JBC INTERFERin siRNA transfection reagent

HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Talor, Z.
Right arrow Articles by Arruda, J. A.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Talor, Z.
Right arrow Articles by Arruda, J. A.
Social Bookmarking
 Add to CiteULike   Add to Complore   Add to Connotea   Add to Del.icio.us   Add to Digg   Add to Reddit   Add to Technorati  
What's this?

J. Biol. Chem., Vol. 260, Issue 29, 15473-15476, 12, 1985

Partial purification and reconstitution of renal basolateral Na+-Ca2+ exchanger into liposomes

Z Talor and JA Arruda

The Na+-Ca2+ exchange system in renal tubular basolateral membranes was partially purified and incorporated into liposomes. Solubilization of basolateral membranes with 1% cholic acid in the presence of 2.5% soybean phospholipids and proteolytic treatment with Pronase (20 micrograms/ml) as described (Wakabayashi, S., and Goshima, K. (1982) Biochim. Biophys. Acta 693, 125-133) allowed partial purification and reconstitution of the Na+-Ca2+ exchange system into liposomes. The Na+- dependent Ca2+ uptake in the reconstituted liposomes was 25 times higher than the Na+-dependent Ca2+ uptake in the native basolateral membranes. Eadie-Hofstee analysis of the Na+-dependent Ca2+ uptake revealed a Vmax of 201 pmol of Ca2+/mg of protein/45 s and a Km for Ca2+ of 2.7 microM. The stoichiometry (n) of the Na+-Ca2+ exchange system was determined from the Na+ gradient which opposes constant membrane potential so that no net Ca2+ transport occurs. In the presence of constant negative membrane potential, the value for n was 3.09 +/- 0.22, and in the presence of constant positive membrane potential, the value for n was 2.89 +/- 0.2. Thus, the stoichiometry of the renal Na+-Ca2+ exchange system is approximately 3Na+:1Ca2+.
Add to CiteULike CiteULike   Add to Complore Complore   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg   Add to Reddit Reddit   Add to Technorati Technorati    What's this?





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 All ASBMB Journals   Molecular and Cellular Proteomics 
 Journal of Lipid Research   ASBMB Today 
Copyright © 1985 by the American Society for Biochemistry and Molecular Biology.