Producing desired ice faces

The ability to prepare single-crystal faces has become central to developing and testing models for chemistry at interfaces, spectacularly demonstrated by heterogeneous catalysis and nanoscience. This ability has been hampered for hexagonal ice, I_h––a fundamental hydrogen-bonded surface––due to two characteristics of ice: ice does not readily cleave along a crystal lattice plane and properties of ice grown on a substrate can differ significantly from those of neat ice. This work describes laboratory-based methods both to determine the I_h crystal lattice orientation relative to a surface and to use that orientation to prepare any desired face. The work builds on previous results attaining nearly 100% yield of high-quality, single-crystal boules. With these methods, researchers can prepare authentic, single-crystal ice surfaces for numerous studies including uptake measurements, surface reactivity, and catalytic activity of this ubiquitous, fundamental solid.Studies of model, single-crystal surfaces have revolutionized understanding of a vast array of heterogeneous catalysts and nanoparticles ranging from pure metals to alloys to semiconductors. Applying the single-crystal surface strategy to ice––arguably one of the most fundamental and ubiquitous hydrogen-bonded interfaces––has been limited due to challenges associated with surface generation. As a result, questions about molecular-level dynamics, surface binding site patterns, and the molecular-level structure remain unanswered (1). Several strategies have been adopted for studying ice: (i) Depositing solid water on a metal or ionic substrate that matches the oxygen lattice (2, 3). However, ice on a substrate often has distinctly different properties from those of neat ice; indeed, such ice can even be hydrophobic (4, 5)! (ii) Uptake measurements often use a Knudsen cell with vapor-deposited ice on a substrate (6) or compacted, finely divided, artificial snow (7) to arrive at a molecular-level picture for gas–particle interaction despite the irregular, highly variable surfaces used. (iii) Small crystallites can be well characterized but, as highlighted by Libbrecht and Rickerby (8), results can be clouded by competition from nearby crystallites; small faces compete with adjacent faces. In addition, crystallites are perturbed by the supporting surface. It is therefore desirable to prepare macroscopic samples with known faces.Interactions at ice surfaces have a particularly profound effect on climate. For example, correlational studies suggest that rain formation depends on ice particles in clouds (9), but not all ice-containing clouds yield rain. It is thought that variation in supersaturation and the mechanism for gathering water molecules by ice particles profoundly affects precipitation. Discrepancies between experiment and theory are often rationalized as a result of irregular shapes, inelastic scattering, or differing binding sites leaving large uncertainties for climate models (10). More reproducible, well-characterized surfaces of I_h––the most stable form of ice at ambient pressure––are needed to bring clarity.Ice is unusual in that the macroscopic sample does not reveal the crystal lattice orientation. Neighboring grain lattice orientation is a critical issue in the ice-core and glaciology communities (11). Hence, previous work (12–14) focused on determining grain orientation with respect to the grain boundary. The most quantitative of these are the two methods of Matsuda (12). The first uses etch pits measuring lengths inside the pit. Large uncertainties in length measurements result in large uncertainties in lattice axis orientation angles; this is not a major issue for grain growth studies but is a serious problem for generating targeted faces. The second method measures only the azimuths, thus incompletely determining orientation. Both methods break down if the optic axis is near-parallel to the surface, and neither provides the tools required to accurately orient a macroscopic sample to generate a targeted face. Lattice orientation could be determined with X-ray methods (15, 16) provided such determination includes a connection to the macroscopic sample. For wide-spread use, a laboratory-based method is preferable. This work describes two methods to fill this important need. The first uses pit perimeter ratio measurements; because the perimeter is sharp, accuracy is greatly improved. The second method locates the optic axis via cross-polarizers (11, 17), then precisely determines the hexagonal orientation via etching. Closed-form, analytical formulas are derived relating lattice orientation to the macroscopic sample. These orientation formulas feed into rotation matrices generating additional analytical formulas enabling precise cutting of any targeted face. The result is illustrated by cutting each of the three major ice faces. These techniques provide researchers with the tools needed to prepare neat ice surfaces.This work specifically describes face preparation from cylindrical boules (18); however, the method is easily adapted to any macroscopic, single-crystal geometry. Due to nearly equal energy faces, ice takes on the shape of the confining container. The near-energy match is demonstrated by growth in the modified Bridgeman apparatus (19). Nucleation occurs on a polycrystalline seed; single-crystal growth is achieved due to competitive growth among the multiple ice–water interfaces (18). Careful thermal management maintains near-equilibrium conditions yielding a large single crystal, but the crystal orientation is not a priori known. [Note: ice seeded by a floating crystal tends to have the optic axis perpendicular to the growth direction but single-crystal yield is low, ~10% (20).] Close energy match among the faces also means that ice does not readily cleave along any lattice plane (21). Thus, successful face preparation for any ice sample begins with characterization of the lattice orientation.     

Local and global structural drivers for the photoactivation of the orange carotenoid protein

Photoprotective mechanisms are of fundamental importance for the survival of photosynthetic organisms. In cyanobacteria, the orange carotenoid protein (OCP), when activated by intense blue light, binds to the light-harvesting antenna and triggers the dissipation of excess captured light energy. Using a combination of small angle X-ray scattering (SAXS), X-ray hydroxyl radical footprinting, circular dichroism, and H/D exchange mass spectrometry, we identified both the local and global structural changes in the OCP upon photoactivation. SAXS and H/D exchange data showed that global tertiary structural changes, including complete domain dissociation, occur upon photoactivation, but with alteration of secondary structure confined to only the N terminus of the OCP. Microsecond radiolytic labeling identified rearrangement of the H-bonding network associated with conserved residues and structural water molecules. Collectively, these data provide experimental evidence for an ensemble of local and global structural changes, upon activation of the OCP, that are essential for photoprotection.Photosynthetic organisms have evolved a protective mechanism known as nonphotochemical quenching (NPQ) to dissipate excess energy, thereby preventing oxidative damage under high light conditions (1). In plants and algae, NPQ involves pH-induced conformation changes in membrane-embedded protein complexes and enzymatic interconversion of carotenoids (2, 3). Cyanobacteria, in contrast, use a relatively simple NPQ mechanism governed by the water soluble orange carotenoid protein (OCP). The OCP is composed of an all α-helical N-terminal domain (NTD) consisting of two discontinuous four-helix bundles and a mixed α/β C-terminal domain (CTD), which is a member of the widely distributed nuclear transport factor 2-like superfamily (Fig. S1A) (4, 5). There are two regions of interaction between the NTD and CTD (4, 5): the major interface, which buries 1,722 Å of surface area, and the interaction between the N-terminal alpha-helix (αA) and the CTD (minor interface) (Fig. S1A). A single noncovalently bound keto-carotenoid [e.g., echinenone (ECN)] spans both domains in the structure of the resting (inactive) form of the protein (OCP^O).Open in a separate windowFig. S1.Structure of the OCP. (A) Crystal structure of Synechocystis OCP (PDB ID code 3MG1) consisting of two domains, NTD and CTD as described in the main text introduction, which form major and minor interfaces. (B) Amino acid residues within 3.9 Å of the carotenoid are shown by sticks. (C) Surface-bound water molecules at the major interface are shown in slate-colored spheres in Synechocystis OCP (PDB ID code 3MG1). This layer of water molecules fully or partially eclipses other water molecules, which are either conserved or found to be at the same location (within 0.5 Å) in the crystal structures of A. maxima and Synechocystis OCP (Fig. 4 A and B. Removal of the slate-colored spheres, exposing partially buried water, is shown in orange in D. The fully buried waters (red spheres) are invisible in the surface diagram of OCP. (E) Cross-sectional view to show the position of fully and partially buried structural waters in OCP^O. (F) Details of water–protein H-bonding network in water cluster 1 at the major interface. The absolutely conserved R155 is closely surrounded (<3.2 Å, capable of forming H-bond) by a number of buried (HOH1151,1200, and 1671) water molecules, which are involved in dense residue-water interactions as discussed in the main text. Similar H-bonding networks are also observed in the water clusters 2 and 3 (6). Exposure to blue light converts OCP^O to the active (red) form, OCP^R (7). OCP^R is involved in protein–protein interactions with the phycobilisome (PB) (5) and the fluorescence recovery protein (FRP), which converts OCP^R back to OCP^O (8). The OCP^R form is therefore central to the photoprotective mechanism, and determining the exact structural changes that accompany its formation are critical for a complete mechanistic understanding of the reversible quenching process in cyanobacteria. Although crystal structures exist of both the (inactive) OCP^O (4, 5) and the active NTD (effector domain) form of the protein (9), crystallization of the activated, full-length OCP^R has not been achieved. To identify the protein structural changes that occur after absorption of light by the OCP’s ECN chromophore, we undertook a hybrid approach to structurally characterize OCP^R in solution.In Synechocystis OCP^O, the 4-keto group on the “β1” ring of ECN is H-bonded to two conserved residues, Y201 and W288, in a hydrophobic pocket in the core of the CTD (Fig. S1B) (5). The other end of the carotenoid is positioned between the two four-helix bundles of the NTD. Several conserved residues within 3.9 Å of the carotenoid are known to interact with its extensive conjugation and result in fine tuning of the spectral characteristics of the OCP (Fig. S1B) (4, 5); these residues have been implicated in photochemical function via mutagenesis studies (5). A recent study of the OCP bound to the carotenoid canthaxanthin (OCP-CAN) showed that photoactivation of the OCP results in a substantial translocation (12 Å) of the carotenoid deeper into the NTD (9). Mutational analyses of the full-length OCP and biochemical studies on the constitutively active NTD [commonly known as the red carotenoid protein (RCP)] suggested that the NTD and CTD at least partially separate, resulting in the breakage of an interdomain salt-bridge (R155–E244) upon photoactivation (9–12). Together, the previous studies suggest that large-scale protein structural changes in the OCP accompany carotenoid translocation upon light activation; however, such changes in the context of the full-length protein have yet to be experimentally demonstrated. Here, we report use of X-ray radiolytic labeling with mass spectrometry (XF-MS) and hydrogen/deuterium exchange with mass spectrometry (HDX-MS), which detect residue-specific changes (13–15), to investigate the structural changes that occur during OCP photoactivation. In conjunction with small angle X-ray scattering (SAXS), which enables characterization of global conformational changes in the solution state (16), we show that dissociation of the NTD and CTD is complete in photoactivated OCP. This separation is accompanied by an unfolding of the N-terminal α-helix that is associated with the CTD in the resting state. We also pinpoint changes in specific amino acids and structurally conserved water molecules, providing insight into the signal propagation pathway from carotenoid to protein surface upon photoactivation. Collectively, these data provide a comprehensive view of both global and local intraprotein structural changes in the OCP upon photoactivation that are essential to a mechanistic understanding of cyanobacterial NPQ.     

From the Cover: PNAS Plus: The essential gene set of a photosynthetic organism

Synechococcus elongatus PCC 7942 is a model organism used for studying photosynthesis and the circadian clock, and it is being developed for the production of fuel, industrial chemicals, and pharmaceuticals. To identify a comprehensive set of genes and intergenic regions that impacts fitness in S. elongatus, we created a pooled library of ∼250,000 transposon mutants and used sequencing to identify the insertion locations. By analyzing the distribution and survival of these mutants, we identified 718 of the organism’s 2,723 genes as essential for survival under laboratory conditions. The validity of the essential gene set is supported by its tight overlap with well-conserved genes and its enrichment for core biological processes. The differences noted between our dataset and these predictors of essentiality, however, have led to surprising biological insights. One such finding is that genes in a large portion of the TCA cycle are dispensable, suggesting that S. elongatus does not require a cyclic TCA process. Furthermore, the density of the transposon mutant library enabled individual and global statements about the essentiality of noncoding RNAs, regulatory elements, and other intergenic regions. In this way, a group I intron located in tRNA^Leu, which has been used extensively for phylogenetic studies, was shown here to be essential for the survival of S. elongatus. Our survey of essentiality for every locus in the S. elongatus genome serves as a powerful resource for understanding the organism’s physiology and defines the essential gene set required for the growth of a photosynthetic organism.Determining the sets of genes necessary for survival of diverse organisms has helped to identify the fundamental processes that sustain life across an array of environments (1). This research has also served as the starting point for efforts by synthetic biologists to design organisms from scratch (2, 3). Despite the importance of essential gene sets, they have traditionally been challenging to gather because of the difficulty of observing mutations that result in lethal phenotypes. More recently, the pairing of transposon mutagenesis with next generation sequencing, referred to collectively as transposon sequencing (Tn-seq), has resulted in a dramatic advance in the identification of essential gene sets (4–7). The key characteristic of Tn-seq is the use of high-throughput sequencing to screen for the fitness of every transposon mutant in a pooled population to measure each mutation’s impact on survival. These data can be used to quantitatively ascertain the effect of loss-of-function mutations at any given locus, intragenic or intergenic, in the conditions under which the library is grown (8). Essential gene sets for 42 diverse organisms distributed across all three domains have now been defined, largely through the use of Tn-seq (9). A recently developed variation on Tn-seq, random barcode transposon site sequencing (RB-TnSeq) (10), further minimizes the library preparation and sequencing costs of whole-genome mutant screens.Despite the proliferation of genome-wide essentiality screens, a complete essential gene set has yet to be defined for a photosynthetic organism. A collection of phenotyped Arabidopsis thaliana mutants has been created but extends to only one-tenth of Arabidopsis genes (11). In algae, efforts are underway to produce a Tn-seq–like system in Chlamydomonas reinhardtii; however, the mutant library currently lacks sufficient saturation to determine gene essentiality (12). To date, the essential genes for photoautotrophs have only been estimated by indirect means, such as by comparative genomics (13). The absence of experimentally determined essential gene sets in photosynthetic organisms, despite their importance to the environment and industrial production, is largely because of the difficulty and time required for genetic modification of these organisms.Cyanobacteria comprise an extensively studied and ecologically important photosynthetic phylum. They are responsible for a large portion of marine primary production and have played a foundational role in research to decipher the molecular components of photosynthesis (14, 15). Synechococcus elongatus PCC 7942 is a particularly well-studied member of this phylum because of its genetic tractability and streamlined genome (16). As a result, it has been developed as a model photosynthetic organism and a production platform for a number of fuel products and high-value chemicals (17). Despite the importance of S. elongatus for understanding photosynthesis and industrial production, 40% of its genes have no functional annotation, and only a small portion of those that do have been studied experimentally.Here, we use RB-TnSeq, a method that pairs high-density transposon mutagenesis and pooled mutant screens, to probe the S. elongatus genome for essential genes and noncoding regions. We categorized 96% of 2,723 genes in S. elongatus as either essential (lethal when mutated), beneficial (growth defect when mutated), or nonessential (no phenotype when mutated) under standard laboratory conditions. Furthermore, we determined the genome-wide essentiality of noncoding RNAs (ncRNAs), regulatory regions, and intergenic regions. Our investigation has produced an extensive analysis of the loci essential for the growth of a photosynthetic organism and developed a powerful genomic tool that can be used for additional screens under a wide array of ecologically and industrially relevant growth conditions.