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

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

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

Externe Organisationen

  • Migal Galilee Technology Center Israel
  • Tel Hai Academic College
Forschungs-netzwerk anzeigen

Details

OriginalspracheEnglisch
Seiten (von - bis)442-450
Seitenumfang9
FachzeitschriftGeomicrobiology journal
Jahrgang26
Ausgabenummer7
PublikationsstatusVeröffentlicht - Okt. 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.

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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, Jahrgang 26, Nr. 7, 10.2009, S. 442-450.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-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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Download

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AU - Zabari, L.

AU - Pastrana, J.

AU - Dultz, S.

N1 - Funding information: X-ray-tomographic microscopy was performed at the TOMCAT beamline at the synchrotron light source of the Paul Scherrer Institute, Villigen, Switzerland. Skillful help by Federica Marone and Marco Stampanoni is gratefully acknowledged. This work was supported by the European Commission under contract no.: RII3-CT-2004-506008. We thank two anonymous reviewers for helpful comments.

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AB - 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.

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