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Cyanobacterial formation of intracellular Ca‐carbonates in undersaturated solutions
Author(s) -
Cam N.,
Benzerara K.,
Georgelin T.,
Jaber M.,
Lambert J.F.,
Poinsot M.,
SkouriPanet F.,
Moreira D.,
LópezGarcía P.,
Raimbault E.,
Cordier L.,
Jézéquel D.
Publication year - 2018
Publication title -
geobiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.859
H-Index - 72
eISSN - 1472-4669
pISSN - 1472-4677
DOI - 10.1111/gbi.12261
Subject(s) - biomineralization , extracellular , cyanobacteria , intracellular , extracellular polymeric substance , carbonate , calcium carbonate , chemistry , biophysics , biology , biochemistry , biofilm , bacteria , paleontology , genetics , organic chemistry
Cyanobacteria have long been thought to induce the formation of Ca‐carbonates as secondary by‐products of their metabolic activity, by shifting the chemical composition of their extracellular environment to conditions favoring mineral precipitation. Some cyanobacterial species forming Ca‐carbonates intracellularly were recently discovered. However, the environmental conditions under which this intracellular biomineralization process can occur and the impact of cyanobacterial species forming Ca‐carbonates intracellularly on extracellular carbonatogenesis are not known. Here, we show that these cyanobacteria can form Ca‐carbonates intracellularly while growing in extracellular solutions undersaturated with respect to all Ca‐carbonate phases, that is, conditions thermodynamically unfavorable to mineral precipitation. This shows that intracellular Ca‐carbonate biomineralization is an active process; that is, it costs energy provided by the cells. The cost of energy may be due to the active accumulation of Ca intracellularly. Moreover, unlike cyanobacterial strains that have been usually considered before by studies on Ca‐carbonate biomineralization, cyanobacteria forming intracellular carbonates may slow down or hamper extracellular carbonatogenesis, by decreasing the saturation index of their extracellular solution following the buffering of the concentration of extracellular calcium to low levels.

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