scholarly journals Biophysical characterization of naturally occurring titin M10 mutations

2015 ◽  
Vol 24 (6) ◽  
pp. 946-955 ◽  
Author(s):  
Michael W. Rudloff ◽  
Alec N. Woosley ◽  
Nathan T. Wright
2013 ◽  
Vol 1828 (2) ◽  
pp. 455-460 ◽  
Author(s):  
V. Cassina ◽  
A. Torsello ◽  
A. Tempestini ◽  
D. Salerno ◽  
D. Brogioli ◽  
...  

eLife ◽  
2018 ◽  
Vol 7 ◽  
Author(s):  
Helen Louise Lightfoot ◽  
Timo Hagen ◽  
Antoine Cléry ◽  
Frédéric Hai-Trieu Allain ◽  
Jonathan Hall

G-quadruplexes are naturally-occurring structures found in RNAs and DNAs. Regular RNA G-quadruplexes are highly stable due to stacked planar arrangements connected by short loops. However, reports of irregular quadruplex structures are increasing and recent genome-wide studies suggest that they influence gene expression. We have investigated a grouping of G2-motifs in the UTRs of eight genes involved in polyamine biosynthesis, and concluded that several likely form novel metastable RNA G-quadruplexes. We performed a comprehensive biophysical characterization of their properties, comparing them to a reference G-quadruplex. Using cellular assays, together with polyamine-depleting and quadruplex-stabilizing ligands, we discovered how some of these motifs regulate and sense polyamine levels, creating feedback loops during polyamine biosynthesis. Using high-resolution 1H-NMR spectroscopy, we demonstrated that a long-looped quadruplex in the AZIN1 mRNA co-exists in salt-dependent equilibria with a hairpin structure. This study expands the repertoire of regulatory G-quadruplexes and demonstrates how they act in unison to control metabolite homeostasis.


2015 ◽  
Vol 108 (2) ◽  
pp. 377a
Author(s):  
Nathan T. Wright ◽  
Michael W. Rudloff

Author(s):  
W. W. Barker ◽  
W. E. Rigsby ◽  
V. J. Hurst ◽  
W. J. Humphreys

Experimental clay mineral-organic molecule complexes long have been known and some of them have been extensively studied by X-ray diffraction methods. The organic molecules are adsorbed onto the surfaces of the clay minerals, or intercalated between the silicate layers. Natural organo-clays also are widely recognized but generally have not been well characterized. Widely used techniques for clay mineral identification involve treatment of the sample with H2 O2 or other oxidant to destroy any associated organics. This generally simplifies and intensifies the XRD pattern of the clay residue, but helps little with the characterization of the original organoclay. Adequate techniques for the direct observation of synthetic and naturally occurring organoclays are yet to be developed.


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