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Biological cycle of silicon in moso bamboo ( Phyllostachys pubescens ) forests in central Japan
Author(s) -
Umemura Mitsutoshi,
Takenaka Chisato
Publication year - 2014
Publication title -
ecological research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.628
H-Index - 68
eISSN - 1440-1703
pISSN - 0912-3814
DOI - 10.1007/s11284-014-1150-5
Subject(s) - bamboo , phyllostachys , biogeochemical cycle , litter , plant litter , environmental science , forest floor , sasa , ecosystem , botany , terrestrial ecosystem , agronomy , ecology , biology , soil water , soil science
Silicon (Si) has various biogeochemical functions, such as regulating soil formation and species composition, not only in terrestrial ecosystems but also in aquatic ones. Bamboo stands accumulate large quantities of amorphous Si. Evaluating Si dynamics in moso bamboo ( Phyllostachys pubescens ) forests, which are currently spreading through eastern Asia, is important in understanding their biogeochemical function as a supply source of phytoliths. We conducted a study on the organic accumulation and biological cycle of Si in three P . pubescens stands in central Japan with different site characteristics. The amounts of Si accumulation aboveground and underground were 200–360 and 180–460 kg/ha, respectively. These values indicate that Si accumulation underground was comparable to that aboveground. Silicon supply to the forest floor through litterfall was 77–330 kg/ha/year corresponding to 165–706 kg/ha/year as phytoliths (SiO 2 ), and 72–88 % was supplied as leaf litter. These results showed that a huge biogenic Si pool derived from bamboo plants exists in the floor of bamboo forests. Furthermore, we estimated the Si turnover time in P . pubescens forests as being 1.3–12.2 years, although this variation may depend on forestry conditions such as soil water content or stem density.