Haddad Mathieu, Vali Hojatollah, Paquette Jeanne, Guiot Serge R
Energy, Mining and Environment Portfolio, National Research Council Canada, Montreal, Quebec, Canada ; Department of Microbiology, Infectiology and Immunology, Université de Montréal, Montreal, Quebec, Canada.
Department of Earth and Planetary Sciences, McGill University, Montreal, Quebec, Canada ; Facility for Electron Microscopy Research, McGill University, Montreal, Quebec, Canada.
PLoS One. 2014 Feb 26;9(2):e89480. doi: 10.1371/journal.pone.0089480. eCollection 2014.
Two previously unknown modes of biomineralization observed in the presence of Carboxydothermus hydrogenoformans are presented. Following the addition of NaHCO3 and the formation of an amorphous calcium phosphate precipitate in a DSMZ medium inoculated with C. hydrogenoformans, two distinct crystalline solids were recovered after 15 and 30 days of incubation. The first of these solids occurred as micrometric clusters of blocky, angular crystals, which were associated with bacterial biofilm. The second solid occurred as 30-50 nm nanorods that were found scattered among the organic products of bacterial lysis. The biphasic mixture of solids was clearly dominated by the first phase. The X-ray diffractometry (XRD) peaks and Fourier transform infrared spectroscopy (FTIR) spectrum of this biphasic material consistently showed features characteristic of Mg-whitlockite. No organic content or protein could be identified by dissolving the solids. In both cases, the mode of biomineralization appears to be biologically induced rather than biologically controlled. Since Mg is known to be a strong inhibitor of the nucleation and growth of CaP, C. hydrogenoformans may act by providing sites that chelate Mg or form complexes with it, thus decreasing its activity as nucleation and crystal growth inhibitor. The synthesis of whitlockite and nano-HAP-like material by C. hydrogenoformans demonstrates the versatility of this organism also known for its ability to perform the water-gas shift reaction, and may have applications in bacterially mediated synthesis of CaP materials, as an environmentally friendly alternative process.
本文介绍了在嗜氢羧基热杆菌存在下观察到的两种前所未知的生物矿化模式。在向接种了嗜氢羧基热杆菌的DSMZ培养基中添加NaHCO₃并形成无定形磷酸钙沉淀后,经过15天和30天的培养,回收了两种不同的结晶固体。其中第一种固体以块状、角状晶体的微米级聚集体形式出现,与细菌生物膜相关。第二种固体以30 - 50纳米的纳米棒形式出现,散布在细菌裂解的有机产物中。固体的双相混合物明显以第一相为主。这种双相材料的X射线衍射(XRD)峰和傅里叶变换红外光谱(FTIR)光谱一致显示出镁白磷钙石的特征。通过溶解固体无法鉴定出有机成分或蛋白质。在这两种情况下,生物矿化模式似乎是生物诱导而非生物控制的。由于已知镁是磷酸钙成核和生长的强抑制剂,嗜氢羧基热杆菌可能通过提供螯合镁或与之形成复合物的位点来发挥作用,从而降低其作为成核和晶体生长抑制剂的活性。嗜氢羧基热杆菌合成白磷钙石和纳米羟基磷灰石样材料证明了这种以能够进行水煤气变换反应而闻名的生物体的多功能性,并且可能在细菌介导的磷酸钙材料合成中具有应用价值,作为一种环境友好的替代工艺。