Abstract

Although fine roots play an integral role in biogeochemical cycling and supporting plant function, fundamental understanding of the mechanisms that control fine root life span is limited. Based on literature, we examined how intrinsic plant characteristics including root diameter, root branching order, rooting depth, and mycorrhizal symbiosis affect fine root life span, and how fine root life span differs with plant life form and foliar habit and between early versus late seral species. We also examined how soil nitrogen and water availability, temperature, and atmospheric carbon dioxide concentration influence fine root life span. We focused on evidence from rhizotron and minirhizotron observations which allow for individual roots to be directly monitored in situ. Fine root life span increased with increasing root diameter, was shorter for more distal than proximal roots, and increased with increasing rooting depth, but was not influenced by mycorrhizal symbiosis. Trees had the longest fine root life spans of all the plant life forms, followed by grasses, lianas, shrubs, and forbs. Among trees, deciduous species had shorter fine root life spans than evergreen species. Fine root life span appears to decrease with increasing temperature and increase with soil water availability, whereas the effects of soil nitrogen availability and atmospheric carbon dioxide concentration on fine root life span were highly inconsistent among studies. Our findings indicate that root morphological characteristics and plant traits are useful predictors of fine root life span. However, environmental influences on fine root life span remain poorly understood due to the limited number of respective studies. Future studies of root demographic processes are needed to better understand environmental controls of fine root life span. It is also critical that research continues into developing more direct and less invasive techniques for studying root demographics.

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