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The legacy of forest disturbance on stream ecosystem functioning

Cite this dataset

Frainer, André; McKie, Brendan (2021). The legacy of forest disturbance on stream ecosystem functioning [Dataset]. Dryad.


1. Forest clearance is a pervasive disturbance worldwide, but many of its impacts are regarded as transient, diminishing in intensity as forest recovers. However, forests can take decades to centuries to recover after severe disturbances, and temporal lags in recovery of ecosystem properties for different forest habitats are mostly unknown. This includes forest streams, where most studies of the impacts of forest clearance are restricted to the first years of recovery, typically finding that temporary increases in light and nutrient runoff diminish as forest recovers. Implications of longer term changes remain little investigated. 2. In a space-for-time substitution experiment, we assessed changes in organic matter processing and in the functional and taxonomic composition of litter-consuming detritivores along a riparian forest age gradient ranging from 1 to 120 years since last timber harvesting. 3. Variation in organic matter processing and detritivore functional diversity along the forest succession gradient were both expressed as second order polynomial relationships (peaking  at ~50 years along the forest age gradient). Decomposition rates were lowest in both the more recently clearcut and older riparian forest streams. 4. Variation of litter decomposition rates among litter-bags within streams, measured by the coefficient of variation, was lowest in recent clearcuts and increased linearly along the succession gradient. This result indicates higher within-stream heterogeneity in decomposition rates in older forest streams. Synthesis and applications: We found that the decomposition of leaf litter, a component of carbon cycling in forests, was higher in streams flowing through intermediately aged forest, and that several key attributes of the organisms regulating litter decomposition also varied systematically with forest age. These findings highlight the longer term consequences of forest succession following forest clearcutting for stream habitats.  Our findings further illustrate complications arising from the use of forested sites as references for newly cleared sites without properly accounting for forest age, given conclusions regarding biotic responses will depend on the age of the reference forests. Finally, our results emphasise the potential of intensive forest management centred on vast, one-time clearcutting events to drive long term homogenisation not only in forest age structure, but also in the functioning of associated forest stream habitats.


Data collected in 10 streams runing through managed boreal forests in northern Sweden (19°07’E–20°21’E, 63°52’N–64°15’N) in autumn 2010 and spring 2011.