{"pageNumber":"187","pageRowStart":"4650","pageSize":"25","recordCount":10466,"records":[{"id":70006137,"text":"70006137 - 2011 - Parasite transmission in social interacting hosts: Monogenean epidemics in guppies","interactions":[],"lastModifiedDate":"2021-05-20T20:25:19.31653","indexId":"70006137","displayToPublicDate":"2011-12-02T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Parasite transmission in social interacting hosts: Monogenean epidemics in guppies","docAbstract":"<div id=\"section1\" class=\"section toc-section\"><h3>Background</h3><p>Infection incidence increases with the average number of contacts between susceptible and infected individuals. Contact rates are normally assumed to increase linearly with host density. However, social species seek out each other at low density and saturate their contact rates at high densities. Although predicting epidemic behaviour requires knowing how contact rates scale with host density, few empirical studies have investigated the effect of host density. Also, most theory assumes each host has an equal probability of transmitting parasites, even though individual parasite load and infection duration can vary. To our knowledge, the relative importance of characteristics of the primary infected host vs. the susceptible population has never been tested experimentally.</p></div><div id=\"section2\" class=\"section toc-section\"><a id=\"\" class=\"link-target\" title=\"Methodology/Principal Findings\" name=\"\"></a><h3>Methodology/Principal Findings</h3><p>Here, we examine epidemics using a common ectoparasite,<span>&nbsp;</span><i>Gyrodactylus turnbulli</i><span>&nbsp;</span>infecting its guppy host (<i>Poecilia reticulata</i>). Hosts were maintained at different densities (3, 6, 12 and 24 fish in 40 L aquaria), and we monitored gyrodactylids both at a population and individual host level. Although parasite population size increased with host density, the probability of an epidemic did not. Epidemics were more likely when the primary infected fish had a high mean intensity and duration of infection. Epidemics only occurred if the primary infected host experienced more than 23 worm days. Female guppies contracted infections sooner than males, probably because females have a higher propensity for shoaling.</p></div><div id=\"section3\" class=\"section toc-section\"><a id=\"\" class=\"link-target\" title=\"Conclusions/Significance\" name=\"\"></a><h3>Conclusions/Significance</h3><p>These findings suggest that in social hosts like guppies, the frequency of social contact largely governs disease epidemics independent of host density.</p></div>","language":"English","publisher":"Public Library of Science","publisherLocation":"San Francisco, CA","doi":"10.1371/journal.pone.0022634","usgsCitation":"Johnson, M.B., Lafferty, K.D., van Oosterhout, C., and Cable, J., 2011, Parasite transmission in social interacting hosts: Monogenean epidemics in guppies: PLoS ONE, v. 6, no. 8, e22634, 6 p., https://doi.org/10.1371/journal.pone.0022634.","productDescription":"e22634, 6 p.","numberOfPages":"6","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":474859,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0022634","text":"Publisher Index Page"},{"id":204163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"8","noUsgsAuthors":false,"publicationDate":"2011-08-29","publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6892d2","contributors":{"authors":[{"text":"Johnson, Mirelle B.","contributorId":89769,"corporation":false,"usgs":true,"family":"Johnson","given":"Mirelle","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":353915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353913,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"van Oosterhout, Cock","contributorId":62089,"corporation":false,"usgs":true,"family":"van Oosterhout","given":"Cock","email":"","affiliations":[],"preferred":false,"id":353914,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cable, Joanne","contributorId":104778,"corporation":false,"usgs":true,"family":"Cable","given":"Joanne","email":"","affiliations":[],"preferred":false,"id":353916,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003814,"text":"70003814 - 2011 - Some possible causes of and corrections for STS-1 response changes in the Global Seismographic Network","interactions":[],"lastModifiedDate":"2021-05-21T17:01:23.445297","indexId":"70003814","displayToPublicDate":"2011-12-01T16:20:00","publicationYear":"2011","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":"Some possible causes of and corrections for STS-1 response changes in the Global Seismographic Network","docAbstract":"The Global Seismographic Network (GSN) (Figure 1) plays a key role in providing seismic data for global earthquake monitoring (<i>e.g.</i>, Benz <i>et al.</i> 2005), earthquake science (<i>e.g.</i>, Tsai <i>et al.</i> 2005), and studies of Earth structure (<i>e.g.</i>, Dalton <i>et al.</i> 2008). One of the key GSN design goals is to \"provide high fidelity digital recordings of all teleseismic ground motions (adequate to resolve at or near ambient noise up to the largest teleseismic signals over the bandwidth from free oscillations (10<sup>-4</sup> Hz) to teleseismic body waves (up to approximately 15 Hz))\" (GSN ad hoc Design Goals Subcommittee 2002). To help meet this goal, Streckeisen STS-1 seismometers were deployed at 80 GSN stations.  Some of the GSN sensors have been deployed for more than 25 years. Several recent studies (Davis <i>et al.</i> 2005; Ekstr&#246;m <i>et al.</i> 2006; Davis and Berger 2007) have examined the question of overall calibration of the GSN. Ekstr&#246;m <i>et al.</i> (2006) indicated that a number of sites showed anomalous responses and suggested a gradual decay in the sensitivity.  We have investigated the anomalous responses at several GSN sites. At least some of the problems observed by Ekstr&#246;m <i>et al.</i> (2006) may be attributed to humid air leaking into the feedback electronics of the STS-1 seismometers, which produces lower than normal sensitivities near the long-period corner of the instrument (360 seconds period). It appears that even though the feedback electronics boxes are designed to be sealed, water vapor can penetrate their interior after they have been exposed to highly humid seismometer vault air for extended periods. Highly humid air was also found to be present inside some STS-1 bell-jars (especially horizontal instruments) after loss of vacuum, resulting in corrosion and leakage between electrical conductors in connectors.","language":"English","publisher":"Seismological Society of America","publisherLocation":"El Cerrito, CA","doi":"10.1785/gssrl.82.4.560","usgsCitation":"Hutt, C., and Ringler, A., 2011, Some possible causes of and corrections for STS-1 response changes in the Global Seismographic Network: Seismological Research Letters, v. 82, no. 4, p. 560-571, https://doi.org/10.1785/gssrl.82.4.560.","productDescription":"12 p.","startPage":"560","endPage":"571","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":204531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"4","noUsgsAuthors":false,"publicationDate":"2011-07-05","publicationStatus":"PW","scienceBaseUri":"505b92d5e4b08c986b31a139","contributors":{"authors":[{"text":"Hutt, C. R. 0000-0001-9033-9195","orcid":"https://orcid.org/0000-0001-9033-9195","contributorId":61910,"corporation":false,"usgs":true,"family":"Hutt","given":"C. R.","affiliations":[],"preferred":false,"id":348982,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ringler, A. T. 0000-0002-9839-4188","orcid":"https://orcid.org/0000-0002-9839-4188","contributorId":99282,"corporation":false,"usgs":true,"family":"Ringler","given":"A. T.","affiliations":[],"preferred":false,"id":348983,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70136247,"text":"70136247 - 2011 - Global seabird responses to forage fish depletion - One-third for the birds","interactions":[],"lastModifiedDate":"2019-06-18T18:08:27","indexId":"70136247","displayToPublicDate":"2011-12-01T14:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Global seabird responses to forage fish depletion - One-third for the birds","docAbstract":"<p><span>Determining the form of key predator-prey relationships is critical for understanding marine ecosystem dynamics. Using a comprehensive global database, we quantified the effect of fluctuations in food abundance on seabird breeding success. We identified a threshold in prey (fish and krill, termed “forage fish”) abundance below which seabirds experience consistently reduced and more variable productivity. This response was common to all seven ecosystems and 14 bird species examined within the Atlantic, Pacific, and Southern Oceans. The threshold approximated one-third of the maximum prey biomass observed in long-term studies. This provides an indicator of the minimal forage fish biomass needed to sustain seabird productivity over the long term.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","publisherLocation":"New York, NY","doi":"10.1126/science.1212928","usgsCitation":"Cury, P.M., Boyd, I.L., Bonhommeau, S., Anker-Nilssen, T., Crawford, R.J., Furness, R.W., Mills, J.A., Murphy, E.J., Osterblom, H., Paleczny, M., Piatt, J.F., Roux, J., Shannon, L., and Sydeman, W., 2011, Global seabird responses to forage fish depletion - One-third for the birds: Science, v. 334, no. 6063, p. 1703-1706, https://doi.org/10.1126/science.1212928.","productDescription":"4 p.","startPage":"1703","endPage":"1706","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-030650","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":474866,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://archimer.ifremer.fr/doc/00056/16770/","text":"External Repository"},{"id":296936,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"334","issue":"6063","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2bb3e4b08de9379b3490","contributors":{"authors":[{"text":"Cury, Philippe M.","contributorId":68986,"corporation":false,"usgs":false,"family":"Cury","given":"Philippe","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":537407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyd, Ian L.","contributorId":10637,"corporation":false,"usgs":false,"family":"Boyd","given":"Ian","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":537408,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonhommeau, Sylvain","contributorId":8306,"corporation":false,"usgs":false,"family":"Bonhommeau","given":"Sylvain","email":"","affiliations":[],"preferred":false,"id":537409,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Anker-Nilssen, Tycho","contributorId":50375,"corporation":false,"usgs":false,"family":"Anker-Nilssen","given":"Tycho","email":"","affiliations":[],"preferred":false,"id":537410,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crawford, Robert J.M.","contributorId":27700,"corporation":false,"usgs":false,"family":"Crawford","given":"Robert","email":"","middleInitial":"J.M.","affiliations":[],"preferred":false,"id":537411,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Furness, Robert W.","contributorId":86588,"corporation":false,"usgs":false,"family":"Furness","given":"Robert","email":"","middleInitial":"W.","affiliations":[{"id":12473,"text":"University of Glasgow","active":true,"usgs":false}],"preferred":false,"id":537412,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mills, James A.","contributorId":32751,"corporation":false,"usgs":false,"family":"Mills","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":537413,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Murphy, Eugene J.","contributorId":80925,"corporation":false,"usgs":false,"family":"Murphy","given":"Eugene","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":537414,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Osterblom, Henrik","contributorId":16244,"corporation":false,"usgs":false,"family":"Osterblom","given":"Henrik","email":"","affiliations":[],"preferred":false,"id":537415,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Paleczny, Michelle","contributorId":35565,"corporation":false,"usgs":false,"family":"Paleczny","given":"Michelle","email":"","affiliations":[],"preferred":false,"id":537416,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":537249,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Roux, Jean-Paul","contributorId":47194,"corporation":false,"usgs":false,"family":"Roux","given":"Jean-Paul","email":"","affiliations":[],"preferred":false,"id":537417,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Shannon, Lynne","contributorId":103896,"corporation":false,"usgs":false,"family":"Shannon","given":"Lynne","email":"","affiliations":[],"preferred":false,"id":537418,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Sydeman, William J.","contributorId":172574,"corporation":false,"usgs":false,"family":"Sydeman","given":"William J.","affiliations":[],"preferred":false,"id":537419,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70006312,"text":"70006312 - 2011 - An adaptive decision framework for the conservation of a threatened plant","interactions":[],"lastModifiedDate":"2012-02-25T00:10:10","indexId":"70006312","displayToPublicDate":"2011-12-01T09:19:00","publicationYear":"2011","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":"An adaptive decision framework for the conservation of a threatened plant","docAbstract":"Mead's milkweed <i>Asclepias meadii</i>, a long-lived perennial herb of tallgrass prairie and glade communities of the central United States, is a species designated as threatened under the U.S. Endangered Species Act. Challenges to its successful management include the facts that much about its life history is unknown, its age at reproductive maturity is very advanced, certain life stages are practically unobservable, its productivity is responsive to unpredictable environmental events, and most of the known populations occur on private lands unprotected by any legal conservation instrument. One critical source of biological uncertainty is the degree to which fire promotes growth and reproductive response in the plant. To aid in its management, we developed a prototype population-level state-dependent decision-making framework that explicitly accounts for this uncertainty and for uncertainties related to stochastic environmental effects and vital rates. To parameterize the decision model, we used estimates found in the literature, and we analyzed data from a long-term monitoring program where fates of individual plants were observed through time. We demonstrate that different optimal courses of action are followed according to how one believes that fire influences reproductive response, and we show that the action taken for certain population states is informative for resolving uncertainty about competing beliefs regarding the effect of fire. We advocate the use of a model-predictive approach for the management of rare populations, particularly when management uncertainty is profound. Over time, an adaptive management approach should reduce uncertainty and improve management performance as predictions of management outcome generated under competing models are continually informed and updated by monitoring data.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Fish and Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","doi":"10.3996/012011-JFWM-007","usgsCitation":"Moore, C., Fonnesbeck, C.J., Shea, K., Lah, K.J., McKenzie, P.M., Ball, L.C., Runge, M.C., and Alexander, H.M., 2011, An adaptive decision framework for the conservation of a threatened plant: Journal of Fish and Wildlife Management, v. 2, no. 2, p. 247-261, https://doi.org/10.3996/012011-JFWM-007.","productDescription":"15 p.","startPage":"247","endPage":"261","numberOfPages":"15","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":474877,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/1808/13193","text":"External Repository"},{"id":204577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":115886,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3996/012011-JFWM-007","linkFileType":{"id":5,"text":"html"}}],"country":"United States","volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e9e2e4b0c8380cd484e4","contributors":{"authors":[{"text":"Moore, Clinton T.","contributorId":9767,"corporation":false,"usgs":true,"family":"Moore","given":"Clinton T.","affiliations":[],"preferred":false,"id":354293,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fonnesbeck, Christopher J.","contributorId":72474,"corporation":false,"usgs":true,"family":"Fonnesbeck","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354295,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shea, Katriona","contributorId":93190,"corporation":false,"usgs":true,"family":"Shea","given":"Katriona","affiliations":[],"preferred":false,"id":354297,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lah, Kristopher J.","contributorId":95194,"corporation":false,"usgs":true,"family":"Lah","given":"Kristopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354298,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McKenzie, Paul M.","contributorId":14902,"corporation":false,"usgs":true,"family":"McKenzie","given":"Paul","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":354294,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ball, Lianne C. 0000-0001-9331-0718 lball@usgs.gov","orcid":"https://orcid.org/0000-0001-9331-0718","contributorId":4274,"corporation":false,"usgs":true,"family":"Ball","given":"Lianne","email":"lball@usgs.gov","middleInitial":"C.","affiliations":[{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true}],"preferred":true,"id":354292,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Runge, Michael C. 0000-0002-8081-536X mrunge@usgs.gov","orcid":"https://orcid.org/0000-0002-8081-536X","contributorId":3358,"corporation":false,"usgs":true,"family":"Runge","given":"Michael","email":"mrunge@usgs.gov","middleInitial":"C.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":354291,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Alexander, Helen M.","contributorId":73334,"corporation":false,"usgs":true,"family":"Alexander","given":"Helen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":354296,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70003684,"text":"70003684 - 2011 - Modelling community dynamics based on species-level abundance models from detection/nondetection data","interactions":[],"lastModifiedDate":"2021-04-29T14:50:01.625624","indexId":"70003684","displayToPublicDate":"2011-12-01T09:10:39","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2163,"text":"Journal of Applied Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Modelling community dynamics based on species-level abundance models from detection/nondetection data","docAbstract":"<p><strong>1.</strong><span>&nbsp;</span>In large‐scale field surveys, a binary recording of each species’ detection or nondetection has been increasingly adopted for its simplicity and low cost. Because of the importance of abundance in many studies, it is desirable to obtain inferences about abundance at species‐, functional group‐, and community‐levels from such binary data.</p><p><strong>2.</strong><span>&nbsp;</span>We developed a novel hierarchical multi‐species abundance model based on species‐level detection/nondetection data. The model accounts for the existence of undetected species, and variability in abundance and detectability among species. Species‐level detection/nondetection is linked to species‐level abundance via a detection model that accommodates the expectation that probability of detection (at least one individuals is detected) increases with local abundance of the species. We applied this model to a 9‐year dataset composed of the detection/nondetection of forest birds, at a single post‐fire site (from 7 to 15 years after fire) in a montane area of central Japan. The model allocated undetected species into one of the predefined functional groups by assuming a prior distribution on individual group membership.</p><p><strong>3.</strong><span>&nbsp;</span>The results suggest that 15–20 species were missed in each year, and that species richness of communities and functional groups did not change with post‐fire forest succession. Overall abundance of birds and abundance of functional groups tended to increase over time, although only in the winter, while decreases in detectabilities were observed in several species.</p><p><strong>4.</strong><span>&nbsp;</span><i>Synthesis and applications</i>. Understanding and prediction of large‐scale biodiversity dynamics partly hinge on how we can use data effectively. Our hierarchical model for detection/nondetection data estimates abundance in space/time at species‐, functional group‐, and community‐levels while accounting for undetected individuals and species. It also permits comparison of multiple communities by many types of abundance‐based diversity and similarity measures under imperfect detection.</p>","language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1111/j.1365-2664.2010.01922.x","usgsCitation":"Yamaura, Y., Royle, J., Kuboi, K., Tada, T., Ikeno, S., and Makino, S., 2011, Modelling community dynamics based on species-level abundance models from detection/nondetection data: Journal of Applied Ecology, v. 48, no. 1, p. 67-75, https://doi.org/10.1111/j.1365-2664.2010.01922.x.","productDescription":"9 p.","startPage":"67","endPage":"75","numberOfPages":"9","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":474878,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-2664.2010.01922.x","text":"Publisher Index Page"},{"id":204341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-12-17","publicationStatus":"PW","scienceBaseUri":"505a5c64e4b0c8380cd6fc68","contributors":{"authors":[{"text":"Yamaura, Yuichi","contributorId":95997,"corporation":false,"usgs":true,"family":"Yamaura","given":"Yuichi","affiliations":[],"preferred":false,"id":348326,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Royle, J. Andrew 0000-0003-3135-2167","orcid":"https://orcid.org/0000-0003-3135-2167","contributorId":80808,"corporation":false,"usgs":true,"family":"Royle","given":"J. Andrew","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":348325,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kuboi, Kouji","contributorId":103784,"corporation":false,"usgs":true,"family":"Kuboi","given":"Kouji","email":"","affiliations":[],"preferred":false,"id":348327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tada, Tsuneo","contributorId":7407,"corporation":false,"usgs":true,"family":"Tada","given":"Tsuneo","email":"","affiliations":[],"preferred":false,"id":348322,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ikeno, Susumu","contributorId":12176,"corporation":false,"usgs":true,"family":"Ikeno","given":"Susumu","email":"","affiliations":[],"preferred":false,"id":348323,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Makino, Shun’ichi","contributorId":66401,"corporation":false,"usgs":true,"family":"Makino","given":"Shun’ichi","email":"","affiliations":[],"preferred":false,"id":348324,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70150346,"text":"70150346 - 2011 - The distributions of one invasive and two native crayfishes in relation to coarse-scale natural and anthropogenic factors","interactions":[],"lastModifiedDate":"2015-06-24T12:37:34","indexId":"70150346","displayToPublicDate":"2011-12-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1696,"text":"Freshwater Biology","active":true,"publicationSubtype":{"id":10}},"title":"The distributions of one invasive and two native crayfishes in relation to coarse-scale natural and anthropogenic factors","docAbstract":"<div class=\"para\">\n<p>1.&ensp;Native crayfishes are often extirpated from portions of their range because of interactions with invasive species, anthropogenic alterations to environmental conditions or a combination of these factors. Our goal was to identify coarse-scale natural and anthropogenic factors related to the current distributions of the invasive crayfish,&nbsp;<i>Orconectes hylas</i>, and two endemic crayfishes,&nbsp;<i>Orconectes peruncus</i>&nbsp;and<i>Orconectes quadruncus</i>&nbsp;in the St. Francis River drainage, Missouri, U.S.A. and to provide wider insights into the potential role of anthropogenic factors in facilitating species displacement.</p>\n</div>\n<div class=\"para\">\n<p>2.&ensp;We used classification trees to model coarse-scale natural and anthropogenic environmental factors and their relation to the presence or absence of each species. Model results were then used to predict probability of presence for each species within each stream segment throughout the entire St. Francis River drainage.</p>\n</div>\n<div class=\"para\">\n<p>3.&ensp;Factors related to geology and soils were the best predictors of species distributions. A dichotomy of these factors explained much of the discrete distributions of the two native species. Agricultural-related factors were identified as the most influential anthropogenic activity related to species distributions. All associations between the invasive species and anthropogenic factors were negative which suggested the invader was not likely to establish in heavily impacted areas. Overall, our models had high correct classification rates, and we were able to reliably predict the presence of the invader in the invaded drainage.</p>\n</div>\n<div class=\"para\">\n<p>4.&ensp;Given the negative associations of the invader with anthropogenic alterations at a coarse spatial scale, we believe other mechanisms are likely to be responsible for the widespread displacement of the two native species. These findings can be used to assist in conservation activities such as creation of refugia for native species and may direct future research to identify the mechanism(s) of species displacement.</p>\n</div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2427.2011.02664.x","usgsCitation":"Westhoff, J.T., Rabeni, C., and Sowa, S., 2011, The distributions of one invasive and two native crayfishes in relation to coarse-scale natural and anthropogenic factors: Freshwater Biology, v. 56, no. 12, p. 2415-2431, https://doi.org/10.1111/j.1365-2427.2011.02664.x.","productDescription":"17 p.","startPage":"2415","endPage":"2431","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-026466","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":302282,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","otherGeospatial":"Big River, Black River, Meramec River, St. Francis River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.8349609375,\n              36.53612263184686\n            ],\n            [\n              -90.087890625,\n              36.73888412439431\n            ],\n            [\n              -90.340576171875,\n              36.98500309285596\n            ],\n            [\n              -90.24169921875,\n              37.501010429493284\n            ],\n            [\n              -90.54931640625,\n              38.151837403006766\n            ],\n            [\n              -90.538330078125,\n              38.53957267203905\n            ],\n            [\n              -90.208740234375,\n              38.59970036588819\n            ],\n            [\n              -90.263671875,\n              38.736946065676\n            ],\n            [\n              -90.5712890625,\n              38.796908303484294\n            ],\n            [\n              -90.933837890625,\n              38.53957267203905\n            ],\n            [\n              -91.68090820312499,\n              38.16911413556086\n            ],\n            [\n              -92.032470703125,\n              37.96152331396616\n            ],\n            [\n              -92.032470703125,\n              37.71859032558816\n            ],\n            [\n              -91.593017578125,\n              37.579412513438385\n            ],\n            [\n              -91.62597656249999,\n              37.142803443716836\n            ],\n            [\n              -91.219482421875,\n              36.8092847020594\n            ],\n            [\n              -90.8349609375,\n              36.53612263184686\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"56","issue":"12","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2011-08-24","publicationStatus":"PW","scienceBaseUri":"558bd4c2e4b0b6d21dd6532b","contributors":{"authors":[{"text":"Westhoff, Jacob T.","contributorId":58106,"corporation":false,"usgs":true,"family":"Westhoff","given":"Jacob","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":556721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rabeni, C.F.","contributorId":67823,"corporation":false,"usgs":true,"family":"Rabeni","given":"C.F.","affiliations":[],"preferred":false,"id":556797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sowa, S.P.","contributorId":43142,"corporation":false,"usgs":true,"family":"Sowa","given":"S.P.","affiliations":[],"preferred":false,"id":556798,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70154836,"text":"70154836 - 2011 - Adaptive management of bull trout populations in the Lemhi Basin","interactions":[],"lastModifiedDate":"2022-11-14T17:45:59.759906","indexId":"70154836","displayToPublicDate":"2011-12-01T00:00:00","publicationYear":"2011","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":"Adaptive management of bull trout populations in the Lemhi Basin","docAbstract":"<p><span>The bull trout&nbsp;</span><i>Salvelinus confluentus</i><span>, a stream-living salmonid distributed in drainages of the northwestern United States, is listed as threatened under the Endangered Species Act because of rangewide declines. One proposed recovery action is the reconnection of tributaries in the Lemhi Basin. Past water use policies in this core area disconnected headwater spawning sites from downstream habitat and have led to the loss of migratory life history forms. We developed an adaptive management framework to analyze which types of streams should be prioritized for reconnection under a proposed Habitat Conservation Plan. We developed a Stochastic Dynamic Program that identified optimal policies over time under four different assumptions about the nature of the migratory behavior and the effects of brook trout&nbsp;</span><i>Salvelinus fontinalis</i><span>&nbsp;on subpopulations of bull trout. In general, given the current state of the system and the uncertainties about the dynamics, the optimal policy would be to connect streams that are currently occupied by bull trout. We also estimated the value of information as the difference between absolute certainty about which of our four assumptions were correct, and a model averaged optimization assuming no knowledge. Overall there is little to be gained by learning about the dynamics of the system in its current state, although in other parts of the state space reducing uncertainties about the system would be very valuable. We also conducted a sensitivity analysis; the optimal decision at the current state does not change even when parameter values are changed up to 75% of the baseline values. Overall, the exercise demonstrates that it is possible to apply adaptive management principles to threatened and endangered species, but logistical and data availability constraints make detailed analyses difficult.</span></p>","language":"English","publisher":"U.S. Fish and Wildlife Service","doi":"10.3996/022011-JFWM-012","usgsCitation":"Tyre, A.J., Peterson, J., Converse, S.J., Bogich, T., Miller, D., Post van der Burg, M., Thomas, C., Thompson, R.J., Wood, J., Brewer, D., and Runge, M.C., 2011, Adaptive management of bull trout populations in the Lemhi Basin: Journal of Fish and Wildlife Management, v. 2, no. 2, p. 262-281, https://doi.org/10.3996/022011-JFWM-012.","productDescription":"20 p.","startPage":"262","endPage":"281","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-020782","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true},{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":306555,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lemhi River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.09459430368548,\n              44.69654927506963\n            ],\n            [\n              -116.58786687508034,\n              45.542245957883324\n            ],\n            [\n              -116.96788815899754,\n              42.73181816081549\n            ],\n            [\n              -113.5842371118099,\n              42.3927075503361\n            ],\n            [\n              -113.09459430368548,\n              44.69654927506963\n            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0000-0002-3719-5441 sconverse@usgs.gov","orcid":"https://orcid.org/0000-0002-3719-5441","contributorId":3513,"corporation":false,"usgs":true,"family":"Converse","given":"Sarah","email":"sconverse@usgs.gov","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":567705,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bogich, Tiffany L.","contributorId":40891,"corporation":false,"usgs":true,"family":"Bogich","given":"Tiffany L.","affiliations":[],"preferred":false,"id":567706,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, Damien","contributorId":146390,"corporation":false,"usgs":false,"family":"Miller","given":"Damien","email":"","affiliations":[],"preferred":false,"id":567707,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Post van der Burg, Max 0000-0002-3943-4194 maxpostvanderburg@usgs.gov","orcid":"https://orcid.org/0000-0002-3943-4194","contributorId":4947,"corporation":false,"usgs":true,"family":"Post van der Burg","given":"Max","email":"maxpostvanderburg@usgs.gov","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":567708,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Thomas, Carmen","contributorId":146391,"corporation":false,"usgs":false,"family":"Thomas","given":"Carmen","email":"","affiliations":[],"preferred":false,"id":567709,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Thompson, Ralph J.","contributorId":96837,"corporation":false,"usgs":true,"family":"Thompson","given":"Ralph","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":567710,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Wood, Jeri stefanie_stavrakas@fws.gov","contributorId":146392,"corporation":false,"usgs":false,"family":"Wood","given":"Jeri","email":"stefanie_stavrakas@fws.gov","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":567711,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Brewer, Donna","contributorId":146394,"corporation":false,"usgs":false,"family":"Brewer","given":"Donna","email":"","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":567712,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Runge, Michael C. 0000-0002-8081-536X mrunge@usgs.gov","orcid":"https://orcid.org/0000-0002-8081-536X","contributorId":3358,"corporation":false,"usgs":true,"family":"Runge","given":"Michael","email":"mrunge@usgs.gov","middleInitial":"C.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":567713,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70236055,"text":"70236055 - 2011 - Hydrologic conditions and terrestrial laser scanning of post-firedebris flows in the San Gabriel Mountains, CA, U.S.A","interactions":[],"lastModifiedDate":"2022-08-29T11:05:22.209441","indexId":"70236055","displayToPublicDate":"2011-11-30T10:32:39","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2122,"text":"Italian Journal of Engineering Geology and Environment","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic conditions and terrestrial laser scanning of post-firedebris flows in the San Gabriel Mountains, CA, U.S.A","docAbstract":"<p><span>To investigate rainfall-runoff conditions that generate post-wildfire debris flows, we instrumented and surveyed steep, small watersheds along the tectonically active front of the San Gabriel Mountains, California. Fortuitously, we recorded runoff-generated debris-flows triggered by one spatially restricted convective event with 28 mm of rainfall falling over 62 minutes. Our rain gages, nested hillslope overland-flow sensors and soil-moisture probes, as well as a time series of terrestrial laser scanning (TLS) revealed the effects of the storm. Hillslope overland-flow response, along two ~10-m long flow lines perpendicular to and originating from a drainage divide, displayed only a 10 to 20 minute delay from the onset of rainfall with accumulated totals of merely 5-10 mm. Depth-stratified soil-moisture probes displayed a greater time delay, roughly 20- 30 minutes, indicating that initial overland flow was Hortonian. Furthermore, a downstream channel-monitoring array recorded a pronounced discharge peak generated by the passage of a debris flow after 18 minutes of rainfall. At this time, only four of the eleven hillslope overland flow sensors confirmed the presence of surface-water flow. Repeat TLS and detailed field mapping using GPS document how patterns of rainsplash, overland-flow scour, and rilling contributed to the generation of metter-scale debris flows. In response to a single small storm, the debris flows deposited irregular levees and lobate terminal snouts on hillslopes and caused wide- spread erosion of the valley axis with ground surface lowering exceeding 1.5 m.</span></p>","conferenceTitle":"5th International Conference on Debris-Flow Hazards Mitigation: Mechanics, Prediction and Assessment","conferenceDate":"June 14-17, 2011","conferenceLocation":"Padua, Italy","language":"English","publisher":"Sapienza Università di Roma","doi":"10.4408/IJEGE.2011-03.B-064","usgsCitation":"Schmidt, K., Hanshaw, M.N., Howle, J., Kean, J., Staley, D.M., Stock, J., and Bawdeng, W., 2011, Hydrologic conditions and terrestrial laser scanning of post-firedebris flows in the San Gabriel Mountains, CA, U.S.A: Italian Journal of Engineering Geology and Environment, p. 583-593, https://doi.org/10.4408/IJEGE.2011-03.B-064.","productDescription":"11 p.","startPage":"583","endPage":"593","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":405686,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Gabriel Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.3172607421875,\n              34.116352469972746\n            ],\n            [\n              -117.44384765625,\n              34.116352469972746\n            ],\n            [\n              -117.44384765625,\n              34.53371242139564\n            ],\n            [\n              -118.3172607421875,\n              34.53371242139564\n            ],\n            [\n              -118.3172607421875,\n              34.116352469972746\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schmidt, K. M. 0000-0003-2365-8035","orcid":"https://orcid.org/0000-0003-2365-8035","contributorId":59830,"corporation":false,"usgs":true,"family":"Schmidt","given":"K. M.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":849861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanshaw, M. N. 0000-0001-9305-307X","orcid":"https://orcid.org/0000-0001-9305-307X","contributorId":56462,"corporation":false,"usgs":true,"family":"Hanshaw","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":849862,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howle, J. F. 0000-0003-0491-6203","orcid":"https://orcid.org/0000-0003-0491-6203","contributorId":66294,"corporation":false,"usgs":true,"family":"Howle","given":"J. F.","affiliations":[],"preferred":false,"id":849863,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kean, J. W. 0000-0003-3089-0369","orcid":"https://orcid.org/0000-0003-3089-0369","contributorId":71679,"corporation":false,"usgs":true,"family":"Kean","given":"J. W.","affiliations":[],"preferred":false,"id":849864,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Staley, Dennis M. 0000-0002-2239-3402 dstaley@usgs.gov","orcid":"https://orcid.org/0000-0002-2239-3402","contributorId":4134,"corporation":false,"usgs":true,"family":"Staley","given":"Dennis","email":"dstaley@usgs.gov","middleInitial":"M.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":849865,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stock, J. D. 0000-0001-8565-3577","orcid":"https://orcid.org/0000-0001-8565-3577","contributorId":79998,"corporation":false,"usgs":true,"family":"Stock","given":"J. D.","affiliations":[],"preferred":false,"id":849866,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bawdeng, W.","contributorId":295737,"corporation":false,"usgs":true,"family":"Bawdeng","given":"W.","email":"","affiliations":[],"preferred":false,"id":849867,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70005858,"text":"70005858 - 2011 - Salinity tolerance of non-native suckermouth armoured catfish (Loricariidae: Pterygoplichthys) in south-eastern Mexico: Implications for invasion and dispersal","interactions":[],"lastModifiedDate":"2021-01-06T13:23:34.787591","indexId":"70005858","displayToPublicDate":"2011-11-30T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":862,"text":"Aquatic Conservation: Marine and Freshwater Ecosystems","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Salinity tolerance of non-native suckermouth armoured catfish (<i>Loricariidae</i>: Pterygoplichthys) in south-eastern Mexico: Implications for invasion and dispersal","title":"Salinity tolerance of non-native suckermouth armoured catfish (Loricariidae: Pterygoplichthys) in south-eastern Mexico: Implications for invasion and dispersal","docAbstract":"<p><strong>1.</strong> Salinity tolerance is one of several important physiological attributes that determine invasion success and the pattern of dispersal of introduced aquatic organisms. Introduced freshwater fishes able to tolerate elevated salinities have the potential to invade and exploit brackish-water (mixohaline) environments and use estuaries and coastal waters as 'bridges' for dispersing from one coastal river system to another. </p><p><strong>2.</strong> Several members of the neotropical suckermouth armoured catfish genus <i>Pterygoplichthys</i> (Siluriformes: Loricariidae) have established non-native populations in inland waters of North and Central America, Asia and islands in the Caribbean, and Pacific and Indian oceans. Loricariids are generally considered to be strictly freshwater; but a few naturally occur in mesohaline habitats. </p><p><strong>3.</strong>Catch and habitat data from 2004–2005 and 2009–2011 fish surveys in the Grijalva–Usumacinta River delta region (south-eastern Mexico) confirmed that introduced <i>Pterygoplichthys</i> populations established in upstream freshwater sites (where these catfish are abundant) have recently dispersed into downstream oligohaline and mesohaline estuarine habitats. During 2009–2011 surveys, these non-native catfish — tentatively identified as <i>P. pardalis</i> or its hybrids — were found in sites with salinities ranging from 1 to 8 ppt (mean 5.2 ppt). </p><p><strong>4.</strong>Acute-salinity experiments were conducted with <i>Pterygoplichthys</i> (110–302 mm standard length, <i>N</i>=140) captured in the Grijalva–Usumacinta Basin to determine upper salinity tolerance levels. Tests demonstrated that individuals maintained in salinities of 0.2 ppt were able to survive abrupt (acute) exposure to salinities up to 10 ppt with little mortality over 10 days (240 h experimental endpoint). A few individuals survived abrupt exposure to 11 and 12 ppt for 20 or more hours, although none survived more than a few hours at 16 ppt or greater. </p><p><strong>5.</strong>These field and experimental results provide quantitative evidence that non-native <i>Pterygoplichthys</i> are physiologically capable of surviving mesohaline conditions for extended periods and that non-native populations in Mexico are invading and presumably exploiting estuarine and other coastal environments, perhaps as feeding areas and potentially as dispersal routes.</p>","language":"English","publisher":"Wiley","publisherLocation":"Amsterdam, Netherlands","doi":"10.1002/aqc.1210","usgsCitation":"Capps, K.A., Nico, L.G., Mendoza-Carranza, M., Arevalo-Frias, W., Ropicki, A., Heilpern, S.A., and Rodiles-Hernandez, R., 2011, Salinity tolerance of non-native suckermouth armoured catfish (Loricariidae: Pterygoplichthys) in south-eastern Mexico: Implications for invasion and dispersal: Aquatic Conservation: Marine and Freshwater Ecosystems, v. 21, no. 6, p. 528-540, https://doi.org/10.1002/aqc.1210.","productDescription":"13 p.","startPage":"528","endPage":"540","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":204481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","otherGeospatial":"Grijalva–Usumacinta River delta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.79876708984375,\n              17.79838094162093\n            ],\n            [\n              -91.77017211914062,\n              17.79838094162093\n            ],\n            [\n              -91.77017211914062,\n              18.777616176328035\n            ],\n            [\n              -92.79876708984375,\n              18.777616176328035\n            ],\n            [\n              -92.79876708984375,\n              17.79838094162093\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"6","noUsgsAuthors":false,"publicationDate":"2011-09-27","publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644725","contributors":{"authors":[{"text":"Capps, Krista A.","contributorId":35456,"corporation":false,"usgs":true,"family":"Capps","given":"Krista","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":353412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nico, Leo G. 0000-0002-4488-7737 lnico@usgs.gov","orcid":"https://orcid.org/0000-0002-4488-7737","contributorId":2913,"corporation":false,"usgs":true,"family":"Nico","given":"Leo","email":"lnico@usgs.gov","middleInitial":"G.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":353410,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mendoza-Carranza, Manuel","contributorId":74870,"corporation":false,"usgs":true,"family":"Mendoza-Carranza","given":"Manuel","email":"","affiliations":[],"preferred":false,"id":353414,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arevalo-Frias, Wendi","contributorId":69703,"corporation":false,"usgs":true,"family":"Arevalo-Frias","given":"Wendi","email":"","affiliations":[],"preferred":false,"id":353413,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ropicki, Andrew J.","contributorId":6181,"corporation":false,"usgs":true,"family":"Ropicki","given":"Andrew J.","affiliations":[],"preferred":false,"id":353411,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Heilpern, Sebastian A.","contributorId":80003,"corporation":false,"usgs":true,"family":"Heilpern","given":"Sebastian","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":353415,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rodiles-Hernandez, Rocio","contributorId":80403,"corporation":false,"usgs":true,"family":"Rodiles-Hernandez","given":"Rocio","email":"","affiliations":[],"preferred":false,"id":353416,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70006010,"text":"70006010 - 2011 - Occurrence of antibiotic resistance and characterization of resistant genes and integrons in Enterobacteriaceae isolated from integrated fish farms south China","interactions":[],"lastModifiedDate":"2021-04-29T18:31:00.477796","indexId":"70006010","displayToPublicDate":"2011-11-25T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2259,"text":"Journal of Environmental Monitoring","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of antibiotic resistance and characterization of resistant genes and integrons in Enterobacteriaceae isolated from integrated fish farms south China","docAbstract":"<div class=\"capsule__text\"><p>Antibiotics<span>&nbsp;</span>are still widely applied in animal husbandry to prevent diseases and used as feed additives to promote animal growth. This could result in<span>&nbsp;</span>antibiotic<span>&nbsp;</span>resistance to bacteria and<span>&nbsp;</span>antibiotic<span>&nbsp;</span>residues in animals. In this paper, Enterobacteriaceae isolated from four integrated fish farms in Zhongshan, South China were tested for<span>&nbsp;</span>antibiotic<span>&nbsp;</span>resistance,<span>&nbsp;</span>tetracycline<span>&nbsp;</span>resistance genes,<span>&nbsp;</span>sulfonamide<span>&nbsp;</span>resistance genes, and class 1 integrons. The Kirby-Bauer disk diffusion method and polymerase<span>&nbsp;</span>chain reaction<span>&nbsp;</span>(PCR) assays were carried out to test<span>&nbsp;</span>antibiotic<span>&nbsp;</span>susceptibility and resistance genes, respectively. Relatively high<span>&nbsp;</span>antibiotic<span>&nbsp;</span>resistance frequencies were found, especially for ampicillin (80%),<span>&nbsp;</span>tetracycline<span>&nbsp;</span>(52%), and<span>&nbsp;</span>trimethoprim<span>&nbsp;</span>(50%). Out of 203 Enterobacteriaceae isolates, 98.5% were resistant to one or more<span>&nbsp;</span>antibiotics<span>&nbsp;</span>tested. Multiple<span>&nbsp;</span>antibiotic<span>&nbsp;</span>resistance (MAR) was found highest in animal manures with a MAR index of 0.56.<span>&nbsp;</span>Tetracycline<span>&nbsp;</span>resistance genes (<i>tet</i>(A),<span>&nbsp;</span><i>tet</i>(C)) and<span>&nbsp;</span>sulfonamide<span>&nbsp;</span>resistance genes (<i>sul2</i>) were detected in more than 50% of the isolates. The<span>&nbsp;</span><i>intI1</i>gene was found in 170 isolates (83.7%). Both classic and non-classic class 1 integrons were found. Four genes,<span>&nbsp;</span><i>aadA5</i>,<span>&nbsp;</span><i>aadA22</i>,<span>&nbsp;</span><i>dfr2</i>, and<span>&nbsp;</span><i>dfrA17</i>, were detected. To our knowledge, this is the first report for molecular characterization of<span>&nbsp;</span>antibiotic<span>&nbsp;</span>resistance genes in Enterobacteriaceae isolated from integrated fish farms in China and the first time that gene cassette array<i>dfrA17-aadA5</i><span>&nbsp;</span>has been detected in such fish farms. Results of this study indicated that fish farms may be a reservoir of highly diverse and abundant<span>&nbsp;</span>antibiotic<span>&nbsp;</span>resistant genes and gene cassettes. Integrons may play a key role in multiple<span>&nbsp;</span>antibiotic<span>&nbsp;</span>resistances posing potential health risks to the general public and aquaculture.</p></div>","language":"English","publisher":"Royal Society of Chemistry Publishing","doi":"10.1039/C1EM10634A","usgsCitation":"Su, H., Ying, G., Tao, R., Zhang, R., Fogarty, L.R., and Kolpin, D.W., 2011, Occurrence of antibiotic resistance and characterization of resistant genes and integrons in Enterobacteriaceae isolated from integrated fish farms south China: Journal of Environmental Monitoring, v. 13, no. 11, p. 3229-3236, https://doi.org/10.1039/C1EM10634A.","productDescription":"8 p.","startPage":"3229","endPage":"3236","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":204361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","city":"Zhongshan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              112.7362060546875,\n              22.06527806776582\n            ],\n            [\n              113.6260986328125,\n              22.06527806776582\n            ],\n            [\n              113.6260986328125,\n              22.983681160330878\n            ],\n            [\n              112.7362060546875,\n              22.983681160330878\n            ],\n            [\n              112.7362060546875,\n              22.06527806776582\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692521","contributors":{"authors":[{"text":"Su, Hao-Chang","contributorId":24083,"corporation":false,"usgs":true,"family":"Su","given":"Hao-Chang","email":"","affiliations":[],"preferred":false,"id":353660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ying, Guang-Guo","contributorId":6576,"corporation":false,"usgs":true,"family":"Ying","given":"Guang-Guo","affiliations":[],"preferred":false,"id":353659,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tao, Ran","contributorId":63519,"corporation":false,"usgs":true,"family":"Tao","given":"Ran","email":"","affiliations":[],"preferred":false,"id":353661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zhang, Rui-Quan","contributorId":103786,"corporation":false,"usgs":true,"family":"Zhang","given":"Rui-Quan","email":"","affiliations":[],"preferred":false,"id":353662,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fogarty, Lisa R. 0000-0003-0329-3251 lrfogart@usgs.gov","orcid":"https://orcid.org/0000-0003-0329-3251","contributorId":2053,"corporation":false,"usgs":true,"family":"Fogarty","given":"Lisa","email":"lrfogart@usgs.gov","middleInitial":"R.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":false,"id":353658,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353657,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70006046,"text":"sir20115138 - 2011 - Observed and forecast flood-inundation mapping application-A pilot study of an eleven-mile reach of the White River, Indianapolis, Indiana","interactions":[],"lastModifiedDate":"2016-06-01T08:40:43","indexId":"sir20115138","displayToPublicDate":"2011-11-23T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2011-5138","title":"Observed and forecast flood-inundation mapping application-A pilot study of an eleven-mile reach of the White River, Indianapolis, Indiana","docAbstract":"<p>Near-real-time and forecast flood-inundation mapping products resulted from a pilot study for an 11-mile reach of the White River in Indianapolis. The study was done by the U.S. Geological Survey (USGS), Indiana Silver Jackets hazard mitigation taskforce members, the National Weather Service (NWS), the Polis Center, and Indiana University, in cooperation with the City of Indianapolis, the Indianapolis Museum of Art, the Indiana Department of Homeland Security, and the Indiana Department of Natural Resources, Division of Water. The pilot project showed that it is technically feasible to create a flood-inundation map library by means of a two-dimensional hydraulic model, use a map from the library to quickly complete a moderately detailed local flood-loss estimate, and automatically run the hydraulic model during a flood event to provide the maps and flood-damage information through a Web graphical user interface. A library of static digital flood-inundation maps was created by means of a calibrated two-dimensional hydraulic model. Estimated water-surface elevations were developed for a range of river stages referenced to a USGS streamgage and NWS flood forecast point colocated within the study reach. These maps were made available through the Internet in several formats, including geographic information system, Keyhole Markup Language, and Portable Document Format. A flood-loss estimate was completed for part of the study reach by using one of the flood-inundation maps from the static library. The Federal Emergency Management Agency natural disaster-loss estimation program HAZUS-MH, in conjunction with local building information, was used to complete a level 2 analysis of flood-loss estimation. A Service-Oriented Architecture-based dynamic flood-inundation application was developed and was designed to start automatically during a flood, obtain near real-time and forecast data (from the colocated USGS streamgage and NWS flood forecast point within the study reach), run the two-dimensional hydraulic model, and produce flood-inundation maps. The application used local building data and depth-damage curves to estimate flood losses based on the maps, and it served inundation maps and flood-loss estimates through a Web-based graphical user interface.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115138","collaboration":"Prepared in cooperation with the City of Indianapolis, the Indianapolis Museum of Art, the Indiana Department of Homeland Security, and the Indiana Department of Natural Resources, Division of Water","usgsCitation":"Kim, M.H., Morlock, S.E., Arihood, L.D., and Kiesler, J.L., 2011, Observed and forecast flood-inundation mapping application-A pilot study of an eleven-mile reach of the White River, Indianapolis, Indiana: U.S. Geological Survey Scientific Investigations Report 2011-5138, viii, 25 p.; Appendices, https://doi.org/10.3133/sir20115138.","productDescription":"viii, 25 p.; 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696419","contributors":{"authors":[{"text":"Kim, Moon H. 0000-0002-4328-8409 mkim@usgs.gov","orcid":"https://orcid.org/0000-0002-4328-8409","contributorId":3211,"corporation":false,"usgs":true,"family":"Kim","given":"Moon","email":"mkim@usgs.gov","middleInitial":"H.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morlock, Scott E. smorlock@usgs.gov","contributorId":3212,"corporation":false,"usgs":true,"family":"Morlock","given":"Scott","email":"smorlock@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":353723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arihood, Leslie D. 0000-0001-5792-3699 larihood@usgs.gov","orcid":"https://orcid.org/0000-0001-5792-3699","contributorId":2357,"corporation":false,"usgs":true,"family":"Arihood","given":"Leslie","email":"larihood@usgs.gov","middleInitial":"D.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353721,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kiesler, James L. jkiesler@usgs.gov","contributorId":4470,"corporation":false,"usgs":true,"family":"Kiesler","given":"James","email":"jkiesler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":353724,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003717,"text":"70003717 - 2011 - Regional geomorphology and history of Titan's Xanadu province","interactions":[],"lastModifiedDate":"2021-02-26T15:57:19.721227","indexId":"70003717","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Regional geomorphology and history of Titan's Xanadu province","docAbstract":"<p><span>Titan’s enigmatic Xanadu province has been seen in some detail with instruments from the Cassini spacecraft. The region contains some of the most rugged, mountainous terrain on Titan, with relief over 2000</span><span>&nbsp;</span><span>m. Xanadu contains evolved and integrated river channels, impact&nbsp;<a title=\"Learn more about Crater from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/crater\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/crater\">craters</a>, and dry basins filled with smooth, radar-dark material, perhaps sediments from past&nbsp;<a title=\"Learn more about Bed (Geology) from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/bed-geology\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/bed-geology\">lake beds</a>. Arcuate and aligned mountain chains give evidence of compressional tectonism, yet the overall elevation of Xanadu is puzzlingly low compared to surrounding sand seas.&nbsp;<a title=\"Learn more about Lineation from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/lineation\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/lineation\">Lineations</a>&nbsp;associated with mountain fronts and valley floors give evidence of extension that probably contributed to this regional lowering. Several locations on Xanadu’s western and southern margins contain flow-like features that may be cryovolcanic in origin, perhaps ascended from lithospheric faults related to regional downdropping late in its history. Radiometry and scatterometry observations are consistent with a water–ice or water–ammonia–ice composition to its exposed, eroded, fractured bedrock; both microwave and visible to&nbsp;<a title=\"Learn more about Near Infrared from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/near-infrared\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/near-infrared\">near-infrared</a>&nbsp;(v-nIR) data indicate a thin overcoating of organics, likely derived from the atmosphere. We suggest Xanadu is one of the oldest terrains on Titan and that its origin and evolution have been controlled and shaped by compressional and then extensional tectonism in the icy crust and ongoing erosion by methane rainfall.</span></p>","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.icarus.2010.07.022","usgsCitation":"Radebaugh, J., Lorenz, R.D., Wall, S.D., Kirk, R.L., Wood, C.A., Lunine, J., Stofan, E.R., Lopes, R., Valora, P., Farr, T., Hayes, A., Stiles, B., Mitri, G., Zebker, H., Janssen, M., Wye, L., LeGall, A., Mitchell, K.L., Paganelli, F., West, R., Schaller, E., and The Cassini Radar Team, 2011, Regional geomorphology and history of Titan's Xanadu province: Icarus, v. 211, no. 1, p. 672-685, https://doi.org/10.1016/j.icarus.2010.07.022.","productDescription":"13 p.","startPage":"672","endPage":"685","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":204281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Titan, Xanadu province","volume":"211","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c57b","contributors":{"authors":[{"text":"Radebaugh, J.","contributorId":34639,"corporation":false,"usgs":false,"family":"Radebaugh","given":"J.","affiliations":[],"preferred":false,"id":348475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorenz, R. D.","contributorId":90441,"corporation":false,"usgs":false,"family":"Lorenz","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":348487,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wall, S. D.","contributorId":86468,"corporation":false,"usgs":false,"family":"Wall","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":348486,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kirk, R. L.","contributorId":94698,"corporation":false,"usgs":true,"family":"Kirk","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":348488,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wood, C. A.","contributorId":35057,"corporation":false,"usgs":false,"family":"Wood","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":348477,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lunine, J. I.","contributorId":51899,"corporation":false,"usgs":false,"family":"Lunine","given":"J. I.","affiliations":[],"preferred":false,"id":348481,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stofan, E. R.","contributorId":103403,"corporation":false,"usgs":false,"family":"Stofan","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":348490,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lopes, R M.C.","contributorId":31634,"corporation":false,"usgs":true,"family":"Lopes","given":"R M.C.","affiliations":[],"preferred":false,"id":348474,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Valora, P.","contributorId":52706,"corporation":false,"usgs":true,"family":"Valora","given":"P.","email":"","affiliations":[],"preferred":false,"id":348482,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Farr, T.G.","contributorId":49932,"corporation":false,"usgs":true,"family":"Farr","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":348480,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Hayes, A.","contributorId":26415,"corporation":false,"usgs":true,"family":"Hayes","given":"A.","affiliations":[],"preferred":false,"id":348473,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Stiles, B.","contributorId":59547,"corporation":false,"usgs":true,"family":"Stiles","given":"B.","email":"","affiliations":[],"preferred":false,"id":348483,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Mitri, Giuseppe","contributorId":35052,"corporation":false,"usgs":false,"family":"Mitri","given":"Giuseppe","email":"","affiliations":[],"preferred":false,"id":348476,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Zebker, H.","contributorId":25276,"corporation":false,"usgs":false,"family":"Zebker","given":"H.","affiliations":[],"preferred":false,"id":348472,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Janssen, M.","contributorId":22893,"corporation":false,"usgs":true,"family":"Janssen","given":"M.","email":"","affiliations":[],"preferred":false,"id":348471,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Wye, L.","contributorId":40333,"corporation":false,"usgs":true,"family":"Wye","given":"L.","affiliations":[],"preferred":false,"id":348479,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"LeGall, A.","contributorId":62735,"corporation":false,"usgs":true,"family":"LeGall","given":"A.","email":"","affiliations":[],"preferred":false,"id":348485,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Mitchell, K. L.","contributorId":62734,"corporation":false,"usgs":false,"family":"Mitchell","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":348484,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Paganelli, F.","contributorId":17353,"corporation":false,"usgs":true,"family":"Paganelli","given":"F.","email":"","affiliations":[],"preferred":false,"id":348469,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"West, R.D.","contributorId":103399,"corporation":false,"usgs":true,"family":"West","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":348489,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Schaller, E.L.","contributorId":22601,"corporation":false,"usgs":true,"family":"Schaller","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":348470,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"The Cassini Radar Team","contributorId":127994,"corporation":true,"usgs":false,"organization":"The Cassini Radar Team","id":535121,"contributorType":{"id":1,"text":"Authors"},"rank":22}]}}
,{"id":70005696,"text":"70005696 - 2011 - Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (Thamnophis rufipunctatus) as revealed by multilocus DNA sequence data","interactions":[],"lastModifiedDate":"2021-05-18T15:33:29.966251","indexId":"70005696","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2774,"text":"Molecular Ecology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (<i>Thamnophis rufipunctatus</i>) as revealed by multilocus DNA sequence data","title":"Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (Thamnophis rufipunctatus) as revealed by multilocus DNA sequence data","docAbstract":"<p><span>Glacial–interglacial cycles of the Pleistocene are hypothesized as one of the foremost contributors to biological diversification. This is especially true for cold‐adapted montane species, where range shifts have had a pronounced effect on population‐level divergence. Gartersnakes of the&nbsp;</span><i>Thamnophis rufipunctatus</i><span>&nbsp;species complex are restricted to cold headwater streams in the highlands of the Sierra Madre Occidental and southwestern USA. We used coalescent and multilocus phylogenetic approaches to test whether genetic diversification of this montane‐restricted species complex is consistent with two prevailing models of range fluctuation for species affected by Pleistocene climate changes. Our concatenated nuDNA and multilocus species analyses recovered evidence for the persistence of multiple lineages that are restricted geographically, despite a mtDNA signature consistent with either more recent connectivity (and introgression) or recent expansion (and incomplete lineage sorting). Divergence times estimated using a relaxed molecular clock and fossil calibrations fall within the Late Pleistocene, and zero gene flow scenarios among current geographically isolated lineages could not be rejected. These results suggest that increased climate shifts in the Late Pleistocene have driven diversification and current range retraction patterns and that the differences between markers reflect the stochasticity of gene lineages (i.e. ancestral polymorphism) rather than gene flow and introgression. These results have important implications for the conservation of&nbsp;</span><i>T.&nbsp;rufipunctatus</i><span>&nbsp;(sensu novo), which is restricted to two drainage systems in the southwestern US and has undergone a recent and dramatic decline.</span></p>","language":"English","publisher":"Wiley","publisherLocation":"Malden, MA","doi":"10.1111/j.1365-294X.2011.05211.x","usgsCitation":"Wood, D.A., Vandergast, A.G., Espinal, A.L., Fisher, R., and Holycross, A., 2011, Refugial isolation and divergence in the Narrowheaded Gartersnake species complex (Thamnophis rufipunctatus) as revealed by multilocus DNA sequence data: Molecular Ecology, v. 20, no. 18, p. 3856-3878, https://doi.org/10.1111/j.1365-294X.2011.05211.x.","productDescription":"23 p.","startPage":"3856","endPage":"3878","numberOfPages":"23","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":204336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"18","noUsgsAuthors":false,"publicationDate":"2011-08-18","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63516f","contributors":{"authors":[{"text":"Wood, Dustin A. 0000-0002-7668-9911 dawood@usgs.gov","orcid":"https://orcid.org/0000-0002-7668-9911","contributorId":4179,"corporation":false,"usgs":true,"family":"Wood","given":"Dustin","email":"dawood@usgs.gov","middleInitial":"A.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vandergast, Amy G. 0000-0002-7835-6571","orcid":"https://orcid.org/0000-0002-7835-6571","contributorId":57201,"corporation":false,"usgs":true,"family":"Vandergast","given":"Amy","middleInitial":"G.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Espinal, A. Lemos","contributorId":81623,"corporation":false,"usgs":false,"family":"Espinal","given":"A.","email":"","middleInitial":"Lemos","affiliations":[],"preferred":false,"id":353080,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fisher, Robert N. 0000-0002-2956-3240","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":51675,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":353077,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Holycross, A.T.","contributorId":79060,"corporation":false,"usgs":false,"family":"Holycross","given":"A.T.","affiliations":[],"preferred":false,"id":353079,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70005590,"text":"70005590 - 2011 - Recovery of little brown bats (Myotis lucifugus) from natural infection with Geomyces destructans, white-nose syndrome","interactions":[],"lastModifiedDate":"2023-10-16T19:08:41.27987","indexId":"70005590","displayToPublicDate":"2011-11-16T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Recovery of little brown bats (<i>Myotis lucifugus</i>) from natural infection with <i>Geomyces destructans</i>, white-nose syndrome","title":"Recovery of little brown bats (Myotis lucifugus) from natural infection with Geomyces destructans, white-nose syndrome","docAbstract":"<p><i>Geomyces destructans</i> produces the white fungal growth on the muzzle and the tacky white discoloration on wings and ears that characterize white-nose syndrome (WNS) in cave-hibernating bats. To test the hypothesis that postemergent WNS-infected bats recover from infection with <i>G. destructans</i>, 30 little brown bats (<i>Myotis lucifugus</i>) were collected in May 2009 from a WNS-affected hibernation site in New Jersey. All bats were confirmed to be infected with <i>G. destructans</i> using a noninvasive fungal tape method to identify the conidia of <i>G. destructans</i> and polymerase chain reaction (PCR). The bats were then held in captivity and given supportive care for 70 days. Of the 26 bats that survived and were humanely killed after 70 days, 25 showed significant improvement in the external appearance of wing membranes, had no microscopic evidence of infection by <i>G. destructans</i>, and had wing tissue samples that were negative for <i>G. destructans</i> by PCR. A subset of the bats was treated topically at the beginning of the rehabilitation study with a dilute vinegar solution, but treatment with vinegar provided no added advantage to recovery. Provision of supportive care to homeothermic bats was sufficient for full recovery from WNS. One bat at day 70 still had both gross pathology and microscopic evidence of WNS in wing membranes and was PCR-positive for <i>G. destructans</i>. Dense aggregates of neutrophils surrounded the hyphae that remained in the wing membrane of this bat.</p>","language":"English","publisher":"Wildlife Disease Association","publisherLocation":"Lawrence, KS","doi":"10.7589/0090-3558-47.3.618","usgsCitation":"Meteyer, C.U., Valent, M., Kashmer, J., Buckles, E.L., Lorch, J.M., Blehert, D., Lollar, A., Berndt, D., Wheeler, E., White, C.L., and Ballmann, A.E., 2011, Recovery of little brown bats (Myotis lucifugus) from natural infection with Geomyces destructans, white-nose syndrome: Journal of Wildlife Diseases, v. 47, no. 3, p. 618-626, https://doi.org/10.7589/0090-3558-47.3.618.","productDescription":"9 p.","startPage":"618","endPage":"626","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-025621","costCenters":[{"id":456,"text":"National Wildlife Health 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,{"id":70003670,"text":"70003670 - 2011 - Rapid cooling rates at an active mid-ocean ridge from zircon thermochronology","interactions":[],"lastModifiedDate":"2021-01-07T21:26:35.20802","indexId":"70003670","displayToPublicDate":"2011-11-09T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Rapid cooling rates at an active mid-ocean ridge from zircon thermochronology","docAbstract":"<p><span>Oceanic spreading ridges are Earth's most productive crust generating environment, but mechanisms and rates of crustal accretion and heat loss are debated. Existing observations on cooling rates are ambiguous regarding the prevalence of conductive vs. convective cooling of lower oceanic crust. Here, we report the discovery and dating of zircon in mid-ocean ridge dacite lavas that constrain magmatic differentiation and cooling rates at an active spreading center. Dacitic lavas erupted on the southern Cleft segment of the Juan de Fuca ridge, an intermediate-rate spreading center, near the intersection with the Blanco transform fault. Their U–Th zircon crystallization ages (29.3</span><sub>−&nbsp;4.6</sub><sup>+&nbsp;4.8</sup><span>&nbsp;</span><span>ka; 1σ standard error s.e.) overlap with the (U–Th)/He zircon eruption age (32.7</span><span>&nbsp;</span><span>±</span><span>&nbsp;</span><span>1.6</span><span>&nbsp;</span><span>ka) within uncertainty. Based on similar&nbsp;</span><sup>238</sup><span>U−</span><sup>230</sup><span>Th disequilibria between southern Cleft dacite glass separates and young mid-ocean ridge basalt (MORB) erupted nearby, differentiation must have occurred rapidly, within ~</span><span>&nbsp;</span><span>10–20</span><span>&nbsp;</span><span>ka at most. Ti-in-zircon thermometry indicates crystallization at 850–900</span><span>&nbsp;</span><span>°C and pressures &gt;</span><span>&nbsp;</span><span>70–150</span><span>&nbsp;</span><span>MPa are calculated from H</span><sub>2</sub><span>O solubility models. These time-temperature constraints translate into a magma cooling rate of ~</span><span>&nbsp;</span><span>2</span><span>&nbsp;</span><span>×</span><span>&nbsp;</span><span>10</span><sup>−&nbsp;2</sup><span>&nbsp;</span><span>°C/a. This rate is at least one order-of-magnitude faster than those calculated for zircon-bearing plutonic rocks from slow spreading ridges. Such short intervals for differentiation and cooling can only be resolved through uranium-series (</span><sup>238</sup><span>U–</span><sup>230</sup><span>Th) decay in young lavas, and are best explained by dissipating heat convectively at high crustal permeability.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.epsl.2010.12.022","usgsCitation":"Schmitt, A., Perfit, M.R., Rubin, K.H., Stockli, D.F., Smith, M.C., Cotsonika, L.A., Zellmer, G.F., and Ridley, W., 2011, Rapid cooling rates at an active mid-ocean ridge from zircon thermochronology: Earth and Planetary Science Letters, v. 302, no. 3-4, p. 349-358, https://doi.org/10.1016/j.epsl.2010.12.022.","productDescription":"10 p.","startPage":"349","endPage":"358","numberOfPages":"10","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":204189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Juan de Fuca ridge and the Blanco transform fault intersection","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -132.5830078125,\n              42.13082130188811\n            ],\n            [\n              -124.8046875,\n              42.13082130188811\n            ],\n            [\n              -124.8046875,\n              50.875311142200765\n            ],\n            [\n              -132.5830078125,\n              50.875311142200765\n            ],\n            [\n              -132.5830078125,\n              42.13082130188811\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"302","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649443","contributors":{"authors":[{"text":"Schmitt, Axel K.","contributorId":69287,"corporation":false,"usgs":true,"family":"Schmitt","given":"Axel K.","affiliations":[],"preferred":false,"id":348262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perfit, Michael R.","contributorId":29123,"corporation":false,"usgs":true,"family":"Perfit","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":348260,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, Kenneth H.","contributorId":90864,"corporation":false,"usgs":true,"family":"Rubin","given":"Kenneth","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":348264,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stockli, Daniel F.","contributorId":78073,"corporation":false,"usgs":true,"family":"Stockli","given":"Daniel","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":348263,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, Matthew C.","contributorId":32287,"corporation":false,"usgs":true,"family":"Smith","given":"Matthew","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":348261,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cotsonika, Laurie A.","contributorId":98869,"corporation":false,"usgs":true,"family":"Cotsonika","given":"Laurie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":348266,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Zellmer, Georg F.","contributorId":93615,"corporation":false,"usgs":true,"family":"Zellmer","given":"Georg","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":348265,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ridley, W. Ian 0000-0001-6787-558X","orcid":"https://orcid.org/0000-0001-6787-558X","contributorId":17269,"corporation":false,"usgs":true,"family":"Ridley","given":"W. Ian","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":348259,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70005002,"text":"70005002 - 2011 - Quantifying differences in the impact of variable chemistry on equilibrium uranium(VI) adsorption properties of aquifer sediments","interactions":[],"lastModifiedDate":"2020-01-11T10:58:03","indexId":"70005002","displayToPublicDate":"2011-11-09T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Quantifying differences in the impact of variable chemistry on equilibrium uranium(VI) adsorption properties of aquifer sediments","docAbstract":"Uranium adsorption-desorption on sediment samples collected from the Hanford 300-Area, Richland, WA varied extensively over a range of field-relevant chemical conditions, complicating assessment of possible differences in equilibrium adsorption properties. Adsorption equilibrium was achieved in 500-1000 h although dissolved uranium concentrations increased over thousands of hours owing to changes in aqueous chemical composition driven by sediment-water reactions. A nonelectrostatic surface complexation reaction, >SOH + UO<sub>2</sub><sup>2+</sup> + 2CO<sub>3</sub><sup>2-</sup> = >SOUO<sub>2</sub>(CO<sub>3</sub>HCO<sub>3</sub>)<sup>2-</sup>, provided the best fit to experimental data for each sediment sample resulting in a range of conditional equilibrium constants (log<i>K</i><sup>c</sup>) from 21.49 to 21.76. Potential differences in uranium adsorption properties could be assessed in plots based on the generalized mass-action expressions yielding linear trends displaced vertically by differences in log<i>K</i><sup>c</sup> values. Using this approach, log<i>K</i><sup>c</sup> values for seven sediment samples were not significantly different. However, a significant difference in adsorption properties between one sediment sample and the fines (<0.063 mm) of another could be demonstrated despite the fines requiring a different reaction stoichiometry. Estimates of log<i>K</i><sup>c</sup> uncertainty were improved by capturing all data points within experimental errors. The mass-action expression plots demonstrate that applying models outside the range of conditions used in model calibration greatly increases potential errors.","language":"English","publisher":"ACS Publications","doi":"10.1021/es202677v","usgsCitation":"Stoliker, D., Kent, D.B., and Zachara, J.M., 2011, Quantifying differences in the impact of variable chemistry on equilibrium uranium(VI) adsorption properties of aquifer sediments: Environmental Science & Technology, v. 45, no. 20, p. 8733-8740, https://doi.org/10.1021/es202677v.","productDescription":"8 p.","startPage":"8733","endPage":"8740","costCenters":[{"id":148,"text":"Branch of Regional Research-Western Region","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":474902,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1021/es202677v","text":"Publisher Index Page"},{"id":204491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","county":"Benton County","city":"Richland","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-119.4525,46.6777],[-119.4572,46.6727],[-119.4487,46.6662],[-119.4461,46.6643],[-119.4428,46.662],[-119.4376,46.6597],[-119.4297,46.6578],[-119.4224,46.6573],[-119.4152,46.6535],[-119.4068,46.6402],[-119.4102,46.6338],[-119.4123,46.6283],[-119.4085,46.6195],[-119.4059,46.6149],[-119.402,46.6108],[-119.3948,46.6071],[-119.3896,46.6001],[-119.3805,46.5936],[-119.372,46.5849],[-119.355,46.5751],[-119.3491,46.5723],[-119.3426,46.5695],[-119.3341,46.5653],[-119.3243,46.5597],[-119.3191,46.5546],[-119.3139,46.5491],[-119.3107,46.5444],[-119.3041,46.5393],[-119.2924,46.5333],[-119.2858,46.5305],[-119.2767,46.5258],[-119.2715,46.5198],[-119.267,46.5143],[-119.2632,46.5051],[-119.2614,46.4973],[-119.2602,46.4904],[-119.2623,46.4821],[-119.2612,46.472],[-119.2613,46.467],[-119.2655,46.4533],[-119.2631,46.4409],[-119.2612,46.4367],[-119.2607,46.4294],[-119.2628,46.4189],[-119.2656,46.4111],[-119.2671,46.4024],[-119.2672,46.3992],[-119.2661,46.3864],[-119.2722,46.3773],[-119.2697,46.3704],[-119.2665,46.3639],[-119.2614,46.3538],[-119.2608,46.3515],[-119.2564,46.3419],[-119.2539,46.3336],[-119.2514,46.3262],[-119.249,46.3143],[-119.2524,46.3093],[-119.2558,46.3038],[-119.2598,46.2988],[-119.2625,46.2943],[-119.2679,46.2865],[-119.2687,46.282],[-119.2681,46.2792],[-119.2642,46.2737],[-119.261,46.2704],[-119.2545,46.2685],[-119.2459,46.2671],[-119.2356,46.2601],[-119.2239,46.2508],[-119.2155,46.2425],[-119.209,46.2383],[-119.1946,46.2345],[-119.1776,46.2312],[-119.1593,46.2278],[-119.1429,46.2276],[-119.1324,46.2248],[-119.1186,46.2228],[-119.099,46.218],[-119.0899,46.2152],[-119.0768,46.2109],[-119.0476,46.1955],[-119.0405,46.1922],[-119.0313,46.1889],[-119.0288,46.1866],[-119.0243,46.181],[-119.0205,46.176],[-119.0133,46.1718],[-119.0094,46.1699],[-119.0069,46.1671],[-119.0043,46.1648],[-118.9985,46.1579],[-118.9934,46.1532],[-118.9857,46.1467],[-118.9766,46.1393],[-118.9716,46.1319],[-118.9711,46.125],[-118.968,46.1168],[-118.9559,46.1015],[-118.9489,46.0927],[-118.9464,46.0858],[-118.9433,46.078],[-118.9429,46.067],[-118.943,46.0615],[-118.9445,46.0542],[-118.946,46.0478],[-118.9468,46.0414],[-118.9431,46.0299],[-118.9458,46.0272],[-118.9478,46.0254],[-118.9564,46.0228],[-118.9643,46.0192],[-118.9684,46.0151],[-118.9756,46.012],[-118.983,46.007],[-118.9857,46.0036],[-118.9904,45.9982],[-118.9964,45.9923],[-119.0038,45.9846],[-119.0111,45.9787],[-119.0224,45.9729],[-119.0284,45.9679],[-119.0376,45.9646],[-119.0481,45.9622],[-119.0587,45.9589],[-119.0692,45.9556],[-119.0771,45.9524],[-119.0857,45.9489],[-119.095,45.9448],[-119.1022,45.9422],[-119.1082,45.9395],[-119.1233,45.9358],[-119.1358,45.9338],[-119.1495,45.9326],[-119.1614,45.9304],[-119.1699,45.9291],[-119.1778,45.9283],[-119.185,45.9265],[-119.1974,45.9273],[-119.2157,45.9305],[-119.2332,45.935],[-119.2482,45.9384],[-119.26,45.9394],[-119.2662,45.9392],[-119.2711,45.9392],[-119.2783,45.9388],[-119.2908,45.9376],[-119.2986,45.9372],[-119.3019,45.9377],[-119.3124,45.9364],[-119.3203,45.9349],[-119.3249,45.9333],[-119.3334,45.9304],[-119.3459,45.9273],[-119.363,45.9254],[-119.3708,45.9241],[-119.3826,45.9228],[-119.3964,45.9215],[-119.4043,45.92],[-119.4128,45.9194],[-119.42,45.9181],[-119.4324,45.9189],[-119.4344,45.9191],[-119.4422,45.9192],[-119.4501,45.9188],[-119.4599,45.917],[-119.4711,45.9148],[-119.4855,45.9103],[-119.4954,45.9072],[-119.5013,45.9063],[-119.5059,45.9054],[-119.5124,45.9055],[-119.5261,45.9072],[-119.5385,45.9116],[-119.5528,45.9179],[-119.5631,45.9225],[-119.5645,45.923],[-119.571,45.9247],[-119.5747,45.9252],[-119.5775,45.9256],[-119.586,45.9243],[-119.5978,45.9212],[-119.607,45.9183],[-119.6103,45.9167],[-119.6163,45.912],[-119.6236,45.9056],[-119.6289,45.9003],[-119.6322,45.8965],[-119.6388,45.8885],[-119.6442,45.8812],[-119.6481,45.8774],[-119.6514,45.8737],[-119.6574,45.8676],[-119.6581,45.867],[-119.664,45.8626],[-119.6699,45.859],[-119.6765,45.8572],[-119.6869,45.8577],[-119.6935,45.8573],[-119.7013,45.8569],[-119.7079,45.8564],[-119.7105,45.8563],[-119.7183,45.8563],[-119.7255,45.8573],[-119.7353,45.8555],[-119.7451,45.8533],[-119.7602,45.8506],[-119.7713,45.8499],[-119.7824,45.8509],[-119.7916,45.8514],[-119.7922,45.8514],[-119.7994,45.851],[-119.8138,45.849],[-119.8301,45.848],[-119.8452,45.8448],[-119.8688,45.8376],[-119.8679,45.8676],[-119.8677,45.9536],[-119.8662,46.0388],[-119.8641,46.1276],[-119.8659,46.215],[-119.8737,46.2155],[-119.8735,46.3067],[-119.8744,46.5638],[-119.877,46.5638],[-119.8764,46.628],[-119.8599,46.6261],[-119.8553,46.6256],[-119.848,46.6251],[-119.8401,46.625],[-119.8308,46.6255],[-119.8229,46.6268],[-119.8116,46.629],[-119.8017,46.6313],[-119.7884,46.6335],[-119.7633,46.6357],[-119.752,46.637],[-119.7447,46.6392],[-119.7341,46.6433],[-119.7235,46.646],[-119.7096,46.6487],[-119.7036,46.6496],[-119.6996,46.65],[-119.6877,46.6504],[-119.682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Chemical Society (ACS)","authors":"Stoliker Deborah L., Kent Douglas B., Zachara John M.","journalName":"Environmental Science & Technology","publicationDate":"10/15/2011","auditedOn":"3/4/2016","publiclyAccessibleDate":"9/16/2011"},"contributors":{"authors":[{"text":"Stoliker, Deborah L. dlstoliker@usgs.gov","contributorId":2954,"corporation":false,"usgs":true,"family":"Stoliker","given":"Deborah L.","email":"dlstoliker@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":351810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kent, Douglas B. 0000-0003-3758-8322 dbkent@usgs.gov","orcid":"https://orcid.org/0000-0003-3758-8322","contributorId":1871,"corporation":false,"usgs":true,"family":"Kent","given":"Douglas","email":"dbkent@usgs.gov","middleInitial":"B.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":351809,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zachara, John M.","contributorId":7421,"corporation":false,"usgs":true,"family":"Zachara","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":351811,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70003642,"text":"70003642 - 2011 - Projected evolution of California's San Francisco Bay-Delta-River System in a century of continuing climate change","interactions":[],"lastModifiedDate":"2017-10-30T12:45:36","indexId":"70003642","displayToPublicDate":"2011-11-09T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Projected evolution of California's San Francisco Bay-Delta-River System in a century of continuing climate change","docAbstract":"<b>Background</b> Accumulating evidence shows that the planet is warming as a response to human emissions of greenhouse gases. Strategies of adaptation to climate change will require quantitative projections of how altered regional patterns of temperature, precipitation and sea level could cascade to provoke local impacts such as modified water supplies, increasing risks of coastal flooding, and growing challenges to sustainability of native species.  <b>Methodology/Principal Findings</b> We linked a series of models to investigate responses of California's San Francisco Estuary-Watershed (SFEW) system to two contrasting scenarios of climate change. Model outputs for scenarios of fast and moderate warming are presented as 2010&ndash;2099 projections of nine indicators of changing climate, hydrology and habitat quality. Trends of these indicators measure rates of: increasing air and water temperatures, salinity and sea level; decreasing precipitation, runoff, snowmelt contribution to runoff, and suspended sediment concentrations; and increasing frequency of extreme environmental conditions such as water temperatures and sea level beyond the ranges of historical observations.  <b>Conclusions/Significance</b> Most of these environmental indicators change substantially over the 21<sup>st</sup> century, and many would present challenges to natural and managed systems. Adaptations to these changes will require flexible planning to cope with growing risks to humans and the challenges of meeting demands for fresh water and sustaining native biota. Programs of ecosystem rehabilitation and biodiversity conservation in coastal landscapes will be most likely to meet their objectives if they are designed from considerations that include: (1) an integrated perspective that river-estuary systems are influenced by effects of climate change operating on both watersheds and oceans; (2) varying sensitivity among environmental indicators to the uncertainty of future climates; (3) inevitability of biological community changes as responses to cumulative effects of climate change and other drivers of habitat transformations; and (4) anticipation and adaptation to the growing probability of ecosystem regime shifts.","language":"English","publisher":"Public Library of Science","publisherLocation":"San Francisco, CA","doi":"10.1371/journal.pone.0024465","usgsCitation":"Cloern, J.E., Knowles, N., Brown, L.R., Cayan, D., Dettinger, M., Morgan, T., Schoellhamer, D., Stacey, M., van der Wegen, M., Wagner, R.W., and Jassby, A.D., 2011, Projected evolution of California's San Francisco Bay-Delta-River System in a century of continuing climate change: PLoS ONE, v. 6, no. 9, Article e24465; 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,{"id":70044886,"text":"70044886 - 2011 - Mineral resource of the month: tin","interactions":[],"lastModifiedDate":"2013-05-08T17:37:57","indexId":"70044886","displayToPublicDate":"2011-11-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: tin","docAbstract":"Tin was one of the earliest-known metals. Because of its hardening effect on copper, tin was used in bronze implements as early as 3500 B.C. Bronze, a copper-tin alloy that can be sharpened and is hard enough to retain a cutting edge, was used during the Bronze Age in construction tools as well as weapons for hunting and war. The geographical separation between tin-producing and tin-consuming nations greatly influenced the patterns of early trade routes. Historians think that as early as 1500 B.C., Phoenicians traveled by sea to the Cornwall district of England to obtain tin. The pure metal was not used unalloyed until about 600 B.C.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geosciences Institute","publisherLocation":"Reston, VA","usgsCitation":"Carlin, J.F., 2011, Mineral resource of the month: tin: Earth, v. 56, no. 11, p. 21-21.","productDescription":"1 p.","startPage":"21","endPage":"21","additionalOnlineFiles":"N","ipdsId":"IP-032230","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":270024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":270022,"type":{"id":11,"text":"Document"},"url":"https://www.agiweb.org/store/library/imprint.php?id=2011_11"}],"volume":"56","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5151720be4b087909f0bbef0","contributors":{"authors":[{"text":"Carlin, James F. Jr. jcarlin@usgs.gov","contributorId":2685,"corporation":false,"usgs":true,"family":"Carlin","given":"James","suffix":"Jr.","email":"jcarlin@usgs.gov","middleInitial":"F.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":false,"id":476433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040685,"text":"70040685 - 2011 - Taxonomy of Greater White-fronted Geese (Aves: Anatidae)","interactions":[],"lastModifiedDate":"2012-11-14T11:04:26","indexId":"70040685","displayToPublicDate":"2011-10-31T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3147,"text":"Proceedings of the Biological Society of Washington","active":true,"publicationSubtype":{"id":10}},"title":"Taxonomy of Greater White-fronted Geese (Aves: Anatidae)","docAbstract":"Five subspecies of the Greater White-fronted Goose, <i>Anser albifrons</i> (Scopoli, 1769), have been named, all on the basis of wintering birds, and up to six subspecies have been recognized. There has been confusion over the application of some names, particularly in North America, because of lack of knowledge of the breeding ranges and type localities, and incorrect taxonomic decisions. There is one clinally varying subspecies in Eurasia, one that breeds in Greenland, and three in North America, one newly named herein.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Biological Society of Washington","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Biological Society of Washington","publisherLocation":"Lawrence, KS","doi":"10.2988/11-14.1","usgsCitation":"Banks, R.C., 2011, Taxonomy of Greater White-fronted Geese (Aves: Anatidae): Proceedings of the Biological Society of Washington, v. 124, no. 3, p. 226-233, https://doi.org/10.2988/11-14.1.","productDescription":"8 p.","startPage":"226","endPage":"233","numberOfPages":"8","ipdsId":"IP-029489","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":263143,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":263142,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2988/11-14.1"}],"volume":"124","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a4cbd5e4b0fd76c7832730","contributors":{"authors":[{"text":"Banks, Richard C.","contributorId":102933,"corporation":false,"usgs":true,"family":"Banks","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":468787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70005843,"text":"sir20105090c - 2011 - Porphyry copper assessment of British Columbia and Yukon Territory, Canada: Chapter C in <i>Global mineral resource assessment</i>","interactions":[{"subject":{"id":70005843,"text":"sir20105090c - 2011 - Porphyry copper assessment of British Columbia and Yukon Territory, Canada: Chapter C in <i>Global mineral resource assessment</i>","indexId":"sir20105090c","publicationYear":"2011","noYear":false,"chapter":"C","title":"Porphyry copper assessment of British Columbia and Yukon Territory, Canada: Chapter C in <i>Global mineral resource assessment</i>"},"predicate":"IS_PART_OF","object":{"id":70040436,"text":"sir20105090 - 2010 - Global mineral resource assessment","indexId":"sir20105090","publicationYear":"2010","noYear":false,"title":"Global mineral resource assessment"},"id":1}],"isPartOf":{"id":70040436,"text":"sir20105090 - 2010 - Global mineral resource assessment","indexId":"sir20105090","publicationYear":"2010","noYear":false,"title":"Global mineral resource assessment"},"lastModifiedDate":"2015-06-19T10:52:47","indexId":"sir20105090c","displayToPublicDate":"2011-10-28T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-5090","chapter":"C","title":"Porphyry copper assessment of British Columbia and Yukon Territory, Canada: Chapter C in <i>Global mineral resource assessment</i>","docAbstract":"<p>The U.S. Geological Survey does regional, national, and global assessments of resources (mineral, energy, water, biologic) to provide science in support of land management and decision making. Mineral resource assessments provide a synthesis of available information about where mineral deposits are known and suspected to be in the Earth&rsquo;s crust, which commodities may be present, and estimates of amounts of resources that may be present in undiscovered deposits.</p>\n<p>Canada is an important source of copper, consistently ranking as one of the top 10 world producers during the past decade (2000&ndash;2010). The preponderance of this production has been from porphyry-copper-type deposits in the western Canadian Cordillera. A probabilistic mineral resource assessment of undiscovered resources associated with porphyry copper deposits in western Canada was completed as part of a global mineral resource assessment. The purpose of the assessment was to (1) compile a database of known deposits and significant prospects, (2) delineate permissive areas (tracts) for undiscovered porphyry copper deposits that may be present in the upper kilometer (minimally) of the Earth&rsquo;s crust, and (3) provide probabilistic estimates of amounts of copper (Cu), molybdenum (Mo), gold (Au), and silver (Ag) that could be contained in undiscovered porphyry copper deposits in the tracts. The study was done by the U.S. Geological Survey (USGS) in collaboration with geologists from the British Columbia Geological Survey, Yukon Geological Survey, and industry consultants.</p>\n<p>The database of known deposits and significant prospects includes an inventory of mineral resources in 89 known porphyry copper (and 2 related copper-bearing polymetallic vein) ore zones, representing 50 porphyry copper deposits, and lists key characteristics of 280 additional porphyry copper and related copper-bearing prospects, as indicated by currently available exploration results, which also are summarized. Resource and exploration and development activity are updated with information current through April 2010.</p>\n<p>The delineation of permissive tracts and probabilistic estimation of resources in undiscovered deposits were done using the USGS three-part mineral resource assessment approach. Permissive tracts are defined in accordance with descriptive models for porphyry copper deposits to include igneous rocks and known deposits and prospects within magmatic arcs related to convergent plate-margin boundary zones. Frequency distributions of total tonnages and average grades of thoroughly explored deposits were used as models for undiscovered deposits and include a new grade and tonnage model for calc-alkaline porphyry Cu&plusmn;Mo&plusmn;Au deposits in western Canada.</p>\n<p>Five permissive tracts for the occurrence of porphyry copper deposits were delineated: 2 island-arc tracts, 1 tract of transitional, mixed island-arc and continental arc affinities, and 2 continental arc tracts. In permissive tract 003pCu2001, calc-alkaline igneous rocks of Middle Triassic to Late Jurassic age in accreted island-arc terranes of the Intermontane belt are assessed for calc-alkaline porphyry Cu&plusmn;Mo&plusmn;Au deposits. The area of this tract is 175,250 km<sup>2</sup>. In 12 known deposits, the total reported tonnage of ore is 8,100 million metric tons (Mt) containing 24.6 Mt copper. An estimated 6.9 undiscovered deposits contain a calculated mean of 8.9 Mt copper and a median of 6.9 Mt copper. The spatial density for the 18.9 known plus estimated undiscovered deposits in this tract is approximately 11 deposits per 100,000 km<sup>2</sup>.</p>\n<p>In permissive tract 003pCu2002, alkaline igneous rocks of Middle Triassic to Late Jurassic age within the Intermontane accreted island-arc terranes are assessed for alkaline porphyry Cu-Au deposits. The area of this tract is 109,290 km<sup>2</sup>. In 12 known deposits the total reported tonnage of ore is 6,440 Mt, containing 20.9 Mt copper. An estimated 7 undiscovered deposits contain a calculated mean of 22 Mt copper and a median of 13 Mt copper. The spatial density for the 19 known plus estimated undiscovered deposits in this tract is approximately 17 deposits per 100,000 km<sup>2</sup>.</p>\n<p>In permissive tract 003pCu2003, calc-alkaline igneous rocks of Late Triassic to Early Cretaceous age within the accreted Insular terranes of mixed island-arc and continental arc affinities are assessed for calc-alkaline porphyry Cu&plusmn;Mo&plusmn;Au deposits. The area of this tract is 58,360 km<sup>2</sup>. The total tonnage of ore reported in the 2 known deposits is 1,160 Mt containing 3.17 Mt copper. An estimated 2.3 undiscovered deposits contain a calculated mean of 3 Mt copper and a median of 1.9 Mt copper. The spatial density for the 4.3 known plus estimated undiscovered deposits in this tract is approximately 7 deposits per 100,000 km<sup>2</sup>.</p>\n<p>In permissive tract 003pCu2004, calc-alkaline igneous rocks in continental magmatic arcs of Jurassic to Eocene age are assessed for porphyry Cu&plusmn;Mo&plusmn;Au deposits. The area of this tract is 639,500 km<sup>2</sup>. The total tonnage of ore reported for the 23 known deposits is 6,520 Mt containing 17.9 Mt copper. An estimated 9.6 undiscovered deposits contain a calculated mean of 13 Mt copper and a median of 11 Mt copper. The spatial density for the 32.6 known deposits plus the estimated undiscovered deposits in this tract is approximately 5 deposits per 100,000 km<sup>2</sup>.</p>\n<p>In permissive tract 003pCu2005, calc-alkaline igneous rocks in continental magmatic arcs of Oligocene to Pliocene age are assessed for porphyry Cu&plusmn;Mo&plusmn;Au deposits. The area of this tract is 32,840 km<sup>2</sup>. The total tonnage of ore reported for the 1 known deposit is 44.8 Mt containing 0.224 Mt copper. An estimated 1.4 undiscovered deposits contain a calculated mean of 1.8 Mt copper and a median of 0.72 Mt copper. The spatial density for the 2.4 known plus estimated undiscovered deposits in this permissive tract is approximately 7 deposits per 100,000 km<sup>2</sup>.</p>\n<p>Western Canada has been thoroughly explored for porphyry copper deposits. The total estimated copper contained in known deposits is about 66.8 Mt (based on 2010 data), as compared to a 49 Mt mean of estimated copper in undiscovered deposits and a 34 Mt median of estimated copper in undiscovered deposits. The copper contained in known porphyry copper deposits represents about 58 percent of the total of known and undiscovered porphyry copper deposits (based on mean values). About 86 percent of the increase in estimated copper resources between 1993 and 2009 resulted from the discovery of extensions to known deposits. Nevertheless, exploration for undiscovered deposits continues, especially in and around significant prospects and in parts of permissive tracts that are mostly hidden beneath younger volcanic, sedimentary, or vegetated surficial cover.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Global mineral resource assessment (Scientific Investigations Report 2010-5090)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20105090c","collaboration":"Prepared in cooperation with the British Columbia Geological Survey, Yukon Geological Survey, and XDM Geological Consultants, Inc.","usgsCitation":"Mihalasky, M.J., Bookstrom, A.A., Frost, T.P., and Ludington, S., 2011, Porphyry copper assessment of British Columbia and Yukon Territory, Canada: Chapter C in <i>Global mineral resource assessment</i> (Version 1.0: Originally posted October 2011; Version 1.1: February 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A. 0000-0003-1336-3364 abookstrom@usgs.gov","orcid":"https://orcid.org/0000-0003-1336-3364","contributorId":1542,"corporation":false,"usgs":true,"family":"Bookstrom","given":"Arthur","email":"abookstrom@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"preferred":true,"id":353363,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frost, Thomas P. 0000-0001-8348-8432 tfrost@usgs.gov","orcid":"https://orcid.org/0000-0001-8348-8432","contributorId":203,"corporation":false,"usgs":true,"family":"Frost","given":"Thomas","email":"tfrost@usgs.gov","middleInitial":"P.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":353362,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ludington, Steve","contributorId":106848,"corporation":false,"usgs":true,"family":"Ludington","given":"Steve","affiliations":[],"preferred":false,"id":353365,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70005765,"text":"sir20115170 - 2011 - Bathymetric surveys at highway bridges crossing the Missouri and Mississippi Rivers near St. Louis, Missouri, 2010","interactions":[],"lastModifiedDate":"2012-03-08T17:16:41","indexId":"sir20115170","displayToPublicDate":"2011-10-18T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2011-5170","title":"Bathymetric surveys at highway bridges crossing the Missouri and Mississippi Rivers near St. Louis, Missouri, 2010","docAbstract":"Bathymetric surveys were conducted by the U.S. Geological Survey, in cooperation with the Missouri Department of Transportation, on the Missouri and Mississippi Rivers in the vicinity of 12 bridges at 7 highway crossings near St. Louis, Missouri, in October 2010. A multibeam echo sounder mapping system was used to obtain channel-bed elevations for river reaches ranging from 3,280 to 4,590 feet long and extending across the active channel of the Missouri and Mississippi Rivers. These bathymetric scans provide a snapshot of the channel conditions at the time of the surveys and provide characteristics of scour holes that may be useful in the development of predictive guidelines or equations for scour holes. These data also may be used by the Missouri Department of Transportation to assess the bridges for stability and integrity issues with respect to bridge scour.\nBathymetric data were collected around every pier that was in water, except those at the edge of water or in extremely shallow water, and one pier that was surrounded by a large debris raft. Scour holes were present at most piers for which bathymetry could be obtained, and ranged from 0 to 16 feet deep except at piers on channel banks or those near or embedded in rock dikes. Scour holes observed at the surveyed bridges were examined with respect to frontal slope and shape, and scour holes near railroad bridges in the vicinity of the highway bridges also were examined. Although exposure of parts of foundational support elements was observed at several piers, the exposure likely can be considered minimal compared to the overall substructure that remains buried at these piers.\nAt piers with well-defined scour holes, the frontal slopes of the holes ranged from 1.70 to 2.94 feet per foot (computed as run over rise), which were similar to recommended values in the literature (generally ranging from 1.0 to 2.0), and the shapes of the scour holes were not substantially affected by the movement of sand waves into the holes. Spur dikes near several of the piers caused localized flow disturbances that caused the resultant scour holes to display characteristics of skewed approach flow. The channel bed in the 2010 surveys was as much as 16 feet lower than the channel bed at the time of construction at the two oldest surveyed bridges, and the range varied with age of the structure, indicating the channel-bed elevations have lowered with time. However, other research has indicated the extremely dynamic nature of the channel bed on the Mississippi River.\nThe size of the scour holes observed at the surveyed sites likely was affected by the low to moderate flow conditions on the Missouri and Mississippi Rivers at the time of the surveys. The scour holes likely would be larger during conditions of increased flow. Artifacts of horizontal positioning errors were present in the data, but an analysis of the surveys indicated that most of the bathymetric data have a total propagated error of less than 0.33 foot.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115170","collaboration":"Prepared in cooperation with the Missouri Department of Transportation","usgsCitation":"Huizinga, R.J., 2011, Bathymetric surveys at highway bridges crossing the Missouri and Mississippi Rivers near St. Louis, Missouri, 2010: U.S. Geological Survey Scientific Investigations Report 2011-5170, viii, 75 p., https://doi.org/10.3133/sir20115170.","productDescription":"viii, 75 p.","additionalOnlineFiles":"Y","temporalStart":"2010-01-01","temporalEnd":"2010-12-31","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":116495,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5170.jpg"},{"id":94414,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5170/","linkFileType":{"id":5,"text":"html"}}],"state":"Missouri","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.66666666666667,38.416666666666664 ], [ -90.66666666666667,38.916666666666664 ], [ -90.08333333333333,38.916666666666664 ], [ -90.08333333333333,38.416666666666664 ], [ -90.66666666666667,38.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635538","contributors":{"authors":[{"text":"Huizinga, Richard J. 0000-0002-2940-2324 huizinga@usgs.gov","orcid":"https://orcid.org/0000-0002-2940-2324","contributorId":2089,"corporation":false,"usgs":true,"family":"Huizinga","given":"Richard","email":"huizinga@usgs.gov","middleInitial":"J.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":353165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70118334,"text":"70118334 - 2011 - Dating of Pliocene Colorado River sediments: implications for cosmogenic burial dating and the evolution of the lower Colorado River","interactions":[],"lastModifiedDate":"2014-07-28T14:05:48","indexId":"70118334","displayToPublicDate":"2011-10-14T14:02:53","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Dating of Pliocene Colorado River sediments: implications for cosmogenic burial dating and the evolution of the lower Colorado River","docAbstract":"<p>We applied cosmogenic <sup>26</sup>Al/<sup>10</sup>Be burial dating to sedimentary deposits of the ancestral Colorado River. We compared cosmogenic burial ages of sediments to the age of an independently well-dated overlying basalt flow at one site, and also applied cosmogenic burial dating to sediments with less precise independent age constraints. All dated gravels yielded old ages that suggest several episodes of sediment burial over the past ∼5.3 m.y. Comparison of burial ages to the overlying 4.4 Ma basalt yielded good agreement and suggests that under the most favorable conditions, cosmogenic burial dating can extend back 4–5 m.y. In contrast, results from other sites with more broadly independent age constraints highlight the complexities inherent in burial dating; these complexities arise from unknown and complicated burial histories, insufficient shielding, postburial production of cosmogenic isotopes by muons, and unknown initial <sup>26</sup>Al/<sup>10</sup>Be ratios. Nevertheless, and in spite of the large range of burial ages and large uncertainties, we identify samples that provide reasonable burial age constraints on the depositional history of sediment along the lower ancestral Colorado River. These samples suggest possible sediment deposition and burial at ca. 5.3, 4.7, and 3.6 Ma.</p>\n<br/>\n<p>Our calculated basinwide erosion rate for sediment transported by the modern Colorado River (∼187 mm k.y.<sup>−1</sup>) is higher than the modern erosion rates inferred from the historic sediment load (80–100 mm k.y.<sup>−1</sup>). In contrast, basinwide paleo-erosion rates calculated from Pliocene sediments are all under 40 mm k.y.<sup>−1</sup> The comparatively lower denudation rates calculated for the Pliocene sediment samples are surprising given that the sampled time intervals include significant Pliocene aggradation and may include much incision of the Grand Canyon and its tributaries. This conflict may arise from extensive storage of sediment along the route of the Colorado River, slower paleobedrock erosion, or the inclusion of sediments that were derived preferentially from higher elevations in the watershed.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","publisherLocation":"New York, NY","doi":"10.1130/B30453.1","usgsCitation":"Matmon, A., Stock, G.M., Granger, D., and Howard, K.A., 2011, Dating of Pliocene Colorado River sediments: implications for cosmogenic burial dating and the evolution of the lower Colorado River: Geological Society of America Bulletin, v. 124, no. 3-4, p. 626-640, https://doi.org/10.1130/B30453.1.","productDescription":"15 p.","startPage":"626","endPage":"640","numberOfPages":"15","costCenters":[],"links":[{"id":291187,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291186,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B30453.1"}],"volume":"124","issue":"3-4","noUsgsAuthors":false,"publicationDate":"2011-10-14","publicationStatus":"PW","scienceBaseUri":"57f7f63be4b0bc0bec0a1b40","contributors":{"authors":[{"text":"Matmon, Ari","contributorId":105831,"corporation":false,"usgs":true,"family":"Matmon","given":"Ari","affiliations":[],"preferred":false,"id":496784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stock, Greg M.","contributorId":88593,"corporation":false,"usgs":true,"family":"Stock","given":"Greg","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":496783,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Granger, Darryl E.","contributorId":40137,"corporation":false,"usgs":true,"family":"Granger","given":"Darryl E.","affiliations":[],"preferred":false,"id":496782,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":496781,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70005647,"text":"70005647 - 2011 - Comparison of statistical and theoretical habitat models for conservation planning: The benefit of ensemble prediction","interactions":[],"lastModifiedDate":"2021-01-11T17:55:31.154275","indexId":"70005647","displayToPublicDate":"2011-10-07T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of statistical and theoretical habitat models for conservation planning: The benefit of ensemble prediction","docAbstract":"Selection of a modeling approach is an important step in the conservation planning process, but little guidance is available. We compared two statistical and three theoretical habitat modeling approaches representing those currently being used for avian conservation planning at landscape and regional scales: hierarchical spatial count (HSC), classification and regression tree (CRT), habitat suitability index (HSI), forest structure database (FS), and habitat association database (HA). We focused our comparison on models for five priority forest-breeding species in the Central Hardwoods Bird Conservation Region: Acadian Flycatcher, Cerulean Warbler, Prairie Warbler, Red-headed Woodpecker, and Worm-eating Warbler. Lacking complete knowledge on the distribution and abundance of each species with which we could illuminate differences between approaches and provide strong grounds for recommending one approach over another, we used two approaches to compare models: rank correlations among model outputs and comparison of spatial correspondence. In general, rank correlations were significantly positive among models for each species, indicating general agreement among the models. Worm-eating Warblers had the highest pairwise correlations, all of which were significant (<i>P</i> , 0.05). Red-headed Woodpeckers had the lowest agreement among models, suggesting greater uncertainty in the relative conservation value of areas within the region. We assessed model uncertainty by mapping the spatial congruence in priorities (i.e., top ranks) resulting from each model for each species and calculating the coefficient of variation across model ranks for each location. This allowed identification of areas more likely to be good targets of conservation effort for a species, those areas that were least likely, and those in between where uncertainty is higher and thus conservation action incorporates more risk. Based on our results, models developed independently for the same purpose (conservation planning for a particular species in a particular geography) yield different answers and thus different conservation strategies. We assert that using only one habitat model (even if validated) as the foundation of a conservation plan is risky. Using multiple models (i.e., ensemble prediction) can reduce uncertainty and increase efficacy of conservation action when models corroborate one another and increase understanding of the system when they do not.","language":"English","publisher":"Ecological Society of America","publisherLocation":"Ithaca, NY","doi":"10.1890/10-1047.1","usgsCitation":"Jones-Farrand, D., Fearer, T.M., Thogmartin, W.E., Thompson, F.R., Nelson, M.D., and Tirpak, J.M., 2011, Comparison of statistical and theoretical habitat models for conservation planning: The benefit of ensemble prediction: Ecological Applications, v. 21, no. 6, p. 2269-2282, https://doi.org/10.1890/10-1047.1.","productDescription":"14 p.","startPage":"2269","endPage":"2282","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":204436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adff6","contributors":{"authors":[{"text":"Jones-Farrand, D. Todd","contributorId":54713,"corporation":false,"usgs":true,"family":"Jones-Farrand","given":"D. Todd","affiliations":[],"preferred":false,"id":352992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fearer, Todd M.","contributorId":42346,"corporation":false,"usgs":true,"family":"Fearer","given":"Todd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":352991,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thogmartin, Wayne E. 0000-0002-2384-4279 wthogmartin@usgs.gov","orcid":"https://orcid.org/0000-0002-2384-4279","contributorId":2545,"corporation":false,"usgs":true,"family":"Thogmartin","given":"Wayne","email":"wthogmartin@usgs.gov","middleInitial":"E.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":352989,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, Frank R. III","contributorId":12608,"corporation":false,"usgs":true,"family":"Thompson","given":"Frank","suffix":"III","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":352990,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nelson, Mark D.","contributorId":107846,"corporation":false,"usgs":true,"family":"Nelson","given":"Mark","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":352994,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tirpak, John M.","contributorId":85704,"corporation":false,"usgs":true,"family":"Tirpak","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":352993,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70003317,"text":"70003317 - 2011 - Physiological effects of potassium chloride, formalin and handling stress on bonytail","interactions":[],"lastModifiedDate":"2021-05-19T14:40:37.333148","indexId":"70003317","displayToPublicDate":"2011-10-05T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Physiological effects of potassium chloride, formalin and handling stress on bonytail","docAbstract":"<p><span>We characterized the sublethal physiological changes in bonytail&nbsp;</span><i>Gila elegans</i><span>&nbsp;subjected to consecutive 750-mg/L potassium chloride (KCl) and 25-mg/L formalin treatments for the removal of zebra mussel&nbsp;</span><i>Dreissena polymorpha</i><span>&nbsp;and quagga mussel&nbsp;</span><i>D. bugensis</i><span>&nbsp;veligers. Plasma cortisol, glucose, and osmolality were measured over 24 h and at 14 d posthandling after exposing bonytail to KCl and one net stressor (capture with a net), KCl plus formalin and two net stressors, and one or two net stressors without chemicals. Elevated plasma cortisol (322–440 ng/mL) and glucose (254–399 mg/dL) concentrations were observed in all treatments compared with the concentrations in control fish (plasma cortisol, 56 ng/mL; glucose, 43 mg/dL). While there were no detectable differences in plasma osmolality among the treatment and control fish, a difference was observed between fish that were handled once versus twice. Chemical effects of stress were not observed in any of the physiological responses when the KCl treatment was compared with the one-net stressor treatment or when the KCl plus formalin treatment was compared with the two-net stressor treatment. Cumulative responses, however, were observed between one net stressor and two net stressors for plasma glucose and osmolality but not for plasma cortisol. Plasma cortisol and glucose levels remained elevated at 24 h posthandling, indicating that bonytail had not completely recovered from the handling stressors and would benefit from a recovery period in protected refugia before being released.</span></p>","language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1080/02755947.2011.576201","usgsCitation":"Sykes, C.L., Caldwell, C.A., and Gould, W., 2011, Physiological effects of potassium chloride, formalin and handling stress on bonytail: North American Journal of Fisheries Management, v. 31, no. 2, p. 291-298, https://doi.org/10.1080/02755947.2011.576201.","productDescription":"7 p.","startPage":"291","endPage":"298","ipdsId":"IP-025136","costCenters":[{"id":204,"text":"Cooperative Research Unit Seattle","active":false,"usgs":true}],"links":[{"id":204540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-04-21","publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a68","contributors":{"authors":[{"text":"Sykes, Catherine L.","contributorId":59936,"corporation":false,"usgs":true,"family":"Sykes","given":"Catherine","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":346870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caldwell, Colleen A. 0000-0002-4730-4867 ccaldwel@usgs.gov","orcid":"https://orcid.org/0000-0002-4730-4867","contributorId":3050,"corporation":false,"usgs":true,"family":"Caldwell","given":"Colleen","email":"ccaldwel@usgs.gov","middleInitial":"A.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":346869,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gould, William R.","contributorId":63780,"corporation":false,"usgs":true,"family":"Gould","given":"William R.","affiliations":[],"preferred":false,"id":346871,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70005419,"text":"70005419 - 2011 - Ecosystem ecology meets adaptive management: food web response to a controlled flood on the Colorado River, Glen Canyon","interactions":[],"lastModifiedDate":"2021-01-11T18:03:07.881267","indexId":"70005419","displayToPublicDate":"2011-10-03T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Ecosystem ecology meets adaptive management: food web response to a controlled flood on the Colorado River, Glen Canyon","docAbstract":"<p><span>Large dams have been constructed on rivers to meet human demands for water, electricity, navigation, and recreation. As a consequence, flow and temperature regimes have been altered, strongly affecting river food webs and ecosystem processes. Experimental high‐flow dam releases, i.e., controlled floods, have been implemented on the Colorado River, USA, in an effort to reestablish pulsed flood events, redistribute sediments, improve conditions for native fishes, and increase understanding of how dam operations affect physical and biological processes. We quantified secondary production and organic matter flows in the food web below Glen Canyon dam for two years prior and one year after an experimental controlled flood in March 2008. Invertebrate biomass and secondary production declined significantly following the flood (total biomass, 55% decline; total production, 56% decline), with most of the decline driven by reductions in two nonnative invertebrate taxa,&nbsp;</span><i>Potamopyrgus antipodarum</i><span>&nbsp;and&nbsp;</span><i>Gammarus lacustris</i><span>. Diatoms dominated the trophic basis of invertebrate production before and after the controlled flood, and the largest organic matter flows were from diatoms to the three most productive invertebrate taxa (</span><i>P. antipodarum</i><span>,&nbsp;</span><i>G. lacustris</i><span>, and Tubificida). In contrast to invertebrates, production of rainbow trout (</span><i>Oncorhynchus mykiss</i><span>) increased substantially (194%) following the flood, despite the large decline in total secondary production of the invertebrate assemblage. This counterintuitive result is reconciled by a post‐flood increase in production and drift concentrations of select invertebrate prey (i.e., Chironomidae and Simuliidae) that supported a large proportion of trout production but had relatively low secondary production. In addition, interaction strengths, measured as species impact values, were strongest between rainbow trout and these two taxa before and after the flood, demonstrating that the dominant consumer–resource interactions were not necessarily congruent with the dominant organic matter flows. Our study illustrates the value of detailed food web analysis for elucidating pathways by which dam management may alter production and strengths of species interactions in river food webs. We suggest that controlled floods may increase production of nonnative rainbow trout, and this information can be used to help guide future dam management decisions.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/10-1719.1","usgsCitation":"Cross, W.F., Baxter, C., Donner, K.C., Rosi-Marshall, E.J., Kennedy, T., Hall, R., Wellard Kelly, H.A., and Rogers, R., 2011, Ecosystem ecology meets adaptive management: food web response to a controlled flood on the Colorado River, Glen Canyon: Ecological Applications, v. 21, no. 6, p. 2016-2033, https://doi.org/10.1890/10-1719.1.","productDescription":"18 p.","startPage":"2016","endPage":"2033","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":204413,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Colorado River, Glen Canyon Dam","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.17315673828125,\n              36.33725319397006\n            ],\n            [\n              -111.14593505859375,\n              36.33725319397006\n            ],\n            [\n              -111.14593505859375,\n              36.99158465967016\n            ],\n            [\n              -112.17315673828125,\n              36.99158465967016\n            ],\n            [\n              -112.17315673828125,\n              36.33725319397006\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625a1c","contributors":{"authors":[{"text":"Cross, Wyatt F.","contributorId":70881,"corporation":false,"usgs":true,"family":"Cross","given":"Wyatt","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":352448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baxter, Colden V.","contributorId":47334,"corporation":false,"usgs":false,"family":"Baxter","given":"Colden V.","affiliations":[{"id":13656,"text":"Idaho State Univ.","active":true,"usgs":false}],"preferred":false,"id":352446,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Donner, Kevin C.","contributorId":105427,"corporation":false,"usgs":true,"family":"Donner","given":"Kevin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":352451,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rosi-Marshall, Emma J.","contributorId":17722,"corporation":false,"usgs":true,"family":"Rosi-Marshall","given":"Emma","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":352445,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kennedy, Theodore A. 0000-0003-3477-3629","orcid":"https://orcid.org/0000-0003-3477-3629","contributorId":50227,"corporation":false,"usgs":true,"family":"Kennedy","given":"Theodore A.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":352447,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hall, Robert O. 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