Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphism

Microorganisms and their biomineralisation processes are widespread in almost every environment on earth. In this work, Streptomyces luteogriseus DHS C014, a dominant lithophilous actinobacteria isolated from microbial mats on limestone rocks, was used to investigate its potential biomineralisation...

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Main Authors: Chengliang eCao, Jihong eJiang, Henry eSun, Ying eHuang, Faxiang eTao, Bin eLian
Format: Article
Language:English
Published: Frontiers Media S.A. 2016-03-01
Series:Frontiers in Microbiology
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fmicb.2016.00366/full
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author Chengliang eCao
Chengliang eCao
Chengliang eCao
Jihong eJiang
Henry eSun
Ying eHuang
Faxiang eTao
Bin eLian
author_facet Chengliang eCao
Chengliang eCao
Chengliang eCao
Jihong eJiang
Henry eSun
Ying eHuang
Faxiang eTao
Bin eLian
author_sort Chengliang eCao
collection DOAJ
description Microorganisms and their biomineralisation processes are widespread in almost every environment on earth. In this work, Streptomyces luteogriseus DHS C014, a dominant lithophilous actinobacteria isolated from microbial mats on limestone rocks, was used to investigate its potential biomineralisation to allow a better understanding of bacterial contributions to carbonate mineralisation in nature. The ammonium carbonate free-drift method was used with mycelium pellets, culture supernatant, and spent culture of the strain. Mineralogical analyses showed that hexagonal prism calcite was only observed in the sub-surfaces of the mycelium pellets, which is a novel morphology mediated by microbes. Hemispheroidal vaterite appeared in the presence of spent culture, mainly because of the effects of soluble microbial products (SMP) during mineralisation. When using the liquid culture, doughnut-like vaterite was favoured by actinobacterial mycelia, which has not yet been captured in previous studies. Our analyses suggested that the effects of mycelium pellets as a molecular template almost gained an advantage over SMP both in crystal nucleation and growth, having nothing to do with biological activity. It is thereby convinced that lithophilous actinobacteria, S. luteogriseus DHS C014, owing to its advantageous genetic metabolism and filamentous structure, showed good biomineralisation abilities, maybe it would have geoactive potential for biogenic carbonate in local microenvironments.
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spelling doaj.art-fd2addc1a5ed46b3be45c4e858eb66be2022-12-21T19:13:34ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2016-03-01710.3389/fmicb.2016.00366182695Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphismChengliang eCao0Chengliang eCao1Chengliang eCao2Jihong eJiang3Henry eSun4Ying eHuang5Faxiang eTao6Bin eLian7Institute of GeochemistryUniversity of Chinese Academy of SciencesJiangsu Normal UniversityJiangsu Normal UniversityDesert Research InstituteInstitute of MicrobiologyInstitute of GeochemistryNanjing Normal UniversityMicroorganisms and their biomineralisation processes are widespread in almost every environment on earth. In this work, Streptomyces luteogriseus DHS C014, a dominant lithophilous actinobacteria isolated from microbial mats on limestone rocks, was used to investigate its potential biomineralisation to allow a better understanding of bacterial contributions to carbonate mineralisation in nature. The ammonium carbonate free-drift method was used with mycelium pellets, culture supernatant, and spent culture of the strain. Mineralogical analyses showed that hexagonal prism calcite was only observed in the sub-surfaces of the mycelium pellets, which is a novel morphology mediated by microbes. Hemispheroidal vaterite appeared in the presence of spent culture, mainly because of the effects of soluble microbial products (SMP) during mineralisation. When using the liquid culture, doughnut-like vaterite was favoured by actinobacterial mycelia, which has not yet been captured in previous studies. Our analyses suggested that the effects of mycelium pellets as a molecular template almost gained an advantage over SMP both in crystal nucleation and growth, having nothing to do with biological activity. It is thereby convinced that lithophilous actinobacteria, S. luteogriseus DHS C014, owing to its advantageous genetic metabolism and filamentous structure, showed good biomineralisation abilities, maybe it would have geoactive potential for biogenic carbonate in local microenvironments.http://journal.frontiersin.org/Journal/10.3389/fmicb.2016.00366/fullBiomineralisationLithophilous actinobacteriaStreptomyces luteogriseus DHS C014Hexagonal prism calciteDoughnut-like vaterite
spellingShingle Chengliang eCao
Chengliang eCao
Chengliang eCao
Jihong eJiang
Henry eSun
Ying eHuang
Faxiang eTao
Bin eLian
Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphism
Frontiers in Microbiology
Biomineralisation
Lithophilous actinobacteria
Streptomyces luteogriseus DHS C014
Hexagonal prism calcite
Doughnut-like vaterite
title Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphism
title_full Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphism
title_fullStr Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphism
title_full_unstemmed Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphism
title_short Carbonate mineral formation under the influence of limestone-colonising actinobacteria: morphology and polymorphism
title_sort carbonate mineral formation under the influence of limestone colonising actinobacteria morphology and polymorphism
topic Biomineralisation
Lithophilous actinobacteria
Streptomyces luteogriseus DHS C014
Hexagonal prism calcite
Doughnut-like vaterite
url http://journal.frontiersin.org/Journal/10.3389/fmicb.2016.00366/full
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