Abstract

Key points Mutagenesis at positively charged amino acids (arginines and lysines) (R1–R4) in the voltage‐sensor domain (transmembrane segment (S) 4) of voltage‐gated Na+, K+ and Ca2+ channels can lead to an alternative ion permeation pathway distinct from the central pore.Recently, a non‐canonical ion permeation pathway was described in TRPM3, a member of the transient receptor potential (TRP) superfamily. The non‐canonical pore exists in the native TRPM3 channel and can be activated by co‐stimulation of the endogenous agonist pregnenolone sulphate and the antifungal drug clotrimazole or by stimulation of the synthetic agonist CIM0216.Alignment of the voltage sensor of Shaker K+ channels with the entire TRPM3 sequence revealed the highest degree of similarity in the putative S4 region of TRPM3, and suggested that only one single gating charge arginine (R2) in the putative S4 region is conserved.Mutagenesis studies in the voltage‐sensing domain of TRPM3 revealed several residues in the voltage sensor (S4) as well as in S1 and S3 that are crucial for the occurrence of the non‐canonical inward currents.In conclusion, this study provides evidence for the involvement of the voltage‐sensing domain of TRPM3 in the formation of an alternative ion permeation pathway. Transient receptor potential (TRP) channels are cationic channels involved in a broad array of functions, including homeostasis, motility and sensory functions. TRP channel subunits consist of six transmembrane segments (S1–S6), and form tetrameric channels with a central pore formed by the region encompassing S5 and S6. Recently, evidence was provided for the existence of an alternative ion permeation pathway in TRPM3, which allows large inward currents upon hyperpolarization independently of the central pore. However, very little knowledge is available concerning the localization of this alternative pathway in the native TRPM3 channel protein. Guided by sequence homology with Shaker K+ channels, in which mutations in S4 can create an analogous ‘omega’ pore, we performed site‐directed mutagenesis studies and patch clamp experiments to identify amino acid residues involved in the formation of the non‐canonical pore in TRPM3. Based on our results, we pinpoint four residues in S4 (W982, R985, D988 and G991) as crucial determinants of the properties of the alternative ion permeation pathway.

Highlights

  • Voltage-gated cation channels are classically described as membrane proteins with a single, central aqueous pore, regulating the flow of cations such as Na+, K+ and Ca2+

  • This alignment indicates that only a single gating charge arginine is conserved in the putative segment 4 (S4) of TRPM3, namely at the position corresponding to the second arginine (R2) of the Shaker K+ channel

  • Evidence was provided for the presence of a non-canonical ion permeation pathway in TRPM3, distinct from the central pore, which can be opened by co-application of pregnenolone sulphate (PS)+Clt or by stimulation with CIM0216 (Vriens et al 2014; Held et al 2015)

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Summary

Introduction

Voltage-gated cation channels are classically described as membrane proteins with a single, central aqueous pore, regulating the flow of cations such as Na+, K+ and Ca2+. Upon depolarization of the cell membrane, S4 movement will occur and accomplish the transport of the positive S4 charges across the membrane electric field (Bezanilla, 2002) This causes a conformational change of the channel and results in opening of the central pore (Horn, 2002; Catterall, 2010). The appearance of the inward rectifying currents at negative voltages could be attributed to the opening of a non-canonical pore in TRPM3 (Vriens et al 2014; Held et al 2015) This non-canonical ion permeation pathway differs from the central pore with respect to its rectification, a lower permeability to Ca2+ and Mg2+, resistance to Ca2+-dependent desensitization and insensitivity to the open pore blocker La3+ (Vriens et al 2014; Held et al 2015). Based on site-directed mutagenesis and homology with the Shaker K+ channel, we here provide evidence for a key role of the S4 domain in mediating the currents through the non-canonical pore in TRPM3

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