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Aquatic Entomology ZOOL 484/584 Policies Course outline - website
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What is Aquatic Entomology? Study of Aquatic Insects, –habitat consists mainly of a body of water have key morphological adaptations to assist them in this habitat. course is based on ecology and taxonomy of aquatic insects
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Where do you find aquatic insects? Water Lentic = Lotic = Highest diversity AI in lotic ecosystems
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Stream ecology Physical Properties Hydrologic cycle
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Water in rivers Discharge –Speed of water in channel –Current velocity U –Varies across stream: –Highest where friction is lowest (surface, center of channel) –Approaches 0 at substrate surface
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Cross-sectional area of stream Width x Depth Total volume at point (discharge, Q) = –W x D x U
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Hydrograph Record of discharge
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Material carried by flow Particles move along bed = bedload Suspended load = silt, clays All sediments from erosion: –Streambed, bank regions
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What causes sediment transports? Flow events that influence channel form Human impacts: –Ag run-off, urban run-off, channelization, etc.
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Discharge relationships Profile: steep headwaters, flatten with distance –Particle size decreases Sinuosity Deposition Erosion
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Discharge relationships Floodplain: Pool-riffle floodplain channel terrace pool riffle pool riffle
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Stream order: always flowing 1 1 2 3 1 1 1 2 1 1 1 2 3
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Rivers change over time
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Effects of flow on organisms Adaptations of aquatic invertebrates –Attachment devices: hooks, sticky stuff, suckers –Body shape: flattened, streamlined
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Substrate Wentworth scale –Boulder: > 256 mm –Cobble: 64-256 mm –Pebble:16-64 mm –Gravel: 2-16 mm –Sand:0.063-2 mm –Silt:< 0.063 mm
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Most stream organisms live in/on substrate Lithophilous = stony substrate Psammophilous = sand substrate Burrowing Xylophilous = wood-dwelling Phytophilous = plants
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Substrate size and organism diversity 0.038348 Particle size mm Species richness
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Water quality and organisms Temperature Oxygen pH Salinity
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Read Poff et al. (1997) Know: What is “natural flow regime” How to characterize?
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How does streamflow affect: Water temperature? Channel geomorphology? Habitat diversity? A “master variable”
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River management has been based on: Species of interest Commercial interests Sportfishing interests Not working!
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Recent advocates suggest understanding/restoring natural flow regime: Magnitude Frequency Duration Timing Rate of change
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Lytle & Poff 2005. TREE 19:94
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Natural flow regime Why do streams differ in flow regimes? How have we altered flow regimes?
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Ecosystem changes along streams River continuum concept (RCC) Vannote et al. (1980) Can. J. Fish. Aquat. Sci. 37:130 Based on forested headwater streams in eastern North America
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Three basic RCC Principles 1. Stream communities are based on continuous gradient of physical variables that change from headwaters to mouth
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Three basic RCC Principles 2. Communities cannot be divorced from riparian zone or geomorphic catchment.
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Three basic RCC Principles 3. Downstream assemblage is inextricably linked to processes occurring upstream.
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Major prediction of RCC Longitudinal changes in abundances of functional feeding groups and their food resources.
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RCC Predictable changes in assemblages with stream distance: Headwaters = leaf inputs -- shredders, collectors
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RCC Midreaches: sunlight = algae -- fewer shredders, more collectors + grazers
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RCC Downstream: deeper = less light to bottom, less allochthonous inputs -- collectors- filterers
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Problems with RCC Not all streams are the same: spring-fed, arid riparian, blackwater Large rivers -- little studied; grazers are present
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Alternatives Flood pulse concept for large rivers (Junk et al. 1989) Allochthonous material has large impact: periodic flooding allows riparian materials to wash into river
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Alternatives Serial discontinuity concept (Stanford + Ward 1983) The effect of a dam is to “reset” the RCC
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Alternatives The riverine ecosystem synthesis. 2006. Thorp, Thoms, Delong. Combines previous ideas: Hydrogeomorphic patches Functional process zones
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Riverine Ecosystem Synthesis
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Underground aquatic habitats Caves, hyporheic zone Organisms live in substrates or in caves Caves typically have high endemism
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Lentic ecosystems Abiotic zones based on light penetration, distance from shore –Littoral, epilimnion, hypolimnion, benthic Stratification
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