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Metasomatism and magmatic assimilation at a gabbro-limestone contact, Christmas Mountains, Big Bend region, Texas

A composite stock of alkaline gabbro and syenite is intrusive into limestone of the Del Carmen, Sue Peake and Santa Elena Formations at the northwest end of the Christmas Mountains. There is abundant evidence of solution of wallrock by magma but nowhere are gabbro and limestone in direct contact. The sequence of lithologies developed across the intrusive contact and across xenoliths is gabbro, pyroxenite, calc-silicate skarn, marble. Pyroxenite is made up of euhedral crystals of titanaugite and sphene in a leucocratic matrix of nepheline, Wollastonite and alkali feldspar. The uneven modal distribution of phases in pyroxenite and the occurrence' of nepheline syenite dikes, intrusive into pyroxenite and skarn, suggest that pyroxenite represents an accumulation of clinopyroxene "cemented" together by late-solidifying residual magma of nepheline syenite composition. Assimilation of limestone by gabbroic magma involves reactions between calcite and magma and/or crystals in equilibrium with magma and crystallization of phases in which the magma is saturated, to supply energy for the solution reaction. Gabbroic magma was saturated with plagioclase and clinopyroxene at the time of emplacement. The textural and mineralogic features of pyroxenite can be produced by the reaction 2( 1-X) CALCITE + AN_XAB_l-X = (1-X) NEPHELINE+ 2(1-X) WOLLASTONITE+ X ANORTHITE+ 2(1-X) CO₂. Plagioclase in pyroxenite has corroded margins and is rimmed by nepheline, suggestive of resorption by magma. Anorthite and wollastonite enter solid solution in titanaugite. For each mole of calcite dissolved, approximately one mole of clinopyroxene was crystallized. Thus the amount of limestone that may be assimilated is limited by the concentration of potential clinopyroxene in the magma. Wollastonite appears as a phase when magma has been depleted in iron and magnesium by crystallization of titanaugite. The predominance of mafic and ultramafic compositions among contaminated rocks and their restriction to a narrow zone along the intrusive contact provides little evidence for the generation of a significant volume of desilicated magma as a result of limestone assimilation.

Within 60 m of the intrusive contact with the gabbro, nodular chert in the Santa Elena Limestone reacted with the enveloping marble to form spherical nodules of high-temperature calc-silicate minerals. The phases wollastonite, rankinite, spurrite, tilleyite and calcite, form a series of sharply-bounded, concentric monomineralic and two-phase shells which record a step-wise decrease in silica content from the core of a nodule to its rim. Mineral zones in the nodules vary 'with distance from the gabbro as follows:

0-5 m CALCITE + SPURRITE + RANKINITE + WOLLASTONITE
5-16 m CALCITE + TILLEYITE ± SPURRITE + RANKINITE + WOLLASTONITE
16-31 m CALCITE + TILLEYITE + WOLLASTONITE
31-60 m CALCITE + WOLLASTONITE
60-plus CALCITE + QUARTZ

The mineral of a one-phase zone is compatible with the phases bounding it on either side but these phases are incompatible in the same volume of P-T-X_CO2.

Growth of a monomineralio zone is initiated by reaction between minerals of adjacent one-phase zones which become unstable with rising temperature to form a thin layer of a new single phase that separates the reactants and is compatible with both of them. Because the mineral of the new zone is in equilibrium with the phases at both of its contacts, gradients in the chemical potentials of the exchangeable components are established across it. Although zone boundaries mark discontinuities in the gradients of bulk composition, two-phase equilibria at the contacts demonstrate that the chemical potentials are continuous. Hence, Ca, Si and CO₂ were redistributed in the growing nodule by diffusion. A monomineralic zone grows at the expense of an adjacent zone by reaction between diffusing components and the mineral of the adjacent zone. Equilibria between two phases at zone boundaries buffers the chemical potentials of the diffusing species. Thus, within a monomineralic zone, the chemical potentials of the diffusing components are controlled external to the local assemblage by the two-phase equilibria at the zone boundaries.

Mineralogically zoned calc-silicate skarn occurs as a narrow band that separates pyroxenite and marble along the intrusive contact and forms a rim on marble xenoliths in gabbro. Skarn consists of melilite or idocrase pseudomorphs of melili te, one or two . stoichiometric calcsilicate phases and accessory Ti-Zr garnet, perovskite and magnetite. The sequence of mineral zones from pyroxenite to marble, defined by a characteristic calc-silicate, is wollastonite, rankinite, spurrite, calcite. Mineral assemblages of adjacent skarn zones are compatible and the set of zones in a skarn band defines a facies type, indicating that the different mineral assemblages represent different bulk compositions recrystallized under identical conditions. The number of phases in each zone is less than the number that might be expected to result from metamorphism of a general bulk composition under conditions of equilibrium, trivariant in P, T and u_CO2. The "special" bulk composition of each zone is controlled by reaction between phases of the zones bounding it on either side. The continuity of the gradients of composition of melilite and garnet solid solutions across the skarn is consistent with the local equilibrium hypothesis and verifies that diffusion was the mechanism of mass transport. The formula proportions of Ti and Zr in garnet from skarn vary antithetically with that of Si Which systematically decreases from pyroxenite to marble. The chemical potential of Si in each skarn zone was controlled by the coexisting stoichiometric calc-silicate phases in the assemblage. Thus the formula proportion of Si in garnet is a direct measure of the chemical potential of Si from point to point in skarn. Reaction between gabbroic magma saturated with plagioclase and clinopyroxene produced nepheline pyroxenite and melilite-wollastonite skarn. The calcsilicate zones result from reaction between calcite and wollastonite to form spurrite and rankinite.

A reparação do dano causado por membro indeterminado de um grupo: por uma relação de complementaridade entre o seguro e a responsabilidade civil

O dano e sua causa apresentam-se, em conjunto, como um dilema inerente a uma sociedade que incorporou o risco como produto do seu próprio desenvolvimento. Desde tempos imemoriais a solidariedade figura como instrumento imprescindível à composição das diferentes formas possíveis para minimizar os efeitos negativos do implemento de um risco seja através da transferência de suas consequências econômicas para quem, por sua atividade o produziu ou, esteja melhor preparado para suportá-lo. Entretanto, as formas privadas tradicionais, isoladamente mostram-se insuficientes para responder satisfatoriamente à necessidade de reparação dos danos na atualidade. Isto porque, via de regra, os instrumentos para tal foram desenvolvidas em uma perspectiva individual, tendo como premissa a identificação da causa do dano e, a partir daí, a possibilidade de imputação de responsabilidade. Contemporaneamente, contudo, os danos usualmente resultam de causas múltiplas e, mesmo quando decorrem de causa única, essa pode estar relacionada a um conjunto de agentes, de forma a não ser possível a individuação do ofensor. Neste contexto, torna-se imprescindível a construção de uma noção jurídica de causalidade, apta a solucionar questões críticas, tais como a do dano causado por membro indeterminado de um grupo. Esta noção, por seu turno, requer uma base solidária mais aprofundada, de sorte a permitir a reparação do dano injusto sofrido pela vítima, sem arruinar o ofensor. Afirma-se, então, que a reparação integral dos danos em uma sociedade de risco depende de uma nova concepção acerca da solidariedade: a solidariedade global. E, indo além, a fase atual impõe a necessidade de se repensar a própria base do sistema de responsabilidade civil, como decorrência necessária de uma nova orientação jus-filosófica, inspirada por valores personalistas e solidaristas e também em razão da própria evolução social que potencializou os problemas que gravitam em torno da solidariedade e do risco, notadamente em razão da coletivização das causas dos danos. Assim, se há cada vez mais solidariedade nas causas e nos danos, deve haver também solidariedade na reparação. Nessa perspectiva, a presente dissertação tratará da coletivização da responsabilidade civil em relação à causa dos danos, na hipótese de responsabilidade grupal, e em referência à reparação dos danos em uma perspectiva convergente dos institutos do seguro e da responsabilidade civil.

Avaliação do cenário para utilização dos recursos florísticos nativos de restingas para inclusão socioeconômica em Caravelas, Bahia.

A conservação dos ecossistemas e dos recursos ambientais neles inclusos é uma condição básica e essencial para o desenvolvimento sustentado de uma dada região. A degradação faz com que a possibilidade dele retornar ao seu estado original seja ínfima pois, sua dinâmica de restauração não seria a mesma do que antes foi sua colonização. A recuperação de áreas degradadas é dificultada devido à complexidade estrutural dos ecossistemas, exemplo das restingas ambientes sujeitos as condições bastante adversas (altas temperaturas, períodos de seca, vento constante, alta salinidade e escassez de nutrientes), por isso demandam de alta tecnologia para o desenvolvimento e produção de mudas, além de alto custo associado. O objetivo deste estudo é a criação de uma proposta para uso socioeconômico das áreas degradadas por plantios de cocos, em formações vegetais de restinga, município de Caravelas, e criar um modelo para que essas áreas sejam mais produtivas economicamente, a médio e longo prazo, a partir da geração de trabalho e renda e, conseqüentemente, inclusão social voltada para o uso sustentável de espécies nativas de restinga, através do extrativismo, considerando-se o potencial e a vocação natural do ecossistema de restinga. Nesse contexto, as categorias de análise desta tese basearam-se nos conflitos e vulnerabilidade socioambiental, etnobotânica, fitofisionomias, bens e serviços associados, tecnologia social, desenvolvimento local, gestão costeira, sustentabilidade ambiental e democrática, produtos florestais não madeiráveis e inclusão social. Os procedimentos metodológicos utilizados neste estudo foram apresentados em cada capítulo desta tese, estando inserido em pesquisas qualitativas (técnicas de observação participante e análise do discurso coletivo) associada aos levantamentos bibliográficos (dados secundários) e as pesquisas quantitativas, por entrevistas semiestruturadas. Os resultados deste estudo subsidiaram a formação de uma rede interativa para implantação de empreendimentos sustentáveis no processo produtivo local, no que se refere à utilização de espécies nativas de restingas com reflorestamento de áreas degradadas por plantios de coco, para fins de geração de trabalho e renda com base no movimento de tecnologia social.

Vegetação e arquitetura das espécies de restinga associadas à ocorrência de Formicivora littoralis (Aves,Thamnophilidae)

O presente estudo teve como objetivo central conhecer a composição florística, a estrutura e a arquitetura das espécies da formação arbustiva fechada pós-praia e investigar possíveis associações com Formicivora littoralis, considerando tática de forrageamento, construção de ninhos e abundância da ave. F. littoralis é endêmica de restingas, e está ameaçada de extinção devido a perda acelerada de habitat. Entretanto, pouco se sabe sobre a vegetação em que ela ocorre, principalmente sobre as áreas de maior abundância da ave localizadas na formação Arbustiva Fechada Pós-praia (AFP) da Restinga da Massambaba, as quais estão inseridas em um Centro de Diversidade Vegetal (CDV) na Região de Cabo Frio. Diante disto, este estudo foi realizado em dois trechos desta formação na Restinga da Massambaba, nos municípios de Araruama e Arraial do Cabo, RJ, Brasil. Foram efetuadas 60 excursões a campo, com coletas aleatórias realizadas ao longo de toda a formação, geração de 20 parcelas de 2x50 m (0,2ha) perpendiculares ao mar, incluindo na amostragem indivíduos com DAP e DAS ≥2,5, estes, foram ainda categorizados em modelos de arquitetura de ramificação considerando número de ramos em dois patamares de altura (DAP e DAS). O levantamento florístico resultou em 327 coletas de 160 espécies, sendo pelo menos 12 espécies vegetais sob algum estado de ameaça, inclusive redescoberta uma Salicaceae (Casearia sessiliflora). Orchidaceae, Leguminosae e Myrtaceae foram as famílias mais ricas. Foram acrescentados 75% mais espécies na lista preliminar da AFP na Massambaba, além de 14 novos registros para o CDV de Cabo Frio. Na estrutura e arquitetura foram analisados 906 indivíduos de 58 espécies. Sendo os maiores valores de importância de Pilosocereus arrabidae (42,30) e Chrysophyllum lucentifolium (23,45). A diversidade de Shannon foi de 3,46 e equabilidade de 0,85. A arquitetura da maior parte dos indivíduos foi complexa, 58% de indivíduos com múltiplas ramificações, e as espécies apresentando variados padrões de ramificação. A densidade populacional de F. littoralis na AFP foi elevada, sendo estimada em 172 ind/km2. A arquitetura da AFP tem influência na ecologia da ave, pois ela foi generalista quanto à espécie utilizada como suporte na construção de ninhos e também para as táticas de forrageamento, mas houve seleção de ramos finos que formavam na horizontal ângulos de até 90 de abertura para construir ninhos. Ramos finos e mais horizontais também foram utilizados com frequência para as táticas de forrageamento. A abundância de F. littoralis esteve correlacionada positivamente à diversidade vegetal e negativamente à altura da vegetação, características marcantes nesta formação. Além disso, elevada taxa de vegetais com síndrome de dispersão zoocórica indica a importância desta formação na oferta de recursos alimentícios para a fauna e atração de pequenos artrópodes, os quais fazem parte da dieta de F. littoralis.

Cook Inlet Belugas, Delphinapterus leucas: Status and Overview

Of the five populations of beluga, Delphinapterus leucas, in Alaska, the most isolated is the one in Cook Inlet (Hazard, 1988; Hill and DeMaster, 1998) (Fig. 1). The geographic and genetic segregation of this stock (O’Corry-Crowe et al., 1997), combined with the beluga’s tendency toward site fidelity in summer, makes this population especially vulnerable to impacts from large or persistent harvests.

Beluga, Delphinapterus leucas, Habitat Associations in Cook Inlet, Alaska

A review of available information describing habitat associations for belugas, Delphinapterus leucas, in Cook Inlet was undertaken to complement population assessment surveys from 1993-2000. Available data for physical, biological, and anthropogenic factors in Cook Inlet are summarized followed by a provisional description of seasonal habitat associations. To summarize habitat preferences, the beluga summer distribution pattern was used to partition Cook Inlet into three regions. In general, belugas congregate in shallow, relatively warm, low-salinity water near major river outflows in upper Cook Inlet during summer (defined as their primary habitat), where prey availability is comparatively high and predator occurrence relatively low. In winter, belugas are seen in the central inlet, but sightings are fewer in number, and whales more dispersed compared to summer. Belugas are associated with a range of ice conditions in winter, from ice-free to 60% ice-covered water. Natural catastrophic events, such as fires, earthquakes, and volcanic eruptions, have had no reported effect on beluga habitat, although such events likely affect water quality and, potentially, prey availability. Similarly, although sewage effluent and discharges from industrial and military activities along Cook Inlet negatively affect water quality, analyses of organochlorines and heavy metal burdens indicate that Cook Inlet belugas are not assimilating contaminant loads greater than any other Alaska beluga stocks. Offshore oil and gas activities and vessel traffic are high in the central inlet compared with other Alaska waters, although belugas in Cook Inlet seem habituated to these anthropogenic factors. Anthropogenic factors that have the highest potential negative impacts on belugas include subsistence hunts (not discussed in this report), noise from transportation and offshore oil and gas extraction (ship transits and aircraft overflights), and water quality degradation (from urban runoff and sewage treatment facilities). Although significant impacts from anthropogenic factors other than hunting are not yet apparent, assessment of potential impacts from human activities, especially those that may effect prey availability, are needed.

Development of Beluga, Delphinapterus leucas, Capture and Satellite Tagging Protocol in Cook Inlet, Alaska

Attempts to capture and place satellite tags on belugas, Delphinapterus leucas, in Cook Inlet, Alaska were conducted during late spring and summer of 1995, 1997, and 1999. In 1995, capture attempts using a hoop net proved impractical in Cook Inlet. In 1997, capture efforts focused on driving belugas into nets. Although this method had been successful in the Canadian High Arctic, it failed in Cook Inlet due to the ability of the whales to detect and avoid nets in shallow and very turbid water. In 1999, belugas were successfully captured using a gillnet encirclement technique. A satellite tag was attached to a juvenile male, which subsequently provided the first documentation of this species’ movements within Cook Inlet during the summer months (31 May–17 September).

A pilot survey of deepwater coral/sponge assemblages and their susceptibility to fishing/harvest impacts at the Olympic Coast National Marine Sanctuary (OCNMS). Cruise report for NOAA Ship McARTHUR II Cruise AR-04-04: Leg 2 (June 1-12, 2004)

The offshore shelf and canyon habitats of the OCNMS are areas of high primary productivity and biodiversity that support extensive groundfish fisheries. Recent acoustic surveys conducted in these waters have indicated the presence of hard-bottom substrates believed to harbor unique deep-sea coral and sponge assemblages. Such fauna are often associated with shallow tropical waters, however an increasing number of studies around the world have recorded them in deeper, cold-water habitats in both northern and southern latitudes. These habitats are of tremendous value as sites of recruitment for commercially important fishes. Yet, ironically, studies have shown how the gear used in offshore demersal fishing, as well as other commercial operations on the seafloor, can cause severe physical disturbances to resident benthic fauna. Due to their exposed structure, slow growth and recruitment rates, and long life spans, deep-sea corals and sponges may be especially vulnerable to such disturbances, requiring very long periods to recover. Potential effects of fishing and other commercial operations in such critical habitats, and the need to define appropriate strategies for the protection of these resources, have been identified as a high-priority management issue for the sanctuary.

Disturbance climate in the Columbia River Basin [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): Climatological events that disturb a landscape are important components in ecosystem processes. Modern ecosystem management plans now hope to incorporate knowledge of the spatial distribution and frequency of disturbance climate. The following describes a few analytic tools developed to help managers include disturbance climate in an ecosystem management plan for areas in the Columbia River Basin of the northwestern United States.

Electroabsoorption-modulated laser light-source module using selective area growth for 10 Gb/s transmission

In this work, a novel light source of strained InGaAsP/InGaAsP MQW EAM monolithically integrated with DFB laser is fabricated by ultra-low-pressure (22 x 10(2) Pa) selective area growth ( SAG) MOCVD technique. Superior device performances have been obtained, sue h as low threshold current of 19 mA, output light power of about 7 mW, and over 16 dB extinction ratio at 5 V applied voltage when coupled into a single mode fiber. Over 10 GHz 3 dB bandwidth in EAM part is developed with a driving voltage of 3 V. After the chip is packaged into a 7-pin butterfly compact module, 10-Gb/s NRZ transmission experiments are successfully performed in standard fiber. A clearly-open eye diagram is achieved in the module output with over 8.3 dB dynamic extinction ratio. Power penalty less than 1.5 dB has been obtained after transmission through 53.3 km of standard fiber, which demonstrates that high-speed, low chirp EAM/DFB integrated light source can be obtained by ultra-low-pressure (22 x 102 Pa) SAG method.

A switch-on mechanism to activate maize ribosome-inactivating protein for targeting HIV-infected cells

Maize ribosome-inactivating protein (RIP) is a plant toxin that inactivates eukaryotic ribosomes by depurinating a specific adenine residue at the a-sarcin/ricin loop of 28S rRNA. Maize RIP is first produced as a proenzyme with a 25-amino acid internal inactivation region on the protein surface. During germination, proteolytic removal of this internal inactivation region generates the active heterodimeric maize RIP with full N-glycosidase activity. This naturally occurring switch-on mechanism provides an opportunity for targeting the cytotoxin to pathogen-infected cells. Here, we report the addition of HIV-1 protease recognition sequences to the internal inactivation region and the activation of the maize RIP variants by HIV-1 protease in vitro and in HIV-infected cells. Among the variants generated, two were cleaved efficiently by HIV-1 protease. The HIV-1 protease-activated variants showed enhanced N-glycosidase activity in vivo as compared to their un-activated counterparts. They also possessed potent inhibitory effect on p24 antigen production in human T cells infected by two HIV-1 strains. This switch-on strategy for activating the enzymatic activity of maize RIP in target cells provides a platform for combating pathogens with a specific protease.

Studies on the nature of the macromolecular condensed state of "nascent" ultra high molar mass polyethylene

Ultra high molar mass polyethylene (UHPE) powder as polymerized in a slurry process has been studied, in its nascent state, after recrystallization on rapid cooling from the melt and after hot compression molding to a film, by DSC, effect of annealing the recrystallized specimen at 120 similar to 130 degreesC, morphology by polarizing optical microscopy and small angle X-ray scattering. Based on the experimental results obtained the macromolecular condensed state of the nascent UHPE powder is a rare case of a multi-chain condensed state of non-interpenetrating chains, involving interlaced extended chain crystalline layers and relaxed parallel chain amorphous layers. On melting, a nematic rubbery state of nanometer size domain resulted. The nematic-isotropic transition temperature was judged from literature data to be at least 220 degreesC, possibly higher than 300 degreesC, the exact temperature is however not sue because of chain degradation at such high temperatures. The recrystallization process from the melt is a crystallization from a nematic rubbery state. The drop of remelting peak temperature by 10 K of the specimen recrystallized from its melt as compared to the nascent state has its origin in the decrease both of the crystalline chain stem length and of the degree of crystallinity. The remelting peak temperature could be returned close to that of the nascent state by annealing at 120 similar to 130 degreesC.

Characterization of a homogeneous taxonomic group of marine magnetotactic cocci within a low tide zone in the China Sea

Magnetotactic bacteria are a heterologous group of motile prokaryotes, ubiquitous in aquatic habitats and cosmopolitan in distribution. Here, we studied the diversity of magnetotactic bacteria in a seawater pond within an intertidal zone at Huiquan Bay in the China Sea. The pond is composed of a permanently submerged part and a low tide subregion. The magnetotactic bacteria collected from the permanently submerged part display diversity in morphology and taxonomy. In contrast, we found a virtually homogenous population of ovoid-coccoid magnetotactic bacteria in the low tide subregion of the pond. They were bilophotrichously flagellated and exhibited polar magnetotactic behaviour. Almost all cells contained two chains of magnetosomes composed of magnetite crystals. Intriguingly, the combination of restriction fragment length polymorphism analysis (RFLP) and sequencing of cloned 16S rDNA genes from the low tide subregion samples as well as fluorescence in situ hybridization (FISH) revealed the presence of a homogenous population. Moreover, phylogenetic analysis indicated that the Qingdao Huiquan low tide magnetotactic bacteria belong to a new genus affiliated with the alpha-subclass of Proteobacteria. This finding suggests the adaptation of the magnetotactic bacterial population to the marine tide.