4.2 Article

Biomineralization of Mg-Enriched Calcium Carbonates by Aerobic Microorganisms Enriched from Rhodoliths

Journal

JOURNAL OF NANOSCIENCE AND NANOTECHNOLOGY
Volume 17, Issue 4, Pages 2329-2332

Publisher

AMER SCIENTIFIC PUBLISHERS
DOI: 10.1166/jnn.2017.13316

Keywords

Calcium; Magnesium; Biomineralization; Calcite; Mg-Rich Calcite

Funding

  1. Korea CCS R&D Center (KCRC) grant - Korean government (Ministry of Science, ICT and Future Planning) [NRF-2012-0008930]
  2. Korean government [2014R1A1A2009549]
  3. National Research Foundation of Korea [2014R1A1A2009549] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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The objective of this study was to investigate the effect of Mg:Ca ratio in the medium on the formation of low-and high-Mg calcite by aerobic microorganisms enriched from rhodoliths (mainly Proteus mirabilis, Wu Do-1). XRD analyses showed that both low-and high-Mg calcites were formed depending on the Mg:Ca ratio in the medium. Calcite was formed at Ca:Mg ratios of 6:0 and 3:1 and high-Mg calcite was formed at Ca:Mg ratios of 1:1 and 1:3 in the medium. Huntite was formed with a Ca:Mg ratio of 0:6. SEM-EDS analyses showed that the low-and high-Mg calcite crystals had a rhombohedron shape and consisted of Ca, Si and Mg with extracellular polymeric substances (EPS). These results indicate that Wu Do-1 induced precipitation of low-and high-Mg calcite crystals depending on the Ca:Mg ratio in the medium. The carbonate minerals were precipitated on the cell walls and EPS via the accumulation of Ca and/or Mg ions. Therefore, microbial formation of carbonate minerals may play an important role in Ca, Mg, and carbon biogeochemistry as well as CO2 fixation in the natural environments.

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