{"pageNumber":"190","pageRowStart":"4725","pageSize":"25","recordCount":10466,"records":[{"id":70174865,"text":"70174865 - 2011 - Mitigating amphibian disease: strategies to maintain wild populations and control chytridiomycosis","interactions":[],"lastModifiedDate":"2017-05-04T10:10:40","indexId":"70174865","displayToPublicDate":"2011-04-11T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5144,"text":"Frontiers in Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Mitigating amphibian disease: strategies to maintain wild populations and control chytridiomycosis","docAbstract":"<div id=\"ASec1\" class=\"AbstractSection\">\n<h3 class=\"Heading\">Background</h3>\n<p class=\"Para\">Rescuing amphibian diversity is an achievable conservation challenge. Disease mitigation is one essential component of population management. Here we assess existing disease mitigation strategies, some in early experimental stages, which focus on the globally emerging chytrid fungus&nbsp;<i class=\"EmphasisTypeItalic\">Batrachochytrium dendrobatidis</i>. We discuss the precedent for each strategy in systems ranging from agriculture to human medicine, and the outlook for each strategy in terms of research needs and long-term potential.</p>\n</div>\n<div id=\"ASec2\" class=\"AbstractSection\">\n<h3 class=\"Heading\">Results</h3>\n<p class=\"Para\">We find that the effects of exposure to&nbsp;<i class=\"EmphasisTypeItalic\">Batrachochytrium dendrobatidis</i>&nbsp;occur on a spectrum from transient commensal to lethal pathogen. Management priorities are divided between (1) halting pathogen spread and developing survival assurance colonies, and (2) prophylactic or remedial disease treatment. Epidemiological models of chytridiomycosis suggest that mitigation strategies can control disease without eliminating the pathogen. Ecological ethics guide wildlife disease research, but several ethical questions remain for managing disease in the field.</p>\n</div>\n<div id=\"ASec3\" class=\"AbstractSection\">\n<h3 class=\"Heading\">Conclusions</h3>\n<p class=\"Para\">Because sustainable conservation of amphibians in nature is dependent on long-term population persistence and co-evolution with potentially lethal pathogens, we suggest that disease mitigation not focus exclusively on the elimination or containment of the pathogen, or on the captive breeding of amphibian hosts. Rather, successful disease mitigation must be context specific with epidemiologically informed strategies to manage already infected populations by decreasing pathogenicity and host susceptibility. We propose population level treatments based on three steps: first, identify mechanisms of disease suppression; second, parameterize epizootiological models of disease and population dynamics for testing under semi-natural conditions; and third, begin a process of adaptive management in field trials with natural populations.</p>\n</div>","language":"English","publisher":"BioMed Central","doi":"10.1186/1742-9994-8-8","usgsCitation":"Woodhams, D.C., Bosch, J., Briggs, C.J., Cashins, S., Davis, L.R., Lauer, A., Muths, E.L., Puschendorf, R., Schmidt, B.R., Sheafor, B., and Voyles, J., 2011, Mitigating amphibian disease: strategies to maintain wild populations and control chytridiomycosis: Frontiers in Zoology, v. 8, no. 8, 23 p., https://doi.org/10.1186/1742-9994-8-8.","productDescription":"23 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-023875","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":475013,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/1742-9994-8-8","text":"Publisher Index Page"},{"id":325429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"578f4f2ee4b0ad6235cf002b","contributors":{"authors":[{"text":"Woodhams, Douglas C.","contributorId":151242,"corporation":false,"usgs":false,"family":"Woodhams","given":"Douglas","email":"","middleInitial":"C.","affiliations":[{"id":13570,"text":"Boston University","active":true,"usgs":false}],"preferred":false,"id":642880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bosch, Jaime","contributorId":167060,"corporation":false,"usgs":false,"family":"Bosch","given":"Jaime","email":"","affiliations":[],"preferred":false,"id":642881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, Cheryl J.","contributorId":127721,"corporation":false,"usgs":false,"family":"Briggs","given":"Cheryl","email":"","middleInitial":"J.","affiliations":[{"id":6710,"text":"University of California, Santa Barbara, CA","active":true,"usgs":false}],"preferred":false,"id":642882,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cashins, Scott","contributorId":172986,"corporation":false,"usgs":false,"family":"Cashins","given":"Scott","email":"","affiliations":[],"preferred":false,"id":642883,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davis, Leyla R.","contributorId":172987,"corporation":false,"usgs":false,"family":"Davis","given":"Leyla","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":642884,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lauer, Antje","contributorId":172988,"corporation":false,"usgs":false,"family":"Lauer","given":"Antje","email":"","affiliations":[],"preferred":false,"id":642885,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Muths, Erin L. 0000-0002-5498-3132 muthse@usgs.gov","orcid":"https://orcid.org/0000-0002-5498-3132","contributorId":1260,"corporation":false,"usgs":true,"family":"Muths","given":"Erin","email":"muthse@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":642886,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Puschendorf, Robert","contributorId":127715,"corporation":false,"usgs":false,"family":"Puschendorf","given":"Robert","email":"","affiliations":[{"id":7119,"text":"Plymouth University","active":true,"usgs":false}],"preferred":false,"id":642887,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schmidt, Benedikt R.","contributorId":151239,"corporation":false,"usgs":false,"family":"Schmidt","given":"Benedikt","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":642888,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sheafor, Brandon","contributorId":172989,"corporation":false,"usgs":false,"family":"Sheafor","given":"Brandon","email":"","affiliations":[],"preferred":false,"id":642889,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Voyles, Jamie","contributorId":127709,"corporation":false,"usgs":false,"family":"Voyles","given":"Jamie","email":"","affiliations":[{"id":7026,"text":"New Mexico Tech","active":true,"usgs":false}],"preferred":false,"id":642890,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70256787,"text":"70256787 - 2011 - Ecosystem services provided by playas in the High Plains: potential influences of USDA conservation programs","interactions":[],"lastModifiedDate":"2024-09-09T16:33:46.545535","indexId":"70256787","displayToPublicDate":"2011-04-01T09:14:05","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 services provided by playas in the High Plains: potential influences of USDA conservation programs","docAbstract":"<p><span>Playas are shallow depressional wetlands and the dominant wetland type in the non-glaciated High Plains of the United States. This region is one of the most intensively cultivated regions in the Western Hemisphere, and playas are profoundly impacted by a variety of agricultural activities. Conservation practices promoted through Farm Bills by the U.S. Department of Agriculture (USDA) that influence playas and surrounding catchments impact ecosystem functions and related services provided by wetlands in this region. As part of a national assessment, we review effects of agricultural cultivation and effectiveness of USDA conservation programs and practices on ecosystem functions and associated services of playas. Services provided by playas are influenced by hydrological function, and unlike other wetland types in the United States, hydrological function of playas is impacted more by accumulated sediments than drainage. Most playas with cultivated catchments have lost greater than 100% of their volume from sedimentation causing reduced hydroperiods. The Conservation Reserve Program (CRP) has the largest influence on playa catchments (the High Plains has &gt;2.8 million ha), and associated sedimentation, of any USDA program. Unfortunately, most practices applied under CRP did not consider restoration of playa ecosystem function as a primary benefit, but rather established dense exotic grass in the watersheds to reduce soil erosion. Although this has reduced soil erosion, few studies have investigated its effects on playa hydrological function and services. Our review demonstrates that the Wetlands Reserve Program (WRP) has seldom been applied in the High Plains outside of south-central Nebraska. However, this is the primary program that exists within the USDA allowing conservation practices that restore wetland hydrology such as sediment removal. In addition to sediment removal, this practice has the greatest potential effect on improving hydrologic function by reducing sedimentation in vegetative buffer strips. We estimate that a 50-m native-grass buffer strip could improve individual playa hydroperiods by up to 90 days annually, enhancing delivery of most natural playa services. The potential for restoration of playa services using USDA programs is extensive, but only if WRP and associated practices are promoted and playas are considered an integral part of CRP contracts.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/09-1133.1","usgsCitation":"Smith, L.M., Haukos, D.A., McMurry, S., and Willis, D., 2011, Ecosystem services provided by playas in the High Plains: potential influences of USDA conservation programs: Ecological Applications, v. 21, no. sp1, p. S82-S92, https://doi.org/10.1890/09-1133.1.","productDescription":"11 p.","startPage":"S82","endPage":"S92","ipdsId":"IP-121660","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":486961,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/11244/321258","text":"External Repository"},{"id":433633,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, Nebraska, New Mexico, Oklahoma, Texas, Wyoming","otherGeospatial":"High Plains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.00717954750166,\n              42.491418601608046\n            ],\n            [\n              -106.00717954750166,\n              31.281299035066382\n            ],\n            [\n              -99.88771786947859,\n              31.281299035066382\n            ],\n            [\n              -99.88771786947859,\n              42.491418601608046\n            ],\n            [\n              -106.00717954750166,\n              42.491418601608046\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"21","issue":"sp1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, Loren M.","contributorId":191878,"corporation":false,"usgs":false,"family":"Smith","given":"Loren","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":912759,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haukos, David A. 0000-0001-5372-9960 dhaukos@usgs.gov","orcid":"https://orcid.org/0000-0001-5372-9960","contributorId":3664,"corporation":false,"usgs":true,"family":"Haukos","given":"David","email":"dhaukos@usgs.gov","middleInitial":"A.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":912760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McMurry, Scott T.","contributorId":344063,"corporation":false,"usgs":false,"family":"McMurry","given":"Scott T.","affiliations":[{"id":7249,"text":"Oklahoma State University","active":true,"usgs":false}],"preferred":false,"id":912761,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Willis, David","contributorId":344064,"corporation":false,"usgs":false,"family":"Willis","given":"David","affiliations":[{"id":7084,"text":"Clemson University","active":true,"usgs":false}],"preferred":false,"id":912762,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179143,"text":"70179143 - 2011 - In Vivo fitness associated with high virulence in a vertebrate virus is a complex trait regulated by host entry, replication, and shedding","interactions":[],"lastModifiedDate":"2016-12-19T13:27:04","indexId":"70179143","displayToPublicDate":"2011-04-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2497,"text":"Journal of Virology","active":true,"publicationSubtype":{"id":10}},"title":"In Vivo fitness associated with high virulence in a vertebrate virus is a complex trait regulated by host entry, replication, and shedding","docAbstract":"<p><span>The relationship between pathogen fitness and virulence is typically examined by quantifying only one or two pathogen fitness traits. More specifically, it is regularly assumed that within-host replication, as a precursor to transmission, is the driving force behind virulence. In reality, many traits contribute to pathogen fitness, and each trait could drive the evolution of virulence in different ways. Here, we independently quantified four viral infection cycle traits, namely, host entry, within-host replication, within-host coinfection fitness, and shedding, </span><i>in vivo</i><span>, in the vertebrate virus </span><span id=\"named-content-1\" class=\"named-content genus-species\">Infectious hematopoietic necrosis virus</span><span> (IHNV). We examined how each of these stages of the viral infection cycle contributes to the fitness of IHNV genotypes that differ in virulence in rainbow trout. This enabled us to determine how infection cycle fitness traits are independently associated with virulence. We found that viral fitness was independently regulated by each of the traits examined, with the largest impact on fitness being provided by within-host replication. Furthermore, the more virulent of the two genotypes of IHNV we used had advantages in all of the traits quantified. Our results are thus congruent with the assumption that virulence and within-host replication are correlated but suggest that infection cycle fitness is complex and that replication is not the only trait associated with virulence.</span></p>","language":"English","publisher":"American Society of Microbiology","doi":"10.1128/JVI.01891-10","usgsCitation":"Wargo, A.R., and Kurath, G., 2011, In Vivo fitness associated with high virulence in a vertebrate virus is a complex trait regulated by host entry, replication, and shedding: Journal of Virology, v. 85, no. 8, p. 3959-3967, https://doi.org/10.1128/JVI.01891-10.","productDescription":"9 p. ","startPage":"3959","endPage":"3967","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":475016,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/3126118","text":"External Repository"},{"id":332280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5859000ee4b03639a6025e4b","contributors":{"authors":[{"text":"Wargo, Andrew R.","contributorId":47260,"corporation":false,"usgs":true,"family":"Wargo","given":"Andrew","email":"","middleInitial":"R.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":656174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":2629,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":656175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70236115,"text":"70236115 - 2011 - Investigating the complex interface where bedrock transforms to regolith","interactions":[],"lastModifiedDate":"2022-08-29T16:11:53.000246","indexId":"70236115","displayToPublicDate":"2011-03-22T11:06:16","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Investigating the complex interface where bedrock transforms to regolith","docAbstract":"<p><span>The interface where bedrock transforms to regolith is not planar but rather has a roughness that varies with the scale of observation. The complexity of this surface is manifested in both element-depth and fragment size-depth distributions and may sometimes be related to the longitudinal profiles of watershed streams. The fractal nature of the bedrock-regolith interface means that the interface has a “thickness” which is &gt;20</span><span>&nbsp;</span><span>m in two ridgetop examples from Pennsylvania and Puerto Rico. Such weathering thicknesses, modeled as a function of one-dimensional fluid flow, are affected by the balance between rates of weathering and erosion. One-dimensional models are consistent with weathering advance rates that vary with equilibrium solubility and porefluid velocities (and not reaction kinetics). However, fluid flow is not strictly downward and one-dimensional. Permeability of regolith changes as particle size and bulk density changes with depth. Thus, both downward and lateral flow occurs especially at reaction fronts where reactions change permeability. The rate of weathering advance is, therefore, affected by the 3-dimensional distribution of reaction zones that affect permeability across the watershed. Quantitative models of such phenomena over a range of spatial and temporal scales are needed.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.apgeochem.2011.03.017","usgsCitation":"Brantley, S.L., Buss, H.L., Lebedeva, M., Fletcher, R., and Ma, I., 2011, Investigating the complex interface where bedrock transforms to regolith: Applied Geochemistry, v. 26, no. Supplement, p. S12-S15, https://doi.org/10.1016/j.apgeochem.2011.03.017.","productDescription":"4 p.","startPage":"S12","endPage":"S15","costCenters":[],"links":[{"id":475019,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://research-information.bris.ac.uk/en/publications/bc556619-d1c0-4619-89d5-1217e6f93eee","text":"External Repository"},{"id":405801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"Supplement","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brantley, S. L.","contributorId":213849,"corporation":false,"usgs":false,"family":"Brantley","given":"S.","email":"","middleInitial":"L.","affiliations":[{"id":25381,"text":"Penn State Univ.","active":true,"usgs":false}],"preferred":false,"id":850124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buss, Heather L. 0000-0002-1852-3657","orcid":"https://orcid.org/0000-0002-1852-3657","contributorId":15478,"corporation":false,"usgs":true,"family":"Buss","given":"Heather","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":850125,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lebedeva, M.","contributorId":295910,"corporation":false,"usgs":false,"family":"Lebedeva","given":"M.","email":"","affiliations":[],"preferred":false,"id":850126,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fletcher, R. C.","contributorId":295911,"corporation":false,"usgs":false,"family":"Fletcher","given":"R. C.","affiliations":[],"preferred":false,"id":850127,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ma, I.","contributorId":295912,"corporation":false,"usgs":false,"family":"Ma","given":"I.","email":"","affiliations":[],"preferred":false,"id":850128,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":99110,"text":"cir1367 - 2011 - U.S. Geological Survey Fundamental Science Practices","interactions":[],"lastModifiedDate":"2012-02-02T00:04:07","indexId":"cir1367","displayToPublicDate":"2011-03-22T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1367","title":"U.S. Geological Survey Fundamental Science Practices","docAbstract":"The USGS has a long and proud tradition of objective, unbiased science in service to the Nation. A reputation for impartiality and excellence is one of our most important assets. To help preserve this vital asset, in 2004 the Executive Leadership Team (ELT) of the USGS was charged by the Director to develop a set of fundamental science practices, philosophical premises, and operational principles as the foundation for all USGS research and monitoring activities. In a concept document, 'Fundamental Science Practices of the U.S. Geological Survey', the ELT proposed 'a set of fundamental principles to underlie USGS science practices.' The document noted that protecting the reputation of USGS science for quality and objectivity requires the following key elements: - Clearly articulated, Bureau-wide fundamental science practices. - A shared understanding at all levels of the organization that the health and future of the USGS depend on following these practices. - The investment of budget, time, and people to ensure that the USGS reputation and high-quality standards are maintained. The USGS Fundamental Science Practices (FSP) encompass all elements of research investigations, including data collection, experimentation, analysis, writing results, peer review, management review, and Bureau approval and publication of information products. The focus of FSP is on how science is carried out and how products are produced and disseminated. FSP is not designed to address the question of what work the USGS should do; that is addressed in USGS science planning handbooks and other documents. Building from longstanding existing USGS policies and the ELT concept document, in May 2006, FSP policies were developed with input from all parts of the organization and were subsequently incorporated into the Bureau's Survey Manual. In developing an implementation plan for FSP policy, the intent was to recognize and incorporate the best of USGS current practices to obtain the optimum overall program for our science. In January 2009, the USGS moved to full implementation of FSP. The FSP Advisory Committee (FSPAC) was formed to serve as the Bureau's working and standing committee to ensure the objectivity and quality of the Bureau's science information products and to provide support for the full implementation of FSP.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/cir1367","usgsCitation":"Fundamental Science Practices Advisory Committee, 2011, U.S. Geological Survey Fundamental Science Practices: U.S. Geological Survey Circular 1367, 8 p., https://doi.org/10.3133/cir1367.","productDescription":"8 p.","additionalOnlineFiles":"N","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":116748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1367.jpg"},{"id":14561,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/1367/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6961f2","contributors":{"authors":[{"text":"Fundamental Science Practices Advisory Committee","contributorId":128236,"corporation":true,"usgs":false,"organization":"Fundamental Science Practices Advisory Committee","id":535049,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70118807,"text":"70118807 - 2011 - Linking microbial and ecosystem ecology using ecological stoichiometry: a synthesis of conceptual and empirical approaches","interactions":[],"lastModifiedDate":"2014-07-30T13:17:02","indexId":"70118807","displayToPublicDate":"2011-03-01T13:15:45","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1478,"text":"Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Linking microbial and ecosystem ecology using ecological stoichiometry: a synthesis of conceptual and empirical approaches","docAbstract":"Currently, one of the biggest challenges in microbial and ecosystem ecology is to develop conceptual models that organize the growing body of information on environmental microbiology into a clear mechanistic framework with a direct link to ecosystem processes. Doing so will enable development of testable hypotheses to better direct future research and increase understanding of key constraints on biogeochemical networks. Although the understanding of phenotypic and genotypic diversity of microorganisms in the environment is rapidly accumulating, how controls on microbial physiology ultimately affect biogeochemical fluxes remains poorly understood. We propose that insight into constraints on biogeochemical cycles can be achieved by a more rigorous evaluation of microbial community biomass composition within the context of ecological stoichiometry. Multiple recent studies have pointed to microbial biomass stoichiometry as an important determinant of when microorganisms retain or recycle mineral nutrients. We identify the relevant cellular components that most likely drive changes in microbial biomass stoichiometry by defining a conceptual model rooted in ecological stoichiometry. More importantly, we show how X-ray microanalysis (XRMA), nanoscale secondary ion mass spectroscopy (NanoSIMS), Raman microspectroscopy, and in situ hybridization techniques (for example, FISH) can be applied in concert to allow for direct empirical evaluation of the proposed conceptual framework. This approach links an important piece of the ecological literature, ecological stoichiometry, with the molecular front of the microbial revolution, in an attempt to provide new insight into how microbial physiology could constrain ecosystem processes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecosystems","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","publisherLocation":"New York, NY","doi":"10.1007/s10021-010-9408-4","usgsCitation":"Hall, E., Maixner, F., Franklin, O., Daims, H., Richter, A., and Battin, T., 2011, Linking microbial and ecosystem ecology using ecological stoichiometry: a synthesis of conceptual and empirical approaches: Ecosystems, v. 14, no. 2, p. 261-273, https://doi.org/10.1007/s10021-010-9408-4.","productDescription":"13 p.","startPage":"261","endPage":"273","numberOfPages":"13","costCenters":[],"links":[{"id":475024,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s10021-010-9408-4","text":"Publisher Index Page"},{"id":291415,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291414,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10021-010-9408-4"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-12-23","publicationStatus":"PW","scienceBaseUri":"57fe7fa1e4b0824b2d147887","contributors":{"authors":[{"text":"Hall, E. K.","contributorId":85501,"corporation":false,"usgs":true,"family":"Hall","given":"E. K.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":497274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maixner, F.","contributorId":56167,"corporation":false,"usgs":true,"family":"Maixner","given":"F.","email":"","affiliations":[],"preferred":false,"id":497272,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Franklin, O.","contributorId":31686,"corporation":false,"usgs":true,"family":"Franklin","given":"O.","email":"","affiliations":[],"preferred":false,"id":497271,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Daims, H.","contributorId":103196,"corporation":false,"usgs":true,"family":"Daims","given":"H.","email":"","affiliations":[],"preferred":false,"id":497276,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Richter, A.","contributorId":71486,"corporation":false,"usgs":true,"family":"Richter","given":"A.","email":"","affiliations":[],"preferred":false,"id":497273,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Battin, T.","contributorId":99903,"corporation":false,"usgs":true,"family":"Battin","given":"T.","email":"","affiliations":[],"preferred":false,"id":497275,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70236116,"text":"70236116 - 2011 - Halloysite nanotubes and bacteria at the saprolite-bedrock interface, Rio Icacos watershed, Puerto Rico","interactions":[],"lastModifiedDate":"2022-08-29T16:28:55.763496","indexId":"70236116","displayToPublicDate":"2011-03-01T11:13:12","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Halloysite nanotubes and bacteria at the saprolite-bedrock interface, Rio Icacos watershed, Puerto Rico","docAbstract":"<p><span>Quartz diorite bedrock underlying the Luquillo Mountains of eastern Puerto Rico undergoes weathering at one of the fastest documented rates for granitic rocks in the world. Although tropical temperatures and precipitation promote rapid weathering in this location, increased bacterial densities in the regolith immediately above the bedrock suggest that microorganisms contribute to mineral weathering as well. Deep saprolite and saprock samples were obtained at the bedrock interface in an upland location (Guaba Ridge) in the Rio Icacos watershed for examination by environmental scanning electron microscopy (ESEM). In ESEM images, mineral nanotubes were observed to occur frequently in association with coccus- and rod-shaped structures resembling bacteria. These nanotubes (50–140-nm width and 150–2700-nm length) were identified as halloysite using transmission electron microscopy. Observations of multiple nanotubes on the surfaces of an individual cell are consistent with the cell's exterior functional groups interacting with Si in pore water to facilitate halloysite nucleation. We propose that one mechanism by which bacteria contribute to the rapid weathering of quartz diorite minerals in this regolith is by lowering the free energy for secondary mineral formation. The presence of bacterial surfaces may result in more rapid removal of Si from solution, thereby increasing the dissolution rates of primary minerals.</span></p>","language":"English","publisher":"American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America","doi":"10.2136/sssaj2010.0126nps","usgsCitation":"Minyard, M.L., Bruns, M.A., Martinez, C.E., Liermann, L., Buss, H.L., and Brantley, S., 2011, Halloysite nanotubes and bacteria at the saprolite-bedrock interface, Rio Icacos watershed, Puerto Rico: Soil Science Society of America Journal, v. 75, no. 2, p. 348-356, https://doi.org/10.2136/sssaj2010.0126nps.","productDescription":"9 p.","startPage":"348","endPage":"356","costCenters":[],"links":[{"id":405802,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Puerto Rico","otherGeospatial":"Rio Icacos watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -65.82,\n              18.26\n            ],\n            [\n              -65.77,\n              18.26\n            ],\n            [\n              -65.77,\n              18.30\n            ],\n            [\n              -65.82,\n              18.30\n            ],\n            [\n              -65.82,\n              18.26\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"75","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Minyard, Morgan L.","contributorId":295913,"corporation":false,"usgs":false,"family":"Minyard","given":"Morgan","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":850129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bruns, Mary Ann","contributorId":214157,"corporation":false,"usgs":false,"family":"Bruns","given":"Mary","email":"","middleInitial":"Ann","affiliations":[{"id":7260,"text":"Pennsylvania State University","active":true,"usgs":false}],"preferred":false,"id":850130,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martinez, Carmen E.","contributorId":295914,"corporation":false,"usgs":false,"family":"Martinez","given":"Carmen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":850131,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Liermann, Laura","contributorId":98632,"corporation":false,"usgs":true,"family":"Liermann","given":"Laura","email":"","affiliations":[],"preferred":false,"id":850132,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Buss, Heather L. 0000-0002-1852-3657","orcid":"https://orcid.org/0000-0002-1852-3657","contributorId":15478,"corporation":false,"usgs":true,"family":"Buss","given":"Heather","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":850133,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brantley, Susan L.","contributorId":38461,"corporation":false,"usgs":true,"family":"Brantley","given":"Susan L.","affiliations":[],"preferred":false,"id":850134,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70042494,"text":"70042494 - 2011 - Epistemic uncertainty in California-wide synthetic seismicity simulations","interactions":[],"lastModifiedDate":"2013-02-15T14:04:32","indexId":"70042494","displayToPublicDate":"2011-03-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Epistemic uncertainty in California-wide synthetic seismicity simulations","docAbstract":"The generation of seismicity catalogs on synthetic fault networks holds the promise of providing key inputs into probabilistic seismic-hazard analysis, for example, the coefficient of variation, mean recurrence time as a function of magnitude, the probability of fault-to-fault ruptures, and conditional probabilities for foreshock–mainshock triggering. I employ a seismicity simulator that includes the following ingredients: static stress transfer, viscoelastic relaxation of the lower crust and mantle, and vertical stratification of elastic and viscoelastic material properties. A cascade mechanism combined with a simple Coulomb failure criterion is used to determine the initiation, propagation, and termination of synthetic ruptures. It is employed on a 3D fault network provided by Steve Ward (unpublished data, 2009) for the Southern California Earthquake Center (SCEC) Earthquake Simulators Group. This all-California fault network, initially consisting of 8000 patches, each of ∼12 square kilometers in size, has been rediscretized into Graphic patches, each of ∼1 square kilometer in size, in order to simulate the evolution of California seismicity and crustal stress at magnitude M∼5–8. Resulting synthetic seismicity catalogs spanning 30,000 yr and about one-half million events are evaluated with magnitude-frequency and magnitude-area statistics. For a priori choices of fault-slip rates and mean stress drops, I explore the sensitivity of various constructs on input parameters, particularly mantle viscosity. Slip maps obtained for the southern San Andreas fault show that the ability of segment boundaries to inhibit slip across the boundaries (e.g., to prevent multisegment ruptures) is systematically affected by mantle viscosity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120100303","usgsCitation":"Pollitz, F., 2011, Epistemic uncertainty in California-wide synthetic seismicity simulations: Bulletin of the Seismological Society of America, v. 101, no. 5, p. 2481-2498, https://doi.org/10.1785/0120100303.","startPage":"2481","endPage":"2498","ipdsId":"IP-029518","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":267575,"type":{"id":11,"text":"Document"},"url":"https://profile.usgs.gov/myscience/upload_folder/ci2011Nov2813384037182AllCalif.pdf"},{"id":267576,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267574,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120100303"}],"country":"United States","state":"California","volume":"101","issue":"5","noUsgsAuthors":false,"publicationDate":"2011-09-26","publicationStatus":"PW","scienceBaseUri":"511f6715e4b03b29402c5dd7","contributors":{"authors":[{"text":"Pollitz, Fred F. fpollitz@usgs.gov","contributorId":2408,"corporation":false,"usgs":true,"family":"Pollitz","given":"Fred F.","email":"fpollitz@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":471642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70150344,"text":"70150344 - 2011 - Age, growth, mortality, and abundance of lake sturgeon in the Grasse River, New York, USA","interactions":[],"lastModifiedDate":"2015-06-29T11:25:12","indexId":"70150344","displayToPublicDate":"2011-02-01T12:30:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2166,"text":"Journal of Applied Ichthyology","active":true,"publicationSubtype":{"id":10}},"title":"Age, growth, mortality, and abundance of lake sturgeon in the Grasse River, New York, USA","docAbstract":"<p>An increased understanding of lake sturgeon (<i>Acipenser fulvescens</i>) population dynamics is a key requirement for successful management efforts. Little is known regarding the Grasse River population of lake sturgeon except that it is one of a few populations in New York State where spawning has been documented. Thus our purpose was to assess the current status of lake sturgeon in the Grasse River system, including age, growth, mortality, and abundance. Age was determined for 196 of 211 lake sturgeon by examination of sectioned pectoral fin rays. Ages ranged from 0 to 32 years and the annual mortality rate for fish between ages 7 and 14 was 16.8%. The weight (<i>W</i>, g) to total length (TL, mm) relationship was <i>W</i> = 1.281 x 10<sup>-6</sup>TL<sup>3.202</sup>. The von Bertalanffy growth equation was TL = 1913(1-<i>e</i><sup>-0.0294(<i>t</i>+9.5691)</sup>). While the range of observed ages was similar to that of nearby St. Lawrence River populations, mean weight at age for an individual at 1000 mm TL was lower than that observed for lake sturgeon within Lake St. Francis of the St. Lawrence River. Predicted growth based on von Bertalanffy parameters was similar to that observed for the nearby Lake St. Francis. An open population estimator using the POPAN sub-module in the Program MARK produced an abundance estimate of 793 lake sturgeon (95% CI = 337-1249).</p>","language":"English","publisher":"Wiley-Blackwell","publisherLocation":"Berlin, Germany","doi":"10.1111/j.1439-0426.2010.01599.x","usgsCitation":"Trested, D., and Isely, J.J., 2011, Age, growth, mortality, and abundance of lake sturgeon in the Grasse River, New York, USA: Journal of Applied Ichthyology, v. 27, no. 1, p. 13-19, https://doi.org/10.1111/j.1439-0426.2010.01599.x.","productDescription":"7 p.","startPage":"13","endPage":"19","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-020803","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":305429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2010-11-16","publicationStatus":"PW","scienceBaseUri":"55926c55e4b0b6d21dd676ae","contributors":{"authors":[{"text":"Trested, D.G.","contributorId":98093,"corporation":false,"usgs":true,"family":"Trested","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":556719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Isely, J. Jeffery","contributorId":97224,"corporation":false,"usgs":true,"family":"Isely","given":"J.","email":"","middleInitial":"Jeffery","affiliations":[],"preferred":false,"id":563918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70142266,"text":"70142266 - 2011 - Effects of herbivory and flooding on reforestation of baldcypress (<i>Taxodium distichum</i> [L.]) saplings planted in Caddo Lake, Texas","interactions":[],"lastModifiedDate":"2015-03-04T13:15:35","indexId":"70142266","displayToPublicDate":"2011-02-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3534,"text":"Texas Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Effects of herbivory and flooding on reforestation of baldcypress (<i>Taxodium distichum</i> [L.]) saplings planted in Caddo Lake, Texas","docAbstract":"<p><span>The effects of herbivory and flooding were examined on survival and growth of planted baldcypress (<i>Taxodium distichum</i> (L.) Rich.) saplings at three sites in Caddo Lake, TX, over a 4-yr period. There were two flood regimes (shallow periodic and deep continuous), where half of the saplings in each flood regime were protected by tree shelters to prevent herbivory. By the end of the first year, over 80% of saplings survived with half of saplings classified as healthy. By the end of the fourth year, only half of the saplings were alive and one-third were healthy. At all three sites, the combination of no protection and continuous flooding resulted in a significant number of missing saplings. Likewise, most unprotected saplings in periodic flooding were missing by the end of the study. Saplings clipped by herbivores showed about 50% chance of recovery, but many of the sprouts were of poor quality. Protected saplings in tree shelters achieved significantly greater survival and height growth.</span></p>","language":"English","publisher":"Texas Academy of Science","publisherLocation":"Plainview, TX","usgsCitation":"Keeland, B.D., Dale, R.O., Darville, R., and McCoy, J.W., 2011, Effects of herbivory and flooding on reforestation of baldcypress (<i>Taxodium distichum</i> [L.]) saplings planted in Caddo Lake, Texas: Texas Journal of Science, v. 63, no. 1/2, p. 47-68.","productDescription":"22 p.","startPage":"47","endPage":"68","numberOfPages":"22","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-023752","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":298291,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana, Texas","otherGeospatial":"Caddo Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.1118049621582,\n              32.667124733120325\n            ],\n            [\n              -94.1118049621582,\n              32.75782970781984\n            ],\n            [\n              -94.010009765625,\n              32.75782970781984\n            ],\n            [\n              -94.010009765625,\n              32.667124733120325\n            ],\n            [\n              -94.1118049621582,\n              32.667124733120325\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"63","issue":"1/2","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54f83abde4b02419550d99ea","contributors":{"authors":[{"text":"Keeland, Bobby D.","contributorId":103506,"corporation":false,"usgs":true,"family":"Keeland","given":"Bobby","email":"","middleInitial":"D.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":541778,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dale, Rassa O. 0000-0001-8532-3287 daler@usgs.gov","orcid":"https://orcid.org/0000-0001-8532-3287","contributorId":3215,"corporation":false,"usgs":true,"family":"Dale","given":"Rassa","email":"daler@usgs.gov","middleInitial":"O.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":541779,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darville, Roy","contributorId":91723,"corporation":false,"usgs":false,"family":"Darville","given":"Roy","email":"","affiliations":[],"preferred":false,"id":541781,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCoy, John W. 0000-0003-3013-730X mccoyj@usgs.gov","orcid":"https://orcid.org/0000-0003-3013-730X","contributorId":3082,"corporation":false,"usgs":true,"family":"McCoy","given":"John","email":"mccoyj@usgs.gov","middleInitial":"W.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":541780,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70038474,"text":"70038474 - 2011 - Rock fall simulation at Timpanogos Cave National Monument, American Fork Canyon, Utah, USA","interactions":[],"lastModifiedDate":"2020-06-19T20:39:38.14519","indexId":"70038474","displayToPublicDate":"2011-01-27T15:38:10","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2604,"text":"Landslides","active":true,"publicationSubtype":{"id":10}},"title":"Rock fall simulation at Timpanogos Cave National Monument, American Fork Canyon, Utah, USA","docAbstract":"Rock fall from limestone cliffs at Timpanogos Cave National Monument in American Fork Canyon east of Provo, Utah, is a common occurrence. The cave is located in limestone cliffs high on the southern side of the canyon. One fatality in 1933 led to the construction of rock fall shelters at the cave entrance and exit in 1976. Numerous rock fall incidents, including a near miss in 2000 in the vicinity of the trail below the cave exit, have led to a decision to extend the shelter at the cave exit to protect visitors from these ongoing rock fall events initiating from cliffs immediately above the cave exit. Three-dimensional rock fall simulations from sources at the top of these cliffs have provided data from which to assess the spatial frequencies and velocities of rock falls from the cliffs and to constrain the design of protective measures to reduce the rock fall hazard. Results from the rock fall simulations are consistent with the spatial patterns of rock fall impacts that have been observed at the cave exit site.","language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/s10346-010-0251-7","usgsCitation":"Harp, E.L., Dart, R.L., and Reichenbach, P., 2011, Rock fall simulation at Timpanogos Cave National Monument, American Fork Canyon, Utah, USA: Landslides, v. 8, no. 3, p. 373-379, https://doi.org/10.1007/s10346-010-0251-7.","productDescription":"7 p.","startPage":"373","endPage":"379","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":257604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Timpanogos Cave National Monument","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.71666666666667,40.43333333333333 ], [ -111.71666666666667,40.45 ], [ -111.7,40.45 ], [ -111.7,40.43333333333333 ], [ -111.71666666666667,40.43333333333333 ] ] ] } } ] }","volume":"8","issue":"3","noUsgsAuthors":false,"publicationDate":"2011-01-27","publicationStatus":"PW","scienceBaseUri":"505aadece4b0c8380cd86fcb","contributors":{"authors":[{"text":"Harp, Edwin L. harp@usgs.gov","contributorId":1290,"corporation":false,"usgs":true,"family":"Harp","given":"Edwin","email":"harp@usgs.gov","middleInitial":"L.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":464326,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dart, Richard L. dart@usgs.gov","contributorId":1209,"corporation":false,"usgs":true,"family":"Dart","given":"Richard","email":"dart@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":464325,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reichenbach, Paola","contributorId":106221,"corporation":false,"usgs":true,"family":"Reichenbach","given":"Paola","email":"","affiliations":[],"preferred":false,"id":464327,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70040391,"text":"70040391 - 2011 - Population estimates and monitoring guidelines for endangered Laysan Teal, Anas Laysanensis, at Midway Atoll: Pilot study results 2008-2010.","interactions":[],"lastModifiedDate":"2018-01-05T12:47:20","indexId":"70040391","displayToPublicDate":"2011-01-19T10:30:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":414,"text":"Technical Report","active":false,"publicationSubtype":{"id":9}},"seriesNumber":"HCSU-021","title":"Population estimates and monitoring guidelines for endangered Laysan Teal, Anas Laysanensis, at Midway Atoll: Pilot study results 2008-2010.","docAbstract":"<p>Accurate estimates of population size are often crucial to determining status and planning recovery of endangered species. The ability to detect trends in survival and population size over time enables conservation managers to make effective decisions for species and refuge management. During 2004&ndash;2007, the translocated population of endangered Laysan Teal (Anas laysanensis; also Laysan Duck) was fitted with radio transmitters providing known (―gold standard‖) measures of survival and reproduction. However, as the population grew, statistically rigorous monitoring protocols were needed that were less labor intensive than radio telemetry. A population die-off and alarmingly high number of carcasses (181) were recorded during a botulism epizootic in August&ndash;October 2008, which further reinforced the need for effective monitoring protocols since this endangered species is vulnerable to catastrophic population declines. In fall 2008, we initiated a pilot study using standardized surveys with uniquely marked birds to monitor abundance and estimate the population growth rate of the reintroduced Laysan Teal. Since few birds carried marks (leg bands) after the 2008 botulism die-off (only about 15% of the population), and standardized surveys were not yet implemented, the magnitude of the die-off on the population size was unknown.</p>\n<p>To learn more about this endangered species' status and develop monitoring protocols useful to refuge managers and recovery planners in the U.S. Fish and Wildlife Service (USFWS), we marked (banded) 252 new Laysan Teal for this pilot project. With skilled refuge staff and trained volunteers, we conducted counts of marked, unmarked, and unknown birds during bimonthly surveys from Oct 2008 to Jan 2010. We recorded the identities of marked birds observed, recovered carcasses, and then used the last date a bird was detected alive and the median resight frequency to conclude if a bird was likely to be alive on a given survey date. Using mark-resight data and individual resight frequencies, we produced a series of abundance estimates from surveys that met accuracy criteria and approached ―closed population‖ assumptions. Since only one year of standardized, atoll-wide surveys were conducted, we analyzed data selected from multiple surveys using Lincoln-Petersen (LP) estimates instead of multi-year likelihood estimators. We adjusted surveys to account for unknown birds (e.g., swimming birds), temporary band loss, and described the frequency of double counting. Double counting is an important consideration in the population estimate because we found a maximum of 13% of marked birds were counted multiple times during a survey.</p>\n<p>These survey protocols allowed us to estimate the species' post-fledging population (combined adults and juveniles), and the methods are comparable to those used on Laysan Island. The Laysan Teal population increased 91% from 247 (95% CI, 233&ndash;260) in 2007 to 439&ndash;508 in early 2010. There was no change from 2009 to 2010 indicating that there was no population growth, however, our 2010 estimate should be considered preliminary since only one month of 2010 resight data was used. We compared a series of direct counts to their corresponding population estimates during 2008&ndash;2009 to evaluate if counts could serve as an unbiased ―index‖ of population abundance. There was a moderate correlation between abundance estimates and total birds counted (r<sup>2</sup> = 0.51) during resight surveys but a low correlation with all-wetland counts (r<sup>2</sup> = 0.02). This indicated that using direct all-wetland counts to predict abundance would result in confidence intervals on the order of &plusmn; 200 birds, which is equal to 50% of the estimate. With such large confidence intervals, it would be unlikely to detect annual changes in abundance or determine the magnitude of a catastrophic decline.</p>\n<p>To improve the Laysan Teal population estimates, we recommend changes to the monitoring protocol. Additional years of data are needed to quantify inter-annual seasonal detection probabilities, which may allow the use of standardized direct counts as an unbiased index of population size. Survey protocols should be enhanced through frequent resights, regular survey intervals, and determining reliable standards to detect catastrophic declines and annual changes in adult abundance. In late 2009 to early 2010, 68% of the population was marked with unique color band combinations. This allowed for potentially accurate adult population estimates and survival estimates without the need to mark new birds in 2010, 2011, and possibly 2012. However, efforts should be made to replace worn or illegible bands so birds can be identified in future surveys. It would be valuable to develop more sophisticated population size and survival models using Program MARK, a state-of-the-art software package which uses likelihood models to analyze mark-recapture data. This would allow for more reliable adult population and survival estimates to compare with the ―source‖ Laysan Teal population on Laysan Island. These models will require additional years of resight data (&gt; 1 year) and, in some cases, an intensive annual effort of marking and recapture. Because data indicate standardized all-wetland counts are a poor index of abundance, monitoring efforts could be improved by expanding resight surveys to include all wetlands, discontinuing the all-wetland counts, and reallocating some of the wetland count effort to collect additional opportunistic resights. Approximately two years of additional bimonthly surveys are needed to validate the direct count as an appropriate index of population abundance. Additional years of individual resight data will allow estimates of adult population size, as specified in recovery criteria, and to track species population dynamics at Midway Atoll.</p>","language":"English","publisher":"University of Hawaii at Hilo","publisherLocation":"Hilo, HI","usgsCitation":"Reynolds, M.H., Brinck, K., and Laniawe, L., 2011, Population estimates and monitoring guidelines for endangered Laysan Teal, Anas Laysanensis, at Midway Atoll: Pilot study results 2008-2010.: Technical Report HCSU-021, ii, 67 p.","productDescription":"ii, 67 p.","numberOfPages":"70","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-021360","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":326617,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b55e4b03bcb0104bc37","contributors":{"authors":[{"text":"Reynolds, Michelle H. 0000-0001-7253-8158 mreynolds@usgs.gov","orcid":"https://orcid.org/0000-0001-7253-8158","contributorId":3871,"corporation":false,"usgs":true,"family":"Reynolds","given":"Michelle","email":"mreynolds@usgs.gov","middleInitial":"H.","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true},{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"preferred":true,"id":645712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brinck, Kevin W. 0000-0001-7581-2482 kbrinck@usgs.gov","orcid":"https://orcid.org/0000-0001-7581-2482","contributorId":3847,"corporation":false,"usgs":true,"family":"Brinck","given":"Kevin W.","email":"kbrinck@usgs.gov","affiliations":[],"preferred":false,"id":645713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laniawe, Leona","contributorId":140109,"corporation":false,"usgs":false,"family":"Laniawe","given":"Leona","affiliations":[{"id":13385,"text":"University of Hawaii at Hilo Cooperative Studies Unit","active":true,"usgs":false}],"preferred":false,"id":645714,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5223321,"text":"5223321 - 2011 - Sampling effort and estimates of species richness based on prepositioned area electrofisher samples","interactions":[],"lastModifiedDate":"2025-03-25T15:41:27.698385","indexId":"5223321","displayToPublicDate":"2011-01-08T12:18:40","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":"Sampling effort and estimates of species richness based on prepositioned area electrofisher samples","docAbstract":"Estimates of species richness based on electrofishing data are commonly used to describe the structure of fish communities.  One electrofishing method for sampling riverine fishes that has become popular in the last decade is the prepositioned area electrofisher (PAE).  We investigated the relationship between sampling effort and fish species richness at seven sites in the Tallapoosa River system, USA based on 1,400 PAE samples collected during 1994 and 1995.  First, we estimated species richness at each site using the first-order jackknife and compared observed values for species richness and jackknife estimates of species richness to estimates based on historical collection data.  Second, we used a permutation procedure and nonlinear regression to examine rates of species accumulation.  Third, we used regression to predict the number of PAE samples required to collect the jackknife estimate of species richness at each site during 1994 and 1995.  We found that jackknife estimates of species richness generally were less than or equal to estimates based on historical collection data.  The relationship between PAE electrofishing effort and species richness in the Tallapoosa River was described by a positive asymptotic curve as found in other studies using different electrofishing gears in wadable streams.  Results from nonlinear regression analyses indicted that rates of species accumulation were variable among sites and between years.  Across sites and years, predictions of sampling effort required to collect jackknife estimates of species richness suggested that doubling sampling effort (to 200 PAEs) would typically increase observed species richness by not more than six species.  However, sampling effort beyond about 60 PAE samples typically increased observed species richness by < 10%.  We recommend using historical collection data in conjunction with a preliminary sample size of at least 70 PAE samples to evaluate estimates of species richness in medium-sized rivers.  Seventy PAE samples should provide enough information to describe the relationship between sampling effort and species richness and thus facilitate evaluation of a sampling effort.","language":"English","publisher":"Wiley","doi":"10.1577/1548-8675(1998)018<0144:SEAEOS>2.0.CO;2","usgsCitation":"Bowen, Z., and Freeman, M.C., 2011, Sampling effort and estimates of species richness based on prepositioned area electrofisher samples: North American Journal of Fisheries Management, v. 18, no. 1, p. 144-153, https://doi.org/10.1577/1548-8675(1998)018<0144:SEAEOS>2.0.CO;2.","productDescription":"10 p.","startPage":"144","endPage":"153","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198603,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"18","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499fe4b07f02db5bd598","contributors":{"authors":[{"text":"Bowen, Zachary H. 0000-0002-8656-1831","orcid":"https://orcid.org/0000-0002-8656-1831","contributorId":26932,"corporation":false,"usgs":true,"family":"Bowen","given":"Zachary H.","affiliations":[],"preferred":false,"id":338415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freeman, Mary C. 0000-0001-7615-6923","orcid":"https://orcid.org/0000-0001-7615-6923","contributorId":99659,"corporation":false,"usgs":true,"family":"Freeman","given":"Mary","email":"","middleInitial":"C.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":338416,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175493,"text":"70175493 - 2011 - Chapter 11: Management considerations","interactions":[{"subject":{"id":70175493,"text":"70175493 - 2011 - Chapter 11: Management considerations","indexId":"70175493","publicationYear":"2011","noYear":false,"chapter":"11","title":"Chapter 11: Management considerations"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":1}],"isPartOf":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"lastModifiedDate":"2020-08-31T14:47:15.690862","indexId":"70175493","displayToPublicDate":"2011-01-03T01:15:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"11","title":"Chapter 11: Management considerations","docAbstract":"<p>We conducted an ecoregional assessment of sagebrush (<i>Artemisia spp.</i>) ecosystems in the Wyoming Basins and surrounding regions (WBEA) to determine broad-scale species-environmental relationships. Our goal was to assess the potential influence from threats to the sagebrush ecosystem on associated wildlife through the use of spatially explicit occurrence and abundance models. These models were developed using information from field surveys conducted along gradients of vegetation productivity and human disturbance integrated with spatial datasets delineating land cover, topography, and human land use in the WBEA area. Our evaluation included all sagebrush-associated wildlife species across multiple taxa whose habitat requirements and distributions were appropriate for modeling and interpretation at the broad scales of this assessment. Dominant land uses were included in delineating the human footprint. Although overall levels of the cumulative human footprint were generally low across the WBEA area, oil and gas activities have decreased the amount of shrubland habitats and increased fragmentation within development regions over the last century. At the scale of this assessment, the influence of humans was primarily expressed as an indirect function through actions that altered or reduced available habitat. We identified 65 plant species of conservation concern; 28 of 40 vertebrate species associated with sagebrush were species of concern in at least one state. We modeled environmental relationships for 15 wildlife species from data collected from surveys conducted in 2005 and 2006 designed to sample multiple species and taxa along land cover and land use gradients across the WBEA area. Occurrence of 3 species was negatively influenced by human features; anthropogenic features were a positive influence for 3 species, 8 had a mixed response, and 1 had no measurable relationship. Sagebrush land cover, considered in all wildlife models, was important to most species but differed among species in the proportion of sagebrush required and at what spatial extent. For most species examined, the spatial extent at which sagebrush cover influenced the probability of occupancy was much larger than an individual’s home range size. Exotic plants were strongly associated with human features, particularly roads, which may function as linear vectors to facilitate spread of exotic plants across the WBEA area. We used coarse-grained spatial and thematic data because of the large spatial extent (350,000 km<sup>2</sup>) of the WBEA area and the need for a consistent land cover map for the region. Distributions of species occurrence or abundance mapped in this assessment need to be corroborated with information on population demographics. In addition, our results should be interpreted relative to assumptions inherent in broad-scale ecoregional assessments. Our assessment provides managers with extensive and detailed maps of occurrence and abundance, allowing for status assessments of native species, diversity and richness, natural communities, and ecological systems present within the Wyoming Basins.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Allen Press","publisherLocation":"Lawrence, Kansas","isbn":"978-0-615-55530-0","usgsCitation":"Knick, S.T., Hanser, S.E., Leu, M., Aldridge, C.L., Nielsen, S.E., Rowland, M.M., Finn, S.P., and Wisdom, M.J., 2011, Chapter 11: Management considerations, chap. 11 <i>of</i> Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins, p. 387-409.","productDescription":"23 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,{"id":70118621,"text":"70118621 - 2011 - Challenges of predicting the potential distribution of a slow-spreading invader: a habitat suitability map for an invasive riparian tree","interactions":[],"lastModifiedDate":"2014-07-29T15:49:53","indexId":"70118621","displayToPublicDate":"2011-01-01T15:48:19","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1018,"text":"Biological Invasions","active":true,"publicationSubtype":{"id":10}},"title":"Challenges of predicting the potential distribution of a slow-spreading invader: a habitat suitability map for an invasive riparian tree","docAbstract":"Understanding the potential spread of invasive species is essential for land managers to prevent their establishment and restore impacted habitat. Habitat suitability modeling provides a tool for researchers and managers to understand the potential extent of invasive species spread. Our goal was to use habitat suitability modeling to map potential habitat of the riparian plant invader, Russian olive (<i>Elaeagnus angustifolia</i>). Russian olive has invaded riparian habitat across North America and is continuing to expand its range. We compiled 11 disparate datasets for Russian olive presence locations (n = 1,051 points and 139 polygons) in the western US and used Maximum entropy (Maxent) modeling to develop two habitat suitability maps for Russian olive in the western United States: one with coarse-scale water data and one with fine-scale water data. Our models were able to accurately predict current suitable Russian olive habitat (Coarse model: training AUC = 0.938, test AUC = 0.907; Fine model: training AUC = 0.923, test AUC = 0.885). Distance to water was the most important predictor for Russian olive presence in our coarse-scale water model, but it was only the fifth most important variable in the fine-scale model, suggesting that when water bodies are considered on a fine scale, Russian olive does not necessarily rely on water. Our model predicted that Russian olive has suitable habitat further west from its current distribution, expanding into the west coast and central North America. Our methodology proves useful for identifying potential future areas of invasion. Model results may be influenced by locations of cultivated individuals and sampling bias. Further study is needed to examine the potential for Russian olive to invade beyond its current range. Habitat suitability modeling provides an essential tool for enhancing our understanding of invasive species spread.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Biological Invasions","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Kluwer Academic Publishers","publisherLocation":"Dordrecht","doi":"10.1007/s10530-010-9798-4","usgsCitation":"Jarnevich, C.S., and Reynolds, L., 2011, Challenges of predicting the potential distribution of a slow-spreading invader: a habitat suitability map for an invasive riparian tree: Biological Invasions, v. 13, no. 1, p. 153-163, https://doi.org/10.1007/s10530-010-9798-4.","productDescription":"11 p.","startPage":"153","endPage":"163","numberOfPages":"11","costCenters":[],"links":[{"id":291359,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291358,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10530-010-9798-4"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-02","publicationStatus":"PW","scienceBaseUri":"57fe7fb6e4b0824b2d1478f8","contributors":{"authors":[{"text":"Jarnevich, Catherine S. 0000-0002-9699-2336 jarnevichc@usgs.gov","orcid":"https://orcid.org/0000-0002-9699-2336","contributorId":3424,"corporation":false,"usgs":true,"family":"Jarnevich","given":"Catherine","email":"jarnevichc@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":497151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Lindsay V.","contributorId":102732,"corporation":false,"usgs":true,"family":"Reynolds","given":"Lindsay V.","affiliations":[],"preferred":false,"id":497152,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70146224,"text":"70146224 - 2011 - Recent and historic drivers of landscape change in the Everglades ridge, slough, and Tree Island mosaic","interactions":[],"lastModifiedDate":"2015-04-14T13:06:19","indexId":"70146224","displayToPublicDate":"2011-01-01T14:15:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1345,"text":"Critical Reviews in Environmental Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Recent and historic drivers of landscape change in the Everglades ridge, slough, and Tree Island mosaic","docAbstract":"<p>More than half of the original Everglades extent formed a patterned peat mosaic of elevated ridges, lower and more open sloughs, and tree islands aligned parallel to the dominant flow direction. This ecologically important landscape structure remained in a dynamic equilibrium for millennia prior to rapid degradation over the past century in response to human manipulation of the hydrologic system. Restoration of the patterned landscape structure is one of the primary objectives of the Everglades restoration effort. Recent research has revealed that three main drivers regulated feedbacks that initiated and maintained landscape structure: the spatial and temporal distribution of surface water depths, surface and subsurface flow, and phosphorus supply. Causes of recent degradation include but are not limited to perturbations to these historically important controls; shifts in mineral and sulfate supply may have also contributed to degradation. Restoring predrainage hydrologic conditions will likely preserve remaining landscape pattern structure, provided a sufficient supply of surface water with low nutrient and low total dissolved solids content exists to maintain a rainfall-driven water chemistry. However, because of hysteresis in landscape evolution trajectories, restoration of areas with a fully degraded landscape could require additional human intervention.</p>","language":"English","publisher":"CRC Press","publisherLocation":"Boca Raton, FL","doi":"10.1080/10643389.2010.531219","usgsCitation":"Larsen, L., Nicholas Aumen, Bernhardt, C.E., Engel, V., Givnish, T.J., S Hagerthey, P.M., Harvey, J., Leonard, L., McCormick, P., McVoy, C., Noe, G.E., Nungesser, M.K., Rutchey, K., Sklar, F., Troxler, T.G., Volin, J.C., and Willard, D.A., 2011, Recent and historic drivers of landscape change in the Everglades ridge, slough, and Tree Island mosaic: Critical Reviews in Environmental Science and Technology, v. 41, no. 1, p. 344-381, https://doi.org/10.1080/10643389.2010.531219.","productDescription":"33 p.","startPage":"344","endPage":"381","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-019250","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":299671,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":299668,"type":{"id":15,"text":"Index Page"},"url":"https://www.tandfonline.com/doi/abs/10.1080/10643389.2010.531219#.VJG9x_nF9qN"}],"volume":"41","issue":"1","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"552e3a30e4b0b22a157fa0ac","contributors":{"authors":[{"text":"Larsen, Laurel G. lglarsen@usgs.gov","contributorId":1987,"corporation":false,"usgs":true,"family":"Larsen","given":"Laurel G.","email":"lglarsen@usgs.gov","affiliations":[],"preferred":false,"id":544849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholas Aumen","contributorId":140210,"corporation":false,"usgs":false,"family":"Nicholas Aumen","affiliations":[{"id":13414,"text":"Loxahatchee National Wildlife Refuge","active":true,"usgs":false}],"preferred":false,"id":544851,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bernhardt, Christopher E. 0000-0003-0082-4731 cbernhardt@usgs.gov","orcid":"https://orcid.org/0000-0003-0082-4731","contributorId":2131,"corporation":false,"usgs":true,"family":"Bernhardt","given":"Christopher","email":"cbernhardt@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":544845,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Engel, Vic 0000-0002-3858-7308","orcid":"https://orcid.org/0000-0002-3858-7308","contributorId":140213,"corporation":false,"usgs":false,"family":"Engel","given":"Vic","affiliations":[{"id":13415,"text":"Everglades National Park","active":true,"usgs":false}],"preferred":false,"id":544854,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Givnish, Thomas J.","contributorId":49648,"corporation":false,"usgs":true,"family":"Givnish","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":544873,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"S Hagerthey, P McCormick","contributorId":140211,"corporation":false,"usgs":false,"family":"S Hagerthey","given":"P","email":"","middleInitial":"McCormick","affiliations":[{"id":7036,"text":"South Florida Water Management District","active":true,"usgs":false}],"preferred":false,"id":544852,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Harvey, Judson 0000-0002-2654-9873 jwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":140228,"corporation":false,"usgs":true,"family":"Harvey","given":"Judson","email":"jwharvey@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - 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,{"id":70118784,"text":"70118784 - 2011 - Hibernacula selection by Townsend's big-eared bat in Southwestern Colorado","interactions":[],"lastModifiedDate":"2014-07-30T11:50:25","indexId":"70118784","displayToPublicDate":"2011-01-01T11:48:52","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Hibernacula selection by Townsend's big-eared bat in Southwestern Colorado","docAbstract":"In western United States, both mine reclamations and renewed mining at previously abandoned mines have increased substantially in the last decade. This increased activity may adversely impact bats that use these mines for roosting. Townsend's big-eared bat (<i>Corynorhinus townsendii</i>) is a species of conservation concern that may be impacted by ongoing mine reclamation and renewed mineral extraction. To help inform wildlife management decisions related to bat use of abandoned mine sites, we used logistic regression, Akaike's information criterion, and multi-model inference to investigate hibernacula use by Townsend's big-eared bats using 9 years of data from surveys inside abandoned mines in southwestern Colorado. Townsend's big-eared bats were found in 38 of 133 mines surveyed (29%), and occupied mines averaged 2.6 individuals per mine. The model explaining the most variability in our data included number of openings and portal temperature at abandoned mines. In southwestern Colorado, we found that abandoned mine sites with more than one opening and portal temperatures near 0°C were more likely to contain hibernating Townsend's big-eared bats. However, mines with only one opening and portal temperatures of ≥10°C were occasionally occupied by Townsend's big-eared bat. Understanding mine use by Townsend's big-eared bat can help guide decisions regarding allocation of resources and placement of bat-compatible closures at mine sites scheduled for reclamation. When feasible we believe that surveys should be conducted inside all abandoned mines in a reclamation project at least once during winter prior to making closure and reclamation recommendations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wildlife Society","publisherLocation":"Washington, D.C.","doi":"10.1002/jwmg.6","usgsCitation":"Hayes, M.A., Schorr, R.A., and Navo, K.W., 2011, Hibernacula selection by Townsend's big-eared bat in Southwestern Colorado: Journal of Wildlife Management, v. 75, no. 1, p. 137-143, https://doi.org/10.1002/jwmg.6.","productDescription":"7 p.","startPage":"137","endPage":"143","numberOfPages":"7","costCenters":[],"links":[{"id":291395,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291394,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/jwmg.6"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,39.3074 ], [ -104.9962,39.3074 ], [ -104.9962,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","volume":"75","issue":"1","noUsgsAuthors":false,"publicationDate":"2011-01-31","publicationStatus":"PW","scienceBaseUri":"57fe7fd9e4b0824b2d14797a","contributors":{"authors":[{"text":"Hayes, Mark A. hayesm@usgs.gov","contributorId":25086,"corporation":false,"usgs":true,"family":"Hayes","given":"Mark","email":"hayesm@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":false,"id":497215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schorr, Robert A.","contributorId":105239,"corporation":false,"usgs":true,"family":"Schorr","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":497217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Navo, Kirk W.","contributorId":89069,"corporation":false,"usgs":true,"family":"Navo","given":"Kirk","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":497216,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70170464,"text":"70170464 - 2011 - Hydrologic effects of urbanization and climate change on the Flint River Basin, Georgia","interactions":[],"lastModifiedDate":"2019-06-21T14:52:35","indexId":"70170464","displayToPublicDate":"2011-01-01T11:45:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1421,"text":"Earth Interactions","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic effects of urbanization and climate change on the Flint River Basin, Georgia","docAbstract":"<p>The potential effects of long-term urbanization and climate change on the freshwater resources of the Flint River basin were examined by using the Precipitation-Runoff Modeling System (PRMS). PRMS is a deterministic, distributed-parameter watershed model developed to evaluate the effects of various combinations of precipitation, temperature, and land cover on streamflow and multiple intermediate hydrologic states. Precipitation and temperature output from five general circulation models (GCMs) using one current and three future climate-change scenarios were statistically downscaled for input into PRMS. Projections of urbanization through 2050 derived for the Flint River basin by the Forecasting Scenarios of Future Land-Cover (FORE-SCE) land-cover change model were also used as input to PRMS. Comparison of the central tendency of streamflow simulated based on the three climate-change scenarios showed a slight decrease in overall streamflow relative to simulations under current conditions, mostly caused by decreases in the surface- runoff and groundwater components. The addition of information about forecasted urbanization of land surfaces to the hydrologic simulation mitigated the decreases in streamflow, mainly by increasing surface runoff.</p>","language":"English","publisher":"American Meteorological Society","publisherLocation":"Boston, MA","doi":"10.1175/2010EI369.1","usgsCitation":"Viger, R.J., Hay, L.E., Markstrom, S.L., Jones, J., and Buell, G.R., 2011, Hydrologic effects of urbanization and climate change on the Flint River Basin, Georgia: Earth Interactions, v. 15, no. 20, 25 p., https://doi.org/10.1175/2010EI369.1.","productDescription":"25 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-021144","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":475051,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/2010ei369.1","text":"Publisher Index 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,{"id":70035898,"text":"70035898 - 2011 - The May 2005 eruption of Fernandina volcano, Galápagos: The first circumferential dike intrusion observed by GPS and InSAR","interactions":[],"lastModifiedDate":"2018-10-30T09:34:17","indexId":"70035898","displayToPublicDate":"2011-01-01T10:30:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"The May 2005 eruption of Fernandina volcano, Galápagos: The first circumferential dike intrusion observed by GPS and InSAR","docAbstract":"The May 2005 eruption of Fernandina volcano, Galápagos, occurred along circumferential fissures parallel to the caldera rim and fed lava flows down the steep southwestern slope of the volcano for several weeks. This was the first circumferential dike intrusion ever observed by both InSAR and GPS measurements and thus provides an opportunity to determine the subsurface geometry of these enigmatic structures that are common on Galápagos volcanoes but are rare elsewhere. Pre- and post- eruption ground deformation between 2002 and 2006 can be modeled by the inflation of two separate magma reservoirs beneath the caldera: a shallow sill at ~1 km depth and a deeper point-source at ~5 km depth, and we infer that this system also existed at the time of the 2005 eruption. The co-eruption deformation is dominated by uplift near the 2005 eruptive fissures, superimposed on a broad subsidence centered on the caldera. Modeling of the co-eruption deformation was performed by including various combinations of planar dislocations to simulate the 2005 circumferential dike intrusion. We found that a single planar dike could not match both the InSAR and GPS data. Our best-fit model includes three planar dikes connected along hinge lines to simulate a curved concave shell that is steeply dipping (~45–60°) toward the caldera at the surface and more gently dipping (~12–14°) at depth where it connects to the horizontal sub-caldera sill. The shallow sill is underlain by the deep point source. The geometry of this modeled magmatic system is consistent with the petrology of Fernandina lavas, which suggest that circumferential eruptions tap the shallowest parts of the system, whereas radial eruptions are fed from deeper levels. The recent history of eruptions at Fernandina is also consistent with the idea that circumferential and radial intrusions are sometimes in a stress-feedback relationship and alternate in time with one another.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Volcanology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00445-010-0433-0","issn":"02588900","usgsCitation":"Chadwick, W., Jonsson, S., Geist, D.J., Poland, M.P., Johnson, D., Batt, S., Harpp, K.S., and Ruiz, A., 2011, The May 2005 eruption of Fernandina volcano, Galápagos: The first circumferential dike intrusion observed by GPS and InSAR: Bulletin of Volcanology, v. 73, no. 6, p. 679-697, https://doi.org/10.1007/s00445-010-0433-0.","productDescription":"19 p.","startPage":"679","endPage":"697","numberOfPages":"19","costCenters":[{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":244249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216385,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00445-010-0433-0"}],"country":"Galápagos Islands","otherGeospatial":"Fernandina volcano","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.666077,-0.514632 ], [ -91.666077,-0.256913 ], [ -91.36665,-0.256913 ], [ -91.36665,-0.514632 ], [ -91.666077,-0.514632 ] ] ] } } ] }","volume":"73","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-12-15","publicationStatus":"PW","scienceBaseUri":"505ba7dae4b08c986b321842","contributors":{"authors":[{"text":"Chadwick, W.W. Jr.","contributorId":35876,"corporation":false,"usgs":true,"family":"Chadwick","given":"W.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":453000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jonsson, Sigurjon","contributorId":72123,"corporation":false,"usgs":true,"family":"Jonsson","given":"Sigurjon","email":"","affiliations":[],"preferred":false,"id":453006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geist, Dennis J.","contributorId":47145,"corporation":false,"usgs":true,"family":"Geist","given":"Dennis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":453001,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Poland, Michael P. 0000-0001-5240-6123 mpoland@usgs.gov","orcid":"https://orcid.org/0000-0001-5240-6123","contributorId":146118,"corporation":false,"usgs":true,"family":"Poland","given":"Michael","email":"mpoland@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":453002,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Daniel J.","contributorId":71970,"corporation":false,"usgs":true,"family":"Johnson","given":"Daniel J.","affiliations":[],"preferred":false,"id":453005,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Batt, S.","contributorId":71414,"corporation":false,"usgs":true,"family":"Batt","given":"S.","email":"","affiliations":[],"preferred":false,"id":453004,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Harpp, Karen S.","contributorId":12271,"corporation":false,"usgs":true,"family":"Harpp","given":"Karen","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":452999,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ruiz, A.","contributorId":52425,"corporation":false,"usgs":true,"family":"Ruiz","given":"A.","email":"","affiliations":[],"preferred":false,"id":453003,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70212839,"text":"70212839 - 2011 - Introduction: An ecoregional assessment of the Wyoming Basins","interactions":[{"subject":{"id":70212839,"text":"70212839 - 2011 - Introduction: An ecoregional assessment of the Wyoming Basins","indexId":"70212839","publicationYear":"2011","noYear":false,"chapter":"Introduction","title":"Introduction: An ecoregional assessment of the Wyoming Basins"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":1}],"isPartOf":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"lastModifiedDate":"2020-08-31T14:50:13.685895","indexId":"70212839","displayToPublicDate":"2011-01-01T09:19:17","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"Introduction","title":"Introduction: An ecoregional assessment of the Wyoming Basins","docAbstract":"<p>The Wyoming Basins Ecoregional Assessment (WBEA) area in the western United States contains a number of important land cover types, including nearly one-fourth of the sagebrush (<i>Artemisia</i> spp.) in North America. Although relatively unappreciated until recent decades, the broad open landscapes dominated by sagebrush communities have received increasing attention for their ecological value and the resources that they contain (Knick and Connelly 2011). As many as 350 wildlife species depend on sagebrush ecosystems for all or part of their life requirements (Wisdom et al. 2005a). Within the WBEA, intact sagebrush landscapes provide an important stronghold for populations of greater sage-grouse (<i>Centrocercus urophasianus</i>), recently listed as a candidate species under the Endangered Species Act (U.S. Department of the Interior 2010). Numerous other plant and vertebrate species of state or national concern also occur within the WBEA study area (Ch. 2). Conserving sagebrush ecosystems is a major conservation challenge that will require an understanding not only of current trajectories and scales of habitat change due to natural and anthropogenic disturbances (Leu and Hanser 2011), but also the potential exacerbation of these trends from climate change (Wiens and Bachelet 2010, Miller et al. 2011).</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Allen Press","publisherLocation":"Lawrence, Kansas","isbn":"978-0-615-55530-0","usgsCitation":"Knick, S.T., Hanser, S.E., Leu, M., Aldridge, C.L., and Wisdom, M.J., 2011, Introduction: An ecoregional assessment of the Wyoming Basins, chap. Introduction <i>of</i> Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins, p. 1-9.","productDescription":"9 p.","startPage":"1","endPage":"9","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":378006,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":378032,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ja/70212839/70212839.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","publicComments":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Knick, Steven T. 0000-0003-4025-1704 steve_knick@usgs.gov","orcid":"https://orcid.org/0000-0003-4025-1704","contributorId":159,"corporation":false,"usgs":true,"family":"Knick","given":"Steven","email":"steve_knick@usgs.gov","middleInitial":"T.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":797614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanser, Steve E. 0000-0002-4430-2073 shanser@usgs.gov","orcid":"https://orcid.org/0000-0002-4430-2073","contributorId":152523,"corporation":false,"usgs":true,"family":"Hanser","given":"Steve","email":"shanser@usgs.gov","middleInitial":"E.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":797615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leu, Matthias","contributorId":68393,"corporation":false,"usgs":true,"family":"Leu","given":"Matthias","affiliations":[],"preferred":false,"id":797616,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aldridge, Cameron L. 0000-0003-3926-6941 aldridgec@usgs.gov","orcid":"https://orcid.org/0000-0003-3926-6941","contributorId":191773,"corporation":false,"usgs":true,"family":"Aldridge","given":"Cameron","email":"aldridgec@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":797617,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wisdom, Michael J.","contributorId":63934,"corporation":false,"usgs":true,"family":"Wisdom","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":797618,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70175156,"text":"70175156 - 2011 - Chapter 2: Sagebrush-associated species of conservation concern","interactions":[{"subject":{"id":70175156,"text":"70175156 - 2011 - Chapter 2: Sagebrush-associated species of conservation concern","indexId":"70175156","publicationYear":"2011","noYear":false,"chapter":"2","title":"Chapter 2: Sagebrush-associated species of conservation concern"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":1}],"isPartOf":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"lastModifiedDate":"2020-08-31T13:52:12.090404","indexId":"70175156","displayToPublicDate":"2011-01-01T01:15:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"2","title":"Chapter 2: Sagebrush-associated species of conservation concern","docAbstract":"<p>Selection of species of concern is a critical early step in conducting broad-scale ecological assessments for conservation planning and management. Many criteria can be used to guide this selection, such as conservation status, existing knowledge base, and association with plant communities of interest. In conducting the Wyoming Basins Ecoregional Assessment (WBEA), we followed a step-wise process to select vascular plant and vertebrate species of concern. Based on our selection process, we identified 65 taxa of sagebrush-associated (<i>Artemisia</i> spp.) vascular plants of conservation concern. The vast majority were forbs, and nearly all are found in Wyoming (n = 59; 91%), reflecting its central location and spatial dominance (51%) of the study area. Forty-eight plants (74%) were ranked either S1 or S2 (state-level ranks indicating imperilment due to rarity, threats, or other factors) in at least one state within the assessment area. Forty vertebrates of concern were selected for our assessment, including 17 mammals, 18 birds, and 4 reptiles. Among these were 7 vertebrates commonly considered sagebrush-obligate species: sagebrush lizard (<i>Sceloporus graciosus</i>), greater sage-grouse (<i>Centrocercus urophasianus</i>), sage thrasher (<i>Oreoscoptes montanus</i>), sage sparrow (<i>Amphispiza belli</i>), Brewer’s sparrow (S<i>pizella breweri</i>), pronghorn (<i>Antilocapra americana</i>), and pygmy rabbit (<i>Brachylagus idahoensis</i>). Several vertebrate species of concern in the Wyoming Basins are either rare or imperiled, including black-footed ferret (<i>Mustela nigripes</i>) and Wyoming pocket gopher (<i>Thomomys clusius</i>).</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Allen Press","publisherLocation":"Lawrence, Kansas","isbn":"978-0-615-55530-0","usgsCitation":"Rowland, M.M., Suring, L., Leu, M., Knick, S.T., and Wisdom, M.J., 2011, Chapter 2: Sagebrush-associated species of conservation concern, chap. 2 <i>of</i> Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins, p. 46-68.","productDescription":"23 p.","startPage":"46","endPage":"68","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":325879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":378011,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ja/70175156/70175156.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee"}],"country":"United States","state":"Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.03881835937499,\n              41.0130657870063\n            ],\n            [\n              -111.03881835937499,\n              44.99588261816546\n            ],\n            [\n              -104.073486328125,\n              44.99588261816546\n            ],\n            [\n              -104.073486328125,\n              41.0130657870063\n            ],\n            [\n              -111.03881835937499,\n              41.0130657870063\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"The U.S. Geological Survey has been given express permission by the publisher to provide full-text access online for this publication, and is posted with the express permission from the Publications Warehouse Guidance Subcommittee","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57a072bce4b060ce18fb2e34","contributors":{"authors":[{"text":"Rowland, Mary M.","contributorId":173292,"corporation":false,"usgs":false,"family":"Rowland","given":"Mary","email":"","middleInitial":"M.","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":644133,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Suring, Lowell H.","contributorId":172226,"corporation":false,"usgs":false,"family":"Suring","given":"Lowell H.","affiliations":[],"preferred":false,"id":644134,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leu, Matthias","contributorId":68393,"corporation":false,"usgs":true,"family":"Leu","given":"Matthias","affiliations":[],"preferred":false,"id":644135,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Knick, Steven T. 0000-0003-4025-1704 steve_knick@usgs.gov","orcid":"https://orcid.org/0000-0003-4025-1704","contributorId":159,"corporation":false,"usgs":true,"family":"Knick","given":"Steven","email":"steve_knick@usgs.gov","middleInitial":"T.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":644136,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wisdom, Michael J.","contributorId":63934,"corporation":false,"usgs":true,"family":"Wisdom","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":644137,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70190329,"text":"70190329 - 2011 - Wave-current interaction in Willapa Bay","interactions":[],"lastModifiedDate":"2017-08-27T10:47:12","indexId":"70190329","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2315,"text":"Journal of Geophysical Research C: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Wave-current interaction in Willapa Bay","docAbstract":"This paper describes the importance of wave-current interaction in an inlet-estuary system. The three-dimensional, fully coupled, Coupled Ocean-Atmosphere-Wave-Sediment Transport (COAWST) modeling system was applied in Willapa Bay (Washington State) from 22 to 29 October 1998 that included a large storm event. To represent the interaction between waves and currents, the vortex-force method was used. Model results were compared with water elevations, currents, and wave measurements obtained by the U.S. Army Corp of Engineers. In general, a good agreement between field data and computed results was achieved, although some discrepancies were also observed in regard to wave peak directions in the most upstream station. Several numerical experiments that considered different forcing terms were run in order to identify the effects of each wind, tide, and wave-current interaction process. Comparison of the horizontal momentum balances results identified that wave-breaking-induced acceleration is one of the leading terms in the inlet area. The enhancement of the apparent bed roughness caused by waves also affected the values and distribution of the bottom shear stress. The pressure gradient showed significant changes with respect to the pure tidal case. During storm conditions the momentum balance in the inlet shares the characteristics of tidal-dominated and wave-dominated surf zone environments. The changes in the momentum balance caused by waves were manifested both in water level and current variations. The most relevant effect on hydrodynamics was a wave-induced setup in the inner part of the estuary.","language":"English","publisher":"AGU Publications","doi":"10.1029/2011JC007387","usgsCitation":"Olabarrieta, M., Warner, J., and Kumar, N., 2011, Wave-current interaction in Willapa Bay: Journal of Geophysical Research C: Oceans, v. 116, no. C12, Article C12014; 27 p., https://doi.org/10.1029/2011JC007387.","productDescription":"Article C12014; 27 p.","ipdsId":"IP-023116","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":475411,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1912/4991","text":"External Repository"},{"id":345174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Willapa Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.178466796875,\n              46.31658418182218\n            ],\n            [\n              -123.67309570312499,\n              46.31658418182218\n            ],\n            [\n              -123.67309570312499,\n              46.77184961467733\n            ],\n            [\n              -124.178466796875,\n              46.77184961467733\n            ],\n            [\n              -124.178466796875,\n              46.31658418182218\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"116","issue":"C12","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2011-12-13","publicationStatus":"PW","scienceBaseUri":"59a3da31e4b077f005673229","contributors":{"authors":[{"text":"Olabarrieta, Maitane 0000-0002-7619-7992 molabarrieta@usgs.gov","orcid":"https://orcid.org/0000-0002-7619-7992","contributorId":81631,"corporation":false,"usgs":true,"family":"Olabarrieta","given":"Maitane","email":"molabarrieta@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":708564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":708565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kumar, Nirnimesh","contributorId":102308,"corporation":false,"usgs":false,"family":"Kumar","given":"Nirnimesh","affiliations":[{"id":27143,"text":"University of South Carolina, Columbia, SC","active":true,"usgs":false}],"preferred":false,"id":708566,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70188858,"text":"70188858 - 2011 - Stratigraphy and chronology of offshore to nearshore deposits associated with the Provo shoreline, Pleistocene Lake Bonneville, Utah","interactions":[],"lastModifiedDate":"2017-06-27T10:16:13","indexId":"70188858","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and chronology of offshore to nearshore deposits associated with the Provo shoreline, Pleistocene Lake Bonneville, Utah","docAbstract":"<p><span>Stratigraphic descriptions and radiocarbon data from eleven field locations are presented in this paper to establish a chronostratigraphic framework for offshore to nearshore deposits of Lake Bonneville. Based on key marker beds and geomorphic position, the deposits are interpreted to have accumulated during the period from the late transgressive phase, through the overflowing phase, into the regressive phase of the lake. Radiocarbon ages of sediments associated with the Provo shoreline indicate that Lake Bonneville dropped rapidly from the Provo shoreline at about 12,600 </span><sup>14</sup><span>C yr BP (15,000 cal yr B.P.). The presence of one or more sand beds in the upper part of the Provo-aged marl indicates rapid lowering of lake level or storm events at the end of the Provo episode. An accurate understanding of the timing and nature of Lake Bonneville's climate-driven regression from the Provo shoreline is critical to correlations with records of regional and hemispheric climate change. The rapid descent of the lake from the Provo shoreline correlates with the decline of Lakes Lahontan and Estancia, and with the onset of the B</span><span class=\"small-caps\">Ø</span><span>lling–Aller</span><span class=\"small-caps\">Ø</span><span>d warming event.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.palaeo.2011.08.005","usgsCitation":"Godsey, H.S., Oviatt, C., Miller, D.M., and Chan, M.A., 2011, Stratigraphy and chronology of offshore to nearshore deposits associated with the Provo shoreline, Pleistocene Lake Bonneville, Utah: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 310, no. 3-4, p. 442-450, https://doi.org/10.1016/j.palaeo.2011.08.005.","productDescription":"9 p.","startPage":"442","endPage":"450","ipdsId":"IP-033313","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":342951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Pleistocene Lake Bonneville","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0380859375,\n              38\n            ],\n            [\n              -111.5,\n              38\n            ],\n            [\n              -111.5,\n              42.22851735620852\n            ],\n            [\n              -114.0380859375,\n              42.22851735620852\n            ],\n            [\n              -114.0380859375,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"310","issue":"3-4","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59536edee4b062508e3c7b05","contributors":{"authors":[{"text":"Godsey, Holly S.","contributorId":193520,"corporation":false,"usgs":false,"family":"Godsey","given":"Holly","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":700883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oviatt, Charles G.","contributorId":13503,"corporation":false,"usgs":true,"family":"Oviatt","given":"Charles G.","affiliations":[],"preferred":false,"id":700884,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, David M. 0000-0003-3711-0441 dmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":140766,"corporation":false,"usgs":true,"family":"Miller","given":"David","email":"dmiller@usgs.gov","middleInitial":"M.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":700885,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chan, Marjorie A.","contributorId":66230,"corporation":false,"usgs":true,"family":"Chan","given":"Marjorie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":700886,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70190325,"text":"70190325 - 2011 - Cold-water coral distributions in the Drake Passage area from towed camera observations - Initial interpretations","interactions":[],"lastModifiedDate":"2017-08-27T11:25:37","indexId":"70190325","displayToPublicDate":"2011-01-01T00:00:00","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":"Cold-water coral distributions in the Drake Passage area from towed camera observations - Initial interpretations","docAbstract":"Seamounts are unique deep-sea features that create habitats thought to have high levels of endemic fauna, productive fisheries and benthic communities vulnerable to anthropogenic impacts. Many seamounts are isolated features, occurring in the high seas, where access is limited and thus biological data scarce. There are numerous seamounts within the Drake Passage (Southern Ocean), yet high winds, frequent storms and strong currents make seafloor sampling particularly difficult. As a result, few attempts to collect biological data have been made, leading to a paucity of information on benthic habitats or fauna in this area, particularly those on primarily hard-bottom seamounts and ridges. During a research cruise in 2008 six locations were examined (two on the Antarctic margin, one on the Shackleton Fracture Zone, and three on seamounts within the Drake Passage), using a towed camera with onboard instruments to measure conductivity, temperature, depth and turbidity. Dominant fauna and bottom type were categorized from 200 randomized photos from each location. Cold-water corals were present in high numbers in habitats both on the Antarctic margin and on the current swept seamounts of the Drake Passage, though the diversity of orders varied. Though the Scleractinia (hard corals) were abundant on the sedimented margin, they were poorly represented in the primarily hard-bottom areas of the central Drake Passage. The two seamount sites and the Shackleton Fracture Zone showed high numbers of stylasterid (lace) and alcyonacean (soft) corals, as well as large numbers of sponges. Though data are preliminary, the geological and environmental variability (particularly in temperature) between sample sites may be influencing cold-water coral biogeography in this region. Each area observed also showed little similarity in faunal diversity with other sites examined for this study within all phyla counted. This manuscript highlights how little is understood of these isolated features, particularly in Polar regions.","language":"English","publisher":"PLoS ONE","doi":"10.1371/journal.pone.0016153","usgsCitation":"Waller, R.G., Catanach, K.S., and Robinson, L.F., 2011, Cold-water coral distributions in the Drake Passage area from towed camera observations - Initial interpretations: PLoS ONE, v. 6, no. 1, Article e16153; 9 p., https://doi.org/10.1371/journal.pone.0016153.","productDescription":"Article e16153; 9 p.","ipdsId":"IP-023955","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":475408,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0016153","text":"Publisher Index Page"},{"id":345177,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Drake Passage","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.419921875,\n              -56.88626540914476\n            ],\n            [\n              -55.966796875,\n              -56.88626540914476\n            ],\n            [\n              -55.966796875,\n              -63.69670647530323\n            ],\n            [\n              -70.419921875,\n              -63.69670647530323\n            ],\n            [\n              -70.419921875,\n              -56.88626540914476\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"1","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2011-01-25","publicationStatus":"PW","scienceBaseUri":"59a3da32e4b077f00567322b","contributors":{"authors":[{"text":"Waller, Rhian G.","contributorId":195852,"corporation":false,"usgs":false,"family":"Waller","given":"Rhian","email":"","middleInitial":"G.","affiliations":[{"id":16143,"text":"University of Hawaii at Manoa, Honolulu, Hawaii","active":true,"usgs":false}],"preferred":false,"id":708567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Catanach, Kathryn Scanlon kscanlon@usgs.gov","contributorId":3085,"corporation":false,"usgs":true,"family":"Catanach","given":"Kathryn","email":"kscanlon@usgs.gov","middleInitial":"Scanlon","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":708568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, Laura F.","contributorId":195851,"corporation":false,"usgs":false,"family":"Robinson","given":"Laura","email":"","middleInitial":"F.","affiliations":[{"id":13294,"text":"Woods Hole Oceanographic Institute","active":true,"usgs":false}],"preferred":false,"id":708569,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175392,"text":"70175392 - 2011 - Chapter 8: Occurrence of large and medium-sized mammals: Occurrence but not count models predict pronghorn distribution","interactions":[{"subject":{"id":70175392,"text":"70175392 - 2011 - Chapter 8: Occurrence of large and medium-sized mammals: Occurrence but not count models predict pronghorn distribution","indexId":"70175392","publicationYear":"2011","noYear":false,"chapter":"8","title":"Chapter 8: Occurrence of large and medium-sized mammals: Occurrence but not count models predict pronghorn distribution"},"predicate":"IS_PART_OF","object":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"id":1}],"isPartOf":{"id":70118768,"text":"70118768 - 2011 - Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","indexId":"70118768","publicationYear":"2011","noYear":false,"title":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins"},"lastModifiedDate":"2020-08-31T14:30:51.708526","indexId":"70175392","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"8","title":"Chapter 8: Occurrence of large and medium-sized mammals: Occurrence but not count models predict pronghorn distribution","docAbstract":"<p>Management of medium to large-sized terrestrial mammals (Antilocapridae, Canidae, Cervidae, Leporidae, Mustelidae, Ochotonidae) in the western United States is multifaceted and complex. Species in this group generally are charismatic and provide economic opportunities, although others are considered a nuisance at one extreme or are listed as species of conservation concern at the other. Understanding the relative influence of land cover, habitat fragmentation, and human land use on their distribution during the breeding season is imperative to inform management decisions on land use and conservation planning for these species. We surveyed medium to large-sized sagebrush (<i>Artemisia</i> spp.)-associated mammal species in 2005 and 2006 on 141 random transects (mean length = 1.1 km) in the Wyoming Basins, an area undergoing rapid land cover transformation due to human actions including energy development. Overall, we observed 10 species but only obtained enough observations of pronghorn (<i>Antilocapra americana</i>) to develop spatially explicit distribution models. For pronghorn, occurrence related positively to proportion of sagebrush land cover within 0.27 km, mixed shrubland land cover within 3 km, riparian land cover within 5 km, Normalized Difference Vegetation Index (NDVI) within 0.27 km, road density within 5 km, and decay distance to power line corridors at 1 km, but negatively to salt-desert shrubland cover within 18 km and an interaction between sagebrush and NDVI within 0.27 km. We found excellent predictive capability of this model when evaluated with independent test data. The model provides a basis for assessing the effects of proposed development on pronghorn and can aid planning efforts to avoid or mitigate adverse effects on pronghorn.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Allen Press","publisherLocation":"Lawrence, Kansas","isbn":"978-0-615-55530-0","usgsCitation":"Leu, M., Hanser, S.E., Aldridge, C.L., Nielsen, S.E., Suring, L.H., and Knick, S.T., 2011, Chapter 8: Occurrence of large and medium-sized mammals: Occurrence but not count models predict pronghorn distribution, chap. 8 <i>of</i> Sagebrush ecosystem conservation and management: Ecoregional assessment tools and models for the Wyoming Basins, p. 315-336.","productDescription":"22 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