The voltage-sensing domain of a hERG1 mutant is a cation-selective channel

  • Meruyert Kudaibergenova
  • , Jiqing Guo
  • , Hanif M. Khan
  • , James Lees-Miller
  • , Mahdi Mousaei
  • , Williams Miranda
  • , Van A. Ngo
  • , Sergei Yu Noskov
  • , D. Peter Tieleman
  • , Henry J. Duff

Research output: Contribution to journalArticlepeer-review

6 Scopus citations

Abstract

A cationic leak current known as an “omega current” may arise from mutations of the first charged residue in the S4 of the voltage sensor domains of sodium and potassium voltage-gated channels. The voltage-sensing domains (VSDs) in these mutated channels act as pores allowing nonspecific passage of cations, such as Li+, K+, Cs+, and guanidinium. Interestingly, no omega currents have been previously detected in the nonswapped voltage-gated potassium channels such as the human-ether-a-go-go-related (hERG1), hyperpolarization-activated cyclic nucleotide-gated, and ether-a-go-go channels. In this work, we discovered a novel omega current by mutating the first charged residue of the S4 of the hERG1, K525 to serine. To characterize this omega current, we used various probes, including the hERG1 pore domain blocker, dofetilide, to show that the omega current does not require cation flux via the canonical pore domain. In addition, the omega flux does not cross the conventional selectivity filter. We also show that the mutated channel (K525S hERG1) conducts guanidinium. These data are indicative of the formation of an omega current channel within the VSD. Using molecular dynamics simulations with replica-exchange umbrella sampling simulations of the wild-type hERG1 and the K525S hERG1, we explored the molecular underpinnings governing the cation flow in the VSD of the mutant. We also show that the wild-type hERG1 may form water crevices supported by the biophysical surface accessibility data. Overall, our multidisciplinary study demonstrates that the VSD of hERG1 may act as a cation-selective channel wherein a mutation of the first charged residue in the S4 generates an omega current. Our simulation uncovers the atomistic underpinning of this mechanism.

Original languageEnglish
Pages (from-to)4585-4599
Number of pages15
JournalBiophysical Journal
Volume121
Issue number23
DOIs
StatePublished - Dec 6 2022
Externally publishedYes

Funding

This work was supported by the Canadian Institutes of Health Research (to S.Y.N., H.J.D., and D.P.T.) and the Discovery Grant Program of Natural Sciences and Engineering Research Council of Canada (NSERC) (to H.J.D.). All calculations were performed on the CFI / NSERC - RTI -supported GlaDos cluster at the University of Calgary and on the West-Grid/Compute Canada clusters under Research Allocation Awards to S.Y.N. M.K. acknowledges funding from Bettina Bahlsen Memorial , Queen Elizabeth II , and Jake Duerksen Memorial scholarships . H.M.K. acknowledges funding from the University of Calgary through the “Eyes High Postdoctoral Fellowship” program. W.M. was supported by a Vanier Canada Graduate scholarship , a Killam scholarship , and an Alberta Innovates Health Solutions studentship . Anton 2 computer time was provided by the Pittsburgh Supercomputing Center through grant R01GM116961 from the National Institutes of Health . The Anton 2 machine at Pittsburgh Supercomputing Center was generously made available by D.E. Shaw Research. D.P.T. acknowledges support from the Canada Research Chair Program .

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