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Great Ideas in Riverine Ecology Linear to Landscapes FISH 7380; Dr. E. Irwin
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Geology and climate (present and historical) River Morphology Hydrology Sediment transport Nutrient/elemental availability Basin flora and fauna Terrestrial communities Systems created by water running downhill depend on: Carbon/solar input Patterns of flows = community function 4) spiraling and retention 5) connectedness 6) biotic/abiotic controls Human interference 1) stream classification 2) longitudinal processes 3) Riparian-river interactions Land use heterotrophy biota Trophic structure Habitat structure
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Classification Streams can be classified Allows managers and scientists to organize river systems Conceptual and regional approaches Climate and geology, but vegetation important also NA-Ecosystem approach (broad scale) Climate, physiography and vegetation
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Hierarchical classification Spatially nested levels of resolution Problem— relatively distinct boundaries
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Stream Order Strahler (1952) and modified by Horton (1945) Variation from headwaters to mouth Ordering gives a measure of position Others-link magnitude, d-link
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Longitudinal Zonation
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River Continuum Concept Downstream transfers of energy and matter Invertebrate functional groups US—DS in lowland rivers=lateral exchanges and vertical fluxes
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River-Riparian Interactions Allochtonous inputs, LWD Flood-pulse concept Annual floods drive organic matter and nutrient input in large floodplain rivers.
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Lateral and vertical bounds revisited
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Longitudinal, lateral and vertical fluxes
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Spiraling and Retention
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Connectedness
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Disturbance Other abiotic controls Biotic? Limiting resources Abiotic and Biotic Control
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Disturbance-structures stream communities High/low flows Especially in headwaters
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Pressure Points Interference: how management can mess things up. Discontinuity- Serial Faunal
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