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<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
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