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<br />ground- <br /> <br />in flood <br />Le catch- <br />Isly con- <br />>arent as <br />md lake <br />:AuIiffe, <br />lIy flood <br />,counng <br /> <br />ver con- <br />:levation <br />)eads on <br />nal tem- <br />el across <br />nization <br />~sity and <br />'egory et <br />lOuntain <br />j diverse <br />i; Lowe- <br />are also <br /> <br />.or <br /> <br />RESTORATION OF REGULATED RIVERS <br /> <br />399 <br /> <br />foci for human activities within the catchment basin (Amoros el af., 1987; Petts et al., 1989; Wissmar el al., <br />1994) <br />Additional data are needed to confirm explicitly the pattern of biodiversity hypothesized in Figure 2 for a <br />spectrum of rivers world-wide, but the importance of alluvial zones as biological 'hot spots' within river con- <br />tinua is very clear (e,g. riparian plants: Junk et ai" 1989; Gregory el al., 1991; benthic insects: Zwick, 1992; <br />Roth et aJ., in press; fishes: Welcomme, 1979; Rieman and McIntyre, 1995), Moreover, metapopulation the- <br />ory suggests that core populations are critical for persistence of metapopulations with core-satellite struc- <br />tures (Schoener 1991; Harrison 1991, 1994). Core populations are relatively large populations occupying <br />high quality habitat. In rivers, large alluvial reaches may support core populations of fishes (Lichatowich <br />and Mobrand, 1995). These productive populations can serve as stable sources of dispersers that can reco- <br />lonize peripheral habitats where less productive satellite populations have undergone local extinctions (Har- <br />rison, 1991, 1994; Reiman and McIntyre 1993; Li el af., 1995; Schlosser and Angermeier, 1995); or, core <br />populations may 'rescue' from extinction satellite populations whose abundance has been severely reduced <br />(Brown and Kodrick-Brown, 1977; Gotelli 1991; Stacey and Taper, 1992). Thus, core populations can buffer <br />meta populations against environmental change and contribute to resiliency of regional fish production. Cer- <br />tain riparian plant species also appear to exist as metapopulations with cores on alluvial floodplains <br />(Decamps and Tabacchi, 1994), Therefore, we propose that alluvial reaches should also be foci for large river <br />conservation and restoration. <br /> <br />THE RIVER DISCONTINUUM: HUMAN ALTERATION OF LARGE RIVER ECOSYSTEMS <br /> <br />Humans vastly reduce the capacity of river ecosystems to sustain natural biodiversity and bioproduction by <br />severing or compromising the dynamic interactive pathways of the river continuum, As described above, <br />native biota of rivers display life history traits that allow populations to survive within a certain range of <br />environmental variation that characterizes a particular river. If this range of variation changes, organisms <br />must locally adapt to the new range of environmental conditions or be extirpated, Recolonization of extir- <br />pated areas may occur over time as environmental constraints ameliorate and/or as a consequence of immi- <br />gration of suitably adapted populations. However, human-mediated environmental change can be so rapid <br />and so severe as to exceed the ability of biota to adapt. The interactive pathways of the river continuum too <br />often are permanently severed by human activities, and native biodiversity and bioproduction decline, <br />Pervasive human perturbations that uncouple important ecological processes linking ecosystem compo- <br />nents in large river basins can be lumped into three broad classes: (a) water pollution of all types; (b) <br />food-web manipulation by harvest, stocking and exotic invasions; and (c) alteration of water, temperature <br />and materials flux by dams. diversions and revetment. Human land use creates direct and diffuse inputs of <br />water-borne wastes from the catchment and its airshed (Hynes, 1966; Warren, 1971), accelerates erosion and <br />sediment loading related to deforestation and road building (Waters, 1995), alters flux rates of materials in <br />rivers (e.g. eutrophication, acidification) and uncouples lotic food-webs by toxic effects, Harvest of fishes and <br />invertebrates, and the purposeful and accidental introduction of non-native species, induces strong interac- <br />tions that alter food-webs by causing biomass and bioproduction shifts, species replacements and other <br />trophic effects (Mooney, 1986) that may cascade through all trophic levels and even involve terrestrial spe- <br />cies that feed on aquatic biota (Spencer el aI., 1991). Pollution and food-web manipulation are interactive <br />with stream regulation effects in most catchments, However, alteration offlow regimes and associated sever- <br />ing of connectivity in the three spatial dimensions of riverine ecosytems perhaps are the most strikingly per- <br />vasive influence of humans on river landscapes world-wide (Dynesius and Nilsson, 1994), <br /> <br />Three first principles of the ecology of stream regulation <br /> <br />At least three fundamental commonalties emerge from the large literature on the ecology of regulated <br />rivers (reviewed by Baxter, 1977; Ward and Stanford, 1979, 1987; Lillehammer and Saltveit, 1984; Petts, <br />1.989; Calow and Petts, 1992), These principles must be recognized in the derivation of large river restora- <br />tion strategies, <br /> <br />], Habitat diversity is substantially reduced. Large storage dams world-wide inundate piedmont or <br /> <br />