{"pageNumber":"2762","pageRowStart":"69025","pageSize":"25","recordCount":184617,"records":[{"id":70027290,"text":"70027290 - 2004 - Age estimation for shovelnose sturgeon: A cautionary note based on annulus formation in pectoral fin rays","interactions":[],"lastModifiedDate":"2012-03-12T17:20:27","indexId":"70027290","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Age estimation for shovelnose sturgeon: A cautionary note based on annulus formation in pectoral fin rays","docAbstract":"Numerous studies have examined the age and growth of shovelnose sturgeon Scaphirhynchus platorynchus, but only one study attempted to validate age estimation techniques. Therefore, our objective was to use marginal increment analysis to validate annulus formation in pectoral fin rays of shovelnose sturgeon collected from the Missouri River. We also compared the precision of age estimates between two different readers. Marginal increment distance indicated that for most of the populations an opaque band was laid down in pectoral fin rays during the summer. However, opaque bands were formed throughout the year in some individuals, which could be problematic when using fin rays for age estimation. The agreement of age estimates by two readers for shovelnose sturgeon was only 18%, and differences in ages between the two readers increased for older fish. The presence of split annuli, false annuli, spawning bands, imbedded rays, and deteriorating sections made individual growth rings difficult to separate. Our findings verified that opaque bands are formed annually during the summer in the pectoral fin rays of most shovelnose sturgeon, but some individuals form opaque bands during other times. Pectoral fin rays will probably continue to be the most practical method of age estimation in shovelnose sturgeon, but ages estimated by this method should be used with caution.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/M03-090.1","issn":"02755947","usgsCitation":"Whiteman, K., Travnichek, V., Wildhaber, M., DeLonay, A., Papoulias, D., and Tillett, D., 2004, Age estimation for shovelnose sturgeon: A cautionary note based on annulus formation in pectoral fin rays: North American Journal of Fisheries Management, v. 24, no. 2, p. 731-734, https://doi.org/10.1577/M03-090.1.","startPage":"731","endPage":"734","numberOfPages":"4","costCenters":[],"links":[{"id":209180,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/M03-090.1"},{"id":235420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationDate":"2004-05-01","publicationStatus":"PW","scienceBaseUri":"5059e8ebe4b0c8380cd47f8f","contributors":{"authors":[{"text":"Whiteman, K.W.","contributorId":41635,"corporation":false,"usgs":true,"family":"Whiteman","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":413045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Travnichek, V.H.","contributorId":104684,"corporation":false,"usgs":true,"family":"Travnichek","given":"V.H.","affiliations":[],"preferred":false,"id":413049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wildhaber, M. L. 0000-0002-6538-9083","orcid":"https://orcid.org/0000-0002-6538-9083","contributorId":62961,"corporation":false,"usgs":true,"family":"Wildhaber","given":"M. L.","affiliations":[],"preferred":false,"id":413046,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"DeLonay, A.","contributorId":103054,"corporation":false,"usgs":true,"family":"DeLonay","given":"A.","email":"","affiliations":[],"preferred":false,"id":413048,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Papoulias, D. 0000-0002-5106-2469","orcid":"https://orcid.org/0000-0002-5106-2469","contributorId":33886,"corporation":false,"usgs":true,"family":"Papoulias","given":"D.","affiliations":[],"preferred":false,"id":413044,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tillett, D.","contributorId":76918,"corporation":false,"usgs":true,"family":"Tillett","given":"D.","affiliations":[],"preferred":false,"id":413047,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70176938,"text":"70176938 - 2004 - A holistic passive integrative sampling approach for assessing the presence and potential impacts of waterborne environmental contaminants","interactions":[],"lastModifiedDate":"2016-10-13T09:52:39","indexId":"70176938","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1226,"text":"Chemosphere","active":true,"publicationSubtype":{"id":10}},"title":"A holistic passive integrative sampling approach for assessing the presence and potential impacts of waterborne environmental contaminants","docAbstract":"<p><span>As an integral part of our continuing research in environmental quality assessment approaches, we have developed a variety of passive integrative sampling devices widely applicable for use in defining the presence and potential impacts of a broad array of contaminants. The semipermeable membrane device has gained widespread use for sampling hydrophobic chemicals from water and air, the polar organic chemical integrative sampler is applicable for sequestering waterborne hydrophilic organic chemicals, the stabilized liquid membrane device is used to integratively sample waterborne ionic metals, and the passive integrative mercury sampler is applicable for sampling vapor phase or dissolved neutral mercury species. This suite of integrative samplers forms the basis for a new passive sampling approach for assessing the presence and potential toxicological significance of a broad spectrum of environmental contaminants. In a proof-of-concept study, three of our four passive integrative samplers were used to assess the presence of a wide variety of contaminants in the waters of a constructed wetland, and to determine the effectiveness of the constructed wetland in removing contaminants. The wetland is used for final polishing of secondary-treatment municipal wastewater and the effluent is used as a source of water for a state wildlife area. Numerous contaminants, including organochlorine pesticides, polycyclic aromatic hydrocarbons, organophosphate pesticides, and pharmaceutical chemicals (e.g., ibuprofen, oxindole, etc.) were detected in the wastewater. Herein we summarize the results of the analysis of the field-deployed samplers and demonstrate the utility of this holistic approach.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.chemosphere.2003.08.015","usgsCitation":"Petty, J.D., Huckins, J., Alvarez, D., Brumbaugh, W.G., Cranor, W., Gale, R., Rastall, A., Jones-Lepp, T., Leiker, T., Rostad, C.E., and Furlong, E., 2004, A holistic passive integrative sampling approach for assessing the presence and potential impacts of waterborne environmental contaminants: Chemosphere, v. 54, no. 6, p. 695-705, https://doi.org/10.1016/j.chemosphere.2003.08.015.","productDescription":"11 p.","startPage":"695","endPage":"705","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":329520,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdf00e4b0824b2d179d0e","contributors":{"authors":[{"text":"Petty, J. D.","contributorId":86722,"corporation":false,"usgs":true,"family":"Petty","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":650792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huckins, J.N.","contributorId":62553,"corporation":false,"usgs":true,"family":"Huckins","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":650793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alvarez, D.A.","contributorId":39481,"corporation":false,"usgs":true,"family":"Alvarez","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":650794,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brumbaugh, W. G.","contributorId":121189,"corporation":false,"usgs":true,"family":"Brumbaugh","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":650795,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cranor, W.L.","contributorId":98261,"corporation":false,"usgs":true,"family":"Cranor","given":"W.L.","affiliations":[],"preferred":false,"id":650796,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gale, R.W.","contributorId":81653,"corporation":false,"usgs":true,"family":"Gale","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":650797,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rastall, A.C.","contributorId":105503,"corporation":false,"usgs":true,"family":"Rastall","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":650798,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jones-Lepp, T. L.","contributorId":11806,"corporation":false,"usgs":true,"family":"Jones-Lepp","given":"T. L.","affiliations":[],"preferred":false,"id":650799,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Leiker, T.J.","contributorId":96719,"corporation":false,"usgs":true,"family":"Leiker","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":650800,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Rostad, C. E.","contributorId":120101,"corporation":false,"usgs":true,"family":"Rostad","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":650801,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Furlong, E. T. 0000-0002-7305-4603","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":98346,"corporation":false,"usgs":true,"family":"Furlong","given":"E. T.","affiliations":[],"preferred":false,"id":650802,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70027286,"text":"70027286 - 2004 - Observations and temperatures of Io's Pele Patera from Cassini and Galileo spacecraft images","interactions":[],"lastModifiedDate":"2018-11-06T12:00:15","indexId":"70027286","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Observations and temperatures of Io's Pele Patera from Cassini and Galileo spacecraft images","docAbstract":"<p><span>Pele has been the most intense high-temperature hotspot on Io to be continuously active during the Galileo monitoring from 1996–2001. A suite of characteristics suggests that Pele is an active lava lake inside a volcanic depression. In 2000–2001, Pele was observed by two spacecraft, Cassini and Galileo. The Cassini observations revealed that Pele is variable in activity over timescales of minutes, typical of active lava lakes in Hawaii and Ethiopia. These observations also revealed that the short-wavelength&nbsp;thermal emission&nbsp;from Pele decreases with rotation of Io by a factor significantly greater than the cosine of the emission angle, and that the color temperature becomes more variable and hotter at high emission angles. This behavior suggests that a significant portion of the visible thermal emission from Pele comes from lava fountains within a topographically confined lava body.&nbsp;High spatial resolution, nightside images from a Galileo flyby in October 2001 revealed a large, relatively cool (&lt;800&nbsp;K) region, ringed by bright hotspots, and a central region of high thermal emission, which is hypothesized to be due to fountaining and convection in the lava lake. Images taken through different filters revealed color temperatures of 1500±80&nbsp;K from Cassini ISS data and 1605±220 and 1420±100&nbsp;K from small portions of Galileo SSI data. Such temperatures are near the upper limit for basaltic compositions. Given the limitations of deriving lava eruption temperature in the absence of&nbsp;</span>in situ measurement<span>, it is possible that Pele has lavas with ultramafic compositions. The long-lived, vigorous activity of what is most likely an actively overturning lava lake in Pele Patera indicates that there is a strong connection to a large, stable&nbsp;magma&nbsp;source region.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.icarus.2003.10.019","issn":"00191035","usgsCitation":"Radebaugh, J., McEwen, A.S., Milazzo, M.P., Keszthelyi, L., Davies, A., Turtle, E.P., and Dawson, D.D., 2004, Observations and temperatures of Io's Pele Patera from Cassini and Galileo spacecraft images: Icarus, v. 169, no. 1, p. 65-79, https://doi.org/10.1016/j.icarus.2003.10.019.","productDescription":"15 p.","startPage":"65","endPage":"79","numberOfPages":"15","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":235345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209133,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2003.10.019"}],"volume":"169","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6a70e4b0c8380cd74177","contributors":{"authors":[{"text":"Radebaugh, Jani","contributorId":101792,"corporation":false,"usgs":true,"family":"Radebaugh","given":"Jani","email":"","affiliations":[],"preferred":false,"id":413032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McEwen, Alfred S.","contributorId":61657,"corporation":false,"usgs":false,"family":"McEwen","given":"Alfred","email":"","middleInitial":"S.","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":413030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Milazzo, Moses P. 0000-0002-9101-2191 moses@usgs.gov","orcid":"https://orcid.org/0000-0002-9101-2191","contributorId":4811,"corporation":false,"usgs":true,"family":"Milazzo","given":"Moses","email":"moses@usgs.gov","middleInitial":"P.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":413028,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keszthelyi, Laszlo P. 0000-0003-1879-4331 laz@usgs.gov","orcid":"https://orcid.org/0000-0003-1879-4331","contributorId":52802,"corporation":false,"usgs":true,"family":"Keszthelyi","given":"Laszlo P.","email":"laz@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":413029,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davies, Ashley G.","contributorId":36827,"corporation":false,"usgs":true,"family":"Davies","given":"Ashley G.","affiliations":[],"preferred":false,"id":413034,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Turtle, Elizabeth P.","contributorId":45443,"corporation":false,"usgs":false,"family":"Turtle","given":"Elizabeth","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":413033,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Dawson, Douglas D.","contributorId":210493,"corporation":false,"usgs":false,"family":"Dawson","given":"Douglas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":413031,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70026258,"text":"70026258 - 2004 - Numerical simulations of large earthquakes: Dynamic rupture propagation on heterogeneous faults","interactions":[],"lastModifiedDate":"2012-03-12T17:20:25","indexId":"70026258","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3208,"text":"Pure and Applied Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Numerical simulations of large earthquakes: Dynamic rupture propagation on heterogeneous faults","docAbstract":"Our current conceptions of earthquake rupture dynamics, especially for large earthquakes, require knowledge of the geometry of the faults involved in the rupture, the material properties of the rocks surrounding the faults, the initial state of stress on the faults, and a constitutive formulation that determines when the faults can slip. In numerical simulations each of these factors appears to play a significant role in rupture propagation, at the kilometer length scale. Observational evidence of the earth indicates that at least the first three of the elements, geometry, material, and stress, can vary over many scale dimensions. Future research on earthquake rupture dynamics needs to consider at which length scales these features are significant in affecting rupture propagation. ?? Birkha??user Verlag, Basel, 2004.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00024-004-2556-8","issn":"00334553","usgsCitation":"Harris, R., 2004, Numerical simulations of large earthquakes: Dynamic rupture propagation on heterogeneous faults: Pure and Applied Geophysics, v. 161, no. 11-12, p. 2171-2181, https://doi.org/10.1007/s00024-004-2556-8.","startPage":"2171","endPage":"2181","numberOfPages":"11","costCenters":[],"links":[{"id":208467,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00024-004-2556-8"},{"id":234221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"161","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6930e4b0c8380cd73bee","contributors":{"authors":[{"text":"Harris, R.A. 0000-0002-9247-0768","orcid":"https://orcid.org/0000-0002-9247-0768","contributorId":41849,"corporation":false,"usgs":true,"family":"Harris","given":"R.A.","affiliations":[],"preferred":false,"id":408758,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70026229,"text":"70026229 - 2004 - Simulation of ventilation efficiency, and pre-closure temperatures in emplacement drifts at Yucca Mountain, Nevada, using Monte Carlo and composite thermal-pulse methods","interactions":[],"lastModifiedDate":"2018-06-07T16:53:44","indexId":"70026229","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Simulation of ventilation efficiency, and pre-closure temperatures in emplacement drifts at Yucca Mountain, Nevada, using Monte Carlo and composite thermal-pulse methods","docAbstract":"Predictions of waste canister and repository driftwall temperatures as functions of space and time are important to evaluate pre-closure performance of the proposed repository for spent nuclear fuel and high-level radioactive waste at Yucca Mountain, Nevada. Variations in the lithostratigraphic features in densely welded and crystallized rocks of the 12.8-million-year-old Topopah Spring Tuff, especially the porosity resulting from lithophysal cavities, affect thermal properties. A simulated emplacement drift is based on projecting lithophysal cavity porosity values 50 to 800 m from the Enhanced Characterization of the Repository Block cross drift. Lithophysal cavity porosity varies from 0.00 to 0.05 cm3/cm3 in the middle nonlithophysal zone and from 0.03 to 0.28 cm3/cm3 in the lower lithophysal zone. A ventilation model and computer program titled \"Monte Carlo Simulation of Ventilation\" (MCSIMVENT), which is based on a composite thermal-pulse calculation, simulates statistical variability and uncertainty of rock-mass thermal properties and ventilation performance along a simulated emplacement drift for a pre-closure period of 50 years. Although ventilation efficiency is relatively insensitive to thermal properties, variations in lithophysal porosity along the drift can result in a range of peak driftwall temperatures can range from 40 to 85??C for the preclosure period. Copyright ?? 2004 by ASME.","largerWorkTitle":"Proceedings of the ASME Heat Transfer/Fluids Engineering Summer Conference 2004, HT/FED 2004","conferenceTitle":"2004 ASME Heat Transfer/Fluids Engineering Summer Conference, HT/FED 2004","conferenceDate":"11 July 2004 through 15 July 2004","conferenceLocation":"Charlotte, NC","language":"English","usgsCitation":"Case, J., and Buesch, D., 2004, Simulation of ventilation efficiency, and pre-closure temperatures in emplacement drifts at Yucca Mountain, Nevada, using Monte Carlo and composite thermal-pulse methods, <i>in</i> Proceedings of the ASME Heat Transfer/Fluids Engineering Summer Conference 2004, HT/FED 2004, v. 2 B, Charlotte, NC, 11 July 2004 through 15 July 2004, p. 1109-1115.","startPage":"1109","endPage":"1115","numberOfPages":"7","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":234321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2 B","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b90b7e4b08c986b319642","contributors":{"authors":[{"text":"Case, J.B.","contributorId":107897,"corporation":false,"usgs":true,"family":"Case","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":408643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buesch, D.C. 0000-0002-4978-5027","orcid":"https://orcid.org/0000-0002-4978-5027","contributorId":73633,"corporation":false,"usgs":true,"family":"Buesch","given":"D.C.","affiliations":[],"preferred":false,"id":408642,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70182135,"text":"70182135 - 2004 - Report of the technical review panel - compatibility of Coleman National Fish Hatchery operations and restoration of anadromous salmonids in Battle Creek","interactions":[],"lastModifiedDate":"2017-02-16T14:45:10","indexId":"70182135","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Report of the technical review panel - compatibility of Coleman National Fish Hatchery operations and restoration of anadromous salmonids in Battle Creek","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"CalFed Bay-Delta Program","publisherLocation":"Sacramento, CA","usgsCitation":"Busack, C., Hankin, D., Hedrick, R., Lichatowich, J., and Reisenbichler, R., 2004, Report of the technical review panel - compatibility of Coleman National Fish Hatchery operations and restoration of anadromous salmonids in Battle Creek, 65 p. .","productDescription":"65 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335772,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a6c83be4b025c4642862da","contributors":{"authors":[{"text":"Busack, C.","contributorId":181846,"corporation":false,"usgs":false,"family":"Busack","given":"C.","email":"","affiliations":[],"preferred":false,"id":669754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hankin, D.","contributorId":46049,"corporation":false,"usgs":true,"family":"Hankin","given":"D.","email":"","affiliations":[],"preferred":false,"id":669755,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hedrick, R.P.","contributorId":76431,"corporation":false,"usgs":true,"family":"Hedrick","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":669756,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lichatowich, J.A.","contributorId":152386,"corporation":false,"usgs":false,"family":"Lichatowich","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":669757,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reisenbichler, R.","contributorId":81291,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.","email":"","affiliations":[],"preferred":false,"id":669758,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70179819,"text":"70179819 - 2004 - Three-dimensional fish tracking to evaluate the removable spillway weir at Lower Granite Dam during 2003,  Annual report 2003","interactions":[],"lastModifiedDate":"2017-01-18T14:13:43","indexId":"70179819","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Three-dimensional fish tracking to evaluate the removable spillway weir at Lower Granite Dam during 2003,  Annual report 2003","docAbstract":"<p>Abstract not available&nbsp;</p>","language":"English","publisher":"U.S. Army Corps of Engineers","usgsCitation":"Cash, K., Hatton, T., Jones, E., Magie, R., Adams, N., and Rondorf, D., 2004, Three-dimensional fish tracking to evaluate the removable spillway weir at Lower Granite Dam during 2003,  Annual report 2003, 102 p. .","productDescription":"102 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333365,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58808d73e4b01dfadfff1565","contributors":{"authors":[{"text":"Cash, K.M","contributorId":178009,"corporation":false,"usgs":false,"family":"Cash","given":"K.M","email":"","affiliations":[],"preferred":false,"id":658821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatton, T.W","contributorId":178014,"corporation":false,"usgs":false,"family":"Hatton","given":"T.W","email":"","affiliations":[],"preferred":false,"id":658822,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, E.C.","contributorId":177747,"corporation":false,"usgs":false,"family":"Jones","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":658823,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Magie, R.J.","contributorId":6676,"corporation":false,"usgs":true,"family":"Magie","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":658824,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Adams, N.S.","contributorId":178351,"corporation":false,"usgs":false,"family":"Adams","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":658825,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rondorf, D.W.","contributorId":80789,"corporation":false,"usgs":true,"family":"Rondorf","given":"D.W.","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":658826,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70026261,"text":"70026261 - 2004 - Preventing, controlling, and managing alien species introduction for the health of aquatic and marine ecosystems","interactions":[],"lastModifiedDate":"2012-03-12T17:20:25","indexId":"70026261","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Preventing, controlling, and managing alien species introduction for the health of aquatic and marine ecosystems","docAbstract":"The introduction and spread of invasive species is an emerging global problem. As economic and ecological impacts continue to grow, there will be an increasing need to develop innovative solutions and global partnerships to combat the increasing rate of invasions and their accompanying impacts. Threats to sustainable fisheries in North America associated with alien species come from many global directions and sources and can be deliberate or the unintended consequence of other actions. Decisions about the role of sustainable fisheries in protecting and restoring the health of aquatic ecosystems become even more complex when economic and social factors are considered along with environmental impacts, because many intentionally introduced species also have associated economic and community costs and benefits. Actions designed to prevent or control alien species in an aquatic ecosystem are often complicated by these nonenvironmental factors as well as public perception and opinion. Aquatic ecosystems are disturbed to varying degrees by alien species, including disease organisms. Prevention is the first and best line of defense. Determining likely pathways and effective countermeasures is more cost-effective than either eradication or control. Our ability to quickly identify new species and their associated risk to ecosystems is critical in designing and implementing effective control and management actions. Lack of infrastructure and necessary resources, clear-cut authority for regulation and action, and scientific information about the biology of alien species and effective control techniques are often limiting factors that prevent the needed action to protect aquatic ecosystems.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fisheries Society Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08922284","usgsCitation":"Short, C., Gross, S., and Wilkinson, D., 2004, Preventing, controlling, and managing alien species introduction for the health of aquatic and marine ecosystems: American Fisheries Society Symposium, v. 2004, no. 43, p. 109-125.","startPage":"109","endPage":"125","numberOfPages":"17","costCenters":[],"links":[{"id":234256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2004","issue":"43","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8b76e4b0c8380cd7e265","contributors":{"authors":[{"text":"Short, C.I.","contributorId":15801,"corporation":false,"usgs":true,"family":"Short","given":"C.I.","email":"","affiliations":[],"preferred":false,"id":408771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gross, S.K.","contributorId":50329,"corporation":false,"usgs":true,"family":"Gross","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":408772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilkinson, D.","contributorId":56424,"corporation":false,"usgs":true,"family":"Wilkinson","given":"D.","email":"","affiliations":[],"preferred":false,"id":408773,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70026263,"text":"70026263 - 2004 - Dynamic rupture modeling of the transition from thrust to strike-slip motion in the 2002 Denali fault earthquake, Alaska","interactions":[],"lastModifiedDate":"2021-07-20T11:32:47.048018","indexId":"70026263","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","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":"Dynamic rupture modeling of the transition from thrust to strike-slip motion in the 2002 Denali fault earthquake, Alaska","docAbstract":"We use three-dimensional dynamic (spontaneous) rupture models to investigate the nearly simultaneous ruptures of the Susitna Glacier thrust fault and the Denali strike-slip fault. With the 1957 Mw 8.3 Gobi-Altay, Mongolia, earthquake as the only other well-documented case of significant, nearly simultaneous rupture of both thrust and strike-slip faults, this feature of the 2002 Denali fault earthquake provides a unique opportunity to investigate the mechanisms responsible for development of these large, complex events. We find that the geometry of the faults and the orientation of the regional stress field caused slip on the Susitna Glacier fault to load the Denali fault. Several different stress orientations with oblique right-lateral motion on the Susitna Glacier fault replicate the triggering of rupture on the Denali fault about 10 sec after the rupture nucleates on the Susitna Glacier fault. However, generating slip directions compatible with measured surface offsets and kinematic source inversions requires perturbing the stress orientation from that determined with focal mechanisms of regional events. Adjusting the vertical component of the principal stress tensor for the regional stress field so that it is more consistent with a mixture of strike-slip and reverse faulting significantly improves the fit of the slip-rake angles to the data. Rotating the maximum horizontal compressive stress direction westward appears to improve the fit even further.","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120040614","usgsCitation":"Aagaard, B.T., Anderson, G., and Hudnut, K., 2004, Dynamic rupture modeling of the transition from thrust to strike-slip motion in the 2002 Denali fault earthquake, Alaska: Bulletin of the Seismological Society of America, v. 94, no. 6B, p. 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Brad T. 0000-0002-8795-9833 baagaard@usgs.gov","orcid":"https://orcid.org/0000-0002-8795-9833","contributorId":192869,"corporation":false,"usgs":true,"family":"Aagaard","given":"Brad","email":"baagaard@usgs.gov","middleInitial":"T.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":408779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, G.","contributorId":26490,"corporation":false,"usgs":true,"family":"Anderson","given":"G.","affiliations":[],"preferred":false,"id":408780,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hudnut, K.W.","contributorId":25179,"corporation":false,"usgs":true,"family":"Hudnut","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":408778,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70182132,"text":"70182132 - 2004 -  Effects of Ichthyophonus on survival and reproductive success of Yukon River Chinook salmon. Final report for study 01-200","interactions":[],"lastModifiedDate":"2017-02-16T14:41:23","indexId":"70182132","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":" Effects of Ichthyophonus on survival and reproductive success of Yukon River Chinook salmon. Final report for study 01-200","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Kocan, R., Hershberger, P., and Winton, J., 2004,  Effects of Ichthyophonus on survival and reproductive success of Yukon River Chinook salmon. Final report for study 01-200, 57 p. .","productDescription":"57 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335768,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a6c83be4b025c4642862dc","contributors":{"authors":[{"text":"Kocan, R.","contributorId":95665,"corporation":false,"usgs":true,"family":"Kocan","given":"R.","affiliations":[],"preferred":false,"id":669737,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hershberger, P.","contributorId":64826,"corporation":false,"usgs":true,"family":"Hershberger","given":"P.","email":"","affiliations":[],"preferred":false,"id":669738,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winton, J.","contributorId":55627,"corporation":false,"usgs":true,"family":"Winton","given":"J.","email":"","affiliations":[],"preferred":false,"id":669739,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70026296,"text":"70026296 - 2004 - Comparison of geodetic and glaciological mass-balance techniques, Gulkana Glacier, Alaska, U.S.A","interactions":[],"lastModifiedDate":"2021-09-09T15:51:40.519526","indexId":"70026296","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2328,"text":"Journal of Glaciology","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of geodetic and glaciological mass-balance techniques, Gulkana Glacier, Alaska, U.S.A","docAbstract":"<p><span>The net mass balance on Gulkana Glacier, Alaska, U.S.A., has been measured since 1966 by the glaciological method, in which seasonal balances are measured at three index sites and extrapolated over large areas of the glacier. Systematic errors can accumulate linearly with time in this method. Therefore, the geodetic balance, in which errors are less time-dependent, was calculated for comparison with the glaciological method. Digital elevation models of the glacier in 1974, 1993 and 1999 were prepared using aerial photographs, and geodetic balances were computed, giving – 6.0 ± 0.7 m w.e. from 1974 to 1993 and -11.8 ± 0.7 m w.e. from 1974 to 1999. These balances are compared with the glaciological balances over the same intervals, which were – 5.8 ± 0.9 and -11.2 ± 1.0 m w.e. respectively; both balances show that the thinning rate tripled in the 1990s. These cumulative balances differ by &lt;6%. For this close agreement, the glaciologically measured mass balance of Gulkana Glacier must be largely free of systematic errors and be based on a time-variable area-altitude distribution, and the photography used in the geodetic method must have enough contrast to enable accurate photogrammetry.</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.3189/172756504781829855","usgsCitation":"Cox, L., and March, R., 2004, Comparison of geodetic and glaciological mass-balance techniques, Gulkana Glacier, Alaska, U.S.A: Journal of Glaciology, v. 50, no. 170, p. 363-370, https://doi.org/10.3189/172756504781829855.","productDescription":"8 p.","startPage":"363","endPage":"370","costCenters":[],"links":[{"id":478257,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3189/172756504781829855","text":"Publisher Index Page"},{"id":234223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulkana Glacier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -145.59391021728516,\n              63.281827557877136\n            ],\n            [\n              -145.59459686279297,\n              63.265924227825494\n            ],\n            [\n              -145.47683715820312,\n              63.26654199650337\n            ],\n            [\n              -145.47683715820312,\n              63.296950744530605\n            ],\n            [\n              -145.59425354003906,\n              63.299110552224185\n            ],\n            [\n              -145.59391021728516,\n              63.281827557877136\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"50","issue":"170","noUsgsAuthors":false,"publicationDate":"2017-09-08","publicationStatus":"PW","scienceBaseUri":"5059f866e4b0c8380cd4d095","contributors":{"authors":[{"text":"Cox, L.H.","contributorId":61609,"corporation":false,"usgs":true,"family":"Cox","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":408908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"March, R.S.","contributorId":16431,"corporation":false,"usgs":true,"family":"March","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":408907,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70184533,"text":"70184533 - 2004 - The microbial arsenic cycle in Mono Lake, California","interactions":[],"lastModifiedDate":"2019-12-16T20:15:25","indexId":"70184533","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1619,"text":"FEMS Microbiology Ecology","onlineIssn":"1574-6941","printIssn":"0168-6496","active":true,"publicationSubtype":{"id":10}},"title":"The microbial arsenic cycle in Mono Lake, California","docAbstract":"<p><span>Significant concentrations of dissolved inorganic arsenic can be found in the waters of a number of lakes located in the western USA and in other water bodies around the world. These lakes are often situated in arid, volcanic terrain. The highest concentrations of arsenic occur in hypersaline, closed basin soda lakes and their remnant brines. Although arsenic is a well-known toxicant to eukaryotes and prokaryotes alike, some prokaryotes have evolved biochemical mechanisms to exploit arsenic oxyanions (i.e., arsenate and arsenite); they can use them either as an electron acceptor for anaerobic respiration (arsenate), or as an electron donor (arsenite) to support chemoautotrophic fixation of CO</span><sub>2</sub><span> into cell carbon. Unlike in freshwater or marine ecosystems, these processes may assume quantitative significance with respect to the carbon cycle in arsenic-rich soda lakes. For the past several years our research has focused on the occurrence and biogeochemical manifestations of these processes in Mono Lake, a particularly arsenic-rich environment. Herein we review some of our findings concerning the biogeochemical arsenic cycle in this lake, with the hope that it may broaden the understanding of the influence of microorganisms upon the speciation of arsenic in more common, less “extreme” environments, such as drinking water aquifers.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.femsec.2003.12.016","usgsCitation":"Oremland, R.S., Stolz, J.F., and Hollibaugh, J., 2004, The microbial arsenic cycle in Mono Lake, California: FEMS Microbiology Ecology, v. 48, no. 1, p. 15-27, https://doi.org/10.1016/j.femsec.2003.12.016.","productDescription":"13 p. ","startPage":"15","endPage":"27","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":488585,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.femsec.2003.12.016","text":"Publisher Index Page"},{"id":337325,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mono Lake ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.14535522460938,\n              37.95286091815649\n            ],\n            [\n              -119.01763916015625,\n              37.931200459333716\n            ],\n            [\n              -118.91601562499999,\n              37.94636345087475\n            ],\n            [\n              -118.89404296875,\n              38.06322991452768\n            ],\n            [\n              -119.01351928710938,\n              38.09133660751176\n            ],\n            [\n              -119.15634155273438,\n              38.04484662140698\n            ],\n            [\n              -119.14535522460938,\n              37.95286091815649\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"48","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c3c944e4b0f37a93ee9b4b","contributors":{"authors":[{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":681892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stolz, John F.","contributorId":179305,"corporation":false,"usgs":false,"family":"Stolz","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":681893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hollibaugh, James T.","contributorId":6878,"corporation":false,"usgs":true,"family":"Hollibaugh","given":"James T.","affiliations":[],"preferred":false,"id":681894,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70026297,"text":"70026297 - 2004 - Geophysical data reveal the crustal structure of the Alaska Range orogen within the aftershock zone of the Mw 7.9 Denali fault earthquake","interactions":[],"lastModifiedDate":"2021-07-15T10:00:50.959113","indexId":"70026297","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","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":"Geophysical data reveal the crustal structure of the Alaska Range orogen within the aftershock zone of the Mw 7.9 Denali fault earthquake","docAbstract":"<p>Geophysical information, including deep-crustal seismic reflection, magnetotelluric (MT), gravity, and magnetic data, cross the aftershock zone of the 3 November 2002 Mw 7.9 Denali fault earthquake. These data and aftershock seismicity, jointly interpreted, reveal the crustal structure of the right-lateral-slip Denali fault and the eastern Alaska Range orogen, as well as the relationship between this structure and seismicity. North of the Denali fault, strong seismic reflections from within the Alaska Range orogen show features that dip as steeply as <span>25°</span> north and extend downward to depths between 20 and 25 km. These reflections reveal crustal structures, probably ductile shear zones, that most likely formed during the Late Cretaceous, but these structures appear to be inactive, having produced little seismicity during the past 20 years. Furthermore, seismic reflections mainly dip north, whereas alignments in aftershock hypocenters dip south. The Denali fault is nonreflective, but modeling of MT, gravity, and magnetic data suggests that the Denali fault dips steeply to vertically. However, in an alternative structural model, the Denali fault is defined by one of the reflection bands that dips to the north and flattens into the middle crust of the Alaska Range orogen. Modeling of MT data indicates a rock body, having low electrical resistivity (&gt;10 ??-m), that lies mainly at depths greater than 10 km, directly beneath aftershocks of the Denali fault earthquake. The maximum depth of aftershocks along the Denali fault is 10 km. This shallow depth may arise from a higher-than-normal geothermal gradient. Alternatively, the low electrical resistivity of deep rocks along the Denali fault may be associated with fluids that have weakened the lower crust and helped determine the depth extent of the after-shock zone.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120040613","usgsCitation":"Fisher, M.A., Ratchkovski, N.A., Nokleberg, W., Pellerin, L., and Glen, J., 2004, Geophysical data reveal the crustal structure of the Alaska Range orogen within the aftershock zone of the Mw 7.9 Denali fault earthquake: Bulletin of the Seismological Society of America, v. 94, no. 6B, p. 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,{"id":70179774,"text":"70179774 - 2004 - Information on habitat use of larval Ash Meadows speckled dace","interactions":[],"lastModifiedDate":"2017-01-17T15:18:19","indexId":"70179774","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Information on habitat use of larval Ash Meadows speckled dace","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Las Vegas, NV","usgsCitation":"McShane, R., Swaim, K., and Scoppettone, G., 2004, Information on habitat use of larval Ash Meadows speckled dace, 7 p. .","productDescription":"7 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333269,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"587f3ddde4b0d96de2564584","contributors":{"authors":[{"text":"McShane, R.R","contributorId":178376,"corporation":false,"usgs":false,"family":"McShane","given":"R.R","email":"","affiliations":[],"preferred":false,"id":658644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swaim, K.M.","contributorId":178377,"corporation":false,"usgs":false,"family":"Swaim","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":658645,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scoppettone, G.G.","contributorId":22793,"corporation":false,"usgs":true,"family":"Scoppettone","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":658646,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70026230,"text":"70026230 - 2004 - Preparation and certification of Re-Os dating reference materials: Molybdenites HLP and JDC","interactions":[],"lastModifiedDate":"2021-12-01T16:03:51.927593","indexId":"70026230","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1822,"text":"Geostandards and Geoanalytical Research","active":true,"publicationSubtype":{"id":10}},"title":"Preparation and certification of Re-Os dating reference materials: Molybdenites HLP and JDC","docAbstract":"<p><span>Two Re-Os dating reference material molybdenites were prepared. Molybdenite JDC and molybdenite HLP are from a carbonate vein-type molybdenum-(lead)-uranium deposit in the Jinduicheng-Huanglongpu area of Shaanxi province, China. The samples proved to be homogeneous, based on the coefficient of variation of analytical results and an analysis of variance test. The sampling weight was 0.1 g for JDC and 0.025 g for HLP. An isotope dilution method was used for the determination of Re and Os. Sample decomposition and pre-concentration of Re and Os prior to measurement were accomplished using a variety of methods: acid digestion, alkali fusion, ion exchange and solvent extraction. Negative thermal ionisation mass spectrometry and inductively coupled plasma-mass spectrometry were used for the determination of Re and&nbsp;</span><sup>187</sup><span>Os concentration and isotope ratios. The certified values include the contents of Re and Os and the model ages. For HLP, the Re content was 283.8 ± 6.2 μg g</span><sup>−1</sup><span>,&nbsp;</span><sup>187</sup><span>Os was 659 ± 14 ng g</span><sup>−1</sup><span>&nbsp;and the Re-Os model age was 221.4 ± 5.6 Ma. For JDC, the Re content was 17.39 ± 0.32 μg g</span><sup>−1</sup><span>,&nbsp;</span><sup>187</sup><span>Os was 25.46 ± 0.60 ng g</span><sup>−1</sup><span>&nbsp;and the Re-Os model age was 139.6 ± 3.8 Ma. Uncertainties for both certified reference materials are stated at the 95% level of confidence. Three laboratories (from three countries: PR. China, USA, Sweden) joined in the certification programme. These certified reference materials are primarily useful for Re-Os dating of molybdenite, sulfides, black shale, etc.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1751-908X.2004.tb01042.x","usgsCitation":"Du, A., Wu, S., Sun, D., Wang, S., Qu, W., Markey, R., Stain, H., Morgan, J., and Malinovskiy, D., 2004, Preparation and certification of Re-Os dating reference materials: Molybdenites HLP and JDC: Geostandards and Geoanalytical Research, v. 28, no. 1, p. 41-52, https://doi.org/10.1111/j.1751-908X.2004.tb01042.x.","productDescription":"12 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,{"id":70182143,"text":"70182143 - 2004 - Xenobiotic impact on Arctic char:  Nutritional modulation and physiological consequences","interactions":[],"lastModifiedDate":"2017-02-16T15:00:30","indexId":"70182143","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Xenobiotic impact on Arctic char:  Nutritional modulation and physiological consequences","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"National Science Foundation","usgsCitation":"Maule, A., 2004, Xenobiotic impact on Arctic char:  Nutritional modulation and physiological consequences.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335780,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a6c83be4b025c4642862d2","contributors":{"authors":[{"text":"Maule, A.G.","contributorId":45067,"corporation":false,"usgs":true,"family":"Maule","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":669778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":70182137,"text":"70182137 - 2004 - Status of Ash Meadows speckled dace in Bradford Springs","interactions":[],"lastModifiedDate":"2017-02-16T14:50:08","indexId":"70182137","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Status of Ash Meadows speckled dace in Bradford Springs","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":" U.S. Fish and Wildlife Service","publisherLocation":"Las Vegas, NV","usgsCitation":"Leavy, T., McShane, R., Swaim, K., and Scoppettone, G., 2004, Status of Ash Meadows speckled dace in Bradford Springs, 12 p. .","productDescription":"12 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335774,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a6c83be4b025c4642862d8","contributors":{"authors":[{"text":"Leavy, T.","contributorId":181847,"corporation":false,"usgs":false,"family":"Leavy","given":"T.","email":"","affiliations":[],"preferred":false,"id":669763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McShane, R.R","contributorId":178376,"corporation":false,"usgs":false,"family":"McShane","given":"R.R","email":"","affiliations":[],"preferred":false,"id":669764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swaim, K.M.","contributorId":178377,"corporation":false,"usgs":false,"family":"Swaim","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":669765,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scoppettone, G.G.","contributorId":22793,"corporation":false,"usgs":true,"family":"Scoppettone","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":669766,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1001067,"text":"1001067 - 2004 - Discrimination among spawning aggregations of lake herring from Lake Superior using whole-body morphometric characters","interactions":[],"lastModifiedDate":"2016-05-18T15:41:29","indexId":"1001067","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Discrimination among spawning aggregations of lake herring from Lake Superior using whole-body morphometric characters","docAbstract":"<p><span>The lake herring (</span><i>Coregonus artedi</i><span>) was one of the most commercially and ecologically valuable Lake Superior fishes, but declined in the second half of the 20th century as the result of overharvest of putatively discrete stocks. No tools were previously available that described lake herring stock structure and accurately classified lake herring to their spawning stocks. The accuracy of discriminating among spawning aggregations was evaluated using whole-body morphometrics based on a truss network. Lake herring were collected from 11 spawning aggregations in Lake Superior and two inland Wisconsin lakes to evaluate morphometrics as a stock discrimination tool. Discriminant function analysis correctly classified 53% of all fish from all spawning aggregations, and fish from all but one aggregation were classified at greater rates than were possible by chance. Discriminant analysis also correctly classified 66% of fish to nearest neighbor groups, which were groups that accounted for the possibility of mixing among the aggregations. Stepwise discriminant analysis showed that posterior body length and depth measurements were among the best discriminators of spawning aggregations. These findings support other evidence that discrete stocks of lake herring exist in Lake Superior, and fishery managers should consider all but one of the spawning aggregations as discrete stocks. Abundance, annual harvest, total annual mortality rate, and exploitation data should be collected from each stock, and surplus production of each stock should be estimated. Prudent management of stock surplus production and exploitation rates will aid in restoration of stocks and will prevent a repeat of the stock collapses that occurred in the middle of the 20th century, when the species was nearly extirpated from the lake.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(04)70399-8","usgsCitation":"Hoff, M.H., 2004, Discrimination among spawning aggregations of lake herring from Lake Superior using whole-body morphometric characters: Journal of Great Lakes Research, v. 30, no. Supplement 1, p. 385-394, https://doi.org/10.1016/S0380-1330(04)70399-8.","productDescription":"10 p.","startPage":"385","endPage":"394","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"Supplement 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64abaf","contributors":{"authors":[{"text":"Hoff, Michael H.","contributorId":23878,"corporation":false,"usgs":true,"family":"Hoff","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":310378,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000880,"text":"1000880 - 2004 - A Holocene history of dune-mediated landscape change along the southeastern shore of Lake Superior","interactions":[],"lastModifiedDate":"2013-01-22T15:45:29","indexId":"1000880","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"A Holocene history of dune-mediated landscape change along the southeastern shore of Lake Superior","docAbstract":"Causal links that connect Holocene high stands of Lake Superior with dune building, stream damming and diversion and reservoir impoundment and infilling are inferred from a multidisciplinary investigation of a small watershed along the SE shore of Lake Superior. Radiocarbon ages of wood fragments from in-place stumps and soil O horizons, recovered from the bottom of 300-ha Grand Sable Lake, suggest that the near-shore inland lake was formed during multiple episodes of late Holocene dune damming of ancestral Sable Creek. Forest drownings at ~3000, 1530, and 300 cal. years BP are highly correlated with local soil burial events that occurred during high stands of Lake Superior. During these and earlier events, Sable Creek was diverted onto eastward-graded late Pleistocene meltwater terraces. Ground penetrating radar (GPR) reveals the early Holocene valley of Sable Creek (now filled) and its constituent sedimentary structures. Near-planar paleosols, identified with GPR, suggest two repeating modes of landscape evolution mediated by levels of Lake Superior. High lake stands drove stream damming, reservoir impoundment, and eolian infilling of impoundments. Falling Lake Superior levels brought decreased sand supply to dune dams and lowered stream base level. These latter factors promoted stream piracy, breaching of dune dams, and aerial exposure and forestation of infilled lakebeds. The bathymetry of Grand Sable Lake suggests that its shoreline configuration and depth varied in response to events of dune damming and subsequent dam breaching. The interrelated late Holocene events apparent in this study area suggest that variations in lake level have imposed complex hydrologic and geomorphic signatures on upper Great Lakes coasts.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.geomorph.2004.01.005","usgsCitation":"Loope, W.L., Fisher, T.G., Jol, H.M., Anderton, J.B., and Blewett, W.L., 2004, A Holocene history of dune-mediated landscape change along the southeastern shore of Lake Superior: Geomorphology, v. 61, no. 3-4, p. 303-322, https://doi.org/10.1016/j.geomorph.2004.01.005.","productDescription":"p. 303-322","startPage":"303","endPage":"322","numberOfPages":"19","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266265,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geomorph.2004.01.005"}],"volume":"61","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b4100","contributors":{"authors":[{"text":"Loope, Walter L. wloope@usgs.gov","contributorId":4616,"corporation":false,"usgs":true,"family":"Loope","given":"Walter","email":"wloope@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":309719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, Timothy G.","contributorId":45659,"corporation":false,"usgs":true,"family":"Fisher","given":"Timothy","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":309722,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jol, Harry M.","contributorId":11571,"corporation":false,"usgs":true,"family":"Jol","given":"Harry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":309720,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Anderton, John B.","contributorId":23880,"corporation":false,"usgs":true,"family":"Anderton","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":309721,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Blewett, William L.","contributorId":57031,"corporation":false,"usgs":true,"family":"Blewett","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":309723,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1001060,"text":"1001060 - 2004 - Late Holocene lake-level variation in southeastern Lake Superior: Tahquamenon Bay, Michigan","interactions":[],"lastModifiedDate":"2021-09-13T12:16:19.394776","indexId":"1001060","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Late Holocene lake-level variation in southeastern Lake Superior: Tahquamenon Bay, Michigan","docAbstract":"<p><span>Internal architecture and ages of 71 beach ridges in the Tahquamenon Bay embayment along the southeastern shore of Lake Superior on the Upper Peninsula of Michigan were studied to generate a late Holocene relative lake-level curve. Establishing a long-term framework is important to examine the context of historic events and help predict potential future changes critical for effective water resource management. Ridges in the embayment formed between about 4,200 and 2,100 calendar years before 1950 (cal. yrs. B.P.) and were created and preserved every 28 ± 4.8 years on average. Groups of three to six beach ridges coupled with inflections in the lake-level curve indicate a history of lake levels fluctuations and outlet changes. A rapid lake-level drop (approximately 4 m) from about 4,100 to 3,800 cal. yrs. B.P. was associated with a fall from the Nipissing II high-water-level phase. A change from a gradual fall to a slight rise was associated with an outlet change from Port Huron, Michigan/Sarnia, Ontario to Sault Ste. Marie, Michigan/Ontario. A complete outlet change occurred after the Algoma high-water-level phase (ca. 2,400 cal. yrs. B.P.). Preliminary rates of vertical ground movement calculated from the strandplain are much greater than rates calculated from historical and geologic data. High rates of vertical ground movement could have caused tectonism in the Whitefish Bay area, modifying the strandplain during the past 2,400 years. A tectonic event at or near the Sault outlet also may have been a factor in the outlet change from Port Huron/Sarnia to Sault Ste. Marie.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(04)70374-3","usgsCitation":"Johnston, J.W., Baedke, S.J., Booth, R.K., Thompson, T.A., and Wilcox, D.A., 2004, Late Holocene lake-level variation in southeastern Lake Superior: Tahquamenon Bay, Michigan: Journal of Great Lakes Research, v. 30, p. 1-19, https://doi.org/10.1016/S0380-1330(04)70374-3.","productDescription":"20 p.","startPage":"1","endPage":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":478252,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/20.500.12648/2263","text":"External Repository"},{"id":133308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","city":"Tahquamenon Bay","otherGeospatial":"Lake Superior","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.08087158203125,\n              46.4662412291809\n            ],\n            [\n              -84.92706298828125,\n              46.4662412291809\n            ],\n            [\n              -84.92706298828125,\n              46.55697169564088\n            ],\n            [\n              -85.08087158203125,\n              46.55697169564088\n            ],\n            [\n              -85.08087158203125,\n              46.4662412291809\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c27","contributors":{"authors":[{"text":"Johnston, John W.","contributorId":71141,"corporation":false,"usgs":true,"family":"Johnston","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":310372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baedke, Steve J.","contributorId":18325,"corporation":false,"usgs":true,"family":"Baedke","given":"Steve","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":310369,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Booth, Robert K.","contributorId":17177,"corporation":false,"usgs":true,"family":"Booth","given":"Robert","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":310368,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, Todd A.","contributorId":38501,"corporation":false,"usgs":true,"family":"Thompson","given":"Todd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310371,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilcox, Douglas A.","contributorId":36880,"corporation":false,"usgs":true,"family":"Wilcox","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310370,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1001068,"text":"1001068 - 2004 - Additions to the aquatic diptera (Chaoboridae, Chironomidae, Culicidae, Tabanidae, Tipulidae) fauna of the White River National Wildlife Refuge, Arkansas","interactions":[],"lastModifiedDate":"2013-02-04T10:41:18","indexId":"1001068","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2531,"text":"Journal of the Arkansas Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"Additions to the aquatic diptera (Chaoboridae, Chironomidae, Culicidae, Tabanidae, Tipulidae) fauna of the White River National Wildlife Refuge, Arkansas","docAbstract":"The dipteran fauna of Arkansas is generally poorly known.  A previous study of the Aquatic macroinvertebrates of the White River National Wildlife Refuge, the largest refuge in Arkansas, reported only 12 diptera taxa out of 219 taxa collected (Chordas et al., 1996).  Most of the dipterans from this study were identified only to the family level.  The family Chironomidae is a large, diverse group and was predicted to be much more diverse in the refuge than indicated by previous studies.  In this study, Chironomidae were targeted, with other aquatic or semiaquatic dipterans also retained, in collections designed to better define the dipteran fauna of the White River National Wildlife Refuge.  Adult dipterans were collected from 22 sites within the refuge using sweep-nets, two types of blacklight traps, and lighted fan traps in June of 2001.  Specimens from previous studies were retrieved and identified to the lowest possible taxonomic level.  A total of 4,917 specimens representing 122 taxa was collected.  The 122 taxa were comprised of the following: two chaoborids, 83 chironomids, 15 culicids, nine tabanids, and 13 tipulids.  Of these, 46 species are new state records for Arkansas.  Nine undescribed species of chironomids were collected, and eight species records represent significant range extensions.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Arkansas Academy of Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Arkansas Academy of Science","usgsCitation":"Chordas, S.W., Hudson, P.L., and Chapman, E.G., 2004, Additions to the aquatic diptera (Chaoboridae, Chironomidae, Culicidae, Tabanidae, Tipulidae) fauna of the White River National Wildlife Refuge, Arkansas: Journal of the Arkansas Academy of Science, v. 58, p. 37-45.","productDescription":"p. 37-45","startPage":"37","endPage":"45","numberOfPages":"8","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266916,"type":{"id":11,"text":"Document"},"url":"https://libinfo.uark.edu/aas/issues/2004v58/v58a6.pdf"}],"volume":"58","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69787a","contributors":{"authors":[{"text":"Chordas, Stephen W. III","contributorId":87089,"corporation":false,"usgs":true,"family":"Chordas","given":"Stephen","suffix":"III","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":310381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Patrick L. 0000-0002-7646-443X phudson@usgs.gov","orcid":"https://orcid.org/0000-0002-7646-443X","contributorId":5616,"corporation":false,"usgs":true,"family":"Hudson","given":"Patrick","email":"phudson@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":310379,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chapman, Eric G.","contributorId":46450,"corporation":false,"usgs":true,"family":"Chapman","given":"Eric","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":310380,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000877,"text":"1000877 - 2004 - Organochlorine compounds in Lake Superior: Chiral polychlorinated biphenyls and biotransformation in the aquatic food web","interactions":[],"lastModifiedDate":"2016-05-12T15:29:29","indexId":"1000877","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Organochlorine compounds in Lake Superior: Chiral polychlorinated biphenyls and biotransformation in the aquatic food web","docAbstract":"<p><span>The enantiomeric composition of seven chiral PCB congeners was measured in the Lake Superior aquatic food web sampled in 1998, to determine the extent of enantioselective biotransformation in aquatic biota. All chiral PCB congeners studied (CBs 91, 95, 136, 149, 174, 176, and 183) biomagnified in the Lake Superior aquatic food web, based on biomagnification and food web magnification factors greater than unity. PCB atropisomers were racemic in phytoplankton and zooplankton, suggesting no biotransformation potential toward PCBs for these low trophic level organisms. However,&nbsp;</span><i>Diporeia</i><span>&nbsp;and mysids had significantly nonracemic residues for most chiral congeners studied. This observation suggests that these macrozooplankton can stereoselectively metabolize chiral congeners. Alternatively, macrozooplankton obtained nonracemic residues from feeding on organic-rich suspended particles and sediments, which would imply that stereoselective microbial PCB biotransformation may be occurring in Lake Superior sediments at PCB concentrations far lower than that previously associated with such activity. Widely nonracemic PCB residues in forage fish (lake herring, rainbow smelt, and slimy sculpin) and lake trout suggest a combination of both in vivo biotransformation and uptake of nonracemic residues from prey for these species. Minimum biotransformation rates, calculated from enantiomer mass balances between predators and prey, suggest metabolic half-lives on the order of 8 yr for CB 136 in lake trout and 2.6 yr for CB 95 in sculpins. This result suggests that significant biotransformation may occur for metaboliz able PCB congeners over the lifespan of these biota. This study highlights the potential of chiral analysis to study biotransformation processes in food webs.</span></p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es0346983","usgsCitation":"Wong, C.S., Mabury, S.A., Whittle, D.M., Backus, S., Teixeira, C., DeVault, D.S., Bronte, C.R., and Muir, D.C., 2004, Organochlorine compounds in Lake Superior: Chiral polychlorinated biphenyls and biotransformation in the aquatic food web: Environmental Science & Technology, v. 38, no. 1, p. 84-92, https://doi.org/10.1021/es0346983.","productDescription":"9 p.","startPage":"84","endPage":"92","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-11-27","publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a784","contributors":{"authors":[{"text":"Wong, Charles S.","contributorId":51239,"corporation":false,"usgs":true,"family":"Wong","given":"Charles","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":309703,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mabury, Scott A.","contributorId":32860,"corporation":false,"usgs":true,"family":"Mabury","given":"Scott","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":309702,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whittle, D. Michael","contributorId":71121,"corporation":false,"usgs":true,"family":"Whittle","given":"D.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":309706,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Backus, Sean M.","contributorId":31335,"corporation":false,"usgs":true,"family":"Backus","given":"Sean M.","affiliations":[],"preferred":false,"id":309701,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Teixeira, Camilla","contributorId":57000,"corporation":false,"usgs":true,"family":"Teixeira","given":"Camilla","email":"","affiliations":[],"preferred":false,"id":309704,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"DeVault, David S.","contributorId":22720,"corporation":false,"usgs":true,"family":"DeVault","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":309700,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bronte, Charles R.","contributorId":83050,"corporation":false,"usgs":true,"family":"Bronte","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":309707,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Muir, Derek C.G.","contributorId":68679,"corporation":false,"usgs":true,"family":"Muir","given":"Derek","email":"","middleInitial":"C.G.","affiliations":[],"preferred":false,"id":309705,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70184487,"text":"70184487 - 2004 - Use of PRD1 bacteriophage in groundwater viral transport, inactivation, and attachment studies","interactions":[],"lastModifiedDate":"2018-02-08T15:29:58","indexId":"70184487","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1619,"text":"FEMS Microbiology Ecology","onlineIssn":"1574-6941","printIssn":"0168-6496","active":true,"publicationSubtype":{"id":10}},"title":"Use of PRD1 bacteriophage in groundwater viral transport, inactivation, and attachment studies","docAbstract":"<p><span>PRD1, an icosahedra-shaped, 62 nm (diameter), double-stranded DNA bacteriophage with an internal membrane, has emerged as an important model virus for studying the manner in which microorganisms are transported through a variety of groundwater environments. The popularity of this phage for use in transport studies involving geologic media is due, in part, to its relative stability over a range of temperatures and low degree of attachment in aquifer sediments. Laboratory and field investigations employing PRD1 are leading to a better understanding of viral attachment and transport behaviors in saturated geologic media and to improved methods for describing mathematically subsurface microbial transport at environmentally significant field scales. Radioisotopic labeling of PRD1 is facilitating additional information about the nature of viral interactions with solid surfaces in geologic media, the importance of iron oxide surfaces, and allowing differentiation between inactivation and attachment in field-scale tracer tests.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.femsec.2003.09.015","usgsCitation":"Harvey, R.W., and Ryan, J.N., 2004, Use of PRD1 bacteriophage in groundwater viral transport, inactivation, and attachment studies: FEMS Microbiology Ecology, v. 49, no. 1, p. 3-16, https://doi.org/10.1016/j.femsec.2003.09.015.","productDescription":"14 p. ","startPage":"3","endPage":"16","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":478364,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.femsec.2003.09.015","text":"Publisher Index Page"},{"id":337290,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c3c944e4b0f37a93ee9b59","contributors":{"authors":[{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":681705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryan, Joseph N.","contributorId":54290,"corporation":false,"usgs":false,"family":"Ryan","given":"Joseph","email":"","middleInitial":"N.","affiliations":[{"id":604,"text":"University of Colorado- Boulder","active":false,"usgs":true}],"preferred":false,"id":681706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}