313 resultados para Channel patterns
Resumo:
The depositional stratigraphy of within-channel deposits in sandy braided rivers is dominated by a variety of barforms (both singular `unit' bars and complex `compound' bars), as well as the infill of individual channels (herein termed `channel fills'). The deposits of bars and channel fills define the key components of facies models for braided rivers and their within-channel heterogeneity, knowledge of which is important for reservoir characterization. However, few studies have sought to address the question of whether the deposits of bars and channel fills can be readily differentiated from each other. This paper presents the first quantitative study to achieve this aim, using aerial images of an evolving modern sandy braided river and geophysical imaging of its subsurface deposits. Aerial photographs taken between 2000 and 2004 document the abandonment and fill of a 1 3 km long, 80 m wide anabranch channel in the sandy braided South Saskatchewan River, Canada. Upstream river regulation traps the majority of very fine sediment and there is little clay (<1%) in the bed sediments. Channel abandonment was initiated by a series of unit bars that stalled and progressively blocked the anabranch entrance, together with dune deposition and stacking at the anabranch entrance and exit. Complete channel abandonment and subsequent fill of up to 3 m of sediment took approximately two years. Thirteen kilometres of ground-penetrating radar surveys, coupled with 18 cores, were obtained over the channel fill and an adjacent 750 m long, 400 m wide, compound bar, enabling a quantitative analysis of the channel and bar deposits. Results show that, in terms of grain-size trends, facies proportions and scale of deposits, there are only subtle differences between the channel fill and bar deposits which, therefore, renders them indistinguishable. Thus, it may be inappropriate to assign different geometric and sedimentological attributes to channel fill and bar facies in object-based models of sandy braided river alluvial architecture.
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Voltage-gated sodium channels (Navs) are glycoproteins composed of a pore-forming α-subunit and associated β-subunits that regulate Nav α-subunit plasma membrane density and biophysical properties. Glycosylation of the Nav α-subunit also directly affects Navs gating. β-subunits and glycosylation thus comodulate Nav α-subunit gating. We hypothesized that β-subunits could directly influence α-subunit glycosylation. Whole-cell patch clamp of HEK293 cells revealed that both β1- and β3-subunits coexpression shifted V ½ of steady-state activation and inactivation and increased Nav1.7-mediated I Na density. Biotinylation of cell surface proteins, combined with the use of deglycosydases, confirmed that Nav1.7 α-subunits exist in multiple glycosylated states. The α-subunit intracellular fraction was found in a core-glycosylated state, migrating at ~250 kDa. At the plasma membrane, in addition to the core-glycosylated form, a fully glycosylated form of Nav1.7 (~280 kDa) was observed. This higher band shifted to an intermediate band (~260 kDa) when β1-subunits were coexpressed, suggesting that the β1-subunit promotes an alternative glycosylated form of Nav1.7. Furthermore, the β1-subunit increased the expression of this alternative glycosylated form and the β3-subunit increased the expression of the core-glycosylated form of Nav1.7. This study describes a novel role for β1- and β3-subunits in the modulation of Nav1.7 α-subunit glycosylation and cell surface expression.
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Abstract The cardiac sodium channel Nav1.5 plays a key role in cardiac excitability and conduction. Its importance for normal cardiac function has been highlighted by descriptions of numerous mutations of SCN5A (the gene encoding Nav1.5), causing cardiac arrhythmias which can lead to sudden cardiac death. The general aim of my PhD research project has been to investigate the regulation of Nav1.5 along two main axes: (1) We obtained experimental evidence revealing an interaction between Nav1.5 and a multiprotein complex comprising dystrophin. The first part of this study reports the characterization of this interaction. (2) The second part of the study is dedicated to the regulation of the cardiac sodium channel by the mineralocorticoid hormone named aldosterone. (1) Early in this study, we showed that Nav1.5 C-terminus was associated with dystrophin and that this interaction was mediated by syntrophin proteins. We used dystrophin-deficient mdx5cv mice to study the role of this interaction. We reported that dystrophin deficiency led to a reduction of both Nav1.5 protein level and the sodium current (INa). We also found that mdx5cv mice displayed atrial and ventricular conduction defects. Our results also indicated that proteasome inhibitor MG132 treatment of mdx5cv mice rescued Nav1.5 protein level and INa in cardiac tissue. (2) We showed that aldosterone treatment of mice cardiomyocytes led to an increase of the sodium current with no modification of Nav1.5 transcript and protein level. Altogether, these results suggest that the sodium current can be increased by distribution of intracellular pools of protein to the plasma membrane (e.g. upon aldosterone stimulation) and that interaction with dystrophin multiprotein complex is required for the stabilization of the channel at the plasma membrane. Finally, we obtained preliminary results suggesting that the proteasome could regulate Nav1.5 in mdx5cv mice. This study defines regulatory mechanisms of Nav1.5 which could play an important role in cardiac arrhythmia and bring new insight in cardiac conduction alterations observed in patients with dystrophinopathies. Moreover, this work suggests that Brugada syndrome, and some of the cardiac alterations seen in Duchenne patients may be caused by overlapping molecular mechanisms leading to a reduction of the cardiac sodium current.
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Abstract The epithelial sodium channel (ENaC) is composed of three homologous subunits α, ß, and γ. This channel is involved in the regulation of sodium balance, which influences the periciliary liquid level in the lung, and blood pressure via the kidney. ENaC expressed in Xenopus laevis oocytes is preferentially and rapidly assembled into heteromeric αßγ complexes. Expression of homomeric α or heteromeric αß and αγ complexes lead to channel expression at the cell surface wíth low activities. Recent studies have demonstrated that α and γ (but not ß) ENaC subunits undergo proteolytic cleavage by endogenous proteases (i.e. furin) correlating with increased channel activity. We therefore assayed the full-length subunits and their cleavage products at the cell surface, as well as in the intracellular pool for all homo- and heteromeric combínations (α, ß, γ, ßγ, αß, αγ, ßγ and αßγ) and measured the corresponding channel activities as amiloride-sensitive sodíum transport (INa). We showed that upon assembly, cleavage of the y ENaC subunit ís responsible for increasing INa. We further demonstrated that in disease states such as cystic fibrosis (CF) where there is disequilibrium in the proteaseprotease inhibitor balance, ENaC is over-activated by the serine protease elastase (NE). We demonstrated that elevated NE concentrations can cleave cell surface expressed γ ENaC (but not α, or ß ENaC), suggesting a causal relationship between γ ENaC cleavage and ENaC activation, taking place at the plasma membrane. In addition, we demonstrated that the serine protease inhibitor (serpin) serpinH1, which is co-expressed with ENaC in the distal nephron is capable of inhibiting the channel by preventing cleavage of the γ ENaC subunit. Aldosterone mediated increases in INa aze known to be inhibted by TGFß. TGFß is also known to increase serpinHl expression. The demonstrated inhibition of γ ENaC cleavage and channel activation by serpinH1 may be responsible for the effect of TGFß on aldosterone stimulation in the distal nephron. In summary, we show that cleavage of the γ subunit, but not the α or ß subunit is linked to channel activation in three seperate contexts. Résumé Le canal épithélial à sodium (ENaC) est constitué de trois sous-unités homologues α, ß, and γ. Ce canal est impliqué dans le maintien de la balance sodique qui influence le niveau du liquide périciliaire du poumon et la pression sanguine via le rein. Dans les ovocytes de Xenopus laevis ENaC est préférentiellement et rapidement exprimé en formant un complexe hétéromérique αßγ. En revanche, l'expression homomérique de α ou hétéromérique des complexes αß et αγ conduit à une expression à la surface cellulaire d'un canal ENaC ne possédant qu'une faible activité. Des études récentes ont mis en évidence que les sous-unités α et γ d'ENaC (mais pas ß) sont coupées par des protéases endogènes (les farines) et que ces clivages augmentent l'activité du canal. Nous avons donc analysé, aussi bien à la surface cellulaire que dans le cytoplasme, les produits des clivages de combinaison homo- et hétéromérique des sous-unités d'ENaC (α, ß, γ, ßγ, αß, αγ, ßγ et αßγ). En parallèle, nous avons étudié l'activité correspondante à ces canaux par la mesure du transport de sodium sensible à l'amiloride (INa). Nous avons montré que lors de l'assemblage des sous-unités d'ENaC, le clivage de γ correspond à l'augmentation de INa. Nous avons également mis en évidence que dans une maladie telle que la fibrose cystique (CF) caractérisée par un déséquilibre de la balance protéase-inhibiteur de protéase, ENaC est suractivé par une sérine protéase nommée élastase (NE). L'augmentation de la concentration de NE clive γ ENaC exprimé à la surface cellulaire (mais pas α, ni ß ENaC) suggérant une causalité entre le clivage d'ENaC et son activation à la membrane plasmique. De plus, nous avons démontré que l'inhibiteur de sérine protéase (serpin) serpinH1, qui est co-exprimé avec ENaC dans le néphron distal, inhibe l'activité du canal en empêchant le clivage de la sous-unité γ ENaC. Il est connu que le INa induit par l'aldostérone peut être inhibé par TGFß. Or TGFß augmente l'expression de serpinH1. L'inhibition du clivage de γ ENaC et de l'activation du canal par la serpinH1 que nous avons mis en évidence pourrait ainsi être responsable de l'effet de TGFß sur la stimulation du courant par l'aldostérone dans le néphron distal. En résumé, nous avons montré que le clivage de la sous-unité γ, mais pas des sous-unités α et ß, est lié à l'activation du canal dans trois contextes distincts. Résumé tout public Le corps humain est composé d'environ 10 000 milliards de cellules et d'approximativement 60% d'eau. Les cellules du corps sont les unités fondamentales de la vie et elles sont dépendantes de certains nutriments et molécules. Ces nutriments et molécules sont dissous dans l'eau qui est présente dans et hors des cellules. Le maintien d'une concentration adéquate - de ces nutriments et de ces molécules dans l'eau à l'intérieur et à l'extérieur des cellules est -..essentiel pour leur survie. L'eau hors des cellules est nommée le fluide extracellulaire et peut être subdivisée en fluide interstitiel, qui se trouve autour des cellules, et en plasma, qui est le fluide des vaisseaux sanguins. Les fluides, les nutriments et les molécules sont constamment échangés entre les cellules, le fluide interstitiel, et le plasma. Le plasma circule dans le système circulatoire afin de distribuer les nutriments et molécules dans tout le corps et afin d'enlever les déchets cellulaires. Le rein joue un rôle essentiel dans la régulation du volume et de la concentration du plasma en éliminant sélectivement les nutriments et les molécules via la formation de l'urine. L'être humain possède deux reins, constitués chacun d'environ 1 million de néphrons. Ces derniers sont responsables de réabsorber et de sécréter sélectivement les nutriments et les molécules. Le canal épithélial à sodium (ENaC) est localisé à la surface cellulaire des néphrons et est responsable de la réabsorption du sodium (Na+). Le Na+ est présent dans quasiment toute la nourriture que nous mangeons et représente, en terme de molécule, 50% du sel de cuisine. Si trop de sodium est consommé, ENaC est inactif, si bien que le Na+ n'est pas réabsorbé et quitte le corps par l'urine. Ce mécanisme permet d'éviter que la concentration plasmatique de Na+ ne devienne trop grande, ce qui résulterait en une augmentation de la pression sanguine. Si trop peu de Na+ est consommé, ENaC réabsorbe le Na+ de l'urine primaire ce qui permet de conserver la concentration de Na+ et de prévenir une diminution de la pression sanguine par une perte de Na+. ENaC est aussi présent dans les cellules des poumons qui sont les organes permettant la respiration. La respiration est aussi essentielle pour la survie des cellules. Les poumons ne doivent pas contenir trop de liquide afin de permettre la respiration, mais en même temps ils ne doivent pas non plus être trop secs. En effet, ceci tuerait les cellules et empêcherait aussi la respiration. ENaC permet de maintenir un niveau d'humidité approprié dans les poumons en absorbant du Na+ ce qui entraîne un mouvement osmotique d'eau. L'absorption de sodium par ENaC ~ est augmentée par les protéases (in vitro et ex vivo). Les protéases sont des molécules qui peuvent couper d'autres molécules à des endroits précis. Nous avons démonté que certaines protéases augmentent l'absorption de Na+ en coupant ENaC à des endroits spécifiques. L'inhibition de ces protéases diminue le transport de Na+ et empêche le clivage d'ENaC. Dans certaines maladies telle que la mucoviscidose, des protéases sont suractivées et augmentent l'activité d'ENaC de manière inappropriée conduisant à une trop forte absorption de Na+ et à un déséquilibre de la muqueuse des poumons. Cette étude est donc particulièrement importante dans le cadre de la recherche thérapeutique de ce genre de maladie.
Resumo:
To date, published studies of alluvial bar architecture in large rivers have been restricted mostly to case studies of individual bars and single locations. Relatively little is known about how the depositional processes and sedimentary architecture of kilometre-scale bars vary within a multi-kilometre reach or over several hundreds of kilometres downstream. This study presents Ground Penetrating Radar and core data from 11, kilometre-scale bars from the Rio Parana, Argentina. The investigated bars are located between 30km upstream and 540km downstream of the Rio Parana - Rio Paraguay confluence, where a significant volume of fine-grained suspended sediment is introduced into the network. Bar-scale cross-stratified sets, with lengths and widths up to 600m and thicknesses up to 12m, enable the distinction of large river deposits from stacked deposits of smaller rivers, but are only present in half the surface area of the bars. Up to 90% of bar-scale sets are found on top of finer-grained ripple-laminated bar-trough deposits. Bar-scale sets make up as much as 58% of the volume of the deposits in small, incipient mid-channel bars, but this proportion decreases significantly with increasing age and size of the bars. Contrary to what might be expected, a significant proportion of the sedimentary structures found in the Rio Parana is similar in scale to those found in much smaller rivers. In other words, large river deposits are not always characterized by big structures that allow a simple interpretation of river scale. However, the large scale of the depositional units in big rivers causes small-scale structures, such as ripple sets, to be grouped into thicker cosets, which indicate river scale even when no obvious large-scale sets are present. The results also show that the composition of bars differs between the studied reaches upstream and downstream of the confluence with the Rio Paraguay. Relative to other controls on downstream fining, the tributary input of fine-grained suspended material from the Rio Paraguay causes a marked change in the composition of the bar deposits. Compared to the upstream reaches, the sedimentary architecture of the downstream reaches in the top ca 5m of mid-channel bars shows: (i) an increase in the abundance and thickness (up to metre-scale) of laterally extensive (hundreds of metres) fine-grained layers; (ii) an increase in the percentage of deposits comprised of ripple sets (to >40% in the upper bar deposits); and (iii) an increase in bar-trough deposits and a corresponding decrease in bar-scale cross-strata (<10%). The thalweg deposits of the Rio Parana are composed of dune sets, even directly downstream from the Rio Paraguay where the upper channel deposits are dominantly fine-grained. Thus, the change in sedimentary facies due to a tributary point-source of fine-grained sediment is primarily expressed in the composition of the upper bar deposits.
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Estimation of the dimensions of fluvial geobodies from core data is a notoriously difficult problem in reservoir modeling. To try and improve such estimates and, hence, reduce uncertainty in geomodels, data on dunes, unit bars, cross-bar channels, and compound bars and their associated deposits are presented herein from the sand-bed braided South Saskatchewan River, Canada. These data are used to test models that relate the scale of the formative bed forms to the dimensions of the preserved deposits and, therefore, provide an insight as to how such deposits may be preserved over geologic time. The preservation of bed-form geometry is quantified by comparing the Alluvial architecture above and below the maximum erosion depth of the modem channel deposits. This comparison shows that there is no significant difference in the mean set thickness of dune cross-strata above and below the basal erosion surface of the contemporary channel, thus suggesting that dimensional relationships between dune deposits and the formative bed-form dimensions are likely to be valid from both recent and older deposits. The data show that estimates of mean bankfull flow depth derived from dune, unit bar, and cross-bar channel deposits are all very similar. Thus, the use of all these metrics together can provide a useful check that all components and scales of the alluvial architecture have been identified correctly when building reservoir models. The data also highlight several practical issues with identifying and applying data relating to cross-strata. For example, the deposits of unit bars were found to be severely truncated in length and width, with only approximately 10% of the mean bar-form length remaining, and thus making identification in section difficult. For similar reasons, the deposits of compound bars were found to be especially difficult to recognize, and hence, estimates of channel depth based on this method may be problematic. Where only core data are available (i.e., no outcrop data exist), formative flow depths are suggested to be best reconstructed using cross-strata formed by dunes. However, theoretical relationships between the distribution of set thicknesses and formative dune height are found to result in slight overestimates of the latter and, hence, mean bankfull flow depths derived from these measurements. This article illustrates that the preservation of fluvial cross-strata and, thus, the paleohydraulic inferences that can be drawn from them, are a function of the ratio of the size and migration rate of bed forms and the time scale of aggradation and channel migration. These factors must thus be considered when deciding on appropriate length:thickness ratios for the purposes of object-based modeling in reservoir characterization.
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In order to evaluate the relationship between the apparent complexity of hillslope soil moisture and the emergent patterns of catchment hydrological behaviour and water quality, we need fine-resolution catchment-wide data on soil moisture characteristics. This study proposes a methodology whereby vegetation patterns obtained from high-resolution orthorectified aerial photographs are used as an indicator of soil moisture characteristics. This enables us to examine a set of hypotheses regarding what drives the spatial patterns of soil moisture at the catchment scale (material properties or topography). We find that the pattern of Juncus effusus vegetation is controlled largely by topography and mediated by the catchment's material properties. Characterizing topography using the topographic index adds value to the soil moisture predictions relative to slope or upslope contributing area (UCA). However, these predictions depart from the observed soil moisture patterns at very steep slopes or low UCAs. Copyright (c) 2012 John Wiley & Sons, Ltd.
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BACKGROUND: No previous studies have explored how closely women follow their psychotropic drug regimens during pregnancy. This study aimed to explore patterns of and factors associated with low adherence to psychotropic medication during pregnancy. METHODS: Multinational web-based study was performed in 18 countries in Europe, North America, and Australia. Uniform data collection was ensured via an electronic questionnaire. Pregnant women were eligible to participate. Adherence was measured via the 8-item Morisky Medication Adherence Scale (MMAS-8). The Beliefs about Prescribed Medicines Questionnaire (BMQ-specific), the Edinburgh Postnatal Depression Scale (EPDS), and a numeric rating scale were utilized to measure women's beliefs, depressive symptoms, and antidepressant risk perception, respectively. Participants reporting use of psychotropic medication during pregnancy (n = 160) were included in the analysis. RESULTS: On the basis of the MMAS-8, 78 of 160 women (48.8%, 95% CI: 41.1-56.4%) demonstrated low adherence during pregnancy. The rates of low adherence were 51.3% for medication for anxiety, 47.2% for depression, and 42.9% for other psychiatric disorders. Smoking during pregnancy, elevated antidepressant risk perception (risk≥6), and depressive symptoms were associated with a significant 3.9-, 2.3-, and 2.5-fold increased likelihood of low medication adherence, respectively. Women on psychotropic polytherapy were less likely to demonstrate low adherence. The belief that the benefit of pharmacotherapy outweighed the risks positively correlated (r = .282) with higher medication adherence. CONCLUSIONS: Approximately one of two pregnant women using psychotropic medication demonstrated low adherence in pregnancy. Life-style factors, risk perception, depressive symptoms, and individual beliefs are important factors related to adherence to psychotropic medication in pregnancy.
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BACKGROUND: Predicting outcome of breast cancer (BC) patients based on sentinel lymph node (SLN) status without axillary lymph node dissection (ALND) is an area of uncertainty. It influences the decision-making for regional nodal irradiation (RNI). The aim of the NORA (NOdal RAdiotherapy) survey was to examine the patterns of RNI. METHODS: A web-questionnaire, including several clinical scenarios, was distributed to 88 EORTC-affiliated centers. Responses were received between July 2013 and January 2014. RESULTS: A total of 84 responses were analyzed. While three-dimensional (3D) radiotherapy (RT) planning is carried out in 81 (96%) centers, nodal areas are delineated in only 51 (61%) centers. Only 14 (17%) centers routinely link internal mammary chain (IMC) and supraclavicular node (SCN) RT indications. In patients undergoing total mastectomy (TM) with ALND, SCN-RT is recommend by 5 (6%), 53 (63%) and 51 (61%) centers for patients with pN0(i+), pN(mi) and pN1, respectively. Extra-capsular extension (ECE) is the main factor influencing decision-making RNI after breast conserving surgery (BCS) and TM. After primary systemic therapy (PST), 49 (58%) centers take into account nodal fibrotic changes in ypN0 patients for RNI indications. In ypN0 patients with inner/central tumors, 23 (27%) centers indicate SCN-RT and IMC-RT. In ypN1 patients, SCN-RT is delivered by less than half of the centers in patients with ypN(i+) and ypN(mi). Twenty-one (25%) of the centers recommend ALN-RT in patients with ypN(mi) or 1-2N+ after ALND. Seventy-five (90%) centers state that age is not considered a limiting factor for RNI. CONCLUSION: The NORA survey is unique in evaluating the impact of SLNB/ALND status on adjuvant RNI decision-making and volumes after BCS/TM with or without PST. ALN-RT is often indicated in pN1 patients, particularly in the case of ECE. Besides the ongoing NSABP-B51/RTOG and ALLIANCE trials, NORA could help to design future specific RNI trials in the SLNB era without ALND in patients receiving or not PST.
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Alternative splicing produces multiple isoforms from the same gene, thus increasing the number of transcripts of the species. Alternative splicing is a virtually ubiquitous mechanism in eukaryotes, for example more than 90% of protein-coding genes in human are alternatively spliced. Recent evolutionary studies showed that alternative splicing is a fast evolving and highly species- specific mechanism. The rapid evolution of alternative splicing was considered as a contribution to the phenotypic diversity between species. However, the function of many isoforms produced by alternative splicing remains unclear and they might be the result of noisy splicing. Thus, the functional relevance of alternative splicing and the evolutionary mechanisms of its rapid divergence among species are still poorly understood. During my thesis, I performed a large-scale analysis of the regulatory mechanisms that drive the rapid evolution of alternative splicing. To study the evolution of alternative splicing regulatory mechanisms, I used an extensive RNA-sequencing dataset comprising 12 tetrapod species (human, chimpanzee and bonobo, gorilla, orangutan, macaque, marmoset, mouse, opossum, platypus, chicken and frog) and 8 tissues (cerebellum, brain, heart, kidney, liver, testis, placenta and ovary). To identify the catalogue of alternative splicing eis-acting regulatory elements in the different tetrapod species, I used a previously defined computational approach. This approach is a statistical analysis of exons/introns and splice sites composition and relies on a principle of compensation between splice sites strength and the presence of additional regulators. With an evolutionary comparative analysis of the exonic eis-acting regulators, I showed that these regulatory elements are generally shared among primates and more conserved than non-regulatory elements. In addition, I showed that the usage of these regulatory elements is also more conserved than expected by chance. In addition to the identification of species- specific eis-acting regulators, these results may explain the rapid evolution of alternative splicing. I also developed a new approach based on evolutionary sequence changes and corresponding alternative splicing changes to identify potential splicing eis-acting regulators in primates. The identification of lineage-specific substitutions and corresponding lineage-specific alternative splicing changes, allowed me to annotate the genomic sequences that might have played a role in the alternative splicing pattern differences among primates. Finally, I showed that the identified splicing eis-acting regulator datasets are enriched in human disease-causing mutations, thus confirming their biological relevance.