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Carboxysomes are closed polyhedral cellular microcompartments that increase the efficiency of carbon fixation in autotrophic bacteria. Carboxysome shells consist of small proteins that form hexameric units with semi-permeable central pores containing binding sites for anions. This feature is thought to selectively allow access to RuBisCO enzymes inside the carboxysome by(the dominant form of CO2in the aqueous solution at pH 7.4) but not O2, which leads to a non-productive reaction. To test this hypothesis, here we use molecular dynamics simulations to characterize the energetics and permeability of CO2, O2, andthrough the central pores of two different shell proteins, namely, CsoS1A of α–carboxysome and CcmK4 of β-carboxysome shells. We find that the central pores are in fact selectively permeable to anions such as, as predicted by the model.

Following decades of research in genetics and biochemistry, the basic metabolism of bacteria is now well understood. In addition to core metabolism, however, bacterial cells also perform a number of mechanical tasks such as maintaining a characteristic shape, moving within their environment, segregating their genome, and dividing. Major advances in imaging technologies including fluorescence light microscopy (fLM) and electron cryotomography (ECT) have provided new insight into the bacterial ultrastructures that accomplish these tasks. It is now clear, for instance, that bacteria are highly organized, possessing cytoskeletons, specifically arranged genomes, internal compartments, and carefully positioned macromolecular machines. These structures and their functions are reviewed here in the form of a progress report toward a complete biomechanical understanding of a generalized bacterial cell. The goal of eventually integrating genetic, biochemical, imaging, and biophysical data into spatially explicit, mechanically predictive models of whole cells is highlighted.

Using electron cryotomography, we show that the Gram-negative sporulating bacterium Acetonema longum synthesizes high-density storage granules at the leading edges of engulfing membranes. The granules appear in the prespore and increase in size and number as engulfment proceeds. Typically, a cluster of 8 to 12 storage granules closely associates with the inner spore membrane and ultimately accounts for ∼7% of the total volume in mature spores. Energy-dispersive X-ray spectroscopy (EDX) analyses show that the granules contain high levels of phosphorus, oxygen, and magnesium and therefore are likely composed of polyphosphate (poly-P). Unlike the Gram-positive Bacilli and Clostridia, A. longum spores retain their outer spore membrane upon germination. To explore the possibility that the granules in A. longum may be involved in this unique process, we imaged purified Bacillus cereus, Bacillus thuringiensis, Bacillus subtilis, and Clostridium sporogenes spores. Even though B. cereus and B. thuringiensis contain the ppk and ppx genes, none of the spores from Gram-positive bacteria had granules. We speculate that poly-P in A. longum may provide either the energy or phosphate metabolites needed for outgrowth while retaining an outer membrane.

Carboxysome provides an efficient mechanism for cyanobacteria and chemoautotrophs to fix carbon dioxide (CO_2) and organic metabolites into building blocks of biomolecules. It is a polyhedral body that encapsulates ribulose-1,5-bisphosphate carboxylase/oxygenase (RuBisCO), an enzyme that carries out the CO_2 fixation and meanwhile competitively reacts with O_2. Its outer surface is coated by the assembly of thousands of small shell proteins. Many of these shell proteins form oligomeric structures with a semi-permeable 2-3A radius central pore, suggesting a favorable feature for the binding of anions such as bicarbonate (HCO_3-), the aqueous soluble form of CO_2. The present study examines the translocation HCO_3-, CO_2 and O_2 through the central pores of different isoforms of shell protein complexes from alpha and beta cyanobacteria. We employed umbrella sampling simulations to calculate partitioning free energy profiles of these small molecules and performed detailed electrostatic analysis of the structures. The results demonstrate that carboxysome shell protein oligomers share a unique feature in that their central pores are preferably selective for HCO_3- over hydrophobic CO_2 and O_2 gases. The pores are found to be hydrated and are electropositive, thus favoring HCO_3- and Cl- anions. Hence, as the carboxysome encapsulates carbonic anhydrase enzymes which dehydrates HCO_3- to CO_2, the preferential uptake of HCO_3-(instead of CO_2) into the carboxysomal lumen from the cytoplasm is an intrinsic way to minimize the reaction between O_2 and the RuBisCO and to increase the concentration of CO_2 around the RuBisCO. The results also provide insight into the assembled orientations of the shell proteins, which is necessary for solving a full atomic model of the carboxysome.

SummaryTwo hallmarks of the Firmicute phylum, which includes the Bacilli and Clostridia classes, are their ability to form endospores and their “Gram-positive” single-membraned, thick-cell-wall envelope structure. Acetonema longum is part of a lesser-known family (the Veillonellaceae) of Clostridia that form endospores but that are surprisingly “Gram negative,” possessing both an inner and outer membrane and a thin cell wall. Here, we present macromolecular resolution, 3D electron cryotomographic images of vegetative, sporulating, and germinating A. longum cells showing that during the sporulation process, the inner membrane of the mother cell is inverted and transformed to become the outer membrane of the germinating cell. Peptidoglycan persists throughout, leading to a revised, “continuous” model of its role in the process. Coupled with genomic analyses, these results point to sporulation as a mechanism by which the bacterial outer membrane may have arisen and A. longum as a potential “missing link” between single- and double-membraned bacteria.

While much is already known about the basic metabolism of bacterial cells, many fundamental questions are still surprisingly unanswered, including for instance how they generate and maintain specific cell shapes, establish polarity, segregate their genomes, and divide. In order to understand these phenomena, imaging technologies are needed that bridge the resolution gap between fluorescence light microscopy and higher-resolution methods such as X-ray crystallography and NMR spectroscopy. Electron cryotomography (ECT) is an emerging technology that does just this, allowing the ultrastructure of cells to be visualized in a near-native state, in three dimensions (3D), with macromolecular resolution (approximately 4nm).(1, 2) In ECT, cells are imaged in a vitreous, frozen-hydrated state in a cryo transmission electron microscope (cryoTEM) at low temperature (< -180 degrees C). For slender cells (up to approximately 500 nm in thickness(3)), intact cells are plunge-frozen within media across EM grids in cryogens such as ethane or ethane/propane mixtures. Thicker cells and biofilms can also be imaged in a vitreous state by first high-pressure freezing and then, cryo-sectioning them. A series of two-dimensional projection images are then collected through the sample as it is incrementally tilted along one or two axes. A three-dimensional reconstruction, or tomogram can then be calculated from the images. While ECT requires expensive instrumentation, in recent years, it has been used in a few labs to reveal the structures of various external appendages, the structures of different cell envelopes, the positions and structures of cytoskeletal filaments, and the locations and architectures of large macromolecular assemblies such as flagellar motors, internal compartments and chemoreceptor arrays.(1, 2) In this video article we illustrate how to image cells with ECT, including the processes of sample preparation, data collection, tomogram reconstruction, and interpretation of the results through segmentation and in some cases correlation with light microscopy.

Carboxysomes are polyhedral inclusion bodies that play a key role in autotrophic metabolism in many bacteria. Using electron cryotomography, we examined carboxysomes in their native states within intact cells of three chemolithoautotrophic bacteria. We found that carboxysomes generally cluster into distinct groups within the cytoplasm, often in the immediate vicinity of polyphosphate granules, and a regular lattice of density frequently connects granules to nearby carboxysomes. Small granular bodies were also seen within carboxysomes. These observations suggest a functional relationship between carboxysomes and polyphosphate granules. Carboxysomes exhibited greater size, shape, and compositional variability in cells than in purified preparations. Finally, we observed carboxysomes in various stages of assembly, as well as filamentous structures that we attribute to misassembled shell protein. Surprisingly, no more than one partial carboxysome was ever observed per cell. Based on these observations, we propose a model for carboxysome assembly in which the shell and the internal RuBisCO (ribulose-1,5-bisphosphate carboxylase/oxygenase) lattice form simultaneously, likely guided by specific interactions between shell proteins and RuBisCOs.

Carboxysomes are organelle-like polyhedral bodies found in cyanobacteria and many chemoautotrophic bacteria that are thought to facilitate carbon fixation. Carboxysomes are bounded by a proteinaceous outer shell and filled with ribulose 1,5-bisphosphate carboxylase/oxygenase (RuBisCO), the first enzyme in the CO(2) fixation pathway, but exactly how they enhance carbon fixation is unclear. Here we report the three-dimensional structure of purified carboxysomes from Synechococcus species strain WH8102 as revealed by electron cryotomography. We found that while the sizes of individual carboxysomes in this organism varied from 114 nm to 137 nm, surprisingly, all were approximately icosahedral. There were on average approximately 250 RuBisCOs per carboxysome, organized into three to four concentric layers. Some models of carboxysome function depend on specific contacts between individual RuBisCOs and the shell, but no evidence of such contacts was found: no systematic patterns of connecting densities or RuBisCO positions against the shell's presumed hexagonal lattice could be discerned, and simulations showed that packing forces alone could account for the layered organization of RuBisCOs.