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7/14/2009 5:01:45 PM
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UCREFRP
UCREFRP Catalog Number
7225
Author
Kaeding, L. R., D. B. Osmundson and C. R. Berry.
Title
Temperature as a Resource Limiting Colorado Squawfish in the Upper Colorado River Basin.
USFW Year
1985.
USFW - Doc Type
\
Copyright Material
YES
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<br />.-. <br />} U 30 <br />J <br />= W <br />~F=..2o <br />~ Q <br />zw. <br />w~io <br />~~ <br />j SPAWNING <br />GROWTH / <br />--•~owER (4.54)- <br />~~MIDDLE (3.59) <br />~.\ <br />•~ <br />- UPPER., • <br />(1.97) \ ~•- <br />J F M A M J J A S O N D <br />. MONTH <br />Figure 4. Comparison of temperature regimes (average mean-monthly <br />temperatures) of the historic lower (near Yuma, Arizona, 1917-1924, <br />from Dill 1944) and middle Colorado River (near Grand Canyon, <br />Arizona, 1943-1947, 195?), and of the present. upper Colorado River <br />(near Colorado-Utah border, 1972-1978). Horizontal lines are <br />temperature thresholds for growth (14 C) and the onset of spawning <br />(20 Cj of Colorado squawfish. Numbers in parentheses are the <br />relative availability of temperatures suitable for Colorado <br />squawfish growth provided by each temperature regime {see text). <br />Temperatures from middle and upper river are from the United States <br />Geological Survey. See Figure 1 for sites of temperature-data <br />collection. <br />suitability indices to temperatures in the growth--rate vs. temperature <br />relation according to the percentage of optimum growth that they provided <br />(Figure 5). Thus 25 C had a suitability index of 1.0, 20 and 30 C had <br />suitability of 0.5, and temperatures of 14 C and cooler had suitability of <br />zero. Indi.ees for intervening temperatures were calculated by interpolation. <br />Mean-monthly temperatures were multiplied by their respective suitability <br />indices, and resulting values were summed aver the year for each of the <br />Colorado River temperature regimes (Figure 4). <br />Temperature regimes of the historic lower and middle--river reaches would <br />have allowed greater annual growth of Colorado squawfish than would that of <br />the upper river. This conclusion is based on our estimates of the relative <br />availability of temperatures suitable for growth as well as nn the length of <br />the growing seasons provided by the temperature. regimes (Figure 4). The <br />growing season of the upper river is less than five months, whereas those of <br />the middle and lower river were about six and eight months, respectively. How <br />rapid growth in the lower river might have been is unknown, however. There is <br />no information on Colorado squawfish growth in nature under conditions <br />(including temperatures) that are more nearly optimal. Pivnicka (1983) <br />reported that seven fish species, including four cyprinids, were able to <br />increase their growth rate 12 fold in optimum conditions. Colorado squawfish <br />might therefore be capable of appreciable annual growth under conditions like <br />those of the historic lower river. Data that support this conclusion has <br />recently been gathered by Osmundson (1985). In October, 1983, Osmundson <br />151 <br />,. _ <br />_ _.-- _~_ <br />
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