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Simkovic M, Ortega-Perez R, Turian G, et al. Developmental changes in the(45)Ca (2+) uptake byTrichoderma viride mycelium. Folia Microbiol (Praha). 1997;42(2):125-9doi: 10.1007/BF02898720.
Simkovic, M., Ortega-Perez, R., Turian, G., Betina, V., Hudecová, D., & Varecka, L. (1997). Developmental changes in the(45)Ca (2+) uptake byTrichoderma viride mycelium. Folia microbiologica, 42(2), 125-9. https://doi.org/10.1007/BF02898720
Simkovic, M, et al. "Developmental changes in the(45)Ca (2+) uptake byTrichoderma viride mycelium." Folia microbiologica vol. 42,2 (1997): 125-9. doi: https://doi.org/10.1007/BF02898720
Simkovic M, Ortega-Perez R, Turian G, Betina V, Hudecová D, Varecka L. Developmental changes in the(45)Ca (2+) uptake byTrichoderma viride mycelium. Folia Microbiol (Praha). 1997 Apr;42(2):125-9. doi: 10.1007/BF02898720. PMID: 18454332.
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Folia Microbiol (Praha). 1997 Apr;42(2):125-9. doi: 10.1007/BF02898720.

Developmental changes in the(45)Ca (2+) uptake byTrichoderma viride mycelium.

Folia microbiologica

M Simkovic, R Ortega-Perez, G Turian, V Betina, D Hudecová, L Varecka

Affiliations

  1. Department of Biochemistry and Microbiology, Slovak Technical University, Bratislava, Slovakia.

PMID: 18454332 DOI: 10.1007/BF02898720

Abstract

The rate of the(45)Ca(2+) uptake by the submergedTrichoderma viride mycelium increased with the age of the culture from 6 h until a maximum which was reached at about 30 h, and then decreased until the uptake was virtually zero. The decrease in the rate of the(45)Ca(2+) uptake was accompanied by an increase of mycelial mass. The uptake rate could not be reactivated upon substituting the medium for a fresh one, without or with dilution of the mycelium. The results suggest that the rate of(45)Ca(2+) uptake reflects the biological age of the submerged culture. The surface-cultivated mycelium took up(45)Ca(2+) proportionally with time. The autoradiography of colonies showed that(45)Ca(2+) was distributed homogeneously throughout the mycelium during vegetative growth while conidiation was accompanied by a massive accumulation of(45)Ca(2+) in conidia.

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