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Stream macrophytes increase invertebrate production and fish habitat utilization in a California stream
Stable flow and thermal regimes, coupled with geologically derived nutrients, are drivers of enhanced productivity in volcanic spring‐fed rivers. However, little information exists on biotic mechanisms or species interactions contributing to elevated productivity at higher trophic levels. In a Calif...
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Published in: | River research and applications 2018-10, Vol.34 (8), p.1003-1012 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Stable flow and thermal regimes, coupled with geologically derived nutrients, are drivers of enhanced productivity in volcanic spring‐fed rivers. However, little information exists on biotic mechanisms or species interactions contributing to elevated productivity at higher trophic levels. In a California stream, juvenile steelhead trout were observed to preferentially select macrophyte habitat at a rate three times greater, on average, than five other habitat types. To understand the potential rearing benefits associated with macrophytes, we conducted a manipulative experiment to determine how macrophytes affect invertebrate prey availability and stream water velocity. Macrophytes supported up to nine times greater abundance of invertebrates than adjacent open gravel habitats. They also doubled invertebrate drift rates and reduced water velocity by up to 42‐fold. The results show that aquatic macrophytes are an important stream habitat feature that may be bioenergetically more favourable for rearing salmonids than more traditional lotic habitats. We suggest that macrophytes have the potential to enhance growth rates of juvenile salmonids when compared with other habitat types. Habitats that confer growth and size advantages may ultimately improve fitness and contribute to conservation of imperilled salmonids. |
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ISSN: | 1535-1459 1535-1467 |
DOI: | 10.1002/rra.3331 |