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Over the last decade, breakthroughs, principally in detector technology, but also in other technical fields, have facilitated a succession of substantial increases in the resolution at which biologically relevant systems can be imaged by transmission electron microscopy (TEM)1,2. Despite the fact that cryo-EM already allows the resolution of high-resolution structures from as little as 50 µg of protein through single-particle analysis (SPA), cryo-EM sample and grid preparation remain major bottlenecks3,4,5. SPA samples consist of macromolecules distributed approximately randomly within a layer of vitreous ice. The ice must be as thin as possible to maximize the contrast difference between the particles and the solvent. Biological macromolecules are more stable (i.e., less likely to lose their native structure) in thicker ice, because they remain better solvated. Moreover, particles are often found to be much better distributed over the field of view in ice much thicker than the particle size6 and frequently may not be found within holes in the carbon films at all.
Additionally, thicker layers of ice decrease the probability of molecules being close to the air-water interface due to the high surface-to-volume ratio, and it has been estimated that using standard plunge-freezing methods for cryo-EM studies results in the adsorption of ~90% of particles to the air-water interface7. Thicker ice results in undesirably high background due to increased scattering events within the solvent and concomitant attenuation of the signal6,7. It is therefore necessary to achieve as thin a layer of vitreous ice as possible; ideally, the layer would be only slightly thicker than the particle. The challenge for the researcher, which must be overcome for every different sample applied to a grid, is to prepare specimens thin enough for high-contrast imaging whilst maintaining the structural integrity of the particles within their sample. Protein adsorption to the air-water interface is accompanied by several, usually deleterious, effects.
First, binding of proteins to this hydrophobic interface often induces denaturation of the protein, which proceeds rapidly and is typically irreversible8,9. A study conducted using yeast fatty-acid synthase showed that up to 90% of adsorbed particles are denatured10. Second, evidence from a study comparing the orientation distribution of 80S ribosome datasets collected either on amorphous carbon11 or without support12 showed that the air-water interface can cause severe preferential orientation compromising 3D reconstruction of the volume13. Methods to reduce particle interaction with the air-water interface include supplementation of the freezing buffer with surfactants (such as detergents), the use of support films, affinity-capture or scaffolding of substrates, and accelerated plunging times. The use of surfactants is associated with its own problems, as some protein samples may behave non-ideally in their presence, whilst affinity-capturing and scaffolding substrates generally require engineering bespoke grid surfaces and capture strategies. Finally, although there is a lot of research on the development of rapid-plunging devices14,15,16, these require apparatus that is generally not widely available.
Although the standard TEM grid for biological cryo-EM already features a perforated amorphous carbon foil17, there are a number of protocols available for the generation of additional support films and their transfer to TEM grids. The use of these films is a long-established method for sample stabilization18. Amorphous carbon supports are generated by evaporation and deposition on crystalline mica sheets19, from which the layers can be floated onto grids, with the utility of floatation supports as useful tools established in prior reports20. Graphene oxide flakes, typically prepared using a modified version of the Hummers method21, have been used as a preferable support structure to amorphous carbon for their decreased background signal as well as the ability to immobilize and stabilize macromolecules22. More recently, there has been a resurging interest in the use of graphene as a TEM support film due to its mechanical stability, high conductivity, extremely low contribution to background noise23, as well as the emergence of reproducible methods for generating macroscopically large areas of monolayer graphene24 and transferring it to TEM grids25. When compared to amorphous carbon, which undergoes beam-induced motions similarly to, or worse, than ice lacking a support film11,12,17, graphene showed a significant reduction in beam-induced motion of cryo-EM images12.
However, while hydrophilized graphene protected fatty acid synthase from air-water interfacial denaturation, the authors of this study noted that the graphene became contaminated during specimen preparation, likely due to a combination of atmospheric hydrocarbon contamination and from the reagent used to hydrophilize the grids10. Indeed, despite many of the superior qualities of graphene, its widespread use is still hindered by the derivatization required to decrease its hydrophobicity12, which ultimately is chemically difficult and requires specialist equipment. This paper reports protocols for the preparation of amorphous carbon, graphene oxide, and graphene sample supports using a three dimensionally (3D) printed sample floatation block27 to directly transfer support films from the substrates on which they were generated to TEM grids (Figure 1). A key advantage of using such a device is the wetted transfer of films, minimizing hydrophobic contamination of the supports and consequently the need for further treatment, and reducing the number of potentially damaging manual handling steps. These approaches are inexpensive to implement and therefore widely accessible and applicable for cryo-EM studies where sample supports are necessary.