Developmental changes in the45Ca2+ uptake byTrichoderma viride mycelium
Author(s) -
Martin Šimkovič,
R. Ortega-Pérez,
G. Turian,
V. Betina,
Daniela Hudecová,
Ĺudovı́t Varečka
Publication year - 1997
Publication title -
folia microbiologica
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.537
H-Index - 48
eISSN - 1874-9356
pISSN - 0015-5632
DOI - 10.1007/bf02898720
Subject(s) - mycelium , conidiation , conidium , biology , trichoderma viride , botany , dilution , biochemistry , physics , mutant , gene , thermodynamics
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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