Metalogenese dos depositos hidrotermais de metais-base e au do ciclo brasiliano no bloco São Gabriel, RS

Os depósitos de metais-base (Camaquã, Santa Maria e na Formação Passo Feio), e Au (Bossoroca) mais importantes do Rio Grande do Sul foram gerados durante o Ciclo Brasiliano ao longo de três eventos distintos, relacionados ao magmatismo e metamorfismo contemporâneos (700, 594 e 562 Ma); os metais foram derivados de fontes relacionadas à crosta juvenil e ao embasamento antigo. O depósito de ouro da Bossoroca (700 Ma) consiste de veios de quartzo com Au e subordinadamente pirita, calcopirita, galena e teluretos, sendo classificado como um depósito orogênico epizonal. Os filões de quartzo aurífero são hospedados por rochas, piroclásticas calcico-alcalinas de composição andesítica, dacítica com basaltos e epiclásticas subordinadas, pertencentes a Formação Campestre. Estudos do zircão através do método U-Pb via SHRIMP mostram que as rochas vulcânicas encaixantes foram geradas a cerca de 760 Ma atrás, no início do Ciclo Brasiliano, e sofreram metamorfismo regional de baixa pressão na transição entre os facies xistos verdes e anfibolito a cerca de 700 Ma. Os depósitos de metais-base do sistema Camaquã Cu (Au, Ag) e Santa Maria Pb-Zn (Cu, Ag) são hidrotermais magmáticos distantes, provavelmente ligados à intrusões graníticas, e foram gerados há cerca de 594 Ma durante o magmatismo pós-colisional do final da Orogenêse Dom Feliciano. As mineralizações de Cu (Au) e Pb hospedados pela Formação Passo Feio são hidrotermais epigenéticas e foram gerados há 562 Ma durante a intrusão do Granito Caçapava. A composição isotópica do Pb dos sulfetos dos depósitos de Camaquã-Santa Maria indica que os metais foram derivados de uma fonte crustal com Pb muito primitivo no final do Ciclo Brasiliano. A composição isotópica do enxofre dos sulfetos desses depósitos (~ 0‰ CDT) indica uma origem magmática para o enxofre. Os metais dos depósitos hidrotermais epigenéticos da Formação Passo Feio foram também derivados do embasamento antigo, com contribuição importante das rochas meta-vulcanosedimentares da Formação Passo Feio. O enxofre dessas mineralizações possui origem mista, originada pela mistura de fluidos magmáticos (Granito Caçapava) com enxofre derivado da lixiviação das meta-vulcanosedimentares da Formação Passo Feio. Os metais concentrados no depósito de Au da Bossoroca foram mobilizados durante o metamorfismo regional dinamotermal através da interação de fluidos de origem profunda que ascenderam através da pilha vulcanosedimentar extraindo Au e outros metais, e depositando-os em níveis crustais mais rasos em sítios estruturalmente favoráveis. A fonte do Pb determinada para o depósito de Au da Bossoroca é de origem profunda e corresponde a mesma fonte do magma de arco juvenil gerador das rochas vulcânicas do arco. Os isótopos de C-O mostram assinaturas compatíveis com uma fonte profunda para estes fluidos mineralizadores.

Metalogênese do depósito de Cu Cerro dos Martins, RS.

Este trabalho revisa a geologia e apresenta dados inéditos do Depósito de Cobre Cerro dos Martins (DCM), incluindo geocronologia Pb-Pb em zircão, inclusões fluidas, isótopos estáveis (C, O e S), composição isotópica do Sr e geoquímica de elementos maiores e traços das rochas vulcânicas encaixantes. O depósito está hospedado na seqüência vulcano-sedimentar do Grupo Bom Jardim, da Bacia do Camaquã, do Neoproterozóico do Escudo Sul Rio-grandense, e possui reservas calculadas de 1.450.000 t, com teor médio de 0,83% Cu. O depósito consiste de um conjunto de veios sulfetados que preenchem fraturas de direção N40º-60ºW em rochas andesíticas e sedimentares clásticas, com disseminações confinadas em níveis de siltito, arenito, andesito e conglomerado, da Formação Hilário do Grupo Bom Jardim. Os minerais do minério filoneano são a calcosina e bornita com calcopirita, pirita, galena e esfalerita subordinadas. Digenita, covelita, malaquita cuprita e azurita ocorrem como minério secundário em ganga constituída de carbonatos, quartzo, minerais argilosos, barita e rara hematita. A composição química das vulcânicas (elementos maiores e traços, incluindo ETR) indicam uma afinidade alcalina para o vulcanismo relacionado à Formação Hilário na região do Cerro dos Martins. Um corpo de quartzo-diorito, intrusivo nas rochas vulcânicas e sedimentares, mostrou idade de 550 ±5 Ma (Pb-Pb em zircões) indicando um valor mínimo para a geração do minério do DCM. Esta idade confirma a posição estratigráfica desta rocha na Formação Acampamento Velho e também fornece uma idade mínima para a deposição da seqüência vulcano-sedimentar encaixante do DCM. Os sulfetos do DCM mostram δS34 CDT com valores relativamente homogêneos entre - 6.2 e + 0.9‰ (n= 7). O valor de δS34 CDT da calcopirita, levemente positivo (+0.9‰), indica uma origem magmática para o S, mas os valores negativos encontrados nestes sulfetos, poderiam indicar o envolvimento de outras fontes com enxofre reduzido. Entretanto, a presença de hematita nas paragêneses minerais indica que o minério foi formado sob condições oxidantes, modificando a composição isotópica original do enxofre magmático (δS34 CDT ~ 0‰) para valores negativos. As baritas analisadas apresentam valores com δS34 CDT entre +9.25 e +10.65‰ (n=4) indicando deposição em condições oxidantes, originadas pela mistura de um fluido magmático-hidrotermal com água meteórica. A composição isotópica do C das calcitas do DCM varia com δC13 PDB entre - 1,90 a -4,45‰, interpretada como resultante da mistura entre carbono de fonte magmática com mármores do embasamento. Inclusões fluidas em quartzo do minério indicam temperaturas de deposição entre 157 e 273 °C com mediana de 215 °C (n = 45). A composição isotópica do oxigênio da água em equilibrio com a calcita do fluido hidrotermal (T= 215 °C) mostra valores de δ O18 SMOW entre 3 e 14, indicando H2O de origem magmática, com contribuição de água meteórica. A razão Sr87/Sr86 das mesmas calcitas mostram valores entre 0,7068 – 0,7087, de crosta superior. Rochas plutônicas e vulcânicas do escudo com idades próximas de 550 Ma possuem razões iniciais Sr87/Sr86 entre 0,704 – 0,710, compatíveis com aquelas encontradas nas calcitas da mineralização. Os fluidos hidrotermais do magmatismo shoshonítico-alcalino com idade de 595 Ma e Sr87/Sr86 entre 0,7041 a 0,7053, também são candidatos a fonte do Sr dos carbonatos hidrotermais, mas necessitariam de um componente mais radiogênico. Assim, a fonte de C-O e Sr das calcitas do minério pode ter sido originada diretamente de um fluido magmático-hidrotermal ou de uma mistura entre este fluido e mármores do embasamento. Portanto, o depósito Cerro dos Martins é interpretado como de origem magmática-hidrotermal, relacionado ao evento magmático alcalinoshoshonítico, pós-colisional da Orogênese Dom Feliciano, com idade entre 595-550 Ma. Novos modelos exploratórios para depósitos de cobre no Escudo do Rio Grande do Sul devem considerar o magmatismo alcalino na gênese dos depósitos.

Biological and structural characterization of a new PLA(2) from the Crotalus durissus collilineatus venom

In the present article we report on the biological characterization and amino acid sequence of a new basic Phospholipases A(2) (PLA(2)) isolated from the Crotalus durissus collilineatus venom (Cdcolli F6), which showed the presence of 122 amino acid residues with a pI value of 8.3, molecular mass of 14 kDa and revealed an amino acid sequence identity of 80% with crotalic PLA(2)s such as Mojave B, Cdt F15, and CROATOX. This homology, however, dropped to 50% if compared to other sources of PLA(2)s such as from the Bothrops snake venom. Also, this PLA(2) induced myonecrosis, although this effect was lower than that of BthTx-I or whole crotoxin and it was able to induce a strong blockage effect on the chick biventer neuromuscular preparation, independently of the presence of the acid subunid (crotapotin). The neurotoxic effect was strongly reduced by pre-incubation with heparin or with anhydrous acetic acid and rho-BPB showed a similar reduction. The rho-BPB did not reduce significantly the myotoxic activity induced by the PLA(2), but the anhydrous acetic acid treatment and the pre-incu-bation of PLA(2) with heparin reduced significantly its effects. This protein showed a strong antimicrobial activity against Xanthomonas axonopodis passiflorae (Gram-negative), which was drastically reduced by incubation of this PLA(2) with rho-BPB, but this effect was marginally reduced after treatment with anhydrous acetic acid. Our findings here allow to speculate that basic amino acid residues on the C-terminal and molecular regions near catalytic site regions such as Calcium binding loop or rho-wing region may be involved in the binding of this PLA(2) to the molecular receptor to induce the neurotoxic effect. The bactericidal effect, however, was completely dependent on the enzymatic activity of this protein.

Abdominal hyperalgesia in secretory phospholipase A(2)-induced rat pancreatitis: Distinct roles of NK1 receptors

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Enzymatic and structural characterization of new PLA2 isoform isolated from white venom of Crotalus durissus ruruima

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Vertical distribution of benthic invertebrate larvae during an upwelling event along a transect off the tropical Brazilian continental margin

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Inhibition of Neurotoxic Secretory Phospholipases A(2) Enzymatic, Edematogenic, and Myotoxic Activities by Harpalycin 2, an Isoflavone Isolated from Harpalyce brasiliana Benth

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Microbiological evaluation of different strategies for management of snakes in captivity

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Insights into the role of oligomeric state on the biological activities of crotoxin: crystal structure of a tetrameric phospholipase A(2) formed by two isoforms of crotoxin B from Cratalus durissus terrificus venom

Crotoxin B (CB or Cdt PLA(2)) is a basic Asp49-PLA(2) found in the venom of Crotalus durissus terrificus and it is one of the subunits that constitute the crotoxin (Cro). This heterodimeric toxin, main component of the C. d. terrificus venom, is completed by an acidic, nontoxic, and nonenzymatic component (crotoxin A, CA or crotapotin), and it is related to important envenomation effects such as neurological disorders, myotoxicity, and renal failure. Although Cro has been crystallized since 1938, no crystal structure of this toxin or its subunits is currently available. In this work, the authors present the crystal structure of novel tetrameric complex formed by two dimers of crotoxin B isoforms (CB1 and CB2). The results suggest that these assemblies are stable in solution and show that Ser1 and Glu92 of CB1 and CB2, respectively, play an important role in the oligomerization. The tetrameric and dimeric conformations resulting from the association of the isoforms may increase the neurotoxicity of the toxin CB by the creation of new binding sites, which could improve the affinity of the molecular complexes to the presynaptic membrane.

Balance, executive functions and falls in elderly with Alzheimer's disease (AD): A longitudinal study

Elderly individuals with AD are more susceptible to falls, which might be associated with decrements in their executive functions and balance, among other things. We aimed to analyze the effects of a program of dual task physical activity on falls, executive functions and balance of elderly individuals with AD. We studied 21 elderly with probable AD, allocated to two groups: the training group (TG), with 10 elderly who participated in a program of dual task physical activity; and the control group (CG), with 11 elderly who were not engaged in regular practice of physical activity. The Clock Drawing Test (CDT) and the Frontal Assessment Battery (FAB) were used in the assessment of the executive functions, while the Berg Balance Scale (BBS) and the Timed Up-and-Go (TUG)-test evaluated balance. The number of falls was obtained by means of a questionnaire. We observed a better performance of the TG as regards balance and executive functions. Moreover, the lower the number of steps in the TUG scale, the higher the scores in the CDT, and in the FAB. The practice of regular physical activity with dual task seems to have contributed to the maintenance and improvement of the motor and cognitive functions of the elderly with AD. (C) 2011 Elsevier B.V. All rights reserved.

Gait and risk of falls associated with frontal cognitive functions at different stages of Alzheimer's disease

The decline in frontal cognitive functions contributes to alterations of gait and increases the risk of falls in patients with dementia, a category which included Alzheimer's disease (AD). The objective of the present study was to compare the gait parameters and the risk of falls among patients at different stages of AD, and to relate these variables with cognitive functions. This is a cross-sectional study with 23 patients with mild and moderate AD. The Clinical Dementia Rating was used to classify the dementia severity. The kinematic parameters of gait (cadence, stride length, and stride speed) were analyzed under two conditions: (a) single task (free gait) and (b) dual task (walking and counting down). The risk of falls was evaluated using the Timed Up-and-Go test. The frontal cognitive functions were evaluated using the Frontal Assessment Battery (FAB), the Clock Drawing Test (CDT) and the Symbol Search Subtest. The patients who were at the moderate stage suffered reduced performance in their stride length and stride speed in the single task and had made more counting errors in the dual task and still had a higher fall risk. Both the mild and the moderate patients exhibited significant decreases in stride length, stride speed and cadence in the dual task. Was detected a significant correlation between CDT, FAB, and stride speed in the dual task condition. We also found a significant correlation between subtest Similarities, FAB and cadence in the dual task condition. The dual task produced changes in the kinematic parameters of gait for the mild and moderate AD patients and the gait alterations are related to frontal cognitive functions, particularly executive functions.

Comparative studies of the anti-leishmanial activity of three Crotalus durissus ssp venoms

In this study, we compared the anti-leishmanial activity of three crotalic venoms (Crotalus durissus terrificus-Cdt, Crotalus durissus cascavella-Cdca, and Crotalus durissus collilineatus-Cdcol). Different concentrations of each venom incubated with Leishmania (Leishmania) amazonensis promastigotes were used. Cdt venom exhibited a higher anti-leishmanial activity (Inhibitory concentration-IC50-value of 4.70 +/- 1.72 mu g/ml) in comparison with that of Cdca venom (IC50 value of 9.41 +/- 1.21 mu g/ml), while Cdcol venom increased parasite numbers in 50% at a concentration of 44.30 +/- 2.18 mu g/ml. In addition, this venom showed a low anti-leishmanial activity in higher concentrations (IC50 value of 281.00 +/- 9.50 mu g/ml). The main fractions of Cdca venom were isolated and assayed under similar conditions used for assessing crude venom. The most active fractions were gyroxin and crotamine that had IC50 values of 3.80 +/- 0.52 mu g/ml and 19.95 +/- 4.21 mu g/ml, respectively. Convulxin also inhibited parasite growth rate, although this effect was not dose-dependent. Crotoxin was the least effective fraction with an IC50 value of 99.80 +/- 2.21 mu g/ml. None of the protein fractions presented cytotoxic effects against J774 cells in culture. In vivo assays using BALB/c mice revealed that crotoxin and crotamine were the main toxic fractions. In conclusion, C. durissus cascavella venom has three main fractions with anti-leishmanial activity. These results open new possibilities to find proteins that might be used as possible agents against cutaneous leishmaniasis.

Distribution of I-125-labeled crotamine in mice tissues

Crotamine is a strong basic polypeptide from Crotalus durissus terrificus (Cdt) venom composed of 42 amino acid residues tightly bound by three disulfide bonds. It causes skeletal muscle spasms leading to spastic paralysis of hind limbs in mice. The objective of this paper was to study the distribution of crotamine injected intraperitoneally (ip) in mice. Crotamine was purified from Cdt venom by gel filtration, followed by ion exchange chromatography, using a fast-performance liquid chromatography (FPLC) system. Purified crotamine was irradiated at 2 kGy in order to detoxify. Both native and irradiated proteins were labeled with 125, using chloramine T method, and separated by get filtration. Male Swiss mice were injected ip with 0.1 mL (2 x 10(6) cpm/mouse) of I-125 native or irradiated crotamine. At various time intervals, the animals were killed by ether inhalation and blood, spleen, liver, kidneys, brain, lungs, heart, and skeletal muscle were collected in order to determine the radioactivity content. The highest levels of radioactivity were found in the kidneys and the liver, and the lowest in the brain. (c) 2006 Elsevier Ltd. All rights reserved.

Exercício, funcionalidade e distúrbios do sono em pacientes com doença de Parkinson

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Investigação de metástases não funcionantes em câncer de tireóide com sestamibi-99mTc e iodo-131: avaliação metodológica comparativa

Pós-graduação em Pesquisa e Desenvolvimento (Biotecnologia Médica) - FMB