{"pageNumber":"2603","pageRowStart":"65050","pageSize":"25","recordCount":184615,"records":[{"id":70182473,"text":"70182473 - 2005 - A risk assessment based approach for the management of whirling disease","interactions":[],"lastModifiedDate":"2022-06-02T14:32:24.008332","indexId":"70182473","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3279,"text":"Reviews in Fisheries Science","active":true,"publicationSubtype":{"id":10}},"title":"A risk assessment based approach for the management of whirling disease","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/10641260500326842","usgsCitation":"Bartholomew, J.L., Kerans, B., Hedrick, R., MacDiarmid, S.C., and Winton, J., 2005, A risk assessment based approach for the management of whirling disease: Reviews in Fisheries Science, v. 13, p. 205-230, https://doi.org/10.1080/10641260500326842.","productDescription":"26 p.","startPage":"205","endPage":"230","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":336079,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","noUsgsAuthors":false,"publicationDate":"2007-01-18","publicationStatus":"PW","scienceBaseUri":"58b002c7e4b01ccd54fb27d9","contributors":{"authors":[{"text":"Bartholomew, J. L.","contributorId":91661,"corporation":false,"usgs":true,"family":"Bartholomew","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":671227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kerans, B.","contributorId":182358,"corporation":false,"usgs":false,"family":"Kerans","given":"B.","email":"","affiliations":[],"preferred":false,"id":671229,"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":671228,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"MacDiarmid, S. C.","contributorId":182359,"corporation":false,"usgs":false,"family":"MacDiarmid","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":671230,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":671231,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028238,"text":"70028238 - 2005 - Spatiotemporal evolution of a transient slip event on the San Andreas fault near Parkfield, California","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70028238","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Spatiotemporal evolution of a transient slip event on the San Andreas fault near Parkfield, California","docAbstract":"In 1993 several baselines of the two-color electronic distance meter (EDM) network at Parkfield, California, deviated from their long-term rates, coincident with anomalous observations from nearby strain meters and a creep meter, as well as an increase in microseismicity. Between October 1992 and December 1994, three M ??? 4.5 earthquakes occurred beneath Middle Mountain, near the hypocenter of the 1934 and 1966 Parkfield M6 events. We analyzed the two-color EDM data using a Kalman-filtering based technique to image the spatiotemporal evolution of slip on the fault at Parkfield between the mid-1980s and 2003. This method accounts for localized random walk motion of the geodetic monuments and a prominent seasonal signal that affects many baselines. We find that a slip rate increase occurred between January 1993 and July 1996 on the upper 8 km of the fault near Middle Mountain. The peak estimated slip rate during this time was 49 mm/yr, which exceeds the long-term geologic rate of ???35 mm/yr. The slip rate evolution appears episodic, with an initial modest increase after the M4.3 earthquake and a much larger jump following the shallower M4.7 event in December 1994. This temporal correlation between inferred slip and seismicity suggests that the moderate earthquakes triggered the aseismic fault slip. The EDM data cannot resolve whether transient slip propagated across the nucleation zone of the 1934 and 1966 M6 Parkfield earthquakes. However, transient slip and its associated stress release in the hypocentral area of previous Parkfield events is consistent with the nucleation of the 2004 M6 Parkfield earthquake elsewhere on the fault. Copyright 2005 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JB003651","issn":"01480227","usgsCitation":"Murray, J., and Segall, P., 2005, Spatiotemporal evolution of a transient slip event on the San Andreas fault near Parkfield, California: Journal of Geophysical Research B: Solid Earth, v. 110, no. 9, p. 1-12, https://doi.org/10.1029/2005JB003651.","startPage":"1","endPage":"12","numberOfPages":"12","costCenters":[],"links":[{"id":210399,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB003651"},{"id":237304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"9","noUsgsAuthors":false,"publicationDate":"2005-09-14","publicationStatus":"PW","scienceBaseUri":"505b94cde4b08c986b31ac59","contributors":{"authors":[{"text":"Murray, J.R.","contributorId":39179,"corporation":false,"usgs":true,"family":"Murray","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":417181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Segall, P.","contributorId":44231,"corporation":false,"usgs":false,"family":"Segall","given":"P.","affiliations":[],"preferred":false,"id":417182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028276,"text":"70028276 - 2005 - Integrated core-log petrofacies analysis in the construction of a reservoir geomodel: A case study of a mature Mississippian carbonate reservoir using limited data","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70028276","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":"Integrated core-log petrofacies analysis in the construction of a reservoir geomodel: A case study of a mature Mississippian carbonate reservoir using limited data","docAbstract":"Small independent operators produce most of the Mississippian carbonate fields in the United States mid-continent, where a lack of integrated characterization studies precludes maximization of hydrocarbon recovery. This study uses integrative techniques to leverage extant data in an Osagian and Meramecian (Mississippian) cherty carbonate reservoir in Kansas. Available data include petrophysical logs of varying vintages, limited number of cores, and production histories from each well. A consistent set of assumptions were used to extract well-level porosity and initial saturations, from logs of different types and vintages, to build a geomodel. Lacking regularly recorded well shut-in pressures, an iterative technique, based on material balance formulations, was used to estimate average reservoir-pressure decline that matched available drillstem test data and validated log-analysis assumptions. Core plugs representing the principal reservoir petrofacies provide critical inputs for characterization and simulation studies. However, assigning plugs among multiple reservoir petrofacies is difficult in complex (carbonate) reservoirs. In a bottom-up approach, raw capillary pressure (Pc) data were plotted on the Super-Pickett plot, and log- and core-derived saturation-height distributions were reconciled to group plugs by facies, to identify core plugs representative of the principal reservoir facies, and to discriminate facies in the logged interval. Pc data from representative core plugs were used for effective pay evaluation to estimate water cut from completions, in infill and producing wells, and guide-selective perforations for economic exploitation of mature fields. The results from this study were used to drill 22 infill wells. Techniques demonstrated here can be applied in other fields and reservoirs. 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":"10.1306/06030504144","issn":"01491423","usgsCitation":"Bhattacharya, S., Doveton, J., Carr, T., Guy, W., and Gerlach, P., 2005, Integrated core-log petrofacies analysis in the construction of a reservoir geomodel: A case study of a mature Mississippian carbonate reservoir using limited data: American Association of Petroleum Geologists Bulletin, v. 89, no. 10, p. 1257-1274, https://doi.org/10.1306/06030504144.","startPage":"1257","endPage":"1274","numberOfPages":"18","costCenters":[],"links":[{"id":210428,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/06030504144"},{"id":237341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3c5de4b0c8380cd62caa","contributors":{"authors":[{"text":"Bhattacharya, S.","contributorId":97226,"corporation":false,"usgs":true,"family":"Bhattacharya","given":"S.","email":"","affiliations":[],"preferred":false,"id":417361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doveton, J.H.","contributorId":30237,"corporation":false,"usgs":true,"family":"Doveton","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":417357,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carr, T.R.","contributorId":37094,"corporation":false,"usgs":true,"family":"Carr","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":417358,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guy, W.R.","contributorId":45891,"corporation":false,"usgs":true,"family":"Guy","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":417360,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gerlach, P.M.","contributorId":39959,"corporation":false,"usgs":true,"family":"Gerlach","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":417359,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028188,"text":"70028188 - 2005 - Effects of spinning-wing decoys on flock behavior and hunting vulnerability of mallards in Minnesota","interactions":[],"lastModifiedDate":"2012-03-12T17:20:43","indexId":"70028188","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Effects of spinning-wing decoys on flock behavior and hunting vulnerability of mallards in Minnesota","docAbstract":"Waterfowl managers in Minnesota and other states are concerned that increased kill rates associated with the use of spinning-wing decoys (SWDs) may negatively affect local breeding populations of mallards (Anas platyrhynchos). Accordingly, we conducted 219 experimental hunts to evaluate hunting vulnerability of mallards to SWDs during the 2002 duck season in Minnesota. During each hunt, we tested 2 SWD treatments: 1) SWDs turned OFF (control), and 2) SWDs turned ON (experimental) during alternate 15-minute sampling periods that were separated by 5-minute buffer periods. We found that mallard flocks (???1 duck) were 2.91 times more likely to respond (i.e., approach within 40 m of hunters), and sizes of responding mallard flocks were 1.25 times larger, on average, when SWDs were turned ON than OFF. Mallards killed/hour/hunter/hunt averaged 4.71 times higher (P < 0.001) when SWDs were turned ON than OFF. More hatch-year (HY) and after-hatch-year (AHY) mallards were killed when SWDs were turned ON than OFF; however, AHYs were relatively less likely than were HYs to be killed with SWDs turned ON. We found no evidence that SWDs reduced crippling or allowed hunters to harvest relatively more drakes than hens. Using a worst-case scenario model, we predicted that if 47% and 79% of Minnesota hunters had used SWDs in 2000 and 2002, respectively, Minnesota mallard harvests would have increased by a factor of 2. However, increasing use of SWDs by northern hunters may result in a partial redistribution of annual mallard harvests if nai??ve ducks are harvested upon initial exposures to SWDs, and those ducks that survive become habituated to SWDs, as suggested by our results. Our study was confined to a single hunting season in Minnesota and thus did not assess whether vulnerability of mallards to hunters using SWDs varied among years or geographically. A multi-year, flyway-wide study is needed to make stronger and more rigorous inferences regarding potential changes in harvest distribution and annual harvest rates of mallards due to increasing use of SWDs by hunters in North America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/0091-7648(2005)33[993:EOSDOF]2.0.CO;2","issn":"00917648","usgsCitation":"Szymanski, M., and Afton, A., 2005, Effects of spinning-wing decoys on flock behavior and hunting vulnerability of mallards in Minnesota: Wildlife Society Bulletin, v. 33, no. 3, p. 993-1001, https://doi.org/10.2193/0091-7648(2005)33[993:EOSDOF]2.0.CO;2.","startPage":"993","endPage":"1001","numberOfPages":"9","costCenters":[],"links":[{"id":237021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210179,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0091-7648(2005)33[993:EOSDOF]2.0.CO;2"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a07d8e4b0c8380cd5187d","contributors":{"authors":[{"text":"Szymanski, M.L.","contributorId":8662,"corporation":false,"usgs":true,"family":"Szymanski","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":416959,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Afton, A. D.","contributorId":83467,"corporation":false,"usgs":true,"family":"Afton","given":"A. D.","affiliations":[],"preferred":false,"id":416960,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028277,"text":"70028277 - 2005 - The role of impoundments in the sediment budget of the conterminous United States","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028277","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"The role of impoundments in the sediment budget of the conterminous United States","docAbstract":"Previous work on sediment budgets for U.S. agricultural regions has concluded that most sediment derived from accelerated erosion is still on the landscape, primarily in colluvial and alluvial deposits. Here we examine the role of small impoundments in the subcontinental sediment budget. A recent inventory based on a 30-m satellite imagery reveals approximately 2.6 million ponds, while extrapolation from a sample of 1:24,000 topographic quadrangles suggests the total may be as large as 8-9 million. These ponds capture an estimated 21% of the total drainage area of the conterminous U.S., representing 25% of total sheet and rill erosion. We estimate the total sedimentation in these small impoundments using three different methods; these estimates range from 0.43 to 1.78 ?? 109 m3 yr-1. Total sedimentation in ???43,000 reservoirs from the National Inventory of Dams is estimated at 1.67 ?? 109 m3 yr-1. Total USLE erosion in 1992 was 2.4 ?? 109 m3 yr-1, and export to coastal areas is estimated at 0.6 ?? 109 m3 yr-1. Total sedimentation in impoundments is large in relation to upland erosion, in apparent contradiction to previous studies that have identified colluvial and alluvial deposition as the primary sinks. Several alternative hypotheses that could help explain this result are proposed. Regardless of which of these alternatives may prove to be the most significant in any given setting, it is clear that most sedimentation is now taking place in subaqueous rather than subaerial environments, and that small impoundments are a major sediment sink. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.geomorph.2004.01.010","issn":"0169555X","usgsCitation":"Renwick, W.H., Smith, S.V., Bartley, J., and Buddemeier, R., 2005, The role of impoundments in the sediment budget of the conterminous United States: Geomorphology, v. 71, no. 1-2, p. 99-111, https://doi.org/10.1016/j.geomorph.2004.01.010.","startPage":"99","endPage":"111","numberOfPages":"13","costCenters":[],"links":[{"id":210022,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geomorph.2004.01.010"},{"id":236815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf78e4b08c986b324804","contributors":{"authors":[{"text":"Renwick, W. H.","contributorId":64794,"corporation":false,"usgs":true,"family":"Renwick","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":417362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, S. V.","contributorId":89284,"corporation":false,"usgs":true,"family":"Smith","given":"S.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":417365,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartley, J.D.","contributorId":88533,"corporation":false,"usgs":true,"family":"Bartley","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":417364,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buddemeier, R. W.","contributorId":86492,"corporation":false,"usgs":true,"family":"Buddemeier","given":"R. W.","affiliations":[],"preferred":false,"id":417363,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028183,"text":"70028183 - 2005 - Geochemistry of speleothem records from southern Illinois: Development of (234U)/(238U) as a proxy for paleoprecipitation","interactions":[],"lastModifiedDate":"2012-03-12T17:20:43","indexId":"70028183","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":"Geochemistry of speleothem records from southern Illinois: Development of (234U)/(238U) as a proxy for paleoprecipitation","docAbstract":"Natural waters universally show fractionation of uranium series (U-series) parent-daughter pairs, with the disequilibrium between 234U and 238U (234U)/(238U) commonly used as a tracer of groundwater flow. Because speleothems provide a temporal record of geochemical variations in groundwater precipitating calcite, (234U)/(238U) variations in speleothems provide a unique method of investigating water-rock interaction processes over millennium time scales. We present high precision Thermal Ionization Mass Spectrometric (TIMS) U-series analyses of speleothems and drip waters from Fogelpole Cave in southern Illinois. Data from all speleothems from the cave show an inverse correlation between (234U)/(238U) and U concentration, following the pattern observed in groundwaters globally. Within a 65-cm-long stalagmite, concordant 234U-238 U-230Th and 235U-231Pa ages for 5 samples indicate accurate chronology from 78.5 ka to 30 ka. Notably, (234U)/(238U)o which differs from most speleothems by having (234U)/(238U)o <1, positively correlates with speleothem growth rate. We generalize this to the observation that speleothems globally show (234U)/ (238U)o deviating farther from secular equilibrium at lower growth rates and approaching secular equilibrium at higher grow rates. Based on the Fogelpole observations, we suggest that groundwater (234U)/(238U) is controlled by the U oxidation state, the U concentration of the water and the fluid velocity. A transport model whereby U-series nuclides react and exchange with mineral surfaces can reproduce the observed trend between growth rate and (234U)/(238U)o. Based on this result, we suggest that (234U)/(238U)o in speleothems may record changes in hydrologic flux with time and thus could provide a useful proxy for long term records of paleoprecipitation. ?? 2005 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.2005.02.005","issn":"00092541","usgsCitation":"Zhou, J., Lundstrom, C., Fouke, B., Panno, S., Hackley, K., and Curry, B., 2005, Geochemistry of speleothem records from southern Illinois: Development of (234U)/(238U) as a proxy for paleoprecipitation: Chemical Geology, v. 221, no. 1-2, p. 1-20, https://doi.org/10.1016/j.chemgeo.2005.02.005.","startPage":"1","endPage":"20","numberOfPages":"20","costCenters":[],"links":[{"id":210096,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2005.02.005"},{"id":236914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"221","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1714e4b0c8380cd5538e","contributors":{"authors":[{"text":"Zhou, Juanzuo","contributorId":59217,"corporation":false,"usgs":true,"family":"Zhou","given":"Juanzuo","email":"","affiliations":[],"preferred":false,"id":416946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lundstrom, C.C.","contributorId":72997,"corporation":false,"usgs":true,"family":"Lundstrom","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":416947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fouke, B.","contributorId":31187,"corporation":false,"usgs":true,"family":"Fouke","given":"B.","affiliations":[],"preferred":false,"id":416943,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Panno, S.","contributorId":42016,"corporation":false,"usgs":true,"family":"Panno","given":"S.","email":"","affiliations":[],"preferred":false,"id":416944,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hackley, K.","contributorId":44343,"corporation":false,"usgs":true,"family":"Hackley","given":"K.","email":"","affiliations":[],"preferred":false,"id":416945,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Curry, B.","contributorId":89320,"corporation":false,"usgs":true,"family":"Curry","given":"B.","email":"","affiliations":[],"preferred":false,"id":416948,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70028192,"text":"70028192 - 2005 - Aminobacter ciceronei sp. nov. and Aminobacter lissarensis sp. nov., isolated from various terrestrial environments","interactions":[],"lastModifiedDate":"2018-10-31T09:30:23","indexId":"70028192","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2076,"text":"International Journal of Systematic and Evolutionary Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Aminobacter ciceronei sp. nov. and Aminobacter lissarensis sp. nov., isolated from various terrestrial environments","docAbstract":"<p>The&nbsp;<span>bacterial strains IMB-1</span><span class=\"jp-sup\">T</span><span>&nbsp;and CC495</span><span class=\"jp-sup\">T</span><span>, which are capable of growth on methyl chloride (CH</span><span class=\"jp-sub\">3</span><span>Cl, chloromethane) and methyl bromide (CH</span><span class=\"jp-sub\">3</span><span>Br, bromomethane), were isolated from agricultural soil in California fumigated with CH</span><span class=\"jp-sub\">3</span><span>Br, and woodland soil in Northern Ireland, respectively. Two pesticide-/herbicide-degrading bacteria, strains ER2 and C147, were isolated from agricultural soil in Canada. Strain ER2 degrades&nbsp;</span><span class=\"jp-italic\">N</span><span>-methyl carbamate insecticides, and strain C147 degrades triazine herbicides widely used in agriculture. On the basis of their morphological, physiological and genotypic characteristics, these four strains are considered to represent two novel species of the genus&nbsp;</span><span class=\"jp-italic\">Aminobacter</span><span>, for which the names&nbsp;</span><span class=\"jp-italic\">Aminobacter ciceronei</span><span>&nbsp;sp. nov. (type strain IMB-1</span><span class=\"jp-sup\">T</span><span>=ATCC 202197</span><span class=\"jp-sup\">T</span><span>=CIP 108660</span><span class=\"jp-sup\">T</span><span>=CCUG 50580</span><span class=\"jp-sup\">T</span><span>; strains ER2 and C147) and&nbsp;</span><span class=\"jp-italic\">Aminobacter lissarensis</span><span>&nbsp;sp. nov. (type strain CC495</span><span class=\"jp-sup\">T</span><span>=NCIMB 13798</span><span class=\"jp-sup\">T</span><span>=CIP 108661</span><span class=\"jp-sup\">T</span><span>=CCUG 50579</span><span class=\"jp-sup\">T</span><span>) are proposed.</span></p>","language":"English","publisher":"Microbiology Society ","doi":"10.1099/ijs.0.63716-0","issn":"14665026","usgsCitation":"McDonald, I., Kampfer, P., Topp, E., Warner, K., Cox, M., Connell, H.T., Miller, L., Larkin, M., Ducrocq, V., Coulter, C., Harper, D., Murrell, J., and Oremland, R., 2005, Aminobacter ciceronei sp. nov. and Aminobacter lissarensis sp. nov., isolated from various terrestrial environments: International Journal of Systematic and Evolutionary Microbiology, v. 55, no. 5, p. 1827-1832, https://doi.org/10.1099/ijs.0.63716-0.","productDescription":"6 p.","startPage":"1827","endPage":"1832","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477815,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://resolver.tudelft.nl/uuid:baf9e3e5-d554-4215-903e-a299daaddb57","text":"Publisher Index Page"},{"id":237093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210233,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1099/ijs.0.63716-0"}],"volume":"55","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e9bce4b0c8380cd48400","contributors":{"authors":[{"text":"McDonald, I.R.","contributorId":23313,"corporation":false,"usgs":true,"family":"McDonald","given":"I.R.","email":"","affiliations":[],"preferred":false,"id":416978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kampfer, P.","contributorId":51525,"corporation":false,"usgs":true,"family":"Kampfer","given":"P.","email":"","affiliations":[],"preferred":false,"id":416982,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Topp, E.","contributorId":51526,"corporation":false,"usgs":true,"family":"Topp","given":"E.","email":"","affiliations":[],"preferred":false,"id":416983,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, K.L.","contributorId":73781,"corporation":false,"usgs":true,"family":"Warner","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":416985,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cox, M.J.","contributorId":22562,"corporation":false,"usgs":true,"family":"Cox","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":416977,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Connell, Hancock T.L.","contributorId":9418,"corporation":false,"usgs":true,"family":"Connell","given":"Hancock","email":"","middleInitial":"T.L.","affiliations":[],"preferred":false,"id":416976,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Miller, L.G.","contributorId":32522,"corporation":false,"usgs":true,"family":"Miller","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":416980,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Larkin, M.J.","contributorId":103856,"corporation":false,"usgs":true,"family":"Larkin","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":416988,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ducrocq, V.","contributorId":33913,"corporation":false,"usgs":true,"family":"Ducrocq","given":"V.","email":"","affiliations":[],"preferred":false,"id":416981,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Coulter, C.","contributorId":64875,"corporation":false,"usgs":true,"family":"Coulter","given":"C.","email":"","affiliations":[],"preferred":false,"id":416984,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Harper, D.B.","contributorId":76506,"corporation":false,"usgs":true,"family":"Harper","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":416986,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Murrell, J.C.","contributorId":25731,"corporation":false,"usgs":true,"family":"Murrell","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":416979,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Oremland, R.S.","contributorId":97512,"corporation":false,"usgs":true,"family":"Oremland","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":416987,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70028835,"text":"70028835 - 2005 - Effects of fire intensity on vital rates of an endemic herb of the Florida keys, USA","interactions":[],"lastModifiedDate":"2022-07-18T16:51:28.023932","indexId":"70028835","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2821,"text":"Natural Areas Journal","active":true,"publicationSubtype":{"id":10}},"title":"Effects of fire intensity on vital rates of an endemic herb of the Florida keys, USA","docAbstract":"Fire intensity is one of the important components of a fire regime. However, relatively few studies have linked fire intensity with post-fire population vital rates. In this study, we explored the effects of fire intensity on population vital rates of Chamaecrista keyensis Pennell (Fabaceae) up to two years post-fire. C. keyensis is an endemic understory plant of pine rockland, a fire-dependent ecosystem of the Lower Florida Keys. We measured one fire intensity indicator, fire temperature reached by steel plates on the ground, during three prescribed fires at different sites. We followed marked individuals up to two years post-fire to derive annual survival, annual growth rate, percentage of fruiting plants, mean number of fruits per reproductive plant, and number of seedlings per census plot (1 m2) of C. keyensis. We found fire intensity had significant effects on reproduction in the first year post-fire only. More specifically, mean number of fruits and percentage of fruiting plants increased as fire intensity increased. Results from this study suggest that extremely low fire intensity caused by very short fire return intervals (e.g., less than three years) may not provide sufficient stimulation to reproduction to achieve the best post-fire recovery for C. keyensis.","language":"English","publisher":"Natural Areas Association","issn":"08858608","usgsCitation":"Liu, H., Menges, E., Snyder, J., Koptur, S., and Ross, M., 2005, Effects of fire intensity on vital rates of an endemic herb of the Florida keys, USA: Natural Areas Journal, v. 25, no. 1, p. 71-76.","productDescription":"6 p.","startPage":"71","endPage":"76","costCenters":[],"links":[{"id":236726,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403928,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/43912368"}],"country":"United States","state":"Florida","otherGeospatial":"Big Pine Key, Florida Keys","geographicExtents":"{\n  \"type\": 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]\n}","volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a06eee4b0c8380cd514b0","contributors":{"authors":[{"text":"Liu, H.","contributorId":12222,"corporation":false,"usgs":true,"family":"Liu","given":"H.","affiliations":[],"preferred":false,"id":419926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Menges, E.S.","contributorId":80479,"corporation":false,"usgs":true,"family":"Menges","given":"E.S.","affiliations":[],"preferred":false,"id":419927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snyder, J.R.","contributorId":96622,"corporation":false,"usgs":true,"family":"Snyder","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":419929,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koptur, S.","contributorId":85379,"corporation":false,"usgs":true,"family":"Koptur","given":"S.","affiliations":[],"preferred":false,"id":419928,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ross, M.S.","contributorId":96781,"corporation":false,"usgs":true,"family":"Ross","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":419930,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028783,"text":"70028783 - 2005 - Characterization of gas chemistry and noble-gas isotope ratios of inclusion fluids in magmatic-hydrothermal and magmatic-steam alunite","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70028783","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of gas chemistry and noble-gas isotope ratios of inclusion fluids in magmatic-hydrothermal and magmatic-steam alunite","docAbstract":"Chemical and isotope data were obtained for the active gas and noble gas of inclusion fluids in coarse-grained samples of magmatic-hydrothermal and magmatic-steam alunite from well-studied deposits (Marysvale, Utah; Tambo, Chile; Tapajo??s, Brazil; Cactus, California; Pierina, Peru), most of which are discussed in this Volume. Primary fluid inclusions in the alunite typically are less than 0.2 ??m but range up to several micrometers. Analyses of the active-gas composition of these alunite-hosted inclusion fluids released in vacuo by both crushing and heating indicate consistent differences in the compositions of magmatic-hydrothermal and magmatic-steam fluids. The compositions of fluids released by crushing were influenced by contributions from significant populations of secondary inclusions that trapped largely postdepositional hydrothermal fluids. Thermally released fluids gave the best representation of the fluids that formed primary alunite. The data are consistent with current models for the evolution of magmatic-hydrothermal and magmatic-steam fluids. Magmatic-steam fluids are vapor-dominant, average about 49 mol% H2O, and contain N2, H2, CH4, CO, Ar, He, HF, and HCl, with SO2 the dominant sulfur gas (average SO2/ H2S=202). In contrast, magmatic-hydrothermal fluids are liquid-dominant, average about 88 mol% H2O, and N2, H2, CO2, and HF, with H2S about as abundant as SO2 (average SO2/H2 S=0.7). The low SO2/H2S and N2/Ar ratios, and the near-absence of He in magmatic-hydrothermal fluids, are consistent with their derivation from degassed condensed magmatic fluids whose evolution from reduced-to-oxidized aqueous sulfur species was governed first by rock and then by fluid buffers. The high SO2/H2S and N2/Ar with significant concentrations of He in magmatic-steam fluids are consistent with derivation directly from a magma. None of the data supports the entrainment of atmospheric gases or mixing of air-saturated gases in meteoric water in either magmatic-hydrothermal or magmatic-steam fluids. Thus, the oxidation of SO2 to aqueous sulfate in the magmatic-steam fluids did not result from mixing with atmospheric oxygen. Both of the fluid types are characterized by high H2 contents that range from 0.2 mol% to the extraordinarily large amounts (66 mol%) observed in some magmatic-steam fluids. Modeling of gas speciation using SOLVGAS requires most of the gas species to have been in disequilibrium at the time of their trapping in the fluid inclusions. The origin of such extreme H2 concentrations, although problematic, is thought to be largely related to accumulation of H2 from the reaction of water with ferrous iron during the rise of magma and probably even after exsolution of fluid from a magma. The large contents of reduced gases in the inclusion fluids are far in excess of those observed in volcanic emanations, and are thought to reflect the close \"sampling position\" of the host alunite relative to the location of the magma. Isotope ratios of He and Ne indicate largely crustal sources for these gases in the alunite parental fluids derived from Tertiary magmas, but a greater mantle component for the gases in alunite parental fluids derived from Proterozoic magmas.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.06.037","issn":"00092541","usgsCitation":"Landis, G.P., and Rye, R.O., 2005, Characterization of gas chemistry and noble-gas isotope ratios of inclusion fluids in magmatic-hydrothermal and magmatic-steam alunite: Chemical Geology, v. 215, no. 1-4 SPEC. ISS., p. 155-184, https://doi.org/10.1016/j.chemgeo.2004.06.037.","startPage":"155","endPage":"184","numberOfPages":"30","costCenters":[],"links":[{"id":236546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209820,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.06.037"}],"volume":"215","issue":"1-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f4c9e4b0c8380cd4befe","contributors":{"authors":[{"text":"Landis, G. P.","contributorId":102846,"corporation":false,"usgs":true,"family":"Landis","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":419741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":419740,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028784,"text":"70028784 - 2005 - A sampler for capturing larval and juvenile Atlantic menhaden","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70028784","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"A sampler for capturing larval and juvenile Atlantic menhaden","docAbstract":"Interest in capturing larval and juvenile Atlantic menhaden Brevoortia tyrannus for use in laboratory studies required the design and construction of a sampling device that would allow us to make collections of live fish from open-water areas. Our device for capturing 1-2.5-in larval-juvenile fish was constructed of a stainless steel frame that supported a 9.84-ft-long (3-m-long)5 cone plankton net with a 3.28-ft-diameter (1-m-diameter) opening and a 0.04-in (1-mm) mesh size. Although the plankton net was similar to that used during typical larval fish collections, the cod end was constructed of Plexiglas and was nearly watertight; this prevented impingement and injury to larval fish and provided a calm-water environment. The cod end was designed for quick release from the plankton net, and the entire cod end could be submerged into a 75-gal onboard holding tank. This design and technique obviated the netting or emerging of fish from the water until they were returned to the laboratory. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/M03-189.1","issn":"02755947","usgsCitation":"Hedrick, J., Hedrick, L., and Margraf, F., 2005, A sampler for capturing larval and juvenile Atlantic menhaden: North American Journal of Fisheries Management, v. 25, no. 1, p. 245-250, https://doi.org/10.1577/M03-189.1.","startPage":"245","endPage":"250","numberOfPages":"6","costCenters":[],"links":[{"id":236547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209821,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/M03-189.1"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-01","publicationStatus":"PW","scienceBaseUri":"5059e567e4b0c8380cd46d45","contributors":{"authors":[{"text":"Hedrick, J.D.","contributorId":105511,"corporation":false,"usgs":true,"family":"Hedrick","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":419744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedrick, L.R.","contributorId":14177,"corporation":false,"usgs":true,"family":"Hedrick","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":419742,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Margraf, F.J.","contributorId":47738,"corporation":false,"usgs":true,"family":"Margraf","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":419743,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028865,"text":"70028865 - 2005 - The ecological - Societal underpinnings of Everglades restoration","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028865","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The ecological - Societal underpinnings of Everglades restoration","docAbstract":"The biotic integrity of the Florida Everglades, a wetland of immense international importance, is threatened as a result of decades of human manipulation for drainage and development. Past management of the system only exacerbated the problems associated with nutrient enrichment and disruption of regional hydrology. The Comprehensive Everglades Restoration Plan (CERP) now being implemented by Federal and State governments is an attempt to strike a balance between the needs of the environment with the complex management of water and the seemingly unbridled economic growth of southern Florida. CERP is expected to reverse negative environmental trends by \"getting the water right\", but successful Everglades restoration will require both geochemical and hydrologic intervention on a massive scale. This will produce ecological trade-offs and will require new and innovative scientific measures to (1) reduce total phosphorus concentrations within the remaining marsh to 10 ??g/L or lower; (2) quantify and link ecological benefits to the restoration of depths, hydroperiods, and flow velocities; and (3) compensate for ecological, economic, and hydrologic uncertainties in the CERP through adaptive management. ?? The Ecological Society of America.","largerWorkTitle":"Frontiers in Ecology and the Environment","language":"English","issn":"15409295","usgsCitation":"Sklar, F.H., Chimney, M., Newman, S., McCormick, P., Gawlik, D., Miao, S., McVoy, C., Said, W., Newman, J., Coronado, C., Crozier, G., Korvela, M., and Rutchey, K., 2005, The ecological - Societal underpinnings of Everglades restoration, <i>in</i> Frontiers in Ecology and the Environment, v. 3, no. 3, p. 161-169.","startPage":"161","endPage":"169","numberOfPages":"9","costCenters":[],"links":[{"id":236652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baaf7e4b08c986b322b18","contributors":{"authors":[{"text":"Sklar, Fred H.","contributorId":23327,"corporation":false,"usgs":true,"family":"Sklar","given":"Fred","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":420084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chimney, M.J.","contributorId":6648,"corporation":false,"usgs":true,"family":"Chimney","given":"M.J.","affiliations":[],"preferred":false,"id":420081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newman, S.","contributorId":7678,"corporation":false,"usgs":true,"family":"Newman","given":"S.","affiliations":[],"preferred":false,"id":420082,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCormick, P.","contributorId":30022,"corporation":false,"usgs":true,"family":"McCormick","given":"P.","email":"","affiliations":[],"preferred":false,"id":420087,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gawlik, D.","contributorId":23742,"corporation":false,"usgs":true,"family":"Gawlik","given":"D.","email":"","affiliations":[],"preferred":false,"id":420085,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Miao, S.","contributorId":79688,"corporation":false,"usgs":true,"family":"Miao","given":"S.","email":"","affiliations":[],"preferred":false,"id":420093,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McVoy, C.","contributorId":24155,"corporation":false,"usgs":true,"family":"McVoy","given":"C.","affiliations":[],"preferred":false,"id":420086,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Said, W.","contributorId":45101,"corporation":false,"usgs":true,"family":"Said","given":"W.","email":"","affiliations":[],"preferred":false,"id":420090,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Newman, J.","contributorId":13764,"corporation":false,"usgs":true,"family":"Newman","given":"J.","email":"","affiliations":[],"preferred":false,"id":420083,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Coronado, C.","contributorId":39998,"corporation":false,"usgs":true,"family":"Coronado","given":"C.","email":"","affiliations":[],"preferred":false,"id":420089,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Crozier, G.","contributorId":50711,"corporation":false,"usgs":true,"family":"Crozier","given":"G.","email":"","affiliations":[],"preferred":false,"id":420091,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Korvela, M.","contributorId":71751,"corporation":false,"usgs":true,"family":"Korvela","given":"M.","affiliations":[],"preferred":false,"id":420092,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Rutchey, K.","contributorId":35825,"corporation":false,"usgs":true,"family":"Rutchey","given":"K.","email":"","affiliations":[],"preferred":false,"id":420088,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70028806,"text":"70028806 - 2005 - Optimal swim speeds for traversing velocity barriers: An analysis of volitional high-speed swimming behavior of migratory fishes","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70028806","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2275,"text":"Journal of Experimental Biology","active":true,"publicationSubtype":{"id":10}},"title":"Optimal swim speeds for traversing velocity barriers: An analysis of volitional high-speed swimming behavior of migratory fishes","docAbstract":"Migrating fish traversing velocity barriers are often forced to swim at speeds greater than their maximum sustained speed (Ums). Failure to select an appropriate swim speed under these conditions can prevent fish from successfully negotiating otherwise passable barriers. I propose a new model of a distance-maximizing strategy for fishes traversing velocity barriers, derived from the relationships between swim speed and fatigue time in both prolonged and sprint modes. The model predicts that fish will maximize traversed distance by swimming at a constant groundspeed against a range of flow velocities, and this groundspeed is equal to the negative inverse of the slope of the swim speed-fatigue time relationship for each mode. At a predictable flow velocity, they should switch from the optimal groundspeed for prolonged mode to that for sprint mode. Data from six migratory fish species (anadromous clupeids: American shad Alosa sapidissima, alewife A. pseudoharengus and blueback herring A. aestivalis; amphidromous: striped bass Morone saxatilis; and potomodromous species: walleye (previously known as Stizostedion vitrium) and white sucker Catostomus commersonii) were used to explore the ability of fish to approximate the predicted distance-maximizing behaviors, as well as the consequences of deviating from the optima. Fish volitionally sprinted up an open-channel flume against fixed flow velocities of 1.5-4.5 m s-1, providing data on swim speeds and fatigue times, as well as their groundspeeds. Only anadromous clupeids selected the appropriate distance-maximizing groundspeed at both prolonged and sprint modes. The other three species maintained groundspeeds appropriate to the prolonged mode, even when they should have switched to the sprint optima. Because of this, these species failed to maximize distance of ascent. The observed behavioral variability has important implications both for distributional limits and fishway design.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Experimental Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1242/jeb.01380","issn":"00220949","usgsCitation":"Castro-Santos, T., 2005, Optimal swim speeds for traversing velocity barriers: An analysis of volitional high-speed swimming behavior of migratory fishes: Journal of Experimental Biology, v. 208, no. 3, p. 421-432, https://doi.org/10.1242/jeb.01380.","startPage":"421","endPage":"432","numberOfPages":"12","costCenters":[],"links":[{"id":477702,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1242/jeb.01380","text":"Publisher Index Page"},{"id":209641,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1242/jeb.01380"},{"id":236304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"208","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6eeae4b0c8380cd7587b","contributors":{"authors":[{"text":"Castro-Santos, T. 0000-0003-2575-9120","orcid":"https://orcid.org/0000-0003-2575-9120","contributorId":12416,"corporation":false,"usgs":true,"family":"Castro-Santos","given":"T.","affiliations":[],"preferred":false,"id":419823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028874,"text":"70028874 - 2005 - Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin","interactions":[],"lastModifiedDate":"2016-05-03T16:33:33","indexId":"70028874","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin","docAbstract":"<p>Fall Chinook salmon Oncorhynchus tshawytscha in the Snake River basin were listed under the Endangered Species Act in 1992. At the time of listing, it was assumed that fall Chinook salmon juveniles in the Snake River basin adhered strictly to an ocean-type life history characterized by saltwater entry at age 0 and first-year wintering in the ocean. Research showed, however, that some fall Chinook salmon juveniles in the Snake River basin spent their first winter in a reservoir and resumed seaward movement the following spring at age 1 (hereafter, reservoir-type juveniles). We collected wild and hatchery ocean-type fall Chinook salmon juveniles in 1997 and wild and hatchery reservoir-type juveniles in 1998 to assess the condition of the reservoir-type juveniles at the onset of seaward movement. The ocean-type juveniles averaged 112-139 mm fork length, and the reservoir-type juveniles averaged 222-224 mm fork length. The large size of the reservoir-type juveniles suggested a high potential for survival to salt water and subsequent return to freshwater. Scale pattern analyses of the fall Chinook salmon spawners we collected during 1998-2003 supported this point. Of the spawners sampled, an overall average of 41% of the wild fish and 51% of the hatchery fish had been reservoir-type juveniles. Males that had been reservoir-type juveniles often returned as small \"minijacks\" (wild, 16% of total; hatchery, 40% of total), but 84% of the wild males, 60% of the hatchery males, and 100% of the wild and hatchery females that had been reservoir-type juveniles returned at ages and fork lengths commonly observed in populations of Chinook salmon. We conclude that fall Chinook salmon in the Snake River basin exhibit two alternative juvenile life histories, namely ocean-type and reservoir-type. ?? Copyright by the American Fisheries Society 2005.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/T03-131.1","issn":"00028487","usgsCitation":"Connor, W., Sneva, J., Tiffan, K., Steinhorst, R., and Ross, D., 2005, Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin: Transactions of the American Fisheries Society, v. 134, no. 2, p. 291-304, https://doi.org/10.1577/T03-131.1.","productDescription":"14 p.","startPage":"291","endPage":"304","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":236791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210005,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T03-131.1"}],"country":"United States","state":"Idaho, Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.76293945312499,\n              43.84245116699036\n            ],\n            [\n              -116.38916015624999,\n              42.85985981506279\n            ],\n            [\n              -117.48779296875,\n              44.000717834282774\n            ],\n            [\n              -117.520751953125,\n              45.87471224890479\n            ],\n            [\n              -118.004150390625,\n              46.41513877649202\n            ],\n            [\n              -119.44335937499999,\n              45.67548217560647\n            ],\n            [\n              -123.12377929687499,\n              45.42158812329091\n            ],\n            [\n              -124.002685546875,\n              46.057985244793024\n            ],\n            [\n              -123.93676757812499,\n              46.33175800051563\n            ],\n            [\n              -122.882080078125,\n              46.263442671779885\n            ],\n            [\n              -122.354736328125,\n              45.81348649679971\n            ],\n            [\n              -120.60791015625,\n              46.03510927947334\n            ],\n            [\n              -119.124755859375,\n              46.34692761055676\n            ],\n            [\n              -118.311767578125,\n              46.74738913515841\n            ],\n            [\n              -116.60888671874999,\n              46.73233101286786\n            ],\n            [\n              -116.290283203125,\n              46.36209301204985\n            ],\n            [\n              -116.03759765625,\n              44.645208223744035\n            ],\n            [\n              -115.850830078125,\n              44.10336537791152\n            ],\n            [\n              -115.76293945312499,\n              43.84245116699036\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"134","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505bb94ae4b08c986b327bac","contributors":{"authors":[{"text":"Connor, W.P.","contributorId":98090,"corporation":false,"usgs":true,"family":"Connor","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":420138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sneva, J.G.","contributorId":7066,"corporation":false,"usgs":true,"family":"Sneva","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":420135,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tiffan, K.F.","contributorId":19327,"corporation":false,"usgs":true,"family":"Tiffan","given":"K.F.","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":420136,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steinhorst, R.K.","contributorId":89833,"corporation":false,"usgs":true,"family":"Steinhorst","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":420137,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ross, D.","contributorId":7049,"corporation":false,"usgs":true,"family":"Ross","given":"D.","affiliations":[],"preferred":false,"id":420134,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028766,"text":"70028766 - 2005 - Bison PRNP genotyping and potential association with Brucella spp. seroprevalence","interactions":[],"lastModifiedDate":"2015-12-11T14:43:30","indexId":"70028766","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":776,"text":"Animal Genetics","active":true,"publicationSubtype":{"id":10}},"title":"Bison PRNP genotyping and potential association with Brucella spp. seroprevalence","docAbstract":"<p>The implication that host cellular prion protein (PrPC) may function as a cell surface receptor and/or portal protein for Brucella abortus in mice prompted an evaluation of nucleotide and amino acid variation within exon 3 of the prion protein gene (PRNP) for six US bison populations. A non-synonymous single nucleotide polymorphism (T50C), resulting in the predicted amino acid replacement M17T (Met ??? Thr), was identified in each population. To date, no variation (T50: Met) has been detected at the corresponding exon 3 nucleotide and/or amino acid position for domestic cattle. Notably, 80% (20 of 25) of the Yellowstone National Park bison possessing the C/C genotype were Brucella spp. seropositive, representing a significant (P = 0.021) association between seropositivity and the C/C genotypic class. Moreover, significant differences in the distribution of PRNP exon 3 alleles and genotypes were detected between Yellowstone National Park bison and three bison populations that were either founded from seronegative stock or previously subjected to test-and-slaughter management to eradicate brucellosis. Unlike domestic cattle, no indel polymorphisms were detected within the corresponding regions of the putative bison PRNP promoter, intron 1, octapeptide repeat region or 3???-untranslated region for any population examined. This study provides the first evidence of a potential association between nucleotide variation within PRNP exon 3 and the presence of Brucella spp. antibodies in bison, implicating PrPC in the natural resistance of bison to brucellosis infection. ?? 2005 International Society for Animal Genetics.</p>","language":"English","publisher":"International Society for Animal Genetics","doi":"10.1111/j.1365-2052.2005.01240.x","issn":"02689146","usgsCitation":"Seabury, C., Halbert, N., Gogan, P., Templeton, J., and Derr, J., 2005, Bison PRNP genotyping and potential association with Brucella spp. seroprevalence: Animal Genetics, v. 36, no. 2, p. 104-110, https://doi.org/10.1111/j.1365-2052.2005.01240.x.","productDescription":"7 p.","startPage":"104","endPage":"110","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science 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,{"id":70028800,"text":"70028800 - 2005 - Foliation development and reaction softening by dissolution and precipitation in the transformation of granodiorite to orthogneiss, Glastonbury Complex, Connecticut, U.S.A","interactions":[],"lastModifiedDate":"2021-06-11T13:49:24.257578","indexId":"70028800","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1177,"text":"Canadian Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Foliation development and reaction softening by dissolution and precipitation in the transformation of granodiorite to orthogneiss, Glastonbury Complex, Connecticut, U.S.A","docAbstract":"<p><span>Textures, microstructures, and patterns of chemical zoning in minerals in a granodioritic orthogneiss in the Glastonbury Complex, Connecticut, lead to the interpretation that foliation development was facilitated by retrograde hydration reactions in the presence of an aqueous fluid. Incomplete replacement of the metastable magmatic minerals K-feldspar + hastingsite + magnetite produced foliation-defining biotite + epidote + quartz. These reaction products did not replace K-feldspar – hastingsite interfaces; rather, either biotite or epidote replaced the amphibole, and plagioclase replaced K-feldspar. Biotite and epidote precipitated syntectonically in discrete layers that define the foliation in the orthogneiss, whereas quartz precipitated primarily in ribbons, further enhancing the fabric. Metastable REE-rich igneous titanite also dissolved, and was incompletely replaced by REE-poor, Al-bearing metamorphic titanite. The similar concentrations of the REE in epidote and titanite show that the REE released by titanite dissolution were precipitated locally as the allanite component in adjacent grains of epidote. The entire process was syntectonic, with most grains showing multiple overgrowths in the direction of extension as defined by stretched xenoliths. Sufficient U was present in the titanite overgrowths to allow SHRIMP dating of cores, mantles, and rims. These results suggest at least three retrograde Alleghanian events of growth in a span of ~30 m.y. Thus the dissolution – transportation –precipitation process not only describes the reaction mechanism but also leads to the redistribution of reaction products into nearly monomineralic layers, thus contributing to metamorphic differentiation and to the development of the foliation. The resulting orthogneiss was much weaker that the granodiorite protolith, owing to this reaction and textural softening.</span></p>","language":"English","publisher":"Mineralogical Association of Canada","doi":"10.2113/gscanmin.43.1.327","usgsCitation":"Wintsch, R., Aleinikoff, J.N., and Yi, K., 2005, Foliation development and reaction softening by dissolution and precipitation in the transformation of granodiorite to orthogneiss, Glastonbury Complex, Connecticut, U.S.A: Canadian Mineralogist, v. 43, no. 1, p. 327-347, https://doi.org/10.2113/gscanmin.43.1.327.","productDescription":"21 p.","startPage":"327","endPage":"347","numberOfPages":"21","costCenters":[],"links":[{"id":236756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut","otherGeospatial":"Glastonbury Complex","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.652587890625,\n              41.67598909594535\n            ],\n            [\n              -72.57877349853516,\n              41.67598909594535\n            ],\n            [\n              -72.57877349853516,\n              41.731354910056446\n            ],\n            [\n              -72.652587890625,\n              41.731354910056446\n            ],\n            [\n              -72.652587890625,\n              41.67598909594535\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"43","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a12afe4b0c8380cd543d8","contributors":{"authors":[{"text":"Wintsch, R. P.","contributorId":104921,"corporation":false,"usgs":false,"family":"Wintsch","given":"R. P.","affiliations":[{"id":13366,"text":"Indiana University, Bloomington, Indiana, USA","active":true,"usgs":false}],"preferred":false,"id":419803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aleinikoff, J. N. 0000-0003-3494-6841","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":75132,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":419801,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yi, K.","contributorId":104271,"corporation":false,"usgs":false,"family":"Yi","given":"K.","affiliations":[],"preferred":false,"id":419802,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028791,"text":"70028791 - 2005 - The soil physics contributions of Edgar Buckingham","interactions":[],"lastModifiedDate":"2018-10-31T10:12:53","indexId":"70028791","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"The soil physics contributions of Edgar Buckingham","docAbstract":"<p><span>During 1902 to 1906 as a soil physicist at the USDA Bureau of Soils (BOS), Edgar Buckingham originated the concepts of matric potential, soil–water retention curves, specific water capacity, and unsaturated hydraulic conductivity (</span><i>K</i><span>) as a distinct property of a soil. He applied a formula equivalent to Darcy's law (though without specific mention of Darcy's work) to unsaturated flow. He also contributed significant research on quasi-empirical formulas for&nbsp;</span><i>K</i><span>as a function of water content, water flow in capillary crevices and in thin films, and scaling. Buckingham's work on gas flow in soils produced paradigms that are consistent with our current understanding. His work on evaporation elucidated the concept of self-mulching and produced sound and sometimes paradoxical generalizations concerning conditions that favor or retard evaporation. Largely overshadowing those achievements, however, is that he launched a theory, still accepted today, that could predict transient water content as a function of time and space. Recently discovered documents reveal some of the arguments Buckingham had with BOS officials, including the text of a two-paragraph conclusion of his famous 1907 report on soil water, and the official letter documenting rejection of that text. Strained interpersonal relations motivated the departure of Buckingham and other brilliant physicists (N.E. Dorsey, F.H. King, and Lyman Briggs) from the BOS during 1903 to 1906. Given that Buckingham and his BOS colleagues had been rapidly developing the means of quantifying unsaturated flow, these strained relations probably slowed the advancement of unsaturated flow theory.</span></p>","language":"English","publisher":"ACSESS","doi":"10.2136/sssaj2005.0328","issn":"03615995","usgsCitation":"Nimmo, J., and Landa, E.R., 2005, The soil physics contributions of Edgar Buckingham: Soil Science Society of America Journal, v. 69, no. 2, p. 328-342, https://doi.org/10.2136/sssaj2005.0328.","productDescription":"15 p.","startPage":"328","endPage":"342","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":236647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb03ce4b08c986b324d02","contributors":{"authors":[{"text":"Nimmo, J. R. 0000-0001-8191-1727","orcid":"https://orcid.org/0000-0001-8191-1727","contributorId":58304,"corporation":false,"usgs":true,"family":"Nimmo","given":"J. R.","affiliations":[],"preferred":false,"id":419766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landa, E. R.","contributorId":100002,"corporation":false,"usgs":true,"family":"Landa","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":419767,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028790,"text":"70028790 - 2005 - Physical controls on total and methylmercury concentrations in streams and lakes of the northeastern USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028790","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1479,"text":"Ecotoxicology","active":true,"publicationSubtype":{"id":10}},"title":"Physical controls on total and methylmercury concentrations in streams and lakes of the northeastern USA","docAbstract":"The physical factors controlling total mercury (HgT) and methylmercury (MeHg) concentrations in lakes and streams of northeastern USA were assessed in a regional data set containing 693 HgT and 385 corresponding MeHg concentrations in surface waters. Multiple regression models using watershed characteristics and climatic variables explained 38% or less of the variance in HgT and MeHg. Land cover percentages and soil permeability generally provided modest predictive power. Percent wetlands alone explained 19% of the variance in MeHg in streams at low-flow, and it was the only significant (p < 0.02) predictor for MeHg in lakes, albeit explaining only 7% of the variance. When stream discharge was added as a variable it became the dominant predictor for HgT in streams, improving the model r 2 from 0.19 to 0.38. Stream discharge improved the MeHg model more modestly, from r 2 of 0.25 to 0.33. Methylation efficiency (MeHg/HgT) was modeled well (r 2 of 0.78) when a seasonal term was incorporated (sine wave with annual period). Physical models explained 18% of the variance in fish Hg concentrations in 134 lakes and 55% in 20 reservoirs. Our results highlight the important role of seasonality and short-term hydrologic changes to the delivery of Hg to water bodies. ?? 2005 Springer Science+Business Media, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecotoxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10646-004-6264-z","issn":"09639292","usgsCitation":"Shanley, J.B., Kamman, N., Clair, T., and Chalmers, A., 2005, Physical controls on total and methylmercury concentrations in streams and lakes of the northeastern USA: Ecotoxicology, v. 14, no. 1-2, p. 125-134, https://doi.org/10.1007/s10646-004-6264-z.","startPage":"125","endPage":"134","numberOfPages":"10","costCenters":[],"links":[{"id":209872,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10646-004-6264-z"},{"id":236615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7aa4e4b0c8380cd78ffc","contributors":{"authors":[{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":419763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kamman, N.C.","contributorId":51079,"corporation":false,"usgs":true,"family":"Kamman","given":"N.C.","affiliations":[],"preferred":false,"id":419762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clair, T.A.","contributorId":84529,"corporation":false,"usgs":true,"family":"Clair","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":419764,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chalmers, A.","contributorId":96858,"corporation":false,"usgs":true,"family":"Chalmers","given":"A.","email":"","affiliations":[],"preferred":false,"id":419765,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028768,"text":"70028768 - 2005 - Estimation and mapping of wet and dry mercury deposition across northeastern North America","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70028768","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1479,"text":"Ecotoxicology","active":true,"publicationSubtype":{"id":10}},"title":"Estimation and mapping of wet and dry mercury deposition across northeastern North America","docAbstract":"Whereas many ecosystem characteristics and processes influence mercury accumulation in higher trophic-level organisms, the mercury flux from the atmosphere to a lake and its watershed is a likely factor in potential risk to biota. Atmospheric deposition clearly affects mercury accumulation in soils and lake sediments. Thus, knowledge of spatial patterns in atmospheric deposition may provide information for assessing the relative risk for ecosystems to exhibit excessive biotic mercury contamination. Atmospheric mercury concentrations in aerosol, vapor, and liquid phases from four observation networks were used to estimate regional surface concentration fields. Statistical models were developed to relate sparsely measured mercury vapor and aerosol concentrations to the more commonly measured mercury concentration in precipitation. High spatial resolution deposition velocities for different phases (precipitation, cloud droplets, aerosols, and reactive gaseous mercury (RGM)) were computed using inferential models. An empirical model was developed to estimate gaseous elemental mercury (GEM) deposition. Spatial patterns of estimated total mercury deposition were complex. Generally, deposition was higher in the southwest and lower in the northeast. Elevation, land cover, and proximity to urban areas modified the general pattern. The estimated net GEM and RGM fluxes were each greater than or equal to wet deposition in many areas. Mercury assimilation by plant foliage may provide a substantial input of methyl-mercury (MeHg) to ecosystems. ?? 2005 Springer Science+Business Media, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecotoxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10646-004-6259-9","issn":"09639292","usgsCitation":"Miller, E., Vanarsdale, A., Keeler, G., Chalmers, A., Poissant, L., Kamman, N., and Brulotte, R., 2005, Estimation and mapping of wet and dry mercury deposition across northeastern North America: Ecotoxicology, v. 14, no. 1-2, p. 53-70, https://doi.org/10.1007/s10646-004-6259-9.","startPage":"53","endPage":"70","numberOfPages":"18","costCenters":[],"links":[{"id":477895,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/2027.42/44443>","text":"External Repository"},{"id":209640,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10646-004-6259-9"},{"id":236303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0b72e4b0c8380cd52718","contributors":{"authors":[{"text":"Miller, E. K.","contributorId":9832,"corporation":false,"usgs":true,"family":"Miller","given":"E. K.","affiliations":[],"preferred":false,"id":419673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vanarsdale, A.","contributorId":44341,"corporation":false,"usgs":true,"family":"Vanarsdale","given":"A.","email":"","affiliations":[],"preferred":false,"id":419675,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keeler, G.J.","contributorId":96449,"corporation":false,"usgs":true,"family":"Keeler","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":419678,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chalmers, A.","contributorId":96858,"corporation":false,"usgs":true,"family":"Chalmers","given":"A.","email":"","affiliations":[],"preferred":false,"id":419679,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Poissant, L.","contributorId":35493,"corporation":false,"usgs":true,"family":"Poissant","given":"L.","email":"","affiliations":[],"preferred":false,"id":419674,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kamman, N.C.","contributorId":51079,"corporation":false,"usgs":true,"family":"Kamman","given":"N.C.","affiliations":[],"preferred":false,"id":419677,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Brulotte, R.","contributorId":47140,"corporation":false,"usgs":true,"family":"Brulotte","given":"R.","email":"","affiliations":[],"preferred":false,"id":419676,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70028873,"text":"70028873 - 2005 - Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028873","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia","docAbstract":"Increased tree growth in temperate and boreal forests has been proposed as a direct consequence of a warming climate. Acid deposition effects on nutrient availability may influence the climate dependency of tree growth, however. This study presents an analysis of archived soil samples that has enabled changes in soil chemistry to be tracked with patterns of tree growth through the 20th century. Soil samples collected in 1926, 1964, and 2001, near St. Petersburg, Russia, showed that acid deposition was likely to have decreased root-available concentrations of Ca (an essential element) and increased root-available concentrations of Al (an inhibitor of Ca uptake). These soil changes coincided with decreased diameter growth and a suppression of climate-tree growth relationships in Norway spruce. Expected increases in tree growth from climate warming may be limited by decreased soil fertility in regions of northern and eastern Europe, and eastern North America, where Ca availability has been reduced by acidic deposition. ?? 2005 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es048759o","issn":"0013936X","usgsCitation":"Lawrence, G., Lapenis, A., Berggren, D., Aparin, B., Smith, K., Shortle, W., Bailey, S., Varlyguin, D., and Babikov, B., 2005, Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia: Environmental Science & Technology, v. 39, no. 7, p. 2004-2010, https://doi.org/10.1021/es048759o.","startPage":"2004","endPage":"2010","numberOfPages":"7","costCenters":[],"links":[{"id":209981,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es048759o"},{"id":236761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"7","noUsgsAuthors":false,"publicationDate":"2005-02-16","publicationStatus":"PW","scienceBaseUri":"5059f651e4b0c8380cd4c6b1","contributors":{"authors":[{"text":"Lawrence, G.B. 0000-0002-8035-2350","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":76347,"corporation":false,"usgs":true,"family":"Lawrence","given":"G.B.","affiliations":[],"preferred":false,"id":420130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapenis, A.G.","contributorId":85701,"corporation":false,"usgs":true,"family":"Lapenis","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":420132,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berggren, D.","contributorId":35531,"corporation":false,"usgs":true,"family":"Berggren","given":"D.","email":"","affiliations":[],"preferred":false,"id":420128,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aparin, B.F.","contributorId":24899,"corporation":false,"usgs":true,"family":"Aparin","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":420126,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, K.T.","contributorId":94807,"corporation":false,"usgs":true,"family":"Smith","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":420133,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shortle, W.C.","contributorId":20919,"corporation":false,"usgs":true,"family":"Shortle","given":"W.C.","affiliations":[],"preferred":false,"id":420125,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bailey, S.W.","contributorId":29113,"corporation":false,"usgs":true,"family":"Bailey","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":420127,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Varlyguin, D.L.","contributorId":84967,"corporation":false,"usgs":true,"family":"Varlyguin","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":420131,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Babikov, B.","contributorId":71752,"corporation":false,"usgs":true,"family":"Babikov","given":"B.","email":"","affiliations":[],"preferred":false,"id":420129,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70028876,"text":"70028876 - 2005 - Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028876","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1905,"text":"Holocene","active":true,"publicationSubtype":{"id":10}},"title":"Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada","docAbstract":"The north-flowing, low-gradient section of the Red River in Manitoba has lost ???60% of its valley gradient since 8 ka cal. BP. An existing hydraulic model of the modern Red River flood zone was used to examine the change in flood extent and depth of a discharge equivalent to the 1997 Red River flood (3970 m3/s) for scenarios of gradients at 8, 6, 4 and 2 ka cal. BP as well as 2 ka in the future. The modelling indicates a broad, shallow flood zone for all of the gradient scenarios, with extent and depth increasing over time. Between the 8 ka cal. BP and present-day scenarios, the flood zone increased from 1186 km2 to 1531 km2 (???29%) with depth increasing along four east-west cross-sections by 0.69 m (???61%), 0.91 m (???82%), 0.56 m (???64%) and 0.48 m (???86%). The flood extent and depths increased by a further 18 km2 (???5%) and 0.04-0.06 m (2-5%), respectively, by 2 ka in the future. Most of these changes to the flood zone occurred between 8 and 2 ka cal. BP, reflecting an exponential loss of gradient. A rise in flood depth equivalent to that which occurred between 8 ka cal. BP and the present-day, is assessed as increasing the long-term flood hazard; in contrast, the slight rise in depth between the present-day and 2 ka in the future does not. ?? 2005 Edward Arnold (Publishers) Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Holocene","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1191/0959683605hl804rp","issn":"09596836","usgsCitation":"Brooks, G.R., Thorleifson, L.H., and Lewis, C., 2005, Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada: Holocene, v. 15, no. 3, p. 347-352, https://doi.org/10.1191/0959683605hl804rp.","startPage":"347","endPage":"352","numberOfPages":"6","costCenters":[],"links":[{"id":210006,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1191/0959683605hl804rp"},{"id":236793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-04-01","publicationStatus":"PW","scienceBaseUri":"505a3b50e4b0c8380cd62401","contributors":{"authors":[{"text":"Brooks, G. R.","contributorId":96312,"corporation":false,"usgs":true,"family":"Brooks","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":420141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorleifson, L. Harvey","contributorId":103430,"corporation":false,"usgs":true,"family":"Thorleifson","given":"L.","email":"","middleInitial":"Harvey","affiliations":[{"id":38105,"text":"Minnesota Geological Survey","active":true,"usgs":false}],"preferred":false,"id":420142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, C.F.M.","contributorId":39971,"corporation":false,"usgs":true,"family":"Lewis","given":"C.F.M.","email":"","affiliations":[],"preferred":false,"id":420140,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028867,"text":"70028867 - 2005 - Offshore marine observation of Willow Ptarmigan, including water landings, Kuskokwim Bay, Alaska","interactions":[],"lastModifiedDate":"2017-03-21T17:40:17","indexId":"70028867","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":"Offshore marine observation of Willow Ptarmigan, including water landings, Kuskokwim Bay, Alaska","docAbstract":"<p>We report an observation of Willow Ptarmigan (<i>Lagopus lagopus</i>) encountered 8 to 17 km from the nearest shoreline on Kuskokwim Bay, Alaska, on 30 August 2003. The ptarmigan were observed flying, landing on our research vessel, and landing and taking off from the water surface. We also report on one other observation of ptarmigan sitting on the water surface and other marine observations of ptarmigan from the North Pacific Pelagic Seabird Database. These observations provide evidence that Willow Ptarmigan are capable of dispersing across large bodies of water and landing and taking off from the water surface.</p>","language":"English","publisher":"Wilson Ornithological Society","doi":"10.1676/04-074","issn":"00435643","usgsCitation":"Zimmerman, C.E., Hillgruber, N., Burril, S., St. Peters, M.A., and Wetzel, J.D., 2005, Offshore marine observation of Willow Ptarmigan, including water landings, Kuskokwim Bay, Alaska: The Wilson Bulletin, v. 117, no. 1, p. 12-14, https://doi.org/10.1676/04-074.","productDescription":"3 p.","startPage":"12","endPage":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":477823,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1676/04-074","text":"External Repository"},{"id":236654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kuskokwim Bay","volume":"117","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6cb8e4b0c8380cd74da6","contributors":{"authors":[{"text":"Zimmerman, Christian E. 0000-0002-3646-0688 czimmerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3646-0688","contributorId":410,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Christian","email":"czimmerman@usgs.gov","middleInitial":"E.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true}],"preferred":true,"id":420100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hillgruber, Nicola","contributorId":138856,"corporation":false,"usgs":false,"family":"Hillgruber","given":"Nicola","email":"","affiliations":[{"id":12548,"text":"University of Alaska Fairbanks, School of Fisheries and Ocean Sciences","active":true,"usgs":false}],"preferred":false,"id":420102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burril, Sean E.","contributorId":56183,"corporation":false,"usgs":true,"family":"Burril","given":"Sean E.","affiliations":[],"preferred":false,"id":420101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"St. Peters, Michelle A.","contributorId":25744,"corporation":false,"usgs":false,"family":"St. Peters","given":"Michelle","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":420099,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wetzel, Jennifer D.","contributorId":92861,"corporation":false,"usgs":false,"family":"Wetzel","given":"Jennifer","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":420103,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028866,"text":"70028866 - 2005 - Spartina alterniflora genotype influences facilitation and suppression of high marsh species colonizing an early successional salt marsh","interactions":[],"lastModifiedDate":"2019-04-29T09:54:18","indexId":"70028866","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2242,"text":"Journal of Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Spartina alterniflora genotype influences facilitation and suppression of high marsh species colonizing an early successional salt marsh","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><ol class=\"rlist hanging\"><li><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span class=\"number\"></span></span>Genetically based phenotypic and ecotypic variation in a dominant plant species can influence ecological functions and patterns of recruitment by other species in plant communities. However, the nature and degree of importance of genotypic differences is poorly understood in most systems.</li><li>The dominant salt marsh species,&nbsp;<i>Spartina alterniflora</i>, is known to induce facilitative and competitive effects in different plant species, and the outcomes of interactions can be affected by nutrients and flooding stress. Clonal genotypes, which maintained their different plant architecture phenotypes throughout 31&nbsp;months of a field experiment, underwent considerable genet‐specific senescence in their centres over the last 12&nbsp;months.</li><li>Different clonal genotypes and different locations (robust edges vs. senescent centres) permitted significantly different levels of light penetration of the canopy (14.8–77.6%), thus establishing spatial heterogeneity for this important environmental factor.</li><li><i>S. alterniflora</i>&nbsp;clonal genotype influenced the degree of suppression of the previously dominant&nbsp;<i>Salicornia bigelovii</i>&nbsp;as well as facilitation of recruitment and growth by other plant species.&nbsp;<i>Aster subulatus</i>&nbsp;and&nbsp;<i>Atriplex patula</i>&nbsp;performed better in&nbsp;<i>Spartina</i>clone centres, and experienced reduced growth in&nbsp;<i>Salicornia</i>‐dominated areas.</li><li>Four other high marsh species (<i>Borrichia frutescens</i>,&nbsp;<i>Aster tenuifolius</i>,&nbsp;<i>Iva frutescens</i>and&nbsp;<i>Limonium carolinianum</i>) colonized only into&nbsp;<i>Spartina</i>&nbsp;clones but not into the&nbsp;<i>Salicornia</i>‐dominated area.</li><li>These results suggest that differences in clone size, centre senescence, stem density, height, total stem length and biomass in different genotypes of a dominant marsh plant species can influence recruitment and growth of other plant species. The spatial pattern of habitat heterogeneity is, at least in part, dependent on the genotypic diversity, and possibly the genetic diversity, of such foundation species.</li><li>We hypothesize that as genotypic diversity increases in populations of a dominant plant species like&nbsp;<i>S. alterniflora</i>, the number and diversity of interactions with other species will increase as well.</li></ol></div></div>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.0022-0477.2005.00983.x","issn":"00220477","usgsCitation":"Proffitt, C., Chiasson, R., Owens, A., Edwards, K., and Travis, S., 2005, Spartina alterniflora genotype influences facilitation and suppression of high marsh species colonizing an early successional salt marsh: Journal of Ecology, v. 93, no. 2, p. 404-416, https://doi.org/10.1111/j.0022-0477.2005.00983.x.","productDescription":"13 p.","startPage":"404","endPage":"416","numberOfPages":"13","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":236653,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-03-09","publicationStatus":"PW","scienceBaseUri":"505b9413e4b08c986b31a856","contributors":{"authors":[{"text":"Proffitt, C.E. 0000-0002-0845-8441","orcid":"https://orcid.org/0000-0002-0845-8441","contributorId":47339,"corporation":false,"usgs":true,"family":"Proffitt","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":420098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chiasson, R.L.","contributorId":41942,"corporation":false,"usgs":true,"family":"Chiasson","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":420097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Owens, A.B.","contributorId":24156,"corporation":false,"usgs":true,"family":"Owens","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":420094,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, K.R.","contributorId":37127,"corporation":false,"usgs":true,"family":"Edwards","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":420096,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Travis, S.E. 0000-0001-9338-8953","orcid":"https://orcid.org/0000-0001-9338-8953","contributorId":28718,"corporation":false,"usgs":true,"family":"Travis","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":420095,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028781,"text":"70028781 - 2005 - Effect of sample handling on thiamine and thiaminolytic activity in alewife","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028781","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2177,"text":"Journal of Aquatic Animal Health","active":true,"publicationSubtype":{"id":10}},"title":"Effect of sample handling on thiamine and thiaminolytic activity in alewife","docAbstract":"Alewives Alosa pseudoharengus were collected to evaluate handling and processing conditions that may affect the measurement of their thiamine-thiaminase content. Fish were captured by otter trawl, and reference samples of live fish were quick-frozen on dry ice immediately following capture. Other samples were placed on wet ice (4??C) or held in ambient lake water (21.5??C) for periods of up to 5 h before freezing. Total thiamine levels for reference samples averaged 26 nmol/g and consisted of 66, 15, and 19% thiamine pyrophosphate (TPP), thiamine monophosphate (TMP), and unphosphorylated thiamine (Th), respectively. After 120 min at either 4??C or 21.5??C, total thiamine concentrations were lower. At 21.5??C, the TPP proportion had decreased by 30 min and the proportion as Th increased after 60 min. In the groups sampled after 5 h, total thiamine concentrations were not altered but the proportion of TPP was lower and that of Th was higher than in reference samples. The stability of thiamine in thawed muscle samples from previously frozen alewives was poor (40% loss by 1 h at 22??C and 30% loss by 2 h at 4??C). Thiaminase activity averaged 5,975 pmol??g wet weight -1??min-1 in reference samples. In fresh-caught alewives, thiaminase activities were remarkably consistent throughout the sampling period. At 4??C, thiaminase activity in muscle tissue from previously frozen alewives was stable for the entire investigation period. At 25??C, the activity initially increased by 40% after 60 min but then decreased to 50% of initial value after 5 h. We conclude that sampling times greater than 25 min could cause some changes in the various thiamine forms and net loss in total thiamine. The thiamine content in previously frozen alewife samples is highly labile, requiring low temperatures during processing for analysis. ?? Copyright by the American Fisheries Society 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Aquatic Animal Health","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/H03-074.1","issn":"08997659","usgsCitation":"Wright, G., Brown, S., Brown, L., Moore, K., Villella, M., Zajicek, J., Tillitt, D.E., Fitzsimons, J., and Honeyfield, D., 2005, Effect of sample handling on thiamine and thiaminolytic activity in alewife: Journal of Aquatic Animal Health, v. 17, no. 1, p. 77-81, https://doi.org/10.1577/H03-074.1.","startPage":"77","endPage":"81","numberOfPages":"5","costCenters":[],"links":[{"id":209771,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/H03-074.1"},{"id":236479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-03-01","publicationStatus":"PW","scienceBaseUri":"505a0603e4b0c8380cd51097","contributors":{"authors":[{"text":"Wright, G.M.","contributorId":104851,"corporation":false,"usgs":true,"family":"Wright","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":419733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, S.B.","contributorId":107636,"corporation":false,"usgs":true,"family":"Brown","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":419734,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, L. R. 0000-0001-6702-4531","orcid":"https://orcid.org/0000-0001-6702-4531","contributorId":66391,"corporation":false,"usgs":true,"family":"Brown","given":"L. R.","affiliations":[],"preferred":false,"id":419728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, K.","contributorId":64432,"corporation":false,"usgs":true,"family":"Moore","given":"K.","email":"","affiliations":[],"preferred":false,"id":419727,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Villella, M.","contributorId":91673,"corporation":false,"usgs":true,"family":"Villella","given":"M.","email":"","affiliations":[],"preferred":false,"id":419732,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zajicek, J.L.","contributorId":87086,"corporation":false,"usgs":true,"family":"Zajicek","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":419731,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tillitt, D. E.","contributorId":83462,"corporation":false,"usgs":true,"family":"Tillitt","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":419730,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fitzsimons, J.D.","contributorId":50845,"corporation":false,"usgs":true,"family":"Fitzsimons","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":419726,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Honeyfield, D. C. 0000-0003-3034-2047","orcid":"https://orcid.org/0000-0003-3034-2047","contributorId":73136,"corporation":false,"usgs":true,"family":"Honeyfield","given":"D. C.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":419729,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70028855,"text":"70028855 - 2005 - Distribution, foraging behavior, and capture results of the spotted bat (Euderma maculatum) in central Oregon","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70028855","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3746,"text":"Western North American Naturalist","onlineIssn":"1944-8341","printIssn":"1527-0904","active":true,"publicationSubtype":{"id":10}},"title":"Distribution, foraging behavior, and capture results of the spotted bat (Euderma maculatum) in central Oregon","docAbstract":"The spotted bat (Euderma maculatum) has been virtually unknown in Oregon despite the existence of potential habitat in many areas of the state. In 2002 and 2003 we searched for spotted bats along the John Day, Deschutes, and Crooked Rivers and at a remote dry canyon southeast of the city of Bend in central Oregon. The species was documented through the use of mist-nets, a bat detector, and recognition of audible spotted bat calls. Spotted bats were found at 11 locations in 6 Oregon counties. Nightly activity patterns of spotted bats were unpredictable. Spotted bats were found in 78% of search areas but on only 48% of survey nights. We observed spotted bats foraging above fields and low upland slopes adjacent to rivers and creeks and along the rims of cliffs. Estimated flying heights of spotted bats ranged from 3 m to 50 m aboveground. The species was difficult to capture and was captured only after considerable experimentation with methods and materials. Three spotted bats were captured toward the end of the project in 2003 and accounted for only 0.5% of all bats captured during the study. Although we attached radio transmitters to 2 spotted bats, we found no roost locations. We believe additional spotted bat surveys in Oregon are warranted, especially in higher-elevation habitats, but recommend that to increase their effectiveness, surveys accommodate the unique foraging behavior of the species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Western North American Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"15270904","usgsCitation":"Rodhouse, T., McCaffrey, M., and Wright, R., 2005, Distribution, foraging behavior, and capture results of the spotted bat (Euderma maculatum) in central Oregon: Western North American Naturalist, v. 65, no. 2, p. 215-222.","startPage":"215","endPage":"222","numberOfPages":"8","costCenters":[],"links":[{"id":236482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a031ee4b0c8380cd5034f","contributors":{"authors":[{"text":"Rodhouse, T.J.","contributorId":10978,"corporation":false,"usgs":true,"family":"Rodhouse","given":"T.J.","affiliations":[],"preferred":false,"id":420035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCaffrey, M.F.","contributorId":90095,"corporation":false,"usgs":true,"family":"McCaffrey","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":420036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, R.G.","contributorId":9622,"corporation":false,"usgs":true,"family":"Wright","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":420034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013554,"text":"1013554 - 2005 - Allocating harvests among polar bear stocks in the Beaufort Sea","interactions":[],"lastModifiedDate":"2021-06-07T15:20:33.189421","indexId":"1013554","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":894,"text":"Arctic","active":true,"publicationSubtype":{"id":10}},"title":"Allocating harvests among polar bear stocks in the Beaufort Sea","docAbstract":"<p><span>Recognition that polar bears are shared by hunters in Canada and Alaska prompted development of the “Polar Bear Management Agreement for the Southern Beaufort Sea.” Under this Agreement, the harvest of polar bears from the southern Beaufort Sea (SBS) is shared between Inupiat hunters of Alaska and Inuvialuit hunters of Canada. Quotas for each jurisdiction are to be reviewed annually in light of the best available scientific information. Ideal implementation of the Agreement has been hampered by the inability to quantify geographic overlap among bears from adjacent populations. We applied new analytical procedures to a more extensive radiotelemetry data set than has previously been available to quantify that overlap and thereby improve the efficacy of the Agreement. We constructed a grid over the eastern Chukchi Sea and Beaufort Sea and used twodimensional kernel smoothing to assign probabilities to the distributions of all instrumented bears. A cluster analysis of radio relocation data identified three relatively discrete groups or “populations” of polar bears: the SBS, Chukchi Sea (CS), and northern Beaufort Sea (NBS) populations. With kernel smoothing, we calculated relative probabilities of occurrence for individual members of each population in each cell of our grid. We estimated the uncertainty in probabilities by bootstrapping. Availability of polar bears from each population varied geographically. Near Barrow, Alaska, 50% of harvested bears are from the CS population and 50% from the SBS population. Nearly 99% of the bears taken by Kaktovik hunters are from the SBS. At Tuktoyaktuk, Northwest Territories, Canada, 50% are from the SBS and 50% from the NBS population. We displayed the occurrence of bears from each population as probabilities for each cell in our grid and as maps with contour lines delineating changes in relative probability. This new analytical approach will greatly improve the accuracy of allocating harvest quotas among hunting communities and jurisdictions while assuring that harvests remain within the bounds of sustainable yield.</span><br></p>","language":"English","publisher":"Arctic Institute of North America","doi":"10.14430/arctic426","usgsCitation":"Amstrup, S.C., Durner, G.M., Stirling, I., and McDonald, T.L., 2005, Allocating harvests among polar bear stocks in the Beaufort Sea: Arctic, v. 58, no. 3, p. 247-259, https://doi.org/10.14430/arctic426.","productDescription":"13 p.","startPage":"247","endPage":"259","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":477744,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.14430/arctic426","text":"External Repository"},{"id":128469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Alaska, Northwest Territories, Yukon","otherGeospatial":"Beaufort Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -126.826171875,\n              70.49557354093136\n            ],\n            [\n              -123.92578125,\n              74.18805166460048\n            ],\n            [\n              -147.65625,\n              74.47290269579455\n            ],\n            [\n              -155.478515625,\n              71.85622888185527\n            ],\n            [\n              -155.7421875,\n              70.52489722821652\n            ],\n            [\n              -136.669921875,\n              68.26938680456564\n            ],\n            [\n              -131.220703125,\n              68.49604022839505\n            ],\n            [\n              -126.826171875,\n              70.49557354093136\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"58","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-01-29","publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c286","contributors":{"authors":[{"text":"Amstrup, Steven C.","contributorId":67034,"corporation":false,"usgs":false,"family":"Amstrup","given":"Steven","email":"","middleInitial":"C.","affiliations":[{"id":13182,"text":"Polar Bears International","active":true,"usgs":false}],"preferred":false,"id":318761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durner, George M. 0000-0002-3370-1191 gdurner@usgs.gov","orcid":"https://orcid.org/0000-0002-3370-1191","contributorId":3576,"corporation":false,"usgs":true,"family":"Durner","given":"George","email":"gdurner@usgs.gov","middleInitial":"M.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":318760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stirling, I.","contributorId":103615,"corporation":false,"usgs":false,"family":"Stirling","given":"I.","email":"","affiliations":[],"preferred":false,"id":318763,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDonald, T. 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