185 resultados para saline conditions
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Here we present a 30 000 years low-resolution climate record reconstructed from groundwater data. The investigated site is located in the Bohemian Cretaceous Basin, in the corridor between the Scandinavian ice sheet and the Alpine ice field. Noble gas temperatures (NGT), obtained from groundwater data, preserved multicentennial temperature variability and indicated a cooling of at least 5-7 °C during the last glacial maximum (LGM). This is further confirmed by the depleted δ18O and δ2H values at the LGM. High excess air (ΔNe) at the end of the Pleistocene is possibly related to abrupt changes in recharge dynamics due to progression and retreat of ice covers and permafrost. These results agree with the fact that during the LGM permafrost and small glaciers developed in the inner valleys of the Giant Mountains (located in the watershed of the aquifers). A temporal decrease of deuterium excess from the pre-industrial Holocene to present days is linked to an increase of the air temperatures, and probably also to an increase of water pressure at the source region of precipitation over the past few hundred years
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When colonizing a new habitat, populations must adapt their sexual behaviour to new ecological constraints. Because caves display drastically different conditions from surface habitats and cave animals are deprived from visual information, hypogean populations are expected to have modified their mate preference and signalling behaviour after cave colonization. Here, we experimentally examined the female preference and the sexual behaviour of brook newts Calotriton asper from different cave and river populations, either in light or in darkness. Our results suggest that females prefer large individuals in both hypogean and epigean populations, but that this preference is only expressed in the light conditions of their native habitat. Hence, some mate choice criteria would be maintained across genetically divergent populations and throughout dissimilar habitats. However, this sexual behaviour is likely to be expressed via a different sensory pathway in the different habitats, suggesting that a sensory shift has occurred in cave populations, enabling animals to communicate through a non-visual channel.
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We conducted an open, randomized, and prospective study to determine the effect of hypertonic saline on the secretion of antidiuretic hormone (ADH) and aldosterone in children with severe head injury (Glasgow coma scale <8). Thirty-one consecutive patients at a level III pediatric intensive care unit at a children's hospital received either lactated Ringer's solution (Ringer's group, n = 16) or hypertonic saline (Hypertonic Saline group, n = 15) over a 3-day period. Serum ADH levels were significantly larger in the Hypertonic Saline group as compared with the Ringer's group (P = 0.001; analysis of variance) and were correlated to sodium intake (Ringer's group: r = 0.39, R(2) = 0.15, P = 0.02; Hypertonic Saline group: r = 0.42, R(2) = 0.18, P = 0.02) and volume of fluids given IV (Ringer's group: r = 0.38, R(2) = 0.15, P = 0.02; Hypertonic Saline group: r = 0.32, R(2) = 0.1, P = not significant). Correlation of ADH to plasma osmolality was significant if plasma osmolality was >280 mOsm/kg (r = 0.5, R(2) = 0.25, P = 0.06), indicating an osmotic threshold for ADH release. Serum aldosterone levels were larger on the first day than during Days 2 and 3 in both groups and inversely correlated to serum sodium levels only in the Ringer's group (r = -0.55, R(2) = 0.3, P < 0.001). This group received a significantly larger fluid volume on Day 1 (P = 0.05, Mann-Whitney U-test) than did patients in the Hypertonic Saline group, indicating hypovolemia during the first day. Head-injured children have appropriate levels of ADH. They may be hypovolemic during the first day of treatment, especially if they receive lactated Ringer's solution. IMPLICATIONS: In head-injured patients, we recommend fluid restriction to avoid inappropriate secretion of antidiuretic hormone. In a prospective, randomized, and controlled study in 31 children, we were able to show that the antidiuretic hormone levels are appropriate in response to hypovolemia, sodium load, or both.
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Active personal dosemeters (APD) have been found to be very efficient tools to reduce occupational doses in many applications of ionizing radiation. In order to be used in interventional radiology and cardiology (IR/IC), APDs should be able to measure low energy photons and pulsed radiation with relatively high instantaneous personal dose equivalent rates. A study concerning the optimization of the use of APDs in IR/IC was performed in the framework of the ORAMED project, a Collaborative Project (2008-2011) supported by the European Commission within its 7th Framework Program. In particular, eight commercial APDs were tested in continuous and pulsed X-ray fields delivered by calibration laboratories in order to evaluate their performances. Most of APDs provide a response in pulsed mode more or less affected by the personal dose equivalent rate, which means they could be used in routine monitoring provided that correction factors are introduced. These results emphasize the importance of adding tests in pulsed mode in type-test procedures for APDs. Some general recommendations are proposed in the end of this paper for the selection and use of APDs at IR/IC workplaces.
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OBJECTIVE: The basolateral Na pump drives renotubular reabsorption. In cultured renal cells, mutant adducins, as well as sub-nanomolar ouabain concentrations, stimulate the Na-K pump. METHODS: To determine whether these factors interact and affect Na handling and blood pressure (BP) in vivo, we studied 155 untreated hypertensive patients subdivided on the basis of their plasma endogenous ouabain or alpha-adducin genotype (ADD1 Gly460Trp-rs4961). RESULTS: Under basal conditions, proximal tubular reabsorption and plasma Na were higher in patients with mutated Trp ADD1 or increased endogenous ouabain (P = 0.002 and 0.05, respectively). BPs were higher in the high plasma endogenous ouabain group (P = 0.001). Following volume loading, the increment in BP (7.73 vs. 4.81 mmHg) and the slopes of the relationship between BP and Na excretion were greater [0.017 +/- 0.002 vs. 0.009 +/- 0.003 mmHg/(muEq min)] in ADD1 Trp vs. ADD1 Gly carriers (P < 0.05). BP changes were similar, whereas the slopes of the relationship between BP and Na excretion were lower [0.016 +/- 0.003 vs. 0.008 +/- 0.002 mmHg/(muEq min)] in patients with low vs. high endogenous ouabain (P < 0.05). In patients with high endogenous ouabain, volume loading increased the BP in the ADD1 Trp group but not in the Gly group (P < 0.05). Thus, patients with ADD1 Trp alleles are sensitive to salt and tubular Na reabsorption remains elevated after volume expansion. CONCLUSION: With saline loading, BP changes are similar in high and low endogenous ouabain patients, whereas tubular Na reabsorption increases in the high endogenous ouabain group. Saline loading unmasks differences in renal Na handling in patients with mutant adducin or high endogenous ouabain and exposes an interaction of endogenous ouabain and Trp alleles on BP.
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Introduction: Therapeutic drug monitoring (TDM) of imatinib has been increasingly proposed for chronic myeloid leukaemia (CML) patients, as several studies have found a correlation between trough concentrations (Cmin) >=1000ng/ml and improved response. The pharmacological monitoring project of EUTOS (European Treatment and Outcome Study) was launched to increase the availability of imatinib TDM, standardize labs, and validate proposed Cmin thresholds. Using the collected data, the objective of this analysis was to characterize imatinib Population pharmacokinetics (Pop-PK) in a large cohort of European patients, to quantify its variability and the influence of demographic factors and comedications, and to derive individual exposure variables suitable for further concentration-effect analyses.¦Methods: 4095 PK samples from 2478 adult patients were analyzed between 2006 and 2010 by LC-MS-MS and considered for Pop-PK analysis by NONMEM®. Model building used data from 973 patients with >=2 samples available (2590 samples). A sensitivity analysis was performed using all data. Available comedications (27%) were classified into inducers or inhibitors of P-glycoprotein, CYP3A4/5 and organic-cation-transporter-1 (hOCT-1).¦Results: A one-compartment model with linear elimination, zero-order absorption fitted the data best. Estimated Pop-PK parameters (interindividual variability, IIV %CV) for a 40-year old male patient were: clearance CL = 17.3 L/h (37.7%), volume V = 429L (51.1%), duration of absorption D1 = 3.2h. Outliers, reflecting potential compliance and time recording errors, were taken into account by estimating an IIV on the residual error (35.4%). Intra-individual residuals were 29.1% (proportional) plus ± 84.6 ng/mL (additive). Female patients had a 15.2% lower CL (14.6 L/h). A piece-wise linear effect of age estimated a CL of 18.7 L/h at 20 years, 17.3 L/h at 40 and 13.8 L/h at 60 years. These covariates explained 2% (CL) and 4.5% (V) of IIV variability. No effect of comedication was found. The sensitivity analysis expectedly estimated increased IIV, but similar fixed effect parameters.¦Conclusion: Imatinib PK was well described in a large cohort of CML patients under field conditions and results were concordant with previous studies. Patient characteristics explain only little IIV, confirming limited utility of prior dosage adjustment. As intra-variability is smaller than inter-patient variability, dose adjustment guided by TDM could however be beneficial in order to bring Cmin into a given therapeutic target.
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Interferon-gamma release assays for the diagnosis of tuberculosis (TB) can give indeterminate results. The prevalence of indeterminate test results (ITRs) among T-SPOT.TB tests was assessed. A retrospective analysis of samples processed in 2005 was performed. ITRs were assessed by age, sex, immunosuppression, distance to the laboratory and season. A subgroup of tests performed for specific indications (contact tracing, migrants with positive tuberculin skin test, TB suspects and immunosuppression) were analysed separately. Of a total of 1,429 tests, 49 (3.4%) were indeterminate. ITRs were significantly associated with old age (>75 versus 5-75 yrs; odds ratio (OR) 7.97, 95% confidence interval (CI) 3.968-15.438) and the season during which samples were transported (autumn and winter versus spring and summer; OR 3.47, 95% CI 1.753-7.514). The incidence of ITR was 302 (2.0%) among TB contacts, 75 (1.6%) among immigrants, 156 (3.0%) in TB suspects and 32 (3.0%) among immunosuppressed patients. Sex, young age and distance to the laboratory were not associated with the rate of ITR. Of the 13 tests with ITR that were repeated, 10 gave a clear positive or negative result. Indeterminate test results with T-SPOT.TB under routine conditions were infrequent and more common in individuals aged >75 yrs than in children and younger adults. The incidence of indeterminate test results was low and similar among healthy tuberculosis contacts, immigrants with a positive tuberculin skin test, tuberculosis suspects and the immunosuppressed. The conditions of transportation may influence the incidence of indeterminate test results.
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Résumé large public Le glucose est une source d'énergie essentielle pour notre organisme, indispensable pour le bon fonctionnement des cellules de notre corps. Les cellules β du pancréas sont chargées de réguler l'utilisation du glucose et de maintenir la glycémie (taux de glucose dans le sang) à un niveau constant. Lorsque la glycémie augmente, ces dernières sécrètent l'insuline, une hormone favorisant l'absorption, l'utilisation et le stockage du glucose. Une sécrétion insuffisante d'insuline provoque une élévation anormale du taux de glucose dans le sang (hyperglycémie) et peut mener au développement du diabète sucré. L'insuline est sécrétée dans le sang par un mécanisme particulier appelé exocytose. Une meilleure compréhension de ce mécanisme est nécessaire dans l'espoir de trouver des nouvelles thérapies pour traiter les 170 millions de personnes atteintes de diabète sucré à travers le monde. L'implication de diverses protéines, comme les SNAREs ou Rabs a déjà été démontrée. Cependant leurs mécanismes d'action restent, à ce jour, peu compris. De plus, l'adaptation de la machinerie d'exocytose à des conditions physiopathologiques, comme l'hyperglycémie, est encore à élucider. Le but de mon travail de thèse a été de clarifier le rôle de deux protéines, Noc2 et Tomosyn, dans l'exocytose ; puis de déterminer les effets d'une exposition prolongée à un taux élevé de glucose sur l'ensemble des protéines de la machinerie d'exocytose. Noc2 est un partenaire potentiel de deux Rabs connues pour leur implication dans les dernières étapes de l'exocytose, Rab3 et Rab27. Grâce à l'étude de différents mutants de Noc2, j'ai montré que l'interaction avec Rab27 permet à la protéine de s'associer avec les organelles de la cellule β contenant l'insuline. De plus, en diminuant sélectivement l'expression de Noc2, j'ai déterminé l'importance de cette protéine pour le bon fonctionnement du processus d'exocytose et le relâchement de l'insuline. Quant à Tomosyn, une protéine interagissant avec les protéines SNAREs, j'ai démontré son importance dans la sécrétion d'insuline en diminuant de manière sélective son expression dans les cellules β. Ensuite, grâce à une combinaison d'approches moléculaires et de microscopie, j'ai mis en évidence le rôle de Tomosyn dans les dernières étapes de l'exocytose. Enfin, puisque la sécrétion d'insuline est diminuée lors d'une hyperglycémie prolongée, j'ai analysé l'adaptation de la machinerie d'exocytose à ces conditions. Ceci m'a permis de découvrir que l'expression de quatre protéines essentielles pour le processus d'exocytose, Noc2, Rab3, Rab27 et Granuphilin, est fortement diminuée lors d'une hyperglycémie chronique. L'ensemble de ces données met en évidence l'importance de Noc2 et Tomosyn dans la sécrétion d'insuline. L'inhibition, par un taux élevé de glucose, de l'expression de Noc2 et d'autres protéines indispensables pour l'exocytose suggère que ce phénomène pourrait contribuer au développement du diabète sucré. Résumé L'exocytose d'insuline, en réponse au glucose circulant dans le sang, est la fonction principale de la cellule β. Celle-ci permet de stabiliser le taux de glucose sanguin (glycémie). Le diabète de type 2 est caractérisé par une glycémie élevée due, principalement, à un défaut de sécrétion d'insuline en réponse au glucose. La compréhension des mécanismes qui contrôlent l'exocytose d'insuline est essentielle pour clarifier les causes du diabète sucré. Plusieurs composants impliqués dans ce processus ont été identifiés. Ceux-ci incluent les SNAREs Syntaxin-1, VAMP2 et SNAP25 et les GTPases Rab3 et Rab27 qui jouent un rôle dans les dernières étapes de l'exocytose. Pendant mon travail de thèse, j'ai étudié le rôle de Noc2, un des partenaires de Rab3 et Rab27, dans l'exocytose d'insuline. Nous avons déterminé que Noc2 s'associe aux granules de sécrétion d'insuline grâce à son interaction avec Rab27. La diminution de l'expression de Noc2 dans la lignée cellulaire β INS-1E, par ARN interférence, influence négativement la sécrétion d'insuline stimulée par différents sécrétagogues et prouve que cette protéine Noc2 est essentielle pour l'exocytose d'insuline. L'interaction avec Munc13, une protéine impliquée dans l'arrimage des vésicules, suggère que Noc2 participe au recrutement des granules d'insuline à la membrane plasmique. Ensuite, j'ai analysé l'adaptation de la machinerie d'exocytose à des concentrations supraphysiologiques de glucose. Le niveau d'expression de Rab3 et Rab27 et de leurs effecteurs Granuphilin/S1p4 et Noc2 est fortement diminué par une exposition prolongée des cellules β à haut glucose. L'effet observé est en relation avec l'induction de l'expression de ICER, un facteur de transcription surexprimé dans des conditions d'hyperglycémie et également dans des modèles génétiques de diabète de type 2. La surexpression de ICER dans des cellules INS-1E diminue l'expression de Rab3, Rab27, Granuphilin/Slp4 et Noc2 et par conséquent l'exocytose d'insuline. Ainsi, l'induction de ICER, après une exposition prolongée à haut glucose, régule négativement l'expression de protéines essentielles pour l'exocytose et altère la sécrétion d'insuline. Ce mécanisme pourrait contribuer au dysfonctionnement de l'exocytose d'insuline dans le diabète de type 2. Dans la dernière partie de ma thèse, j'ai investigué le rôle de la protéine Tomosyn-1 dans la formation du complexe SNARE. Cette protéine a une forte affinité pour Syntaxin-1 et contient un domaine SNARE. Tomosyn-1 est concentrée dans les régions cellulaires enrichies en granules de sécrétion. La diminution sélective de l'expression de Tomosyn-1 induit une réduction de l'exocytose stimulée par différents sécrétagogues. Cet effet est dû à un défaut de fusion des granules avec la membrane plasmique. Ceci nous indique que Tomosyn-1 intervient dans une phase importante de la préparation des vésicules à la fusion, qui est nécessaire à l'exocytose. Abstract: Insulin exocytosis from pancreatic β-cells plays a central role in blood glucose homeostasis. Diabetes mellitus is a complex metabolic disorder characterized by secretory dysfunctions in pancreatic β-cells and release of amounts of insulin that are inappropriate to maintain blood glucose concentration within normal physiological ranges. To define the causes of β-cell failure a basic understanding of the molecular mechanisms that control insulin exocytosis is essential. Some of the molecular components involved in this process have been identified, including the SNARE proteins VAMP2, Syntaxin-1 and SNAP25 and the two GTPases, Rab3 and Rab27, that regulate the final steps of insulin secretion. I first investigated the role of Noc2, a potential Rab3 and Rab27 partner, in insulin secretion. I found that Noc2 associates with Rab27 and is recruited by this GTPase on insulin- containing granules. Silencing of the Noc2 gene by RNA interference led to a strong impairment in the capacity of the β-cell line INS-1E to respond to secretagogues, indicating that appropriate levels of the protein are essential for insulin exocytosis. I also showed that Noc2 interacts with Munc13, a protein that controls vesicle priming, suggesting a possible involvement of Noc2 in the recruitment of secretory granules at the plasma membrane. In the second part of my thesis, I investigated the adaptation of the molecular machinery of exocytosis to physiopathological conditions. I found that the expression of Rab3, Rab27 and of their effectors Granuphilin/Slp4 and Noc2 is dramatically decreased by chronic exposure of β-ce1ls to supraphysiological glucose levels. The observed glucotoxic effect is a consequence of the induction of ICER, a transcriptional repressor that is increased by prolonged hyperglycemia and in genetic models of type 2 diabetes. Overexpression of ICER reduced Granuphilin, Noc2, Rab3 and Rab27 levels and inhibited exocytosis. These results suggest that the presence of inappropriate levels of ICER diminishes the expression of a group of proteins essential for exocytosis and contributes to defective insulin release in type 2 diabetes. In the last part of my thesis, I focused my attention on the role of Tomosyn-1, a Syntaxin-1 binding protein possessing a SNARE-like motif, in the control of SNARE complex assembly. I found that Tomosyn-1 is concentrated in cellular compartments enriched in insulin-containing secretory granules. Silencing of Tomosyn-1 did not affect the number of secretory granules docked at the plasma membrane but decreased their release probability, resulting in a reduction in stimulus-induced insulin exocytosis. These findings suggest that Tomosyn-1 is involved in a post-docking event that prepares secretory granules for fusion and is necessary to sustain exocytosis in response to insulin secretagogues.
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The large Cerro de Pasco Cordilleran base metal deposit in central Peru is located on the eastern margin of a middle Miocene diatreme-dome complex and comprises two mineralization stages. The first stage consists of a large pyrite-quartz body replacing Lower Mesozoic Pucara carbonate rocks and, to a lesser extent, diatreme breccia. This body is composed of pyrite with pyrrhotite inclusions, quartz, and black and red chalcedony (containing hypogene hematite). At the contact with the pyrite-quartz body, the diatreme breccia is altered to pyrite-quartz-sericite-pyrite. This body was, in part, replaced by pipelike pyrrhotite bodies zoned outward to carbonate-replacement Zn-Pb ores hearing Fe-rich sphalerite (up to 24 mol % Fes). The second mineralization stage is partly superimposed on the first and consists of zoned east-west-trending Cu-Ag-(Au-Zn-Pb) enargite-pyrite veins hosted in the diatreme breccia in the western part of the deposit and well-zoned Zn-Pb-(Bi-Ag-Cu) carbonate-replacement orebodies; in both cases, sphalerite is Fe poor and the inner parts of the orebodies show typically advanced argillic alteration assemblages, including aluminum phosphate Sulfate (APS) minerals. The zoned enargite-pyrite veins display mineral zoning, from a core of enargite-pyrite +/- alunite with traces of Au, through an intermediate zone of tennantite, chalcopyrite, and Bi minerals to a poorly developed Outer zone hearing sphalerite-galena +/- kaolinite. The carbonate-hosted replacement ores are controlled along N 35 degrees E, N 90 degrees E, N 120 degrees E, and N 170 degrees E faults. They form well-zoned upward-flaring pipelike orebodies with a core of famatinite-pyrite and alunite, an intermediate zone with tetrahedrite-pyrite, chalcopyrite, matildite, cuprobismutite, emplectite, and other Bi minerals accompanied by APS minerals, kaolinite, and dickite, and an outer zone composed of Fe-poor sphalerite (in the range of 0.05-3.5 mol % Fes) and galena. The outermost zone consists of hematite, magnetite, and Fe-Mn-Zn-Ca-Mg carbonates. Most of the second-stage carbonate-replacement orebodies plunge between 25 degrees and 60 degrees to the west, suggesting that the hydrothermal fluids ascended from deeper levels and that no lateral feeding from the veins to the carbonate-replacement orebodies took place. In the Venencocha and Santa Rosa areas, located 2.5 km northwest of the Cerro de Pasco open pit and in the southern part of the deposit, respectively, advanced argillic altered dacitic domes and oxidized veins with advanced argillic alteration halos occur. The latter veins are possibly the oxidized equivalent of the second-stage enargite-pyrite veins located in the western part of the deposit. The alteration assemblage quartz-muscovite-pyrite associated with the pyrite-quartz body suggests that the first stage precipitated at slightly, acidic fin. The sulfide mineral assemblages define an evolutionary path close to the pyrite-pyrrhotite boundary and are characteristic of low-sulfidation states; they suggest that the oxidizing slightly acidic hydrothermal fluid was buffered by phyllite, shale, and carbonate host rock. However, the presence in the pyrite-quartz body of hematite within quartz suggests that, locally, the fluids were less buffered by the host rock. The mineral assemblages of the second mineralization stage are characteristic of high- to intermediate-sulfidation states. High-sulfidation states and oxidizing conditions were achieved and maintained in the cores of the second-stage orebodies, even in those replacing carbonate rocks. The observation that, in places, second-stage mineral assemblages are found in the inner and outer zones is explained in terms of the hydrothermal fluid advancing and waning. Microthermometric data from fluid inclusions in quartz indicate that the different ores of the first mineralization stage formed at similar temperatures and moderate salinities (200 degrees-275 degrees C and 0.2-6.8 wt % NaCl equiv in the pyrite-quartz body; 192 degrees-250 degrees C and 1.1-4.3 wt % NaCl equiv in the pyrrhotite bodies; and 183 degrees-212 degrees C and 3.2-4.0 wt % NaCl equiv in the Zn-Pb ores). These values are similar to those obtained for fluid inclusions in quartz and sphalerite from the second-stage ores (187 degrees-293 degrees C and 0.2-5.2 wt % NaCl equiv in the enargite-pyrite veins: 178 degrees-265 degrees C and 0.2-7.5 wt % NaCl equiv in quartz of carbonate-replacement orebodies; 168 degrees-999 degrees C and 3-11.8 wt % NaCl equiv in sphalerite of carbonate-replacement orebodies; and 245 degrees-261 degrees C and 3.2-7.7 wt % NaCl equiv in quartz from Venencocha). Oxygen and hydrogen isotope compositions oil kaolinite from carbonate-replacement orebodies (delta(18)O = 5.3-11.5%o, delta D = -82 to -114%o) and on alunite from the Venencocha and Santa Rosa areas (delta(18)O = 1.9-6.9%o, delta D = -56 to -73%o). Oxygen isotope compositions of quartz from the first and second stages have 6180 values from 9.1 to 1.7.8 per mil. Calculated fluids in equilibrium with kaolinite have delta(18)O values of 2.0 to 8.2 and delta D values of -69 to -97 per mil; values in equilibrium with alunite are -1.4 to -6.4 and -62 to -79 per mil. Sulfur isotope compositions of sulfides from both stages have a narrow range of delta(34)S values, between -3.7 and +4.2 per mil; values for sulfates from the second stage are between 4.2 and 31.2 per mil. These results define two mixing trends for the ore-forming fluids. The first trend reflects mixing between a moderately saline (similar to 10 wt % NaCl equiv) magmatic end member that had degassed (as indicated by the low delta D values) and meteoric water. The second mixing indicates condensation of magmatic vapor with HCl and SO(2) into meteoric water, which formed alunite. The hydrothermal system at Cerro de Pasco was emplaced at a shallow depth (similar to 500 m) in the epithermal and upper part of a porphyry environment. The similar temperatures and salinities obtained for the first stage and second stages, together with the stable isotope data, indicate that both stages are linked and represent successive stages of epithermal polymetallic mineralization in the upper part of a porphyry system.
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Identifying the factors that mediate covariation between an ornament and other phenotypic attributes is important to determine the signaling function of ornaments. Sign and magnitude of a covariation may vary across environments if the expression of the ornament or of its linked genes regulating correlated phenotypes is condition-dependent. I investigated in the barn owl Tyto alba whether sign and magnitude of covariation between body mass and two heritable melanin-based plumage ornaments change with food supply, along the reproductive cycle and from the morning to the evening. Using a dataset of 1,848 measurements of body mass in 336 breeding females, I found that females displaying large black spots were heavier than conspecifics with smaller spots in the afternoon (i.e., a long time after the last feeding) but not in the morning (i.e., a short time after the last feeding). This is consistent with the recently proposed hypothesis that eumelanin-based ornaments are associated with the ability to maintain energy balance between food intake and energy expenditure. Thus, covariation between melanin-based coloration and body mass can be detected only under specific conditions potentially explaining why it has been reported in only ten out of 28 vertebrate species. The proposition that ornamented individuals achieve a higher fitness than drab conspecifics only in specific environments should be tested for other ornaments.