Aquatic Food Base Response to the 1996 Test Flood below Glen Canyon Dam, Colorado River, Arizona

We examined the impact of the 1996 test flood released from Glen Canyon Dam (GCD) on the aquatic food base in the Colorado River through Grand Canyon National Park, Arizona, USA. Benthic scour and entrainment of both primary and secondary producers occurred at all study sites along the 385-km river...

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Bibliographic Details
Published in:Ecological applications 2001-06, Vol.11 (3), p.672-685
Main Authors: Shannon, Joseph P., Blinn, Dean W., McKinney, Ted, Benenati, Emma P., Wilson, Kevin P., O'Brien, Chris
Format: Article
Language:English
Subjects:
adaptive management
aquatic food base
Biomass
Canyons
Chara
Cladophora
Cobbles
Colorado River
Dams
desert biome
discharge
disturbance
Elodea
Ferries
flood
Floods
Glen Canyon Dam
Invertebrata
Invited Feature: Colorado River Ecosystem Restoration Using Planned Flooding
Lotic systems
Macroinvertebrates
organic drift
Potamogeton
River regulation
Streams
USA, Arizona
USA, Arizona, Glen Canyon Dam
USA, Colorado R
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Summary:We examined the impact of the 1996 test flood released from Glen Canyon Dam (GCD) on the aquatic food base in the Colorado River through Grand Canyon National Park, Arizona, USA. Benthic scour and entrainment of both primary and secondary producers occurred at all study sites along the 385-km river corridor. The majority of the organic drift occurred within the first 48 h of the test flood with the arrival of the hydrostatic wave. Recent macrophyte colonizers (Chara, Potamogeton, and Elodea) of fine sediment in the tailwaters were scoured from the channel bottom, with recovery to pre-flood estimates within 1-7 months depending on taxa. Macroinvertebrates and filamentous algae recovered within three months depending on taxa. The test flood removed suspended particles from the water column and increased water clarity, which enhanced benthic recovery. The test-flood hydrograph was designed primarily as an experiment in sand transport and occurred during a period of sustained high releases from GCD starting in June 1995 due to above-average inflow into Lake Powell. We discuss the implications of the hydrograph shape, pre- and post-riverine conditions, and the slow response time of biological resources for design of aquatic ecosystem experiments.
ISSN:1051-0761
1939-5582
DOI:10.1890/1051-0761(2001)011[0672:AFBRTT]2.0.CO;2