Long‐term impacts of forest disturbances: Comparing cumulative effects of clearcut logging versus landslide on stream conditions and abundance of a headwater stonefly Scopura montana

When forest disturbance impacts adjacent headwater streams, the recovery of habitat conditions and populations can take over several decades. Thus, considering long‐term, historical legacies of forest disturbances is key for understanding and managing forest–stream linkages. We focused on small‐scal...

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Veröffentlicht in:Freshwater biology 2021-10, Vol.66 (10), p.2004-2015
Hauptverfasser: Ohira, Mitsuru, Watanabe, Yu’usuke, Gomi, Takashi, Sakai, Masaru
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Sprache:eng
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Zusammenfassung:When forest disturbance impacts adjacent headwater streams, the recovery of habitat conditions and populations can take over several decades. Thus, considering long‐term, historical legacies of forest disturbances is key for understanding and managing forest–stream linkages. We focused on small‐scale forest disturbances such as small‐block harvesting and landslides. We compared the long‐term (past 100 years) cumulative effects between the anthropogenic and natural forest disturbances on stream conditions and the abundance of a headwater specialist, Scopura montana (Plecoptera: Scopuridae). Sampling was conducted in 10 m reaches of 39 first‐order streams with a catchment area up to 5.9 ha during late summer in central Japan. We quantified past clearcut logging areas using plantation records of each harvest block and past landslide areas from contour maps within each catchment. Piecewise structural equation models using the cumulative area of each forest disturbance as an independent variable, revealed different indirect effects of clearcut logging (average area: 1.74 ha) and landslides (0.21 ha) on S. montana abundance through modified stream conditions. Canopy openness and wetted channel width were higher with a larger logged area, and S. montana abundance was lower with higher water temperature (daily maximum). When the magnitude of clearcut logging was similar to the landslide area (
ISSN:0046-5070
1365-2427
DOI:10.1111/fwb.13811