Deciphering pyritization-kerogenization gradient for fish soft-tissue preservation.

Soft-tissue preservation provides palaeobiological information that is otherwise lost during fossilization. In Brazil, the Early Cretaceous Santana Formation contains fish with integument, muscles, connective tissues, and eyes that are still preserved. Our study revealed that soft-tissues were pyritized or kerogenized in different microfacies, which yielded distinct preservation fidelities. Indeed, new data provided the first record of pyritized vertebrate muscles and eyes. We propose that the different taphonomic pathways were controlled by distinct sedimentation rates in two different microfacies. Through this process, carcasses deposited in each of these microfacies underwent different residence times in sulphate-reduction and methanogenesis zones, thus yielding pyritized or kerogenized softtissues, and a similar process has previously been suggested in studies of a late Ediacaran lagerst?tte

Protective Effect of Metformin Against Walker 256 Tumor Growth is Not Dependent on Metabolism Improvement

Background/Aims: The objective of the current work was to test the effect of metformin on the tumor growth in rats with metabolic syndrome. Methods: We obtained pre-diabetic hyperinsulinemic rats by neonatal treatment with monosodium L-glutamate (MSG), which were chronically treated every day, from weaning to 100 day old, with dose of metformin (250 mg/kg body weight). After the end of metformin treatment, the control and MSG rats, treated or untreated with metformin, were grafted with Walker 256 carcinoma cells. Tumor weight was evaluated 14 days after cancer cell inoculation. The blood insulin, glucose levels and glucose-induced insulin secretion were evaluated. Results: Chronic metformin treatment improved the glycemic homeostasis in pre-diabetic MSG-rats, glucose intolerance, tissue insulin resistance, hyperinsulinemia and decreased the fat tissue accretion. Meanwhile, the metformin treatment did not interfere with the glucose insulinotropic effect on isolated pancreatic islets. Chronic treatment with metformin was able to decrease the Walker 256 tumor weight by 37% in control and MSG rats. The data demonstrated that the anticancer effect of metformin is not related to its role in correcting metabolism imbalances, such as hyperinsulinemia. However, in morphological assay to apoptosis, metformin treatment increased programmed cell death. Conclusion: Metformin may have a direct effect on cancer growth, and it may programs the rat organism to attenuate the growth of Walker 256 carcinoma

O conhecimento de pediatras sobre alergia alimentar: estudo piloto Pediatricians' knowledge on food allergy: pilot study

OBJETIVO: Avaliar o conhecimento de pediatras sobre alergia alimentar. MÉTODOS: Dados obtidos de questionário padronizado, postado e respondido por pediatras filiados à Sociedade Brasileira de Pediatria (SBP). Digitação dos dados em planilha Excel e análise de freqüência de respostas afirmativas em porcentagem. RESULTADOS: Foram analisados 895 questionários preenchidos por pediatras de todo o país, com predomínio da região Sudeste (61,6%). Segundo os pediatras entrevistados, as manifestações diagnósticas de alergia alimentar são: respiratórias, cutâneas e sistêmicas, em iguais proporções. Ainda segundo estes pediatras, leite de vaca (98,9%), clara de ovo (58,7%) e amendoim (50,9%) são os principais alimentos associados a essas manifestações. Embora 74,8% dos respondedores tivessem identificados os corantes e aditivos alimentares como responsáveis pela alergia alimentar, apenas 19,4% conheciam o código de identificação da tartrazina. CONCLUSÕES: Os dados apresentados reforçam a necessidade de ampliação dos conhecimentos dos profissionais de saúde sobre o diagnóstico e tratamento da alergia alimentar, com o objetivo de garantir o uso de critérios diagnósticos e terapêuticos mais adequados.<br>OBJECTIVE: To evaluate the knowledge of Brazilian pediatricians about food allergy. METHODS: Data was obtained from a sent back posted written questionnaire. It was filled in by Brazilian pediatricians, affiliated to the Brazilian Society of Pediatrics. Data was transcript to an Excel spread sheet and the frequency of affirmative responses was reported as percentages. RESULTS: Data from 895 written questionnaire of pediatricians from all over Brazil, (mainly from the southeastern region - 61.6%), were analyzed. The main clinical expressions of food allergy determined by the pediatricians were: respiratory, cutaneous and systemic symptoms (equal proportions). According to these pediatricians, cow's milk (98.9%), egg white (58.7%) and peanuts (50.9%) were the main allergens related to food allergy symptoms. Although 74.8% of the responders have indicated food dyes and food additives as associated to food allergies, only 19.4% of them knew the identification code of tartrarzine. CONCLUSIONS: The presented data reinforce the need to improve the pediatricians' knowledge about the diagnosis and treatment of food allergy, in order to assure the use of appropriate diagnostic and treatment criteria

Paleoproterozoic (~1.88Ga) felsic volcanism of the Iricoumé Group in the Pitinga Mining District area, Amazonian Craton, Brazil: insights in ancient volcanic processes from field and petrologic data

The Iricoumé Group correspond to the most expressive Paleoproterozoic volcanism in the Guyana Shield, Amazonian craton. The volcanics are coeval with Mapuera granitoids, and belong to the Uatumã magmatism. They have U-Pb ages around 1880 Ma, and geochemical signatures of &#945;-type magmas. Iricoumé volcanics consist of porphyritic trachyte to rhyolite, associated to crystal-rich ignimbrites and co-ignimbritic fall tuffs and surges. The amount and morphology of phenocrysts can be useful to distinguish lava (flow and dome) from hypabyssal units. The morphology of ignimbrite crystals allows the distinction between effusive units and ignimbrite, when pyroclasts are obliterated. Co-ignimbritic tuffs are massive, and some show stratifications that suggest deposition by current traction flow. Zircon and apatite saturation temperatures vary from 799°C to 980°C, are in agreement with most temperatures of &#945;-type melts and can be interpreted as minimum liquidus temperature. The viscosities estimation for rhyolitic and trachytic compositions yield values close to experimentally determined melts, and show a typical exponential decay with water addition. The emplacement of Iricoumé volcanics and part of Mapuera granitoids was controlled by ring-faults in an intracratonic environment. A genesis related to the caldera complex setting can be assumed for the Iricoumé-Mapuera volcano-plutonic association in the Pitinga Mining District.<br>O Grupo Iricoumé corresponde ao mais expressivo vulcanismo Paleoproterozóico do Escudo das Guianas, craton Amazônico. As rochas vulcânicas são coexistentes com os granitóides Mapuera, e pertencem ao magmatismo Uatumã. Possuem idades U-Pb em torno 1888 Ma, e assinaturas geoquímicas de magmas tipo-A. As vulcânicas do Iricoumé consistem de traquitos a riolitos porfiríticos, associados a ignimbritos ricos em cristal e tufos co-ignimbríticos de queda e surge. A quantidade e a morfologia dos fenocristais podem ser utilizadas para distinguir lava (fluxo e domo) de unidades hipabissais. A morfologia dos cristais em ignimbritos permite a distinção entre unidades efusivas e ignimbritos, quando os piroclastos estão obliterados. Tufos co-ignimbríticos são maciços e alguns exibem estratificações que sugerem deposição por correntes de tração. Temperaturas de cristalização de zircão e apatita variam de 799°C a 980°C, são compatíveis com temperaturas de líquidos tipo-A e podem ser interpretadas como temperatura liquidus mínima. Estimativas de viscosidade para composições riolíticas e traquíticas fornecem valores próximos a de líquidos determinadas experimentalmente e ilustram curvas típicas de decaimento exponencial, com a adição de água. O posicionamento das vulcânicas Iricoumé e de parte dos granitóides Mapuera foi controlado por falhas anelares em ambiente intracratônico. Uma gênese relacionada a ambiente de complexo de caldeiras pode ser assumida para a associação vulcano-plutônica Iricoumé-Mapuera no Distrito Mineiro de Pitinga