Abstract
To test the reliability of the radiocarbon method for determining root age, we analyzed fine roots (originating from the years 1985–1993) from ingrowth cores with known maximum root age (1–6 years old). For this purpose, three Scots pine (Pinus sylvestris L.) stands were selected from boreal forests in Finland. We analyzed root 14C age by the radiocarbon method and compared it with the above-mentioned known maximum fine root age. In general, ages determined by the two methods (root 14C age and ingrowth core root maximum age) were in agreement with each other for roots of small diameter (<0.5 mm). By contrast, in most of the samples of fine roots of larger diameter (1.5–2 mm), the 14C age of root samples of 1987–1989 exceeded the ingrowth core root maximum age by 1–10 years. This shows that these roots had received a large amount of older stored carbon from unknown sources in addition to atmospheric CO2 directly from photosynthesis. We conclude that the 14C signature of fine roots, especially those of larger diameter, may not always be indicative of root age, and that further studies are needed concerning the extent of possible root uptake of older carbon and its residence time in roots.
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Acknowledgements
We are grateful to forest engineer Erkki Salo for sampling and preparing the tree ring samples. We are also grateful to persons contributing to sampling and sorting of the original root material: Dr. Kirsi Makkonen, forest engineers Pekka Välikangas and Reijo Hautajärvi, and the staff of the Salla Office of the Finnish Forest Research Institute. We gratefully acknowledge the help of the personnel of the Dating Laboratory, Finnish Museum of Natural History, University of Helsinki, Finland for their technical assistance in radiocarbon analysis. This work was supported by the Academy of Finland.
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Sah, S.P., Jungner, H., Oinonen, M. et al. Does the age of fine root carbon indicate the age of fine roots in boreal forests?. Biogeochemistry 104, 91–102 (2011). https://doi.org/10.1007/s10533-010-9485-7
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DOI: https://doi.org/10.1007/s10533-010-9485-7