, 2009 and Meijer et al , 2009), are now appearing in the 2009 pa

, 2009 and Meijer et al., 2009), are now appearing in the 2009 pandemic virus (Duan et al., 2010, Hamelin et al., 2010 and Ujike

et al., 2011). New broad-spectrum counter-measures, which do not result in virus resistance, are urgently required. Oseltamivir was preclinically tested in ferrets and these animals are the preferred model for studying study new viruses and investigating oseltamivir-resistant strains (Boltz et al., 2008, Govorkova et al., 2006, Govorkova et al., 2011, Hamelin et al., 2010, Herlocher et al., 2004, Itoh et al., this website 2009 and Mendel et al., 1998). Thus we have used this model to compare the protective abilities of cloned DI 244/PR8 and oseltamivir. Data presented here show that a single

intranasal dose of 2 μg of DI RNA is overall more effective than 10 doses of 2.5 mg/kg bodyweight administered twice daily over five days (25 mg/kg in total) of oseltamivir at ameliorating the effects of pandemic influenza virus A/California/04/09 (H1N1). Ferret work was conducted according to UK Home Office legislation and was approved by the local ethical committee. Thirty outbred male ferrets (Mustela putorius furo), 3–4 months of age, selleck screening library weighing 860–1367 g (mean 1082 g), were obtained from Highgate Farm, UK. They were seronegative for antibodies to A/Cal as determined by haemagglutination-inhibition. Ferrets were separated into 4 groups each comprising five animals: groups were treated intranasally with +300 μg active 244 DI virus and infected with A/Cal 2 h later, treated with oseltamivir by oral gavage (see below) and infected with A/Cal

2 h later, infected with A/Cal, and inoculated with saline. An identifier chip (idENTICHIP, Bio-Thermo) was inserted subcutaneously into the scruff of each animal. Ferrets receiving 244 DI virus (see below) were Low-density-lipoprotein receptor kinase sedated by isoflurane inhalation before intranasal delivery of 500 μl (250 μl per nostril) of a single dose of 2 μg of 244 RNA in 300 μg of carrier virus. Ferrets receiving oseltamivir treatment were given 2.5 mg/kg bodyweight administered by oral gavage twice-daily every twelve hours (5 mg/kg bodyweight/day) over a period of five days as used by others ( Govorkova et al., 2007 and Hurt et al., 2010), which is comparable to an oral prophylactic human dose of 75 mg/kg bodyweight/day ( Ward et al., 2005). Oseltamivir phosphate was acquired as oseltamivir powder (Roche) for oral suspension and was reconstituted with sterile water to a final concentration of 12 mg/ml. The volume of oseltamivir solution required for each ferret was calculated from the weight of each ferret recorded each morning on the day of administration. This oseltamivir dose and schedule protected ferrets from the highly virulent H5N1 virus (A/Vietnam/1023/04) when administered at 4 h after infection and then twice daily for 5 days ( Govorkova et al., 2007).

Finally, to assess the effects of visual strategies (foil categor

Finally, to assess the effects of visual strategies (foil categories), visual complexity, task-order, grammar abilities and non-verbal intelligence, we used a semiparametric regression technique called Generalized Estimating Equations (GEE), a technique useful when analyzing binomial data with within-subjects effects (Hanley, 2003). We created several models containing

different variables: ‘grade’ and ‘task-order’ as between-subjects variables; ‘task’, ‘foil category’ and ‘visual complexity’ as within-subjects variables; and ‘grammar’ and ‘intelligence’ raw scores as covariates. All analyses were performed with SPSS® 19. General overview: correct responses by grade. On average, the 26 children attending the fourth grade (M = 0.80, SD = 0.21) had a significantly higher proportion of correct responses in VRT than children attending Selleckchem LDN 193189 the second grade (M = 0.59,

SD = 0.17) (Mann–Whitney U: z = −3.70, p < 0.001; Fig. 7). selleck compound Moreover, while 69.2% of fourth graders had a proportion of correct answers above chance, only 26.9% of the second graders had so. This difference was also significant (χ2 = 9.43, p = 0.002). One child in the fourth grade and one in the second grade had performance scores lower than predicted by chance (i.e. equal or lower than 26%). This means that these children discriminated recursive items from foils more than 74% of the trials, but still consistently chose the foils. These two participants were excluded from further regression and correlation analyses involving VRT because even though they induced a rule that allowed them to distinguish recursive items from foils, they would be treated as performing worse than other participants performing randomly. Since

Mirabegron we were interested in investigating the cognitive underpinnings of the ability to represent recursion, these two subjects would be ambiguous and noisy data points. 2 Visual strategies. A central issue concerning our method is the question of whether participants were able to represent the structural self-similarity present in the recursive images; and to apply this knowledge throughout different VRT trials. One possible alternative to the representation of self-similarity would be the usage of heuristic strategies, based on the detection of simple salient features within the foils, which would allow their exclusion without an understanding of the underlying structure. In order to prevent the emergence of a systematic ‘choice-by-exclusion’ strategy, we used different categories of foils. Our assumption was that, if individuals were able to represent self-similarity, they would perform adequately in all different foil categories. At the group level, the number of correct choices was significantly above chance for all foil categories and for both grade groups (Binomial test, p < 0.005). For detailed analyses comparing performance across categories see Appendix C. Visual complexity.

Sediment cores were obtained from the deepest point of each lake

Sediment cores were obtained from the deepest point of each lake using a 7.6 cm diameter Glew or Kaja–Brinkhurst gravity corer (Glew et al., 2001). Cores were extruded at 0.25–1 cm intervals for standard bulk physical property analyses and 210Pb radiometric dating using a Constant Rate of Supply (CRS) model (Turner and Delorme, 1996). MyCore Scientific Inc. (Deep River, Ontario, Canada) completed all of the 210Pb dating and sedimentation rate calculations. GIS databases were used to store spatiotemporal data relating check details to catchment topography and land use history. Base topographic data was obtained from the Terrain Resource Inventory Management

(TRIM) program (1:20k) (Geographic Data BC, 2002) for catchments in British Columbia and from the National Topographic System (NTS) database (1:50k) (Natural Resources Canada, 2009) for catchments in Alberta. Land use features were extracted and dated from provincial forest cover maps, remotely sensed imagery (aerial photography and Landsat imagery), and other land management maps, where available. Additional methodological details associated with initial development of the lake catchment inventories are provided by Spicer (1999), Schiefer et al. (2001a), and Schiefer and Immell (2012). We combined the three pre-existing

datasets into a single dataset (104 lake catchments) to represent contemporary patterns of lake sedimentation and catchment land use in western Canada. The 210Pb-based sedimentation rate profiles

were smoothed from their irregular raw chronologies to fixed, 5-year intervals from 1952–1957 to 1992–1997 (n = 9) (1952–1957 RNA Synthesis inhibitor to 2002–2007 (n = 11) for the more recent Schiefer and Immell (2012) data) to simplify the modeling and interpretation of nonlinear changes in sedimentation rates over time, and to approximately match the average observation frequency of land use covariates. The ending of the last resampled intervals at 1997 and 2007 was convenient because those were the sediment sampling years in the previous studies used for this reanalysis. For smoothing, we calculated the average sedimentation rate within each interval based on linear interpolation between Tideglusib raw chronology dates. Minimal land use activity had taken place in the study catchments during the first half of the 20th century. We therefore used the median value from 1900 to 1952 as a measure of the pre-land use disturbance, or ‘background’, sedimentation rate for each lake. Use of a median filter reduces the influence of episodically high sediment delivery associated with extreme hydrogeomorphic events, such as severe floods and extensive mass wasting. We chose not to use a minimum pre-disturbance sedimentation rate as a measure of background because analytical and sampling constraints in 210Pb dating can yield erroneously old ages for deeper sections of core, which could result in underestimation of background rates (e.g. MacKenzie et al., 2011).

The increase in hepatic triglyceride accumulation after EtOH feed

The increase in hepatic triglyceride accumulation after EtOH feeding was significantly inhibited by RGE treatment (Fig. 2A). Lipid accumulation was also assessed by Oil Red O staining. Control mice did not show steatosis, whereas EtOH-fed mice exhibited a substantial increase in lipid droplets, which was in line with the results of H&E microscopy (Fig. 2B). RGE completely inhibited lipid infiltration in the liver, confirming high throughput screening compounds the ability of RGE to prevent hepatic fat accumulation. The expression of hepatic fat metabolism-related genes was also assessed by quantitative real-time PCR. As shown in Fig. 3A, hepatic expression of

several lipogenic gene, including SREBP-1, FAS, and ACC was Cobimetinib cell line upregulated by EtOH feeding. This enhancement was completely reversed by RGE treatment. As previously reported, chronic alcohol consumption decreased fat oxidation-related genes, such as

Sirt1 and PPARα. However, RGE prevented EtOH-mediated decreases in lipogenic gene expression (Fig. 3A). Furthermore, RGE abolished the EtOH-induced enhancement SREBP-1 and depletion of PPARα protein in the liver (Fig. 3B). These results demonstrate that RGE inhibits EtOH-induced lipogenesis and restores alcohol-mediated decreases in fatty acid oxidation. Sustained exposure to EtOH leads to prolonged oxidative stress, which promotes lipid peroxidation and generation of reactive aldehydes, such as 4-HNE [27]. Previously, 4-HNE-positive cells were markedly increased in mice fed alcohol. However, RGE treatment led to a significant, dose-dependent reduction in 4-HNE positive cells (Fig. 4A). These data provide direct evidence that RGE

effectively inhibits lipid peroxidation and the formation of 4-HNE to protect hepatocytes from necrotic changes caused by EtOH. It is well known that prolonged reactive oxygen species (ROS) exposure leads to increased nitrotyrosine levels [28]. Nitrotyrosine immunoreactive cells were increased in the chronic EtOH-administration group as compared with the GABA Receptor control. However, RGE treatment dramatically reduced the number of nitrotyrosine positive cells (Fig. 4B). We next assessed whether RGE treatment inhibited the induction of CYP2E1 caused by chronic alcohol intake. As anticipated, RGE significantly repressed the induction of CYP2E1 by EtOH (Fig. 4C). Our present data suggest that RGE protects against chronic alcohol-induced oxidative stress and hepatic injury. Next, we examined whether the effect of RGE on hepatic steatosis is associated with AMPK activation. Immunoblot analysis showed that the level of phosphorylated AMPKα in liver homogenates notably decreased after 4 weeks of alcohol administration as previously reported (Fig. 5) [24]. Treatment of alcohol-fed mice with RGE resulted in a complete recovery of AMPKα phosphorylation levels. We further measured the levels of phosphorylated ACC, a direct downstream substrate of AMPK.

Londoño (2008) highlighted the effect of abandonment on the Inca

Londoño (2008) highlighted the effect of abandonment on the Inca agricultural terraces since ∼1532 A.D., represented by the development of rills and channels on terraces where the vegetation is absent. Lesschen et al. (2008) underlined the fact that that terracing, although intended as a conservation practice, enhances erosion (gully erosion through the terrace walls), especially after abandonment. These authors carried out a study in the Carcavo basin, a semi-arid area in southeastern Spain. More

than half of the abandoned fields in the catchment area are subject to moderate and severe erosion. According to these studies, the land abandonment, the steeper terrace slope, the loam texture of the soils, the valley bottom position, and the presence of shrubs on the terrace walls are all factors that increase the risk of terrace failure. Construction of new terraces should therefore be carefully planned find more and be built according to sustainable design criteria (Lesschen et al., 2008). Lesschen et al. (2008) provided guidelines to avoid the land erosion due to abandonment. They suggested the maintenance of terrace walls in combination with an increase in vegetation cover on the terrace, and the re-vegetation of indigenous grass species on zones with concentrated flow to prevent gully erosion. Lesschen et al. (2009) simulated the runoff

and sediment yield of a landscape scenario without agricultural terraces. They found values higher by ALOX15 factors of four and nine, respectively, when compared to areas with terraces. Meerkerk et al. (2009) examined http://www.selleckchem.com/products/cobimetinib-gdc-0973-rg7420.html the effect of terrace removal and failure on hydrological connectivity and peak discharge in a study area of 475 ha in southeastern Spain. They considered three scenarios: 1956 (with terraces), 2006 (with abandoned terraces), and S2 (without terraces). The analysis

was carried out with a storm return interval of 8.2 years. The results show that the decrease in intact terraces is related to a significant increase in connectivity and discharge. Conversely, catchments with terraces have a lower connectivity, contributing area of concentrated flow, and peak discharge. Bellin et al. (2009) presented a case study from southeastern Spain on the abandonment of soil and water conservation structures in Mediterranean ecosystems. Extensive and increasing mechanization of rainfed agriculture in marginal areas has led to a change in cropping systems. They observed that step terraces have decreased significantly during the last 40 years. Many terraces have not been maintained, and flow traces indicate that they no longer retain water. Furthermore, the distance between the step terraces has increased over time, making them vulnerable to erosion. Petanidou et al. (2008) presented a case study of the abandonment of cultivation terraces on Nisyros Island (Greece).


“The authors regret that there is an error in the ‘Abstrac


“The authors regret that there is an error in the ‘Abstract’ of this published article. The corrected abstract is as follows: We know that from mid-childhood onwards

most new words are learned implicitly via reading; however, most word learning studies have taught novel items explicitly. We examined incidental word learning during reading by focusing on the well-documented finding that words which are acquired early in life are processed more quickly than those acquired SCR7 chemical structure later. Novel words were embedded in meaningful sentences and were presented to adult readers early (day 1) or later (day 2) during a five-day exposure phase. At test adults read the novel words in semantically neutral sentences. Participants’ eye movements were monitored throughout exposure and test. Adults also completed a surprise memory test in which they had to match each novel word with its definition. Results showed a decrease in reading times for all novel words over exposure, and significantly shorter total reading times at test for early than late novel words. Early-presented novel words were also remembered better in the offline test. Our results show that order of presentation influences processing time early in the course of acquiring a new word, consistent with partial PD0325901 solubility dmso and incremental growth

in knowledge occurring as a function of an individual’s experience with each word. “
“Eutrophication drives numerous lakes worldwide to a deteriorated state where phytoplankton dominate over macrophytes (Smith et al., 1999). As a result, species composition changes (Jeppesen et al., 2000 and Smith et al., 1999), toxic algal blooms proliferate (Paerl et al., 2011a) and drinking Methocarbamol water supplies dwindle (Falconer and Humpage, 2005 and Smith et al., 1999). The transition to a phytoplankton dominated state is often non-linear and in many cases catastrophic (Scheffer et al., 2000). In case of a catastrophic transition, a change from the macrophyte dominating

state to the alternative phytoplankton state will be rapid and recovery may show hysteresis (alternative stable states) when positive feedbacks between macrophytes and phytoplankton are strong (Scheffer et al., 1993). Small lakes are more likely to exhibit a macrophyte-rich state than large lakes (Van Geest et al., 2003) primarily because small lakes are less prone to destructive wind forces (Janse et al., 2008) and fish are less abundant (Scheffer and Van Nes, 2007). Examples of small lakes that shifted between the macrophyte and phytoplankton dominated state are the gravel pit lakes in England (< 1 km2, < 2 m depth) (Scheffer et al., 1993 and Wright and Phillips, 1992) and Lake Veluwe in the Netherlands (30 km2, 1.5 m depth) (Meijer, 2000). But there are also larger lakes with macrophytes, and where alternative stable states are presumed.

(2007) cite Pakistan Irrigation Department data indicating that 7

(2007) cite Pakistan Irrigation Department data indicating that 7.2 Gt of sediment was delivered to the Indus Delta at a mean rate of 100.6 Mt/y. Therefore if the delivery of 100 Mt/y of river sediment results in a net land loss equivalent of 47 Mt/y, then the pre-Anthropocene flux estimate of 250 Mt/y (Milliman FG4592 et al., 1984) would result in an active Indus Delta able to both aggrade and prograde seaward. The sediment budget remains qualitative, as it does not take into account subsidence across the delta, for lack of quantitative data. Satellite analysis suggests that there is significant sedimentation

within the inner tidal flats of the Rann of Kachchh (Fig. 10), further complicating a full quantitative assessment. Although part of the Rann of Kachchh (Lake Sindri south of the Allah Bund) underwent >1 m of incremental tectonic subsidence in 1819 it is not known

whether slow secular subsidence occurs between earthquakes, either due to tectonic subsidence or sediment compaction. The 1945 Makran earthquake resulted in a tsunami that inundated the ports of Karachi and Mumbai, but no record of its effects have been preserved in the delta region (Bilham et al., 2007). The recent 2001 Mw = 7.6 Bhuj earthquake (Fig. 3) resulted in local subsidence in the southeastern Rann of Kachchh and was responsible for an estimated 20,000 deaths (Bodin and Horton, 2004). Tidal energy has been focused toward the eastern margins of the delta, apparently responding to changed hydraulic gradients or to the absence PD-1/PD-L1 inhibitor clinical trial of sediments from the now inactive eastern distributaries. Evidently the sediment supply to Lake Sindri in the past 200 years has been insufficient to fill the tectonically induced basin since it remains a 20 km × 30 km basin, 1–2 m deep (Fig. 10). In contrast, the tidal flats in the western part of the Indus Delta appear

to be more stable, possibly protected from tidal and wave reworking of the shoreline by the absence of tectonic subsidence or possibly due to the presence of slow uplift. The effects of the transition to the Anthropocene delta due to its much-increased these abstraction of water upstream are pronounced and well documented: seawater intrusion, soil salinization, deforestation of mangroves, reduced supply of surface- and ground-derived drinking water, low irrigation flows, and greatly depleted fisheries. Shrimp production has decreased by 90% (Inam et al., 2007). The delta’s mangrove forest, which covered ∼2500 km2, has been reduced by 60% (Kamal, 2004). The degraded mangrove ecosystem is virtually mono-specific, comparatively stunted, with losses of about 2% per year (Asianics Agro-Dev 2000). The increase in salinity during periods of low flow, and from the effects of upstream irrigation, has reduced the suitability of the delta for the cultivation of red rice, and for raising livestock.

The Chilia III lobe begun developing at the open coast sometimes

The Chilia III lobe begun developing at the open coast sometimes around 1700 AD (Mikhailova and Levashova, 2001). Although still primitive, the earliest realistically detailed map of the Danube delta region dating from 1771 (Fig. 2a; Panin and Overmars, 2012) provides important information about the earliest growth phase of the lobe. Its wave-dominated

deflected morphology (sensu Bhattacharya and Giosan, 2003) is evident. Two thalwegs at the mouth separated by a submerged middle-ground bar are oriented southward in the direction of the dominant longshore drift. Updrift of the mouth, the offshore-recurving shape of the contemporary Jebrieni beach see more plain ridges clearly indicates that the submarine deltaic deposition was already significant. Only a few islets were emergent on the

updrift side of the submarine channel, but a shallow submerged depositional platform appears to have developed on its downdrift side ( Fig. 2a). Subsequently, as recorded in numerous maps and charts since 1830 ( Fig. 4a), the Chilia III lobe evolved as a typical river-dominated delta in a frictional regime, which has led to repeated bifurcations selleck chemicals via formation of middle-ground bars ( Giosan et al., 2005). The influence of the longshore drift, expressed as a southward deflection of main distributary of Old Stambul, remained noticeable until the end of the 19th century as documented by a survey in 1871 (Fig. 4a). The isometric shape of the lobe acquired after that time resulted from the infilling of the shallow bay left between the deflected part delta plain and the mainland (Fig. 4a). Throughout the history of Chilia III growth, deltaic progradation was favored at northern Oceacov mouth, which advanced into the dominant direction of the waves, and the southern Old Stambul distributary mouth, which grew in the direction longshore drift. Slower progradation

is evident along the central coast (Fig. 4a) fed by eastward directed distributaries that had to contend with the strong longshore drift removing sediments Idelalisib clinical trial southward (Giosan et al., 2005). The decrease in new fluvial sediment delivered per unit shoreline as the lobe grew larger and advanced into deeper water resulted in progressively slower growth of the entire lobe in the 20th century (Fig. 4a). By 1940, clear signs of erosion were apparent, and a general erosional trend continues until today leading to a wave-dominated morphology characterized by barrier islands and spit development (Fig. 4b and c). Our reconstruction of the Chilia lobe evolution supports the idea that the rapid Danube delta growth in the late Holocene (Giosan et al., 2012) led to its radical reorganization via flow redistribution across the delta. Initially the southernmost St. George branch was reactivated around 2000 years BP and constructed the bulk of its wave-dominated open coast lobe (Fig. 1) in the last 1000–1500 years (Giosan et al., 2006 and Giosan et al.

One problem with meta-analyses, which may not be confined to the

One problem with meta-analyses, which may not be confined to the field of neuroimaging (Ioannidis, 2005), is the potential overrepresentation of positive findings in the published literature. A recent evaluation of meta-analyses of regional brain volume changes

in psychiatric disorders reported evidence for a considerable overreporting of significant group differences (except for the cerebral ventricles) (Ioannidis, 2011). Potential reasons include publication bias, selective reporting of brain regions showing group differences, and other arbitrary decisions that can be summarily termed “researcher degrees of freedom” (Simmons et al., 2011). However, the evaluation by Ioannidis (2011) did not include whole-brain volumetric studies that implement whole-brain correction for multiple comparisons, which this website should be less vulnerable to the selective reporting bias. Suggested improvements included the increase of power through multicenter studies, preregistration of clinical imaging studies, and definition of standardized analysis protocols (Ioannidis, 2011). Clinical

phenotypes in mental disorders may just be the endpoints of multiple converging pathophysiological pathways that are triggered by different combinations of genetic predisposition and environmental stress (Figure 2). As such, one way of improving the consistency of imaging findings in psychiatry may SRT1720 mw be to probe the biological pathways implicated these in specific mental disorders.

Current genetic models posit that multiple common variants with small effects or rare variants with larger effects confer the genetic vulnerability to psychotic disorders (Owen et al., 2010). Studies on patient samples that are not further differentiated by genotype may therefore obscure specific biological effects, whereas it may be possible to elucidate pathways to the disorder (Meyer-Lindenberg, 2010) through the effects of the risk variants on parameters of structural or functional neuroimaging, radioligand binding, or noninvasive neurophysiology. A particularly attractive aspect of this approach is that, in principle, it allows targeting any protein for which a functionally relevant genetic variant exists and would thus greatly expand the list of molecular mechanisms that can be investigated with neuroimaging (Table 2). It may also help overcome the lack of cellular resolution of current non-invasive neuroimaging techniques. Although high-resolution MRI at 7 Tesla can resolve the laminar structure of human cortex (Sánchez-Panchuelo et al., 2011), each layer contains a multitude of functionally and structurally diverse neurons that cannot be differentiated.

47 This is important, as multiple studies have observed a relatio

47 This is important, as multiple studies have observed a relationship between low muscle mass and impaired physical function in older adults.13 and 48 The aging process has also been associated with increases in muscle lipid content,46, 49 and 50 an independent risk factor for mobility limitations.46 Notably, older women have significantly lower mid-thigh muscle attenuation (greater muscle lipid infiltration) than older men.22 Moreover, there may be sex differences in the relative

importance of body composition determinants of physical function. For instance, an analysis from the Health, Aging, and Body Composition (Health ABC) study found that the strongest independent predictor of physical function was total body fat in older women, whereas the most important body composition determinant Olaparib manufacturer in men was Decitabine mw thigh muscle CSA.51 Findings from other studies support the notion that excess adiposity has a stronger impact on physical function in older women relative to men.20, 52 and 53 Despite these results, it was recently reported that body mass index did not differentially impact the relationship between muscle quality and physical function in older

women,54 suggesting that muscle capacity is critical for function regardless of body size. In summary, older women tend to gain adiposity and lose muscle mass as they age, and these changes in body composition (especially adiposity) can have a profound, negative impact on physical

function. Compared to younger individuals, older adults have lower muscle carotenoids strength23, 55 and 56 with older women having lower strength than age-matched males.23 Specifically, data from the Health ABC study show that isokinetic quadriceps torque is 38.1% lower in older women compared to older men (81.85 Nm vs. 132.15 Nm, respectively). 56 Even when muscle strength is normalized for muscle mass or fat free mass (e.g., muscle quality), there is a significant difference between older men and women. 56 and 57 Furthermore, in comparison to younger women, older women have lower concentric quadriceps strength 58 and 59 by as much as 56%–78%, 59 as well as lower isometric quadriceps strength (35%). 47 Moreover, longitudinal studies indicate an age-associated loss of muscle strength, termed dynapenia.60 and 61 A longitudinal study including generally healthy older adults, reported a loss of quadriceps muscle strength of 3.6% and 2.8% annually in men and women, respectively.62 Interestingly, the loss of muscle strength over a 5-year period in endurance trained older adults was even greater: 3%–4% decline in knee flexion strength and 4%–5% decline in knee extension strength (no significant differences between men and women).61 Thus, although older women have lower absolute muscle strength than men, the annual rate of decline may be lower, though additional studies are warranted. In older women, muscle strength is related to physical function.