The intracellular accumulation of inorganic carbon (C_i) by microalgae and cyanobacteria under ambient atmospheric CO₂ levels was first documented in the 80s of the 20th Century. Hence, a third variety of the CO₂-concentrating mechanism (CCM), acting in aquatic photoautotrophs with the C₃ photosynthetic pathway, was revealed in addition to the then-known schemes of CCM, functioning in CAM and C₄ higher plants. Despite the low affinity of ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco) of microalgae and cyanobacteria for the CO₂ substrate and low CO₂/O₂ specificity, CCM allows them to perform efficient CO₂ fixation in the reductive pentose phosphate (RPP) cycle. CCM is based on the coordinated operation of strategically located carbonic anhydrases and CO₂/HCO₃⁻ uptake systems. This cooperation enables the intracellular accumulation of HCO₃⁻, which is then employed to generate a high concentration of CO₂ molecules in the vicinity of Rubisco’s active centers compensating up for the shortcomings of enzyme features. CCM functions as an add-on to the RPP cycle while also acting as an important regulatory link in the interaction of dark and light reactions of photosynthesis. This review summarizes recent advances in the study of CCM molecular and cellular organization in microalgae and cyanobacteria, as well as the fundamental principles of its functioning and regulation.

Carbonic anhydrase (CA) is a metalloenzyme that performs interconversion between CO₂ and the bicarbonate ion (HCO₃^–). CAs appear among all taxonomic groups of three domains of life. Wide spreading of CAs in nature is explained by the fact that carbon, which is the major constituent of the enzyme’s substrates, is a key element of life on the Earth. Despite the diversity of CAs, they all carry out the same reaction of СО₂/HCO₃^– interconversion. Thus, CA obviously represents a universal enzyme of the carbon-based life. Within the classification of CAs, here we proposed the existence of an extensive family of CA-related proteins (γCA-RPs) – the inactive forms of γ-CAs, which are widespread among the Archaea, Bacteria, and, to a lesser extent, in Eukarya. This review focuses on the history of CAs discovery and integrates the most recent data on their classification, catalytic mechanisms, and physiological roles at various organisms.

Recent advances in research techniques have enabled rapid progress in the study of spirulina, an ancient edible cyanobacteria. Nowadays, spirulina species are classified into three genera: Spirulina, Arthrospira, and Limnospira. The latter now refers to industrially manufactured spirulina strains. Whole-genome sequencing revealed gene clusters involved in metabolite production, and the physiology of spirulina. Omics technologies demonstrated the absence of hazardous compounds in spirulina cells, confirming the safety of this biomass as a food product. Spirulina is a good source of different chemicals used in food manufacturing, food supplements, and pharmaceuticals. Spirulina’s enrichment with inherent biologically active substances makes it a potential supplier of natural products for dietary and pharmaceutical applications. Spirulina is also a prospective component of both terrestrial and space-based life support systems. Here, we review current breakthroughs in spirulina research and clarify fallacies that can be found in both professional literature and public media.

The bases of modern type biosphere were laid down about two billion years ago during the predominance of prokaryotes on the Earth. Cyanobacteria changed radically the composition of the Proterozoic atmosphere by saturating it with photosynthetic oxygen. At the same time, large quantities of atmospheric CO₂ became sequestered in carbonates owing to mineralization of ancient cyano-bacterial communities; the latter have reached us in the form of laminated limestone deposits, termed stromatolites. The mechanism of carbonate depositing by cyanobacteria is still poorly understood. It is not yet clear whether physiological processes are involved in cell mineralization or if the outer membranes of cyanobacteria serve as a kind of crystallization center and arrange the structure for natural accumulation of sediments. We proposed that a key role in the mechanism of biomineralization belongs to the enzyme carbonic anhydrase (CA), which regulates the equilibrium between the inorganic carbon forms (C_i), including bicarbonate that participates in natural sedimentation of calcium. Since the deposition of calcium carbonate by prokaryotes occurs in the pericellular space and this deposition is controlled by pH, it seems likely that CA, localized on the periphery of cyanobacterial cells, is involved in stabilizing the external pH and in promoting cell mineralization. This review summarizes information concerning possible mechanisms of biogenic calcification (CaCO₃ deposition). The function of CA in the living cell and the role of this enzyme in biological processes are considered, and the data on localization of CA in cyano-bacterial cells are presented. Based on available evidence, a scheme is suggested to describe the role of extracellular CA in photosynthetic carbon assimilation and to relate this process with CaCO₃ deposition during mineralization of cyanobacteria.