Fluctuations in abundance of burrowing mayflies in Southern Indian Lake, Manitoba : mechanisms and implications for environmental monitoring

In the mid-1970's, Manitoba Hydro impounded Southern Indian Lake (SIL) and diverted much of the flow of the Churchill River into the Nelson river catchment for hydroelectric power generation. A subsequent dramatic decline in burrowing mayfly (Hexagenia) populations was originally attributed to...

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Bibliographic Details
Main Author: Giberson, D. J.
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: 1991
Subjects:
Online Access:http://hdl.handle.net/1993/7221
Description
Summary:In the mid-1970's, Manitoba Hydro impounded Southern Indian Lake (SIL) and diverted much of the flow of the Churchill River into the Nelson river catchment for hydroelectric power generation. A subsequent dramatic decline in burrowing mayfly (Hexagenia) populations was originally attributed to the manipulation, until recovery of the population was observed despite ongoing physical impacts from impoundment and diversion. In 1986, an intensive study on Hexagenia in SIL was implemented to determine the actual mechanisms controlling population abundance in the lake to aid in the interpretation of the long-term monitoring data. The major factors affecting the population dynamics of Hexagenia in SIL during the study period were related to weather variables, primarily water temperature during development (and its relationship to air temperature during the open water period) and weather conditions (wind, air temperature) during the emergence period. The two species in the lake, H. limbata and H. rigida, approach their northern range limit at or near SIL. Their life cycles were similar in the study regions and closely related to thermal regime; requiring 3-yr in warmer areas of SIL and 4-yr in the coldest study region. Subimago emergence occurred from mid-July to mid-August in warm years and warm locations, but not until September in colder years or regions. September weather at SIL was often stormy and cold, and these conditions hindered emergence success. After emmergence, transformation to the adult (imago) stage was dependent on air temperatures; the final moult required ~24-48 h at 10-25oC and was unsuccessful at very low temperatures (near 0oC). Size of nymphs at maturity was related to thermal regime and the length of the life cycle. Mean body length of mature nymphs declined with decreasing thermal regime in the lake regions where 3-yr life cycles predominated. In the coldest region investigated, where the life cycle length increased from 3-yr to 4-yr, body size was similar to that from the warmest location. Body ...