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dc.contributor.authorMalison, Rachel
dc.contributor.authorKuzishchin, Kirill V.
dc.contributor.authorStanford, Jack A.
dc.date.accessioned2016-09-08T11:15:57Z
dc.date.accessioned2016-09-15T12:13:03Z
dc.date.available2016-09-08T11:15:57Z
dc.date.available2016-09-15T12:13:03Z
dc.date.issued2016
dc.identifier.citationPeerJ 2016nb_NO
dc.identifier.issn2167-8359
dc.identifier.urihttp://hdl.handle.net/11250/2407556
dc.description.abstractSubjects Fisheries and Fish Science, Ecology Alaska, Alluvial river floodplains, Kamchatka, North American beaver, Castor canadensis, Pacific salmon, Salmon ecology, Salmon productionnb_NO
dc.description.abstractBeaver have expanded in their native habitats throughout the northern hemisphere in recent decades following reductions in trapping and reintroduction efforts. Beaver have the potential to strongly influence salmon populations in the side channels of large alluvial rivers by building dams that create pond complexes. Pond habitat may improve salmon productivity or the presence of dams may reduce productivity if dams limit habitat connectivity and inhibit fish passage. Our intent in this paper is to contrast the habitat use and production of juvenile salmon on expansive floodplains of two geomorphically similar salmon rivers: the Kol River in Kamchatka, Russia (no beavers) and the Kwethluk River in Alaska (abundant beavers), and thereby provide a case study on how beavers may influence salmonids in large floodplain rivers. We examined important rearing habitats in each floodplain, including springbrooks, beaver ponds, beaver-influenced springbrooks, and shallow shorelines of the river channel. Juvenile coho salmon dominated fish assemblages in all habitats in both rivers but other species were present. Salmon density was similar in all habitat types in the Kol, but in the Kwethluk coho and Chinook densities were 3 12 lower in mid- and late-successional beaver ponds than in springbrook and main channel habitats. In the Kol, coho condition (length: weight ratios) was similar among habitats, but Chinook condition was highest in orthofluvial springbrooks. In the Kwethluk, Chinook condition was similar among habitats, but coho condition was lowest in main channel versus other habitats (0.89 vs. 0.99 1.10). Densities of juvenile salmon were extremely low in beaver ponds located behind numerous dams in the orthofluvial zone of the Kwethluk River floodplain, whereas juvenile salmon were abundant in habitats throughout the entire floodplain in the Kol River. If beavers were not present on the Kwethluk, floodplain habitats would be fully interconnected and theoretically could produce 2 the biomass (between June August, 1,174 vs. 667 kg) and rear 3 the number of salmon (370,000 vs. 140,000) compared to the existing condition with dams present. The highly productive Kol river produces an order of magnitude more salmon biomass and rears 40 the individuals compared to the Kwethluk. If beavers were introduced to the Kol River, we estimate that off-channel habitats would produce half as much biomass (2,705 vs. 5,404 kg) and 3 fewer individuals (1,482,346 vs. 4,856,956) owing to conversion of inter-connected, productive springbrooks into inaccessible pond complexes. We concluded that beaver dams may limit the total amount of floodplain habitat available for salmon rearing in the Kwethluk river and that the introduction of beavers to the Kol river could be How to detrimental to salmon populations. The introduction of beavers to other large alluvial rivers like those found in Kamchatka could have negative consequences for salmon production.nb_NO
dc.language.isoengnb_NO
dc.rightsNavngivelse-Ikkekommersiell-IngenBearbeidelse 3.0 Norge*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/no/*
dc.titleDo beaver dams reduce habitat connectivity and salmon productivity in expansive river floodplains?nb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.date.updated2016-09-08T11:15:57Z
dc.source.volume4nb_NO
dc.source.journalPeerJnb_NO
dc.identifier.doi10.7717/peerj.2403
dc.identifier.cristin1379307


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Navngivelse-Ikkekommersiell-IngenBearbeidelse 3.0 Norge
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