Laserfiche WebLink
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />~' <br />It\' <br />ji <br />!!f. <br />i <br />f" <br /> <br />~ <br /> <br />s: <br /> <br />~. <br /> <br />- <br /> <br />5 <br /> <br />growth and development is usually short, food is rarely limiting due to substantial <br /> <br /> <br />increases in allochthonous input and increased access to fringing and connected slack- <br /> <br /> <br />water habitats. Predators are relatively scarce due to a dilution effect of increased habitat <br /> <br /> <br />space during flooding (Bayley 1988; Winemiller 1989). Predation and resource <br /> <br /> <br />limitations come into play afterward, when juveniles are concentrated in the channel as <br /> <br /> <br />floods recede. Adult populations may remain relatively stable, while juveniles suffer <br /> <br /> <br />severe mortality with few ultimately surviving to recruit. Many species are considered <br /> <br />flood exploitive and year class strength is positively correlated to discharge (Ross and <br />Baker 1983; Welcomme 1985). <br /> <br /> <br />Many of these species, particularly those that are widely dispersed, may persist as <br /> <br /> <br />meta-populations with the spatial arrangement of habitat features acting as a template of <br /> <br /> <br />organization (Schlosser and Angermeier 1995; Stanford et al. 1995). Such <br /> <br /> <br />metapopulation structure may be the rule for many salmonid species (Rieman and <br /> <br /> <br />McIntyre 1993). The heterogenous mosaic of floodplain vs. constrained reaches <br /> <br /> <br />combined with local events result in local successes and extinctions for populations <br /> <br />which are then recolonized from adjacent populations (Stanford et al. 1995). Similarly, <br /> <br /> <br />many habitats may only support one life-history phase and represent sinks which are <br /> <br /> <br />continually recolonized from other sources (pulliam 1988). <br /> <br /> <br />As in other highly seasonal systems (Urban et al. 1987 ; Walker et al. 1995), the <br /> <br /> <br />natural, temporal regime of variation and disturbance of the Colorado River has been <br /> <br />dramatically altered by human intervention. Where not reservoir dominated at present, <br /> <br /> <br />the system is far more typified than before by longitudinal processes proposed for a river <br />