{"pageNumber":"2578","pageRowStart":"64425","pageSize":"25","recordCount":184617,"records":[{"id":70180867,"text":"70180867 - 2005 - Association of ice and river channel morphology determined using ground-penetrationg radar in the Kuparuk River, Alaska","interactions":[],"lastModifiedDate":"2021-06-07T15:28:23.590715","indexId":"70180867","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":899,"text":"Arctic, Antarctic, and Alpine Research","active":true,"publicationSubtype":{"id":10}},"title":"Association of ice and river channel morphology determined using ground-penetrationg radar in the Kuparuk River, Alaska","docAbstract":"<p><span>We collected ground-penetrating radar data at 10 sites along the Kuparuk River and its main tributary, the Toolik River, to detect unfrozen water beneath river ice. We used 250 MHz and 500 MHz antennas to image both the ice-water interface and the river channel in late April 2001, when daily high temperatures were consistently freezing and river ice had attained its maximum seasonal thickness. The presence of water below the river ice appears as a strong, horizontal reflection observed in the radar data and is confirmed by drill hole data. A downstream transition occurs from ice that is frozen to the bed, called bedfast ice, to ice that is floating on unfrozen water, called floating ice. This transition in ice type corresponds to a downstream change in channel size that was detected in previously conducted hydraulic geometry surveys of the Kuparuk River. We propose a conceptual model wherein the downstream transition from bedfast ice to floating ice is responsible for an observed step change in channel size due to enhanced bank erosion in large channels by floating ice.</span></p>","language":"English","publisher":"Institute of Arctic and Alpine Research","publisherLocation":"Boulder, CO","doi":"10.1657/1523-0430(2005)037[0157:AOIARC]2.0.CO;2","usgsCitation":"Best, H., McNamara, J.P., and Liberty, L.M., 2005, Association of ice and river channel morphology determined using ground-penetrationg radar in the Kuparuk River, Alaska: Arctic, Antarctic, and Alpine Research, v. 37, no. 2, https://doi.org/10.1657/1523-0430(2005)037[0157:AOIARC]2.0.CO;2.","productDescription":"6 p.","startPage":"162","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":477782,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1657/1523-0430(2005)037[0157:aoiarc]2.0.co;2","text":"External Repository"},{"id":334798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kuparuk River, Toolik River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -150.194091796875,\n              68.46379955520322\n            ],\n            [\n              -150.194091796875,\n              70.67088107015755\n            ],\n            [\n              -147.7001953125,\n              70.67088107015755\n            ],\n            [\n              -147.7001953125,\n              68.46379955520322\n            ],\n            [\n              -150.194091796875,\n              68.46379955520322\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"2","edition":"157","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"589847a6e4b0efcedb7072d3","contributors":{"authors":[{"text":"Best, Heather","contributorId":179100,"corporation":false,"usgs":false,"family":"Best","given":"Heather","affiliations":[],"preferred":false,"id":662636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNamara, J. P.","contributorId":105551,"corporation":false,"usgs":false,"family":"McNamara","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":662637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Liberty, Lee M.","contributorId":89631,"corporation":false,"usgs":true,"family":"Liberty","given":"Lee","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":662638,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028800,"text":"70028800 - 2005 - Foliation development and reaction softening by dissolution and precipitation in the transformation of granodiorite to orthogneiss, Glastonbury Complex, Connecticut, U.S.A","interactions":[],"lastModifiedDate":"2021-06-11T13:49:24.257578","indexId":"70028800","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1177,"text":"Canadian Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Foliation development and reaction softening by dissolution and precipitation in the transformation of granodiorite to orthogneiss, Glastonbury Complex, Connecticut, U.S.A","docAbstract":"<p><span>Textures, microstructures, and patterns of chemical zoning in minerals in a granodioritic orthogneiss in the Glastonbury Complex, Connecticut, lead to the interpretation that foliation development was facilitated by retrograde hydration reactions in the presence of an aqueous fluid. Incomplete replacement of the metastable magmatic minerals K-feldspar + hastingsite + magnetite produced foliation-defining biotite + epidote + quartz. These reaction products did not replace K-feldspar – hastingsite interfaces; rather, either biotite or epidote replaced the amphibole, and plagioclase replaced K-feldspar. Biotite and epidote precipitated syntectonically in discrete layers that define the foliation in the orthogneiss, whereas quartz precipitated primarily in ribbons, further enhancing the fabric. Metastable REE-rich igneous titanite also dissolved, and was incompletely replaced by REE-poor, Al-bearing metamorphic titanite. The similar concentrations of the REE in epidote and titanite show that the REE released by titanite dissolution were precipitated locally as the allanite component in adjacent grains of epidote. The entire process was syntectonic, with most grains showing multiple overgrowths in the direction of extension as defined by stretched xenoliths. Sufficient U was present in the titanite overgrowths to allow SHRIMP dating of cores, mantles, and rims. These results suggest at least three retrograde Alleghanian events of growth in a span of ~30 m.y. Thus the dissolution – transportation –precipitation process not only describes the reaction mechanism but also leads to the redistribution of reaction products into nearly monomineralic layers, thus contributing to metamorphic differentiation and to the development of the foliation. The resulting orthogneiss was much weaker that the granodiorite protolith, owing to this reaction and textural softening.</span></p>","language":"English","publisher":"Mineralogical Association of Canada","doi":"10.2113/gscanmin.43.1.327","usgsCitation":"Wintsch, R., Aleinikoff, J.N., and Yi, K., 2005, Foliation development and reaction softening by dissolution and precipitation in the transformation of granodiorite to orthogneiss, Glastonbury Complex, Connecticut, U.S.A: Canadian Mineralogist, v. 43, no. 1, p. 327-347, https://doi.org/10.2113/gscanmin.43.1.327.","productDescription":"21 p.","startPage":"327","endPage":"347","numberOfPages":"21","costCenters":[],"links":[{"id":236756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut","otherGeospatial":"Glastonbury Complex","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.652587890625,\n              41.67598909594535\n            ],\n            [\n              -72.57877349853516,\n              41.67598909594535\n            ],\n            [\n              -72.57877349853516,\n              41.731354910056446\n            ],\n            [\n              -72.652587890625,\n              41.731354910056446\n            ],\n            [\n              -72.652587890625,\n              41.67598909594535\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"43","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a12afe4b0c8380cd543d8","contributors":{"authors":[{"text":"Wintsch, R. P.","contributorId":104921,"corporation":false,"usgs":false,"family":"Wintsch","given":"R. P.","affiliations":[{"id":13366,"text":"Indiana University, Bloomington, Indiana, USA","active":true,"usgs":false}],"preferred":false,"id":419803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aleinikoff, J. N. 0000-0003-3494-6841","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":75132,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":419801,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yi, K.","contributorId":104271,"corporation":false,"usgs":false,"family":"Yi","given":"K.","affiliations":[],"preferred":false,"id":419802,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028806,"text":"70028806 - 2005 - Optimal swim speeds for traversing velocity barriers: An analysis of volitional high-speed swimming behavior of migratory fishes","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70028806","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2275,"text":"Journal of Experimental Biology","active":true,"publicationSubtype":{"id":10}},"title":"Optimal swim speeds for traversing velocity barriers: An analysis of volitional high-speed swimming behavior of migratory fishes","docAbstract":"Migrating fish traversing velocity barriers are often forced to swim at speeds greater than their maximum sustained speed (Ums). Failure to select an appropriate swim speed under these conditions can prevent fish from successfully negotiating otherwise passable barriers. I propose a new model of a distance-maximizing strategy for fishes traversing velocity barriers, derived from the relationships between swim speed and fatigue time in both prolonged and sprint modes. The model predicts that fish will maximize traversed distance by swimming at a constant groundspeed against a range of flow velocities, and this groundspeed is equal to the negative inverse of the slope of the swim speed-fatigue time relationship for each mode. At a predictable flow velocity, they should switch from the optimal groundspeed for prolonged mode to that for sprint mode. Data from six migratory fish species (anadromous clupeids: American shad Alosa sapidissima, alewife A. pseudoharengus and blueback herring A. aestivalis; amphidromous: striped bass Morone saxatilis; and potomodromous species: walleye (previously known as Stizostedion vitrium) and white sucker Catostomus commersonii) were used to explore the ability of fish to approximate the predicted distance-maximizing behaviors, as well as the consequences of deviating from the optima. Fish volitionally sprinted up an open-channel flume against fixed flow velocities of 1.5-4.5 m s-1, providing data on swim speeds and fatigue times, as well as their groundspeeds. Only anadromous clupeids selected the appropriate distance-maximizing groundspeed at both prolonged and sprint modes. The other three species maintained groundspeeds appropriate to the prolonged mode, even when they should have switched to the sprint optima. Because of this, these species failed to maximize distance of ascent. The observed behavioral variability has important implications both for distributional limits and fishway design.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Experimental Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1242/jeb.01380","issn":"00220949","usgsCitation":"Castro-Santos, T., 2005, Optimal swim speeds for traversing velocity barriers: An analysis of volitional high-speed swimming behavior of migratory fishes: Journal of Experimental Biology, v. 208, no. 3, p. 421-432, https://doi.org/10.1242/jeb.01380.","startPage":"421","endPage":"432","numberOfPages":"12","costCenters":[],"links":[{"id":477702,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1242/jeb.01380","text":"Publisher Index Page"},{"id":209641,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1242/jeb.01380"},{"id":236304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"208","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6eeae4b0c8380cd7587b","contributors":{"authors":[{"text":"Castro-Santos, T. 0000-0003-2575-9120","orcid":"https://orcid.org/0000-0003-2575-9120","contributorId":12416,"corporation":false,"usgs":true,"family":"Castro-Santos","given":"T.","affiliations":[],"preferred":false,"id":419823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028835,"text":"70028835 - 2005 - Effects of fire intensity on vital rates of an endemic herb of the Florida keys, USA","interactions":[],"lastModifiedDate":"2022-07-18T16:51:28.023932","indexId":"70028835","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2821,"text":"Natural Areas Journal","active":true,"publicationSubtype":{"id":10}},"title":"Effects of fire intensity on vital rates of an endemic herb of the Florida keys, USA","docAbstract":"Fire intensity is one of the important components of a fire regime. However, relatively few studies have linked fire intensity with post-fire population vital rates. In this study, we explored the effects of fire intensity on population vital rates of Chamaecrista keyensis Pennell (Fabaceae) up to two years post-fire. C. keyensis is an endemic understory plant of pine rockland, a fire-dependent ecosystem of the Lower Florida Keys. We measured one fire intensity indicator, fire temperature reached by steel plates on the ground, during three prescribed fires at different sites. We followed marked individuals up to two years post-fire to derive annual survival, annual growth rate, percentage of fruiting plants, mean number of fruits per reproductive plant, and number of seedlings per census plot (1 m2) of C. keyensis. We found fire intensity had significant effects on reproduction in the first year post-fire only. More specifically, mean number of fruits and percentage of fruiting plants increased as fire intensity increased. Results from this study suggest that extremely low fire intensity caused by very short fire return intervals (e.g., less than three years) may not provide sufficient stimulation to reproduction to achieve the best post-fire recovery for C. keyensis.","language":"English","publisher":"Natural Areas Association","issn":"08858608","usgsCitation":"Liu, H., Menges, E., Snyder, J., Koptur, S., and Ross, M., 2005, Effects of fire intensity on vital rates of an endemic herb of the Florida keys, USA: Natural Areas Journal, v. 25, no. 1, p. 71-76.","productDescription":"6 p.","startPage":"71","endPage":"76","costCenters":[],"links":[{"id":236726,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403928,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/43912368"}],"country":"United States","state":"Florida","otherGeospatial":"Big Pine Key, Florida Keys","geographicExtents":"{\n  \"type\": 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]\n}","volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a06eee4b0c8380cd514b0","contributors":{"authors":[{"text":"Liu, H.","contributorId":12222,"corporation":false,"usgs":true,"family":"Liu","given":"H.","affiliations":[],"preferred":false,"id":419926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Menges, E.S.","contributorId":80479,"corporation":false,"usgs":true,"family":"Menges","given":"E.S.","affiliations":[],"preferred":false,"id":419927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snyder, J.R.","contributorId":96622,"corporation":false,"usgs":true,"family":"Snyder","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":419929,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koptur, S.","contributorId":85379,"corporation":false,"usgs":true,"family":"Koptur","given":"S.","affiliations":[],"preferred":false,"id":419928,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ross, M.S.","contributorId":96781,"corporation":false,"usgs":true,"family":"Ross","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":419930,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028791,"text":"70028791 - 2005 - The soil physics contributions of Edgar Buckingham","interactions":[],"lastModifiedDate":"2018-10-31T10:12:53","indexId":"70028791","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"The soil physics contributions of Edgar Buckingham","docAbstract":"<p><span>During 1902 to 1906 as a soil physicist at the USDA Bureau of Soils (BOS), Edgar Buckingham originated the concepts of matric potential, soil–water retention curves, specific water capacity, and unsaturated hydraulic conductivity (</span><i>K</i><span>) as a distinct property of a soil. He applied a formula equivalent to Darcy's law (though without specific mention of Darcy's work) to unsaturated flow. He also contributed significant research on quasi-empirical formulas for&nbsp;</span><i>K</i><span>as a function of water content, water flow in capillary crevices and in thin films, and scaling. Buckingham's work on gas flow in soils produced paradigms that are consistent with our current understanding. His work on evaporation elucidated the concept of self-mulching and produced sound and sometimes paradoxical generalizations concerning conditions that favor or retard evaporation. Largely overshadowing those achievements, however, is that he launched a theory, still accepted today, that could predict transient water content as a function of time and space. Recently discovered documents reveal some of the arguments Buckingham had with BOS officials, including the text of a two-paragraph conclusion of his famous 1907 report on soil water, and the official letter documenting rejection of that text. Strained interpersonal relations motivated the departure of Buckingham and other brilliant physicists (N.E. Dorsey, F.H. King, and Lyman Briggs) from the BOS during 1903 to 1906. Given that Buckingham and his BOS colleagues had been rapidly developing the means of quantifying unsaturated flow, these strained relations probably slowed the advancement of unsaturated flow theory.</span></p>","language":"English","publisher":"ACSESS","doi":"10.2136/sssaj2005.0328","issn":"03615995","usgsCitation":"Nimmo, J., and Landa, E.R., 2005, The soil physics contributions of Edgar Buckingham: Soil Science Society of America Journal, v. 69, no. 2, p. 328-342, https://doi.org/10.2136/sssaj2005.0328.","productDescription":"15 p.","startPage":"328","endPage":"342","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":236647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb03ce4b08c986b324d02","contributors":{"authors":[{"text":"Nimmo, J. R. 0000-0001-8191-1727","orcid":"https://orcid.org/0000-0001-8191-1727","contributorId":58304,"corporation":false,"usgs":true,"family":"Nimmo","given":"J. R.","affiliations":[],"preferred":false,"id":419766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landa, E. R.","contributorId":100002,"corporation":false,"usgs":true,"family":"Landa","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":419767,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028790,"text":"70028790 - 2005 - Physical controls on total and methylmercury concentrations in streams and lakes of the northeastern USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028790","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1479,"text":"Ecotoxicology","active":true,"publicationSubtype":{"id":10}},"title":"Physical controls on total and methylmercury concentrations in streams and lakes of the northeastern USA","docAbstract":"The physical factors controlling total mercury (HgT) and methylmercury (MeHg) concentrations in lakes and streams of northeastern USA were assessed in a regional data set containing 693 HgT and 385 corresponding MeHg concentrations in surface waters. Multiple regression models using watershed characteristics and climatic variables explained 38% or less of the variance in HgT and MeHg. Land cover percentages and soil permeability generally provided modest predictive power. Percent wetlands alone explained 19% of the variance in MeHg in streams at low-flow, and it was the only significant (p < 0.02) predictor for MeHg in lakes, albeit explaining only 7% of the variance. When stream discharge was added as a variable it became the dominant predictor for HgT in streams, improving the model r 2 from 0.19 to 0.38. Stream discharge improved the MeHg model more modestly, from r 2 of 0.25 to 0.33. Methylation efficiency (MeHg/HgT) was modeled well (r 2 of 0.78) when a seasonal term was incorporated (sine wave with annual period). Physical models explained 18% of the variance in fish Hg concentrations in 134 lakes and 55% in 20 reservoirs. Our results highlight the important role of seasonality and short-term hydrologic changes to the delivery of Hg to water bodies. ?? 2005 Springer Science+Business Media, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecotoxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10646-004-6264-z","issn":"09639292","usgsCitation":"Shanley, J.B., Kamman, N., Clair, T., and Chalmers, A., 2005, Physical controls on total and methylmercury concentrations in streams and lakes of the northeastern USA: Ecotoxicology, v. 14, no. 1-2, p. 125-134, https://doi.org/10.1007/s10646-004-6264-z.","startPage":"125","endPage":"134","numberOfPages":"10","costCenters":[],"links":[{"id":209872,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10646-004-6264-z"},{"id":236615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7aa4e4b0c8380cd78ffc","contributors":{"authors":[{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":419763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kamman, N.C.","contributorId":51079,"corporation":false,"usgs":true,"family":"Kamman","given":"N.C.","affiliations":[],"preferred":false,"id":419762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clair, T.A.","contributorId":84529,"corporation":false,"usgs":true,"family":"Clair","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":419764,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chalmers, A.","contributorId":96858,"corporation":false,"usgs":true,"family":"Chalmers","given":"A.","email":"","affiliations":[],"preferred":false,"id":419765,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028855,"text":"70028855 - 2005 - Distribution, foraging behavior, and capture results of the spotted bat (Euderma maculatum) in central Oregon","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70028855","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3746,"text":"Western North American Naturalist","onlineIssn":"1944-8341","printIssn":"1527-0904","active":true,"publicationSubtype":{"id":10}},"title":"Distribution, foraging behavior, and capture results of the spotted bat (Euderma maculatum) in central Oregon","docAbstract":"The spotted bat (Euderma maculatum) has been virtually unknown in Oregon despite the existence of potential habitat in many areas of the state. In 2002 and 2003 we searched for spotted bats along the John Day, Deschutes, and Crooked Rivers and at a remote dry canyon southeast of the city of Bend in central Oregon. The species was documented through the use of mist-nets, a bat detector, and recognition of audible spotted bat calls. Spotted bats were found at 11 locations in 6 Oregon counties. Nightly activity patterns of spotted bats were unpredictable. Spotted bats were found in 78% of search areas but on only 48% of survey nights. We observed spotted bats foraging above fields and low upland slopes adjacent to rivers and creeks and along the rims of cliffs. Estimated flying heights of spotted bats ranged from 3 m to 50 m aboveground. The species was difficult to capture and was captured only after considerable experimentation with methods and materials. Three spotted bats were captured toward the end of the project in 2003 and accounted for only 0.5% of all bats captured during the study. Although we attached radio transmitters to 2 spotted bats, we found no roost locations. We believe additional spotted bat surveys in Oregon are warranted, especially in higher-elevation habitats, but recommend that to increase their effectiveness, surveys accommodate the unique foraging behavior of the species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Western North American Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"15270904","usgsCitation":"Rodhouse, T., McCaffrey, M., and Wright, R., 2005, Distribution, foraging behavior, and capture results of the spotted bat (Euderma maculatum) in central Oregon: Western North American Naturalist, v. 65, no. 2, p. 215-222.","startPage":"215","endPage":"222","numberOfPages":"8","costCenters":[],"links":[{"id":236482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a031ee4b0c8380cd5034f","contributors":{"authors":[{"text":"Rodhouse, T.J.","contributorId":10978,"corporation":false,"usgs":true,"family":"Rodhouse","given":"T.J.","affiliations":[],"preferred":false,"id":420035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCaffrey, M.F.","contributorId":90095,"corporation":false,"usgs":true,"family":"McCaffrey","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":420036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, R.G.","contributorId":9622,"corporation":false,"usgs":true,"family":"Wright","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":420034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028784,"text":"70028784 - 2005 - A sampler for capturing larval and juvenile Atlantic menhaden","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70028784","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"A sampler for capturing larval and juvenile Atlantic menhaden","docAbstract":"Interest in capturing larval and juvenile Atlantic menhaden Brevoortia tyrannus for use in laboratory studies required the design and construction of a sampling device that would allow us to make collections of live fish from open-water areas. Our device for capturing 1-2.5-in larval-juvenile fish was constructed of a stainless steel frame that supported a 9.84-ft-long (3-m-long)5 cone plankton net with a 3.28-ft-diameter (1-m-diameter) opening and a 0.04-in (1-mm) mesh size. Although the plankton net was similar to that used during typical larval fish collections, the cod end was constructed of Plexiglas and was nearly watertight; this prevented impingement and injury to larval fish and provided a calm-water environment. The cod end was designed for quick release from the plankton net, and the entire cod end could be submerged into a 75-gal onboard holding tank. This design and technique obviated the netting or emerging of fish from the water until they were returned to the laboratory. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/M03-189.1","issn":"02755947","usgsCitation":"Hedrick, J., Hedrick, L., and Margraf, F., 2005, A sampler for capturing larval and juvenile Atlantic menhaden: North American Journal of Fisheries Management, v. 25, no. 1, p. 245-250, https://doi.org/10.1577/M03-189.1.","startPage":"245","endPage":"250","numberOfPages":"6","costCenters":[],"links":[{"id":236547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209821,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/M03-189.1"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-01","publicationStatus":"PW","scienceBaseUri":"5059e567e4b0c8380cd46d45","contributors":{"authors":[{"text":"Hedrick, J.D.","contributorId":105511,"corporation":false,"usgs":true,"family":"Hedrick","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":419744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedrick, L.R.","contributorId":14177,"corporation":false,"usgs":true,"family":"Hedrick","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":419742,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Margraf, F.J.","contributorId":47738,"corporation":false,"usgs":true,"family":"Margraf","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":419743,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028783,"text":"70028783 - 2005 - Characterization of gas chemistry and noble-gas isotope ratios of inclusion fluids in magmatic-hydrothermal and magmatic-steam alunite","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70028783","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of gas chemistry and noble-gas isotope ratios of inclusion fluids in magmatic-hydrothermal and magmatic-steam alunite","docAbstract":"Chemical and isotope data were obtained for the active gas and noble gas of inclusion fluids in coarse-grained samples of magmatic-hydrothermal and magmatic-steam alunite from well-studied deposits (Marysvale, Utah; Tambo, Chile; Tapajo??s, Brazil; Cactus, California; Pierina, Peru), most of which are discussed in this Volume. Primary fluid inclusions in the alunite typically are less than 0.2 ??m but range up to several micrometers. Analyses of the active-gas composition of these alunite-hosted inclusion fluids released in vacuo by both crushing and heating indicate consistent differences in the compositions of magmatic-hydrothermal and magmatic-steam fluids. The compositions of fluids released by crushing were influenced by contributions from significant populations of secondary inclusions that trapped largely postdepositional hydrothermal fluids. Thermally released fluids gave the best representation of the fluids that formed primary alunite. The data are consistent with current models for the evolution of magmatic-hydrothermal and magmatic-steam fluids. Magmatic-steam fluids are vapor-dominant, average about 49 mol% H2O, and contain N2, H2, CH4, CO, Ar, He, HF, and HCl, with SO2 the dominant sulfur gas (average SO2/ H2S=202). In contrast, magmatic-hydrothermal fluids are liquid-dominant, average about 88 mol% H2O, and N2, H2, CO2, and HF, with H2S about as abundant as SO2 (average SO2/H2 S=0.7). The low SO2/H2S and N2/Ar ratios, and the near-absence of He in magmatic-hydrothermal fluids, are consistent with their derivation from degassed condensed magmatic fluids whose evolution from reduced-to-oxidized aqueous sulfur species was governed first by rock and then by fluid buffers. The high SO2/H2S and N2/Ar with significant concentrations of He in magmatic-steam fluids are consistent with derivation directly from a magma. None of the data supports the entrainment of atmospheric gases or mixing of air-saturated gases in meteoric water in either magmatic-hydrothermal or magmatic-steam fluids. Thus, the oxidation of SO2 to aqueous sulfate in the magmatic-steam fluids did not result from mixing with atmospheric oxygen. Both of the fluid types are characterized by high H2 contents that range from 0.2 mol% to the extraordinarily large amounts (66 mol%) observed in some magmatic-steam fluids. Modeling of gas speciation using SOLVGAS requires most of the gas species to have been in disequilibrium at the time of their trapping in the fluid inclusions. The origin of such extreme H2 concentrations, although problematic, is thought to be largely related to accumulation of H2 from the reaction of water with ferrous iron during the rise of magma and probably even after exsolution of fluid from a magma. The large contents of reduced gases in the inclusion fluids are far in excess of those observed in volcanic emanations, and are thought to reflect the close \"sampling position\" of the host alunite relative to the location of the magma. Isotope ratios of He and Ne indicate largely crustal sources for these gases in the alunite parental fluids derived from Tertiary magmas, but a greater mantle component for the gases in alunite parental fluids derived from Proterozoic magmas.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.06.037","issn":"00092541","usgsCitation":"Landis, G.P., and Rye, R.O., 2005, Characterization of gas chemistry and noble-gas isotope ratios of inclusion fluids in magmatic-hydrothermal and magmatic-steam alunite: Chemical Geology, v. 215, no. 1-4 SPEC. ISS., p. 155-184, https://doi.org/10.1016/j.chemgeo.2004.06.037.","startPage":"155","endPage":"184","numberOfPages":"30","costCenters":[],"links":[{"id":236546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209820,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.06.037"}],"volume":"215","issue":"1-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f4c9e4b0c8380cd4befe","contributors":{"authors":[{"text":"Landis, G. P.","contributorId":102846,"corporation":false,"usgs":true,"family":"Landis","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":419741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":419740,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028781,"text":"70028781 - 2005 - Effect of sample handling on thiamine and thiaminolytic activity in alewife","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028781","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"Effect of sample handling on thiamine and thiaminolytic activity in alewife","docAbstract":"Alewives Alosa pseudoharengus were collected to evaluate handling and processing conditions that may affect the measurement of their thiamine-thiaminase content. Fish were captured by otter trawl, and reference samples of live fish were quick-frozen on dry ice immediately following capture. Other samples were placed on wet ice (4??C) or held in ambient lake water (21.5??C) for periods of up to 5 h before freezing. Total thiamine levels for reference samples averaged 26 nmol/g and consisted of 66, 15, and 19% thiamine pyrophosphate (TPP), thiamine monophosphate (TMP), and unphosphorylated thiamine (Th), respectively. After 120 min at either 4??C or 21.5??C, total thiamine concentrations were lower. At 21.5??C, the TPP proportion had decreased by 30 min and the proportion as Th increased after 60 min. In the groups sampled after 5 h, total thiamine concentrations were not altered but the proportion of TPP was lower and that of Th was higher than in reference samples. The stability of thiamine in thawed muscle samples from previously frozen alewives was poor (40% loss by 1 h at 22??C and 30% loss by 2 h at 4??C). Thiaminase activity averaged 5,975 pmol??g wet weight -1??min-1 in reference samples. In fresh-caught alewives, thiaminase activities were remarkably consistent throughout the sampling period. At 4??C, thiaminase activity in muscle tissue from previously frozen alewives was stable for the entire investigation period. At 25??C, the activity initially increased by 40% after 60 min but then decreased to 50% of initial value after 5 h. We conclude that sampling times greater than 25 min could cause some changes in the various thiamine forms and net loss in total thiamine. The thiamine content in previously frozen alewife samples is highly labile, requiring low temperatures during processing for analysis. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Aquatic Animal Health","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/H03-074.1","issn":"08997659","usgsCitation":"Wright, G., Brown, S., Brown, L., Moore, K., Villella, M., Zajicek, J., Tillitt, D.E., Fitzsimons, J., and Honeyfield, D., 2005, Effect of sample handling on thiamine and thiaminolytic activity in alewife: Journal of Aquatic Animal Health, v. 17, no. 1, p. 77-81, https://doi.org/10.1577/H03-074.1.","startPage":"77","endPage":"81","numberOfPages":"5","costCenters":[],"links":[{"id":209771,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/H03-074.1"},{"id":236479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-03-01","publicationStatus":"PW","scienceBaseUri":"505a0603e4b0c8380cd51097","contributors":{"authors":[{"text":"Wright, G.M.","contributorId":104851,"corporation":false,"usgs":true,"family":"Wright","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":419733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, S.B.","contributorId":107636,"corporation":false,"usgs":true,"family":"Brown","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":419734,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, L. R. 0000-0001-6702-4531","orcid":"https://orcid.org/0000-0001-6702-4531","contributorId":66391,"corporation":false,"usgs":true,"family":"Brown","given":"L. R.","affiliations":[],"preferred":false,"id":419728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, K.","contributorId":64432,"corporation":false,"usgs":true,"family":"Moore","given":"K.","email":"","affiliations":[],"preferred":false,"id":419727,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Villella, M.","contributorId":91673,"corporation":false,"usgs":true,"family":"Villella","given":"M.","email":"","affiliations":[],"preferred":false,"id":419732,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zajicek, J.L.","contributorId":87086,"corporation":false,"usgs":true,"family":"Zajicek","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":419731,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tillitt, D. E.","contributorId":83462,"corporation":false,"usgs":true,"family":"Tillitt","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":419730,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fitzsimons, J.D.","contributorId":50845,"corporation":false,"usgs":true,"family":"Fitzsimons","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":419726,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Honeyfield, D. C. 0000-0003-3034-2047","orcid":"https://orcid.org/0000-0003-3034-2047","contributorId":73136,"corporation":false,"usgs":true,"family":"Honeyfield","given":"D. C.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":419729,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70028768,"text":"70028768 - 2005 - Estimation and mapping of wet and dry mercury deposition across northeastern North America","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70028768","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1479,"text":"Ecotoxicology","active":true,"publicationSubtype":{"id":10}},"title":"Estimation and mapping of wet and dry mercury deposition across northeastern North America","docAbstract":"Whereas many ecosystem characteristics and processes influence mercury accumulation in higher trophic-level organisms, the mercury flux from the atmosphere to a lake and its watershed is a likely factor in potential risk to biota. Atmospheric deposition clearly affects mercury accumulation in soils and lake sediments. Thus, knowledge of spatial patterns in atmospheric deposition may provide information for assessing the relative risk for ecosystems to exhibit excessive biotic mercury contamination. Atmospheric mercury concentrations in aerosol, vapor, and liquid phases from four observation networks were used to estimate regional surface concentration fields. Statistical models were developed to relate sparsely measured mercury vapor and aerosol concentrations to the more commonly measured mercury concentration in precipitation. High spatial resolution deposition velocities for different phases (precipitation, cloud droplets, aerosols, and reactive gaseous mercury (RGM)) were computed using inferential models. An empirical model was developed to estimate gaseous elemental mercury (GEM) deposition. Spatial patterns of estimated total mercury deposition were complex. Generally, deposition was higher in the southwest and lower in the northeast. Elevation, land cover, and proximity to urban areas modified the general pattern. The estimated net GEM and RGM fluxes were each greater than or equal to wet deposition in many areas. Mercury assimilation by plant foliage may provide a substantial input of methyl-mercury (MeHg) to ecosystems. ?? 2005 Springer Science+Business Media, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecotoxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10646-004-6259-9","issn":"09639292","usgsCitation":"Miller, E., Vanarsdale, A., Keeler, G., Chalmers, A., Poissant, L., Kamman, N., and Brulotte, R., 2005, Estimation and mapping of wet and dry mercury deposition across northeastern North America: Ecotoxicology, v. 14, no. 1-2, p. 53-70, https://doi.org/10.1007/s10646-004-6259-9.","startPage":"53","endPage":"70","numberOfPages":"18","costCenters":[],"links":[{"id":477895,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/2027.42/44443>","text":"External Repository"},{"id":209640,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10646-004-6259-9"},{"id":236303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0b72e4b0c8380cd52718","contributors":{"authors":[{"text":"Miller, E. K.","contributorId":9832,"corporation":false,"usgs":true,"family":"Miller","given":"E. K.","affiliations":[],"preferred":false,"id":419673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vanarsdale, A.","contributorId":44341,"corporation":false,"usgs":true,"family":"Vanarsdale","given":"A.","email":"","affiliations":[],"preferred":false,"id":419675,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keeler, G.J.","contributorId":96449,"corporation":false,"usgs":true,"family":"Keeler","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":419678,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chalmers, A.","contributorId":96858,"corporation":false,"usgs":true,"family":"Chalmers","given":"A.","email":"","affiliations":[],"preferred":false,"id":419679,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Poissant, L.","contributorId":35493,"corporation":false,"usgs":true,"family":"Poissant","given":"L.","email":"","affiliations":[],"preferred":false,"id":419674,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kamman, N.C.","contributorId":51079,"corporation":false,"usgs":true,"family":"Kamman","given":"N.C.","affiliations":[],"preferred":false,"id":419677,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Brulotte, R.","contributorId":47140,"corporation":false,"usgs":true,"family":"Brulotte","given":"R.","email":"","affiliations":[],"preferred":false,"id":419676,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70028766,"text":"70028766 - 2005 - Bison PRNP genotyping and potential association with Brucella spp. seroprevalence","interactions":[],"lastModifiedDate":"2015-12-11T14:43:30","indexId":"70028766","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":776,"text":"Animal Genetics","active":true,"publicationSubtype":{"id":10}},"title":"Bison PRNP genotyping and potential association with Brucella spp. seroprevalence","docAbstract":"<p>The implication that host cellular prion protein (PrPC) may function as a cell surface receptor and/or portal protein for Brucella abortus in mice prompted an evaluation of nucleotide and amino acid variation within exon 3 of the prion protein gene (PRNP) for six US bison populations. A non-synonymous single nucleotide polymorphism (T50C), resulting in the predicted amino acid replacement M17T (Met ??? Thr), was identified in each population. To date, no variation (T50: Met) has been detected at the corresponding exon 3 nucleotide and/or amino acid position for domestic cattle. Notably, 80% (20 of 25) of the Yellowstone National Park bison possessing the C/C genotype were Brucella spp. seropositive, representing a significant (P = 0.021) association between seropositivity and the C/C genotypic class. Moreover, significant differences in the distribution of PRNP exon 3 alleles and genotypes were detected between Yellowstone National Park bison and three bison populations that were either founded from seronegative stock or previously subjected to test-and-slaughter management to eradicate brucellosis. Unlike domestic cattle, no indel polymorphisms were detected within the corresponding regions of the putative bison PRNP promoter, intron 1, octapeptide repeat region or 3???-untranslated region for any population examined. This study provides the first evidence of a potential association between nucleotide variation within PRNP exon 3 and the presence of Brucella spp. antibodies in bison, implicating PrPC in the natural resistance of bison to brucellosis infection. ?? 2005 International Society for Animal Genetics.</p>","language":"English","publisher":"International Society for Animal Genetics","doi":"10.1111/j.1365-2052.2005.01240.x","issn":"02689146","usgsCitation":"Seabury, C., Halbert, N., Gogan, P., Templeton, J., and Derr, J., 2005, Bison PRNP genotyping and potential association with Brucella spp. seroprevalence: Animal Genetics, v. 36, no. 2, p. 104-110, https://doi.org/10.1111/j.1365-2052.2005.01240.x.","productDescription":"7 p.","startPage":"104","endPage":"110","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science 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J.W.","contributorId":101436,"corporation":false,"usgs":true,"family":"Templeton","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":419667,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Derr, J.N.","contributorId":86550,"corporation":false,"usgs":true,"family":"Derr","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":419666,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028873,"text":"70028873 - 2005 - Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028873","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia","docAbstract":"Increased tree growth in temperate and boreal forests has been proposed as a direct consequence of a warming climate. Acid deposition effects on nutrient availability may influence the climate dependency of tree growth, however. This study presents an analysis of archived soil samples that has enabled changes in soil chemistry to be tracked with patterns of tree growth through the 20th century. Soil samples collected in 1926, 1964, and 2001, near St. Petersburg, Russia, showed that acid deposition was likely to have decreased root-available concentrations of Ca (an essential element) and increased root-available concentrations of Al (an inhibitor of Ca uptake). These soil changes coincided with decreased diameter growth and a suppression of climate-tree growth relationships in Norway spruce. Expected increases in tree growth from climate warming may be limited by decreased soil fertility in regions of northern and eastern Europe, and eastern North America, where Ca availability has been reduced by acidic deposition. ?? 2005 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es048759o","issn":"0013936X","usgsCitation":"Lawrence, G., Lapenis, A., Berggren, D., Aparin, B., Smith, K., Shortle, W., Bailey, S., Varlyguin, D., and Babikov, B., 2005, Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia: Environmental Science & Technology, v. 39, no. 7, p. 2004-2010, https://doi.org/10.1021/es048759o.","startPage":"2004","endPage":"2010","numberOfPages":"7","costCenters":[],"links":[{"id":209981,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es048759o"},{"id":236761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"7","noUsgsAuthors":false,"publicationDate":"2005-02-16","publicationStatus":"PW","scienceBaseUri":"5059f651e4b0c8380cd4c6b1","contributors":{"authors":[{"text":"Lawrence, G.B. 0000-0002-8035-2350","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":76347,"corporation":false,"usgs":true,"family":"Lawrence","given":"G.B.","affiliations":[],"preferred":false,"id":420130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapenis, A.G.","contributorId":85701,"corporation":false,"usgs":true,"family":"Lapenis","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":420132,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berggren, D.","contributorId":35531,"corporation":false,"usgs":true,"family":"Berggren","given":"D.","email":"","affiliations":[],"preferred":false,"id":420128,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aparin, B.F.","contributorId":24899,"corporation":false,"usgs":true,"family":"Aparin","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":420126,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, K.T.","contributorId":94807,"corporation":false,"usgs":true,"family":"Smith","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":420133,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shortle, W.C.","contributorId":20919,"corporation":false,"usgs":true,"family":"Shortle","given":"W.C.","affiliations":[],"preferred":false,"id":420125,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bailey, S.W.","contributorId":29113,"corporation":false,"usgs":true,"family":"Bailey","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":420127,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Varlyguin, D.L.","contributorId":84967,"corporation":false,"usgs":true,"family":"Varlyguin","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":420131,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Babikov, B.","contributorId":71752,"corporation":false,"usgs":true,"family":"Babikov","given":"B.","email":"","affiliations":[],"preferred":false,"id":420129,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70028874,"text":"70028874 - 2005 - Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin","interactions":[],"lastModifiedDate":"2016-05-03T16:33:33","indexId":"70028874","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin","docAbstract":"<p>Fall Chinook salmon Oncorhynchus tshawytscha in the Snake River basin were listed under the Endangered Species Act in 1992. At the time of listing, it was assumed that fall Chinook salmon juveniles in the Snake River basin adhered strictly to an ocean-type life history characterized by saltwater entry at age 0 and first-year wintering in the ocean. Research showed, however, that some fall Chinook salmon juveniles in the Snake River basin spent their first winter in a reservoir and resumed seaward movement the following spring at age 1 (hereafter, reservoir-type juveniles). We collected wild and hatchery ocean-type fall Chinook salmon juveniles in 1997 and wild and hatchery reservoir-type juveniles in 1998 to assess the condition of the reservoir-type juveniles at the onset of seaward movement. The ocean-type juveniles averaged 112-139 mm fork length, and the reservoir-type juveniles averaged 222-224 mm fork length. The large size of the reservoir-type juveniles suggested a high potential for survival to salt water and subsequent return to freshwater. Scale pattern analyses of the fall Chinook salmon spawners we collected during 1998-2003 supported this point. Of the spawners sampled, an overall average of 41% of the wild fish and 51% of the hatchery fish had been reservoir-type juveniles. Males that had been reservoir-type juveniles often returned as small \"minijacks\" (wild, 16% of total; hatchery, 40% of total), but 84% of the wild males, 60% of the hatchery males, and 100% of the wild and hatchery females that had been reservoir-type juveniles returned at ages and fork lengths commonly observed in populations of Chinook salmon. We conclude that fall Chinook salmon in the Snake River basin exhibit two alternative juvenile life histories, namely ocean-type and reservoir-type. ?? Copyright by the American Fisheries Society 2005.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/T03-131.1","issn":"00028487","usgsCitation":"Connor, W., Sneva, J., Tiffan, K., Steinhorst, R., and Ross, D., 2005, Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin: Transactions of the American Fisheries Society, v. 134, no. 2, p. 291-304, https://doi.org/10.1577/T03-131.1.","productDescription":"14 p.","startPage":"291","endPage":"304","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":236791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210005,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T03-131.1"}],"country":"United States","state":"Idaho, Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.76293945312499,\n              43.84245116699036\n            ],\n            [\n              -116.38916015624999,\n              42.85985981506279\n            ],\n            [\n              -117.48779296875,\n              44.000717834282774\n            ],\n            [\n              -117.520751953125,\n              45.87471224890479\n            ],\n            [\n              -118.004150390625,\n              46.41513877649202\n            ],\n            [\n              -119.44335937499999,\n              45.67548217560647\n            ],\n            [\n              -123.12377929687499,\n              45.42158812329091\n            ],\n            [\n              -124.002685546875,\n              46.057985244793024\n            ],\n            [\n              -123.93676757812499,\n              46.33175800051563\n            ],\n            [\n              -122.882080078125,\n              46.263442671779885\n            ],\n            [\n              -122.354736328125,\n              45.81348649679971\n            ],\n            [\n              -120.60791015625,\n              46.03510927947334\n            ],\n            [\n              -119.124755859375,\n              46.34692761055676\n            ],\n            [\n              -118.311767578125,\n              46.74738913515841\n            ],\n            [\n              -116.60888671874999,\n              46.73233101286786\n            ],\n            [\n              -116.290283203125,\n              46.36209301204985\n            ],\n            [\n              -116.03759765625,\n              44.645208223744035\n            ],\n            [\n              -115.850830078125,\n              44.10336537791152\n            ],\n            [\n              -115.76293945312499,\n              43.84245116699036\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"134","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505bb94ae4b08c986b327bac","contributors":{"authors":[{"text":"Connor, W.P.","contributorId":98090,"corporation":false,"usgs":true,"family":"Connor","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":420138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sneva, J.G.","contributorId":7066,"corporation":false,"usgs":true,"family":"Sneva","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":420135,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tiffan, K.F.","contributorId":19327,"corporation":false,"usgs":true,"family":"Tiffan","given":"K.F.","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":420136,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steinhorst, R.K.","contributorId":89833,"corporation":false,"usgs":true,"family":"Steinhorst","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":420137,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ross, D.","contributorId":7049,"corporation":false,"usgs":true,"family":"Ross","given":"D.","affiliations":[],"preferred":false,"id":420134,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028876,"text":"70028876 - 2005 - Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028876","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1905,"text":"Holocene","active":true,"publicationSubtype":{"id":10}},"title":"Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada","docAbstract":"The north-flowing, low-gradient section of the Red River in Manitoba has lost ???60% of its valley gradient since 8 ka cal. BP. An existing hydraulic model of the modern Red River flood zone was used to examine the change in flood extent and depth of a discharge equivalent to the 1997 Red River flood (3970 m3/s) for scenarios of gradients at 8, 6, 4 and 2 ka cal. BP as well as 2 ka in the future. The modelling indicates a broad, shallow flood zone for all of the gradient scenarios, with extent and depth increasing over time. Between the 8 ka cal. BP and present-day scenarios, the flood zone increased from 1186 km2 to 1531 km2 (???29%) with depth increasing along four east-west cross-sections by 0.69 m (???61%), 0.91 m (???82%), 0.56 m (???64%) and 0.48 m (???86%). The flood extent and depths increased by a further 18 km2 (???5%) and 0.04-0.06 m (2-5%), respectively, by 2 ka in the future. Most of these changes to the flood zone occurred between 8 and 2 ka cal. BP, reflecting an exponential loss of gradient. A rise in flood depth equivalent to that which occurred between 8 ka cal. BP and the present-day, is assessed as increasing the long-term flood hazard; in contrast, the slight rise in depth between the present-day and 2 ka in the future does not. ?? 2005 Edward Arnold (Publishers) Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Holocene","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1191/0959683605hl804rp","issn":"09596836","usgsCitation":"Brooks, G.R., Thorleifson, L.H., and Lewis, C., 2005, Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada: Holocene, v. 15, no. 3, p. 347-352, https://doi.org/10.1191/0959683605hl804rp.","startPage":"347","endPage":"352","numberOfPages":"6","costCenters":[],"links":[{"id":210006,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1191/0959683605hl804rp"},{"id":236793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-04-01","publicationStatus":"PW","scienceBaseUri":"505a3b50e4b0c8380cd62401","contributors":{"authors":[{"text":"Brooks, G. R.","contributorId":96312,"corporation":false,"usgs":true,"family":"Brooks","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":420141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorleifson, L. Harvey","contributorId":103430,"corporation":false,"usgs":true,"family":"Thorleifson","given":"L.","email":"","middleInitial":"Harvey","affiliations":[{"id":38105,"text":"Minnesota Geological Survey","active":true,"usgs":false}],"preferred":false,"id":420142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, C.F.M.","contributorId":39971,"corporation":false,"usgs":true,"family":"Lewis","given":"C.F.M.","email":"","affiliations":[],"preferred":false,"id":420140,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003641,"text":"1003641 - 2005 - Exertional myopathy in whooping cranes (Grus americana) with prognostic guidlelines","interactions":[],"lastModifiedDate":"2022-05-26T16:01:57.259703","indexId":"1003641","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2514,"text":"Journal of Zoo and Wildlife Medicine","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Exertional myopathy in whooping cranes (<i>Grus americana</i>) with prognostic guidlelines","title":"Exertional myopathy in whooping cranes (Grus americana) with prognostic guidlelines","docAbstract":"<p><span>Exertional myopathy developed in three whooping cranes (</span><i><span class=\"genus-species\">Grus americana</span></i><span>) secondary to routine capture, handling, and trauma. Presumptive diagnosis of exertional myopathy was based on history of recent capture or trauma, clinical signs, and elevation of aspartate aminotransferase, alanine aminotransferase, creatine kinase, lactate dehydrogenase, and serum potassium. Treatments were attempted in each case, but ultimately were not successful. Gross and microscopic lesions at necropsy confirmed the diagnosis in each case, with the leg musculature most severely affected. Guidelines for determining prognosis of exertional myopathy in cranes have been included based on the analysis of these cases and others in the literature. As treatment is largely unrewarding, prevention remains the key in controlling exertional myopathy. Identification of predisposing factors and proper handling, immobilization, and transportation techniques can help prevent development of exertional myopathy in cranes.</span></p>","language":"English","publisher":"American Association of Zoo Veterinarians","doi":"10.1638/04-047.1","usgsCitation":"Hanley, C.S., Thomas, N.J., Paul-Murphy, J.R., and Hartup, B.K., 2005, Exertional myopathy in whooping cranes (Grus americana) with prognostic guidlelines: Journal of Zoo and Wildlife Medicine, v. 36, no. 3, p. 489-497, https://doi.org/10.1638/04-047.1.","productDescription":"9 p.","startPage":"489","endPage":"497","numberOfPages":"9","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":134168,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af0e4b07f02db691765","contributors":{"authors":[{"text":"Hanley, C. S.","contributorId":63777,"corporation":false,"usgs":true,"family":"Hanley","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":313786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Nancy J. 0000-0002-0161-0391 nthomas@usgs.gov","orcid":"https://orcid.org/0000-0002-0161-0391","contributorId":1673,"corporation":false,"usgs":true,"family":"Thomas","given":"Nancy","email":"nthomas@usgs.gov","middleInitial":"J.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":false,"id":313785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paul-Murphy, Joanne R.","contributorId":138654,"corporation":false,"usgs":false,"family":"Paul-Murphy","given":"Joanne","email":"","middleInitial":"R.","affiliations":[{"id":12479,"text":"Department of Medicine and Epidemiology, School of Veterinary Medicine, University of California, Davis, DA","active":true,"usgs":false}],"preferred":false,"id":313784,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hartup, Barry K.","contributorId":112921,"corporation":false,"usgs":true,"family":"Hartup","given":"Barry","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":313783,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1001777,"text":"1001777 - 2005 - Landscape composition, patch size, and distance to edges: Interactions affecting duck reproductive success","interactions":[],"lastModifiedDate":"2017-11-16T10:55:32","indexId":"1001777","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Landscape composition, patch size, and distance to edges: Interactions affecting duck reproductive success","docAbstract":"<p><span>Prairies and other North American grasslands, although highly fragmented, provide breeding habitat for a diverse array of species, including species of tremendous economic and ecological importance. Conservation and management of these species requires some understanding of how reproductive success is affected by edge effects, patch size, and characteristics of the landscape. We examined how differences in the percentage of grassland in the landscape influenced the relationships between the success of nests of upland-nesting ducks and (1) field size and (2) distance to nearest field and wetland edges. We collected data on study areas composed of 15–20% grassland and areas composed of 45–55% grassland in central North Dakota, USA during the 1996 and 1997 nesting seasons. Daily survival rates (DSRs) of duck nests were greater in study areas with 45–55% grassland than with 15–20% grassland. Within study areas, we detected a curvilinear relationship between DSR and field size: DSRs were highest in small and large fields and lowest in moderately sized fields. In study areas with 15–20% grassland, there was no relationship between probability of hatching and distance to nearest field edge, whereas in study areas with 45–55% grassland, there was a positive relationship between these two variables. Results of this study support the conclusion that both landscape composition and configuration affect reproductive success of ground-nesting birds. We are prompted to question conservation strategies that favor clustering moderately sized patches of nesting habitat within agricultural landscapes because our results show that such patches would have low nest success, most likely caused by predation. Understanding the pattern of nest success, and the predator–prey mechanisms that produce the pattern, will enable design of patch configurations that are most conducive to meeting conservation goals.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/03-5254","usgsCitation":"Horn, D.J., Phillips, M.L., Koford, R.R., Clark, W.R., Sovada, M.A., and Greenwood, R.J., 2005, Landscape composition, patch size, and distance to edges: Interactions affecting duck reproductive success: Ecological Applications, v. 15, no. 4, p. 1367-1376, https://doi.org/10.1890/03-5254.","productDescription":"10 p.","startPage":"1367","endPage":"1376","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6aba9b","contributors":{"authors":[{"text":"Horn, David Joseph","contributorId":174793,"corporation":false,"usgs":false,"family":"Horn","given":"David","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":311751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, Michael L.","contributorId":149855,"corporation":false,"usgs":false,"family":"Phillips","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":311748,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koford, Rolf R.","contributorId":16347,"corporation":false,"usgs":true,"family":"Koford","given":"Rolf","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":311746,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, William R.","contributorId":174794,"corporation":false,"usgs":false,"family":"Clark","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":311749,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sovada, Marsha A. msovada@usgs.gov","contributorId":2601,"corporation":false,"usgs":true,"family":"Sovada","given":"Marsha","email":"msovada@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":311747,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Greenwood, Raymond J.","contributorId":174570,"corporation":false,"usgs":false,"family":"Greenwood","given":"Raymond","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":311750,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70029644,"text":"70029644 - 2005 - Transmission of atmospherically derived trace elements through an undeveloped, forested Maryland watershed","interactions":[],"lastModifiedDate":"2018-10-31T10:14:56","indexId":"70029644","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Transmission of atmospherically derived trace elements through an undeveloped, forested Maryland watershed","docAbstract":"<p class=\"Para\">The transmission of atmospherically derived trace elements (Al, As, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Se, and Zn) was evaluated in a small, undeveloped, forested watershed located in north-central Maryland. Atmospheric input was determined for wet-only and vegetative throughfall components. Annual throughfall fluxes were significantly enriched over incident precipitation for most elements, although some elements exhibited evidence of canopy release (Mn) or preferential uptake (As, Cr, and Se). Stream export was gauged based on systematic sampling under varied flow regimes. Particle loading appears to contribute significantly to watershed export (&gt; 10%) for only As, Pb, and Fe, and then only during large precipitation/runoff events. The degree of watershed transmission for each trace element was evaluated based on a comparison of total, net atmospheric input (throughfall) to stream export over an annual hydrologic cycle. This comparison indicates that the atmospheric input of some elements (Al, Cd, Ni, Zn) is effectively transmitted through the watershed, but other elements (Pb, As, Se, Fe, Cr, Cu) appear to be strongly sequestered, in the respective orders noted. Results suggest that precipitation and subsequent soil pH are the primary factors that determine the mobility of sequestered trace element phases.</p><p class=\"Para\">To further resolve primary atmospheric and secondary weathering components, the geochemical model NETPATH was applied. Results indicate that minerals dissolved include chlorite, plagioclase feldspar, epidote, and potassium feldspar; phases formed were kaolinite, pyrite, and silica. The model also indicates that weathering processes contribute negligible amounts of trace elements to stream export, indicative of the unreactive orthoquartzite bedrock lithology underlying the watershed. Thus, the stream export of trace elements primarily reflects atmospheric deposition to the local watershed.</p>","language":"English","publisher":"Springer","doi":"10.1007/s11270-005-8135-5","issn":"00496979","usgsCitation":"Scudlark, J., Rice, K.C., Conko, K.M., Bricker, O.P., and Church, T., 2005, Transmission of atmospherically derived trace elements through an undeveloped, forested Maryland watershed: Water, Air, & Soil Pollution, v. 163, no. 1, p. 53-79, https://doi.org/10.1007/s11270-005-8135-5.","productDescription":"27 p.","startPage":"53","endPage":"79","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":240571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.7777099609375,\n              39.32155002466662\n            ],\n            [\n              -77.7777099609375,\n              39.70296052957233\n            ],\n            [\n              -77.32040405273436,\n              39.70296052957233\n            ],\n            [\n              -77.32040405273436,\n              39.32155002466662\n            ],\n            [\n              -77.7777099609375,\n              39.32155002466662\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"163","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb729e4b08c986b3270c0","contributors":{"authors":[{"text":"Scudlark, J.R.","contributorId":86952,"corporation":false,"usgs":true,"family":"Scudlark","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":423611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":423610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Conko, Kathryn M. 0000-0001-6361-4921 kmconko@usgs.gov","orcid":"https://orcid.org/0000-0001-6361-4921","contributorId":2930,"corporation":false,"usgs":true,"family":"Conko","given":"Kathryn","email":"kmconko@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":423609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bricker, Owen P.","contributorId":25142,"corporation":false,"usgs":true,"family":"Bricker","given":"Owen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":423608,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Church, T.M.","contributorId":18581,"corporation":false,"usgs":true,"family":"Church","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":423607,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029668,"text":"70029668 - 2005 - A spatial model of potential jaguar habitat in Arizona","interactions":[],"lastModifiedDate":"2016-05-05T15:29:44","indexId":"70029668","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"A spatial model of potential jaguar habitat in Arizona","docAbstract":"<p>The jaguar (Panthera onca) is an endangered species that occasionally visits the southwestern United States from Mexico. The number of jaguar sightings per decade has declined over the last 100 years in Arizona, USA, raising conservation concerns for the species at a local and national level. In 1997, state, federal, and local governments with land-management responsibilities agreed to characterize and identify potential jaguar habitat in Arizona and New Mexico. Specifically, the objectives of our analysis were 2-fold: (1) characterize potential jaguar habitat in Arizona from historic sighting records and (2) create a statewide habitat suitability map. We used a Geographic Information System (GIS) to characterize potential jaguar habitat by overlaying historic jaguar sightings (25) on landscape and habitat features believed important (e.g., vegetation biomes and series, elevation, terrain ruggedness, proximity to perennial or intermittent water sources, human density). The amount of Arizona (%) identified as potential jaguar habitat ranged from 21% to 30% depending on the input variables. Most jaguar sightings were in scrub grasslands between 1,220 and 1,829-m elevation in southeastern Arizona, in intermediately to extremely rugged terrain, and within 10 km of a water source. Conservation efforts should focus on protecting the most suitable jaguar habitat in southeastern Arizona (i.e., Santa Cruz, Pima, Cochise, Pinal, Graham counties), travel corridors within and outside Arizona, and jaguar habitat in the Sierra Madres of Sonora, Mexico.</p>","language":"English","publisher":"Bioone","doi":"10.2193/0022-541X(2005)069[1024:ASMOPJ]2.0.CO;2","issn":"0022541X","usgsCitation":"Hatten, J., Averill-Murray, A., and van Pelt, W., 2005, A spatial model of potential jaguar habitat in Arizona: Journal of Wildlife Management, v. 69, no. 3, p. 1024-1033, https://doi.org/10.2193/0022-541X(2005)069[1024:ASMOPJ]2.0.CO;2.","productDescription":"10 p.","startPage":"1024","endPage":"1033","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":240375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212828,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0022-541X(2005)069[1024:ASMOPJ]2.0.CO;2"}],"volume":"69","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e5a1e4b0c8380cd46ea1","contributors":{"authors":[{"text":"Hatten, J.R.","contributorId":39564,"corporation":false,"usgs":true,"family":"Hatten","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":423738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Averill-Murray, A.","contributorId":64456,"corporation":false,"usgs":true,"family":"Averill-Murray","given":"A.","email":"","affiliations":[],"preferred":false,"id":423739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"van Pelt, W.E.","contributorId":73013,"corporation":false,"usgs":true,"family":"van Pelt","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":423740,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003642,"text":"1003642 - 2005 - The impact of disease in the American white pelican in North America","interactions":[],"lastModifiedDate":"2018-01-17T13:36:08","indexId":"1003642","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"The impact of disease in the American white pelican in North America","docAbstract":"<p>Records of reported die-offs of the American White Pelican (Pelicanus erythrorhynchos) held by the U.S. Geological Survey National Wildlife Health Center from 1978 through 2003 indicate that type C botulism (caused by Clostridium botulinum) was the major cause of mortality. In 1996, over 15,000 birds, including 8,500 American White Pelicans, were estimated to have died from type C botulism at the Salton Sea in California. This was the largest documented die-off of any pelican species and was estimated to represent 15-20% of the western metapopulation. This event was also notable in that it was the first time that fish, specifically Tilapia (Oreochromis mossambicus), were implicated as the source of type C botulinum toxin for birds. Type C botulism has recurred in both North American species of pelicans at the Salton Sea every year since, although the magnitude of mortality is much lower. West Nile virus caused mortality in both adult and immature American White Pelicans, but may have a more significant impact on nestlings. Emaciation and mortality is common in pelican nesting colonies. Further clarification of the cause of nestling mortality and the ability to differentiate background mortality from mortality due to infectious disease agents such as West Nile virus and Newcastle disease virus would be important in determining the impact of disease in pelicans. Although definitive conclusions cannot be drawn, the number of die-offs and the estimated losses of American White Pelicans appears to have increased along with declines in number in western U.S.</p>","language":"English","publisher":"The Waterbird Society","doi":"10.1675/1524-4695(2005)28[87:TIODIT]2.0.CO;2","usgsCitation":"Rocke, T.E., Converse, K.A., Meteyer, C.U., and McLean, R., 2005, The impact of disease in the American white pelican in North America: Waterbirds, v. 28, no. 1, p. 87-94, https://doi.org/10.1675/1524-4695(2005)28[87:TIODIT]2.0.CO;2.","productDescription":"8 p.","startPage":"87","endPage":"94","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":135836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United 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Tonie E. 0000-0003-3933-1563 trocke@usgs.gov","orcid":"https://orcid.org/0000-0003-3933-1563","contributorId":2665,"corporation":false,"usgs":true,"family":"Rocke","given":"Tonie","email":"trocke@usgs.gov","middleInitial":"E.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":313789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Converse, Kathryn A. kathy_converse@usgs.gov","contributorId":16802,"corporation":false,"usgs":true,"family":"Converse","given":"Kathryn","email":"kathy_converse@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":false,"id":313788,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meteyer, Carol U. 0000-0002-4007-3410 cmeteyer@usgs.gov","orcid":"https://orcid.org/0000-0002-4007-3410","contributorId":111,"corporation":false,"usgs":true,"family":"Meteyer","given":"Carol","email":"cmeteyer@usgs.gov","middleInitial":"U.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":false,"id":313787,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McLean, R.","contributorId":107230,"corporation":false,"usgs":true,"family":"McLean","given":"R.","affiliations":[],"preferred":false,"id":313790,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031426,"text":"70031426 - 2005 - Reply to \"Comment on 'How can seismic hazard around the New Madrid seismic zone be similar to that in California?' by Arthur Frankel\", by Zhenming Wang, Baoping Shi, and John D. Kiefer","interactions":[],"lastModifiedDate":"2022-06-03T14:35:02.130098","indexId":"70031426","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Reply to \"Comment on 'How can seismic hazard around the New Madrid seismic zone be similar to that in California?' by Arthur Frankel\", by Zhenming Wang, Baoping Shi, and John D. Kiefer","docAbstract":"[No abstract available]","language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.76.4.472","usgsCitation":"Frankel, A., 2005, Reply to \"Comment on 'How can seismic hazard around the New Madrid seismic zone be similar to that in California?' by Arthur Frankel\", by Zhenming Wang, Baoping Shi, and John D. Kiefer: Seismological Research Letters, v. 76, no. 4, p. 472-475, https://doi.org/10.1785/gssrl.76.4.472.","productDescription":"4 p.","startPage":"472","endPage":"475","numberOfPages":"4","costCenters":[],"links":[{"id":240135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa75be4b0c8380cd8537f","contributors":{"authors":[{"text":"Frankel, Arthur","contributorId":103761,"corporation":false,"usgs":true,"family":"Frankel","given":"Arthur","affiliations":[],"preferred":false,"id":431452,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029654,"text":"70029654 - 2005 - Paleobiogeographic patterns in Late Mississippian trilobites of the United States with new species from Montana","interactions":[],"lastModifiedDate":"2012-03-12T17:21:38","indexId":"70029654","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":790,"text":"Annals of Carnegie Museum","active":true,"publicationSubtype":{"id":10}},"title":"Paleobiogeographic patterns in Late Mississippian trilobites of the United States with new species from Montana","docAbstract":"Two new species of trilobites, Weberides chamberlaini new species and Weberides samwaysi new species, are described from the Heath Formation (Serpukhovian, Mississippian) of Montana. Based upon phylogenetic analysis, the assignment of these species to the genus Weberides represents the first recognition of this genus in North America. Brooks Parsimony Analysis of the single phylogenetic tree suggests that the northern Cordillera acted as an ancestral area for the typically European genus Weberides. Thus, the North American vicariants of Weberides share a common ancestral area with the genus Paladin. Vicariance patterns suggest that interchange with the type Weberides areas of Europe was through the northern Cordilleran region rather than through the Rheic Ocean, as others have suggested.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Annals of Carnegie Museum","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00974463","usgsCitation":"Brezinski, D., 2005, Paleobiogeographic patterns in Late Mississippian trilobites of the United States with new species from Montana: Annals of Carnegie Museum, v. 74, no. 2, p. 77-89.","startPage":"77","endPage":"89","numberOfPages":"13","costCenters":[],"links":[{"id":240702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a73b0e4b0c8380cd771b4","contributors":{"authors":[{"text":"Brezinski, D. K.","contributorId":39010,"corporation":false,"usgs":true,"family":"Brezinski","given":"D. K.","affiliations":[],"preferred":false,"id":423658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027821,"text":"70027821 - 2005 - Statistical characterization of a large geochemical database and effect of sample size","interactions":[],"lastModifiedDate":"2012-03-12T17:21:18","indexId":"70027821","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Statistical characterization of a large geochemical database and effect of sample size","docAbstract":"The authors investigated statistical distributions for concentrations of chemical elements from the National Geochemical Survey (NGS) database of the U.S. Geological Survey. At the time of this study, the NGS data set encompasses 48,544 stream sediment and soil samples from the conterminous United States analyzed by ICP-AES following a 4-acid near-total digestion. This report includes 27 elements: Al, Ca, Fe, K, Mg, Na, P, Ti, Ba, Ce, Co, Cr, Cu, Ga, La, Li, Mn, Nb, Nd, Ni, Pb, Sc, Sr, Th, V, Y and Zn. The goal and challenge for the statistical overview was to delineate chemical distributions in a complex, heterogeneous data set spanning a large geographic range (the conterminous United States), and many different geological provinces and rock types. After declustering to create a uniform spatial sample distribution with 16,511 samples, histograms and quantile-quantile (Q-Q) plots were employed to delineate subpopulations that have coherent chemical and mineral affinities. Probability groupings are discerned by changes in slope (kinks) on the plots. Major rock-forming elements, e.g., Al, Ca, K and Na, tend to display linear segments on normal Q-Q plots. These segments can commonly be linked to petrologic or mineralogical associations. For example, linear segments on K and Na plots reflect dilution of clay minerals by quartz sand (low in K and Na). Minor and trace element relationships are best displayed on lognormal Q-Q plots. These sensitively reflect discrete relationships in subpopulations within the wide range of the data. For example, small but distinctly log-linear subpopulations for Pb, Cu, Zn and Ag are interpreted to represent ore-grade enrichment of naturally occurring minerals such as sulfides. None of the 27 chemical elements could pass the test for either normal or lognormal distribution on the declustered data set. Part of the reasons relate to the presence of mixtures of subpopulations and outliers. Random samples of the data set with successively smaller numbers of data points showed that few elements passed standard statistical tests for normality or log-normality until sample size decreased to a few hundred data points. Large sample size enhances the power of statistical tests, and leads to rejection of most statistical hypotheses for real data sets. For large sample sizes (e.g., n > 1000), graphical methods such as histogram, stem-and-leaf, and probability plots are recommended for rough judgement of probability distribution if needed. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.apgeochem.2005.06.006","issn":"08832927","usgsCitation":"Zhang, C., Manheim, F., Hinde, J., and Grossman, J.N., 2005, Statistical characterization of a large geochemical database and effect of sample size: Applied Geochemistry, v. 20, no. 10, p. 1857-1874, https://doi.org/10.1016/j.apgeochem.2005.06.006.","startPage":"1857","endPage":"1874","numberOfPages":"18","costCenters":[],"links":[{"id":211232,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.apgeochem.2005.06.006"},{"id":238470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9722e4b08c986b31b8d4","contributors":{"authors":[{"text":"Zhang, C.","contributorId":16646,"corporation":false,"usgs":true,"family":"Zhang","given":"C.","email":"","affiliations":[],"preferred":false,"id":415358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":415361,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinde, J.","contributorId":25353,"corporation":false,"usgs":true,"family":"Hinde","given":"J.","email":"","affiliations":[],"preferred":false,"id":415359,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grossman, J. N.","contributorId":41840,"corporation":false,"usgs":true,"family":"Grossman","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":415360,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031547,"text":"70031547 - 2005 - Late Quaternary eolian and alluvial response to paleoclimate, Canyonlands, southeastern Utah","interactions":[],"lastModifiedDate":"2012-03-12T17:21:11","indexId":"70031547","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Late Quaternary eolian and alluvial response to paleoclimate, Canyonlands, southeastern Utah","docAbstract":"In upland areas of Canyonlands National Park, Utah, thin deposits and paleosols show late Quaternary episodes of eolian sedimentation, pedogenesis, and climate change. Interpretation of the stratigraphy and optically stimulated luminescence ages of eolian and nearby alluvial deposits, their pollen, and intercalated paleosols yields the following history: (1) Eolian deposition at ca. 46 ka, followed by several episodes of alluviation from some time before ca. 40 ka until after 16 ka (calibrated). (2) Eolian deposition from ca. 17 ka to 12 ka, interrupted by periods of pedogenesis, coinciding with late Pleistocene alluviation as local climate became warmer and wetter. (3) A wetter period from 12 to 8.5 ka corresponding to the peak of summer monsoon influence, during which soils formed relatively quickly by infiltration of eolian silt and clay, and trees and grasses were more abundant. (4) A drier period between ca. 8.5 and 6 ka during which sheetwash deposits accumulated and more desertlike vegetation was dominant; some dunes were reactivated at ca. 8 ka. (5) Episodic eolian and fluvial deposition during a wetter, cooler period that began at ca. 6 ka and ended by ca. 3-2 ka, followed by a shift to drier modern conditions; localized mobilization of dune sand has persisted to the present. These interpretations are similar to those of studies at the Chaco dune field, New Mexico, and the Tusayan dune field, Arizona, and are consistent with paleoclimate interpretations of pollen and packrat middens in the region. A period of rapid deposition and infiltration of eolian dust derived from distant igneous source terranes occurred between ca. 12 and 8 ka. Before ca. 17 ka, and apparently back to at least 45 ka, paleosols contain little or no such infiltrated dust. After ca. 8 ka, either the supply of dust was reduced or the more arid climate inhibited translocation of dust into the soils. ?? 2005 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/B25631.1","issn":"00167606","usgsCitation":"Reheis, M., Reynolds, R.L., Goldstein, H., Roberts, H., Yount, J.C., Axford, Y., Cummings, L., and Shearin, N., 2005, Late Quaternary eolian and alluvial response to paleoclimate, Canyonlands, southeastern Utah: Geological Society of America Bulletin, v. 117, no. 7-8, p. 1051-1069, https://doi.org/10.1130/B25631.1.","startPage":"1051","endPage":"1069","numberOfPages":"19","costCenters":[],"links":[{"id":212329,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B25631.1"},{"id":239796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"7-8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4529e4b0c8380cd670a7","contributors":{"authors":[{"text":"Reheis, M.C. 0000-0002-8359-323X","orcid":"https://orcid.org/0000-0002-8359-323X","contributorId":36128,"corporation":false,"usgs":true,"family":"Reheis","given":"M.C.","affiliations":[],"preferred":false,"id":432034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, R. 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C.","contributorId":69553,"corporation":false,"usgs":true,"family":"Yount","given":"J.","middleInitial":"C.","affiliations":[],"preferred":false,"id":432036,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Axford, Y.","contributorId":20547,"corporation":false,"usgs":true,"family":"Axford","given":"Y.","affiliations":[],"preferred":false,"id":432032,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cummings, L.S.","contributorId":42783,"corporation":false,"usgs":true,"family":"Cummings","given":"L.S.","affiliations":[],"preferred":false,"id":432035,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Shearin, N.","contributorId":23760,"corporation":false,"usgs":true,"family":"Shearin","given":"N.","email":"","affiliations":[],"preferred":false,"id":432033,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70027565,"text":"70027565 - 2005 - Growth, dispersal, mortality, and contribution of largemouth bass stocked into Chickamauga Lake, Tennessee","interactions":[],"lastModifiedDate":"2012-03-12T17:21:16","indexId":"70027565","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Growth, dispersal, mortality, and contribution of largemouth bass stocked into Chickamauga Lake, Tennessee","docAbstract":"Marked fingerling largemouth bass Micropterus salmoides (both northern M. s. salmoides and Florida subspecies M. s. floridanus and their hybrid) were stocked into Chickamauga Lake, Tennessee, to enhance angling and introgress the Florida subspecies into the local gene pool. We evaluated mass marking and stocking success by sampling the stocked fish for 1 year poststocking. More than 128,000 fingerlings (35-64 mm total length) were immersed in a solution of 500 mg/L oxytetracycline (OTC) for 6 h and stocked into four embayments in the lake in spring 2002; two additional embayments served as controls and were not stocked (these embayments contained only wild, indigenous fish). In a blind test, 97% of sagittal otoliths were correctly scored as marked or unmarked. In a subsequent test, the OTC marks were clearly visible on every otolith removed from 240 OTC-treated bass held for 30 d. Age-0 largemouth bass were sampled with DC electrofishing gear at 7-19, 44-61, and 119-139 d after stocking, and sampling was conducted along 100-m transects within 1 km of the stocking sites in each embayment. Of all recaptures in the first sample, 31% occurred more than 600 m from the nearest stocking site, indicating rapid dispersal by some fish. Survival of stocked and wild age-0 largemouth bass was similar and low (4.5-6.9%) in two embayments; in the other two embayments, stocked fish survived at lower rates (0-4.3%) than wild fish (33.7-49.9%). Mean catches of all age-0 largemouth bass in the first sample were positively related to the number of fish stocked. By October 2002, the mean catch of all age-0 largemouth bass was similar among embayments. Contribution of stocked fish declined to approximately 2% (2 of 91 fish) the following spring. Cost per fingerling increased from US$0.35 at stocking to $12.00 at 140 d poststocking. Increasing the abundance of largemouth bass was not the primary objective of this stocking effort, but stocked fish will have to survive much better if managers hope to introgress Florida largemouth bass genes into the resident population genome.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/M04-164.1","issn":"02755947","usgsCitation":"Hoffman, K., and Bettoli, P., 2005, Growth, dispersal, mortality, and contribution of largemouth bass stocked into Chickamauga Lake, Tennessee: North American Journal of Fisheries Management, v. 25, no. 4, p. 1518-1527, https://doi.org/10.1577/M04-164.1.","startPage":"1518","endPage":"1527","numberOfPages":"10","costCenters":[],"links":[{"id":211223,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/M04-164.1"},{"id":238455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-11-01","publicationStatus":"PW","scienceBaseUri":"505a2e11e4b0c8380cd5c295","contributors":{"authors":[{"text":"Hoffman, K.J.","contributorId":13809,"corporation":false,"usgs":true,"family":"Hoffman","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":414177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bettoli, P.W.","contributorId":80606,"corporation":false,"usgs":true,"family":"Bettoli","given":"P.W.","affiliations":[],"preferred":false,"id":414178,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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