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Last modified
7/14/2009 5:02:35 PM
Creation date
5/20/2009 10:17:31 AM
Metadata
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UCREFRP
UCREFRP Catalog Number
9404
Author
Douglas, M. E. and P. C. Marsh.
Title
Ecology and Conservation Biology of Humpback Chub (Gila cypha) in the Little Colorado River.
USFW Year
1996.
USFW - Doc Type
Tempe.
Copyright Material
NO
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Movements by G. cypha within the LCR.---Our results contrast with <br />those of Kaeding and Zimmerman (1983), who found no consistent <br />relationship between catch rate and river reach within the LCR <br />(where 'river reaches' were 5 km increments, beginning at RKM 2 <br />and ending at Blue Springs (RKM 21; Fig. 1--2b)). In our <br />analyses, river reaches were more extensive, and only encompassed <br />those RKM within which G. cypha was active (i.e., 0--14.9). <br />The confluence has often been considered a staging area for <br />G. cypha (R. R. Miller, GCNP report, 1975, unpubl.; R. D. <br />Suttkus, G. H. Clemmer, C. Jones, and C. R. Shoop, GCNP report, <br />1976, unpubl.; C. 0. Minckley, unpubl. field notes, 1977). <br />Extent of G. cypha's movement within the LCR was not clarified <br />until September 1977, when three large individuals (278--295 mm <br />TL) were captured 12.8 RKM above the confluence (C. 0. Minckley, <br />unpubl. field notes, 1977). From these data, and from AZGF <br />monitoring efforts in spring 1987--1990 (C. 0. Minckley, <br />unpubl.), it was believed that G. cypha actively moved into the <br />LCR in spring (i.e., April/May) to reproduce, then quickly <br />returned to the mainstem. Greater numbers of G. cypha at the <br />confluence during spring of 1992 support an hypothesis of staging <br />prior to upstream movement. Downstream (i.e „ postreproductive) <br />movement also clearly occurred, but spanned a long period and was <br />diffuse. Movements between LCR reaches during a given sampling <br />period were negligible, suggesting temporal closure during <br />periods of sampling. There was no evidence of explosive or <br />extensive reproductive movements. <br />Our results indicate population stasis within reaches, <br />particularly summer through winter, suggesting that G. cypha is <br />more of a resident component of the LCR than previously imagined. <br />These observations support similar data collected by Karp and <br />Tyus (1990) in the Yampa River. There, G. cypha remained in or <br />near specific eddies for extended periods, and even returned to <br />the same eddy during the spawning season in different years. It <br />could not be ascertained whether individual chub deposited eggs <br />in the eddies or simply used them for staging, resting, or <br />feeding. <br />Habitat use.-- rata on habitat use by G. cypha are primarily <br />anecdotal and --,servational. Adults characterize whitewater <br />reaches, where they occupy deep, swirling eddies along canyon <br />walls or concentrate in zones of turbulence near boulders and <br />submerged rocks (Minckley 1991:150). Similarly, Kaeding et al. <br />(1990) noted that commonality among G. cypha habitats is not <br />great depth, but dynamic flow vectors that result from water <br />moving rapidly among large, angular boulders and shoreline rock <br />outcrops. Within other areas of the Colorado River, G. cypha <br />often associates with large-scale riprap material from riverside <br />railroad and highway construction (Kaeding et al., 1990). <br />Karp and Tyus (1990) argued that eddy habitat was crucial to <br />10
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