalaia, situada no estado do Pará (Brasil), e o desenvolvimento de diretrizes para a implementação de programas de gestão costeira. Os dados foram coletados entre novembro/2008 e novembro/2010. Quatro conjuntos de variáveis foram avaliados: (i) variáveis físicas (climatologia, hidrodinâmica e morfodinâmica), (ii) variáveis hidrológicas (temperatura da água, salinidade, pH, turbidez, oxigênio dissolvido e nutrientes inorgânicos dissolvidos, clorofila a e níveis de coliformes termotolerantes), (iii) desenvolvimento urbano e (iv) distribuição espacial de serviços e infraestrutura. Os resultados indicam que o clima e as condições hidrodinâmicas foram os principais fatores responsáveis pelas flutuações na qualidade de água, turbidez, oxigênio dissolvido, nutrientes inorgânicos dissolvidos e concentrações de clorofila a. A descarga de esgoto doméstico não tratado foi responsável pela contaminação bacteriológica, embora a rápida turbulência decorrente da alta energia hidrodinâmica do ambiente tenha limitado a contaminação por coliformes termotolerantes. Esta alta energia hidrodinâmica, principalmente durante as marés equinociais de sizígia e a falta de planejamento urbano gera outros problemas, tais como a erosão costeira. A área de estudo é caracterizada por altas taxas pluviométricas (> 1900 mm durante a estação chuvosa), ventos de NE com velocidades médias mensais superiores a 4,36 m/s na estação seca e 3,06 m/s na estação chuvosa, condições de macromaré (alcance da maré > 4,0 m), velocidades moderadas de correntes de maré (superior a 0,5 m/s) e alturas de ondas significantes superior a 1,5 m. Em março e junho (meses chuvosos), a corrente de maré vazante alcançou um máximo de 0,4 m/s. O ciclo de maré foi fracamente assimétrico com a maré vazante durando mais de 6 horas e 40 minutos. A energia das ondas foram fracamente moduladas pela maré baixa devido à atenuação das ondas em bancos de areia. A temperatura da água foi relativamente homogênea (27,4°C a 29,3°C). A salinidade variou de 5,7 (junho) a 37,4 (novembro). A água foi bem oxigenada (superior a 9,17 mg/L), turva (superior a 118 NTU), alcalina (acima de 8,68) e eutrófica (máximo de 2,36 μmol/L para nitrito, 24,34 μmol/L para nitrato, 0,6 μmol/L para fosfato e 329,7 μmol/L para silicato), além de apresentar altas concentrações de clorofila a (acima de 82 mg/m³). As condições naturais observadas no presente estudo indicam a necessidade de uma revisão dos critérios hidrológicos usados para avaliação de praias por agências nacionais e internacionais e sua adaptação para a realidade da costa amazônica. A falta de sistema de saneamento público levou a contaminação bacteriológica e a perda da qualidade da água. Com relação ao estado morfodinâmico, as condições dissipativas foram encontradas durante alta a moderada energia hidrodinâmica (condições equinociais e não-equinociais), porém em novembro as maiores alturas de ondas geraram características de barred dissipative, enquanto nos outros meses características nonbarred foram dominantes. Desta forma, o modelo proposto por Masselink & Short (1993) parece não ser ideal para ser aplicado em praias com características similares a praia de Atalaia, na qual a energia das ondas é modulada pela presença de bancos de areia durante algumas fases da maré.

A sensibilidade do lugar: uma proposta metodológica para aplicação da percepção ambiental nos planos de emergência a derrames de óleo

Pós-graduação em Geografia - IGCE

Patient Education and Self-Care for the Management of Jaw Pain upon Awakening: A Randomized Controlled Clinical Trial Comparing the Effectiveness of Adding Pharmacologic Treatment with Cyclobenzaprine or Tizanidine

Aims: To compare the effectiveness of adding cyclobenzaprine, tizanidine, or placebo to patient education and a self-care management program for patients with myofascial pain and specifically presenting with jaw pain upon awakening. Methods: Forty-five patients with a diagnosis of myofascial pain based on the guidelines of the American Academy of Orofacial Pain participated in this 3-week study. The subjects were randomly assigned into one of three groups: placebo group, TZA group (tizanidine 4 mg), or CYC group (cyclobenzaprine 10 mg). Patients were evaluated for changes in pain intensity, frequency, and duration by using the modified Severity Symptoms Index and changes in sleep quality with the use of the Pittsburgh Sleep Quality Index. Data were analyzed by ANOVA and post-hoc or nonparametric statistical tests as appropriate. Results: All three groups had a reduction in pain symptoms and improvement of sleep quality based on a comparison of pretreatment and treatment scores. However, no significant differences among the groups were observed at the posttreatment evaluation. Conclusion: The use of tizanidine or cyclobenzaprine in addition to self-care management and patient education was not more effective than placebo for the management of patients with myofascial jaw pain upon awakening.

Feral swine damage and damage management in forested ecosystems

Invasive feral swine (Sus scrofa) cause deleterious impacts to ecosystem processes and functioning throughout their worldwide distribution, including forested ecosystems in the United States. Unfortunately, many feral swine damage management programs are conducted in a piecemeal fashion, are not adequately funded, and lack clearly stated or realistic objectives. This review paper identifies damage caused by feral swine to forest resources and presents techniques used to prevent and control feral swine damage. Concluding points related to planning a feral swine damage management program are: (1) the value of using a variety of techniques in an integrated fashion cannot be overstated; (2) there is value in using indices for both feral swine populations and their damage pre and post management activities; (3) innovative technologies will increasing be of value in the pursuit of feral swine damage reduction; and (4) though not appropriate in every situation, there is value in involving the public in feral swine damage management decisions and activities.

Wildlife Risk Management at Vancouver International Airport

The Vancouver International Airport (YVR) is the second busiest airport in Canada. YVR is located on Sea Island in the Fraser River Estuary - a world-class wintering and staging area for hundreds of thousands of migratory birds. The Fraser Delta supports Canada’s largest wintering populations of waterfowl, shorebirds, and raptors. The large number of aircraft movements and the presence of many birds near YVR pose a wide range of considerable aviation safety hazards. Until the late 1980s when a full-time Wildlife Control Program (WCP) was initiated, YVR had the highest number of bird strikes of any Canadian commercial airport. Although the risks of bird strikes associated with the operation of YVR are generally well known by airport managers, and a number of risk assessments have been conducted associated with the Sea Island Conservation Area, no quantitative assessment of risks of bird strikes has been conducted for airport operations at YVR. Because the goal of all airports is to operate safely, an airport wildlife management program strives to reduce the risk of bird strikes. A risk assessment establishes the current risk of strikes, which can be used as a benchmark to focus wildlife control activities and to assess the effectiveness of the program in reducing bird strike risks. A quantitative risk assessment also documents the process and information used in assessing risk and allows the assessment to be repeated in the future in order to measure the change in risk over time in an objective and comparative manner. This study was undertaken to comply with new Canadian legislation expected to take effect in 2006 requiring airports in Canada to conduct a risk assessment and develop a wildlife management plan. Although YVR has had a management plan for many years, it took this opportunity to update the plan and conduct a risk assessment.

A process evaluation of the childhood lead poisoning prevention program in Houston, Texas, 1992--1995

A process evaluation of the Houston Childhood Lead Poisoning Prevention Program, 1992-1995, was conducted. The Program's goal is to reduce lead poisoning prevalence. The study proposed to determine to what extent the Program was implemented as planned by measuring how well Program services were actually: (1) received by the intended target population; (2) delivered to children with elevated blood lead levels; (3) delivered in compliance with the Centers for Disease Control and Prevention and Program guidelines and timetables; and (4) able to reduce lead poisoning prevalence among those rescreened. Utilizing a program monitoring design, the Program's pre-collected computer records were reviewed. The study sample consisted of 820 children whose blood lead levels were above 15 micrograms per deciLiter, representing approximately 2.9% of the 28,406 screened over this period. Three blood lead levels from each participant were examined: the initial elevated result; the confirmatory result; and the next rescreen result, after the elevated confirmatory level. Results showed that the Program screened approximately 18% (28,406 of 161,569) of Houston's children under age 6 years for lead poisoning. Based on Chi-square tests of significance, results also showed that lead-poisoned participants were more likely to be younger than 3 years, male and Hispanic, compared to those not lead poisoned. The age, gender and ethnic differences observed were statistically significant (p =.01, p =.00, p =.00). Four of the six Program services: medical evaluations, rescreening, environmental inspections and confirmation, had satisfactory delivery completion rates of 71%-98%. Delivery timetable compliance rates for three of the six services examined: outreach contacts, home visits and environmental inspections were below 32%. However, dangerously elevated blood lead levels fell and lead poisoning prevalence dropped from 3.3% at initial screening to 1.2% among those rescreened, after intervention. From a public health perspective, reductions in lead poisoning prevalence are very meaningful. Based on these findings, the following are recommendations for future research: (1) integrate Program database files by utilizing a computer database management program; (2) target services at Hispanic male children under age 3 years living in the highest risk neighborhoods; (3) increase resources to: improve tracking and documentation of service delivery and provide more non-medical case management and environmental services; and (4) share the evaluation methodology/findings with the Centers for Disease Control and Prevention administrators; the implications may be relevant to other program managers conducting such assessments. ^

Some hydrophysical and hydrochemical parameters of the upper part of the hydrogen sulfide zone in the Black Sea, September 11-22, 1994

Features of spatial variability of hydrogen sulfide in the northeastern part of the Black Sea are estimated. Some technical aspects of H2S concentration determination in the anoxic zone are discussed: in its upper part at H2S concentration <30 µmol/l, the photometric method is recommended, while for deeper layers the iodometric method should be used. With linearity of vertical distribution of hydrogen sulfide and ammonium taken into account their vertical gradients are estimated as 0.49+/-0.04 µmol/m and 0.19+/-0.06 µmol/m respectively. It is shown that the upper boundary of the H2S layer corresponds to the isopycnal surface with Sigma_t = 16.19+/-0.05 arbitrary units. Special attention is paid to relationship of hydrogen sulfide distribution with hydrophysical features in the region under study, in particular in the coastal zone. It is shown that hydrodynamic conditions control spatial distribution of hydrogen sulfide. On the basis of isopycnal treatment of the H2S field existence of a coastal convergence zone is proved, and peculiarities are recognized of vertical circulation in the main Black Sea gyre and coastal anticyclonic eddies; here hydrogen sulfide serves as a tracer of hydrophysical mixing processes.

Near-coastal circum-Antarctic iceberg size distributions determined from Synthetic Aperture Radar images

The Radarsat-1 Antarctic Mapping Project (RAMP) compiled a mosaic of Antarctica and the adjacent ocean zone from more than 3000 high-resolution Synthetic Aperture Radar (SAR) images acquired in September and October 1997. The mosaic with a pixel size of 100 m was used to determine iceberg size distributions around Antarctica, combining an automated detection with a visual control of all icebergs larger than 5 km**2 and correction of recognized false detections. For icebergs below 5 km**2 in size, the numbers of false detections and accuracies of size retrievals were analyzed for three test sites. Nearly 7000 icebergs with horizontal areas between 0.3 and 4717.7 km**2 were identified in a near-coastal zone of varying width between 20 and 300 km. The spatial distributions of icebergs around Antarctica were calculated for zonal segments of 20° angular width and related to the types of the calving fronts in the respective section. Results reveal that regional variations of the size distributions cannot be neglected. The highest ice mass accumulations were found at positions of giant icebergs (> 18.5 km) but also in front of ice shelves from which larger numbers of smaller icebergs calve almost continuously. Although the coastal oceanic zone covered by RAMP is too narrow compared to the spatial coverage needed for oceanographic research, this study nevertheless demonstrates the usefulness of SAR images for iceberg research and the need for repeated data acquisitions extending ocean-wards over distances of 500 km and more from the coast to monitor iceberg melt and disintegration and the related freshwater input into the ocean.

Downward particle fluxes at the oligotrophic and mesotrophic site of the EUMELI program

A two year record of downward particle flux was obtained with moored sediment traps at several depths of the water column in two regions characterized by different primary production levels (mesotrophic and oligotrophic) of the eastern subtropical North Atlantic Ocean in the framework of the EUMELI program. Settling particles were collected with multisample conical sediment-traps moored at 1000 and 2500 depths in the water column. Time-series samples were obtained between February 1991 and November 1992. During this time, sampling intervals varied from 8 to 10 d and were synchronized at all depths and also between the oligotrophic and mesotrophic moorings. Sediment-trap sampling procedures were consistent with JGOF and described elsewhere. The data shown here are mass, particulate organic carbon (POC), particulate inorganic carbon (PIC), coccolithophore, opal, and lithogenic downward fluxes obtained during the entire sediment-trap deployments at both sites.

Coastal floods and decadal changes: the climate factor

Observation has widely shown for nearly all last century that the Spanish (Dynamic) Maritime Climate was following around 10 to 11 year cycles in its most significant figure, wind wave, despite it being better to register cycles of 20 to 22 years, in analogical way with the semi-diurnal and diurnal cycles of Cantabrian tides. Those cycles were soon linked to sun activity and, at the end of the century, the latter was related to the Solar System evolution. We know now that waves and storm surges are coupled and that (Dynamic) Maritime Climate forms part of a more complex “Thermal Machine” including Hydrological cycle. The analysis of coastal floods could so facilitate the extension of that experience. According to their immediate cause, simple flood are usually sorted out into flash, pluvial, fluvial, groundwater and coastal types, considering the last as caused by sea waters. But the fact is that most of coastal floods are the result of the concomitance of several former simple types. Actually, the several Southeastern Mediterranean coastal flood events show to be the result of the superposition within the coastal zone of flash, fluvial, pluvial and groundwater flood types under boundary condition imposed by the concomitant storm sea level rise. This work shall be regarded as an attempt to clarify that cyclic experience, through an in-depth review of a past flood events in Valencia (Turia and Júcar basins), as in Murcia (Segura’s) as well.

Metodología para la caracterización de zonas costeras basada en un modelo sistémico

Las obras de infraestructura que construye el ser humano para optimizar los recursos naturales y satisfacer sus necesidades, producen impactos tanto positivos como negativos en el ambiente. México cuenta con una gran cantidad de recursos naturales y lugares que han sido favorecidos por la naturaleza, donde la sobrecarga de las actividades antropogénicas genera problemas de impacto ambiental, especialmente en las zonas costeras y en su entorno. El objetivo del presente trabajo fue aportar información acerca de las principales presiones que recibe el sistema y cómo esto afecta a las propuestas de soluciones integrales y a la capacidad para recuperar el estado de equilibrio en las zonas costeras. En la presente investigación, se desarrolló una metodología para la caracterización de zonas costeras, basada en un modelo sistémico, con el propósito de tener una herramienta de planificación para proyectos ambientalmente sustentables, integrando una base de datos con las mejores prácticas de planificación, lo que facilitará el diagnóstico y la evaluación de la capacidad adaptativa de recuperación del sistema. Asimismo, se utilizó un modelo sistémico como una metodología para organizar la gran complejidad que implica la interrelación e interconexión que existe entre los múltiples componentes, y con ello obtener el conocimiento para su caracterización. Con base en el modelo de Zachman, se realizó un análisis para la detección de las fortalezas y debilidades del sistema, lo que permitió visualizar el impacto de los riesgos a que está expuesta una zona costera. Las principales aportaciones de este trabajo fueron el desarrollo de la FICHA DE CARACTERIZACIÓN DE LA ZONA COSTERA y la inclusión, en dicha ficha, de la estimación del nivel de la resiliencia física, ambiental, social, económica y política. La metodología propuesta, es una aportación que permite integrar los componentes, las relaciones e interconexiones que existen en el sistema costero. La metodología tiene la ventaja de ser flexible y se pueden agregar o desechar componentes de acuerdo a las particularidades de cada caso de estudio; adicionalmente, se propone utilizar esta herramienta como ayuda en el monitoreo periódico del sistema. Lo anterior como parte de un observatorio integrado al Sistema Nacional de Gestión Costera que se propone como parte de futuras líneas de investigación. Como caso de estudio, se realizó la caracterización del complejo sistema Banco Chinchorro, lo que resultó en la inclusión (en la FICHA DE CARACTERIZACIÓN DE LA ZONA COSTERA), de las lecciones aprendidas con la detección de buenas y malas prácticas, esto redundó en la mejora de la metodología propuesta para la gestión de la zona costera. All infrastructures that build the human being to optimize natural resources and meet their needs, generate both, positive and negative impacts on the environment, since the acquisition and transformation of resources in coastal areas affect their balance. Mexico has a large number of natural resources and places that have been favored by nature, whereas the overhead of anthropogenic activities leads to problems of environmental impact, especially in coastal areas and in its surroundings. The aim of this study was to provide information about the main pressures that a system receives and how this affects the proposed solutions and the ability to restore the state of balance in coastal areas. In this research, a methodology for the characterization of coastal zones, based on a systemic model, in order to develop a planning tool for environmentally sustainable projects, was developed, integrating a database with the best practices for planning, conservation and balance of coastal areas. This will facilitate the diagnosis and evaluation of the adaptive resilience of the system. A systemic model was used as a methodology to organize the vast complexity of the relationship and interconnection between the multiple components, and so thus gain knowledge for its characterization. Based on the Zachman model, an analysis to detect the strengths and weaknesses of the system was performed, allowing visualizing the impact of the risks that the coastal zone is exposed to. The main contributions of this study was the development of the COASTAL CHARACTERIZATION RECORD, and the inclusion, on that record, of the estimation of the physical, environmental, social, economic and political resilience. The proposed methodology is a contribution that allows integrating the components, relationships and interconnections existing in the coastal system. The methodology has the advantage of being flexible and components can be added or discarded according to the particularities of each case study; Additionally, this is not only a diagnostic tool, it is proposed to use it as an aid in monitoring periodically the system, this as part of an integrated monitoring into the National System of Coastal Management that is proposed as part of future research. As a case study, the characterization of the coastal zone “Banco Chinchorro” was done, resulting in the inclusion, in the COASTAL CHARACTERIZATION RECORD, of the documented lessons learned from the good and bad practices detection, improvement of the methodology proposed for the management of the coastal zone.

Comprehensive Greenhouse Gas Management for the Electric Generating Industry

Climate change is becoming more visible in the political arena. Electric generating companies will likely be impacted by future regulation of climate change related emissions. Even though few climate related programs are mandatory, electric generating companies should begin to implement greenhouse gas management systems. This report includes a review of issues facing the electric generating industry, an examination of current emission management programs, and recommendations for an effective greenhouse gas management framework. An effective greenhouse gas management program allows a company to continually improve their impact on climate change by reducing emissions using the plan, do, check, act process. To ease the reporting burden, companies should apply de minimis exemptions to sources that produce less than 5% of emissions.

(Table 1) Abundance of selected diatom taxa in the mid-Pliocene of ODP Hole 167-1022A

Diatom assemblages from the middle part of the Pliocene (3.2-2.5 Ma) were investigated from Ocean Drilling Program Sites 1016, 1021, and 1022 in an effort to infer paleotemperature fluctuations off California. Diatoms are very sparse in virtually all of the samples that were examined from Sites 1016 and 1021. This is presumably because these sites were seaward (west) of the coastal zone of diatom productivity during the middle part of the Pliocene. Diatoms are relatively common in the vast majority of samples that were examined from Hole 1022A. Diatom assemblages are dominated by Chaetoceros spores (a coastal upwelling component), the cold-water (subarctic) taxa Neodenticula kamtschatica and its descendant Neodenticula koizumii, and Thalassionema nitzschioides, a temperate taxon that is typically found at the seaward edge of coastal upwelling zones. Paleotemperature interpretations, however, are not possible at this time because of the scarcity of comparative modern core-top data.

High-extraction coal mining in Illinois : effects on crop production, 1985-1987 /

"IMSRP-IV."