L. M. Gerasimenko

Microcoleus Mats from Alkaliphilic and Halophilic Communities

A detailed description of the macrostructure, the ultrastructure, and the species diversity of alkaliphilic mat from Lake Khilganta (Buryatiya) is presented. The structure of this mat was found to be similar to that of halophilic mats from hypersaline lagoons of Lake Sivash (Crimea) that we studied earlier. Microcoleus chthonoplastes was the dominant form of cyanobacteria in both mats (in the alkaliphilic mat, Phormidium molle was another dominant form). Both mats had a pronounced laminated structure. However, unlike halophilic mats with calcium carbonate and gypsum laminas, the alkaliphilic mat contained calcium phosphate laminas instead of gypsum ones. The species diversity of microorganisms in the alkaliphilic mat was at least as rich as that in the halophilic mat; however, in the halophilic mat, the distribution of organisms between layers was more clear-cut. In the alkaliphilic mat, the highest species diversity was observed in the upper mat layers, at the boundary between zones of oxygenic and anoxygenic photosynthesis. This fact can be explained by the ephemeral nature of soda lakes.

Ecophysiology and polymorphism of the unicellular extremely natronophilic cyanobacterium Euhalothece sp. Z-M001 from Lake Magadi

Strain Z-M001 of a unicellular cyanobacterium, assigned by analysis of the 16S rRNA gene sequence to the phylogenetic group of the generic level Euhalothece, was isolated from soda Lake Magadi. It was shown that strain Z-M001, unlike all other known cultured and uncultured organisms of the Euhalothece group, is extremely natronophilic, and it was named accordingly “Euhalothece natronophila”. In its ecophysiological characteristics, it is comparable to extremely alkaliphilic organotrophic natronobacteria, which is essential for soda ecosystems, because cyanobacteria belong to primary producers. E. natronophila exhibits considerable morphological variability depending on the concentration of carbonates in the medium. The polymorphism of “ E. natronophila” is primarily connected to limitation by utilizable forms of carbon.

Laboratory simulations of cyanobacterial mats of the alkaline geochemical barrier

The goal of this work was to illustrate a possible interaction between the “soda continent” and the ocean. A laboratory simulation was undertaken of the development of alkaliphilic mat with calcium carbonate and calcium phosphate interlayers in the zone where ocean waters, containing calcium and manganese, come into contact with carbonate- and phosphate-rich alkaline waters. The macrostructure of the layered cyanobacterial mat turned out to be little dependent on the chemical conditions causing sediment formation. The chemical composition of freshly formed mineral interlayers of the mat was found to vary with the medium composition. The mineralogical composition of the sediment is determined by diagenesis conditions in its depth, which can cause mineral phase conversions.

Transformation of clay minerals caused by an alkaliphilic cyanobacterial community.

Transformation of clay minerals (smectite-zeolite, illite, kaolinite, and bentonite) and admixtures of iron oxides (hydroxides) under the action of an alkaline cyanobacterial community was studied. The results demonstrate that the processes of transformation of clay minerals such as intensification of removal of exchange bases and dissolution of silicates and iron oxides occurred in the presence of the alkaliphilic cyanobacterial community. The main factor that determines resistance of a mineral to biochemical weathering is its composition. Transformations of clay minerals in the course of active cyanobacterial photosynthesis (up to 14 days) and at decomposition of organic matter (OM) (28–60 days) are different. For smectite-zeolite and illite, these processes are dissolution of silicates and oxides (removal of Si and Fe) and removal of exchange bases (K), which were observed at both the of biomass production and OM destruction stages. For two other clays, the processes of neosynthesis are more typical: formation of carbonates (most probably siderite for bentonite clay and Mg-calcite for kaolin clay) and transformation of ferrihydrite into the more thermodynamically stable goethite.

The role of cyanobacteria in crystallization of magnesium calcites

Laboratory experiments showed the effect of the cyanobacterium Microcoleus chthonoplastes on the formation of magnesium calcites, using model solutions (2.14M MgCl2-0.05M CaCl2-0.6M NaCl-0.18M NaHCO3). The conditions of existence of cyanobacteria in such solutions in light or darkness significantly alter the structure of the sediment and the shape and size of the carbonate crystals. Cyanobacteria slow down crystallization due to the formation of exometabolites with a chelating effect, which leads to the precipitation of high-magnesium calcites. In the photosynthetic environment the presence of huntite (CaMg3(CO3)4), possible forerunner of dolomite, is prominent.

Halophilic algal-bacterial and cyanobacterial communities and their role in carbonate precipitation

This work studies the diversity of cyanobacterial and algal-bacterial communities of saline water bodies in the Crimean Peninsula and Altai Region. Plant-bacterial communities are described for the first time. The dependence of the production and destruction on the season and salinity of the water body is shown. The development of planktonic cyanobacteria is related to the presence of zooplankton, the development of which is controlled by hydrogen sulfide. The high hydrogen sulfide tolerance of benthic cyanobacteria secures the integrity of cyanobacterial communities. Observations in nature and laboratory modeling show that the formation of mineral layers is restricted to conditions of supersaturation with mineral components. Carbonate precipitation can take place in cyanobacterial communities under conditions of mixing sea water enriched with Ca and Mg with continental water enriched with sodium carbonate. Cyanobacteria are able to form and transform various Ca-Mg-carbonates. Dolomite formation is a derived process that occurs in cyanobacterial mats in the presence of sulfate-reducing bacteria. Carbonatization of cyanobacterial cells is considered using the example of the unicellular halophilic-alkaliphilic cyanobacterium Euhalothece sp. The accomplished study is of certain interest for interpretation of geological and paleontological data in the context of the supposed analogy between cyanobacterial mats and ancient stromatolites.

[Transformation of carbonate minerals in a cyano-bacterial mat in the course of laboratory modeling].

A laboratory model of a cyano-bacterial mat with mineral layers of carbonates was used to examine the dynamics of the transformation of calcium-magnesium carbonate under the conditions of a soda lake. The activity of various organisms of the cyanobacterial community results in conditions under which the Ca-Mg carbonate precipitate undergoes changes. The crystal lattice of the initial carbonate is restructured; its mineralogical composition changes depending on the conditions of the mat. In magnesium calcites, which are formed under such low-temperature conditions, a rudimentary cation adjustment can occur with the formation of dolomite domains. These experiments confirm the hypothesis that the dolomite found in stromatolites is of a secondary origin and can be formed in the course of transformation of Ca-Mg carbonates under alkaline conditions in an alkaliphilic cyanobacterial community.

Significance of bacteria in natural and experimental sedimentation of carbonates, phosphates, and silicates

The role of bacteria in sedimentation of phosphorites, siliceous and carbonate rocks is discussed. Preservation of bacterial bodies in fossil condition, even in very ancient deposits, is connected with their very early mineralization. A series of laboratory experiments allowed conditions to be reproduced that could have led to mineralization of cyanobacteria and their preservation in sedimentary deposits. The experiments have also shown the important role of cyanobacteria and their metabolic products in the formation of some carbonate minerals, as well as in the accumulation of stromatolites.

Fossilization of the cells of natronophilic endoevaporite cyanobacterium ‘Euhalothece natronophila’ in a modelling system

Laboratory simulation of fossilization of cyanobacterial cells in the high-carbonate medium in the presence of calcium was carried out for the haloalkaliphilic natronophilic cyanobacterium ‘Euhalothece natronophila’ Z-M001. This organism was isolated from the Magadi soda lake, where the bioherms consisting of mineralized coccoid cyanobacteria were found in the Quaternary sediments. The structural and chemical heterogeneity of the minerals produced during this process was established, with calcium carbonate and trona being the main products. The differences in the process of cyanobacterial cell carbonatization in soda lakes and marine or freshwater systems were determined. Initial precipitation of calcium carbonate was shown to occur due to a chemical reaction not involving cyanobacteria. At the subsequent stages, amorphous CaCO3 is sorbed and crystallized on the surface of some of the cells within a cyanobacterial population, resulting in formation of a shell-like mineral layer. The cells embedded in trona in the same system were shown to undergo deformation and destruction. In both cases the mineralized cells were shown to lose their photosynthetic activity.

Carbonic anhydrase of the alkaliphilic cyanobacterium Microcoleus chthonoplastes

The activity of carbonic anhydrase (CA) was studied in different cell fractions of the alkaliphilic cyanobacterium Microcoleus chthonoplastes. The activity of this enzyme was found in the soluble and membrane protein fractions, as well as in intact cells and in a thick glycocalyx layer enclosing the cyanobacterium cells. The localization of CA in glycocalyx of M. chthonoplastes was shown by western blot analysis and by immunoelectron microscopy studies with antibodies to the thylakoid CA from Chlamydomonas reinhardtii (Cah3). At least one of the CA forms occurring in M. chthonoplastes CA was shown to be an α-type enzyme. A possible mechanism of the involvement of the glycocalyx CA in calcification of cyanobacteria is discussed.