an intermittent stream riffle during the wet se<strong>as</strong>on is more likely to resemble that <strong>of</strong> a perennialstream riffle, while a small pool remaining <strong>as</strong> the intermittent stream dries will harbor aninvertebrate community more similar to that <strong>of</strong> an ephemeral habitat. The extent <strong>of</strong> the averageannual dry period in an intermittent stream can also influence invertebrate communitycomposition; in Oregon, both Dieterich (1992) and Banks (2005) found that a continuous flowperiod <strong>of</strong> 4-5 months or longer in intermittent headwater streams w<strong>as</strong> correlated with amacroinvertebrate community more similar to that <strong>of</strong> perennial headwaters in the same region.In addition, intermittent streams with substantial connectivity or proximity to perennial watersare likely to be re-colonized by aerial adults, upstream or downstream movements <strong>of</strong> aquaticforms, or by upward movement <strong>of</strong> organisms from deeper substrates (Williams & Hynes, 1976a;Williams, 1977; Gray & Fisher, 1981; Shivoga, 2001).Influence <strong>of</strong> additional abiotic factors<strong>Flow</strong> duration is a strong driver <strong>of</strong> macroinvertebrate community composition, but additionalabiotic factors also have a significant effect on faunal <strong>as</strong>semblages. Environmental variablessuch <strong>as</strong> stream bed composition, water velocity, predictability <strong>of</strong> drying/wetting regime, extent<strong>of</strong> drying (i.e. completely dry vs. small seeps, pools, or moist interstitial spaces), and amount <strong>of</strong>woody debris, leaf litter, and streambank vegetation strongly affect macroinvertebratepersistence and community composition. The macroinvertebrate community typically inhabitinga first-order, high-elevation, forested headwater stream, for example, would be expected to differfrom that in a higher-order, open meadow stream meandering through a valley, even if bothstreams are intermittent.Channel substrate/type (i.e. bedrock, boulder c<strong>as</strong>cade, pool, riffle, or rapid) w<strong>as</strong> found to be <strong>as</strong>trong determinant <strong>of</strong> invertebrate distribution (Halw<strong>as</strong> et al., 2005), <strong>as</strong> it affected the degree <strong>of</strong>stream bed drying and types <strong>of</strong> invertebrate refugia available. Positive correlations wereobserved between the degree <strong>of</strong> sediment moisture and the number <strong>of</strong> invertebrates in soil coresin a dry desert stream bed (Stanley et al., 1994). The presence or absence <strong>of</strong> a shading canopyh<strong>as</strong> also been seen <strong>as</strong> an important driver <strong>of</strong> invertebrate community structure in streams <strong>of</strong>differing flow duration (Dieterich, 1992; Dieterich et al., 1997), because the level <strong>of</strong> sunlight(insolation) regulates the amount and type <strong>of</strong> food b<strong>as</strong>e present. Studies conducted in Oregonhave shown that macroinvertebrate density and diversity can differ in streams flowing throughclearcut vs. forested are<strong>as</strong> (Banks, 2005; Herlihy et al., 2005; Banks et. al, 2007) <strong>as</strong> the result <strong>of</strong>the canopy reduction and incre<strong>as</strong>ed sedimentation <strong>as</strong>sociated with logging.Indicator <strong>as</strong>semblagesDespite numerous contradictions in the literature, some commonalities emerge that make itpossible to discriminate between invertebrates in streams with differing flow regimes. At thebroadest level, taxa diversity (number <strong>of</strong> taxa and their relative abundance) and/or richness (totalnumber <strong>of</strong> taxa present) tends to be higher in perennial streams compared to intermittent (Wrightet al., 1984; Feminella, 1996; Williams, 1996; del Rosario & Resh, 2000; Meyer & Meyer, 2000;Fritz & Dodds, 2005; Wood et al., 2005). Both diversity and abundance are lowest in ephemeralstreams (Dieterich, 1992; Price et al., 2003; Halw<strong>as</strong> et al., 2005). However, it should be noted<strong>Macroinvertebrates</strong> <strong>as</strong> indicators <strong>of</strong> stream flow duration,The Xerces Society for Invertebrate Conservation6
that some studies have found similar diversity in perennial and intermittent streams (Bottorff &Knight, 1988; Delucchi, 1988; Miller & Golladay, 1996; Shivoga, 2001; Price et al., 2003).Results for the density <strong>of</strong> organisms in different cl<strong>as</strong>ses <strong>of</strong> stream may also differ; Miller &Golladay (1996) found that total invertebrate density w<strong>as</strong> consistently about twice <strong>as</strong> high inperennial streams, but other studies have found greater invertebrate densities in intermittentstreams, <strong>as</strong> the drying process reduces and fragments wetted habitat, leaving remaining poolscrowded with surviving organisms (Boulton & Lake, 1992b; Stanley et al., 1994). Conflictingresults may be due to the fact that intermittent streams can have greater taxa richness or diversityduring periods <strong>of</strong> high flow, when the habitat is more similar to a perennial stream, but thenumber <strong>of</strong> taxa decre<strong>as</strong>es <strong>as</strong> the stream dries down and organisms die, migrate, or take refuge(Boulton, 2003).Invertebrate abundance and diversity in temporary streams can also decre<strong>as</strong>e following floodsthat scour out occupied habitat (Wright et al., 1984; Stanley et al., 1994; Miller & Golladay,1996). Fritz & Dodds (2005) found that intermittent prairie streams experiencing harsherconditions, including a long dry period, low flow predictability, high flood frequency, and/or lowsurface connectivity, had consistently lower taxa richness. This suggests that sites may varyannually in richness depending on differences in precipitation patterns (i.e. drought years vs.flood years). In addition, the drying regime in intermittent streams is affected by the types <strong>of</strong>habitat available; for example, intermittent streams with exposed bedrock channels retain fewermoist pools and seeps that could serve <strong>as</strong> refugia during the dry ph<strong>as</strong>e than intermittent streamswith abundant gravel, cobble, or woody debris (Clifford, 1966; Chadwick & Huryn, 2007).Although streams with differing flow duration <strong>of</strong>ten have many species in common, a smallsubset <strong>of</strong> taxa may predominate in either the perennial or intermittent system. SpanishMediterranean streams with different flow categories showed distinct biological differences, withintermittent streams dominated by taxa with pool-like strategies and ephemeral streamsdominated by taxa with life-history adaptations for surviving floods and droughts (Bonada et al.,2007). Taxa in permanent streams in this study exhibited few significant biological traits, mostlikely due to greater habitat stability (i.e. continuing presence <strong>of</strong> both riffles and pools), andperennial and intermittent streams had similar taxa richness, although both exhibited greaterrichness than ephemeral sites (Bonada et al., 2007). It should be noted that even whenintermittent and perennial streams are observed to have similar abundance and diversity <strong>of</strong> majortaxonomic groups, less similarity is seen when species-level identifications are made (Bottorff &Knight, 1988; Wood et al., 2005), although this level <strong>of</strong> taxonomic resolution is not alwayspossible.Community compositionA positive relationship h<strong>as</strong> been noted between the proportion and/or abundance <strong>of</strong> EPT taxa andincre<strong>as</strong>ing flow permanence (Feminella, 1996; Smith et al. 2003; Wood et al., 2005). This is notsurprising, <strong>as</strong> these orders are known in general to require cold, well-oxygenated, f<strong>as</strong>t-flowingwater (Merritt et al., 2007; Wiggins, 1996; Stewart & Stark, 2002). However, some taxa in theseorders possess adaptations that render them more tolerant <strong>of</strong> temporary and/or slow-movingwaters. Several species within these three orders have been found in temporary streams, in someinstances <strong>as</strong> dominant components <strong>of</strong> the invertebrate community (Lehmkuhl, 1971; Tew, 1971;<strong>Macroinvertebrates</strong> <strong>as</strong> indicators <strong>of</strong> stream flow duration,The Xerces Society for Invertebrate Conservation7
- Page 1 and 2: Using Aquatic Macroinvertebratesas
- Page 3 and 4: GoalsThe goal of this project is to
- Page 5: supported different macroinvertebra
- Page 9 and 10: DispersalAdult invertebrates with s
- Page 11 and 12: majority of all caddisflies collect
- Page 13 and 14: North CarolinaAquatic macroinverteb
- Page 15 and 16: Amphipoda), water mites (subclass H
- Page 17 and 18: ScoringThe current Oregon Draft Str
- Page 20 and 21: To sample riffle or run/glide habit
- Page 22 and 23: However, the degree of dryness in b
- Page 24 and 25: Boulton A.J. & Lake P.S. 1992b. Ben
- Page 26 and 27: Li, J., Herlihy, A., Gerth, W., Kau
- Page 28 and 29: Williams, D. D., 1996. Environmenta
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- Page 32 and 33: • Dytiscidae (predaceous diving b