scholarly journals Osmolyte transport inStaphylococcus aureusand the role in pathogenesis

2016 ◽  
Vol 6 (2) ◽  
pp. 22 ◽  
Author(s):  
William R Schwan ◽  
Keith J Wetzel
Keyword(s):  
Hepatology ◽  
1999 ◽  
Vol 29 (1) ◽  
pp. 173-180 ◽  
Author(s):  
Thorsten Peters-Regehr ◽  
Johannes G. Bode ◽  
Ralf Kubitz ◽  
Dieter Häussinger

2018 ◽  
Vol 26 (3) ◽  
pp. 175-185 ◽  
Author(s):  
Fabian M. Commichau ◽  
Johannes Gibhardt ◽  
Sven Halbedel ◽  
Jan Gundlach ◽  
Jörg Stülke

2004 ◽  
Vol 96 (5) ◽  
pp. 1886-1893 ◽  
Author(s):  
Cristina E. Davis ◽  
Joshua J. Rychak ◽  
Bouvard Hosticka ◽  
Scott C. Davis ◽  
J. Edward John ◽  
...  

Many cell types regulate their volume in response to extracellular tonicity changes through a complex series of adaptive mechanisms. Several methods that are presently used to measure cell volume changes include Coulter counters, fluorescent techniques, electronic impedance, and video microscopy. Although these methods are widely used and accepted, there are limitations associated with each technique. This paper describes a new method to measure changes in cell volume based on the principle that fluid flow within a rigid system is well determined. For this study, cos-7 cells were plated to line the inner lumen of a glass capillary and stimulated to swell or shrink by altering the osmolarity of the perfusing solution. The cell capillary was connected in series with a blank reference capillary, and differential pressure changes across each tube were monitored. The advantages of this method include 1) ability to continuously monitor changes in volume during rapid solution changes, 2) independence from cell morphology, 3) presence of physiological conditions with cell surface contacts and cell-cell interactions, 4) no phototoxic effects such as those associated with fluorescent methods, and 5) ability to report from large populations of cells. With this method, we could detect the previously demonstrated enhanced volume regulation of cells overexpressing the membrane phosphoprotein phospholemman, which has been implicated in osmolyte transport.


1993 ◽  
Vol 265 (6) ◽  
pp. C1449-C1455 ◽  
Author(s):  
J. S. Handler ◽  
H. M. Kwon

Madin-Darby canine kidney cells accumulate several nonperturbing organic osmolytes when cultured in a hypertonic medium. Myo-inositol, betaine, and taurine are accumulated secondary to an increase in uptake, the first coupled to sodium entry, the latter two coupled to sodium and chloride entry. The transport rates increase as the result of an increase in maximum velocity for each cotransporter, with peak activity 24 h after the increase in tonicity. The cDNA for each cotransporter has been cloned. Their sequences indicate that the myo-inositol cotransporter belongs to the gene family that includes the sodium-coupled glucose transporter (SGLT1); the betaine and taurine cotransporters belong to the gene family of sodium- and chloride-coupled transporters that are responsible for neuronal uptake of many neurotransmitters. Assays of mRNA abundance and nuclear run-on assays reveal that shifts in tonicity have a major effect on transcription of the genes for the sodium-myo-inositol (SMIT) and sodium-chloride-betaine (BGT1) cotransporters. The ensuing increase in mRNA abundance for the two cotransporters and presumed increase in synthesis of the cotransporter proteins can explain the increase in transport activity in response to changes in tonicity.


1989 ◽  
Vol 145 (1) ◽  
pp. 147-156
Author(s):  
JOHN C. FERGUSON

Time course studies employing the fluorescent, high molecular weight tracer, fluorescein isothiocyanate dextran, confirm that there is a steady entry of sea water through the madreporite of the starfish, Echinaster graminicola, even under constant environmental conditions. This entry serves to supply replacement fluid to both the water vascular system and the perivisceral coelom, with more going to the latter than the former (10.67 vs 6.35μl h−1 for a 7.25 g animal). Since nearly 2.4 days may be required for an animal to take up 1 ml of sea water through the madreporite, the rate of entry is too low to be easily seen in direct observation, or to have immediate physiological consequences if prevented. Nevertheless, the rate is probably sufficient to make a substantial contribution to fluid volume regulation, functioning along with osmolyte transport and other processes that have been emphasized in recent literature.


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