4.6 Article

The C Terminus of Bax Inhibitor-1 Forms a Ca2+-permeable Channel Pore

Journal

JOURNAL OF BIOLOGICAL CHEMISTRY
Volume 287, Issue 4, Pages 2544-2557

Publisher

AMER SOC BIOCHEMISTRY MOLECULAR BIOLOGY INC
DOI: 10.1074/jbc.M111.275354

Keywords

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Funding

  1. Deutsche Forschungsgemeinschaft [ME1922/9-1]
  2. Forschungskommission of the Heinrich Heine-University Dusseldorf
  3. Research Foundation-Flanders (F. W. O.) [G.0604.07N, G.0788.11N, G.0724.09]
  4. Research Council of the K.U. Leuven [GOA/09/012]
  5. OT START [SRT/10/044]
  6. Interuniversity Attraction Poles Program Belgian Science Policy [P6/28]

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Bax inhibitor-1 (BI-1) is a multitransmembrane domain-spanning endoplasmic reticulum (ER)-located protein that is evolutionarily conserved and protects against apoptosis and ER stress. Furthermore, BI-1 is proposed to modulate ER Ca2+ homeostasis by acting as a Ca2+-leak channel. Based on experimental determination of the BI-1 topology, we propose that its C terminus forms a Ca2+ pore responsible for its Ca2+-leak properties. We utilized a set of C-terminal peptides to screen for Ca2+ leak activity in unidirectional Ca-45(2+)-flux experiments and identified an alpha-helical 20-amino acid peptide causing Ca2+ leak from the ER. The Ca2+ leak was independent of endogenous ER Ca2+-release channels or other Ca2+-leak mechanisms, namely translocons and presenilins. The Ca2+-permeating property of the peptide was confirmed in lipid-bilayer experiments. Using mutant peptides, we identified critical residues responsible for the Ca2+-leak properties of this BI-1 peptide, including a series of critical negatively charged aspartate residues. Using peptides corresponding to the equivalent BI-1 domain from various organisms, we found that the Ca2+-leak properties were conserved among animal, but not plant and yeast orthologs. By mutating one of the critical aspartate residues in the proposed Ca2+-channel pore in full-length BI-1, we found that Asp-213 was essential for BI-1-dependent ER Ca2+ leak. Thus, we elucidated residues critically important for BI-1-mediated Ca2+ leak and its potential channel pore. Remarkably, one of these residues was not conserved among plant and yeast BI-1 orthologs, indicating that the ER Ca2+-leak properties of BI-1 are an added function during evolution.

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