Dynamics of fine root carbon in Amazonian tropical ecosystems and the contribution of roots to soil respiration

Abstract

Radiocarbon ( 14 C) provides a measure of the mean age of carbon (C) in roots, or the time elapsed since the C making up root tissues was fixed from the atmosphere. Radiocarbon signatures of live and dead fine ( 40 years). Measurements of 14 C in the structural tissues of roots known to have grown during 2002 demonstrate that new roots are constructed from recent ( 14 C values in live roots most likely indicate the mean lifetime of the root rather than the isotopic signature of inherited C or C taken up from the soil. Estimates of the mean residence time of C in forest fine roots (inventory divided by loss rate) are substantially shorter (1–3 years) than the age of standing fine root C stocks obtained from radiocarbon (4–11 years). By assuming positively skewed distributions for root ages, we can effectively decouple the mean age of C in live fine roots (measured using 14 C) from the rate of C flow through the live root pool, and resolve these apparently disparate estimates of root C dynamics. Explaining the 14 C values in soil pore space CO 2 , in addition, requires that a portion of the decomposing roots be cycled through soil organic matter pools with decadal turnover time.

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