Contribution of SHRIMP U-Pb zircon geochronology to unravelling the evolution of Brazilian Neoproterozoic fold belts

The South-American continent is constituted of three major geologic-geotectonic entities the homonym platform (consolidated at the end of the Cambrian) the Andean chain (essentially Meso-Cenozoic) and the Patagonian terrains affected by tectonism and magmatism through almost all of the Phanerozoic The platform is constituted by a series of cratonic nuclei (pre-Tonian fragments of the Rodinia fission) surrounded by a complex fabric of Neoproterozoic structural provinces Two major groups of orogenic processes (plate interaction cycles) constitute the evolution of these provinces the older occurred in the Tonian (smaller in area) and the younger Brasiliano that is present in all provinces The Tonian cycles (pre-Rodinia fission?) are still being sorted out and many questions still need to be answered The Brasiliano orogenic collage events (post-Rodinia fission?) developed in three main stages in part coeval from a province to another and are 650-600 580-560 and 540-500 Ma respectively (the late event reaching the Ordovician) The first group of orogenies is recorded in practically all provinces The third group is restricted to part of the Mantiqueira Province (southeast of the platform Buzios Orogeny) and present in the Pampean province (SW of the platform) For all these groups of orogenic events there are considerable records of rock assemblages related to processes of convergent plate interaction opening accretion collision and further extrusion There is a good correlation between the geologic and geotectonic data and geochemical and isotopic data The late tectonic processes (post-orogenic magmatism foreland basins etc) of the first two groups compete in time in distinct spaces with the peak of orogenic processes in the third group The introduction of the SHRIMP U-Pb methodology was fundamental to separate the Tonian and post-Tonian orogenic groups and their respective divisions in time and space Thus there are still many open points/problems which lead to expectations of addressing these issues in the near future with the more Intense use of this methodology (C) 2010 Elsevier B V All rights reserved

The link between partial melting, granitization and granulite development in central Ribeira Fold Belt, SE Brazil: New evidence from elemental and Sr-Nd isotopic geochemistry

Elemental and Sr-Nd isotopic data on metatexites, diatexites, orthogneisses and charnockites from the central Ribeira Fold Belt indicate that they are LILE-enriched weakly peraluminous granodiorites. Harker and Th-Hf-La correlation trends suggest that these rocks represent a co-genetic sequence, whereas variations on CaO, MnO, Y and HREE for charnockites can be explained by garnet consumption during granulitic metamorphism. Similar REE patterns and isotopic results of epsilon(565)(Nd) = -5.4 to -7.3 and (87)Sr/(86)Sr(565) = 0.706-0.711 for metatexites, diatexites, orthogneisses and charnockites, as well as similar T(DM) ages between 2.0 and 1.5 Ga are consistent with evolution from a relatively homogeneous and enriched common crustal (metasedimentary) protolith. Results suggest a genetic link between metatexites, diatexites, orthogneisses and charnockites and a two-step process for charnockite development: (a) generation of the hydrated igneous protoliths by anatexis of metasedimentary rocks; (b) continuous high-grade metamorphism that transformed the ""S-type granitoids"" (leucosomes and diatexites) into orthogneisses and, as metamorphism and dehydration progressed, into charnockites. (C) 2011 Elsevier Ltd. All rights reserved.

Thermochronology of central Ribeira Fold Belt, SE Brazil: Petrological and geochronological evidence for long-term high temperature maintenance during Western Gondwana amalgamation

The studied sector of the central Ribeira Fold Belt (SE Brazil) comprises metatexites, diatexites, charnockites and blastomylonites. This study integrates petrological and thermochronological data in order to constrain the thermotectonic and geodynamic evolution of this Neoproterozoic-Ordovician mobile belt during Western Gondwana amalgamation. New data indicate that after an earlier collision stage at similar to 610 Ma (zircon, U-Pb age), peak metamorphism and lower crust partial melting, coeval with the main regional high grade D(1) thrust deformation, occurred at 572-562 Ma (zircon, U-Pb ages). The overall average cooling rate was low (<5 degrees C/Ma) from 750 to 250 degrees C (at similar to 455 Ma; biotite-WR Rb-Sr age), but disparate cooling paths indicate differential uplift between distinct lithotypes: (a) metatexites and blastomylonites show a overall stable 3-5 degrees C/Ma cooling rate; (b) charnockites and associated rocks remained at T>650 degrees C during sub-horizontal D(2) shearing until similar to 510-470 Ma (garnet-WR Sm-Nd ages) (1-2 degrees C/Ma), being then rapidly exhumed/cooled (8-30 degrees C/Ma) during post-orogenic D(3) deformation with late granite emplacement at similar to 490 Ma (zircon, U-Pb age). Cooling rates based on garnet-biotite Fe-Mg diffusion are broadly consistent with the geochronological cooling rates: (a) metatexites were cooled faster at high temperatures (6 degrees C/Ma) and slowly at low temperatures (0.1 degrees C/Ma), decreasing cooling rates with time; (b) charnockites show low cooling rates (2 degrees C/Ma) near metamorphic peak conditions and high cooling rates (120 degrees C/Ma) at lower temperatures, increasing cooling rates during retrogression. The charnockite thermal evolution and the extensive production of granitoid melts in the area imply that high geothermal gradients were sustained fora long period of time (50-90 Ma). This thermal anomaly most likely reflects upwelling of asthenospheric mantle and magma underplating coupled with long-term generation of high HPE (heat producing elements) granitoids. These factors must have sustained elevated crustal geotherms for similar to 100 Ma, promoting widespread charnockite generation at middle to lower crustal levels. (C) 2010 Elsevier B.V. All rights reserved.

Metamorphic P-T evolution of granulites in the central Ribeira Fold Belt, SE Brazil

Pseudosections, geothermobarometric estimates and careful petrographic observations of gneissic migmatites and granulites from Neoproterozoic central Ribeira Fold Belt (SE Brazil) were performed in order to quantify the metamorphic P-T conditions during prograde and retrograde evolution of the Brasiliano Orogeny. Results establish a prograde metamorphic trajectory from amphibolite facies conditions to metamorphic peak (T = 850 +/- 50 A degrees C; P = 8 +/- 1 kbar) that promoted widespread dehydrationmelting of 30 to 40% of the gneisses and high-grade granitization. After the metamorphic peak, migmatites evolved with cooling and decompression to T a parts per thousand 500 A degrees C and P a parts per thousand 5 kbar coupled with aH2O increase, replacing the high-grade paragenesis plagioclase-quartz-K-feldspar-garnet by quartz-biotite-sillimanite-(muscovite). Cordierite absence, microtextural observations and P-T results constrain the migmatite metamorphic evolution in the pseudosections as a clockwise P-T path with retrograde cooling and decompression. High-temperature conditions further dehydrated the lower crust with biotite and amphibole-dehydration melting and granulite formation coupled with 10% melt generation. Granulites can thus be envisaged as middle to lower crust dehydrated restites. Granulites were slowly (nearly isobarically) cooled, followed by late exhumation/retrograde rapid decompression and cooling, reflecting a two step P-T path. This retrograde evolution, coupled with water influx, chemically reequilibrated the rocks from granulite to amphibolite/greenschist facies, promoting the replacement of the plagioclase-quartz-garnet-hypersthene peak assemblage by quartz-biotite- K-feldspar symplectites.

P-T-Fluid evolution and graphite deposition during retrograde metamorphism in Ribeira Fold Belt, SE Brazil: Oxygen fugacity, fluid inclusions and C-O-H isotopic evidence

Combined fluid inclusion (FI) microthermometry, Raman spectroscopy, X-ray diffraction, C-O-H isotopes and oxygen fugacities of granulites from central Ribeira Fold Belt, SE Brazil, provided the following results: i) Magnetite-Hematite fO(2) estimates range from 10(-11.5) bar (QFM + 1) to 10(-18.3) bar (QFM - 1) for the temperature range of 896 degrees C-656 degrees C, implying fO(2) decrease from metamorphic peak temperatures to retrograde conditions; ii) 5 main types of fluid inclusions were observed: a) CO(2) and CO(2)-N(2) (0-11 mol%) high to medium density (1.01-0.59 g/cm(3)) FI; b) CO(2) and CO(2)-N(2) (0-36 mol%) low density (0.19-0.29 g/cm(3)) FI; c) CO(2) (94-95 mol%)-N(2) (3 mol%)-CH(4) (2-3 mol%)-H(2)O (water phi(v) (25 degrees C) = 0.1) FI; d) low-salinity H(2)O-CO(2) FI; and e) late low-salinity H(2)O FI; iii) Raman analyses evidence two graphite types in khondalites: an early highly ordered graphite (T similar to 450 degrees C) overgrown by a disordered kind (T similar to 330 degrees C); iv) delta(18)O quartz results of 10.3-10.7 parts per thousand, imply high-temperature CO(2) delta(18)O values of 14.4-14.8 parts per thousand, suggesting the involvement of a metamorphic fluid, whereas lower temperature biotite delta(18)O and delta D results of 7.5-8.5 parts per thousand and -54 to -67 parts per thousand respectively imply H(2)O delta(18)O values of 10-11 parts per thousand and delta D(H2O) of -23 to -36 parts per thousand suggesting delta(18)O depletion and increasing fluid/rock ratio from metamorphic peak to retrograde conditions. Isotopic results are compatible with low-temperature H(2)O influx and fO(2) decrease that promoted graphite deposition in retrograde granulites, simultaneous with low density CO(2), CO(2)-N(2) and CO(2)-N(2)-CH(4)-H(2)O fluid inclusions at T = 450-330 degrees C. Graphite delta(13)C results of -10.9 to -11.4 parts per thousand imply CO(2) delta(13)C values of -0.8 to -1.3 parts per thousand suggesting decarbonation of Cambrian marine carbonates with small admixture of lighter biogenic or mantle derived fluids. Based on these results, it is suggested that metamorphic fluids from the central segment of Ribeira Fold Belt evolved to CO(2)-N(2) fluids during granulitic metamorphism at high fO(2), followed by rapid pressure drop at T similar to 400-450 degrees C during late exhumation that caused fO(2) reduction induced by temperature decrease and water influx, turning carbonic fluids into CO(2)-H(2)O (depleting biotite delta(18)O and delta D values), and progressively into H(2)O. When fO(2) decreased substantially by mixture of carbonic and aqueous fluids, graphite deposited forming khondalites. (C) 2010 Elsevier Ltd. All rights reserved.

Two New Ternary Complexes of Copper(II) with Tetracycline or Doxycycline and 1,10-Phenanthroline and Their Potential as Antitumoral: Cytotoxicity and DNA Cleavage

This paper reports on the synthesis and characterization of two new ternary copper(II) complexes: [Cu(doxy-cycline)(1,10-phenanthroline)(H(2)O)(ClO(4))](ClO(4)) (1) and [Cu(tetracycline)(1,10-phenanthroline)(H(2)O)(ClO(4))](ClO(4)) (2). These compounds exhibit a distorted tetragonal geometry around copper, which is coordinated to two bidentate ligands, 1,10-phenanthroline and tetracycline or doxycyline, a water molecule, and a perchlorate ion weakly bonded in the axial positions. In both compounds, copper(II) binds to tetracyclines`. via the oxygen of the hydroxyl group and oxygen of the amide group at ring A and to 1,10-phenanthroline via its two heterocyclic nitrogens. We have evaluated the binding of the new complexes to DNA, their capacity to cleave it, their cytotoxic activity, and uptake in tumoral cells. The complexes bind to DNA preferentially by the major groove, and then cleave its strands by an oxidative mechanism involving the generation of ROS. The cleavage of DNA was inhibited by radical inhibitors and/or trappers such as superoxide dismutase, DMSO, and the copper(I) chelator bathocuproine. The enzyme T4 DNA ligase was not able to relegate the products of DNA cleavage, which indicates that the cleavage does not occur via a hydrolytic mechanism. Both complexes present an expressive plasmid DNA cleavage activity generating single- and double-strand breaks, under mild reaction conditions, and even in the absence of any additional oxidant or reducing agent. In the same experimental conditions, [Cu(phen)(2)](2+) is approximately 100-fold less active than our complexes. These complexes are among the most potent DNA cleavage agents reported so far. Both complexes inhibit the growth of K562 cells With the IC(50) values of 1.93 and 2.59 mu mol L(-1) for compounds I and 2, respectively. The complexes are more active than the free ligands, and their cytotoxic activity correlates with intracellular copper concentration and the number of Cu-DNA adducts formed inside cells.

Investigation of the CO tolerance mechanism at several Pt-based bimetallic anode electrocatalysts in a PEM fuel cell

The electrocatalysis of CO tolerance of Pt/C, PtRu/C, PtFe/C, PtMo/C, and PtW/C at a PEM fuel cell anode has been investigated using single cell polarization and online electrochemical mass spectrometry (EMS) measurements, and cyclic voltammetry, X-ray diffraction (XRD), in situ X-ray absorption near edge structure (XANES) analyses of the electrocatalysts. For all bimetallic electrocatalysts, which presented higher CO tolerance, EMS results have shown that the production of CO(2) start at lower hydrogen electrode overpotentials as compared to Pt/C, confirming the occurrence of the so-called bifunctional mechanism. On the other hand, XANES results indicate an increase in the Pt 5d-band vacancies for the bimetallic catalysts, particulary for PtFe/C, this leading to a weakening of the Pt-CO bond, helping to increase the CO tolerance (the so-called electronic effect). For PtMo/C and PtRu/C supplied with H(2)/CO, the formation of CO(2) is observed even when the cell is at open circuit, confirming some elimination of CO by a chemical process, most probably the water gas shift reaction. (C) 2008 Elsevier Ltd. All rights reserved.

Modeling and simulation of the anode in direct ethanol fuels cells

Mathematical modeling has been extensively applied to the study and development of fuel cells. In this work, the objective is to characterize a mechanistic model for the anode of a direct ethanol fuel cell and perform appropriate simulations. The software Comsol Multiphysics (R) (and the Chemical Engineering Module) was used in this work. The software Comsol Multiphysics (R) is an interactive environment for modeling scientific and engineering applications using partial differential equations (PDEs). Based on the finite element method, it provides speed and accuracy for several applications. The mechanistic model developed here can supply details of the physical system, such as the concentration profiles of the components within the anode and the coverage of the adsorbed species on the electrode surface. Also, the anode overpotential-current relationship can be obtained. To validate the anode model presented in this paper, experimental data obtained with a single fuel cell operating with an ethanol solution at the anode were used. (C) 2008 Elsevier B.V. All rights reserved.

Potential oscillations in a proton exchange membrane fuel cell with a Pd-Pt/C anode

We report in this paper the occurrence of potential oscillations in a proton exchange membrane fuel cell (PEMFC) with a Pd-Pt/C anode, fed with H(2)/100 ppm CO, and operated at 30 degrees C. We demonstrate that the use of Pd-Pt/C anode enables the emergence of dynamic instabilities in a PEMFC. Oscillations are characterized by the presence of very high oscillation amplitude, ca. 0.8 V. which is almost twice that observed in a PEMFC with a Pt-Ru/C anode under similar conditions. The effects of the H(2)/CO flow rate and cell current density on the oscillatory dynamics were investigated and the mechanism rationalized in terms of the CO oxidation and adsorption processes. We also discuss the fundamental aspects concerning the operation of a PEMFC under oscillatory regime in terms of the benefit resulting from the higher average power output. (c) 2010 Elsevier B.V. All rights reserved.

The effects of hydrogen sulfide on the polymer electrolyte membrane fuel cell anode catalyst: H(2)S-Pt/C interaction products

The performance of a polymer electrolyte membrane fuel cell (PEMFC) operating on a simulated hydrocarbon reformate is described. The anode feed stream consisted of 80% H(2),similar to 20% N(2), and 8 ppm hydrogen sulfide (H(2)S). Cell performance losses are calculated by evaluating cell potential reduction due to H(2)S contamination through lifetime tests. It is found that potential, or power, loss under this condition is a result of platinum surface contamination with elemental sulfur. Electrochemical mass spectroscopy (EMS) and electrochemical techniques are employed, in order to show that elemental sulfur is adsorbed onto platinum, and that sulfur dioxide is one of the oxidation products. Moreover, it is demonstrated that a possible approach for mitigating H(2)S poisoning on the PEMFC anode catalyst is to inject low levels of air into the H(2)S-contaminated anode feeding stream. (C) 2011 Elsevier B.V. All rights reserved.

Study of ethanol electro-oxidation in acid environment on Pt(3)Sn/C anode catalysts prepared by a modified polymeric precursor method under controlled synthesis conditions

A carbon-supported binary Pt(3)Sn catalyst has been prepared using a modified polymeric precursor method under controlled synthesis conditions This material was characterized using X-ray diffraction (XRD). and the results indicate that 23% (of a possible 25%) of Sn is alloyed with Pt, forming a dominant Pt(3)Sn phase. Transmission election microscopy (TEM) shows good dispersion of the electrocatalyst and small particle sizes (3 6 nm +/- 1 nm) The polarization curves for a direct ethanol fuel cell using Pt(3)Sn/C as the anode demonstrated Improved performance compared to that of a PtSn/C E-TEK. especially in the intrinsic resistance-controlled and mass transfer regions. This behavior is probably associated with the Pt(3)Sn phase. The maximum power density for the Pt(3)Sn/C electrocatalyst (58 mW cm(-2)) is nearly twice that of a PtSn/C E-TEK electrocatalyst (33 mW cm(-2)) This behavior is attributed to the presence of a mixed Pt(9)Sn and Pt(3)Sn alloy phase in the commercial catalysts (C) 2009 Elsevier B V All rights reserved

Fatores de risco para óbito precoce em crianças e em adolescentes submetidos a tranplante hepático eletivo no Hospital de Clínicas de Porto Alegre

No próximo ano, completam-se 40 anos desde a primeira tentativa de transplante hepático (TxH) em seres humanos. Há quase 20 anos, o transplante (Tx) tornou-se uma opção terapêutica real para os pacientes portadores de doença hepática terminal. Atualmente, o TxH é o tratamento de escolha para diversas enfermidades hepáticas, agudas ou crônicas. Dos transplantes realizados na Europa ou nos EUA, em torno de 12% dos pacientes são crianças e adolescentes. No Brasil, 20,9% dos pacientes transplantados de fígado em 2001 tinham até 18 anos de idade e, destes, 60,7% tinham 5 anos ou menos. O objetivo do TxH é a manutenção da vida dos pacientes com doença hepática irreversível, e a principal forma de avaliação de sucesso é a sobrevida após o Tx. A primeira semana que se segue ao TxH, apesar dos excelentes progressos dos últimos anos, continua sendo o período mais crítico. A maioria dos óbitos ou das perdas do enxerto ocorrem nas primeiras semanas, em particular, nos primeiros 7 dias de TxH. Diversos fatores de risco para o resultado do TxH podem ser identificados na literatura, porém há poucos estudos específicos do Tx pediátrico. As crianças pequenas apresentam características particulares que os diferenciam do Tx nos adultos e nas crianças maiores. Com o objetivo de identificar fatores de risco para o óbito nos 7 primeiros dias após os transplantes hepáticos eletivos realizados em 45 crianças e adolescentes no Hospital de Clínicas de Porto Alegre entre março de 1995 e agosto de 2001, foi realizado um estudo de caso-controle. Entre os 6 casos (13,3%) e os 39 controles foram comparadas características relacionadas ao receptor, ao doador e ao procedimento cirúrgico e modelos prognósticos. Das variáveis relacionadas ao receptor, o gênero, o escore Z do peso e da estatura para a idade, a atresia de vias biliares, a cirurgia abdominal prévia, a cirurgia de Kasai, a história de ascite, de peritonite bacteriana espontânea, de hemorragia digestiva e de síndrome hepatopulmonar, a albuminemia, o INR, o tempo de tromboplastina parcial ativada e o fator V não foram associados com o óbito na primeira semana. A mortalidade inicial foi maior nas crianças com menor idade (p=0,0035), peso (p=0,0062) e estatura (p<0,0001), bilirrubinemia total (BT) (p=0,0083) e bilirrubinemia não conjugada (BNC) (p=0,0024) elevadas, e colesterolemia reduzida (p=0,0385). Os receptores menores de 3 anos tiveram um risco 25,5 vezes maior de óbito que as crianças maiores (IC 95%: 1,3–487,7). A chance de óbito após o Tx dos pacientes com BT superior a 20 mg/dL e BNC maior que 6 mg/dL foi 7,8 (IC95%: 1,2–50,1) e 12,7 (IC95%: 1,3–121,7) vezes maior que daqueles com níveis inferiores, respectivamente. Das características relacionadas ao doador e ao Tx, as variáveis gênero, doador de gênero e grupo sangüíneo ABO não idênticos ao do receptor, razão peso do doador/receptor, causa do óbito do doador, enxerto reduzido, tempo em lista de espera e experiência do Programa não foram associados com o óbito nos primeiros 7 dias. Transplantes com enxertos de doadores de idade até 3 anos, ou de peso até 12 Kg representaram risco para o óbito dos receptores 6,8 (IC95%: 1,1–43,5) e 19,3 (IC95%: 1,3–281,6) vezes maior, respectivamente. O tempo de isquemia total foi em média de 2 horas maior nos transplantes dos receptores não sobreviventes (p=0,0316). Os modelos prognósticos Child-Pugh, Rodeck e UNOS não foram preditivos do óbito. Os pacientes classificados como alto risco no modelo de Malatack apresentaram razão de chances para o óbito 18,0 (IC95%: 1,2–262,7) vezes maior que aqueles com baixo risco. A mortalidade na primeira semana foi associada a valores elevados do escore PELD. O risco de óbito foi de 11,3 (IC95%: 1,2–107,0) nas crianças com valor do PELD maior que 10. As crianças pequenas e com maior disfunção hepática apresentaram maior risco de óbito precoce. Doador de pequeno porte e prolongamento do tempo de isquemia também foram associados à mortalidade. Somente os modelos de Malatack e PELD foram preditivos da sobrevida.

A análise estratégica como orientação ao processo de inteligência competitiva (IC) num caso empresarial do segmento industrial alimentício do vale do Taquari (VT/RS)

Esta pesquisa, desenvolvida sob forma de estudo de caso, teve como objetivo verificar a aplicabilidade de modelos e de métodos de análise estratégica para compreender e orientar o processo de inteligência competitiva numa empresa. A empresa selecionada pertence ao segmento alimentício do setor de candies. A pesquisa envolveu cinco etapas: a) levantamento de métodos de análise e contato com o setor; b) conhecimento da empresa; c) conhecimento do ambiente concorrencial; d) aplicação dos modelos de análise e coleta de informações; e) validação interna dos procedimentos metodológicos. Como resultado foram identificadas, as principais variáveis do ambiente concorrencial, as variáveis sobre as quais a empresa deverá aprimorar seu processo de monitoramento e a necessidade de distribuir internamente as informações capturadas. A validação interna, realizada com o grupo diretivo da empresa, permite considerar que a metodologia é pertinente ao objeto estudado e aporta informações e conhecimentos consideráveis às fases preliminares da implantação do processo de inteligência competitiva em pequenas e médias empresas (PMEs).

Impacto clínico e econômico da redefinição dos critérios diagnósticos de infarto do miocárdio

Introdução: Estudos sobre implicações clínicas da nova definição de infarto do miocárdio (IAM), incorporando novos marcadores de lesão miocárdica, são escassos na literatura. A prevalência de IAM e das suas complicações são diretamente dependentes do critério diagnóstico utilizado. Objetivo: Avaliar o impacto diagnóstico, prognóstico e econômico da nova definição de IAM proposta pela AHA/ ESC usando troponina T (TnT) como marcador de lesão cardíaca. Métodos: Um total de 740 pacientes com dor torácica admitidos na Emergência do Hospital de Clínicas de Porto Alegre no período de julho/ 1999 a janeiro/ 2002 foram incluídos no estudo. Creatina quinase total (CK), CK-MB atividade e TnT foram dosados em uma amostra de 363 pacientes, representativa de toda a coorte. Para redefinição de IAM foram utilizados como ponto de corte valores pico de TnT > 0,2 mg/dl. Os desfechos avaliados foram classificados como eventos cardíacos maiores (angina recorrente, insuficiência cardíaca congestiva, choque cardiogênico e óbito) e como procedimentos de revascularização. Também foram avaliados o manejo prescrito, os custos e o faturamento hospitalar. Resultados: Nos 363 pacientes com marcadores dosados, foram diagnosticados 59 casos de IAM (16%) pelos critérios clássicos; enquanto 40 pacientes (11%) tiveram o diagnóstico de IAM pelo critério redefinido, o que corresponde a um incremento de 71% na incidência. Pacientes com IAM redefinido eram significativamente mais idosos e do sexo masculino, apresentaram mais dor atípica e diabetes mellitus. Na análise multivariada, pacientes com infarto redefinido tiveram um risco 5,1 [IC 95% 1,0-28] vezes maior para óbito hospitalar e 3,4 [IC 95% 1,1-10] vezes maior para eventos combinados em relação aqueles sem IAM. O manejo dos casos de IAM redefinido foi semelhante ao manejo daqueles com IAM tradicional, exceto pelos procedimentos de revascularização que foram menos freqüentes (25% vs. 51%, P < 0,001). O grupo com IAM redefinido permaneceu mais tempo internado e foi submetido a procedimentos mais tardiamente. Do ponto de vista institucional, o uso dos novos critérios para IAM poderia resultar em um aumento de 9% (mais R$ 2.756,00 por grupo de 100 pacientes avaliados) no faturamento baseado em diagnóstico segundo a tabela do SUS. Conclusões: O novo diagnóstico de IAM acrescenta um número expressivo de indivíduos com infarto aos serviços de emergência. A incorporação deste critério é importante na medida que estes pacientes têm um prognóstico semelhante aos demais casos tradicionalmente diagnosticados. Como a identificação destes casos poderia resultar em um manejo mais qualificado e eficiente destes pacientes, esforços deveriam ser adotados para reforçar a adoção da redefinição de IAM.