The role of canopy cover on the recovery of periphyton and macroinvertebrate communities after a month-long flood

被引:0
|
作者
Randall L. Fuller
Christine LaFave
Matthew Anastasi
Jennifer Molina
Hector Salcedo
Sophia Ward
机构
[1] Colgate University,Biology Department
来源
Hydrobiologia | 2008年 / 598卷
关键词
Stream disturbance; Flood effects; Canopy cover; Chironomidae; Baetidae; Periphyton;
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学科分类号
摘要
We studied the recovery of periphyton and macroinvertebrate communities in a second order stream after a month-long spate that began as increased discharge due to snowmelt in April 2000 but continued through May as a result of frequent rainstorms. We sampled macroinvertebrates and periphyton in June 2000 at three different sites—an upstream site in a conifer tree plantation, a second site ca. 800 m downstream in a mixed hardwood forest, and a third site ca. 1.4 km downstream where there was an open canopy. Periphyton abundance was low on 6 June at all sites but increased 10-fold at the open canopy site the following week (13 June), appearing as a thick mat of Ulothrix. By 26 June, periphyton biomass (as both chlorophyll a and ash free dry mass) had decreased by 80% whereas densities of Chironomidae increased 50-fold and Baetidae increased 4-fold at the open canopy site; little change had occurred in periphyton and macroinvertebrate communities at the forested sites from early to late June. Our results suggest that baetids and chironomids rapidly responded to the increased algal resource at the open canopy site due to their life history characteristics and high growth rates. Chironomids decreased the green mat of Ulothrix by using this alga in tube construction and both chironomids and baetids likely consumed this alga. The varied responses of the periphyton and macroinvertebrate communities at the forested versus open sites demonstrate a resistance to impacts by floods at the forested sites, whereas at the open canopy site periphyton and macroinvertebrate communities were more resilient to the flood disturbance.
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页码:47 / 57
页数:10
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