Abstract
The composition of plant secondary metabolites (PSMs) extensively impacts ecosystem functioning. It is vital that we understand temporal patterns in the plants’ allocation of resources to PSMs, particularly those influenced by human activity. Existing data are insufficient in the long-term perspective of perennial plants (age or ontogeny). We analysed phenolic concentrations in foliage from birch (Betula pubescens Ehr.) considered to be undamaged and growing on 5, 10 and 15 years old clear-cuts in two boreal forest landscapes in Norway, sampled at the peak of the growing season. In sum, low molecular weight phenolic concentrations decreased with age. Apart from one apigenin glycoside, the low molecular weight phenolics co-varied similarly at all ages, suggesting a lack of temporal compound-specific prioritisation of this group. In contrast, the concentration of MeOH-soluble condensed tannins increased with age. The compositional shift fits well with several hypotheses that may provide proximate explanations for age patterns in PSM allocations, including both resource constraints and external pressures. Regardless of these explanations, our study adds an important perennial perspective (plant age) to temporal PSM patterns already well-known in boreal plant phenology (foliage age).
Highlights
The composition of plant secondary metabolites (PSMs) extensively impacts ecosystem functioning (Hagerman and Robbins 1993; Kraus et al 2003; Provenza et al 2007)
We examine how PSM concentrations in foliage from an abundant woody species in the northern boreal forest of Eurasia, the downy birch (Betula pubescens Ehrh.), vary with plant age
The low molecular weight phenolics decreased with age
Summary
The composition of plant secondary metabolites (PSMs) extensively impacts ecosystem functioning (Hagerman and Robbins 1993; Kraus et al 2003; Provenza et al 2007). All meta-analyses of temporal PSM patterns have been made in a phenological context (i.e. within season development) A seasonal decrease in the total PSM concentration seems most prevalent across genotypes and species, but divergent trends are often observed between herbaceous and woody plants (Koricheva and Barton 2012). One proposed explanation is the fact that herbaceous plants have no dormant above-ground parts that require protection during the cool season. This highlights how ontogeny, by often spanning longer periods, is a different context than
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