Characterization of calcium deposition induced by Synechocystis sp PCC6803 in BG11 culture medium
Yan Huaxiao1; Han Zuozhen2,3; Zhao Hui1,2; Zhou Shixue1; Chi Naijie2; Han Mei2; Kou Xiaoyan1; Zhang Yan1; Xu Linlin1; Tian Chenchen1; Qin Song4; Han, ZZ (reprint author), Shandong Univ Sci & Technol, Coll Geol Sci & Engn, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Peoples R China. hanzz@163.com; yzsxue@126.com
发表期刊CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
ISSN0254-4059
2014-05-01
卷号32期号:3页码:503-510
关键词Synechocystis Sp Pcc6803 Preferred Orientation Biomineralization Calcium Carbonate Thermal Stability
DOI10.1007/s00343-014-3150-2
产权排序[Yan Huaxiao; Zhao Hui; Zhou Shixue; Kou Xiaoyan; Zhang Yan; Xu Linlin; Tian Chenchen] Shandong Univ Sci & Technol, Coll Chem & Environm Engn, Qingdao 266590, Peoples R China; [Han Zuozhen; Zhao Hui; Chi Naijie; Han Mei] Shandong Univ Sci & Technol, Coll Geol Sci & Engn, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Peoples R China; [Han Zuozhen] Shandong Univ Sci & Technol, State Key Lab Min Disaster Prevent & Control, Qingdao 266590, Peoples R China; [Qin Song] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
作者部门海岸带生物学与生物资源利用所重点实验室
英文摘要Calcium carbonate (CaCO3) crystals in their preferred orientation were obtained in BG11 culture media inoculated with Synechocystis sp. PCC6803 (inoculated BG11). In this study, the features of calcium carbonate deposition were investigated. Inoculated BG11 in different calcium ion concentrations was used for the experimental group, while the BG11 culture medium was used for the control group. The surface morphologies of the calcium carbonate deposits in the experimental and control groups were determined by scanning and transmission electron microscopy. The deposits were analyzed by electronic probe micro-analysis, Fourier transform infrared spectrum, X-ray diffraction, thermal gravimetric analysis and differential scanning calorimetry. The results show that the surfaces of the crystals in the experimental group were hexahedral in a scaly pattern. The particle sizes were micrometer-sized and larger than those in the control group. The deposits of the control group contained calcium (Ca), carbon (C), oxygen (O), phosphorus (P), iron (Fe), copper (Cu), zinc (Zn), and other elements. The deposits in the experimental group contained Ca, C, and O only. The deposits of both groups contained calcite. The thermal decomposition temperature of the deposits in the control group was lower than those in the experimental group. It showed that the CaCO3 deposits of the experimental group had higher thermal stability than those of the control group. This may be due to the secondary metabolites produced by the algae cells, which affect the carbonate crystal structure and result in a close-packed structure. The algae cells that remained after thermal weight loss were heavier in higher calcium concentrations in BG11 culture media. There may be more calcium-containing crystals inside and outside of these cells. These results shall be beneficial for understanding the formation mechanism of carbonate minerals.; Calcium carbonate (CaCO3) crystals in their preferred orientation were obtained in BG11 culture media inoculated with Synechocystis sp. PCC6803 (inoculated BG11). In this study, the features of calcium carbonate deposition were investigated. Inoculated BG11 in different calcium ion concentrations was used for the experimental group, while the BG11 culture medium was used for the control group. The surface morphologies of the calcium carbonate deposits in the experimental and control groups were determined by scanning and transmission electron microscopy. The deposits were analyzed by electronic probe micro-analysis, Fourier transform infrared spectrum, X-ray diffraction, thermal gravimetric analysis and differential scanning calorimetry. The results show that the surfaces of the crystals in the experimental group were hexahedral in a scaly pattern. The particle sizes were micrometer-sized and larger than those in the control group. The deposits of the control group contained calcium (Ca), carbon (C), oxygen (O), phosphorus (P), iron (Fe), copper (Cu), zinc (Zn), and other elements. The deposits in the experimental group contained Ca, C, and O only. The deposits of both groups contained calcite. The thermal decomposition temperature of the deposits in the control group was lower than those in the experimental group. It showed that the CaCO3 deposits of the experimental group had higher thermal stability than those of the control group. This may be due to the secondary metabolites produced by the algae cells, which affect the carbonate crystal structure and result in a close-packed structure. The algae cells that remained after thermal weight loss were heavier in higher calcium concentrations in BG11 culture media. There may be more calcium-containing crystals inside and outside of these cells. These results shall be beneficial for understanding the formation mechanism of carbonate minerals.
文章类型Article
资助机构Marine & Freshwater Biology ; Oceanography
收录类别SCI
语种英语
关键词[WOS]CARBONATE PRECIPITATION ; PHASE ; TRANSFORMATION ; SYNECHOCOCCUS ; CYANOBACTERIA
研究领域[WOS]Marine & Freshwater Biology ; Oceanography
WOS记录号WOS:000335767800002
引用统计
被引频次:19[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cn/handle/133337/8555
专题海岸带生物学与生物资源利用重点实验室_海岸带生物学与生物资源保护实验室
通讯作者Han, ZZ (reprint author), Shandong Univ Sci & Technol, Coll Geol Sci & Engn, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Peoples R China. hanzz@163.com; yzsxue@126.com
作者单位1.Shandong Univ Sci & Technol, Coll Chem & Environm Engn, Qingdao 266590, Peoples R China
2.Shandong Univ Sci & Technol, Coll Geol Sci & Engn, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Peoples R China
3.Shandong Univ Sci & Technol, State Key Lab Min Disaster Prevent & Control, Qingdao 266590, Peoples R China
4.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
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Yan Huaxiao,Han Zuozhen,Zhao Hui,et al. Characterization of calcium deposition induced by Synechocystis sp PCC6803 in BG11 culture medium[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2014,32(3):503-510.
APA Yan Huaxiao.,Han Zuozhen.,Zhao Hui.,Zhou Shixue.,Chi Naijie.,...&yzsxue@126.com.(2014).Characterization of calcium deposition induced by Synechocystis sp PCC6803 in BG11 culture medium.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,32(3),503-510.
MLA Yan Huaxiao,et al."Characterization of calcium deposition induced by Synechocystis sp PCC6803 in BG11 culture medium".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 32.3(2014):503-510.
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