StemBell therapy stabilizes atherosclerotic plaques after myocardial infarction

Background aims. After a myocardial infarction (MI) atherosclerosis is accelerated leading to destabilization of the atherosclerotic plaque. mesenchymal stromal cells are a promising therapeutic option for atherosclerosis. Previously, we demonstrated a novel stem cell delivery technique, with adipose stem cells coupled to microbubbles (i.e., StemBells) as therapy after MI. In this study, we aim to investigate the effect of StemBell therapy on atherosclerotic plaques in an atherosclerotic mouse model after MI. Methods. MI was induced in atherosclerotic Apolipoprotein E–deficient mice that were fed a high-fat Western diet. Six days post-MI, the mice received either 5?×?10⁵/100 µL StemBells or vehicle intravenously. The effects of StemBell treatment on the size and stability of aortic root atherosclerotic plaques and the infarcted heart were determined 28 days post-MI via (immuno)histological analyses. Moreover, monocyte subtypes and lipids in the blood were studied. Results. StemBell treatment resulted in significantly increased cap thickness, decreased intra-plaque macrophage density and increased percentage of intra-plaque anti-inflammatory macrophages and chemokines, without affecting plaque size and serum cholesterol/triglycerides. Furthermore, StemBell treatment significantly increased the percentage of anti-inflammatory macrophages within the infarcted myocardium but did not affect cardiac function nor infarct size. Finally, also the average percentage of anti-inflammatory monocytes in the circulation was increased after StemBell therapy. Discussion. StemBell therapy increased cap thickness and decreased intra-plaque inflammation after MI, indicative of stabilized atherosclerotic plaque. It also induced a shift of circulating monocytes and intra-plaque and intra-cardiac macrophages towards anti-inflammatory phenotypes. Hence, StemBell therapy may be a therapeutic option to prevent atherosclerosis acceleration after MI.     

Stress Responses in Avian Embryos

The day 13–14 chicken embryo is a useful model for studieson prenatal stress responses. Free dopamine, norepinephrineand epinephrine in its plasma, amniotic and allantoic fluidrespond to a variety of stresses. The allantoic fluid also containsconjugated catecholamines and conjugated steroids. However,a blood/allantois barrier excludes free thyroid hormones andfree steroids, and insulin. On the other hand, the allantoicfluid contains at least 40 amino acids (including six excitatoryamino acids) and related compounds. Most, possibly all, componentsof the allantoic fluid are regulated at specific blood/allantoisand amnion/allantois barriers, and they respond to ethanol stressand metabolite loading differentially. The avian allantois isa depot for important metabolites and messenger substances whichseems to be controlled by as yet unidentified hormones     

Response of plant species richness and primary productivity in shrublands along a north–south gradient in Europe to seven years of experimental warming and drought: reductions in primary productivity in the heat and drought year of 2003

We used a nonintrusive field experiment carried out at six sites – Wales (UK), Denmark (DK), the Netherlands (NL), Hungary (HU), Sardinia (Italy – IT), and Catalonia (Spain – SP) – along a climatic and latitudinal gradient to examine the response of plant species richness and primary productivity to warming and drought in shrubland ecosystems. The warming treatment raised the plot daily temperature by ca. 1 °C, while the drought treatment led to a reduction in soil moisture at the peak of the growing season that ranged from 26% at the SP site to 82% in the NL site. During the 7 years the experiment lasted (1999–2005), we used the pin‐point method to measure the species composition of plant communities and plant biomass, litterfall, and shoot growth of the dominant plant species at each site. A significantly lower increase in the number of species pin‐pointed per transect was found in the drought plots at the SP site, where the plant community was still in a process of recovering from a forest fire in 1994. No changes in species richness were found at the other sites, which were at a more mature and stable state of succession and, thus less liable to recruitment of new species. The relationship between annual biomass accumulation and temperature of the growing season was positive at the coldest site and negative at the warmest site. The warming treatment tended to increase the aboveground net primary productivity (ANPP) at the northern sites. The relationship between annual biomass accumulation and soil moisture during the growing season was not significant at the wettest sites, but was positive at the driest sites. The drought treatment tended to reduce the ANPP in the NL, HU, IT, and SP sites. The responses to warming were very strongly related to the Gaussen aridity index (stronger responses the lower the aridity), whereas the responses to drought were not. Changes in the annual aboveground biomass accumulation, litterfall, and, thus, the ANPP, mirrored the interannual variation in climate conditions: the most outstanding change was a decrease in biomass accumulation and an increase in litterfall at most sites during the abnormally hot year of 2003. Species richness also tended to decrease in 2003 at all sites except the cold and wet UK site. Species‐specific responses to warming were found in shoot growth: at the SP site, Globularia alypum was not affected, while the other dominant species, Erica multiflora, grew 30% more; at the UK site, Calluna vulgaris tended to grow more in the warming plots, while Empetrum nigrum tended to grow less. Drought treatment decreased plant growth in several studied species, although there were some species such as Pinus halepensis at the SP site or C. vulgaris at the UK site that were not affected. The magnitude of responses to warming and drought thus depended greatly on the differences between sites, years, and species and these multiple plant responses may be expected to have consequences at ecosystem and community level. Decreases in biodiversity and the increase in E. multiflora growth at the SP site as a response to warming challenge the assumption that sensitivity to warming may be less well developed at more southerly latitudes; likewise, the fact that one of the studied shrublands presented negative ANPP as a response to the 2003 heat wave also challenges the hypothesis that future climate warming will lead to an enhancement of plant growth and carbon sequestration in temperate ecosystems. Extreme events may thus change the general trend of increased productivity in response to warming in the colder sites.     

Experimental Evolution and Its Role in Evolutionary Physiology

Four general approaches to the study of evolutionary physiology—phylogenetically-basedcomparisons, genetic analyses and manipulations, phenotypicplasticity and manipulation, and selection studies—areoutlined and discussed. We provide an example of the latter,the application of laboratory selection experiments to the studyof a general issue in environmental adaptation, differencesin adaptive patterns of generalists and specialists. A cloneof the bacterium Escherichia coli that had evolved in a constantenvironment of 37°C was replicated into 6 populations andallowed to reproduce for 2,000 generations in a variable thermalenvironment alternating between 32 and 42°C. As predictedby theory, fitness and efficiency of resource use increasedin this new environment, as did stress resistance. Contraryto predictions, however, fitness and efficiency in the constantancestral environment of 37°C did not decrease, nor didthermal niche breadth or phenotypic plasticity increase. Selectionexperiments can thus provide a valuable approach to testinghypotheses and assumptions about the evolution of functionalcharacters.     

Effects of testosterone on growth, plumage pigmentation, and mortality in Black-headed Gull chicks

In the Black-headed Gull Larus ridibundus, sibling chicks defend small territories against conspecifics with testosterone-dependent aggressive behaviour. The energetic requirements for the performance of this behaviour may trade off against the energetic requirements for growth. There are indications that testosterone suppresses growth in birds and, therefore, regulate this trade-off. In this study, the effect of testosterone on growth and plumage pigmentation of Black-headed Gull chicks was analysed. Young chicks in small groups were treated for ten days with testosterone or sham treated. Testosterone-treated birds showed decreased growth rate (daily increase in body mass, head-bill length and tarsus-length) and a marked decrease in juvenile pigmentation of the plumage (tail-bar, back, and secondary coverts). Field measurements revealed a negative correlation between nest density, which correlates positively with aggressive behaviour of adults, and plumage coloration. Furthermore, these measurements showed an increase in mortality of chicks that had low levels of pigmentation early in life. The data suggest that chicks face a testosterone-regulated trade-off between growth and territory defence.     

Contrasting effects of repeated summer drought on soil carbon efflux in hydric and mesic heathland soils

Current predictions of climate change include altered rainfall patterns throughout Europe, continental USA and areas such as the Amazon. The effect of this on soil carbon efflux remains unclear although several modelling studies have highlighted the potential importance of drought for carbon storage. To test the importance of drought, and more importantly repeated drought year-on-year, we used automated retractable curtains to exclude rain and produce repeated summer drought in three heathlands at varying moisture conditions. This included a hydric system limited by water-excess (in the UK) and two mesic systems with seasonal water limitation in Denmark (DK) and the Netherlands (NL). The experimental rainfall reductions were set to reflect single year droughts observed in the last decade with exclusion of rain for 2–3 months of the year resulting in a 20–26% reduction in annual rainfall and 23–38% reduction in mean soil moisture during the drought period. Unexpectedly, sustained reduction in soil moisture over winter (between drought periods) was also observed at all three sites, along with a reduction in the maximum water-holding capacity attained. Three hypotheses are discussed which may have contributed to this lack of recovery in soil moisture: hydrophobicity of soil organic matter, increased water use by plants and increased cracking of the soil. The responses of soil respiration to this change in soil moisture varied among the sites: decreased rates were observed at the water-limited NL and DK sites whilst they increased at the UK site. Reduced sensitivity of soil respiration to soil temperature was observed at soil moisture contents above 55% at the UK site and below 20% and 13% at the NL and DK sites, respectively. Soil respiration rates recovered to predrought levels in the NL and DK sites during the winter re-wetting period that indicates any change in soil C storage due to changes in soil C efflux may be short lived in these mesic systems. In contrast, in the hydric UK site after 2 years of drought treatment, the persistent reduction in soil moisture throughout the year resulted in a year-round increase in soil respiration flux, a response that accelerated over time to 40% above control levels. These findings suggest that carbon-rich soils with high organic matter content may act as a significant source of CO₂ to the atmosphere following repeated summer drought. Nonrecovery of soil moisture and a persistent increase in soil respiration may be the primary mechanism underlying the reported substantial losses of soil carbon from UK organic soils over the last 20 years. These findings indicate that the water status of an ecosystem will be a critical factor to consider in determining the impact of drought on the soil carbon fluxes and storage.     

Characterization of Genotypes of Enterocytozoon bieneusi in Immunosuppressed and Immunocompetent Patient Groups

ABSTRACT. A retrospective phylogenetic analysis was performed on isolates of Enterocytozoon bieneusi to characterize the genotypes in different patient cohorts. Fifty-seven isolates, collected from patients living in Malawi and the Netherlands, were classified by age and immune status of the hosts. Sequence analysis of the internal transcribed spacer (ITS) region identified 16 genotypes; nine have not previously been described. Genotypes K and D were most prevalent among patient groups, whereas genotype C was restricted to transplantation patients receiving immunosupressives and genotype B showed a predisposition toward patients living with HIV/AIDS. Different genotypes showed more dispersion among isolates from Malawi compared with those from the Netherlands. A constructed map estimating the genealogy of the ITS region reveals a dynamic evolutionary process between the genotypes.     

Forest–flood relation still tenuous – comment on 'Global evidence that deforestation amplifies flood risk and severity in the developing world' by C. J. A. Bradshaw, N.S. Sodi, K. S.-H. Peh and B.W. Brook

In a recent paper in this journal, Bradshaw and colleagues analyse country statistics on flood characteristics, land cover and land cover change, and conclude that deforestation amplifies flood risk and severity in the developing world. The study addresses an important and long-standing question, but we identify important flaws. Principal among these are difficulties in interpreting country statistics and the correlation between population and floods. We review current knowledge, which suggests that the removal of trees does not affect large flood events, although associated landscape changes can under some circumstances. Reanalysis of the data analysed by Bradshaw and colleagues shows that population density alone already explains up to 83% of the variation in reported flood occurrences, considerably more than forest cover or deforestation (<10%). Feasible explanations for this statistical finding – whether spurious or causative – are not difficult to conceive. We, therefore, consider the conclusion of Bradshaw and colleagues to be unsupported. However, their study is a valuable first step to show how these or similar flood data might be used to further explore the relationship between land cover and flooding.