4.6 Article

Bio-mineralisation, characterization, and stability of calcium carbonate containing organic matter

Journal

RSC ADVANCES
Volume 11, Issue 24, Pages 14415-14425

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/d1ra00615k

Keywords

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Funding

  1. National Key Technology R&D Program of China [2019YFC180510303]
  2. Jiangsu Provincial Marine Science and Technology Innovation Special Project [HY2019-3]
  3. National Natural Science Foundation of China [41867032]
  4. Jiangxi Provincial Natural Science Foundation [20202BABL215028]

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This study elucidates the bio-mineralisation and stability of amorphous calcium carbonate and vaterite containing organic matter induced by Bacillus subtilis. The bacteria can induce various structural forms of CaCO3 using bacterial cells as templates. Results show that Ca2+ concentration affects the crystal structure of CaCO3, and organic matter plays a crucial role in the stability of biogenic ACC and vaterite. Our findings provide valuable insights for future research on organic-CaCO3 complexes.
The composition of organic matter in biogenic calcium carbonate has long been a mystery, and its role has not received sufficient attention. This study is aimed at elucidating the bio-mineralisation and stability of amorphous calcium carbonate (ACC) and vaterite containing organic matter, as induced by Bacillus subtilis. The results showed that the bacteria could induce various structural forms of CaCO3, such as biogenic ACC (BACC) or biogenic vaterite (BV), using the bacterial cells as their template, and the carbonic anhydrase secreted by the bacteria plays an important role in the mineralisation of CaCO3. The effects of Ca2+ concentration on the crystal structure of CaCO3 were ascertained; when the amount of CaCl2 increased from 0.1% (m/v) to 0.8% (m/v), the ACC was transformed to polycrystalline vaterite. The XRD results demonstrated that the ACC and vaterite have good stability in air or deionised water for one year, or even when heated to 200 degrees C or 300 degrees C for 2 h. Moreover, the FTIR results indicated that the BACC or BV is rich in organic matter, and the contents of organic matter in biogenic ACC and vaterite are 39.67 wt% and 28.47 wt%, respectively. The results of bio-mimetic mineralisation experiments suggest that the protein secreted by bacterial metabolism may be inclined to inhibit the formation of calcite, while polysaccharide may be inclined to promote the formation of vaterite. Our findings advance our knowledge of the CaCO3 family and are valuable for future research into organic-CaCO3 complexes.

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