文石
碳酸盐
碳酸钙
无定形碳酸钙
生物矿化
化学
碱度
蓝藻
溶解
生物物理学
方解石
矿物学
生物
生物化学
细菌
天体生物学
有机化学
遗传学
作者
Hengchao Xu,Xiaotong Peng,Shijie Bai,Kaiwen Ta,Shouye Yang,Shuangquan Liu,Ho Bin Jang,Zixiao Guo
摘要
Abstract. Viruses have been acknowledged as important components of the marine system for the past two decades, but the understanding of their role in the functioning of the geochemical cycle remains poor. Viral induced rupturing of cyanobacteria are theoretically capable of releasing intracellular bicarbonate and inducing the homogeneous nucleation of calcium carbonate, but experimental-based support for viral induced calcification is lacking. In this laboratory study, both water carbonate chemistry and precipitates were monitored during the cyanophage infection and lysis of host cells. Our results show that viral lysis of cyanobacteria can influence the carbonate equilibrium system remarkably and promotes the nucleation and stabilization of carbonate minerals. Amorphous calcium carbonate (ACC) and aragonite were evident in the lysate compared to the brucite precipitate in non-infection cultures implying that a different precipitation process had occurred. Based on the carbonate chemistry change and microstructure of the precipitation, the viral induced calcification may initiate by rapid intracellular calcification because of the unfettered intracellular access of Ca2+ and react with cytoplasmic alkalinity after the virus attacks and breaks down the cell wall. The experimental results raised here first demonstrate the pathway and result regarding how viruses influence the mineralization of carbonate minerals. Furthermore, our results also imply that viruses play a crucial role in seawater carbonate chemistry and may balance the geochemical element budget within the earth system.
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