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,{"id":70155949,"text":"70155949 - 2015 - Mechanics of sediment suspension and transport within a fringing reef","interactions":[],"lastModifiedDate":"2021-01-14T16:08:03.974181","indexId":"70155949","displayToPublicDate":"2015-12-31T10:07:38","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mechanics of sediment suspension and transport within a fringing reef","docAbstract":"<p><span>Large bottom roughness is a characteristic of most coral reef environments and this has been shown to have a substantial impact on hydrodynamic processes in these environments. In this paper, we evaluate suspended sediment concentration (SSC) data as well detailed hydrodynamic data over a coral reef flat in Ningaloo Reef, Western Australia, to understand how this bottom roughness affects these processes. A well-developed logarithmic velocity layer consistently developed above a canopy layer during the experiment. Estimates of bottom stresses from these logarithmic profiles were comparable with estimates obtained directly from turbulent Reynolds stresses, and an order of magnitude greater than those typically reported for sandy beach environments having similar flow. Nevertheless, the sediment grain size distribution of the suspended load was very fine relative to what should be mobilized by these stresses, indicated the large roughness substantially suppressed sediment transport.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The proceedings of the coastal sediments 2015","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Coastal Sediments 2015","conferenceDate":"May 11-15, 2015","conferenceLocation":"San Diego, CA","language":"English","publisher":"World Scientific","doi":"10.1142/9789814689977_0086","usgsCitation":"Pomeroy, A.W., Lowe, R.J., Ghisalberti, M., Storlazzi, C.D., Cutter, M., and Symonds, G., 2015, Mechanics of sediment suspension and transport within a fringing reef, <i>in</i> The proceedings of the coastal sediments 2015, San Diego, CA, May 11-15, 2015, 14 p., https://doi.org/10.1142/9789814689977_0086.","productDescription":"14 p.","ipdsId":"IP-063073","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":382162,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Australia","city":"Tantabiddi","otherGeospatial":"Ningaloo Reef","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              113.62060546875,\n              -22.024545601240337\n            ],\n            [\n              114.00375366210938,\n              -22.024545601240337\n            ],\n            [\n              114.00375366210938,\n              -21.644664169522265\n            ],\n            [\n              113.62060546875,\n              -21.644664169522265\n            ],\n            [\n              113.62060546875,\n              -22.024545601240337\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2015-04-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Pomeroy, A. W. M.","contributorId":146291,"corporation":false,"usgs":false,"family":"Pomeroy","given":"A.","email":"","middleInitial":"W. M.","affiliations":[{"id":16662,"text":"University of Western Australia","active":true,"usgs":false}],"preferred":false,"id":567319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lowe, R. J.","contributorId":146292,"corporation":false,"usgs":false,"family":"Lowe","given":"R.","email":"","middleInitial":"J.","affiliations":[{"id":16662,"text":"University of Western Australia","active":true,"usgs":false}],"preferred":false,"id":567320,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ghisalberti, M.","contributorId":146293,"corporation":false,"usgs":false,"family":"Ghisalberti","given":"M.","affiliations":[{"id":16662,"text":"University of Western Australia","active":true,"usgs":false}],"preferred":false,"id":567321,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Storlazzi, Curt D. 0000-0001-8057-4490 cstorlazzi@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":140584,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt","email":"cstorlazzi@usgs.gov","middleInitial":"D.","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":567318,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cutter, M.","contributorId":146294,"corporation":false,"usgs":false,"family":"Cutter","given":"M.","email":"","affiliations":[{"id":16662,"text":"University of Western Australia","active":true,"usgs":false}],"preferred":false,"id":567322,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Symonds, G.","contributorId":146295,"corporation":false,"usgs":false,"family":"Symonds","given":"G.","email":"","affiliations":[{"id":12494,"text":"CSIRO Land and Water, Australia","active":true,"usgs":false}],"preferred":false,"id":567323,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70160033,"text":"sir20155174 - 2015 - Groundwater and surface-water interaction and effects of pumping in a complex glacial-sediment aquifer, phase 2, east-central Massachusetts","interactions":[],"lastModifiedDate":"2016-01-05T07:59:04","indexId":"sir20155174","displayToPublicDate":"2015-12-31T10:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-5174","title":"Groundwater and surface-water interaction and effects of pumping in a complex glacial-sediment aquifer, phase 2, east-central Massachusetts","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the Town of Framingham, Massachusetts, has investigated the potential of proposed groundwater withdrawals at the Birch Road well site to affect nearby surface water bodies and wetlands, including Lake Cochituate, the Sudbury River, and the Great Meadows National Wildlife Refuge in east-central Massachusetts. In 2012, the U.S. Geological Survey developed a Phase 1 numerical groundwater model of a complex glacial-sediment aquifer to synthesize hydrogeologic information and simulate potential future pumping scenarios. The model was developed with MODFLOW-NWT, an updated version of a standard USGS numerical groundwater flow modeling program that improves solution of unconfined groundwater flow problems. The groundwater model and investigations of the aquifer improved understanding of groundwater&ndash;surface-water interaction and the effects of groundwater withdrawals on surface-water bodies and wetlands in the study area. The initial work also revealed a need for additional information and model refinements to better understand this complex aquifer system.</p>\n<p>In this second phase of the study, the original groundwater flow model was revised to improve representation of groundwater and surface-water hydrology, stabilize the model, and reduce model error. The model was simplified by reducing the number of layers from 5 to 3 and adding the MODFLOW lake package (LAK) to simulate Lake Cochituate and Pod Meadow Pond and better represent interaction between the lakes and the aquifer. Model revisions improved stability and shortened run times, allowing use of automated parameter estimation software (PEST) to further refine the model hydraulic parameters and reduce simulation errors.</p>\n<p>Model simulations indicate that under average base-flow conditions, the Birch Road wells have a small effect on flow in the Sudbury River during most months, even at the maximum pumping rate of 4.9 ft<sup>3</sup>/s (3.17 Mgal/d). Maximum percent streamflow depletion in the Sudbury River caused by simulated pumping takes place during simulated drought conditions, when streamflow decreased by as much as 21 percent under maximum continuous pumping. Simulations also indicate that groundwater withdrawals at the Birch Road site could be managed so that adverse streamflow impacts are substantially ameliorated. Under the most ecologically conservative simulated drought conditions, simulated streamflow depletion was reduced from 21 percent to 3 percent by pumping at the maximum rate for 6 months rather than for 12 months. Simulations that return 10 percent of the Birch Road well withdrawals to Pod Meadow Pond indicate a modest reduction in the Sudbury River streamflow depletion and provide a larger percentage increase to streamflow just downstream of the pond. The groundwater model also indicates that well locations can have a large effect on the sustainable pumping rate and so should be chosen carefully. The model provides a tool for evaluating alternative pumping rates and schedules not included in this analysis.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20155174","collaboration":"Prepared in cooperation with the Town of Framingham, Massachusetts","usgsCitation":"Eggleston, J.R., Zarriello, P.J., and Carlson, C.S., 2015, Groundwater and surface-water interaction and effects of pumping in a complex glacial-sediment aquifer, Phase 2, east-central Massachusetts: U.S. Geological Survey Scientific Investigations Report 2015–5174, 38 p., https://dx.doi.org/10.3133/sir20155174.","productDescription":"viii, 38 p.","numberOfPages":"50","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-070584","costCenters":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"links":[{"id":312906,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2015/5174/sir20155174.pdf","text":"Report","size":"2.42 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2015-5174"},{"id":312905,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2015/5174/coverthb.jpg"}],"country":"United States","state":"Massachusetts","city":"Framingham","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.40366554260254,\n              42.311021393971345\n            ],\n            [\n              -71.40366554260254,\n              42.357085148806945\n            ],\n            [\n              -71.36615753173828,\n              42.357085148806945\n            ],\n            [\n              -71.36615753173828,\n              42.311021393971345\n            ],\n            [\n              -71.40366554260254,\n              42.311021393971345\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"mailto:dc_nweng@usgs.gov\">Director</a>, New England Water Science Center<br />U.S. Geological Survey<br />10 Bearfoot Road<br />Northborough, MA 01532<br />Or visit our Web site at: <br /> <a href=\"http://newengland.water.usgs.gov\">http://newengland.water.usgs.gov</a></p>","tableOfContents":"<ul>\n<li>Acknowledgments</li>\n<li>Abstract</li>\n<li>Introduction</li>\n<li>Data</li>\n<li>Groundwater Model Modifications</li>\n<li>Effects of Pumping</li>\n<li>Summary and Conclusions</li>\n<li>References Cited</li>\n</ul>","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"publishedDate":"2015-12-31","noUsgsAuthors":false,"publicationDate":"2015-12-31","publicationStatus":"PW","scienceBaseUri":"568651b8e4b0e7594ee74ca2","contributors":{"authors":[{"text":"Eggleston, Jack R.","contributorId":20011,"corporation":false,"usgs":true,"family":"Eggleston","given":"Jack","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":581682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zarriello, Phillip J. 0000-0001-9598-9904 pzarriel@usgs.gov","orcid":"https://orcid.org/0000-0001-9598-9904","contributorId":1868,"corporation":false,"usgs":true,"family":"Zarriello","given":"Phillip","email":"pzarriel@usgs.gov","middleInitial":"J.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":581683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlson, Carl S. 0000-0001-7142-3519 cscarlso@usgs.gov","orcid":"https://orcid.org/0000-0001-7142-3519","contributorId":1694,"corporation":false,"usgs":true,"family":"Carlson","given":"Carl","email":"cscarlso@usgs.gov","middleInitial":"S.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":581684,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70220303,"text":"70220303 - 2015 - Use of historic Persian water system data in groundwater models: Examples from Afghanistan and Emirates","interactions":[],"lastModifiedDate":"2021-05-06T11:47:58.073282","indexId":"70220303","displayToPublicDate":"2015-12-31T08:49:49","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Use of historic Persian water system data in groundwater models: Examples from Afghanistan and Emirates","docAbstract":"Obtaining calibration data for models depicting conditions during pre-development periods can be challenging as such periods are characteristically data poor.  This study presents two examples where simulation of historic water conveyance structures were used to help characterize historic, or pre-modern, conditions in calibration of groundwater flow models. Persian water conveyance structures, called ‘aflaj’ (or singular ‘falaj’) in the Emirates, ‘karezes’ in Afghanistan, or ‘qanats’ in some other regions, consists of a hand dug tunnels, hundreds to thousands of meters long, that intersect upgradient water table surfaces and convey water downgradient for domestic use and irrigation of small farms. These structures can be identified, using remote imagery, by the presence of regularly spaced access holes that were used to create and maintain these tunnel systems. This type of water-supply system was commonly used throughout North Africa, the Middle East, and Asia for centuries. They are generally not used today having largely been supplanted by modern groundwater wells, and, in many areas these structures have failed because of water-table declines caused by groundwater development and/or climate change. Evidence of these systems from satellite imagery provides an indication of pre-modern water levels and this information was used in the calibration of two contrasting pre-development models in Afghanistan and the Emirates.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"MODLFOW and more 2015, modeling a complex world proceedings","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"International Groundwater Modeling Center","usgsCitation":"Mack, T., and Eggleston, J., 2015, Use of historic Persian water system data in groundwater models: Examples from Afghanistan and Emirates, <i>in</i> MODLFOW and more 2015, modeling a complex world proceedings, p. 403-406.","productDescription":"4 p.","startPage":"403","endPage":"406","ipdsId":"IP-066075","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":385450,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Afghanistan, United Arab Emirates","state":"Abu Dhabi Emirate","otherGeospatial":"Chakari Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              55.50018310546874,\n              23.976214626638292\n            ],\n            [\n              56.02958679199219,\n              23.976214626638292\n            ],\n            [\n              56.02958679199219,\n              24.35773102145271\n            ],\n            [\n              55.50018310546874,\n              24.35773102145271\n            ],\n            [\n              55.50018310546874,\n              23.976214626638292\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              68.79089355468749,\n              33.78827853625996\n            ],\n            [\n              69.6478271484375,\n              33.78827853625996\n            ],\n            [\n              69.6478271484375,\n              35.191766965947394\n            ],\n            [\n              68.79089355468749,\n              35.191766965947394\n            ],\n            [\n              68.79089355468749,\n              33.78827853625996\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mack, Thomas J. 0000-0002-0496-3918","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":218727,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas J.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":815073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eggleston, Jack R. 0000-0001-6633-3041","orcid":"https://orcid.org/0000-0001-6633-3041","contributorId":204628,"corporation":false,"usgs":true,"family":"Eggleston","given":"Jack R.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true}],"preferred":true,"id":815074,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70160133,"text":"70160133 - 2015 - Construction ages of the Upton Stone Chamber: Preliminary findings and suggestions for future luminescence research","interactions":[],"lastModifiedDate":"2017-04-26T14:51:57","indexId":"70160133","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3216,"text":"Quaternary Geochronology","active":true,"publicationSubtype":{"id":10}},"title":"Construction ages of the Upton Stone Chamber: Preliminary findings and suggestions for future luminescence research","docAbstract":"The Upton Chamber in Massachusetts, an earth-covered stone structure 3.4 meters (m) in diameter, with a corbelled stone dome, and a 4.3 m long entrance passageway, is studied with the aim of determining whether optically stimulated luminescence (OSL) dating methods can be used to establish the approximate construction date of the entranceway. Three samples, taken from soil behind the lowest stones in the wall of the entrance passageway, returned OSL ages between 385 and 660 years ago (or from 1625 A.D. to 1350 A.D.; using the year 2011 as the 0 year). One sample, taken below the bottom of the artifact layers in an archeological test pit in front of the chamber entrance, returned OSL ages between 650 and 880 years ago. A modern sample collected from a nearby fluvial channel returned an age between 55 and 175 years. The Upton Chamber OSL sampling results are challenging to interpret because there are mixtures in the samples of both younger and older grains that likely result from human modification, root or soil processes, animal bioturbation (i.e. ants and worms), and/or partial bleaching. The ages were determined using the lowest component of the finite mixture model as applied to a distribution of quartz grains. Further research may enable us to determine whether older components are of anthropomorphic or geological origin.","language":"English","publisher":"Elsevier","doi":"10.1016/j.quageo.2015.05.017","usgsCitation":"Mahan, S.A., Martin, F., and Taylor, C., 2015, Construction ages of the Upton Stone Chamber: Preliminary findings and suggestions for future luminescence research: Quaternary Geochronology, v. 30 , no. Part B, p. 422-430, https://doi.org/10.1016/j.quageo.2015.05.017.","productDescription":"9 p.","startPage":"422","endPage":"430","ipdsId":"IP-060880","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":340470,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Upton Chamber","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.69128417968749,\n              42.05337156043361\n            ],\n            [\n              -71.3507080078125,\n              42.05337156043361\n            ],\n            [\n              -71.3507080078125,\n              42.20614200929954\n            ],\n            [\n              -71.69128417968749,\n              42.20614200929954\n            ],\n            [\n              -71.69128417968749,\n              42.05337156043361\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30 ","issue":"Part B","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5901b1bce4b0c2e071a99ba4","contributors":{"authors":[{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":581986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Frederick","contributorId":150514,"corporation":false,"usgs":false,"family":"Martin","given":"Frederick","email":"","affiliations":[{"id":18040,"text":"Massachusetts Archeological Society (member)","active":true,"usgs":false}],"preferred":false,"id":581987,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Cathy","contributorId":150515,"corporation":false,"usgs":false,"family":"Taylor","given":"Cathy","email":"","affiliations":[{"id":18041,"text":"Town of Upton Historical Commission","active":true,"usgs":false}],"preferred":false,"id":581988,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70192491,"text":"70192491 - 2015 - Factors affecting female space use in ten populations of prairie chickens","interactions":[],"lastModifiedDate":"2017-11-28T15:15:01","indexId":"70192491","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1475,"text":"Ecosphere","active":true,"publicationSubtype":{"id":10}},"title":"Factors affecting female space use in ten populations of prairie chickens","docAbstract":"<p><span>Conservation of wildlife depends on an understanding of the interactions between animal movements and key landscape factors. Habitat requirements of wide-ranging species often vary spatially, but quantitative assessment of variation among replicated studies at multiple sites is rare. We investigated patterns of space use for 10 populations of two closely related species of prairie grouse: Greater Prairie-Chickens (</span><i>Tympanuchus cupido</i><span>) and Lesser Prairie-Chickens (</span><i>T. pallidicinctus</i><span>). Prairie chickens require large, intact tracts of native grasslands, and are umbrella species for conservation of prairie ecosystems in North America. We used resource utilization functions to investigate space use by female prairie chickens during the 6-month breeding season from March through August in relation to lek sites, habitat conditions, and anthropogenic development. Our analysis included data from 382 radio-marked individuals across a major portion of the extant range. Our project is a unique opportunity to study comparative space use of prairie chickens, and we employed standardized methods that facilitated direct comparisons across an ecological gradient of study sites. Median home range size of females varied ~10-fold across 10 sites (3.6–36.7 km</span><sup>2</sup><span>), and home ranges tended to be larger at sites with higher annual precipitation. Proximity to lek sites was a strong and consistent predictor of space use for female prairie chickens at all 10 sites. The relative importance of other predictors of space use varied among sites, indicating that generalized habitat management guidelines may not be appropriate for these two species. Prairie chickens actively selected for prairie habitats, even at sites where ~90% of the land cover within the study area was prairie. A majority of the females monitored in our study (&gt;95%) had activity centers within 5 km of leks, suggesting that conservation efforts can be effectively concentrated near active lek sites. Our data on female space use suggest that lek surveys of male prairie chickens can indirectly assess habitat suitability for females during the breeding season. Lek monitoring and surveys for new leks provide information on population trends, but can also guide management actions aimed at improving nesting and brood-rearing habitats.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/ES14-00536.1","usgsCitation":"Winder, V.L., Carrlson, K.M., Gregory, A.J., Hagen, C.A., Haukos, D.A., Kesler, D.C., Larsson, L.C., Matthews, T.W., McNew, L.B., Patten, M., Pitman, J.C., Powell, L., Smith, J.A., Thompson, T., Wolfe, D.H., and Sandercock, B.K., 2015, Factors affecting female space use in ten populations of prairie chickens: Ecosphere, v. 6, no. 9, p. 1-17, https://doi.org/10.1890/ES14-00536.1.","productDescription":"Article 166; 17 p.","startPage":"1","endPage":"17","ipdsId":"IP-058167","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":471539,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index 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A.","affiliations":[],"preferred":false,"id":723927,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Smith, Jennifer A.","contributorId":200953,"corporation":false,"usgs":false,"family":"Smith","given":"Jennifer","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":723928,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Thompson, Tom","contributorId":200954,"corporation":false,"usgs":false,"family":"Thompson","given":"Tom","email":"","affiliations":[],"preferred":false,"id":723929,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Wolfe, Donald H.","contributorId":200956,"corporation":false,"usgs":false,"family":"Wolfe","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":723930,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Sandercock, Brett 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,{"id":70160734,"text":"70160734 - 2015 - Great Lakes prey fish populations: A cross-basin Overview of status and trends based on bottom trawl surveys, 1978-2014","interactions":[],"lastModifiedDate":"2017-04-26T09:32:47","indexId":"70160734","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Great Lakes prey fish populations: A cross-basin Overview of status and trends based on bottom trawl surveys, 1978-2014","docAbstract":"The assessment of Great Lakes prey fish stocks have been conducted annually with bottom trawls since the 1970s by the Great Lakes Science Center, sometimes assisted by partner agencies. These stock assessments provide data on the status and trends of prey fish that are consumed by important commercial and recreational fishes. Although all these annual surveys are conducted using\nbottom trawls, they differ among the lakes in the proportion of the lake covered, seasonal timing, trawl gear used, and the manner in which the trawl is towed (across or along bottom contours). Because each assessment is unique, population indices were standardized to the highest value for a time series within each lake for the following prey species: Cisco (Coregonus artedi), Bloater (C. hoyi), Rainbow Smelt (Osmerus mordax), Alewife (Alosa pseudoharengus), and Round Goby (Neogobius melanostomus). In this report, standardized indices are presented in graphical form along with synopses to provide a short, informal cross-basin summary of the status and trends of principal prey fishes.","largerWorkTitle":"Compiled reports to the Great Lakes Fishery Commission of the Annual Bottom Trawl and Acoustics Surveys, 2014","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Great Lakes Fishery Commission, Ontario Ministry of Natural Resources, Ohio Department of Natural Resources, New York State Department of Environmental Conservation, Pennsylvania Fish and Boat Commission","usgsCitation":"Gorman, O.T., and Weidel, B., 2015, Great Lakes prey fish populations: A cross-basin Overview of status and trends based on bottom trawl surveys, 1978-2014, 10 p.","productDescription":"10 p.","startPage":"96","endPage":"105","ipdsId":"IP-063855","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":340433,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313014,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/lakecom/common_docs/Compiled%20Reports%20from%20USGS%202015.pdf"}],"publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5901b1bce4b0c2e071a99ba2","contributors":{"authors":[{"text":"Gorman, Owen T. 0000-0003-0451-110X otgorman@usgs.gov","orcid":"https://orcid.org/0000-0003-0451-110X","contributorId":2888,"corporation":false,"usgs":true,"family":"Gorman","given":"Owen","email":"otgorman@usgs.gov","middleInitial":"T.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":583726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weidel, Brian 0000-0001-6095-2773 bweidel@usgs.gov","orcid":"https://orcid.org/0000-0001-6095-2773","contributorId":2485,"corporation":false,"usgs":true,"family":"Weidel","given":"Brian","email":"bweidel@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":583727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70191674,"text":"70191674 - 2015 - User-interactive sediment budgets in a browser: A web application for river science and management","interactions":[],"lastModifiedDate":"2018-02-20T13:56:00","indexId":"70191674","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"displayTitle":"User-interactive sediment budgets in a browser: A web application for river science and management","title":"User-interactive sediment budgets in a browser: A web application for river science and management","docAbstract":"Decision-support tools providing accurate, near-real-time data and user-friendly interactive visualizations are of critical value to resource managers tasked with planning and carrying out management programs in their domain. Creating a system to continuously aggregate datasets and recompute derived values is difficult and error-prone when attempted by hand. To address this need for river managers in support of sediment budgeting, we have created a web-based, open source suite of tools and processes that 1) continually aggregate data of interest, 2) recompute derived values based upon latest available data, and 3) update visualizations on-demand, providing simple front-end tools available to resource managers and the public. For the first time, engineers and scientists can access these tools freely over the web to assist them with planning and adaptive management decisions.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 5th Federal Interagency Hydrologic Modeling Conference and the 10th Federal Interagency Sedimentation Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"5th Federal Interagency Hydrologic Modeling Conference and the 10th Federal Interagency Sedimentation Conference ","conferenceDate":"April 19-23, 2015","conferenceLocation":"Reno, NV","language":"English","publisher":"U.S. Department of Interior","usgsCitation":"Sibley, D.M., Topping, D., Hines, M., and Garner, B.D., 2015, User-interactive sediment budgets in a browser: A web application for river science and management, <i>in</i> Proceedings of the 5th Federal Interagency Hydrologic Modeling Conference and the 10th Federal Interagency Sedimentation Conference, Reno, NV, April 19-23, 2015, p. 595-605.","productDescription":"11 p.","startPage":"595","endPage":"605","ipdsId":"IP-076433","costCenters":[{"id":5054,"text":"Office of Water Information","active":true,"usgs":true}],"links":[{"id":351830,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":346747,"type":{"id":15,"text":"Index Page"},"url":"https://acwi.gov/sos/pubs/3rdJFIC/index.html"}],"publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5afeeb10e4b0da30c1bfc644","contributors":{"authors":[{"text":"Sibley, David M. dmsibley@usgs.gov","contributorId":4813,"corporation":false,"usgs":true,"family":"Sibley","given":"David","email":"dmsibley@usgs.gov","middleInitial":"M.","affiliations":[{"id":160,"text":"Center for Integrated Data Analytics","active":false,"usgs":true},{"id":5054,"text":"Office of Water Information","active":true,"usgs":true}],"preferred":true,"id":713025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Topping, David J. 0000-0002-2104-4577 dtopping@usgs.gov","orcid":"https://orcid.org/0000-0002-2104-4577","contributorId":197244,"corporation":false,"usgs":true,"family":"Topping","given":"David J.","email":"dtopping@usgs.gov","affiliations":[],"preferred":true,"id":713026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hines, Megan 0000-0002-9845-4849 mhines@usgs.gov","orcid":"https://orcid.org/0000-0002-9845-4849","contributorId":4783,"corporation":false,"usgs":true,"family":"Hines","given":"Megan","email":"mhines@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":160,"text":"Center for Integrated Data Analytics","active":false,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":5054,"text":"Office of Water Information","active":true,"usgs":true}],"preferred":true,"id":713027,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Garner, Bradley D. 0000-0002-6912-5093 bdgarner@usgs.gov","orcid":"https://orcid.org/0000-0002-6912-5093","contributorId":2133,"corporation":false,"usgs":true,"family":"Garner","given":"Bradley","email":"bdgarner@usgs.gov","middleInitial":"D.","affiliations":[{"id":5054,"text":"Office of Water Information","active":true,"usgs":true}],"preferred":true,"id":713028,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70193502,"text":"70193502 - 2015 - Soil formation: Chapter 6","interactions":[],"lastModifiedDate":"2017-11-29T14:46:29","indexId":"70193502","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Soil formation: Chapter 6","docAbstract":"<p><span>Soil formation reflects the complex interaction of many factors, among the most important of which are (i) the nature of the soil parent material, (ii) regional climate, (iii) organisms, including humans, (iv) topography and (v) time. These processes operate in Earth's critical zone; the thin veneer of our planet where rock meets life. Understanding the operation of these soil-forming factors requires an interdisciplinary approach and is a necessary predicate to charactering soil processes and functions, mitigating soil degradation and adapting soil management to environmental change. In this chapter, we discuss how these soil-forming factors operate both singly and in concert in natural and human modified environments. We emphasize the role that soil organic matter plays in these processes to provide context for understanding the benefits that it bestows on humanity.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Soil carbon: Science, management and policy for multiple benefits","language":"English","publisher":"CABI","doi":"10.1079/9781780645322.0082","usgsCitation":"Goldhaber, M.B., and Banwart, S.A., 2015, Soil formation: Chapter 6, chap. <i>of</i> Soil carbon: Science, management and policy for multiple benefits, p. 82-97, https://doi.org/10.1079/9781780645322.0082.","productDescription":"16 p.","startPage":"82","endPage":"97","ipdsId":"IP-046328","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":349563,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2014-12-03","publicationStatus":"PW","scienceBaseUri":"5a60fe3be4b06e28e9c252d1","contributors":{"authors":[{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":719262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banwart, Steven A.","contributorId":199483,"corporation":false,"usgs":false,"family":"Banwart","given":"Steven","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":719263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70193365,"text":"70193365 - 2015 - Extreme variation of sulfur isotopic compositions in pyrite from the Qiuling sediment-hosted gold deposit, West Qinling orogen, central China: An in situ SIMS study with implications for the source of sulfur","interactions":[],"lastModifiedDate":"2017-11-01T09:38:40","indexId":"70193365","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2746,"text":"Mineralium Deposita","active":true,"publicationSubtype":{"id":10}},"title":"Extreme variation of sulfur isotopic compositions in pyrite from the Qiuling sediment-hosted gold deposit, West Qinling orogen, central China: An in situ SIMS study with implications for the source of sulfur","docAbstract":"High spatial resolution textural (scanning electron microscope (SEM)), chemical (electron microprobe (EMP)) and laser ablation-inductively coupled plasma-mass spec- trometry (LA-ICP-MS)), and sulfur isotopic (secondary ion mass spectrometry (SIMS)) analyses of pyrite from the Qiuling sediment-hosted gold deposit (232±4 Ma) in the West Qinling orogen, central China were conducted to distinguish pyrite types and gain insights into the source and evolution of sulfur in hydrothermal fluids. The results reveal an enormous variation (−27.1 to +69.6‰) in sulfur isotopic composition of pyrite deposited during three paragenetic stages. Pre-ore framboidal pyrite, which is characterized by low concentra- tions of As, Au, Cu, Co, and Ni, has negative δ34S values of −27.1 to −7.6‰ that are interpreted in terms of bacterial re- duction of marine sulfate during sedimentation and diagenesis of the Paleozoic carbonate and clastic sequences, the predom- inant lithologies in the deposit area, and the most important hosts of many sediment-hosted gold deposits throughout the West Qinling orogen. The ore-stage hydrothermal pyrite con- tains high concentrations of Au, As, Cu, Sb, Tl, and Bi and hasa relatively narrow range of positive δ34S values ranging from +8.1 to +15.2‰. The sulfur isotope data are comparable to those of ore pyrite from many Triassic orogenic gold deposits and Paleozoic sedimentary exhalative (SEDEX) Pb-Zn de- posits in the West Qinling orogen, both being hosted mainly in the Devonian sequence. This similarity indicates that sulfur, responsible for the auriferous pyrite at Qiuling, was largely derived from the metamorphic devolatization of Paleozoic marine sedimentary rocks. Post-ore-stage pyrite, which is sig- nificantly enriched in Co and Ni but depleted in Au and As, has unusually high δ34S values ranging from +37.4 to +69.6 ‰, that are interpreted to result from thermochemical reduc- tion of evaporite sulfates in underlying Cambrian sedimentary rocks with very high δ34S values. The variations in Au content and sulfur isotopic compositions across a single ore-stage py- rite grain may reflect displacement of indigenous groundwater with low δ34S values by auriferous metamorphic fluids with high δ34S values. The very low-grade metamorphism of the host rocks and the metamorphic derivation of sulfur for the ore pyrite indicate that the Qiuling sediment-hosted gold deposit is an epizonal manifestation of an orogenic gold system in the West Qinling orogen.","language":"English","publisher":"Springer","doi":"10.1007/s00126-015-0597-9","usgsCitation":"Chen, L., Li, X., Li, J., Hofstra, A.H., Liu, Y., and Koenig, A.E., 2015, Extreme variation of sulfur isotopic compositions in pyrite from the Qiuling sediment-hosted gold deposit, West Qinling orogen, central China: An in situ SIMS study with implications for the source of sulfur: Mineralium Deposita, v. 50, no. 6, p. 643-656, https://doi.org/10.1007/s00126-015-0597-9.","productDescription":"14 p.","startPage":"643","endPage":"656","ipdsId":"IP-061524","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science 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,{"id":70193847,"text":"70193847 - 2015 - Effects of population reduction on white-tailed deer home-range dynamics","interactions":[],"lastModifiedDate":"2017-11-07T12:19:46","indexId":"70193847","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2898,"text":"Northeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Effects of population reduction on white-tailed deer home-range dynamics","docAbstract":"<p><span>Management strategies designed to reduce the negative impacts of overabundant&nbsp;</span><i>Odocoileus virginianus</i><span><span>&nbsp;</span>(White-tailed Deer) populations on forest regeneration may be influenced by changes in both population density and timber harvest. However, there is conflicting evidence as to how such changes in per capita resource availability influence home-range patterns. We compared home-range patterns of 33 female White-tailed Deer from a low-density population at a site with abundant browse to patterns of a sample of &gt;100 females prior to a 75% reduction in population density and a doubling in timber harvest area. Home-range and core-area sizes were approximately 3 times larger than were found prior to population decline and timber harvest increase, consistent with predictions related to intraspecific competition. We also observed greater site fidelity than previously exhibited, although this may be an artifact of increased home-range sizes. Our results support previous research suggesting that White-tailed Deer home-range size is inversely related to population density and is driven, in part, by intraspecific competition for resources. Relationships among population density, resource availability, and home-range patterns among female White-tailed Deer appear to be complex and context specific.</span></p>","language":"English","publisher":"BioOne","doi":"10.1656/045.022.0215","usgsCitation":"Crimmins, S.M., Edwards, J.W., Campbell, T.A., Ford, W., Keyser, P.D., Miller, B.F., and Miller, K.V., 2015, Effects of population reduction on white-tailed deer home-range dynamics: Northeastern Naturalist, v. 22, no. 2, p. 403-412, https://doi.org/10.1656/045.022.0215.","productDescription":"10 p.","startPage":"403","endPage":"412","ipdsId":"IP-050131","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":348369,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia","county":"Randolph County","otherGeospatial":"MeadWestvaco Wildlife and Ecosystem Research 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,{"id":70192338,"text":"70192338 - 2015 - The effect of UV-C exposure on larval survival of the dreissenid quagga mussel","interactions":[],"lastModifiedDate":"2017-10-25T09:55:27","indexId":"70192338","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"The effect of UV-C exposure on larval survival of the dreissenid quagga mussel","docAbstract":"<p>The rapid spread of quagga mussels (<i>Dreissena rostriformis bugensis</i>) has lead to their invasion of Lake Mead, Nevada, the largest reservoir in North America and partially responsible for providing water to millions of people in the southwest. Current strategies for mitigating the growth and spread of quagga mussels primarily include physical and chemical means of removing adults within water treatment, delivery, and hydropower facilities. In the present study, germicidal ultraviolet light (UV-C) was used to target the larval stage of wild-caught quagga mussel. The lethal effect of UV-C was evaluated at four different doses, 0.0, 13.1, 26.2, and 79.6 mJ/cm<sup>2</sup>. Tested doses were determined based on results from preliminary trials. The results demonstrate that germicidal UV-C is effective in controlling the free-swimming life history stages of larval quagga mussels.</p>","language":"English","publisher":"PLOS One","doi":"10.1371/journal.pone.0133039","usgsCitation":"Stewart-Malone, A., Misamore, M., Wilmoth, S.K., Reyes, A., Wong, W.H., and Gross, J., 2015, The effect of UV-C exposure on larval survival of the dreissenid quagga mussel: PLoS ONE, v. 10 , no. 7,  e0133039; 11 p., https://doi.org/10.1371/journal.pone.0133039.","productDescription":" e0133039; 11 p.","ipdsId":"IP-055533","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":471553,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0133039","text":"Publisher Index Page"},{"id":347312,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","city":"Lake Mead","volume":"10 ","issue":"7","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-07-17","publicationStatus":"PW","scienceBaseUri":"59f1a2a8e4b0220bbd9d9f96","contributors":{"authors":[{"text":"Stewart-Malone, Alecia","contributorId":198233,"corporation":false,"usgs":false,"family":"Stewart-Malone","given":"Alecia","email":"","affiliations":[],"preferred":false,"id":715433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Misamore, Michael","contributorId":198234,"corporation":false,"usgs":false,"family":"Misamore","given":"Michael","email":"","affiliations":[],"preferred":false,"id":715434,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilmoth, Siri K. swilmoth@usgs.gov","contributorId":5501,"corporation":false,"usgs":true,"family":"Wilmoth","given":"Siri","email":"swilmoth@usgs.gov","middleInitial":"K.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":715432,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reyes, Alejandro","contributorId":152369,"corporation":false,"usgs":false,"family":"Reyes","given":"Alejandro","email":"","affiliations":[{"id":18921,"text":"USGS Northern Rocky Mountain Science Center","active":true,"usgs":false}],"preferred":false,"id":715435,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wong, Wai Hing","contributorId":198235,"corporation":false,"usgs":false,"family":"Wong","given":"Wai","email":"","middleInitial":"Hing","affiliations":[],"preferred":false,"id":715436,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gross, Jackson","contributorId":198236,"corporation":false,"usgs":false,"family":"Gross","given":"Jackson","affiliations":[],"preferred":false,"id":715437,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70192313,"text":"70192313 - 2015 - Gopherus Agassizii (Agassiz’s Desert Tortoise). Mechanical Injury","interactions":[],"lastModifiedDate":"2017-10-26T09:46:57","indexId":"70192313","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"title":"Gopherus Agassizii (Agassiz’s Desert Tortoise). Mechanical Injury","docAbstract":"<p>On 3 June 2015 at 1024 h, a team of U.S. Geological Survey scientists located an immature Gopherus agassizii (Agassiz’s desert tortoise) at Joshua Tree National Park, near the southern Cottonwood Canyon entrance. The habitat in the area is typical of the Sonoran Desert in that part of California with various trees and shrubs including Larrea tridentate (creosote bush), Parkinsonia florida (blue palo verde), Olneya tesota (ironwood), Fouquieria splendens (ocotillo) and Psorothamnus spinosus (smoketree), as well as numerous species of cacti, herbaceous plants and shrubs. The 89.4 mm in carapace length G. agassizii was estimated to be four years old by counting growth rings on the plastron, and weighed 160g. It was found basking on a flat spot on a north-facing, steep, rocky slope with a Ferocactus cylindraceus (California barrel cactus) spine impaling the G. agassizii under the right leg.</p>","language":"English","publisher":"Society for the Study of Amphibians and Reptiles","usgsCitation":"Smith, A., Tennant, L.A., Lovich, J.E., and Arundel, T.R., 2015, Gopherus Agassizii (Agassiz’s Desert Tortoise). Mechanical Injury: Herpetological Review, v. 46, no. 3, p. 423-424.","productDescription":"2 p.","startPage":"423","endPage":"424","ipdsId":"IP-066261","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":347335,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":347260,"type":{"id":15,"text":"Index Page"},"url":"https://ssarherps.org/herpetological-review-pdfs/"}],"country":"United States","state":"California","otherGeospatial":"Joshua Tree National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.57318115234375,\n              34.025347738147936\n            ],\n            [\n              -116.56219482421874,\n              33.970697997361626\n     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Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":715253,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovich, Jeffrey E. 0000-0002-7789-2831 jeffrey_lovich@usgs.gov","orcid":"https://orcid.org/0000-0002-7789-2831","contributorId":458,"corporation":false,"usgs":true,"family":"Lovich","given":"Jeffrey","email":"jeffrey_lovich@usgs.gov","middleInitial":"E.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":715251,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arundel, Terence R. 0000-0003-0324-4249 tarundel@usgs.gov","orcid":"https://orcid.org/0000-0003-0324-4249","contributorId":139242,"corporation":false,"usgs":true,"family":"Arundel","given":"Terence","email":"tarundel@usgs.gov","middleInitial":"R.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":715254,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70176290,"text":"70176290 - 2015 - Head-of-tide bottleneck of particulate material transport from watersheds to estuaries","interactions":[],"lastModifiedDate":"2016-09-07T15:46:49","indexId":"70176290","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Head-of-tide bottleneck of particulate material transport from watersheds to estuaries","docAbstract":"<p><span>We measured rates of sediment, C, N, and P accumulation at four floodplain sites spanning the nontidal through oligohaline Choptank and Pocomoke Rivers, Maryland, USA. Ceramic tiles were used to collect sediment for a year and sediment cores were collected to derive decadal sedimentation rates using </span><sup>137</sup><span>Cs. The results showed highest rates of short- and long-term sediment, C, N, and P accumulation occurred in tidal freshwater forests at the head of tide on the Choptank and the oligohaline marsh of the Pocomoke River, and lowest rates occurred in the downstream tidal freshwater forests in both rivers. Presumably, watershed material was mostly trapped at the head of tide, and estuarine material was trapped in oligohaline marshes. This hydrologic transport bottleneck at the head of tide stores most available watershed sediment, C, N, and P creating a sediment shadow in lower tidal freshwater forests potentially limiting their resilience to sea level rise.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1002/2015GL066830","usgsCitation":"Ensign, S., Noe, G.E., Hupp, C.R., and Skalak, K., 2015, Head-of-tide bottleneck of particulate material transport from watersheds to estuaries: Geophysical Research Letters, v. 42, no. 24, p. 10671-10679, https://doi.org/10.1002/2015GL066830.","productDescription":"9 p.","startPage":"10671","endPage":"10679","ipdsId":"IP-070264","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":471541,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2015gl066830","text":"Publisher Index Page"},{"id":328341,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"24","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2015-12-23","publicationStatus":"PW","scienceBaseUri":"57d13a3ce4b0571647cf8dd9","contributors":{"authors":[{"text":"Ensign, Scott H.","contributorId":81397,"corporation":false,"usgs":true,"family":"Ensign","given":"Scott H.","affiliations":[],"preferred":false,"id":648207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noe, Gregory E. 0000-0002-6661-2646 gnoe@usgs.gov","orcid":"https://orcid.org/0000-0002-6661-2646","contributorId":139100,"corporation":false,"usgs":true,"family":"Noe","given":"Gregory","email":"gnoe@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":648206,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hupp, Cliff R. 0000-0003-1853-9197 crhupp@usgs.gov","orcid":"https://orcid.org/0000-0003-1853-9197","contributorId":2344,"corporation":false,"usgs":true,"family":"Hupp","given":"Cliff","email":"crhupp@usgs.gov","middleInitial":"R.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":648208,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skalak, Katherine 0000-0003-4122-1240 kskalak@usgs.gov","orcid":"https://orcid.org/0000-0003-4122-1240","contributorId":3990,"corporation":false,"usgs":true,"family":"Skalak","given":"Katherine","email":"kskalak@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":648209,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70193220,"text":"70193220 - 2015 - Alamo impact olistoliths in Antler orogenic foreland, Warm Springs–Milk Spring area, Hot Creek Range, central Nevada","interactions":[],"lastModifiedDate":"2022-01-24T15:34:39.693256","indexId":"70193220","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Alamo impact olistoliths in Antler orogenic foreland, Warm Springs–Milk Spring area, Hot Creek Range, central Nevada","docAbstract":"<p>The 45 km<sup>2</sup><span>&nbsp;</span>map area is situated at the south end of the Hot Creek Range in central Nevada, ~16 km east of the buried leading edge of the Mississippian Roberts Mountains thrust. Three eastward-trending left-slip faults divide the area into four structural blocks. The southernmost block is occupied solely by upper Oligocene volcanic rocks. The narrow northernmost block, now occupied surficially by valley fill and volcanic rocks, represents the south end of the main part of the Hot Creek Range, from which the study area is offset. The middle two blocks display different aspects of the eastward-traveled outer crater rim created by the ca. 382 Ma (early Late Devonian, middle Frasnian) Alamo impact.</p><p>The Alamo impact was produced by a 5-km-diameter bolide, most likely a comet, which excavated a transient submarine crater 44–65 km in diameter. Comparison of thin (8–12 m) Alamo Breccia deposits in the northern of the middle two blocks with a more easterly, thick (35–42 m) Alamo deposit in the main Hot Creek Range, 4 km north of the map area, suggests that these blocks traveled many kilometers eastward. The northern of the middle two blocks contains a large olistolith capped by the thin breccia, whereas the southern block contains a larger olistolith lacking an Alamo Breccia cap.</p><p>Three Devonian pulses of the Antler orogeny are better documented in the chapter on the Bisoni-McKay area. Here, the first Antler pulse in latest Middle Devonian time is obscured within an ~9 m.y. hiatus enlarged by excavation of the Alamo impact crater. The second Antler pulse is recorded by the ~4 m.y. hiatus produced by the regional unconformity between the lower and upper members of the Woodruff Formation. The third Antler pulse is documented by an ~8 m.y. regional hiatus between the Mississippian Webb Formation and Upper Devonian Woodruff Formation. In previous papers, we had interpreted this pulse to initiate the Antler orogeny.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Unusual central Nevada geologic terranes produced by Late Devonian antler orogeny and Alamo impact","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/2015.2517(02)","usgsCitation":"Poole, F.G., and Sandberg, C., 2015, Alamo impact olistoliths in Antler orogenic foreland, Warm Springs–Milk Spring area, Hot Creek Range, central Nevada, chap. <i>of</i> Unusual central Nevada geologic terranes produced by Late Devonian antler orogeny and Alamo impact, p. 39-104, https://doi.org/10.1130/2015.2517(02).","productDescription":"66 p.","startPage":"39","endPage":"104","ipdsId":"IP-064956","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science 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,{"id":70189616,"text":"70189616 - 2015 - Shaking intensity from injection-induced versus tectonic earthquakes in the central-eastern United States","interactions":[],"lastModifiedDate":"2017-07-19T11:10:27","indexId":"70189616","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3568,"text":"The Leading Edge","active":true,"publicationSubtype":{"id":10}},"title":"Shaking intensity from injection-induced versus tectonic earthquakes in the central-eastern United States","docAbstract":"<p><span>Although instrumental recordings of earthquakes in the central and eastern United States (CEUS) remain sparse, the U. S. Geological Survey's “Did you feel it?” (DYFI) system now provides excellent characterization of shaking intensities caused by induced and tectonic earthquakes. Seventeen CEUS events are considered between 2013 and 2015. It is shown that for 15 events, observed intensities at epicentral distances greater than ≈ 10 km are lower than expected given a published intensity-prediction equation for the region. Using simple published relations among intensity, magnitude, and stress drop, the results suggest that 15 of the 17 events have low stress drop. For those 15 events, intensities within ≈ 10-km epicentral distance are closer to predicted values, which can be explained as a consequence of relatively shallow source depths. The results suggest that those 15 events, most of which occurred in areas where induced earthquakes have occurred previously, were likely induced. Although moderate injection-induced earthquakes in the central and eastern United States will be felt widely because of low regional attenuation, the damage from shallow earthquakes induced by injection will be more localized to event epicenters than shaking tectonic earthquakes, which tend to be somewhat deeper. Within approximately 10 km of the epicenter, intensities are generally commensurate with predicted levels expected for the event magnitude.</span><br></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/tle34060690.1","usgsCitation":"Hough, S.E., 2015, Shaking intensity from injection-induced versus tectonic earthquakes in the central-eastern United States: The Leading Edge, v. 34, no. 6, p. 690-697, https://doi.org/10.1190/tle34060690.1.","productDescription":"6 p.","startPage":"690","endPage":"697","ipdsId":"IP-063054","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":344018,"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              -79.89257812499999,\n              41.178653972331674\n            ],\n            [\n              -106.171875,\n              44.77793589631623\n            ],\n            [\n              -106.12792968749999,\n              42.97250158602597\n            ],\n            [\n              -104.94140625,\n              32.76880048488168\n            ],\n            [\n              -81.5185546875,\n              33.358061612778876\n            ],\n            [\n              -79.89257812499999,\n              41.178653972331674\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"6","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59706fb8e4b0d1f9f065a8b0","contributors":{"authors":[{"text":"Hough, Susan E. 0000-0002-5980-2986 hough@usgs.gov","orcid":"https://orcid.org/0000-0002-5980-2986","contributorId":587,"corporation":false,"usgs":true,"family":"Hough","given":"Susan","email":"hough@usgs.gov","middleInitial":"E.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":705454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70189952,"text":"70189952 - 2015 - Groundwater: The disregarded component in lake water and nutrient budgets, Part 1: Effects of groundwater on hydrology","interactions":[],"lastModifiedDate":"2017-08-01T14:35:16","indexId":"70189952","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater: The disregarded component in lake water and nutrient budgets, Part 1: Effects of groundwater on hydrology","docAbstract":"Lake eutrophication is a large and growing problem in many parts of the world, commonly due to anthropogenic sources of\nnutrients. Improved quantification of nutrient inputs is required to address this problem, including better determination of\nexchanges between groundwater and lakes. This first of a two-part review provides a brief history of the evolution of the study of\ngroundwater exchange with lakes, followed by a listing of the most commonly used methods for quantifying this exchange.\nRates of exchange between lakes and groundwater compiled from the literature are statistically summarized for both exfiltration\n(flow from groundwater to a lake) and infiltration (flow from a lake to groundwater), including per cent contribution of\ngroundwater to lake-water budgets. Reported rates of exchange between groundwater and lakes span more than five orders of\nmagnitude. Median exfiltration is 0.74 cm/day, and median infiltration is 0.60 cm/day. Exfiltration ranges from near 0% to 94%\nof input terms in lake-water budgets, and infiltration ranges from near 0% to 91% of loss terms. Median values for exfiltration\nand infiltration as percentages of input and loss terms of lake-water budgets are 25% and 35%, respectively. Quantification of the\ngroundwater term is somewhat method dependent, indicating that calculating the groundwater component with multiple methods\ncan provide a better understanding of the accuracy of estimates. The importance of exfiltration to a lake budget ranges widely for\nlakes less than about 100 ha in area but generally decreases with increasing lake area, particularly for lakes that exceed 100 ha in\narea. No such relation is evident for lakes where infiltration occurs, perhaps because of the smaller sample size. Copyright ©\n2014 John Wiley & Sons, Ltd.","language":"English","publisher":"Wiley","doi":"10.1002/hyp.10403","usgsCitation":"Rosenberry, D.O., Lewandowski, J., Meinikmann, K., and Nutzmann, G., 2015, Groundwater: The disregarded component in lake water and nutrient budgets, Part 1: Effects of groundwater on hydrology: Hydrological Processes, v. 29, no. 13, p. 2895-2921, https://doi.org/10.1002/hyp.10403.","productDescription":"27 p.","startPage":"2895","endPage":"2921","ipdsId":"IP-053819","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":344509,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"13","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-01-08","publicationStatus":"PW","scienceBaseUri":"59819315e4b0e2f5d463b7a1","contributors":{"authors":[{"text":"Rosenberry, Donald O. 0000-0003-0681-5641 rosenber@usgs.gov","orcid":"https://orcid.org/0000-0003-0681-5641","contributorId":1312,"corporation":false,"usgs":true,"family":"Rosenberry","given":"Donald","email":"rosenber@usgs.gov","middleInitial":"O.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":706861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewandowski, Jorg","contributorId":195317,"corporation":false,"usgs":false,"family":"Lewandowski","given":"Jorg","email":"","affiliations":[],"preferred":false,"id":706862,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meinikmann, Karin","contributorId":195318,"corporation":false,"usgs":false,"family":"Meinikmann","given":"Karin","email":"","affiliations":[],"preferred":false,"id":706863,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nutzmann, Gunnar","contributorId":195319,"corporation":false,"usgs":false,"family":"Nutzmann","given":"Gunnar","email":"","affiliations":[],"preferred":false,"id":706864,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70159389,"text":"70159389 - 2015 - Science foundation Chapter 5 Appendix 5.1: Case study dabbling ducks","interactions":[],"lastModifiedDate":"2017-05-09T09:21:30","indexId":"70159389","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Science foundation Chapter 5 Appendix 5.1: Case study dabbling ducks","docAbstract":"<p>Dabbling ducks are the most abundant group of waterfowl that overwinter in the shallow wetlands and ponds of San Francisco Bay (SFB). Species within this group are primarily omnivorous, feeding on both plant material and macroinvertebrate prey by “tipping” to access benthic foods in bottom sediments or by foraging in the water column. Although the majority of these ducks are migratory, smaller numbers also nest locally in the SFB. These species vary in body size, ranging from the large mallard (<i>Anas platyrhynchos</i>) to the small green-winged teal (<i>Anas crecca</i>). Other dabbling duck species present in the SFB include American wigeon (<i>Anas americana</i>), gadwall (<i>Anas strepera</i>), cinnamon teal (<i>Anas cyanoptera</i>), northern shoveler (<i>Anas clypeata</i>), northern pintail (<i>Anas acuta</i>), and wood duck (<i>Aix sponsa</i>). </p><p>Most of these dabbling duck species are known to breed in the SFB with the exception of the American wigeon and green-winged teal. However, the majority of wintering ducks originate from breeding grounds in the Central Valley of California, Pacific Coast States, Alaska, and Intermountain States/provinces, prairie potholes, and boreal forest. Their wintering populations in SFB are greatest between October and January, and dabbling duck species are found in all SFB regions. However, most dabbling duck use is associated with former salt production ponds and in the north and south bays, and managed wetlands of the Suisun Marsh.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The baylands and climate change what we can do: Baylands ecosystem habitat goals science update 2015","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"California State Coastal Conservancy","usgsCitation":"Yarris, G., and Ackerman, J., 2015, Science foundation Chapter 5 Appendix 5.1: Case study dabbling ducks, 6 p.","productDescription":"6 p.","ipdsId":"IP-060903","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":340984,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":310636,"type":{"id":15,"text":"Index Page"},"url":"https://baylandsgoals.org/case-studies/"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.29406738281249,\n              36.86204269508728\n            ],\n            [\n              -120.8551025390625,\n              36.86204269508728\n            ],\n            [\n              -120.8551025390625,\n              38.44498466889473\n            ],\n            [\n              -123.29406738281249,\n              38.44498466889473\n            ],\n            [\n              -123.29406738281249,\n              36.86204269508728\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5912d53ae4b0e541a03d452f","contributors":{"authors":[{"text":"Yarris, Gregory S.","contributorId":115361,"corporation":false,"usgs":true,"family":"Yarris","given":"Gregory S.","affiliations":[],"preferred":false,"id":578354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":578353,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70157372,"text":"70157372 - 2015 - Adaptive harvest management for the Svalbard population of pink-footed geese: 2015 progress summary","interactions":[],"lastModifiedDate":"2017-05-10T09:46:42","indexId":"70157372","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":296,"text":"Technical Report from DCE - Danish Centre for Environment and Energy","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64","title":"Adaptive harvest management for the Svalbard population of pink-footed geese: 2015 progress summary","docAbstract":"This document describes progress to date on the development of an adaptive harvest management strategy for maintaining the Svalbard population of pink‐footed geese (Anser brachyrhynchus) near their agreed target level (60,000) by providing for sustainable harvests in Norway and Denmark. This report provides an assessment of the most recent monitoring information (1991-2014) and its implications for the harvest management strategy, and it is an update of an initial assessment for 2013-2015 (see http://pinkfootedgoose.aewa.info/). By combining varying hypotheses about survival and reproduction, a suite of nine models have been developed that represent a wide range of possibilities concerning the extent to which demographic rates are density dependent or independent. Current updated model weights suggest little evidence for density-dependent survival and reproduction, suggesting that the population may have recently experienced a release from density-dependent mechanisms, corresponding to the period of most rapid growth in population size. The optimal harvest strategy for the 2013–2015 hunting seasons prescribed a harvest quota of 15,000 per year. The harvest in the 2014 hunting season was 14,991, compared to 11,081 in 2013, mostly due to an increase in harvest in Denmark during January 2015. The percentage of young in the fall of 2014 was 10.3%, which is lower than average. The observed population size of 59,000 in May 2015 was much lower than expected. For the 2015 hunting season, observed population size and temperature days suggest that an emergency closure should be considered. In the event a harvest of 15,000 is maintained, predicted population size in May 2016 is 51,700 (95% CL: 41,600-64,300), based on observed TempDays = 9 in May 2015 and the most recent model weights. On the other hand, if the season were closed this year, we would expect a population size of 66,700 (95% CL: 53,600-82,900) in May 2016. A total harvest of 6,700 would be expected to result in a 2016 population size at goal (i.e., 60,000).","largerWorkTitle":"Danish Centre for Environment and Energy","language":"English","publisher":"Aarhus University, DCE - Danish Centre for Environment and Energy","collaboration":"Aarhus University, Denmark","usgsCitation":"Johnson, F.A., and Madsen, J., 2015, Adaptive harvest management for the Svalbard population of pink-footed geese: 2015 progress summary: Technical Report from DCE - Danish Centre for Environment and Energy 64, Report: v, 24 p.","productDescription":"Report: v, 24 p.","ipdsId":"IP-066789","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":341049,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":308358,"type":{"id":15,"text":"Index Page"},"url":"https://pinkfootedgoose.aewa.info/node/193"}],"country":"Denmark, Norway","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[12.69001,55.60999],[12.08999,54.80001],[11.04354,55.36486],[10.90391,55.77995],[12.3709,56.11141],[12.69001,55.60999]]],[[[10.91218,56.45862],[10.6678,56.08138],[10.36999,56.19001],[9.64998,55.47],[9.92191,54.9831],[9.28205,54.83087],[8.52623,54.96274],[8.12031,55.51772],[8.08998,56.54001],[8.25658,56.80997],[8.54344,57.11],[9.42447,57.17207],[9.77556,57.44794],[10.58001,57.73002],[10.54611,57.21573],[10.25,56.89002],[10.36999,56.60998],[10.91218,56.45862]]],[[[28.16555,71.18547],[31.29342,70.45379],[30.00544,70.18626],[31.10108,69.55808],[29.39958,69.15692],[28.59193,69.06478],[29.01557,69.76649],[27.73229,70.16419],[26.17962,69.8253],[25.68921,69.09211],[24.73568,68.64956],[23.66205,68.89125],[22.35624,68.84174],[21.24494,69.37044],[20.64559,69.10625],[20.02527,69.06514],[19.87856,68.40719],[17.99387,68.56739],[17.72918,68.01055],[16.76888,68.01394],[16.10871,67.30246],[15.10841,66.19387],[13.55569,64.78703],[13.91991,64.44542],[13.57192,64.04911],[12.57994,64.06622],[11.93057,63.12832],[11.99206,61.80036],[12.63115,61.29357],[12.30037,60.11793],[11.46827,59.43239],[11.02737,58.85615],[10.35656,59.46981],[8.382,58.31329],[7.04875,58.07888],[5.66584,58.58816],[5.30823,59.66323],[4.99208,61.971],[5.9129,62.61447],[8.55341,63.45401],[10.52771,64.48604],[12.35835,65.87973],[14.76115,67.81064],[16.43593,68.56321],[19.18403,69.81744],[21.37842,70.25517],[23.02374,70.20207],[24.54654,71.0305],[26.37005,70.98626],[28.16555,71.18547]]],[[[24.72412,77.85385],[22.49032,77.44493],[20.72601,77.67704],[21.41611,77.93504],[20.8119,78.25463],[22.88426,78.45494],[23.28134,78.07954],[24.72412,77.85385]]],[[[18.25183,79.70175],[21.54383,78.95611],[19.02737,78.5626],[18.47172,77.82669],[17.59441,77.63796],[17.1182,76.80941],[15.91315,76.77045],[13.76259,77.38035],[14.66956,77.73565],[13.1706,78.02493],[11.22231,78.8693],[10.44453,79.65239],[13.17077,80.01046],[13.71852,79.66039],[15.14282,79.67431],[15.52255,80.01608],[16.99085,80.05086],[18.25183,79.70175]]],[[[25.44763,80.40734],[27.40751,80.05641],[25.92465,79.51783],[23.02447,79.40001],[20.07519,79.56682],[19.89727,79.84236],[18.46226,79.85988],[17.36802,80.3189],[20.45599,80.59816],[21.90794,80.35768],[22.91925,80.65714],[25.44763,80.40734]]]]},\"properties\":{\"name\":\"Denmark\"}}]}","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"591426bce4b0e541a03e9604","contributors":{"authors":[{"text":"Johnson, Fred A. 0000-0002-5854-3695 fjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-5854-3695","contributorId":2773,"corporation":false,"usgs":true,"family":"Johnson","given":"Fred","email":"fjohnson@usgs.gov","middleInitial":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":572902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Madsen, Jesper","contributorId":9950,"corporation":false,"usgs":true,"family":"Madsen","given":"Jesper","affiliations":[],"preferred":false,"id":572903,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189611,"text":"70189611 - 2015 - Earthquake geology of the Bulnay Fault (Mongolia)","interactions":[],"lastModifiedDate":"2017-07-19T09:56:15","indexId":"70189611","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake geology of the Bulnay Fault (Mongolia)","docAbstract":"<p>The Bulnay earthquake of July 23, 1905 (M<sub>w</sub> 8.3-8.5), in north-central Mongolia, is one of the world's largest recorded intracontinental earthquakes and one of four great earthquakes that occurred in the region during the 20th century. The 375-km-long surface rupture of the left-lateral, strike-slip, N095°E trending Bulnay Fault associated with this earthquake is remarkable for its pronounced expression across the landscape and for the size of features produced by previous earthquakes. Our field observations suggest that in many areas the width and geometry of the rupture zone is the result of repeated earthquakes; however, in those areas where it is possible to determine that the geomorphic features are the result of the 1905 surface rupture alone, the size of the features produced by this single earthquake are singular in comparison to most other historical strike-slip surface ruptures worldwide. Along the 80 km stretch, between 97.18°E and 98.33°E, the fault zone is characterized by several meters width and the mean left-lateral 1905 offset is 8.9 ± 0.6 m with two measured cumulative offsets that are twice the 1905 slip. These observations suggest that the displacement produced during the penultimate event was similar to the 1905 slip. Morphotectonic analyses carried out at three sites along the eastern part of the Bulnay fault, allow us to estimate a mean horizontal slip rate of 3.1 ± 1.7 mm/yr over the Late Pleistocene-Holocene period. In parallel, paleoseismological investigations show evidence for two earthquakes prior to the 1905 event with recurrence intervals of ~2700-4000 years.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120140119","usgsCitation":"Rizza, M., Ritz, J., Prentice, C.S., Vassallo, R., Braucher, R., Larroque, C., Arzhannikova, A., Arzhanikov, S., Mahan, S.A., Massault, M., Michelot, J., and Todbileg, M., 2015, Earthquake geology of the Bulnay Fault (Mongolia): Bulletin of the Seismological Society of America, v. 105, no. 1, p. 72-93, https://doi.org/10.1785/0120140119.","productDescription":"22 p.","startPage":"72","endPage":"93","ipdsId":"IP-060346","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":471550,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hal.science/hal-01179837","text":"External Repository"},{"id":344024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mongolia","otherGeospatial":"Bulnay Fault","volume":"105","issue":"1","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2015-01-13","publicationStatus":"PW","scienceBaseUri":"59706fb9e4b0d1f9f065a8b9","contributors":{"authors":[{"text":"Rizza, Magali","contributorId":194806,"corporation":false,"usgs":false,"family":"Rizza","given":"Magali","email":"","affiliations":[],"preferred":false,"id":705412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ritz, Jean-Franciois","contributorId":194807,"corporation":false,"usgs":false,"family":"Ritz","given":"Jean-Franciois","email":"","affiliations":[],"preferred":false,"id":705413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prentice, Carol S. 0000-0003-3732-3551 cprentice@usgs.gov","orcid":"https://orcid.org/0000-0003-3732-3551","contributorId":2676,"corporation":false,"usgs":true,"family":"Prentice","given":"Carol","email":"cprentice@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":705411,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vassallo, Ricardo","contributorId":194808,"corporation":false,"usgs":false,"family":"Vassallo","given":"Ricardo","email":"","affiliations":[],"preferred":false,"id":705414,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Braucher, Regis","contributorId":194809,"corporation":false,"usgs":false,"family":"Braucher","given":"Regis","email":"","affiliations":[],"preferred":false,"id":705415,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Larroque, Christophe","contributorId":194810,"corporation":false,"usgs":false,"family":"Larroque","given":"Christophe","email":"","affiliations":[],"preferred":false,"id":705416,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Arzhannikova, A.","contributorId":194811,"corporation":false,"usgs":false,"family":"Arzhannikova","given":"A.","email":"","affiliations":[],"preferred":false,"id":705417,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Arzhanikov, S.","contributorId":194812,"corporation":false,"usgs":false,"family":"Arzhanikov","given":"S.","email":"","affiliations":[],"preferred":false,"id":705418,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":705419,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Massault, M.","contributorId":194813,"corporation":false,"usgs":false,"family":"Massault","given":"M.","email":"","affiliations":[],"preferred":false,"id":705420,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Michelot, J-L.","contributorId":194814,"corporation":false,"usgs":false,"family":"Michelot","given":"J-L.","email":"","affiliations":[],"preferred":false,"id":705421,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Todbileg, M.","contributorId":194815,"corporation":false,"usgs":false,"family":"Todbileg","given":"M.","email":"","affiliations":[],"preferred":false,"id":705422,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70157104,"text":"70157104 - 2015 - Mechanisms of sediment flux between shallows and marshes","interactions":[],"lastModifiedDate":"2017-05-10T12:05:44","indexId":"70157104","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mechanisms of sediment flux between shallows and marshes","docAbstract":"We conducted a field study to investigate temporal variation and forcing mechanisms of sediment flux between a salt marsh and adjacent shallows in northern San Francisco Bay. Suspended-sediment concentration (SSC), tidal currents, and wave properties were measured over the marsh, in marsh creeks, and in bay shallows. Cumulative sediment flux in the marsh creeks was bayward during the study, and was dominated by large bayward flux during the largest tides of the year. This result was unexpected because extreme high tides with long inundation periods are commonly assumed to supply sediment to marshes, and long-term accretion estimates show that the marsh in the study site is depositional. A water mass-balance shows that some landward transport bypassed the creeks, most likely across the marsh-bay interface. An estimate of transport by this pathway based on observed SSC and inferred volume indicates that it was likely much less than the observed export.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Proceedings of Coastal Sediments 2015","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Coastal Sediments 2015","conferenceDate":"May 11-15, 2015","conferenceLocation":"San Diego, CA","language":"English","publisher":"World Scientific","doi":"10.1142/9789814689977_0082","collaboration":"San Francisco Bay National Estuarine Research Reserve","usgsCitation":"Lacy, J.R., Schile, L., Callaway, J., and Ferner, M., 2015, Mechanisms of sediment flux between shallows and marshes, <i>in</i> The Proceedings of Coastal Sediments 2015, San Diego, CA, May 11-15, 2015, https://doi.org/10.1142/9789814689977_0082.","ipdsId":"IP-063014","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":341065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.06335449218749,\n              37.3002752813443\n            ],\n            [\n              -121.4373779296875,\n              37.3002752813443\n            ],\n            [\n              -121.4373779296875,\n              38.28131307922966\n            ],\n            [\n              -123.06335449218749,\n              38.28131307922966\n            ],\n            [\n              -123.06335449218749,\n              37.3002752813443\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2015-04-15","publicationStatus":"PW","scienceBaseUri":"591426bee4b0e541a03e960c","contributors":{"authors":[{"text":"Lacy, Jessica R. 0000-0002-2797-6172 jlacy@usgs.gov","orcid":"https://orcid.org/0000-0002-2797-6172","contributorId":3158,"corporation":false,"usgs":true,"family":"Lacy","given":"Jessica","email":"jlacy@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":571659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schile, L.M.","contributorId":68013,"corporation":false,"usgs":true,"family":"Schile","given":"L.M.","affiliations":[],"preferred":false,"id":571660,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Callaway, J.C.","contributorId":147426,"corporation":false,"usgs":false,"family":"Callaway","given":"J.C.","affiliations":[{"id":16849,"text":"University of San Francisco","active":true,"usgs":false}],"preferred":false,"id":571661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ferner, M.C.","contributorId":147427,"corporation":false,"usgs":false,"family":"Ferner","given":"M.C.","affiliations":[{"id":16850,"text":"San Francisco Bay NERR","active":true,"usgs":false}],"preferred":false,"id":571662,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70157102,"text":"70157102 - 2015 - The role of suspension events in cross-shore and longshore suspended sediment transport in the surf zone","interactions":[],"lastModifiedDate":"2017-05-10T12:11:32","indexId":"70157102","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The role of suspension events in cross-shore and longshore suspended sediment transport in the surf zone","docAbstract":"Suspension of sand in the surf zone is intermittent. Especially striking in a time series of concentration are periods of intense suspension, suspension events, when the water column suspended sediment concentration is an order of magnitude greater than the mean concentration. The prevalence, timing, and contribution of suspension events to cross-shore and longshore suspended sediment transport are explored using field data collected in the inner half of the surf zone during a large storm at Duck, NC. Suspension events are defined as periods when the concentration is above a threshold. Events tended to occur during onshore flow under the wave crest, resulting in an onshore contribution to the suspended sediment transport. Even though large events occurred less than 10 percent of the total time, at some locations onshore transport associated with suspension events was greater than mean-current driven offshore-directed transport during non-event periods, causing the net suspended sediment transport to be onshore. Events and fluctuations in longshore velocity were not correlated. However, events did increase the longshore suspended sediment transport by approximately the amount they increase the mean concentration, which can be up to 35%. Because of the lack of correlation, the longshore suspended sediment transport can be modeled without considering the details of the intensity and time of events as the vertical integration of the product of the time-averaged longshore velocity and an event-augmented time-averaged concentration.  However, to accurately model cross-shore suspended sediment transport, the timing and intensity of suspension events must be reproduced.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Proceedings of the Coastal Sediments 2015","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Coastal Sediments 2015","conferenceDate":"May 11-15, 2015","conferenceLocation":"San Diego, CA","language":"English","publisher":"World Scientific","usgsCitation":"Jaffe, B.E., 2015, The role of suspension events in cross-shore and longshore suspended sediment transport in the surf zone, <i>in</i> The Proceedings of the Coastal Sediments 2015, San Diego, CA, May 11-15, 2015.","ipdsId":"IP-063552","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":341066,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","city":"Duck","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.036376953125,\n              36.0624217151089\n            ],\n            [\n              -75.6134033203125,\n              36.0624217151089\n            ],\n            [\n              -75.6134033203125,\n              36.53832942872818\n            ],\n            [\n              -76.036376953125,\n              36.53832942872818\n            ],\n            [\n              -76.036376953125,\n              36.0624217151089\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"591426bee4b0e541a03e960e","contributors":{"authors":[{"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":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":571652,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70141198,"text":"70141198 - 2015 - Long-term monitoring program: Evaluating chronic exposure of harlequin ducks and sea otters to lingering Exxon Valdez Oil in Western Prince William Sound","interactions":[],"lastModifiedDate":"2018-02-14T13:08:31","indexId":"70141198","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Long-term monitoring program: Evaluating chronic exposure of harlequin ducks and sea otters to lingering Exxon Valdez Oil in Western Prince William Sound","docAbstract":"<p>We found that average cytochrome P4501A induction (as measured by EROD activity) during March 2014 was not elevated in wintering harlequin ducks captured in areas of Prince William Sound oiled by the 1989 <i>Exxon Valdez</i> oil spill, relative to those captured in unoiled areas. This result is consistent with findings from March 2013. We interpret these findings to indicate that exposure of harlequin ducks to residual<i> Exxon Valdez</i> oil abated within 24 years after the original spill. Results from preceding sampling in 2011 indicated that EROD activity was elevated in harlequin ducks in oiled relative to unoiled areas, although the magnitude of elevation was lower than in previous years (1998-2009), suggesting that the rate or intensity of exposure was diminishing by 2011. The data presented in this report add to a growing body of literature indicating that persistence of oil in the environment, and exposure of wildlife to that oil, can occur over much longer time frames than previously assumed.</p>","language":"English","publisher":"Exxon Valdez Oil Spill Trustee Council","publisherLocation":"Anchorage, AK","usgsCitation":"Esler, D., Bowen, L., Miles, A.K., Ballachey, B.E., and Bodkin, J.L., 2015, Long-term monitoring program: Evaluating chronic exposure of harlequin ducks and sea otters to lingering Exxon Valdez Oil in Western Prince William Sound, 46 p.","productDescription":"46 p.","ipdsId":"IP-061863","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":342376,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -164.50927734375,\n              54.533832507944304\n            ],\n            [\n              -164.50927734375,\n              54.20101023973888\n            ],\n            [\n              -163.9599609375,\n              53.77468884583577\n            ],\n            [\n              -162.26806640625,\n              53.74871079689897\n            ],\n            [\n              -159.609375,\n              54.149567212540525\n            ],\n            [\n              -155.85205078125,\n              54.61025498157912\n            ],\n            [\n              -153.6767578125,\n              55.7642131648377\n            ],\n            [\n              -152.314453125,\n              56.27996083172844\n            ],\n            [\n              -144.4921875,\n              60.4788788301667\n            ],\n            [\n              -144.0087890625,\n              60.80206374467983\n            ],\n            [\n              -144.580078125,\n              61.20679804263029\n            ],\n            [\n              -144.7998046875,\n              61.52269494598361\n            ],\n            [\n              -145.74462890625,\n              61.554109444927185\n            ],\n            [\n              -146.44775390625,\n              61.77312286453146\n            ],\n            [\n              -148.6669921875,\n              61.91827102335593\n            ],\n            [\n              -149.6337890625,\n              61.7419302246182\n            ],\n            [\n              -150.6005859375,\n              61.37567331572747\n            ],\n            [\n              -153.91845703125,\n              59.93300042374631\n            ],\n            [\n              -154.51171875,\n              59.567723306212955\n            ],\n            [\n              -155.32470703125,\n              59.108308258604964\n            ],\n            [\n              -155.17089843749997,\n              58.81374171570782\n            ],\n            [\n              -155.50048828125,\n              58.35563036280964\n            ],\n            [\n              -156.533203125,\n              57.69240553526455\n            ],\n            [\n              -159.19189453125,\n              56.64414704199467\n            ],\n            [\n              -160.7958984375,\n              55.91227293006361\n            ],\n            [\n              -162.8173828125,\n              55.2415520356525\n            ],\n            [\n              -164.50927734375,\n              54.533832507944304\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"593fa833e4b0764e6c627954","contributors":{"authors":[{"text":"Esler, Daniel 0000-0001-5501-4555 desler@usgs.gov","orcid":"https://orcid.org/0000-0001-5501-4555","contributorId":5465,"corporation":false,"usgs":true,"family":"Esler","given":"Daniel","email":"desler@usgs.gov","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":12437,"text":"Simon Fraser University, Centre for Wildlife Ecology","active":true,"usgs":false}],"preferred":true,"id":540565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowen, Lizabeth 0000-0001-9115-4336 lbowen@usgs.gov","orcid":"https://orcid.org/0000-0001-9115-4336","contributorId":4539,"corporation":false,"usgs":true,"family":"Bowen","given":"Lizabeth","email":"lbowen@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":697858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miles, A. 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,{"id":70157355,"text":"70157355 - 2015 - An environmental survey of Serpentine Hot Springs: Geology, hydrology, geochemistry, and microbiology","interactions":[],"lastModifiedDate":"2017-05-10T09:56:32","indexId":"70157355","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":273,"text":"Natural Resource Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"NPS/BELA/NRR—2015/1019","title":"An environmental survey of Serpentine Hot Springs: Geology, hydrology, geochemistry, and microbiology","docAbstract":"<p><span>Serpentine Hot Springs is the most visited site in the Bering Land Bridge National Preserve. The hot springs have traditionally been used by the Native people of the Seward Peninsula for religious, medicinal and spiritual purposes and continue to be used in many of the same ways by Native people today. The hot springs are also popular with non-Native users from Nome and other communities, recreational users and pilots from out of the area, and hunters and hikers. </span></p>","largerWorkTitle":"US Park Service","language":"English","usgsCitation":"Nordstrom, D.K., Hasselbach, L., Ingebritsen, S.E., Skorupa, D., McCleskey, R.B., and McDermott, T.R., 2015, An environmental survey of Serpentine Hot Springs: Geology, hydrology, geochemistry, and microbiology: Natural Resource Report NPS/BELA/NRR—2015/1019, Report: xii, 90 p.","productDescription":"Report: xii, 90 p.","ipdsId":"IP-056340","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"links":[{"id":341051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341050,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://irma.nps.gov/DataStore/Reference/Profile/2224027"}],"country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula, Serpentine Hot Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -169.87060546875,\n              64.00486735371551\n            ],\n            [\n              -160.9716796875,\n              64.00486735371551\n            ],\n            [\n              -160.9716796875,\n              67.82583637985663\n            ],\n            [\n              -169.87060546875,\n              67.82583637985663\n            ],\n            [\n              -169.87060546875,\n              64.00486735371551\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"591426bce4b0e541a03e9606","contributors":{"authors":[{"text":"Nordstrom, D. 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