4.6 Article

Lithoautotrophical oxidation of elemental sulfur by fungi including Fusarium solani isolated from sandstone Angkor temples

Journal

INTERNATIONAL BIODETERIORATION & BIODEGRADATION
Volume 126, Issue -, Pages 95-102

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.ibiod.2017.10.005

Keywords

Deterioration of sandstones; Elemental sulfur; Chemolithotrophic fungi; Fusarium solani; Fungal growth; Cultural heritage

Funding

  1. Japanese Government Team for Safeguarding Angkor
  2. Ministry of Education, Culture, Sports, and Technology of Japan [15K14590]
  3. Grants-in-Aid for Scientific Research [17H01628, 15K14590] Funding Source: KAKEN

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Previous study about Fusarium solani THIF01, isolated from deteriorated sandstones of Angkor Wat, Cambodia, has suggested that this fungal strain harbored an endobacterium Bradyrhizobium sp. and oxidized elemental sulfur (S-0) in carbon-free media. Here we eliminated the endobacterium in THIF01 and confirmed that the cured THIF01 retained the ability of chemolithoautotrophic growth on S-0. In addition, thirteen out of eighteen identified fungal strains formed clearing zone on the agarose-solidified basal salts medium containing S-0.F. solani f.sp. pisi NBRC9425 grew in carbon-free liquid medium oxidizing S-0 to thiosulfate and sulfate. Furthermore, we proved that various fungi were capable of growth chemolithotrophically on S-0. An addition of up to 15 mg l(-1) of yeast extract to mineral-salts medium containing S-0 enhanced the production of thiosulfate and sulfate, and higher concentration of yeast extract shifted the metabolism from chemolithotroph to chemoorganotroph. Fungal hyphae were observed to attach to the S-0 granules when growing with less than 100 mg l(-1) yeast extract in the medium, but no such association was evident when incubated with 200 mg l(-1) or more yeast extract. Glucose at concentrations of up to 1 mg l(-1) did not show any negative effect on the sulfur oxidation, indicating there was a threshold concentration of organic compounds affecting the chemolithotrophic growth that has been observed before in the chemolithoautotrophic and chemolithomixotrophic sulfur oxidizing bacteria.

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