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Structure of gramicidin D-RbCl complex at atomic resolution from low-temperature synchrotron data: interactions of double-stranded gramicidin channel contents and cations with channel wall

Gramicidin D (gD) is a naturally occurring ionophoric antibiotic that forms membrane channels specific for monovalent cations. The crystal structure of the RbCl complex of gD has been determined at 1.14 Å resolution from low‐temperature (100 K) synchrotron‐radiation data with a final R of 16%. The s...

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Bibliographic Details
Published in:Acta crystallographica. Section D, Biological crystallography. Biological crystallography., 2005-04, Vol.61 (4), p.433-441
Main Authors: Główka, M. L., Olczak, A., Bojarska, J., Szczesio, M., Duax, W. L., Burkhart, B. M., Pangborn, W. A., Langs, D. A., Wawrzak, Z.
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Language:English
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Summary:Gramicidin D (gD) is a naturally occurring ionophoric antibiotic that forms membrane channels specific for monovalent cations. The crystal structure of the RbCl complex of gD has been determined at 1.14 Å resolution from low‐temperature (100 K) synchrotron‐radiation data with a final R of 16%. The structure was refined with anisotropic temperature factors for all non‐H atoms and with partial occupancies for many of them. The asymmetric unit in the crystal contains four crystallographically independent molecules that form two right‐handed antiparallel double‐stranded dimers. There are seven distinct rubidium‐binding sites in each dimeric channel. The occupancy factors of Rb cations are between 0.11 and 0.35 and the total ion contents of the two crystallographically independent channels are 1.59 and 1.22 ions, respectively. Although each channel is `chemically symmetrical', the side‐chain conformations, the distributions of rubidium cations and their binding sites in the two independent channels are not. Cations are `coordinated' by delocalized π‐electrons of three to five carbonyl groups that together with peptide backbone chains form the gramicidin channel walls. The water:cation ratio in the channel interior is four or five:one, and five or six waters separate Rb cations during their passage through the channel.
ISSN:1399-0047
0907-4449
1399-0047
DOI:10.1107/S0907444905000399