{"pageNumber":"1140","pageRowStart":"28475","pageSize":"25","recordCount":165359,"records":[{"id":70160784,"text":"70160784 - 2015 - Large-scale control site selection for population monitoring: an example assessing Sage-grouse trends","interactions":[],"lastModifiedDate":"2015-12-31T13:03:13","indexId":"70160784","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Large-scale control site selection for population monitoring: an example assessing Sage-grouse trends","docAbstract":"<p>Human impacts on wildlife populations are widespread and prolific and understanding wildlife responses to human impacts is a fundamental component of wildlife management. The first step to understanding wildlife responses is the documentation of changes in wildlife population parameters, such as population size. Meaningful assessment of population changes in potentially impacted sites requires the establishment of monitoring at similar, nonimpacted, control sites. However, it is often difficult to identify appropriate control sites in wildlife populations. We demonstrated use of Geographic Information System (GIS) data across large spatial scales to select biologically relevant control sites for population monitoring. Greater sage-grouse (Centrocercus urophasianus; hearafter, sage-grouse) are negatively affected by energy development, and monitoring of sage-grouse population within energy development areas is necessary to detect population-level responses. Weused population data (1995&ndash;2012) from an energy development area in Wyoming, USA, the Atlantic Rim Project Area (ARPA), and GIS data to identify control sites that were not impacted by energy development for population monitoring. Control sites were surrounded by similar habitat and were within similar climate areas to the ARPA. We developed nonlinear trend models for both the ARPA and control sites and compared long-term trends from the 2 areas. We found little difference between the ARPA and control sites trends over time. This research demonstrated an approach for control site selection across large landscapes and can be used as a template for similar impact-monitoring studies. It is important to note that identification of changes in population parameters between control and treatment sites is only the first step in understanding the mechanisms that underlie those changes. Published 2015. This article is a U.S. Government work and is in the public domain in the USA.</p>","language":"English","publisher":"Wiley","doi":"10.1002/wsb.601","usgsCitation":"Fedy, B.C., O’Donnell, M.S., and Bowen, Z.H., 2015, Large-scale control site selection for population monitoring: an example assessing Sage-grouse trends: Wildlife Society Bulletin, v. 39, no. 4, p. 700-712, https://doi.org/10.1002/wsb.601.","productDescription":"13 p.","startPage":"700","endPage":"712","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-053414","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":499960,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doaj.org/article/1512b0d458ea4c8ab77bd670ee6a3220","text":"External Repository"},{"id":313148,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"South-Central","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.226806640625,\n              42.99259451971113\n            ],\n            [\n              -109.21508789062499,\n              42.97250158602597\n            ],\n            [\n              -109.97863769531249,\n              43.11702412135048\n            ],\n            [\n              -110.841064453125,\n              43.56845179881218\n            ],\n            [\n              -110.841064453125,\n              43.28920196020127\n            ],\n            [\n              -110.9124755859375,\n              42.601619944327965\n            ],\n            [\n              -111.05529785156249,\n              42.589488572714245\n            ],\n            [\n              -111.03881835937499,\n              41.000629848685385\n            ],\n            [\n              -108.2208251953125,\n              41.01721057822846\n            ],\n            [\n              -108.1109619140625,\n              41.27367811566259\n            ],\n            [\n              -107.0562744140625,\n              41.611335399441735\n            ],\n            [\n              -106.3421630859375,\n              41.693424216151314\n            ],\n            [\n              -106.226806640625,\n              42.99259451971113\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"39","issue":"4","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-11-13","publicationStatus":"PW","scienceBaseUri":"56865fc8e4b0e7594ee74ccf","contributors":{"authors":[{"text":"Fedy, Bradley C.","contributorId":64080,"corporation":false,"usgs":true,"family":"Fedy","given":"Bradley","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":583891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Donnell, Michael S. 0000-0002-3488-003X odonnellm@usgs.gov","orcid":"https://orcid.org/0000-0002-3488-003X","contributorId":140876,"corporation":false,"usgs":true,"family":"O’Donnell","given":"Michael","email":"odonnellm@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":583890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowen, Zachary H. 0000-0002-8656-1831 bowenz@usgs.gov","orcid":"https://orcid.org/0000-0002-8656-1831","contributorId":821,"corporation":false,"usgs":true,"family":"Bowen","given":"Zachary","email":"bowenz@usgs.gov","middleInitial":"H.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":583892,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70161742,"text":"70161742 - 2015 - Predicting spatial distribution of postfire debris flows and potential consequences for native trout in headwater streams","interactions":[],"lastModifiedDate":"2016-01-05T16:39:19","indexId":"70161742","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1699,"text":"Freshwater Science","active":true,"publicationSubtype":{"id":10}},"title":"Predicting spatial distribution of postfire debris flows and potential consequences for native trout in headwater streams","docAbstract":"<p>Habitat fragmentation and degradation and invasion of nonnative species have restricted the distribution of native trout. Many trout populations are limited to headwater streams where negative effects of predicted climate change, including reduced stream flow and increased risk of catastrophic fires, may further jeopardize their persistence. Headwater streams in steep terrain are especially susceptible to disturbance associated with postfire debris flows, which have led to local extirpation of trout populations in some systems. We conducted a reach-scale spatial analysis of debris-flow risk among 11 high-elevation watersheds of the Colorado Rocky Mountains occupied by isolated populations of Colorado River Cutthroat Trout (Oncorhynchus clarkii pleuriticus). Stream reaches at high risk of disturbance by postfire debris flow were identified with the aid of a qualitative model based on 4 primary initiating and transport factors (hillslope gradient, flow accumulation pathways, channel gradient, and valley confinement). This model was coupled with a spatially continuous survey of trout distributions in these stream networks to assess the predicted extent of trout population disturbances related to debris flows. In the study systems, debris-flow potential was highest in the lower and middle reaches of most watersheds. Colorado River Cutthroat Trout occurred in areas of high postfire debris-flow risk, but they were never restricted to those areas. Postfire debris flows could extirpate trout from local reaches in these watersheds, but trout populations occupy refugia that should allow recolonization of interconnected, downstream reaches. Specific results of our study may not be universally applicable, but our risk assessment approach can be applied to assess postfire debris-flow risk for stream reaches in other watersheds.</p>","language":"English","publisher":"JSTOR","doi":"10.1086/684094","usgsCitation":"Sedell, E.R., Gresswell, R.E., and McMahon, T., 2015, Predicting spatial distribution of postfire debris flows and potential consequences for native trout in headwater streams: Freshwater Science, v. 34, no. 4, p. 1558-1570, https://doi.org/10.1086/684094.","productDescription":"13 p.","startPage":"1558","endPage":"1570","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-060323","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":471600,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1086/684094","text":"External Repository"},{"id":313872,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313823,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org.proxybz.lib.montana.edu/stable/10.1086/684094?seq=1#page_scan_tab_contents"}],"country":"United States","state":"Colorado","otherGeospatial":"Upper Colorado River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.89971923828124,\n              39.82752244475985\n            ],\n            [\n              -107.7978515625,\n              39.768436410838426\n            ],\n            [\n              -107.9681396484375,\n              39.57605638518604\n            ],\n            [\n              -108.11370849609375,\n              39.189690821096804\n            ],\n            [\n              -107.9296875,\n              39.10022600175344\n            ],\n            [\n              -107.435302734375,\n              38.98076276501633\n            ],\n            [\n              -106.95465087890625,\n              39.191819549771694\n            ],\n            [\n              -106.74041748046875,\n              39.459523110465156\n            ],\n            [\n              -106.76239013671875,\n              39.812755695478124\n            ],\n            [\n              -106.89971923828124,\n              39.82752244475985\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"4","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf748e4b0e7a44bc0f17f","contributors":{"authors":[{"text":"Sedell, Edwin R","contributorId":152039,"corporation":false,"usgs":false,"family":"Sedell","given":"Edwin","email":"","middleInitial":"R","affiliations":[{"id":18862,"text":"Oregon Department of Fish and Wildlife, La Grand Fish Research, La Grand, OR, USA 97850","active":true,"usgs":false}],"preferred":false,"id":587622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gresswell, Robert E. 0000-0003-0063-855X bgresswell@usgs.gov","orcid":"https://orcid.org/0000-0003-0063-855X","contributorId":152031,"corporation":false,"usgs":true,"family":"Gresswell","given":"Robert","email":"bgresswell@usgs.gov","middleInitial":"E.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":587621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McMahon, Thomas E.","contributorId":93548,"corporation":false,"usgs":true,"family":"McMahon","given":"Thomas E.","affiliations":[],"preferred":false,"id":587623,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70161741,"text":"70161741 - 2015 - Fire effects on aquatic ecosystems: An assessment of the current state of the science","interactions":[],"lastModifiedDate":"2025-06-25T13:19:04.034953","indexId":"70161741","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1699,"text":"Freshwater Science","active":true,"publicationSubtype":{"id":10}},"title":"Fire effects on aquatic ecosystems: An assessment of the current state of the science","docAbstract":"<p><span>Fire is a prevalent feature of many landscapes and has numerous and complex effects on geological, hydrological, ecological, and economic systems. In some regions, the frequency and intensity of wildfire have increased in recent years and are projected to escalate with predicted climatic and landuse changes. In addition, prescribed burns continue to be used in many parts of the world to clear vegetation for development projects, encourage desired vegetation, and reduce fuel loads. Given the prevalence of fire on the landscape, authors of papers in this special series examine the complexities of fire as a disturbance shaping freshwater ecosystems and highlight the state of the science. These papers cover key aspects of fire effects that range from vegetation loss and recovery in watersheds to effects on hydrology and water quality with consequences for communities (from algae to fish), food webs, and ecosystem processes (e.g., organic matter subsidies, nutrient cycling) across a range of scales. The results presented in this special series of articles expand our knowledge of fire effects in different biomes, water bodies, and geographic regions, encompassing aquatic population, community, and ecosystem responses. In this overview, we summarize each paper and emphasize its contributions to knowledge on fire ecology and freshwater ecosystems. This overview concludes with a list of 7 research foci that are needed to further our knowledge of fire effects on aquatic ecosystems, including research on: 1) additional biomes and geographic regions; 2) additional habitats, including wetlands and lacustrine ecosystems; 3) different fire severities, sizes, and spatial configurations; and 4) additional response variables (e.g., ecosystem processes) 5) over long (&gt;5 y) time scales 6) with more rigorous study designs and data analyses, and 7) consideration of the effects of fire management practices and policies on aquatic ecosystems.</span></p>","language":"English","publisher":"University of Chicago Press","doi":"10.1086/684073","usgsCitation":"Bixby, R.J., Cooper, S., Gresswell, R.E., Brown, L.E., Dahm, C.N., and Dwire, K.A., 2015, Fire effects on aquatic ecosystems: An assessment of the current state of the science: Freshwater Science, v. 34, no. 4, p. 1340-1350, https://doi.org/10.1086/684073.","productDescription":"11 p.","startPage":"1340","endPage":"1350","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-068454","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":471611,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://escholarship.org/uc/item/5q9165nf","text":"External Repository"},{"id":381478,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"4","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf741e4b0e7a44bc0f156","contributors":{"authors":[{"text":"Bixby, Rebecca J.","contributorId":147389,"corporation":false,"usgs":false,"family":"Bixby","given":"Rebecca","email":"","middleInitial":"J.","affiliations":[{"id":16834,"text":"Dept. of Biology and Museum of Southwestern Biology, Univ of NM","active":true,"usgs":false}],"preferred":false,"id":807071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Scott D.","contributorId":152035,"corporation":false,"usgs":false,"family":"Cooper","given":"Scott D.","affiliations":[{"id":18860,"text":"Department of Ecology, Evolution, and Marine Biology and Marine Science Institute      University of California","active":true,"usgs":false}],"preferred":false,"id":807072,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gresswell, Robert E. 0000-0003-0063-855X bgresswell@usgs.gov","orcid":"https://orcid.org/0000-0003-0063-855X","contributorId":152031,"corporation":false,"usgs":true,"family":"Gresswell","given":"Robert","email":"bgresswell@usgs.gov","middleInitial":"E.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":587615,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brown, Lee E.","contributorId":152036,"corporation":false,"usgs":false,"family":"Brown","given":"Lee","email":"","middleInitial":"E.","affiliations":[{"id":18861,"text":"School of Geography, University of Leeds, Leeds, LS2 9JT, United Kingdom","active":true,"usgs":false}],"preferred":false,"id":807073,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dahm, Clifford N.","contributorId":152037,"corporation":false,"usgs":false,"family":"Dahm","given":"Clifford","email":"","middleInitial":"N.","affiliations":[{"id":7000,"text":"Department of Biology, University of New Mexico","active":true,"usgs":false}],"preferred":false,"id":587619,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dwire, Kathleen A.","contributorId":225615,"corporation":false,"usgs":false,"family":"Dwire","given":"Kathleen","email":"","middleInitial":"A.","affiliations":[{"id":41171,"text":"US Forest Service, Rocky Mountain Research Station, Fort Collins, CO","active":true,"usgs":false}],"preferred":false,"id":807075,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70158953,"text":"70158953 - 2015 - Aniakchak National Monument and Preserve: Geologic resources inventory report","interactions":[],"lastModifiedDate":"2017-04-13T10:56:23","indexId":"70158953","displayToPublicDate":"2015-12-01T00:00:00","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/NRSS/GRD/NRR—2015/1033","title":"Aniakchak National Monument and Preserve: Geologic resources inventory report","docAbstract":"<p><span>This GRI report is a companion document to previously completed GRI digital geologic map data. It was written for resource managers to support science-informed decision making. It may also be useful for interpretation. The report was prepared using available geologic information, and the NPS Geologic Resources Division conducted no new fieldwork in association with its preparation. Sections of the report discuss distinctive geologic features and processes within the park, highlight geologic issues facing resource managers, describe the geologic history leading to the present-day landscape, and provide information about the GRI geologic map data. A poster illustrates these data. The Map Unit Properties Table summarizes report content for each geologic map unit.</span></p>","language":"English","publisher":"National Park Service","publisherLocation":"Fort Collins, CO","usgsCitation":"Hults, C.P., and Neal, C.A., 2015, Aniakchak National Monument and Preserve: Geologic resources inventory report: Natural Resource Report NPS/NRSS/GRD/NRR—2015/1033, xii, 82 p.","productDescription":"xii, 82 p.","numberOfPages":"109","ipdsId":"IP-063183","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":339674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":309785,"type":{"id":15,"text":"Index Page"},"url":"https://www.nature.nps.gov/geology/inventory/publications/s_summaries/ALAG-ANIA-KATM-KEFJ-LACL_scoping_summary_20051031.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Aniakchak National Monument and Preserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -158.34457397460938,\n              56.66603819878973\n            ],\n            [\n              -157.61260986328125,\n              56.66603819878973\n            ],\n            [\n              -157.61260986328125,\n              57.10567321405914\n            ],\n            [\n              -158.34457397460938,\n              57.10567321405914\n            ],\n            [\n              -158.34457397460938,\n              56.66603819878973\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58f08e61e4b06911a29fa856","contributors":{"authors":[{"text":"Hults, Chad P. chults@usgs.gov","contributorId":1930,"corporation":false,"usgs":true,"family":"Hults","given":"Chad","email":"chults@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":false,"id":690851,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neal, Christina A. 0000-0002-7697-7825 tneal@usgs.gov","orcid":"https://orcid.org/0000-0002-7697-7825","contributorId":131135,"corporation":false,"usgs":true,"family":"Neal","given":"Christina","email":"tneal@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":577033,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70159597,"text":"70159597 - 2015 - Estimating the risks for adverse effects of total phosphorus in receiving streams with the Stochastic Empirical Loading and Dilution Model (SELDM)","interactions":[],"lastModifiedDate":"2019-02-21T15:33:24","indexId":"70159597","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Estimating the risks for adverse effects of total phosphorus in receiving streams with the Stochastic Empirical Loading and Dilution Model (SELDM)","docAbstract":"<p>Studies from North Carolina (NC) indicate that increasing concentrations of total phosphorus (TP) and other constituents are correlated to adverse effects on stream ecosystems as evidenced by differences in benthic macroinvertebrate populations in streams across the state. As a result, stringent in-stream criteria based on the Water Quality Assessed by Benthic macroinvertebrate health ratings (WQABI) have been proposed for regulating TP concentrations in stormwater discharges and for selecting stormwater best management practices (BMPs). The WQABI criteria concentrations may not be suitable for evaluating stormwater discharges because they are based on baseflow concentration statistics, the criteria do not include a clearly defined allowable exceedance frequency, and there are substantial uncertainties in estimating the quality of runoff, BMP discharge, and receiving waters for sites without monitoring data.</p>\n<p>The Stochastic Empirical Loading and Dilution Model (SELDM), which was developed by the U.S. Geological Survey in cooperation with the Federal Highway Administration, was used to simulate the quality of runoff, BMP discharge, and receiving waters to evaluate risks for water-quality exceedances with different criteria concentrations, allowable exceedance frequencies, and selected water-quality statistics. Water-quality data from two neighboring basins in the Piedmont ecoregion in NC were used to simulate in-stream stormwater quality. Data collected at 15 sites in NC were used to simulate runoff quality. Statistics for stochastic modeling of volume reduction, hydrograph extension, and water-quality treatment by BMPs, were used to simulate potential effect of these treatments on discharge quality and downstream stormwater quality. Results of these long-term 30-year simulations were used to evaluate criteria concentrations, the potential frequency of water-quality exceedances, and the effect of data selection on risks for water-quality exceedances.</p>\n<p>The simulations indicate that the potential frequency for exceeding instream and stormwater discharge criteria depend on the detailed definition of the criteria and the data that are selected for simulating water quality. Data and simulation results indicate that the baseflow concentrations do not represent stormwater concentrations, even in predominantly forested basins. There is substantial uncertainty in applying stormwater statistics to unmonitored sites, even if these statistics are applied to neighboring basins such as in this example. Over a period of several years (or more) it would be impossible to meet many of the proposed instream and stormwater discharge quality criteria unless these criteria include an allowable exceedance frequency because stormwater concentrations commonly vary by orders of magnitude. Selection of BMPs by using concentration reduction as the sole criteria may underestimate potential benefits of BMPs that also provide volume reduction, which reduces discharge loads, and hydrograph extension, which increases the dilution of runoff into a larger proportion of the upstream stormflow.</p>\n<p>Results of this study indicate the potential benefits of the multi-decade simulations that SELDM provides because these simulations quantify risks and uncertainties that affect decisions made with available data and statistics. Results of the SELDM simulations indicate that the WQABI criteria concentrations may be too stringent for evaluating the stormwater quality in receiving streams, highway runoff, and BMP discharges; especially with the substantial uncertainties inherent in selecting representative data.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 2015 International Conference on Ecology and Transportation (ICOET 2015)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2015 International conference on ecology and transportation","conferenceDate":"September 20, 2015","conferenceLocation":"Raleigh, NC","language":"English","publisher":"Center for Transportation and the Environment","usgsCitation":"Granato, G.E., and Jones, S.C., 2015, Estimating the risks for adverse effects of total phosphorus in receiving streams with the Stochastic Empirical Loading and Dilution Model (SELDM), <i>in</i> Proceedings of the 2015 International Conference on Ecology and Transportation (ICOET 2015), Raleigh, NC, September 20, 2015, p. 1-19.","productDescription":"19 p.","startPage":"1","endPage":"19","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-065909","costCenters":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"links":[{"id":311831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"566175cae4b06a3ea36c56a5","contributors":{"authors":[{"text":"Granato, Gregory E. 0000-0002-2561-9913 ggranato@usgs.gov","orcid":"https://orcid.org/0000-0002-2561-9913","contributorId":147346,"corporation":false,"usgs":true,"family":"Granato","given":"Gregory","email":"ggranato@usgs.gov","middleInitial":"E.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":false,"id":579637,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Susan C. 0000-0002-5891-5209","orcid":"https://orcid.org/0000-0002-5891-5209","contributorId":64716,"corporation":false,"usgs":false,"family":"Jones","given":"Susan","email":"","middleInitial":"C.","affiliations":[{"id":34302,"text":"Federal Highway Administration (United States)","active":true,"usgs":false}],"preferred":false,"id":579638,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70159962,"text":"70159962 - 2015 - Categorisation of northern California rainfall for periods with and without a radar brightband using stable isotopes and a novel automated precipitation collector","interactions":[],"lastModifiedDate":"2015-12-04T15:46:35","indexId":"70159962","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3527,"text":"Tellus, Series A: Dynamic Meteorology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Categorisation of northern California rainfall for periods with and without a radar brightband using stable isotopes and a novel automated precipitation collector","docAbstract":"<p><span>During landfall of extratropical cyclones between 2005 and 2011, nearly 1400 precipitation samples were collected at intervals of 30-min time resolution with novel automated collectors at four NOAA sites in northern California [Alta (ATA), Bodega Bay (BBY), Cazadero (CZD) and Shasta Dam (STD)] during 43 events. Substantial decreases were commonly followed hours later by substantial increases in hydrogen isotopic composition (</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;where VSMOW is Vienna Standard Mean Ocean Water) and oxygen isotopic composition (</span><i>&delta;</i><sup>18</sup><span>O</span><sub>VSMOW</sub><span>) of precipitation. These variations likely occur as pre-cold frontal precipitation generation transitions from marine vapour masses having low rainout to cold cloud layers having much higher rainout (with concomitant brightband signatures measured by an S-band profiling radar and lower&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;values of precipitation), and finally to shallower, warmer precipitating clouds having lower rainout (with non-brightband signatures and higher&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;values of precipitation), in accord with &lsquo;seeder&ndash;feeder&rsquo; precipitation. Of 82 intervals identified, a remarkable 100.5 &permil; decrease in&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;value was observed for a 21 January 2010 event at BBY. Of the 61 intervals identified with increases in&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;values as precipitation transitioned to shallower, warmer clouds having substantially less rainout (the feeder part of the seeder&ndash;feeder mechanism), a remarkable increase in&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;value of precipitation of 82.3 &permil; was observed for a 10 February 2007 event at CZD. All CZD and ATA events having&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;values of precipitation below &minus;105 &permil; were atmospheric rivers (ARs), and of the 13 events having&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>values of precipitation below &minus;80 &permil;, 77 % were ARs. Cloud echo-top heights (a proxy for atmospheric temperature) were available for 23 events. The mean echo-top height is greater for higher rainout periods than that for lower rainout periods in 22 of the 23 events. The lowest&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;of precipitation of 28 CZD events was &minus;137.9 &permil; on 16 February 2009 during an AR with cold precipitating clouds and very high rainout with tops &gt;6.5 km altitude. An altitude effect of &minus;2.5 &permil; per 100 m was measured from BBY and CZD&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;data and of &minus;1.8 &permil; per 100 m for CZD and ATA&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;data. We present a new approach to categorise rainfall intervals using&nbsp;</span><i>&delta;</i><sup>2</sup><span>H</span><sub>VSMOW</sub><span>&nbsp;values of precipitation and rainfall rates. We term this approach the algorithmic-isotopic categorisation of rainfall, and we were able to identify higher rainout and/or lower rainout periods during all events in this study. We conclude that algorithmic-isotopic categorisation of rainfall can enable users to distinguish between tropospheric vapour masses having relatively high rainout (typically with brightband rain and that commonly are ARs) and vapour masses having lower rainout (commonly with non-brightband rain).</span></p>","language":"English","publisher":"International Meteorological Institute","publisherLocation":"Stockholm, Sweden","doi":"10.3402/tellusb.v67.28574","usgsCitation":"Coplen, T.B., Paul J. Neiman, Allen B. White, and Ralph, F.M., 2015, Categorisation of northern California rainfall for periods with and without a radar brightband using stable isotopes and a novel automated precipitation collector: Tellus, Series A: Dynamic Meteorology and Oceanography, v. 67, p. 1-48, https://doi.org/10.3402/tellusb.v67.28574.","productDescription":"48 p.","startPage":"1","endPage":"48","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-069509","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":471616,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3402/tellusb.v67.28574","text":"Publisher Index Page"},{"id":311949,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311948,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.3402/tellusb.v67.28574"}],"country":"United States","state":"California","otherGeospatial":"Northern California: Bodega Bay, Cazadero, Alta and Shasta Dam","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.05837631225586,\n              38.33600115904974\n            ],\n            [\n              -123.04987907409668,\n              38.33566453597907\n            ],\n            [\n              -123.03897857666014,\n              38.32825843276099\n            ],\n            [\n              -123.03091049194336,\n              38.316339750609366\n            ],\n            [\n              -123.03245544433592,\n              38.31283784445829\n            ],\n            [\n              -123.05322647094727,\n              38.29936739855925\n            ],\n            [\n              -123.05940628051756,\n              38.2978854967878\n            ],\n       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,{"id":70160353,"text":"70160353 - 2015 - Strong-motion observations of the M 7.8 Gorkha, Nepal, earthquake sequence and development of the N-shake strong-motion network","interactions":[],"lastModifiedDate":"2018-10-24T16:48:39","indexId":"70160353","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Strong-motion observations of the M 7.8 Gorkha, Nepal, earthquake sequence and development of the N-shake strong-motion network","docAbstract":"<p>We present and describe strong-motion data observations from the 2015 M 7.8 Gorkha, Nepal, earthquake sequence collected using existing and new Quake-Catcher Network (QCN) and U.S. Geological Survey NetQuakes sensors located in the Kathmandu Valley. A comparison of QCN data with waveforms recorded by a conventional strong-motion (NetQuakes) instrument validates the QCN data. We present preliminary analysis of spectral accelerations, and peak ground acceleration and velocity for earthquakes up to M 7.3 from the QCN stations, as well as preliminary analysis of the mainshock recording from the NetQuakes station. We show that mainshock peak accelerations were lower than expected and conclude the Kathmandu Valley experienced a pervasively nonlinear response during the mainshock. Phase picks from the QCN and NetQuakes data are also used to improve aftershock locations. This study confirms the utility of QCN instruments to contribute to ground-motion investigations and aftershock response in regions where conventional instrumentation and open-access seismic data are limited. Initial pilot installations of QCN instruments in 2014 are now being expanded to create the Nepal&ndash;Shaking Hazard Assessment for Kathmandu and its Environment (N-SHAKE) network.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0220150146","usgsCitation":"Dixit, A., Ringler, A.T., Sumy, D.F., Cochran, E.S., Hough, S.E., Martin, S., Gibbons, S., Luetgert, J.H., Galetzka, J., Shrestha, S., Rajaure, S., and McNamara, D.E., 2015, Strong-motion observations of the M 7.8 Gorkha, Nepal, earthquake sequence and development of the N-shake strong-motion network: Seismological Research Letters, v. 86, no. 6, p. 1533-1539, https://doi.org/10.1785/0220150146.","productDescription":"7 p.","startPage":"1533","endPage":"1539","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-066938","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":471599,"rank":0,"type":{"id":41,"text":"Open Access External 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,{"id":70160135,"text":"70160135 - 2015 - Natural and unnatural oil slicks in the Gulf of Mexico","interactions":[],"lastModifiedDate":"2016-02-01T13:31:39","indexId":"70160135","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2315,"text":"Journal of Geophysical Research C: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Natural and unnatural oil slicks in the Gulf of Mexico","docAbstract":"<p><span>When wind speeds are 2 &ndash; 10 m s</span><span>&minus;1</span><span>, reflective contrasts in the ocean surface make oil slicks visible to synthetic aperture radar (SAR) under all sky conditions. Neural network analysis of satellite SAR images quantified the magnitude and distribution of surface oil in the Gulf of Mexico from persistent, natural seeps and from the Deepwater Horizon (DWH) discharge. This analysis identified 914 natural oil seep zones across the entire Gulf of Mexico in pre-2010 data. Their &sim;0.1 &micro;m slicks covered an aggregated average of 775 km</span><span>2</span><span>. Assuming an average volume of 77.5 m</span><span>3</span><span>over an 8 &ndash; 24 h lifespan per oil slick, the floating oil indicates a surface flux of 2.5 &ndash; 9.4 &times; 10</span><span>4</span><span>&nbsp;m</span><span>3</span><span>&nbsp;y</span><span>&minus;1</span><span>. Oil from natural slicks was regionally concentrated: 68%, 25%, 7%, and &lt;1% of the total was observed in the NW, SW, NE and SE Gulf, respectively. This reflects differences in basin history and hydrocarbon generation. SAR images from 2010 showed that the 87-day DWH discharge produced a surface-oil footprint fundamentally different from background seepage, with an average ocean area of 11,200 km</span><span>2</span><span>&nbsp;(SD 5,028) and a volume of 22,600 m</span><span>3</span><span>&nbsp;(SD 5,411). Peak magnitudes of oil were detected during equivalent, &sim;14-day intervals around 23 May and 18 June, when wind speeds remained &lt;5 m s</span><span>&minus;1</span><span>. Over this interval, aggregated volume of floating oil decreased by 21%; area covered increased by 49% (</span><i>p</i><span>&thinsp;&lt;&thinsp;.1), potentially altering its ecological impact. The most likely causes were increased applications of dispersant and surface burning operations.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/2015JC011062","collaboration":"Florida State University, Woods Hole Oceanographic Institution, NOAA, RPS ASA, Univ. of Southern Florida, Bubbleology Research International, Stratus Consulting","usgsCitation":"MacDonald, I.R., O. Garcia-Pineda, Beet, A., Asl, S.D., Feng, L., Graettinger, D.G., French-McCay, D., Holmes, J., C. Hu, F. Huffer, I. Leifer, Mueller-Karger, F., Solow, A., Silva, M., and Swayze, G.A., 2015, Natural and unnatural oil slicks in the Gulf of Mexico: Journal of Geophysical Research C: Oceans, v. 120, no. 12, p. 8364-8380, https://doi.org/10.1002/2015JC011062.","productDescription":"15 p.","startPage":"8364","endPage":"8380","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-063451","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":471615,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2015jc011062","text":"Publisher Index Page"},{"id":312210,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gulf of Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.650390625,\n              24.647017162630366\n            ],\n            [\n              -85.0341796875,\n              22.471954507739227\n            ],\n            [\n              -87.4951171875,\n              21.69826549685252\n            ],\n            [\n              -90,\n              21.493963563064455\n            ],\n            [\n              -90.791015625,\n              20.756113874762082\n            ],\n            [\n              -90.703125,\n              19.766703551716976\n            ],\n            [\n              -91.845703125,\n              18.812717856407776\n            ],\n            [\n              -94.52636718749999,\n              18.35452552912664\n            ],\n            [\n              -96.85546875,\n              20.673905264672843\n            ],\n            [\n              -97.8662109375,\n              22.87744046489713\n            ],\n            [\n              -97.3388671875,\n              25.958044673317843\n            ],\n            [\n              -97.2509765625,\n              27.449790329784214\n            ],\n            [\n              -96.0205078125,\n              28.729130483430154\n            ],\n            [\n              -94.04296874999999,\n              29.611670115197377\n            ],\n            [\n              -91.7138671875,\n              29.611670115197377\n            ],\n            [\n              -89.47265625,\n              28.8831596093235\n            ],\n            [\n              -88.76953125,\n              29.113775395114416\n            ],\n            [\n              -89.2529296875,\n              29.76437737516313\n            ],\n            [\n              -89.07714843749999,\n              30.031055426540206\n            ],\n            [\n              -88.6376953125,\n              30.372875188118016\n            ],\n            [\n              -86.8798828125,\n              30.221101852485987\n            ],\n            [\n              -84.814453125,\n              29.6880527498568\n            ],\n            [\n              -83.84765625,\n              29.76437737516313\n            ],\n            [\n              -83.0126953125,\n              28.536274512989916\n            ],\n            [\n              -82.4853515625,\n              27.0982539061379\n            ],\n            [\n              -81.474609375,\n              25.363882272740256\n            ],\n            [\n              -80.85937499999999,\n              25.045792240303445\n            ],\n            [\n              -81.650390625,\n              24.647017162630366\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"120","issue":"12","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-12-28","publicationStatus":"PW","scienceBaseUri":"566c01ece4b09cfe53ca5af4","contributors":{"authors":[{"text":"MacDonald, Ian R.","contributorId":150517,"corporation":false,"usgs":false,"family":"MacDonald","given":"Ian","email":"","middleInitial":"R.","affiliations":[{"id":7092,"text":"Florida State University","active":true,"usgs":false}],"preferred":false,"id":582005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O. 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Daneshgar","contributorId":150520,"corporation":false,"usgs":false,"family":"Asl","given":"S.","email":"","middleInitial":"Daneshgar","affiliations":[{"id":7092,"text":"Florida State University","active":true,"usgs":false}],"preferred":false,"id":582008,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Feng, L.","contributorId":150528,"corporation":false,"usgs":false,"family":"Feng","given":"L.","email":"","affiliations":[{"id":7163,"text":"University of South Florida","active":true,"usgs":false}],"preferred":false,"id":582016,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Graettinger, D. G.","contributorId":150521,"corporation":false,"usgs":false,"family":"Graettinger","given":"D.","email":"","middleInitial":"G.","affiliations":[{"id":18042,"text":"NOAA OR&R","active":true,"usgs":false}],"preferred":false,"id":582009,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"French-McCay, D.","contributorId":150522,"corporation":false,"usgs":false,"family":"French-McCay","given":"D.","email":"","affiliations":[{"id":18043,"text":"RSP ASA","active":true,"usgs":false}],"preferred":false,"id":582010,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Holmes, J.","contributorId":150529,"corporation":false,"usgs":false,"family":"Holmes","given":"J.","email":"","affiliations":[{"id":18045,"text":"Stratus Consulting Inc.","active":true,"usgs":false}],"preferred":false,"id":582017,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"C. Hu","contributorId":150523,"corporation":false,"usgs":false,"family":"C. Hu","affiliations":[{"id":7163,"text":"University of South Florida","active":true,"usgs":false}],"preferred":false,"id":582011,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"F. Huffer","contributorId":150524,"corporation":false,"usgs":false,"family":"F. Huffer","affiliations":[{"id":7092,"text":"Florida State University","active":true,"usgs":false}],"preferred":false,"id":582012,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"I. Leifer","contributorId":150525,"corporation":false,"usgs":false,"family":"I. Leifer","affiliations":[{"id":18044,"text":"Bubbleology Research International","active":true,"usgs":false}],"preferred":false,"id":582013,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Mueller-Karger, F.","contributorId":150526,"corporation":false,"usgs":false,"family":"Mueller-Karger","given":"F.","email":"","affiliations":[{"id":7163,"text":"University of South Florida","active":true,"usgs":false}],"preferred":false,"id":582014,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Solow, A.","contributorId":150527,"corporation":false,"usgs":false,"family":"Solow","given":"A.","email":"","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":582015,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Silva, M.","contributorId":150530,"corporation":false,"usgs":false,"family":"Silva","given":"M.","email":"","affiliations":[{"id":7092,"text":"Florida State University","active":true,"usgs":false}],"preferred":false,"id":582018,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Swayze, Gregg A. 0000-0002-1814-7823 gswayze@usgs.gov","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":518,"corporation":false,"usgs":true,"family":"Swayze","given":"Gregg","email":"gswayze@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":582004,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70148335,"text":"70148335 - 2015 - Shoal basses: A clade of cryptic identity","interactions":[],"lastModifiedDate":"2016-12-06T13:11:22","indexId":"70148335","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Shoal basses: A clade of cryptic identity","docAbstract":"Shoal basses are a cryptic clade composed of Micropterus spp. restricted to\nthe Apalachicola River system and three southeastern Atlantic slope river drainages in the southeastern United States. This reciprocally monophyletic clade includes the Shoal Bass M. cataractae (endemic to the Apalachicola River system), the Chattahoochee Bass M. chattahoochae, and two undescribed forms from the Altamaha, Ogeechee, and Savannah River drainages. Members of the shoal bass clade can be distinguished from all other species of Micropterus basses using 20 diagnostic characters (characteristic attributes) found in mitochondrial DNA (NADH dehydrogenase subunit 2) gene sequences. Each member of the clade\nadditionally possesses unique characteristic attributes, which along with morphological and meristic characters can be used to diagnose this cryptic biodiversity. Biologists and managers have previously regarded the shoal basses in the Chattahoochee, Savannah, Altamaha and Ogeechee River systems as belonging to a single taxon synonymous with the Redeye Bass\nM. coosae, which is endemic to the Mobile River drainage. With these and previous analyses (including description of the Shoal Bass), we now recognize that what was once considered a single taxon actually comprises seven species, each of which is endemic to a single southeastern drainage. Recognizing and documenting the actual diversity of Micropterus spp. provides important information for managers who may wish to avoid stocking or translocations that could compromise the genetic integrity of native bass populations. Introductions of nonnative basses, including Alabama Bass M. henshalli, Spotted Bass M. punctulatus, and Smallmouth\nBass M. dolomieu currently threaten the integrity of native shoal bass species in streams of the Chattahoochee, Altamaha, Ogeechee, and Savannah River systems.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Black bass diversity: Multidisciplinary science for conservation","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Fisheries Society","isbn":"978-1-934874-40-0","usgsCitation":"Freeman, B.J., Taylor, A.T., Oswald, K.J., Wares, J., Freeman, M., Quattro, J.M., and Leitner, J., 2015, Shoal basses: A clade of cryptic identity, <i>in</i> Black bass diversity: Multidisciplinary science for conservation, p. 449-466.","productDescription":"18 p.","startPage":"449","endPage":"466","ipdsId":"IP-061653","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":331569,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":300825,"type":{"id":15,"text":"Index Page"},"url":"https://fisheries.org/shop/54082c"}],"publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5847dc7de4b06d80b7af6ab3","contributors":{"authors":[{"text":"Freeman, Byron J.","contributorId":49782,"corporation":false,"usgs":false,"family":"Freeman","given":"Byron","email":"","middleInitial":"J.","affiliations":[{"id":12697,"text":"University of Georgia","active":true,"usgs":false}],"preferred":false,"id":654972,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Andrew T.","contributorId":177197,"corporation":false,"usgs":false,"family":"Taylor","given":"Andrew","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":654973,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oswald, Kenneth J.","contributorId":177198,"corporation":false,"usgs":false,"family":"Oswald","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":654974,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wares, John","contributorId":177199,"corporation":false,"usgs":false,"family":"Wares","given":"John","affiliations":[],"preferred":false,"id":654975,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Freeman, Mary 0000-0001-7615-6923 mcfreeman@usgs.gov","orcid":"https://orcid.org/0000-0001-7615-6923","contributorId":3528,"corporation":false,"usgs":true,"family":"Freeman","given":"Mary","email":"mcfreeman@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":547700,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Quattro, Joseph M.","contributorId":177200,"corporation":false,"usgs":false,"family":"Quattro","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":654976,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leitner, Jean","contributorId":177201,"corporation":false,"usgs":false,"family":"Leitner","given":"Jean","email":"","affiliations":[],"preferred":false,"id":654977,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70192077,"text":"70192077 - 2015 - The nest-concealment hypothesis: New insights from a comparative analysis","interactions":[],"lastModifiedDate":"2017-10-26T13:50:36","indexId":"70192077","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3784,"text":"Wilson Journal of Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"The nest-concealment hypothesis: New insights from a comparative analysis","docAbstract":"<p><span>Selection of a breeding site is critical for many animals, especially for birds whose offspring are stationary during development. Thus, birds are often assumed to prefer concealed nest sites. However, 74% of studies (</span><i>n</i><span><span>&nbsp;</span>= 106) that have evaluated this relationship for open-cup nesting songbirds in North America failed to support the nest-concealment hypothesis. We conducted a comparative analysis to identify factors that contribute to variation in the ability of researchers to find support for the nest-concealment hypothesis. We found that some of the discrepancy among studies can be explained by interspecific differences in morphological and extrinsic factors that affect nest predation. Moreover, methods that investigators used to estimate concealment affected whether studies found support for the nest-concealment hypothesis; 33% of the studies that used quantitative estimates found support for the nest-concealment hypothesis whereas only 10% of the studies that used qualitative estimates found support. The timing of measurements also explained some of the ambiguity; studies that provided little information regarding the timing of their foliage density estimates were less likely to support the nest-concealment hypothesis. Species with more conspicuous male plumage were less likely to support the nest-concealment hypothesis when we analyzed studies that used visual estimates. Whereas species with more conspicuous female plumage were more likely to support the nest-concealment hypothesis when we analyzed studies that used quantitative measures. Our results demonstrate that support for the nest-concealment hypothesis has been equivocal, but that some of the ambiguity can be explained by morphological traits and methods used to measure concealment.</span></p>","language":"English","publisher":"The Wilson Ornithological Society","doi":"10.1676/14-162.1","usgsCitation":"Borgmann, K.L., and Conway, C.J., 2015, The nest-concealment hypothesis: New insights from a comparative analysis: Wilson Journal of Ornithology, v. 127, no. 4, p. 646-660, https://doi.org/10.1676/14-162.1.","productDescription":"15 p.","startPage":"646","endPage":"660","ipdsId":"IP-056235","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":347480,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"127","issue":"4","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a07eb2ae4b09af898c8ccc2","contributors":{"authors":[{"text":"Borgmann, Kathi L.","contributorId":171647,"corporation":false,"usgs":false,"family":"Borgmann","given":"Kathi","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":716418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conway, Courtney J. 0000-0003-0492-2953 cconway@usgs.gov","orcid":"https://orcid.org/0000-0003-0492-2953","contributorId":2951,"corporation":false,"usgs":true,"family":"Conway","given":"Courtney","email":"cconway@usgs.gov","middleInitial":"J.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":714091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189524,"text":"70189524 - 2015 - Long-term anoxia and release of ancient, labile carbon upon thaw of Pleistocene permafrost","interactions":[],"lastModifiedDate":"2017-07-14T12:19:21","indexId":"70189524","displayToPublicDate":"2015-12-01T00:00:00","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":"Long-term anoxia and release of ancient, labile carbon upon thaw of Pleistocene permafrost","docAbstract":"<p><span>The fate of permafrost carbon upon thaw will drive feedbacks to climate warming. Here we consider the character and context of dissolved organic carbon (DOC) in yedoma permafrost cores from up to 20 m depth in central Alaska. We observed high DOC concentrations (4 to 129 mM) and consistent low molecular weight organic acid concentrations in three cores. We estimate a DOC production rate of 12 µmol DOC m</span><sup>−2</sup><span> yr</span><sup>−1</sup><span><span>&nbsp;</span>based on model ages of up to ~200 kyr derived from uranium isotopes. Acetate C accounted for 24 ± 1% of DOC in all samples. This proportion suggests long-term anaerobiosis and is likely to influence thaw outcomes due to biolability of acetate upon release in many environments. The combination of uranium isotopes, ammonium concentrations, and calcium concentrations explained 86% of the variation in thaw water DOC concentrations, suggesting that DOC production may be related to both reducing conditions and mineral dissolution over time.</span></p>","language":"English","publisher":"AGU","doi":"10.1002/2015GL066296","usgsCitation":"Ewing, S.A., O’Donnell, J.A., Aiken, G.R., Butler, K.D., Butman, D., Windham-Myers, L., and Kanevskiy, M., 2015, Long-term anoxia and release of ancient, labile carbon upon thaw of Pleistocene permafrost: Geophysical Research Letters, v. 42, no. 24, p. 10730-10738, https://doi.org/10.1002/2015GL066296.","productDescription":"9 p.","startPage":"10730","endPage":"10738","ipdsId":"IP-066085","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":471606,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2015gl066296","text":"Publisher Index Page"},{"id":343868,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"24","noUsgsAuthors":false,"publicationDate":"2015-12-23","publicationStatus":"PW","scienceBaseUri":"5969d82ce4b0d1f9f060a195","contributors":{"authors":[{"text":"Ewing, Stephanie A.","contributorId":50065,"corporation":false,"usgs":true,"family":"Ewing","given":"Stephanie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":705028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Donnell, Jonathan A.","contributorId":84138,"corporation":false,"usgs":true,"family":"O’Donnell","given":"Jonathan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":705029,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aiken, George R. 0000-0001-8454-0984 graiken@usgs.gov","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":1322,"corporation":false,"usgs":true,"family":"Aiken","given":"George","email":"graiken@usgs.gov","middleInitial":"R.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":705030,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, Kenna D. 0000-0001-9604-4603 kebutler@usgs.gov","orcid":"https://orcid.org/0000-0001-9604-4603","contributorId":178885,"corporation":false,"usgs":true,"family":"Butler","given":"Kenna","email":"kebutler@usgs.gov","middleInitial":"D.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":705031,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Butman, David 0000-0003-3520-7426 dbutman@usgs.gov","orcid":"https://orcid.org/0000-0003-3520-7426","contributorId":174187,"corporation":false,"usgs":true,"family":"Butman","given":"David","email":"dbutman@usgs.gov","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":705032,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Windham-Myers, Lisamarie lwindham-myers@usgs.gov","contributorId":167489,"corporation":false,"usgs":true,"family":"Windham-Myers","given":"Lisamarie","email":"lwindham-myers@usgs.gov","affiliations":[],"preferred":true,"id":705033,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kanevskiy, Mikhail","contributorId":60511,"corporation":false,"usgs":true,"family":"Kanevskiy","given":"Mikhail","affiliations":[],"preferred":false,"id":705034,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70189525,"text":"70189525 - 2015 - Removal of terrestrial DOC in aquatic ecosystems of a temperate river network","interactions":[],"lastModifiedDate":"2017-07-14T12:24:34","indexId":"70189525","displayToPublicDate":"2015-12-01T00:00:00","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":"Removal of terrestrial DOC in aquatic ecosystems of a temperate river network","docAbstract":"<div class=\"article-section__content mainAbstract\"><p>Surface waters play a potentially important role in the global carbon balance. Dissolved organic carbon (DOC) fluxes are a major transfer of terrestrial carbon to river systems, and the fate of DOC in aquatic systems is poorly constrained. We used a unique combination of spatially distributed sampling of three DOC fractions throughout a river network and modeling to quantify the net removal of terrestrial DOC during a summer base flow period. We found that aquatic reactivity of terrestrial DOC leading to net loss is low, closer to conservative chloride than to reactive nitrogen. Net removal occurred mainly from the hydrophobic organic acid fraction, while hydrophilic and transphilic acids showed no net change, indicating that partitioning of bulk DOC into different fractions is critical for understanding terrestrial DOC removal. These findings suggest that river systems may have only a modest ability to alter the amounts of terrestrial DOC delivered to coastal zones.</p></div>","language":"English","publisher":"AGU","doi":"10.1002/2015GL064647","usgsCitation":"Wollheim, W.M., Stewart, R.J., Aiken, G.R., Butler, K.D., Morse, N.B., and Salisbury, J., 2015, Removal of terrestrial DOC in aquatic ecosystems of a temperate river network: Geophysical Research Letters, v. 42, no. 16, p. 6671-6679, https://doi.org/10.1002/2015GL064647.","productDescription":"9 p.","startPage":"6671","endPage":"6679","ipdsId":"IP-064250","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":471609,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2015gl064647","text":"Publisher Index Page"},{"id":343869,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Ipswich River","volume":"42","issue":"16","noUsgsAuthors":false,"publicationDate":"2015-08-19","publicationStatus":"PW","scienceBaseUri":"5969d82ce4b0d1f9f060a191","contributors":{"authors":[{"text":"Wollheim, W. M.","contributorId":10912,"corporation":false,"usgs":false,"family":"Wollheim","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":705035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, R. J.","contributorId":194685,"corporation":false,"usgs":false,"family":"Stewart","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":705036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aiken, George R. 0000-0001-8454-0984 graiken@usgs.gov","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":1322,"corporation":false,"usgs":true,"family":"Aiken","given":"George","email":"graiken@usgs.gov","middleInitial":"R.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":705037,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, Kenna D. kebutler@usgs.gov","contributorId":3283,"corporation":false,"usgs":true,"family":"Butler","given":"Kenna","email":"kebutler@usgs.gov","middleInitial":"D.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":705038,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Morse, Nathaniel B.","contributorId":139747,"corporation":false,"usgs":false,"family":"Morse","given":"Nathaniel","email":"","middleInitial":"B.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":705039,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Salisbury, J.","contributorId":194686,"corporation":false,"usgs":false,"family":"Salisbury","given":"J.","affiliations":[],"preferred":false,"id":705040,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70191099,"text":"70191099 - 2015 - Combining NLCD and MODIS to create a land cover-albedo database for the continental United States","interactions":[],"lastModifiedDate":"2017-09-26T14:06:20","indexId":"70191099","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Combining NLCD and MODIS to create a land cover-albedo database for the continental United States","docAbstract":"<p><span>Land surface albedo is an essential climate variable that is tightly linked to land cover, such that specific land cover classes (e.g., deciduous broadleaf forest, cropland) have characteristic albedos. Despite the normative of land-cover class specific albedos, there is considerable variability in albedo within a land cover class. The National Land Cover Database (NLCD) and the Moderate Resolution Imaging Spectroradiometer (MODIS) albedo product were combined to produce a long-term (14&nbsp;years) integrated land cover-albedo database for the continental United States that can be used to examine the temporal behavior of albedo as a function of land cover. The integration identifies areas of homogeneous land cover at the nominal spatial resolution of the MODIS (MCD43A) albedo product (500&nbsp;m&nbsp;×&nbsp;500&nbsp;m) from the NLCD product (30&nbsp;m&nbsp;×&nbsp;30&nbsp;m), and provides an albedo data record per 500&nbsp;m&nbsp;×&nbsp;500&nbsp;m pixel for 14 of the 16 NLCD land cover classes. Individual homogeneous land cover pixels have up to 605 albedo observations, and 75% of the pixels have at least 319 MODIS albedo observations (≥&nbsp;50% of the maximum possible number of observations) for the study period (2000–2013). We demonstrated the utility of the database by conducting a multivariate analysis of variance of albedo for each NLCD land cover class, showing that locational (pixel-to-pixel) and inter-annual variability were significant factors in addition to expected seasonal (intra-annual) and geographic (latitudinal) effects.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.rse.2015.09.012","usgsCitation":"Wickham, J., Barnes, C., Nash, M., and Wade, T., 2015, Combining NLCD and MODIS to create a land cover-albedo database for the continental United States: Remote Sensing of Environment, v. 170, p. 143-152, https://doi.org/10.1016/j.rse.2015.09.012.","productDescription":"10 p.","startPage":"143","endPage":"152","ipdsId":"IP-069951","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":346099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"170","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59cb6734e4b017cf3141c6a7","contributors":{"authors":[{"text":"Wickham, J.","contributorId":102230,"corporation":false,"usgs":true,"family":"Wickham","given":"J.","email":"","affiliations":[],"preferred":false,"id":711200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Christopher A. 0000-0002-4608-4364 christopher.barnes.ctr@usgs.gov","orcid":"https://orcid.org/0000-0002-4608-4364","contributorId":178108,"corporation":false,"usgs":true,"family":"Barnes","given":"Christopher A.","email":"christopher.barnes.ctr@usgs.gov","affiliations":[],"preferred":false,"id":711201,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nash, M.S.","contributorId":43946,"corporation":false,"usgs":true,"family":"Nash","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":711202,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wade, T.G.","contributorId":74113,"corporation":false,"usgs":true,"family":"Wade","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":711203,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70189516,"text":"70189516 - 2015 - The effect of natural organic matter on mercury methylation by Desulfobulbus propionicus 1pr3","interactions":[],"lastModifiedDate":"2018-09-04T15:40:41","indexId":"70189516","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1702,"text":"Frontiers in Microbiology","onlineIssn":"1664-302X","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The effect of natural organic matter on mercury methylation by <i>Desulfobulbus propionicus</i> 1pr3","title":"The effect of natural organic matter on mercury methylation by Desulfobulbus propionicus 1pr3","docAbstract":"<p><span>Methylation of tracer and ambient mercury (</span><sup>200</sup><span>Hg and<span>&nbsp;</span></span><sup>202</sup><span>Hg, respectively) equilibrated with four different natural organic matter (NOM) isolates was investigated<span>&nbsp;</span></span><i>in vivo</i><span><span>&nbsp;</span>using the Hg-methylating sulfate-reducing bacterium<span>&nbsp;</span></span><i>Desulfobulbus propionicus</i><span><span>&nbsp;</span>1pr3.<span>&nbsp;</span></span><i>Desulfobulbus</i><span><span>&nbsp;</span>cultures grown fermentatively with environmentally representative concentrations of dissolved NOM isolates, Hg[II], and HS</span><sup>−</sup><span><span>&nbsp;</span>were assayed for absolute methylmercury (MeHg) concentration and conversion of Hg(II) to MeHg relative to total unfiltered Hg(II). Results showed the<span>&nbsp;</span></span><sup>200</sup><span>Hg tracer was methylated more efficiently in the presence of hydrophobic NOM isolates than in the presence of transphilic NOM, or in the absence of NOM. Different NOM isolates were associated with variable methylation efficiencies for either the<span>&nbsp;</span></span><sup>202</sup><span>Hg tracer or ambient<span>&nbsp;</span></span><sup>200</sup><span>Hg. One hydrophobic NOM, F1 HpoA derived from dissolved organic matter from the Florida Everglades, was equilibrated for different times with Hg tracer, which resulted in different methylation rates. A 5 day equilibration with F1 HpoA resulted in more MeHg production than either the 4 h or 30 day equilibration periods, suggesting a time dependence for NOM-enhanced Hg bioavailability for methylation.</span></p>","language":"English","publisher":"Frontiers","doi":"10.3389/fmicb.2015.01389","usgsCitation":"Moreau, J.W., Gionfriddo, C.M., Krabbenhoft, D.P., Ogorek, J.M., DeWild, J.F., Aiken, G.R., and Roden, E.E., 2015, The effect of natural organic matter on mercury methylation by Desulfobulbus propionicus 1pr3: Frontiers in Microbiology, v. 6, p. 1-15, https://doi.org/10.3389/fmicb.2015.01389.","productDescription":"Article 1389; 15 p.","startPage":"1","endPage":"15","ipdsId":"IP-070733","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":471604,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/fmicb.2015.01389","text":"Publisher Index Page"},{"id":343858,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","noUsgsAuthors":false,"publicationDate":"2015-12-18","publicationStatus":"PW","scienceBaseUri":"5969d82ce4b0d1f9f060a197","contributors":{"authors":[{"text":"Moreau, John W.","contributorId":151017,"corporation":false,"usgs":false,"family":"Moreau","given":"John","email":"","middleInitial":"W.","affiliations":[{"id":18167,"text":"University of Melbourne, Melbour","active":true,"usgs":false}],"preferred":false,"id":704997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gionfriddo, Caitlin M.","contributorId":194676,"corporation":false,"usgs":false,"family":"Gionfriddo","given":"Caitlin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":704998,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":704999,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ogorek, Jacob M. 0000-0002-6327-0740 jmogorek@usgs.gov","orcid":"https://orcid.org/0000-0002-6327-0740","contributorId":4960,"corporation":false,"usgs":true,"family":"Ogorek","given":"Jacob","email":"jmogorek@usgs.gov","middleInitial":"M.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":705000,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeWild, John F. 0000-0003-4097-2798 jfdewild@usgs.gov","orcid":"https://orcid.org/0000-0003-4097-2798","contributorId":2525,"corporation":false,"usgs":true,"family":"DeWild","given":"John","email":"jfdewild@usgs.gov","middleInitial":"F.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":705001,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Aiken, George R. 0000-0001-8454-0984 graiken@usgs.gov","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":1322,"corporation":false,"usgs":true,"family":"Aiken","given":"George","email":"graiken@usgs.gov","middleInitial":"R.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":705002,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roden, Eric E.","contributorId":127525,"corporation":false,"usgs":false,"family":"Roden","given":"Eric","email":"","middleInitial":"E.","affiliations":[{"id":7009,"text":"Department of Geoscience and NASA Astrobiology Institute, University of Wisconsin, Madison","active":true,"usgs":false}],"preferred":false,"id":705003,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70192724,"text":"70192724 - 2015 - Differences in ecosystem carbon distribution and nutrient cycling linked to forest tree species composition in a mid-successional boreal forest","interactions":[],"lastModifiedDate":"2017-11-08T13:41:24","indexId":"70192724","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1478,"text":"Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Differences in ecosystem carbon distribution and nutrient cycling linked to forest tree species composition in a mid-successional boreal forest","docAbstract":"<p><span>In the boreal forest of Alaska, increased fire severity associated with climate change is expanding deciduous forest cover in areas previously dominated by black spruce (</span><i class=\"EmphasisTypeItalic \">Picea mariana</i><span>). Needle-leaf conifer and broad-leaf deciduous species are commonly associated with differences in tree growth, carbon (C) and nutrient cycling, and C accumulation in soils. Although this suggests that changes in tree species composition in Alaska could impact C and nutrient pools and fluxes, few studies have measured these linkages. We quantified C, nitrogen, phosphorus, and base cation pools and fluxes in three stands of black spruce and Alaska paper birch (</span><i class=\"EmphasisTypeItalic \">Betula neoalaskana</i><span>) that established following a single fire event in 1958. Paper birch consistently displayed characteristics of more rapid C and nutrient cycling, including greater aboveground net primary productivity, higher live foliage and litter nutrient concentrations, and larger ammonium and nitrate pools in the soil organic layer (SOL). Ecosystem C stocks (aboveground&nbsp;+&nbsp;SOL&nbsp;+&nbsp;0–10&nbsp;cm mineral soil) were similar for the two species; however, in black spruce, 78% of measured C was found in soil pools, primarily in the SOL, whereas aboveground biomass dominated ecosystem C pools in birch forest. Radiocarbon analysis indicated that approximately one-quarter of the black spruce SOL C accumulated prior to the 1958 fire, whereas no pre-fire C was observed in birch soils. Our findings suggest that tree species exert a strong influence over C and nutrient cycling in boreal forest and forest compositional shifts may have long-term implications for ecosystem C and nutrient dynamics.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10021-015-9912-7","usgsCitation":"Melvin, A.M., Mack, M., Johnstone, J.F., McGuire, A.D., Genet, H., and Schuur, E.A., 2015, Differences in ecosystem carbon distribution and nutrient cycling linked to forest tree species composition in a mid-successional boreal forest: Ecosystems, v. 18, no. 8, p. 1472-1488, https://doi.org/10.1007/s10021-015-9912-7.","productDescription":"17 p.","startPage":"1472","endPage":"1488","ipdsId":"IP-063589","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":348463,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"8","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2015-09-08","publicationStatus":"PW","scienceBaseUri":"5a0425c2e4b0dc0b45b453fd","contributors":{"authors":[{"text":"Melvin, April M.","contributorId":200151,"corporation":false,"usgs":false,"family":"Melvin","given":"April","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":721276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mack, Michelle C.","contributorId":140367,"corporation":false,"usgs":false,"family":"Mack","given":"Michelle C.","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":721277,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnstone, Jill F.","contributorId":179336,"corporation":false,"usgs":false,"family":"Johnstone","given":"Jill","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":721278,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McGuire, A. David 0000-0003-4646-0750 ffadm@usgs.gov","orcid":"https://orcid.org/0000-0003-4646-0750","contributorId":166708,"corporation":false,"usgs":true,"family":"McGuire","given":"A.","email":"ffadm@usgs.gov","middleInitial":"David","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":716777,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Genet, Helene","contributorId":95370,"corporation":false,"usgs":true,"family":"Genet","given":"Helene","affiliations":[],"preferred":false,"id":721279,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schuur, Edward A.G.","contributorId":50026,"corporation":false,"usgs":true,"family":"Schuur","given":"Edward","email":"","middleInitial":"A.G.","affiliations":[],"preferred":false,"id":721280,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70192950,"text":"70192950 - 2015 - Developing a conservation strategy to maximize persistence of an endangered freshwater mussel species while considering management effectiveness and cost","interactions":[],"lastModifiedDate":"2017-11-29T13:52:49","indexId":"70192950","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1699,"text":"Freshwater Science","active":true,"publicationSubtype":{"id":10}},"title":"Developing a conservation strategy to maximize persistence of an endangered freshwater mussel species while considering management effectiveness and cost","docAbstract":"<p>We used a structured decision-making process to develop conservation strategies to increase persistence of Dwarf Wedgemussel (<i>Alasmidonta heterodon</i>) in North Carolina, USA, while accounting for uncertainty in management effectiveness and considering costs. Alternative conservation strategies were portfolios of management actions that differed by location of management actions on the landscape. Objectives of the conservation strategy were to maximize species persistence, maintain genetic diversity, maximize public support, and minimize management costs. We compared 4 conservation strategies: 1) the ‘status quo’ strategy represented current management, 2) the ‘protect the best’ strategy focused on protecting the best populations in the Tar River basin, 3) the ‘expand the distribution’ strategy focused on management of extant populations and establishment of new populations in the Neuse River basin, and 4) the ‘hybrid’ strategy combined elements of each strategy to balance conservation in the Tar and Neuse River basins. A population model informed requirements for population management, and experts projected performance of alternative strategies over a 20-y period. The optimal strategy depended on the relative value placed on competing objectives, which can vary among stakeholders. The protect the best and hybrid strategies were optimal across a wide range of relative values with 2 exceptions: 1) if minimizing management cost was of overriding concern, then status quo was optimal, or 2) if maximizing population persistence in the Neuse River basin was emphasized, then expand the distribution strategy was optimal. The optimal strategy was robust to uncertainty in management effectiveness. Overall, the structured decision process can help identify the most promising strategies for endangered species conservation that maximize conservation benefit given the constraint of limited funding.</p>","language":"English","publisher":"University of Chicago Press","doi":"10.1086/683121","usgsCitation":"Smith, D.R., McRae, S.E., Augspurger, T., Ratcliffe, J.A., Nichols, R.B., Eads, C.B., Savidge, T., and Bogan, A.E., 2015, Developing a conservation strategy to maximize persistence of an endangered freshwater mussel species while considering management effectiveness and cost: Freshwater Science, v. 34, no. 4, p. 1324-1339, https://doi.org/10.1086/683121.","productDescription":"16 p.","startPage":"1324","endPage":"1339","ipdsId":"IP-057103","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":348665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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,{"id":70184227,"text":"70184227 - 2015 - Seismic source characterization for the 2014 update of the U.S. National Seismic Hazard Model","interactions":[],"lastModifiedDate":"2017-03-06T11:05:53","indexId":"70184227","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Seismic source characterization for the 2014 update of the U.S. National Seismic Hazard Model","docAbstract":"<p><span>We present the updated seismic source characterization (SSC) for the 2014 update of the National Seismic Hazard Model (NSHM) for the conterminous United States. Construction of the seismic source models employs the methodology that was developed for the 1996 NSHM but includes new and updated data, data types, source models, and source parameters that reflect the current state of knowledge of earthquake occurrence and state of practice for seismic hazard analyses. We review the SSC parameterization and describe the methods used to estimate earthquake rates, magnitudes, locations, and geometries for all seismic source models, with an emphasis on new source model components. We highlight the effects that two new model components—incorporation of slip rates from combined geodetic-geologic inversions and the incorporation of adaptively smoothed seismicity models—have on probabilistic ground motions, because these sources span multiple regions of the conterminous United States and provide important additional epistemic uncertainty for the 2014 NSHM.</span></p>","language":"English","publisher":"EERI","doi":"10.1193/110514EQS183M","usgsCitation":"Moschetti, M.P., Powers, P.M., Petersen, M.D., Boyd, O.S., Chen, R., Field, E.H., Frankel, A.D., Haller, K., Harmsen, S., Mueller, C.S., Wheeler, R., and Zeng, Y., 2015, Seismic source characterization for the 2014 update of the U.S. National Seismic Hazard Model: Earthquake Spectra, v. 31, no. S1, p. S31-S57, https://doi.org/10.1193/110514EQS183M.","productDescription":"27 p.","startPage":"S31","endPage":"S57","ipdsId":"IP-066842","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":471608,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1193/110514eqs183m","text":"Publisher Index Page"},{"id":336861,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"S1","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-12-01","publicationStatus":"PW","scienceBaseUri":"58be833de4b014cc3a3a99f9","contributors":{"authors":[{"text":"Moschetti, Morgan P. 0000-0001-7261-0295 mmoschetti@usgs.gov","orcid":"https://orcid.org/0000-0001-7261-0295","contributorId":1662,"corporation":false,"usgs":true,"family":"Moschetti","given":"Morgan","email":"mmoschetti@usgs.gov","middleInitial":"P.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":680636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powers, Peter M. 0000-0003-2124-6184 pmpowers@usgs.gov","orcid":"https://orcid.org/0000-0003-2124-6184","contributorId":176814,"corporation":false,"usgs":true,"family":"Powers","given":"Peter","email":"pmpowers@usgs.gov","middleInitial":"M.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":680637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petersen, Mark D. 0000-0001-8542-3990 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afrankel@usgs.gov","orcid":"https://orcid.org/0000-0001-9119-6106","contributorId":146285,"corporation":false,"usgs":true,"family":"Frankel","given":"Arthur","email":"afrankel@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":680641,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Haller, Kathleen 0000-0001-8847-7302 haller@usgs.gov","orcid":"https://orcid.org/0000-0001-8847-7302","contributorId":172556,"corporation":false,"usgs":true,"family":"Haller","given":"Kathleen","email":"haller@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":680642,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Harmsen, Stephen harmsen@usgs.gov","contributorId":152128,"corporation":false,"usgs":true,"family":"Harmsen","given":"Stephen","email":"harmsen@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards 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,{"id":70184233,"text":"70184233 - 2015 - The 2014 update to the National Seismic Hazard Model in California","interactions":[],"lastModifiedDate":"2017-03-06T10:50:05","indexId":"70184233","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"The 2014 update to the National Seismic Hazard Model in California","docAbstract":"<p><span>The 2014 update to the U. S. Geological Survey National Seismic Hazard Model in California introduces a new earthquake rate model and new ground motion models (GMMs) that give rise to numerous changes to seismic hazard throughout the state. The updated earthquake rate model is the third version of the Uniform California Earthquake Rupture Forecast (UCERF3), wherein the rates of all ruptures are determined via a self-consistent inverse methodology. This approach accommodates multifault ruptures and reduces the overprediction of moderate earthquake rates exhibited by the previous model (UCERF2). UCERF3 introduces new faults, changes to slip or moment rates on existing faults, and adaptively smoothed gridded seismicity source models, all of which contribute to significant changes in hazard. New GMMs increase ground motion near large strike-slip faults and reduce hazard over dip-slip faults. The addition of very large strike-slip ruptures and decreased reverse fault rupture rates in UCERF3 further enhances these effects.</span></p>","language":"English","publisher":"EERI","doi":"10.1193/110314EQS176M","usgsCitation":"Powers, P.M., and Field, E.H., 2015, The 2014 update to the National Seismic Hazard Model in California: Earthquake Spectra, v. 31, no. S1, p. 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,{"id":70187774,"text":"70187774 - 2015 - Conodont biostratigraphy of the Permian-Triassic boundary sequence at Lung Cam, Vietnam","interactions":[],"lastModifiedDate":"2017-05-18T14:33:41","indexId":"70187774","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Conodont biostratigraphy of the Permian-Triassic boundary sequence at Lung Cam, Vietnam","docAbstract":"<p><span>The occurrences of a few specimens of Clarkina and many specimens of Hindeodus at the Permian-Triassic boundary section at Lung Cam, Vietnam allow accurate graphic correlation to the P-T boundary stratotype at Meishan, China. One species of Clarkina, ten species and two subspecies of Hindeodus, and the apparatuses of Hindeodus latidentatus and Merrillina ultima are described and illustrated.</span></p>","language":"English","publisher":"Micropaleontology Press","usgsCitation":"Wardlaw, B.R., Nestell, M.K., Nestell, G.P., Ellwood, B.B., and Lan, L., 2015, Conodont biostratigraphy of the Permian-Triassic boundary sequence at Lung Cam, Vietnam: Micropaleontology, v. 61, p. 313-334.","productDescription":"22 p.","startPage":"313","endPage":"334","ipdsId":"IP-062992","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":341485,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341484,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.micropress.org/microaccess/micropaleontology/issue-320/article-1953"}],"country":"Vietnam","volume":"61","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"591eb2e3e4b0a7fdb4418b94","contributors":{"authors":[{"text":"Wardlaw, Bruce R. bwardlaw@usgs.gov","contributorId":266,"corporation":false,"usgs":true,"family":"Wardlaw","given":"Bruce","email":"bwardlaw@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":695567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nestell, Merlynd K.","contributorId":68603,"corporation":false,"usgs":false,"family":"Nestell","given":"Merlynd","email":"","middleInitial":"K.","affiliations":[{"id":12734,"text":"University of Texas at Arlington","active":true,"usgs":false}],"preferred":false,"id":695568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nestell, Galina P.","contributorId":22651,"corporation":false,"usgs":false,"family":"Nestell","given":"Galina","email":"","middleInitial":"P.","affiliations":[{"id":12734,"text":"University of Texas at Arlington","active":true,"usgs":false}],"preferred":false,"id":695569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ellwood, Brooks B.","contributorId":44814,"corporation":false,"usgs":false,"family":"Ellwood","given":"Brooks","email":"","middleInitial":"B.","affiliations":[{"id":5115,"text":"Louisiana State University","active":true,"usgs":false}],"preferred":false,"id":695570,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lan, Luu Thi Phuong","contributorId":192129,"corporation":false,"usgs":false,"family":"Lan","given":"Luu Thi Phuong","affiliations":[],"preferred":false,"id":695571,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70187762,"text":"70187762 - 2015 - Evaluation of the Global Land Data Assimilation System (GLDAS) air temperature data products","interactions":[],"lastModifiedDate":"2017-05-17T11:19:03","indexId":"70187762","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2344,"text":"Journal of Hydrometeorology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of the Global Land Data Assimilation System (GLDAS) air temperature data products","docAbstract":"<p><span>There is a high demand for agrohydrologic models to use gridded near-surface air temperature data as the model input for estimating regional and global water budgets and cycles. The Global Land Data Assimilation System (GLDAS) developed by combining simulation models with observations provides a long-term gridded meteorological dataset at the global scale. However, the GLDAS air temperature products have not been comprehensively evaluated, although the accuracy of the products was assessed in limited areas. In this study, the daily 0.25° resolution GLDAS air temperature data are compared with two reference datasets: 1) 1-km-resolution gridded Daymet data (2002 and 2010) for the conterminous United States and 2) global meteorological observations (2000–11) archived from the Global Historical Climatology Network (GHCN). The comparison of the GLDAS datasets with the GHCN datasets, including 13 511 weather stations, indicates a fairly high accuracy of the GLDAS data for daily temperature. The quality of the GLDAS air temperature data, however, is not always consistent in different regions of the world; for example, some areas in Africa and South America show relatively low accuracy. Spatial and temporal analyses reveal a high agreement between GLDAS and Daymet daily air temperature datasets, although spatial details in high mountainous areas are not sufficiently estimated by the GLDAS data. The evaluation of the GLDAS data demonstrates that the air temperature estimates are generally accurate, but caution should be taken when the data are used in mountainous areas or places with sparse weather stations.</span></p>","language":"English","publisher":"American Meteorological Society","doi":"10.1175/JHM-D-14-0230.1","usgsCitation":"Ji, L., Senay, G.B., and Verdin, J.P., 2015, Evaluation of the Global Land Data Assimilation System (GLDAS) air temperature data products: Journal of Hydrometeorology, v. 16, p. 2463-2480, https://doi.org/10.1175/JHM-D-14-0230.1.","productDescription":"18 p.","startPage":"2463","endPage":"2480","ipdsId":"IP-060871","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":471619,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/jhm-d-14-0230.1","text":"Publisher Index Page"},{"id":341434,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","noUsgsAuthors":false,"publicationDate":"2015-11-17","publicationStatus":"PW","scienceBaseUri":"593e26a5e4b0764e6c61b754","contributors":{"authors":[{"text":"Ji, Lei 0000-0002-6133-1036 lji@usgs.gov","orcid":"https://orcid.org/0000-0002-6133-1036","contributorId":139587,"corporation":false,"usgs":true,"family":"Ji","given":"Lei","email":"lji@usgs.gov","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":695522,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senay, Gabriel B. 0000-0002-8810-8539 senay@usgs.gov","orcid":"https://orcid.org/0000-0002-8810-8539","contributorId":3114,"corporation":false,"usgs":true,"family":"Senay","given":"Gabriel","email":"senay@usgs.gov","middleInitial":"B.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":695523,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Verdin, James P. 0000-0003-0238-9657 verdin@usgs.gov","orcid":"https://orcid.org/0000-0003-0238-9657","contributorId":720,"corporation":false,"usgs":true,"family":"Verdin","given":"James","email":"verdin@usgs.gov","middleInitial":"P.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":695524,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70187255,"text":"70187255 - 2015 - Annual survival rate estimate of satellite transmitter–marked eastern population greater sandhill cranes","interactions":[],"lastModifiedDate":"2017-04-28T11:42:48","indexId":"70187255","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2287,"text":"Journal of Fish and Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Annual survival rate estimate of satellite transmitter–marked eastern population greater sandhill cranes","docAbstract":"<p><span>Several surveys have documented the increasing population size and geographic distribution of Eastern Population greater sandhill cranes </span><i>Grus canadensis tabida</i><span> since the 1960s. Sport hunting of this population of sandhill cranes started in 2012 following the provisions of the Eastern Population Sandhill Crane Management Plan. However, there are currently no published estimates of Eastern Population sandhill crane survival rate that can be used to inform harvest management. As part of two studies of Eastern Population sandhill crane migration, we deployed solar-powered global positioning system platform transmitting terminals on Eastern Population sandhill cranes (</span><i>n</i><span>  =  42) at key concentration areas from 2009 to 2012. We estimated an annual survival rate for Eastern Population sandhill cranes from data resulting from monitoring these cranes by using the known-fates model in the MARK program. Estimated annual survival rate for adult Eastern Population sandhill cranes was 0.950 (95% confidence interval  =  0.885–0.979) during December 2009–August 2014. All fatalities (</span><i>n</i><span>  =  5) occurred after spring migration in late spring and early summer. We were unable to determine cause of death for crane fatalities in our study. Our survival rate estimate will be useful when combined with other population parameters such as the population index derived from the U.S. Fish and Wildlife Service fall survey, harvest, and recruitment rates to assess the effects of harvest on population size and trend and evaluate the effectiveness of management strategies.</span></p>","language":"English","publisher":"Scientific Journals","doi":"10.3996/042015-JFWM-035","usgsCitation":"Fronczak, D.L., Andersen, D., Hanna, E.E., and Cooper, T.R., 2015, Annual survival rate estimate of satellite transmitter–marked eastern population greater sandhill cranes: Journal of Fish and Wildlife Management, v. 6, no. 2, p. 464-471, https://doi.org/10.3996/042015-JFWM-035.","productDescription":"8 p.","startPage":"464","endPage":"471","ipdsId":"IP-064500","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":471612,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3996/042015-jfwm-035","text":"Publisher Index Page"},{"id":340606,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"2","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2015-07-01","publicationStatus":"PW","scienceBaseUri":"590454a6e4b022cee40dc248","contributors":{"authors":[{"text":"Fronczak, David L.","contributorId":191560,"corporation":false,"usgs":false,"family":"Fronczak","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":693470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andersen, David E. 0000-0001-9535-3404 dea@usgs.gov","orcid":"https://orcid.org/0000-0001-9535-3404","contributorId":2168,"corporation":false,"usgs":true,"family":"Andersen","given":"David E.","email":"dea@usgs.gov","affiliations":[{"id":34539,"text":"Minnesota Cooperative Fish and Wildlife Research Unit","active":true,"usgs":false},{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":693113,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hanna, Everett E.","contributorId":191561,"corporation":false,"usgs":false,"family":"Hanna","given":"Everett","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":693471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cooper, Thomas R.","contributorId":191468,"corporation":false,"usgs":false,"family":"Cooper","given":"Thomas","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":693472,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70187776,"text":"70187776 - 2015 - Conodont faunas from a complete basinal succession of the upper part of the Wordian (Middle Permian, Guadalupian, West Texas)","interactions":[],"lastModifiedDate":"2017-05-18T14:30:57","indexId":"70187776","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Conodont faunas from a complete basinal succession of the upper part of the Wordian (Middle Permian, Guadalupian, West Texas)","docAbstract":"<p>In the southern part of the Patterson Hills just to the west of the Guadalupe Mountains escarpment ofWest Texas, a 29m outcrop of alternating calcareous siltstone and silty limestone with a few thin fine sandstone interbeds displays the overlap occurrence of a narrowmorphotype of Jinogondolella nankingensis (herein named J. nankingensis behnkeni) with J. aserrata near its base. The transition of Jinogondolella aserrata to J. postserrata is present near the top of this section and marks theWordian-Capitanian boundary, therefore displaying a significant portion of the upper part of theWordian in one short continuous section. Pseudohindeodus brevis n. sp. and H. capitanensis n. sp. are described. Pseudohindeodus ramovsi, Caenodontus serrulatus, Hindeodus wordensis, Sweetina triticum, Jinogondolella palmata, and J. errata also occur in this succession.</p>","language":"English","publisher":"Micropaleontology Press","usgsCitation":"Wardlaw, B.R., and Nestell, M.K., 2015, Conodont faunas from a complete basinal succession of the upper part of the Wordian (Middle Permian, Guadalupian, West Texas): Micropaleontology, v. 61, p. 257-292.","productDescription":"36 p.","startPage":"257","endPage":"292","ipdsId":"IP-071644","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":341454,"type":{"id":15,"text":"Index Page"},"url":"https://www.micropress.org/microaccess/micropaleontology/issue-320/article-1950"},{"id":341483,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","volume":"61","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"591eb2e3e4b0a7fdb4418b8f","contributors":{"authors":[{"text":"Wardlaw, Bruce R. bwardlaw@usgs.gov","contributorId":266,"corporation":false,"usgs":true,"family":"Wardlaw","given":"Bruce","email":"bwardlaw@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":695573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nestell, Merlynd K.","contributorId":68603,"corporation":false,"usgs":false,"family":"Nestell","given":"Merlynd","email":"","middleInitial":"K.","affiliations":[{"id":12734,"text":"University of Texas at Arlington","active":true,"usgs":false}],"preferred":false,"id":695574,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70196071,"text":"70196071 - 2015 - Sources and transport of phosphorus to rivers in California and adjacent states, U.S., as determined by SPARROW modeling","interactions":[],"lastModifiedDate":"2018-09-13T16:50:34","indexId":"70196071","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Sources and transport of phosphorus to rivers in California and adjacent states, U.S., as determined by SPARROW modeling","docAbstract":"<p><span>The SPARROW (SPAtially Referenced Regression on Watershed attributes) model was used to simulate annual phosphorus loads and concentrations in unmonitored stream reaches in California, U.S., and portions of Nevada and Oregon. The model was calibrated using de-trended streamflow and phosphorus concentration data at 80 locations. The model explained 91% of the variability in loads and 51% of the variability in yields for a base year of 2002. Point sources, geological background, and cultivated land were significant sources. Variables used to explain delivery of phosphorus from land to water were precipitation and soil clay content. Aquatic loss of phosphorus was significant in streams of all sizes, with the greatest decay predicted in small- and intermediate-sized streams. Geological sources, including volcanic rocks and shales, were the principal control on concentrations and loads in many regions. Some localized formations such as the Monterey shale of southern California are important sources of phosphorus and may contribute to elevated stream concentrations. Many of the larger point source facilities were located in downstream areas, near the ocean, and do not affect inland streams except for a few locations. Large areas of cultivated land result in phosphorus load increases, but do not necessarily increase the loads above those of geological background in some cases because of local hydrology, which limits the potential of phosphorus transport from land to streams.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/1752-1688.12326","usgsCitation":"Domagalski, J.L., and Saleh, D., 2015, Sources and transport of phosphorus to rivers in California and adjacent states, U.S., as determined by SPARROW modeling: Journal of the American Water Resources Association, v. 51, no. 6, p. 1463-1486, https://doi.org/10.1111/1752-1688.12326.","productDescription":"24 p.","startPage":"1463","endPage":"1486","ipdsId":"IP-052538","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":352579,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"6","noUsgsAuthors":false,"publicationDate":"2015-07-14","publicationStatus":"PW","scienceBaseUri":"5afeeb20e4b0da30c1bfc64a","contributors":{"authors":[{"text":"Domagalski, Joseph L. 0000-0002-6032-757X joed@usgs.gov","orcid":"https://orcid.org/0000-0002-6032-757X","contributorId":1330,"corporation":false,"usgs":true,"family":"Domagalski","given":"Joseph","email":"joed@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":731207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saleh, Dina 0000-0002-1406-9303 dsaleh@usgs.gov","orcid":"https://orcid.org/0000-0002-1406-9303","contributorId":939,"corporation":false,"usgs":true,"family":"Saleh","given":"Dina","email":"dsaleh@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":731208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70193797,"text":"70193797 - 2015 - Determining climate change management priorities: A case study from Wisconsin ","interactions":[],"lastModifiedDate":"2017-11-10T10:32:00","indexId":"70193797","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2231,"text":"Journal of Conservation Planning","active":true,"publicationSubtype":{"id":10}},"title":"Determining climate change management priorities: A case study from Wisconsin ","docAbstract":"<p>A burgeoning dialogue exists regarding how to allocate resources to maximize the likelihood of long-term biodiversity conservation within the context of climate change. To make effective decisions in natural resource management, an iterative, collaborative, and learning-based decision process may be more successful than a strictly consultative approach. One important, early step in a decision process is to identify priority species or systems. Although this promotes the conservation of select species or systems, it may inadvertently alter the future of non-target species and systems. We describe a process to screen terrestrial wildlife for potential sensitivity to climate change and then use the results to engage natural resource professionals in a process of identifying priorities for monitoring, research, and adaptation strategy implementation. We demonstrate this approach using a case study from Wisconsin. In Wisconsin, experts identified 23 out of 353 species with sufficient empirical research and management understanding to inform targeted action. Habitat management and management of hydrological conditions were the common strategies for targeted action. Although there may be an interest in adaptation strategy implementation for many species and systems, experts considered existing information inadequate to inform targeted action. According to experts, 40% of the vertebrate species in Wisconsin will require near-term intervention for climate adaptation. These results will inform state-wide conservation planning as well as regional efforts. </p>","language":"English","publisher":"The Conservation Fund","usgsCitation":"LeDee, O., and Ribic, C., 2015, Determining climate change management priorities: A case study from Wisconsin : Journal of Conservation Planning, v. 11, no. 1, p. 1-12.","productDescription":"12 p.","startPage":"1","endPage":"12","ipdsId":"IP-040823","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":348449,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":348216,"type":{"id":15,"text":"Index Page"},"url":"https://www.journalconsplanning.org/"}],"country":"United 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,{"id":70177798,"text":"70177798 - 2015 - Evaluation of three aging techniques and back-calculated growth for introduced Blue Catfish from Lake Oconee, Georgia","interactions":[],"lastModifiedDate":"2016-10-21T15:08:42","indexId":"70177798","displayToPublicDate":"2015-12-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3444,"text":"Southeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of three aging techniques and back-calculated growth for introduced Blue Catfish from Lake Oconee, Georgia","docAbstract":"<p><span>Back-calculation of length-at-age from otoliths and spines is a common technique employed in fisheries biology, but few studies have compared the precision of data collected with this method for catfish populations. We compared precision of back-calculated lengths-at-age for an introduced</span><i>Ictalurus furcatus</i><span> (Blue Catfish) population among 3 commonly used cross-sectioning techniques. We used gillnets to collect Blue Catfish (</span><i>n</i><span> = 153) from Lake Oconee, GA. We estimated ages from a basal recess, articulating process, and otolith cross-section from each fish. We employed the Frasier-Lee method to back-calculate length-at-age for each fish, and compared the precision of back-calculated lengths among techniques using hierarchical linear models. Precision in age assignments was highest for otoliths (83.5%) and lowest for basal recesses (71.4%). Back-calculated lengths were variable among fish ages 1–3 for the techniques compared; otoliths and basal recesses yielded variable lengths at age 8. We concluded that otoliths and articulating processes are adequate for age estimation of Blue Catfish.</span></p>","language":"English","publisher":"Eagle Hill Institute","doi":"10.1656/058.014.0417","usgsCitation":"Homer, M.D., Peterson, J., and Jennings, C.A., 2015, Evaluation of three aging techniques and back-calculated growth for introduced Blue Catfish from Lake Oconee, Georgia: Southeastern Naturalist, v. 14, no. 4, p. 740-756, https://doi.org/10.1656/058.014.0417.","productDescription":"17 p.","startPage":"740","endPage":"756","ipdsId":"IP-036204","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":330326,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"Lake Oconee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.37867736816406,\n              33.338559712732525\n            ],\n            [\n              -83.37867736816406,\n              33.714630486382156\n            ],\n            [\n              -83.14178466796875,\n              33.714630486382156\n            ],\n            [\n              -83.14178466796875,\n              33.338559712732525\n            ],\n            [\n              -83.37867736816406,\n              33.338559712732525\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"4","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2015-12-18","publicationStatus":"PW","scienceBaseUri":"5810c6d6e4b0f497e79733f7","contributors":{"authors":[{"text":"Homer, Michael D. Jr.","contributorId":176188,"corporation":false,"usgs":false,"family":"Homer","given":"Michael","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":651837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, James T. 0000-0002-7709-8590 james_peterson@usgs.gov","orcid":"https://orcid.org/0000-0002-7709-8590","contributorId":2111,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"james_peterson@usgs.gov","middleInitial":"T.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":651838,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jennings, Cecil A. 0000-0002-6159-6026 jennings@usgs.gov","orcid":"https://orcid.org/0000-0002-6159-6026","contributorId":874,"corporation":false,"usgs":true,"family":"Jennings","given":"Cecil","email":"jennings@usgs.gov","middleInitial":"A.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":651821,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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