Laserfiche WebLink
<br /> <br />BIBLIOGRAPHY <br /> <br />1. Abbott, D. M., 1975, Theprecambriangeology of the East Inlet area, southwestRocky Mountain <br />National Park, Colorado: Golden, Colo., Colorado School of Mines, MS thesis, 96 p. <br /> <br />2. Adams, A.M., 1984, Infestation of Fundulus kmlsae (Garman) (Pisces: Cyprinodontidae) by the <br />copepod Ler/wea cyprinacea Linnaeus, 1758, in the South Platte River, Nebraska: Am. MidI. Nat., <br />v. 112, no. 1, p. 131-137. <br /> <br />Fundulus kal1sae (Garman) is a host for Lernaea cypril1acea Linnaeus, 1758, a copepod, <br />reported for the first time from the South Platte River at Ogallala, Nebraska, in the <br />summer of 1980. The parasitic copepod was not obtained from collections of F. kal1sae <br />taken during the 5 years prior to 1980, nor during the 2 summers thereafter (1981- <br />1982). The introduction of the copepod in 1980 followed flooding of the river and <br />surrounding areas. The parasite was eliminated from the study area by the following <br />summer and was probably affected by a low winter population and a spring flood of <br />lesser magnitude than that of 1980. The parasite population was clumped <br />(overdispersed) and both the negative binomial and log-series distributions provided <br />good fits to the observed data, with the log-series giving a closer fit for the entire <br />copepod population as well as for the subpopulations of adult and larval copepods. <br /> <br />3. Adams, A.M., 1985, Parasites on the gills of the plains killifish, FUl1dulus kal1sae, in the South <br />Platte River, Nebraska: Transactions Am. Microsc. Soc., v. 104, no. 3, p. 278-284. <br /> <br />4. Adams, A.M., 1986, The parasite community on the gills of FUl1dulus kal1sae (Garman) from the <br />South Platte River, Nebraska: Acta Parasitol. Pol., v. 31, no. 6, p. 47-54. <br /> <br />5. Adams, J.W. and Sharp, W.N., 1970, Thalenite in the white cloud pegmatite, South Platte <br />District, Jefferson County, Colorado (abstr.), in Geological Association of Canada-Mineralogical <br />Association of Canada, Joint Annual Meetings, Abstracts of Papers: Winnipeg, Manitoba, <br />CClntlda. <br /> <br />6. Adams, J,W., and Sharp, W.N., 1972, Thalenite and allanite derived from yttrofluorite in the <br />White Cloud Pegmatite, South Platte area, Colorado: U.S. Geological Survey Professional Paper <br />800-C, C63-C69 p. <br /> <br />Third reported occurrence of thalenite in North America, rare earth X-ray fluorescence <br />analyses of thalenite, allanite, yttrian fluorite, and yttrofluorite <br /> <br />7. Ahern, J., and Baird, C, 1983, Acid precipitation in southeastern Wyoming: Laramie, Wyo., <br />Wyoming Water Research Center, W84- 00639; OWRT-A-032-WYO(I), 105 p. <br /> <br />Snowfall, snow pack, and rainfall samples were collected in Laramie, Wyoming and in <br />the Snowy Range west of Laramie from March to June 1981 to determine the <br />occurrence and sources of acid precipitation in southeast Wyoming. Electrodes <br />measured different pH values in the samples; however, fast-response electrodes <br />yielded higher and apparently more accurate pH measurements. The pH values in the <br />Laramie precipitation and snow pack were typically greater t'han 5.0, but all the Snowy <br />Range snow pack pH values were less than 5.0. The lower pH values in the Snowy <br />Range snowpack were caused by higher concentrations of the acid-forming nitrate and <br /> <br />8 Bibliography of Water-Related Studies, South Platte River Basln--Colorado, Nebraska, and Wyoming <br />