Role of fungal mycelium in the formation of carbonate concretions in growing media-an investigation by SEM and synchrotron-based X-ray tomographic microscopy

Research output: Contribution to journalArticleResearchpeer review

Authors

  • S. Masaphy
  • L. Zabari
  • J. Pastrana
  • S. Dultz

External Research Organisations

  • Migal Galilee Technology Center Israel
  • Tel Hai Academic College
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Details

Original languageEnglish
Pages (from-to)442-450
Number of pages9
JournalGeomicrobiology journal
Volume26
Issue number7
Publication statusPublished - Oct 2009

Abstract

Soil fungi can facilitate calcification. Mushroom Morchella sp. mycelium induced the formation of carbonate concretions on the surface of an organic-based growing media amended with sand and ground limestone. According to SEM observation and X-ray-tomographic microscopy a dense mycelial network induced calcification. The CaCO3 content of concretions (Ø: 0.3-1.5 cm) was found to be at 30%. Microsparitic calcite cemented the pores between the sand grains forming a dense clogging microstructure. Besides water uptake by the mycelium, a high evaporation rate and a decrease in pCO2 contributed to the formation of the concretions. Fungal mycelium in the concretions is surrounded by voids indicating that at the surface of the mycelium, calcification is counteracted most probably by the release of organic acids.

Keywords

    Calcification, Growing media, Microstructure, Morchella, SEM, X-ray-tomographic microscopy

ASJC Scopus subject areas

Cite this

Role of fungal mycelium in the formation of carbonate concretions in growing media-an investigation by SEM and synchrotron-based X-ray tomographic microscopy. / Masaphy, S.; Zabari, L.; Pastrana, J. et al.
In: Geomicrobiology journal, Vol. 26, No. 7, 10.2009, p. 442-450.

Research output: Contribution to journalArticleResearchpeer review

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abstract = "Soil fungi can facilitate calcification. Mushroom Morchella sp. mycelium induced the formation of carbonate concretions on the surface of an organic-based growing media amended with sand and ground limestone. According to SEM observation and X-ray-tomographic microscopy a dense mycelial network induced calcification. The CaCO3 content of concretions ({\O}: 0.3-1.5 cm) was found to be at 30%. Microsparitic calcite cemented the pores between the sand grains forming a dense clogging microstructure. Besides water uptake by the mycelium, a high evaporation rate and a decrease in pCO2 contributed to the formation of the concretions. Fungal mycelium in the concretions is surrounded by voids indicating that at the surface of the mycelium, calcification is counteracted most probably by the release of organic acids.",
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AU - Zabari, L.

AU - Pastrana, J.

AU - Dultz, S.

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