{"pageNumber":"2579","pageRowStart":"64450","pageSize":"25","recordCount":184617,"records":[{"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":70029553,"text":"70029553 - 2005 - Survival and selection of migrating salmon from capture-recapture models with individual traits","interactions":[],"lastModifiedDate":"2021-07-02T16:35:04.572632","indexId":"70029553","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Survival and selection of migrating salmon from capture-recapture models with individual traits","docAbstract":"<p><span>Capture–recapture studies are powerful tools for studying animal population dynamics, providing information on population abundance, survival rates, population growth rates, and selection for phenotypic traits. In these studies, the probability of observing a tagged individual reflects both the probability of the individual surviving to the time of recapture and the probability of recapturing an animal, given that it is alive. If both of these probabilities are related to the same phenotypic trait, it can be difficult to distinguish effects on survival probabilities from effects on recapture probabilities. However, when animals are individually tagged and have multiple opportunities for recapture, we can properly partition observed trait-related variability into survival and recapture components. We present an overview of capture–recapture models that incorporate individual variability and develop methods to incorporate results from these models into estimates of population survival and selection for phenotypic traits. We conducted a series of simulations to understand the performance of these estimators and to assess the consequences of ignoring individual variability when it exists. In addition, we analyzed a large data set of &gt;153 000 juvenile chinook salmon (Oncorhynchus tshawytscha) and steelhead (O. mykiss) of known length that were PIT-tagged during their seaward migration. Both our simulations and the case study indicated that the ability to precisely estimate selection for phenotypic traits was greatly compromised when differential recapture probabilities were ignored. Estimates of population survival, however, were far more robust. In the chinook salmon and steelhead study, we consistently found that smaller fish had a greater probability of recapture. We also uncovered length-related survival relationships in over half of the release group/river segment combinations that we observed, but we found both positive and negative relationships between length and survival probability. These results have important implications for the management of salmonid populations.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/04-0940","usgsCitation":"Zabel, R., Wagner, T., Congleton, J., Smith, S.G., and Williams, J.G., 2005, Survival and selection of migrating salmon from capture-recapture models with individual traits: Ecological Applications, v. 15, no. 4, p. 1427-1439, https://doi.org/10.1890/04-0940.","productDescription":"13 p.","startPage":"1427","endPage":"1439","numberOfPages":"13","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":237457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2b9e4b08c986b31f8f5","contributors":{"authors":[{"text":"Zabel, Richard","contributorId":219280,"corporation":false,"usgs":false,"family":"Zabel","given":"Richard","affiliations":[{"id":39987,"text":"Western Forestry and Conservation Association, Portland, OR","active":true,"usgs":false}],"preferred":false,"id":423256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Tyler 0000-0003-1726-016X twagner@usgs.gov","orcid":"https://orcid.org/0000-0003-1726-016X","contributorId":1050,"corporation":false,"usgs":true,"family":"Wagner","given":"Tyler","email":"twagner@usgs.gov","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":423252,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Congleton, James","contributorId":100239,"corporation":false,"usgs":true,"family":"Congleton","given":"James","email":"","affiliations":[],"preferred":false,"id":423254,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Steven G. sgsmith@usgs.gov","contributorId":1560,"corporation":false,"usgs":true,"family":"Smith","given":"Steven","email":"sgsmith@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":423255,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, John G.","contributorId":10270,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":423253,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"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":70029544,"text":"70029544 - 2005 - Genetic evaluation of a Great Lakes lake trout hatchery program","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029544","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Genetic evaluation of a Great Lakes lake trout hatchery program","docAbstract":"Efforts over several decades to restore lake trout Salvelinus namaycush in U.S. waters of the upper Great Lakes have emphasized the stocking of juveniles from each of six hatchery broodstocks. Retention of genetic diversity across all offspring life history stages throughout the hatchery system has been an important component of the restoration hatchery and stocking program. Different stages of the lake trout hatchery program were examined to determine how effective hatchery practices have been in minimizing the loss of genetic diversity in broodstock adults and in progeny stocked. Microsatellite loci were used to estimate allele frequencies, measures of genetic diversity, and relatedness for wild source populations, hatchery broodstocks, and juveniles. We also estimated the effective number of breeders for each broodstock. Hatchery records were used to track destinations of fertilized eggs from all spawning dates to determine whether adult contributions to stocking programs were proportional to reproductive effort. Overall, management goals of maintaining genetic diversity were met across all stages of the hatchery program; however, we identified key areas where changes in mating regimes and in the distribution of fertilized gametes and juveniles could be improved. Estimates of effective breeding population size (Nb) were 9-41% of the total number of adults spawned. Low estimates of Nb were primarily attributed to spawning practices, including the pooling of gametes from multiple males and females and the reuse of males. Nonrandom selection and distribution of fertilized eggs before stocking accentuated declines in effective breeding population size and increased levels of relatedness of juveniles distributed to different rearing facilities and stocking locales. Adoption of guidelines that decrease adult reproductive variance and promote more equitable reproductive contributions of broodstock adults to juveniles would further enhance management goals of maintaining genetic diversity and minimize probabilities of consanguineous matings among stocked individuals when sexually mature. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/T04-074.1","issn":"00028487","usgsCitation":"Page, K., Scribner, K., Bast, D., Holey, M., and Burnham-Curtis, M.K., 2005, Genetic evaluation of a Great Lakes lake trout hatchery program: Transactions of the American Fisheries Society, v. 134, no. 4, p. 872-891, https://doi.org/10.1577/T04-074.1.","startPage":"872","endPage":"891","numberOfPages":"20","costCenters":[],"links":[{"id":210848,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T04-074.1"},{"id":237892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"4","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505a1576e4b0c8380cd54e1a","contributors":{"authors":[{"text":"Page, K.S.","contributorId":47332,"corporation":false,"usgs":true,"family":"Page","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":423209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scribner, K.T.","contributorId":97033,"corporation":false,"usgs":true,"family":"Scribner","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":423211,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bast, D.","contributorId":101860,"corporation":false,"usgs":true,"family":"Bast","given":"D.","email":"","affiliations":[],"preferred":false,"id":423212,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holey, M.E.","contributorId":68957,"corporation":false,"usgs":true,"family":"Holey","given":"M.E.","affiliations":[],"preferred":false,"id":423210,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burnham-Curtis, M. K.","contributorId":39328,"corporation":false,"usgs":true,"family":"Burnham-Curtis","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":423208,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029289,"text":"70029289 - 2005 - Bioassessment of fish communities of the upper Delaware River","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70029289","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2898,"text":"Northeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Bioassessment of fish communities of the upper Delaware River","docAbstract":"We assessed the biotic integrity of the middle-to-upper Delaware River. We sampled fish and assembled water quality data for eight stations and three habitat types (pool, riffle, and submerged aquatic vegetation [SAV]) of the Delaware River and applied an existing index of biotic integrity (IBI) recently developed for the northern mid-Atlantic slope drainages. We used Spearman's correlation to test IBI scores against measures of water quality (WQI) and cultural pollution. IBI scores were not significantly correlated with WQI, but were significantly negatively correlated with sewage load of adjacent tributaries (rs = -0.647, p = 0.08). Sites ranged from good to fair in biotic integrity. Fish assemblage composition from all three habitat types was necessary in order to accurately characterize biotic integrity. Of the three habitat types, fish assemblages from SAV habitats had the greatest positive effect on biotic integrity. Continued application of the IBI may be useful as a long-term monitoring tool as this river corridor becomes increasingly urbanized.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Northeastern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"10926194","usgsCitation":"van Snik Gray, E., Ross, R.M., and Bennett, R.M., 2005, Bioassessment of fish communities of the upper Delaware River: Northeastern Naturalist, v. 12, no. 2, p. 203-216.","startPage":"203","endPage":"216","numberOfPages":"14","costCenters":[],"links":[{"id":237875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f13ce4b0c8380cd4aaf7","contributors":{"authors":[{"text":"van Snik Gray, E.","contributorId":35846,"corporation":false,"usgs":true,"family":"van Snik Gray","given":"E.","email":"","affiliations":[],"preferred":false,"id":422089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, R. M.","contributorId":39311,"corporation":false,"usgs":true,"family":"Ross","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":422090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, R. M.","contributorId":97852,"corporation":false,"usgs":true,"family":"Bennett","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":422091,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":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":70029613,"text":"70029613 - 2005 - Simulating the evolution of coastal morphology and stratigraphy with a new morphological-behaviour model (GEOMBEST)","interactions":[],"lastModifiedDate":"2018-04-09T12:31:37","indexId":"70029613","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Simulating the evolution of coastal morphology and stratigraphy with a new morphological-behaviour model (GEOMBEST)","docAbstract":"<p>A new morphological-behaviour model is used to simulate evolution of coastal morphology associated with cross-shore translations of the shoreface, barrier, and estuary. The model encapsulates qualitative principles drawn from established geological concepts that are parameterized to provide quantitative predictions of morphological change on geological time scales (order 10 3 years), as well as shorter time scales applicable for long-term coastal management (order 101 to 102 years). Changes in sea level, and sediment volume within the shoreface, barrier, and estuary, drive the model behaviour. Further parameters, defining substrate erodibility, sediment composition, and time-dependent shoreface response, constrain the evolution of the shoreface towards an equilibrium profile. Results from numerical experiments are presented for the low-gradient autochthonous setting of North Carolina and the steep allochthonous setting of the Washington shelf. Simulations in the Currituck region of North Carolina examined the influence of sediment supply, substrate composition, and substrate erodibility on barrier transgression. Results demonstrate that the presence of a lithified substrate reduces the rate of barrier transgression compared to scenarios where an erodible, sand-rich substrate exists. Simulations of the Washington coast, 20 km north of the Columbia River, confirmed that the model can reproduce complex stratigraphy involving regressive and transgressive phases of coastal evolution. Results suggest that the first major addition of sediment to the shelf occurred around 12 900 years ago and resulted from the rapid addition of sediment volume from the Columbia River attributed to the Missoula floods. This was followed by a period where little or no sediment was added (12 400-9100 BP) and a third period when most sediment was added to the shelf (9100 BP to present) from the Columbia River. Comparing results from each setting demonstrates an indirect control that substrate slope has on shoreface transgression rates. Shoreface transgression is shown to be sensitive to the rate of estuarine sedimentation, with the sensitivity increasing as substrate slope decreases.&nbsp;</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.margeo.2005.02.019","issn":"00253227","usgsCitation":"Stolper, D., List, J.H., and Thieler, E., 2005, Simulating the evolution of coastal morphology and stratigraphy with a new morphological-behaviour model (GEOMBEST): Marine Geology, v. 218, no. 1-4, p. 17-36, https://doi.org/10.1016/j.margeo.2005.02.019.","productDescription":"20 p.","startPage":"17","endPage":"36","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":237826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.3275146484375,\n              35.72421761691415\n            ],\n            [\n              -75.377197265625,\n              35.72421761691415\n            ],\n            [\n              -75.377197265625,\n              37.020098201368114\n            ],\n            [\n              -76.3275146484375,\n              37.020098201368114\n            ],\n            [\n              -76.3275146484375,\n              35.72421761691415\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"218","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8fd7e4b08c986b31918a","contributors":{"authors":[{"text":"Stolper, D.","contributorId":56846,"corporation":false,"usgs":true,"family":"Stolper","given":"D.","email":"","affiliations":[],"preferred":false,"id":423453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"List, J. H.","contributorId":70406,"corporation":false,"usgs":true,"family":"List","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":423454,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thieler, E.R. 0000-0003-4311-9717","orcid":"https://orcid.org/0000-0003-4311-9717","contributorId":93082,"corporation":false,"usgs":true,"family":"Thieler","given":"E.R.","affiliations":[],"preferred":false,"id":423455,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":70029630,"text":"70029630 - 2005 - A comparison of American Oystercatcher reproductive success on barrier beach and river island habitats in coastal North Carolina","interactions":[],"lastModifiedDate":"2022-06-06T14:30:32.199438","indexId":"70029630","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"A comparison of American Oystercatcher reproductive success on barrier beach and river island habitats in coastal North Carolina","docAbstract":"<div class=\"div0\"><div class=\"row ArticleContentRow\"><p id=\"ID0EF\" class=\"first\">American Oystercatcher (<i><span class=\"genus-species\">Haematopus palliatus</span></i>) numbers along the east coast of the United States are declining in some areas and expanding in others. Researchers have suggested that movement from traditional barrier beach habitats to novel inland habitats and coastal marshes may explain some of these changes, but few studies have documented oystercatcher reproductive success in non-traditional habitats. This study compares the reproductive success of the American Oystercatcher on three river islands in the lower Cape Fear River of North Carolina with that of birds nesting on barrier island beach habitat of Cape Lookout National Seashore. There were 17.6 times more oystercatcher breeding pairs per kilometer on the river island habitat than barrier beach habitat. The Mayfield estimate of daily nest content survival was 0.97 (S.E. ± 0.0039) on river islands, significantly higher than 0.92 (S.E. ± 0.0059) on barrier islands. The primary identifiable cause of nest failure on the river islands was flooding while the main cause of nest failure on the barrier islands was mammalian predation. Fledging success was equally low at both study sites. Only 0.19 chicks fledged per pair in 2002, and 0.21 chicks fledged per pair in 2003 on the river islands and 0.14 chicks fledged per pair in 2002 and 0.20 chicks fledged per pair in 2003 on the barrier islands. Many questions are still unanswered and more research is needed to fully understand the causes of chick mortality and the functional significance of non-traditional nesting habitats for the American Oystercatcher in the eastern United States.</p></div></div>","language":"English","publisher":"The Waterbird Society","doi":"10.1675/1524-4695(2005)028[0150:ACOAOR]2.0.CO;2","usgsCitation":"McGowan, C., Simons, T.R., Golder, W., and Cordes, J., 2005, A comparison of American Oystercatcher reproductive success on barrier beach and river island habitats in coastal North Carolina: Waterbirds, v. 28, no. 2, p. 150-155, https://doi.org/10.1675/1524-4695(2005)028[0150:ACOAOR]2.0.CO;2.","productDescription":"6 p.","startPage":"150","endPage":"155","numberOfPages":"6","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":237538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Cape Fear River, Cape Lookout National Seashore","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.03314208984375,\n              33.815666308702774\n            ],\n            [\n              -77.838134765625,\n              33.815666308702774\n            ],\n            [\n              -77.838134765625,\n              34.076549928891744\n            ],\n            [\n              -78.03314208984375,\n              34.076549928891744\n            ],\n            [\n              -78.03314208984375,\n              33.815666308702774\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.377197265625,\n              35.1760533659996\n            ],\n            [\n              -75.62713623046875,\n              35.33305256126513\n            ],\n            [\n              -76.343994140625,\n              34.93548199355901\n            ],\n            [\n              -76.63787841796875,\n              34.56764471968292\n            ],\n            [\n              -76.53350830078125,\n              34.538237527295756\n            ],\n            [\n              -75.92376708984375,\n              35.043489514314686\n            ],\n            [\n              -75.377197265625,\n              35.1760533659996\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"28","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e353e4b0c8380cd45f83","contributors":{"authors":[{"text":"McGowan, Conor P. 0000-0002-7330-9581 cmcgowan@usgs.gov","orcid":"https://orcid.org/0000-0002-7330-9581","contributorId":3381,"corporation":false,"usgs":true,"family":"McGowan","given":"Conor P.","email":"cmcgowan@usgs.gov","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":false,"id":423526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simons, Theodore R. 0000-0002-1884-6229 tsimons@usgs.gov","orcid":"https://orcid.org/0000-0002-1884-6229","contributorId":2623,"corporation":false,"usgs":true,"family":"Simons","given":"Theodore","email":"tsimons@usgs.gov","middleInitial":"R.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":423527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Golder, W.","contributorId":8279,"corporation":false,"usgs":true,"family":"Golder","given":"W.","email":"","affiliations":[],"preferred":false,"id":423525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordes, J.","contributorId":88942,"corporation":false,"usgs":true,"family":"Cordes","given":"J.","email":"","affiliations":[],"preferred":false,"id":423528,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029555,"text":"70029555 - 2005 - The World Coal Quality Inventory: A status report","interactions":[],"lastModifiedDate":"2012-03-12T17:20:53","indexId":"70029555","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"The World Coal Quality Inventory: A status report","docAbstract":"National and international policy makers and industry require accurate information on coal, including coal quality data, to make informed decisions regarding international import needs and export opportunities, foreign policy, technology transfer policies, foreign investment prospects, environmental and health assessments, and byproduct use and disposal issues. Unfortunately, the information needed is generally proprietary and does not exist in the public domain. The U.S. Geological Survey (USGS), in conjunction with partners in about 60 countries, is developing a digital compilation of worldwide coal quality. The World Coal Quality Inventory (WoCQI) will contain coal quality information for samples obtained from major coal beds in countries having significant coal production, as well as from many countries producing smaller volumes of coal, with an emphasis on coals currently being burned. The information that will be incorporated includes, but is not limited to, proximate and ultimate analyses; sulfur-form data; major, minor, and trace element analysis; and semi-quantitative analyses of minerals, modes of occurrence, and petrography. The coal quality information will eventually be linked to a Geographic Information System (GIS) that shows the coal basins and sample locations along with geologic, land use, transportation, industrial, and cultural information. The WoCQI will be accessible on the USGS web page and new data added periodically. This multi-national collaboration is developing global coal quality data that contain a broad array of technologic, economic, and environmental parameters, which should help to ensure the efficient and environmentally compatible use of global coal resources in the 21st century.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Coal Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coal.2005.02.013","issn":"01665162","usgsCitation":"Tewalt, S., Willett, J., and Finkelman, R.B., 2005, The World Coal Quality Inventory: A status report: International Journal of Coal Geology, v. 63, no. 1-2 SPEC. ISS., p. 190-194, https://doi.org/10.1016/j.coal.2005.02.013.","startPage":"190","endPage":"194","numberOfPages":"5","costCenters":[],"links":[{"id":210542,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coal.2005.02.013"},{"id":237496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"1-2 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba98ae4b08c986b322328","contributors":{"authors":[{"text":"Tewalt, S.J.","contributorId":55838,"corporation":false,"usgs":true,"family":"Tewalt","given":"S.J.","affiliations":[],"preferred":false,"id":423261,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willett, J.C.","contributorId":41858,"corporation":false,"usgs":true,"family":"Willett","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":423260,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Finkelman, R. B.","contributorId":20341,"corporation":false,"usgs":true,"family":"Finkelman","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":423259,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029642,"text":"70029642 - 2005 - Estimation of regional material yield from coastal landslides based on historical digital terrain modelling","interactions":[],"lastModifiedDate":"2012-03-12T17:21:10","indexId":"70029642","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1425,"text":"Earth Surface Processes and Landforms","active":true,"publicationSubtype":{"id":10}},"title":"Estimation of regional material yield from coastal landslides based on historical digital terrain modelling","docAbstract":"High-resolution historical (1942) and recent (1994) digital terrain models were derived from aerial photographs along the Big Sur coastline in central California to measure the long-term volume of material that enters the nearshore environment. During the 52-year measurement time period, an average of 21 000 ?? 3100 m3 km-1 a-1 of material was eroded from nine study sections distributed along the coast, with a low yield of 1000 ?? 240 m3 km-1 a-1 and a high of 46 700 ?? 7300 m3 km-1 a-1. The results compare well with known volumes from several deep-seated landslides in the area and suggest that the processes by which material is delivered to the coast are episodic in nature. In addition, a number of parameters are investigated to determine what influences the substantial variation in yield along the coast. It is found that the magnitude of regional coastal landslide sediment yield is primarily related to the physical strength of the slope-forming material. Coastal Highway 1 runs along the lower portion of the slope along this stretch of coastline, and winter storms frequently damage the highway. The California Department of Transportation is responsible for maintaining this scenic highway while minimizing the impacts to the coastal ecosystems that are part of the Monterey Bay National Marine Sanctuary. This study provides environmental managers with critical background data on the volumes of material that historically enter the nearshore from landslides, as well as demonstrating the application of deriving historical digital terrain data to model landscape evolution. Published in 2005 by John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth Surface Processes and Landforms","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/esp.1168","issn":"01979337","usgsCitation":"Hapke, C., 2005, Estimation of regional material yield from coastal landslides based on historical digital terrain modelling: Earth Surface Processes and Landforms, v. 30, no. 6, p. 679-697, https://doi.org/10.1002/esp.1168.","startPage":"679","endPage":"697","numberOfPages":"19","costCenters":[],"links":[{"id":240541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212969,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/esp.1168"}],"volume":"30","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-04-29","publicationStatus":"PW","scienceBaseUri":"505a0ba4e4b0c8380cd527f6","contributors":{"authors":[{"text":"Hapke, C.J.","contributorId":108233,"corporation":false,"usgs":true,"family":"Hapke","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":423599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028820,"text":"70028820 - 2005 - Origin and development of plains-type folds in the mid-continent (United States) during the late Paleozoic","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028820","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Origin and development of plains-type folds in the mid-continent (United States) during the late Paleozoic","docAbstract":"Plains-type folds are local, subtle anticlines formed in the thin sedimentary package overlying a shallow, crystalline basement on the craton. They are small in areal extent (usually less than 1-3 km 2 [0.4-1.2 mi2]), and their amplitude increases with depth (usually tens of meters), which is mainly the result of differential compaction of sediments (usually clastic units) over tilted, rigid, basement fault blocks. The development of these structural features by continuous but intermittent movement of the basement fault blocks in the late Paleozoic in the United States mid-continent is substantiated by a record of stratigraphic and sedimentological evidence. The recurrent structural movement, which reflects adjustment to external stresses, is expressed by the change in thickness of stratigraphic units over the crest of the fold compared to the flanks. By plotting the change in thickness for different stratigraphic units of anticlines on different fault blocks, it is possible to determine the timing of movement of the blocks that reflect structural adjustment. These readjustments are confirmed by sedimentological evidence, such as convolute, soft-sediment deformation features and small intraformational faults. The stratigraphic interval change in thickness for numerous structures in the Cherokee, Forest City, and Salina basins and on the Nemaha anticline of the mid-continent United States was determined and compared for location and timing of the adjustments. Most of the adjustment occurred during and after time of deposition of the Permian-Pennsylvanian clastic units, which, in turn, reflect tectonic disturbance in adjacent areas, and the largest amount of movement on the plains-type structures occurred on those nearest and semiparallel to major positive features, such as the Nemaha anticline. Depending on the time of origin and development of plains-type folds, they may control the entrapment and occurrence of oil and gas. Copyright ??2005. The American Association of Petroleum Geologists. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Association of Petroleum Geologists Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1306/08050404013","issn":"01491423","usgsCitation":"Merriam, D.F., 2005, Origin and development of plains-type folds in the mid-continent (United States) during the late Paleozoic: American Association of Petroleum Geologists Bulletin, v. 89, no. 1, p. 101-118, https://doi.org/10.1306/08050404013.","startPage":"101","endPage":"118","numberOfPages":"18","costCenters":[],"links":[{"id":209798,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/08050404013"},{"id":236515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a709ee4b0c8380cd7612e","contributors":{"authors":[{"text":"Merriam, D. F.","contributorId":63175,"corporation":false,"usgs":true,"family":"Merriam","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":419881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70029365,"text":"70029365 - 2005 - Watershed-based survey designs","interactions":[],"lastModifiedDate":"2017-04-11T09:54:06","indexId":"70029365","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":"Watershed-based survey designs","docAbstract":"<p><span>Watershed-based sampling design and assessment tools help serve the multiple goals for water quality monitoring required under the Clean Water Act, including assessment of regional conditions to meet Section 305(b), identification of impaired water bodies or watersheds to meet Section 303(d), and development of empirical relationships between causes or sources of impairment and biological responses. Creation of GIS databases for hydrography, hydrologically corrected digital elevation models, and hydrologic derivatives such as watershed boundaries and upstream–downstream topology of subcatchments would provide a consistent seamless nationwide framework for these designs. The elements of a watershed-based sample framework can be represented either as a continuous infinite set defined by points along a linear stream network, or as a discrete set of watershed polygons. Watershed-based designs can be developed with existing probabilistic survey methods, including the use of unequal probability weighting, stratification, and two-stage frames for sampling. Case studies for monitoring of Atlantic Coastal Plain streams, West Virginia wadeable streams, and coastal Oregon streams illustrate three different approaches for selecting sites for watershed-based survey designs.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10661-005-4774-7","issn":"01676369","usgsCitation":"Detenbeck, N., Cincotta, D., Denver, J.M., Greenlee, S., Olsen, A., and Pitchford, A., 2005, Watershed-based survey designs: Environmental Monitoring and Assessment, v. 103, no. 1, p. 59-81, https://doi.org/10.1007/s10661-005-4774-7.","productDescription":"23 p.","startPage":"59","endPage":"81","numberOfPages":"23","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":210839,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10661-005-4774-7"},{"id":237881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"103","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcf87e4b08c986b32e95a","contributors":{"authors":[{"text":"Detenbeck, N.E.","contributorId":7073,"corporation":false,"usgs":true,"family":"Detenbeck","given":"N.E.","affiliations":[],"preferred":false,"id":422423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cincotta, D.","contributorId":48753,"corporation":false,"usgs":true,"family":"Cincotta","given":"D.","affiliations":[],"preferred":false,"id":422425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denver, J. M.","contributorId":100356,"corporation":false,"usgs":true,"family":"Denver","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":422428,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Greenlee, S.K.","contributorId":38353,"corporation":false,"usgs":true,"family":"Greenlee","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":422424,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Olsen, A.R.","contributorId":98089,"corporation":false,"usgs":true,"family":"Olsen","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":422427,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pitchford, A.M.","contributorId":75593,"corporation":false,"usgs":true,"family":"Pitchford","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":422426,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70029459,"text":"70029459 - 2005 - The onset of metamorphism in ordinary and carbonaceous chondrites","interactions":[],"lastModifiedDate":"2022-05-27T15:37:26.495123","indexId":"70029459","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2715,"text":"Meteoritics and Planetary Science","active":true,"publicationSubtype":{"id":10}},"title":"The onset of metamorphism in ordinary and carbonaceous chondrites","docAbstract":"<p><span>Ordinary and carbonaceous chondrites of the lowest petrologic types were surveyed by X-ray mapping techniques. A variety of metamorphic effects were noted and subjected to detailed analysis using electron microprobe, scanning electron microscopy (SEM), transmission electron microscopy (TEM), and cathodoluminescence (CL) methods. The distribution of Cr in FeO-rich olivine systematically changes as metamorphism increases between type 3.0 and type 3.2. Igneous zoning patterns are replaced by complex ones and Cr-rich coatings develop on all grains. Cr distributions in olivine are controlled by the exsolution of a Cr-rich phase, probably chromite. Cr in olivine may have been partly present as tetrahedrally coordinated Cr</span><sup>3+</sup><span>. Separation of chromite is nearly complete by petrologic type 3.2. The abundance of chondrules showing an inhomogeneous distribution of alkalis in mesostasis also increases with petrologic type. TEM shows this to be the result of crystallization of albite. Residual glass compositions systematically change during metamorphism, becoming increasingly rich in K. Glass in type I chondrules also gains alkalis during metamorphism. Both types of chondrules were open to an exchange of alkalis with opaque matrix and other chondrules. The matrix in the least metamorphosed chondrites is rich in S and Na. The S is lost from the matrix at the earliest stages of metamorphism due to coalescence of minute grains. Progressive heating also results in the loss of sulfides from chondrule rims and increases sulfide abundances in coarse matrix assemblages as well as inside chondrules. Alkalis initially leave the matrix and enter chondrules during early metamorphism. Feldspar subsequently nucleates in the matrix and Na re-enters from chondrules. These metamorphic trends can be used to refine classification schemes for chondrites. Cr distributions in olivine are a highly effective tool for assigning petrologic types to the most primitive meteorites and can be used to subdivide types 3.0 and 3.1 into types 3.00 through 3.15. On this basis, the most primitive ordinary chondrite known is Semarkona, although even this meteorite has experienced a small amount of metamorphism. Allan Hills (ALH) A77307 is the least metamorphosed CO chondrite and shares many properties with the ungrouped carbonaceous chondrite Acfer 094. Analytical problems are significant for glasses in type II chondrules, as Na is easily lost during microprobe analysis. As a result, existing schemes for chondrule classification that are based on the alkali content of glasses need to be revised.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1945-5100.2005.tb00366.x","usgsCitation":"Grossman, J.N., and Brearley, A.J., 2005, The onset of metamorphism in ordinary and carbonaceous chondrites: Meteoritics and Planetary Science, v. 40, no. 1, p. 87-122, https://doi.org/10.1111/j.1945-5100.2005.tb00366.x.","productDescription":"36 p.","startPage":"87","endPage":"122","numberOfPages":"36","costCenters":[],"links":[{"id":477719,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1945-5100.2005.tb00366.x","text":"Publisher Index Page"},{"id":237708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-01-26","publicationStatus":"PW","scienceBaseUri":"505bae54e4b08c986b324003","contributors":{"authors":[{"text":"Grossman, Jeffrey N. 0000-0001-9099-9628","orcid":"https://orcid.org/0000-0001-9099-9628","contributorId":37317,"corporation":false,"usgs":true,"family":"Grossman","given":"Jeffrey","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":422825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brearley, Adrian J.","contributorId":211911,"corporation":false,"usgs":false,"family":"Brearley","given":"Adrian","email":"","middleInitial":"J.","affiliations":[{"id":36307,"text":"University of New Mexico","active":true,"usgs":false}],"preferred":false,"id":422826,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029382,"text":"70029382 - 2005 - Unusually low rates of slip on the Santa Rosa Range fault zone, northern Nevada","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029382","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Unusually low rates of slip on the Santa Rosa Range fault zone, northern Nevada","docAbstract":"The Santa Rosa Range fault zone (SRRFZ) is one of the most topographically prominent normal fault systems in the northern Basin and Range province of the western United States. It has been assigned high rates of vertical slip by others and has been identified as a possible site of the future extension of the central Nevada seismic belt (CNSB). We use detailed trench mapping and luminescence dating to estimate displacements and timing of the last several large-magnitude paleoearthquakes on the southern part of the SRRFZ at a trench site near Orovada, Nevada. Coseismic vertical displacements ranged from 1 to 2.8 m for each of the last four events. Luminescence ages provide time limits for the last three events of 125-155 ka, 90-108 ka, and 11-16 ka. These data yield recurrence intervals of 17-65 k.y. and 74-97 k.y. and an elapsed time of 11-16 k.y. since the youngest event. Slip-rate determinations at the Orovada site are complicated by multiple fault strands, but rates calculated from a variety of data are surprisingly low (0.01-0.16 mm/yr), given the topographic prominence of the Santa Rosa Range. A lack of compelling patterns in a comparison of paleoseismic parameters indicate that the SRRFZ is no more likely a location for a large-magnitude earthquake than previously identified seismic gaps or along faults that lie directly north of the CNSB.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/0120040001","issn":"00371106","usgsCitation":"Personius, S., and Mahan, S., 2005, Unusually low rates of slip on the Santa Rosa Range fault zone, northern Nevada: Bulletin of the Seismological Society of America, v. 95, no. 1, p. 319-333, https://doi.org/10.1785/0120040001.","startPage":"319","endPage":"333","numberOfPages":"15","costCenters":[],"links":[{"id":237597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210621,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120040001"}],"volume":"95","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbd09e4b08c986b328e9c","contributors":{"authors":[{"text":"Personius, S. F. 0000-0001-8347-7370","orcid":"https://orcid.org/0000-0001-8347-7370","contributorId":31408,"corporation":false,"usgs":true,"family":"Personius","given":"S. F.","affiliations":[],"preferred":false,"id":422496,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahan, S. A. 0000-0001-5214-7774","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":94333,"corporation":false,"usgs":true,"family":"Mahan","given":"S. A.","affiliations":[],"preferred":false,"id":422497,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029640,"text":"70029640 - 2005 - Acute and chronic toxicity of lead in water and diet to the amphipod Hyalella azteca","interactions":[],"lastModifiedDate":"2020-11-16T15:48:36.205977","indexId":"70029640","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":"Acute and chronic toxicity of lead in water and diet to the amphipod Hyalella azteca","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>We evaluated the influence of waterborne and dietary lead (Pb) exposure on the acute and chronic toxicity of Pb to the amphipod<span>&nbsp;</span><i>Hyalella azteca</i>. Test solutions were generated by a modified diluter with an extended (24‐h) equilibration period. Acute (96‐h) toxicity of Pb varied with water hardness in the range of 71 to 275 mg/L as CaCO<sub>3</sub>, despite similar dissolved Pb concentrations. Acute toxicity was greatest in soft test water, with less than 50% survival at the lowest dissolved Pb concentration (151 μg/L). Survival also was significantly reduced in medium‐hardness water but not in hard test water. In chronic (42‐d) studies, amphipods were exposed to waterborne Pb and fed either a control diet or a diet equilibrated with waterborne Pb levels. For animals fed the control diet, the median lethal concentration (LC50) for Pb was 24 μg/L (as dissolved Pb), and significant reductions in survival occurred at 16 μg/L. Exposure to Pb‐treated diets significantly increased toxicity across a wide range of dissolved Pb concentrations, with a LC50 of 16 μg/L and significant reductions in growth and reproduction at 3.5 μg/L. Significant effects on growth and reproduction occurred at dissolved Pb concentrations close to the current U.S. chronic water‐quality criterion. Our results suggest that both aqueous‐ and dietary‐exposure pathways contribute significantly to chronic Pb exposure and toxic effects in aquatic biota.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1897/04-480R.1","issn":"07307268","usgsCitation":"Besser, J., Brumbaugh, W.G., Brunson, E., and Ingersoll, C., 2005, Acute and chronic toxicity of lead in water and diet to the amphipod Hyalella azteca: Environmental Toxicology and Chemistry, v. 24, no. 7, p. 1807-1815, https://doi.org/10.1897/04-480R.1.","productDescription":"9 p.","startPage":"1807","endPage":"1815","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":240509,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"7","noUsgsAuthors":false,"publicationDate":"2005-07-01","publicationStatus":"PW","scienceBaseUri":"5059e6d3e4b0c8380cd4765f","contributors":{"authors":[{"text":"Besser, J.M.","contributorId":91569,"corporation":false,"usgs":true,"family":"Besser","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":423595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brumbaugh, W. G.","contributorId":106441,"corporation":false,"usgs":true,"family":"Brumbaugh","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":423596,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brunson, E.L.","contributorId":29924,"corporation":false,"usgs":true,"family":"Brunson","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":423593,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ingersoll, C.G. 0000-0003-4531-5949","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":56338,"corporation":false,"usgs":true,"family":"Ingersoll","given":"C.G.","affiliations":[],"preferred":false,"id":423594,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1003677,"text":"1003677 - 2005 - Attempts to identify the source of avian vacuolar myelinopathy for waterbirds","interactions":[],"lastModifiedDate":"2022-11-07T15:30:56.421904","indexId":"1003677","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Attempts to identify the source of avian vacuolar myelinopathy for waterbirds","docAbstract":"<p><span>Attempts were made to reproduce avian vacuolar myelinopathy (AVM) in a number of test animals in order to determine the source of the causative agent for birds and to find a suitable animal model for future studies. Submerged vegetation, plankton, invertebrates, forage fish, and sediments were collected from three lakes with ongoing outbreaks of AVM and fed to American coots (</span><i>Fulica americana</i><span>), mallard ducks and ducklings (</span><i>Anas platyrhynchos</i><span>), quail (</span><i>Coturnix japonica</i><span>), and laboratory mice either via gavage or ad libitum. Tissues from AVM-affected coots with brain lesions were fed to ducklings, kestrels (</span><i>Falco sparverius</i><span>), and American crows (</span><i>Corvus brachyrhynchos</i><span>). Two mallards that ingested one sample of&nbsp;</span><i>Hydrilla verticillata</i><span>&nbsp;along with any biotic or abiotic material associated with its external surface developed brain lesions consistent with AVM, although neither of the ducks had clinical signs of disease. Ingestion of numerous other samples of&nbsp;</span><i>Hydrilla</i><span>&nbsp;from the AVM affected lakes and a lake with no prior history of AVM, other materials (sediments, algae, fish, invertebrates, and water from affected lakes), or tissues from AVM-affected birds did not produce either clinical signs or brain lesions in any of the other test animals in our studies. These results suggest that waterbirds are most likely exposed to the causative agent of AVM while feeding on aquatic vegetation, but we do not believe the vegetation itself is the agent. We hypothesize that the causative agent of AVM might either be accumulated by aquatic vegetation, such as&nbsp;</span><i>Hydrilla</i><span>, or associated with biotic or abiotic material on its external surfaces. In support of that hypothesis, two coots that ingested&nbsp;</span><i>Hydrilla</i><span>&nbsp;sampled from a lake with an ongoing AVM outbreak in wild birds developed neurologic signs within 9 days (ataxia, limb weakness, and incoordination), and one of two coots that ingested&nbsp;</span><i>Hydrilla</i><span>&nbsp;collected from the same site 13 days later became sick and died within 38 days. None of these three sick coots had definitive brain lesions consistent with AVM by light microscopy, but they had no gross or histologic lesions in other tissues. It is unclear if these birds died of AVM. Perhaps they did not ingest a dose sufficient to produce brain lesions or the lesions were ultrastructural. Alternatively, it is possible that a separate neurotoxic agent is responsible for the morbidity and mortality observed in these coots.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-41.1.163","usgsCitation":"Rocke, T.E., Thomas, N.J., Meteyer, C.U., Quist, C., Fischer, J.R., Augspurger, T., and Ward, S.E., 2005, Attempts to identify the source of avian vacuolar myelinopathy for waterbirds: Journal of Wildlife Diseases, v. 41, no. 1, p. 163-170, https://doi.org/10.7589/0090-3558-41.1.163.","productDescription":"8 p.","startPage":"163","endPage":"170","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":488171,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://www.bioone.org/doi/10.7589/0090-3558-41.1.163","text":"External 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Female eider ducks (</span><i>Somateria mollissima</i><span>) may rear broods alone, or they may pool their broods and share brood-rearing. Females are philopatric, and it has been suggested that colonies may largely consist of related females, which could promote interactions among relatives. Alternatively, shared brood care could be random with respect to relatedness, either because brood amalgamations are accidental and nonadaptive, or through group augmentation, assuming that the fitness of all group members increases with group size. We tested these alternatives by measuring the relatedness of co-tending eider females in enduring coalitions with microsatellite markers. Females formed enduring brood-rearing coalitions with each other at random with respect to relatedness. However, based on previous data, partner choice is nonrandom and dependent on female body condition. We discuss potential mechanisms underlying eider communal brood-rearing decisions, which may be driven by the specific ecological conditions under which sociality has evolved in this species.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-294X.2005.02694.x","usgsCitation":"Ost, M., Vitikainen, E., Waldeck, P., Sundstrom, L., Lindstrom, K., Hollmen, T.E., Franson, J.C., and Kilpi, M., 2005, Eider females form non-kin brood-rearing coalitions: Molecular Ecology, v. 14, no. 12, p. 3903-3908, https://doi.org/10.1111/j.1365-294X.2005.02694.x.","productDescription":"6 p.","startPage":"3903","endPage":"3908","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":477742,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-294x.2005.02694.x","text":"Publisher Index 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Christian 0000-0002-0251-4238 jfranson@usgs.gov","orcid":"https://orcid.org/0000-0002-0251-4238","contributorId":177499,"corporation":false,"usgs":true,"family":"Franson","given":"J.","email":"jfranson@usgs.gov","middleInitial":"Christian","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":313768,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kilpi, Mikaei","contributorId":102428,"corporation":false,"usgs":true,"family":"Kilpi","given":"Mikaei","affiliations":[],"preferred":false,"id":313769,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70029487,"text":"70029487 - 2005 - Ground-motion parameters of the southwestern Indiana earthquake of 18 June 2002 and the disparity between the observed and predicted values","interactions":[],"lastModifiedDate":"2022-06-03T15:03:06.948597","indexId":"70029487","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Ground-motion parameters of the southwestern Indiana earthquake of 18 June 2002 and the disparity between the observed and predicted values","docAbstract":"<div id=\"12244517\" class=\"article-section-wrapper js-article-section js-content-section  \"><p>The<span>&nbsp;</span><strong>M</strong><span>&nbsp;</span>4.5 southwestern Indiana earthquake of 18 June 2002 triggered 46 blast monitors in Indiana, Illinois, and Kentucky. The resulting flee-field particle velocity records, along with similar data from previous earthquakes in the study area, provide a clear standard for judging the reliability of current maps for predicting ground motions greater than 2 Hz in southwestern Indiana and southeastern Illinois. Peak horizontal accelerations and velocities, and 5% damped pseudo-accelerations for the earthquake, generally exceeded ground motions predicted for the top of the bedrock by factors of 2 or more, even after soil amplifications were taken into consideration. It is suggested, but not proven, that the low shear-wave velocity and weathered bedrock in the area are also amplifying the higher-frequency ground motions that have been repeatedly recorded by the blast monitors in the study area. It is also shown that there is a good correlation between the peak ground motions and 5% pseudo-accelerations recorded for the event, and the Modified Mercalli intensities interpreted for the event by the U.S. Geological Survey.</p></div>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.76.4.512","usgsCitation":"Street, R., Wiegand, J., Woolery, E., and Hart, P., 2005, Ground-motion parameters of the southwestern Indiana earthquake of 18 June 2002 and the disparity between the observed and predicted values: Seismological Research Letters, v. 76, no. 4, p. 512-530, https://doi.org/10.1785/gssrl.76.4.512.","productDescription":"19 p.","startPage":"512","endPage":"530","numberOfPages":"19","costCenters":[],"links":[{"id":237527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Kentucky","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.033203125,\n              36.756490329505176\n            ],\n            [\n              -85.80322265625,\n              36.756490329505176\n            ],\n            [\n              -85.80322265625,\n              39.605688178320804\n            ],\n            [\n              -89.033203125,\n              39.605688178320804\n            ],\n            [\n              -89.033203125,\n              36.756490329505176\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2b6ee4b0c8380cd5b993","contributors":{"authors":[{"text":"Street, R.","contributorId":35097,"corporation":false,"usgs":true,"family":"Street","given":"R.","email":"","affiliations":[],"preferred":false,"id":422941,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiegand, J.","contributorId":85055,"corporation":false,"usgs":true,"family":"Wiegand","given":"J.","email":"","affiliations":[],"preferred":false,"id":422944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woolery, E.W.","contributorId":53548,"corporation":false,"usgs":true,"family":"Woolery","given":"E.W.","affiliations":[],"preferred":false,"id":422943,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hart, P.","contributorId":45107,"corporation":false,"usgs":true,"family":"Hart","given":"P.","affiliations":[],"preferred":false,"id":422942,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70035154,"text":"70035154 - 2005 - Subtle structural influences on coal thickness and distribution: Examples from the Lower Broas-Stockton coal (Middle Pennsylvanian), Eastern Kentucky Coal Field, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:57","indexId":"70035154","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Subtle structural influences on coal thickness and distribution: Examples from the Lower Broas-Stockton coal (Middle Pennsylvanian), Eastern Kentucky Coal Field, USA","docAbstract":"The Lower Broas-Stockton coal is a heavily mined coal of the Central Appalachian Basin. Coal thickness, distribution, composition, and stratigraphic position were compared with basement structure, gas and oil field trends, and sequence strat- igraphic and paleoclimate interpretations to better understand the geology of the Stockton coal bed in eastern Kentucky. The thickest coal occurs south of the Warfield structural trend and east of the Paint Creek Uplift, two basement-related structures. Along the Warfield trend, coal beds in the underlying Peach Orchard coal zone locally merge with the Stockton coal to form a seam more than 3 m thick. Other areas of thick coal occur in elongate trends. Two pairs of elongate, conjugate trends in Stockton coal thickness are interpreted as regional paleofractures that influenced paleotopography and groundwater during peat accumulation. Compositional group analyses indicate that the Stockton peat infilled depressions in the paleotopography as a topogenous to soligenous mire codominated by tree ferns and lycopsid trees. Flooding from adjacent paleochannels is indicated by partings and seam splits along the margins of the mineable coal body. One or more increments of low-vitrinite coal, dominated by tree ferns and shrubby, Densosporites-producing lycopsids occur at all sample sites. Similar assemblages have been previously used to identify ombrogenous, domed mire origins for Early and Middle Pennsylvanian coals in which ash yields were less than 10%. It is difficult, however, to reconcile ombrogenous conditions with the partings in the Stockton coal in this area. Low-ash, low-vitrinite increments may have been formed in topogenous to soligenous mires with periodic drying or water-table fluctuations, rather than widespread doming. This is consistent with interpretations of increasingly seasonal paleoclimates in the late Middle and Late Pennsylvanian and fracture-influenced groundwater conditions. ??2005 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Special Paper of the Geological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/0-8137-2387-6.31","issn":"00721077","usgsCitation":"Greb, S., Eble, C., and Hower, J., 2005, Subtle structural influences on coal thickness and distribution: Examples from the Lower Broas-Stockton coal (Middle Pennsylvanian), Eastern Kentucky Coal Field, USA: Special Paper of the Geological Society of America, no. 387, p. 31-50, https://doi.org/10.1130/0-8137-2387-6.31.","startPage":"31","endPage":"50","numberOfPages":"20","costCenters":[],"links":[{"id":215484,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/0-8137-2387-6.31"},{"id":243292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"387","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d9ce4b08c986b31d94d","contributors":{"authors":[{"text":"Greb, S.F.","contributorId":48294,"corporation":false,"usgs":true,"family":"Greb","given":"S.F.","email":"","affiliations":[],"preferred":false,"id":449520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eble, C.F.","contributorId":35346,"corporation":false,"usgs":true,"family":"Eble","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":449519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hower, J.C.","contributorId":100541,"corporation":false,"usgs":true,"family":"Hower","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":449521,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027980,"text":"70027980 - 2005 - Hazard map calculations using grid computing","interactions":[],"lastModifiedDate":"2022-06-03T15:18:21.711676","indexId":"70027980","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Hazard map calculations using grid computing","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.76.5.565","usgsCitation":"Field, E.H., Gupta, V., Gupta, N., Maechling, P., and Jordan, T., 2005, Hazard map calculations using grid computing: Seismological Research Letters, v. 76, no. 5, p. 565-573, https://doi.org/10.1785/gssrl.76.5.565.","productDescription":"9 p.","startPage":"565","endPage":"573","numberOfPages":"9","costCenters":[],"links":[{"id":236974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2fc6e4b0c8380cd5d08c","contributors":{"authors":[{"text":"Field, E. H.","contributorId":86915,"corporation":false,"usgs":true,"family":"Field","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":416017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gupta, V.","contributorId":10959,"corporation":false,"usgs":false,"family":"Gupta","given":"V.","email":"","affiliations":[],"preferred":false,"id":416014,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gupta, N.","contributorId":12252,"corporation":false,"usgs":false,"family":"Gupta","given":"N.","email":"","affiliations":[],"preferred":false,"id":416015,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maechling, P.","contributorId":102666,"corporation":false,"usgs":false,"family":"Maechling","given":"P.","email":"","affiliations":[],"preferred":false,"id":416018,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jordan, T.H.","contributorId":83320,"corporation":false,"usgs":true,"family":"Jordan","given":"T.H.","affiliations":[],"preferred":false,"id":416016,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029444,"text":"70029444 - 2005 - Preliminary analysis of strong-motion recordings from the 28 September 2004 Parkfield, California earthquake","interactions":[],"lastModifiedDate":"2022-06-02T15:52:27.687945","indexId":"70029444","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary analysis of strong-motion recordings from the 28 September 2004 Parkfield, California earthquake","docAbstract":"<div id=\"12240558\" class=\"article-section-wrapper js-article-section js-content-section  \"><p>The 2004<span>&nbsp;</span><i>M<sub>w</sub></i><span>&nbsp;</span>6.0 Parkfield earthquake of 28 September 2004 occurred on the San Andreas Fault near the small town of Parkfield in central California. As a result of a widely accepted likelihood of an earthquake in the area, a large number of strong-motion stations and other types of seismic stations had been deployed in the area.</p></div><div id=\"12240559\" class=\"article-section-wrapper js-article-section js-content-section  \"><p>The Parkfield earthquake occurred along the same segment of the San Andreas Fault that ruptured during the 1966 Parkfield earthquake, resulting in a unique set of strong-motion measurements by arrays designed specifically for the purpose of recording an event along this fault segment. The most extensive and dense set of near-fault strong-motion recordings yet obtained for any earthquake in California was obtained in this event. This paper provides a detailed description of the arrays and the resultant strong-motion measurements of the mainshock, as well as preliminary observations. We also invite interested parties to participate in the Turkey Flat blind prediction experiment, described later in the paper. More general preliminary seismological results for this earthquake can be found in Langbein<span>&nbsp;</span><i>et al.</i><span>&nbsp;</span>(<a class=\"link link-ref link-reveal xref-bibr\" data-open=\"REF15\">2005</a>, this issue).</p></div>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.76.1.27","usgsCitation":"Shakal, A., Graizer, V., Huang, M., Borcherdt, R., Haddadi, H., Lin, K., Stephens, C.D., and Roffers, P., 2005, Preliminary analysis of strong-motion recordings from the 28 September 2004 Parkfield, California earthquake: Seismological Research Letters, v. 76, no. 1, p. 27-39, https://doi.org/10.1785/gssrl.76.1.27.","productDescription":"13 p.","startPage":"27","endPage":"39","numberOfPages":"13","costCenters":[],"links":[{"id":237486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Parkfield","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.728759765625,\n              35.22767235493586\n            ],\n            [\n              -119.3719482421875,\n              35.22767235493586\n            ],\n            [\n              -119.3719482421875,\n              36.914764288955936\n            ],\n            [\n              -120.728759765625,\n              36.914764288955936\n            ],\n            [\n              -120.728759765625,\n              35.22767235493586\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a82cde4b0c8380cd7bc58","contributors":{"authors":[{"text":"Shakal, Anthony","contributorId":198760,"corporation":false,"usgs":false,"family":"Shakal","given":"Anthony","email":"","affiliations":[],"preferred":false,"id":422769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graizer, Vladimir","contributorId":138813,"corporation":false,"usgs":false,"family":"Graizer","given":"Vladimir","affiliations":[{"id":12536,"text":"U.S. Nuclear Regulatory Commission","active":true,"usgs":false}],"preferred":false,"id":422775,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huang, Moh","contributorId":146970,"corporation":false,"usgs":false,"family":"Huang","given":"Moh","email":"","affiliations":[],"preferred":false,"id":422773,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Borcherdt, Rodger D. 0000-0002-8668-0849","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":96151,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Rodger D.","affiliations":[],"preferred":false,"id":422774,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haddadi, Hamid","contributorId":39891,"corporation":false,"usgs":true,"family":"Haddadi","given":"Hamid","email":"","affiliations":[],"preferred":false,"id":422768,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lin, Kuo-Wan klin@usgs.gov","contributorId":152049,"corporation":false,"usgs":true,"family":"Lin","given":"Kuo-Wan","email":"klin@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":422771,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stephens, Christopher D. 0000-0003-0858-3709 cdstephens@usgs.gov","orcid":"https://orcid.org/0000-0003-0858-3709","contributorId":2788,"corporation":false,"usgs":true,"family":"Stephens","given":"Christopher","email":"cdstephens@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":422770,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Roffers, P.","contributorId":66471,"corporation":false,"usgs":true,"family":"Roffers","given":"P.","email":"","affiliations":[],"preferred":false,"id":422772,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":1003625,"text":"1003625 - 2005 - NPLichen: a database of lichens in the U.S. national parks","interactions":[],"lastModifiedDate":"2015-05-04T13:42:20","indexId":"1003625","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1597,"text":"Evansia","active":true,"publicationSubtype":{"id":10}},"title":"NPLichen: a database of lichens in the U.S. national parks","docAbstract":"<p>NPLichen, a database of lichens in the U. S. National Parks (Wetmore and Bennett, 1992), has been extensively revised and expanded, and is now available for public use at www.ies.wisc.edu/nplichen. As of this writing, the database contains 25,995 records of lichens in 144 national park units. The number of records of lichens not in the North American lichen checklist (Esslinger 1997) is 161, for a total of 26,156. These records include multiple occurrences of a species in some parks because more than one reference has reported presence of species. Consequently, the number of species in parks records (including new to North America) without these duplicate references is 14,986. 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With the use of methods developed in laboratory challenge trials (Samuel et al., 2003a) and a serotype-specific polymerase chain reaction method for identification of P. multocida serotype 1, we found that a small proportion of 322 wild birds (&lt;5%) were carriers of pathogenic P. multocida. On the basis of serology, an additional group of these birds (&lt;10%) were survivors of recent avian cholera infection. Our results confirm the hypothesis that wild waterfowl are carriers of avian cholera and add support for the hypothesis that wild birds are a reservoir for this disease. In concert with other research, this work indicates that enzootic infection with avian cholera occurs in lesser snow goose (Chen caerulescens caerulescens) populations throughout their annual cycle. Although fewer Rossa??s geese (Chen rossii) were sampled, we also found these birds were carriers of P. multocida. Even in the absence of disease outbreaks, serologic evidence indicates that chronic disease transmission and recent infection are apparently occurring year-round in these highly gregarious birds and that a small portion of these populations are potential carriers with active infection.</p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-41.1.48","usgsCitation":"Samuel, M., Shadduck, D., Goldberg, D., and Johnson, W., 2005, Avian cholera in waterfowl: the role of lesser snow and Ross's geese as carriers of avian cholera in the Playa Lakes region: Journal of Wildlife Diseases, v. 41, no. 1, p. 48-57, https://doi.org/10.7589/0090-3558-41.1.48.","productDescription":"10 p.","startPage":"48","endPage":"57","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health 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