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Movement and habitat use of juvenile Lake Sturgeon ( Acipenser fulvescens , Rafinesque, 1817) in a large hydroelectric reservoir (Nelson River, Canada)
Author(s) -
Hrenchuk C. L.,
McDougall C. A.,
Nelson P. A.,
Barth C. C.
Publication year - 2017
Publication title -
journal of applied ichthyology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.392
H-Index - 62
eISSN - 1439-0426
pISSN - 0175-8659
DOI - 10.1111/jai.13378
Subject(s) - lake sturgeon , thalweg , foraging , fishery , habitat , acipenser , hydrology (agriculture) , juvenile fish , juvenile , environmental science , fish measurement , ecology , biology , oceanography , sturgeon , sediment , fish <actinopterygii> , geology , paleontology , geotechnical engineering
Summary Movement and habitat utilization of juvenile Lake Sturgeon ( Acipenser fulvescens ) were examined in Stephens Lake, a large hydroelectric reservoir on the Nelson River, Manitoba, Canada, between 21 June 2011, and 15 October 2012. Stephens Lake is defined by a sharp hydraulic gradient at the upstream end (Gull Rapids) and a pronounced reservoir transition zone ( RTZ ), characterized by a change in substrate composition from coarse to fine. Twenty juvenile Lake Sturgeon <600 mm fork length were captured in the RTZ , implanted with acoustic transmitters, and tracked using stationary receivers. Our primary hypothesis considered that, if foraging behaviour was contingent on sand substrate, these fish would spend the majority of the open‐water season foraging in the relatively small area where hydraulic gradients dictate sand deposition. Data indicated that tracked individuals were highly bottom oriented, and utilized deeper thalweg habitats exclusively during the first open‐water season. On average, juveniles spent only 22% of their open‐water time in the RTZ (river kilometer [rkm] 4.5–7.0). Most fish spent more time upstream as opposed to downstream, but a few individuals did utilize backwatered thalweg areas, suggesting that silt‐overlay habitats may be suitable for foraging. A seasonal spatial shift in distribution was also observed. Juveniles vacated the RTZ as winter progressed, moving further downstream and occasionally laterally into backwatered shallows, potentially avoiding extreme ice conditions and a large hanging ice dam that develops downstream of Gull Rapids. After ice break‐up, most individuals with active tags returned to the upstream end of Stephens Lake. The results add to the growing body of evidence that suggests factors other than habitat suitability influence Lake Sturgeon movement and utilization patterns, raising questions about the mechanisms for core‐area affinity in this species.