821 resultados para weight cycling


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A obesidade está associada com a inflamação crônica atribuída à liberação de citocinas e adipocinas, à homeostase desregulda da glicemia e à dislipidemia. Intervenções nutricionais são frequentemente acompanhadas por episódios repetidos de perda e recuperação do peso, fenômeno conhecido como efeito sanfona ou ciclagem da massa corporal. Foram avaliados os efeitos da ciclagem da massa corporal sobre os parâmetros: eficiência alimentar, massa corporal (MC), perfil lipídico, metabolismo de carboidratos, indíce de adiposidade corporal, marcadores inflamatórios, esteatose hepática e triglicerídeo (TG) hepático em camundongos C57BL/6 machos que ciclaram a massa corporal duas ou três vezes consecutivas pela alternância de dieta hiperlipídica (high-fat, HF) e dieta padrão (standard-chow,SC). Após cada ciclo de dieta HF, os animais ficavam cada vez mais pesados e, após cada ciclo de dieta SC, os animais perdiam cada vez menos peso. A ciclagem da massa corporal provocou flutuação nas reservas de gordura e nos lipídeos sanguíneos. O colesterol total dos animais, após mudança da dieta HF para dieta SC, apresentou redução dos seus valores, assim como os TG plasmáticos. No teste oral de tolerância à glicose, após o perído de ingestão da dieta HF, os animais apresentaram intolerância à glicose e, após a troca para dieta SC, os animais continuaram com intolerância à glicose. Em relação as adipocinas e citocinas, a leptina, resistina e o fator de necrose tumoral (TNF) alfa séricos aumentaram após o ciclo da dieta HF e diminuíram após a troca por dieta SC. Ao contrário, a adiponectina sérica diminuiu após dieta HF e aumentou após troca por dieta SC. A IL-6 aumentou após ingestão da dieta HF, porém após a troca para dieta SC, a IL-6 permaneceu elevada. Enquanto o MCP-1 não variou durante as trocas de dietas. A expressão da adiponectina no tecido adiposo diminuiu após a dieta HF e os valores permaneceram reduzidos mesmo após a troca para dieta SC. As expressões da leptina e IL-6 no tecido adiposo aumentaram após dieta HF e continuaram aumentados mesmo após a troca para dieta SC. Da mesma forma, a esteatose hepática e os TG hepáticos não reduziram após a mudança da dieta HF para dieta SC. Tanto a dieta HF, como a ciclagem da massa corporal são relevantes para o remodelamento do tecido adiposo e provoca repercussões nos lipídios séricos, na homeostase da glicose, na secreção de adipocinas e provoca acúmulo de gordura no fígado. A troca para dieta SC e redução da MC não são capazes de normalizar a secreção de adipocinas no tecido adiposo e nem das citocinas pró-inflamatórias que permaneceram aumentadas. A esteatose hepática e os TG hepáticos também não são recuperados com a troca para dieta SC e redução da massa corporal. Estes resultados indicam que a ciclagem da MC cria um ambiente inflamatório, que é agraado com adipocinas alteradas, intolerância à glicose e acúmulo de gordura no fígado

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Les personnes atteintes de diabète sont plus à risque de développer la dépression, un fardeau additionnel dans leurs activités quotidiennes. Notre étude auprès d’adultes diabétiques résidant au Québec vise à en déterminer les caractéristiques lorsque la dépression fait partie du tableau clinique. Hypothèse 1: Les adultes québécois atteints de diabète et de dépression (dépression majeure et mineure) seront plus prédisposés à avoir des indicateurs reliés aux habitudes de vie, aux soins du diabète et à l’efficacité personnelle vis-à-vis du contrôle du poids et de la quantité d’aliments consommés, moins favorables que les sujets diabétiques sans dépression. Hypothèse 2: Chez les Québécois atteints de diabète de type 2, l’association entre la dépression et l’obésité sera affectée par les indicateurs de la Variation Cyclique du Poids (VCP) et de l’efficacité personnelle. Hypothèse 3: Chez les Québécois atteints de diabète de type 2, ceux qui auront développé ou maintenu une dépression au cours de 12 mois, seront plus susceptibles de détériorer les indicateurs reliés à leurs habitudes de vie et à leur efficacité personnelle. Des personnes diabétiques au Québec ont été recrutées à l’aide d’un sondage téléphonique. Des adultes, hommes et femmes, âgés de 18 à 80 ans étaient éligibles à participer. La dépression était déterminée par le questionnaire PHQ-9 « Patient Health Questionnaire-9 ». Au total, 3 221 individus ont été contactés au départ de l’étude; 2 003 ont participé à l’étude (93% type 2)et 1 234 ont participé au suivi de 12 mois. La prévalence de dépression mineure et majeure était de 10,9% et 8,7%, respectivement. Cinquante-trois pourcent des sujets avec dépression majeure avaient deux ou trois indicateurs malsains (tabagisme, inactivité ou obésité), 33% des sujets avaient une dépression mineure et 21% des sujets étaient non déprimés. Les résultats des analyses de régression logistique ont révélé que les sujets dépressifs étaient plus susceptibles d’être de sexe féminin, moins instruits, non mariés,sédentaires, fumeurs, percevaient plus souvent avoir une faible maîtrise du contrôle de la quantité d’aliments ingérés et tendaient davantage à mesurer leur glycémie au moins une fois par jour (p<0,05). Chez les patients avec le diabète de type 2, l’association entre la dépression et l’obésité a été affectée par les variables de la VCP et d’efficacité personnelle. Une année après le début de l’étude, 11,5% des sujets ont développé une dépression et 10% ont maintenu leur état dépressif. Les sujets ayant développé une dépression ou persisté dans leur état de dépression étaient plus susceptibles d’avoir été inactifs au début de l’étude ou d’être restés inactifs au suivi de 12 mois, et d’avoir maintenu une perception d’un faible contrôle de leur poids corporel et de la quantité d’aliments ingérés. Cependant, les changements de statut de dépression n’étaient pas associés à des changements de l’indice de masse corporelle. En conclusion, l’inactivité physique et une faible efficacité personnelle sont des facteurs importants dans le développement et la persistance de la dépression chez les patients diabétiques et méritent d’être considérés dans le traitement.

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The aim of this study was to explore soil microbial activities related to C and N cycling and the occurrence and concentrations of two important groups of plant secondary compounds, terpenes and phenolic compounds, under silver birch (Betula pendula Roth), Norway spruce (Picea abies (L.) Karst) and Scots pine (Pinus sylvestris L.) as well as to study the effects of volatile monoterpenes and tannins on soil microbial activities. The study site, located in Kivalo, northern Finland, included ca. 70-year-old adjacent stands dominated by silver birch, Norway spruce and Scots pine. Originally the soil was very probably similar in all three stands. All forest floor layers (litter (L), fermentation layer (F) and humified layer (H)) under birch and spruce showed higher rates of CO2 production, greater net mineralisation of nitrogen and higher amounts of carbon and nitrogen in microbial biomass than did the forest floor layers under pine. Concentrations of mono-, sesqui-, di- and triterpenes were higher under both conifers than under birch, while the concentration of total water-soluble phenolic compounds as well as the concentration of condensed tannins tended to be higher or at least as high under spruce as under birch or pine. In general, differences between tree species in soil microbial activities and in concentrations of secondary compounds were smaller in the H layer than in the upper layers. The rate of CO2 production and the amount of carbon in the microbial biomass correlated highly positively with the concentration of total water-soluble phenolic compounds and positively with the concentration of condensed tannins. Exposure of soil to volatile monoterpenes and tannins extracted and fractionated from spruce and pine needles affected carbon and nitrogen transformations in soil, but the effects were dependent on the compound and its molecular structure. Monoterpenes decreased net mineralisation of nitrogen and probably had a toxic effect on part of the microbial population in soil, while another part of the microbes seemed to be able to use monoterpenes as a carbon source. With tannins, low-molecular-weight compounds (also compounds other than tannins) increased soil CO2 production and nitrogen immobilisation by soil microbes while the higher-molecular-weight condensed tannins had inhibitory effects. In conclusion, plant secondary compounds may have a great potential in regulation of C and N transformations in forest soils, but the real magnitude of their significance in soil processes is impossible to estimate.

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High-molecular-weight dissolved organic matter (HMW-DOM, > 1,000 Daltons) is actively involved in the global biogeochemical cycling of many elements, but its carbon sources and detailed formation pathways are still not well understood. In this study, we measured bulk stable carbon and nitrogen isotopic ratios, lipid composition, and compound-specific carbon isotopic ratios of HMW-DOM samples collected from four U.S. estuaries (Boston Harbor/Massachusetts Bay, Delaware/Chesapeake Bay, San Diego Bay, and San Francisco Bay). Analytical results show (1) a fraction of HMW-DOM (lipid associated) in estuarine and coastal waters is derived from bacteria and phytoplankton; (2) this fraction of HMW-DOM is formed by various release processes of bacterial membrane components and bacterial reworking of phytoplankton-derived material; (3) this fraction of HMW-DOM is generally present in all samples from different coastal systems despite variable organic matter inputs and environmental conditions, suggesting an important bacterial role in HMW-DOM formation.

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High molecular weight dissolved organic matter (HMW-DOM, > 1000 Da) represents a major fraction (> 30%) of dissolved organic carbon (DOC) in the ocean and thus plays an important role in the global biogeochemical cycling of carbon and many other elements. Its organic sources and formation mechanisms, however, are still not well understood especially in estuarine and coastal regions where multiple natural and anthropogenic sources contribute to total HMW-DOM. In this paper we report our measurements of natural radiocarbon (C-14) abundances and stable carbon isotope (C-13) compositions of the major biochemical compound classes: amino acids, carbohydrates and lipids separated from eight HMW-DOM samples collected from five US estuaries as part of our on-going study of sources, distribution and transport of chromophoric dissolved organic matter (CDOM) in estuarine and coastal waters. Distinct differences in both C-14 and C-13 values were found among the bulk HMW-DOM samples as well as the individual compound classes. Radiocarbon ages of the major compound classes varied by as much as 27,000 years in a single sample. The calculated average radiocarbon ages of the compound fractions of HMW-DOM indicate that the total lipid fraction is very "old", while the acid-insoluble fraction is slightly younger. Total amino acid and carbohydrate fractions, however, have relatively modern apparent C-14 ages. The significant variability in C-14 ages among the compound classes indicates not only multiple organic carbon sources but also different formation and turnover pathways controlling the cycling of different biochemical components of HMW-DOM in estuarine and coastal waters. (c) 2006 Elsevier Ltd. All rights reserved.

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:ofiedian lethal temperatures ( LT50' s ) were determined for rainbow trout, Salmo gairdnerii, acclimated for a minimum of 21 days at 5 c onstant temperatures between 4 and 20 0 C. and 2 diel temperature fluctuations ( sinewave curves of amplitudes ± 4 and ± 7 0 C. about a mean temperature of 12 0 C. ) . Twenty-four-, 48-, and 96-hour LT50 estimates were c alculated f ollowing standard flow-through aquatic bioassay techniques and probi t transformation of mortality data. The phenomenon of delayed thermal mortality was also investigated. Shifts in upper incipient lethal temperature occurred as a result of previous thermal conditioning. It was shown that increases in constant acclimation temperature result in proportional l inear increases in thermal tolerances. The increase i n estimated 96-hour LT50's was approximately 0.13 0 c. X 1 0 C:1 between 8 and 20 0 C. The effect of acclimation to both cyclic temperature regimes was an increase in LT50 to values between the mean and maximum constant equivalent daily temperatures of the cycles. Twenty-four-, 48-, and 96-hour LT50 estimates of both cycles corresponded approximately to the LT50 values of the 16 0 C. c onstant temperature equivalent . This increase i n thermal tolerance was further demonstrated by the delayed thermal mortality experiments . Cycle amplitudes appeared to i nfluence thermal resistance through alterations in initi al mortality since mortality patterns characteristic of base temperature acclimations re-appeared after approximately 68 hours exposure to test temperatures for the 12 + 4 0 C. group, whereas mortality patterns stabilized and remained constant for a period greater than 192 hours with the larger therma l cycle ( 12 + 7 0 C. ). NO s ignificant corre lations between s pecimen weight and time-to-death was apparent. Data are discussed in relation to the establishment of thermal criteria for important commercial and sport fishes , such as the salmonids , as is the question whether previously reported values on lethal temperature s may have been under estimated.

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Food restriction (FR) has been shown to promote myocardial dysfunction in rats. The aim of this study was to verify the participation of calcium and beta-adrenergic system on myocardial mechanical alteration in rats submitted to FR. Myocardial performance was studied in isolated left ventricular papillar muscle from young Wistar-Kyoto rats (WKY) submitted to FR or to control diet. The groups subjected to FR were fed 50% less food than the control group for 90 days. Mechanical function was studied in isometric contraction at post-rest contraction of 30 seconds (PRC), calcium chloride concentration 5.20 mM, and beta-adrenergic stimulation with isoproterenol 10(-6) M. FR decreased the body weight, and left and right ventricular weight. In basal condition (1.25 MM of calcium) time to peak tension (TPT) and time from peak tension to 50% relaxation (RT50) were greater in the FR group. Muscle function was. The same in both PRC groups. TPT decrease in both high calcium groups, more in FR rats; RT50 dropped only in FR animals. TPT decreased in both Isoproterenol groups, more intensely in the FR group. This result suggests that food restriction impairs myocardial performance and these changes may be attributed to alterations in the intracellular calcium cycling and beta-adrenergic system. (C) 2003 Elsevier B.V. All rights reserved.

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The maximal lactate steady state (MLSS) is the highest blood lactate concentration that can be identified as maintaining a steady state during a prolonged submaximal constant workload. The objective of the present study was to analyze the influence of the aerobic capacity on the validity of anaerobic threshold (AT) to estimate the exercise intensity at MLSS (MLSS intensity) during cycling. Ten untrained males (UC) and 9 male endurance cyclists (EC) matched for age, weight and height performed one incremental maximal load test to determine AT and two to four 30-min constant submaximal load tests on a mechanically braked cycle ergometer to determine MLSS and MLSS intensity. AT was determined as the intensity corresponding to 3.5 mM blood lactate. MLSS intensity was defined as the highest workload at which blood lactate concentration did not increase by more than 1 mM between minutes 10 and 30 of the constant workload. MLSS intensity (EC = 282.1 ± 23.8 W; UC = 180.2 ± 24.5 W) and AT (EC = 274.8 ± 24.9 W; UC = 187.2 ± 28.0 W) were significantly higher in trained group. However, there was no significant difference in MLSS between EC (5.0 ± 1.2 mM) and UC (4.9 ± 1.7 mM). The MLSS intensity and AT were not different and significantly correlated in both groups (EC: r = 0.77; UC: r = 0.81). We conclude that MLSS and the validity of AT to estimate MLSS intensity during cycling, analyzed in a cross-sectional design (trained x sedentary), do not depend on the aerobic capacity.

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

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[EN] In order to establish the potential role of Antarctic krill (Euphausia superba) in the recycling of bioactive elements, we have quantified the release of iron, phosphate, and ammonia by these organisms along the Antarctic Peninsula sector of the Southern Ocean. The experimental results suggested that the presence of krill has a significant impact on ambient iron concentrations, as large amounts of this trace element were released by the krill (22–689 nmol Fe g Dry Weight−1 h−1, equivalent to 0.2 to 4.3 nmol Fe L−1 d−1). Half of this iron release occurred within the first hour of the experiment, and differences in iron and phosphate release rates (3.1 to 14.0 μmol PO43− g DW−1 h−1) seemed to reflect differences in food availability. These results identify krill as a major node in iron cycling in the Southern Ocean, potentially influencing iron residence time in the upper water column of this region.

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BACKGROUND: Intradialytic exercise has been described to improve blood pressure stability and dialysis efficacy. However, comorbid conditions in the dialysis population often preclude the widespread use of active intradialytic exercise. Therefore, we investigated the effect of intradialytic transcutaneous muscle stimulation (TEMS) and passive cycling movements (PCMs) on blood pressure and dialysis efficacy in patients. STUDY DESIGN: Prospective, controlled, randomized, crossover investigation. SETTING ; PARTICIPANTS: Ten patients were randomly allocated to TEMS, PCMs, or no intervention (NI) for 9 consecutive dialysis sessions. INTERVENTION: Participants were studied with NI, PCMs using a motor-driven ergometer, and bilateral TEMS of the leg musculature. Individual dialysis prescriptions were unchanged during the investigation. OUTCOMES ; MEASUREMENTS: The effect of TEMS and PCMs on blood pressure and dialysis efficacy in patients was assessed. RESULTS: Mean blood pressure increased from 121/64 +/- 21/15 mm Hg with NI to 132/69 +/- 21/15 mm Hg (P < 0.001) during sessions with PCMs and 125/66 +/- 22/16 mm Hg (P < 0.05) during sessions with TEMS. Urea and phosphate removal during dialysis were significantly (P < 0.001) greater with TEMS (19.4 +/- 3.7 g/dialysis and 1,197 +/- 265 mg/dialysis) or PCMs (20.1 +/- 3.4 g/dialysis and 1,172 +/- 315 mg/dialysis) than with NI (15.1 +/- 3.9 g/dialysis and 895 +/- 202 mg/dialysis). Body weight, ultrafiltration, Kt/V, and increases in hemoglobin and albumin levels during dialysis did not differ among the NI, PCMs, and TEMS groups. LIMITATIONS: The study design does not allow extension of the findings to prolonged treatment. CONCLUSION: Future studies during longer observation periods will have to prove the persistence of these acute findings. Both TEMS and PCMs deserve future investigations in dialysis patients because they increase intradialytic blood pressure and facilitate urea and phosphate removal when applied short term.

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Major ice sheets were permanently established on Antarctica approximately 34 million years ago, close to the Eocene/ Oligocene boundary, at the same time as a permanent deepening of the calcite compensation depth in the world's oceans. Until recently, it was thought that Northern Hemisphere glaciation began much later, between 11 and 5million years ago. This view has been challenged, however, by records of ice rafting at high northern latitudes during the Eocene epoch and by estimates of global ice volume that exceed the storage capacity of Antarctica at the same time as a temporary deepening of the calcite compensation depth 41.6 million years ago. Here we test the hypothesis that large ice sheets were present in both hemispheres 41.6 million years ago using marine sediment records of oxygen and carbon isotope values and of calcium carbonate content from the equatorial Atlantic Ocean. These records allow, at most, an ice budget that can easily be accommodated on Antarctica, indicating that large ice sheets were not present in the Northern Hemisphere. The records also reveal a brief interval shortly before the temporary deepening of the calcite compensation depth during which the calcite compensation depth shoaled, ocean temperatures increased and carbon isotope values decreased in the equatorial Atlantic. The nature of these changes around 41.6 million years ago implies common links, in terms of carbon cycling, with events at the Eocene/Oligocene boundary and with the 'hyperthermals' of the Early Eocene climate optimum. Our findings help to resolve the apparent discrepancy between the geological records of Northern Hemisphere glaciation and model results that indicate that the threshold for continental glaciation was crossed earlier in the Southern Hemisphere than in the Northern Hemisphere.

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Purpose: The impact of acute weight loss on rowing performance was assessed when generous nutrient intake was provided in 2 h of recovery after making weight. Methods: Competitive rowers (N = 17) completed four ergometer trials, each separated by 48 h. Two trials were performed after a 4% body mass loss in the previous 24 h (WT) and two were performed after no weight restrictions, that is, unrestricted (UNR). In addition, two trials (I X WT, I X UNR) were in a thermoneutral environment (NEUTRAL, mean 21.1 +/- SD 0.7 degrees C, 29.0 +/- 4.5% RH) and two were in the heat (HOT 32.4, +/- 0.4 degrees C, 60.4 +/- 2.7% RH). Trials were performed in a counterbalanced fashion according to a Latin square design. Aggressive nutritional recovery strategies (WT 2.3 g(.)kg(-11) carbohydrate, 34 mg-kg(-1) Na, 28.4 mL(.)kg(-1) fluid; UNR ad libitum) were employed in the 2 h after weigh-in. Results: Both WT (mean 2.1, 95% CI 0.7-3.4 s; P = 0.003) and HOT (4.1, 2.7 - 5.4 s; P < 0.001) compromised 2000-m time-trial performance. Whereas WT resulted in hypohydration, the associated reduction in plasma volume explained only part of the performance compromise observed (0.2 s for every 1% decrement) Moreover, WT did not influence core temperature or indices of cardiovascular function. Conclusions: Acute weight loss compromised performance, despite generous nutrient intake in recovery, although the effect was small. Performance decrements were further exacerbated when exercise was performed in the heat.