{"pageNumber":"248","pageRowStart":"6175","pageSize":"25","recordCount":10466,"records":[{"id":70028487,"text":"70028487 - 2006 - A new probabilistic seismic hazard assessment for greater Tokyo","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70028487","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3047,"text":"Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences","active":true,"publicationSubtype":{"id":10}},"title":"A new probabilistic seismic hazard assessment for greater Tokyo","docAbstract":"Tokyo and its outlying cities are home to one-quarter of Japan's 127 million people. Highly destructive earthquakes struck the capital in 1703, 1855 and 1923, the last of which took 105 000 lives. Fuelled by greater Tokyo's rich seismological record, but challenged by its magnificent complexity, our joint Japanese-US group carried out a new study of the capital's earthquake hazards. We used the prehistoric record of great earthquakes preserved by uplifted marine terraces and tsunami deposits (17 M???8 shocks in the past 7000 years), a newly digitized dataset of historical shaking (10 000 observations in the past 400 years), the dense modern seismic network (300 000 earthquakes in the past 30 years), and Japan's GeoNet array (150 GPS vectors in the past 10 years) to reinterpret the tectonic structure, identify active faults and their slip rates and estimate their earthquake frequency. We propose that a dislodged fragment of the Pacific plate is jammed between the Pacific, Philippine Sea and Eurasian plates beneath the Kanto plain on which Tokyo sits. We suggest that the Kanto fragment controls much of Tokyo's seismic behaviour for large earthquakes, including the damaging 1855 M???7.3 Ansei-Edo shock. On the basis of the frequency of earthquakes beneath greater Tokyo, events with magnitude and location similar to the M??? 7.3 Ansei-Edo event have a ca 20% likelihood in an average 30 year period. In contrast, our renewal (time-dependent) probability for the great M??? 7.9 plate boundary shocks such as struck in 1923 and 1703 is 0.5% for the next 30 years, with a time-averaged 30 year probability of ca 10%. The resulting net likelihood for severe shaking (ca 0.9g peak ground acceleration (PGA)) in Tokyo, Kawasaki and Yokohama for the next 30 years is ca 30%. The long historical record in Kanto also affords a rare opportunity to calculate the probability of shaking in an alternative manner exclusively from intensity observations. This approach permits robust estimates for the spatial distribution of expected shaking, even for sites with few observations. The resulting probability of severe shaking is ca 35% in Tokyo, Kawasaki and Yokohama and ca 10% in Chiba for an average 30 year period, in good agreement with our independent estimate, and thus bolstering our view that Tokyo's hazard looms large. Given $1 trillion estimates for the cost of an M???7.3 shock beneath Tokyo, our probability implies a $13 billion annual probable loss. ?? 2006 The Royal Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1098/rsta.2006.1808","issn":"1364503X","usgsCitation":"Stein, R., Toda, S., Parsons, T., Grunewald, E., Blong, R., Sparks, S., Shah, H., and Kennedy, J., 2006, A new probabilistic seismic hazard assessment for greater Tokyo: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, v. 364, no. 1845, p. 1965-1988, https://doi.org/10.1098/rsta.2006.1808.","startPage":"1965","endPage":"1988","numberOfPages":"24","costCenters":[],"links":[{"id":477548,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://zenodo.org/record/1236084","text":"External Repository"},{"id":210438,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1098/rsta.2006.1808"},{"id":237353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"364","issue":"1845","noUsgsAuthors":false,"publicationDate":"2006-06-30","publicationStatus":"PW","scienceBaseUri":"5059e4aee4b0c8380cd46831","contributors":{"authors":[{"text":"Stein, R.S.","contributorId":8875,"corporation":false,"usgs":true,"family":"Stein","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":418292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toda, S.","contributorId":102228,"corporation":false,"usgs":true,"family":"Toda","given":"S.","email":"","affiliations":[],"preferred":false,"id":418298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parsons, T.","contributorId":48288,"corporation":false,"usgs":true,"family":"Parsons","given":"T.","email":"","affiliations":[],"preferred":false,"id":418296,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grunewald, E.","contributorId":62820,"corporation":false,"usgs":true,"family":"Grunewald","given":"E.","email":"","affiliations":[],"preferred":false,"id":418297,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Blong, R.","contributorId":20141,"corporation":false,"usgs":true,"family":"Blong","given":"R.","email":"","affiliations":[],"preferred":false,"id":418293,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sparks, S.","contributorId":106694,"corporation":false,"usgs":true,"family":"Sparks","given":"S.","email":"","affiliations":[],"preferred":false,"id":418299,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shah, H.","contributorId":35327,"corporation":false,"usgs":true,"family":"Shah","given":"H.","email":"","affiliations":[],"preferred":false,"id":418294,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kennedy, J.","contributorId":43559,"corporation":false,"usgs":true,"family":"Kennedy","given":"J.","affiliations":[],"preferred":false,"id":418295,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70190534,"text":"70190534 - 2006 - Is a healthy ecosystem one that is rich in parasites?","interactions":[],"lastModifiedDate":"2017-09-06T14:12:20","indexId":"70190534","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3653,"text":"Trends in Ecology and Evolution","active":true,"publicationSubtype":{"id":10}},"title":"Is a healthy ecosystem one that is rich in parasites?","docAbstract":"<p><span>Historically, the role of parasites in ecosystem functioning has been considered trivial because a cursory examination reveals that their relative biomass is low compared with that of other trophic groups. However there is increasing evidence that parasite-mediated effects could be significant: they shape host population dynamics, alter interspecific competition, influence energy flow and appear to be important drivers of biodiversity. Indeed they influence a range of ecosystem functions and have a major effect on the structure of some food webs. Here, we consider the bottom-up and top-down processes of how parasitism influences ecosystem functioning and show that there is evidence that parasites are important for biodiversity and production; thus, we consider a healthy system to be one that is rich in parasite species.</span></p>","language":"English","publisher":"Cell Press","doi":"10.1016/j.tree.2006.04.007","usgsCitation":"Hudson, P., Dobson, A.P., and Lafferty, K.D., 2006, Is a healthy ecosystem one that is rich in parasites?: Trends in Ecology and Evolution, v. 21, no. 7, p. 381-385, https://doi.org/10.1016/j.tree.2006.04.007.","productDescription":"5 p.","startPage":"381","endPage":"385","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":345505,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59b10936e4b020cdf7d8da00","contributors":{"authors":[{"text":"Hudson, Peter J.","contributorId":85056,"corporation":false,"usgs":true,"family":"Hudson","given":"Peter J.","affiliations":[],"preferred":false,"id":709667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dobson, Andrew P.","contributorId":63693,"corporation":false,"usgs":true,"family":"Dobson","given":"Andrew","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":709668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":709669,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028530,"text":"70028530 - 2006 - Diet, prey delivery rates, and prey biomass of Northern Goshawks in East-Central Arizona","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70028530","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3489,"text":"Studies in Avian Biology","active":true,"publicationSubtype":{"id":10}},"title":"Diet, prey delivery rates, and prey biomass of Northern Goshawks in East-Central Arizona","docAbstract":"Recent concern over persistence of Northern Goshawk (Accipiter gentilis) populations in Arizona has stemmed from two long-term demography studies that report substantial yearly fluctuations in productivity and evidence of a declining population. Although many factors could be involved in changes in productivity and population declines, availability of food is one such factor. As part of a demography study on the Sitgreaves portion of the Apache-Sitgreaves National Forest in Arizona, we used remote cameras to assess diets of goshawks. Northern Goshawks preyed upon 22 species during two nesting seasons. Adult pairs tended to specialize on particular species of prey. Prey delivery rates decreased throughout the nesting season with a corresponding increase in biomass in the latter stages of the nestling and fledgling periods. Adults appeared to take larger prey as nestlings increased in age.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Studies in Avian Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01979922","usgsCitation":"Rogers, A.S., DeStefano, S., and Ingraldi, M., 2006, Diet, prey delivery rates, and prey biomass of Northern Goshawks in East-Central Arizona: Studies in Avian Biology, no. 31, p. 219-227.","startPage":"219","endPage":"227","numberOfPages":"9","costCenters":[],"links":[{"id":236424,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"31","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a00d9e4b0c8380cd4f95d","contributors":{"authors":[{"text":"Rogers, A. S.","contributorId":101448,"corporation":false,"usgs":true,"family":"Rogers","given":"A.","middleInitial":"S.","affiliations":[],"preferred":false,"id":418481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeStefano, S.","contributorId":84309,"corporation":false,"usgs":true,"family":"DeStefano","given":"S.","email":"","affiliations":[],"preferred":false,"id":418480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingraldi, M.F.","contributorId":41214,"corporation":false,"usgs":true,"family":"Ingraldi","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":418479,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70030336,"text":"70030336 - 2006 - Distribution of stress drop, stiffness, and fracture energy over earthquake rupture zones","interactions":[],"lastModifiedDate":"2012-03-12T17:21:03","indexId":"70030336","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of stress drop, stiffness, and fracture energy over earthquake rupture zones","docAbstract":"Using information provided by slip models and the methodology of McGarr and Fletcher (2002), we map static stress drop, stiffness (k = ????/u, where ???? is static stress drop and u is slip), and fracture energy over the slip surface to investigate the earthquake rupture process and energy budget. For the 1994 M6.7 Northridge, 1992 M7.3 Landers, and 1995 M6.9 Kobe earthquakes, the distributions of static stress drop show strong heterogeneity, emphasizing the importance of asperities in the rupture process. Average values of static stress drop are 17, 11, and 4 Mpa for Northridge, Landers, and Kobe, respectively. These values are substantially higher than estimates based on simple crack models, suggesting that the failure process involves the rupture of asperities within the larger fault zone. Stress drop as a function of depth for the Northridge and Landers earthquakes suggests that stress drops are limited by crustal strength. For these two earthquakes, regions of high slip are surrounded by high values of stiffness. Particularly for the Northridge earthquake, the prominent patch of high slip in the central part of the fault is bordered by a ring of high stiffness and is consistent with expectations based on the failure of an asperity loaded at its edge due to exterior slip. Stiffness within an asperity is inversely related to its dimensions. Estimates of fracture energy, based on static stress drop, slip, and rupture speed, were used to investigate the nature of slip weakening at four locations near the hypocenter of the Kobe earthquake for comparison with independent results based on a dynamic model of this earthquake. One subfault updip and to the NE of the hypocenter has a fracture energy of 1.1 MJ/m2 and a slip-weakening distance, Dc, of 0.66 m. Right triangles, whose base and height are Dc and the dynamic stress drop, respectively, approximately overlie the slip-dependent stress given by Ide and Takeo (1997) for the same locations near the hypocenter. The total fracture energy for the Kobe earthquake, 3.7 ?? 1014 J, is about the same as the seismic energy (Ea = 3.2 ?? 1014 J.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2004JB003396","issn":"01480227","usgsCitation":"Fletcher, J.B., and McGarr, A., 2006, Distribution of stress drop, stiffness, and fracture energy over earthquake rupture zones: Journal of Geophysical Research B: Solid Earth, v. 111, no. 3, https://doi.org/10.1029/2004JB003396.","costCenters":[],"links":[{"id":477433,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jb003396","text":"Publisher Index Page"},{"id":211715,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JB003396"},{"id":239059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-03-23","publicationStatus":"PW","scienceBaseUri":"505a0303e4b0c8380cd502d5","contributors":{"authors":[{"text":"Fletcher, Joe B.","contributorId":8850,"corporation":false,"usgs":true,"family":"Fletcher","given":"Joe","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":426736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGarr, Art 0000-0001-9769-4093","orcid":"https://orcid.org/0000-0001-9769-4093","contributorId":43491,"corporation":false,"usgs":true,"family":"McGarr","given":"Art","affiliations":[],"preferred":false,"id":426737,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028590,"text":"70028590 - 2006 - Tidal saltmarsh fragmentation and persistence of San Pablo Song Sparrows (Melospiza melodia samuelis): Assessing benefits of wetland restoration in San Francisco Bay","interactions":[],"lastModifiedDate":"2017-08-26T16:38:15","indexId":"70028590","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3489,"text":"Studies in Avian Biology","active":true,"publicationSubtype":{"id":10}},"title":"Tidal saltmarsh fragmentation and persistence of San Pablo Song Sparrows (Melospiza melodia samuelis): Assessing benefits of wetland restoration in San Francisco Bay","docAbstract":"The San Pablo Song Sparrow (Melospiza melodia samuelis) is one of three morphologically distinct Song Sparrow subspecies in tidal marshes of the San Francisco Bay estuary. These subspecies are rare, because as the human population has grown, diking and development have resulted in loss of 79% of the historic tidal marshes. Hundreds of projects have been proposed in the past decade to restore tidal marshes and benefit endemic populations. To evaluate the value of these restoration projects for Song Sparrows, we developed a population viability analysis (PVA) model to examine persistence of samuelis subspecies in relation to parcel size, connectivity, and catastrophe in San Pablo Bay. A total of 101 wetland parcels were identified from coverages of modern and historic tidal marshes. Parcels were grouped into eight fragments in the historical landscape and 10 in the present landscape. Fragments were defined as a group of parcels separated by >1 km, a distance that precluded regular interchange. Simulations indicated that the historic (circa 1850) samuelis population was three times larger than the modern population. However, only very high levels (>70% mortality) of catastrophe would threaten their persistence. Persistence of populations was sensitive to parcel size at a carrying capacity of <10 pairs, but connectivity of parcels was found to have little importance because habitats were dominated by a few large parcels. Our analysis indicates little risk of extinction of the samuelis subspecies with the current extent of tidal marshes, but the vulnerability of the small-est parcels suggests that restoration should create larger continuous tracts. Thus, PVA models may be useful tools for balancing the costs and benefits of restoring habitats for threatened tidal-marsh populations in wetland restoration planning.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Studies in Avian Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01979922","isbn":"0943610702; 9780943610702","usgsCitation":"Takekawa, J.Y., Sacks, B., Woo, I., Johnson, M., and Wylie, G., 2006, Tidal saltmarsh fragmentation and persistence of San Pablo Song Sparrows (Melospiza melodia samuelis): Assessing benefits of wetland restoration in San Francisco Bay: Studies in Avian Biology, no. 32, p. 238-246.","startPage":"238","endPage":"246","numberOfPages":"9","costCenters":[],"links":[{"id":236326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"32","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb37ae4b08c986b325ded","contributors":{"editors":[{"text":"Greenberg R.Maldonado J.E.Droege S.McDonald M.V.","contributorId":128314,"corporation":true,"usgs":false,"organization":"Greenberg R.Maldonado J.E.Droege S.McDonald M.V.","id":536637,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":418747,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sacks, B.N.","contributorId":64431,"corporation":false,"usgs":true,"family":"Sacks","given":"B.N.","affiliations":[],"preferred":false,"id":418748,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woo, I.","contributorId":45861,"corporation":false,"usgs":true,"family":"Woo","given":"I.","email":"","affiliations":[],"preferred":false,"id":418746,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, M.L.","contributorId":39525,"corporation":false,"usgs":true,"family":"Johnson","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":418745,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wylie, G.D.","contributorId":68238,"corporation":false,"usgs":true,"family":"Wylie","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":418749,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031177,"text":"70031177 - 2006 - Detection probabilities and site occupancy estimates for amphibians at Okefenokee National Wildlife Refuge","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031177","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Detection probabilities and site occupancy estimates for amphibians at Okefenokee National Wildlife Refuge","docAbstract":"We conducted an amphibian inventory at Okefenokee National Wildlife Refuge from August 2000 to June 2002 as part of the U.S. Department of the Interior's national Amphibian Research and Monitoring Initiative. Nineteen species of amphibians (15 anurans and 4 caudates) were documented within the Refuge, including one protected species, the Gopher Frog Rana capito. We also collected 1 y of monitoring data for amphibian populations and incorporated the results into the inventory. Detection probabilities and site occupancy estimates for four species, the Pinewoods Treefrog (Hyla femoralis), Pig Frog (Rana grylio), Southern Leopard Frog (R. sphenocephala) and Carpenter Frog (R. virgatipes) are presented here. Detection probabilities observed in this study indicate that spring and summer surveys offer the best opportunity to detect these species in the Refuge. Results of the inventory suggest that substantial changes may have occurred in the amphibian fauna within and adjacent to the swamp. However, monitoring the amphibian community of Okefenokee Swamp will prove difficult because of the logistical challenges associated with a rigorous statistical assessment of status and trends.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Midland Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1674/0003-0031(2006)155[0149:DPASOE]2.0.CO;2","issn":"00030031","usgsCitation":"Smith, L.L., Barichivich, W., Staiger, J., Smith, K.G., and Dodd, C., 2006, Detection probabilities and site occupancy estimates for amphibians at Okefenokee National Wildlife Refuge: American Midland Naturalist, v. 155, no. 1, p. 149-161, https://doi.org/10.1674/0003-0031(2006)155[0149:DPASOE]2.0.CO;2.","startPage":"149","endPage":"161","numberOfPages":"13","costCenters":[],"links":[{"id":211462,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1674/0003-0031(2006)155[0149:DPASOE]2.0.CO;2"},{"id":238755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"155","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff7be4b0c8380cd4f201","contributors":{"authors":[{"text":"Smith, L. L.","contributorId":6791,"corporation":false,"usgs":true,"family":"Smith","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":430373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barichivich, W.J. 0000-0003-1103-6861","orcid":"https://orcid.org/0000-0003-1103-6861","contributorId":91435,"corporation":false,"usgs":true,"family":"Barichivich","given":"W.J.","affiliations":[],"preferred":false,"id":430377,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staiger, J.S.","contributorId":45664,"corporation":false,"usgs":true,"family":"Staiger","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":430374,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Kimberly G.","contributorId":47720,"corporation":false,"usgs":true,"family":"Smith","given":"Kimberly","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":430375,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dodd, C.K. Jr.","contributorId":86286,"corporation":false,"usgs":true,"family":"Dodd","given":"C.K.","suffix":"Jr.","affiliations":[],"preferred":false,"id":430376,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031176,"text":"70031176 - 2006 - Lake Sturgeon, Acipenser fulvescens, movements in Rainy Lake, Minnesota and Ontario","interactions":[],"lastModifiedDate":"2021-05-06T21:45:01.845269","indexId":"70031176","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1163,"text":"Canadian Field-Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Lake Sturgeon, Acipenser fulvescens, movements in Rainy Lake, Minnesota and Ontario","docAbstract":"<p><span>Rainy Lake, Minnesota-Ontario, contains a native population of Lake Sturgeon (</span><i>Acipenser fulvescens</i><span>) that has gone largely unstudied. The objective of this descriptive study was to summarize generalized Lake Sturgeon movement patterns through the use of biotelemetry. Telemetry data reinforced the high utilization of the Squirrel Falls geographic location by Lake Sturgeon, with 37% of the re-locations occurring in that area. Other spring aggregations occurred in areas associated with Kettle Falls, the Pipestone River, and the Rat River, which could indicate spawning activity. Movement of Lake Sturgeon between the Seine River and the South Arm of Rainy Lake indicates the likelihood of one integrated population on the east end of the South Arm. The lack of re-locations in the Seine River during the months of September and October may have been due to Lake Sturgeon moving into deeper water areas of the Seine River and out of the range of radio telemetry gear or simply moving back into the South Arm. Due to the movements between Minnesota and Ontario, coordination of management efforts among provincial, state, and federal agencies will be important.</span></p>","language":"English","publisher":"Canadian Field-Naturalist","doi":"10.22621/cfn.v120i1.249","issn":"00083550","usgsCitation":"Adams, W., Kallemeyn, L., and Willis, D., 2006, Lake Sturgeon, Acipenser fulvescens, movements in Rainy Lake, Minnesota and Ontario: Canadian Field-Naturalist, v. 120, no. 1, p. 71-82, https://doi.org/10.22621/cfn.v120i1.249.","productDescription":"12 p.","startPage":"71","endPage":"82","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":486990,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.22621/cfn.v120i1.249","text":"Publisher Index Page"},{"id":385519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Minnesota","otherGeospatial":"Rainy Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.7957763671875,\n              48.17707562779612\n            ],\n            [\n              -93.40576171875,\n              48.17707562779612\n            ],\n            [\n              -93.40576171875,\n              48.50204750525715\n            ],\n            [\n              -93.7957763671875,\n              48.50204750525715\n            ],\n            [\n              -93.7957763671875,\n              48.17707562779612\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"120","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-01-01","publicationStatus":"PW","scienceBaseUri":"505a4154e4b0c8380cd65495","contributors":{"authors":[{"text":"Adams, W.E. Jr.","contributorId":23489,"corporation":false,"usgs":true,"family":"Adams","given":"W.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":430370,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kallemeyn, L.W.","contributorId":44864,"corporation":false,"usgs":true,"family":"Kallemeyn","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":430371,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willis, D.W.","contributorId":56179,"corporation":false,"usgs":true,"family":"Willis","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":430372,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031136,"text":"70031136 - 2006 - Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks","interactions":[],"lastModifiedDate":"2023-04-14T13:56:50.490695","indexId":"70031136","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks","docAbstract":"Using detrital zircon geochronology, turbidite deposystems fed from distinct sediment sources can be distinguished within the Songpan-Ganzi complex, a collapsed Middle to Late Triassic turbidite basin of central China. A southern Songpan-Ganzi deposystem initially was sourced solely by erosion of the Qinling-Dabie orogen during early Late Triassic time, then by Qinling-Dabie orogen, North China block, and South China block sources during middle to late Late Triassic time. A northern Songpan-Ganzi system was sourced by erosion of the Qinling-Dabie orogen and the North China block throughout its deposition. These separate deposystems were later tectonically amalgamated to form one complex and then uplifted as the eastern Tibet Plateau. ?? 2006 Geological Society of America.","language":"English","publisher":"Geological Society of America","doi":"10.1130/G21929.1","usgsCitation":"Weislogel, A., Graham, S.A., Chang, E.Z., Wooden, J., Gehrels, G., and Yang, H., 2006, Detrital zircon provenance of the Late Triassic Songpan-Ganzi complex: Sedimentary record of collision of the North and South China blocks: Geology, v. 34, no. 2, p. 97-100, https://doi.org/10.1130/G21929.1.","productDescription":"4 p.","startPage":"97","endPage":"100","numberOfPages":"4","costCenters":[],"links":[{"id":238749,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              100,\n              35.25\n            ],\n            [\n              100,\n              29.75\n            ],\n            [\n              106,\n              29.75\n            ],\n            [\n              106,\n              35.25\n            ],\n            [\n              100,\n              35.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"34","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0000e4b0c8380cd4f521","contributors":{"authors":[{"text":"Weislogel, Amy","contributorId":243156,"corporation":false,"usgs":false,"family":"Weislogel","given":"Amy","email":"","affiliations":[{"id":48650,"text":"West Virginia University,Department of Geology and Geography","active":true,"usgs":false}],"preferred":false,"id":430201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graham, Stephan A.","contributorId":45902,"corporation":false,"usgs":true,"family":"Graham","given":"Stephan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":430204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chang, E. Z.","contributorId":8287,"corporation":false,"usgs":false,"family":"Chang","given":"E.","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":430199,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wooden, Joseph L.","contributorId":32209,"corporation":false,"usgs":true,"family":"Wooden","given":"Joseph L.","affiliations":[],"preferred":false,"id":430203,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gehrels, George E.","contributorId":270803,"corporation":false,"usgs":false,"family":"Gehrels","given":"George E.","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":430200,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Yang, H.","contributorId":48385,"corporation":false,"usgs":true,"family":"Yang","given":"H.","email":"","affiliations":[],"preferred":false,"id":430202,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031110,"text":"70031110 - 2006 - Updated streamflow reconstructions for the Upper Colorado River Basin","interactions":[],"lastModifiedDate":"2018-04-03T11:16:30","indexId":"70031110","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Updated streamflow reconstructions for the Upper Colorado River Basin","docAbstract":"<p><span>Updated proxy reconstructions of water year (October–September) streamflow for four key gauges in the Upper Colorado River Basin were generated using an expanded tree ring network and longer calibration records than in previous efforts. Reconstructed gauges include the Green River at Green River, Utah; Colorado near Cisco, Utah; San Juan near Bluff, Utah; and Colorado at Lees Ferry, Arizona. The reconstructions explain 72–81% of the variance in the gauge records, and results are robust across several reconstruction approaches. Time series plots as well as results of cross‐spectral analysis indicate strong spatial coherence in runoff variations across the subbasins. The Lees Ferry reconstruction suggests a higher long‐term mean than previous reconstructions but strongly supports earlier findings that Colorado River allocations were based on one of the wettest periods in the past 5 centuries and that droughts more severe than any 20th to 21st century event occurred in the past.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005WR004455","usgsCitation":"Woodhouse, C.A., Gray, S., and Meko, D.M., 2006, Updated streamflow reconstructions for the Upper Colorado River Basin: Water Resources Research, v. 42, no. 5, Article W05415; 16 p., https://doi.org/10.1029/2005WR004455.","productDescription":"Article W05415; 16 p.","costCenters":[],"links":[{"id":238910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Upper Colorado River Basin","volume":"42","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-05-11","publicationStatus":"PW","scienceBaseUri":"505bbd1ce4b08c986b328ece","contributors":{"authors":[{"text":"Woodhouse, Connie A.","contributorId":187601,"corporation":false,"usgs":false,"family":"Woodhouse","given":"Connie","email":"","middleInitial":"A.","affiliations":[{"id":32413,"text":"University of Arizona, Tucson, AZ, USA, 85721","active":true,"usgs":false}],"preferred":false,"id":430076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, Stephen T. sgray@usgs.gov","contributorId":221,"corporation":false,"usgs":true,"family":"Gray","given":"Stephen T.","email":"sgray@usgs.gov","affiliations":[{"id":107,"text":"Alaska Climate Science Center","active":true,"usgs":true}],"preferred":true,"id":430074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meko, David M.","contributorId":145887,"corporation":false,"usgs":false,"family":"Meko","given":"David","email":"","middleInitial":"M.","affiliations":[{"id":6624,"text":"University of Arizona, Laboratory of Tree-Ring Research","active":true,"usgs":false}],"preferred":false,"id":430075,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031060,"text":"70031060 - 2006 - The quest for the perfect gravity anomaly: Part 1 - New calculation standards","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031060","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3317,"text":"SEG Technical Program Expanded Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"The quest for the perfect gravity anomaly: Part 1 - New calculation standards","docAbstract":"The North American gravity database together with databases from Canada, Mexico, and the United States are being revised to improve their coverage, versatility, and accuracy. An important part of this effort is revision of procedures and standards for calculating gravity anomalies taking into account our enhanced computational power, modern satellite-based positioning technology, improved terrain databases, and increased interest in more accurately defining different anomaly components. The most striking revision is the use of one single internationally accepted reference ellipsoid for the horizontal and vertical datums of gravity stations as well as for the computation of the theoretical gravity. The new standards hardly impact the interpretation of local anomalies, but do improve regional anomalies. Most importantly, such new standards can be consistently applied to gravity database compilations of nations, continents, and even the entire world. ?? 2005 Society of Exploration Geophysicists.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"SEG Technical Program Expanded Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1190/1.2370391","issn":"10523812","usgsCitation":"Li, X., Hildenbrand, T., Hinze, W.J., Keller, G.R., Ravat, D., and Webring, M., 2006, The quest for the perfect gravity anomaly: Part 1 - New calculation standards: SEG Technical Program Expanded Abstracts, v. 25, no. 1, p. 859-863, https://doi.org/10.1190/1.2370391.","startPage":"859","endPage":"863","numberOfPages":"5","costCenters":[],"links":[{"id":211365,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1190/1.2370391"},{"id":238644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-10-06","publicationStatus":"PW","scienceBaseUri":"505baeeae4b08c986b324414","contributors":{"authors":[{"text":"Li, X.","contributorId":67635,"corporation":false,"usgs":true,"family":"Li","given":"X.","email":"","affiliations":[],"preferred":false,"id":429869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hildenbrand, T.G.","contributorId":83892,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":429871,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinze, W. J.","contributorId":52607,"corporation":false,"usgs":false,"family":"Hinze","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":429868,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keller, Gordon R.","contributorId":90280,"corporation":false,"usgs":true,"family":"Keller","given":"Gordon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":429872,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ravat, D.","contributorId":102971,"corporation":false,"usgs":true,"family":"Ravat","given":"D.","email":"","affiliations":[],"preferred":false,"id":429873,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Webring, M.","contributorId":67662,"corporation":false,"usgs":true,"family":"Webring","given":"M.","affiliations":[],"preferred":false,"id":429870,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031029,"text":"70031029 - 2006 - A new species of freshwater mussel (Bivalvia: Unionidae), Pleurobema athearni, from the Coosa River Drainage of Alabama, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031029","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3814,"text":"Zootaxa","onlineIssn":"1175-5334","printIssn":"1175-5326","active":true,"publicationSubtype":{"id":10}},"title":"A new species of freshwater mussel (Bivalvia: Unionidae), Pleurobema athearni, from the Coosa River Drainage of Alabama, USA","docAbstract":"The Mobile Basin historically supported one of the most diverse freshwater mussel (Bivalvia: Unionidae) assemblages in North America. More than 65 species of mussels are known from the Basin, but it is difficult to determine how many species were present historically. The drainage's unique physical habitat was largely destroyed between the late 1800s and mid-1900s by impoundment and channel modifications of most of the larger rivers. Many species that were once common are now restricted to small headwater rivers and mid-sized tributaries. Recent Coosa River tributary surveys revealed a new, undescribed species of Pleurobema. This new species, Pleurobema athearni, is distinctive in outward appearance, shell morphometry and reproductive morphology, and can be distinguished from other Coosa River drainage unionids. Our analysis indicates that P. athearni is morphologically different from other similar taxa. It differs both in shell width/length and width/height ratios and thus provides a simple, quantitative means to differentiate this species from P. georgianum (Lea, 1841) Fusconaia barnesiana (Lea, 1838), and F. cerina (Conrad, 1838), which it superficially resembles and that also occur in the area. Our morphological diagnosis of this species is supported by recent molecular analyses that suggest this species is a Pleurobema and one closely related to other endemic Coosa River drainage unionids. The discovery of a new species of large, long-lived macroinvertebrate from a relatively well-sampled drainage in a populated region of the southeast United States underscores the need for more detailed surveys in isolated stretches of tributary streams. It should also serve as a reminder that almost 40 species of aquatic mollusks have been extirpated from the Mobile Basin before anything could be learned about their habitat or life history requirements. Copyright ?? 2006 Magnolia Press.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Zootaxa","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"11755326","usgsCitation":"Gangloff, M., Williams, J., and Feminella, J., 2006, A new species of freshwater mussel (Bivalvia: Unionidae), Pleurobema athearni, from the Coosa River Drainage of Alabama, USA: Zootaxa, no. 1118, p. 43-56.","startPage":"43","endPage":"56","numberOfPages":"14","costCenters":[],"links":[{"id":238642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"1118","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4b6e4b0c8380cd46878","contributors":{"authors":[{"text":"Gangloff, M.M.","contributorId":76938,"corporation":false,"usgs":true,"family":"Gangloff","given":"M.M.","affiliations":[],"preferred":false,"id":429692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, J.D.","contributorId":74701,"corporation":false,"usgs":true,"family":"Williams","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":429691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Feminella, J.W.","contributorId":50269,"corporation":false,"usgs":true,"family":"Feminella","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":429690,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031007,"text":"70031007 - 2006 - Scaling uncertainties in estimating canopy foliar maintenance respiration for black spruce ecosystems in Alaska","interactions":[],"lastModifiedDate":"2012-03-12T17:21:16","indexId":"70031007","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2764,"text":"Mitigation and Adaptation Strategies for Global Change","active":true,"publicationSubtype":{"id":10}},"title":"Scaling uncertainties in estimating canopy foliar maintenance respiration for black spruce ecosystems in Alaska","docAbstract":"A major challenge confronting the scientific community is to understand both patterns of and controls over spatial and temporal variability of carbon exchange between boreal forest ecosystems and the atmosphere. An understanding of the sources of variability of carbon processes at fine scales and how these contribute to uncertainties in estimating carbon fluxes is relevant to representing these processes at coarse scales. To explore some of the challenges and uncertainties in estimating carbon fluxes at fine to coarse scales, we conducted a modeling analysis of canopy foliar maintenance respiration for black spruce ecosystems of Alaska by scaling empirical hourly models of foliar maintenance respiration (Rm) to estimate canopy foliar Rm for individual stands. We used variation in foliar N concentration among stands to develop hourly stand-specific models and then developed an hourly pooled model. An uncertainty analysis identified that the most important parameter affecting estimates of canopy foliar Rm was one that describes R m at 0??C per g N, which explained more than 55% of variance in annual estimates of canopy foliar Rm. The comparison of simulated annual canopy foliar Rm identified significant differences between stand-specific and pooled models for each stand. This result indicates that control over foliar N concentration should be considered in models that estimate canopy foliar Rm of black spruce stands across the landscape. In this study, we also temporally scaled the hourly stand-level models to estimate canopy foliar Rm of black spruce stands using mean monthly temperature data. Comparisons of monthly Rm between the hourly and monthly versions of the models indicated that there was very little difference between the estimates of hourly and monthly models, suggesting that hourly models can be aggregated to use monthly input data with little loss of precision. We conclude that uncertainties in the use of a coarse-scale model for estimating canopy foliar Rm at regional scales depend on uncertainties in representing needle-level respiration and on uncertainties in representing the spatial variability of canopy foliar N across a region. The development of spatial data sets of canopy foliar N represents a major challenge in estimating canopy foliar maintenance respiration at regional scales. ?? Springer 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mitigation and Adaptation Strategies for Global Change","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11027-006-1015-5","issn":"13812386","usgsCitation":"Zhang, X., McGuire, A., and Ruess, R.W., 2006, Scaling uncertainties in estimating canopy foliar maintenance respiration for black spruce ecosystems in Alaska: Mitigation and Adaptation Strategies for Global Change, v. 11, no. 1, p. 147-174, https://doi.org/10.1007/s11027-006-1015-5.","startPage":"147","endPage":"174","numberOfPages":"28","costCenters":[],"links":[{"id":211480,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11027-006-1015-5"},{"id":238775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-01-01","publicationStatus":"PW","scienceBaseUri":"505b871ce4b08c986b316302","contributors":{"authors":[{"text":"Zhang, X.","contributorId":30193,"corporation":false,"usgs":true,"family":"Zhang","given":"X.","email":"","affiliations":[],"preferred":false,"id":429613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGuire, A. D.","contributorId":16552,"corporation":false,"usgs":true,"family":"McGuire","given":"A. D.","affiliations":[],"preferred":false,"id":429612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruess, Roger W.","contributorId":45483,"corporation":false,"usgs":false,"family":"Ruess","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":429614,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031002,"text":"70031002 - 2006 - Presence and distribution of wastewater-derived pharmaceuticals in soil irrigated with reclaimed water","interactions":[],"lastModifiedDate":"2018-10-22T10:23:41","indexId":"70031002","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Presence and distribution of wastewater-derived pharmaceuticals in soil irrigated with reclaimed water","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Three sites in the Front Range of Colorado, USA, were monitored from May through September 2003 to assess the presence and distribution of pharmaceuticals in soil irrigated with reclaimed water derived from urban wastewater. Soil cores were collected monthly, and 19 pharmaceuticals, all of which were detected during the present study, were measured in 5‐cm increments of the 30‐cm cores. Samples of reclaimed water were analyzed three times during the study to assess the input of pharmaceuticals. Samples collected before the onset of irrigation in 2003 contained numerous pharmaceuticals, likely resulting from the previous year's irrigation. Several of the selected pharmaceuticals increased in total soil concentration at one or more of the sites. The four most commonly detected pharmaceuticals were erythromycin, carbamazepine, fluoxetine, and diphenhydramine. Typical concentrations of the individual pharmaceuticals observed were low (0.02–15 μg/kg dry soil). The existence of subsurface maximum concentrations and detectable concentrations at the lowest sampled soil depth might indicate interactions of soil components with pharmaceuticals during leaching through the vadose zone. Nevertheless, the present study demonstrates that reclaimed‐water irrigation results in soil pharmaceutical concentrations that vary through the irrigation season and that some compounds persist for months after irrigation.</p></div></div>","language":"English","publisher":"SETAC","doi":"10.1897/05-187R.1","issn":"07307268","usgsCitation":"Kinney, C., Furlong, E., Werner, S., and Cahill, J., 2006, Presence and distribution of wastewater-derived pharmaceuticals in soil irrigated with reclaimed water: Environmental Toxicology and Chemistry, v. 25, no. 2, p. 317-326, https://doi.org/10.1897/05-187R.1.","productDescription":"10 p.","startPage":"317","endPage":"326","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":211422,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/05-187R.1"},{"id":238707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-02-01","publicationStatus":"PW","scienceBaseUri":"505a8b3be4b0c8380cd7e1c2","contributors":{"authors":[{"text":"Kinney, C.A.","contributorId":90516,"corporation":false,"usgs":true,"family":"Kinney","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":429595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Furlong, E. T. 0000-0002-7305-4603","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":98346,"corporation":false,"usgs":true,"family":"Furlong","given":"E. T.","affiliations":[],"preferred":false,"id":429596,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Werner, S.L.","contributorId":82734,"corporation":false,"usgs":true,"family":"Werner","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":429594,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cahill, J.D.","contributorId":77342,"corporation":false,"usgs":true,"family":"Cahill","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":429593,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70030925,"text":"70030925 - 2006 - Influence of landscape-scale factors in limiting brook trout populations in Pennsylvania streams","interactions":[],"lastModifiedDate":"2012-03-12T17:21:16","indexId":"70030925","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Influence of landscape-scale factors in limiting brook trout populations in Pennsylvania streams","docAbstract":"Landscapes influence the capacity of streams to produce trout through their effect on water chemistry and other factors at the reach scale. Trout abundance also fluctuates over time; thus, to thoroughly understand how spatial factors at landscape scales affect trout populations, one must assess the changes in populations over time to provide a context for interpreting the importance of spatial factors. We used data from the Pennsylvania Fish and Boat Commission's fisheries management database to investigate spatial factors that affect the capacity of streams to support brook trout Salvelinus fontinalis and to provide models useful for their management. We assessed the relative importance of spatial and temporal variation by calculating variance components and comparing relative standard errors for spatial and temporal variation. We used binary logistic regression to predict the presence of harvestable-length brook trout and multiple linear regression to assess the mechanistic links between landscapes and trout populations and to predict population density. The variance in trout density among streams was equal to or greater than the temporal variation for several streams, indicating that differences among sites affect population density. Logistic regression models correctly predicted the absence of harvestable-length brook trout in 60% of validation samples. The r 2-value for the linear regression model predicting density was 0.3, indicating low predictive ability. Both logistic and linear regression models supported buffering capacity against acid episodes as an important mechanistic link between landscapes and trout populations. Although our models fail to predict trout densities precisely, their success at elucidating the mechanistic links between landscapes and trout populations, in concert with the importance of spatial variation, increases our understanding of factors affecting brook trout abundance and will help managers and private groups to protect and enhance populations of wild brook trout. ?? Copyright by the American Fisheries Society 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1577/T04-175.1","issn":"00028487","usgsCitation":"Kocovsky, P., and Carline, R., 2006, Influence of landscape-scale factors in limiting brook trout populations in Pennsylvania streams: Transactions of the American Fisheries Society, v. 135, no. 1, p. 76-88, https://doi.org/10.1577/T04-175.1.","startPage":"76","endPage":"88","numberOfPages":"13","costCenters":[],"links":[{"id":211328,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T04-175.1"},{"id":238599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"1","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505a3b4ae4b0c8380cd623d5","contributors":{"authors":[{"text":"Kocovsky, P.M.","contributorId":78447,"corporation":false,"usgs":true,"family":"Kocovsky","given":"P.M.","affiliations":[],"preferred":false,"id":429251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carline, R.F.","contributorId":107444,"corporation":false,"usgs":true,"family":"Carline","given":"R.F.","affiliations":[],"preferred":false,"id":429252,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028636,"text":"70028636 - 2006 - Occurrence and fate of organic contaminants during onsite wastewater treatment","interactions":[],"lastModifiedDate":"2018-10-26T08:48:33","indexId":"70028636","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence and fate of organic contaminants during onsite wastewater treatment","docAbstract":"<div class=\"hlFld-Abstract\"><div id=\"abstractBox\"><p class=\"articleBody_abstractText\">Onsite wastewater treatment systems serve approximately 25% of the U.S. population. However, little is known regarding the occurrence and fate of organic wastewater contaminants (OWCs), including endocrine disrupting compounds, during onsite treatment. A range of OWCs including surfactant metabolites, steroids, stimulants, metal-chelating agents, disinfectants, antimicrobial agents, and pharmaceutical compounds was quantified in wastewater from 30 onsite treatment systems in Summit and Jefferson Counties, CO. The onsite systems represent a range of residential and nonresidential sources. Eighty eight percent of the 24 target compounds were detected in one or more samples, and several compounds were detected in every wastewater sampled. The wastewater matrices were complex and showed unique differences between source types due to differences in water and consumer product use. Nonresidential sources generally had more OWCs at higher concentrations than residential sources. Additional aerobic biofilter-based treatment beyond the traditional anaerobic tank-based treatment enhanced removal for many OWCs. Removal mechanisms included volatilization, biotransformation, and sorption with efficiencies from &lt;1% to &gt;99% depending on treatment type and physico chemical properties of the compound. Even with high removal rates during confined unit onsite treatment, OWCs are discharged to soil dispersal units at loadings up to 20 mg/m<sup>2</sup>/d, emphasizing the importance of understanding removal mechanisms and efficiencies in onsite treatment systems that discharge to the soil and water environments.</p></div></div><div class=\"hlFld-Fulltext\"><br data-mce-bogus=\"1\"></div>","language":"English","publisher":"ACS","doi":"10.1021/es0605117","issn":"0013936X","usgsCitation":"Conn, K., Barber, L.B., Brown, G., and Siegrist, R., 2006, Occurrence and fate of organic contaminants during onsite wastewater treatment: Environmental Science & Technology, v. 40, no. 23, p. 7358-7366, https://doi.org/10.1021/es0605117.","productDescription":"9 p.","startPage":"7358","endPage":"7366","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":209735,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es0605117"},{"id":236432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"23","noUsgsAuthors":false,"publicationDate":"2006-10-26","publicationStatus":"PW","scienceBaseUri":"505a6b65e4b0c8380cd74676","contributors":{"authors":[{"text":"Conn, K.E.","contributorId":64433,"corporation":false,"usgs":true,"family":"Conn","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":418957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barber, L. B.","contributorId":64602,"corporation":false,"usgs":true,"family":"Barber","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":418958,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, G.K.","contributorId":62362,"corporation":false,"usgs":true,"family":"Brown","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":418956,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Siegrist, R.L.","contributorId":54005,"corporation":false,"usgs":true,"family":"Siegrist","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":418955,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028724,"text":"70028724 - 2006 - Emplacement of the Kodiak batholith and slab-window migration","interactions":[],"lastModifiedDate":"2018-10-18T12:23:36","indexId":"70028724","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Emplacement of the Kodiak batholith and slab-window migration","docAbstract":"<p>The Kodiak batholith is one of the largest, most elongate intrusive bodies in the forearc Sanak-Baranof plutonic belt located in southern Alaska. This belt is interpreted to have formed during the subduction of an oceanic spreading center and the associated migration of a slab window. Individual plutons of the Kodiak batholith track the location and evolution of the underlying slab window. Six U/Pb zircon ages from the axis of the batholith exhibit a northeastward-decreasing age progression of 59.2 &plusmn; 0.2 Ma at the southwest end to 58.4 &plusmn; 0.2 Ma at the northeast tip. The trench-parallel rate of age progression is within error of the average slab-window migration rate for the entire Sanak-Baranof belt (~19 cm/yr). Structural relationships, U/Pb ages, and a model of new gravity data indicate that magma from the Kodiak batholith ascended 5-10 km as a northeastward-younging series of 1-8-km-diameter viscoelastic diapirs. Individual plutons ascended by multiple emplacement mechanisms including downward flow, collapse of wall rock, stoping, and diking. Stokes flow xenolith calculations suggest ascent rates of 5-100 m/yr and an effective magmatic viscosity of 107-108 Pa s. Pre-existing structural or lithologic heterogeneities did not dominantly control the location of the main batholith. Instead, its location was determined by migration of the slab window at depth.&nbsp;</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/B25718.1","usgsCitation":"Farris, D.W., Haeussler, P.J., Friedman, R., Paterson, S.R., Saltus, R.W., and Ayuso, R.A., 2006, Emplacement of the Kodiak batholith and slab-window migration: Geological Society of America Bulletin, v. 118, no. 11-12, p. 1360-1376, https://doi.org/10.1130/B25718.1.","productDescription":"17 p.","startPage":"1360","endPage":"1376","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":236718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"11-12","noUsgsAuthors":false,"publicationDate":"2006-12-13","publicationStatus":"PW","scienceBaseUri":"505a0914e4b0c8380cd51dc0","contributors":{"authors":[{"text":"Farris, David W.","contributorId":99360,"corporation":false,"usgs":false,"family":"Farris","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":419443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeussler, Peter J. 0000-0002-1503-6247 pheuslr@usgs.gov","orcid":"https://orcid.org/0000-0002-1503-6247","contributorId":503,"corporation":false,"usgs":true,"family":"Haeussler","given":"Peter","email":"pheuslr@usgs.gov","middleInitial":"J.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":419440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, Richard","contributorId":59363,"corporation":false,"usgs":true,"family":"Friedman","given":"Richard","affiliations":[],"preferred":false,"id":419438,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paterson, Scott R.","contributorId":38338,"corporation":false,"usgs":false,"family":"Paterson","given":"Scott","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":419439,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":419441,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ayuso, Robert A. 0000-0002-8496-9534 rayuso@usgs.gov","orcid":"https://orcid.org/0000-0002-8496-9534","contributorId":2654,"corporation":false,"usgs":true,"family":"Ayuso","given":"Robert","email":"rayuso@usgs.gov","middleInitial":"A.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":419442,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70028726,"text":"70028726 - 2006 - Photometric properties of Titan's surface from Cassini VIMS: Relevance to titan's hemispherical albedo dichotomy and surface stability","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028726","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3083,"text":"Planetary and Space Science","active":true,"publicationSubtype":{"id":10}},"title":"Photometric properties of Titan's surface from Cassini VIMS: Relevance to titan's hemispherical albedo dichotomy and surface stability","docAbstract":"The Visual and Infrared Mapping Spectrometer (VIMS) instrument on the Cassini Saturn Orbiter returned spectral imaging data as the spacecraft undertook six close encounters with Titan beginning 7 July, 2004. Three of these flybys each produced overlapping coverage of two distinct regions of Titan's surface. Twenty-four points were selected on approximately opposite hemispheres to serve as photometric controls. Six points were selected in each of four reflectance classes. On one hemisphere each control point was observed at three distinct phase angles. From the derived phase coefficients, preliminary normal reflectances were derived for each reflectance class. The normal reflectance of Titan's surface units at 2.0178 ??m ranged from 0.079 to 0.185 for the most absorbing to the most reflective units assuming no contribution from absorbing haze. When a modest haze contribution of ??=0.1 is considered these numbers increase to 0.089-0.215. We find that the lowest three reflectance classes have comparable normal reflectance on either hemisphere. However, for the highest brightness class the normal reflectance is higher on the hemisphere encompassing longitude 14-65?? compared to the same high brightness class for the hemisphere encompassing 122-156?? longitude. We conclude that an albedo dichotomy observed in continental sized units on Titan is due not only to one unit having more areal coverage of reflective material than the other but the material on the brighter unit is intrinsically more reflective than the most reflective material on the other unit. This suggests that surface renewal processes are more widespread on Titan's more reflective units than on its less reflective units. We note that one of our photometric control points has increased in reflectance by 12% relative to the surrounding terrain from July of 2004 to April and May of 2005. Possible causes of this effect include atmospheric processes such as ground fog or orographic clouds; the suggestion of active volcanism cannot be ruled out. Several interesting circular features which resembled impact craters were identified on Titan's surface at the time of the initial Titan flyby in July of 2004. We traced photometric profiles through two of these candidate craters and attempted to fit these profiles to the photometric properties expected from model depressions. We find that the best-fit attempt to model these features as craters requires that they be unrealistically deep, approximately 70 km deep. We conclude that despite their appearance, these circular features are not craters, however, the possibility that they are palimpsests cannot be ruled out. We used two methods to test for the presence of vast expanses of liquids on Titan's surface that had been suggested to resemble oceans. Specular reflection of sunlight would be indicative of widespread liquids on the surface; we found no evidence of this. A large liquid body should also show uniformity in photometric profile; we found the profiles to be highly variable. The lack of specular reflection and the high photometric variability in the profiles across candidate oceans is inconsistent with the presence of vast expanses of flat-lying liquids on Titan's surface. While liquid accumulation may be present as small, sub-pixel-sized bodies, or in areas of the surface which still remain to be observed by VIMS, the presence of large ocean-sized accumulations of liquids can be ruled out. The Cassini orbital tour offers the opportunity for VIMS to image the same parts of Titan's surface repeatedly at many different illumination and observation geometries. This creates the possibility of understanding the properties of Titan's atmosphere and haze by iteratively adapting models to create a best fit to the surface reflectance properties. ?? 2006 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Planetary and Space Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.pss.2006.06.014","issn":"00320633","usgsCitation":"Nelson, R., Brown, R.H., Hapke, B., Smythe, W.D., Kamp, L., Boryta, M., Leader, F., Baines, K.H., Bellucci, G., Bibring, J., Buratti, B.J., Capaccioni, F., Cerroni, P., Clark, R.N., Combes, M., Coradini, A., Cruikshank, D.P., Drossart, P., Formisano, V., Jaumann, R., Langevin, Y., Matson, D.L., McCord, T.B., Mennella, V., Nicholson, P.D., Sicardy, B., and Sotin, C., 2006, Photometric properties of Titan's surface from Cassini VIMS: Relevance to titan's hemispherical albedo dichotomy and surface stability: Planetary and Space Science, v. 54, no. 15, p. 1540-1551, https://doi.org/10.1016/j.pss.2006.06.014.","startPage":"1540","endPage":"1551","numberOfPages":"12","costCenters":[],"links":[{"id":209998,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.pss.2006.06.014"},{"id":236784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"15","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7a2ce4b0c8380cd78d92","contributors":{"authors":[{"text":"Nelson, R.M.","contributorId":38316,"corporation":false,"usgs":true,"family":"Nelson","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":419458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":419450,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hapke, B.W.","contributorId":7899,"corporation":false,"usgs":true,"family":"Hapke","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":419449,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smythe, W. D.","contributorId":90878,"corporation":false,"usgs":false,"family":"Smythe","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":419472,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kamp, L.","contributorId":32312,"corporation":false,"usgs":true,"family":"Kamp","given":"L.","email":"","affiliations":[],"preferred":false,"id":419454,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Boryta, M.D.","contributorId":21337,"corporation":false,"usgs":true,"family":"Boryta","given":"M.D.","affiliations":[],"preferred":false,"id":419451,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leader, F.","contributorId":37942,"corporation":false,"usgs":true,"family":"Leader","given":"F.","email":"","affiliations":[],"preferred":false,"id":419457,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Baines, K. H.","contributorId":37868,"corporation":false,"usgs":false,"family":"Baines","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":419456,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Bellucci, G.","contributorId":46256,"corporation":false,"usgs":true,"family":"Bellucci","given":"G.","email":"","affiliations":[],"preferred":false,"id":419460,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Bibring, J.-P.","contributorId":86083,"corporation":false,"usgs":true,"family":"Bibring","given":"J.-P.","email":"","affiliations":[],"preferred":false,"id":419470,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Buratti, B. J.","contributorId":69280,"corporation":false,"usgs":false,"family":"Buratti","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":419467,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Capaccioni, F.","contributorId":90900,"corporation":false,"usgs":true,"family":"Capaccioni","given":"F.","email":"","affiliations":[],"preferred":false,"id":419473,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Cerroni, P.","contributorId":7869,"corporation":false,"usgs":true,"family":"Cerroni","given":"P.","affiliations":[],"preferred":false,"id":419448,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":419447,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Combes, M.","contributorId":66892,"corporation":false,"usgs":true,"family":"Combes","given":"M.","affiliations":[],"preferred":false,"id":419466,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Coradini, A.","contributorId":34679,"corporation":false,"usgs":true,"family":"Coradini","given":"A.","affiliations":[],"preferred":false,"id":419455,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Cruikshank, D. P.","contributorId":51434,"corporation":false,"usgs":false,"family":"Cruikshank","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":419461,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Drossart, P.","contributorId":29574,"corporation":false,"usgs":true,"family":"Drossart","given":"P.","affiliations":[],"preferred":false,"id":419453,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Formisano, V.","contributorId":44694,"corporation":false,"usgs":true,"family":"Formisano","given":"V.","email":"","affiliations":[],"preferred":false,"id":419459,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Jaumann, R.","contributorId":81232,"corporation":false,"usgs":false,"family":"Jaumann","given":"R.","email":"","affiliations":[],"preferred":false,"id":419469,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Langevin, Y.","contributorId":24900,"corporation":false,"usgs":true,"family":"Langevin","given":"Y.","email":"","affiliations":[],"preferred":false,"id":419452,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Matson, D. L.","contributorId":59940,"corporation":false,"usgs":false,"family":"Matson","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":419465,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"McCord, T. B.","contributorId":69695,"corporation":false,"usgs":false,"family":"McCord","given":"T.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":419468,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Mennella, V.","contributorId":88522,"corporation":false,"usgs":true,"family":"Mennella","given":"V.","affiliations":[],"preferred":false,"id":419471,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Nicholson, P. D.","contributorId":54330,"corporation":false,"usgs":false,"family":"Nicholson","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":419463,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Sicardy, B.","contributorId":57622,"corporation":false,"usgs":true,"family":"Sicardy","given":"B.","affiliations":[],"preferred":false,"id":419464,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Sotin, Christophe","contributorId":53924,"corporation":false,"usgs":false,"family":"Sotin","given":"Christophe","email":"","affiliations":[],"preferred":false,"id":419462,"contributorType":{"id":1,"text":"Authors"},"rank":27}]}}
,{"id":70028728,"text":"70028728 - 2006 - Titan: Preliminary results on surface properties and photometry from VIMS observations of the early flybys","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70028728","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3083,"text":"Planetary and Space Science","active":true,"publicationSubtype":{"id":10}},"title":"Titan: Preliminary results on surface properties and photometry from VIMS observations of the early flybys","docAbstract":"Cassini observations of the surface of Titan offer unprecedented views of its surface through atmospheric windows in the 1-5 ??m region. Images obtained in windows for which the haze opacity is low can be used to derive quantitative photometric parameters such as albedo and albedo distribution, and physical properties such as roughness and particle characteristics. Images from the early Titan flybys, particularly T0, Ta, and T5 have been analyzed to create albedo maps in the 2.01 and 2.73 ??m windows. We find the average normal reflectance at these two wavelengths to be 0.15??0.02 and 0.035??0.003, respectively. Titan's surface is bifurcated into two albedo regimes, particularly at 2.01 ??m. Analysis of these two regimes to understand the physical character of the surface was accomplished with a macroscopic roughness model. We find that the two types of surface have substantially different roughness, with the low-albedo surface exhibiting mean slope angles of ???18??, and the high-albedo terrain having a much more substantial roughness with a mean slope angle of ???34??. A single-scattering phase function approximated by a one-term Henyey-Greenstein equation was also fit to each unit. Titan's surface is back-scattering (g???0.3-0.4), and does not exhibit substantially different backscattering behavior between the two terrains. Our results suggest that two distinct geophysical domains exist on Titan: a bright region cut by deep drainage channels and a relatively smooth surface. The two terrains are covered by a film or a coating of particles perhaps precipitated from the satellite's haze layer and transported by eolian processes. Our results are preliminary: more accurate values for the surface albedo and physical parameters will be derived as more data is gathered by the Cassini spacecraft and as a more complete radiative transfer model is developed from both Cassini orbiter and Huygens Lander measurements. ?? 2006 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Planetary and Space Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.pss.2006.06.015","issn":"00320633","usgsCitation":"Buratti, B.J., Sotin, C., Brown, R.H., Hicks, M., Clark, R.N., Mosher, J.A., McCord, T.B., Jaumann, R., Baines, K.H., Nicholson, P.D., Momary, T., Simonelli, D., and Sicardy, B., 2006, Titan: Preliminary results on surface properties and photometry from VIMS observations of the early flybys: Planetary and Space Science, v. 54, no. 15, p. 1498-1509, https://doi.org/10.1016/j.pss.2006.06.015.","startPage":"1498","endPage":"1509","numberOfPages":"12","costCenters":[],"links":[{"id":209607,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.pss.2006.06.015"},{"id":236261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"15","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb41fe4b08c986b3261c5","contributors":{"authors":[{"text":"Buratti, B. J.","contributorId":69280,"corporation":false,"usgs":false,"family":"Buratti","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":419493,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sotin, Christophe","contributorId":53924,"corporation":false,"usgs":false,"family":"Sotin","given":"Christophe","email":"","affiliations":[],"preferred":false,"id":419490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":419486,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hicks, M.D.","contributorId":7045,"corporation":false,"usgs":true,"family":"Hicks","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":419484,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clark, R. N.","contributorId":6568,"corporation":false,"usgs":true,"family":"Clark","given":"R.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":419483,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mosher, J. A.","contributorId":34605,"corporation":false,"usgs":false,"family":"Mosher","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":419487,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McCord, T. B.","contributorId":69695,"corporation":false,"usgs":false,"family":"McCord","given":"T.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":419494,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jaumann, R.","contributorId":81232,"corporation":false,"usgs":false,"family":"Jaumann","given":"R.","email":"","affiliations":[],"preferred":false,"id":419495,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Baines, K. H.","contributorId":37868,"corporation":false,"usgs":false,"family":"Baines","given":"K.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":419488,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Nicholson, P. D.","contributorId":54330,"corporation":false,"usgs":false,"family":"Nicholson","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":419491,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Momary, T.","contributorId":17415,"corporation":false,"usgs":true,"family":"Momary","given":"T.","affiliations":[],"preferred":false,"id":419485,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Simonelli, D.P.","contributorId":42373,"corporation":false,"usgs":true,"family":"Simonelli","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":419489,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Sicardy, B.","contributorId":57622,"corporation":false,"usgs":true,"family":"Sicardy","given":"B.","affiliations":[],"preferred":false,"id":419492,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70028861,"text":"70028861 - 2006 - Does body size affect a bird's sensitivity to patch size and landscape structure?","interactions":[],"lastModifiedDate":"2017-08-31T13:24:03","indexId":"70028861","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Does body size affect a bird's sensitivity to patch size and landscape structure?","docAbstract":"<p><span>Larger birds are generally more strongly affected by habitat loss and fragmentation than are smaller ones because they require more resources and thus larger habitat patches. Consequently, conservation actions often favor the creation or protection of larger over smaller patches. However, in grassland systems the boundaries between a patch and the surrounding landscape, and thus the perceived size of a patch, can be indistinct. We investigated whether eight grassland bird species with different body sizes perceived variation in patch size and landscape structure in a consistent manner. Data were collected from surveys conducted in 44 patches of northern tallgrass prairie during 1998–2001. The response to patch size was very similar among species regardless of body size (density was little affected by patch size), except in the Greater Prairie-Chicken (</span><i>Tympanuchus cupido</i><span>), which showed a threshold effect and was not found in patches smaller than 140 ha. In landscapes containing 0%–30% woody vegetation, smaller species responded more negatively to increases in the percentage of woody vegetation than larger species, but above an apparent threshold of 30%, larger species were not detected. Further analyses revealed that the observed variation in responses to patch size and landscape structure among species was not solely due to body size per se, but to other differences among species. These results indicate that a stringent application of concepts requiring larger habitat patches for larger species appears to limit the number of grassland habitats that can be protected and may not always be the most effective conservation strategy.</span></p>","language":"English","publisher":"American Ornithological Society","doi":"10.1650/0010-5422(2006)108[808:DBSAAB]2.0.CO;2","issn":"00105422","usgsCitation":"Winter, M., Johnson, D.H., and Shaffer, J.A., 2006, Does body size affect a bird's sensitivity to patch size and landscape structure?: Condor, v. 108, no. 4, p. 808-816, https://doi.org/10.1650/0010-5422(2006)108[808:DBSAAB]2.0.CO;2.","productDescription":"9 p.","startPage":"808","endPage":"816","numberOfPages":"9","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":477445,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1650/0010-5422(2006)108[808:dbsaab]2.0.co;2","text":"Publisher Index Page"},{"id":236553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209825,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1650/0010-5422(2006)108[808:DBSAAB]2.0.CO;2"}],"volume":"108","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a038ce4b0c8380cd50524","contributors":{"authors":[{"text":"Winter, Maiken","contributorId":174790,"corporation":false,"usgs":false,"family":"Winter","given":"Maiken","email":"","affiliations":[],"preferred":false,"id":420065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Douglas H. 0000-0002-7778-6641 douglas_h_johnson@usgs.gov","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":1387,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"douglas_h_johnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":420066,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaffer, Jill A. 0000-0003-3172-0708 jshaffer@usgs.gov","orcid":"https://orcid.org/0000-0003-3172-0708","contributorId":3184,"corporation":false,"usgs":true,"family":"Shaffer","given":"Jill","email":"jshaffer@usgs.gov","middleInitial":"A.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":420064,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028886,"text":"70028886 - 2006 - Cloud-to-ground lightning and surface rainfall in warm-season Florida thunderstorms","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70028886","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2316,"text":"Journal of Geophysical Research D: Atmospheres","active":true,"publicationSubtype":{"id":10}},"title":"Cloud-to-ground lightning and surface rainfall in warm-season Florida thunderstorms","docAbstract":"Relationships between cloud-to-ground (CG) lightning and surface rainfall have been examined in nine isolated, warm-season thunderstorms on the east coast of central Florida. CG flashes and the associated rain volumes were measured as a function of time in storm-centered reference frames that followed each storm over a network of rain gauges. Values of the storm-average rain volume per CG flash ranged from 0.70 ?? 104 to 6.4 ?? 104 m3/CG flash, with a mean (and standard deviation) of 2.6 ?? 104 ?? 2.1 ?? 104 m3/CG flash. Values of the rain volume concurrent with CG flashes ranged from 0.11 ?? 104 to 4.9 ?? 104 m3/CG flash with a mean of 2.1 ?? 104 ?? 2.0 ?? 104 m3/CG flash. The lag-time between the peak CG flash rate and the peak rainfall rate (using 5 min bins), and the results of a lag correlation analysis, show that surface rainfall tends to follow the lightning (positive lag) by up to 20 min in six storms. In one storm the rainfall preceded the lightning by 5 min, and two storms had nonsignificant lags. Values of the lagged rain volume concurrent with CG flashes ranged from 0.43 ?? 104 to 4.9 ?? 104 m3/CG flash, and the mean was 1.9 ?? 104 ?? 1.7 ?? 104 m3/CG flash. For the five storms that produced 12 or more flashes and had significant lags, a plot of the optimum lag time versus the total number of CG flashes shows a linear trend (R2 = 0.56). The number of storms is limited, but the lag results do indicate that large storms tend to have longer lags. A linear fit to the lagged rain volume vs. the number of concurrent CG flashes has a slope of 1.9 ?? 104 m3/CG flash (R2 = 0.83). We conclude that warm-season Florida thunderstorms produce a roughly constant rain volume per CG flash and that CG lightning can be used to estimate the location and intensity of convective rainfall in that weather regime. Copyright 2006 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research D: Atmospheres","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JD006802","issn":"01480227","usgsCitation":"Gungle, B., and Krider, E., 2006, Cloud-to-ground lightning and surface rainfall in warm-season Florida thunderstorms: Journal of Geophysical Research D: Atmospheres, v. 111, no. 19, https://doi.org/10.1029/2005JD006802.","costCenters":[],"links":[{"id":477402,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jd006802","text":"Publisher Index Page"},{"id":209746,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JD006802"},{"id":236447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"19","noUsgsAuthors":false,"publicationDate":"2006-10-11","publicationStatus":"PW","scienceBaseUri":"5059f676e4b0c8380cd4c79d","contributors":{"authors":[{"text":"Gungle, B.","contributorId":90920,"corporation":false,"usgs":true,"family":"Gungle","given":"B.","affiliations":[],"preferred":false,"id":420184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krider, E.P.","contributorId":107914,"corporation":false,"usgs":true,"family":"Krider","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":420185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028897,"text":"70028897 - 2006 - Sampling blood from big brown bats (Eptesicus fuscus) in the field with and without anesthesia: Impacts on survival","interactions":[],"lastModifiedDate":"2012-03-12T17:20:41","indexId":"70028897","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Sampling blood from big brown bats (Eptesicus fuscus) in the field with and without anesthesia: Impacts on survival","docAbstract":"Blood was collected from wild big brown bats (Eptesicus fuscus) with and without anesthesia in Fort Collins, Colorado in 2004 to assess the impacts of these procedures on short-term survival and 1-yr return rates. Short-term survival and 1-yr return rates after release were passively monitored using PIT tag detection hoops placed at selected buildings. Comparison of 14-day maximum likelihood survival estimates from bats not bled (142 adult females, 62 volant juveniles), and bats sampled for blood with anesthesia (96 adult females, 23 volant juveniles) and without anesthesia (112 adult females, 22 volant juveniles) indicated no adverse effects of either treatment (juveniles: X2=53.38, df=41, P=0.09; adults: X2=39.09, df=44, P=0.68). Return rates of bats one year after sampling were similar among adult female controls (75.4%, n=142, 95% CI=67.4-82.2%), females sampled for blood with anesthesia (83.0%, n=112, 95% CI=74.8-89.5%), and females sampled without anesthesia (87.5%, n=96, 95% CI=79.2-93.4%). Lack of an effect was also noted in 1-yr return rates of juvenile females. These data suggest that the use of anesthesia during sampling of blood has no advantages in terms of enhancement of survival in big brown bats. ?? Wildlife Disease Association 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Diseases","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00903558","usgsCitation":"Ellison, L., O'Shea, T., Wimsatt, J., Pearce, R., Neubaum, D., Neubaum, M., and Bowen, R.A., 2006, Sampling blood from big brown bats (Eptesicus fuscus) in the field with and without anesthesia: Impacts on survival: Journal of Wildlife Diseases, v. 42, no. 4, p. 849-852.","startPage":"849","endPage":"852","numberOfPages":"4","costCenters":[],"links":[{"id":236655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ab073e4b0c8380cd87afa","contributors":{"authors":[{"text":"Ellison, L.E.","contributorId":103610,"corporation":false,"usgs":true,"family":"Ellison","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":420402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O'Shea, T. J. 0000-0002-0758-9730","orcid":"https://orcid.org/0000-0002-0758-9730","contributorId":50100,"corporation":false,"usgs":true,"family":"O'Shea","given":"T. J.","affiliations":[],"preferred":false,"id":420398,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wimsatt, J.","contributorId":78289,"corporation":false,"usgs":true,"family":"Wimsatt","given":"J.","affiliations":[],"preferred":false,"id":420400,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearce, R.D.","contributorId":45439,"corporation":false,"usgs":true,"family":"Pearce","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":420397,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Neubaum, D.J.","contributorId":43720,"corporation":false,"usgs":true,"family":"Neubaum","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":420396,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Neubaum, M.A.","contributorId":50866,"corporation":false,"usgs":true,"family":"Neubaum","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":420399,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bowen, R. A.","contributorId":80623,"corporation":false,"usgs":false,"family":"Bowen","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":420401,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70028898,"text":"70028898 - 2006 - Abundance and distribution of selected elements in soils, stream sediments, and selected forage plants from desert tortoise habitats in the Mojave and Colorado deserts, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:41","indexId":"70028898","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2183,"text":"Journal of Arid Environments","active":true,"publicationSubtype":{"id":10}},"title":"Abundance and distribution of selected elements in soils, stream sediments, and selected forage plants from desert tortoise habitats in the Mojave and Colorado deserts, USA","docAbstract":"A baseline and background chemical survey was conducted in southeastern California, USA, to identify potential sources of toxicants in natural and anthropogenically-altered habitats of the threatened desert tortoise (Gopherus agassizii). Soil, stream sediment, and plant samples were collected from six tortoise habitat study areas in the Mojave and Colorado deserts and analysed for up to 66 different elements. The chemical analyses provided new information on the abundances and distributions of selected elements in this region. Soil, stream-sediment, and plant analyses showed distinct variations in bulk chemistries from locality to locality. Variations were, in general, consistent with the many types of exposed rock units in the region, their highly variable bulk mineralogies, and chemical contents. Of elements in soils that might have been toxic to tortoises, only As seemed to be anomalous region-wide. Some soil and plant anomalies were clearly anthropogenic. In the Rand and Atolia mining districts, soil anomalies for As, Au, Cd, Hg, Sb, and(or) W and plant anomalies for As, Sb, and(or) W extend as far as ???15 km outward from the present area of mining; soils containing anomalous Hg were found at least 6 km away from old piles of tailings. The anomalous concentrations of As and Hg may have been the source of elevated levels of these elements found in ill tortoises from the region. In the Goldstone mining district, soil anomalies extended several km from the mining area. These areas probably represented anthropogenic surface contamination of dust redistributed by wind, vehicles, and rainfall. One of two study areas transected by a paved road (Chemehuevi Valley) showed weakly elevated levels of Pb, which extended as far as ???22 m from the pavement edge and were probably related to vehicle exhaust. No soil or plant samples from historically used military areas (Goldstone, Goffs, Chemehuevi Valley, Chuckwalla Bench) contained anomalous concentrations of the elements As, Cu, Cr, Fe, Pb, or Zn that could be ascribed to military maneuvers, vehicles, or ordnance. For future studies, the distribution and abundance of elements in the tortoise forage plants need to be evaluated for the respective roles of dust and systemic uptake. Additional chemical data from tortoise necropsies and nutritional studies are needed to determine the effects of potentially toxic elements in tortoise habitats on their health. ?? 2006 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Arid Environments","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jaridenv.2006.09.018","issn":"01401963","usgsCitation":"Chaffee, M., and Berry, K., 2006, Abundance and distribution of selected elements in soils, stream sediments, and selected forage plants from desert tortoise habitats in the Mojave and Colorado deserts, USA: Journal of Arid Environments, v. 67, no. SUPPL., p. 35-87, https://doi.org/10.1016/j.jaridenv.2006.09.018.","startPage":"35","endPage":"87","numberOfPages":"53","costCenters":[],"links":[{"id":209906,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jaridenv.2006.09.018"},{"id":236656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"SUPPL.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e659e4b0c8380cd47365","contributors":{"authors":[{"text":"Chaffee, M.A.","contributorId":108049,"corporation":false,"usgs":true,"family":"Chaffee","given":"M.A.","affiliations":[],"preferred":false,"id":420404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, K.H.","contributorId":17934,"corporation":false,"usgs":true,"family":"Berry","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":420403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1016485,"text":"1016485 - 2006 - Sex determination of Pohnpei Micronesian kingfishers using morphological and molecular genetic techniques","interactions":[],"lastModifiedDate":"2012-02-02T00:04:51","indexId":"1016485","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2284,"text":"Journal of Field Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"Sex determination of Pohnpei Micronesian kingfishers using morphological and molecular genetic techniques","docAbstract":"Conservation-oriented studies of Micronesian Kingfishers (Todiramphus cinnamominus) have been hindered by a lack of basic natural history information, despite the status of the Guam subspecies (T. c. cinnamominus) as one of the most endangered species in the world. We used tissue samples and morphometric measures from museum specimens and wild-captured Pohnpei Micronesian Kingfishers (T. c. reichenbachii) to develop methods for sex determination. We present a modified molecular protocol and a discriminant function that yields the probability that a particular individual is male or female. Our results revealed that females were significantly larger than males, and the discriminant function correctly predicted sex in 73% (30/41) of the individuals. The sex of 86% (18/21) of individuals was correctly assigned when a moderate reliability threshold was set. Sex determination using molecular genetic techniques was more reliable than methods based on morphology. Our results will facilitate recovery efforts for the critically endangered Guam Micronesian Kingfisher and provide a basis for sex determination in the 11 other endangered congeners in the Pacific Basin.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Field Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Kesler, D.C., Lopes, I., and Haig, S.M., 2006, Sex determination of Pohnpei Micronesian kingfishers using morphological and molecular genetic techniques: Journal of Field Ornithology, v. 77, no. 2, p. 229-232.","productDescription":"p. 229-232","startPage":"229","endPage":"232","numberOfPages":"4","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":134234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4ad6","contributors":{"authors":[{"text":"Kesler, Dylan C.","contributorId":14358,"corporation":false,"usgs":false,"family":"Kesler","given":"Dylan","email":"","middleInitial":"C.","affiliations":[{"id":6769,"text":"University of Missouri, Columbia, MO","active":true,"usgs":false}],"preferred":false,"id":324296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lopes, I.F.","contributorId":85558,"corporation":false,"usgs":true,"family":"Lopes","given":"I.F.","email":"","affiliations":[],"preferred":false,"id":324297,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haig, Susan M. 0000-0002-6616-7589 susan_haig@usgs.gov","orcid":"https://orcid.org/0000-0002-6616-7589","contributorId":719,"corporation":false,"usgs":true,"family":"Haig","given":"Susan","email":"susan_haig@usgs.gov","middleInitial":"M.","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":324295,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1015122,"text":"1015122 - 2006 - A permutation test for quantile regression","interactions":[],"lastModifiedDate":"2017-12-30T10:33:35","indexId":"1015122","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2151,"text":"Journal of Agricultural, Biological, and Environmental Statistics","active":true,"publicationSubtype":{"id":10}},"title":"A permutation test for quantile regression","docAbstract":"<p>A drop in dispersion, <i class=\"EmphasisTypeItalic \">F</i>-ratio like, permutation test (<i class=\"EmphasisTypeItalic \">D</i>) for linear quantile regression estimates (0≤τ≤1) had relative power ≥1 compared to quantile rank score tests (<i class=\"EmphasisTypeItalic \">T</i>) for hypotheses on parameters other than the intercept. Power was compared for combinations of sample sizes (<i class=\"EmphasisTypeItalic \">n</i>=20−300) and quantiles (τ=0.50−0.99) where both tests maintained valid Type I error rates in simulations with <i class=\"EmphasisTypeItalic \">p</i>=2 and 6 parameters in homogeneous and heterogeneous error models. The <i class=\"EmphasisTypeItalic \">D</i> test required two modifications of permuting residuals from null, reduced parameter models to maintain correct Type I error rates when null models were constrained through the origin or included multiple parameters. A double permutation scheme was used when null models were constrained through the origin and all but 1 of the zero residuals were deleted for null models with multiple parameters. Although there was considerable overlap in sample size, quantiles, and hypotheses where both the <i class=\"EmphasisTypeItalic \">D</i> and rank score tests maintained correct Type I error rates, we identified regions at smaller <i class=\"EmphasisTypeItalic \">n</i> and more extreme quantiles where one or the other maintained better error rates. Confidence intervals on parameters for an ecological application relating Lahontan cutthroat trout densities to stream channel width:depth were estimated by test inversion, demonstrating a smoother pattern of slightly narrower intervals across quantiles than those provided by the rank score test.</p>","language":"English","publisher":"Springer","doi":"10.1198/108571106X96835","usgsCitation":"Cade, B.S., and Richards, J.D., 2006, A permutation test for quantile regression: Journal of Agricultural, Biological, and Environmental Statistics, v. 11, no. 1, p. 106-126, https://doi.org/10.1198/108571106X96835.","productDescription":"21 p.","startPage":"106","endPage":"126","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":131759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab830","contributors":{"authors":[{"text":"Cade, Brian S. 0000-0001-9623-9849 cadeb@usgs.gov","orcid":"https://orcid.org/0000-0001-9623-9849","contributorId":1278,"corporation":false,"usgs":true,"family":"Cade","given":"Brian","email":"cadeb@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":322233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richards, Jon D.","contributorId":181580,"corporation":false,"usgs":false,"family":"Richards","given":"Jon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":322232,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028915,"text":"70028915 - 2006 - Coseismic and postseismic slip of the 2004 Parkfield earthquake from space-geodetic data","interactions":[],"lastModifiedDate":"2012-03-12T17:20:58","indexId":"70028915","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Coseismic and postseismic slip of the 2004 Parkfield earthquake from space-geodetic data","docAbstract":"We invert interferometric synthetic aperture radar (InSAR) data jointly with campaign and continuous global positioning system (GPS) data for slip in the coseismic and postseismic periods of the 2004 Parkfield earthquake. The InSAR dataset consists of eight interferograms from data collected by the Envisat and Radarsat satellites spanning the time of the earthquake and variable amounts of the postseismic period. The two datasets complement each other, with the InSAR providing dense sampling of motion in the range direction of the satellite and the GPS providing more sparse, but three-dimensional measurements of ground motion. The model assumes exponential decay of the postseismic slip with a decay time constant of 0.087 years, determined from time series modeling of continuous GPS and creepmeter data. We find a geodetic moment magnitude of M 6.2 for a 1-day coseismic model and Mw 6.1 for the entire postseismic period. The coseismic rupture occurred mainly in two slip asperities; one near the hypocenter and the other 15-20 km north. Postseismic slip occurred on the shallow portions of the fault and near the rupture areas of two M 5.0 aftershocks. A comparison of the geodetic slip models with seismic moment estimates suggests that the coseismic moment release of the Parkfield earthquake is as little as 25% of the total. This underlines the importance of aseismic slip in the slip budget for the Parkfield segment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/0120050818","issn":"00371106","usgsCitation":"Johanson, I., Fielding, E., Rolandone, F., and Burgmann, R., 2006, Coseismic and postseismic slip of the 2004 Parkfield earthquake from space-geodetic data: Bulletin of the Seismological Society of America, v. 96, no. 4 B, https://doi.org/10.1785/0120050818.","costCenters":[],"links":[{"id":209701,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120050818"},{"id":236381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"4 B","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc5be4b0c8380cd4e23d","contributors":{"authors":[{"text":"Johanson, I.A.","contributorId":36735,"corporation":false,"usgs":true,"family":"Johanson","given":"I.A.","email":"","affiliations":[],"preferred":false,"id":420534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fielding, E.J.","contributorId":64871,"corporation":false,"usgs":true,"family":"Fielding","given":"E.J.","affiliations":[],"preferred":false,"id":420536,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rolandone, F.","contributorId":54783,"corporation":false,"usgs":true,"family":"Rolandone","given":"F.","affiliations":[],"preferred":false,"id":420535,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burgmann, R.","contributorId":10167,"corporation":false,"usgs":true,"family":"Burgmann","given":"R.","affiliations":[],"preferred":false,"id":420533,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}