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dc.contributor.authorHarvey, GLen_US
dc.contributor.authorHenshaw, AJen_US
dc.contributor.authorMoorhouse, TPen_US
dc.contributor.authorClifford, NJen_US
dc.contributor.authorHolah, Hen_US
dc.contributor.authorGrey, Jen_US
dc.contributor.authorMacdonald, DWen_US
dc.date.accessioned2016-04-12T12:51:53Z
dc.date.issued2014-01-01en_US
dc.date.submitted2016-03-02T09:57:44.252Z
dc.identifier.issn0197-9337en_US
dc.identifier.urihttp://qmro.qmul.ac.uk/xmlui/handle/123456789/11788
dc.description.abstractDespite increasing recognition of the potential of aquatic biota to act as 'geomorphic agents', key knowledge gaps exist in relation to biotic drivers of fine sediment dynamics at microscales and particularly the role of invasive species. This study explores the impacts of invasive signal crayfish on suspended sediment dynamics at the patch scale through laboratory and field study. Three hypotheses are presented and tested: (1) that signal crayfish generate pulses of fine sediment mobilisation through burrowing and movement that are detectable in the flow field; (2) that such pulses may be more frequent during nocturnal periods when signal crayfish are known to be most active; and (3) that cumulatively the pulses would be sufficient to drive an overall increase in turbidity. Laboratory mesocosm experiments were used to explore crayfish impacts on suspended sediment concentrations for two treatments: clay banks and clay bed substrate. For the field study, high frequency near-bed and mid-flow turbidity time series from a lowland river with known high densities of signal crayfish were examined. Laboratory data demonstrate the direct influence of signal crayfish on mobilisation of pulses of fine sediment through burrowing into banks and fine bed material, with evidence of enhanced activity levels around the mid-point of the nocturnal period. Similar patterns of pulsed fine sediment mobilisation identified under field conditions follow a clear nocturnal trend and appear capable of driving an increase in ambient turbidity levels. The findings indicate that signal crayfish have the potential to influence suspended sediment yields, with implications for morphological change, physical habitat quality and the transfer of nutrients and contaminants. This is particularly important given the spread of signal crayfish across Europe and their presence in extremely high densities in many catchments. Further process-based studies are required to develop a full understanding of impacts across a range of river styles. © 2013 John Wiley & Sons, Ltd.en_US
dc.description.sponsorshipThe research was supported by a British Society for Geomorphology Research Grant (‘Field evidence for signal crayfish impacts on fine sediment dynamics in a lowland river’). Tom Moorhouse was funded by the Esmée Fairbairn Foundation.en_US
dc.format.extent259 - 271en_US
dc.relation.ispartofEarth Surface Processes and Landformsen_US
dc.rights“The final publication is available at http://onlinelibrary.wiley.com/doi/10.1002/esp.3486/full”
dc.titleInvasive crayfish as drivers of fine sediment dynamics in rivers: Field and laboratory evidenceen_US
dc.typeArticle
dc.rights.holder© 2013 John Wiley & Sons, Ltd.
dc.identifier.doi10.1002/esp.3486en_US
pubs.issue2en_US
pubs.notesNot knownen_US
pubs.publication-statusPublisheden_US
pubs.volume39en_US


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