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  • 2015-2019  (2)
  • 1
    Publication Date: 2019
    Description: 〈p〉G protein–coupled receptors (GPCRs) that couple to G〈sub〉i/o〈/sub〉 proteins modulate neurotransmission presynaptically by inhibiting exocytosis. Release of Gβ subunits from activated G proteins decreases the activity of voltage-gated Ca〈sup〉2+〈/sup〉 channels (VGCCs), decreasing excitability. A less understood Gβ-mediated mechanism downstream of Ca〈sup〉2+〈/sup〉 entry is the binding of Gβ to SNARE complexes, which facilitate the fusion of vesicles with the cell plasma membrane in exocytosis. Here, we generated mice expressing a form of the SNARE protein SNAP25 with premature truncation of the C terminus and that were therefore partially deficient in this interaction. SNAP253 homozygote mice exhibited normal presynaptic inhibition by GABA〈sub〉B〈/sub〉 receptors, which inhibit VGCCs, but defective presynaptic inhibition by receptors that work directly on the SNARE complex, such as 5-hydroxytryptamine (serotonin) 5-HT〈sub〉1b〈/sub〉 receptors and adrenergic α〈sub〉2a〈/sub〉 receptors. Simultaneously stimulating receptors that act through both mechanisms showed synergistic inhibitory effects. SNAP253 homozygote mice had various behavioral phenotypes, including increased stress-induced hyperthermia, defective spatial learning, impaired gait, and supraspinal nociception. These data suggest that the inhibition of exocytosis by G〈sub〉i/o〈/sub〉-coupled GPCRs through the Gβ-SNARE interaction is a crucial component of numerous physiological and behavioral processes.〈/p〉
    Print ISSN: 1945-0877
    Electronic ISSN: 1937-9145
    Topics: Biology , Medicine
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  • 2
    Publication Date: 2019
    Description: Abstract Quantifying the eddy diffusion coefficient profile in the mesosphere and lower thermosphere (MLT) is critical to the constituent density distributions in the upper mesosphere and thermosphere. Previous work by ?Swenson_2018 Swenson et al. (2018) estimated the global mean eddy diffusion (kzz) values in the upper mesosphere using atomic oxygen (O), derived from Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) hydroxyl (OH). In this study, vertical eddy diffusive transport velocities of O were determined from continuity of mass in the mesopause region (80‐97 km), primarily via the HOx chemistry. Global average constituent climatology from previously deduced SABER ozone (O3) and atomic hydrogen (H) was applied. Furthermore, we extended the global mean eddy transport velocities to new heights (105 km) in the MLT using the newly‐available global mean Scanning Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY) data. The combined method of determining O3 loss and O density climatology from SCIAMACHY, as well as an improved global mean background atmosphere from SABER, provide new information for eddy diffusion determination in the MLT. Three prominent results to emerge from this study include: (i) Global mean kzz profiles between 80 and 105 km derived from MLT constituent climatologies, SABER and SCIAMACHY global mean O density profiles averaged for approximately one solar cycle, (ii) Determination of O eddy diffusion velocities in the MLT consistent between two satellite measurements and the TIME‐GCM (thermosphere ionosphere mesosphere electrodynamics‐general circulation model), and (iii) Resolution of historically large differences between deduced kzz determined from O versus CO2 by analysis of SABER and SCIAMACHY measurements.
    Print ISSN: 2169-897X
    Electronic ISSN: 2169-8996
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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