short communications
A step towards long-wavelength protein crystallography: subjecting protein crystals to a vacuum
aAustralian Synchrotron, 800 Blackburn Road, Clayton, VIC 3168, Australia, and bDepartment of Physics, Astronomy and Medical Radiation Physics, Curtin University, Bentley, WA 6102, Australia
*Correspondence e-mail: alan.r-t@synchrotron.org.au
Using the UHV experimental endstation on the soft X-ray beamline at the Australian Synchrotron, lysozyme and proteinase K crystals have been exposed to a vacuum of 10−5 mbar, prior to flash-cooling in a bath of liquid nitrogen. Subsequent data collection on the MX2 beamline at the Australian Synchrotron demonstrated that, for lysozyme and proteinase K, it is possible to subject these mounted crystals to a vacuum pressure of 10−5 mbar without destroying the Despite the lower data quality of the vacuum-pumped crystals compared with control crystals, it is demonstrated that the protein crystals can survive in a vacuum under suitable conditions.
Keywords: lysozyme; proteinase K; vacuum; long-wavelength crystallography; sulfur single-wavelength anomalous diffraction.
1. Introduction
It is relatively easy to produce proteins for crystallization experiments, and the use of robotics has allowed a wider range of crystallization space to be sampled quickly and efficiently. Furthermore, owing to improvements at synchrotron sources and in detector technology, diffraction experiments can now be performed on ever smaller crystals. However, there is still a bottleneck in solving structures which have no (or not enough) similarity to existing structures in the Protein Data Bank (https:/www.rscb.org; Berman et al., 2000) to allow the structure to be determined by These cases will require structure solution to be carried out by experimental phasing methods (i.e. heavy-atom soaks, Se–Met incorporation etc.) which are often time-consuming.
Phasing experiments using sulfur as a scatterer were first undertaken in the early 1980s (Hendrickson & Teeter, 1981). Since then, improvements in synchrotron radiation sources and detectors have allowed the determination of many structures using this method.
In order to maximize the anomalous differences of these intrinsic elements, one must use X-rays with a very long wavelength (the sulfur edge at 2.485 keV gives ∼4 electrons, as does phosphor at 2.173 keV). As these wavelengths are `unreachable' on current macromolecular crystallography beamlines, data are more often collected in the region of 4–7 keV (3–1.77 Å). However, at these wavelengths air absorption becomes a real problem. To date, either the air absorption problem has been ignored or attempts to overcome the absorption effect have been undertaken by replacing the air path with a helium path. This entails affixing a `sock' reaching from the sample to the detector. In order to maintain the helium atmosphere, the sample needs to be cooled using a helium cryostat (a piece of equipment that is expensive, as is the use of helium).
This system obviously has limitations, i.e. the detector cannot easily be moved with a `sock' bolted onto the front, and it is expensive to run. More commonly, the air absorption problem has been ignored, meaning only well diffracting crystals have been amenable to phasing from sulfur single-wavelength anomalous diffraction (S-SAD).
However, recent work has shown the possibility of using multiple crystal averaging as an approach for et al., 2012, 2013, 2014; Omari et al., 2014) and using an X-ray free-electron laser (X-FEL) (Barends et al., 2013) at energies between 6 and 7 keV.
using S-SAD, and this process has been demonstrated on conventional-sized crystals (LiuDiamond Light Source (Didcot, UK) is currently commissioning a beamline designed specifically for long-wavelength crystallography and has removed the air absorption/scatter problem by removing the air path completely by holding the crystal in a vacuum. In this paper, we show a proof of principle that protein crystals (lysozyme and proteinase K) can survive in a vacuum of 10−5 mbar (1 bar = 100 000 Pa) for 5 min or more without suffering damage through loss of solvent. To the best of our knowledge, these are the first experiments where diffraction patterns have been collected on hydrated crystals subjected to a vacuum. Earlier work was undertaken by Perutz & Rogers (1946) in the 1940s in which dehydrated crystals were subjected to X-ray diffraction experiments in a specially built vacuum tank. The elimination of air scattering allowed Bragg reflections from haemoglobin crystals to be observed, which were otherwise lost in the background.
2. Materials and methods
Lyophilized powders of lysozyme and proteinase K (purity ≥90%) were purchased from Sigma–Aldrich. Crystals of lysozyme suitable for this investigation were obtained under `standard' conditions (50 mg ml−1 solution in 0.1 M sodium acetate trihydrate pH 4.6, mixed in a ratio of 1:1 with a reservoir solution containing 1.0 M NaCl and 0.1 M sodium acetate trihydrate pH 4.6), as were proteinase K crystals (20 mg ml−1 in 50 mM HEPES pH 7.0, mixed in a ratio of 1:1 with a reservoir of 1.2 M ammonium sulfate and Tris–HCl pH 8.0). Four crystals of lysozyme were mounted on four different 20 µm diameter nylon loops and coated with a layer of Paratone oil. In the text below they are referred to as follows:
(1) 30 min Control. The crystal was looped out of mother liquor from a drop and a thick coating of Paratone-N was applied. It was left at atmospheric pressure for 30 min, whereafter it was immediately flash-cooled.
(2) Control 1. The crystal was looped out of mother liquor from a drop and cryo-protected by Paratone-N, whereafter it was immediately flash-cooled.
(3) Vacuum Thick. The crystal was looped out of mother liquor from a drop and a thick coating of Paratone-N was applied. It was then subjected to a vacuum of 1.5 × 10−5 mbar for 5 min, whereafter it was immediately flash-cooled.
(4) Vacuum Thin. The crystal was looped out of mother liquor from a drop and a thin coating of Paratone-N was applied. It was then subjected to a vacuum of 1.5 × 10−5 mbar for 5 min, whereafter it was immediately flash-cooled.
For proteinase K, only one crystal was mounted on a 20 µm diameter nylon loop and coated with a layer of Paratone-N oil. The proteinase K diffraction data statistics and structure were compared with a standard proteinase K structure from the PDB (comparison data not shown).
The crystals were taken to the soft X-ray experimental endstation vacuum chamber and inserted into the loadlock chamber, which has a 360 l s−1 Leybold turbo pump attached as well as an Edwards XDS10 scroll pump, allowing us to evacuate the atmosphere to a pressure of 1.5 × 10−5 mbar within a few minutes. Subsequently, the chamber was vented to atmospheric pressure with nitrogen, whereafter the samples were immediately removed from the vacuum chamber and flash-cooled in liquid nitrogen. The lysozyme Control 1 crystal was mounted, flash-cooled and used immediately in a diffraction experiment. The second reference sample (30 min Control) was kept at atmospheric pressure on the bench for 30 min (the amount of time it took to loop, coat with oil, transfer to the soft X-ray chamber, mount on sample holders, and pump down the Vacuum Thin and Vacuum Thick crystals). All crystals were flash-cooled in a bath of liquid nitrogen prior to transfer to the MX2 beamline for data collection.
The data used for XDS (Kabsch, 2010) and reduced using Scala (Evans, 1993). S-SAD phasing was successful for the Vacuum Thick data, but difficult for the given quality of the Vacuum Thin data. Therefore, the structures of all the crystals were solved by the method (McCoy et al., 2007; Vagin & Teplyakov, 2000) within Auto-Rickshaw (Panjikar et al., 2005), with further using REFMAC5 (Vagin et al., 2004) from the CCP4 suite of programs (Winn et al., 2011).
of all the crystals were collected on an ADSC Q315r CCD diffractometer attached to the 3ID1 beamline at the Australian Synchrotron, using monochromatic radiation of 7 keV for the lysozyme crystals and 13 keV for the proteinase K crystal. All crystals were held in a stream of nitrogen gas at 100 K. Diffraction data were processed using3. Results
Results are shown in the tables of data-collection statistics (Table 1) and (Table 2) for the crystals investigated in this manuscript.
‡Rmerge = ∑hkl∑i|Ii(hkl) − 〈I(hkl)〉|/∑hkl∑iIi(hkl) and Rmeas (Rr.i.m.) = ∑hkl[N/(N − 1)]1/2∑i|Ii(hkl) − 〈I(hkl)〉|/∑hkl∑iIi(hkl), where Ii(hkl) is the ith intensity measurement of reflection hkl, 〈I(hkl)〉 is its average and N is the redundancy of a given reflection. |
|
4. Discussion
We have demonstrated that it is possible to subject mounted lysozyme and proteinase K crystals to vacuum pressures of 10−5 mbar without destroying the When undertaking subsequent diffraction experiments post vacuum subjection, we see some deterioration of the diffraction and data quality of the crystals. It should be stressed that the crystals have been under a vacuum and brought back to atmospheric pressure, whereafter they were flash-cooled. The crystals survived in a vacuum because of the layer of oil over them. The use of organic cryo-protectants such as glycerol or ethylene glycol destroyed the crystals after vacuum exposure. There are two reasons why our vacuum-exposed and oil-covered crystals lost diffraction quality: firstly the change from a vacuum to atmospheric pressure, and secondly the dehydration of the crystals in oil while under a vacuum or atmospheric pressure.
The two proteins we have used in these experiments, lysozyme and proteinase K, have solvent contents of ∼37 and ∼46%, respectively. A greater change in the c axis of the from the standard ∼37 Å observed in both of the control samples and the Vacuum Thick sample to a smaller ∼34 Å for the Vacuum Thin sample, while no significant change is observed for the proteinase K crystal exposed to a vacuum compared with the control sample (PDB code 2g4v; Mueller-Dieckmann et al., 2007).
of the protein crystal with the higher solvent content (proteinase K) was expected when exposed to a vacuum. However, this is not the case, as we see a shift for lysozyme in theEven though the crystals were coated in Paratone-N, the Vacuum Thin lysozyme sample did lose solvent whilst under a vacuum (the change in the (a).
was not observed in either of the control crystals nor the Vacuum Thick crystal), and this loss of solvent caused a change in the overall shape of the monomer, with the two lobes coming closer together, as seen in Fig. 1The Vacuum Thin and control lysozyme crystals were compared and the average root mean-square deviation (RMSD) over 129 residues was 1.4 Å. Significant RMSDs were observed between residues 43 and 50, and between residues 64 and 73 (Fig. 1b). These regions belong to the two lobes and point towards the solvent channel in the crystal packing.
In the experiment presented here, we had to allow the samples to return to atmospheric pressure prior to cooling and during data acquisition. This has an impact on the diffraction and data quality of the crystals. However, if the diffraction from an oil-coated crystal could be recorded under a vacuum at room temperature, relatively good quality data might be collected. Keeping the crystals cold under a vacuum could provide further advantages, with a reduction in radiation damage, an increase in the lifetime of the protein crystals and an improvement in data quality.
Acknowledgements
This research was undertaken on the MX2 and SXR beamlines at the Synchrotron Light Source Australia (SLSA), Victoria, Australia. The authors thank Armin Wagner for fruitful discussions.
References
Barends, T. R. M. et al. (2013). Acta Cryst. D69, 838–842. Web of Science CrossRef IUCr Journals Google Scholar
Berman, H. M., Westbrook, J., Feng, Z., Gilliland, G., Bhat, T. N., Weissig, H., Shindyalov, I. N. & Bourne, P. E. (2000). Nucleic Acids Res. 28, 235–242. Web of Science CrossRef PubMed CAS Google Scholar
El Omari, K., Iourin, O., Kadlec, J., Fearn, R., Hall, D. R., Harlos, K., Grimes, J. M. & Stuart, D. I. (2014). Acta Cryst. D70, 2197–2203. Web of Science CrossRef IUCr Journals Google Scholar
Evans, P. R. (1993). Proceedings of the CCP4 Study Weekend. Data Collection and Processing, edited by L. Sawyer, N. Isaacs & S. Bailey, pp. 114–122. Warrington: Daresbury Laboratory. Google Scholar
Hendrickson, W. A. & Teeter, M. M. (1981). Nature, 290, 107–113. CrossRef CAS Web of Science Google Scholar
Kabsch, W. (2010). Acta Cryst. D66, 125–132. Web of Science CrossRef CAS IUCr Journals Google Scholar
Laskowski, R. A., MacArthur, M. W., Moss, D. S. & Thornton, J. M. (1993). J. Appl. Cryst. 26, 283–291. CrossRef CAS Web of Science IUCr Journals Google Scholar
Liu, Q., Dahmane, T., Zhang, Z., Assur, Z., Brasch, J., Shapiro, L., Mancia, F. & Hendrickson, W. A. (2012). Science, 336, 1033–1037. Web of Science CrossRef CAS PubMed Google Scholar
Liu, Q., Guo, Y., Chang, Y., Cai, Z., Assur, Z., Mancia, F., Greene, M. I. & Hendrickson, W. A. (2014). Acta Cryst. D70, 2544–2557. Web of Science CrossRef IUCr Journals Google Scholar
Liu, Q., Liu, Q. & Hendrickson, W. A. (2013). Acta Cryst. D69, 1314–1332. Web of Science CrossRef CAS IUCr Journals Google Scholar
McCoy, A. J., Grosse-Kunstleve, R. W., Adams, P. D., Winn, M. D., Storoni, L. C. & Read, R. J. (2007). J. Appl. Cryst. 40, 658–674. Web of Science CrossRef CAS IUCr Journals Google Scholar
Mueller-Dieckmann, C., Panjikar, S., Schmidt, A., Mueller, S., Kuper, J., Geerlof, A., Wilmanns, M., Singh, R. K., Tucker, P. A. & Weiss, M. S. (2007). Acta Cryst. D63, 366–380. Web of Science CrossRef CAS IUCr Journals Google Scholar
Panjikar, S., Parthasarathy, V., Lamzin, V. S., Weiss, M. S. & Tucker, P. A. (2005). Acta Cryst. D61, 449–457. Web of Science CrossRef CAS IUCr Journals Google Scholar
Perutz, M. F. & Rogers, G. L. (1946). J. Sci. Instrum. 23, 217. CrossRef Web of Science Google Scholar
Vagin, A. A., Steiner, R. A., Lebedev, A. A., Potterton, L., McNicholas, S., Long, F. & Murshudov, G. N. (2004). Acta Cryst. D60, 2184–2195. Web of Science CrossRef CAS IUCr Journals Google Scholar
Vagin, A. & Teplyakov, A. (2000). Acta Cryst. D56, 1622–1624. Web of Science CrossRef CAS IUCr Journals Google Scholar
Winn, M. D. et al. (2011). Acta Cryst. D67, 235–242. Web of Science CrossRef CAS IUCr Journals Google Scholar
This is an open-access article distributed under the terms of the Creative Commons Attribution (CC-BY) Licence, which permits unrestricted use, distribution, and reproduction in any medium, provided the original authors and source are cited.