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streams. Typical of cool, flowing waters in the Rocky <br />• Mountain West and elsewhere are species such as Hannaea <br />arcus, Diatoms vulgare, Cladophora glomerate, Gomphonema <br />sp., Achnanthes lanceolate, Nostoc sp., Hydrurus foetidus, <br />and vario- us species'~Nitzsci~nd NavicuTa whit- w~ ere <br />well represented in the collections. Most o~ these taxa <br />reached abundant numbers sometime during the study period. <br />A general trend was observed in pollution tolerant tax a. <br />Lower stations usually supported more pollution tolerant <br />taxa and at higher relative abundance than did upstream <br />stations. Periphyton species such as Hydrurus foetidus, <br />Gomphonema olivaceum, Nitzschia sp., and Diatoma vulgare are <br />considered to be indicative of stream waters which may have <br />elevated organic concentrations. The general trend is for <br />decrease in species and increase in pollution tolerant forms <br />from upstream to downstream locations. The North Fork of <br />the Gunnison River illustrated the least decrease in species <br />as opposed to the other sampling points. <br />Many of the species observed on the North Fork of the <br />Gunnison River are ubiquitous in distribution (i.e., occur- <br />ring in many different types of habitats under various <br />environmental conditions). Most of the taxa are alkali- <br />philous, indicating alkaline conditions as preferred water <br />quality. Most of the taxa identified are common in the <br />cold, fast flowing streams of the Rocky Mountain West. <br />• Although the periphyton study was qualitative, field <br />observations indicated a definite seasonal cycle of abun- <br />dance. In general, high flows in the spring and early <br />Sumner scour the periphyton growth from the stream sub- <br />strates. The substrates were recolonized during Sumner <br />and early fall, and periphytic algae remained fairly common <br />until winter. During the winter a decline in abundance <br />occurred because the streams were frozen over and many other <br />physical conditions were below optimum for good growth. <br />Scour was highly evident in the North Fork of the <br />Gunnison River. Even though the physical factors respon- <br />sible for the seasonal cycle varied in degree between <br />systems, maximum standing crops of periphytic algae in this <br />stream occurred in late summer and fall, and minimum growths <br />occurred in winter to early Sumner. <br />thic Mac roinvertebrates <br />Although the streams on the Mt. Gunnison No. 1 Mine <br />study area differed widely in physical characteristics <br />(width, depth, rate of flow, etc.), there were many simi- <br />larities in their benthic fauna. One characteristic of all <br />C~ <br />2.04-70 <br />