research papers
Exploiting fast detectors to enter a new dimension in room-temperature crystallography
aDiamond Light Source, Harwell Science and Innovation Campus, Didcot OX11 0DE, England, bDectris Ltd, Neuenhofer Strasse 107, 5400 Baden, Switzerland, and cDivision of Structural Biology, University of Oxford, The Henry Wellcome Building for Genomic Medicine, Roosevelt Drive, Oxford OX3 7BN, England
*Correspondence e-mail: robin.owen@diamond.ac.uk
A departure from a linear or an exponential intensity decay in the diffracting power of protein crystals as a function of absorbed dose is reported. The observation of a
raises the possibility of collecting significantly more data from crystals held at room temperature before an intolerable intensity decay is reached. A simple model accounting for the form of the intensity decay is reintroduced and is applied for the first time to high frame-rate room-temperature data collection.1. Introduction
Room-temperature data collection remains an important tool in macromolecular crystallography (MX), despite the dominance of cryocrystallography. Cryoprotection and the subsequent cooling process can damage samples, making the assessment of crystallization conditions difficult or even impossible. Furthermore, cryocooling can also hide conformational diversity (Fraser et al., 2011) or introduce artefacts in side-chain interactions (Juers & Matthews, 2004), making a room-temperature structure desirable even in cases where samples prove amenable to cryocooling.
New facilities for in situ crystallography such as those described by Jacquamet et al. (2004), Bingel-Erlenmeyer et al. (2011) and Axford et al. (2012) have aided a renaissance in room-temperature MX at synchrotron sites, removing the need for crystal manipulation by allowing a crystallization tray to be mounted directly in the X-ray beam. The concomitant development of crystallization trays, chips and other hardware has resulted in simplified experimental setups and reduced diffuse scatter, and has furthered the uptake of the method (Soliman et al., 2011; Kisselman et al., 2011) so that useful biological results can now be readily obtained (see, for instance, Wang et al., 2012; Porta et al., 2013).
Despite these advances a fundamental challenge remains: the seemingly inevitable rapid onset of radiation damage means that the amount of data that can be collected from room-temperature crystals is severely limited. This impacts both crystal screening and structure solution and is the primary reason why data collection at room temperature is not routine at all synchrotron sources. In the case of crystal screening the rapid onset of radiation damage limits the use of tools such as the diffraction grid scan (Aishima et al., 2010; Bowler et al., 2010; Cherezov et al., 2009) to find and assess crystals, and precludes diffraction-based screening of room-temperature crystals prior to cryocooling. In situ crystallography is by no means limited to crystal screening, however. Some samples, most notably viruses, can prove virtually impossible to successfully cryocool, meaning that all data must be collected at room temperature, and, as noted above, a physiologically more relevant structure determined at room temperature may provide additional insight or confirmation of the absence of cooling-induced artefacts.
For room-temperature structure solution, radiation damage usually severely limits the amount of data that can be collected from each sample. This generally imposes the need for a large number of (isomorphous and well diffracting) crystals, which in turn can make subsequent steps in the structure-solution pipeline such as data integration, scaling and phasing more challenging. Increasing the amount of data that can be collected from crystals by changing the manner of data collection would alleviate these problems and allow useful data to be collected from more weakly diffracting crystals.
In contrast to 100 K, where little or no dose-rate effect has been observed (Sliz et al., 2003; Garman, 2010), at room temperature the rate at which data are collected can have a profound effect on the volume of data that it is possible to obtain. Recent experiments have revealed a systematic, and significant, increase in the dose tolerance of room-temperature protein and virus crystals as a function of dose rate (Owen et al., 2012; Warkentin et al., 2011, 2012). The collection of diffraction data continuously and at dose rates in excess of ∼0.7 MGy s−1 allowed more data to be collected from each crystal. In contrast, other recent studies (for example, Warkentin et al., 2013; Leal et al., 2013) conducted at lower dose rates have reported little dose-rate dependence at room temperature.
A dose-rate-dependent increase in lifetime raises the possibility of at least partly addressing the radiation damage-induced challenges outlined above. The physical origin of a dose-rate effect has previously been attributed to the rate of diffusion of free radicals through the
quenching of radicals by solvent molecules and free-radical recombination, although a model relating these effects to the diffracting power of the crystal has until now remained elusive. In order to shed light on the mechanisms of radiation damage at room temperature, we now report data collected at significantly higher dose rates and with the diffracting power sampled with increased temporal resolution.Despite the use of a state-of-the-art PILATUS2 6M detector (Dectris, Baden, Switzerland), the experiments previously reported were limited to a minimum exposure time of 40 ms (maximum 25 frames per second; fps). A firmware upgrade to the I24 6M detector now allows data collection at 200 fps (minimum exposure time 5 ms;
2.3 ms) when reading out a subarea of the detector, and recently a new generation of PILATUS detectors have become available offering increased frame rates and a reduced The PILATUS3 300K detector is able to continuously record data at up to 500 fps (minimum exposure time 2 ms; 0.95 ms), allowing X-ray beam-induced effects in protein and virus crystals to be followed on much shorter timescales.In the work described here, we report a significant deviation from previous observations of a simple exponential or linear decay in the diffracting power of crystals at room temperature. Instead, two phases of decay are observed: an initial slow linear decay, or
which is then followed by a faster The presence of an initial truly raises the prospect of collecting largely complete data sets from room-temperature microcrystals. We show that data of comparable quality to those collected from cryocooled crystals can be collected from room-temperature crystals at high dose and frame rates. A macroscopic four-state model outlining the physical origin of this is reintroduced and discussed.2. Sample preparation and data collection
2.1. Sample preparation
Bovine enterovirus serotype 2 (BEV 2) crystals of ∼30 × 30 × 30 µm in size were grown in F23, with unit-cell parameters a = b = c ≃ 436.6 Å, in 1.5 M ammonium sulfate, 0.1 M bis-tris propane pH 7.0 using the sitting-drop method (Walter et al., 2005). Thaumatin was purchased from Sigma (product No. T7638) and was dissolved in double-distilled H2O to a concentration of 40 mg ml−1. 4 µl protein solution was mixed with 2 µl reservoir solution consisting of 50 mM ADA pH 6.8, 0.6 M potassium/sodium tartrate, 20% glycerol, resulting in crystals of approximately 50 × 50 × 50 µm. Foot and mouth disease virus (FMDV) A22-wt crystals with average dimensions of 50 × 50 × 5 µm were grown in I222, with unit-cell parameters a = 328, b = 341, c = 363 Å, in 4 M ammonium acetate, 100 mM bis-tris propane pH 7.0 using the sitting-drop method (Porta et al., 2013).
2.2. Data collection
Diffraction data were collected on beamline I24 at Diamond Light Source using a beam size of 10 × 10 or 20 × 20 µm (FWHM of Gaussian profile) at a temperature of 295 K. Data were collected with X-rays of energy 12.8 keV with a 12 photons s−1 in the unattenuated beam. Data were also collected at 9.2 keV with an incident of 3.2 × 1012 photons s−1. This allowed dose rates of up to 4.8 MGy s−1 (12.8 keV) and 25 MGy s−1 (9.2 keV) to be realised. The at the sample position was measured using a silicon PIN diode and was calculated as described by Owen et al. (2009). The estimated error in calculation of in this manner is <5%. The dose in MGy absorbed by each crystal during a data set was determined using RADDOSE (Paithankar et al., 2009).
of 1.4 × 10Unless otherwise stated, diffraction images were pseudo-stills with an oscillation range of 1 mdeg per image. A continuous rotation, rather than repeated still images, was collected from each crystal as 1 mdeg was the minimum rotation range permitted by the data-collection software. While this method of tracking the diffracting power has the advantage of avoiding the introduction of new material into the beam, it is susceptible to increases in mosaic spread and cell-dimension changes triggered by radiation damage. These changes have the potential to alter reflection centroids and widths and thus introduce new reflections to the image or remove previously observed reflections. In between these extremes we would expect to observe increases and decreases in individual reflections. One of the assumptions that we make is that Bragg spot intensity variations owing to the cell and mosaic effects outlined above will average out over the several hundred recorded reflections in each diffraction image. This assumption is justified in part by the results obtained: data collected from multiple crystals in random orientations exhibit the same trend in intensity decay, with no strong variation in diffracting power between sequential images as would be expected if variation in the XDS (Kabsch, 2010; details of the data analysis are given in §2.3) showed the variation in unit-cell dimensions to be typically less than 0.5% over the duration of a data set, demonstrating that any contribution to intensity variation arising from changes in unit-cell size is small.
and mosaicity resulted in significant changes to the total diffracting power. Furthermore,Diffraction data were recorded using two different area detectors: a PILATUS2 6M-F (P2) and a PILATUS3 300K (P3). A software upgrade to the P2 detector allowed the central two modules to be read out at up to 200 fps (minimum exposure time 5 ms). The 6 counts per pixel per second. The P3 300K detector is able to continuously record data at up to 500 fps (minimum exposure time 2 ms, 0.95 ms, maximum count rate >12 × 106 counts per pixel per second). The P3 detector also differs from the P2 detector in that instant retrigger of the counter means that the of the detector is reduced to the duration of a single interaction (Loeliger et al., 2012).
of this detector is 2.3 ms and the maximum count rate is 2.4 × 102.3. Data analysis
X-ray diffraction data were analysed in two ways. Firstly, data were analysed using LABELIT (Sauter & Poon, 2010), using the program DISTL to determine the integrated signal strength given in counted photons above the local background of all Bragg candidates. This quantity was calculated on a per-image basis and was defined as the diffracting power of the crystal. Data were also integrated using XDS (Kabsch, 2010) with the diffracting power defined as the sum total of I/σ(I) over all indexed reflections on the diffraction image. The trend in intensity decay observed was independent of the analysis method used, although we found that the XDS approach provided smoother decay curves for weak data.
2.4. Intensity decay model
Sygusch & Allaire (1988) proposed a model of sequential radiation damage developed from that described by Blake & Phillips (1962). The Blake and Phillips model postulates that an irradiated protein crystal is made up of three fractions, unchanged, damaged and destroyed, the first two of which contribute to the observed diffraction pattern. This three-state model predicts a simple in the diffracting power of a crystal. The Sygusch and Allaire four-state model includes an additional state which also contributes to the observed diffracting power. This state was defined as being characterized by protein that has undergone a number of ionization events or suffered site-specific damage but is broadly unchanged in terms of its scattering power with respect to the unchanged state. In this four-state model, radiation damage follows three steps:
For clarity, we use here the nonclementure N, S, D and A to refer to the four states. The contribution of the N, S and D states to the observed diffraction pattern varies as a function of absorbed dose d, i.e..
The contribution of D is resolution-dependent, but when tracking the total diffracting power of each crystal this dependence can be neglected. Solution of the rate equations derived from this model allows the diffracting power of a crystal to be predicted as a function of absorbed dose. A solution can be determined in two regimes: when d < 1/k0′ and when d > 1/k0′, where k0′ = k0I0. Initial analysis of intensity-decay profiles indicated that they are best described by the model in the case when k1 = k2 ≠ 0 in both of these regimes. The intensity-decay curve is thus described by only two variables k0 and k1. In the first regime, when the absorbed dose d is less than 1/k0′, Sygusch and Allaire showed that the diffracting power of a crystal varies as
and in the second regime when d > 1/k0′ and k1 = k2 as
The diffracting power of each crystal as a function of dose was fitted with a dose-response curve of the form (2) in the low-dose region (typically when I/I0 > 0.5) and of the form (3) in the high-dose region.
The model predicts that the diffracting power tends to zero at high absorbed doses. However, in practice, using the background-subtraction models in the software we used, even images showing no diffraction spots appear to possess nonzero diffracting power, presumably owing to imperfect modelling of the diffuse scatter present on the detector. At very low count levels, the background exhibits strong pixel-to-pixel variation; thus, calculation of the Bragg intensity above background may be overestimated when the diffracting power of the crystal is low. A nonzero diffracting power in the absence of observable spots is best illustrated by the BEV data shown in Fig. 1: at doses above 2 MGy (times of >500 ms) the diffracting power remains constant at ∼0.15. In this dose and time domain no Bragg spots are visible on the diffraction images and the diffracting power no longer changes as a function of absorbed dose. This baseline intensity of 0.15 must thus be subtracted from the diffracting power if the model is to describe the data well. Changing the threshold for the minimum number of counts in a spot reduces this value at the expense of causing weak high-resolution reflections at the start of the data set to be ignored. The low mosaicity of room-temperature crystals also has an effect: Bragg spots are often 1–2 pixels in size, so the threshold on the minimum number of pixels in a spot must also be set at a low value contributing to integration of background. Owing to this need to both rescale and normalize the data, analysis of the decay of all crystals described in this paper has been performed twice: firstly on normalized and scaled data using the Sygusch and Allaire decay functions presented above and secondly on raw data using a dose-response curve as described below.
Intensity variation as a function of dose was also fitted with a standard dose-response curve of the form
where A2 represents the upper asymptote (i.e. the diffracting power at zero dose), A1 represents the lower asymptote (the final diffracting power), logx0 the midpoint of the function, p the Hill slope and d the absorbed dose using OriginPro (OriginLab). This function was chosen as the standard form of the dose-response inhibition curve, i.e. a slow initial decay followed by a rapid decay, closely resembles the nonlinear decays in diffracting power observed. A crystal lifetime was defined as the dose when the diffracting power fell to 85% of its initial value, as historically this was seen as the point at which room-temperature data collection should be halted (Blundell & Johnson, 1976).
3. Results
The intensity decay of three crystal types as a function of absorbed dose is shown in Fig. 1(a). At high dose rates (>1 MGy s−1) a clear lasting ∼500 kGy is visible. The dependence of the on the dose rate is illustrated by the contrasting intensity decay of thaumatin at incident dose rates of 1.32 and 0.36 MGy s−1. The data from FMDV crystals were collected at a lower energy of 9.2 keV at a significantly higher dose rate of 25.2 MGy s−1, but do not show a significantly increased in comparison to the thaumatin and BEV data (all collected at 12.8 keV). Rate constants obtained by fitting Sygusch–Allaire intensity decays are given in Table 1. Fig. 1(b) shows the same intensity decays as a function of time: in contrast to Fig. 1(a) no correlation is observed between different crystal types. This lack of correlation in the time domain is true for both the duration of the and the rate of the subsequent faster decay. Thaumatin and FMDV data were recorded using the P3 detector. The BEV 2 data were recorded using the P2 detector.
In all of the experiments described here, the maximum observed count rates were well below the maximum count rate recordable by the detector. The maximum count rates (counts per second; cps) recorded for each crystal type were: BEV 2 (P2), 0.304 Mcps (12.5% of the maximum); thaumatin (P3), 5.35 Mcps (44% of the maximum); FMDV, 1.2 Mcps (9.9% of the maximum). Note that all of the above refer to the single most intense spot within a data set: average spot intensities are an order of magnitude lower than this. For example, in the thaumatin data set, in which a maximum count rate of 5.35 Mcps was recorded, the maximum count rate in the second most intense spot is 2.55 Mcps (21% of the maximum). It is clear from this that the experiments are well within the valid count rate ranges of the detectors used.
Fig. 2(a)1 shows the intensity decay of a thaumatin crystal with a dose-response curve (4) and Sygusch–Allaire low-dose and high-dose domain (equations 2 and 3) curves fitted. (2) was fitted in the region I/I0 > 0.5 and (3) in the region I/I0 < 0.5. Greater agreement between the rate constants can be obtained by fitting (3) to the region where the absorbed dose d is more than or equal to the value of (1/k0) obtained from (2). If this is performed, then in the high-dose region 1/k0 and 1/k1 become 517 ± 25 and 174 ± 12 kGy, respectively. Fig. 2(b) illustrates the variation in the rate of intensity decay for different resolution shells. Rate constants for each fit are given in Table 2. For the highest resolution shell it was not possible to fit (3) to the data, presumably because the becomes small compared with the duration of an image.
|
The presence of a and Table 3. An effect of crystal rotation is the introduction of artefacts into the diffracting power as a function of frame number. What is clear is the lack of variation in scales and Rmerge for the first half of the data set. Scaling the first 350 images (bottom row of Fig. 3; Table 2) results in a data set indistinguishable in quality from one collected at 100 K as judged by the scaling metrics detailed above and the statistics in Table 3.
raises the question of how this can be usefully exploited in room-temperature MX. In order to assess the possibility of exploiting the data were collected from a room-temperature lysozyme crystal at 500 fps using the unattenuated beam at I24. For this experiment the beamsize was increased to 50 × 50 µm to match the crystal size and an oscillation angle of 0.1° per image was used. Scaling statistics for 700 images (total exposure time 1.4 s, cumulative absorbed dose 2.35 MGy) are shown in the top row of Fig. 3
|
Fig. 4 compares further the contrast between room temperature and 100 K. Fig. 4(a) shows the resolution-dependent change in diffracting power of a thaumatin crystal as a function of absorbed dose at 100 K. The absence of a dose-rate effect at 100 K (Sliz et al., 2003) means that the difference in dose rate between the samples should not affect the comparison despite the differing dose rates used. While a is not immediately apparent, deviation from a linear or is visible at low doses (Fig. 4a, inset). This is most clearly visible for the low-resolution data (green triangles), but is also apparent for `all data' (red triangles). If an is fitted then the residual is approximately constant over the whole data range except at very low doses (<1 MGy), when it increases sharply, indicating that an function describes this region relatively poorly. A Sygusch–Allaire intensity decay (2) has been fitted to the low-dose domain of the total intensity decay with 1/k0 = 26.2 ± 10 kGy and 1/k1 = 336 ± 6 kGy, and while this shows some deviation at doses of <1 MGy, it provides a better description of the observed decay than a simple function.
Fig. 4(b) overlays data from Figs. 2(b) (room temperature) and 4(a) (100 K). The dose required to halve the diffracting power of the crystal (all resolution shells) at 100 K is 19.4 MGy, whereas the dose required to halve the diffracting power of the room-temperature crystal is 525 kGy, a factor of ∼37 less. The short duration of the room-temperature coupled with frame-to-frame variations in the diffracting power make it difficult to determine what the crystal lifetime would be if this slow rate of decay were to be extended by, for example, collecting at higher dose rates or reducing the temperature. Based on a linear fit to data within the room-temperature (the first 50 data points), if the could be extended further, then the dose required to halve the diffracting power at room temperature would be ∼1.8 MGy, a factor of only 7.5 less than the lifetime at 100 K.
4. Discussion
Following observation of X-ray-induced decay of myoglobin crystals, Blake & Phillips (1962) proposed that irradiated protein crystals are made up of a linear combination of three states: an unchanged fraction A1, a disordered fraction A2 and an amorphous fraction A3. The fractions A1 and A2 contribute to the observed diffraction pattern such that the diffracting power of the crystal falls off in the form
as a function of time (or dose). An intensity decay of this form is unable to describe the observations detailed in §3 of a followed by a rapid The limiting aspect of the model is that only two states can contribute to the diffracting power of the crystal: this limitation also applies to developments of the three-state model (for example, Hendrickson, 1976). The Sygusch and Allaire model described in §2.4 postulates that upon irradiation the diffracting power of a protein crystal can be described by sequential progression through four states [native (N), site-specific (S), disordered (D) and amorphous (A)]. In this model, three states (N, S and D) contribute to the diffracting power.
The four-state model predicts nonlinear and non-exponential intensity decay, in agreement with the observed intensity decays presented here. The diffraction data presented here are best described by the NSDA model in the case when k1 (S→D) is equal to k2 (D→A). Provided that the timescale (1/k0) of the transition from native to site-specific (N→S) within the sample is slow compared with the experiment, a clearly resolvable delay in the apparent onset of radiation damage results. This is the observed in Figs. 1 and 2. A was first observed in a Laue experiment through the use of a by Moffat et al. (1986), but to our knowledge was not pursued. This effect has not been observed on a monochromatic source as until now the frame rate at which detectors can operate has been significantly larger than the timescale of this transition. Prophetically, Sygusch and Allaire remarked `this delay could be advantageously exploited by efficient two-dimensional detection systems', as is the case here with a detector capable of collecting 500 frames per second.
Following determination of the rate constants k0 and k1, the population of each fraction of the crystal in both regions can be plotted as a function of absorbed dose. This is shown for the thaumatin crystal decay shown in Fig. 2 in Fig. 5. Fig. 5 highlights the result of the sequential damage process on the observed intensity decay. At low doses the intensity decay is slow while the undamaged fraction of the crystal is converted to the dose-dependent state S characterized by site-specific rather than global damage. Subsequent to this significant disruption to the lattice occurs, represented by the increasing population of the states D and A, and the diffracting power follows an exponential-like decay. The diffracting power mirrors the fraction of the crystal in the amorphous state A.
Comparison of room-temperature and cryogenic rates of decay (Fig. 4b) shows that the temperature-dependence of k0, which represents the rate at which the population of the site-specific fraction of the crystal increases, is large. The change in 1/k0 observed between thaumatin held at room temperature (417 kGy) and 100 K (26.2 MGy) is a factor of 63. This is remarkably similar to the factor of ∼70 increase in lifetime previously reported in the literature (Southworth-Davies et al., 2008), although it should be noted that the accompanying change in k1 (a factor of 1.8) also results in a change in the rate of intensity decay. The large decrease in k0 at low temperatures is a result of the reduced mobility of free radicals, particularly hydroxyl (), at 100 K, resulting in a greatly reduced rate of site-specific damage. The presence of a dose-rate effect at room temperature can, as previously postulated, be attributed to a number of effects: the rate of diffusion of free radicals through the the quenching of radicals by solvent molecules and free-radical recombination. While it is not yet possible to say which of these dominates, the net result is reflected by a change in the k0.
It should be noted the increase in 1/k0 at low temperatures does not imply that cryocooling completely mitigates rapid site-specific damage, or that structures determined at 100 K are free of damage artefacts. Numerous studies in the literature, in particular those making use of complementary methods, have reported the extremely rapid onset of site-specific damage even at temperatures below 130 K. Several approaches, including (Oliéric et al., 2007), UV–Vis (Beitlich et al., 2007) and EPR plus UV–Vis (Sutton et al., 2013), have reported lifetimes of less than 1 MGy in comparison to lifetimes of >20 MGy based on intensity decay. For room-temperature data collection it is a concern that data sets, or partial data sets, predominantly represent a damaged rather than the native structure. From Fig. 5 it can be seen that the estimated population of the site-specific state does not become greater than the population of the native state until I/I0 ≃ 0.70.
Beam-induced heating is a potentially limiting problem if the et al. (2012) suggests a steady-state temperature difference of 32.5 K for the high dose-rate (4.8 MGy s−1) BEV data described here. As the crystals used were larger than the beam size, the so-called `fin effect' acts to minimize any temperature increase within the irradiated volume. Measurements by Snell et al. (2007) of the temperature change induced by X-rays within glass beads suggests that a is not reached for ∼5 s, although approximately half of the final temperature rise is realised within ∼1 s of exposure to X-rays. For samples smaller than the 1 and 2 mm diameter glass beads used by Snell and coworkers, it can be expected that temperature changes occur on faster timescales. However, given the short duration of the experiments described here (<1 s), we believe the steady-state figure of 33 K provides an upper bound for the potential temperature rise in the typical lifetime of crystals (<0.5 s). Using the same model, a greater temperature rise (a factor of 5.3) would be expected for the FMDV data shown in Fig. 1. Observation of crystals during exposure to X-rays at these dose rates (∼25 MGy s−1) suggests that a major temperature rise is not realised, since no obvious signs of boiling are observed. Nevertheless, at higher temperatures rates of diffusion and reaction rates are increased and thus beam-induced heating may well result in a narrowing of the lag-phase window. We cannot rule out that this may have a significant effect on some of the results presented here, and beam-induced heating may prevent full exploitation of the when samples are subjected to higher fluxes, which will lead to larger and faster temperature changes. The use of humidifier devices providing a continuous flow of gas at, or just below, room temperature may partially alleviate heating effects, but proper quantification of this is required.
is to be fully exploited. A calculation based on equation 8 in WarkentinFig. 6 compares the data in this study with the lifetimes reported in Owen et al. (2012). Consistent with these earlier results, we here observe a dose-rate dependence of crystal lifetime, with increased lifetimes at higher dose rates. The origin of a dose-rate effect was postulated to result from three effects: free-radical diffusion, solvent quenching and recombination. The work here provides evidence for a macroscopic model explaining the form of the X-ray-induced decay in the diffracting power of crystals but does not directly shed light onto the processes and species causing this decay. The model does provide approximate dose scales for when diffusion, quenching and recombination occur as these might be considered to be most significant before the transition from the native to the site-specific state (N→S) is complete.
Despite the relatively small window before crystal destruction, it is possible to collect high-quality room-temperature diffraction data at high dose and frame rates (Table 2). Despite a of 0.95 ms per 2 ms exposure, good scaling statistics are obtained. This is presumably owing in part to the mosaicity of the crystal (reported to be 0.36° by XDS) being significantly larger than the oscillation angle of 0.1° per image. While the data in the example shown are incomplete, the possibility of collecting significant wedges of data from room-temperature microcrystals significantly increases the scope of in situ MX for, for example, high-throughput rapid ligand-screening experiments, removing the need to mount and cryocool samples.
It is important to note variation between different crystal types: this highlights the usefulness of the information that can be provided by exploratory data sets (Krojer & von Delft, 2011). At room temperature, we suggest that the optimal approach to confirm what the is for a particular crystal type with the at the beamline being used would be the collection of stills, or very small oscillation, images from a sacrificial crystal. Data collection using still images minimizes any contribution from crystal rotation as observed in Fig. 3. Nonetheless, some variation between crystals should still be expected.
In conclusion, the data presented here show a clear departure from a linear or an
in the diffracting power of room-temperature protein crystals. The presence of a at low doses can be explained through consideration of a sequential four-state model, the first three states of which contribute to the observed diffraction pattern. Comparison of data from crystals held at cryogenic and room temperatures illustrates the applicability of the model to both cases. The ability to rapidly collect diffraction data from room-temperature crystals within the raises the possibility of significantly reducing the number of crystals required for room-temperature structure solution.Supporting information
Supporting Information. DOI: https://doi.org/10.1107/S1399004714005379/wa5063sup1.pdf
Acknowledgements
We would like to thank Wolfgang Kabsch for useful advice on how to best integrate still or pseudo-still images using XDS, and Colin Nave and Marc Allaire for useful discussions. We would also particularly like to thank Sebastian Commichau for his valuable assistance with the P3 detector. The work undertaken on beamline I24 at Diamond Light Source was under proposal NT5968.
References
Aishima, J., Owen, R. L., Axford, D., Shepherd, E., Winter, G., Levik, K., Gibbons, P., Ashton, A. & Evans, G. (2010). Acta Cryst. D66, 1032–1035. Web of Science CrossRef CAS IUCr Journals Google Scholar
Axford, D. et al. (2012). Acta Cryst. D68, 592–600. Web of Science CrossRef CAS IUCr Journals Google Scholar
Beitlich, T., Kühnel, K., Schulze-Briese, C., Shoeman, R. L. & Schlichting, I. (2007). J. Synchrotron Rad. 14, 11–23. Web of Science CrossRef CAS IUCr Journals Google Scholar
Bingel-Erlenmeyer, R., Olieric, V., Grimshaw, J. P. A., Gabadinho, J., Wang, X., Ebner, S. G., Isenegger, A., Schneider, R., Schneider, J., Glettig, W., Pradervand, C., Panepucci, E. H., Tomizaki, T., Wang, M. & Schulze-Briese, C. (2011). Cryst. Growth Des. 11, 916–923. CAS Google Scholar
Blake, C. & Phillips, D. (1962). Biological Effects of Ionizing Radiation at the Molecular Level, pp. 183–191. Vienna: International Atomic Energy Agency. Google Scholar
Blundell, S. & Johnson, L. (1976). Protein Crystallography. New York: Academic Press. Google Scholar
Bowler, M. W., Guijarro, M., Petitdemange, S., Baker, I., Svensson, O., Burghammer, M., Mueller-Dieckmann, C., Gordon, E. J., Flot, D., McSweeney, S. M. & Leonard, G. A. (2010). Acta Cryst. D66, 855–864. Web of Science CrossRef CAS IUCr Journals Google Scholar
Cherezov, V., Hanson, M. A., Griffith, M. T., Hilgart, M. C., Sanishvili, R., Nagarajan, V., Stepanov, S., Fischetti, R. F., Kuhn, P. & Stevens, R. C. (2009). J. R. Soc. Interface, 6, S587–S597. Web of Science CrossRef PubMed CAS Google Scholar
Fraser, J. S., van den Bedem, H., Samelson, A. J., Lang, P. T., Holton, J. M., Echols, N. & Alber, T. (2011). Proc. Natl Acad. Sci. USA, 108, 16247–16252. Web of Science CrossRef CAS PubMed Google Scholar
Garman, E. F. (2010). Acta Cryst. D66, 339–351. Web of Science CrossRef CAS IUCr Journals Google Scholar
Hendrickson, W. A. (1976). J. Mol. Biol. 106, 889–893. CrossRef CAS PubMed Web of Science Google Scholar
Jacquamet, L., Ohana, J., Joly, J., Legrand, P., Kahn, R., Borel, F., Pirocchi, M., Charrault, P., Carpentier, P. & Ferrer, J.-L. (2004). Acta Cryst. D60, 888–894. Web of Science CrossRef CAS IUCr Journals Google Scholar
Juers, D. H. & Matthews, B. W. (2004). Acta Cryst. D60, 412–421. Web of Science CrossRef CAS IUCr Journals Google Scholar
Kabsch, W. (2010). Acta Cryst. D66, 125–132. Web of Science CrossRef CAS IUCr Journals Google Scholar
Karplus, P. A & Diederichs, K. (2012). Science, 336, 1030–1033. Web of Science CrossRef CAS PubMed Google Scholar
Kisselman, G., Qiu, W., Romanov, V., Thompson, C. M., Lam, R., Battaile, K. P., Pai, E. F. & Chirgadze, N. Y. (2011). Acta Cryst. D67, 533–539. Web of Science CrossRef CAS IUCr Journals Google Scholar
Krojer, T. & von Delft, F. (2011). J. Synchrotron Rad. 18, 387–397. Web of Science CrossRef CAS IUCr Journals Google Scholar
Leal, R. M. F., Bourenkov, G., Russi, S. & Popov, A. N. (2013). J. Synchrotron Rad. 20, 14–22. Web of Science CrossRef CAS IUCr Journals Google Scholar
Loeliger, T., Bronnimann, C., Donath, T., Schneebeli, M., Schnyder, R. & Trub, P. (2012). Nuclear Science Symposium and Medical Imaging Conference (NSS/MIC), 2012 IEEE, pp. 610–615. doi:10.1109/NSSMIC.2012.6551180. Google Scholar
Moffat, K., Bilderback, D., Schildkamp, W., Szebenyli, D. & Loane, R. (1986). Structural Biological Applications of X-ray Absorption, Scattering and Diffraction, edited by H. D. Bartunik & B. Chance, pp. 125–133. New York: Academic Press. Google Scholar
Oliéric, V., Ennifar, E., Meents, A., Fleurant, M., Besnard, C., Pattison, P., Schiltz, M., Schulze-Briese, C. & Dumas, P. (2007). Acta Cryst. D63, 759–768. Web of Science CrossRef IUCr Journals Google Scholar
Owen, R. L., Axford, D., Nettleship, J. E., Owens, R. J., Robinson, J. I., Morgan, A. W., Doré, A. S., Lebon, G., Tate, C. G., Fry, E. E., Ren, J., Stuart, D. I. & Evans, G. (2012). Acta Cryst. D68, 810–818. Web of Science CrossRef CAS IUCr Journals Google Scholar
Owen, R. L., Holton, J. M., Schulze-Briese, C. & Garman, E. F. (2009). J. Synchrotron Rad. 16, 143–151. Web of Science CrossRef CAS IUCr Journals Google Scholar
Paithankar, K. S., Owen, R. L. & Garman, E. F. (2009). J. Synchrotron Rad. 16, 152–162. Web of Science CrossRef CAS IUCr Journals Google Scholar
Porta, C., Kotecha, A., Burman, A., Jackson, T., Ren, J., Loureiro, S., Jones, I. M., Fry, E. E., Stuart, D. I. & Charleston, B. (2013). PLoS Pathog. 9, e1003255. Web of Science CrossRef PubMed Google Scholar
Sauter, N. K. & Poon, B. K. (2010). J. Appl. Cryst. 43, 611–616. Web of Science CrossRef CAS IUCr Journals Google Scholar
Sliz, P., Harrison, S. C. & Rosenbaum, G. (2003). Structure, 11, 13–19. Web of Science CrossRef PubMed CAS Google Scholar
Snell, E. H., Bellamy, H. D., Rosenbaum, G. & van der Woerd, M. J. (2007). J. Synchrotron Rad. 14, 109–115. Web of Science CrossRef CAS IUCr Journals Google Scholar
Soliman, A. S. M., Warkentin, M., Apker, B. & Thorne, R. E. (2011). Acta Cryst. D67, 646–656. Web of Science CrossRef CAS IUCr Journals Google Scholar
Southworth-Davies, R. J., Medina, M., Carmichel, I. & Garman, E. (2008). Structure, 12, 1531–1541. Google Scholar
Sutton, K. A., Black, P. J., Mercer, K. R., Garman, E. F., Owen, R. L., Snell, E. H. & Bernhard, W. A. (2013). Acta Cryst. D69, 2381–2394. Web of Science CrossRef CAS IUCr Journals Google Scholar
Sygusch, J. & Allaire, M. (1988). Acta Cryst. A44, 443–448. CrossRef CAS Web of Science IUCr Journals Google Scholar
Walter, T. S. et al. (2005). Acta Cryst. D61, 651–657. Web of Science CrossRef CAS IUCr Journals Google Scholar
Wang, X. et al. (2012). Nature Struct. Mol. Biol. 19, 424–429. Web of Science CrossRef CAS Google Scholar
Warkentin, M., Badeau, R., Hopkins, J. B., Mulichak, A. M., Keefe, L. J. & Thorne, R. E. (2012). Acta Cryst. D68, 124–133. Web of Science CrossRef CAS IUCr Journals Google Scholar
Warkentin, M., Badeau, R., Hopkins, J. & Thorne, R. E. (2011). Acta Cryst. D67, 792–803. Web of Science CrossRef CAS IUCr Journals Google Scholar
Warkentin, M., Hopkins, J. B., Badeau, R., Mulichak, A. M., Keefe, L. J. & Thorne, R. E. (2013). J. Synchrotron Rad. 20, 7–13. 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.