The FgfrL1 receptor is required for development of slow muscle fibers

FgfrL1, which interacts with Fgf ligands and heparin, is a member of the fibroblast growth factor receptor (Fgfr) family. FgfrL1-deficient mice show two significant alterations when compared to wildtype mice: They die at birth due to a malformed diaphragm and they lack metanephric kidneys. Utilizing gene arrays, qPCR and in situ hybridization we show here that the diaphragm of FgfrL1 knockout animals lacks any slow muscle fibers at E18.5 as indicated by the absence of slow fiber markers Myh7, Myl2 and Myl3. Similar lesions are also found in other skeletal muscles that contain a high proportion of slow fibers at birth, such as the extraocular muscles. In contrast to the slow fibers, fast fibers do not appear to be affected as shown by expression of fast fiber markers Myh3, Myh8, Myl1 and MylPF. At early developmental stages (E10.5, E15.5), FgfrL1-deficient animals express slow fiber genes at normal levels. The loss of slow fibers cannot be attributed to the lack of kidneys, since Wnt4 knockout mice, which also lack metanephric kidneys, show normal expression of Myh7, Myl2 and Myl3. Thus, FgfrL1 is specifically required for embryonic development of slow muscle fibers.     

Design and optimization of new piperidines as renin inhibitors

The discovery of a new series of piperidine-based renin inhibitors is described herein. SAR optimization upon the P3 renin sub-pocket is described, leading to the discovery of 9 and 41, two bioavailable renin inhibitors orally active at low doses in a transgenic rat model of hypertension.     

Weathering-Associated Bacteria from the Damma Glacier Forefield: Physiological Capabilities and Impact on Granite Dissolution

Several bacterial strains isolated from granitic rock material in front of the Damma glacier (Central Swiss Alps) were shown (i) to grow in the presence of granite powder and a glucose-NH₄Cl minimal medium without additional macro- or micronutrients and (ii) to produce weathering-associated agents. In particular, four bacterial isolates (one isolate each of Arthrobacter sp., Janthinobacterium sp., Leifsonia sp., and Polaromonas sp.) were weathering associated. In comparison to what was observed in abiotic experiments, the presence of these strains caused a significant increase of granite dissolution (as measured by the release of Fe, Ca, K, Mg, and Mn). These most promising weathering-associated bacterial species exhibited four main features rendering them more efficient in mineral dissolution than the other investigated isolates: (i) a major part of their bacterial cells was attached to the granite surfaces and not suspended in solution, (ii) they secreted the largest amounts of oxalic acid, (iii) they lowered the pH of the solution, and (iv) they formed significant amounts of HCN. As far as we know, this is the first report showing that the combined action of oxalic acid and HCN appears to be associated with enhanced elemental release from granite, in particular of Fe. This suggests that extensive microbial colonization of the granite surfaces could play a crucial role in the initial soil formation in previously glaciated mountain areas.Glaciers in alpine regions are highly sensitive to changes in climatic conditions (29). Increasing global atmospheric temperatures over the last decades have resulted in the recession of alpine glaciers (18). Forefields of temperate alpine glaciers provide unique opportunities to study initial soil formation as well as microbial and plant succession along the chronosequences (12, 26, 34, 36). The forefields close to the glacier terminus are initially vegetation free and consist mainly of rock material with high fractions of silt-sized grains with low C and N content and small amounts of available nutrients (14). Mineral weathering is a key process in the formation of soils (1, 26), and the crucial importance of microbially promoted mineral weathering for nutrient acquisition is increasingly recognized (2, 4, 39, 46). Recently exposed rock surfaces can be considered primary ecosystems where only a few microbes that are adapted due to their mineral-weathering abilities can grow (17). Some cations of rock-forming minerals are essential for proper cell functions. However, our understanding of geochemically significant microbes in forefields of temperate alpine glacier is still very limited but is crucial for increasing our knowledge of nutrient mobilization and the buildup of organic matter that is essential for the development of macroorganisms.The area of the Damma glacier in Central Switzerland is characterized by a relatively homogenous granitic rock basement and is used as field site of the interdisciplinary research project “Biosphere-Geosphere interactions: Linking climate change, weathering, soil formation and ecosystem evolution (BigLink)” (5). In the frame of this research project, we studied the functional roles of granite-colonizing microbes as biotic weathering agents in previously glaciated areas. So far, relatively little is known about microbe-granite interactions, especially regarding the release of trace elements. Several studies have examined the dissolution of specific granite-forming minerals in the presence of actively metabolizing bacteria or compounds that simulate metabolic activity (24, 30, 31, 37, 38, 44). There is a general agreement that microbially produced organic acids, siderophores, and extracellular polysaccharides can all promote dissolution of minerals. Previous dissolution experiments have mainly been performed with (i) commercially obtained minerals (23, 45), (ii) model microorganisms that were commercially obtained from culture collections (3, 35, 45), or (iii) laboratory strains, such as those of Bacillus subtilis (23) and Burkholderia fungorum (47). Most studies have focused on individual mineral specimens rather than on the mixture of minerals that are present in granite rock (47). Few studies observed mineral weathering of collected rock and bacteria isolated from volcanic areas covered with vegetation (30, 31). Moreover, there are no studies on microbial weathering for such immediately deglaciated environments combining functional and taxonomic investigations, probably due to the difficulties in obtaining heterotrophic bacterial isolates from granitic glacier forefields. In spite of this, a comprehensive culture collection containing approximately 500 bacterial strains, which were isolated from the glacier tongue of the Damma glacier, was established. Full-length 16S rRNA gene sequences of 120 isolates revealed that many isolates obtained from oligotrophic media were closely related to readily cultivable heterotrophic bacteria (e.g., Arthrobacter sp., Collimonas sp., Paenibacillus sp., and Pseudomonas sp.). These bacteria have been found to enhance mineral dissolution (39).Our aim was to characterize the impact of microorganisms on granite weathering. We performed laboratory dissolution experiments with sterile crushed granite rock material, 12 bacterial strains, and 1 algal strain. To investigate the potential weathering abilities of these isolates, granite dissolution experiments were performed abiotically with model agents, such as HCl for proton-promoted weathering or oxalate and citrate and KCN for ligand-promoted weathering.     

Measurement of the isometric dorsiflexion and plantar flexion force in the ankle joint]

This article describes an easy to use test equipment for measuring the isometric force in the ankle joints in dorsiflexion and plantar flexion. The combination of the test equipment for measuring the voluntary maximal isometric muscle force in the ankle joint, the surface electromyograms and the motion analysis of the measured leg allow an objective comparison of the strength of the muscular force between the left and right leg. It might be also used as a control setup during rehabilitation after surgical treatment or injuries.     

Association of specific expansins with growth in maize leaves is maintained under environmental, genetic, and developmental sources of variation

We aimed to evaluate whether changes in maize (Zea mays) leaf expansion rate in response to environmental stimuli or developmental gradients are mediated by common or specific expansins, a class of proteins known to enhance cell wall extensibility. Among the 33 maize expansin or putative expansin genes analyzed, 19 were preferentially expressed at some point of the leaf elongation zone and these expansins could be organized into three clusters related to cell division, maximal leaf expansion, and cell wall differentiation. Further analysis of the spatial distribution of expression was carried out for three expansins in leaves displaying a large range of expansion rates due to water deficit, genotype, and leaf developmental stage. With most sources of variation, the three genes showed similar changes in expression and consistent association with changes in leaf expansion. Moreover, our analysis also suggested preferential association of each expansin with elongation, widening, or both of these processes. Finally, using in situ hybridization, expression of two of these genes was increased in load-bearing tissues such as the epidermis and differentiating xylem. Together, these results suggest that some expansins may be preferentially related to elongation and widening after integrating several spatial, environmental, genetic, and developmental cues.     

Neutrophil transmigration under shear flow conditions in vitro is junctional adhesion molecule-C independent

Endothelial cell junctional adhesion molecule (JAM)-C has been proposed to regulate neutrophil migration. In the current study, we used function-blocking mAbs against human JAM-C to determine its role in human leukocyte adhesion and transendothelial cell migration under flow conditions. JAM-C surface expression in HUVEC was uniformly low, and treatment with inflammatory cytokines TNF-alpha, IL-1beta, or LPS did not increase its surface expression as assessed by FACS analysis. By immunofluorescence microscopy, JAM-C staining showed sparse localization to cell-cell junctions on resting or cytokine-activated HUVEC. Surprisingly, staining of detergent-permeabilized HUVEC revealed a large intracellular pool of JAM-C that showed little colocalization with von Willebrand factor. Adhesion studies in an in vitro flow model showed that functional blocking JAM-C mAb alone had no inhibitory effect on polymorphonuclear leukocyte (PMN) adhesion or transmigration, whereas mAb to ICAM-1 significantly reduced transmigration. Interestingly, JAM-C-blocking mAbs synergized with a combination of PECAM-1, ICAM-1, and CD99-blocking mAbs to inhibit PMN transmigration. Overexpression of JAM-C by infection with a lentivirus JAM-C GFP fusion protein did not increase adhesion or extent of transmigration of PMN or evoke a role for JAM-C in transendothelial migration. These data suggest that JAM-C has a minimal role, if any, in PMN transmigration in this model and that ICAM-1 is the preferred endothelial-expressed ligand for PMN beta(2) integrins during transendothelial migration.     

Mimetics of the tri- and tetrasaccharide epitope of GQ1balpha as myelin-associated glycoprotein (MAG) ligands

The synthesis of phenoxyphenyl, phenoxybenzyl, biphenyl, and phenyltriazole substituted sialic acid derivatives as mimics of the tri- and tetrasaccharide epitopes of GQ1balpha is described. These synthetically easily available sialosides show comparable or even enhanced affinity to MAG compared with the natural tri- and tetrasaccharide epitopes and form a new class of potential MAG antagonists.