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Do stream macroinvertebrates use instream refugia in response to severe short‐term flow reduction in New Zealand streams?
Author(s) -
JAMES ALEXANDER B.W.,
DEWSON ZOË S.,
DEATH RUSSELL G.
Publication year - 2008
Publication title -
freshwater biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.297
H-Index - 156
eISSN - 1365-2427
pISSN - 0046-5070
DOI - 10.1111/j.1365-2427.2008.01969.x
Subject(s) - invertebrate , streams , environmental science , hyporheic zone , sediment , hydrology (agriculture) , habitat , ecology , abundance (ecology) , aquatic insect , hydrobiology , flow conditions , urban stream , community structure , flow (mathematics) , surface water , water quality , biology , geology , environmental engineering , aquatic environment , paleontology , computer network , geotechnical engineering , geometry , mathematics , computer science
Summary 1. Demand for water is increasing and water managers need to know how much they can remove from a stream before there are significant detrimental effects on its biological integrity. Flow reduction alters a number of habitat variables known to be important to aquatic invertebrates such as depth, velocity, temperature and fine sediment accumulation. Some taxa may attempt to use instream refugia to mitigate the effects of flow reduction. 2. We experimentally manipulated flows by constructing weirs and diversions in three small New Zealand streams. Discharge was reduced by 88–96%. We tested the hypothesis that macroinvertebrates would use pools and the hyporheic zone as refugia during short‐term (1‐month) periods of reduced flow. 3. We sampled hyporheic invertebrates with colonization chambers and pool invertebrates with kick nets within a before‐after, control‐impact (BACI) experimental design. A suite of physicochemical parameters was measured concurrently including surface and hyporheic temperatures. 4. Flow reduction significantly decreased velocity (60–69%) in all streams. Depth (18–61%) and wetted width (24–31%) tended to decrease but these changes were not always significant. Sediment cover increased the most in farmland streams (10–80%). Apart from decreasing temperature range (18–26%), flow reduction had little impact on the surface water temperatures. 5. Flow reduction had no impact on the abundance of common pool macroinvertebrates or on the abundance, vertical distribution or community composition of hyporheic macroinvertebrates. 6. Our results suggest that aquatic macroinvertebrates are resistant to short‐term, severe flow reduction as long as some water remains.