Biomarkers of oxidative stress tethered to cardiovascular diseases.

Cardiovascular disease (CVD) is a broad term that incorporated a group of conditions that affect the blood vessels and the heart. CVD is a foremost cause of fatalities around the world. Multiple pathophysiological mechanisms are involved in CVD; however, oxidative stress plays a vital role in generating reactive oxygen species (ROS). Oxidative stress occurs when the concentration of oxidants exceeds the potency of antioxidants within the body while producing reactive nitrogen species (RNS). ROS generated by oxidative stress disrupts cell signaling, DNA damage, lipids, and proteins, thereby resulting in inflammation and apoptosis. Mitochondria is the primary source of ROS production within cells. Increased ROS production reduces nitric oxide (NO) bioavailability, which elevates vasoconstriction within the arteries and contributes to the development of hypertension. ROS production has also been linked to the development of atherosclerotic plaque. Antioxidants can decrease oxidative stress in the body; however, various therapeutic drugs have been designed to treat oxidative stress damage due to CVD. The present review provides a detailed narrative of the oxidative stress and ROS generation with a primary focus on the oxidative stress biomarker and its association with CVD. We have also discussed the complex relationship between inflammation and endothelial dysfunction in CVD as well as oxidative stress-induced obesity in CVD. Finally, we discussed the role of antioxidants in reducing oxidative stress in CVD

Avian influenza (H7N9) virus infection in chinese tourist in Malaysia, 2014

10.3201/eid2101.141092Emerging Infectious Diseases211142-14

A comparison of doses from ¹³⁷Cs and ²¹⁰ Po in marine food: A major international study

Radioactivity levels of natural 210Po and anthropogenic 137Cs in sea water and biota (fish and shellfish) have been estimated for the FAO fishing areas on the basis of measurements carried out in recent years. Collective doses resulting from seafood consumption are calculated for each FAO area using radioactivity data for water and biota. Good agreement is observed between the results calculated by these two methods, with the exception of the doses from 210Po via shellfish consumption. The collective effective close commitment from 137Cs in marine food in 1990 has been estimated at 160 man Sv with an uncertainly of 50%. The corresponding dose from 210Po is 30,000 man Sv with an estimated uncertainty of a factor of 5. The results confirm that the dominant contribution to doses derives from natural 210Po in fish and shellfish and that the contribution from anthropogenic 137Cs (mainly originating from nuclear weapons tests) is negligible

Avaliação da porosidade e placa férrica de raízes de arroz cultivado em hipoxia Evaluation of porosity and iron plaque on rice roots grown under hypoxia

A alta difusividade do oxigênio em diversos materiais dificulta a criação e, ou, manutenção de um ambiente livre de O2. As técnicas utilizadas são pouco eficientes na exclusão do O2 e, portanto, não expressam a condição do solo alagado. Os objetivos deste trabalho foram desenvolver um método para obtenção de raízes em condição de hipoxia e avaliar a placa férrica e a formação de aerênquima no arroz. Foi criada uma condição de hipoxia semelhante à do solo alagado em tanques de 50 L, explorando a capacidade de difusão do O2 por meio do vinil em contato com solo reduzido. Cada tanque preenchido com solo (Gleissolo háplico) recebeu cinco sacos de vinil e foi mantido alagado. Plantas dos genótipos IRGA 423 e IRGA 424 previamente cultivadas em campo foram coletadas, tendo as raízes cortadas junto ao colo, lavadas e um terço da lâmina foliar removido. Cada saco de vinil recebeu 12 plantas de cada genótipo e solução nutritiva. Após sete dias, as novas raízes adventícias formadas foram utilizadas na determinação da porosidade e a da placa férrica em segmentos de 0-2, 2-4 e 4-6 cm a partir da ponta da raiz. As raízes foram colocadas em contato com a solução de um solo em processo de redução por 4 h e a placa férrica determinada após a extração do Fe com HCl 0,5 mol L-1. A porosidade foi determinada pela aplicação de ciclos de vácuo, com auxílio de seringas. A diferença de peso antes e depois do tratamento com vácuo e entrada de água foi assumida como sendo a estimativa da magnitude do aerênquima ao longo da raiz. A eficácia do método foi testada com a produção de raízes adventícias em saco de vinil com aeração e hipoxia. A porosidade nas raízes foi maior em ambiente hipóxico, comparado à aeração. A porosidade foi maior na proximidade da base da planta e, à medida que a porosidade aumentou, houve aumento do conteúdo de Fe na superfície das raízes, indicando que a placa férrica pode servir como estimativa da formação de aerênquima no arroz. O método de obtenção de raízes foi eficiente em promover a eliminação de O2 do saco de vinil para estudar a formação do aerênquima.<br>The high oxygen diffusion in different materials makes the establishment and maintenance of oxygen-free environments difficult. The techniques used to obtain oxygen-free environments are little efficient and not representative of flooded soil conditions. The purpose of this study was to develop a method for obtaining roots in a hypoxic environment to evaluate iron plaque and aerenchyma formation in rice plants. A hypoxic condition similar to that of flooded soils was created in 50 L tanks, based on the oxygen diffusion capacity through vinyl plastic in contact with flooded soil. Each tank was filled with soil (Gley soil), five vinyl bags and then flooded. Rice plants of the genotypes IRGA 423 and IRGA 424 grown in the field were collected, the roots cut at the stem, washed and 1/3 of the leaves removed. Each bag was filled with 12 plants of each genotype and nutrient solution. After seven days, the new adventitious roots were used to determine the iron plaque and aerenchyma formation in the segments 0-2, 2-4 and 4-6 cm from the root tips. The roots were exposed the solution of a flooded soil for 4 hours. The iron plaque was determined in the root segments after iron extraction with HCl 0.5 mol L-1. Porosity was determined in vacuum cycles applied with a syringe. The weight difference before and after vacuum treatment and water entrance was assumed as estimate of the magnitude of the aerenchyma of the roots. The method was tested with the production of new adventitious roots in vinyl bags under aerated and hypoxic conditions. Root porosity was higher in the hypoxic than in the aerated environment. Porosity was higher near plant base and as porosity increased, iron increased near the root surface, indicating the iron plaque as a parameter to estimate aerenchyma formation in rice roots. The tested root-growth method was efficient in eliminating O2 from the vinyl bags to study aerenchyma formation