The Coho
Local populations of Coho salmon are listed as "endangered" under the endangered species act (ESA) (both state and federal). The ESA's provide legal tools intended to aid in slowing the loss of the beautiful diversity of life to extinction. As with nearly all legal tools, it does not always work well. Sometimes these laws conflict with their goals.
Many salmon and steelhead populations have been listed as “Threatened” or “Endangered” under state and federal law. The decline of the salmon and how best to reverse the trend is an extremely complex issue. Some information on the history of this tragedy can be found in the books Salmon Without Rivers by Lichatowich (2001, Island Press) and A Common Fate, by Cone (1995, Henry Holt and Co., N.Y.).
It is not entirely clear that the coho are “native” to streams south of San Francisco. Existing historical evidence has been called into question on the basis of a number of inconsistencies and questionable reports. It has been determined that much hatchery fish planting has taken place over many years, with fish from numerous sources. Some archeological evidence indicates that coho bones are not found in local Native American “kitchen middens,” the presumption being that if the fish were available, the people would have eaten them- as they did eat steelhead (whose bones are found in local middens). For some compelling information indicating that coho are not native to streams south of San Francisco connect to http://www.ccfassociation.org.
The ESA was intended to apply to natural native populations. President George W. Bush, early in the summer of 2004, further complicated an already complex and confusing situation by declaring that all hatchery-produced fish should be counted in the determination of a salmon population’s status with respect to the ESA (this was in direct contradiction to the advice of a panel of scientists commissioned to advise President Bush on the subject).
The native or non-native status of the local coho needs to be resolved as best as is possible. Protection and support of introduced species that are outside their natural range can have undesirable consequences in unbalancing local ecosystems and cause socio-political backlash that reflects poorly on the ESA.
The coho of Scotts Creek are being well supported. The MBSTP supports the population by a supplementation process that is condoned by the scientists most knowledgeable about that process in NMFS and DFG. The financial support for MBSTP comes from the private sector (primarily small donors from the local area). Agency financial support is very limited as a result of serious questions that have been raised about the role of hatcheries in general, which has led to a failure to support the unique mission, technique, and role of the MBSTP hatchery.
It appears that the most probable future for coho in our watershed will not be determined by the ESA, but by the degree of local political will to assist the fish population in the face of several potential outcomes: 1) coho become more-robustly self-supporting (this would likely require a climate change on the central coast of California); 2) it becomes clear that the coho are not native here, are damaging to the local ecology and should be intentionally extirpated; 3) the decision is made to see if they can make it on their own without supplementation or concerted year-class replacement efforts (recent history indicates that ceasing supplementation would very likely result in extirpation); or finally 4) continue hatchery support in maintenance of a “wild” population that is best adapted to local conditions.
The Water
There are no longer any heavy demands on surface waters in the watershed. One particularly egregious agricultural overuse problem that occurred in the early 90s was stopped by DFG. Currently all agricultural water use (with one exception) is from deep wells. A draw-down test demonstrated that maximal pumping of these wells does not affect creek flow volume. A small area of pasture is irrigated with creek water. The pasture is maintained for cattle (replacement heifers) by pumping water from the lowermost reach of a tributary to Scotts Creek. Pump rates are limited to between 35 and 50 gallons per minute (0.11 CFS maximum). The diversion is operated for short periods of time with sensitivity to the creek habitat. If visible drawdown of the creek occurs, the diversion rate is slowed. During low flows the irrigation frequency is reduced. The reach from which the water is drawn is a short, steep, fast-moving riffle with little cover for rearing salmonids. Temporary minor reductions in flow volume may not have an appreciable effect on aquatic life in this location.
The Lockheed Martin facility in the upper watershed has a registered right to draw up to 10,000 gallons a day from its storage reservoir on Mill Creek. All other surface water use is for rural domestic purposes. A small number of homes operate diversions (exercising their riparian right). These diversions are usually supplementary to an alternate source such as a spring or well and suction hoses are all properly screened to protect aquatic life. Well water is generally not favored because high iron sulfide content makes it unpleasant and in some cases unpalatable. Special treatment of this well water helps but does not totally alleviate the problem. Nevertheless, most homes in the watershed do use well water. It is important to note that properly functioning septic systems return the majority (90%) of domestically used water to the natural ground water system in a sanitary way. It does not appear that domestic diversions (either individually or cumulatively) appreciably affect creek flow volumes or water quality.
An attempt should be made to achieve a better understanding of the specific relationship between creek flow volumes and the level of the water table. The study should be designed to answer the questions of when, where, and to what degree are creeks in the system likely to become influent versus effluent (losing water to the zone of saturation as opposed to gaining water from the zone of saturation). Information on influency should be correlated to rainfall history, flow volume history, and geology of the alluvial aquifer as best as is possible. A proper study of this type would need to be fairly long-term in order to get a clear understanding of the relationships.
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