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<br />~, <br />~. <br /> <br />468 <br /> <br />EMLEN ET AL. <br /> <br />numbered in the hundreds of thousands. The most <br />recent large run, in 1969, was speculated to contain <br />about 100,000 fish. Adults originating from the <br />last major run before 1969, the one in 1950, are <br />now few, contributing only slightly to recruitment. <br />From 1970 to 1979 there was only modest re- <br />cruitment from some river access in high-water <br />years and from spawning in the Pyramid Lake <br />fishway. In the 8 years from 1980 through 1987, <br />there were seven runs; with the exception of the <br />run in 1986, these were very small (average, 12,000 <br />fish; range, 5,000-36,300). The 1986 run, occur- <br />ring in a 100-year-flood year, produced about 200 <br />million larvae and, with some contribution from <br />other smaller runs, led to an approximately three- <br />fold increase in adult population from about <br />100,000 adults in 1983 to about 300,000 in 1990. <br />Since 1987, however, there have been no runs at <br />all, the result of drought and human water use <br />(diversion and storage). <br />The apparent dramatic decline in the cui-ui pop- <br />ulation led the federal government to institute pro- <br />tective measures in 1967 and eventually to list the <br />species as endangered. Because upriver passage is <br />frequently blocked by a delta (Scoppettone et at. <br />1986), the Marble Bluff Fish Facility, including a <br />dam and a fish way, were constructed in 1975 to <br />facilitate migration. However, only a tiny fraction <br />of the potential spawners use this fish passage in <br />low-water years. Upriver passage still depends on <br />high lake levels and high flows to inundate the <br />delta. <br />It is not only access to the lower Truckee River <br />that requires critical amounts of water. The pre- <br />spawning aggregate forms only if there has been <br />sufficient "attractant" flow in the river for several <br />weeks before passage is to occur (Scoppettone et <br />al. 1986). In addition, variation in reproduction <br />and larvae survival appears to be overwhelmingly <br />controlled by hydrology (Scoppettone et al. 1981). <br />Finally, viability of cui-ui eggs is temperature de- <br />pendent (Coleman et at. 1987) and river temper- <br />ature is strongly related to flow. The plight of the <br />cui-ui thus comes into focus when we consider that <br />for almost a century this species has had to com- <br />pete for water with humans, whose agricultural <br />and other demands have cut the supply to Pyramid <br />Lake by an average of 250,000 acre-feet per year, <br />approximately 50% of the historical runoff. This <br />decrease in river flow has brought reductions in <br />the frequency and size of the spawning migration <br />and, via ~sed temperatures, higher egg mortality. <br />Because cui-ui live to about 40 years, a 40-year <br />sequence of dry years, or years in which human <br /> <br />water use is such to preclude spawning, might ex- <br />terminate the population. There is no record of <br />drought lasting this long, and no reason to believe <br />that anthropogenic effects will produce such a long <br />run of poor years for the fish. On the other hand, <br />a series of poor years could lead to cumulative <br />damage that would eventually result in extinction. <br />Thus, there is no assurance the population would <br />disappear after 40 sterile years and, similarly, no <br />guarantee it would persist after a few much shorter <br />sequences of poor years. Extinction is largely a <br />function of the probability that sterile-year se- <br />quences of whatever duration will threaten per- <br />sistence of the cui-ui. This probability is related <br />to population size. The chance in any given year <br />that at least one male and one female fish of re- <br />productive age are present, and that at least one <br />such pair will spawn, increases with the number <br />of individuals in a population. Thus the likelihood <br />of extinction rises markedly with decreasing pop- <br />ulation size of spawners. Finally, total population <br />size invariably drops following years without re- <br />production, and is likely to drop even if repro- <br />duction occurs when low water level limits the <br />number of spawners or survival of the eggs. It <br />follows that even when poor conditions occur in <br />sets of much less than 40 years, a disconnected <br />but sufficiently proximate string of such short se- <br />quences easily could lead to a collapse of the cui- <br />ui population. <br />Clearly, recovery depends on the restoration, or <br />at least partial restoration, of the local historical <br />hydrology. But will supplemental water result in <br />cui-ui persistence and recovery? To answer this <br />question it is necessary to predict future cui-ui <br />populations as a function of the amount of water <br />restored to the lower Truckee River. The following <br />presentation is offered as an exposition and illus- <br />tration of a general approach to population pro- <br />jection that may prove useful in population as- <br />sessments and recovery planning. <br /> <br />Methods <br /> <br />Definition of Terms <br />What constitutes recovery? An endangered spe- <br />cies can be said to be capable of recovery when a <br />management plan that predicts indefinite persis- <br />tence with some acceptable level of probability, <br />and shows convincing evidence that the plan will <br />perform as indicated, is implemented. Two ad- <br />ditional terms need definition. <br />Indefinite persistence implies continued exis- <br />tence in perpetuity. However, this definition is not <br />