{"pageNumber":"1900","pageRowStart":"47475","pageSize":"25","recordCount":184982,"records":[{"id":70155365,"text":"70155365 - 2010 - Founding population size of an aquatic invasive species","interactions":[],"lastModifiedDate":"2015-08-07T11:52:16","indexId":"70155365","displayToPublicDate":"2010-10-01T13:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1324,"text":"Conservation Genetics","active":true,"publicationSubtype":{"id":10}},"title":"Founding population size of an aquatic invasive species","docAbstract":"<p><span>Non-native species of fish threaten native fishes throughout North America, and in the Rocky Mountains, introduced populations of lake trout threaten native populations of bull trout. Effective management of lake trout and other exotic species require understanding the dynamics of invasion in order to either suppress non-native populations or to prevent their spread. In this study, we used microsatellite genetic data to estimate the number of lake trout that invaded a population of bull trout in Swan Lake, MT. Examination of genetic diversity and allele frequencies within the Swan Lake populations showed that most of the genes in the lake trout population are descended from two founders. This emphasizes the importance of preventing even a few lake trout from colonizing new territory.</span></p>","language":"English","publisher":"Kluwer Academic Publishers","publisherLocation":"Dordrecht","doi":"10.1007/s10592-009-0041-8","usgsCitation":"Kalinowski, S.T., Muhlfeld, C.C., Guy, C.S., and Benjamin Cox, 2010, Founding population size of an aquatic invasive species: Conservation Genetics, v. 11, no. 5, p. 2049-2053, https://doi.org/10.1007/s10592-009-0041-8.","productDescription":"5 p.","startPage":"2049","endPage":"2053","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-015953","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":306504,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"5","publishingServiceCenter":{"id":3,"text":"Helena PSC"},"noUsgsAuthors":false,"publicationDate":"2010-09-16","publicationStatus":"PW","scienceBaseUri":"57fe821de4b0824b2d148457","contributors":{"authors":[{"text":"Kalinowski, Steven T.","contributorId":145736,"corporation":false,"usgs":false,"family":"Kalinowski","given":"Steven","email":"","middleInitial":"T.","affiliations":[{"id":16214,"text":"Montana State University, Department of Ecology","active":true,"usgs":false}],"preferred":false,"id":565555,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muhlfeld, Clint C. 0000-0002-4599-4059 cmuhlfeld@usgs.gov","orcid":"https://orcid.org/0000-0002-4599-4059","contributorId":924,"corporation":false,"usgs":true,"family":"Muhlfeld","given":"Clint","email":"cmuhlfeld@usgs.gov","middleInitial":"C.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":565553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guy, Christopher S. 0000-0002-9936-4781 cguy@usgs.gov","orcid":"https://orcid.org/0000-0002-9936-4781","contributorId":2876,"corporation":false,"usgs":true,"family":"Guy","given":"Christopher","email":"cguy@usgs.gov","middleInitial":"S.","affiliations":[{"id":5062,"text":"Office of the Chief Scientist for Ecosystems","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":565552,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Benjamin Cox","contributorId":145879,"corporation":false,"usgs":false,"family":"Benjamin Cox","affiliations":[{"id":6765,"text":"Montana State University, Department of Land Resources and Environmental Sciences","active":true,"usgs":false}],"preferred":false,"id":565554,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70202250,"text":"70202250 - 2010 - Fundamental changes in the activity of the natrocarbonatite volcano Oldoinyo Lengai, Tanzania","interactions":[],"lastModifiedDate":"2021-01-28T20:30:17.852547","indexId":"70202250","displayToPublicDate":"2010-10-01T12:25:47","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"Fundamental changes in the activity of the natrocarbonatite volcano Oldoinyo Lengai, Tanzania","docAbstract":"<p><span>On September 4, 2007, after 25&nbsp;years of effusive natrocarbonatite eruptions, the eruptive activity of Oldoinyo Lengai (OL), N Tanzania, changed abruptly to episodic explosive eruptions. This transition was preceded by a voluminous lava eruption in March 2006, a year of quiescence, resumption of natrocarbonatite eruptions in June 2007, and a volcano-tectonic earthquake swarm in July 2007. Despite the lack of ground-based monitoring, the evolution in OL eruption dynamics is documented based on the available field observations, ASTER and MODIS satellite images, and almost-daily photos provided by local pilots. Satellite data enabled identification of a phase of voluminous lava effusion in the 2&nbsp;weeks prior to the onset of explosive eruptions. After the onset, the activity varied from 100&nbsp;m high ash jets to 2–15&nbsp;km high violent, steady or unsteady, eruption columns dispersing ash to 100&nbsp;km distance. The explosive eruptions built up a ∼400&nbsp;m wide, ∼75&nbsp;m high intra-crater pyroclastic cone. Time series data for eruption column height show distinct peaks at the end of September 2007 and February 2008, the latter being associated with the first pyroclastic flows to be documented at OL. Chemical analyses of the erupted products, presented in a companion paper (Keller et al.&nbsp;</span><a id=\"ref-link-section-d14976e534\" title=\"Keller J, Klaudius J, Kervyn M, Ernst GGJ, Mattsson HB (2010) Fundamental changes in the activity of the natrocarbonatite volcano Oldoinyo Lengai, Tanzania. I. New magma composition. Bull Volcanol. doi:\n                    10.1007/s00445-010-0371-x\n                    \n                  \n                        \" href=\"https://link.springer.com/article/10.1007/s00445-010-0360-0#ref-CR30\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 2010\" data-mce-href=\"https://link.springer.com/article/10.1007/s00445-010-0360-0#ref-CR30\">2010</a><span>), show that the 2007–2008 explosive eruptions are associated with an undersaturated carbonated silicate melt. This new phase of explosive eruptions provides constraints on the factors causing the transition from natrocarbonatite effusive eruptions to explosive eruptions of carbonated nephelinite magma, observed repetitively in the last 100&nbsp;years at OL.</span></p>","language":"English","publisher":"Springer Link","doi":"10.1007/s00445-010-0360-0","usgsCitation":"Kervyn, M., Ernst, G.G., Keller, J., Vaughan, R.G., Klaudius, J., Pradal, E., Belton, F., Mattsson, H.B., Mbede, E., and Jacobs, P., 2010, Fundamental changes in the activity of the natrocarbonatite volcano Oldoinyo Lengai, Tanzania: Bulletin of Volcanology, v. 72, no. 8, p. 913-931, https://doi.org/10.1007/s00445-010-0360-0.","productDescription":"19 p.","startPage":"913","endPage":"931","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":361317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Tanzania","otherGeospatial":"Oldoinyo Lengai","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              35.068359375,\n              -3.510679621863856\n            ],\n            [\n              35.068359375,\n              -2.2077054557053954\n            ],\n            [\n              36.6558837890625,\n              -2.2077054557053954\n            ],\n            [\n              36.6558837890625,\n              -3.510679621863856\n            ],\n            [\n              35.068359375,\n              -3.510679621863856\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"72","issue":"8","noUsgsAuthors":false,"publicationDate":"2010-05-16","publicationStatus":"PW","contributors":{"authors":[{"text":"Kervyn, Matthieu","contributorId":213338,"corporation":false,"usgs":false,"family":"Kervyn","given":"Matthieu","email":"","affiliations":[],"preferred":false,"id":757494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ernst, Gerald G.J.","contributorId":213339,"corporation":false,"usgs":false,"family":"Ernst","given":"Gerald","email":"","middleInitial":"G.J.","affiliations":[],"preferred":false,"id":757495,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keller, Jorg","contributorId":213340,"corporation":false,"usgs":false,"family":"Keller","given":"Jorg","email":"","affiliations":[],"preferred":false,"id":757496,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vaughan, R. Greg 0000-0002-0850-6669","orcid":"https://orcid.org/0000-0002-0850-6669","contributorId":69030,"corporation":false,"usgs":true,"family":"Vaughan","given":"R.","email":"","middleInitial":"Greg","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":757497,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klaudius, Jurgis","contributorId":213341,"corporation":false,"usgs":false,"family":"Klaudius","given":"Jurgis","email":"","affiliations":[],"preferred":false,"id":757498,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pradal, Evelyne","contributorId":213342,"corporation":false,"usgs":false,"family":"Pradal","given":"Evelyne","email":"","affiliations":[],"preferred":false,"id":757499,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Belton, Frederic","contributorId":213343,"corporation":false,"usgs":false,"family":"Belton","given":"Frederic","email":"","affiliations":[],"preferred":false,"id":757500,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mattsson, Hannes B.","contributorId":213344,"corporation":false,"usgs":false,"family":"Mattsson","given":"Hannes","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":757501,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Mbede, Evelyne","contributorId":213345,"corporation":false,"usgs":false,"family":"Mbede","given":"Evelyne","email":"","affiliations":[],"preferred":false,"id":757502,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Jacobs, Patric","contributorId":213346,"corporation":false,"usgs":false,"family":"Jacobs","given":"Patric","email":"","affiliations":[],"preferred":false,"id":757503,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70199843,"text":"70199843 - 2010 - Tree growth and mortality during 20 years of managing a Green-Tree Reservoir in Arkansas, USA","interactions":[],"lastModifiedDate":"2018-10-01T11:51:24","indexId":"70199843","displayToPublicDate":"2010-10-01T11:44:14","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Tree growth and mortality during 20 years of managing a Green-Tree Reservoir in Arkansas, USA","docAbstract":"<p><span>Green-Tree Reservoirs (GTR) are bottomland hardwood forests that are flooded during late fall and winter to provide waterfowl habitat. Early reports suggested that increased moisture improved tree growth and mast production; however, recent reports showed reduced vigor and growth. This study examines the effects of 20&nbsp;years of GTR management practices in the Felsenthal National Wildlife Refuge, Crossett, Arkansas. Tree species composition, size characteristics, and vigor classes were measured in 1990, 1995, 2001, and 2006. The overall annual tree mortality rate was 2.6%, with high elevations at 1.7% and low elevations at 3.1%. Annual mortality rates exceeded 3% for willow oak (</span><i class=\"EmphasisTypeItalic \">Quercus phellos</i><span>) and water hickory (</span><i class=\"EmphasisTypeItalic \">Carya aquatica</i><span>), while rates for Nuttall oak (</span><i class=\"EmphasisTypeItalic \">Q. texana</i><span>), overcup oak (</span><i class=\"EmphasisTypeItalic \">Q. lyrata</i><span>), and sweetgum (</span><i class=\"EmphasisTypeItalic \">Liquidambar styraciflua</i><span>.) were lower at 2.8, 2.4, and 1.5%, respectively. Tree health (vigor) has degraded substantially for over 60% of trees initially rated in good or fair condition. Statistical probit models were generated to predict short-term (5&nbsp;years) and long-term (15&nbsp;years) vigor degradation. Low numbers of saplings and little advanced regeneration indicated lack of tree replacement, suggesting that inundation strategies of the GTR management may have long-term impacts on forest structure and composition in the southeastern United States.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s13157-010-0062-6","usgsCitation":"Keeland, B.D., Draugelis-Dale, R.O., and McCoy, J.W., 2010, Tree growth and mortality during 20 years of managing a Green-Tree Reservoir in Arkansas, USA: Wetlands, v. 30, p. 405-416, https://doi.org/10.1007/s13157-010-0062-6.","productDescription":"12 p.","startPage":"405","endPage":"416","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":357951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas","volume":"30","noUsgsAuthors":false,"publicationDate":"2010-05-04","publicationStatus":"PW","scienceBaseUri":"5c10c655e4b034bf6a7f3e23","contributors":{"authors":[{"text":"Keeland, Bobby D.","contributorId":103506,"corporation":false,"usgs":true,"family":"Keeland","given":"Bobby","email":"","middleInitial":"D.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":746864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Draugelis-Dale, Rassa O. 0000-0001-8532-3287 daler@usgs.gov","orcid":"https://orcid.org/0000-0001-8532-3287","contributorId":20422,"corporation":false,"usgs":true,"family":"Draugelis-Dale","given":"Rassa","email":"daler@usgs.gov","middleInitial":"O.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":746865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCoy, John W. 0000-0003-3013-730X mccoyj@usgs.gov","orcid":"https://orcid.org/0000-0003-3013-730X","contributorId":3082,"corporation":false,"usgs":true,"family":"McCoy","given":"John","email":"mccoyj@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":746866,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70236491,"text":"70236491 - 2010 - Persistent organic pollutants in the blood of free-ranging sea otters (Enhydra lutris ssp.) in Alaska and California","interactions":[],"lastModifiedDate":"2022-09-08T16:53:09.211391","indexId":"70236491","displayToPublicDate":"2010-10-01T11:30:16","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Persistent organic pollutants in the blood of free-ranging sea otters (<i>Enhydra lutris</i> ssp.) in Alaska and California","title":"Persistent organic pollutants in the blood of free-ranging sea otters (Enhydra lutris ssp.) in Alaska and California","docAbstract":"<p>As part of tagging and ecologic research efforts in 1997 and 1998, apparently healthy sea otters of four age-sex classes in six locations in Alaska and three in California were sampled for persistent organic pollutants (POPs) and other chemicals of ecologic or environmental concern (COECs). Published techniques for the detection of POPs (specifically Σpolychlorinated biphenyls [PCBs], ΣDDTs, Σhexachlorocyclohexanes [HCHs], Σpolycyclic aromatic hydrocarbons [PAHs], Σchlordanes [CHLs], hexachlorobenzene [HCB], dieldrin, and mirex) in the tissue of dead otters were modified for use with serum from live sea otters. Toxic equivalencies (TEQs) were calculated for POPs with proven bioactivity. Strong location effects were seen for most POPs and COECs; sea otters in California generally showed higher mean concentrations than those in Alaska. Differences in contaminant concentrations were detected among age and sex classes, with high levels frequently observed in subadults. Very high levels of ΣDDT were detected in male sea otters in Elkhorn Slough, California, where strong freshwater outflow from agricultural areas occurs seasonally. All contaminants except mirex differed among Alaskan locations; only ΣDDT, HCB, and chlorpyrifos differed within California. High levels of ΣPCB (particularly larger, more persistent congeners) were detected at two locations in Alaska where associations between elevated PCBs and military activity have been established, while higher PCB levels were found at all three locations in California where no point source of PCBs has been identified. Although POP and COEC concentrations in blood may be less likely to reflect total body burden, concentrations in blood of healthy animals may be more biologically relevant and less influenced by state of nutrition or perimortem factors than other tissues routinely sampled.</p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-46.4.1214","usgsCitation":"Jessup, D., Johnson, C., Estes, J.A., Carlson-Bremer, D., Jarman, W.M., Reese, S., Dodd, E., Tinker, M.T., and Ziccardi, M.H., 2010, Persistent organic pollutants in the blood of free-ranging sea otters (Enhydra lutris ssp.) in Alaska and California: Journal of Wildlife Diseases, v. 46, no. 4, p. 1214-1233, https://doi.org/10.7589/0090-3558-46.4.1214.","productDescription":"20 p.","startPage":"1214","endPage":"1233","costCenters":[],"links":[{"id":475658,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-46.4.1214","text":"Publisher Index 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,{"id":70101966,"text":"70101966 - 2010 - Wayward youth: Trans-Beringian movement and differential southward migration by juvenile sharp-tailed sandpipers","interactions":[],"lastModifiedDate":"2021-01-08T18:29:30.165691","indexId":"70101966","displayToPublicDate":"2010-10-01T10:17:01","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":894,"text":"Arctic","active":true,"publicationSubtype":{"id":10}},"title":"Wayward youth: Trans-Beringian movement and differential southward migration by juvenile sharp-tailed sandpipers","docAbstract":"<p><span>The sharp-tailed sandpiper (</span><i>Calidris acuminata</i><span>) is a long-distance migrant that travels each year from breeding grounds in the Russian Arctic to nonbreeding areas in Australasia. Most adults migrate rapidly from breeding grounds along a largely inland route through Asia. Here we report on the highly unusual migratory strategy of this species in which some juveniles, but virtually no adults, take a pronounced detour to western Alaska before proceeding on southward migration. We analyzed data from our own studies in this region and published and unpublished observations and specimen records of sharptailed sandpipers from the entire Pacific Basin. Each autumn, sharp-tailed sandpipers began arriving on coastal graminoid meadows and intertidal habitats throughout western Alaska during the last half of August and the last sandpipers departed from southwestern Alaska during October and November. Body mass of birds banded or collected across multiple years and sites in western Alaska (</span><i>n</i><span>&nbsp;= 330) increased by an average of 0.57 ± 0.06 g per day between mid-August and late October. Records suggest a small, regular movement of juveniles (and a very few adults) along the Asiatic coast, but we estimate from surveys that a few tens of thousands of juveniles stage in western Alaska each autumn. The distribution of sight and specimen records from the Pacific Basin during autumn suggests strongly age-segregated migration routes, with the principal migration of juveniles crossing central and western Oceania in a possible nonstop trans-Pacific flight from Alaska. This is only the second well-documented case of differential migration among birds that involves different routes for adults and juveniles, and it raises intriguing questions about how and why this system has evolved.&nbsp;</span></p>","language":"English","publisher":"Arctic Institute of North America","doi":"10.14430/arctic1492","usgsCitation":"Handel, C.M., and Gill, R., 2010, Wayward youth: Trans-Beringian movement and differential southward migration by juvenile sharp-tailed sandpipers: Arctic, v. 63, no. 3, p. 273-288, https://doi.org/10.14430/arctic1492.","productDescription":"16 p.","startPage":"273","endPage":"288","ipdsId":"IP-016704","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":475659,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14430/arctic1492","text":"Publisher Index Page"},{"id":382035,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-09-01","publicationStatus":"PW","scienceBaseUri":"535595dfe4b0120853e8c305","contributors":{"authors":[{"text":"Handel, Colleen M. 0000-0002-0267-7408 cmhandel@usgs.gov","orcid":"https://orcid.org/0000-0002-0267-7408","contributorId":3067,"corporation":false,"usgs":true,"family":"Handel","given":"Colleen","email":"cmhandel@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":492817,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":492818,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70236110,"text":"70236110 - 2010 - Development of characterization technology for fault zone hydrology","interactions":[],"lastModifiedDate":"2022-08-29T15:40:00.044797","indexId":"70236110","displayToPublicDate":"2010-10-01T10:06:32","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Development of characterization technology for fault zone hydrology","docAbstract":"<p>Several deep trenches were cut, and a number of geophysical surveys were conducted across the Wildcat Fault in the hills east of Berkeley, California. The Wildcat Fault is believed to be a strike-slip fault and a member of the Hayward Fault System, with over 10 km of displacement. So far, three boreholes of ∼ 150m deep have been core-drilled and borehole geophysical logs were conducted. The rocks are extensively sheared and fractured; gouges were observed at several depths and a thick cataclasitic zone was also observed. While confirming some earlier, published conclusions from shallow observations about Wildcat, some unexpected findings were encountered. Preliminary analysis indicates that Wildcat near the field site consists of multiple faults. The hydraulic test data suggest the dual properties of the hydrologic structure of the fault zone. A fourth borehole is planned to penetrate the main fault believed to lie in-between the holes. The main philosophy behind our approach for the hydrologic characterization of such a complex fractured system is to let the system take its own average and monitor a long term behavior instead of collecting a multitude of data at small length and time scales, or at a discrete fracture scale and to “up-scale,” which is extremely tenuous.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Conference proceedings: International Conference on Environmental Remediation and Radioactive Waste Management","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"13th International Conference on Environmental Remediation and Radioactive Waste Management","conferenceDate":"October 3-7, 2010","conferenceLocation":"Tsukuba, Japan","language":"English","publisher":"American Society of Mechanical Engineers","doi":"10.1115/ICEM2010-40121","usgsCitation":"Karasaki, K., Onishi, C.T., Gasperikova, E., Goto, J., Tsuchi, H., Miwa, T., Ueta, K., Kiho, K., and Miyakawa, K., 2010, Development of characterization technology for fault zone hydrology, <i>in</i> Conference proceedings: International Conference on Environmental Remediation and Radioactive Waste Management, Tsukuba, Japan, October 3-7, 2010, p. 297-303, https://doi.org/10.1115/ICEM2010-40121.","productDescription":"ICEM2010-40121, 7 p.","startPage":"297","endPage":"303","costCenters":[],"links":[{"id":475661,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc1014656/","text":"External Repository"},{"id":405795,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Berkeley Hills, Wildcat Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.431640625,\n              37.96477144899956\n            ],\n            [\n              -122.34649658203124,\n              37.769629187677\n            ],\n            [\n              -122.16796875,\n              37.790251927933284\n            ],\n            [\n              -122.27508544921875,\n              38.04592811939909\n            ],\n            [\n              -122.37533569335936,\n              38.023213306976814\n            ],\n            [\n              -122.431640625,\n              37.96477144899956\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationDate":"2011-04-05","publicationStatus":"PW","contributors":{"authors":[{"text":"Karasaki, K.","contributorId":30004,"corporation":false,"usgs":true,"family":"Karasaki","given":"K.","email":"","affiliations":[],"preferred":false,"id":850094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Onishi, Celia Tiemi","contributorId":295897,"corporation":false,"usgs":false,"family":"Onishi","given":"Celia","email":"","middleInitial":"Tiemi","affiliations":[],"preferred":false,"id":850095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gasperikova, Erika","contributorId":193561,"corporation":false,"usgs":false,"family":"Gasperikova","given":"Erika","affiliations":[],"preferred":false,"id":850096,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goto, Junichi","contributorId":295898,"corporation":false,"usgs":false,"family":"Goto","given":"Junichi","email":"","affiliations":[],"preferred":false,"id":850097,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tsuchi, Hiroyuki","contributorId":295899,"corporation":false,"usgs":false,"family":"Tsuchi","given":"Hiroyuki","email":"","affiliations":[],"preferred":false,"id":850098,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Miwa, Tadashi","contributorId":295900,"corporation":false,"usgs":false,"family":"Miwa","given":"Tadashi","email":"","affiliations":[],"preferred":false,"id":850099,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ueta, Keiichi","contributorId":295901,"corporation":false,"usgs":false,"family":"Ueta","given":"Keiichi","email":"","affiliations":[],"preferred":false,"id":850100,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kiho, Kenzo","contributorId":295902,"corporation":false,"usgs":false,"family":"Kiho","given":"Kenzo","email":"","affiliations":[],"preferred":false,"id":850101,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Miyakawa, Kimio","contributorId":295903,"corporation":false,"usgs":false,"family":"Miyakawa","given":"Kimio","email":"","affiliations":[],"preferred":false,"id":850102,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70236312,"text":"70236312 - 2010 - Monitoring land-surface deformation on Bicycle Lake playa, Fort Irwin, California, USA","interactions":[],"lastModifiedDate":"2022-09-01T14:46:53.207125","indexId":"70236312","displayToPublicDate":"2010-10-01T09:34:03","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Monitoring land-surface deformation on Bicycle Lake playa, Fort Irwin, California, USA","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Eighth International Symposium on Land Subsidence","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"8th International Symposium on Land Subsidence","conferenceDate":"October 17-22, 2010","conferenceLocation":"Querétaro, Mexico","language":"English","publisher":"International Association of Hydrological Sciences Press","usgsCitation":"Densmore, J.N., Ellett, K., Howle, J.F., Carpenter, M.C., and Sneed, M., 2010, Monitoring land-surface deformation on Bicycle Lake playa, Fort Irwin, California, USA, <i>in</i> Eighth International Symposium on Land Subsidence, Querétaro, Mexico, October 17-22, 2010, p. 39-43.","productDescription":"5 p.","startPage":"39","endPage":"43","costCenters":[],"links":[{"id":406065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Fort Irwin","otherGeospatial":"Bicycle Lake playa, Mojave Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.63274765014648,\n              35.263842186385766\n            ],\n            [\n              -116.62141799926756,\n              35.266224903216894\n            ],\n            [\n              -116.61523818969727,\n              35.27288212294965\n            ],\n            [\n              -116.6113758087158,\n              35.28381279171024\n            ],\n            [\n              -116.60751342773436,\n              35.29544252406548\n            ],\n            [\n              -116.62442207336426,\n              35.29621310995517\n            ],\n            [\n              -116.64570808410643,\n              35.28276182997691\n            ],\n            [\n              -116.65145874023438,\n              35.27302226906422\n            ],\n            [\n              -116.64931297302246,\n              35.26965869539278\n            ],\n            [\n              -116.63678169250488,\n              35.266645375384165\n            ],\n            [\n              -116.63274765014648,\n              35.263842186385766\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Densmore, Jill N. 0000-0002-5345-6613 jidensmo@usgs.gov","orcid":"https://orcid.org/0000-0002-5345-6613","contributorId":197491,"corporation":false,"usgs":true,"family":"Densmore","given":"Jill","email":"jidensmo@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":850570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellett, Kevin","contributorId":66398,"corporation":false,"usgs":true,"family":"Ellett","given":"Kevin","affiliations":[],"preferred":false,"id":850571,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howle, James F. 0000-0003-0491-6203 jfhowle@usgs.gov","orcid":"https://orcid.org/0000-0003-0491-6203","contributorId":2225,"corporation":false,"usgs":true,"family":"Howle","given":"James","email":"jfhowle@usgs.gov","middleInitial":"F.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":850572,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carpenter, Michael C. mcarpent@usgs.gov","contributorId":3977,"corporation":false,"usgs":true,"family":"Carpenter","given":"Michael","email":"mcarpent@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":850573,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sneed, Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":850574,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70209190,"text":"70209190 - 2010 - Historical seismograms for unravelling a mysterious earthquake: The 1907 Sumatra Earthquake","interactions":[],"lastModifiedDate":"2020-03-23T09:35:19","indexId":"70209190","displayToPublicDate":"2010-10-01T09:24:57","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Historical seismograms for unravelling a mysterious earthquake: The 1907 Sumatra Earthquake","docAbstract":"<p>History of instrumental seismology is short. Seismograms are available only for a little more than 100 years; high-quality seismograms are available only for the last 50 years and the seismological database is very limited in time. To extend the database, seismograms of old events are of vital importance. Many unusual earthquakes are known to have occurred, but their seismological characteristics are poorly known. The 1907 Sumatra earthquake is one of them (1907 January 4,<span>&nbsp;</span><i>M</i>= 7.6). Gutenberg and Richter located this event in the outer-rise area of the Sunda arc. This earthquake is known to be anomalous because of its extensive tsunami, which is disproportionate of its magnitude. The tsunami affected the coastal areas over 950 km along the Sumatran coast. We investigated this earthquake using the historical seismograms we could collect from several seismological observatories. We examined the<span>&nbsp;</span><i>P</i>-wave arrival times listed in the Strassburg Bulletin (1912) and other station bulletins. The scatter of the Observed−Computed traveltime residuals ranges from –30 to 30 s, too large to locate the event accurately. The uncertainty of the epicentre estimated from an S-P grid-search relocation study is at least 1° (∼110 km). We interpreted the Omori seismograms from Osaka, Mizusawa and Tokyo, and the Wiechert seismograms from Göttingen and Uppsala by comparing them with the seismograms simulated from modern broad-band seismograms of the 2002, 2008 and two 2010 Sumatra earthquakes which occurred near the 1907 earthquake. From the amplitude of Rayleigh waves recorded on the Omori seismograms we conclude that the magnitude of the 1907 earthquake at about 30 to 40 s is about 7.8 (i.e. 7.5 to 8.0). The<span>&nbsp;</span><i>SH</i><span>&nbsp;</span>waveforms recorded on the Göttingen and Uppsala seismograms suggest that the 1907 earthquake is a thrust earthquake at a shallow depth around 30 km. The most likely scenario is that the 1907 earthquake initiated on the subduction interface, and slowly ruptured up-dip into the shallow sediments and caused the extensive tsunami. Although their quantity and quality are limited, historical seismograms provide key quantitative information about old events that cannot be obtained otherwise. This underscores the importance of preserving historical seismograms.</p>","language":"English","publisher":"Oxford Academic ","doi":"10.1111/j.1365-246X.2010.04731.x","usgsCitation":"Kanamori, H., Rivera, L., and Lee, W., 2010, Historical seismograms for unravelling a mysterious earthquake: The 1907 Sumatra Earthquake: Geophysical Journal International, v. 183, no. 1, p. 358-374, https://doi.org/10.1111/j.1365-246X.2010.04731.x.","productDescription":"17 p.","startPage":"358","endPage":"374","costCenters":[],"links":[{"id":475662,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.2010.04731.x","text":"Publisher Index Page"},{"id":373435,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Indonesia 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Hiroo","contributorId":106120,"corporation":false,"usgs":true,"family":"Kanamori","given":"Hiroo","affiliations":[],"preferred":false,"id":785303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rivera, Luis","contributorId":102367,"corporation":false,"usgs":true,"family":"Rivera","given":"Luis","email":"","affiliations":[],"preferred":false,"id":785304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, W.H.K.","contributorId":35303,"corporation":false,"usgs":true,"family":"Lee","given":"W.H.K.","affiliations":[],"preferred":false,"id":785305,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70236311,"text":"70236311 - 2010 - Preface: Developments in land subsidence investigation","interactions":[],"lastModifiedDate":"2022-09-01T14:30:11.948251","indexId":"70236311","displayToPublicDate":"2010-10-01T09:21:06","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Preface: Developments in land subsidence investigation","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Eighth International Symposium on Land Subsidence","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"8th International Symposium on Land Subsidence,","conferenceDate":"October 17-22, 2010","conferenceLocation":"Querétaro, Mexico","language":"English","publisher":"International Association of Hydrological Sciences Press","usgsCitation":"Carreon-Freyre, D., Cerca, M., and Galloway, D.L., 2010, Preface: Developments in land subsidence investigation, <i>in</i> Eighth International Symposium on Land Subsidence, Querétaro, Mexico, October 17-22, 2010, p. v-viii.","productDescription":"4 p.","startPage":"v","endPage":"viii","costCenters":[],"links":[{"id":406064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Carreon-Freyre, Dora","contributorId":203530,"corporation":false,"usgs":false,"family":"Carreon-Freyre","given":"Dora","email":"","affiliations":[{"id":36644,"text":"Centro de Geociencias, Universidad Nacional Autónoma de México, Campus Juriquilla, Queretaro, Mexico","active":true,"usgs":false}],"preferred":false,"id":850567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cerca, Mariano","contributorId":296082,"corporation":false,"usgs":false,"family":"Cerca","given":"Mariano","email":"","affiliations":[],"preferred":false,"id":850568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":850569,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70199988,"text":"70199988 - 2010 - Effects of light and nutrients on seasonal phytoplankton succession in a temperate eutrophic coastal lagoon","interactions":[],"lastModifiedDate":"2018-10-10T09:04:24","indexId":"70199988","displayToPublicDate":"2010-10-01T09:03:46","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":"Effects of light and nutrients on seasonal phytoplankton succession in a temperate eutrophic coastal lagoon","docAbstract":"<p><span>Rodeo Lagoon, a low-salinity coastal lagoon in the Golden Gate National Recreation Area, California, United States, has been identified as an important ecosystem due to the presence of the endangered goby (</span><i class=\"EmphasisTypeItalic \">Eucyclogobius newberri</i><span>). Despite low anthropogenic impacts, the lagoon exhibits eutrophic conditions and supports annual episodes of very high phytoplankton biomass. Weekly assessments (February–December 2007) of phytoplankton indicated diatoms,&nbsp;</span><i class=\"EmphasisTypeItalic \">Nodularia spumigena</i><span>,&nbsp;</span><i class=\"EmphasisTypeItalic \">Chaetoceros muelleri</i><span>&nbsp;var.&nbsp;</span><i class=\"EmphasisTypeItalic \">muelleri</i><span>, flagellated protozoa, a mixed assemblage, and&nbsp;</span><i class=\"EmphasisTypeItalic \">Microcystis aeruginosa</i><span>&nbsp;dominated the algal community in successive waves. Phytoplankton succession was significantly correlated (</span><i class=\"EmphasisTypeItalic \">r</i><span>&nbsp;</span><sup>2</sup><span>&nbsp;=&nbsp;0.37,&nbsp;</span><i class=\"EmphasisTypeItalic \">p</i><span>&nbsp;&lt;&nbsp;0.001) with averaged daily irradiance (max&nbsp;=&nbsp;29.7&nbsp;kW&nbsp;m</span><sup>−2</sup><span>&nbsp;d</span><sup>−1</sup><span>), water column light attenuation (max&nbsp;=&nbsp;14&nbsp;m</span><sup>−1</sup><span>), and orthophosphate and dissolved inorganic carbon concentrations (max&nbsp;=&nbsp;1.5 and 2920&nbsp;μM, respectively). Negative effects of phytoplankton growth and decay included excessive ammonia concentrations (exceeded EPA guidelines on 77% of sampling days), hypoxia (&lt;3&nbsp;mg&nbsp;l</span><sup>−1</sup><span>dissolved oxygen), and introduction of several microcystins, all in the latter half of the year. Our one-year study suggests that this coastal lagoon is a highly seasonal system with strong feedbacks between phytoplankton and geochemical processes.</span></p>","language":"English","publisher":"Springer Netherlands","doi":"10.1007/s10750-010-0380-y","usgsCitation":"Drake, J.L., Carpenter, E.J., Cousins, M., Nelson, K.L., Guido-Zarate, A., and Loftin, K.A., 2010, Effects of light and nutrients on seasonal phytoplankton succession in a temperate eutrophic coastal lagoon: Hydrobiologia, v. 654, no. 1, p. 177-192, https://doi.org/10.1007/s10750-010-0380-y.","productDescription":"16 p.","startPage":"177","endPage":"192","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":475663,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s10750-010-0380-y","text":"Publisher Index Page"},{"id":358227,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Rodeo Lagoon, Golden Gate National Recreation Area","volume":"654","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-30","publicationStatus":"PW","scienceBaseUri":"5c10c655e4b034bf6a7f3e29","contributors":{"authors":[{"text":"Drake, Jeana L.","contributorId":208544,"corporation":false,"usgs":false,"family":"Drake","given":"Jeana","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":747639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Edward J.","contributorId":208545,"corporation":false,"usgs":false,"family":"Carpenter","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":747640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cousins, Mary","contributorId":208546,"corporation":false,"usgs":false,"family":"Cousins","given":"Mary","email":"","affiliations":[],"preferred":false,"id":747641,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, Kara L.","contributorId":208547,"corporation":false,"usgs":false,"family":"Nelson","given":"Kara","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":747642,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Guido-Zarate, Alejandro","contributorId":208548,"corporation":false,"usgs":false,"family":"Guido-Zarate","given":"Alejandro","email":"","affiliations":[],"preferred":false,"id":747643,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Loftin, Keith A. 0000-0001-5291-876X kloftin@usgs.gov","orcid":"https://orcid.org/0000-0001-5291-876X","contributorId":868,"corporation":false,"usgs":true,"family":"Loftin","given":"Keith","email":"kloftin@usgs.gov","middleInitial":"A.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":747644,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70231418,"text":"70231418 - 2010 - Ancient earthquakes from archaeoseismic evidence during the Visigothic and Islamic periods in the archaeological site of “Tolmo de Minateda” (SE Spain)","interactions":[],"lastModifiedDate":"2022-05-10T14:19:36.704814","indexId":"70231418","displayToPublicDate":"2010-10-01T09:01:52","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Ancient earthquakes from archaeoseismic evidence during the Visigothic and Islamic periods in the archaeological site of “Tolmo de Minateda” (SE Spain)","docAbstract":"<p><span>The ruins of the ancient settlement of “El Tolmo de Minateda” are one of the best representative archaeological sites within the Albacete Province (SE Spain), characterized by a well-preserved record for the last ~3800 yr. The present ruins record an almost continuous of occupation from the Late Bronze Age (Iberian Culture, from ca. third century B.C.) to the High Middle Ages, including intervening and successive Roman, Visigoth, and Muslim city remains. The eventual Muslim settlement was abruptly abandoned and destroyed during the ninth–tenth centuries A.D., leaving a lack of any archaeological evidence of war or decay. Another previous anomalous archaeological episode of abrupt city abandonment and destruction is recorded during the Visigothic Period (seventh century). The archaeological record of this city supports evidence for earthquake damage linked to both periods of city abandonment and destruction, including oriented collapse of walls, watchtowers, and columns, oriented cracking of walls and column drums, as well as in situ broken pottery, abrupt abandonment of kilns, and anomalous sedimentary infilling of canals and water-supply facilities. Additionally, large-scale rockfalls containing Visigothic carved tombs are also apparently associated with both episodes, constituting one of the few instances of combined geoarchaeological evidence of earthquake ground effects ever reported. As a means of testing the theoretical archaeoseismic potential of this site, we obtained an archaeoseismic quality factor (AQF) value of 0.074.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Ancient earthquakes","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/2010.2471(15)","usgsCitation":"Rodriguez-Pascua, M., Silva, P.G., Garduno-Monroy, V.H., Perez-Lopez, R., Israde-Alcántara, I., Giner-Robles, J.L., Bischoff, J.L., and Calvo, J.P., 2010, Ancient earthquakes from archaeoseismic evidence during the Visigothic and Islamic periods in the archaeological site of “Tolmo de Minateda” (SE Spain), chap. <i>of</i> Ancient earthquakes, v. 471, p. 100-108, https://doi.org/10.1130/2010.2471(15).","productDescription":"9 p.","startPage":"100","endPage":"108","costCenters":[],"links":[{"id":400387,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Spain","otherGeospatial":"Tolmo de Minateda","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -1.646919250488281,\n              38.43799313099272\n            ],\n            [\n              -1.5686416625976562,\n              38.43799313099272\n            ],\n            [\n              -1.5686416625976562,\n              38.50062390460539\n            ],\n            [\n              -1.646919250488281,\n              38.50062390460539\n            ],\n            [\n              -1.646919250488281,\n              38.43799313099272\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"471","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rodriguez-Pascua, M. A.","contributorId":67325,"corporation":false,"usgs":true,"family":"Rodriguez-Pascua","given":"M. A.","affiliations":[],"preferred":false,"id":842543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silva, P. G.","contributorId":291578,"corporation":false,"usgs":false,"family":"Silva","given":"P.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":842544,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garduno-Monroy, Victor H.","contributorId":10962,"corporation":false,"usgs":true,"family":"Garduno-Monroy","given":"Victor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":842545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perez-Lopez, R.","contributorId":291579,"corporation":false,"usgs":false,"family":"Perez-Lopez","given":"R.","affiliations":[],"preferred":false,"id":842546,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Israde-Alcántara, I.","contributorId":60422,"corporation":false,"usgs":true,"family":"Israde-Alcántara","given":"I.","affiliations":[],"preferred":false,"id":842547,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Giner-Robles, J. L.","contributorId":22602,"corporation":false,"usgs":true,"family":"Giner-Robles","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":842548,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":842549,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Calvo, J. P.","contributorId":24136,"corporation":false,"usgs":true,"family":"Calvo","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":842550,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70056340,"text":"70056340 - 2010 - Creative use of pilot points to address site and regional scale heterogeneity in a variable-density model","interactions":[],"lastModifiedDate":"2014-04-18T08:45:58","indexId":"70056340","displayToPublicDate":"2010-10-01T08:36:03","publicationYear":"2010","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Creative use of pilot points to address site and regional scale heterogeneity in a variable-density model","docAbstract":"Pilot points for parameter estimation were creatively used to address heterogeneity at both the well field and regional scales in a variable-density groundwater flow and solute transport model designed to test multiple hypotheses for upward migration of fresh effluent injected into a highly transmissive saline carbonate aquifer. Two sets of pilot points were used within in multiple model layers, with one set of inner pilot points (totaling 158) having high spatial density to represent hydraulic conductivity at the site, while a second set of outer points (totaling 36) of lower spatial density was used to represent hydraulic conductivity further from the site. Use of a lower spatial density outside the site allowed (1) the total number of pilot points to be reduced while maintaining flexibility to accommodate heterogeneity at different scales, and (2) development of a model with greater  areal extent in order to simulate proper boundary conditions that have a limited effect on the area of interest. The parameters associated with the inner pilot points were log transformed hydraulic conductivity multipliers of the conductivity field obtained by interpolation from outer pilot points. The use of this dual inner-outer scale parameterization (with inner parameters constituting multipliers for outer parameters) allowed smooth transition of hydraulic conductivity from the site scale, where greater spatial variability of hydraulic properties exists, to the regional scale where less spatial variability was necessary for model calibration. While the model is highly parameterized to accommodate potential aquifer heterogeneity, the total number of pilot points is kept at a minimum to enable reasonable calibration run times.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"PEST Conference 2009 Proceedings","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"conferenceTitle":"PEST Conference","conferenceDate":"2009-11-02T00:00:00","conferenceLocation":"Potomac, MD","language":"English","publisher":"S.S. Papadopulos & Associates, Inc.","usgsCitation":"Dausman, A., Doherty, J., and Langevin, C.D., 2010, Creative use of pilot points to address site and regional scale heterogeneity in a variable-density model.","ipdsId":"IP-016465","costCenters":[{"id":286,"text":"Florida Water Science Center-Ft. Lauderdale","active":false,"usgs":true}],"links":[{"id":286411,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":279193,"type":{"id":15,"text":"Index Page"},"url":"https://www.lulu.com/shop/ss-papadopulos-associates-inc/pest-conference-2009-proceedings-potomac-maryland-color/paperback/product-12914428.html"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ffee4b0120853e8be9f","contributors":{"authors":[{"text":"Dausman, Alyssa M.","contributorId":64337,"corporation":false,"usgs":true,"family":"Dausman","given":"Alyssa M.","affiliations":[],"preferred":false,"id":486536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doherty, John","contributorId":43843,"corporation":false,"usgs":true,"family":"Doherty","given":"John","affiliations":[],"preferred":false,"id":486535,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langevin, Christian D. 0000-0001-5610-9759 langevin@usgs.gov","orcid":"https://orcid.org/0000-0001-5610-9759","contributorId":1030,"corporation":false,"usgs":true,"family":"Langevin","given":"Christian","email":"langevin@usgs.gov","middleInitial":"D.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":486534,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70193175,"text":"70193175 - 2010 - Habitat use by fishes in groundwater-dependent streams of southern Oklahoma","interactions":[],"lastModifiedDate":"2017-11-15T16:40:18","indexId":"70193175","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5153,"text":"The American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Habitat use by fishes in groundwater-dependent streams of southern Oklahoma","docAbstract":"<p><span>Habitat use by fishes in groundwater-dependent ecosystems with springs and spring-fed creeks is not widely studied or well understood. We evaluated habitat use by three disjunct populations of fish species (</span><i>Phoxinus erythrogaster</i><span>,<span>&nbsp;</span></span><i>Nocomis asper</i><span><span>&nbsp;</span>and<span>&nbsp;</span></span><i>Etheostoma microperca</i><span>) and, a widespread species,<span>&nbsp;</span></span><i>E. spectabile</i><span><span>&nbsp;</span>in spring-fed streams draining the Arbuckle-Simpson aquifer of southern Oklahoma. Habitat preference for each species was classified based on depth, velocity, substrate and cover.<span>&nbsp;</span></span><i>Phoxinus erthyrogaster</i><span><span>&nbsp;</span>and<span>&nbsp;</span></span><i>N. asper</i><span><span>&nbsp;</span>were associated with pools with little cover, while<span>&nbsp;</span></span><i>E. microperca</i><span><span>&nbsp;</span>was found in heavily vegetated areas.<span>&nbsp;</span></span><i>Etheostoma spectabile</i><span><span>&nbsp;</span>used habitat in riffles with rapid velocity and large substrate types. We classified habitat selection and avoidance with Chesson's α and observed significant differences in habitat use among species in the study sites. Overall differences in habitat use for<span>&nbsp;</span></span><i>P. erythrogaster</i><span><span>&nbsp;</span>among the three study sites were primarily related to differences in available habitat between springs. Our study provides vital ecological information about disjunct populations of groundwater-dependent fishes in an aquifer that is experiencing development pressure for water abstraction.</span></p>","language":"English","publisher":"University of Notre Dame","doi":"10.1674/0003-0031-164.2.201","usgsCitation":"Seilheimer, T.S., and Fisher, W.L., 2010, Habitat use by fishes in groundwater-dependent streams of southern Oklahoma: The American Midland Naturalist, v. 164, no. 2, p. 201-216, https://doi.org/10.1674/0003-0031-164.2.201.","productDescription":"16 p.","startPage":"201","endPage":"216","ipdsId":"IP-012120","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":348941,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","volume":"164","issue":"2","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a610aaae4b06e28e9c256c4","contributors":{"authors":[{"text":"Seilheimer, Titus S.","contributorId":50772,"corporation":false,"usgs":true,"family":"Seilheimer","given":"Titus","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":722316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, William L. wfisher@usgs.gov","contributorId":1229,"corporation":false,"usgs":true,"family":"Fisher","given":"William","email":"wfisher@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":718124,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70136147,"text":"70136147 - 2010 - Bison conservation initiative: Bison conservation genetics workshop: Report and recommendations","interactions":[],"lastModifiedDate":"2020-12-02T13:50:56.163269","indexId":"70136147","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":53,"text":"Natural Resource Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"NPS/NRPC/BRMD/NRR—2010/257","title":"Bison conservation initiative: Bison conservation genetics workshop: Report and recommendations","docAbstract":"One of the first outcomes of the Department of the Interior (DOI) Bison Conservation Initiative was the Bison Conservation Genetics Workshop held in Nebraska in September 2008. The workshop brought together scientists from government agencies and non-governmental organizations with professional population geneticists to develop guidance for the genetic management of the federal bison herds. The scientists agreed on the basic tenets of genetic management for the DOI herds and discussed different approaches to meeting those goals. First, the 12 DOI herds are an irreplaceable resource for the long-term conservation of North American plains bison. Most of the herds show low levels of cattle introgression dating from the time when they were saved from extirpation; those herds should not be mixed without careful consideration as to their origin. Herds that show no evidence of cattle ancestry by the current molecular methods are the highest priority for protection from genetic mixing with any other bison herds. Second, despite the fact that most of the herds now managed by the U.S. government were founded with very few bison and have been maintained for many generations at relatively low population sizes, they do not show obvious effects of inbreeding. They have retained significant amounts of genetic variation by the standard measures, heterozygosity and allelic diversity. This may be explained in part by the fact that most of these herds are not remnants of a single population. Third, to preserve genetic variation in federal bison herds over decades and centuries, herds should be managed at a population or metapopulation level of 1,000 animals or more, with a sex ratio that enables competition between breeding bulls. The parks and refuges that currently have bison herds, with the exception of Yellowstone National Park, do not have enough land to support a population of this size. In the short term, it will be important to develop satellite herds to attain population targets, and develop a metapopulation structure between herds.\r\nFourth and finally, the current methods used to evaluate the DOI bison herds, using mitochondrial DNA and a suite of nuclear DNA microsatellites, are highly informative at the herd level. They have confirmed relatedness of herds that we know from historical records have a common origin. They have detected cattle ancestry in most of the herds where it was suspected and have shown some loss of rare alleles. However, they do not sample across the bison genome, and the use of neutral genetic markers as the basis for selection of individual bison—either to breed or move to other herds—would be better supported by more high-resolution molecular methods currently under development.","language":"English","publisher":"National Park Service","usgsCitation":"Gogan, P.J., and Dratch, P., 2010, Bison conservation initiative: Bison conservation genetics workshop: Report and recommendations: Natural Resource Report NPS/NRPC/BRMD/NRR—2010/257, vii, 38 p.","productDescription":"vii, 38 p.","numberOfPages":"50","ipdsId":"IP-025356","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":332333,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":348896,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://permanent.fdlp.gov/gpo131592/Bison_Genetics_Report__nrpc.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585a51c4e4b01224f329b603","contributors":{"authors":[{"text":"Gogan, Peter J. 0000-0002-7821-133X peter_gogan@usgs.gov","orcid":"https://orcid.org/0000-0002-7821-133X","contributorId":1771,"corporation":false,"usgs":true,"family":"Gogan","given":"Peter","email":"peter_gogan@usgs.gov","middleInitial":"J.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":537155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dratch, Peter","contributorId":131078,"corporation":false,"usgs":false,"family":"Dratch","given":"Peter","email":"","affiliations":[{"id":7231,"text":"National Park Service, Natural Resource Program Center","active":true,"usgs":false}],"preferred":false,"id":537156,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70160812,"text":"70160812 - 2010 - Determination of biologically significant hydrologic condition metrics in urbanizing watersheds: an empirical analysis over a range of environmental settings","interactions":[],"lastModifiedDate":"2015-12-31T10:59:15","indexId":"70160812","displayToPublicDate":"2010-10-01T00:00:00","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":"Determination of biologically significant hydrologic condition metrics in urbanizing watersheds: an empirical analysis over a range of environmental settings","docAbstract":"<p>We investigated the relations among 83 hydrologic condition metrics (HCMs) and changes in algal, invertebrate, and fish communities in five metropolitan areas across the continental United States. We used a statistical approach that employed Spearman correlation and regression tree analysis to identify five HCMs that are strongly associated with observed biological variation along a gradient of urbanization. The HCMs related to average flow magnitude, high-flow magnitude, high-flow event frequency, high-flow duration, and rate of change of stream cross-sectional area were most consistently associated with changes in aquatic communities. Although our investigation used an urban gradient design with short hydrologic periods of record (&le;1 year) of hourly cross-sectional area time series, these five HCMs were consistent with previous investigations using long-term daily-flow records. The ecological sampling day often was included in the hydrologic period. Regression tree models explained up to 73, 92, and 79% of variance for specific algal, invertebrate, and fish community metrics, respectively. National models generally were not as statistically significant as models for individual metropolitan areas. High-flow event frequency, a hydrologic metric found to be transferable across stream type and useful for classifying habitat by previous research, was found to be the most ecologically relevant HCM; transformation by precipitation increased national-scale applicability. We also investigated the relation between measures of stream flashiness and land-cover indicators of urbanization and found that land-cover characteristic and pattern variables, such as road density, percent wetland, and proximity of developed land, were strongly related to HCMs at both a metropolitan and national scale and, therefore, may be effective land-use management options in addition to wholesale impervious-area reduction.</p>","language":"English","publisher":"Springer","doi":"10.1007/s10750-010-0362-0","usgsCitation":"Steuer, J.J., Stensvold, K.A., and Gregory, M., 2010, Determination of biologically significant hydrologic condition metrics in urbanizing watersheds: an empirical analysis over a range of environmental settings: Hydrobiologia, v. 654, no. 1, p. 27-55, https://doi.org/10.1007/s10750-010-0362-0.","productDescription":"29 p.","startPage":"27","endPage":"55","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013743","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":313128,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Milwaukee-Green Bay; Boston; Raleigh; Atlanta; Birmingham; Dallas-Fort Worth; Denver; Salt Lake City; Portland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.08837890625,\n              44.61393394730626\n            ],\n            [\n              -88.65966796875,\n              44.174324837518895\n            ],\n            [\n              -88.74755859375,\n              43.874138181474734\n            ],\n            [\n              -88.406982421875,\n              43.01268088642034\n            ],\n            [\n              -87.82470703125,\n  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PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-19","publicationStatus":"PW","scienceBaseUri":"56865fbfe4b0e7594ee74cb9","contributors":{"authors":[{"text":"Steuer, Jeffrey J.","contributorId":75136,"corporation":false,"usgs":true,"family":"Steuer","given":"Jeffrey","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":584037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stensvold, Krista A.","contributorId":48007,"corporation":false,"usgs":true,"family":"Stensvold","given":"Krista","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":584038,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gregory, Mark B.","contributorId":151024,"corporation":false,"usgs":false,"family":"Gregory","given":"Mark B.","affiliations":[],"preferred":false,"id":584039,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70003677,"text":"70003677 - 2010 - Quarterly wildlife mortality report April to June 2010","interactions":[],"lastModifiedDate":"2023-10-13T16:22:25.104224","indexId":"70003677","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3769,"text":"Wildlife Disease Association Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Quarterly wildlife mortality report April to June 2010","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","publisherLocation":"Lawrence, KS","usgsCitation":"Ballmann, A., White, C.L., and Bradsby, J., 2010, Quarterly wildlife mortality report April to June 2010: Wildlife Disease Association Newsletter, p. 9-11.","productDescription":"3 p.","startPage":"9","endPage":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-024887","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":257856,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -180.17578125,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              17.14079039331665\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9270e4b0c8380cd8085c","contributors":{"authors":[{"text":"Ballmann, Anne 0000-0002-0380-056X","orcid":"https://orcid.org/0000-0002-0380-056X","contributorId":104631,"corporation":false,"usgs":true,"family":"Ballmann","given":"Anne","affiliations":[],"preferred":false,"id":348297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, C. LeAnn 0000-0002-5004-5165","orcid":"https://orcid.org/0000-0002-5004-5165","contributorId":29571,"corporation":false,"usgs":true,"family":"White","given":"C.","email":"","middleInitial":"LeAnn","affiliations":[],"preferred":false,"id":348295,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradsby, Jennifer","contributorId":33664,"corporation":false,"usgs":true,"family":"Bradsby","given":"Jennifer","email":"","affiliations":[],"preferred":false,"id":348296,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176258,"text":"70176258 - 2010 - Improving and integrating data on invasive species collected by citizen scientists","interactions":[],"lastModifiedDate":"2016-09-06T14:22:54","indexId":"70176258","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1018,"text":"Biological Invasions","active":true,"publicationSubtype":{"id":10}},"title":"Improving and integrating data on invasive species collected by citizen scientists","docAbstract":"<p><span>Limited resources make it difficult to effectively document, monitor, and control invasive species across large areas, resulting in large gaps in our knowledge of current and future invasion patterns. We surveyed 128 citizen science program coordinators and interviewed 15 of them to evaluate their potential role in filling these gaps. Many programs collect data on invasive species and are willing to contribute these data to public databases. Although resources for education and monitoring are readily available, groups generally lack tools to manage and analyze data. Potential users of these data also retain concerns over data quality. We discuss how to address these concerns about citizen scientist data and programs while preserving the advantages they afford. A unified yet flexible national citizen science program aimed at tracking invasive species location, abundance, and control efforts could be designed using centralized data sharing and management tools. Such a system could meet the needs of multiple stakeholders while allowing efficiencies of scale, greater standardization of methods, and improved data quality testing and sharing. Finally, we present a prototype for such a system (see </span><span class=\"ExternalRef\"><a rel=\"noopener noreferrer\" href=\"http://www.citsci.org/\" target=\"_blank\" data-mce-href=\"http://www.citsci.org/\"><span class=\"RefSource\">www.citsci.org</span></a></span><span>).</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10530-010-9740-9","usgsCitation":"Springer, 2010, Improving and integrating data on invasive species collected by citizen scientists: Biological Invasions, v. 12, no. 10, p. 3419-3428, https://doi.org/10.1007/s10530-010-9740-9.","productDescription":"10 p.","startPage":"3419","endPage":"3428","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":328264,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"10","noUsgsAuthors":false,"publicationDate":"2010-03-07","publicationStatus":"PW","scienceBaseUri":"57cfe8b7e4b04836416a0dc4"}
,{"id":70194397,"text":"70194397 - 2010 - A population genetic analysis of the midget faded rattlesnake in Wyoming","interactions":[],"lastModifiedDate":"2017-11-27T15:51:07","indexId":"70194397","displayToPublicDate":"2010-10-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1324,"text":"Conservation Genetics","active":true,"publicationSubtype":{"id":10}},"title":"A population genetic analysis of the midget faded rattlesnake in Wyoming","docAbstract":"<p><span>Little is known about the population biology of midget faded rattlesnakes, a sensitive subspecies of the Western Rattlesnake, despite conservation efforts to protect them. We conducted a molecular genetic study of midget faded rattlesnakes in southwestern Wyoming to investigate population genetic structure in this area, particularly with reference to Flaming Gorge Reservoir and its associated human activities, and to document levels of genetic diversity. We genotyped 229 snakes from 11 sampling sites using 9 microsatellite loci. We found significant levels of genetic structure among sites that were better explained by geographic region and isolation by distance than by position relative to waterways. Sites on either side of the reservoir at its widest point were not significantly different. Six of the sites showed signatures of a population bottleneck using an alpha value of 0.05. Three of these bottlenecked sites (the three most northern) were the most genetically distinct and occur in areas of greatest impact from human activity.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10592-009-0043-6","usgsCitation":"Oyler-McCance, S.J., and Parker, J., 2010, A population genetic analysis of the midget faded rattlesnake in Wyoming: Conservation Genetics, v. 11, no. 5, p. 1623-1629, https://doi.org/10.1007/s10592-009-0043-6.","productDescription":"7 p.","startPage":"1623","endPage":"1629","ipdsId":"IP-012717","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":349391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Flaming Gorge Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.70123291015625,\n              40.9964840143779\n            ],\n            [\n              -109.2755126953125,\n              40.9964840143779\n            ],\n            [\n              -109.2755126953125,\n              41.62160222224564\n            ],\n            [\n              -109.70123291015625,\n              41.62160222224564\n            ],\n            [\n              -109.70123291015625,\n              40.9964840143779\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-10-01","publicationStatus":"PW","scienceBaseUri":"5a610aaae4b06e28e9c256c2","contributors":{"authors":[{"text":"Oyler-McCance, Sara J. 0000-0003-1599-8769 sara_oyler-mccance@usgs.gov","orcid":"https://orcid.org/0000-0003-1599-8769","contributorId":1973,"corporation":false,"usgs":true,"family":"Oyler-McCance","given":"Sara","email":"sara_oyler-mccance@usgs.gov","middleInitial":"J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":723688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, J.M.","contributorId":87497,"corporation":false,"usgs":true,"family":"Parker","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":723689,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006209,"text":"70006209 - 2010 - Efficacy of commercial canarypox vaccine for protecting Hawai'i 'Amakihi from field isolates of <i>Avipoxvirus</i>","interactions":[],"lastModifiedDate":"2017-06-30T15:31:42","indexId":"70006209","displayToPublicDate":"2010-09-30T14:29:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Efficacy of commercial canarypox vaccine for protecting Hawai'i 'Amakihi from field isolates of <i>Avipoxvirus</i>","docAbstract":"At least three variants of avian pox virus are present in Hawai&#8216;i - Fowlpox from domestic poultry and a group of genetically distinct viruses that cluster within two clades (Pox Variant 1 and Pox Variant 2) that are most similar to Canarypox based on DNA sequence of the virus 4b core protein gene. We tested whether Hawai&#8216;i &#8216;Amakihi can be protected from wild virus isolates with an attenuated live Canarypox vaccine that is closely related to isolates that cluster within clade 1 (Pox Variant 1) based on sequence of the attenuated Canarypox virus 4b core protein. Thirty-one (31) Hawai`i &#8216;Amakihi (<i>Hemignathus virens</i>) with no prior physical evidence of pox infection were collected on Mauna Kea from xeric, high elevation habitats with low pox prevalence and randomly divided into two groups. One group of 16 was vaccinated with Poximmune C&reg; while the other group received a sham vaccination with virus diluent. Four of 15 (27%) vaccinated birds developed potentially life-threatening disseminated lesions or lesions of unusually long duration, while one bird never developed a vaccine-associated lesion or \"take\". After vaccine-associated lesions healed, vaccinated birds were randomly divided into three groups of five and challenged with either a wild isolate of Fowlpox, a Hawai`i `Amakihi isolate of a Canarypox-like virus from clade 1 (Pox Variant 1) or a Hawai`i `Amakihi isolate of a Canarypox-like virus from clade 2 (Pox Variant 2). Similarly, three random groups of five unvaccinated &#8216;Amakihi were challenged with the same virus isolates. Vaccinated and unvaccinated &#8216;Amakihi challenged with Fowlpox had transient infections with no clinical signs of infection. Mortality in vaccinated &#8216;Amakihi that were challenged with Pox Variant 1 and Pox Variant 2 ranged from 0% (0/5) for Pox Variant 1 to 60% (3/5) for Pox Variant 2. Mortality in unvaccinated &#8216;Amakihi ranged from 40% (2/5) for Pox Variant 1 to 100% (5/5) for Pox Variant 2. While the vaccine provided some protection against Pox Variant 1, serious side effects and low efficacy against Pox Variant 2 make it risky to use in captive or wild honeycreepers.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hawaii Cooperative Studies Unit Technical Report HCSU-019","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"Hawaii Cooperative Studies Unit, University of Hawaii at Hilo, Pacific Aquaculture and Coastal Resources Center","publisherLocation":"Hilo, HI","usgsCitation":"Atkinson, C.T., Wiegand, K.C., Triglia, D., and Jarvi, S.I., 2010, Efficacy of commercial canarypox vaccine for protecting Hawai'i 'Amakihi from field isolates of <i>Avipoxvirus</i>, iv, 18 p.; Figures.","productDescription":"iv, 18 p.; Figures","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":256976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":256970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://hilo.hawaii.edu/hcsu/documents/TRHCSU-019Atkinson_Avian_Pox.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Hawai'i","otherGeospatial":"O'ahu;Maui;Moloka'i","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0858e4b0c8380cd51aad","contributors":{"authors":[{"text":"Atkinson, Carter T. 0000-0002-4232-5335 catkinson@usgs.gov","orcid":"https://orcid.org/0000-0002-4232-5335","contributorId":1124,"corporation":false,"usgs":true,"family":"Atkinson","given":"Carter","email":"catkinson@usgs.gov","middleInitial":"T.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true},{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"preferred":true,"id":354065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiegand, Kimberly C.","contributorId":94142,"corporation":false,"usgs":true,"family":"Wiegand","given":"Kimberly","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":354068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Triglia, Dennis","contributorId":77780,"corporation":false,"usgs":true,"family":"Triglia","given":"Dennis","email":"","affiliations":[],"preferred":false,"id":354067,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jarvi, Susan I.","contributorId":47748,"corporation":false,"usgs":true,"family":"Jarvi","given":"Susan","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":354066,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209636,"text":"70209636 - 2010 - Chemical and textural controls on phosphorus mobility in drylands of southeastern Utah","interactions":[],"lastModifiedDate":"2020-04-16T18:46:53.753027","indexId":"70209636","displayToPublicDate":"2010-09-30T13:40:19","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1007,"text":"Biogeochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Chemical and textural controls on phosphorus mobility in drylands of southeastern Utah","docAbstract":"<p><span>We investigated several forms of phosphorus (P) in dryland soils to examine the chemical and textural controls on P stabilization on a diverse set of substrates. We examined three P fractions including labile, moderately labile, and occluded as determined by a modified Hedley fractionation technique. The P fractions were compared to texture measurements and total elemental concentrations determined by inductively coupled plasma-atomic emission spectroscopy (ICP-AES). Labile P related to the absence of materials involved in P sorption. Moderately labile P was most strongly associated with high total Al &amp; Fe content that we interpret to represent oxides and 1:1 clay minerals. The occluded P fraction was strongly associated with low total Al &amp; Fe environments and interpreted to represent 2:1 clay minerals where ligand exchange tightly sequesters P. The results indicate that the controls on P fraction distribution are initially closely tied to the chemical and physical properties of the bedrock units that contribute to soil formation. Further, these results suggest that the progression of stabilized P forms in dryland areas differs from the progression observed in mesic environments. Soil development in dryland settings, such as the formation of pedogenic carbonates, may lead to differing controls on P availability and the proportional size of the moderately labile fraction.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10533-010-9408-7","usgsCitation":"Buckingham, S.E., Neff, J., Titiz-Maybach, B., and Reynolds, R.L., 2010, Chemical and textural controls on phosphorus mobility in drylands of southeastern Utah: Biogeochemistry, v. 100, p. 105-120, https://doi.org/10.1007/s10533-010-9408-7.","productDescription":"16 p.","startPage":"105","endPage":"120","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Canyonlands National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.5499267578125,\n              37.483576550426996\n            ],\n            [\n              -109.12170410156249,\n              37.483576550426996\n            ],\n            [\n              -109.12170410156249,\n              38.75408327579141\n            ],\n            [\n              -110.5499267578125,\n              38.75408327579141\n            ],\n            [\n              -110.5499267578125,\n              37.483576550426996\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"100","noUsgsAuthors":false,"publicationDate":"2010-02-11","publicationStatus":"PW","contributors":{"authors":[{"text":"Buckingham, Susan E.","contributorId":184077,"corporation":false,"usgs":false,"family":"Buckingham","given":"Susan","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":787299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neff, Jason","contributorId":167084,"corporation":false,"usgs":false,"family":"Neff","given":"Jason","affiliations":[{"id":6709,"text":"University of Colorado, Denver","active":true,"usgs":false}],"preferred":false,"id":787300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Titiz-Maybach, Behan","contributorId":224205,"corporation":false,"usgs":false,"family":"Titiz-Maybach","given":"Behan","email":"","affiliations":[],"preferred":false,"id":787301,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":147880,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":271,"text":"Federal Center","active":false,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787302,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70043523,"text":"70043523 - 2010 - To burn or not to burn Oriental bittersweet: A fire manager’s conundrum","interactions":[],"lastModifiedDate":"2022-09-02T18:15:05.312539","indexId":"70043523","displayToPublicDate":"2010-09-30T10:44:13","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"To burn or not to burn Oriental bittersweet: A fire manager’s conundrum","docAbstract":"<p>This is the second progress report detailing the research about Oriental bittersweet (<i>Celastrus orbiculatus</i>) and fire which has been ongoing for two years. We highlight the further results from three components of the study: 1) Susceptibility of different habitats to invasion of Oriental bittersweet, 2) The impact of fire on established individuals of Oriental bittersweet, and 3) Modeling Oriental bittersweet invasion proliferation and presence on the basis of fire history and vegetation. </p>","language":"English","publisher":"Joint Fire Science Program","usgsCitation":"Pavlovic, N.B., Leicht-Young, S.A., Frohnapple, K., Morford, D., and Mulconrey, N., 2010, To burn or not to burn Oriental bittersweet: A fire manager’s conundrum, 39 p.","productDescription":"39 p.","ipdsId":"IP-025751","costCenters":[{"id":324,"text":"Great Lakes Science 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,{"id":98751,"text":"fs20103069 - 2010 - Groundwater resources of Mosteiros basin, island of Fogo, Cape Verde, West Africa","interactions":[],"lastModifiedDate":"2018-03-21T15:13:26","indexId":"fs20103069","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-3069","title":"Groundwater resources of Mosteiros basin, island of Fogo, Cape Verde, West Africa","docAbstract":"Groundwater resources in Cape Verde provide water for agriculture, industry, and human consumption. These resources are limited and susceptible to contamination. Additional groundwater resources are needed for continued agricultural development, particularly during times of drought, but increased use and (or) climatic change may have adverse effects on the quantity and quality of freshwater available. In volcanic island aquifers such as those of Cape Verde, a lens of fresh groundwater typically ?floats? upon a layer of brackish water at the freshwater/saltwater boundary, and increased pumping may cause salt water intrusion or other contamination. A recent U.S. Geological Survey study assessed baseline groundwater conditions in watersheds on three islands of Cape Verde to provide the scientific basis for sustainably developing water resources and minimizing future groundwater depletion and contamination.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20103069","collaboration":"Prepared in cooperation with the Millennium Challenge Corporation","usgsCitation":"Heilweil, V.M., Gingerich, S.B., Plummer, N., and Verstraeten, I.M., 2010, Groundwater resources of Mosteiros basin, island of Fogo, Cape Verde, West Africa: U.S. Geological Survey Fact Sheet 2010-3069, 3 p.; PDF do Relatório em Português (PDF of Report in Portuguese), https://doi.org/10.3133/fs20103069.","productDescription":"3 p.; PDF do Relatório em Português (PDF of Report in Portuguese)","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":125996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2010_3069.jpg"},{"id":334722,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2010/3069/pdf/fs20103069Port.pdf","text":"Relatório em Português (Report in Portuguese)","size":"1.1 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":334721,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2010/3069/pdf/fs20103069Eng.pdf","text":"Report in English","size":"1.1 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":14161,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2010/3069/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","projection":"Cabo Verde National Grid Projection","country":"Cape Verde","otherGeospatial":"Island of Fogo, Mosteiros Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -25.333333333333332,14.75 ], [ -25.333333333333332,17.333333333333332 ], [ -22.666666666666668,17.333333333333332 ], [ -22.666666666666668,14.75 ], [ -25.333333333333332,14.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656979","contributors":{"authors":[{"text":"Heilweil, Victor M. heilweil@usgs.gov","contributorId":837,"corporation":false,"usgs":true,"family":"Heilweil","given":"Victor","email":"heilweil@usgs.gov","middleInitial":"M.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":306352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":306353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":306355,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Verstraeten, Ingrid M. imverstr@usgs.gov","contributorId":3630,"corporation":false,"usgs":true,"family":"Verstraeten","given":"Ingrid","email":"imverstr@usgs.gov","middleInitial":"M.","affiliations":[{"id":5066,"text":"Office of the Director USGS","active":true,"usgs":true}],"preferred":true,"id":306354,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98750,"text":"ofr20101238 - 2010 - Otolith analysis of pre-restoration habitat use by Chinook salmon in the delta-flats and nearshore regions of the Nisqually River Estuary","interactions":[],"lastModifiedDate":"2012-02-10T00:11:57","indexId":"ofr20101238","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1238","title":"Otolith analysis of pre-restoration habitat use by Chinook salmon in the delta-flats and nearshore regions of the Nisqually River Estuary","docAbstract":"The Nisqually Fall Chinook population is one of 27 salmon stocks in the Puget Sound (Washington) evolutionarily significant unit listed as threatened under the federal Endangered Species Act (ESA). Extensive restoration of the Nisqually River delta ecosystem is currently taking place to assist in recovery of the stock as juvenile Fall Chinook salmon are dependent on the estuary. A pre-restoration baseline that includes the characterization of life history strategies, estuary residence times, growth rates, and habitat use is needed to evaluate the potential response of hatchery and natural origin Chinook salmon to restoration efforts and to determine restoration success. Otolith analysis was selected as a tool to examine Chinook salmon life history, growth, and residence in the Nisqually River estuary. Previously funded work on samples collected in 2004 (marked and unmarked) and 2005 (unmarked only) partially established a juvenile baseline on growth rates and length of residence associated with various habitats (freshwater, forested riverine tidal, emergent forested transition, estuarine emergent marsh, delta-flats and nearshore). However, residence times and growth rates for the delta-flats (DF) and nearshore (NS) habitats have been minimally documented due to small sample sizes. The purpose of the current study is to incorporate otolith microstructural analysis using otoliths from fish collected within the DF and NS habitats during sampling years 2004-08 to increase sample size and further evaluate between-year variation in otolith microstructure. Our results from this analysis indicated the delta-flats check (DFCK) on unmarked and marked Chinook samples in 2005-08 varied slightly in appearance from that seen on samples previously analyzed only from 2004. A fry migrant life history was observed on otoliths of unmarked Chinook collected in 2005, 2007, and 2008. Generally, freshwater mean increment width of unmarked fish, on average, was smaller compared to marked Chinook followed by tidal delta and DF/NS portions respectively. On average, the complete tidal delta growth rate was higher for marked Chinook compared to unmarked Chinook. The DF/NS growth rate was highest for unmarked and marked Chinook during 2008 compared to all other sampling years. The average DF/NS growth rate on unmarked Chinook was consistently lower than marked Chinook during all years; however, sample sizes were small during some years. Unmarked Chinook, on average, spent longer in the tidal delta compared to marked Chinook. Our results from this report suggest that otolith microstructural analysis can be a valuable tool in establishing baseline information on the utilization of Nisqually River estuary habitats by juvenile Chinook salmon prior to the newly funded restoration efforts.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101238","collaboration":"Final Report Presented to the Nisqually Indian Tribe","usgsCitation":"Lind-Null, A., and Larsen, K., 2010, Otolith analysis of pre-restoration habitat use by Chinook salmon in the delta-flats and nearshore regions of the Nisqually River Estuary: U.S. Geological Survey Open-File Report 2010-1238, iv, 28 p., https://doi.org/10.3133/ofr20101238.","productDescription":"iv, 28 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2005-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":125999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1238.jpg"},{"id":14160,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1238/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.66666666666667,47 ], [ -122.66666666666667,47.25 ], [ -122.5,47.25 ], [ -122.5,47 ], [ -122.66666666666667,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4a7","contributors":{"authors":[{"text":"Lind-Null, Angie","contributorId":9369,"corporation":false,"usgs":true,"family":"Lind-Null","given":"Angie","affiliations":[],"preferred":false,"id":306350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larsen, Kim","contributorId":101762,"corporation":false,"usgs":true,"family":"Larsen","given":"Kim","affiliations":[],"preferred":false,"id":306351,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98757,"text":"ds303 - 2010 - Database for the geologic map of the Bend 30- x 60-minute quadrangle, central Oregon","interactions":[],"lastModifiedDate":"2023-11-01T21:42:54.683315","indexId":"ds303","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"303","title":"Database for the geologic map of the Bend 30- x 60-minute quadrangle, central Oregon","docAbstract":"The Bend 30- x 60-minute quadrangle has been the locus of volcanism, faulting, and sedimentation for the past 35 million years. It encompasses parts of the Cascade Range and Blue Mountain geomorphic provinces, stretching from snowclad Quaternary stratovolcanoes on the west to bare rocky hills and sparsely forested juniper plains on the east. The Deschutes River and its large tributaries, the Metolius and Crooked Rivers, drain the area. Topographic relief ranges from 3,157 m (10,358 ft) at the top of South Sister to 590 m (1,940 ft) at the floor of the Deschutes and Crooked Rivers where they exit the area at the north-central edge of the map area. The map encompasses a part of rapidly growing Deschutes County. The city of Bend, which has over 70,000 people living in its urban growth boundary, lies at the south-central edge of the map. Redmond, Sisters, and a few smaller villages lie scattered along the major transportation routes of U.S. Highways 97 and 20.\r\n\r\nThis geologic map depicts the geologic setting as a basis for structural and stratigraphic analysis of the Deschutes basin, a major hydrologic discharge area on the east flank of the Cascade Range. The map also provides a framework for studying potentially active faults of the Sisters fault zone, which trends northwest across the map area from Bend to beyond Sisters.\r\n\r\nThis digital release contains all of the information used to produce the geologic map published as U.S. Geological Survey Geologic Investigations Series I-2683 (Sherrod and others, 2004). The main component of this digital release is a geologic map database prepared using ArcInfo GIS. This release also contains files to view or print the geologic map and accompanying descriptive pamphlet from I-2683.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds303","usgsCitation":"Koch, R.D., Ramsey, D.W., Sherrod, D.R., Taylor, E.M., Ferns, M., Scott, W.E., Conrey, R.M., and Smith, G.A., 2010, Database for the geologic map of the Bend 30- x 60-minute quadrangle, central Oregon: U.S. Geological Survey Data Series 303, HTML Document; CD-ROM, https://doi.org/10.3133/ds303.","productDescription":"HTML Document; CD-ROM","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":271,"text":"Federal Center","active":false,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":422320,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_94310.htm","linkFileType":{"id":5,"text":"html"}},{"id":14167,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/303/","linkFileType":{"id":5,"text":"html"}},{"id":125990,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds_303.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Bend 30- x 60-minute quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122,\n              44.5\n            ],\n            [\n              -122,\n              44\n            ],\n            [\n              -121,\n              44\n            ],\n            [\n              -121,\n              44.5\n            ],\n            [\n              -122,\n              44.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672a4d","contributors":{"authors":[{"text":"Koch, Richard D. rkoch@usgs.gov","contributorId":4413,"corporation":false,"usgs":true,"family":"Koch","given":"Richard","email":"rkoch@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":306380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ramsey, David W. 0000-0003-1698-2523 dramsey@usgs.gov","orcid":"https://orcid.org/0000-0003-1698-2523","contributorId":3819,"corporation":false,"usgs":true,"family":"Ramsey","given":"David","email":"dramsey@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":306379,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherrod, David R. 0000-0001-9460-0434 dsherrod@usgs.gov","orcid":"https://orcid.org/0000-0001-9460-0434","contributorId":527,"corporation":false,"usgs":true,"family":"Sherrod","given":"David","email":"dsherrod@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":306377,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taylor, Edward M.","contributorId":65932,"corporation":false,"usgs":true,"family":"Taylor","given":"Edward","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":306383,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ferns, Mark L.","contributorId":13703,"corporation":false,"usgs":true,"family":"Ferns","given":"Mark L.","affiliations":[],"preferred":false,"id":306381,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Scott, William E. 0000-0001-8156-979X wescott@usgs.gov","orcid":"https://orcid.org/0000-0001-8156-979X","contributorId":1725,"corporation":false,"usgs":true,"family":"Scott","given":"William","email":"wescott@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":306378,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Conrey, Richard M.","contributorId":41911,"corporation":false,"usgs":true,"family":"Conrey","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":306382,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Smith, Gary A.","contributorId":81196,"corporation":false,"usgs":true,"family":"Smith","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":306384,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":98760,"text":"ofr20101180 - 2010 - Description of extreme-wave deposits on the northern coast of Bonaire, Netherlands Antilles","interactions":[],"lastModifiedDate":"2012-02-02T00:15:44","indexId":"ofr20101180","displayToPublicDate":"2010-09-30T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1180","title":"Description of extreme-wave deposits on the northern coast of Bonaire, Netherlands Antilles","docAbstract":"To develop a better understanding of the origins of extreme-wave deposits and to help assess the potential risk of future overwash events, a field mapping survey was conducted in November 2006 on the northern coast of Bonaire, Netherlands Antilles. Deposits were mapped and analyzed to help develop a systematic sedimentological approach to distinguish the type of extreme-wave event (tsunamis or storms) or combination of events that formed and modified the deposits over time. \r\n\r\nExtreme-wave deposits on the northern coast of Bonaire between Boka Onima and Boka Olivia have formed sand sheets, poly-modal ridge complexes, and boulder fields on a Pleistocene limestone platform 3?8 meters above sea level. The deposits exhibit characteristics that are consistent with both large storm and tsunami processes that often overlap one another. Sand sheets occur as low-relief features underlying and incorporated with boulder field deposits. The seaward edge of ridge complexes are deposited up to 70 m from the shoreline and can extend over 200 m inland. Over 600 clasts were measured in fields and range in size from coarse gravel to fine block, weigh up to 165 metric tons, and are placed over 280 m from the shoreline. \r\n\r\nOur analyses indicate that the deposits may have been produced by a combination of hurricane and tsunami events spanning 10s to 1000s of years. Comparing the different deposit morphologies between study sites highlights the importance of shoreline orientation to the distribution of extreme-wave deposits onshore. However, further investigation is required to fully understand the processes that have produced and modified these deposits over time. \r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101180","usgsCitation":"Watt, S.G., Jaffe, B.E., Morton, R., Richmond, B.M., and Gelfencaum, G., 2010, Description of extreme-wave deposits on the northern coast of Bonaire, Netherlands Antilles: U.S. Geological Survey Open-File Report 2010-1180, vi, 64 p., https://doi.org/10.3133/ofr20101180.","productDescription":"vi, 64 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":125985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1180.jpg"},{"id":14170,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1180/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc2a","contributors":{"authors":[{"text":"Watt, Steven G.","contributorId":48675,"corporation":false,"usgs":true,"family":"Watt","given":"Steven","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":306395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":306393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":306396,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Richmond, Bruce M. 0000-0002-0056-5832 brichmond@usgs.gov","orcid":"https://orcid.org/0000-0002-0056-5832","contributorId":2459,"corporation":false,"usgs":true,"family":"Richmond","given":"Bruce","email":"brichmond@usgs.gov","middleInitial":"M.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":306394,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gelfencaum, Guy","contributorId":96389,"corporation":false,"usgs":true,"family":"Gelfencaum","given":"Guy","email":"","affiliations":[],"preferred":false,"id":306397,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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