Evolução de sistemas de solos laterítico e podzolizado: inferências sobre a forma atual da vertente-bacia do Alto Rio Preto - MG

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Revisão taxonômica de Tometes Valenciennes, 1850 (Characiformes: Serrasalmidae) das drenagens do Escudo das Guianas

O gênero Tometes Valenciennes, 1850 foi descrito originalmente para abrigar a espécie-tipo T. trilobatus, por apresentar dentes incisiformes bi- a tricuspidados. No entanto, o gênero foi colocado como sinonímia de Myleus Müller e Troschell, 1844 onde ficou por aproximadamente um século e meio até a sua revalidação. A revalidação do gênero e da espécie-tipo propiciou a descrição de outras duas espécies, T. lebaili e T. makue. O presente estudo apresenta uma revisão taxonômica de Tometes para o escudo das Guianas onde as três espécies nominais são reconhecidas válidas e aqui re-descritas, e uma nova espécie para a bacia do rio Trombetas foi caracterizada, ampliando a diversidade e a área de distribuição do gênero. Dentre as características principais de diagnose das espécies foi observado: T. trilobatus é diagnosticado dos demais congêneres por apresentar dentes no dentário e pré-maxilar com cúspide central com cume baixo e arredondado (vs. dentes com cúspide central ou cúspide principal com cume alto e agudo). T. lebaili é diferenciado por apresentar boca oblíqua orientada dorsalmente (vs. boca terminal). T. makue possui o menor número de espinhos na serra pré-pélvica, sempre entre 0 e 9 espinhos pré-pélvicos (vs. mais de 9 espinhos pré-pélvicos). Já a espécie nova apresenta o perfil dorsal do neurocrânio com uma suave concavidade ao nível da barra epifiseal e tamanho de escamas irregulares sobre o flanco (vs. perfil dorsal do neurocrânio retilíneo e escamas de tamanho regular sobre todo o flanco). Todas as espécies de Tometes são estritamente reofílicas e ocorrem exclusivamente nas zonas encachoeiradas dos rios de escudo, biótopos complexos, frágeis e ameaçados por ações antropogênicas. As conclusões deste estudo destacam o desafio urgente quanto à compreensão das relações espécies/habitat.

Tometes camunani (Characiformes: Serrasalmidae), a new species of phytophagous fish from the Guiana Shield, rio Trombetas basin, Brazil

Uma espécie nova de Serrasalmidae, Tometes camunani, é descrita para as drenagens superiores da bacia do rio Trombetas, estado do Pará, Brasil. A espécie nova distingue-se dos congêneres pela presença de uma ligeira concavidade no neurocrânio na altura do frontal (vs. concavidade ausente, perfil dorsal do neurocrânio reto). Também pode ser adicionalmente distinguido dos seus congêneres por possuir dentes com a cúspide central mais alta e cume agudo (vs. cúspide central mais baixa e com cume arredondado em T. trilobatus), a boca terminal (vs. boca orientada para cima em T. lebaili), e 12-26 espinhos pré-pélvicos (vs. 0-9 em T. makue). A espécie nova é estritamente reofílica, como as demais espécies de Tometes, e ocorre exclusivamente nas zonas encachoeiradas dos rios de escudo, biótopos complexos, frágeis e ameaçados por ações antropogênicas. Uma chave de identificação para as espécies do grupo Myleus é apresentada.

Geologia, petrografia e geoquímica dos granitóides arqueanos de Sapucaia - Província Carajás-PA

Os estudos geológicos desenvolvidos na porção leste do Subdomínio de Transição, Província Carajás, a sul da cidade de Canaã dos Carajás e a norte de Sapucaia, permitiram a identificação, individualização e caracterização de uma diversidade de unidades arqueanas, anteriormente englobadas no Complexo Xingu. A unidade mais antiga da área compreende anfibólio tonalitos correlacionados ao Tonalito São Carlos (~2,92 Ga), com foliação orientada segundo NW-SE a E-W, ou, por vezes, aspecto homogêneo. Geoquimicamente, diferem das típicas associações tonalito-trondhjemito-granodiorito (TTG) arqueanas por apresentarem enriquecimento em TiO₂, MgO e CaO, baixos teores de Sr e similares de Rb para amostras com menores teores de sílica, que se refletem em razões Rb/Sr mais elevadas e Sr/Ba mais baixas. Os padrões dos ETR mostram baixo a moderado fracionamento de ETR pesados em relação aos leves, e anomalias negativas de Eu discretas ou moderadas. Seguindo na estratigrafia, e também como a unidade de maior expressão na área, ocorrem rochas de afinidade TTG correspondentes ao Trodhjemito Colorado (~2,87 Ga), intensamente deformadas, com foliações NW-SE a E-W. Intrusivos nesta unidade, ao sul da área, aflora um corpo de aproximadamente 40 km², de rochas de composição leucogranodiorítica porfirítica denominados de Leucogranodiorito Pantanal, e seccionado em sua porção oeste por leucogranitos deformados de composição monzogranítica. O Leucogranodiorito Pantanal têm afinidade cálcio-alcalina peraluminosa, enriquecimento em Ba e Sr, e padrões de ETR sem anomalias expressivas de Eu e com acentuado fracionamento de ETRP, que refletem em altas razões La/Yb semelhante com a Suíte Guarantã (~2,87 Ga) do Domínio Rio Maria. Os leucogranitos revelam assinatura geoquímica de granitos tipo-A reduzidos, possivelmente, originados a partir da fusão desidratada de rochas cálcico-alcalinas peraluminosas durante o Neoarqueano. Além dessas unidades, na porção leste do Leucogranodiorito Pantanal, hornblenda-biotita granito neoarquenos tipo-A oxidados da Suíte Vila Jussara. Ainda correlacionáveis ao magmatismo subalcalino neoarqueano, na porção norte, ocorrem dois stocks graniticos. São tonalitos a granodioritos com assinatura geoquímica de granitos tipo-A oxidados similares a Suíte Vila Jussara, e monzogranitos com assinatura de granitos tipo-A reduzidos que se assemelham a Suíte Planalto. Ao norte da área ocorre uma associação máfico-enderbitica composta de hornblendanoritos, piroxênio-hornblenda-gabros, piroxênio-hornblenda-monzonito, hornblenda-gabros, anfibolitos e enderbitos. Essas rochas estão intensamente deformadas e recristalizadas, provavelmente por retrometamorfismo na presença de água de rochas de série noríticavii charnockítica de origem ígnea associada com outras variedades de rochas não necessariamente cogenéticas. Seu comportamento geoquímico sugere que os hornblendanorito, hornblenda-gabros e anfibolitos são toleíticos subalcalinos, enquanto que os enderbitos, piroxênio-hornblenda-gabro e piroxênio-hornblenda-monzonito têm assinatura cálcico-alcalina. As baixas razões La/Yb das rochas máficas indicam baixo grau de fracionamento, enquanto que as altas razões La/Yb dos enderbitos é indicativo de fracionamento expressivo dos ETR pesados durante a formação ou diferenciação dos seus magmas, e a concavidade no padrão de ETR pesados, indica provável influência de fracionamento de anfibólio durante sua evolução. Na porção central e centro-norte da área ocorrem biotita-monzogranitos peraluminosos, de assinatura cálcio-alcalina, que podem ser desdobrados em dois grupos geoquímicos distindo. Um tem altas razões Sr/Y e (La/Yb)n, mostram possível afinidade com o Granito Bom Jesus da área de Canaã dos Carajás. O outro tem mais baixa razão (La/Yb)n se aproxima mais do Granito Serra Dourada e do Granito Cruzadão também da área de Canaã dos Carajás. Essa comparação deverá ser aprofundada com dados geocronológicos e maior número de amostras.

325 degrees C thermoluminescence peak growth in quartz related to oxygen vacancies

The thermoluminescence intensity as a function of gamma-ray dose of the 325 degreesC peak, in quartz grains extracted from sea sediments and from fluvial aeolic dunes, is studied. It is found that the response curve at low doses has a concavity directed opposite to that of quartz grains extracted from archaeological potteries. To explain this behavior a model is proposed here based on oxygen vacancies and [AlO4/h](0) centers. The experimentally observed ESR intensity of E-I'-centers as a function of radiation dose can also be explained by this model.

Osteologia craniana comparada de Caracara cheriway (Jacquin, 1784) e Caracara plancus (Miller, 1777) (AVES: FALCONIDAE)

The Caracara genus (Aves: Falconidae) is composed by species C. cheriway, ("Crested Caracara"), and C. plancus (Southern Caracara). This study aimed to describe in detail and compared the cranial osteology of C. cheriway and C. plancus, identifying osteological cranial characters for a future systematic work. The two common characters of Caracara species are: the projection of rostro parasphenoid reaches 50% of the distance from the occipital condyle to the pterygoid; the upper maxilla has about 4/9 of the total length of theskull, the symphysial portion of mandible occupies about 1/7 of its total length, the proximal portion of lacrimal bone ends in a rounded shape and has about 1/4 of the width of the distal portion. The unique characters of C. cheriway are: the interorbital width is about 1/2 of the parietal region, shows a frontal bone prominence; presence of lacrimal process of frontal bone; the proximal portion of the lacrimal bone reaches 1/5 of the distance from the orbital arc to the jugal bone; the distance between the distal portions of two lacrimal bones reach 5/6 of the parietal width, the ratio between the interorbital diameter and parietal region ranges from 2 times; the zygomatic process occupies about 40% of the distance between its origin in the skull and jugal bone. The unique characters of C. plancus are: the interorbital width is approximately 4/7 of the parietal width; show a rostral medial concavity; the proximal portion of the lacrimal bone is about 1/4 of the width of the distal; the proximal portion of the lacrimal bone reaches 1/7 of the distance from the orbital arc to the jugal bone; the distance between the distal portions of two lacrimal bones reaches 6/7 of the width parietal one; the ratio between the interorbital diameter and parietal region varies 1, 75 times, the zygomatic process occupies about 35% of the distance between its origin in the skull and jugal bone.

Building Math Esteem in Fifth Grade Students

In this action research study of my classroom of 5th grade mathematics, I investigate the levels of math esteem in each student and as a classroom. The definition of esteem on which I am basing my research is the judgment or estimation of the self-assurance of a student in math. I discovered that several of the students entered my classroom with a middle to low level of esteem in math, and about a third of the class already exhibited a positive, high esteem in math. After implementation of the research, and interpreting the data, I believe almost all the students achieved higher math esteem by the end of the school year. The surveys and interviews I performed with the parents and students lead me to believe the four components of my research had an affect on this outcome. As a result of this research, I plan to continue to facilitate a high level of math esteem in each one of my students.

Generators of supersymmetric polynomials in positive characteristic

In Kantor and Trishin (1997) [3], Kantor and Trishin described the algebra of polynomial invariants of the adjoint representation of the Lie superalgebra gl(m vertical bar n) and a related algebra A, of what they called pseudosymmetric polynomials over an algebraically closed field K of characteristic zero. The algebra A(s) was investigated earlier by Stembridge (1985) who in [9] called the elements of A(s) supersymmetric polynomials and determined generators of A(s). The case of positive characteristic p of the ground field K has been recently investigated by La Scala and Zubkov (in press) in [6]. We extend their work and give a complete description of generators of polynomial invariants of the adjoint action of the general linear supergroup GL(m vertical bar n) and generators of A(s).

Partial projective representations and partial actions II

This paper is a continuation of Dokuchaev and Novikov (2010) [8]. The interaction between partial projective representations and twisted partial actions of groups considered in Dokuchaev and Novikov (2010) [8] is treated now in a categorical language. In the case of a finite group G, a structural result on the domains of factor sets of partial projective representations of G is obtained in terms of elementary partial actions. For arbitrary G we study the component pM'(G) of totally-defined factor sets in the partial Schur multiplier pM(G) using the structure of Exel's semigroup. A complete characterization of the elements of pM'(G) is obtained for algebraically closed fields. (C) 2011 Elsevier B.V. All rights reserved.

Erosione e sollevamento nell'arco calabro-peloritano

The Calabrian-Peloritani arc represents key site to unravel evolution of surface processes on top of subducting lithosphere. During the Pleistocene, in fact the arc uplifted at rate of the order of about 1mm/yr, forming high-standing low-relief upland (figure 2). Our study is focused on the relationship between tectonic and land evolution in the Sila Massif, Messina strait and Peloritani Mts. Landforms reflect a competition between tectonic, climatic, and surficial processes. Many landscape evolution models that explore feedbacks between these competing processes, given steady forcing, predict a state of erosional equilibrium, where the rates of river incision and hillslope erosion balance rock uplift. It has been suggested that this may be the final constructive stage of orogenic systems. Assumptions of steady erosion and incision are used in the interpretation of exhumation and uplift rates from different geologic data, and in the formulation of fluvial incision and hillslope evolution models. In the Sila massif we carried out cosmogenic isotopes analysis on 24 samples of modern fluvial sediments to constrain long-term (~103 yr) erosion rate averaged on the catchment area. 35 longitudinal rivers profiles have been analyzed to study the tectonic signal on the landscape evolution. The rivers analyzed exhibit a wide variety of profile forms, diverging from equilibrium state form. Generally the river profiles show at least 2 and often 3 distinct concave-up knickpoint-bounded segments, characterized by different value of concavity and steepness indices. River profiles suggest three main stages of incision. The values of ks and θ in the lower segments evidence a decrease in river incision, due probably to increasing uplift rate. The cosmogenic erosion rates pointed out that old landscape upland is eroding slowly at ~0.1 mm/yr. In the contrary, the flanks of the massif is eroding faster with value from 0.4 to 0.5 mm/yr due to river incision and hillslope processes. Cosmogenic erosion rates mach linearly with steepness indices and with average hillslope gradient. In the Messina area the long term erosion rate from low-T thermochronometry are of the same order than millennium scale cosmogenic erosion rate (1-2 mm/yr). In this part of the chain the fast erosion is active since several million years, probably controlled by extensional tectonic regime. In the Peloritani Mts apatite fission-track and (U-Th)/He thermochronometry are applied to constraint the thermal history of the basement rock. Apatite fission-track ages range between 29.0±5.5 and 5.5±0.9 Ma while apatite (U-Th)/He ages vary from 19.4 to 1.0 Ma. Most of the AFT ages are younger than the overlying terrigenous sequence that in turn postdates the main orogenic phase. Through the coupling of the thermal modelling with the stratigraphic record, a Middle Miocene thermal event due to tectonic burial is unravel. This event affected a inner-intermediate portion of the Peloritani belt confined by young AFT data (<15 Ma) distribution. We interpret this thermal event as due to an out-of–sequence thrusting occurring in the inner portion of the belt. Young (U-Th)/He ages (c. 5 Ma) record a final exhumation stage with increasing rates of denudation since the Pliocene times due to postorogenic extensional tectonics and regional uplift. In the final chapter we change the spatial scale to insert digital topography analysis and field data within a geodynamic model that can explain surface evidence produced by subduction process.

Fish quality assessment through the application of chemico-physical, sensory and microbiological analyses

The quality of fish products is indispensably linked to the freshness of the raw material modulated by appropriate manipulation and storage conditions, specially the storage temperature after catch. The purpose of the research presented in this thesis, which was largely conducted in the context of a research project funded by Italian Ministry of Agricultural, Food and Forestry Policies (MIPAAF), concerned the evaluation of the freshness of farmed and wild fish species, in relation to different storage conditions, under ice (0°C) or at refrigeration temperature (4°C). Several specimens of different species, bogue (Boops boops), red mullet (Mullus barbatus), sea bream (Sparus aurata) and sea bass (Dicentrarchus labrax), during storage, under the different temperature conditions adopted, have been examined. The assessed control parameters were physical (texture, through the use of a dynamometer; visual quality using a computer vision system (CVS)), chemical (through footprint metabolomics 1H-NMR) and sensory (Quality Index Method (QIM). Microbiological determinations were also carried out on the species of hake (Merluccius merluccius). In general obtained results confirmed that the temperature of manipulation/conservation is a key factor in maintaining fish freshness. NMR spectroscopy showed to be able to quantify and evaluate the kinetics for unselected compounds during fish degradation, even a posteriori. This can be suitable for the development of new parameters related to quality and freshness. The development of physical methods, particularly the image analysis performed by computer vision system (CVS), for the evaluation of fish degradation, is very promising. Among CVS parameters, skin colour, presence and distribution of gill mucus, and eye shape modification evidenced a high sensibility for the estimation of fish quality loss, as a function of the adopted storage conditions. Particularly the eye concavity index detected on fish eye showed a high positive correlation with total QIM score.

Multilevel Domain Decomposition Algorithms for Monolithic Fluid-Structure Interaction Problems with Application to Haemodynamics

Finite element techniques for solving the problem of fluid-structure interaction of an elastic solid material in a laminar incompressible viscous flow are described. The mathematical problem consists of the Navier-Stokes equations in the Arbitrary Lagrangian-Eulerian formulation coupled with a non-linear structure model, considering the problem as one continuum. The coupling between the structure and the fluid is enforced inside a monolithic framework which computes simultaneously for the fluid and the structure unknowns within a unique solver. We used the well-known Crouzeix-Raviart finite element pair for discretization in space and the method of lines for discretization in time. A stability result using the Backward-Euler time-stepping scheme for both fluid and solid part and the finite element method for the space discretization has been proved. The resulting linear system has been solved by multilevel domain decomposition techniques. Our strategy is to solve several local subproblems over subdomain patches using the Schur-complement or GMRES smoother within a multigrid iterative solver. For validation and evaluation of the accuracy of the proposed methodology, we present corresponding results for a set of two FSI benchmark configurations which describe the self-induced elastic deformation of a beam attached to a cylinder in a laminar channel flow, allowing stationary as well as periodically oscillating deformations, and for a benchmark proposed by COMSOL multiphysics where a narrow vertical structure attached to the bottom wall of a channel bends under the force due to both viscous drag and pressure. Then, as an example of fluid-structure interaction in biomedical problems, we considered the academic numerical test which consists in simulating the pressure wave propagation through a straight compliant vessel. All the tests show the applicability and the numerical efficiency of our approach to both two-dimensional and three-dimensional problems.

Clinical results with two different methods of root-end preparation and filling in apical surgery: mineral trioxide aggregate and adhesive resin composite

INTRODUCTION: The aim of apical surgery is to hermetically seal the root canal system after root-end resection, thereby enabling periradicular healing. The objective of this nonrandomized prospective clinical study was to report results of 2 different root-end preparation and filling methods, ie, mineral trioxide aggregate (MTA) and an adhesive resin composite (Retroplast). METHODS: The study included 353 consecutive cases with endodontic lesions limited to the periapical area. Root-end cavities were prepared with sonic microtips and filled with MTA (n = 178), or alternatively, a shallow concavity was prepared in the cut root face, with subsequent placement of an adhesive resin composite (Retroplast) (n = 175). Patients were recalled after 1 year. Cases were defined as healed when no clinical signs or symptoms were present and radiographs demonstrated complete or incomplete (scar tissue) healing of previous radiolucencies. RESULTS: The overall rate of healed cases was 85.5%. MTA-treated teeth demonstrated a significantly (P = .003) higher rate of healed cases (91.3%) compared with Retroplast-treated teeth (79.5%). Within the MTA group, 89.5%-100% of cases were classified as healed, depending on the type of treated tooth. In contrast, more variable rates ranging from 66.7%-100% were found in the Retroplast group. In particular, mandibular premolars and molars demonstrated considerably lower rates of healed cases when treated with Retroplast. CONCLUSIONS: MTA can be recommended for root-end filling in apical surgery, irrespective of the type of treated tooth. Retroplast should be used with caution for root-end sealing in apical surgery of mandibular premolars and molars.

Modeling Yield Surfaces of Various Structural Shapes

This study investigates the possibility of custom fitting a widely accepted approximate yield surface equation (Ziemian, 2000) to the theoretical yield surfaces of five different structural shapes, which include wide-flange, solid and hollow rectangular, and solid and hollow circular shapes. To achieve this goal, a theoretically “exact” but overly complex representation of the cross section’s yield surface was initially obtained by using fundamental principles of solid mechanics. A weighted regression analysis was performed with the “exact” yield surface data to obtain the specific coefficients of three terms in the approximate yield surface equation. These coefficients were calculated to determine the “best” yield surface equation for a given cross section geometry. Given that the exact yield surface shall have zero percentage of concavity, this investigation evaluated the resulting coefficient of determination (

The influence of bedrock orientation on the landscape evolution, surface morphology and denudation (10Be) at the Niesen, Switzerland

Landscape evolution and surface morphology in mountainous settings are a function of the relative importance between sediment transport processes acting on hillslopes and in channels, modulated by climate variables. The Niesen nappe in the Swiss Penninic Prealps presents a unique setting in which opposite facing flanks host basins underlain by identical lithologies, but contrasting litho-tectonic architectures where lithologies either dip parallel to the topographic slope or in the opposite direction (i.e. dip slope and non-dip slope). The north-western facing Diemtigen flank represents such a dip slope situation and is characterized by a gentle topography, low hillslope gradients, poorly dissected channels, and it hosts large landslides. In contrast, the south-eastern facing Frutigen side can be described as non-dip slope flank with deeply incised bedrock channels, high mean hillslope gradients and high relief topography. Results from morphometric analysis reveal that noticeable differences in morphometric parameters can be related to the contrasts in the relative importance of the internal hillslope-channel system between both valley flanks. While the contrasting dip-orientations of the underlying flysch bedrock has promoted hillslope and channelized processes to contrasting extents and particularly the occurrence of large landslides on the dip slope flank, the flank averaged beryllium-10 (10Be)-derived denudation rates are very similar and range between 0.20 and 0.26 mm yr−1. In addition, our denudation rates offer no direct relationship to basin's slope, area, steepness or concavity index, but reveal a positive correlation to mean basin elevation that we interpret as having been controlled by climatically driven factors such as frost-induced processes and orographic precipitation. Our findings illustrate that while the landscape properties in this part of the northern Alpine border can mainly be related to the tectonic architecture of the underlying bedrock, the denudation rates have a strong orographic control through elevation dependent mean annual temperature and precipitation.