Thermodynamics of protein‐cation interaction: Ca+2 and Mg+2 binding to the fifth binding module of the LDL receptor

The ligand binding domain of the LDL receptor (LDLR) contains seven structurally homologous repeats. The fifth repeat (LR5) is considered to be the main module responsible for the binding of lipoproteins LDL and β‐VLDL. LR5, like the other homologous repeats, is around 40‐residue long and contains three disulfide bonds and a conserved cluster of negatively charged residues surrounding a hexacoordinated calcium ion. The calcium coordinating cage is formed by the backbone oxygens of W193 and D198, and side‐chain atoms of D196, D200, D206, and E207. The functionality of LDLR is closely associated with the presence of calcium. Magnesium ions are to some extent similar to calcium ions. However, they appear to be involved in different physiological events and their concentrations in extracellular and intracellular compartments are regulated by different mechanisms. Whether magnesium ions can play a role in the complex cycle of LDLR internalization and recycling is not known. We report here a detailed study of the interaction between LR5 and these two cations combining ITC, emission fluorescence, high resolution NMR, and MD simulations, at extracellular and endosomal pHs. Our results indicate that the conformational stability and internal dynamics of LR5 are strongly modulated by the specific bound cation. It appears that the difference in binding affinity for these cations is somewhat compensated by their different concentrations in late LDL‐associated endosomes. While the mildly acidic and calcium‐depleted environment in late endosomes has been proposed to contribute significantly to LDL release, the presence of magnesium might assist in efficient LDLR recycling. Proteins 2010. © 2009 Wiley‐Liss, Inc.     

The formation of titan cells in Cryptococcus neoformans depends on the mouse strain and correlates with induction of Th2‐type responses

Cryptococcus neoformans is a pathogenic yeast that can form titan cells in the lungs, which are fungal cells of abnormal enlarged size. Little is known about the factors that trigger titan cells. In particular, it is not known how the host environment influences this transition. In this work, we describe the formation of titan cells in two mouse strains, CD1 and C57BL/6J. We found that the proportion of C. neoformans titan cells was significantly higher in C57BL/6J mice than in CD1. This higher proportion of titan cells was associated with a higher dissemination of the yeasts to the brain. Histology sections demonstrated eosinophilia in infected animals, although it was significantly lower in the CD1 mice which presented infiltration of lymphocytes. Both mouse strains presented infiltration of granulocytes, but the amount of eosinophils was higher in C57BL/6J. CD1 mice showed a significant accumulation of IFN‐γ, TNF‐α and IL17, while C57BL/BL mice had an increase in the anti‐inflammatory cytokine IL‐4. IgM antibodies to the polysaccharide capsule and total IgE were more abundant in the sera from C57BL/6J, confirming that these animals present a Th2‐type response. We conclude that titan cell formation in C. neoformans depends, not only on microbe factors, but also on the host environment.     

Global change‐driven effects on dissolved organic matter composition: Implications for food webs of northern lakes

Northern ecosystems are experiencing some of the most dramatic impacts of global change on Earth. Rising temperatures, hydrological intensification, changes in atmospheric acid deposition and associated acidification recovery, and changes in vegetative cover are resulting in fundamental changes in terrestrial–aquatic biogeochemical linkages. The effects of global change are readily observed in alterations in the supply of dissolved organic matter (DOM)—the messenger between terrestrial and lake ecosystems—with potentially profound effects on the structure and function of lakes. Northern terrestrial ecosystems contain substantial stores of organic matter and filter or funnel DOM, affecting the timing and magnitude of DOM delivery to surface waters. This terrestrial DOM is processed in streams, rivers, and lakes, ultimately shifting its composition, stoichiometry, and bioavailability. Here, we explore the potential consequences of these global change‐driven effects for lake food webs at northern latitudes. Notably, we provide evidence that increased allochthonous DOM supply to lakes is overwhelming increased autochthonous DOM supply that potentially results from earlier ice‐out and a longer growing season. Furthermore, we assess the potential implications of this shift for the nutritional quality of autotrophs in terms of their stoichiometry, fatty acid composition, toxin production, and methylmercury concentration, and therefore, contaminant transfer through the food web. We conclude that global change in northern regions leads not only to reduced primary productivity but also to nutritionally poorer lake food webs, with discernible consequences for the trophic web to fish and humans.     

Protected areas buffer the Brazilian semi‐arid biome from climate change

The Caatinga is a botanically unique semi‐arid ecosystem in northeast Brazil whose vegetation is adapted to the periodic droughts that characterize this region. However, recent extreme droughts events caused by anthropogenic climate change have challenged its ecological resilience. Here, we evaluate how deforestation and protection status affect the response of the Caatinga vegetation to drought. Specifically, we compared vegetation responses to drought in natural and deforested areas as well as inside and outside protected areas, using a time‐series of satellite‐derived Normalized Difference Vegetation Index (NDVI) and climatic data for 2008–2013. We observed a strong effect of deforestation and land protection on overall vegetation productivity and in productivity dynamics in response to precipitation. Overall, deforested areas had significantly lower NDVI and delayed greening in response to precipitation. By contrast, strictly protected areas had higher productivity and considerable resilience to low levels of precipitation, when compared to sustainable use or unprotected areas. These results highlight the importance of protected areas in protecting ecosystem processes and native vegetation in the Caatinga against the negative effects of climate change and deforestation. Given the extremely small area of the Caatinga currently under strict protection, the creation of new conservation areas must be a priority to ensure the sustainability of ecological processes and to avoid further desertification.     

Mrc1 is required for normal progression of replication forks throughout chromatin in S. cerevisiae

Mrc1 associates with replication forks, where it transmits replication stress signals and is required for normal replisome pausing in response to nucleotide depletion. Mrc1 also plays a poorly understood role in DNA replication, which appears distinct from its role in checkpoint signaling. Here, we demonstrate that Mrc1 functions constitutively to promote normal replication fork progression. In mrc1Delta cells, replication forks proceed slowly throughout chromatin, rather than being specifically defective in pausing and progression through loci that impede fork progression. Analysis of genetic interactions with Rrm3, a DNA helicase required to resolve paused forks, indicates that Mrc1 checkpoint signaling is dispensable for the resolution of stalled replication forks and suggests that replication forks lacking Mrc1 create DNA damage that must be repaired by Rrm3. These findings elucidate a central role for Mrc1 in normal replisome function, which is distinct from its role as a checkpoint mediator, but nevertheless critical to genome stability.     

P2X4 Activation Modulates Volume-sensitive Outwardly Rectifying Chloride Channels in Rat Hepatoma Cells

Volume-sensitive outwardly rectifying (VSOR) Cl⁻ channels are critical for the regulatory volume decrease (RVD) response triggered upon cell swelling. Recent evidence indicates that H₂O₂ plays an essential role in the activation of these channels and that H₂O₂ per se activates the channels under isotonic isovolumic conditions. However, a significant difference in the time course for current onset between H₂O₂-induced and hypotonicity-mediated VSOR Cl⁻ activation is observed. In several cell types, cell swelling induced by hypotonic challenges triggers the release of ATP to the extracellular medium, which in turn, activates purinergic receptors and modulates cell volume regulation. In this study, we have addressed the effect of purinergic receptor activation on H₂O₂-induced and hypotonicity-mediated VSOR Cl⁻ current activation. Here we show that rat hepatoma cells (HTC) exposed to a 33% hypotonic solution responded by rapidly activating VSOR Cl⁻ current and releasing ATP to the extracellular medium. In contrast, cells exposed to 200 μm H₂O₂ VSOR Cl⁻ current onset was significantly slower, and ATP release was not detected. In cells exposed to either 11% hypotonicity or 200 μm H₂O₂, exogenous addition of ATP in the presence of extracellular Ca²⁺ resulted in a decrease in the half-time for VSOR Cl⁻ current onset. Conversely, in cells that overexpress a dominant-negative mutant of the ionotropic receptor P2X4 challenged with a 33% hypotonic solution, the half-time for VSOR Cl⁻ current onset was significantly slowed down. Our results indicate that, at high hypotonic imbalances, swelling-induced ATP release activates the purinergic receptor P2X4, which in turn modulates the time course of VSOR Cl⁻ current onset in a extracellular Ca²⁺-dependent manner.