2013
DOI: 10.1111/fwb.12262
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The relative contributions of refugium types to the persistence of benthic invertebrates in a seasonal snowmelt flood

Abstract: 1. Flow refugia, characterised by low hydraulic stress during a flood, are key habitats that contribute to the persistence of benthic invertebrate. We investigated the use of different refugium types distributed across stream and floodplains and clarified which refugia contributed most to the persistence of assemblage and population during a seasonal snowmelt flood. 2. We sampled invertebrates and measured physical variables from six or nine types of channel units ('riffle', 'run ', 'lateral pool', 'backwater'… Show more

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Cited by 20 publications
(19 citation statements)
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“…In the run and pool mesohabitats, LPF events lead to an increase in drag producing a decrease in the total taxa richness (i.e., several taxa abandoned these habitats). The latter has been observed in similar studies carried out at mountainous regions (Angradi, 1997) as well as in lower and flatter areas (Sueyoshi, Nakano, & Nakamura, 2014). In this study region, situated at an altitude over 3,500 m a.s.l.…”
Section: Key Hydrological Indicessupporting
confidence: 83%
See 1 more Smart Citation
“…In the run and pool mesohabitats, LPF events lead to an increase in drag producing a decrease in the total taxa richness (i.e., several taxa abandoned these habitats). The latter has been observed in similar studies carried out at mountainous regions (Angradi, 1997) as well as in lower and flatter areas (Sueyoshi, Nakano, & Nakamura, 2014). In this study region, situated at an altitude over 3,500 m a.s.l.…”
Section: Key Hydrological Indicessupporting
confidence: 83%
“…and having significant slopes (Mosquera et al, ), only run, riffle, and pool mesohabitats are present. No other mesohabitats types were found, such as abandoned pool, side channel, inundation area, usually existing at flatter (and lower) regions, or leaf pack and organic debris packs at mountainous regions (Angradi, ) that may serve as refuge for the taxa that are leaving run, riffle, and pool mesohabitats upon peak flow events (Sueyoshi et al, ). In the current study region, these taxa are likely washed away by the increasing current.…”
Section: Discussionmentioning
confidence: 99%
“…Independent-sample t-tests were performed on the hyporheic flux patterns and macroinvertebrate indices were calculated at each site to determine the effect of exchange patterns on the macroinvertebrate community. In this study, higher taxonomic levels of data classified by living habits (burrowers, swimmers, climbers, sprawlers, clingers, and divers) were used [65][66][67], because macroinvertebrates are sensitive to habitat changes [68,69].…”
Section: Macroinvertebrate Samplingmentioning
confidence: 99%
“…These areas of relatively mild currents are called “flow refugia” (Lancaster & Hildrew, 1993a; 1993b). Functionally available flow refugia can be found in shallow bankside areas (Negishi, Inoue, & Nunokawa, 2002; Sueyoshi, Nakano, & Nakamura, 2013), deep pools (Matthews, 1986), complex habitats with woody debris and plant roots (Borchardt, 1993; Palmer, Arensburger, Martin, & Denman, 1996), hyporheic zones (Williams & Hynes, 1974), and tributaries (Koizumi, Kanazawa, & Tanaka, 2013), including spring-fed streams. This indicates that maintaining habitat heterogeneity, including a variety of flow refugia, is important for conserving stream biodiversity (Sedell, Reeves, Hauer, Stanford, & Hawkins, 1990).…”
Section: Introductionmentioning
confidence: 99%