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10篇 您的检索式:作者名="Carla Neto"
    题名 作者 年代 出处 被引量
1Clinical and Diagnostic Laboratory Immunology显示文摘Roigo Ribeiro-Rodrigues Lauro Ferreira da Silva Pilva Pinto Neto Carla B Cunha 200310(2):303-3072003,10,2:1
2Clinical and Diagnostic Laboratory Immunology显示文摘Roigo Ribeiro-Rodrigues Lauro Ferreira da Silva Pilva Pinto Neto Carla B Cunha 200310(2):303-3072003,10,2:1
3Steatosis in chronic hepatitis C: Relationship to the virus and host risk factors显示文摘Carla ALMatos Renata MPerez Mauricio SPacheco Claudio GFigueiredo‐Mendes EdmundoLopes‐Neto Evandro BOliveira Valeria PLanzoni Antonio EBSilva Maria LGFerraz 2006Journal of Gastroenterology and Hepatology2006,,8:1
4Synthesis, characterization and evaluation of CeO2/Mg,Al- mixed oxides as catalysts for SOx removal 显示文摘Carla Maria Salerno Polato Cristiane Assumpcao Henriques Arnaldo Alcover Neto 2005Journal of Molecular Catalysis A Chemical2005,241,12:1
5Clinical and Diagnostics Laboratory Immunology显示文摘Roigo Ribeiro-Rodrigues Lauro Ferreira da Silva Pilva Pinto Neto Carla B Cunha 200310(2) :303- 3072003,10,2:1
6Clinical and Diagnostics Laboratory Immunology显示文摘Roigo Ribeiro-Rodrigues Lauro Ferreira da Silva Pilva Pinto Neto Carla B Cunha 200310(2):303-3072003,10,2:1
7Neoarchean and Rhyacian TTG-Sanukitoid suites in the southern S?o Francisco Paleocontinent,Brazil:Evidence for diachronous change towards modern tectonics显示文摘The southern portion of the Sao Francisco Palaeocontinent in Brazil is denoted by Archean nuclei and Paleoproterozoic magmatic arcs that were amalgamated during Siderian to Orosirian orogenic processes(ca.2.4-2.1 Ga).New isotopic U-Pb in zircon and Sm-Nd whole rock combined with major and trace element composition analyses constrain the crystallization history of the Neoarchean Piedade block(at ca.2.6 Ga)and the Paleoproterozoic Mantiqueira Complex(ca.2.1-1.9 Ga).These therefore display quite different magmatic histories prior to their amalgamation at ca.2.05 Ga.Sm-Nd and Rb-Sr isotopes imply a mixed mantle-crustal origin for the samples in both units.A complete Palaeoproterozoic orogenic cycle,from subduction to collision and collapse,is recorded in the Piedade Block and the Mantiqueira Complex.Rhyacian to Orosirian subduction processes(ca.2.2-2.1 Ga)led to the generation of coeval(ca.2.16 Ga)TTG suites and sanukitoids,followed by late(2.10-2.02 Ga)high-K granitoids that mark the collisional stage.The collisional accretion of the Mantiqueira Complex against the Piedade Block at 2.08-2.04 Ga is also recorded by granulite facies metamorphism in the latter terrane,along the Ponte Nova suture zone.The collisional stage was closely followed by the emplacement of within-plate tholeiites at ca.2.04 Ga and by alkaline rocks(syenites and enriched basic rocks)at ca.1.98 Ga,marking the transition to an extensional tectonic regime.The discovery of two episodes of TTG and sanukitoid magmatism,one during the Neoarchean in the Piedade Complex and another during the Rhyacian in the Mantiqueira Complex,indicates that the onset of subduction-related melting of metasomatized mantle was not restricted to Neoarchean times,as generally believed,but persisted much later into the Paleoproterozoic.Henrique Bruno Vitalino Elizeu Monica Heilbron Claudio de Morisson Valeriano Rob Strachan Mike Fowler Samuel Bersan Hugo Moreira Ivo Dussin Luiz Guilherme do Eirado Silva Miguel Tupinamba Julio Almeida Carla Neto Craig Storey 2020Geoscience Frontiers2020,11,5:0
8Morphological Characterization of Mango (Mangifera indica) Accessions Based on Brazilian Adapted Descriptors显示文摘Ierla Carla Nunes dos Santos Ribeirol Carlos Antonio Femandes Santos Francisco Pinheiro Lima Neto 2013Journal of Agricultural Science and Technology(B)2013,3,11:0
9Fecal microbiota transplantation in patients with metabolic syndrome and obesity:A randomized controlled trial显示文摘BACKGROUND Metabolic syndrome is a multifactorial disease,and the gut microbiota may play a role in its pathogenesis.Obesity,especially abdominal obesity,is associated with insulin resistance,often increasing the risk of type two diabetes mellitus,vascular endothelial dysfunction,an abnormal lipid profile,hypertension,and vascular inflammation,all of which promote the development of atherosclerotic cardiovascular disease.AIM To evaluate the outcomes of fecal microbiota transplantation(FMT)in patients with metabolic syndrome.METHODS This was a randomized,single-blind placebo-controlled trial comparing FMT and a sham procedure in patients with metabolic syndrome.We selected 32 female patients,who were divided into eight groups of four patients each.All of the patients were submitted to upper gastrointestinal endoscopy.In each group,two patients were randomly allocated to undergo FMT,and the other two patients received saline infusion.The patients were followed for one year after the procedures,during which time anthropometric,bioimpedance,and biochemical data were collected.The patients also had periodic consultations with a nutritionist and an endocrinologist.The primary end point was a change in the gut microbiota.RESULTS There was evidence of a postprocedural change in microbiota composition in the patients who underwent FMT in relation to that observed in those who underwent the sham procedure.However,we found no difference between the two groups in terms of the clinical parameters evaluated.CONCLUSION There were no significant differences in biochemical or anthropometric parameters,between the two groups evaluated.Nevertheless,there were significant postprocedural differences in the microbiota composition between the placebo group.To date,clinical outcomes related to FMT remain uncertain.Alberto Machado da Ponte Neto Aniele Cristine Ott Clemente Paula Waki Rosa Igor Braga Ribeiro Mateus Pereira Funari Gabriel Cairo Nunes Luana Moreira Luiz Gustavo Sparvoli Ramon Cortez Carla Romano Taddei Márcio C Mancini Eduardo Guimarães Hourneaux de Moura 2023World Journal of Clinical Cases2023,11,19:0
10Rhyacian-Orosirian tectonic history of the Juiz de Fora Complex:Evidence for an Archean crustal reservoir within an island-arc system显示文摘The southern São Francisco Paleocontinent(SFP)comprises Archean nuclei and Paleoproterozoic complexes encompassing magmatic arcs juxtaposed during a Rhyacian to Orosirian orogenic event.The Juiz de Fora Complex(JFC)represents an imbricated thrust system that comprises orthogranulites with a wide compositional range formed in an intra-oceanic setting during the Siderian to the Orosirian and later accreted to the southeastern margin of the SFP.Here we report new petrological,geochemical,whole-rock Nd and Sr data,as well as zircon U–Pb ages from felsic and mafic orthogranulites from the JFC.The new data is combined with a regional compilation that enables an evaluation of the interaction between magmatism and orogenetic episodes in the context of the consolidation of São Francisco Paleocontinent during the Rhyacian–Orosirian.Pre collisional Island Arc tholeiites(IAT),Tonalites-Tron dhjemites-Granodiorites(TTGs)and sanukitoid magmatism occurred from 2200 Ma to 2085 Ma.This was followed by post-collisional magmatism,which is represented by hybrid granitoids coeval with the emplacement of E-MORB basic rocks.Crustal signatures for the Rhyacian to Orosirian evolution are highlighted by the dominance of negativeεNd(t)associated with Meso-to Neoarchean Nd TDMmodel ages as well as inherited zircon grains from the hybrid granitoids.The JFC is extensively highlighted in the literature as a primitive intra-oceanic arc,but here we propose the reworking or recycling of ancient crustal segments within the mature arc stage of the JFC,suggesting a Mesoarchean crustal source involved in the JFC evolution.Rasec Almeida Vitalino Elizeu Henrique Bruno Samuel Moreira Bersan Lucas Eduardo de Abreu Barbosa Araujo Ivo Dussin Claudio de Morisson Valeriano Carla Neto Monica Heilbron 2022Geoscience Frontiers2022,13,5:0
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