{"pageNumber":"2604","pageRowStart":"65075","pageSize":"25","recordCount":184615,"records":[{"id":70029366,"text":"70029366 - 2005 - A new synziphosurine (Chelicerata: Xiphosura) from the Late Llandovery (Silurian) Waukesha Lagerstatte, Wisconsin, USA","interactions":[],"lastModifiedDate":"2022-05-24T16:02:17.12566","indexId":"70029366","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"A new synziphosurine (Chelicerata: Xiphosura) from the Late Llandovery (Silurian) Waukesha Lagerstatte, Wisconsin, USA","docAbstract":"<p><span>A new synziphosurine (Chelicerata:Xiphosura) is described from the Late Llandovery (Silurian) Konservat-Lagerstätte of Waukesha, Wisconsin, USA.&nbsp;</span><i><span class=\"genus-species\">Venustulus waukeshaensis</span></i><span><i>&nbsp;</i>n.gen. and sp. is characterized by a semicircular carapace with a slightly procurved posterior margin lacking genal spines and an opisthosoma composed of 10 freely articulating segments, divided into a preabdomen of seven segments with blunt pleurae and a postabdomen of three segments lacking pleurae. The tail spine is short and styliform. This is the earliest known unequivocal synziphosurine, extending their fossil record from the Wenlock to the Llandovery, and only the second species to be described with prosomal appendages; the presence of six pairs (a pair of chelicerae and five pairs of walking legs) contrasts with the seven in the synziphosurine&nbsp;</span><i><span class=\"genus-species\">Weinbergina opitzi</span></i><span>, but is comparable to the number in modern horseshoe crabs.&nbsp;</span><i><span class=\"genus-species\">V. waukeshaensis</span></i><span>&nbsp;n. gen. and sp. is not assigned to a family here pending a wider revision, but it bears most resemblance to the Weinberginidae.</span></p>","language":"English","publisher":"Society of Economic Paleontologists and Mineralogists","doi":"10.1666/0022-3360(2005)079%3C0242:ANSCXF%3E2.0.CO;2","usgsCitation":"Moore, R.A., Briggs, D.E., Braddy, S.J., Anderson, L.I., Mikulic, D.G., and Kluessendorf, J., 2005, A new synziphosurine (Chelicerata: Xiphosura) from the Late Llandovery (Silurian) Waukesha Lagerstatte, Wisconsin, USA: Journal of Paleontology, v. 79, no. 2, p. 242-250, https://doi.org/10.1666/0022-3360(2005)079%3C0242:ANSCXF%3E2.0.CO;2.","productDescription":"9 p.","startPage":"242","endPage":"250","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":237917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.4124755859375,\n              42.93229601903058\n            ],\n            [\n              -88.0059814453125,\n              42.93229601903058\n            ],\n            [\n              -88.0059814453125,\n              43.167125915000284\n            ],\n            [\n              -88.4124755859375,\n              43.167125915000284\n            ],\n            [\n              -88.4124755859375,\n              42.93229601903058\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"79","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4b8e4b0c8380cd4688a","contributors":{"authors":[{"text":"Moore, R. A.","contributorId":89713,"corporation":false,"usgs":false,"family":"Moore","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":422434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, D. E. G.","contributorId":11758,"corporation":false,"usgs":false,"family":"Briggs","given":"D.","email":"","middleInitial":"E. G.","affiliations":[],"preferred":false,"id":422429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Braddy, S. J.","contributorId":61631,"corporation":false,"usgs":false,"family":"Braddy","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422433,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Anderson, L. I.","contributorId":46300,"corporation":false,"usgs":false,"family":"Anderson","given":"L.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":422431,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mikulic, Donald G.","contributorId":61159,"corporation":false,"usgs":true,"family":"Mikulic","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":422432,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kluessendorf, Joanne","contributorId":41965,"corporation":false,"usgs":true,"family":"Kluessendorf","given":"Joanne","email":"","affiliations":[],"preferred":false,"id":422430,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70029368,"text":"70029368 - 2005 - Origin of secondary sulfate minerals on active andesitic stratovolcanoes","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029368","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":"Origin of secondary sulfate minerals on active andesitic stratovolcanoes","docAbstract":"Sulfate minerals in altered rocks on the upper flanks and summits of active andesitic stratovolcanoes result from multiple processes. The origin of these sulfates at five active volcanoes, Citlalte??petl (Mexico), and Mount Adams, Hood, Rainier, and Shasta (Cascade Range, USA), was investigated using field observations, petrography, mineralogy, chemical modeling, and stable-isotope data. The four general groups of sulfate minerals identified are: (1) alunite group, (2) jarosite group, (3) readily soluble Fe- and Al-hydroxysulfates, and (4) simple alkaline-earth sulfates such as anhydrite, gypsum, and barite. Generalized assemblages of spatially associated secondary minerals were recognized: (1) alunite+silica??pyrite??kaolinite?? gypsum??sulfur, (2) jarosite+alunite+silica; (3) jarosite+smectite+silica??pyrite, (4) Fe- and Al-hydroxysulfates+silica, and (5) simple sulfates+silica??Al-hydroxysulfates??alunite. Isotopic data verify that all sulfate and sulfide minerals and their associated alteration assemblages result largely from the introduction of sulfur-bearing magmatic gases into meteoric water in the upper levels of the volcanoes. The sulfur and oxygen isotopic data for all minerals indicate the general mixing of aqueous sulfate derived from deep (largely disproportionation of SO2 in magmatic vapor) and shallow (oxidation of pyrite or H2S) sources. The hydrogen and oxygen isotopic data of alunite indicate the mixing of magmatic and meteoric fluids. Some alunite-group minerals, along with kaolinite, formed from sulfuric acid created by the disproportionation of SO2 in a condensing magmatic vapor. Such alunite, observed only in those volcanoes whose interiors are exposed by erosion or edifice collapse, may have ??34S values that reflect equilibrium (350??50 ??C) between aqueous sulfate and H2S. Alunite with ??34S values indicating disequilibrium between parent aqueous sulfate and H2S may form from aqueous sulfate created in higher level low-temperature environments in which SO2 is scrubbed out by groundwater or where H2S is oxidized. Jarosite-group minerals associated with smectite in only slightly altered volcanic rock are formed largely from aqueous sulfate derived from supergene oxidation of hydrothermal pyrite above the water table. Soluble Al- and Fehydroxysulfates form in low-pH surface environments, especially around fumaroles, and from the oxidation of hydrothermal pyrite. Anhydrite/gypsum, often associated with native sulfur and occasionally with small amounts of barite, also commonly form around fumaroles. Some occurrences of anhydrite/gypsum may be secondary, derived from the dissolution and reprecipitation of soluble sulfate. Edifice collapse may also reveal deep veins of anhydrite/gypsum??barite that formed from the mixing of saline fluids with magmatic sulfate and dilute meteoric water. Alteration along structures associated with both hydrothermal and supergene sulfates, as well as the position of paleo-water tables, may be important factors in edifice collapse and resulting debris flows at some volcanoes. ?? 2004 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.06.056","issn":"00092541","usgsCitation":"Zimbelman, D.R., Rye, R.O., and Breit, G.N., 2005, Origin of secondary sulfate minerals on active andesitic stratovolcanoes: Chemical Geology, v. 215, no. 1-4 SPEC. ISS., p. 37-60, https://doi.org/10.1016/j.chemgeo.2004.06.056.","startPage":"37","endPage":"60","numberOfPages":"24","costCenters":[],"links":[{"id":210453,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.06.056"},{"id":237374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"215","issue":"1-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a70f2e4b0c8380cd76362","contributors":{"authors":[{"text":"Zimbelman, D. R.","contributorId":43768,"corporation":false,"usgs":true,"family":"Zimbelman","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":422438,"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":422439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Breit, G. N.","contributorId":94664,"corporation":false,"usgs":true,"family":"Breit","given":"G.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":422440,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029374,"text":"70029374 - 2005 - Relative abundance, age, growth, and fecundity of grubby Myoxocephalus aenaeus in Niantic River and Niantic Bay, Long Island Sound","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029374","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2449,"text":"Journal of Sea Research","active":true,"publicationSubtype":{"id":10}},"title":"Relative abundance, age, growth, and fecundity of grubby Myoxocephalus aenaeus in Niantic River and Niantic Bay, Long Island Sound","docAbstract":"Grubby (Myoxocephalus aenaeus, Cottidae) is a common benthic fish of inshore waters and estuaries of eastern Long Island Sound; however, little information exists on their life history or population demographics. This study utilised a long-term data series (1976-2002) to assess grubby life history and population demographics and explores trends in the Niantic River and Niantic Bay populations. In addition, we examined the age, size, and fecundity of adult grubby in 2001-02 to determine the population characteristics in the region. Mean grubby catch per unit effort (CPUE) in Niantic Bay ranged from 0.4 per trawl in 1976 to 2.9 per trawl in 1984 while river CPUE ranged from 0.4 per trawl in 1977 to 7.6 per trawl in 1989. Catch of grubby in bottom trawls varied seasonally with highest CPUE occurring in winter. Highest entrainment of grubby larvae occurred in 2001 while the lowest entrainment observed was in 1991. Four age classes, 0+ through III+, were derived from otolith analysis (N = 51) although length frequency analysis suggested the possibility of older fish in the population. The total number of eggs in ovaries ranged from 286 to 16 451 for grubby (N = 64) between 52 mm and 155 mm TL. Results of this study indicated a decline in abundance of adult grubby over the 26-year period, possibly related to concurrent declines in eelgrass (Zostera marina) abundance and/or increased water temperature. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sea Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.seares.2005.02.002","issn":"13851101","usgsCitation":"Roseman, E., Tomichek, C., Maynard, T., and Burton, J., 2005, Relative abundance, age, growth, and fecundity of grubby Myoxocephalus aenaeus in Niantic River and Niantic Bay, Long Island Sound: Journal of Sea Research, v. 53, no. 4, p. 309-318, https://doi.org/10.1016/j.seares.2005.02.002.","startPage":"309","endPage":"318","numberOfPages":"10","costCenters":[],"links":[{"id":237446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210508,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.seares.2005.02.002"}],"volume":"53","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa670e4b0c8380cd84e5b","contributors":{"authors":[{"text":"Roseman, E.F. 0000-0002-5315-9838","orcid":"https://orcid.org/0000-0002-5315-9838","contributorId":76531,"corporation":false,"usgs":true,"family":"Roseman","given":"E.F.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":422464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tomichek, C.A.","contributorId":90926,"corporation":false,"usgs":true,"family":"Tomichek","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":422465,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maynard, T.","contributorId":105904,"corporation":false,"usgs":true,"family":"Maynard","given":"T.","email":"","affiliations":[],"preferred":false,"id":422466,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burton, J.A.","contributorId":41205,"corporation":false,"usgs":true,"family":"Burton","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":422463,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029379,"text":"70029379 - 2005 - Distribution patterns of mercury in Lakes and Rivers of northeastern North America","interactions":[],"lastModifiedDate":"2016-08-24T17:30:01","indexId":"70029379","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":"Distribution patterns of mercury in Lakes and Rivers of northeastern North America","docAbstract":"<p><span>We assembled 831 data points for total mercury (Hg</span><sub>t</sub><span>) and 277 overlapping points for methyl mercury (CH</span><sub>3</sub><span>Hg</span><sup>+</sup><span>) in surface waters from Massachussetts, USA to the Island of Newfoundland, Canada from State, Provincial, and Federal government databases. These geographically indexed values were used to determine: (a) if large-scale spatial distribution patterns existed and (b) whether there were significant relationships between the two main forms of aquatic Hg as well as with total organic carbon (TOC), a well know complexer of metals. We analyzed the catchments where samples were collected using a Geographical Information System (GIS) approach, calculating catchment sizes, mean slope, and mean wetness index. Our results show two main spatial distribution patterns. We detected loci of high Hg</span><sub>t</sub><span> values near urbanized regions of Boston MA and Portland ME. However, except for one unexplained exception, the highest Hg</span><sub>t</sub><span> and CH</span><sub>3</sub><span>Hg</span><sup>+</sup><span> concentrations were located in regions far from obvious point sources. These correlated to topographically flat (and thus wet) areas that we relate to wetland abundances. We show that aquatic Hg</span><sub>t</sub><span> and CH</span><sub>3</sub><span>Hg</span><sup>+</sup><span> concentrations are generally well correlated with TOC and with each other. Over the region, CH</span><sub>3</sub><span>Hg</span><sup>+</sup><span> concentrations are typically approximately 15% of Hg</span><sub>t</sub><span>. There is an exception in the Boston region where CH</span><sub>3</sub><span>Hg</span><sup>+</sup><span> is low compared to the high Hg</span><sub>t</sub><span> values. This is probably due to the proximity of point sources of inorganic Hg and a lack of wetlands. We also attempted to predict Hg concentrations in water with statistical models using catchment features as variables. We were only able to produce statistically significant predictive models in some parts of regions due to the lack of suitable digital information, and because data ranges in some regions were too narrow for meaningful regression analyses.</span></p>","language":"English","publisher":"Chapman & Hall","doi":"10.1007/s10646-004-6263-0","issn":"09639292","usgsCitation":"Dennis, I.F., Clair, T.A., Driscoll, C.T., Kamman, N., Chalmers, A.T., Shanley, J., Norton, S.A., and Kahl, S., 2005, Distribution patterns of mercury in Lakes and Rivers of northeastern North America: Ecotoxicology, v. 14, no. 1-2, p. 113-123, https://doi.org/10.1007/s10646-004-6263-0.","productDescription":"11 p.","startPage":"113","endPage":"123","costCenters":[],"links":[{"id":237559,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Maine, Massachusetts, New Brunswick, New Hampshire, New York, Newfoundland, Nova Scotia, 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chalmers@usgs.gov","orcid":"https://orcid.org/0000-0002-5199-8080","contributorId":1443,"corporation":false,"usgs":true,"family":"Chalmers","given":"Ann","email":"chalmers@usgs.gov","middleInitial":"T.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":422486,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shanley, Jamie","contributorId":72922,"corporation":false,"usgs":true,"family":"Shanley","given":"Jamie","email":"","affiliations":[],"preferred":false,"id":422482,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Norton, Stephen A.","contributorId":84384,"corporation":false,"usgs":true,"family":"Norton","given":"Stephen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":422481,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kahl, Steve","contributorId":174043,"corporation":false,"usgs":false,"family":"Kahl","given":"Steve","email":"","affiliations":[{"id":7063,"text":"University of Maine","active":true,"usgs":false}],"preferred":false,"id":422484,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70029380,"text":"70029380 - 2005 - Broad-scale predictors of canada lynx occurrence in eastern North America","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029380","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":"Broad-scale predictors of canada lynx occurrence in eastern North America","docAbstract":"The Canada lynx (Lynx canadensis) is listed as a threatened species throughout the southern extent of its geographic range in the United States. Most research on lynx has been conducted in the western United States and Canada; little is known about the ecology of lynx in eastern North America. To fill critical knowledge gaps about this species, we modeled and mapped lynx occurrence using habitat and weather data from 7 eastern states and 3 Canadian provinces. Annual snowfall, road density, bobcat (L. rufus) harvest, deciduous forest, and coniferous forest were compared at 1,150 lynx locations and 1,288 random locations. Nineteen a priori models were developed using the information-theoretic approach, and logistic regression models were ranked using Akaike's Information Criterion (AIC) and by our ability to correctly classify reserved data (Kappa). Annual snowfall and deciduous forest predicted lynx presence and absence for a reserved dataset (n = 278) with 94% accuracy. A map of the probability of lynx occurrence throughout the region revealed that 92% of the potential habitat (i.e., >50% probability of occurrence) was concentrated in a relatively contiguous complex encompassing northern Maine, New Brunswick, and the Gaspe?? peninsula of Quebec. Most of the remaining potential habitat (5%) was on northern Cape Breton Island in Nova Scotia. Potential habitat in New Hampshire, Vermont, and New York was small (1,252 km2), fragmented, and isolated (>200 km) from known lynx populations. When federally listed as threatened in the contiguous United States in 2000, inadequate regulations on federal lands were cited as the primary threat to Canada lynx. However, the majority of potential lynx habitat in the eastern United States is on private lands and continuous with potential habitat in Canada. Therefore, lynx conservation in eastern North America will need to develop partnerships across national, state, and provincial boundaries as well as with private landowners.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/0022-541X(2005)069[0739:BPOCLO]2.0.CO;2","issn":"0022541X","usgsCitation":"Hoving, C., Harrison, D., Krohn, W., Joseph, R., and O'Brien, M., 2005, Broad-scale predictors of canada lynx occurrence in eastern North America: Journal of Wildlife Management, v. 69, no. 2, p. 739-751, https://doi.org/10.2193/0022-541X(2005)069[0739:BPOCLO]2.0.CO;2.","startPage":"739","endPage":"751","numberOfPages":"13","costCenters":[],"links":[{"id":210590,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0022-541X(2005)069[0739:BPOCLO]2.0.CO;2"},{"id":237560,"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":"5059f286e4b0c8380cd4b20f","contributors":{"authors":[{"text":"Hoving, C.L.","contributorId":32333,"corporation":false,"usgs":true,"family":"Hoving","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":422488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, D.J.","contributorId":82022,"corporation":false,"usgs":true,"family":"Harrison","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":422492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krohn, W.B.","contributorId":64355,"corporation":false,"usgs":true,"family":"Krohn","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":422490,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Joseph, R.A.","contributorId":69331,"corporation":false,"usgs":true,"family":"Joseph","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":422491,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O'Brien, M.","contributorId":57980,"corporation":false,"usgs":true,"family":"O'Brien","given":"M.","affiliations":[],"preferred":false,"id":422489,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029420,"text":"70029420 - 2005 - Factors controlling tungsten concentrations in ground water, Carson Desert, Nevada","interactions":[],"lastModifiedDate":"2018-11-05T09:02:28","indexId":"70029420","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":"Factors controlling tungsten concentrations in ground water, Carson Desert, Nevada","docAbstract":"<p>n investigation of a childhood leukemia cluster by US Centers for Disease Control and Prevention revealed that residents of the Carson Desert, Nevada, are exposed to high levels of W and this prompted an investigation of W in aquifers used as drinking water sources. Tungsten concentrations in 100 ground water samples from all aquifers used as drinking water sources in the area ranged from 0.27 to 742 μg/l. Ground water in which W concentrations exceed 50 μg/l principally occurs SE of Fallon in a geothermal area. The principal sources of W in ground water are natural and include erosion of W-bearing mineral deposits in the Carson River watershed upstream of Fallon, and, possibly, upwelling geothermal waters. Ground water in the Fallon area is strongly reducing and reductive dissolution of Fe and Mn oxyhydroxides may be releasing W; however, direct evidence that the metal oxides contain W is not available.</p><p>Although W and Cl concentrations in the Carson River, a lake, and water from many wells, appear to be controlled by evaporative concentration, evaporation alone cannot explain the elevated W concentrations found in water from some of the wells. Concentrations of W exceeding 50 μg/l are exclusively associated with<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mrow is=&quot;true&quot;><mi mathvariant=&quot;normal&quot; is=&quot;true&quot;>Na</mi><ms is=&quot;true&quot;>&amp;#x2013;</ms><msub is=&quot;true&quot;><mrow is=&quot;true&quot;><mi mathvariant=&quot;normal&quot; is=&quot;true&quot;>HCO</mi></mrow><mrow is=&quot;true&quot;><mn is=&quot;true&quot;>3</mn></mrow></msub></mrow></math>\"><span class=\"MJX_Assistive_MathML\">Na–HCO3</span></span></span><span>&nbsp;</span>and Na–Cl water types and pH&nbsp;&gt;&nbsp;8.0; in these waters, geochemical modeling indicates that W exhibits &lt;10% adsorption. Tungsten concentrations are strongly and positively correlated with As, B, F, and P, indicating either common sources or common processes controlling their concentrations. Geochemical modeling indicates W concentrations are consistent with pH-controlled adsorption of W.</p><p>The geochemical model PHREEQC was used to calculate IAP values, which were compared with published Ksp values for primary W minerals. FeWO<sub>4</sub>, MnWO<sub>4</sub>, Na<sub>2</sub>WO<sub>4</sub>, and MgWO<sub>4</sub><span>&nbsp;</span>were undersaturated and CaWO<sub>4</sub><span>&nbsp;</span>and SrWO<sub>4</sub>were approaching saturation. These conclusions are tentative because of uncertainty in the thermodynamic data.</p><p>The similar behavior of As and W observed in this study suggests ground water in areas where elevated As concentrations are present also may contain elevated W concentrations, particularly if there is a mineral or geothermal source of W and reducing conditions develop in the aquifer.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.apgeochem.2004.09.002","issn":"08832927","usgsCitation":"Seiler, R.L., Stollenwerk, K., and Garbarino, J., 2005, Factors controlling tungsten concentrations in ground water, Carson Desert, Nevada: Applied Geochemistry, v. 20, no. 2, p. 423-441, https://doi.org/10.1016/j.apgeochem.2004.09.002.","productDescription":"19 p.","startPage":"423","endPage":"441","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237670,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210675,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.apgeochem.2004.09.002"}],"country":"United States","state":"Nevada","otherGeospatial":"Carson Desert ","volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0ec0e4b0c8380cd535e7","contributors":{"authors":[{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":422683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stollenwerk, K.G.","contributorId":71199,"corporation":false,"usgs":true,"family":"Stollenwerk","given":"K.G.","affiliations":[],"preferred":false,"id":422681,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garbarino, J.R.","contributorId":76326,"corporation":false,"usgs":true,"family":"Garbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":422682,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029428,"text":"70029428 - 2005 - Biomass, production and woody detritus in an old coast redwood (Sequoia sempervirens) forest","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029428","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3086,"text":"Plant Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Biomass, production and woody detritus in an old coast redwood (Sequoia sempervirens) forest","docAbstract":"We examined aboveground biomass dynamics, aboveground net primary production (ANPP), and woody detritus input in an old Sequoia sempervirens stand over a three-decade period. Our estimates of aboveground biomass ranged from 3300 to 5800 Mg ha-1. Stem biomass estimates ranged from 3000 to 5200 Mg ha-1. Stem biomass declined 7% over the study interval. Biomass dynamics were patchy, with marked declines in recent tree-fall patches <0.05 ha in size. Larger tree-fall patches approaching 0.2 ha in size were observed outside the study plot. Our estimates of ANPP ranged from 6 to 14 Mg ha -1yr-1. Estimates of 7 to 10 Mg ha-1yr -1 were considered to be relatively accurate. Thus, our estimates based on long-term data corroborated the findings of earlier short-term studies. ANPP of old, pure stands of Sequoia was not above average for temperate forests. Even though production was potentially high on a per stem basis, it was moderate at the stand level. We obtained values of 797 m3 ha -1 and 262 Mg ha-1 for coarse woody detritus volume and mass, respectively. Fine woody detritus volume and mass were estimated at 16 m3 ha-1 and 5 Mg ha-1, respectively. Standing dead trees (or snags) comprised 7% of the total coarse detritus volume and 8% of the total mass. Coarse detritus input averaged 5.7 to 6.9 Mg ha -1yr-1. Assuming steady-state input and pool of coarse detritus, we obtained a decay rate constant of 0.022 to 0.026. The old-growth stand of Sequoia studied had extremely high biomass, but ANPP was moderate and the amount of woody detritus was not exceptionally large. Biomass accretion and loss were not rapid in this stand partly because of the slow population dynamics and low canopy turnover rate of Sequoia at the old-growth stage. Nomenclature: Hickman (1993). ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Plant Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11258-005-2322-8","issn":"13850237","usgsCitation":"Busing, R.T., and Fujimori, T., 2005, Biomass, production and woody detritus in an old coast redwood (Sequoia sempervirens) forest: Plant Ecology, v. 177, no. 2, p. 177-188, https://doi.org/10.1007/s11258-005-2322-8.","startPage":"177","endPage":"188","numberOfPages":"12","costCenters":[],"links":[{"id":210755,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11258-005-2322-8"},{"id":237774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"177","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f18ce4b0c8380cd4acca","contributors":{"authors":[{"text":"Busing, R. T.","contributorId":72162,"corporation":false,"usgs":true,"family":"Busing","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":422705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fujimori, T.","contributorId":86926,"corporation":false,"usgs":true,"family":"Fujimori","given":"T.","email":"","affiliations":[],"preferred":false,"id":422706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029429,"text":"70029429 - 2005 - Pliocene transpressional modification of depositional basins by convergent thrusting adjacent to the \"Big Bend\" of the San Andreas fault: An example from Lockwood Valley, southern California","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029429","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Pliocene transpressional modification of depositional basins by convergent thrusting adjacent to the \"Big Bend\" of the San Andreas fault: An example from Lockwood Valley, southern California","docAbstract":"The \"Big Bend\" of the San Andreas fault in the western Transverse Ranges of southern California is a left stepping flexure in the dextral fault system and has long been recognized as a zone of relatively high transpression compared to adjacent regions. The Lockwood Valley region, just south of the Big Bend, underwent a profound change in early Pliocene time (???5 Ma) from basin deposition to contraction, accompanied by widespread folding and thrusting. This change followed the recently determined initiation of opening of the northern Gulf of California and movement along the southern San Andreas fault at about 6.1 Ma, with the concomitant formation of the Big Bend. Lockwood Valley occupies a 6-km-wide, fault-bounded structural basin in which converging blocks of Paleoproterozoic and Cretaceous crystalline basement and upper Oligocene and lower Miocene sedimentary rocks (Plush Ranch Formation) were thrust over Miocene and Pliocene basin-fill sedimentary rocks (in ascending order, Caliente Formation, Lockwood Clay, and Quatal Formation). All the pre-Quatal sedimentary rocks and most of the Pliocene Quatal Formation were deposited during a mid-Tertiary period of regional transtension in a crustal block that underwent little clockwise vertical-axis rotation as compared to crustal blocks to the south. Ensuing Pliocene and Quaternary transpression in the Big Bend region began during deposition of the poorly dated Quatal Formation and was marked by four converging thrust systems, which decreased the areal extent of the sedimentary basin and formed the present Lockwood Valley structural basin. None of the thrusts appears presently active. Estimated shortening across the center of the basin was about 30 percent. The fortnerly defined eastern Big Pine fault, now interpreted to be two separate, oppositely directed, contractional reverse or thrust faults, marks the northwestern structural boundary of Lockwood Valley. The complex geometry of the Lockwood Valley basin is similar to other Tertiary structural basins in southern California, such those that underlie Cuyama Valley, the Ridge basin, and the east Ventura basin.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Tectonics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2003TC001610","issn":"02787407","usgsCitation":"Kellogg, K., and Minor, S., 2005, Pliocene transpressional modification of depositional basins by convergent thrusting adjacent to the \"Big Bend\" of the San Andreas fault: An example from Lockwood Valley, southern California: Tectonics, v. 24, no. 1, p. 1-12, https://doi.org/10.1029/2003TC001610.","startPage":"1","endPage":"12","numberOfPages":"12","costCenters":[],"links":[{"id":487541,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2003tc001610","text":"Publisher Index Page"},{"id":210756,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2003TC001610"},{"id":237775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-01-26","publicationStatus":"PW","scienceBaseUri":"505a7c81e4b0c8380cd79a0d","contributors":{"authors":[{"text":"Kellogg, K.S.","contributorId":99145,"corporation":false,"usgs":true,"family":"Kellogg","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":422708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":422707,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029438,"text":"70029438 - 2005 - Surface water acidification responses and critical loads of sulfur and nitrogen deposition in Loch Vale watershed, Colorado","interactions":[],"lastModifiedDate":"2018-04-02T15:51:41","indexId":"70029438","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Surface water acidification responses and critical loads of sulfur and nitrogen deposition in Loch Vale watershed, Colorado","docAbstract":"<p><span>We evaluated the sensitivity of The Loch, a subalpine lake in Rocky Mountain National Park in Colorado, to acidification in response to increased atmospheric loading of sulfur (S) and nitrogen (N) using the Model of Acidification of Groundwater in Catchments (MAGIC). Lake water acid‐base chemistry was moderately sensitive to changes in both S and N deposition. However, the loads of S deposition that would drive chronic lake water acid neutralizing capacity (ANC) to below 0 or 20 μeq L</span><sup>−1</sup><span><span>&nbsp;</span>were estimated to be 11 and 8 kg S ha</span><sup>−1</sup><span><span>&nbsp;</span>yr</span><sup>−1</sup><span>, respectively, assuming constant future N deposition at current levels. Comparable loads for N deposition, assuming constant future S deposition, were estimated to be 21 and 12 kg N ha</span><sup>−1</sup><span><span>&nbsp;</span>yr</span><sup>−1</sup><span>, respectively. Modeling results for Andrews Creek, an alpine tributary to The Loch, suggested critical loads for surface water acidification that averaged about one third lower. Surface water ANC = 50 μeq L</span><sup>−1</sup><span><span>&nbsp;</span>was projected to occur in 50 years in The Loch if S or N deposition increased by a moderate amount (&lt;40%) but could not be achieved in Andrews Creek by reducing either S or N deposition to zero. On the basis of the results of synoptic surveys of lake water chemistry, about one fifth of the wilderness lakes in the Colorado Front Range are more acid‐sensitive than The Loch. This modeling exercise suggests the need for a regional analysis of critical loads for the larger population of acid‐sensitive aquatic resources in order to provide part of the scientific foundation for federally mandated land management decisions.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2004WR003414","usgsCitation":"Sullivan, T., Cosby, B., Tonnessen, K., and Clow, D.W., 2005, Surface water acidification responses and critical loads of sulfur and nitrogen deposition in Loch Vale watershed, Colorado: Water Resources Research, v. 41, no. 1, Article W01021; 15 p., https://doi.org/10.1029/2004WR003414.","productDescription":"Article W01021; 15 p.","costCenters":[],"links":[{"id":477813,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004wr003414","text":"Publisher Index Page"},{"id":237378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-01-29","publicationStatus":"PW","scienceBaseUri":"505b9fc4e4b08c986b31e7fb","contributors":{"authors":[{"text":"Sullivan, T.J.","contributorId":83734,"corporation":false,"usgs":true,"family":"Sullivan","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":422740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cosby, B.J.","contributorId":96455,"corporation":false,"usgs":true,"family":"Cosby","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":422741,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tonnessen, K.A.","contributorId":30196,"corporation":false,"usgs":true,"family":"Tonnessen","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":422739,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clow, D. W.","contributorId":23531,"corporation":false,"usgs":true,"family":"Clow","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":422738,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029446,"text":"70029446 - 2005 - Male Texas Horned Lizards increase daily movements and area covered in spring: A mate searching strategy?","interactions":[],"lastModifiedDate":"2022-05-24T14:36:03.728311","indexId":"70029446","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Male Texas Horned Lizards increase daily movements and area covered in spring: A mate searching strategy?","docAbstract":"<p><span>Texas Horned Lizards,&nbsp;</span><i><span class=\"genus-species\">Phrynosoma cornutum</span></i><span>, were tracked using fluorescent powder to determine exact daily movements. Daily linear movements and daily space use were compared between adult males and females. Lizards that traveled the greatest linear distances also covered the largest areas. In Oklahoma, adults emerge from hibernation in late April and early May and mate soon afterward. Males traveled significantly greater distances (and covered significantly larger areas in a day) than females in May but not after May. We propose that males move more and cover more area than females early in the mating season to intercept receptive females.</span></p>","language":"English","publisher":"Society for the Study of Amphibians and Reptiles","doi":"10.1670/0022-1511(2005)039[0168:MTHLID]2.0.CO;2","usgsCitation":"Stark, R.C., Fox, S.F., and Leslie, D., 2005, Male Texas Horned Lizards increase daily movements and area covered in spring: A mate searching strategy?: Journal of Herpetology, v. 39, no. 1, p. 169-173, https://doi.org/10.1670/0022-1511(2005)039[0168:MTHLID]2.0.CO;2.","productDescription":"5 p.","startPage":"169","endPage":"173","numberOfPages":"5","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":237488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","county":"Payne County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.9277,36.246],[-96.8216,36.245],[-96.8212,36.1593],[-96.6245,36.1605],[-96.6228,35.9427],[-97.1428,35.9442],[-97.1423,35.9641],[-97.1557,35.9485],[-97.1729,35.9428],[-97.1872,35.9426],[-97.2013,35.9469],[-97.2163,35.9576],[-97.2252,35.9677],[-97.236,35.9683],[-97.2461,35.9721],[-97.2523,35.9744],[-97.2734,35.9734],[-97.2841,35.9767],[-97.2863,35.9795],[-97.2862,35.9835],[-97.2883,35.9931],[-97.2927,36.0004],[-97.2982,36.0091],[-97.3055,36.011],[-97.3203,36.0108],[-97.3329,36.0078],[-97.3359,36.0024],[-97.34,35.9947],[-97.3475,35.9885],[-97.3556,35.9841],[-97.3569,36.1583],[-97.1426,36.1588],[-97.1417,36.245],[-96.9277,36.246]]]},\"properties\":{\"name\":\"Payne\",\"state\":\"OK\"}}]}","volume":"39","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c3ee4b0c8380cd69af9","contributors":{"authors":[{"text":"Stark, Richard C.","contributorId":28425,"corporation":false,"usgs":true,"family":"Stark","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":422779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fox, S. F.","contributorId":100984,"corporation":false,"usgs":true,"family":"Fox","given":"S.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":422780,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leslie, David 0000-0002-3884-1484 cleslie@usgs.gov","orcid":"https://orcid.org/0000-0002-3884-1484","contributorId":169989,"corporation":false,"usgs":true,"family":"Leslie","given":"David","email":"cleslie@usgs.gov","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":422778,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029447,"text":"70029447 - 2005 - Benthic invertebrate community structure is influenced by forest succession after clearcut logging in southeastern Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029447","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Benthic invertebrate community structure is influenced by forest succession after clearcut logging in southeastern Alaska","docAbstract":"To assess the effects of timber harvesting on headwater streams in upland forests, benthic community structure was contrasted among four dominant forest management types (old growth, red alder-dominated young growth, conifer-dominated young growth, clearcut) and instream habitats (woody debris, cobble, gravel) in southeastern Alaska. Benthos in streams of previously harvested areas resulted in increased richness, densities and biomass relative to old growth types, particularly in young growth stands with a red alder-dominated riparian canopy. Woody debris and gravel habitats supported a combination of higher densities and biomass of invertebrates than cobble habitats. In addition, woody debris also supported a richer and more diverse invertebrate fauna than either cobble or gravel substrates. Maintaining both a woody debris source and a red alder component in regenerating riparian forests following timber harvesting should support greater invertebrate densities and diversity following clearcutting. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10750-004-2105-6","issn":"00188158","usgsCitation":"Hernandez, O., Merritt, R., and Wipfli, M., 2005, Benthic invertebrate community structure is influenced by forest succession after clearcut logging in southeastern Alaska: Hydrobiologia, v. 533, no. 1, p. 45-59, https://doi.org/10.1007/s10750-004-2105-6.","startPage":"45","endPage":"59","numberOfPages":"15","costCenters":[],"links":[{"id":210564,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10750-004-2105-6"},{"id":237525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"533","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f0bbe4b0c8380cd4a8aa","contributors":{"authors":[{"text":"Hernandez, O.","contributorId":76929,"corporation":false,"usgs":true,"family":"Hernandez","given":"O.","email":"","affiliations":[],"preferred":false,"id":422783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merritt, R.W.","contributorId":30588,"corporation":false,"usgs":true,"family":"Merritt","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":422781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wipfli, M.S.","contributorId":51963,"corporation":false,"usgs":true,"family":"Wipfli","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":422782,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029486,"text":"70029486 - 2005 - Absorption of p,p'-dichlorodiphenyldichloroethylene and dieldrin in largemouth bass from a 60-D slow-release pellet and detection using a novel enzyme-linked immunosorbent assay method for blood plasma","interactions":[],"lastModifiedDate":"2015-05-04T11:42:46","indexId":"70029486","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Absorption of p,p'-dichlorodiphenyldichloroethylene and dieldrin in largemouth bass from a 60-D slow-release pellet and detection using a novel enzyme-linked immunosorbent assay method for blood plasma","docAbstract":"<p><span>This work describes the uptake of two organochlorine pesticides from slow-release pellets by largemouth bass and the utility of a blood plasma enzyme-linked immunosorbent assay (ELISA) method for exposure verification. We measured blood and tissue levels by gas chromatography/mass spectrometry and by a novel ELISA method, and present a critical comparison of the results.</span></p>","language":"English","publisher":"Wiley","doi":"10.1897/04-492R.1","issn":"07307268","usgsCitation":"Muller, J.K., Sepulveda, M.S., Borgert, C.J., and Gross, T.S., 2005, Absorption of p,p'-dichlorodiphenyldichloroethylene and dieldrin in largemouth bass from a 60-D slow-release pellet and detection using a novel enzyme-linked immunosorbent assay method for blood plasma: Environmental Toxicology and Chemistry, v. 24, no. 8, p. 1979-1983, https://doi.org/10.1897/04-492R.1.","productDescription":"5 p.","startPage":"1979","endPage":"1983","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":237491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210539,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/04-492R.1"}],"volume":"24","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-08-01","publicationStatus":"PW","scienceBaseUri":"5059e64de4b0c8380cd47329","contributors":{"authors":[{"text":"Muller, Jennifer K.","contributorId":89702,"corporation":false,"usgs":true,"family":"Muller","given":"Jennifer","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":422938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sepulveda, Maria S.","contributorId":60960,"corporation":false,"usgs":true,"family":"Sepulveda","given":"Maria","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":422940,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Borgert, Christopher J.","contributorId":83713,"corporation":false,"usgs":true,"family":"Borgert","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422937,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gross, Timothy S.","contributorId":45381,"corporation":false,"usgs":true,"family":"Gross","given":"Timothy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":422939,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029490,"text":"70029490 - 2005 - Longer-term effects of selective thinning on microarthropod communities in a late-successional coniferous forest","interactions":[],"lastModifiedDate":"2021-07-09T20:37:28.06054","indexId":"70029490","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1536,"text":"Environmental Entomology","active":true,"publicationSubtype":{"id":10}},"title":"Longer-term effects of selective thinning on microarthropod communities in a late-successional coniferous forest","docAbstract":"<p><span>Microarthropod densities within late-successional coniferous forests thinned 16–41 yr before sampling were compared with adjacent unthinned stands to identify longer term effects of thinning on this community. Soil and forest floor layers were sampled separately on eight paired sites. Within the forest floor oribatid, mesostigmatid, and to a marginal extent, prostigmatid mites, were reduced in thinned stands compared with unthinned stands. No differences were found for Collembola in the forest floor or for any mite suborder within the soil. Family level examination of mesostigmatid and prostigmatid mites revealed significant differences between stand types for both horizons. At the species level, thinning influenced numerous oribatid mites and Collembola. For oribatid mites, significant or marginally significant differences were found for seven of 15 common species in the forest floor and five of 16 common species in soil. Collembola were affected less, with differences found for one of 11 common species in the forest floor and three of 13 common species in soil. Multivariate analysis of variance and ordination indicated that forest thinning had little influence on the composition of oribatid mite and collembolan communities within either the forest floor or soil. Differences in microclimate or in the accumulation of organic matter on the forest floor were likely most responsible for the observed patterns of abundance. Considering the role that microarthropods play in nutrient cycling, determining the functional response of a wide range of taxa to thinning may be important to effective ecosystem management.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1603/0046-225X-34.3.646","usgsCitation":"Peck, R., and Niwa, C.G., 2005, Longer-term effects of selective thinning on microarthropod communities in a late-successional coniferous forest: Environmental Entomology, v. 34, no. 3, p. 646-655, https://doi.org/10.1603/0046-225X-34.3.646.","productDescription":"10 p.","startPage":"646","endPage":"655","numberOfPages":"10","costCenters":[],"links":[{"id":477777,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1603/0046-225x-34.3.646","text":"Publisher Index Page"},{"id":237566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Medford Resource Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.61566162109375,\n              42.05745022024682\n            ],\n            [\n              -122.38151550292969,\n              42.05745022024682\n            ],\n            [\n              -122.38151550292969,\n              42.24173542549948\n            ],\n            [\n              -122.61566162109375,\n              42.24173542549948\n            ],\n            [\n              -122.61566162109375,\n              42.05745022024682\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-06-01","publicationStatus":"PW","scienceBaseUri":"505a49b6e4b0c8380cd6881a","contributors":{"authors":[{"text":"Peck, Robert W. 0000-0002-8739-9493","orcid":"https://orcid.org/0000-0002-8739-9493","contributorId":193088,"corporation":false,"usgs":false,"family":"Peck","given":"Robert W.","affiliations":[],"preferred":false,"id":422955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Niwa, C. G.","contributorId":34315,"corporation":false,"usgs":false,"family":"Niwa","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":422954,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029492,"text":"70029492 - 2005 - A frictional population model of seismicity rate change","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029492","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"A frictional population model of seismicity rate change","docAbstract":"We study models of seismicity rate changes caused by the application of a static stress perturbation to a population of faults and discuss our results with respect to the model proposed by Dieterich (1994). These models assume distribution of nucleation sites (e.g., faults) obeying rate-state frictional relations that fail at constant rate under tectonic loading alone, and predicts a positive static stress step at time to will cause an immediate increased seismicity rate that decays according to Omori's law. We show one way in which the Dieterich model may be constructed from simple general idead, illustratted using numerically computed synthetic seismicity and mathematical formulation. We show that seismicity rate change predicted by these models (1) depend on the particular relationship between the clock-advanced failure and fault maturity, (2) are largest for the faults closest to failure at to, (3) depend strongly on which state evolution law faults obey, and (4) are insensitive to some types of population hetrogeneity. We also find that if individual faults fail repeatedly and populations are finite, at timescales much longer than typical aftershock durations, quiescence follows at seismicity rate increase regardless of the specific frictional relations. For the examined models the quiescence duration is comparable to the ratio of stress change to stressing rate ????/??,which occurs after a time comparable to the average recurrence interval of the individual faults in the population and repeats in the absence of any new load may pertubations; this simple model may partly explain observations of repeated clustering of earthquakes. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003404","issn":"01480227","usgsCitation":"Gomberg, J., Reasenberg, P., Cocco, M., and Belardinelli, M., 2005, A frictional population model of seismicity rate change: Journal of Geophysical Research B: Solid Earth, v. 110, no. 5, p. 1-10, https://doi.org/10.1029/2004JB003404.","startPage":"1","endPage":"10","numberOfPages":"10","costCenters":[],"links":[{"id":210627,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003404"},{"id":237603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-04-22","publicationStatus":"PW","scienceBaseUri":"5059e3e4e4b0c8380cd462a4","contributors":{"authors":[{"text":"Gomberg, J.","contributorId":95994,"corporation":false,"usgs":true,"family":"Gomberg","given":"J.","email":"","affiliations":[],"preferred":false,"id":422962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reasenberg, P.","contributorId":22913,"corporation":false,"usgs":true,"family":"Reasenberg","given":"P.","email":"","affiliations":[],"preferred":false,"id":422960,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cocco, M.","contributorId":70128,"corporation":false,"usgs":true,"family":"Cocco","given":"M.","email":"","affiliations":[],"preferred":false,"id":422961,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belardinelli, M.E.","contributorId":107464,"corporation":false,"usgs":true,"family":"Belardinelli","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":422963,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029493,"text":"70029493 - 2005 - Impact of longer-term modest climate shifts on architecture of high-frequency sequences (Cyclothems), Pennsylvanian of midcontinent U.S.A","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029493","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2451,"text":"Journal of Sedimentary Research","onlineIssn":"1938-3681","printIssn":"1527-1404","active":true,"publicationSubtype":{"id":10}},"title":"Impact of longer-term modest climate shifts on architecture of high-frequency sequences (Cyclothems), Pennsylvanian of midcontinent U.S.A","docAbstract":"Pennsylvanian glacioeustatic cyclothems exposed in Kansas and adjacent areas provide a unique opportunity to test models of the impact of relative sea level and climate on stratal architecture. A succession of eight of these high-frequency sequences, traced along dip for 500 km, reveal that modest climate shifts from relatively dry-seasonal to relatively wet-seasonal with a duration of several sequences (???600,000 to 1 million years) had a dominant impact on facies, sediment dispersal patterns, and sequence architecture. The climate shifts documented herein are intermediate, both in magnitude and duration, between previously documented longer-term climate shifts throughout much of the Pennsylvanian and shorter-term shifts described within individual sequences. Climate indicators are best preserved at sequence boundaries and in incised-valley fills of the lowstand systems tracts (LST). Relatively drier climate indicators include high-chroma paleosols, typically with pedogenic carbonates, and plant assemblages that are dominated by gymnosperms, mostly xerophytic walchian conifers. The associated valleys are small (<2 km wide and <11 m deep) and are commonly filled with locally derived limestone clasts, which indicate small drainage networks. Relatively wetter climates are indicated by locally preserved paleosols exhibiting both low-chroma and high-chroma variants, common coals, and plant assemblages that are dominated by fern foliage, seed ferns, and sphenopsids. The incised-valley fills associated with these facies are large (>4 km wide and >20 m deep), and dominated by quartz sandstones derived from distant source areas, reflecting large drainage networks. Transgressive systems tracts (TST) in all eight sequences gen erally are characterized by thin, extensive limestones and thin marine shales, suggesting that the dominant control on TST facies distribution was the sequestration of siliciclastic sediment in updip positions. Highstand systems tracts (HST) were significantly impacted by the intermediate-scale climate cycle in that HSTs from relatively drier climates consist of thin marine shales overlain by extensive, thick regressive limestones, whereas HSTs from relatively wetter climates are dominated by thick marine shales. Previously documented relative sea-level changes do not track the climate cycles, indicating that climate played a role distinct from that of relative sea-level change. These intermediate-scale modest climate shifts had a dominant impact on sequence architecture. This independent measure of climate and relative sea level may allow the testing of models of climate and sediment supply based on modern systems. Copyright ?? 2005, SEPM.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2110/jsr.2005.028","issn":"15271404","usgsCitation":"Feldman, H.R., Franseen, E.K., Joeckel, R.M., and Heckel, P., 2005, Impact of longer-term modest climate shifts on architecture of high-frequency sequences (Cyclothems), Pennsylvanian of midcontinent U.S.A: Journal of Sedimentary Research, v. 75, no. 3, p. 350-368, https://doi.org/10.2110/jsr.2005.028.","startPage":"350","endPage":"368","numberOfPages":"19","costCenters":[],"links":[{"id":210649,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2110/jsr.2005.028"},{"id":237637,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-06-16","publicationStatus":"PW","scienceBaseUri":"505a38c0e4b0c8380cd6169c","contributors":{"authors":[{"text":"Feldman, H. R.","contributorId":29581,"corporation":false,"usgs":true,"family":"Feldman","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":422965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franseen, E. K.","contributorId":30367,"corporation":false,"usgs":false,"family":"Franseen","given":"E.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":422966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Joeckel, R. M.","contributorId":37103,"corporation":false,"usgs":false,"family":"Joeckel","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":422967,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Heckel, P.H.","contributorId":18486,"corporation":false,"usgs":true,"family":"Heckel","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":422964,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029494,"text":"70029494 - 2005 - Novel biomarkers of perchlorate exposure in zebrafish","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029494","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Novel biomarkers of perchlorate exposure in zebrafish","docAbstract":"Perchlorate inhibits iodide uptake by thyroid follicles and lowers thyroid hormone production. Although several effects of perchlorate on the thyroid system have been reported, the utility of these pathologies as markers of environmental perchlorate exposures has not been adequately assessed. The present study examined time-course and concentration-dependent effects of perchlorate on thyroid follicle hypertrophy, colloid depletion, and angiogenesis; alterations in whole-body thyroxine (T4) levels; and somatic growth and condition factor of subadult and adult zebrafish. Changes in the intensity of the colloidal T4 ring previously observed in zebrafish also were examined immunohistochemically. Three-month-old zebrafish were exposed to ammonium perchlorate at measured perchlorate concentrations of 0, 11, 90, 1,131, and 11,480 ppb for 12 weeks and allowed to recover in clean water for 12 weeks. At two weeks of exposure, the lowest-observed-effective concentrations (LOECs) of perchlorate that induced angiogenesis and depressed the intensity of colloidal T4 ring were 90 and 1,131 ppb, respectively; other parameters were not affected (whole-body T4 was not determined at this time). At 12 weeks of exposure, LOECs for colloid depletion, hypertrophy, angiogenesis, and colloidal T4 ring were 11,480, 1,131, 90, and 11 ppb, respectively. All changes were reversible, but residual effects on angiogenesis and colloidal T4 ring intensity were still present after 12 weeks of recovery (LOEC, 11,480 ppb). Whole-body T 4 concentration, body growth (length and weight), and condition factor were not affected by perchlorate. The sensitivity and longevity of changes in colloidal T4 ring intensity and angiogenesis suggest their usefulness as novel markers of perchlorate exposure. The 12-week LOEC for colloidal T4 ring is the lowest reported for any perchlorate biomarker in aquatic vertebrates. ?? 2005 SETAC.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Toxicology and Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1897/04-270R.1","issn":"07307268","usgsCitation":"Mukhi, S., Carr, J., Anderson, T., and Patino, R., 2005, Novel biomarkers of perchlorate exposure in zebrafish: Environmental Toxicology and Chemistry, v. 24, no. 5, p. 1107-1115, https://doi.org/10.1897/04-270R.1.","startPage":"1107","endPage":"1115","numberOfPages":"9","costCenters":[],"links":[{"id":210679,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/04-270R.1"},{"id":237674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-01","publicationStatus":"PW","scienceBaseUri":"505a68b1e4b0c8380cd73959","contributors":{"authors":[{"text":"Mukhi, S.","contributorId":83721,"corporation":false,"usgs":true,"family":"Mukhi","given":"S.","affiliations":[],"preferred":false,"id":422970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, J.A.","contributorId":106692,"corporation":false,"usgs":true,"family":"Carr","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":422971,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, T.A.","contributorId":77344,"corporation":false,"usgs":true,"family":"Anderson","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":422969,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Patino, R.","contributorId":39915,"corporation":false,"usgs":true,"family":"Patino","given":"R.","email":"","affiliations":[],"preferred":false,"id":422968,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1015281,"text":"1015281 - 2005 - Movements and home ranges of mountain plovers raising broods in three Colorado landscapes","interactions":[],"lastModifiedDate":"2017-12-27T10:53:06","indexId":"1015281","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Movements and home ranges of mountain plovers raising broods in three Colorado landscapes","docAbstract":"<p>We report movements and home-range sizes of adult Mountain Plovers (<i>Charadrius montanus</i>) with broods on rangeland, agricultural fields, and prairie dog habitats in eastern Colorado. Estimates of home range size (95% fixed kernel) were similar across the three habitats: rangeland (146.1 ha ± 101.5), agricultural fields (131.6 ha ± 74.4), and prairie dog towns (243.3 ha ± 366.3). Our minimum convex polygon estimates of home-range size were comparable to those on rangeland reported by <a class=\"ref\" onclick=\"popRef2('i0043-5643-117-2-128-Knopf2','','','' ); return false;\">Knopf and Rupert (1996)</a>. In addition, movements—defined as the distance between consecutive locations of adults with broods—were equivalent across habitats. However, our findings on prairie dog habitat suggest that home-range size for brood rearing may be related to whether the prairie dog habitat is in a complex of towns or in an isolated town.</p>","language":"English","publisher":"The Wilson Ornithological Society","doi":"10.1676/03-116","usgsCitation":"Dreitz, V., Wunder, M., and Knopf, F., 2005, Movements and home ranges of mountain plovers raising broods in three Colorado landscapes: The Wilson Bulletin, v. 117, no. 2, p. 128-132, https://doi.org/10.1676/03-116.","productDescription":"5 p.","startPage":"128","endPage":"132","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":477847,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1676/03-116","text":"External Repository"},{"id":132700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698c3a","contributors":{"authors":[{"text":"Dreitz, V.J.","contributorId":65432,"corporation":false,"usgs":true,"family":"Dreitz","given":"V.J.","affiliations":[],"preferred":false,"id":322750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wunder, Michael B.","contributorId":65406,"corporation":false,"usgs":false,"family":"Wunder","given":"Michael B.","affiliations":[{"id":6674,"text":"Department of Integrative Biology, University of Colorado Denver","active":true,"usgs":false}],"preferred":false,"id":322749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knopf, F.L.","contributorId":26998,"corporation":false,"usgs":true,"family":"Knopf","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":322748,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029495,"text":"70029495 - 2005 - Selenium in the Blackfoot, Salt, and Bear River Watersheds","interactions":[],"lastModifiedDate":"2017-05-22T15:45:32","indexId":"70029495","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"Selenium in the Blackfoot, Salt, and Bear River Watersheds","docAbstract":"<p><span>Nine stream sites in the Blackfoot River, Salt River, and Bear River watersheds in southeast Idaho, USA were sampled in May 2001 for water, surficial sediment, aquatic plants, aquatic invertebrates, and fish. Selenium was measured in these aquatic ecosystem components, and a hazard assessment was performed on the data. Water quality characteristics such as pH, hardness, and specific conductance were relatively uniform among the nine sites. Of the aquatic components assessed, water was the least contaminated with selenium because measured concentrations were below the national water quality criterion of 5 μ g/L at eight of the nine sites. In contrast, selenium was elevated in sediment, aquatic plants, aquatic invertebrates, and fish from several sites, suggesting deposition in sediments and food web cycling through plants and invertebrates. Selenium was elevated to concentrations of concern in fish at eight sites (&gt; 4 μ g/g in whole body). A hazard assessment of selenium in the aquatic environment suggested a moderate hazard at upper Angus Creek (UAC) and Smoky Creek (SC), and high hazard at Little Blackfoot River (LiB), Blackfoot River gaging station (BGS), State Land Creek (SLC), upper (UGC) and lower Georgetown Creek (LGC), Deer Creek (DC), and Crow Creek (CC). The results of this study indicate that selenium concentrations from the phosphate mining area of southeast Idaho were sufficiently elevated in several ecosystem components to cause adverse effects to aquatic resources in southeastern Idaho.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10661-005-1618-4","issn":"01676369","usgsCitation":"Hamilton, S.J., and Buhl, K., 2005, Selenium in the Blackfoot, Salt, and Bear River Watersheds: Environmental Monitoring and Assessment, v. 104, no. 1-3, p. 309-339, https://doi.org/10.1007/s10661-005-1618-4.","productDescription":"31 p.","startPage":"309","endPage":"339","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":210680,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10661-005-1618-4"},{"id":237675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"104","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8cf6e4b08c986b3181e2","contributors":{"authors":[{"text":"Hamilton, S. J.","contributorId":27817,"corporation":false,"usgs":false,"family":"Hamilton","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buhl, K.J.","contributorId":19728,"corporation":false,"usgs":true,"family":"Buhl","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":422972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029496,"text":"70029496 - 2005 - Progress in NTHMP Hazard Assessment","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029496","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2822,"text":"Natural Hazards","active":true,"publicationSubtype":{"id":10}},"title":"Progress in NTHMP Hazard Assessment","docAbstract":"The Hazard Assessment component of the U.S. National Tsunami Hazard Mitigation Program has completed 22 modeling efforts covering 113 coastal communities with an estimated population of 1.2 million residents that are at risk. Twenty-three evacuation maps have also been completed. Important improvements in organizational structure have been made with the addition of two State geotechnical agency representatives to Steering Group membership, and progress has been made on other improvements suggested by program reviewers. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Hazards","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11069-004-2406-0","issn":"0921030X","usgsCitation":"Gonzalez, F., Titov, V., Mofjeld, H., Venturato, A., Simmons, R., Hansen, R., Combellick, R., Eisner, R., Hoirup, D., Yanagi, B., Yong, S., Darienzo, M., Priest, G.R., Crawford, G., and Walsh, T.J., 2005, Progress in NTHMP Hazard Assessment: Natural Hazards, v. 35, no. 1, p. 89-110, https://doi.org/10.1007/s11069-004-2406-0.","startPage":"89","endPage":"110","numberOfPages":"22","costCenters":[],"links":[{"id":237710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210704,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11069-004-2406-0"}],"volume":"35","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8e64e4b0c8380cd7f17b","contributors":{"authors":[{"text":"Gonzalez, F.I.","contributorId":68100,"corporation":false,"usgs":true,"family":"Gonzalez","given":"F.I.","email":"","affiliations":[],"preferred":false,"id":422982,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titov, V.V.","contributorId":48752,"corporation":false,"usgs":true,"family":"Titov","given":"V.V.","email":"","affiliations":[],"preferred":false,"id":422980,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mofjeld, H.O.","contributorId":27103,"corporation":false,"usgs":true,"family":"Mofjeld","given":"H.O.","email":"","affiliations":[],"preferred":false,"id":422975,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Venturato, A.J.","contributorId":102265,"corporation":false,"usgs":true,"family":"Venturato","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":422985,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Simmons, R.S.","contributorId":97695,"corporation":false,"usgs":true,"family":"Simmons","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":422984,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hansen, R.","contributorId":56370,"corporation":false,"usgs":true,"family":"Hansen","given":"R.","affiliations":[],"preferred":false,"id":422981,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Combellick, Rodney","contributorId":106305,"corporation":false,"usgs":false,"family":"Combellick","given":"Rodney","email":"","affiliations":[],"preferred":false,"id":422987,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Eisner, R.K.","contributorId":103859,"corporation":false,"usgs":true,"family":"Eisner","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":422986,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hoirup, D.F.","contributorId":30811,"corporation":false,"usgs":true,"family":"Hoirup","given":"D.F.","affiliations":[],"preferred":false,"id":422976,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Yanagi, B.S.","contributorId":108312,"corporation":false,"usgs":true,"family":"Yanagi","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":422988,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Yong, S.","contributorId":34317,"corporation":false,"usgs":true,"family":"Yong","given":"S.","email":"","affiliations":[],"preferred":false,"id":422978,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Darienzo, M.","contributorId":41525,"corporation":false,"usgs":true,"family":"Darienzo","given":"M.","email":"","affiliations":[],"preferred":false,"id":422979,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Priest, G. R.","contributorId":19572,"corporation":false,"usgs":true,"family":"Priest","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":422974,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Crawford, G.L.","contributorId":75325,"corporation":false,"usgs":true,"family":"Crawford","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":422983,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Walsh, T. J.","contributorId":33725,"corporation":false,"usgs":true,"family":"Walsh","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422977,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70029498,"text":"70029498 - 2005 - Trends in hydrophobic organic contaminants in urban and reference lake sediments across the United States, 1970-2001","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029498","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":"Trends in hydrophobic organic contaminants in urban and reference lake sediments across the United States, 1970-2001","docAbstract":"A shift in national policy toward stronger environmental protection began in the United States in about 1970. Conversely, urban land use, population, energy consumption, and vehicle use have increased greatly since then. To assess the effects of these changes on water quality, the U.S. Geological Survey used sediment cores to reconstruct water-quality histories for38 urban and reference lakes across the United States. Cores were age-dated, and concentration profiles of polycyclic aromatic hydrocarbons (PAHs) and chlorinated hydrocarbons were tested statistically. Significant trends in total DDT, p,p???-DDE, and total PCBs were all downward. Trends in chlordane were split evenly between upward and downward, and trends in PAHs were mostly upward. Significant trends did not occur in about one-half of cases tested. Concentrations of p,p???-DDE, p,p???-DDD, and PCBs were about one-half as likely to exceed the probable effect concentration (PEC), a sediment quality guideline, in sediments deposited in the 1990s as in 1965-1975, whereas PAHs were twice as likely to exceed the PEC in the more recently deposited sediments. Concentrations of all contaminants evaluated correlated strongly with urban land use. Upward trends in PAH concentrations, the strong association of PAH with urban settings, and rapid urbanization occurring in the United States suggest that PAHs could surpass chlorinated hydrocarbons in the threat they pose to aquatic biota in urban streams and lakes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es0503175","issn":"0013936X","usgsCitation":"Van Metre, P., and Mahler, B., 2005, Trends in hydrophobic organic contaminants in urban and reference lake sediments across the United States, 1970-2001: Environmental Science & Technology, v. 39, no. 15, p. 5567-5574, https://doi.org/10.1021/es0503175.","startPage":"5567","endPage":"5574","numberOfPages":"8","costCenters":[],"links":[{"id":210732,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es0503175"},{"id":237747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"15","noUsgsAuthors":false,"publicationDate":"2005-06-22","publicationStatus":"PW","scienceBaseUri":"505bb7eae4b08c986b327574","contributors":{"authors":[{"text":"Van Metre, P. C.","contributorId":92999,"corporation":false,"usgs":true,"family":"Van Metre","given":"P. C.","affiliations":[],"preferred":false,"id":422993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahler, B.J.","contributorId":36888,"corporation":false,"usgs":true,"family":"Mahler","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":422992,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029669,"text":"70029669 - 2005 - The crane flies (Diptera: Tipuloidea) of Great Smoky Mountains National Park","interactions":[],"lastModifiedDate":"2022-06-07T13:56:37.821154","indexId":"70029669","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3814,"text":"Zootaxa","onlineIssn":"1175-5334","printIssn":"1175-5326","active":true,"publicationSubtype":{"id":10}},"title":"The crane flies (Diptera: Tipuloidea) of Great Smoky Mountains National Park","docAbstract":"<p>The list of crane flies (Diptera: Ptychopteridae, Tipuloidea, Trichoceridae) known from Great Smoky Mountains National Park is updated. Sampling in association with the All Taxa Biodiversity Inventory of Great Smoky Mountains National Park resulted in the addition of 107 new Park records, bringing the current list to 250 species. This species assemblage is much richer than those of surrounding areas, although similar in composition. Total richness is estimated to be between 450 and 500 species for Great Smoky Mountains National Park.</p>","language":"English","publisher":"Magnolia Press","doi":"10.11646/zootaxa.1013.1.1","usgsCitation":"Petersen, M.J., Parker, C.R., and Bernard, E., 2005, The crane flies (Diptera: Tipuloidea) of Great Smoky Mountains National Park: Zootaxa, v. 1013, no. 1, p. 1-18, https://doi.org/10.11646/zootaxa.1013.1.1.","productDescription":"18 p.","startPage":"1","endPage":"18","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":486801,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://zenodo.org/record/5049176","text":"External Repository"},{"id":240376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina, Tennesse","otherGeospatial":"Great Smoky Mountains National Park","geographicExtents":"{\n  \"type\": 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]\n}","volume":"1013","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-06-30","publicationStatus":"PW","scienceBaseUri":"505baa6de4b08c986b322822","contributors":{"authors":[{"text":"Petersen, Matthew J.","contributorId":168692,"corporation":false,"usgs":false,"family":"Petersen","given":"Matthew","email":"","middleInitial":"J.","affiliations":[{"id":6911,"text":"Iowa State University","active":true,"usgs":false}],"preferred":false,"id":423741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Charles R. chuck_parker@usgs.gov","contributorId":4489,"corporation":false,"usgs":true,"family":"Parker","given":"Charles","email":"chuck_parker@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":423743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bernard, Ernest","contributorId":168693,"corporation":false,"usgs":false,"family":"Bernard","given":"Ernest","email":"","affiliations":[{"id":12716,"text":"University of Tennessee","active":true,"usgs":false}],"preferred":false,"id":423742,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029666,"text":"70029666 - 2005 - Effects of urban development in the Puget Lowland, Washington, on interannual streamflow patterns: Consequences for channel form and streambed disturbance","interactions":[],"lastModifiedDate":"2018-04-02T16:12:36","indexId":"70029666","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Effects of urban development in the Puget Lowland, Washington, on interannual streamflow patterns: Consequences for channel form and streambed disturbance","docAbstract":"<p><span>Recovery and protection of streams in urban areas depend on a comprehensive understanding of how human activities affect stream ecosystems. The hydrologic effects of urban development and the consequences for stream channel form and streambed stability were examined in 16 streams in the Puget Lowland, Washington, using three streamflow metrics that integrate storm‐scale effects of urban development over annual to decadal timescales: the fraction of time that streamflow exceeds the mean streamflow (T</span><sub>Qmean</sub><span>), the coefficient of variation of annual maximum streamflow (CV</span><sub>AMF</sub><span>), and the fraction of time that streamflow exceeds the 0.5‐year flood (T</span><sub>0.5</sub><span>). Urban streams had low interannual variability in annual maximum streamflow and brief duration of frequent high flows, as indicated by significant correlations between road density and both CV</span><sub>AMF</sub><span>and T</span><sub>0.5</sub><span>. The broader distribution of streamflow indicated by T</span><sub>Qmean</sub><span><span>&nbsp;</span>may be affected by urban development, but differences in T</span><sub>Qmean</sub><span><span>&nbsp;</span>between streams are also likely a result of other physiographic factors. The increase in the magnitude of frequent high flows due to urban development but not their cumulative duration has important consequences for channel form and bed stability in gravel bed streams because geomorphic equilibrium depends on moderate duration streamflow (e.g., exceeded 10% of the time). Streams with low values of T</span><sub>Qmean</sub><span><span>&nbsp;</span>and T</span><sub>0.5</sub><span><span>&nbsp;</span>are narrower than expected from hydraulic geometry. Dimensionless boundary shear stress (t*) for the 0.5‐year flood was inversely related to T</span><sub>0.5</sub><span><span>&nbsp;</span>among the streams, indicating frequent and extensive bed disturbance in streams with low values of T</span><sub>0.5</sub><span>. Although stream channels expand and the size of bed material increases in response to urban streamflow patterns, these adjustments may be insufficient to reestablish the disturbance regime in urban streams because of the differential increase in the magnitude of frequent high flows causing disturbance relative to any changes in longer duration, moderate flows that establish a stable channel.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005WR004097","usgsCitation":"Konrad, C.P., Booth, D.B., and Burges, S.J., 2005, Effects of urban development in the Puget Lowland, Washington, on interannual streamflow patterns: Consequences for channel form and streambed disturbance: Water Resources Research, v. 41, no. 7, Article W07009; 15 p., https://doi.org/10.1029/2005WR004097.","productDescription":"Article W07009; 15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":240339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"7","noUsgsAuthors":false,"publicationDate":"2005-07-13","publicationStatus":"PW","scienceBaseUri":"505a0820e4b0c8380cd519b5","contributors":{"authors":[{"text":"Konrad, Christopher P. 0000-0002-7354-547X cpkonrad@usgs.gov","orcid":"https://orcid.org/0000-0002-7354-547X","contributorId":1716,"corporation":false,"usgs":true,"family":"Konrad","given":"Christopher","email":"cpkonrad@usgs.gov","middleInitial":"P.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":423732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Booth, Derek B.","contributorId":100873,"corporation":false,"usgs":false,"family":"Booth","given":"Derek","email":"","middleInitial":"B.","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":423733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burges, Stephen J.","contributorId":8567,"corporation":false,"usgs":false,"family":"Burges","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":423734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029663,"text":"70029663 - 2005 - Succession on subalpine placer mine spoil: Effects of revegetation with Alnus viridis, Alaska, U.S.A.","interactions":[],"lastModifiedDate":"2021-06-07T15:35:22.467586","indexId":"70029663","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}},"displayTitle":"Succession on subalpine placer mine spoil: Effects of revegetation with <i>Alnus viridis</i>, Alaska, U.S.A.","title":"Succession on subalpine placer mine spoil: Effects of revegetation with Alnus viridis, Alaska, U.S.A.","docAbstract":"<p><i>Alnus viridis</i><span> seedlings were planted on placer mine spoil in an Alaskan subalpine watershed to bypass a seedling establishment bottleneck for </span><i>A. viridis,</i><span> and to evaluate the interaction between </span><i>A. viridis</i><span> and the dominant riparian woody plants,</span><i> Salix alaxensis</i><span> and </span><i>Populus balsamifera</i><span>. The study area was divided into 11 replicate blocks, each on a homogeneous recontoured spoil pile. Blocks were divided into two 0.01 ha plots, and treatments without (control) and with 84 planted </span><i>A. viridis</i><span> seedlings were randomly assigned to plots. After 10 years, the </span><i>Alnus</i><span> treatment had a dense stand of </span><i>A. viridis</i><span> 1–2 m tall, while the control had fewer, smaller seedlings. Compared to the control, planted </span><i>A. viridis</i><span> had a neutral effect on </span><i>S. alaxensis</i><span> and inhibited </span><i>P. balsamifera</i><span> at the seedling establishment stage, but facilitated the growth of established plants of both species, with many plants overtopping the </span><i>A. viridis</i><span> canopy. Compared to the control, </span><i>S. alaxensis</i><span> plants in the </span><i>Alnus</i><span> treatment had higher levels of foliar N and δ15N values closer to those of </span><i>A. viridis</i><span>, indicating the importance of N fixation by </span><i>A. viridis</i><span>. Planting </span><i>A. viridis</i><span> accelerated the rate of succession by stimulating growth of woody dominants.</span></p>","language":"English","publisher":"Institute of Arctic and Alpine Research","publisherLocation":"Boulder, CO","doi":"10.1657/1523-0430(2005)037[0297:SOSPMS]2.0.CO;2","usgsCitation":"Densmore, R.V., 2005, Succession on subalpine placer mine spoil: Effects of revegetation with Alnus viridis, Alaska, U.S.A.: Arctic, Antarctic, and Alpine Research, v. 37, no. 3, p. 297-303, https://doi.org/10.1657/1523-0430(2005)037[0297:SOSPMS]2.0.CO;2.","productDescription":"7 p.","startPage":"297","endPage":"303","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":477773,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://www.bioone.org/doi/10.1657/1523-0430%282005%29037%5B0297%3ASOSPMS%5D2.0.CO%3B2","text":"External Repository"},{"id":240304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Denali National Park and Preserve, Glen Creek watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -150.7866668701172,\n              63.51779683618753\n            ],\n            [\n              -150.7866668701172,\n              63.58\n            ],\n            [\n              -150.6778335571289,\n              63.58\n            ],\n            [\n              -150.6778335571289,\n              63.51779683618753\n            ],\n            [\n              -150.7866668701172,\n              63.51779683618753\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9da8e4b08c986b31d9aa","contributors":{"authors":[{"text":"Densmore, Roseann V.","contributorId":24022,"corporation":false,"usgs":true,"family":"Densmore","given":"Roseann","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":423693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029502,"text":"70029502 - 2005 - Wildlife as valuable natural resources vs. intolerable pests: A suburban wildlife management model","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029502","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3669,"text":"Urban Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Wildlife as valuable natural resources vs. intolerable pests: A suburban wildlife management model","docAbstract":"Management of wildlife in suburban environments involves a complex set of interactions between both human and wildlife populations. Managers need additional tools, such as models, that can help them assess the status of wildlife populations, devise and apply management programs, and convey this information to other professionals and the public. We present a model that conceptualizes how some wildlife populations can fluctuate between extremely low (rare, threatened, or endangered status) and extremely high (overabundant) numbers over time. Changes in wildlife abundance can induce changes in human perceptions, which continually redefine species as a valuable resource to be protected versus a pest to be controlled. Management programs thatincorporate a number of approaches and promote more stable populations of wildlife avoid the problems of the resource versus pest transformation, are less costly to society, and encourage more positive and less negative interactions between humans and wildlife. We presenta case example of the beaver Castor canadensis in Massachusetts to illustrate how this model functions and can be applied. ?? 2005 Springer Science + Business Media, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Urban Ecosystems","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11252-005-4379-5","issn":"10838155","usgsCitation":"DeStefano, S., and Deblinger, R., 2005, Wildlife as valuable natural resources vs. intolerable pests: A suburban wildlife management model: Urban Ecosystems, v. 8, no. 2 SPEC. ISS., p. 179-190, https://doi.org/10.1007/s11252-005-4379-5.","startPage":"179","endPage":"190","numberOfPages":"12","costCenters":[],"links":[{"id":237780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210760,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11252-005-4379-5"}],"volume":"8","issue":"2 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd0e4e4b08c986b32f10d","contributors":{"authors":[{"text":"DeStefano, S.","contributorId":84309,"corporation":false,"usgs":true,"family":"DeStefano","given":"S.","email":"","affiliations":[],"preferred":false,"id":423017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deblinger, R.D.","contributorId":8946,"corporation":false,"usgs":true,"family":"Deblinger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":423016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029661,"text":"70029661 - 2005 - Karst database development in Minnesota: Design and data assembly","interactions":[],"lastModifiedDate":"2012-03-12T17:21:06","indexId":"70029661","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Karst database development in Minnesota: Design and data assembly","docAbstract":"The Karst Feature Database (KFD) of Minnesota is a relational GIS-based Database Management System (DBMS). Previous karst feature datasets used inconsistent attributes to describe karst features in different areas of Minnesota. Existing metadata were modified and standardized to represent a comprehensive metadata for all the karst features in Minnesota. Microsoft Access 2000 and ArcView 3.2 were used to develop this working database. Existing county and sub-county karst feature datasets have been assembled into the KFD, which is capable of visualizing and analyzing the entire data set. By November 17 2002, 11,682 karst features were stored in the KFD of Minnesota. Data tables are stored in a Microsoft Access 2000 DBMS and linked to corresponding ArcView applications. The current KFD of Minnesota has been moved from a Windows NT server to a Windows 2000 Citrix server accessible to researchers and planners through networked interfaces. ?? Springer-Verlag 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00254-005-1240-3","issn":"09430105","usgsCitation":"Gao, Y., Alexander, E., and Tipping, R., 2005, Karst database development in Minnesota: Design and data assembly: Environmental Geology, v. 47, no. 8, p. 1072-1082, https://doi.org/10.1007/s00254-005-1240-3.","startPage":"1072","endPage":"1082","numberOfPages":"11","costCenters":[],"links":[{"id":240268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212734,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00254-005-1240-3"}],"volume":"47","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-04-09","publicationStatus":"PW","scienceBaseUri":"505a405fe4b0c8380cd64cec","contributors":{"authors":[{"text":"Gao, Y.","contributorId":82437,"corporation":false,"usgs":true,"family":"Gao","given":"Y.","email":"","affiliations":[],"preferred":false,"id":423687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, E.C. Jr.","contributorId":94062,"corporation":false,"usgs":true,"family":"Alexander","given":"E.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":423688,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tipping, R.G.","contributorId":67272,"corporation":false,"usgs":true,"family":"Tipping","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":423686,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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