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Tim Grüne K + Transport through Membrane Channels Crystallography and Molecular Dynamics: Water–Free K + Transport through Membrane Channels Tim Gruene Paul Scherrer Institute [email protected] Regio Meeting 2015 1/18

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Tim Grüne K+ Transport through Membrane Channels

Crystallography and Molecular Dynamics:

Water–Free K+ Transport through Membrane Channels

Tim GruenePaul Scherrer Institute

[email protected]

Regio Meeting 2015 1/18

Tim Grüne K+ Transport through Membrane Channels

Potassium Channels — Transport Properties

• Transport of Potassium ions across cell membranes• Abundant in pro– and eukaryotes (≥ 78 genes in humans)• Nervous signal transduction, muscle contraction• Highly K+ specific selectivity• Passive transport, i.e. gradient driven• Transport rate nearly diffusion limited

(PDB-ID 1R3J)

Regio Meeting 2015 2/18

Tim Grüne K+ Transport through Membrane Channels

The Selectivity Filter

1998 First Crystal Structures of the K+ channel KcsA by Roderick MacKinnon.

• Core of channel: 12Å tube• Scav→ S4→ S1: transport into membrane compartment• Conserved sequence TVGYG• K+–O≈ 2.8Å• (Backbone–) oxygen atoms mimic 1st hydration shell⇒ Blocks other ions, e.g. Na+,Ca2+: X–O≈ 2.4Å

Regio Meeting 2015 3/18

Tim Grüne K+ Transport through Membrane Channels

The “KWKW ” Conduction Mechanism

• A. L. Hodgkin, R. D. Keynes (1955): electrostatic repulsion prohibits K+K+K+K+. Shielding by water molecules

• Morais–Cabral, Zhou, MacKinnon, Nature (2001), 414, 37–42: determination of electron density with K+ andRb+

• Zhou & MacKinnon, JMB (2003), 333, 965–975: Crystallographic occupancy by means of the anomalous signalof T l+ and K+

1. T l+–O≈ K+–O≈ 2.8Å: interchangeable2. Occupancy refinement based on the anomal-

ous signal of T l+

3. Comparison with K+–density⇒ on average 2 K+ inside filter⇒ Crystal structure = mixture between “KWKW ”

and “WKWK” K+ K+

K+K+

K+ K+K+ K+

K+

K+

K+

W

K+

K+

S1 S2 S3 S4

W W

WW

W WW W

W

W

W

W

W

W

W

Established view: co–transport of water through Selectivity Filter

Regio Meeting 2015 4/18

Tim Grüne K+ Transport through Membrane Channels

The de Groot/Köpfer Mechanism

Based on Molecular Dynamics: no water inside Selectivity Filter

Köpfer, Song, Gruene, Sheldrick, Zachariae, de Groot: Science (2014), 346, pp. 352–355Regio Meeting 2015 5/18

Tim Grüne K+ Transport through Membrane Channels

Molecular Dynamics: Transport Model

Crystallography: Experimental Data

MD simulation contradicts established model. Crystallogrpahy:

Can K+ ions occupy adjacent sites within the selectivity filter?

Regio Meeting 2015 6/18

Tim Grüne K+ Transport through Membrane Channels

Crystallography: Occupancy vs. thermal vibration

0 2 4 6 8

10 12 14 16 18 20

10Å 5Å 3Å 2Å 1Å

Scat

terin

g fa

ctor

f(θ

)

Resolution d (=1/2s)

occ*e-Bs2*f0(θ)

occ=0.8, B=30Å2

occ=1.0, B=50Å2

occ=0.6, B=10Å2

f0(θ) K+: 18e-

Refinement “sees” the area underneath each curveRegio Meeting 2015 7/18

Tim Grüne K+ Transport through Membrane Channels

Atomic Resolution does not Resolve all Problems

• Correlation between atomic displacement parameter and occupancy > 90%

• Restraints: bind B–values to chemical environment?

• K+ ions on 4–fold symmetry axis: artefacts (1R3J (T l+))

Regio Meeting 2015 8/18

Tim Grüne K+ Transport through Membrane Channels

Step 1: Anomalous Signal in Reciprocal Space

Regio Meeting 2015 9/18

Tim Grüne K+ Transport through Membrane Channels

Relative Occupancy of T l+ from SAD Phasing

Advantages

• Only anomalous signal: no contribution from water molecules

• “Normalized structure factors”: point like atoms at 0 K, i.e. independence from B–values

Drawback: occupancies only relative to strongest peak

Regio Meeting 2015 10/18

Tim Grüne K+ Transport through Membrane Channels

Results Step 1: Ions equally distributed inside Selectivity Filter

1r3j fa.res T l+

S1 S2 S3 S4 Scav #6relative occ. 1.0 0.9 0.9 1.0 0.6 0.12

experimental anomalous electron density

Drawback: occupancies only relative to strongest peak

Regio Meeting 2015 11/18

Tim Grüne K+ Transport through Membrane Channels

Consequence from Equal Distribution for Occupancy

SAD Phasing: occ(S1) = occ(S2) = occ(S3) = occ(S4), unknown absolute.

Possible Scenarios:

average SF content Distribution occupancy⟨1 T l+

⟩Tl W W WW Tl W WW W Tl WW W W Tl 〈occ〉 ≤ 0.25⟨

2 T l+⟩

Tl W Tl WW Tl W Tl 〈occ〉 ≤ 0.5⟨

3 T l+⟩

Tl Tl Tl WTl W Tl TlW Tl Tl TlTl Tl W Tl 〈occ〉 ≤ 0.75⟨

4 T l+⟩

Tl Tl Tl Tl 〈occ〉 ≤ 1.00

Ion separation by water requires all four occupancy at least < 0.75.

Regio Meeting 2015 12/18

Tim Grüne K+ Transport through Membrane Channels

Step 2: Absolute Occupancy of T l+ from Structure Refinement

• T l+: unrestrained B–values

• T l+: anisotropic B–values

• including anomalous signal

Regio Meeting 2015 13/18

Tim Grüne K+ Transport through Membrane Channels

Result Step 2: Ions in Selectivity Filter fully occupied

1R3J (T l+)S1 S2 S3 S4 Scav

absolute occupancy (SHELXL) 1.02 (4) 0.93 (3) 0.92 (4) 0.99 (4) 0.47 (3)B[Å2] 28(1) 26(1) 25(1) 27(1) 20(2)relative occupancy (SHELXD) 1.0 0.9 0.9 1.0 0.6

• No occupancy < 75%

⇒ T l+T l+T l+T l+ predominant in crystal

Regio Meeting 2015 14/18

Tim Grüne K+ Transport through Membrane Channels

Why are the Results Different from the Original Work?

3LDC: MthK pore with 100mM K+, dmin = 1.45Å

S4 S3 S2 S1occupancy:1.00 1.00 0.80 0.92

B-value: 20(1) 18(1) 17(1) 18(1)

S4 S3 S2 S1occupancy:0.50 0.50 0.50 0.50

B-value: 12 12 11 12

Refined occupancies Fixed occupancies: 50% K+, 50% H2O

(Especially) S2: Fluctuations in map due to B↔ occ

Regio Meeting 2015 15/18

Tim Grüne K+ Transport through Membrane Channels

Conclusions

• Molecular dynamics simulations correct “text book” mechanism

• Crystallographic experimental data confirm molecular dynamics simulations

• K+–transport through membrane channels without shielding water

Regio Meeting 2015 16/18

Tim Grüne K+ Transport through Membrane Channels

Acknowledgements

B. de GrootD. KöpferG.M. Sheldrick

Roderick MacKinnon

Reference: Köpfer, Song, Gruene, Sheldrick, Zachariae, de Groot: Science (2014), 346, pp. 352–355

Regio Meeting 2015 17/18