The impacts of reduced flow on instream habitat condition and macroinvertebrate behaviour : a thesis presented in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Ecology at Massey University, Palmerston North, New Zealand
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The allocation of water and setting of minimum flows is a contentious issue. Despite this, there is little research into the impacts of reduced stream flows on instream habitat and biota. Previous studies tend to concentrate on fish or macroinvertebrate community structure with few studies investigating the behavioural responses of macroinvertebrates to flow reduction. Therefore the aim of my thesis was to assess the impact of severe flow reduction on habitat condition and macroinvertebrate behaviour (drift and refugia use) using before-after, control-impact (BACI) experimental manipulations in natural (Wairarapa, New Zealand) and artificial stream channels (Canterbury, New Zealand). Instream channels were also used to assess the impact of flow reduction duration and magnitude on macroinvertebrate community structure and vertical distribution in the substrate. Reduced flow tended to decrease depth, velocity, and wetted width and increase fine sediment deposition. However, the common assertion that it would lead to increased temperatures and lowered dissolved oxygen levels was not supported by my results, although this may occur in some streams. I found that severely reduced flow in small streams had minimal effect on water temperature, although it can depress nighttime dissolved oxygen minima. Flow reduction markedly increased the drift propensity of some taxa immediately following flow reduction, before it fell back to near background levels for the rest of the reduced flow period. This increased drift occurred as animals redistributed themselves to more suitable microhabitats within the stream. Additionally, flow reduction reduced the drift distance of animals making it unlikely that drifting would be a viable way of escaping low flow conditions. Flow reduction had no impact on the densities or vertical distribution of animals within the substrate, however, most species were present at all depths sampled in the hyporheic zone, providing a source of colonists should some event (flood or drying) denude the benthos of animals. An instream channel experiment showed that apart from changes to the relative abundances of a few common taxa, flow reduction magnitude (up to 98% reduction) had little impact on the macroinvertebrates of a lowland river. Overall, my results suggested that severe flow reduction stresses a number of taxa, causing them to drift as they redistribute themselves within the stream. I found no evidence that animals actively seek refuge in the hyporheic zone, and in a lowland river, the magnitude and duration of flow reduction had minimal effect on the macroinvertebrate community.
Stream ecology, Streamflow, New Zealand