21 research outputs found

    Global maps of soil temperature.

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    Research in global change ecology relies heavily on global climatic grids derived from estimates of air temperature in open areas at around 2 m above the ground. These climatic grids do not reflect conditions below vegetation canopies and near the ground surface, where critical ecosystem functions occur and most terrestrial species reside. Here, we provide global maps of soil temperature and bioclimatic variables at a 1-km <sup>2</sup> resolution for 0-5 and 5-15 cm soil depth. These maps were created by calculating the difference (i.e. offset) between in situ soil temperature measurements, based on time series from over 1200 1-km <sup>2</sup> pixels (summarized from 8519 unique temperature sensors) across all the world's major terrestrial biomes, and coarse-grained air temperature estimates from ERA5-Land (an atmospheric reanalysis by the European Centre for Medium-Range Weather Forecasts). We show that mean annual soil temperature differs markedly from the corresponding gridded air temperature, by up to 10°C (mean = 3.0 ± 2.1°C), with substantial variation across biomes and seasons. Over the year, soils in cold and/or dry biomes are substantially warmer (+3.6 ± 2.3°C) than gridded air temperature, whereas soils in warm and humid environments are on average slightly cooler (-0.7 ± 2.3°C). The observed substantial and biome-specific offsets emphasize that the projected impacts of climate and climate change on near-surface biodiversity and ecosystem functioning are inaccurately assessed when air rather than soil temperature is used, especially in cold environments. The global soil-related bioclimatic variables provided here are an important step forward for any application in ecology and related disciplines. Nevertheless, we highlight the need to fill remaining geographic gaps by collecting more in situ measurements of microclimate conditions to further enhance the spatiotemporal resolution of global soil temperature products for ecological applications

    DNA microarrays: Implications for cardiovascular medicine

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    10.1161/01.RES.0000036019.55901.62Circulation Research917559-56

    Proton Inhibition of Sodium Channels: Mechanism of Gating Shifts and Reduced Conductance

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    International audienceExtracellular acidosis affects both permeation and gating of the expressed rat skeletal muscle Na+ channel (micro1). Reduction of the extracellular pH produced a progressive decrease in the maximal whole-cell conductance and a depolarizing shift in the whole-cell current-voltage relationship. A smaller depolarizing shift in the steady-state inactivation curve was observed. The pK of the reduction of maximal conductance was 6.1 over the pH range studied. An upper limit estimate of the pK of the shift of the half-activation voltage was 6.1. The relative reduction in the maximal whole-cell conductance did not change with higher [Na+]o. The conductance of single fenvalerate-modified Na+ channels was reduced by extracellular protons. Although the single-channel conductance increased with higher [Na+]o, the maximal conductances at pH 7.6, 7.0 and 6.0 did not converge at [Na+]o up to 280 mm, inconsistent with a simple electrostatic effect. A model incorporating both Na+ and H+ binding in the pore and cation binding to a Gouy-Chapman surface charge provided a robust fit to the single-channel conductance data with an estimated surface charge density of 1e-/439A2. Neither surface charge nor proton block alone suffices to explain the effects of extracellular acidosis on Na+ channel permeation; both effects play major roles in mediating the response to extracellular pH

    Mutations affecting agonist sensitivity of the nicotinic acetylcholine receptor

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    The nicotinic acetylcholine receptor (AChR) is a pentameric transmembrane protein (alpha 2 beta gamma delta) that binds the neurotransmitter acetylcholine (ACh) and transduces this binding into the opening of a cation selective channel. The agonist, competitive antagonist, and snake toxin binding functions of the AChR are associated with the alpha subunit (Kao et al., 1984; Tzartos and Changeux, 1984; Wilson et al., 1985; Kao and Karlin, 1986; Pederson et al., 1986). We used site-directed mutagenesis and expression of AChR in Xenopus oocytes to identify amino acid residues critical for ligand binding and channel activation. Several mutations in the alpha subunit sequence were constructed based on information from sequence homology and from previous biochemical (Barkas et al., 1987; Dennis et al., 1988; Middleton and Cohen, 1990) and spectroscopic (Pearce and Hawrot, 1990; Pearce et al., 1990) studies. We have identified one mutation, Tyr190 to Phe (Y190F), that had a dramatic effect on ligand binding and channel activation. These mutant channels required more than 50-fold higher concentrations of ACh for channel activation than did wild type channels. This functional change is largely accounted for by a comparable shift in the agonist binding affinity, as assessed by the ability of ACh to compete with alpha-bungarotoxin binding. Other mutations at nearby conserved positions of the alpha subunit (H186F, P194S, Y198F) produce less dramatic changes in channel properties. Our results demonstrate that ligand binding and channel gating are separable properties of the receptor protein, and that Tyr190 appears to play a specific role in the receptor site for acetylcholine
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