Responses of benthic invertebrates to repeated hydropeaking in semi-natural flume simulations

被引:45
|
作者
Bruno, Maria Cristina [1 ]
Cashman, Matthew J. [2 ]
Maiolini, Bruno [1 ]
Biffi, Sofia [3 ]
Zolezzi, Guido [4 ]
机构
[1] IASMA Res & Innovat Ctr, Sustainable Agroecosyst & Bioresources Dept, Fdn E Mach, Via E Mach 1, I-38010 San Michele All Adige, TN, Italy
[2] Queen Mary Univ London, Sch Geog, London, England
[3] Univ Milan, Dept Earth Sci, Milan, Italy
[4] Univ Trento, Dept Civil Environm & Mech Engn, Trento, Italy
关键词
hydropeaking; drift; macroinvertebrates; semi-natural flumes; alpine stream; hydropower; ALPINE STREAM TRENTINO; MAYFLIES EPHEMEROPTERA; COMMUNITY STRUCTURE; DRIFT; FLOW; DISTURBANCE; RIVER; MACROINVERTEBRATES; PLECOPTERA; IMPACT;
D O I
10.1002/eco.1611
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
We assessed the effects of repeated hydropeaking over five consecutive days on the zoobenthic community by manipulating discharge in five experimental flumes directly fed by an Alpine stream. Treatment consisted of two different hydropeaking intensities which increased discharge two- and threefold from baseflow and lasted for 5h each day. The resulting sudden changes in flow directly affected benthic invertebrates through the induction of catastrophic drift as a direct response to high (hydropeaking) flow conditions, and of behavioural drift in the low, baseflow conditions (at the conclusion of each hydropeaking event) for some taxa. We observed: an initial strong peak in catastrophic drift within the first 3min of increased discharge, followed by a decreased drift rate throughout the following hours of the experiment; a strong response in the first day of the simulation, with successive days having substantially decreased drift; taxa-specific responses over the short and long-time scales: least-resistant taxa (i.e. Baetis spp.) were removed via the initial catastrophic drift, while more resistant taxa began to behaviourally drift later in each hydropeak (i.e. Simuliidae). Peaks in drift rates corresponded to the initial removal of CPOM which, during low flows, provided habitat and food resource for a high number of individuals and taxa. Quantification of drift responses over time scales larger than the single hydropeaking event underlines the relevance of the typical intermittency and repetition frequency as a stress factor for benthic communities, and that the response to hydropeaking is closely related to the time elapsed since the last perturbation. Copyright (c) 2015 John Wiley & Sons, Ltd.
引用
收藏
页码:68 / 82
页数:15
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