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However, PAHs do not appear to be a limiting factor to native fishes in the San Juan at this time <br />(Holden 2000). <br />Selenium (a trace element) occurs naturally in many soil types, and is abundant in the drier soils <br />of the West. Selenium enters surface waters through erosion, leaching and runoff. Sources of <br />selenium, both anthropogenic and natural, in the San Juan River, have been reported by O'Brien <br />(1987), Blanchard et al. (1993), and Thomas et al. (1998). Selenium, although required in the <br />diet of fish at very low concentrations (less than 0.5 micrograms per gram on a dry weight basis <br />(gg/g), is toxic at higher levels (> 3 pg/g), and may be adversely affecting endangered fish in the <br />upper Colorado River Basin (Hamilton et al. 2004). Excess dietary selenium causes elevated <br />concentrations of selenium to be deposited into developing eggs, particularly the yolk. If <br />concentrations in the egg are sufficiently high, developing proteins and enzymes become <br />dysfunctional and lead to deformed embryos.that may be at higher risk for mortality. <br />Selenium concentrations in the San Juan River Basin are of particular concern because of its <br />documented effects on fish and wildlife reproduction and survival and high levels detected in <br />some locations within the Basin (Blanchard et al. 1993, Wilson et al. 1995, Thomas et al. 1998). <br />Selenium concentrations can be elevated in areas where irrigation occurs on soils which are <br />derived from or which overlie Upper Cretaceous marine sediments. In fact, Thomas et al. (1998) <br />found that: <br />"Water samples from sites with Cretaceous soils had significantly greater selenium <br />concentrations than water samples from sites with non-Cretaceous soils. Water samples <br />from Department of the Interior project irrigation-drainage sites developed on Cretaceous <br />soils contained a mean selenium concentration about 10 times greater than those in <br />samples from Department of the Interior project sites developed on non-Cretaceous <br />soils." <br />Percolation of irrigation water through these soils and sediments leaches selenium into receiving <br />waters. Other sources of selenium include power plant fly ash and oil refineries. Water <br />depletions, by reducing dilution effects, can increase the concentrations of selenium and other <br />contaminants in water, sediments, and biota (Osmundson et al. 2000). <br />Tributaries to the San Juan carry higher concentrations of selenium than found in the mainstem <br />river immediately upstream from their confluence with the San Juan. Increased selenium <br />concentrations may also result from the introduction of ground water to the mainstem of the river <br />along its course. Although these levels are diluted by the flow of the San Juan, the net effect is a <br />gradual accumulation of the element in the river's flow as it travels downstream. For example, <br />concentrations of selenium in water samples collected from the mainstem of the San Juan River <br />exhibited a general increase in concentration levels with distance downstream from Archuleta, <br />New Mexico, to Bluff, Utah, (<1 µg/1 to 4 µg11) (Wilson et al. 1995). The safe levels of selenium <br />concentrations for protection of fish and wildlife in water are considered to be <2 µg/l and toxic <br />levels are considered to be >2.7 µg/1(Lemly 1993, Maier and Knight 1994, Wilson et al. 1995). <br />In 1995, Colorado's Water Quality Control Commission reduced the chronic selenium standard <br />from 17 µg/L to 5 µg/L. The Service recommended the level be lowered to 2 µg/L (Service <br />1998). <br />21