2016
DOI: 10.1016/j.apgeochem.2016.10.017
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Effects of freshwater Synechococcus sp. cyanobacteria pH buffering on CaCO 3 precipitation: Implications for CO 2 sequestration

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Cited by 14 publications
(14 citation statements)
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“…The growth of a microbialite, incorporating geochemical as well as biologically induced (or influenced) precipitation, requires a continual influx of ambient water into the microenvironment to provide adequate ions for mineral growth (Webb and Kamber, 2011 ). The surface crypts allow the formation of micro-niches (with different oxygen, light and nutrient availability) favorable for the settlement and development of average size bacteria (~2 μm); it is in these micro-sites where diverse metabolic processes mediate or influence mineral precipitations (see physicochemical models in Riding, 1991 , 2000 ; Reid et al, 2000 ; Dupraz and Visscher, 2005 ; Dupraz et al, 2009 ; Martinez et al, 2016 ). Additionally, polymeric biogenic silica has been shown to act as a buffer for carbonic anhydrase in diatoms conducting the CO 2 system to carbonates in the surface of diatoms (Milligan and Morel, 2002 ).…”
Section: Discussionmentioning
confidence: 99%
“…The growth of a microbialite, incorporating geochemical as well as biologically induced (or influenced) precipitation, requires a continual influx of ambient water into the microenvironment to provide adequate ions for mineral growth (Webb and Kamber, 2011 ). The surface crypts allow the formation of micro-niches (with different oxygen, light and nutrient availability) favorable for the settlement and development of average size bacteria (~2 μm); it is in these micro-sites where diverse metabolic processes mediate or influence mineral precipitations (see physicochemical models in Riding, 1991 , 2000 ; Reid et al, 2000 ; Dupraz and Visscher, 2005 ; Dupraz et al, 2009 ; Martinez et al, 2016 ). Additionally, polymeric biogenic silica has been shown to act as a buffer for carbonic anhydrase in diatoms conducting the CO 2 system to carbonates in the surface of diatoms (Milligan and Morel, 2002 ).…”
Section: Discussionmentioning
confidence: 99%
“…Carbon storage methods, or carbon concentration mechanisms (CCM), need to be developed urgently in order to reduce the CO2 impact on Earth's terrestrial and aquatic environments. The ability of cyanobacteria to induce the biomineralization of CO2 is an option which is still in its infancy and could possibly be used in the near-future to decrease atmospheric CO2 levels (Martinez et al, 2016). Previous studies have proven the link between cyanobacteria photosynthesis and the presence of metallic cations could lead to carbonate precipitation in the presence of atmospheric CO2 and under suitable solution conditions (Jansson and Northen, 2010;Martinez et al, 2016;Obst et al, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…Cyanobacteria are autophototrophic microorganisms. They are primary producers, which generate their own nutrients by carrying out the oxygenic photosynthesis (Martinez et al, 2016). This metabolism needs carbon as a source of inorganic carbon in the form of dissolved CO2, natural light as source of energy and water to provide electrons needed in the redox transformation of carbon (Schubert et al, 1997).…”
Section: Introductionmentioning
confidence: 99%
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“…Second, which part of intracellular pH regulation is achieved by the functioning of Ca 2+ /H + exchangers vs other H + transporters in calcifying cyanobacteria? Third, there is still some debate about the way cyanobacteria impact carbonatogenesis: do they induce carbonatogenesis through their metabolic activity as stressed on in the above lines [97,98], or do they influence it through inactive heterogeneous nucleation (e.g. biologically influenced mineralization, see above).…”
mentioning
confidence: 99%