Abstract
This chapter focuses on how radiocarbon (14C) is used both as a tracer of source pools and for determining age on multiple time scales, providing a powerful approach for understanding the dynamics of terrestrial ecosystems. A range of applications is introduced, from estimating the lifespan of whole organisms to using the age of respired carbon (C) to partition sources of respired CO2. This chapter also provides examples that apply models introduced in Chapter 3 to the soil organic C pool. Lastly, this chapter introduces several new 14C approaches including low-level labeling to understand C cycling processes occurring on shorter time scales from minutes to months.
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Schuur, E.A.G., Carbone, M.S., Hicks Pries, C.E., Hopkins, F.M., Natali, S.M. (2016). Radiocarbon in Terrestrial Systems. In: Schuur, E., Druffel, E., Trumbore, S. (eds) Radiocarbon and Climate Change. Springer, Cham. https://doi.org/10.1007/978-3-319-25643-6_6
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