Soil carbon source and accumulation over 12,000years in a semi-natural Miscanthus sinensis grassland in southern Japan

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Miscanthus , a promising feedstock for the production of lignocellulosic ethanol, will likely see a considerable increase in cultivation and production in the U.S. and Europe in the coming decades. To better predict the effect of this change on soil edaphic resources, we examined a Miscanthus sinensis -dominated grassland in its native range in southern Japan. Soil organic carbon age, accumulated carbon stock, and carbon source were determined on pyrolysis volatile (Py-V) and pyrolysis residue (Py-R) fractions of soil organic matter. Stable carbon isotopic composition of soil organic matter was also determined. Values of total sequestered C summed from two soil profiles (0–1.5 m) were 515 and 559 Mg C ha − 1 . Stable isotope analysis showed that about 66.8% of soil C, ranging from 52.0 to 84.8%, was derived from C 4 plants. Variation of soil age indicated by 14 C dates of Py-V and Py-R fractions was correlated linearly with soil depths with a R 2 value ranging from 0.98 to 0.99. Phytolith data showed an increase in abundance of M. sinensis and Pleioblastus sect. Nezasa following a pyroclastic eruption 7 kyrs ago, and a decrease in Sasa sect. Crassinodi from 12 to 7 kyrs ago. Organic carbon flux ranged from 0.85 to 1.63 Mg C ha − 1 yr − 1 through 1.5-m soil profiles, and Miscanthus -derived carbon flux was distributed in a similar pattern to the total C throughout the soil profiles. Over a 12,000 year history of land use at the Aso caldera, Japan, M. sinensis was found to be a major contributor to soil carbon and a sink for atmospheric CO 2 , which, under certain constraints, has implications for the potential sequestration of soil carbon under Miscanthus in cultivated conditions. ► Soil carbon stock source was determined on Miscanthus sinensis grassland in Japan. ► Total soil carbon stock on two profiles of 1.5 m ranged from 515 to 559 Mg C ha − 1 . ► Isotopic analysis demonstrated that 66.8% of soil C was derived from a C 4 source. ► Radiocarbon-ages of soil fractions were highly correlated with soil depth (R 2 = 0.99). ► Miscanthus has been a significant contributor to soil carbon for ~ 7300 yrs.