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<br />thus far been observed to have a higher standing crop of <br />periphyton and macro invertebrates than small <br />substrates, such as gravel and sand (Figure 7). <br /> <br /> 30 <br />C;; 20 <br />.!: <br />1 <br />.. <br />--' <br />:r 10 <br />u <br /> 0 <br /> .01 <br /> <br />, <br />I <br />I <br />I <br />,t-----t" ! <br />I 'I <br />"'~ <br /> <br />k, <br /> <br />I <br />I <br />I <br />I <br />I <br />, <br />',..,' <br /> <br />0.1 <br /> <br />1.0 <br /> <br />10.0 <br /> <br />SUBS TRA TE Cem) <br /> <br />· 15 <br />" <br />E <br />~ <br /> <br />60 <br /> <br />o <br /> <br />~ 10 <br />I- <br />< <br />a: <br />III <br />w <br />I- <br />a:. <br />w 5 <br />> <br />z <br />6 <br />a: <br />U <br />< <br />::. 0 <br />.01 <br /> <br />if b <br /> <br />.. <br />.. <br />40 ~ <br />:r <br />u <br />i< <br />.. <br />"' <br />20 8 <br />Q. <br />., <br /> <br />0.1 1.0 <br />SUBSTRA TE (ern) <br /> <br />10 <br /> <br />Figure 7. The distribution of biological <br />parameters by substrate sizes in the White <br />River, Utah. Bars denote 95% confidence <br />intervals. <br /> <br />Even among the rocky substrates, large differences have <br />been observed in algal standing crop between rock types, <br />probably due to textural and mineral differences. Thus, <br />the distribution of habitat types (pools and riffles) <br />which result from the dissipation of energy within the <br />study sections should be mapped and the size, texture and <br />chemistry of substrate types determined. <br /> <br />The response of primary producers is often <br />stochastic, depending upon random changes in flow and, <br />hence, sediment movement. Overall, increased levels of <br />suspended sediment reduce light intensity and limit <br />photosynthesis; however, the presence of associated <br /> <br />273 <br />