Anderson S, Appanna V D, Huang J, Viswanatha T
Department of Chemistry and Biochemistry, Laurentian University, Sudbury, Ont., Canada.
FEBS Lett. 1992 Aug 10;308(1):94-6. doi: 10.1016/0014-5793(92)81059-u.
Calcium carbonate (CaCO3) minerals are known to be deposited in a wide array of different organisms, ranging from microbes to vertebrates [(1989) On Biomineralization, Oxford University Press, New York]. Calcite, aragonite and vaterite are the major crystalline structural polymorphs of CaCO3 associated with living systems, and participate in a variety of biological functions [(1989) Biomineralization: Chemical and Biochemical Perspectives, VCH Publishers, Weinham, Germany; (1991) Advances in Inorganic Chemistry 36, 137-200]. Here we report on the ability of a soil bacterium to synthesize calcite in a calcium-stressed environment. The elaboration of this exocellular crystalline residue enables the organism to regulate its calcium content. The attainment of calcium homeostasis via the exocellular deposition of bacterial calcite with unique crystal habits is a novel biological phenomenon.
碳酸钙(CaCO₃)矿物质已知会在从微生物到脊椎动物等各种各样的不同生物体中沉积[(1989年)《生物矿化》,牛津大学出版社,纽约]。方解石、文石和球霰石是与生命系统相关的CaCO₃的主要晶体结构多晶型物,并参与多种生物学功能[(1989年)《生物矿化:化学和生物化学视角》,VCH出版社,德国魏因海姆;(1991年)《无机化学进展》36,137 - 200]。在此我们报告一种土壤细菌在钙胁迫环境中合成方解石的能力。这种细胞外晶体残留物的形成使该生物体能够调节其钙含量。通过具有独特晶体习性的细菌方解石的细胞外沉积实现钙稳态是一种新的生物学现象。