Effect of calcitonin on glycosaminoglycan synthesis by embryo calf bone cells in vitro

Zusammenfassung Es wurde gefunden, dass rohe Calcitoninpräparate die Inkorporation von¹⁴C-Glucose in die Glycosaminoglycan-(GAG)-Synthese fördern. Unter denselben Zellkulturbedingungen wurde Calcitonin mit stark spezifischer Aktivität rasch inaktiviert und zeigte keine stimulierende Wirkung; wurde aber der Serumgehalt im Milieu stark eingeschränkt, so verursachte das Calcitonin (50 Einheiten/mg) eine hundertprozentige Erhöhung der¹⁴C-GAG-Synthese.     

A physiological correlate of disuse-induced sprouting at the neuromuscular junction.

Recent investigations have established that many of the normal properties of muscle fibres are maintained, at least in part, by muscle activity. Thus, a fall in resting membrane potential, an increase in input resistance, and spread of acetylcholine receptors to extrajunctional sites can all be induced by abolishing muscle activity and prevented by direct stimulation of denervated muscle fibres. Muscle activity also exerts a trophic influence on the innervating motoneurones; furthermore it may be a factor in the regulation of sprouting. Brown and Ironton found fine, "ultra-terminal sprouts" emanating from the endplates of muscles rendered inactive by chronic conduction block of the muscle nerve. Pestronk and Drachman saw increased branching of the motor nerve terminal and a consequent increase in endplate size in similar conditions. If these sprouts at the endplates of inactive muscles were functional, one might expect more transmitter to be released in response to nerve stimulation. We report here that both quantum content and spontaneous miniature endplate potential (m.e.p.p) frequency are increased at the terminals of inactive (disused) muscles.     

Structure of the DNA deaminase domain of the HIV-1 restriction factor APOBEC3G

The human APOBEC3G (apolipoprotein B messenger-RNA-editing enzyme, catalytic polypeptide-like 3G) protein is a single-strand DNA deaminase that inhibits the replication of human immunodeficiency virus-1 (HIV-1), other retroviruses and retrotransposons. APOBEC3G anti-viral activity is circumvented by most retroelements, such as through degradation by HIV-1 Vif. APOBEC3G is a member of a family of polynucleotide cytosine deaminases, several of which also target distinct physiological substrates. For instance, APOBEC1 edits APOB mRNA and AID deaminates antibody gene DNA. Although structures of other family members exist, none of these proteins has elicited polynucleotide cytosine deaminase or anti-viral activity. Here we report a solution structure of the human APOBEC3G catalytic domain. Five alpha-helices, including two that form the zinc-coordinating active site, are arranged over a hydrophobic platform consisting of five beta-strands. NMR DNA titration experiments, computational modelling, phylogenetic conservation and Escherichia coli-based activity assays combine to suggest a DNA-binding model in which a brim of positively charged residues positions the target cytosine for catalysis. The structure of the APOBEC3G catalytic domain will help us to understand functions of other family members and interactions that occur with pathogenic proteins such as HIV-1 Vif.     

Increasing risk of Amazonian drought due to decreasing aerosol pollution

The Amazon rainforest plays a crucial role in the climate system, helping to drive atmospheric circulations in the tropics by absorbing energy and recycling about half of the rainfall that falls on it. This region (Amazonia) is also estimated to contain about one-tenth of the total carbon stored in land ecosystems, and to account for one-tenth of global, net primary productivity. The resilience of the forest to the combined pressures of deforestation and global warming is therefore of great concern, especially as some general circulation models (GCMs) predict a severe drying of Amazonia in the twenty-first century. Here we analyse these climate projections with reference to the 2005 drought in western Amazonia, which was associated with unusually warm North Atlantic sea surface temperatures (SSTs). We show that reduction of dry-season (July-October) rainfall in western Amazonia correlates well with an index of the north-south SST gradient across the equatorial Atlantic (the 'Atlantic N-S gradient'). Our climate model is unusual among current GCMs in that it is able to reproduce this relationship and also the observed twentieth-century multidecadal variability in the Atlantic N-S gradient, provided that the effects of aerosols are included in the model. Simulations for the twenty-first century using the same model show a strong tendency for the SST conditions associated with the 2005 drought to become much more common, owing to continuing reductions in reflective aerosol pollution in the Northern Hemisphere.