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<br />Hypothesis of Historical Effects from Selenium <br /> <br />1957). The lake was filled from water from several canals carrying irrigation <br />drain water for reuse in irrigation in the Uncompahgre Valley. Barnhart <br />(1957) evaluated several possible causes of the fish die-offs, and conclude that <br />selenium was probably the cause. In one portion of his research, fish held in <br />cages in the lake survived 4 months, but those released in the lake failed to <br />survive longer than 2 months. Barnhart (1957) may have been the first inves- <br />tigator to attribute fish die-offs to selenium uptake through the aquatic food <br />chain. Although flannelmouth sucker were abundant in the lake, he did not <br />find any reproduction occurring, but rather reported several pathological <br />abnormalities in the species. <br />Birkner (1978) reported elevated selenium in water, and in aquatic inver- <br />tebrates and fish samples (reported on a dry weight basis) from Highline <br />Resen'oir, Grand Junction, CO, Sweitzer Lake, Delta, CO, and Desert Reser- <br />voir, GrandJunction, CO. At Highline Resen'oir, water samples had 4.2Ilg/L, <br />aquatic invertebrates had 4 to 28 Ilg1 g, and plankton had 8 Ilg1 g. At Sweitzer <br />Lake, water had 9.4 Ilg/L, aquatic invertebrates had 20 to 45 Ilg/g, plankton <br />had 42 Ilg1 g, and fish had 26 to 79 Ilg1 g. At Desert Resen'oir, water had <br />12.5Ilg/L, aquatic invertebrates had 18 to 58 Ilg/g, plankton had 31 Ilg/g, <br />and fish had 611lg/g. Selenium concentrations at these three sites show that <br />selenium was elevated in food organisms and fish in the 1970s. <br /> <br />HYPOTHESIS <br /> <br />In 1890 native fish in the Colorado River basin were widespread and <br />abundant, including currently endangered fish. Many physical changes to the <br />rivers in the basin have resulted from dams and water diversions for domestic <br />and agricultural use, as well as biotic changes from non-native fish introduc- <br />tions. Chemical changes in rivers in the basin have occurred due to widespread <br />use of irrigation and the concomitant disposal of drainwater starting in about <br />the 1890s. Documentation from several DOA and university studies of very <br />high selenium concentrations (55 - >2000 Ilg/L) in drainwater, tributaries, <br />and many rivers in the upper and lower Colorado River basin in the mid-1930s, <br />combined with the disappearance of adult endangered fish and the striking <br />historical absence of young fish from both the upper and lower basins before <br />influences from several mainstem reservoirs occurred. suggests the hypothesis <br />that historical selenium contamination in the 1890 to 1910 period caused the <br />decline of native fish inhabiting big rivers such as Colorado pikeminnow, <br />razorback sucker, and possibly others such as bonytail in the 1910 to 1920 <br />period in the upper basin and in the 1925 to 1935 period in the lower basin <br />(Table 1). <br />University studies in the 1970s and NIWQP studies in the 1990s have <br />documented elevated selenium concentrations in water, sediment, and biota <br />throughout the entire Colorado River basin. Recent DOl studies designed to <br />determine the biological effects of selenium on lan'al and adult endangered <br />fish in the upper Colorado River basin, have shown adverse effects at concen- <br /> <br />Hum. Eco\. Risk Assess. Va\. 5. No.6, 1999 <br /> <br />1173 <br />