{"pageNumber":"2883","pageRowStart":"72050","pageSize":"25","recordCount":184617,"records":[{"id":70026213,"text":"70026213 - 2003 - Predator selection of prairie landscape features and its relation to duck nest success","interactions":[],"lastModifiedDate":"2018-01-04T13:05:14","indexId":"70026213","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Predator selection of prairie landscape features and its relation to duck nest success","docAbstract":"Mammalian predation is a major cause of mortality for breeding waterfowl in the U.S. Northern Great Plains, and yet we know little about the selection of prairie habitats by predators or how this influences nest success in grassland nesting cover. We selected 2 41.4-km2 study areas in both 1996 and 1997 in North Dakota, USA, with contrasting compositions of perennial grassland. A study area contained either 15-20% perennial grassland (Low Grassland Composition [LGC]) or 45-55% perennial grassland (High Grassland Composition [HGC]). We used radiotelemetry to investigate the selection of 9 landscape cover types by red fox (Vulpes vulpes) and striped skunk (Mephitis mephitis), while simultaneously recording duck nest success within planted cover. The cover types included the edge and core areas of planted cover, wetland edges within planted cover or surrounded by cropland, pastureland, hayland, cropland, roads, and miscellaneous cover types. Striped skunks selected wetland edges surrounded by agriculture over all other cover types in LGC landscapes (P-values for all pairwise comparisons were <0.05). Striped skunks also selected wetland edges surrounded by agriculture over all other cover types in HGC landscapes (P < 0.05), except for wetland edges within planted cover (P = 0.12). Red foxes selected the edge and core areas of planted cover, as well as wetland edges within planted cover in LGC landscapes (i.e., they were attracted to the more isolated patches of planted cover). However, in HGC landscapes, red foxes did not select interior areas of planted cover (i.e., core areas of planted cover and wetland edges in planted cover) as frequently as edges of planted cover (P < 0.05). Red foxes selected core areas of planted cover more frequently in LGC than in HGC landscapes (P < 0.05) and selected pastureland more frequently in HGC than in LGC landscapes (P < 0.05). Furthermore, red foxes selected the isolated patches of planted cover more than pastureland in LGC landscapes (P < 0.05). Duck nest success was greater in HGC landscapes than in LGC landscapes for planted-cover core (P < 0.0001), planted-cover edge (P < 0.001) and planted cover-wetland edge (P < 0.001). Both the increased amount of planted-cover core area and the increased pastureland selection in HGC landscapes may have diluted predator foraging efficiency in the interior areas of planted cover and contributed to higher nest success in HGC landscapes. Our observations of predator cover-type selection not only support the restoration and management of large blocks of grassland but also indicate the influence of alternative cover types for mitigating nest predation in the Prairie Pothole Region.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0022541X","usgsCitation":"Phillips, M., Clark, W., Sovada, M., Horn, D., Koford, R.R., and Greenwood, R.J., 2003, Predator selection of prairie landscape features and its relation to duck nest success: Journal of Wildlife Management, v. 67, no. 1, p. 104-114.","productDescription":"11 p.","startPage":"104","endPage":"114","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":234596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8174e4b0c8380cd7b536","contributors":{"authors":[{"text":"Phillips, M.L.","contributorId":68249,"corporation":false,"usgs":true,"family":"Phillips","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":408584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, W.R.","contributorId":70716,"corporation":false,"usgs":true,"family":"Clark","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":408585,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sovada, M.A.","contributorId":54534,"corporation":false,"usgs":true,"family":"Sovada","given":"M.A.","affiliations":[],"preferred":false,"id":408583,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Horn, D.J.","contributorId":80614,"corporation":false,"usgs":true,"family":"Horn","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":408587,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Koford, Rolf R.","contributorId":16347,"corporation":false,"usgs":true,"family":"Koford","given":"Rolf","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":408582,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Greenwood, R. J.","contributorId":74326,"corporation":false,"usgs":true,"family":"Greenwood","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":408586,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":1013529,"text":"1013529 - 2003 - Correlates to survival of juvenile sea otters in Prince William Sound, Alaska, 1992-1993","interactions":[],"lastModifiedDate":"2017-06-28T15:42:14","indexId":"1013529","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Correlates to survival of juvenile sea otters in Prince William Sound, Alaska, 1992-1993","docAbstract":"We estimated survival of sea otters (Enhydra lutris) for 1 year post weaning during 1992-1993 in Prince William Sound (PWS), location of the 1989 Exxon Valdez oil spill. We sampled 38 pups in eastern PWS (EPWS), an unoiled area occupied by sea otters for <15 years, and 33 pups from oiled western PWS (WPWS), occupied for >25 years. We compared survival between areas, sexes, and condition groups. We also examined the relation of blood parameters to survival. Survival was estimated at 0.74 in EPWS and 0.52 in WPWS. Female survival was 0.86 in EPWS and 0.64 in WPWS, whereas male survival was lower, 0.61 in EPWS and 0.44 in WPWS. Sea otters from EPWS were in better condition (mass/length) than WPWS sea otters. Pups in better condition had higher survival in EPWS but not in WPWS. Foraging success was greater in EPWS than in WPWS, consistent with either an effect of length of occupation or the effects of oil on the prey base or a combination of these effects. Area differences in blood parameters suggested liver damage in WPWS sea otters, perhaps resulting from continued exposure to oil. Thus, both length of occupation and oiling history likely influenced juvenile survival in PWS.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Zoology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Ballachey, B.E., Bodkin, J.L., Howlin, S., Doroff, A., and Rebar, A., 2003, Correlates to survival of juvenile sea otters in Prince William Sound, Alaska, 1992-1993: Canadian Journal of Zoology, v. 81, no. 9, p. 1494-1510.","productDescription":"pp. 1494-1510","startPage":"1494","endPage":"1510","numberOfPages":"17","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":128475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":11259,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.nrc-cnrc.gc.ca/cgi-bin/rp/rp2_abst_e?cjz_z03-121_81_ns_nf_cjz9-03","linkFileType":{"id":5,"text":"html"}}],"volume":"81","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6849aa","contributors":{"authors":[{"text":"Ballachey, Brenda E. 0000-0003-1855-9171 bballachey@usgs.gov","orcid":"https://orcid.org/0000-0003-1855-9171","contributorId":2966,"corporation":false,"usgs":true,"family":"Ballachey","given":"Brenda","email":"bballachey@usgs.gov","middleInitial":"E.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":318736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bodkin, James L. 0000-0003-1641-4438 jbodkin@usgs.gov","orcid":"https://orcid.org/0000-0003-1641-4438","contributorId":748,"corporation":false,"usgs":true,"family":"Bodkin","given":"James","email":"jbodkin@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":318735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howlin, S.","contributorId":94624,"corporation":false,"usgs":true,"family":"Howlin","given":"S.","affiliations":[],"preferred":false,"id":318739,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Doroff, A. M.","contributorId":92995,"corporation":false,"usgs":false,"family":"Doroff","given":"A. M.","affiliations":[],"preferred":false,"id":318738,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rebar, A.H.","contributorId":40150,"corporation":false,"usgs":true,"family":"Rebar","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":318737,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70025799,"text":"70025799 - 2003 - Paleolimnology of Lake Tanganyika, East Africa, over the past 100 k yr","interactions":[],"lastModifiedDate":"2012-03-12T17:20:32","indexId":"70025799","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Paleolimnology of Lake Tanganyika, East Africa, over the past 100 k yr","docAbstract":"New sediment core data from a unique slow-sedimentation rate site in Lake Tanganyika contain a much longer and continuous record of limnological response to climate change than have been previously observed in equatorial regions of central Africa. The new core site was first located through an extensive seismic reflection survey over the Kavala Island Ridge (KIR), a sedimented basement high that separates the Kigoma and Kalemie Basins in Lake Tanganyika. Proxy analyses of paleoclimate response carried out on core T97-52V include paleomagnetic and index properties, TOC and isotopic analyses of organic carbon, and diatom and biogenic silica analyses. A robust age model based on 11 radiocarbon (AMS) dates indicates a linear, continuous sedimentation rate nearly an order of magnitude slower here compared to other core sites around the lake. This age model indicates continuous sedimentation over the past 79 k yr, and a basal age in excess of 100 k yr. The results of the proxy analyses for the past ??? 20 k yr are comparable to previous studies focused on that interval in Lake Tanganyika, and show that the lake was about 350 m lower than present at the Last Glacial Maximum (LGM). Repetitive peaks in TOC and corresponding drops in ??13C over the past 79 k yr indicate periods of high productivity and mixing above the T97-52V core site, probably due to cooler and perhaps windier conditions. From ??? 80 through ??? 58 k yr the ??13C values are relatively negative (-26 to -28???) suggesting predominance of algal contributions to bottom sediments at this site during this time. Following this interval there is a shift to higher values of ??13C, indicating a possible shift to C-4 pathway-dominated grassland-type vegetation in the catchment, and indicating cooler, dryer conditions from ??? 55 k yr through the LGM. Two seismic sequence boundaries are observed at shallow stratigraphic levels in the seismic reflection data, and the upper boundary correlates to a major discontinuity near the base of T97-52V. We interpret these discontinuities to reflect major, prolonged drops in lake level below the core site (393 m), with the lower boundary correlating to marine oxygen isotope Stage 6. This suggests that the previous glacial period was considerably cooler and more arid in the equatorial tropics than was the last glacial period.","largerWorkTitle":"Journal of Paleolimnology","language":"English","doi":"10.1023/A:1025522116249","issn":"09212728","usgsCitation":"Scholz, C., King, J., Ellis, G., Swart, P.K., Stager, J., and Colman, S.M., 2003, Paleolimnology of Lake Tanganyika, East Africa, over the past 100 k yr, <i>in</i> Journal of Paleolimnology, v. 30, no. 2, p. 139-150, https://doi.org/10.1023/A:1025522116249.","startPage":"139","endPage":"150","numberOfPages":"12","costCenters":[],"links":[{"id":487517,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.uri.edu/gsofacpubs/1734","text":"External Repository"},{"id":208849,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1023/A:1025522116249"},{"id":234902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a73fee4b0c8380cd77395","contributors":{"authors":[{"text":"Scholz, C.A.","contributorId":76810,"corporation":false,"usgs":true,"family":"Scholz","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":406620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, J.W.","contributorId":19265,"corporation":false,"usgs":true,"family":"King","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":406619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, G.S. 0000-0003-4519-3320","orcid":"https://orcid.org/0000-0003-4519-3320","contributorId":91064,"corporation":false,"usgs":true,"family":"Ellis","given":"G.S.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":406623,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swart, Peter K.","contributorId":96832,"corporation":false,"usgs":false,"family":"Swart","given":"Peter","email":"","middleInitial":"K.","affiliations":[{"id":5112,"text":"University of Miami","active":true,"usgs":false}],"preferred":false,"id":406624,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stager, J.C.","contributorId":88923,"corporation":false,"usgs":true,"family":"Stager","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":406622,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Colman, Steven M. 0000-0002-0564-9576","orcid":"https://orcid.org/0000-0002-0564-9576","contributorId":77482,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":406621,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70025545,"text":"70025545 - 2003 - Role of colloidal material in the removal of 234Th in the Canada basin of the Arctic Ocean","interactions":[],"lastModifiedDate":"2012-03-12T17:21:00","indexId":"70025545","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1370,"text":"Deep-Sea Research Part I: Oceanographic Research Papers","active":true,"publicationSubtype":{"id":10}},"title":"Role of colloidal material in the removal of 234Th in the Canada basin of the Arctic Ocean","docAbstract":"The phase partitioning of 234Th between dissolved (< 10-kiloDalton, kD), colloidal (10 kD - 0.4 ??m), and particulate (???0.5 ??m) matter across a horizontal transect, from a coastal station to the deep Canada Basin, and a vertical profile in the deep Canada Basin of the western Arctic Ocean was investigated. Concentrations of suspended particulate matter (SPM), dissolved, colloidal and particulate organic carbon, particulate organic nitrogen and nutrients (silicate, phosphate and nitrate) were also measured to assess transport and scavenging processes. Total 234Th (colloidal + particulate + dissolved) indicated deficiencies relative to secular equilibrium with its parent, 238U in the upper 100 m, which suggests active scavenging of 234Th onto particle surfaces. In contrast, at depths > 200m, general equilibrium existed between total 234Th and 238U. The inventory of SPM and the specific activity of particulate 234Th in the Canada Basin was about an order of magnitude higher than the profile reported for the Alpha Ridge ice camp station. This higher concentration of SPM in the southwestern Canada Basin is likely derived from ice-rafted sedimentary particles. Inventories of nutrients, and dissolved organic carbon and nitrogen in the upper 100 m of the Canada Basin are comparable to the other estimates for the central Arctic Ocean. Comparison of the mass concentrations of colloidal and filter-retained particulate matter as well as the activity of 234Th in these phases indicates that only a very small component of the colloidal material is actively involved in Th scavenging. Lower values of the conditional partition coefficient between the colloidal and dissolved phase indicate that the Arctic colloids are less reactive than colloidal material from other regions. The conditional partition coefficient between the filter-retained and dissolved phases (Kf) is generally higher than that for other regions, which is attributed to the higher complexation capacity of glacio-marine sedimentary particles in these waters. The 234Th-derived export of POC for the shelf and deep Canada Basin ranges between 5.6 and 6.5 mmol m-2 d-1, and is in agreement with other estimates reported for the central Arctic Ocean and Beaufort Sea. ?? 2003 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Deep-Sea Research Part I: Oceanographic Research Papers","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0967-0637(03)00140-7","issn":"09670637","usgsCitation":"Baskaran, M., Swarzenski, P., and Porcelli, D., 2003, Role of colloidal material in the removal of 234Th in the Canada basin of the Arctic Ocean: Deep-Sea Research Part I: Oceanographic Research Papers, v. 50, no. 10-11, p. 1353-1373, https://doi.org/10.1016/S0967-0637(03)00140-7.","startPage":"1353","endPage":"1373","numberOfPages":"21","costCenters":[],"links":[{"id":236049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209509,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0967-0637(03)00140-7"}],"volume":"50","issue":"10-11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aae4be4b0c8380cd87079","contributors":{"authors":[{"text":"Baskaran, M.","contributorId":96627,"corporation":false,"usgs":true,"family":"Baskaran","given":"M.","affiliations":[],"preferred":false,"id":405598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swarzenski, P.W. 0000-0003-0116-0578","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":29487,"corporation":false,"usgs":true,"family":"Swarzenski","given":"P.W.","affiliations":[],"preferred":false,"id":405596,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Porcelli, D.","contributorId":35912,"corporation":false,"usgs":true,"family":"Porcelli","given":"D.","email":"","affiliations":[],"preferred":false,"id":405597,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1008615,"text":"1008615 - 2003 - Large carnivores response to recreational big game hunting along the Yellowstone National Park and Absaroka-Beartooth Wilderness boundary","interactions":[],"lastModifiedDate":"2017-05-10T12:23:01","indexId":"1008615","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Large carnivores response to recreational big game hunting along the Yellowstone National Park and Absaroka-Beartooth Wilderness boundary","docAbstract":"<p><span>The Greater Yellowstone Ecosystem contains the rare combination of an intact guild of native large carnivores, their prey, and differing land management policies (National Park versus National Forest; no hunting versus hunting). Concurrent field studies on large carnivores allowed us to investigate activities of humans and carnivores on Yellowstone National Park's (YNP) northern boundary. Prior to and during the backcountry big-game hunting season, we monitored movements of grizzly bears (<i>Ursus arctos</i>), wolves (<i>Canis</i> <i>lupus</i>), and cougars (<i>Puma concolor</i>) on the northern boundary of YNP. Daily aerial telemetry locations (September 1999), augmented with weekly telemetry locations (August and October 1999), were obtained for 3 grizzly bears, 7 wolves in 2 groups of 1 pack, and 3 cougars in 1 family group. Grizzly bears were more likely located inside the YNP boundary during the pre-hunt period and north of the boundary once hunting began. The cougar family tended to be found outside YNP during the pre-hunt period and moved inside YNP when hunting began. Wolves did not significantly change their movement patterns during the pre-hunt and hunting periods. Qualitative information on elk (<i>Cervus elaphus</i>) indicated they moved into YNP once hunting started, suggesting that cougars followed living prey or responded to hunting activity, grizzly bears focused on dead prey (e.g., gut piles, crippled elk), and wolves may have taken advantage of both. Measures of association (Jacob's Index) were positive within carnivore species but inconclusive among species. Further collaborative research and the use of new technologies such as Global Positioning System (GPS) telemetry collars will advance our ability to understand these species, the carnivore community and its interactions, and human influences on carnivores.</span></p>","language":"English","publisher":"Wiley","usgsCitation":"Ruth, T., Smith, D., Haroldson, M., Buotte, P., Schwartz, C., Quigley, H., Cherry, S., Tyres, D., and Frey, K., 2003, Large carnivores response to recreational big game hunting along the Yellowstone National Park and Absaroka-Beartooth Wilderness boundary: Wildlife Society Bulletin, v. 31, no. 4, p. 1150-1161.","productDescription":"12 p.","startPage":"1150","endPage":"1161","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":131061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269040,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/3784463"}],"volume":"31","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a90fd","contributors":{"authors":[{"text":"Ruth, T.E.","contributorId":52468,"corporation":false,"usgs":true,"family":"Ruth","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":318247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, D.W.","contributorId":24726,"corporation":false,"usgs":true,"family":"Smith","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":318243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haroldson, M.A. 0000-0002-7457-7676","orcid":"https://orcid.org/0000-0002-7457-7676","contributorId":108047,"corporation":false,"usgs":true,"family":"Haroldson","given":"M.A.","affiliations":[],"preferred":false,"id":318250,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buotte, P.C.","contributorId":105480,"corporation":false,"usgs":true,"family":"Buotte","given":"P.C.","affiliations":[],"preferred":false,"id":318248,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schwartz, C.C.","contributorId":33658,"corporation":false,"usgs":true,"family":"Schwartz","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":318244,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Quigley, H.B.","contributorId":15325,"corporation":false,"usgs":true,"family":"Quigley","given":"H.B.","email":"","affiliations":[],"preferred":false,"id":318242,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cherry, S.","contributorId":50480,"corporation":false,"usgs":true,"family":"Cherry","given":"S.","email":"","affiliations":[],"preferred":false,"id":318246,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tyres, D.","contributorId":46384,"corporation":false,"usgs":true,"family":"Tyres","given":"D.","email":"","affiliations":[],"preferred":false,"id":318245,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Frey, K.","contributorId":106837,"corporation":false,"usgs":true,"family":"Frey","given":"K.","email":"","affiliations":[],"preferred":false,"id":318249,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70025327,"text":"70025327 - 2003 - Effects of soil amendments on germination and emergence of downy brome (Bromus tectorum) and Hilaria jamesii","interactions":[],"lastModifiedDate":"2017-11-21T17:53:34","indexId":"70025327","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3738,"text":"Weed Science","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Effects of soil amendments on germination and emergence of downy brome (<i>Bromus tectorum</i>) and <i>Hilaria jamesii</i>","title":"Effects of soil amendments on germination and emergence of downy brome (Bromus tectorum) and Hilaria jamesii","docAbstract":"<div class=\"row\"><div class=\"large-10 medium-10 small-12 columns\"><div class=\"description\"><div class=\"abstract\" data-abstract-type=\"normal\"><p>Downy brome is an introduced Mediterranean annual grass that now dominates millions of hectares of western U.S. rangelands. The presence of this grass has eliminated many native species and accelerated wildfire cycles. The objective of this study was to identify soil additives that allowed germination but inhibited emergence of downy brome, while not affecting germination or emergence of the native perennial grass <span class=\"italic\">Hilaria jamesii</span>. On the basis of data from previous studies, we focused on additives that altered the availability of soil nitrogen (N), phosphorus (P), and potassium (K). Most water-soluble treatments inhibited downy brome germination and emergence. We attribute the inhibitory effects of these treatments to excessive salinity and ion-specific effects of the additives themselves. An exception to this was oxalic acid, which showed no effect. Most water-insoluble treatments had no effect in soils with high P but did have an effect in soils with low P. Zeolite was effective regardless of P level, probably due to the high amounts of Na<span class=\"sup\">+</span> it added to the soil solution. Most treatments at higher concentrations resulted in lower downy brome emergence rates in soils currently dominated by downy brome than in uninvaded (but theoretically invadable) <span class=\"italic\">Hilaria</span> soils. This difference is possibly attributable to inherent differences in labile soil P. In <span class=\"italic\">Stipa</span> soils, where <span class=\"italic\">Stipa</span> spp. grow, but which are generally considered to be uninvadable by downy brome, additions of high amounts of N resulted in lower emergence. This may have been an effect of NH<span class=\"sub\">4</span> <span class=\"sup\">+</span> interference with uptake of K or other cations or toxicity of high N. We also saw a positive relationship between downy brome emergence and pH in <span class=\"italic\">Stipa</span> soils. <span class=\"italic\">Hilaria</span> development parameters were not as susceptible to the treatments, regardless of concentration, as downy brome. Our results suggest that there are additions that may be effective management tools for inhibiting downy brome in calcareous soils, including (1) high salt applications, (2) K-reducing additions (e.g., Mg), and (3) P-reducing additions.</p></div></div></div></div>","language":"English","publisher":"Cambridge University Press","doi":"10.1614/0043-1745(2003)051[0371:EOSAOG]2.0.CO;2","usgsCitation":"Belnap, J., Sherrod, S.K., and Miller, M.E., 2003, Effects of soil amendments on germination and emergence of downy brome (Bromus tectorum) and Hilaria jamesii: Weed Science, v. 51, no. 3, p. 371-378, https://doi.org/10.1614/0043-1745(2003)051[0371:EOSAOG]2.0.CO;2.","productDescription":"8 p.","startPage":"371","endPage":"378","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":236186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a07d1e4b0c8380cd51855","contributors":{"authors":[{"text":"Belnap, J. 0000-0001-7471-2279","orcid":"https://orcid.org/0000-0001-7471-2279","contributorId":23872,"corporation":false,"usgs":true,"family":"Belnap","given":"J.","affiliations":[],"preferred":false,"id":404772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherrod, S. K.","contributorId":9209,"corporation":false,"usgs":false,"family":"Sherrod","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":404771,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, M. E.","contributorId":104003,"corporation":false,"usgs":false,"family":"Miller","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":404773,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025484,"text":"70025484 - 2003 - Variable near-surface deformation along the Commerce segment of the Commerce geophysical lineament, southeast Missouri to southern Illinois, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70025484","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Variable near-surface deformation along the Commerce segment of the Commerce geophysical lineament, southeast Missouri to southern Illinois, USA","docAbstract":"Recent studies have demonstrated a plausible link between surface and near-surface tectonic features and the vertical projection of the Commerce geophysical lineament (CGL). The CGL is a 5- to 10-km-wide zone of basement magnetic and gravity anomalies traceable for more than 600 km, extending from Arkansas through southeast Missouri and southern Illinois and into Indiana. Twelve kilometers of high-resolution seismic reflection data, collected at four sites along a 175-km segment of the CGL projection, are interpreted to show varying amounts of deformation involving Tertiary and some Quaternary sediments. Some of the locally anomalous geomorphic features in the northern Mississippi embayment region (i.e., paleoliquefaction features, anomalous directional changes in stream channels, and areas of linear bluff escarpments) overlying the CGL can be correlated with specific faults and/or narrow zones of deformed (faulted and folded) strata that are imaged on high-resolution seismic reflection data. There is an observable change in near-surface deformation style and complexity progressing from the southwest to the northeast along the trace of the CGL. The seismic reflection data collaborate mapping evidence which suggests that this region has undergone a complex history of deformation, some of which is documented to be as young as Quaternary, during multiple episodes of reactivation under varying stress fields. This work, along with that of other studies presented in this volume, points to the existence of at least one major crustal feature outside the currently defined zone of seismic activity (New Madrid Seismic Zone) that should be considered as a significant potential source zone for seismogenic activity within the midcontinent region of the United States. ?? 2003 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Tectonophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0040-1951(03)00156-2","issn":"00401951","usgsCitation":"Odum, J.K., Stephenson, W.J., and Williams, R.A., 2003, Variable near-surface deformation along the Commerce segment of the Commerce geophysical lineament, southeast Missouri to southern Illinois, USA: Tectonophysics, v. 368, no. 1-4, p. 155-170, https://doi.org/10.1016/S0040-1951(03)00156-2.","startPage":"155","endPage":"170","numberOfPages":"16","costCenters":[],"links":[{"id":209593,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0040-1951(03)00156-2"},{"id":236233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"368","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc143e4b08c986b32a4df","contributors":{"authors":[{"text":"Odum, J. K.","contributorId":105705,"corporation":false,"usgs":true,"family":"Odum","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":405378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephenson, W. J.","contributorId":87982,"corporation":false,"usgs":true,"family":"Stephenson","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":405377,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, R. A.","contributorId":82323,"corporation":false,"usgs":true,"family":"Williams","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":405376,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1008249,"text":"1008249 - 2003 - Use of radio telemetry in studies of shorebirds: past contributions and future directions","interactions":[],"lastModifiedDate":"2017-08-26T16:38:47","indexId":"1008249","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3704,"text":"Wader Study Group Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Use of radio telemetry in studies of shorebirds: past contributions and future directions","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wader Study Group Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Warnock, N., and Takekawa, J.Y., 2003, Use of radio telemetry in studies of shorebirds: past contributions and future directions: Wader Study Group Bulletin, v. 100, p. 138-150.","productDescription":"p. 138-150","startPage":"138","endPage":"150","numberOfPages":"13","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"100","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604471","contributors":{"authors":[{"text":"Warnock, N.","contributorId":80615,"corporation":false,"usgs":true,"family":"Warnock","given":"N.","email":"","affiliations":[],"preferred":false,"id":317146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":317145,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70025717,"text":"70025717 - 2003 - Winter-time circulation and sediment transport in the Hudson Shelf Valley","interactions":[],"lastModifiedDate":"2017-10-05T19:04:24","indexId":"70025717","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1333,"text":"Continental Shelf Research","active":true,"publicationSubtype":{"id":10}},"title":"Winter-time circulation and sediment transport in the Hudson Shelf Valley","docAbstract":"The Hudson Shelf Valley is a bathymetric low that extends across the continental shelf offshore of New York and New Jersey. From December 1999 to April 2000 a field experiment was carried out to investigate the transport of sediment in the shelf and valley system. Near-bed tripods and water-column moorings were deployed at water depths from 38 to 75 m in the axis of the shelf valley and at about 26 m on the adjacent shelves offshore of New Jersey and Long Island, New York. These measured suspended sediment concentrations, current velocities, waves, and water column properties. This paper analyzes observations made during December 1999 and January 2000, and presents the first direct near-bed measurements of suspended sediment concentration and sediment flux from the region. Sediment transport within the Hudson Shelf Valley was coherent over tens of kilometers, and usually aligned with the axis of the shelf valley. Down-valley (off-shore) transport was associated with energetic waves, winds from the east, moderate current velocities (5-10 cm/s), and sea level setup at Sandy Hook, NJ. Up-valley (shoreward) transport occurred frequently, and was associated with winds from the west, low wave energy, high current velocities (20-40 cm/s), and sea level set-down at the coast. Within the shelf valley, net sediment flux (the product of near-bed concentration and velocity) was directed shoreward, up the axis of the valley. Current velocities and suspended sediment fluxes on the New York and New Jersey continental shelves were lower than within the shelf valley, and exhibited greater variability in alignment. Longer term meteorological data indicate that wind, setup, and wave conditions during the study period were more conducive to up-valley transport than seasonal data suggest as average. To relate the observed up-valley sediment flux to observed accumulation of contaminants within the Hudson Shelf Valley requires consideration of transport over longer timescales than those observed here, and methods that account for the region's complex bathymetry, sediment distribution, and circulation. ?? 2003 Elsevier Science Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Continental Shelf Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0278-4343(03)00025-6","issn":"02784343","usgsCitation":"Harris, C.K., Butman, B., and Traykovski, P., 2003, Winter-time circulation and sediment transport in the Hudson Shelf Valley: Continental Shelf Research, v. 23, no. 8, p. 801-820, https://doi.org/10.1016/S0278-4343(03)00025-6.","productDescription":"20 p.","startPage":"801","endPage":"820","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":234781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":208785,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0278-4343(03)00025-6"}],"country":"United States","state":"New Jersey, New York","otherGeospatial":"Hudson Shelf Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.59716796875,\n              39.816975090490004\n            ],\n            [\n              -72.542724609375,\n              39.816975090490004\n            ],\n            [\n              -72.542724609375,\n              41.18692242290296\n            ],\n            [\n              -74.59716796875,\n              41.18692242290296\n            ],\n            [\n              -74.59716796875,\n              39.816975090490004\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"23","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd164e4b08c986b32f3de","contributors":{"authors":[{"text":"Harris, C. K.","contributorId":80337,"corporation":false,"usgs":true,"family":"Harris","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":406291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butman, B.","contributorId":85580,"corporation":false,"usgs":true,"family":"Butman","given":"B.","email":"","affiliations":[],"preferred":false,"id":406292,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Traykovski, P.","contributorId":76484,"corporation":false,"usgs":true,"family":"Traykovski","given":"P.","affiliations":[],"preferred":false,"id":406290,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025216,"text":"70025216 - 2003 - Origin of high-grade gold ore, source of ore fluid components, and genesis of the Meikle and neighboring Carlin-type deposits, Northern Carlin Trend, Nevada","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70025216","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of high-grade gold ore, source of ore fluid components, and genesis of the Meikle and neighboring Carlin-type deposits, Northern Carlin Trend, Nevada","docAbstract":"The Meikle mine exploits one of the world's highest grade Carlin-type gold deposits with reserves of ca. 220 t gold at an average grade of 24.7 g/t. Locally, gold grades exceed 400 g/t. Several geologic events converged at Meikle to create these spectacular gold grades. Prior to mineralization, a Devonian hydrothermal system altered the Bootstrap limestone to Fe-rich dolomite. Subsequently the rocks were brecciated by faulting and Late Jurassic intrusive activity. The resulting permeability focused flow of late Eocene Carlin-type ore fluids and allowed them to react with the Fe-rich dolomite. Fluid inclusion data and mineral assemblages indicate that these fluids were hot (ca. 220??C),of moderate salinity (<6 wt % NaCl equiv), acidic, and H2S rich. Gold-rich pyrite formed by dissolution of dolomite and sulfidation of its contained Fe. Where dissolution and replacement were complete, ore-stage pyrite and other insoluble minerals were all that remained. Locally, these minerals accumulated as internal sediments in dissolution cavities to form ore with gold grades >400 g/t. Petrographic observations, geochemical data, and stable isotope results from the Meikle mine and other deposits at the Goldstrike mine place important constraints on genetic models for Meikle and other Carlin-type gold deposits on the northern Carlin trend. The ore fluids were meteoric water (??D = -135???, ??18O = -5???) that interacted with sedimentary rocks at a water/rock ratio of ca. 1 and temperatures of ca. 220??C. The absence of significant silicification suggests that there was little cooling of the ore fluids during mineralization. These two observations strongly suggest that ore fluids were not derived from deep sources but instead flowed parallel to isotherms. The gold was transported by H2S (??34S = 9???), which was derived from Paleozoic sedimentary rocks. The presence of auriferous sedimentary exhalative mineralization in the local stratigraphic sequence raises the possibility that preexisting concentrations of gold contributed to the Carlin-type deposits. Taken together our observations suggest that meteoric water evolved to become an ore fluid by shallow circulation through previously gold- and sulfur-enriched rocks. Carlin-type gold deposits formed where these fluids encountered permeable, reactive Fe-rich rocks.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Economic Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03610128","usgsCitation":"Emsbo, P., Hofstra, A., Lauha, E., Griffin, G., and Hutchinson, R., 2003, Origin of high-grade gold ore, source of ore fluid components, and genesis of the Meikle and neighboring Carlin-type deposits, Northern Carlin Trend, Nevada: Economic Geology, v. 98, no. 6, p. 1069-1100.","startPage":"1069","endPage":"1100","numberOfPages":"32","costCenters":[],"links":[{"id":236180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"98","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a70dbe4b0c8380cd762c3","contributors":{"authors":[{"text":"Emsbo, P.","contributorId":59901,"corporation":false,"usgs":true,"family":"Emsbo","given":"P.","affiliations":[],"preferred":false,"id":404273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hofstra, A. H. 0000-0002-2450-1593","orcid":"https://orcid.org/0000-0002-2450-1593","contributorId":41426,"corporation":false,"usgs":true,"family":"Hofstra","given":"A. H.","affiliations":[],"preferred":false,"id":404271,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lauha, E.A.","contributorId":100595,"corporation":false,"usgs":true,"family":"Lauha","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":404274,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Griffin, G.L.","contributorId":26870,"corporation":false,"usgs":true,"family":"Griffin","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":404270,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hutchinson, R.W.","contributorId":52743,"corporation":false,"usgs":true,"family":"Hutchinson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":404272,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70025306,"text":"70025306 - 2003 - Flood Frequency of Unregulated Streams of Tennessee Using Regional-Regression Equations and the Region-of-Influence Method","interactions":[],"lastModifiedDate":"2012-03-12T17:20:29","indexId":"70025306","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Flood Frequency of Unregulated Streams of Tennessee Using Regional-Regression Equations and the Region-of-Influence Method","docAbstract":"The region-of-influence method and regional-regression equations are used to predict flood frequency of unregulated and ungaged rivers and streams of Tennessee. The prediction methods have been developed using strem-gage records from unregulated streams draining basins having 1-30% total impervious area. A computer application automates the calculation of the flood frequencies of the unregulated streams. Average deleted-residual prediction errors for the region-of-influence method are found to be slightly smaller than those for the regional regression methods.","largerWorkTitle":"World Water and Environmental Resources Congress","conferenceTitle":"World Water and Environmental Resources Congress 2003","conferenceDate":"23 June 2003 through 26 June 2003","conferenceLocation":"Philadelphia, PA","language":"English","isbn":"0784406855","usgsCitation":"Law, G., and Tasker, G.D., 2003, Flood Frequency of Unregulated Streams of Tennessee Using Regional-Regression Equations and the Region-of-Influence Method, <i>in</i> World Water and Environmental Resources Congress, Philadelphia, PA, 23 June 2003 through 26 June 2003, p. 24-33.","startPage":"24","endPage":"33","numberOfPages":"10","costCenters":[],"links":[{"id":235852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a10dfe4b0c8380cd53e3b","contributors":{"editors":[{"text":"Bizier, P.","contributorId":113211,"corporation":false,"usgs":true,"family":"Bizier","given":"P.","email":"","affiliations":[],"preferred":false,"id":508810,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"DeBarry, P.","contributorId":111431,"corporation":false,"usgs":true,"family":"DeBarry","given":"P.","email":"","affiliations":[],"preferred":false,"id":508809,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Law, G.S.","contributorId":74182,"corporation":false,"usgs":true,"family":"Law","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":404697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":83097,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":404698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1008245,"text":"1008245 - 2003 - Effects of backpack radiotags on female northern pintails wintering in California","interactions":[],"lastModifiedDate":"2016-09-28T14:42:32","indexId":"1008245","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Effects of backpack radiotags on female northern pintails wintering in California","docAbstract":"<p> To test whether backpack radiotags impacted the wintering biology of northern pintails (Anas acuta), I attached spear-suture (SSU, n=82 in 1993) or harness (HAR, n=337 in 1991-1993) backpack radiotags to female Hatch-Year (HY) and After-Hatch-Year (AHY) pintails after their autumn arrival in California. I evaluated impacts of radiotags on 1) wintering population distribution; 2) flock status, flock size, and body mass at harvest; and 3) August-March survival. I also compared retention of SSU and HAR following attachment. Distribution, flock status, and flock size at harvest of HAR, SSU, and unmarked (UMK) pintails were similar. However, harvest mass of HAR pintails averaged 1 33 g (SE=25 g) less than UMK pintails; loss tended to be greatest for heavier HY females in 1 993. Daily survival rates during 1 993-1 994 of HAR vs. SSU pintails were similar for both HY (0.9979 vs. 0.9974) and AHY (0.9988 vs. 0.9986) female pintails. Retention ranged from 30-1 58 days (x=81 d, SE=5 d) for the 37 SSU that I confirmed as being shed; all other SSU failed 1-month studies due to poor retention past a month. </p>","language":"English","publisher":"Wildlife Society","usgsCitation":"Fleskes, J.P., 2003, Effects of backpack radiotags on female northern pintails wintering in California: Wildlife Society Bulletin, v. 31, no. 1, p. 212-219.","productDescription":"8 p.","startPage":"212","endPage":"219","numberOfPages":"8","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":131462,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6249d3","contributors":{"authors":[{"text":"Fleskes, Joseph P. 0000-0001-5388-6675 joe_fleskes@usgs.gov","orcid":"https://orcid.org/0000-0001-5388-6675","contributorId":1889,"corporation":false,"usgs":true,"family":"Fleskes","given":"Joseph","email":"joe_fleskes@usgs.gov","middleInitial":"P.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":317136,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70025901,"text":"70025901 - 2003 - Simulation of ground motion using the stochastic method","interactions":[],"lastModifiedDate":"2012-03-12T17:20:24","indexId":"70025901","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3208,"text":"Pure and Applied Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of ground motion using the stochastic method","docAbstract":"A simple and powerful method for simulating ground motions is to combine parametric or functional descriptions of the ground motion's amplitude spectrum with a random phase spectrum modified such that the motion is distributed over a duration related to the earthquake magnitude and to the distance from the source. This method of simulating ground motions often goes by the name \"the stochastic method.\" It is particularly useful for simulating the higher-frequency ground motions of most interest to engineers (generally, f>0.1 Hz), and it is widely used to predict ground motions for regions of the world in which recordings of motion from potentially damaging earthquakes are not available. This simple method has been successful in matching a variety of ground-motion measures for earthquakes with seismic moments spanning more than 12 orders of magnitude and in diverse tectonic environments. One of the essential characteristics of the method is that it distills what is known about the various factors affecting ground motions (source, path, and site) into simple functional forms. This provides a means by which the results of the rigorous studies reported in other papers in this volume can be incorporated into practical predictions of ground motion.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00334553","usgsCitation":"Boore, D., 2003, Simulation of ground motion using the stochastic method: Pure and Applied Geophysics, v. 160, no. 3-4, p. 635-676.","startPage":"635","endPage":"676","numberOfPages":"42","costCenters":[],"links":[{"id":234757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"160","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b902ae4b08c986b319365","contributors":{"authors":[{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":407005,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70025936,"text":"70025936 - 2003 - Rejuvenated-stage volcanism after 0.6-m.y. quiescence at West Maui Volcano, Hawaii: New evidence from K-Ar ages and chemistry of Lahaina Volcanics","interactions":[],"lastModifiedDate":"2012-03-12T17:20:24","indexId":"70025936","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Rejuvenated-stage volcanism after 0.6-m.y. quiescence at West Maui Volcano, Hawaii: New evidence from K-Ar ages and chemistry of Lahaina Volcanics","docAbstract":"West Maui's rejuvenated-stage Lahaina Volcanics were erupted from four discrete sites. New KAr ages indicate two pulses of volcanism, the older about 0.6 Ma and the younger about 0.4 Ma. Compositionally the lava flows are entirely basanitic, but each pulse is diverse. The underlying postshield-stage Honolua Volcanics were emplaced by about 1.2 Ma on the basis of previously published ages. Therefore the duration of volcanic quiescence prior to rejuvenation is about 0.6 m.y. at West Maui, much longer than estimated previously. ?? 2002 Elsevier Science B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0377-0273(02)00385-2","issn":"03770273","usgsCitation":"Tagami, T., Nishimitsu, Y., and Sherrod, D.R., 2003, Rejuvenated-stage volcanism after 0.6-m.y. quiescence at West Maui Volcano, Hawaii: New evidence from K-Ar ages and chemistry of Lahaina Volcanics: Journal of Volcanology and Geothermal Research, v. 120, no. 3-4, p. 207-214, https://doi.org/10.1016/S0377-0273(02)00385-2.","startPage":"207","endPage":"214","numberOfPages":"8","costCenters":[],"links":[{"id":208775,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0377-0273(02)00385-2"},{"id":234759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"120","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a61be4b0e8fec6cdc0be","contributors":{"authors":[{"text":"Tagami, Takahiro","contributorId":7474,"corporation":false,"usgs":true,"family":"Tagami","given":"Takahiro","email":"","affiliations":[],"preferred":false,"id":407158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nishimitsu, Yoshitomo","contributorId":17808,"corporation":false,"usgs":true,"family":"Nishimitsu","given":"Yoshitomo","email":"","affiliations":[],"preferred":false,"id":407159,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherrod, D. R.","contributorId":44559,"corporation":false,"usgs":true,"family":"Sherrod","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":407160,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70025292,"text":"70025292 - 2003 - The behavior of U- and Th-series nuclides in groundwater","interactions":[],"lastModifiedDate":"2012-03-12T17:20:29","indexId":"70025292","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3281,"text":"Reviews in Mineralogy and Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"The behavior of U- and Th-series nuclides in groundwater","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Reviews in Mineralogy and Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"15296466","usgsCitation":"Porcelli, D., and Swarzenski, P., 2003, The behavior of U- and Th-series nuclides in groundwater: Reviews in Mineralogy and Geochemistry, v. 52.","costCenters":[],"links":[{"id":235658,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba9e2e4b08c986b32259c","contributors":{"authors":[{"text":"Porcelli, D.","contributorId":35912,"corporation":false,"usgs":true,"family":"Porcelli","given":"D.","email":"","affiliations":[],"preferred":false,"id":404646,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swarzenski, P.W. 0000-0003-0116-0578","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":29487,"corporation":false,"usgs":true,"family":"Swarzenski","given":"P.W.","affiliations":[],"preferred":false,"id":404645,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013575,"text":"1013575 - 2003 - Assessing chick growth from a single visit to a seabird colony","interactions":[],"lastModifiedDate":"2017-11-18T09:33:09","indexId":"1013575","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2675,"text":"Marine Ornithology: Journal of Seabird Research and Conservation","onlineIssn":"2074-1235","printIssn":"1018-3337","active":true,"publicationSubtype":{"id":10}},"title":"Assessing chick growth from a single visit to a seabird colony","docAbstract":"We tested an approach to the collection of seabird chick growth data that utilizes a one-time sampling of chick measurements obtained during a single visit to a seabird colony. We assessed the development of Black-legged Kittiwake Rissa tridactyla chicks from a sample of measurements made on a single day during six years and compared these results to linear growth rates (g/day), determined from repeated measurements of the same chicks. We used two one-time sampling methods to obtain indices of chick-condition, 1) overall body-size (wing, head-plus-bill, tarsus) vs. mass, and 2) wing vs. mass; both were consistent with repeated measurements in identifying annual variations in chick growth. Thus, we suggest that chick-condition indices obtained from measurements collected on a single visit to a seabird colony are a useful tool for monitoring chick growth, especially at colonies where multiple visits and/or repeated measurements of individual chicks are impractical.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Benson, J., Suryan, R., and Piatt, J.F., 2003, Assessing chick growth from a single visit to a seabird colony: Marine Ornithology: Journal of Seabird Research and Conservation, v. 31, no. 2, p. 181-184.","productDescription":"pp. 181-184","startPage":"181","endPage":"184","numberOfPages":"4","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":129485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":11262,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.marineornithology.org/PDF/31_2/31_2_181-184.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"31","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672ab7","contributors":{"authors":[{"text":"Benson, J.","contributorId":57793,"corporation":false,"usgs":true,"family":"Benson","given":"J.","email":"","affiliations":[],"preferred":false,"id":318781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Suryan, R.M.","contributorId":52919,"corporation":false,"usgs":true,"family":"Suryan","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":318780,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":318782,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1008295,"text":"1008295 - 2003 - Individual variation in space use by female spotted hyenas","interactions":[],"lastModifiedDate":"2021-04-07T13:42:25.048112","indexId":"1008295","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Individual variation in space use by female spotted hyenas","docAbstract":"<p><span>Large carnivores range more widely than many other terrestrial mammals, and this behavior tends to bring them into frequent conflict with humans. Within any carnivore population, individual variation in patterns of space use should be expected to make some animals more vulnerable than others to risks of mortality from humans and other sources. In this study, our goal was to document variation among individuals in space use by female spotted hyenas (</span><i>Crocuta crocuta</i><span>). We examined predictions of hypotheses suggesting that space use by female hyenas is affected by reproductive state, social rank, and local prey abundance. Home-range size, distance at which females were found from the current communal den, and distance at which they were found from the nearest territorial boundary all varied significantly with the 3 independent variables. Females with den-dwelling cubs had smaller home ranges, were found closer to the communal den, and were found farther from the territorial boundary than were females with no den-dwelling cubs. Neither social rank nor prey availability significantly influenced the space-use patterns of females with den-dwelling cubs. Among females with no den-dwelling cubs, high-ranking females had smaller home ranges, were closer to the communal den, and were farther from the territorial boundary than were low-ranking females. The females ranging most widely were low-ranking individuals with no den-dwelling cubs when they were observed during periods of prey scarcity.</span></p>","language":"English","publisher":"Oxford University Press","doi":"10.1644/BOS-038","usgsCitation":"Boydston, E.E., Kapheim, K.M., Szykman, M., and Holekamp, K.E., 2003, Individual variation in space use by female spotted hyenas: Journal of Mammalogy, v. 84, no. 3, p. 1006-1018, https://doi.org/10.1644/BOS-038.","productDescription":"13 p.","startPage":"1006","endPage":"1018","numberOfPages":"13","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":478563,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1644/bos-038","text":"Publisher Index Page"},{"id":132514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"84","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1697","contributors":{"authors":[{"text":"Boydston, Erin E. 0000-0002-8452-835X eboydston@usgs.gov","orcid":"https://orcid.org/0000-0002-8452-835X","contributorId":1705,"corporation":false,"usgs":true,"family":"Boydston","given":"Erin","email":"eboydston@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":317302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kapheim, Karen M.","contributorId":174970,"corporation":false,"usgs":false,"family":"Kapheim","given":"Karen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":317301,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Szykman, Micaela","contributorId":174963,"corporation":false,"usgs":false,"family":"Szykman","given":"Micaela","email":"","affiliations":[],"preferred":false,"id":317300,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holekamp, Kay E.","contributorId":174966,"corporation":false,"usgs":false,"family":"Holekamp","given":"Kay","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":317299,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1008297,"text":"1008297 - 2003 - Altered behavior in spotted hyenas associated with increased human activity","interactions":[],"lastModifiedDate":"2016-09-28T15:07:37","indexId":"1008297","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":774,"text":"Animal Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Altered behavior in spotted hyenas associated with increased human activity","docAbstract":"<p><span>To investigate how anthropogenic activity might affect large carnivores, we studied the behaviour of spotted hyenas (</span><i>Crocuta crocuta</i><span>) during two time periods. From 1996 to 1998, we documented the ecological correlates of space utilization patterns exhibited by adult female hyenas defending a territory at the edge of a wildlife reserve in Kenya. Hyenas preferred areas near dense vegetation but appeared to avoid areas containing the greatest abundance of prey, perhaps because these were also the areas of most intensive livestock grazing. We then compared hyena behaviour observed in 1996–98 with that observed several years earlier and found many differences. Female hyenas in 1996–98 were found farther from dens, but closer to dense vegetation and to the edges of their territory, than in 1988–90. Recent females also had larger home ranges, travelled farther between consecutive sightings, and were more nocturnal than in 1988–90. Finally, hyenas occurred in smaller groups in 1996–98 than in 1988–90. We also found several changes in hyena demography between periods. We next attempted to explain differences observed between time periods by testing predictions of hypotheses invoking prey abundance, climate, interactions with lions, tourism and livestock grazing. Our data were consistent with the hypothesis that increased reliance on the reserve for livestock grazing was responsible for observed changes. That behavioural changes were not associated with decreased hyena population density suggests the behavioural plasticity typical of this species may protect it from extinction.</span></p>","language":"English","publisher":"Wiley","doi":"10.1017/S1367943003003263","usgsCitation":"Boydston, E.E., Kapheim, K.M., Watts, H.E., Szykman, M., and Holekamp, K.E., 2003, Altered behavior in spotted hyenas associated with increased human activity: Animal Conservation, v. 6, no. 3, p. 207-219, https://doi.org/10.1017/S1367943003003263.","productDescription":"13 p.","startPage":"207","endPage":"219","numberOfPages":"13","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":132539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-02-28","publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68750f","contributors":{"authors":[{"text":"Boydston, Erin E. 0000-0002-8452-835X eboydston@usgs.gov","orcid":"https://orcid.org/0000-0002-8452-835X","contributorId":1705,"corporation":false,"usgs":true,"family":"Boydston","given":"Erin","email":"eboydston@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":317312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kapheim, Karen M.","contributorId":174970,"corporation":false,"usgs":false,"family":"Kapheim","given":"Karen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":317311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watts, Heather E.","contributorId":174985,"corporation":false,"usgs":false,"family":"Watts","given":"Heather","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":317310,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Szykman, Micaela","contributorId":174963,"corporation":false,"usgs":false,"family":"Szykman","given":"Micaela","email":"","affiliations":[],"preferred":false,"id":317309,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Holekamp, Kay E.","contributorId":174966,"corporation":false,"usgs":false,"family":"Holekamp","given":"Kay","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":317308,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70025480,"text":"70025480 - 2003 - Uptake of elements from seawater by ferromanganese crusts: Solid-phase associations and seawater speciation","interactions":[],"lastModifiedDate":"2012-03-12T17:20:59","indexId":"70025480","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Uptake of elements from seawater by ferromanganese crusts: Solid-phase associations and seawater speciation","docAbstract":"Marine Fe-Mn oxyhydroxide crusts form by precipitation of dissolved components from seawater. Three hydrogenetic crust samples (one phosphatized) and two hydrothermal Mn-oxide samples were subjected to a sequential-leaching procedure in order to determine the host phases of 40 elements. Those host-phase associations are discussed with respect to element speciation in seawater. The partitioning of elements between the two major phases, Mn oxide and Fe oxyhydroxide, can in a first-order approximation be explained by a simple sorption model related to the inorganic speciation of the elements in seawater, as has been proposed in earlier models. Free and weakly complexed cations, such as alkali and alkaline earth metals, Mn, Co, Ni, Zn, T1(I), and partly Y, are sorbed preferentially on the negatively charged surface of the MnO2 in hydrogenetic crusts. The driving force is a strong coulombic interaction. All neutral or negatively charged chloro (Cd, Hg, T1), carbonate (Cu, Y, Pb, and U), and hydroxide (Be, Sc, Ti, Fe, Zr, Nb, In, Sn, Sb, Te, Hf, Ta, Bi, Th, and T1(III)) complexes and oxyanions (V, Cr, As, Se, Mo, and W) bind to the slightly positively charged surface of the amorphous FeOOH phase. While coulombic interaction can explain the sorption of the negatively charged species, the binding of neutral species is based on specific chemical interaction. Organic complexation of elements in deep-ocean water seems to be at most of minor importance. Surface oxidation can explain some strong metal associations, e.g. of Co and T1 with the MnO2 and Te with the FeOOH. Sorption reactions initially driven by coulombic forces are often followed by the formation of specific bonds between the adsorbate and the atoms of the oxide surface. Differences in the associations of some metals between the non-phosphatized and phosphatized hydrogenetic crusts and between the hydrogenetic and the hydrothermal samples reflect the different physico-chemical environments of formation and speciations in oxic seawater vs. less-oxic fluids, especially for the redox-sensitive metals such as Mo and V. These environmental-related differences indicate that the methodology of chemical speciation used here in combination with spectroscopic methods may allow for the detection of changes in paleoceanographic conditions recorded during the several tens of millions of years of crust growth. ?? 2003 Elsevier Science B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0025-3227(03)00122-1","issn":"00253227","usgsCitation":"Koschinsky, A., and Hein, J., 2003, Uptake of elements from seawater by ferromanganese crusts: Solid-phase associations and seawater speciation: Marine Geology, v. 198, no. 3-4, p. 331-351, https://doi.org/10.1016/S0025-3227(03)00122-1.","startPage":"331","endPage":"351","numberOfPages":"21","costCenters":[],"links":[{"id":209562,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0025-3227(03)00122-1"},{"id":236160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"198","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbd76e4b08c986b329041","contributors":{"authors":[{"text":"Koschinsky, A.","contributorId":42724,"corporation":false,"usgs":true,"family":"Koschinsky","given":"A.","affiliations":[],"preferred":false,"id":405364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hein, J.R. 0000-0002-5321-899X","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":61429,"corporation":false,"usgs":true,"family":"Hein","given":"J.R.","affiliations":[],"preferred":false,"id":405365,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70025360,"text":"70025360 - 2003 - Enhancement and management of eel fisheries affected by hydroelectric dams in New Zealand","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70025360","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Enhancement and management of eel fisheries affected by hydroelectric dams in New Zealand","docAbstract":"Two freshwater anguillid eel species, Anguilla australis and A. dieffenbachia, form the basis of important traditional, recreational, and commercial fisheries in New Zealand. These fisheries have been affected by the damming of many of the major waterways for hydroelectric generation. To create fisheries in reservoirs that would be otherwise inaccessible, elvers have been transferred from the base of dams into habitats upstream. Operations in three catchments: the Patea River (Lake Rotorangi), Waikato River (eight reservoirs notably the two lowermost, lakes Karapiro and Arapuni), and Rangitaiki River (lakes Matahina and Aniwhenua) are discussed. In all reservoirs, the transfers have successfully established fishable populations within six years of the first transfers and, in Lake Arapuni eels have reached the marketable size of 220 g in less than four years. In comparison, it typically takes from 13 to 17 years before eel populations are fishable in the lower Waikato River where direct access to the sea is available. Telemetry and monitoring at the screens and tailraces of several power stations have been used to determine migration timing, triggers, and pathways of mature eels. Successful downstream transfer of mature migrating adults has been achieved by spillway opening and netting in headraces during rain events in autumn, but means of preventing eels from impinging and entraining at the intakes are still required. An integrated, catchment-wide management system will be required to ensure sustainability of the fisheries. ?? Copyright by the American Fisheries Society 2003.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fisheries Society Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08922284","usgsCitation":"Boubee, J., Chisnall, B., Watene, E., Williams, E., Roper, D., and Haro, A., 2003, Enhancement and management of eel fisheries affected by hydroelectric dams in New Zealand: American Fisheries Society Symposium, v. 2003, no. 33, p. 191-205.","startPage":"191","endPage":"205","numberOfPages":"15","costCenters":[],"links":[{"id":236152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2003","issue":"33","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0971e4b0c8380cd51f00","contributors":{"authors":[{"text":"Boubee, J.","contributorId":75739,"corporation":false,"usgs":true,"family":"Boubee","given":"J.","email":"","affiliations":[],"preferred":false,"id":404896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chisnall, B.","contributorId":18953,"corporation":false,"usgs":true,"family":"Chisnall","given":"B.","email":"","affiliations":[],"preferred":false,"id":404893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watene, E.","contributorId":35931,"corporation":false,"usgs":true,"family":"Watene","given":"E.","affiliations":[],"preferred":false,"id":404895,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, E.","contributorId":15560,"corporation":false,"usgs":true,"family":"Williams","given":"E.","affiliations":[],"preferred":false,"id":404892,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Roper, D.","contributorId":24975,"corporation":false,"usgs":true,"family":"Roper","given":"D.","email":"","affiliations":[],"preferred":false,"id":404894,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Haro, A.","contributorId":6792,"corporation":false,"usgs":true,"family":"Haro","given":"A.","email":"","affiliations":[],"preferred":false,"id":404891,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":1008286,"text":"1008286 - 2003 - Keeping the herds healthy and alert: Implications of predator control for infectious disease","interactions":[],"lastModifiedDate":"2016-09-28T13:55:40","indexId":"1008286","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1466,"text":"Ecology Letters","active":true,"publicationSubtype":{"id":10}},"title":"Keeping the herds healthy and alert: Implications of predator control for infectious disease","docAbstract":"<p><span>Predator control programmes are generally implemented in an attempt to increase prey population sizes. However, predator removal could prove harmful to prey populations that are regulated primarily by parasitic infections rather than by predation. We develop models for microparasitic and macroparasitic infection that specify the conditions where predator removal will (a) increase the incidence of parasitic infection, (b) reduce the number of healthy individuals in the prey population and (c) decrease the overall size of the prey population. In general, predator removal is more likely to be harmful when the parasite is highly virulent, macroparasites are highly aggregated in their prey, hosts are long-lived and the predators select infected prey.</span></p>","language":"English","publisher":"Wiley","doi":"10.1046/j.1461-0248.2003.00500.x","usgsCitation":"Packer, C., Holt, R.D., Hudson, P., Lafferty, K.D., and Dobson, A.P., 2003, Keeping the herds healthy and alert: Implications of predator control for infectious disease: Ecology Letters, v. 6, no. 9, p. 797-802, https://doi.org/10.1046/j.1461-0248.2003.00500.x.","productDescription":"6 p.","startPage":"797","endPage":"802","numberOfPages":"6","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":478423,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://escholarship.org/uc/item/4m06g1m6","text":"External Repository"},{"id":132909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"9","noUsgsAuthors":false,"publicationDate":"2003-07-28","publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46e7","contributors":{"authors":[{"text":"Packer, Craig","contributorId":78592,"corporation":false,"usgs":true,"family":"Packer","given":"Craig","affiliations":[],"preferred":false,"id":317281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holt, Robert D.","contributorId":80584,"corporation":false,"usgs":true,"family":"Holt","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":317280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hudson, Peter J.","contributorId":85056,"corporation":false,"usgs":true,"family":"Hudson","given":"Peter J.","affiliations":[],"preferred":false,"id":317283,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":317282,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dobson, Andrew P.","contributorId":63693,"corporation":false,"usgs":true,"family":"Dobson","given":"Andrew","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":317279,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70025682,"text":"70025682 - 2003 - Unprecedented last-glacial mass accumulation rates determined by luminescence dating of loess from western Nebraska","interactions":[],"lastModifiedDate":"2012-03-12T17:20:32","indexId":"70025682","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Unprecedented last-glacial mass accumulation rates determined by luminescence dating of loess from western Nebraska","docAbstract":"A high-resolution chronology for Peoria (last glacial period) Loess from three sites in Nebraska, midcontinental North America, is determined by applying optically stimulated luminescence (OSL) dating to 35-50 ??m quartz. At Bignell Hill, Nebraska, an OSL age of 25,000 yr near the contact of Peoria Loess with the underlying Gilman Canyon Formation shows that dust accumulation occurred early during the last glacial maximum (LGM), whereas at Devil's Den and Eustis, Nebraska, basal OSL ages are significantly younger (18,000 and 21,000 yr, respectively). At all three localities, dust accumulation ended at some time after 14,000 yr ago. Mass accumulation rates (MARs) for western Nebraska, calculated using the OSL ages, are extremely high from 18,000 to 14,000 yr-much higher than those calculated for any other pre-Holocene location worldwide. These unprecedented MARs coincide with the timing of a mismatch between paleoenvironmental evidence from central North America, and the paleoclimate simulations from atmospheric global circulation models (AGCMs). We infer that the high atmospheric dust loading implied by these MARs may have played an important role, through radiative forcing, in maintaining a colder-than-present climate over central North America for several thousand years after summer insolation exceeded present-day values. ?? 2003 Elsevier Science (USA). All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/S0033-5894(03)00040-1","issn":"00335894","usgsCitation":"Roberts, H., Muhs, D., Wintle, A., Duller, G., and Bettis, E., 2003, Unprecedented last-glacial mass accumulation rates determined by luminescence dating of loess from western Nebraska: Quaternary Research, v. 59, no. 3, p. 411-419, https://doi.org/10.1016/S0033-5894(03)00040-1.","startPage":"411","endPage":"419","numberOfPages":"9","costCenters":[],"links":[{"id":208806,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0033-5894(03)00040-1"},{"id":234814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505bbcdae4b08c986b328e3f","contributors":{"authors":[{"text":"Roberts, H.M.","contributorId":12245,"corporation":false,"usgs":true,"family":"Roberts","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":406148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muhs, D.R. 0000-0001-7449-251X","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":61460,"corporation":false,"usgs":true,"family":"Muhs","given":"D.R.","affiliations":[],"preferred":false,"id":406150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wintle, A.G.","contributorId":43952,"corporation":false,"usgs":true,"family":"Wintle","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":406149,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Duller, G.A.T.","contributorId":106292,"corporation":false,"usgs":true,"family":"Duller","given":"G.A.T.","email":"","affiliations":[],"preferred":false,"id":406152,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bettis, E. Arthur III","contributorId":72822,"corporation":false,"usgs":true,"family":"Bettis","given":"E. Arthur","suffix":"III","affiliations":[],"preferred":false,"id":406151,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1008238,"text":"1008238 - 2003 - The use of multi-temporal Landsat Normalized Difference Vegetation Index (NDVI) data for mapping fuels in Yosemite National Park, USA","interactions":[],"lastModifiedDate":"2016-09-28T11:30:24","indexId":"1008238","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"The use of multi-temporal Landsat Normalized Difference Vegetation Index (NDVI) data for mapping fuels in Yosemite National Park, USA","docAbstract":"<p><span>The objective of this study was to test the applicability of using Normalized Difference Vegetation Index (NDVI) values derived from a temporal sequence of six Landsat Thematic Mapper (TM) scenes to map fuel models for Yosemite National Park, USA. An unsupervised classification algorithm was used to define 30 unique spectral-temporal classes of NDVI values. A combination of graphical, statistical and visual techniques was used to characterize the 30 classes and identify those that responded similarly and could be combined into fuel models. The final classification of fuel models included six different types: short annual and perennial grasses, tall perennial grasses, medium brush and evergreen hardwoods, short-needled conifers with no heavy fuels, long-needled conifers and deciduous hardwoods, and short-needled conifers with a component of heavy fuels. The NDVI, when analysed over a season of phenologically distinct periods along with ancillary data, can elicit information necessary to distinguish fuel model types. Fuels information derived from remote sensors has proven to be useful for initial classification of fuels and has been applied to fire management situations on the ground.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01431160210144679","usgsCitation":"Van Wagtendonk, J.W., and Root, R.R., 2003, The use of multi-temporal Landsat Normalized Difference Vegetation Index (NDVI) data for mapping fuels in Yosemite National Park, USA: International Journal of Remote Sensing, v. 24, no. 8, p. 1639-1651, https://doi.org/10.1080/01431160210144679.","productDescription":"13 p.","startPage":"1639","endPage":"1651","numberOfPages":"13","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":132207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"8","noUsgsAuthors":false,"publicationDate":"2010-11-26","publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634851","contributors":{"authors":[{"text":"Van Wagtendonk, Jan W. jan_van_wagtendonk@usgs.gov","contributorId":2648,"corporation":false,"usgs":true,"family":"Van Wagtendonk","given":"Jan","email":"jan_van_wagtendonk@usgs.gov","middleInitial":"W.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":317115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Root, Ralph R.","contributorId":174937,"corporation":false,"usgs":false,"family":"Root","given":"Ralph","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":317116,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70025876,"text":"70025876 - 2003 - The early Mesozoic Birdsboro central Atlantic margin basin in the Mid-Atlantic region, eastern United States","interactions":[],"lastModifiedDate":"2012-03-12T17:20:33","indexId":"70025876","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"The early Mesozoic Birdsboro central Atlantic margin basin in the Mid-Atlantic region, eastern United States","docAbstract":"The early Mesozoic Birdsboro basin (new name) was a single, elongate depositional trough in the present Mid-Atlantic area of the eastern United States, extending north-eastward from central Virginia across Maryland, Pennsylvania, and New Jersey into southern New York. What now remains after erosion comprises the Barboursville, Culpeper, Gettysburg, and Newark remnants. Some 7?? km of late Triassic and early Jurassic continental sediments of varying provenances entered and spread across in the Birdsboro basin in several depositional environments. The five resulting sedimentary lithosomes include feldspathic sandstone, quartzose sandstone, red silty mudstone, gray shale, and fanglomerate. The extensive interbedding, intertonguing, and lateral gradation among these lithosomes suggest that they were contemporary and closely interrelated. The feldspathic sandstone lithosome contains sediment with a southeastern provenance that accumulated in a bajada environment extending the length of the southeastern side of the basin. Sediment in the quartzose sandstone lithosome had a northwestern provenance-the coarse-grained fraction formed regional alluvial fans at the mouths of four major input centers. The finer-grained fraction was deposited in the distal reaches of these fans and in the playa environments in the interfan areas; this fraction formed the red silty mudstone lithosome. Gray/black shales and argillites of the gray shale lithosome accumulated in lacustrine environments in the interfan areas. The fanglomerate lithosome comprises numerous small, lobate deposits of poorly sorted sediment along both basin margins. The location and time of activity of the northwest input centers largely determined the distribution and areal extent of the various depositional environments and consequent lithosome along the length and across the width of the basin. The Birdsboro basin was deformed (tilted, faulted, and folded) sometime after the deposition of the youngest preserved rocks (early Sinemurian). The deformation varied along the length of the basin, producing differences in the amount of tilting, structural elevation, and subsequent erosion. The present erosional remnants create the illusion of four originally separate depositional basins.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/0016-7606(2003)115<0406:TEMBCA>2.0.CO;2","issn":"00167606","usgsCitation":"Faill, R.T., 2003, The early Mesozoic Birdsboro central Atlantic margin basin in the Mid-Atlantic region, eastern United States: Geological Society of America Bulletin, v. 115, no. 4, p. 406-421, https://doi.org/10.1130/0016-7606(2003)115<0406:TEMBCA>2.0.CO;2.","startPage":"406","endPage":"421","numberOfPages":"16","costCenters":[],"links":[{"id":208873,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/0016-7606(2003)115<0406:TEMBCA>2.0.CO;2"},{"id":234942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baaede4b08c986b322add","contributors":{"authors":[{"text":"Faill, R. T.","contributorId":79639,"corporation":false,"usgs":true,"family":"Faill","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":406921,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70025693,"text":"70025693 - 2003 - Using noble gases to investigate mountain-front recharge","interactions":[],"lastModifiedDate":"2012-03-12T17:20:31","indexId":"70025693","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Using noble gases to investigate mountain-front recharge","docAbstract":"Mountain-front recharge is a major component of recharge to inter-mountain basin-fill aquifers. The two components of mountain-front recharge are (1) subsurface inflow from the mountain block (subsurface inflow), and (2) infiltration from perennial and ephemeral streams near the mountain front (stream seepage). The magnitude of subsurface inflow is of central importance in source protection planning for basin-fill aquifers and in some water rights disputes, yet existing estimates carry large uncertainties. Stable isotope ratios can indicate the magnitude of mountain-front recharge relative to other components, but are generally incapable of distinguishing subsurface inflow from stream seepage. Noble gases provide an effective tool for determining the relative significance of subsurface inflow, specifically. Dissolved noble gas concentrations allow for the determination of recharge temperature, which is correlated with recharge elevation. The nature of this correlation cannot be assumed, however, and must be derived for the study area. The method is applied to the Salt Lake Valley Principal Aquifer in northern Utah to demonstrate its utility. Samples from 16 springs and mine tunnels in the adjacent Wasatch Mountains indicate that recharge temperature decreases with elevation at about the same rate as the mean annual air temperature, but is on average about 2??C cooler. Samples from 27 valley production wells yield recharge elevations ranging from the valley elevation (about 1500 m) to mid-mountain elevation (about 2500 m). Only six of the wells have recharge elevations less than 1800 m. Recharge elevations consistently greater than 2000 m in the southeastern part of the basin indicate that subsurface inflow constitutes most of the total recharge in this area. ?? 2003 Published by Elsevier Science B.V.","largerWorkTitle":"Journal of Hydrology","language":"English","doi":"10.1016/S0022-1694(03)00043-X","issn":"00221694","usgsCitation":"Manning, A.H., and Solomon, D.K., 2003, Using noble gases to investigate mountain-front recharge, <i>in</i> Journal of Hydrology, v. 275, no. 3-4, p. 194-207, https://doi.org/10.1016/S0022-1694(03)00043-X.","startPage":"194","endPage":"207","numberOfPages":"14","costCenters":[],"links":[{"id":208909,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0022-1694(03)00043-X"},{"id":235002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"275","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc083e4b08c986b32a17d","contributors":{"authors":[{"text":"Manning, A. H.","contributorId":26491,"corporation":false,"usgs":true,"family":"Manning","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":406195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solomon, D. K.","contributorId":98324,"corporation":false,"usgs":false,"family":"Solomon","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":406196,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}