Abstract. Temperate rainforest soils of the Pacific Northwest are often carbon (C)
rich and encompass a wide range of fertility, reflecting varying nitrogen (N)
and phosphorus (P) availability. Soil resource stoichiometry (C : N : P) may
provide an effective measure of site nutrient status and help refine
species-dependent patterns in forest productivity across edaphic gradients.
We determined mineral soil and forest floor nutrient concentrations across
very wet (perhumid) rainforest sites of southwestern Vancouver Island
(Canada) and employed soil element ratios as covariates in a long-term
planting density trial to test their utility in defining basal area growth
response of four conifer species. There were strong positive correlations in
mineral soil C, N, and organic P (Po) concentrations and close
alignment in C : N and C : Po both among and between substrates. Stand
basal area after 5 decades was best reflected by mineral soil and forest
floor C : N, but in either case included a significant species–soil
interaction. The conifers with ectomycorrhizal fungi had diverging growth
responses displaying either competitive (Picea sitchensis) or stress-tolerant (Tsuga heterophylla,
Pseudotsuga menziesii) attributes, in contrast to a more generalist response by an arbuscular
mycorrhizal tree (Thuja plicata). Despite the consistent patterns in organic matter
quality, we found no evidence for increased foliar P concentrations with
declining element ratios (C : Po or C : Ptotal) as we did for N. The
often high C : Po ratios (as much as 3000) of these soils may reflect a
stronger immobilization sink for P than N, which, along with ongoing
sorption of PO4-, could limit the utility of C : Po or
N : Po to adequately reflect P supply. The dynamics and availability of
soil P to trees, particularly as Po, deserves greater attention, as many
perhumid rainforests were co-limited by N and P, or, in some stands,
possibly P alone.