Lee Brady D, Apel William A, Walton Michelle R
Biotechnology Department, Idaho National Engineering and Environmental Laboratory, PO Box 1625, Idaho Falls, Idaho, USA.
Biotechnol Prog. 2004 Sep-Oct;20(5):1345-51. doi: 10.1021/bp0343561.
Species of cyanobacteria in the genera Synechococcus and Synechocystis are known to be the catalysts of a phenomenon called "whitings", which is the formation and precipitation of fine-grained CaCO3 particles. Whitings occur when the cyanobacteria fix atmospheric CO2 through the formation of CaCO3 on their cell surfaces, which leads to precipitation to the ocean floor and subsequent entombment in mud. Whitings represent one potential mechanism for CO2 sequestration. Research was performed to determine the ability of various strains of Synechocystis and Synechococcus to calcify when grown in microcosms amended with 2.5 mM HCO(3-) and 3.4 mM Ca2+. Results indicated that although all strains tested have the ability to calcify, only two Synechococcus species, strains PCC 8806 and PCC 8807, were able to calcify to the extent that a CaCO3 precipitate was formed. Enumeration of the cyanobacterial cultures during testing indicated that cell density did not appear to have a direct effect on calcification. Factors that had the greatest effect on calcification were CO2 removal and subsequent generation of alkaline pH. Whereas cell density was similar for all strains tested, differences in maximum pH were demonstrated. As CO2 was removed, growth medium pH increased and soluble Ca2+ was removed from solution. The largest increases in growth medium pH occurred when CO2 levels dropped below 400 ppmv. Research presented demonstrates that, under the conditions tested, many species of cyanobacteria in the genera Synechocystis and Synechococcus are able to calcify but only two species of Synechococcus were able to calcify to an extent that led to the precipitation of calcium carbonate.
已知聚球藻属和集胞藻属中的蓝藻物种是一种名为“白化现象”的催化剂,“白化现象”是细粒碳酸钙颗粒的形成和沉淀过程。当蓝藻通过在其细胞表面形成碳酸钙来固定大气中的二氧化碳时,就会发生白化现象,这会导致沉淀到海底并随后被埋入泥中。白化现象是二氧化碳封存的一种潜在机制。开展了相关研究,以确定集胞藻属和聚球藻属的各种菌株在添加了2.5 mM HCO₃⁻和3.4 mM Ca²⁺的微观环境中生长时的钙化能力。结果表明,尽管所有测试菌株都有钙化能力,但只有两种聚球藻物种,即菌株PCC 8806和PCC 8807,能够钙化到形成碳酸钙沉淀的程度。测试期间对蓝藻培养物的计数表明,细胞密度似乎对钙化没有直接影响。对钙化影响最大的因素是二氧化碳的去除以及随后产生的碱性pH值。尽管所有测试菌株的细胞密度相似,但最大pH值存在差异。随着二氧化碳被去除,生长培养基的pH值升高,可溶性Ca²⁺从溶液中被去除。当二氧化碳水平降至400 ppmv以下时,生长培养基的pH值升高幅度最大。所呈现的研究表明,在测试条件下,集胞藻属和聚球藻属中的许多蓝藻物种都能够钙化,但只有两种聚球藻物种能够钙化到导致碳酸钙沉淀的程度。