Y. Ohmae et al., The plant growth inhibitor nagilactone does not work directly in a stabilized Podocarpus nagi forest, J CHEM ECOL, 25(4), 1999, pp. 969-984
Nagilactones isolated from Podocarpus nagi are known for poisonous physiolo
gical activities to organisms. To clarify the allelopathic potential of nag
ilactone to wild plants, the seasonal changes in nagilactone contents in th
roughfall, leaf litter, and soil were monitored monthly in a podocarp fores
t at Mt. Mikasa, Nara City, central Japan. The average annual nagilactone c
oncentrations in throughfall, leaf litter, and surface soil at 0-10 cm dept
h were 4.7 x 10(-12) g/ml, 3.8 x 10(-4) g/g and 3.1 x 10(-7) g/g, respectiv
ely. The nagilactone flux from canopy leaves to the forest Root via through
fall was 5.2 x 10(-2) g/ha/yr, which was far smaller than that via leaf lit
terfall: 765.3 g/ha/year. The disappearance of nagilactones from leaf litte
r and the nagilactone accumulation in the Ao layer and mineral soil were al
so studied. Nagilactone in leaf litter rapidly disappeared and its relative
disappearance rate was 5.8/yr. Nagilactone concentration in mineral soil a
lso decreased rapidly with an increase in soil depth and could not be detec
ted in soil at 40-100 cm depth. The total mass of nagilactones was 177.3 g/
ha in the Ao layer and 105.0 g/ha in mineral soil. These quantities in nagi
lactone dynamics give a very rapid turnover time of 0.37 year (4.4 months)
in a soil nagilactone pool, implying the possibility of the reabsorption of
nagilactone by P. nagi, while the allelopathic effects of nagilactone to o
ther plants in the podocarp forest are questionable.