Structural and functional characterization of a calcium-activated cation channel from Tsukamurella paurometabola.

The selectivity filter is an essential functional element of K+ channels that is highly conserved both in terms of its primary sequence and its three-dimensional structure. Here, we investigate the properties of an ion channel from the Gram-positive bacterium Tsukamurella paurometabola with a selectivity filter formed by an uncommon proline-rich sequence. Electrophysiological recordings show that it is a non-selective cation channel and that its activity depends on Ca2+ concentration. In the crystal structure, the selectivity filter adopts a novel conformation with Ca2+ ions bound within the filter near the pore helix where they are coordinated by backbone oxygen atoms, a recurrent motif found in multiple proteins. The binding of Ca2+ ion in the selectivity filter controls the widening of the pore as shown in crystal structures and in molecular dynamics simulations. The structural, functional and computational data provide a characterization of this calcium-gated cationic channel.

A structural study of ion permeation in OmpF porin from anomalous X-ray diffraction and molecular dynamics simulations.

OmpF, a multiionic porin from Escherichia coli, is a useful protypical model system for addressing general questions about electrostatic interactions in the confinement of an aqueous molecular pore. Here, favorable anion locations in the OmpF pore were mapped by anomalous X-ray scattering of Br(­) ions from four different crystal structures and compared with Mg(2+) sites and Rb(+) sites from a previous anomalous diffraction study to provide a complete picture of cation and anion transfer paths along the OmpF channel. By comparing structures with various crystallization conditions, we find that anions bind in discrete clusters along the entire length of the OmpF pore, whereas cations find conserved binding sites with the extracellular, surface-exposed loops. Results from molecular dynamics simulations are consistent with the experimental data and help highlight the critical residues that preferentially contact either cations or anions during permeation. Analysis of these results provides new insights into the molecular mechanisms that determine ion selectivity in OmpF porin.

Alternative binding modes of l-histidine guided by metal ions for the activation of the antiterminator protein HutP of Bacillus subtilis.

Anti-terminator proteins control gene expression by recognizing control signals within cognate transcripts and then preventing transcription termination. HutP is such a regulatory protein that regulates the expression of the histidine utilization (hut) operon in Bacillus subtilis by binding to cis-acting regulatory sequences in hut mRNAs. During the anti-termination process, l-histidine and a divalent ion are required for hutP to bind to the specific sequence within the hut mRNA. Our previous crystal structure of the HutP-l-histidine-Mg(2+)-RNA ternary complex demonstrated that the l-histidine ligand and Mg(2+) bind together such that the backbone nitrogen and carboxyl oxygen of l-histidine coordinate with Mg(2+). In addition to the Mg(2+), other divalent ions are also known to efficiently support the l-histidine-dependent anti-termination of the hut operon, and the best divalent ion is Zn(2+). In this study, we determined the crystal structure of the HutP-l-histidine-Zn(2+) complex and found that the orientation of l-histidine coordinated to Zn(2+) is reversed relative to that of l-histidine coordinated to Mg(2+), i.e., the imidazole side chain nitrogen of l-histidine coordinates to Zn(2+). This alternative binding mode of the l-histidine ligand to a divalent ion provides further insight into the mechanisms responsible for the activation of RNA binding during the hut anti-termination process.

Cation-selective pathway of OmpF porin revealed by anomalous X-ray diffraction.

The OmpF porin from the Escherichia coli outer membrane folds into a trimer of beta-barrels, each forming a wide aqueous pore allowing the passage of ions and small solutes. A long loop (L3) carrying multiple acidic residues folds into the beta-barrel pore to form a narrow "constriction zone". A strong and highly conserved charge asymmetry is observed at the constriction zone, with multiple basic residues attached to the wall of the beta-barrel (Lys16, Arg42, Arg82 and Arg132) on one side, and multiple acidic residues of L3 (Asp107, Asp113, Glu117, Asp121, Asp126, Asp127) on the other side. Several computational studies have suggested that a strong transverse electric field could exist at the constriction zone as a result of such charge asymmetry, giving rise to separate permeation pathways for cations and anions. To examine this question, OmpF was expressed, purified and crystallized in the P6(3) space group and two different data sets were obtained at 2.6 A and 3.0 A resolution with K(+) and Rb(+), respectively. The Rb(+)-soaked crystals were collected at the rubidium anomalous wavelength of 0.8149 A and cation positions were determined. A PEG molecule was observed in the pore region for both the K(+) and Rb(+)-soaked crystals, where it interacts with loop L3. The results reveal the separate pathways of anions and cations across the constriction zone of the OmpF pore.