Transdifferentiation of autologous bone marrow cells on a collagen-poly(ε-caprolactone) scaffold for tissue engineering in complete lack of native urothelium.

Urological reconstructive surgery is sometimes hampered by a lack of tissue. In some cases, autologous urothelial cells (UCs) are not available for cell expansion and ordinary tissue engineering. In these cases, we wanted to explore whether autologous mesenchymal stem cells (MSCs) from bone marrow could be used to create urological transplants. MSCs from human bone marrow were cultured in vitro with medium conditioned by normal human UCs or by indirect co-culturing in culture well inserts. Changes in gene expression, protein expression and cell morphology were studied after two weeks using western blot, RT-PCR and immune staining. Cells cultured in standard epithelial growth medium served as controls. Bone marrow MSCs changed their phenotype with respect to growth characteristics and cell morphology, as well as gene and protein expression, to a UC lineage in both culture methods, but not in controls. Urothelial differentiation was also accomplished in human bone marrow MSCs seeded on a three-dimensional poly(ε-caprolactone) (PCL)-collagen construct. Human MSCs could easily be harvested by bone marrow aspiration and expanded and differentiated into urothelium. Differentiation could take place on a three-dimensional hybrid PCL-reinforced collagen-based scaffold for creation of a tissue-engineered autologous transplant for urological reconstructive surgery.

Roots and associated fungi drive long-term carbon sequestration in boreal forest.

Boreal forest soils function as a terrestrial net sink in the global carbon cycle. The prevailing dogma has focused on aboveground plant litter as a principal source of soil organic matter. Using (14)C bomb-carbon modeling, we show that 50 to 70% of stored carbon in a chronosequence of boreal forested islands derives from roots and root-associated microorganisms. Fungal biomarkers indicate impaired degradation and preservation of fungal residues in late successional forests. Furthermore, 454 pyrosequencing of molecular barcodes, in conjunction with stable isotope analyses, highlights root-associated fungi as important regulators of ecosystem carbon dynamics. Our results suggest an alternative mechanism for the accumulation of organic matter in boreal forests during succession in the long-term absence of disturbance.

Coping and thought suppression as predictors of suicidal ideation in depressed older adults with personality disorders.

Suicide rates are higher among older adults than any other age group and suicidal ideation is one of the best predictors of completed suicide in older adults. Despite this, few studies have evaluated predictors of suicidal ideation and other correlates of death by suicide (e.g. hopelessness) among older adults. Even fewer studies on this topic have been conducted among samples characterized as poor responders to treatments (e.g. depressed individuals with co-occurring personality disorder). The purpose of this study was to examine coping styles and thought suppression as predictors of a suicide risk composite score in a sample of depressed older adults with co-occurring personality disorders. Based on the extant literature, it was hypothesized that maladaptive coping (i.e. emotional and avoidance coping) and chronic thought suppression would significantly predict suicide risk. The results of this study indicated that elevated emotional coping and thought suppression were associated with increased suicide risk. Contrary to hypotheses, lower avoidance coping was associated with increased risk, although this finding is moderated by Axis II diagnosis Thus, treatments that focus on decreasing emotional coping and chronic thought suppression may result in decreased suicidal ideation and hopelessness for older adults with depression and Axis II pathology.

Can isotopic fractionation during respiration explain the 13C-enriched sporocarps of ectomycorrhizal and saprotrophic fungi?

The mechanism behind the (13)C enrichment of fungi relative to plant materials is unclear and constrains the use of stable isotopes in studies of the carbon cycle in soils. Here, we examined whether isotopic fractionation during respiration contributes to this pattern by comparing delta(13)C signatures of respired CO(2), sporocarps and their associated plant materials, from 16 species of ectomycorrhizal or saprotrophic fungi collected in a Norway spruce forest. The isotopic composition of respired CO(2) and sporocarps was positively correlated. The differences in delta(13)C between CO(2) and sporocarps were generally small, < +/-1 per thousand in nine out of 16 species, and the average shift for all investigated species was 0.04 per thousand. However, when fungal groups were analysed separately, three out of six species of ectomycorrhizal basidiomycetes respired (13)C-enriched CO(2) (up to 1.6 per thousand), whereas three out of five species of polypores respired (13)C-depleted CO(2) (up to 1.7 per thousand; P < 0.05). The CO(2) and sporocarps were always (13)C-enriched compared with wood, litter or roots. Loss of (13)C-depleted CO(2) may have enriched some species in (13)C. However, that the CO(2) was consistently (13)C-enriched compared with plant materials implies that other processes must be found to explain the consistent (13)C-enrichment of fungal biomass compared with plant materials.

Large-scale forest girdling shows that current photosynthesis drives soil respiration.

The respiratory activities of plant roots, of their mycorrhizal fungi and of the free-living microbial heterotrophs (decomposers) in soils are significant components of the global carbon balance, but their relative contributions remain uncertain. To separate mycorrhizal root respiration from heterotrophic respiration in aboreal pine forest, we conducted a large-scale tree-girdling experiment, comprising 9 plots each containing about 120 trees. Tree-girdling involves stripping the stem bark to the depth of the current xylem at breast height terminating the supply of current photosynthates to roots and their mycorrhizal fungi without physically disturbing the delicate root-microbe-soil system. Here we report that girdling reduced soil respiration within 1-2 months by about 54% relative to respiration on ungirdled control plots, and that decreases of up to 37% were detected within 5 days. These values clearly show that the flux of current assimilates to roots is a key driver of soil respiration; they are conservative estimates of root respiration, however, because girdling increased the use of starch reserves in the roots. Our results indicate that models of soil respiration should incorporate measures of photosynthesis and of seasonal patterns of photosynthate allocation to roots.

Natural abundance of 13C in CO2 respired from forest soils reveals speed of link between tree photosynthesis and root respiration.

Soil respiration from a boreal mixed coniferous forest showed large seasonal variation in natural abundance of 13C, ranging from -21.6‰ to -26.5‰. We tested if weather conditions could explain this variation in δ13C of respired CO2, and found that the air relative humidity 1-4 days before the days of CO2 sampling best explained the variation. This suggested that high δ13C values were caused by effects of air humidity on isotope fractionation during photosynthesis and that it took 1-4 days for the C from canopy photosynthesis of 20-25 m trees to become available for root/rhizosphere respiration. We calculated that these new photoassimilates could account for at least 65% of total soil respiration.