Red spruce (Picea rubens Sarg.) was investigated at its lower elevational range limit in northwestern New Jersey, USA, where small disjunct populations of scattered young trees occur in bogs and on adjacent rocky upland slopes. The bog habitat, unusual for the species elsewhere in its range, supported slower tree growth but more robust populations, with older trees, more cone production, more trees of canopy status, and higher seedling densities. Sur- rounding upland slopes supported short-lived, increasingly drought-sensitive populations with somewhat higher inci- dence of nonlethal adelgid galls and old leader damage. Tree ring chronologies showed a decrease in growth rate within four of five populations beginning around 1975, 15 years after such a decrease in mature red spruce elsewhere in its range, with recovery from decline seen after 1983 for younger but not for older trees. Existing trees exhibited low levels of crown discoloration but fairly extensive (24% of trees) defoliation due to insect leader damage. Roots were heavily colonized by ectomycorrhizae, though with less di- versity in wetlands and with the stress-indicator Cenococ- cum geophilum dominating in all populations. Inexplicably dead trees were found in high numbers (22%) in both bog and upland populations at one of three localities. Tree ring index chronologies reveal a lack of climate sen- sitivity in bog populations and one upland population, where no monthly temperature or precipitation variable ex- plains growth decline. The other two upland populations re- corded consistent climatic signals, with better growth during years with a wet June, wet March, or warm January; these two upland populations also showed increasing drought sensitivity over time, indicating an uncoupling of climate/growth relationships like that attributed elsewhere to regional air pollution.
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Webb et al. (1993) studied this question.
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