{"pageNumber":"810","pageRowStart":"20225","pageSize":"25","recordCount":68927,"records":[{"id":70034666,"text":"70034666 - 2010 - Do larval fishes exhibit diel drift patterns in a large, turbid river?","interactions":[],"lastModifiedDate":"2012-03-12T17:21:41","indexId":"70034666","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2166,"text":"Journal of Applied Ichthyology","active":true,"publicationSubtype":{"id":10}},"title":"Do larval fishes exhibit diel drift patterns in a large, turbid river?","docAbstract":"Previous research suggested larval fishes do not exhibit a diel drift cycle in turbid rivers (transparency <30 cm). We evaluated this hypothesis in the turbid, lower Missouri River, Missouri. We also reviewed diel patterns of larval drift over a range of transparencies in rivers worldwide. Larval fishes were collected from the Missouri River primary channel every 4 h per 24-h period during spring-summer 2002. Water transparency was measured during this period and summarized for previous years. Diel drift patterns were analyzed at the assemblage level and lower taxonomic levels for abundant groups. Day and night larval fish catch-per-unit-effort (CPUE) was compared for the entire May through August sampling period and spring (May - June) and summer (July - August) seasons separately. There were no significant differences between day and night CPUE at the assemblage level for the entire sampling period or for the spring and summer seasons. However, Hiodon alosoides, Carpiodes/Ictiobus spp. and Macrhybopsis spp. exhibited a diel cycle of abundance within the drift. This pattern was evident although mean Secchi depth (transparency) ranged from 4 to 25 cm during the study and was <30 cm from May through August over the previous nine years. Larval diel drift studies from 48 rivers excluding the Missouri River indicated the primary drift period for larval fishes was at night in 38 rivers and during the day for five, with the remaining rivers showing no pattern. Water transparency was reported for 10 rivers with six being <30 cm or 'low'. Two of these six turbid rivers exhibited significant diel drift patterns. The effect of water transparency on diel drift of larval fishes appears taxa-specific and patterns of abundant taxa could mask patterns of rare taxa when analyzed only at the assemblage level. ?? 2010 Blackwell Verlag, Berlin.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Applied Ichthyology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1439-0426.2010.01481.x","issn":"01758659","usgsCitation":"Reeves, K., and Galat, D., 2010, Do larval fishes exhibit diel drift patterns in a large, turbid river?: Journal of Applied Ichthyology, v. 26, no. 4, p. 571-577, https://doi.org/10.1111/j.1439-0426.2010.01481.x.","startPage":"571","endPage":"577","numberOfPages":"7","costCenters":[],"links":[{"id":475796,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1439-0426.2010.01481.x","text":"Publisher Index Page"},{"id":215723,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1439-0426.2010.01481.x"},{"id":243545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-03-04","publicationStatus":"PW","scienceBaseUri":"505a0362e4b0c8380cd5046f","contributors":{"authors":[{"text":"Reeves, K.S.","contributorId":40824,"corporation":false,"usgs":true,"family":"Reeves","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":446941,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galat, D.L.","contributorId":54546,"corporation":false,"usgs":true,"family":"Galat","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":446942,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70034638,"text":"70034638 - 2010 - Occurrence of the Great Lake's most recent invader, <i>Hemimysis anomala</i>, in the diet of fishes in southeastern Lake Ontario","interactions":[],"lastModifiedDate":"2013-02-28T13:39:08","indexId":"70034638","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of the Great Lake's most recent invader, <i>Hemimysis anomala</i>, in the diet of fishes in southeastern Lake Ontario","docAbstract":"The Ponto-Caspian mysid, <i>Hemimysis anomala</i>, was first observed in southeastern Lake Ontario in May 2006. During July and August 2007, gill nets were fished in 6 to 8 m of water at two locations of known <i>Hemimysis</i> colonization in southeastern Lake Ontario to determine if fish that consume macroinvertebrates were beginning to include this new invasive mysid in their diets. Of nine fish species captured in August, September, and October 2007, three species had consumed <i>Hemimysis</i>: alewife (<i>Alosa pseudoharengus</i>), rock bass (<i>Ambloplites rupestris</i>), and yellow perch (<i>Perca flavescens</i>); and six species had not: round goby <i>Apollonia melanostoma</i>, smallmouth bass <i>Micropterus dolomieu</i>, spottail shiner <i>Notropis hudsonius</i>, gizzard shad <i>Dorosoma cepedianum</i>, white perch <i>Morone americana</i> and log perch <i>Percina caprodes</i>. Diets of alewives from all samples were composed predominantly of <i>Hemimysis</i> (69.6% -100% frequency of occurrence, 46.0%–74.5% dry weight diet composition). Two of 6 rock bass stomachs sampled in August contained ≥ 98.9% <i>Hemimysis</i> (10 and 40 individuals each) and one of 61 yellow perch stomachs sampled in September contained 10.0% <i>Hemimysis</i> (6 individuals) and 90.0% fish. While <i>Hemimysis</i> were observed only sparsely in the diet of most nearshore fish, their predominance in alewife diets and their omnivorous feeding behavior indicated that they have the potential to alter energy flow in Great Lakes' foodwebs.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.jglr.2009.12.002","issn":"03801330","usgsCitation":"Lantry, B., Walsh, M.G., Johnson, J.H., and McKenna, J., 2010, Occurrence of the Great Lake's most recent invader, <i>Hemimysis anomala</i>, in the diet of fishes in southeastern Lake Ontario: Journal of Great Lakes Research, v. 36, no. 1, p. 179-183, https://doi.org/10.1016/j.jglr.2009.12.002.","productDescription":"5 p.","startPage":"179","endPage":"183","costCenters":[{"id":357,"text":"Lake Ontario Biological Station","active":false,"usgs":true}],"links":[{"id":215779,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jglr.2009.12.002"},{"id":243604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Lake Ontario","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.1391,43.073 ], [ -80.1391,44.2705 ], [ -75.9829,44.2705 ], [ -75.9829,43.073 ], [ -80.1391,43.073 ] ] ] } } ] }","volume":"36","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6c39e4b0c8380cd74afe","contributors":{"authors":[{"text":"Lantry, B.F.","contributorId":19105,"corporation":false,"usgs":true,"family":"Lantry","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":446812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walsh, M. G.","contributorId":72172,"corporation":false,"usgs":true,"family":"Walsh","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":446814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, J. H.","contributorId":54914,"corporation":false,"usgs":true,"family":"Johnson","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":446813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKenna, J.E. Jr.","contributorId":106065,"corporation":false,"usgs":true,"family":"McKenna","given":"J.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":446815,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034636,"text":"70034636 - 2010 - Fine scale daily movements and habitat use of East Pacific green turtles at a shallow coastal lagoon in Baja California Sur, Mexico","interactions":[],"lastModifiedDate":"2017-05-17T09:25:51","indexId":"70034636","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2277,"text":"Journal of Experimental Marine Biology and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Fine scale daily movements and habitat use of East Pacific green turtles at a shallow coastal lagoon in Baja California Sur, Mexico","docAbstract":"<p>Green turtles spend most of their lives in coastal foraging areas where they face multiple anthropogenic impacts. Therefore, understanding their spatial use in this environment is a priority for conservation efforts. We studied the fine scale daily movements and habitat use of East Pacific green turtles (<i>Chelonia mydas</i>) at Laguna San Ignacio, a shallow coastal lagoon in Baja California Sur, Mexico where sea turtles are subject to high levels of gillnet bycatch and directed hunting. Six turtles ranging from 44.6 to 83.5&nbsp;cm in straight carapace length were tracked for short deployments (1 to 6 d) with GPS-VHF telemetry. Turtles were active throughout diurnal, nocturnal, and crepuscular periods. Although they moved greater total distances during daytime, their speed of travel and net displacement remained consistent throughout 24-h periods. A positive selection for areas of seagrass and moderate water depth (5 to 10&nbsp;m) was determined using Ivlev's electivity index, with neutral selection for shallow water (&lt;&nbsp;5&nbsp;m) and avoidance of deep water (&gt;&nbsp;10&nbsp;m). Turtles exhibited two distinct behavioral movement patterns: circular movements with high fidelity to the capture&ndash;release location and meandering movements with low fidelity to the capture&ndash;release location. Our results indicate that green turtles were active throughout the diel cycle while traveling large distances and traversing multiple habitats over short temporal scales.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jembe.2010.06.017","issn":"00220981","usgsCitation":"Senko, J., Koch, V., Megill, W.M., Carthy, R.R., Templeton, R.P., and Nichols, W.J., 2010, Fine scale daily movements and habitat use of East Pacific green turtles at a shallow coastal lagoon in Baja California Sur, Mexico: Journal of Experimental Marine Biology and Ecology, v. 391, no. 1-2, p. 92-100, https://doi.org/10.1016/j.jembe.2010.06.017.","productDescription":"9 p.","startPage":"92","endPage":"100","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-022304","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":243572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":215749,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jembe.2010.06.017"}],"country":"Mexico","state":"Baja California Sur","otherGeospatial":"Laguna San Ignacio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.05892944335936,\n              26.60756044926576\n            ],\n            [\n              -113.05343627929688,\n              26.64009391980515\n            ],\n            [\n              -113.15231323242186,\n              26.754807764968632\n            ],\n            [\n              -113.12759399414062,\n              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rayc@usgs.gov","orcid":"https://orcid.org/0000-0001-8978-5083","contributorId":3685,"corporation":false,"usgs":true,"family":"Carthy","given":"Raymond","email":"rayc@usgs.gov","middleInitial":"R.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":446796,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Templeton, R.obert P.","contributorId":44003,"corporation":false,"usgs":false,"family":"Templeton","given":"R.obert","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":446792,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nichols, Wallace J.","contributorId":81106,"corporation":false,"usgs":false,"family":"Nichols","given":"Wallace","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":446795,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034635,"text":"70034635 - 2010 - A late Miocene-early Pliocene chain of lakes fed by the Colorado River: Evidence from Sr, C, and O isotopes of the Bouse Formation and related units between Grand Canyon and the Gulf of California","interactions":[],"lastModifiedDate":"2021-12-03T15:31:17.791811","indexId":"70034635","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"A late Miocene-early Pliocene chain of lakes fed by the Colorado River: Evidence from Sr, C, and O isotopes of the Bouse Formation and related units between Grand Canyon and the Gulf of California","docAbstract":"<p><span>We report strontium isotopic results for the late Miocene Hualapai Limestone of the Lake Mead area (Arizona-Nevada) and the latest Miocene to early Pliocene Bouse Formation and related units of the lower Colorado River trough (Arizona-California-Nevada), together with parallel oxygen and carbon isotopic analyses of Bouse samples, to constrain the lake-overflow model for integration of the Colorado River. Sr isotopic analyses on the basal 1–5 cm of marl, in particular along a transect over a range of altitude in the lowest-altitude basin that contains freshwater, brackish, and marine fossils, document the&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr of first-arriving Bouse waters. Results reinforce the similarity between the&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr of Bouse Formation carbonates and present-day Colorado River water, and the systematic distinction of these values from Neogene marine Sr. Basal Bouse samples show that&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr decreased from 0.7111 to values in the range 0.7107–0.7109 during early basin filling.&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr values from a recently identified marl in the Las Vegas area are within the range of Bouse Sr ratios.&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr values from the Hualapai Limestone decrease upsection from 0.7195 to 0.7137, in the approach to a time soon after 6 Ma when Hualapai deposition ceased and the Colorado River became established through the Lake Mead area. Bouse Formation δ</span><sup>18</sup><span>O values range from –12.9‰ to +1.0‰ Vienna Pee Dee belemnite (VPDB), and δ</span><sup>13</sup><span>C between –6.5‰ and +3.4‰ VPDB. Negative δ</span><sup>18</sup><span>O values appear to require a continental origin for waters, and the trend to higher δ</span><sup>18</sup><span>O suggests evaporation in lake waters. Sr and stable isotopic results for sectioned barnacle shells and from bedding planes of the marine fish fossil&nbsp;</span><i>Colpichthys regis</i><span>&nbsp;demonstrate that these animals lived in saline freshwater, and that there is no evidence for incursions of marine water, either long-lived or brief in duration. Lack of correlation of Sr and O isotopic variations in the same samples also argue strongly against systematic replacement of Sr in Bouse carbonates after deposition. Our results reinforce the conclusion that the Bouse Formation was deposited in a descending series of basins connected by overflow of Colorado River water. The Hualapai Limestone records a separate and earlier lake that may have been progressively influenced by Colorado River water as the time of river integration approached.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/B30186.1","issn":"00167606","usgsCitation":"Roskowski, J.A., Patchett, P., Spencer, J., Pearthree, P., Dettman, D.L., Faulds, J.E., and Reynolds, A.C., 2010, A late Miocene-early Pliocene chain of lakes fed by the Colorado River: Evidence from Sr, C, and O isotopes of the Bouse Formation and related units between Grand Canyon and the Gulf of California: Geological Society of America Bulletin, v. 122, no. 9-10, p. 1625-1636, https://doi.org/10.1130/B30186.1.","productDescription":"12 p.","startPage":"1625","endPage":"1636","numberOfPages":"12","costCenters":[],"links":[{"id":243571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico, United States","state":"Arizona, Baja California, California, Nevada, Sonora","otherGeospatial":"Colorado River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.75195312499999,\n              31.38177878211098\n            ],\n            [\n              -113.99414062499999,\n              31.38177878211098\n            ],\n            [\n              -113.99414062499999,\n              35.96911507577482\n            ],\n            [\n              -115.75195312499999,\n              35.96911507577482\n            ],\n            [\n              -115.75195312499999,\n              31.38177878211098\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"122","issue":"9-10","noUsgsAuthors":false,"publicationDate":"2010-05-10","publicationStatus":"PW","scienceBaseUri":"5059e434e4b0c8380cd464c4","contributors":{"authors":[{"text":"Roskowski, J. A.","contributorId":95292,"corporation":false,"usgs":true,"family":"Roskowski","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":446789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patchett, P. J.","contributorId":55152,"corporation":false,"usgs":true,"family":"Patchett","given":"P. J.","affiliations":[],"preferred":false,"id":446785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spencer, J.E.","contributorId":91542,"corporation":false,"usgs":true,"family":"Spencer","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":446788,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearthree, P. A.","contributorId":77236,"corporation":false,"usgs":false,"family":"Pearthree","given":"P. A.","affiliations":[],"preferred":false,"id":446786,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dettman, D. L.","contributorId":100538,"corporation":false,"usgs":true,"family":"Dettman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":446790,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Faulds, J. E.","contributorId":84854,"corporation":false,"usgs":true,"family":"Faulds","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":446787,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Reynolds, A. C.","contributorId":35110,"corporation":false,"usgs":true,"family":"Reynolds","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":446784,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70034370,"text":"70034370 - 2010 - Calibration and use of continuous heat-type automated seepage meters for submarine groundwater discharge measurements","interactions":[],"lastModifiedDate":"2012-03-12T17:21:47","indexId":"70034370","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1587,"text":"Estuarine, Coastal and Shelf Science","active":true,"publicationSubtype":{"id":10}},"title":"Calibration and use of continuous heat-type automated seepage meters for submarine groundwater discharge measurements","docAbstract":"Submarine groundwater discharge (SGD) assessments were conducted both in the laboratory and at a field site in the northeastern Gulf of Mexico, using a continuous heat-type automated seepage meter (seepmeter). The functioning of the seepmeter is based on measurements of a temperature gradient in the water between downstream and upstream positions in its flow pipe. The device has the potential of providing long-term, high-resolution measurements of SGD. Using a simple inexpensive laboratory set-up, we have shown that connecting an extension cable to the seepmeter has a negligible effect on its measuring capability. Similarly, the observed influence of very low temperature (???3 ??C) on seepmeter measurements can be accounted for by conducting calibrations at such temperatures prior to field deployments. Compared to manual volumetric measurements, calibration experiments showed that at higher water flow rates (&gt;28 cm day<sup>-1</sup> or cm<sup>3</sup> cm<sup>-2</sup> day<sup>-1</sup>) an analog flowmeter overestimated flow rates by ???7%. This was apparently due to flow resistance, turbulence and formation of air bubbles in the seepmeter water flow tubes. Salinity had no significant effect on the performance of the seepmeter. Calibration results from fresh water and sea water showed close agreement at a 95% confidence level significance between the data sets from the two media (R<sup>2</sup> = 0.98). Comparatively, the seepmeter SGD measurements provided data that are comparable to manually-operated seepage meters, the radon geochemical tracer approach, and an electromagnetic (EM) seepage meter. ?? 2009 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Estuarine, Coastal and Shelf Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.ecss.2009.12.001","issn":"02727714","usgsCitation":"Mwashote, B., Burnett, W.C., Chanton, J., Santos, I., Dimova, N., and Swarzenski, P., 2010, Calibration and use of continuous heat-type automated seepage meters for submarine groundwater discharge measurements: Estuarine, Coastal and Shelf Science, v. 87, no. 1, p. 1-10, https://doi.org/10.1016/j.ecss.2009.12.001.","startPage":"1","endPage":"10","numberOfPages":"10","costCenters":[],"links":[{"id":216559,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ecss.2009.12.001"},{"id":244437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f30fe4b0c8380cd4b59a","contributors":{"authors":[{"text":"Mwashote, B.M.","contributorId":27709,"corporation":false,"usgs":true,"family":"Mwashote","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":445463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burnett, W. C.","contributorId":39779,"corporation":false,"usgs":false,"family":"Burnett","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":445465,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chanton, J.","contributorId":10641,"corporation":false,"usgs":true,"family":"Chanton","given":"J.","affiliations":[],"preferred":false,"id":445462,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Santos, I.R.","contributorId":94499,"corporation":false,"usgs":true,"family":"Santos","given":"I.R.","email":"","affiliations":[],"preferred":false,"id":445467,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dimova, N.","contributorId":66051,"corporation":false,"usgs":true,"family":"Dimova","given":"N.","affiliations":[],"preferred":false,"id":445466,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Swarzenski, P.W. 0000-0003-0116-0578","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":29487,"corporation":false,"usgs":true,"family":"Swarzenski","given":"P.W.","affiliations":[],"preferred":false,"id":445464,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034319,"text":"70034319 - 2010 - Hydrodynamic modeling of juvenile mussel dispersal in a large river: The potential effects of bed shear stress and other parameters","interactions":[],"lastModifiedDate":"2012-03-12T17:21:47","indexId":"70034319","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydrodynamic modeling of juvenile mussel dispersal in a large river: The potential effects of bed shear stress and other parameters","docAbstract":"Because unionid mussels have a parasitic larval stage, they are able to disperse upstream and downstream as larvae while attached to their host fish and with flow as juveniles after excystment from the host. Understanding unionid population ecology requires knowledge of the processes that affect juvenile dispersal prior to establishment. We examined presettlement (transport and dispersion with flow) and early postsettlement (bed shear stress) hydraulic processes as negative censoring mechanisms. Our approach was to model dispersal using particle tracking through a 3-dimensional flow field output from hydrodynamic models of a reach of the Upper Mississippi River. We tested the potential effects of bed shear stress (??b) at 5 flow rates on juvenile mussel dispersal and quantified the magnitude of these effects as a function of flow rate. We explored the reach-scale relationships of Froude number (Fr), water depth (H), local bed slope (S), and unit stream power (QS) with the likelihood of juvenile settling (??). We ran multiple dispersal simulations at each flow rate to estimate ??, the parameter of a Poisson distribution, from the number of juveniles settling in each grid cell, and calculated dispersal distances. Virtual juveniles that settled in areas of the river where b &gt; critical shear stress (c) were resuspended in the flow and transported further downstream, so we ran simulations at 3 different conditions for ??c (??c = ??? no resuspension, 0.1, and 0.05 N/m2). Differences in virtual juvenile dispersal distance were significantly dependent upon c and flow rate, and effects of b on settling distribution were dependent upon c. Most simulations resulted in positive correlations between ?? and ??b, results suggesting that during early postsettlement, ??b might be the primary determinant of juvenile settling distribution. Negative correlations between ?? and ??b occurred in some simulations, a result suggesting that physical or biological presettlement processes might determine juvenile settling distributions. Field data are needed to test these hypotheses. Results support the idea that flow patterns and b can act as negative censoring mechanisms controlling settling distributions. Furthermore, a river reach probably has a quantifiable threshold range of flow rates. Above the upper threshold, ??b probably is the primary determinant of juvenile settling distribution. Relationships of ?? with H, Fr, S, and QS were relatively weak. Important physical processes that affect dispersal probably are not captured by approximations based on large-scale hydraulic parameters, such as Fr and H. ?? 2010 The North American Benthological Society.","largerWorkTitle":"Journal of the North American Benthological Society","language":"English","doi":"10.1899/09-118.1","issn":"08873593","usgsCitation":"Daraio, J., Weber, L., and Newton, T., 2010, Hydrodynamic modeling of juvenile mussel dispersal in a large river: The potential effects of bed shear stress and other parameters, <i>in</i> Journal of the North American Benthological Society, v. 29, no. 3, p. 838-851, https://doi.org/10.1899/09-118.1.","startPage":"838","endPage":"851","numberOfPages":"14","costCenters":[],"links":[{"id":244589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216703,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1899/09-118.1"}],"volume":"29","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a333de4b0c8380cd5ee52","contributors":{"authors":[{"text":"Daraio, J.A.","contributorId":51577,"corporation":false,"usgs":true,"family":"Daraio","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":445223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weber, L.J.","contributorId":79988,"corporation":false,"usgs":true,"family":"Weber","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":445224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newton, T.J.","contributorId":104428,"corporation":false,"usgs":true,"family":"Newton","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":445225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70034190,"text":"70034190 - 2010 - Influence of shell morphology on distributions of unionids in the upper Mississippi River","interactions":[],"lastModifiedDate":"2012-03-12T17:21:45","indexId":"70034190","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2393,"text":"Journal of Molluscan Studies","active":true,"publicationSubtype":{"id":10}},"title":"Influence of shell morphology on distributions of unionids in the upper Mississippi River","docAbstract":"Attempts to predict the distribution of unionids from readily measurable microhabitat descriptors (i.e. water depth, current velocity, stream size, sediment type) have been largely unsuccessful, but certain biological and calculated hydraulic variables have recently shown some predictive power. We used historic and recent data on unionids (from 1987 to 2003) and hydraulic conditions at 438 sample locations over a 38-km reach of the Upper Mississippi River (Navigation Pool 8) to compare the distribution of unionids with different shell morphologies. We evaluated whether sculptured, thick-shelled (STK) species would be found in areas with higher velocity and shear stress, compared to nonsculptured, thin-shelled (NSTN) species. We used classification trees to model the presence and absence of STK and NSTN species to determine which variables were most likely to predict their distribution. Candidate predictor variables included sampling gear, field substrate, water depth (bathymetry), slope, velocity, shear stress and Froude number under low, moderate and high discharges. Our models predicted that STK mussels would occupy a larger portion of the total aquatic area in this reach of the river than NSTN mussels. However, our data demonstrated that NSTN species used areas of higher shear stress and velocity than STK species, but were also present in backwaters with low energy, thus rejecting our hypothesis. The presence of NSTN species over a wide range of shear stress and velocity was probably due to the wide array of life histories displayed within this guild. Overall, these results are consistent with the flow refuge concept in which unionids are more prevalent in areas with low to moderate hydraulic stresses, regardless of shell morphology, and demonstrate the importance of incorporating abiotic and biotic variables into predictive models.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Molluscan Studies","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1093/mollus/eyp045","issn":"02601230","usgsCitation":"Bartsch, M., Zigler, S.J., Newton, T., and Sauer, J., 2010, Influence of shell morphology on distributions of unionids in the upper Mississippi River: Journal of Molluscan Studies, v. 76, no. 1, p. 67-76, https://doi.org/10.1093/mollus/eyp045.","startPage":"67","endPage":"76","numberOfPages":"10","costCenters":[],"links":[{"id":475945,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/mollus/eyp045","text":"Publisher Index Page"},{"id":216759,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1093/mollus/eyp045"},{"id":244646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-09-29","publicationStatus":"PW","scienceBaseUri":"505a3b7be4b0c8380cd62580","contributors":{"authors":[{"text":"Bartsch, M.R.","contributorId":42908,"corporation":false,"usgs":true,"family":"Bartsch","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":444532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zigler, S. J.","contributorId":21513,"corporation":false,"usgs":true,"family":"Zigler","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":444531,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newton, T.J.","contributorId":104428,"corporation":false,"usgs":true,"family":"Newton","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":444533,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sauer, J.S.","contributorId":106455,"corporation":false,"usgs":true,"family":"Sauer","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":444534,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034188,"text":"70034188 - 2010 - Vulnerability of age-0 pallid sturgeon Scaphirhynchus albus to fish predation","interactions":[],"lastModifiedDate":"2012-03-12T17:21:46","indexId":"70034188","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2166,"text":"Journal of Applied Ichthyology","active":true,"publicationSubtype":{"id":10}},"title":"Vulnerability of age-0 pallid sturgeon Scaphirhynchus albus to fish predation","docAbstract":"Stocking is a commonly employed conservation strategy for endangered species such as the pallid sturgeon, Scaphirhynchus albus. However, decisions about when, where and at what size pallid sturgeon should be stocked are hindered because vulnerability of pallid sturgeon to fish predation is not known. The objective of this study was to evaluate the vulnerability of age-0 pallid sturgeon to predation by two Missouri River predators under different flow regimes, and in combination with alternative prey. To document vulnerability, age-0 pallid sturgeon (&lt;100 mm) were offered to channel catfish Ictalurus punctatus and smallmouth bass Micropterus dolomieu in laboratory experiments. Selection of pallid sturgeon by both predators was measured by offering pallid sturgeon and an alternative prey, fathead minnows Pimephales promelas, in varying prey densities. Smallmouth bass consumed more age-0 pallid sturgeon (0.95 h<sup>-1</sup>) than did channel catfish (0.13 h<sup>-1</sup>), and predation rates did not differ between water velocities supporting sustained (0 m s<sup>-1</sup>) or prolonged swimming speeds (0.15 m s<sup>-1</sup>). Neither predator positively selected pallid sturgeon when alternative prey was available. Both predator species consumed more fathead minnows than pallid sturgeon across all prey density combinations. Results indicate that the vulnerability of age-0 pallid sturgeon to predation by channel catfish and smallmouth bass is low, especially in the presence of an alternative fish prey. ?? 2009 Blackwell Verlag GmbH.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Applied Ichthyology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1439-0426.2009.01356.x","issn":"01758659","usgsCitation":"French, W.E., Graeb, B.D., Chipps, S., Bertrand, K., Selch, T., and Klumb, R.A., 2010, Vulnerability of age-0 pallid sturgeon Scaphirhynchus albus to fish predation: Journal of Applied Ichthyology, v. 26, no. 1, p. 6-10, https://doi.org/10.1111/j.1439-0426.2009.01356.x.","startPage":"6","endPage":"10","numberOfPages":"5","costCenters":[],"links":[{"id":216727,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1439-0426.2009.01356.x"},{"id":244613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc377e4b08c986b32b1c3","contributors":{"authors":[{"text":"French, William E.","contributorId":97355,"corporation":false,"usgs":true,"family":"French","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":444526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graeb, B. D. S.","contributorId":80916,"corporation":false,"usgs":true,"family":"Graeb","given":"B.","email":"","middleInitial":"D. S.","affiliations":[],"preferred":false,"id":444524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chipps, S. R. 0000-0001-6511-7582","orcid":"https://orcid.org/0000-0001-6511-7582","contributorId":40369,"corporation":false,"usgs":true,"family":"Chipps","given":"S. R.","affiliations":[],"preferred":false,"id":444522,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bertrand, K.N.","contributorId":52381,"corporation":false,"usgs":true,"family":"Bertrand","given":"K.N.","email":"","affiliations":[],"preferred":false,"id":444523,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Selch, T.M.","contributorId":34327,"corporation":false,"usgs":true,"family":"Selch","given":"T.M.","affiliations":[],"preferred":false,"id":444521,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klumb, Robert A.","contributorId":86606,"corporation":false,"usgs":true,"family":"Klumb","given":"Robert","email":"","middleInitial":"A.","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false},{"id":561,"text":"South Dakota Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true},{"id":5089,"text":"South Dakota State University","active":true,"usgs":false}],"preferred":false,"id":444525,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034144,"text":"70034144 - 2010 - Influence of organic matter on the transport of Cryptosporidium parvum oocysts in a ferric oxyhydroxide-coated quartz sand saturated porous medium","interactions":[],"lastModifiedDate":"2018-10-10T13:09:06","indexId":"70034144","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"Influence of organic matter on the transport of Cryptosporidium parvum oocysts in a ferric oxyhydroxide-coated quartz sand saturated porous medium","docAbstract":"<p>To assess the effect of organic matter on the transport of Cryptosporidium parvum oocysts in a geochemically heterogeneous saturated porous medium, we measured the breakthrough and collision efficiencies of oocysts as a function of dissolved organic matter concentration in a flow-through column containing ferric oxyhydroxide-coated sand. We characterized the surface properties of the oocysts and ferric oxyhydroxide-coated sand using microelectrophoresis and streaming potential, respectively, and the amount of organic matter adsorbed on the ferric oxyhydroxide-coated sand as a function of the concentration of dissolved organic matter (a fulvic acid isolated from Florida Everglades water). The dissolved organic matter had no significant effect on the zeta potential of the oocysts. Low concentrations of dissolved organic matter were responsible for reversing the charge of the ferric oxyhydroxide-coated sand surface from positive to negative. The charge reversal and accumulation of negative charge on the ferric oxyhydroxide-coated sand led to increases in oocyst breakthrough and decreases in oocyst collision efficiency with increasing dissolved organic matter concentration. The increase in dissolved organic matter concentration from 0 to 20 mg L<sup>-1</sup> resulted in a two-fold decrease in the collision efficiency.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier Ltd.","doi":"10.1016/j.watres.2009.09.039","issn":"00431354","usgsCitation":"Abudalo, R., Ryan, J.N., Harvey, R.W., Metge, D.W., and Landkamer, L.L., 2010, Influence of organic matter on the transport of Cryptosporidium parvum oocysts in a ferric oxyhydroxide-coated quartz sand saturated porous medium: Water Research, v. 44, no. 4, p. 1104-1113, https://doi.org/10.1016/j.watres.2009.09.039.","productDescription":"10 p.","startPage":"1104","endPage":"1113","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":244514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216633,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.watres.2009.09.039"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b62e4b0c8380cd624a4","contributors":{"authors":[{"text":"Abudalo, R.A.","contributorId":64445,"corporation":false,"usgs":true,"family":"Abudalo","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":444311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryan, J. N.","contributorId":102649,"corporation":false,"usgs":true,"family":"Ryan","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":444313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":444309,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Metge, David W. dwmetge@usgs.gov","contributorId":663,"corporation":false,"usgs":true,"family":"Metge","given":"David","email":"dwmetge@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":444310,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Landkamer, Lee L.","contributorId":65679,"corporation":false,"usgs":true,"family":"Landkamer","given":"Lee","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":444312,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70034118,"text":"70034118 - 2010 - The spatial and temporal variability of groundwater recharge in a forested basin in northern Wisconsin","interactions":[],"lastModifiedDate":"2012-03-12T17:21:45","indexId":"70034118","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"The spatial and temporal variability of groundwater recharge in a forested basin in northern Wisconsin","docAbstract":"Recharge varies spatially and temporally as it depends on a wide variety of factors (e.g. vegetation, precipitation, climate, topography, geology, and soil type), making it one of the most difficult, complex, and uncertain hydrologic parameters to quantify. Despite its inherent variability, groundwater modellers, planners, and policy makers often ignore recharge variability and assume a single average recharge value for an entire watershed. Relatively few attempts have been made to quantify or incorporate spatial and temporal recharge variability into water resource planning or groundwater modelling efforts. In this study, a simple, daily soil-water balance model was developed and used to estimate the spatial and temporal distribution of groundwater recharge of the Trout Lake basin of northern Wisconsin for 1996-2000 as a means to quantify recharge variability. For the 5 years of study, annual recharge varied spatially by as much as 18 cm across the basin; vegetation was the predominant control on this variability. Recharge also varied temporally with a threefold annual difference over the 5-year period. Intra-annually, recharge was limited to a few isolated events each year and exhibited a distinct seasonal pattern. The results suggest that ignoring recharge variability may not only be inappropriate, but also, depending on the application, may invalidate model results and predictions for regional and local water budget calculations, water resource management, nutrient cycling, and contaminant transport studies. Recharge is spatially and temporally variable, and should be modelled as such. Copyright ?? 2009 John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrological Processes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/hyp.7497","issn":"08856087","usgsCitation":"Dripps, W.R., and Bradbury, K.R., 2010, The spatial and temporal variability of groundwater recharge in a forested basin in northern Wisconsin: Hydrological Processes, v. 24, no. 4, p. 383-392, https://doi.org/10.1002/hyp.7497.","startPage":"383","endPage":"392","numberOfPages":"10","costCenters":[],"links":[{"id":216690,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/hyp.7497"},{"id":244575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationDate":"2009-11-16","publicationStatus":"PW","scienceBaseUri":"505bb059e4b08c986b324ddc","contributors":{"authors":[{"text":"Dripps, W. R.","contributorId":27978,"corporation":false,"usgs":true,"family":"Dripps","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":444184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradbury, K. R.","contributorId":86070,"corporation":false,"usgs":true,"family":"Bradbury","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":444185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70034090,"text":"70034090 - 2010 - New and interesting species of the genus Muelleria (Bacillariophyta) from the Antarctic region and South Africa","interactions":[],"lastModifiedDate":"2012-03-12T17:21:45","indexId":"70034090","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3055,"text":"Phycologia","active":true,"publicationSubtype":{"id":10}},"title":"New and interesting species of the genus Muelleria (Bacillariophyta) from the Antarctic region and South Africa","docAbstract":"During a survey of the terrestrial diatom flora of some sub-Antarctic islands in the southern Indian and Atlantic Oceans and of the Antarctic continent, more than 15 taxa belonging to the genus Muelleria were observed. Nine of these taxa are described as new species using light and scanning electron microscopy. Comments are made on their systematic position and how they are distinguished from other species in the genus. Additionally, two previously unrecognized taxa within the genus were discovered in samples from South Africa. One of these, Muelleria taylorii Van de Vijver & Cocquyt sp. nov., is new to science; the other, Muelleria vandermerwei (Cholnoky) Van de Vijver & Cocquyt nov. comb., had been included in the genus Diploneis. The large number of new Muelleria taxa on the (sub)-Antarctic locations is not surprising. Species in Muelleria occur rarely in collections; in many habitats, it is unusual to find more than 1-2 valves in any slide preparation. As a result, records are scarce. The practice of \"force-fitting\" (shoehorning) specimens into descriptions from common taxonomic keys (and species drift) results in European species, such as M. gibbula and M. linearis, being applied to Antarctic forms in ecological studies. Finally, the typical terrestrial habitats of soils, mosses and ephemeral water bodies of most of these taxa have been poorly studied in the past.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Phycologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2216/09-27.1","issn":"00318884","usgsCitation":"Van De Vijver, B., Mataloni, G., Stanish, L., and Spaulding, S., 2010, New and interesting species of the genus Muelleria (Bacillariophyta) from the Antarctic region and South Africa: Phycologia, v. 49, no. 1, p. 22-41, https://doi.org/10.2216/09-27.1.","startPage":"22","endPage":"41","numberOfPages":"20","costCenters":[],"links":[{"id":476044,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/11336/53537","text":"External Repository"},{"id":244605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216719,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2216/09-27.1"}],"volume":"49","issue":"1","noUsgsAuthors":false,"publicationDate":"2019-03-27","publicationStatus":"PW","scienceBaseUri":"505a6553e4b0c8380cd72b72","contributors":{"authors":[{"text":"Van De Vijver, B.","contributorId":19782,"corporation":false,"usgs":true,"family":"Van De Vijver","given":"B.","affiliations":[],"preferred":false,"id":444033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mataloni, G.","contributorId":67756,"corporation":false,"usgs":true,"family":"Mataloni","given":"G.","affiliations":[],"preferred":false,"id":444035,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stanish, L.","contributorId":31232,"corporation":false,"usgs":true,"family":"Stanish","given":"L.","affiliations":[],"preferred":false,"id":444034,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Spaulding, S. A. 0000-0002-9787-7743","orcid":"https://orcid.org/0000-0002-9787-7743","contributorId":74390,"corporation":false,"usgs":true,"family":"Spaulding","given":"S. A.","affiliations":[],"preferred":false,"id":444036,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034057,"text":"70034057 - 2010 - Response of benthic macroinvertebrate communities to highway construction in an Appalachian watershed","interactions":[],"lastModifiedDate":"2012-03-12T17:21:44","indexId":"70034057","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Response of benthic macroinvertebrate communities to highway construction in an Appalachian watershed","docAbstract":"Highway construction in mountainous areas can result in sedimentation of streams, negatively impacting stream habitat, water quality, and biotic communities. We assessed the impacts of construction of a segment of Corridor H, a four-lane highway, in the Lost River watershed, West Virginia, by monitoring benthic macroinvertebrate communities and water quality, before, during, and after highway construction and prior to highway use at upstream and downstream sites from 1997 through 2007. Data analysis of temporal impacts of highway construction followed a Before-After-Control-Impact (BACI) study design. Highway construction impacts included an increase in stream sedimentation during the construction phase. This was indicated by an increase in turbidity and total suspended solids. Benthic macroinvertebrate metrics indicated a community more tolerant during and after construction than in the period before construction. The percent of Chironomidae and the Hilsenhoff Biotic Index (HBI) increased, while percent of Ephemeroptera, Plecoptera, and Trichoptera (EPT) decreased. Our 10-year study addressed short-term impacts of highway construction and found that impacts were relatively minimal. A recovery of the number of EPT taxa collected after construction indicated that the benthic macroinvertebrate community may be recovering from impacts of highway construction. However, this study only addressed a period of 3 years before, 3 years during, and 4 years post construction. Inferences cannot be made concerning the long-term impacts of the highway, highway traffic, runoff, and other factors associated with highway use. Continual monitoring of the watershed is necessary to determine if the highway has a continual impact on stream habitat, water quality, and biotic integrity. ?? 2010 Springer Science+Business Media B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10750-009-0070-9","issn":"00188158","usgsCitation":"Hedrick, L.B., Welsh, S., Anderson, J.T., Lin, L., Chen, Y., and Wei, X., 2010, Response of benthic macroinvertebrate communities to highway construction in an Appalachian watershed: Hydrobiologia, v. 641, no. 1, p. 115-131, https://doi.org/10.1007/s10750-009-0070-9.","startPage":"115","endPage":"131","numberOfPages":"17","costCenters":[],"links":[{"id":216687,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10750-009-0070-9"},{"id":244572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"641","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-01-12","publicationStatus":"PW","scienceBaseUri":"505aaa35e4b0c8380cd861e4","contributors":{"authors":[{"text":"Hedrick, Lara B.","contributorId":50346,"corporation":false,"usgs":true,"family":"Hedrick","given":"Lara","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":443852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welsh, S.A. 0000-0003-0362-054X","orcid":"https://orcid.org/0000-0003-0362-054X","contributorId":10191,"corporation":false,"usgs":true,"family":"Welsh","given":"S.A.","affiliations":[],"preferred":false,"id":443850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, James T.","contributorId":28071,"corporation":false,"usgs":false,"family":"Anderson","given":"James","email":"","middleInitial":"T.","affiliations":[{"id":12432,"text":"West Virginia University","active":true,"usgs":false}],"preferred":false,"id":443851,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lin, L.-S.","contributorId":66093,"corporation":false,"usgs":true,"family":"Lin","given":"L.-S.","email":"","affiliations":[],"preferred":false,"id":443854,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chen, Y.","contributorId":7019,"corporation":false,"usgs":true,"family":"Chen","given":"Y.","email":"","affiliations":[],"preferred":false,"id":443849,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wei, X.","contributorId":50636,"corporation":false,"usgs":true,"family":"Wei","given":"X.","email":"","affiliations":[],"preferred":false,"id":443853,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034038,"text":"70034038 - 2010 - Impacts of precipitation seasonality and ecosystem types on evapotranspiration in the Yukon River Basin, Alaska","interactions":[],"lastModifiedDate":"2017-04-06T12:17:35","indexId":"70034038","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Impacts of precipitation seasonality and ecosystem types on evapotranspiration in the Yukon River Basin, Alaska","docAbstract":"<p><span>Evapotranspiration (ET) is the largest component of water loss from terrestrial ecosystems; however, large uncertainties exist when estimating the temporal and spatial variations of ET because of concurrent shifts in the magnitude and seasonal distribution of precipitation as well as differences in the response of ecosystem ET to environmental variabilities. In this study, we examined the impacts of precipitation seasonality and ecosystem types on ET quantified by eddy covariance towers from 2002 to 2004 in three ecosystems (grassland, deciduous broadleaf forest, and evergreen needleleaf forest) in the Yukon River Basin, Alaska. The annual precipitation changed greatly in both magnitude and seasonal distribution through the three investigated years. Observations and model results showed that ET was more sensitive to precipitation scarcity in the early growing season than in the late growing season, which was the direct result of different responses of ET components to precipitation in different seasons. The results demonstrated the importance of seasonal variations of precipitation in regulating annual ET and overshadowing the function of annual precipitation. Comparison of ET among ecosystems over the growing season indicated that ET was largest in deciduous broadleaf, intermediate in evergreen needleleaf, and lowest in the grassland ecosystem. These ecosystem differences in ET were related to differences in successional stages and physiological responses.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/2009WR008119","issn":"00431397","usgsCitation":"Yuan, W., Liu, S., Liu, H., Randerson, J.T., Yu, G., and Tieszen, L., 2010, Impacts of precipitation seasonality and ecosystem types on evapotranspiration in the Yukon River Basin, Alaska: Water Resources Research, v. 46, no. 2, p. 1-16, https://doi.org/10.1029/2009WR008119.","productDescription":"W02514; 16 p.","startPage":"1","endPage":"16","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":475833,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009wr008119","text":"Publisher Index Page"},{"id":244799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216900,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009WR008119"}],"volume":"46","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-02-16","publicationStatus":"PW","scienceBaseUri":"505a38f4e4b0c8380cd61755","contributors":{"authors":[{"text":"Yuan, W.","contributorId":35955,"corporation":false,"usgs":true,"family":"Yuan","given":"W.","email":"","affiliations":[],"preferred":false,"id":443769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liu, S.","contributorId":93170,"corporation":false,"usgs":true,"family":"Liu","given":"S.","affiliations":[],"preferred":false,"id":443772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Liu, H.","contributorId":12222,"corporation":false,"usgs":true,"family":"Liu","given":"H.","affiliations":[],"preferred":false,"id":443767,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Randerson, J. T.","contributorId":41181,"corporation":false,"usgs":false,"family":"Randerson","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":443770,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yu, G.","contributorId":61198,"corporation":false,"usgs":true,"family":"Yu","given":"G.","email":"","affiliations":[],"preferred":false,"id":443771,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tieszen, L.L.","contributorId":24046,"corporation":false,"usgs":true,"family":"Tieszen","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":443768,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70034028,"text":"70034028 - 2010 - Seismicity and fluid geochemistry at Lassen Volcanic National Park, California: Evidence for two circulation cells in the hydrothermal system","interactions":[],"lastModifiedDate":"2016-12-14T13:43:18","indexId":"70034028","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Seismicity and fluid geochemistry at Lassen Volcanic National Park, California: Evidence for two circulation cells in the hydrothermal system","docAbstract":"<p><span>Seismic analysis and geochemical interpretations provide evidence that two separate hydrothermal cells circulate within the greater Lassen hydrothermal system. One cell originates south to SW of Lassen Peak and within the Brokeoff Volcano depression where it forms a reservoir of hot fluid (235–270°C) that boils to feed steam to the high-temperature fumarolic areas, and has a plume of degassed reservoir liquid that flows southward to emerge at Growler and Morgan Hot Springs. The second cell originates SSE to SE of Lassen Peak and flows southeastward along inferred faults of the Walker Lane belt (WLB) where it forms a reservoir of hot fluid (220–240°C) that boils beneath Devils Kitchen and Boiling Springs Lake, and has an outflow plume of degassed liquid that boils again beneath Terminal Geyser. Three distinct seismogenic zones (identified as the </span><i>West</i><span>, </span><i>Middle</i><span>, and </span><i>East</i><span> seismic clusters) occur at shallow depths (&lt;6&nbsp;km) in Lassen Volcanic National Park, SW to SSE of Lassen Peak and adjacent to areas of high-temperature (≤161°C) fumarolic activity (Sulphur Works, Pilot Pinnacle, Little Hot Springs Valley, and Bumpass Hell) and an area of cold, weak gas emissions (Cold Boiling Lake). The three zones are located within the inferred Rockland caldera in response to interactions between deeply circulating meteoric water and hot brittle rock that overlies residual magma associated with the Lassen Volcanic Center. Earthquake focal mechanisms and stress inversions indicate primarily N–S oriented normal faulting and E–W extension, with some oblique faulting and right lateral shear in the </span><i>East</i><span> cluster. The different focal mechanisms as well as spatial and temporal earthquake patterns for the </span><i>East</i><span> cluster indicate a greater influence by regional tectonics and inferred faults within the WLB. A fourth, deeper (5–10&nbsp;km) seismogenic zone (the </span><i>Devils Kitchen</i><span> seismic cluster) occurs SE of the </span><i>East</i><span> cluster and trends NNW from Sifford Mountain toward the Devils Kitchen thermal area where fumarolic temperatures are ≤123°C. Lassen fumaroles discharge geothermal gases that indicate mixing between a N</span><sub>2</sub><span>-rich, arc-type component and gases derived from air-saturated meteoric recharge water. Most gases have relatively weak isotopic indicators of upper mantle or volcanic components, except for gas from Sulphur Works where </span><i>δ</i><sup>13</sup><span>C–CO</span><sub>2</sub><span>, </span><i>δ</i><sup>34</sup><span>S–H</span><sub>2</sub><span>S, and </span><i>δ</i><sup>15</sup><span>N–N</span><sub>2</sub><span> values indicate a contribution from the mantle and a subducted sediment source in an arc volcanic setting.</span></p>","language":"English","publisher":"Elsevier Science","doi":"10.1016/j.jvolgeores.2009.11.014","issn":"03770273","usgsCitation":"Janik, C.J., and McLaren, M.K., 2010, Seismicity and fluid geochemistry at Lassen Volcanic National Park, California: Evidence for two circulation cells in the hydrothermal system: Journal of Volcanology and Geothermal Research, v. 189, no. 3-4, p. 257-277, https://doi.org/10.1016/j.jvolgeores.2009.11.014.","productDescription":"21 p.","startPage":"257","endPage":"277","numberOfPages":"21","costCenters":[],"links":[{"id":244667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.3,\n              40.6\n            ],\n            [\n              -121.3,\n              40.3\n            ],\n            [\n              -121.7,\n              40.3\n            ],\n            [\n              -121.7,\n              40.6\n            ],\n            [\n              -121.3,\n              40.6\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"189","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8b8de4b08c986b317909","contributors":{"authors":[{"text":"Janik, Cathy J.","contributorId":139041,"corporation":false,"usgs":false,"family":"Janik","given":"Cathy","email":"","middleInitial":"J.","affiliations":[{"id":12608,"text":"USGS, retired","active":true,"usgs":false}],"preferred":false,"id":443724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLaren, Marcia K.","contributorId":139042,"corporation":false,"usgs":false,"family":"McLaren","given":"Marcia","email":"","middleInitial":"K.","affiliations":[{"id":12624,"text":"PG&E","active":true,"usgs":false}],"preferred":false,"id":443725,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70033920,"text":"70033920 - 2010 - Enzyme stabilization by glass-derived silicates in glass-exposed aqueous solutions","interactions":[],"lastModifiedDate":"2012-03-12T17:21:33","indexId":"70033920","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1906,"text":"Homeopathy","active":true,"publicationSubtype":{"id":10}},"title":"Enzyme stabilization by glass-derived silicates in glass-exposed aqueous solutions","docAbstract":"Objectives: To analyze the solutes leaching from glass containers into aqueous solutions, and to show that these solutes have enzyme activity stabilizing effects in very dilute solutions. Methods: Enzyme assays with acetylcholine esterase were used to analyze serially succussed and diluted (SSD) solutions prepared in glass and plastic containers. Aqueous SSD preparations starting with various solutes, or water alone, were prepared under several conditions, and tested for their solute content and their ability to affect enzyme stability in dilute solution. Results: We confirm that water acts to dissolve constituents from glass vials, and show that the solutes derived from the glass have effects on enzymes in the resultant solutions. Enzyme assays demonstrated that enzyme stability in purified and deionized water was enhanced in SSD solutions that were prepared in glass containers, but not those prepared in plastic. The increased enzyme stability could be mimicked in a dose-dependent manner by the addition of silicates to the purified, deionized water that enzymes were dissolved in. Elemental analyses of SSD water preparations made in glass vials showed that boron, silicon, and sodium were present at micromolar concentrations. Conclusions: These results show that silicates and other solutes are present at micromolar levels in all glass-exposed solutions, whether pharmaceutical or homeopathic in nature. Even though silicates are known to have biological activity at higher concentrations, the silicate concentrations we measured in homeopathic preparations were too low to account for any purported in vivo efficacy, but could potentially influence in vitro biological assays reporting homeopathic effects. ?? 2009 The Faculty of Homeopathy.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Homeopathy","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.homp.2009.11.006","issn":"14754916","usgsCitation":"Ives, J., Moffett, J., Arun, P., Lam, D., Todorov, T., Brothers, A., Anick, D., Centeno, J., Namboodiri, M., and Jonas, W., 2010, Enzyme stabilization by glass-derived silicates in glass-exposed aqueous solutions: Homeopathy, v. 99, no. 1, p. 15-24, https://doi.org/10.1016/j.homp.2009.11.006.","startPage":"15","endPage":"24","numberOfPages":"10","costCenters":[],"links":[{"id":214185,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.homp.2009.11.006"},{"id":241879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"99","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a09f6e4b0c8380cd52123","contributors":{"authors":[{"text":"Ives, J.A.","contributorId":64901,"corporation":false,"usgs":true,"family":"Ives","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":443181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moffett, J.R.","contributorId":36767,"corporation":false,"usgs":true,"family":"Moffett","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":443179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arun, P.","contributorId":24581,"corporation":false,"usgs":true,"family":"Arun","given":"P.","email":"","affiliations":[],"preferred":false,"id":443176,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lam, D.","contributorId":96102,"corporation":false,"usgs":true,"family":"Lam","given":"D.","email":"","affiliations":[],"preferred":false,"id":443183,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Todorov, T.I.","contributorId":10995,"corporation":false,"usgs":true,"family":"Todorov","given":"T.I.","email":"","affiliations":[],"preferred":false,"id":443175,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brothers, A.B.","contributorId":77751,"corporation":false,"usgs":true,"family":"Brothers","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":443182,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Anick, D.J.","contributorId":25774,"corporation":false,"usgs":true,"family":"Anick","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":443177,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Centeno, J.","contributorId":103481,"corporation":false,"usgs":true,"family":"Centeno","given":"J.","email":"","affiliations":[],"preferred":false,"id":443184,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Namboodiri, M.A.A.","contributorId":34732,"corporation":false,"usgs":true,"family":"Namboodiri","given":"M.A.A.","email":"","affiliations":[],"preferred":false,"id":443178,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Jonas, W.B.","contributorId":42442,"corporation":false,"usgs":true,"family":"Jonas","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":443180,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70033887,"text":"70033887 - 2010 - Incubating rainbow trout in soft water increased their later sensitivity to cadmium and zinc","interactions":[],"lastModifiedDate":"2016-10-19T15:40:23","indexId":"70033887","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Incubating rainbow trout in soft water increased their later sensitivity to cadmium and zinc","docAbstract":"<p>Water hardness is well known to affect the toxicity of some metals; however, reports on the influence of hardness during incubation or acclimation on later toxicity to metals have been conflicting. We incubated rainbow trout (<i class=\"EmphasisTypeItalic \">Oncorhynchus mykiss</i>) near the confluence of two streams, one with soft water and one with very-soft water (average incubation hardnesses of about 21 and 11&nbsp;mg/L as CaCO<sub>3</sub>, respectively). After developing to the swim-up stage, the fish were exposed for 96-h to a mixture of cadmium (Cd) and zinc (Zn) in water with a hardness of 27&nbsp;mg/L as CaCO<sub>3</sub>. The fish incubated in the higher hardness water were about two times more resistant than the fish incubated in the extremely soft water. This difference was similar or greater than the difference that would have been predicted by criteria hardness equations had the fish been tested in the different acclimation waters. We think it is plausible that the energy demands for fish to maintain homeostasis in the lower hardness water make the fish more sensitive to metals that inhibit ionoregulation such as Cd and Zn. We suggest that if important decisions were to be based upon test results, assumptions of adequate hardness acclimation should be carefully considered and short acclimation periods avoided. If practical, incubating rainbow trout in the control waters to be tested may reduce uncertainties in the possible influences of differing rearing water hardness on the test results.</p>","language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1007/s11270-009-0070-4","issn":"00496979","usgsCitation":"Mebane, C.A., Hennessy, D.P., and Dillon, F.S., 2010, Incubating rainbow trout in soft water increased their later sensitivity to cadmium and zinc: Water, Air, & Soil Pollution, v. 205, no. 1-4, p. 245-250, https://doi.org/10.1007/s11270-009-0070-4.","productDescription":"6 p.","startPage":"245","endPage":"250","costCenters":[],"links":[{"id":241877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"205","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2009-04-29","publicationStatus":"PW","scienceBaseUri":"505a3a0be4b0c8380cd61b1c","contributors":{"authors":[{"text":"Mebane, Christopher A. 0000-0002-9089-0267 cmebane@usgs.gov","orcid":"https://orcid.org/0000-0002-9089-0267","contributorId":110,"corporation":false,"usgs":true,"family":"Mebane","given":"Christopher","email":"cmebane@usgs.gov","middleInitial":"A.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":443025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hennessy, Daniel P.","contributorId":44782,"corporation":false,"usgs":true,"family":"Hennessy","given":"Daniel","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":443023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dillon, Frank S.","contributorId":81740,"corporation":false,"usgs":true,"family":"Dillon","given":"Frank","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":443024,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70178483,"text":"70178483 - 2010 - Post-construction monitoring of a Core-Loc™ breakwater using tripod-based LiDAR","interactions":[],"lastModifiedDate":"2017-01-20T10:59:44","indexId":"70178483","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Post-construction monitoring of a Core-Loc™ breakwater using tripod-based LiDAR","docAbstract":"<p>The goal of the technology application described herein is to determine whether breakwater monitoring data collected using Tripod (or Terrestrial) Light Detection and Ranging (T-LiDAR) can give insight into processes such as how Core-Loc™ concrete armour units nest following construction, and in turn how settlement affects armour layer stability, concrete cap performance, and armour unit breakage. &nbsp;A further objective is that this information can then be incorporated into the design of future projects using concrete armour units. &nbsp;The results of this application of T-LiDAR, including the challenges encountered and the conclusions drawn regarding initial concrete armour unit movement will be presented in this paper.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coasts, marine structures and breakwaters: Adapting to change","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Thomas Telford Limitied","doi":"10.1680/cmsb.41301.0039","usgsCitation":"Podoski, J.H., Bawden, G.W., Bond, S., Smith, T.D., and Foster, J., 2010, Post-construction monitoring of a Core-Loc™ breakwater using tripod-based LiDAR, chap. <i>of</i> Coasts, marine structures and breakwaters: Adapting to change, https://doi.org/10.1680/cmsb.41301.0039.","ipdsId":"IP-012418","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":333550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-02","publicationStatus":"PW","scienceBaseUri":"58833023e4b0d002316377a2","contributors":{"authors":[{"text":"Podoski, Jessica H.","contributorId":178488,"corporation":false,"usgs":false,"family":"Podoski","given":"Jessica","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":659195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bawden, Gerald W. gbawden@usgs.gov","contributorId":1071,"corporation":false,"usgs":true,"family":"Bawden","given":"Gerald","email":"gbawden@usgs.gov","middleInitial":"W.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bond, Sandra 0000-0003-0522-5287 sbond@usgs.gov","orcid":"https://orcid.org/0000-0003-0522-5287","contributorId":3328,"corporation":false,"usgs":true,"family":"Bond","given":"Sandra","email":"sbond@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659197,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Thomas D.","contributorId":178489,"corporation":false,"usgs":false,"family":"Smith","given":"Thomas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":659198,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Foster, James","contributorId":38598,"corporation":false,"usgs":true,"family":"Foster","given":"James","affiliations":[],"preferred":false,"id":659199,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70033861,"text":"70033861 - 2010 - Individual and colony-specific wintering areas of Pacific northern fulmars (Fulmarus glacialis)","interactions":[],"lastModifiedDate":"2020-11-02T14:47:39.854648","indexId":"70033861","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Individual and colony-specific wintering areas of Pacific northern fulmars (Fulmarus glacialis)","docAbstract":"Seabird mortality associated with longline fishing in the eastern Bering Sea occurs mainly from September to May, with northern fulmars (Fulmarus glacialis) comprising the majority (60%) of the bycatch. Along the west coast of North America, winter dieoffs of fulmars may be increasing in frequency and magnitude, the most severe on record being a wreck that peaked in October-November 2003. We deployed satellite transmitters on fulmars from the four main Alaska colonies and tracked individuals for up to 2 years. Fulmars from Hall Island (northern Bering Sea) moved to Russian coastal waters after breeding, while Pribilof Island fulmars (southeastern Bering Sea) remained relatively sedentary yearround. Birds from Chagulak Island (eastern Aleutians) preferred passes between the Aleutian Islands in winter or foraged widely over deep waters of the central Bering Sea and North Pacific. Fulmars from the Semidi Islands (western Gulf of Alaska) migrated directly to waters of the California Current. Individuals from St. George Island (Pribilofs) and Chagulak were consistent in the places that they visited in two successive winters. The Pribilof Islands population is most affected by winter longlining for groundfish, whereas the Semidi Islands colony sustains most of the natural mortality that occurs off Washington, Oregon, and California.","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/F09-184","issn":"0706652X","usgsCitation":"Hatch, S.A., Gill, V., and Mulcahy, D.M., 2010, Individual and colony-specific wintering areas of Pacific northern fulmars (Fulmarus glacialis): Canadian Journal of Fisheries and Aquatic Sciences, v. 67, no. 2, p. 386-400, https://doi.org/10.1139/F09-184.","productDescription":"15 p.","startPage":"386","endPage":"400","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":438846,"rank":1,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P992BR5E","text":"USGS data release","linkHelpText":"Tracking Data for Northern Fulmars (Fulmarus glacialis)"},{"id":241970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -166.201171875,\n              61.689872200460016\n            ],\n            [\n              -165.673828125,\n              61.689872200460016\n            ],\n            [\n              -171.03515625,\n              62.91523303947614\n            ],\n            [\n              -176.044921875,\n              60.50052541051131\n            ],\n            [\n              -175.869140625,\n              58.49369382056807\n            ],\n            [\n              -174.111328125,\n              54.1109429427243\n            ],\n            [\n              -171.650390625,\n              51.23440735163459\n            ],\n            [\n              -167.16796875,\n              50.958426723359935\n            ],\n            [\n              -158.81835937499997,\n              52.482780222078226\n            ],\n            [\n              -154.51171875,\n              57.088515327886505\n            ],\n            [\n              -159.345703125,\n              58.95000823335702\n            ],\n            [\n              -166.201171875,\n              61.689872200460016\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"67","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3a9ae4b0c8380cd61dee","contributors":{"authors":[{"text":"Hatch, Scott A. 0000-0002-0064-8187 shatch@usgs.gov","orcid":"https://orcid.org/0000-0002-0064-8187","contributorId":2625,"corporation":false,"usgs":true,"family":"Hatch","given":"Scott","email":"shatch@usgs.gov","middleInitial":"A.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":442878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, Verena A.","contributorId":140658,"corporation":false,"usgs":false,"family":"Gill","given":"Verena A.","affiliations":[{"id":6678,"text":"U.S. Fish and Wildlife Service, Alaska Maritime National Wildlife Refuge","active":true,"usgs":false}],"preferred":false,"id":442876,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulcahy, Daniel M. dmulcahy@usgs.gov","contributorId":3102,"corporation":false,"usgs":true,"family":"Mulcahy","given":"Daniel","email":"dmulcahy@usgs.gov","middleInitial":"M.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":442877,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70033859,"text":"70033859 - 2010 - MTBE, TBA, and TAME attenuation in diverse hyporheic zones","interactions":[],"lastModifiedDate":"2018-10-10T09:49:38","indexId":"70033859","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"MTBE, TBA, and TAME attenuation in diverse hyporheic zones","docAbstract":"<p>Groundwater contamination by fuel-related compounds such as the fuel oxygenates methyl tert-butyl ether (MTBE), tert-butyl alcohol (TBA), and tert-amyl methyl ether (TAME) presents a significant issue to managers and consumers of groundwater and surface water that receives groundwater discharge. Four sites were investigated on Long Island, New York, characterized by groundwater contaminated with gasoline and fuel oxygenates that ultimately discharge to fresh, brackish, or saline surface water. For each site, contaminated groundwater discharge zones were delineated using pore water geochemistry data from 15 feet (4.5 m) beneath the bottom of the surface water body in the hyporheic zone and seepage-meter tests were conducted to measure discharge rates. These data when combined indicate that MTBE, TBA, and TAME concentrations in groundwater discharge in a 5-foot (1.5-m) thick section of the hyporheic zone were attenuated between 34% and 95%, in contrast to immeasurable attenuation in the shallow aquifer during contaminant transport between 0.1 and 1.5 miles (0.1 to 2.4 km). The attenuation observed in the hyporheic zone occurred primarily by physical processes such as mixing of groundwater and surface water. Biodegradation also occurred as confirmed in laboratory microcosms by the mineralization of U- <sup>14</sup>C-MTBE and U- <sup>14</sup>C-TBA to <sup>14</sup>CO<sub>2</sub> and the novel biodegradation of U- <sup>14</sup>C-TAME to <sup>14</sup>CO<sub>2</sub> under oxic and anoxic conditions. The implication of fuel oxygenate attenuation observed in diverse hyporheic zones suggests an assessment of the hyporheic zone attenuation potential (HZAP) merits inclusion as part of site assessment strategies associated with monitored or engineered attenuation.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2009.00608.x","issn":"0017467X","usgsCitation":"Landmeyer, J., Bradley, P.M., Trego, D., Hale, K., and Haas, J., 2010, MTBE, TBA, and TAME attenuation in diverse hyporheic zones: Ground Water, v. 48, no. 1, p. 30-41, https://doi.org/10.1111/j.1745-6584.2009.00608.x.","productDescription":"12 p.","startPage":"30","endPage":"41","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":241938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":214238,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2009.00608.x"}],"volume":"48","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-12-23","publicationStatus":"PW","scienceBaseUri":"505a4affe4b0c8380cd691fd","contributors":{"authors":[{"text":"Landmeyer, James 0000-0002-5640-3816 jlandmey@usgs.gov","orcid":"https://orcid.org/0000-0002-5640-3816","contributorId":3257,"corporation":false,"usgs":true,"family":"Landmeyer","given":"James","email":"jlandmey@usgs.gov","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":442870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradley, Paul M. 0000-0001-7522-8606 pbradley@usgs.gov","orcid":"https://orcid.org/0000-0001-7522-8606","contributorId":361,"corporation":false,"usgs":true,"family":"Bradley","given":"Paul","email":"pbradley@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":442867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trego, D.A.","contributorId":66930,"corporation":false,"usgs":true,"family":"Trego","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":442869,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hale, K.G.","contributorId":40436,"corporation":false,"usgs":true,"family":"Hale","given":"K.G.","email":"","affiliations":[],"preferred":false,"id":442868,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haas, J.E. II","contributorId":107113,"corporation":false,"usgs":true,"family":"Haas","given":"J.E.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":442871,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70179617,"text":"70179617 - 2010 - Effects of natural-channel-design restoration on habitat quality in Catskill Mountain streams, New York","interactions":[],"lastModifiedDate":"2017-04-25T16:53:44","indexId":"70179617","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"Effects of natural-channel-design restoration on habitat quality in Catskill Mountain streams, New York","docAbstract":"<p><span>Stream restoration has received much attention in recent years, yet there has been little effort to evaluate its impacts on physical habitat, stability, and biota. A popular but controversial stream restoration approach is natural channel design (NCD), which cannot be adequately evaluated without a long-term, independent assessment of its effects on stream habitat. Six reaches of five Catskill Mountain streams in southeastern New York were restored during 2000–2003 following NCD techniques to decrease bed and bank degradation, decrease sediment loads, and improve water quality. Habitat surveys were conducted during summer low flows from 2001 to 2007. The effects of the NCD projects on stream condition were assessed via a before–after–control–impact study design to quantify the net changes in stream and bank habitat variables relative to those in unaltered control reaches. Analysis of variance tests of three different measures of bank stability show that on average stream stability increased at treatment sites for 2–5 years after restoration. Mean channel depth, thalweg depth, and the pool–riffle ratio generally increased, whereas mean channel width, percent streambank coverage by trees, and shade decreased. Habitat suitability indices for local salmonid species increased at four of six reaches after restoration. The changes in channel dimensions rendered them generally more characteristic of stabler stream forms in the given valley settings. Although these studies were done relatively soon after project completion, our findings demonstrate that habitat conditions can be improved in degraded Catskill Mountain streams through NCD restoration.</span></p>","language":"English","publisher":"Taylor and Francis","doi":"10.1577/T08-153.1","usgsCitation":"Ernst, A.G., Baldigo, B.P., Mulvihill, C., and Vian, M., 2010, Effects of natural-channel-design restoration on habitat quality in Catskill Mountain streams, New York: Transactions of the American Fisheries Society, v. 139, no. 2, p. 468-482, https://doi.org/10.1577/T08-153.1.","productDescription":"15 p.","startPage":"468","endPage":"482","ipdsId":"IP-005439","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":332939,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Catskill Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.4,\n              42\n            ],\n            [\n              -74.4,\n              42.3167\n            ],\n            [\n              -74,\n              42.3167\n            ],\n            [\n              -74,\n              42\n            ],\n            [\n              -74.4,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"139","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"58772b2ae4b0315b4c11fea0","contributors":{"authors":[{"text":"Ernst, Anne G.","contributorId":149841,"corporation":false,"usgs":false,"family":"Ernst","given":"Anne","email":"","middleInitial":"G.","affiliations":[{"id":17837,"text":"USGS NY Water Science Center","active":true,"usgs":false}],"preferred":false,"id":657912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldigo, Barry P. 0000-0002-9862-9119 bbaldigo@usgs.gov","orcid":"https://orcid.org/0000-0002-9862-9119","contributorId":1234,"corporation":false,"usgs":true,"family":"Baldigo","given":"Barry","email":"bbaldigo@usgs.gov","middleInitial":"P.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":657913,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulvihill, Christiane mulvihil@usgs.gov","contributorId":1078,"corporation":false,"usgs":true,"family":"Mulvihill","given":"Christiane","email":"mulvihil@usgs.gov","affiliations":[],"preferred":true,"id":657914,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vian, Mark","contributorId":178095,"corporation":false,"usgs":false,"family":"Vian","given":"Mark","email":"","affiliations":[],"preferred":false,"id":657915,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70187016,"text":"70187016 - 2010 - Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","interactions":[],"lastModifiedDate":"2017-04-19T10:02:29","indexId":"70187016","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","docAbstract":"<p>No abstract available.<br></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tropical montane cloud forests: science for conservation and management","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","usgsCitation":"Giambelluca, T.W., DeLay, J.K., Nullet, M., Scholl, M.A., and 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K.","contributorId":191118,"corporation":false,"usgs":false,"family":"DeLay","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":691904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nullet, M.A.","contributorId":191119,"corporation":false,"usgs":false,"family":"Nullet","given":"M.A.","affiliations":[],"preferred":false,"id":691905,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scholl, Martha A. 0000-0001-6994-4614 mascholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6994-4614","contributorId":1920,"corporation":false,"usgs":true,"family":"Scholl","given":"Martha","email":"mascholl@usgs.gov","middleInitial":"A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":691903,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gingerich, Stephen B. 0000-0002-4381-0746 sbginger@usgs.gov","orcid":"https://orcid.org/0000-0002-4381-0746","contributorId":1426,"corporation":false,"usgs":true,"family":"Gingerich","given":"Stephen","email":"sbginger@usgs.gov","middleInitial":"B.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":691906,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70179616,"text":"70179616 - 2010 - Variable responses of fish assemblages, habitat, and stability to natural-channel-design restoration in Catskill Mountain streams","interactions":[],"lastModifiedDate":"2017-04-25T16:53:25","indexId":"70179616","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"Variable responses of fish assemblages, habitat, and stability to natural-channel-design restoration in Catskill Mountain streams","docAbstract":"<p><span>Natural-channel-design (NCD) restorations were recently implemented within large segments of five first- and second-order streams in the Catskill Mountains of New York in an attempt to increase channel stability, reduce bed and bank erosion, and sustain water quality. In conjunction with these efforts, 54 fish and habitat surveys were done from 1999 to 2007 at six restored reaches and five stable control reaches to evaluate the effects of NCD restoration on fish assemblages, habitat, and bank stability. A before–after–control–impact study design and two-factor analysis of variance were used to quantify the net changes in habitat and fish population and community indices at treatment reaches relative to those at unaltered control reaches. The density and biomass of fish communities were often dominated by one or two small prey species and no or few predator species before restoration and by one or more trout (Salmonidae) species after restoration. Significant increases in community richness (30%), diversity (40%), species or biomass equitability (32%), and total biomass (up to 52%) in at least four of the six restored reaches demonstrate that NCD restorations can improve the health and sustainability of fish communities in geomorphically unstable Catskill Mountain streams over the short to marginally long term. Bank stability, stream habitat, and trout habitat suitability indices (HSIs) generally improved significantly at the restored reaches, but key habitat features and trout HSIs did not change or decreased at two of them. Fish communities and trout populations at these two reaches were not positively affected by NCD restorations. Though NCD restorations often had a positive effect on habitat and fish communities, our results show that the initial habitat conditions limit the relative improvements than can be achieved, habitat quality and stability do not necessarily respond in unison, and biotic and abiotic responses cannot always be generalized.</span></p>","language":"English","publisher":"Taylor and Francis","doi":"10.1577/T08-152.1","usgsCitation":"Baldigo, B.P., Ernst, A.G., Warren, D.R., and Miller, S.J., 2010, Variable responses of fish assemblages, habitat, and stability to natural-channel-design restoration in Catskill Mountain streams: Transactions of the American Fisheries Society, v. 139, no. 2, p. 449-467, https://doi.org/10.1577/T08-152.1.","startPage":"449","endPage":"467","ipdsId":"IP-006022","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":332938,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Catskill Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.4,\n              42\n            ],\n            [\n              -74.4,\n              42.3167\n            ],\n            [\n              -74,\n              42.3167\n            ],\n            [\n              -74,\n              42\n            ],\n            [\n              -74.4,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"139","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"58772b2be4b0315b4c11fea2","contributors":{"authors":[{"text":"Baldigo, Barry P. 0000-0002-9862-9119 bbaldigo@usgs.gov","orcid":"https://orcid.org/0000-0002-9862-9119","contributorId":1234,"corporation":false,"usgs":true,"family":"Baldigo","given":"Barry","email":"bbaldigo@usgs.gov","middleInitial":"P.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":657908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ernst, Anne G.","contributorId":149841,"corporation":false,"usgs":false,"family":"Ernst","given":"Anne","email":"","middleInitial":"G.","affiliations":[{"id":17837,"text":"USGS NY Water Science Center","active":true,"usgs":false}],"preferred":false,"id":657909,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warren, Dana R.","contributorId":96139,"corporation":false,"usgs":true,"family":"Warren","given":"Dana","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":657910,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Sarah J.","contributorId":72857,"corporation":false,"usgs":true,"family":"Miller","given":"Sarah","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":657911,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037483,"text":"70037483 - 2010 - Hydrated mineral stratigraphy of Ius Chasma, Valles Marineris","interactions":[],"lastModifiedDate":"2012-03-12T17:22:09","indexId":"70037483","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Hydrated mineral stratigraphy of Ius Chasma, Valles Marineris","docAbstract":"New high-resolution spectral and morphologic imaging of deposits on walls and floor of Ius Chasma extend previous geomorphic mapping, and permit a new interpretation of aqueous processes that occurred during the development of Valles Marineris. We identify hydrated mineralogy based on visible-near infrared (VNIR) absorptions. We map the extents of these units with CRISM spectral data as well as morphologies in CTX and HiRISE imagery. Three cross-sections across Ius Chasma illustrate the interpreted mineral stratigraphy. Multiple episodes formed and transported hydrated minerals within Ius Chasma. Polyhydrated sulfate and kieserite are found within a closed basin at the lowest elevations in the chasma. They may have been precipitates in a closed basin or diagenetically altered after deposition. Fluvial or aeolian processes then deposited layered Fe/Mg smectite and hydrated silicate on the chasma floor, postdating the sulfates. The smectite apparently was weathered out of Noachian-age wallrock and transported to the depositional sites. The overlying hydrated silicate is interpreted to be an acid-leached phyllosilicate transformed from the underlying smectite unit, or a smectite/jarosite mixture. The finely layered smectite and massive hydrated silicate units have an erosional unconformity between them, that marks a change in surface water chemistry. Landslides transported large blocks of wallrock, some altered to contain Fe/Mg smectite, to the chasma floor. After the last episode of normal faulting and subsequent landslides, opal was transported short distances into the chasma from a few m-thick light-toned layer near the top of the wallrock, by sapping channels in Louros Valles. Alternatively, the material was transported into the chasma and then altered to opal. The superposition of different types of hydrated minerals and the different fluvial morphologies of the units containing them indicate sequential, distinct aqueous environments, characterized by alkaline, then circum-neutral, and finally very acidic surface or groundwater chemistry. ?? 2009 Elsevier Inc. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.icarus.2009.09.003","issn":"00191035","usgsCitation":"Roach, L., Mustard, J., Swayze, G., Milliken, R., Bishop, J., Murchie, S., and Lichtenberg, K., 2010, Hydrated mineral stratigraphy of Ius Chasma, Valles Marineris: Icarus, v. 206, no. 1, p. 253-268, https://doi.org/10.1016/j.icarus.2009.09.003.","startPage":"253","endPage":"268","numberOfPages":"16","costCenters":[],"links":[{"id":217127,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2009.09.003"},{"id":245045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"206","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a32c5e4b0c8380cd5ea7d","contributors":{"authors":[{"text":"Roach, L.H.","contributorId":80906,"corporation":false,"usgs":true,"family":"Roach","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":461270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mustard, J.F.","contributorId":91605,"corporation":false,"usgs":true,"family":"Mustard","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":461272,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swayze, G. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":55131,"corporation":false,"usgs":true,"family":"Swayze","given":"G.","affiliations":[],"preferred":false,"id":461268,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Milliken, R.E.","contributorId":98022,"corporation":false,"usgs":true,"family":"Milliken","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":461273,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bishop, J.L.","contributorId":83244,"corporation":false,"usgs":true,"family":"Bishop","given":"J.L.","affiliations":[],"preferred":false,"id":461271,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Murchie, S.L.","contributorId":7369,"corporation":false,"usgs":true,"family":"Murchie","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":461267,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lichtenberg, K.","contributorId":65343,"corporation":false,"usgs":true,"family":"Lichtenberg","given":"K.","email":"","affiliations":[],"preferred":false,"id":461269,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037380,"text":"70037380 - 2010 - A trial of two trouts: Comparing the impacts of rainbow and brown trout on a native galaxiid","interactions":[],"lastModifiedDate":"2017-11-17T15:39:12","indexId":"70037380","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":774,"text":"Animal Conservation","active":true,"publicationSubtype":{"id":10}},"title":"A trial of two trouts: Comparing the impacts of rainbow and brown trout on a native galaxiid","docAbstract":"Rainbow trout Oncorhynchus mykiss and brown trout Salmo trutta are the world's two most widespread exotic fishes, dominate the fish communities of most cold-temperate waters in the southern hemisphere and are implicated in the decline and extirpation of native fish species. Here, we provide the first direct comparison of the impacts of rainbow and brown trout on populations of a native fish by quantifying three components of exotic species impact: range, abundance and effect. We surveyed 54 small streams on the island of Chilo?? in Chilean Patagonia and found that the rainbow trout has colonized significantly more streams and has a wider geographic range than brown trout. The two species had similar post-yearling abundances in allopatry and sympatry, and their abundances depended similarly on reach-level variation in the physical habitat. The species appeared to have dramatically different effects on native drift-feeding Aplochiton spp., which were virtually absent from streams invaded by brown trout but shared a broad sympatric range with rainbow trout. Within this range, the species' post-yearling abundances varied independently before and after controlling for variation in the physical habitat. In the north of the island, Aplochiton spp. inhabited streams uninvaded by exotic trouts. Our results provide a context for investigating the mechanisms responsible for apparent differences in rainbow and brown trout invasion biology and can help inform conservation strategies for native fishes in Chilo?? and elsewhere. ?? 2010 The Authors. Journal compilation ?? 2010 The Zoological Society of London.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Animal Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1469-1795.2010.00354.x","issn":"13679430","usgsCitation":"Young, K., Dunham, J., Stephenson, J., Terreau, A., Thailly, A., Gajardo, G., and de Leaniz, C.G., 2010, A trial of two trouts: Comparing the impacts of rainbow and brown trout on a native galaxiid: Animal Conservation, v. 13, no. 4, p. 399-410, https://doi.org/10.1111/j.1469-1795.2010.00354.x.","startPage":"399","endPage":"410","numberOfPages":"12","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":245229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217294,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1469-1795.2010.00354.x"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-23","publicationStatus":"PW","scienceBaseUri":"5059e606e4b0c8380cd470e6","contributors":{"authors":[{"text":"Young, K.A.","contributorId":77775,"corporation":false,"usgs":true,"family":"Young","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":460781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunham, J. B. 0000-0002-6268-0633","orcid":"https://orcid.org/0000-0002-6268-0633","contributorId":96637,"corporation":false,"usgs":true,"family":"Dunham","given":"J. B.","affiliations":[],"preferred":false,"id":460782,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stephenson, J.F.","contributorId":33556,"corporation":false,"usgs":true,"family":"Stephenson","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":460777,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Terreau, A.","contributorId":101120,"corporation":false,"usgs":true,"family":"Terreau","given":"A.","email":"","affiliations":[],"preferred":false,"id":460783,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thailly, A.F.","contributorId":33557,"corporation":false,"usgs":true,"family":"Thailly","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":460778,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gajardo, G.","contributorId":45932,"corporation":false,"usgs":true,"family":"Gajardo","given":"G.","affiliations":[],"preferred":false,"id":460779,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"de Leaniz, C. G.","contributorId":54047,"corporation":false,"usgs":true,"family":"de Leaniz","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":460780,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70037542,"text":"70037542 - 2010 - Liquefaction caused by the 2009 Olancha, California (USA), <i>M</i>5.2 earthquake","interactions":[],"lastModifiedDate":"2012-12-18T10:38:21","indexId":"70037542","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1517,"text":"Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"Liquefaction caused by the 2009 Olancha, California (USA), <i>M</i>5.2 earthquake","docAbstract":"The October 3, 2009 (01:16:00 UTC), Olancha <i>M</i>5.2 earthquake caused extensive liquefaction as well as permanent horizontal ground deformation within a 1.2 km<sup>2</sup>area earthquake in Owens Valley in eastern California (USA). Such liquefaction is rarely observed during earthquakes of <i>M</i> ≤ 5.2. We conclude that subsurface conditions, not unusual ground motion, were the primary factors contributing to the liquefaction. The liquefaction occurred in very liquefiable sands at shallow depth (< 2 m) in an area where the water table was near the land surface. Our investigation is relevant to both geotechnical engineering and geology. The standard engineering method for assessing liquefaction potential, the Seed–Idriss simplified procedure, successfully predicted the liquefaction despite the small earthquake magnitude. The field observations of liquefaction effects highlight a need for caution by earthquake geologists when inferring prehistoric earthquake magnitudes from paleoliquefaction features because small magnitude events may cause such features.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Engineering Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.enggeo.2010.07.009","issn":"00137952","usgsCitation":"Holzer, T., Jayko, A.S., Hauksson, E., Fletcher, J., Noce, T., Bennett, M., Dietel, C., and Hudnut, K., 2010, Liquefaction caused by the 2009 Olancha, California (USA), <i>M</i>5.2 earthquake: Engineering Geology, v. 116, no. 1-2, p. 184-188, https://doi.org/10.1016/j.enggeo.2010.07.009.","productDescription":"5 p.","startPage":"184","endPage":"188","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":218072,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.enggeo.2010.07.009"},{"id":246052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Olancha","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.035125,36.22622 ], [ -118.035125,36.315234 ], [ -117.968329,36.315234 ], [ -117.968329,36.22622 ], [ -118.035125,36.22622 ] ] ] } } ] }","volume":"116","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a47eae4b0c8380cd67a98","contributors":{"authors":[{"text":"Holzer, T.L.","contributorId":35739,"corporation":false,"usgs":true,"family":"Holzer","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":461529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jayko, A. S. 0000-0002-7378-0330","orcid":"https://orcid.org/0000-0002-7378-0330","contributorId":18011,"corporation":false,"usgs":true,"family":"Jayko","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":461527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hauksson, E.","contributorId":10932,"corporation":false,"usgs":true,"family":"Hauksson","given":"E.","affiliations":[],"preferred":false,"id":461525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fletcher, J.P.B.","contributorId":96936,"corporation":false,"usgs":true,"family":"Fletcher","given":"J.P.B.","email":"","affiliations":[],"preferred":false,"id":461532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Noce, T.E.","contributorId":54285,"corporation":false,"usgs":true,"family":"Noce","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":461530,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bennett, M.J.","contributorId":67504,"corporation":false,"usgs":true,"family":"Bennett","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":461531,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Dietel, C.M.","contributorId":11245,"corporation":false,"usgs":true,"family":"Dietel","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":461526,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hudnut, K.W.","contributorId":25179,"corporation":false,"usgs":true,"family":"Hudnut","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":461528,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
]}