Changes in the cell ultrastructure of the haloalkaliphilic endoevaporite cyanobacterium <Emphasis Type="Italic">‘Euhalothece natronophila’</Emphasis> during fossilization

The ultrastructure of the haloalkaliphilic endoevaporite cyanobacterium ‘Euhalothece natronophila’ Z-M001 from the soda Lake Magadi was investigated during the initial stages of fossilization in a model experimental system. The cyanobacterium was cultivated in concentrated carbonate solution supplemented with calcium chloride. It was revealed that the amorphous CaCO₃ formed under these conditions could interact with the cell wall during the first stages of ‘E. natronophila’ calcification. Evidence is presented that the surface layer of the ‘E. natronophila’ envelope, presumably containing polysaccharide and/or (glyco)protein components, can be involved in the adsorption and subsequent crystallization of CaCO₃ with the formation of a massive “shell” embedding the morphologically intact cells. It was established that the ultrastructure of the cell wall and the intrathylakoid space changed during CaCO₃ mineralization. During the later fossilization stages, cells covered by the calcium-containing “shell” were apparently mummified, and mostly retained their original shape. The encapsulation of cyanobacteria in the trona globule was characterized by a different pattern. It probably involved tight binding of the growing crystal to the glycocalyx components that are anchored in the outer membrane. This may result in its detachment from the underlying peptidoglycan layer. The peptidoglycan was retained, and the protoplasts were ultrastructurally similar to the intact ones. Cyanobacteria incorporated in large trona crystals underwent degradation, deformation, and destruction. This accounts for the fact that massive trona deposits of Lake Magadi lack cyanobacterial fossils that are abundant in calcium-containing strata.