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M.L. Jones

Publications and source records attributed to M.L. Jones.

At least 19 recordsLinked to original sources

Thiamine and fatty acid content of Lake Michigan Chinook salmon

Nutritional status of Lake Michigan Chinook salmon (Oncorhynchus tshawytscha) is inadequately documented. An investigation was conducted to determine muscle and liver thiamine content and whole body fatty acid composition in small, medium and large Chinook salmon. Muscle and liver thiamine concentrations were highest in small salmon, and tended to decrease with increasing fish size. Muscle thiamine was higher in fall than spring in large salmon. The high percentage of Chinook salmon (24-32% in fall and 58-71% in spring) with muscle thiamine concentration below 500 pmol/g, which has been associated with loss of equilibrium and death in other Great Lake salmonines, suggest that Chinook appear to rely less on thiamine than other Great Lakes species for which such low concentrations would be associated with thiamine deficiency (Brown et al. 2005b). A positive correlation was observed between liver total thiamine and percent liver lipids (r = 0.53, P < 0.0001, n = 119). In medium and large salmon, liver lipids were observed to be low in fish with less than 4,000 pmol/g liver total thiamine. In individuals with greater than 4,000 pmol/g liver thiamine, liver lipid increased with thiamine concentration. Individual fatty acids declined between fall and spring. Essential omega-3 fatty acids appear to be conserved as lipid content declined. Arachidonic acid (C20:4n6), an essential omega-6 fatty acid was not different between fall and spring, although the sum of omega-6 (Sw6) fatty acids declined over winter. Elevated concentrations of saturated fatty acids (sum) were observed in whole body tissue lipid. In summary, thiamine, a dietary essential vitamin, and individual fatty acids were found to vary in Lake Michigan Chinook salmon by fish size and season of the year.

Journal of Great Lakes Research↗

Low-head sea lamprey barrier effects on stream habitat and fish communities in the Great Lakes basin

Low-head barriers are used to block adult sea lamprey (Petromyzon marinus) from upstream spawning habitat. However, these barriers may impact stream fish communities through restriction of fish movement and habitat alteration. During the summer of 1996, the fish community and habitat conditions in twenty-four stream pairs were sampled across the Great Lakes basin. Seven of these stream pairs were re-sampled in 1997. Each pair consisted of a barrier stream with a low-head barrier and a reference stream without a low-head barrier. On average, barrier streams were significantly deeper (df = 179, P = 0.0018) and wider (df = 179, P = 0.0236) than reference streams, but temperature and substrate were similar (df = 183, P = 0.9027; df = 179, P = 0.999). Barrier streams contained approximately four more fish species on average than reference streams. However, streams with low-head barriers showed a greater upstream decline in species richness compared to reference streams with a net loss of 2.4 species. Barrier streams also showed a peak in richness directly downstream of the barriers, indicating that these barriers block fish movement upstream. Using S??renson's similarity index (based on presence/absence), a comparison of fish community assemblages above and below low-head barriers was not significantly different than upstream and downstream sites on reference streams (n = 96, P > 0.05), implying they have relatively little effect on overall fish assemblage composition. Differences in the frequency of occurrence and abundance between barrier and reference streams was apparent for some species, suggesting their sensitivity to barriers.

Conference Paper↗

Water resources data, Idaho, water year 1994: Volume 1. Great Basin and Snake River Basin above King Hill

Water resources data for the 1994 water year for Idaho consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of groundwater. The two volumes of this report contain discharge records for 191 stream-gaging stations and 36 irrigation diversions; stage only records for 4 stream-gaging stations; stage only for 9 lakes and reservoirs; contents only for 23 lakes and reservoirs; water-quality for 67 stream-gaging stations, 444 wells, and 6 lake sites; daily totals for 1 precipitation gage; and water levels for 553 observation wells. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data, Idaho, water year 1994: Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill

Water resources data for the 1994 water year for Idaho consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of groundwater. The two volumes of this report contain discharge records for 191 stream-gaging stations and 36 irrigation diversions; stage only records for 4 stream-gaging stations; stage only for 9 lakes and reservoirs; contents only for 23 lakes and reservoirs; water-quality for 67 stream-gaging stations, 444 wells, and 6 lake sites; daily totals for 1 precipitation gage; and water levels for 553 observation wells. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data, Idaho, water year 1993: Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill

Water resources data for the 1993 water year for Idaho consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. The two volumes of this report contain discharge records for 189 stream-gaging stations and 39 irrigation diversions; stage only records for 4 stream-gaging stations; stage only for 7 lakes and reservoirs; contents only for 23 lakes and reservoirs; water-quality for 61 stream-gaging stations, 489 wells, and 6 lake sites; daily totals for 1 precipitation gage; and water levels for 571 observation wells. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data, Idaho, water year 1992: Volume 1. Great Basin and Snake River Basin above King Hill

Water resources data for the 1992 water year for Idaho consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. The two volumes of this report contain discharge records for 194 stream-gaging stations and 42 irrigation diversions; stage only records for 4 stream-gaging stations; stage only for 7 lakes and reservoirs; contents only for 24 lakes and reservoirs; water-quality for 50 stream-gaging stations, 400 wells, and 11 lakes; daily totals for 1 precipitation gage; and water levels for 475 observation wells. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data, Idaho, water year 1992: Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill

Water resources data for the 1992 water year for Idaho consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. The two volumes of this report contain discharge records for 194 stream-gaging stations and 42 irrigation diversions; stage only records for 4 stream-gaging stations; stage only for 7 lakes and reservoirs; contents only for 24 lakes and reservoirs; water-quality for 50 stream-gaging stations, 400 wells, and 11 lakes; daily totals for 1 precipitation gage; and water levels for 475 observation wells. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data, Idaho, water year 1993: Volume 1. Great Basin and Snake River Basin above King Hill

Water resources data for the 1993 water year for Idaho consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. The two volumes of this report contain discharge records for 189 stream-gaging stations and 39 irrigation diversions; stage only records for 4 stream-gaging stations; stage only for 7 lakes and reservoirs; contents only for 23 lakes and reservoirs; water-quality for 61 stream-gaging stations, 489 wells, and 6 lake sites; daily totals for 1 precipitation gage; and water levels for 571 observation wells. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S.Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data, Idaho, water year 1991: Volume 1. Great Basin and Snake River Basin above King Hill

Water resources data for the 1991 water year for Idaho consist of records ofstage, discharge, and water quality of streams; stage, contents, and water qualityof lakes and reservoirs; discharge of irrigation diversions; and water levels andwater quality of ground water. The two volumes of this report contain dischargerecords for 197 stream-gaging stations and 38 irrigation diversions; stage onlyrecords for 6 stream-gaging stations; stage only for 7 lakes and reservoirs;contents only for 23 lakes and reservoirs; water-quality for 50 stream-gagingstations, 400 wells, and 11 lakes; daily totals for 1 precipitation gage; andwater levels for 475 observation wells. Additional water data were collected atvarious sites not involved in the systematic data collection program and arepublished as miscellaneous measurements. These data represent that part of theNational Water Data System operated by the U.S. Geological Survey and cooperatingState and Federal Agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data, Idaho, water year 1991: Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill

Water resources data for the 1991 water year for Idaho consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. The two volumes of this report contain discharge records for 197 stream-gaging stations and 38 irrigation diversions; stage only records for 6 stream-gaging stations; stage only for 7 lakes and reservoirs; contents only for 23 lakes and reservoirs; water-quality for 50 stream-gaging stations, 400 wells, and 11 lakes; daily totals for 1 precipitation gage; and water levels for 475 observation wells. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal Agencies in Idaho, adjacent States, and Canada.

Idaho↗

Aquifer-test results, direction of ground-water flow, and 1984-90 annual ground-water pumpage for irrigation, lower Big Lost River Valley, Idaho

The study area (see index map of Idaho), part of the Big Lost River drainage basin, is at the northern side of the eastern Snake River Plain. The lower Big Lost River Valley extends from the confluence of Antelope Creek and the Big Lost River to about 4 mi south of Arco and encompasses about 145 mi 2 (see map showing water-level contours). The study area is about 18 mi long and, at its narrowest, 4 mi wide. Arco, Butte City, and Moore, with populations of 1,016, 59, and 190, respectively, in 1990, are the only incorporated towns. The entire study area, except the extreme northwestern part, is in Butte City. The study area boundary is where alluvium and colluvium pinch out and abut against the White Knob Mountains (chiefly undifferentiated sedimentary rock with lesser amounts of volcanic rock) on the west and the Lost River Range (chiefly sedimentary rock) on the east. Gravel and sand in the valley fill compose the main aquifer. The southern boundary is approximately where Big Lost River valley fill intercalates with or abuts against basalt of the Snake River Group. Spring ground-water levels and flow in the Big Lost River depend primarily on temperature and the amount and timing of precipitation within the entire drainage basin. Periods of abundant water supply and water shortages are, therefore, related to the amount of annual precipitation. Surface reservoir capacity in the valley (Mackay Reservoir, about 20 mi northwest of Moore) is only 20 percent of the average annual flow of the Big Lost River (Crosthwaite and others, 1970, p. 3). Stored surface water is generally unavailable for carryover from years of abundant water supply to help relieve drought conditions in subsequent years. Many farmers have drilled irrigation wells to supplement surface-water supplies and to increase irrigated acreage. Average annual flow of the Big Lost River below Mackay Reservoir near Mackay (gaging station 13127000, not shown) in water years 1905, 1913-14, and 1920-90 was about 224,600 acre-ft; average annual flow of the Big Lost River near Arco (gaging station 13132500; see map showing water-level contours) in water years 1947-61, 1967-80, and 1983-90 was about 79,000 acre-ft (Harenberg and others, 1991, p. 254-255). Moore Canal and East Side Ditch divert water from the Big Lost River at the Moore Diversion, 3 mi north of Moore (see map showing water-level contours) and supply water for irrigation near the margins of the valley. When water supply is average or greater, water in the Big Lost River flows through the study area and onto the Snake River Plain, where it evaporates or infiltrates into the Snake River Plain aquifer. When water supply is below average, water in the Big Lost River commonly does not reach Arco; rather, it is diverted for irrigation in the interior of the valley, evaporates, or infiltrates to the valley-fill aquifer. This report describes the results of a study by the U.S. Geological Survey, in cooperation with the Idaho Department of Water Resources, to collect hydrologic data needed to help address water-supply problems in the Big Lost River Valley. Work involved (1) field inventory of 81 wells, including 46 irrigation wells; (2) measurement of water levels in 154 wells in March 1991; (3) estimation of annual ground-water pumpage for irrigation from 1984 through 1990; and (4) analysis of results of an aquifer test conducted southwest of Moore. All data obtained during this study may be inspected at the U.S. Geological Survey, Idaho District office, Boise.

Idaho↗

Water resources data, Idaho, water year 1990

Water resources data for the 1990 water year for Idaho consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. This report contains discharge records for 202 stream-gaging stations and 41 irrigation diversions; stage only records for 2 stream-gaging stations; stage only for 6 lakes and reservoirs; contents only for 21 lakes and reservoirs; water quality for 50 stream-gaging stations, 97 wells, and 1 lake; daily totals for 1 precipitation gage; and water levels for 473 observation wells. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Results of test drilling and hydrologic monitoring in the Indian Bathtub area, Owyhee County, southwestern Idaho, January 1989 through September 1990

This report presents data collected during the period January 1989 through September 1990 from eight test holes and selected thermal-water wells and springs in the Indian Bathtub area, southwestern Idaho. The data include completion, lithologic, and gamma logs for eight test holes, hydrographs of water levels in the test holes and ten other wells, hydrographs of discharges at four springs, and chemical and isotopic analyses of water from six of the test holes. These data were collected as part of a continuing study to determine the cause or causes of decreased discharge at Indian Bathtub Spring and other thermal springs along Hot Creek.

Idaho↗

Water resources data, Idaho, water year 1989

Water resources data for the 1989 water year for Idaho consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. This report contains discharge records for 207 stream-gaging stations; 43 irrigation diversions; stage only records for 2 stream-gaging stations; stage only for 8 lakes and reservoirs; contents only for 23 lakes and reservoirs; water quality for 44 stream-gaging stations, 150 wells, and 1 lake; and water levels for 452 observation wells. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data for Idaho, water year 1988

Water resources data for the 1988 water year for Idaho consist of records ofstage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; discharge of irrigation diversions; and water levels and water quality of ground water. This report contains discharge records for 208 stream-gaging stations; 36 irrigation diversions; stage only records for 2 stream-gaging stations; stage only for 8 lakes and reservoirs; contents only for 23 lakes and reservoirs; water quality for 25 stream-gaging stations, 64 wells, and 1 lake; and water levels for 452 observation wells. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Idaho, adjacent States, and Canada.

Idaho↗

Water resources data for Idaho, water year 1987

Water resources data for the 1987 water year for Idaho consist of records ofstage, discharge, and water quality of streams; stage, contents, and water qualityof lakes and reservoirs; and water levels and water quality of ground water. Thisreport contains discharge records for 230 gaging stations; stage only records for2 gaging stations; stage only for 11 lakes and reservoirs; contents only for 25 lakesand reservoirs; water quality for 24 gaging stations and 52 wells; and water levelsfor 467 observation wells. Additional water data were collected at various sites, notinvolved in the systematic data collection program, and are published as miscellaneousmeasurements. These data represent that part of the National Water Data System operatedby the U.S. Geological Survey and cooperating State and Federal agencies in Idaho,adjacent States, and Canada.

Idaho↗

Selected water-quality data for the Burley irrigation district, south-central Idaho, March-April, 1987

This map report presents selected March-April 1987, water quality data, principally dissolved nitrite plus nitrate as nitrogen, and depth-to-water measurements for 118 wells in the Burley Irrigation District, south-central Idaho. Nitrogen concentrations ranged from 0.37 to 30 mg/L; the median concentration was 8.0 mg/L. Nitrogen concentrations in 19 wells equaled or exceeded the U.S. Environmental Protection Agency public drinking water limit of 10 mg/L. (USGS)

Idaho↗