Journal of Energy Engineering (에너지공학)

The Korean Society for Energy (한국에너지학회)
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A brief review on Oyster shells origin and sedimentary evolution for the formation of limestone

  • Ramakrishna, Chilakala (Department of Bio-based Materials, School of Agriculture and Life Science, Chungnam National University) ;
  • Thriveni, Thenepalli (Department of R&D Team, Hanil Cement Corporation) ;
  • Whan, Ahn Ji (Center for Carbon Mineralization, Climate Change Mitigation and Sustainability Division, Korea Institute of Geosciences and Mineral Resources (KIGAM))
  • Received : 2018.08.07
  • Accepted : 2018.09.14
  • Published : 2018.09.30
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Abstract

The shell waste biomineralization process has known a tremendous metamorphosis and also the nanostructure with the identification of matrix proteins in oyster shells. However, proteins are represented in minor shell components and they are the major macromolecules that control biocrystal synthesis. Aragonite and calcite were derived from molluscan shells and evaluated the source of carbonate minerals and it helps for the formation of limestone. The oyster shell wastes are large and massive. The paleoecological study of oyster beds has discovered a near-shore and thin Upper Rudeis formation with storm influence during the accumulation of oysters with highly altered by disarticulation, bioerosion, and encrustation. It is possible even in the Paleozoic mollusks provided sufficient carbonate entirely to the source of microcrystalline of limestone. The present review is to discuss paleoecologically a number of oyster shell beds accumulated and sediment to form the different types of limestone during the Middle Miocene time.

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References

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