Infectious haematopoietic necrosis virus (IHNV) is one of the most important viral pathogens of salmonids. In rainbow trout, IHNV isolates in the M genogroup are highly pathogenic, while U genogroup isolates are significantly less pathogenic. We show here that, at a multiplicity of infection (MOI) of 1, a representative U type strain yielded 42‐fold less infectious virus than an M type strain in the rainbow trout–derived RTG‐2 cell line at 24 h post‐infection (p.i.). However, at an MOI of 10, there was only fivefold difference in the yield of infectious virus between the U and M strains. Quantification of extracellular viral genomic RNA suggested that the number of virus particles released from cells infected with the U strain at a MOI of 1 was 47‐fold lower than from M‐infected cells, but U and M virions were equally infectious by particle to infectivity ratios. At an MOI of 1, U strain intracellular viral genome accumulation and transcription were 37‐ and 12‐fold lower, respectively, than those of the M strain at 24 h p.i. Viral nucleocapsid (N) protein accumulation in U strain infections was fivefold lower than in M strain infections. These results suggest that the block in U type strain growth in RTG‐2 cells was because of the effects of reduced genome replication and transcription. The reduced growth of the U strain does not seem to be caused by defective genes, because the U and M strains grew equally well in the permissive epithelioma papulosum cyprini cell line at an MOI of 1. This suggests that host‐specific factors in RTG‐2 cells control the growth of the IHNV U and M strains differently, leading to growth restriction of the U type virus during the RNA synthesis step.
","language":"English","publisher":"Wiley","publisherLocation":"Oxford, UK","doi":"10.1111/j.1365-2761.2010.01153.x","usgsCitation":"Park, J.W., Moon, C.H., Wargo, A., Purcell, M., and Kurath, G., 2010, Differential growth of U and M type infectious haematopoietic necrosis virus in a rainbow trout–derived cell line, RTG-2: Journal of Fish Diseases, v. 33, no. 7, p. 583-591, https://doi.org/10.1111/j.1365-2761.2010.01153.x.","productDescription":"9 p.","startPage":"583","endPage":"591","numberOfPages":"9","ipdsId":"IP-019735","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":270779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"33","issue":"7","noUsgsAuthors":false,"publicationDate":"2010-06-09","publicationStatus":"PW","scienceBaseUri":"516689e0e4b0bba30b388bcb","contributors":{"authors":[{"text":"Park, Jeong Woo","contributorId":40489,"corporation":false,"usgs":true,"family":"Park","given":"Jeong","email":"","middleInitial":"Woo","affiliations":[],"preferred":false,"id":474113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moon, Chang Hoon","contributorId":68193,"corporation":false,"usgs":true,"family":"Moon","given":"Chang","email":"","middleInitial":"Hoon","affiliations":[],"preferred":false,"id":474114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wargo, Andrew","contributorId":73480,"corporation":false,"usgs":true,"family":"Wargo","given":"Andrew","affiliations":[],"preferred":false,"id":474115,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Purcell, Maureen K. mpurcell@usgs.gov","contributorId":3061,"corporation":false,"usgs":true,"family":"Purcell","given":"Maureen K.","email":"mpurcell@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":474112,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":2629,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":474111,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70043682,"text":"70043682 - 2010 - Characterization of mannitol in Curvularia protuberata hyphae by FTIR and Raman spectromicroscopy","interactions":[],"lastModifiedDate":"2021-04-22T20:33:41.067139","indexId":"70043682","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":759,"text":"Analyst","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Characterization of mannitol in Curvularia protuberata hyphae by FTIR and Raman spectromicroscopy","title":"Characterization of mannitol in Curvularia protuberata hyphae by FTIR and Raman spectromicroscopy","docAbstract":"FTIR and Raman spectromicroscopy were used to characterize the composition of Curvularia protuberata hyphae, and to compare a strain isolated from plants inhabiting geothermal soils with a non-geothermal isolate. Thermal IR source images of hyphae have been acquired with a 64 × 64 element focal plane array detector; single point IR spectra have been obtained with synchrotron source light. In some C. protuberata hyphae, we have discovered the spectral signature of crystalline mannitol, a fungal polyol with complex protective roles. With FTIR-FPA imaging, we have determined that the protein content in cells remains fairly constant throughout the length of a hypha, whereas the mannitol is found at discrete, irregular locations. This is the first direct observation of mannitol in intact fungal hyphae. Since the concentration of mannitol in cells varies with respect to position and is not present in all hyphae, this discovery may be related to habitat adaptation, fungal structure and growth stages.
A common clinical sign of ichthyophoniasis in herring and trout is “sandpaper” skin, a roughening of the epidermis characterized by the appearance of small papules, followed by ulceration and sloughing of the epithelium; early investigators hypothesized that these ulcers might be a means of transmitting the parasite, Ichthyophonus sp., without the necessity of ingesting an infected host. We examined the cells associated with the epidermal lesions and confirmed that they were viable Ichthyophonus sp. cells that were readily released from the skin into the mucous layer and ultimately into the aquatic environment. The released cells were infectious when injected into the body cavity of specific-pathogen-free herring. Our hypothesis is that different mechanisms of transmission occur in carnivorous and planktivorous hosts: Planktonic feeders become infected by ingestion of ulcer-derived cells, while carnivores become infected by ingestion of whole infected fish.
","language":"English","publisher":"American Society of Parasitologists","doi":"10.1645/GE-2292.1","usgsCitation":"Hershberger, P., Gregg, J.L., and Kocan, R.M., 2010, Release of infectious cells from epidermal ulcers in Ichthyophonus sp.–infected Pacific Herring (Clupea pallasii): Evidence for multiple mechanisms of transmission: Journal of Parasitology, v. 96, no. 2, p. 348-352, https://doi.org/10.1645/GE-2292.1.","productDescription":"5 p.","startPage":"348","endPage":"352","ipdsId":"IP-016955","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":270781,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":270780,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1645/GE-2292.1"}],"volume":"96","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516689e4e4b0bba30b388be2","contributors":{"authors":[{"text":"Hershberger, Paul K. phershberger@usgs.gov","contributorId":1945,"corporation":false,"usgs":true,"family":"Hershberger","given":"Paul K.","email":"phershberger@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":474082,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gregg, Jacob L. jgregg@usgs.gov","contributorId":2884,"corporation":false,"usgs":true,"family":"Gregg","given":"Jacob","email":"jgregg@usgs.gov","middleInitial":"L.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":474083,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kocan, R. M.","contributorId":41783,"corporation":false,"usgs":true,"family":"Kocan","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":474084,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70044283,"text":"70044283 - 2010 - Heat Flow and Hydrologic Characteristics at the AND-1B borehole, ANDRILL McMurdo Ice Shelf Project, Antarctica","interactions":[],"lastModifiedDate":"2013-04-10T13:44:58","indexId":"70044283","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1820,"text":"Geosphere","active":true,"publicationSubtype":{"id":10}},"title":"Heat Flow and Hydrologic Characteristics at the AND-1B borehole, ANDRILL McMurdo Ice Shelf Project, Antarctica","docAbstract":"The Antarctic Drilling Program (ANDRILL) successfully drilled and cored a borehole, AND-1B, beneath the McMurdo Ice Shelf and into a flexural moat basin that surrounds Ross Island. Total drilling depth reached 1285 m below seafloor (mbsf) with 98 percent core recovery for the detailed study of glacier dynamics. With the goal of obtaining complementary information regarding heat flow and permeability, which is vital to understanding the nature of marine hydrogeologic systems, a succession of three temperature logs was recorded over a five-day span to monitor the gradual thermal recovery toward equilibrium conditions. These data were extrapolated to true, undisturbed temperatures, and they define a linear geothermal gradient of 76.7 K/km from the seafloor to 647 mbsf. Bulk thermal conductivities of the sedimentary rocks were derived from empirical mixing models and density measurements performed on core, and an average value of 1.5 W/mK ± 10 percent was determined. The corresponding estimate of heat flow at this site is 115 mW/m2. This value is relatively high but is consistent with other elevated heat-flow data associated with the Erebus Volcanic Province. Information regarding the origin and frequency of pathways for subsurface fluid flow is gleaned from drillers' records, complementary geophysical logs, and core descriptions. Only two prominent permeable zones are identified and these correspond to two markedly different features within the rift basin; one is a distinct lithostratigraphic subunit consisting of a thin lava flow and the other is a heavily fractured interval within a single thick subunit.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geosphere","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/GES00512.1","usgsCitation":"Morin, R.H., Williams, T., Henry, S., Diana Magens and Frank Niessen, and Hansaraj, D., 2010, Heat Flow and Hydrologic Characteristics at the AND-1B borehole, ANDRILL McMurdo Ice Shelf Project, Antarctica: Geosphere, v. 6, no. 4, p. 370-378, https://doi.org/10.1130/GES00512.1.","startPage":"370","endPage":"378","numberOfPages":"9","ipdsId":"IP-005777","costCenters":[{"id":435,"text":"National Research Program - Central Region","active":false,"usgs":true}],"links":[{"id":475609,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1130/ges00512.1","text":"Publisher Index Page"},{"id":270793,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":270792,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/GES00512.1"},{"id":270791,"type":{"id":11,"text":"Document"},"url":"https://digitalcommons.unl.edu/cgi/viewcontent.cgi?article=1023&context=andrillrespub"}],"country":"United States","volume":"6","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-08-11","publicationStatus":"PW","scienceBaseUri":"516689e3e4b0bba30b388bde","contributors":{"authors":[{"text":"Morin, Roger H. rhmorin@usgs.gov","contributorId":2432,"corporation":false,"usgs":true,"family":"Morin","given":"Roger","email":"rhmorin@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":475236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Trevor","contributorId":70662,"corporation":false,"usgs":true,"family":"Williams","given":"Trevor","email":"","affiliations":[],"preferred":false,"id":475239,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henry, Stuart","contributorId":82594,"corporation":false,"usgs":true,"family":"Henry","given":"Stuart","email":"","affiliations":[],"preferred":false,"id":475240,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Diana Magens and Frank Niessen","contributorId":128028,"corporation":true,"usgs":false,"organization":"Diana Magens and Frank Niessen","id":535449,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hansaraj, Dhiresh","contributorId":29713,"corporation":false,"usgs":true,"family":"Hansaraj","given":"Dhiresh","email":"","affiliations":[],"preferred":false,"id":475237,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70156310,"text":"70156310 - 2010 - Mercury-contaminated hydraulic mining debris in San Francisco Bay","interactions":[],"lastModifiedDate":"2018-10-10T14:49:54","indexId":"70156310","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3331,"text":"San Francisco Estuary and Watershed Science","active":true,"publicationSubtype":{"id":10}},"title":"Mercury-contaminated hydraulic mining debris in San Francisco Bay","docAbstract":"The hydraulic gold-mining process used during the California Gold Rush and in many developing countries today contributes enormous amounts of sediment to rivers and streams. Commonly, accompanying this sediment are contaminants such as elemental mercury and cyanide used in the gold extraction process. We show that some of the mercurycontaminated sediment created by hydraulic gold mining in the Sierra Nevada, between 1852 and 1884, ended up over 250 kilometers (km) away in San Francisco Bay; an example of the far-reaching extent of contamination from such activities.
\nA combination of radionuclide dating, bathymetric reconstruction, and geochemical tracers were used to distinguish the hydraulic mining sediment from sediment deposited in the bay before hydraulic mining started (pre-Gold Rush sediment) and sediment deposited after hydraulic mining stopped (modern sediment). Three San Francisco Bay cores were studied as well as source material from the abandoned hydraulic gold mines and river sediment between the mines and bay. Isotopic and geochemical compositions of the core sediments show a geochemical shift in sediment deposited during the time of hydraulic mining. The geochemical shift is characterized by a decrease in εNd, total organic carbon (TOC), Sr and Ca concentrations, Ca/Sr, and Ni/Zr; and, an increase in 87Sr/86Sr, Al/Ca, Hg concentrations, and quartz/plagioclase. This shift is in the direction of the geochemical signature of sediments from rivers and gold mines in hydraulic mining areas. Mixing calculations using Nd isotopes and concentrations estimate that the hydraulic mining debris comprises up to 56% of the sediment in core sediments deposited during the time of hydraulic mining. The surface sediment of cores taken in 1990 were found to contain up to 43% hydraulic mining debris, reflecting a continuing remobilization and redistribution of the debris within the bay and transport from the watershed.
\nMercury concentrations in pre-Gold Rush sediment range between 0.03 and 0.08 μg g-1. In core sediments that have characteristics of the gold deposits and were deposited during the time of hydraulic mining, mercury concentrations can be up to 0.45 μg/g. Modern sediment (post-1952 deposition) contains mercury concentrations up to 0.79 μg/g and is likely a mix of hydraulic mining mercury and mercury introduced from other sources.
","language":"English","publisher":"John Muir Institute of the Environment","usgsCitation":"Bouse, R.M., Fuller, C.C., Luoma, S.N., Hornberger, M.I., Jaffe, B.E., and Smith, R., 2010, Mercury-contaminated hydraulic mining debris in San Francisco Bay: San Francisco Estuary and Watershed Science, v. 8, no. 1, p. 1-28.","productDescription":"ii, 28 p.","startPage":"1","endPage":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":306948,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306947,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://escholarship.org/uc/item/15j0b0z4"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay, San Pablo Bay, Sierra Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {\n \"stroke\": \"#555555\",\n \"stroke-width\": 2,\n \"stroke-opacity\": 1,\n \"fill\": \"#555555\",\n \"fill-opacity\": 0.5\n },\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.200927734375,\n 36.910372213522535\n ],\n [\n -123.804931640625,\n 39.15136267949032\n ],\n [\n -120.58593749999999,\n 39.838068180000015\n ],\n [\n -120.50354003906249,\n 37.00255267215955\n ],\n [\n -122.200927734375,\n 36.910372213522535\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d5a8b2e4b0518e3546a4d2","contributors":{"authors":[{"text":"Bouse, Robin M.","contributorId":27076,"corporation":false,"usgs":true,"family":"Bouse","given":"Robin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":568631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuller, Christopher C.","contributorId":146651,"corporation":false,"usgs":false,"family":"Fuller","given":"Christopher","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":568632,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":568633,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446 mhornber@usgs.gov","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":1037,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"mhornber@usgs.gov","middleInitial":"I.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":568634,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":568635,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, Richard E.","contributorId":146652,"corporation":false,"usgs":false,"family":"Smith","given":"Richard E.","affiliations":[],"preferred":false,"id":568636,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70043448,"text":"70043448 - 2010 - Effectiveness of Wildlife Underpasses and Fencing to Reduce Wildlife–Vehicle Collisions","interactions":[],"lastModifiedDate":"2013-02-15T21:13:28","indexId":"70043448","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Effectiveness of Wildlife Underpasses and Fencing to Reduce Wildlife–Vehicle Collisions","docAbstract":"Transportation planners are increasingly incorporating roadway design features to mitigate impacts of highways on wildlife and to increase driver safety. We used camera and track surveys to evaluate wildlife use before and after construction of 3 wildlife underpasses and associated fencing on a new section of United States Highway 64 in Washington County, North Carolina, USA. We recorded 242 occasions of white-tailed deer (Odocoileus virginianus) use of underpass areas before highway construction began. Following completion of the highway, we collected 2,433 photographs of 9 species with deer representing 93% of all crossings. Adjusting for differences in number of monitoring days, white-tailed deer use of underpass areas averaged 6.7 times greater after the new highway and underpasses were completed. We recorded 3,614 wildlife crossings of ≥20 species based on track counts, representing most medium and large mammals known to occur in the area and several reptiles and birds. After completion of the highway, we documented wildlife mortality due to vehicle collisions during a 13-month period and recorded 128 incidences representing ≥24 species. Within fenced highway segments, mortalities were lowest near underpasses and increased with distance from the underpasses. However, we also documented more mortalities in fenced areas compared with unfenced areas. With greater distance from an underpass, animals with smaller home ranges seemed less likely to reach the underpass and instead attempted to climb over or crawl under fencing. Based on collision reports from adjacent highway sections, the new section of United States Highway 64 experienced approximately 58% fewer wildlife mortalities (primarily white-tailed deer), suggesting underpasses and fencing reduced the number of deer–vehicle collisions. Continuous fencing between underpasses may further reduce the number of vehicle collisions for deer but additional design features (e.g., buried fencing) should be considered for other wildlife species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Wildlife Society","doi":"10.2193/2009-535","usgsCitation":"Frank Van Manen, and McCollister, M.F., 2010, Effectiveness of Wildlife Underpasses and Fencing to Reduce Wildlife–Vehicle Collisions: Journal of Wildlife Management, v. 74, no. 8, p. 1722-1731, https://doi.org/10.2193/2009-535.","startPage":"1722","endPage":"1731","ipdsId":"IP-017625","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":267602,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267601,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/2009-535"}],"country":"United States","volume":"74","issue":"8","noUsgsAuthors":false,"publicationDate":"2010-12-13","publicationStatus":"PW","scienceBaseUri":"511f6714e4b03b29402c5dcf","contributors":{"authors":[{"text":"Frank Van Manen","contributorId":128278,"corporation":true,"usgs":false,"organization":"Frank Van Manen","id":535407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCollister, Matthew F.","contributorId":107161,"corporation":false,"usgs":true,"family":"McCollister","given":"Matthew","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":473607,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70042355,"text":"70042355 - 2010 - Imaging hydraulic fractures in a geothermal reservoir","interactions":[],"lastModifiedDate":"2013-02-17T19:55:01","indexId":"70042355","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Imaging hydraulic fractures in a geothermal reservoir","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1029/2009GL040933","usgsCitation":"Julian, B.R., and Foulger, G.R., 2010, Imaging hydraulic fractures in a geothermal reservoir: Geophysical Research Letters, v. 37, no. 7, https://doi.org/10.1029/2009GL040933.","ipdsId":"IP-011002","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":488140,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://durham-repository.worktribe.com/output/1504263","text":"External Repository"},{"id":267616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267615,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009GL040933"}],"country":"United States","volume":"37","issue":"7","noUsgsAuthors":false,"publicationDate":"2010-04-08","publicationStatus":"PW","scienceBaseUri":"51220a00e4b0b37542fda86e","contributors":{"authors":[{"text":"Julian, Bruce R.","contributorId":50063,"corporation":false,"usgs":true,"family":"Julian","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":471371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foulger, Gillian R.","contributorId":34796,"corporation":false,"usgs":true,"family":"Foulger","given":"Gillian","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":471370,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70160338,"text":"70160338 - 2010 - Alternative aircraft anti-icing formulations with reduced aquatic toxicity and biochemical oxygen demand","interactions":[],"lastModifiedDate":"2015-12-17T15:05:13","indexId":"70160338","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Alternative aircraft anti-icing formulations with reduced aquatic toxicity and biochemical oxygen demand","docAbstract":"The current research was conducted to identify alternative aircraft and pavement deicer and anti-icer formulations with improved environmental characteristics compared to currently used commercial products (2007). The environmental characteristics of primary concern are the biochemical oxygen demand (BOD) and aquatic toxicity of the fully formulated products. Except when the distinction among products is necessary for clarity, “deicer” will refer to aircraft-deicing fluids (ADFs), aircraft anti-icing fluids (AAFs), and pavementdeicing materials (PDMs).
","language":"English","publisher":"Cooperative Research Programs","usgsCitation":"Gold, H., Joback, K., Geis, S., Bowman, G., Mericas, D., Corsi, S., and Ferguson, L., 2010, Alternative aircraft anti-icing formulations with reduced aquatic toxicity and biochemical oxygen demand, 141 p.","productDescription":"141 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-020755","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":312477,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":312462,"type":{"id":15,"text":"Index Page"},"url":"https://www.trb.org/Publications/Blurbs/163310.aspx"}],"publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5673eabbe4b0da412f4f8213","contributors":{"authors":[{"text":"Gold, Harris","contributorId":150659,"corporation":false,"usgs":false,"family":"Gold","given":"Harris","email":"","affiliations":[{"id":18063,"text":"Infoscitex","active":true,"usgs":false}],"preferred":false,"id":582608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Joback, Kevin","contributorId":150660,"corporation":false,"usgs":false,"family":"Joback","given":"Kevin","email":"","affiliations":[{"id":18064,"text":"Molecular Knowledge Systems Inc.","active":true,"usgs":false}],"preferred":false,"id":582609,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geis, Steven","contributorId":150665,"corporation":false,"usgs":false,"family":"Geis","given":"Steven","affiliations":[{"id":17815,"text":"Wisconsin State Laboratory of Hygiene","active":true,"usgs":false}],"preferred":false,"id":582610,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bowman, George","contributorId":150664,"corporation":false,"usgs":false,"family":"Bowman","given":"George","email":"","affiliations":[{"id":17815,"text":"Wisconsin State Laboratory of Hygiene","active":true,"usgs":false}],"preferred":false,"id":582607,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mericas, Dean","contributorId":150658,"corporation":false,"usgs":false,"family":"Mericas","given":"Dean","email":"","affiliations":[{"id":18062,"text":"CH2MHILL, Austin, TX","active":true,"usgs":false}],"preferred":false,"id":582606,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Corsi, Steven R. srcorsi@usgs.gov","contributorId":150657,"corporation":false,"usgs":true,"family":"Corsi","given":"Steven R.","email":"srcorsi@usgs.gov","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":582605,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ferguson, Lee","contributorId":150671,"corporation":false,"usgs":false,"family":"Ferguson","given":"Lee","email":"","affiliations":[],"preferred":false,"id":582632,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70173569,"text":"70173569 - 2010 - Health evaluation of western arctic King Eiders (Somateria spectabilis)","interactions":[],"lastModifiedDate":"2016-06-13T15:04:03","indexId":"70173569","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","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":"Health evaluation of western arctic King Eiders (Somateria spectabilis)","docAbstract":"The western arctic population of King Eiders (Somateria spectabilis) has declined by >50% in recent years. A health assessment was conducted for adult King Eiders breeding on the north slope of Alaska, USA, to evaluate body condition (n=90, 2002–2006) and baseline biochemical and hematologic values (n=20–30, 2005–2006). Body condition for males and females was excellent. Total protein, calcium, alkaline phosphatase, amylase, and globulin were significantly higher in females than in males, likely because of differences in reproductive physiology. These baseline health data can be used to promote conservation of King Eiders and other closely related species of concern.
","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-46.4.1290","usgsCitation":"Scott, C.A., Mazet, J.A., and Powell, A.N., 2010, Health evaluation of western arctic King Eiders (Somateria spectabilis): Journal of Wildlife Diseases, v. 46, no. 4, p. 1290-1294, https://doi.org/10.7589/0090-3558-46.4.1290.","productDescription":"5 p.","startPage":"1290","endPage":"1294","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-012134","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":475614,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-46.4.1290","text":"Publisher Index Page"},{"id":323514,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"575fd92de4b04f417c2baa25","contributors":{"authors":[{"text":"Scott, Cheryl A.","contributorId":171768,"corporation":false,"usgs":false,"family":"Scott","given":"Cheryl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":638585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mazet, Jonna A.K.","contributorId":68444,"corporation":false,"usgs":true,"family":"Mazet","given":"Jonna","email":"","middleInitial":"A.K.","affiliations":[],"preferred":false,"id":638586,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, Abby N. 0000-0002-9783-134X abby_powell@usgs.gov","orcid":"https://orcid.org/0000-0002-9783-134X","contributorId":171426,"corporation":false,"usgs":true,"family":"Powell","given":"Abby","email":"abby_powell@usgs.gov","middleInitial":"N.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":637351,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70173507,"text":"70173507 - 2010 - Implementation of genetic conservation practices in a muskellunge propagation and stocking program","interactions":[],"lastModifiedDate":"2018-02-28T14:37:51","indexId":"70173507","displayToPublicDate":"2011-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"Implementation of genetic conservation practices in a muskellunge propagation and stocking program","docAbstract":"Conservation of genetic resources is a challenging issue for agencies managing popular sport fishes. To address the ongoing potential for genetic risks, we developed a comprehensive set of recommendations to conserve genetic diversity of muskellunge (Esox masquinongy) in Wisconsin, and evaluated the extent to which the recommendations can be implemented. Although some details are specific to Wisconsin's muskellunge propagation program, many of the practical issues affecting implementation are applicable to other species and production systems. We developed guidelines to restrict future broodstock collection operations to lakes with natural reproduction and to develop a set of brood lakes to use on a rotational basis within regional stock boundaries, but implementation will require considering lakes with variable stocking histories. Maintaining an effective population size sufficient to minimize the risk of losing alleles requires limiting broodstock collection to large lakes. Recommendations to better approximate the temporal distribution of spawning in hatchery operations and randomize selection of brood fish are feasible. Guidelines to modify rearing and distribution procedures face some logistic constraints. An evaluation of genetic diversity of hatchery-produced fish during 2008 demonstrated variable success representing genetic variation of the source population. Continued evaluation of hatchery operations will optimize operational efficiency while moving toward genetic conservation goals.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8446-35.8.388","usgsCitation":"Jennings, M.J., Sloss, B.L., Hatzenbeler, G.R., Kampa, J.M., Simonson, T.D., Avelallemant, S.P., Lindenberger, G.A., and Underwood, B.D., 2010, Implementation of genetic conservation practices in a muskellunge propagation and stocking program: Fisheries, v. 35, no. 8, p. 388-395, https://doi.org/10.1577/1548-8446-35.8.388.","productDescription":"8 p.","startPage":"388","endPage":"395","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-020405","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":324214,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"8","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2010-08-01","publicationStatus":"PW","scienceBaseUri":"576bb6b6e4b07657d1a228c3","contributors":{"authors":[{"text":"Jennings, Martin J.","contributorId":6570,"corporation":false,"usgs":true,"family":"Jennings","given":"Martin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":640325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sloss, Brian L. bsloss@usgs.gov","contributorId":702,"corporation":false,"usgs":true,"family":"Sloss","given":"Brian","email":"bsloss@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":637219,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hatzenbeler, Gene R.","contributorId":60505,"corporation":false,"usgs":true,"family":"Hatzenbeler","given":"Gene","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":640326,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kampa, Jeffrey M.","contributorId":40092,"corporation":false,"usgs":true,"family":"Kampa","given":"Jeffrey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":640327,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Simonson, Timothy D.","contributorId":99439,"corporation":false,"usgs":true,"family":"Simonson","given":"Timothy","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":640328,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Avelallemant, Steven P.","contributorId":81764,"corporation":false,"usgs":true,"family":"Avelallemant","given":"Steven","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":640329,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lindenberger, Gary A.","contributorId":42104,"corporation":false,"usgs":true,"family":"Lindenberger","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":640330,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Underwood, Bruce D.","contributorId":105610,"corporation":false,"usgs":true,"family":"Underwood","given":"Bruce","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":640331,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70207942,"text":"70207942 - 2010 - Mapping the onset and progression of marsh dieback","interactions":[],"lastModifiedDate":"2020-01-20T15:08:05","indexId":"70207942","displayToPublicDate":"2010-12-31T15:01:33","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Mapping the onset and progression of marsh dieback","docAbstract":"Along the Gulf of Mexico (GOM) coasts, vast wetlands inject valuable nutrients and suspended and dissolved materials into the coastal ocean. Juncus roemerianus (black needlerush) wetlands, dominating coastlines in the northeastern GOM, transition to the Spartina alternifl ora (smooth cordgrass) coastline of Louisiana. Mixed marsh and mangrove barrier island systems occupy the southeastern and southwestern GOM [1,2].
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Remote sensing of coastal environments","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor & Francis","usgsCitation":"Ramsey III, E., and Rangoonwala, A., 2010, Mapping the onset and progression of marsh dieback, chap. of Remote sensing of coastal environments, p. 123-149.","productDescription":"28 p.","startPage":"123","endPage":"149","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":371396,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":371395,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.taylorfrancis.com/books/9780429143540/chapters/10.1201/9781420094428-11"}],"country":"United States","state":"Louisiana","otherGeospatial":"Coastal Louisiana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.010498046875,\n 28.275358281817105\n ],\n [\n -88.758544921875,\n 28.275358281817105\n ],\n [\n -88.758544921875,\n 30.06909396443887\n ],\n [\n -92.010498046875,\n 30.06909396443887\n ],\n [\n -92.010498046875,\n 28.275358281817105\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ramsey III, Elijah 0000-0002-4518-5796","orcid":"https://orcid.org/0000-0002-4518-5796","contributorId":212009,"corporation":false,"usgs":true,"family":"Ramsey III","given":"Elijah","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":779834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rangoonwala, Amina 0000-0002-0556-0598","orcid":"https://orcid.org/0000-0002-0556-0598","contributorId":204795,"corporation":false,"usgs":true,"family":"Rangoonwala","given":"Amina","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":779835,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70204487,"text":"70204487 - 2010 - The role of soil fertility in restoring Louisiana's coastal prairie","interactions":[],"lastModifiedDate":"2019-07-26T12:24:57","indexId":"70204487","displayToPublicDate":"2010-12-31T12:15:52","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"The role of soil fertility in restoring Louisiana's coastal prairie","docAbstract":"Studies have shown that soil nutrients, especially nitrogen (N), play an important role in the reestablishment of native prairie plant species. Soil N favors early succession species while long-lived native perennials compete favorably in N poor soils and numerous restoration studies have employed carbon additions in the form of sawdust and/or sucrose to immobilize soil nitrogen. However, this technique poses financial and logistical challenges when reconstructing coastal prairie in former agricultural fields. In this study the germination and survival of native prairie species were studied along a nutrient gradient established in an old rice field in Gueydan, Louisiana. Fifty plots, planted with seeds of 22 native prairie species, received one of five treatments: a low or high rate of nitrogen, no addition, and a low or high rate of carbon (sawdust and sucrose). Vegetation coverage by species was sampled every September from 2004 - 2007. Precipitation was well below normal from 2003 to the middle of 2006 except for April - June 2004. Above ground productivity showed a strong response to nitrogen levels as measured by the percentage of available sunlight reaching the ground. Species richness increased with increasing fertility, but despite the increase in biomass as fertility increased there was no statistical difference in species conservatism values with conservative species germinating and surviving in all treatments. These results suggest that factors other than N may influence the outcome of succession in coastal prairie. It is hypothesized that drought adapted prairie perennials are superior competitors in heavy clay prairie soils when receiving low levels of precipitation.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 21st North American Prairie Conference : The prairie meets the river ","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"21st North American Prairie Conference : The prairie meets the river","conferenceDate":"August 4-8, 2008","conferenceLocation":"Winona, Minnesota","language":"English","publisher":"Winona State University","usgsCitation":"Allain, L.K., 2010, The role of soil fertility in restoring Louisiana's coastal prairie, in Proceedings of the 21st North American Prairie Conference : The prairie meets the river , v. 21, Winona, Minnesota, August 4-8, 2008, p. 54-62.","productDescription":"9 p.","startPage":"54","endPage":"62","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":365990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","county":"Vermillion Parish","city":"Gueydan","volume":"21","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Allain, Larry K. 0000-0002-7717-9761 allainl@usgs.gov","orcid":"https://orcid.org/0000-0002-7717-9761","contributorId":2414,"corporation":false,"usgs":true,"family":"Allain","given":"Larry","email":"allainl@usgs.gov","middleInitial":"K.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":767212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70209318,"text":"70209318 - 2010 - Inside the crater, outside the crater: Stratigraphic details of the margin of the Chesapeake Bay impact structure, Virginia, USA","interactions":[],"lastModifiedDate":"2020-03-31T14:02:28","indexId":"70209318","displayToPublicDate":"2010-12-31T11:47:30","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Inside the crater, outside the crater: Stratigraphic details of the margin of the Chesapeake Bay impact structure, Virginia, USA","docAbstract":"Two cores at the outer margin of the Chesapeake Bay impact structure show significant structural and depositional variations that illuminate its history. Detailed stratigraphy of the Watkins School core reveals that this site is outside the disruption boundary of the crater with respect to its lower part (nonmarine Cretaceous Potomac Formation), but just inside the boundary with respect to its upper part (Exmore Formation and a succession of upper Eocene to Pleistocene postimpact deposits). The site of the U.S. Geological Survey-National Aeronautics and Space Administration Langley core, 6.4 km to the east, lies wholly within the annular trough of the crater. The Potomac Formation in the Watkins School core is not noticeably impact disrupted. The lower part of crater unit A in the Langley core represents stratigraphically lower, but similarly undeformed material. The Exmore Formation is only 7.8 m thick in the Watkins School core, but it is over 200 m thick in the Langley core, where it contains blocks up to 24 m in intersected diameter. The upper part of the Exmore Formation in the two cores is a polymict diamicton with a stratified zone at the top. The postimpact sedimentary units in the two cores have similar late Eocene and late Miocene depositional histories and contrasting Oligocene, early Miocene, and middle Miocene histories. A paleochannel of the James River removed Pliocene deposits at the Watkins School site, to be filled later with thick Pleistocene deposits. At the Langley site, a thick Pliocene and thinner Pleistocene record is preserved. © 2010 The Geological Society of America. All rights reserved.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","publisherLocation":"Large Meteorite Impacts and Planetary Evolution IV","doi":"10.1130/2010.2465(19)","usgsCitation":"Edwards, L.E., Powars, D.S., Horton,, J., Gohn, G., Self-Trail, J., and Litwin, R.J., 2010, Inside the crater, outside the crater: Stratigraphic details of the margin of the Chesapeake Bay impact structure, Virginia, USA, v. 465, p. 319-393, https://doi.org/10.1130/2010.2465(19).","productDescription":"74 p.","startPage":"319","endPage":"393","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":373644,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Virginia ","otherGeospatial":"Chesapeake Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.63787841796875,\n 36.9806150652861\n ],\n [\n -76.26708984375,\n 36.9806150652861\n ],\n [\n -76.26708984375,\n 37.293720520228696\n ],\n [\n -76.63787841796875,\n 37.293720520228696\n ],\n [\n -76.63787841796875,\n 36.9806150652861\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"465","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":786032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powars, David S. 0000-0002-6787-8964 dspowars@usgs.gov","orcid":"https://orcid.org/0000-0002-6787-8964","contributorId":1181,"corporation":false,"usgs":true,"family":"Powars","given":"David","email":"dspowars@usgs.gov","middleInitial":"S.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":786033,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton,, J. Wright Jr. 0000-0001-6756-6365","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":219824,"corporation":false,"usgs":true,"family":"Horton,","given":"J. Wright","suffix":"Jr.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":786034,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gohn, Gregory 0000-0003-2000-479X ggohn@usgs.gov","orcid":"https://orcid.org/0000-0003-2000-479X","contributorId":219822,"corporation":false,"usgs":true,"family":"Gohn","given":"Gregory","email":"ggohn@usgs.gov","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":786035,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Self-Trail, Jean 0000-0002-3018-4985 jstrail@usgs.gov","orcid":"https://orcid.org/0000-0002-3018-4985","contributorId":147370,"corporation":false,"usgs":true,"family":"Self-Trail","given":"Jean","email":"jstrail@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":786036,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Litwin, R. J.","contributorId":92284,"corporation":false,"usgs":true,"family":"Litwin","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":786037,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70201981,"text":"70201981 - 2010 - Interpretation and analysis of planetary structures","interactions":[],"lastModifiedDate":"2019-02-04T11:29:24","indexId":"70201981","displayToPublicDate":"2010-12-31T11:28:47","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2468,"text":"Journal of Structural Geology","active":true,"publicationSubtype":{"id":10}},"title":"Interpretation and analysis of planetary structures","docAbstract":"Structural geology is an integral part of planetary science. Planetary structures provide the framework for determining the character and sequence of crustal deformation while simultaneously establishing the observational basis required to test geodynamic hypotheses for the deformation of planetary and satellite lithospheres. The availability of datasets that record spatial and topographic information with a resolution that matches or, in many cases, exceeds, what is available for Earth-based studies permits the deformation of several planets and satellites to be investigated down to the local or outcrop scales. The geometry and kinematics of common planetary structures such as joints, igneous dikes, deformation bands, faults, and folds can be determined with confidence from their distinctive morphologic and topographic signatures, enabling the structural histories and deformation magnitudes to be determined. Segmentation, displacement profiles, relay ramps, footwall anticlines, displacement-controlled depocenters, and other well-known characteristics of terrestrial normal fault and graben systems reveal the sequence and processes of fault growth in numerous planetary examples. Systems of thrust faults having both blind and surface-breaking components are important elements on several bodies including Mercury, the Moon, and Mars. Strike-slip faults have been identified on bodies including Mars and Europa with oblique extension found on Ganymede. Using field-based studies of Earth-based structures as a guide, planetary structures provide a means to explore and evaluate the causative stresses. Despite the wide range in structural styles across the solar system, plate tectonics is recognized only on the Earth, with the other planets and satellites deforming in the absence of large-scale horizontal motions and attendant plate recycling.
","language":"English","publisher":"Elsevier","doi":"10.1016/j.jsg.2009.09.005","usgsCitation":"Schultz, R.A., Hauber, E., Kattenhorn, S.A., Okubo, C.H., and Watters, T.R., 2010, Interpretation and analysis of planetary structures: Journal of Structural Geology, v. 32, no. 6, p. 855-875, https://doi.org/10.1016/j.jsg.2009.09.005.","productDescription":"21 p.","startPage":"855","endPage":"875","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":360970,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars, Mercury, Moon","volume":"32","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schultz, Richard A.","contributorId":49869,"corporation":false,"usgs":true,"family":"Schultz","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":756418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hauber, Ernst","contributorId":212713,"corporation":false,"usgs":false,"family":"Hauber","given":"Ernst","email":"","affiliations":[],"preferred":false,"id":756419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kattenhorn, Simon A.","contributorId":26951,"corporation":false,"usgs":true,"family":"Kattenhorn","given":"Simon","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":756420,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Okubo, Chris H. 0000-0001-9776-8128 cokubo@usgs.gov","orcid":"https://orcid.org/0000-0001-9776-8128","contributorId":140482,"corporation":false,"usgs":true,"family":"Okubo","given":"Chris","email":"cokubo@usgs.gov","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":756421,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Watters, Thomas R.","contributorId":212714,"corporation":false,"usgs":false,"family":"Watters","given":"Thomas","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":756422,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70209743,"text":"70209743 - 2010 - The use of scenario analysis to assess water ecosystem services in response to future land use change in the Willamette River Basin, Oregon","interactions":[],"lastModifiedDate":"2020-05-04T16:04:23.132004","indexId":"70209743","displayToPublicDate":"2010-12-31T11:14:39","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"5","title":"The use of scenario analysis to assess water ecosystem services in response to future land use change in the Willamette River Basin, Oregon","docAbstract":"Human pressures on the natural resources of the United States have resulted in many unintended changes in our ecosystems, e.g., loss of biodiversity, habitat degradation, increases in the number of endangered species, and increases in contamination and water pollution. Environmental managers are concerned about broad-scale changes in land use and landscape pattern and their cumulative impact on hydrologic and ecological processes that affect stream conditions. The type of land use and land cover has direct consequences for most ecosystem services, including water quantity and water quality, erosion control, and biodiversity. As human pressure continues to increase, ecosystem services worldwide are projected to suffer continued loss and degradation, thus reducing the capacity of ecosystems to provide essential goods and services that contribute to human well-being (MEA 2005). The ability to assess, report, and forecast the life support functions of ecosystems is absolutely critical to our capacity to make informed decisions which will maintain the sustainable nature of our environmental services and secure these resources into the future. This study presents an integrated approach to identify areas with potential water quality problems as a result of land cover change projected by stakeholders within a moderately large river basin in the Pacific Northwest (USA). A process-based hydrologic watershed model was used to examine the contribution of land use/land cover to sediment yield, and nitrate and phosphorous loadings, and identify subwatersheds within the Willamette River basin that would be most affected in the year 2050 relative to three possible future scenarios which include inherent differences related to conservation, existing planning trends, and open development. Thus, the objective of this study was to evaluate the effects of alternative future scenarios that describe varying degrees of urban development and human use on hydrological response related to water quality. Results of this study suggest that the amount of forest along streams and agriculture consistently explained a high percentage of variation in nutrients. The AGWA-SWAT model was used to simulate change in sediment yield, nitrate and phosphorus transported with surface runoff for the three future scenarios. With regard to nitrate, the greatest increase was associated with subwatersheds with agricultural land use and urban areas. Although the model predicted some improvement in basin headwaters for all scenarios, nitrate loadings are expected to decrease under the conservation scenario. The largest decrease was observed in the Coast Range. With regard to phosphorous loadings, the lowest reduction was observed in subwatersheds draining predominantly forest areas. The greatest increase was observed under the open development scenario in subwatersheds with agricultural land use. Urbanization and agriculture are presumed to be the major environmental stressors affecting watershed condition of the Willamette River Basin.
","language":"English","publisher":"IOS Press","usgsCitation":"Hernandez, M., Kepner, W., Goodrich, D.G., and Semmens, D.J., 2010, The use of scenario analysis to assess water ecosystem services in response to future land use change in the Willamette River Basin, Oregon, v. , p. -.","productDescription":"15 p.","startPage":"","endPage":"","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374229,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":374228,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://cfpub.epa.gov/si/si_public_record_report.cfm?Lab=NERL&dirEntryId=218684"}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.70629882812499,\n 45.54098421805075\n ],\n [\n -123.1787109375,\n 45.67932023569538\n ],\n [\n -123.25012207031249,\n 45.6178796835697\n ],\n [\n -123.3489990234375,\n 45.158800738352106\n ],\n [\n -123.46984863281249,\n 45.07352060670971\n ],\n [\n -123.3709716796875,\n 44.94536144236941\n ],\n [\n -123.2720947265625,\n 44.67255939212045\n ],\n [\n -123.431396484375,\n 44.42593442145313\n ],\n [\n -123.26660156249999,\n 44.05601169578525\n ],\n [\n -123.02490234375,\n 44.02442151965934\n ],\n [\n -122.79968261718749,\n 44.35920579433503\n ],\n [\n -122.64587402343751,\n 44.953136827528816\n ],\n [\n -122.398681640625,\n 45.18590859850545\n ],\n [\n -122.34374999999999,\n 45.36758436884978\n ],\n [\n -122.3822021484375,\n 45.52944081525666\n ],\n [\n -122.70629882812499,\n 45.54098421805075\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hernandez, M.","contributorId":10234,"corporation":false,"usgs":true,"family":"Hernandez","given":"M.","affiliations":[],"preferred":false,"id":787794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kepner, W. G.","contributorId":101703,"corporation":false,"usgs":true,"family":"Kepner","given":"W. G.","affiliations":[],"preferred":false,"id":787795,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodrich, D. G.","contributorId":224333,"corporation":false,"usgs":false,"family":"Goodrich","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":787796,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Semmens, Darius J. 0000-0001-7924-6529 dsemmens@usgs.gov","orcid":"https://orcid.org/0000-0001-7924-6529","contributorId":1714,"corporation":false,"usgs":true,"family":"Semmens","given":"Darius","email":"dsemmens@usgs.gov","middleInitial":"J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787797,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70041286,"text":"70041286 - 2010 - Hydrothermal alteration of the Late Eocene Caetano ash-flow caldera, north-central Nevada: A field and ASTER remote sensing study","interactions":[],"lastModifiedDate":"2022-09-14T16:25:50.06349","indexId":"70041286","displayToPublicDate":"2010-12-31T11:06:15","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydrothermal alteration of the Late Eocene Caetano ash-flow caldera, north-central Nevada: A field and ASTER remote sensing study","docAbstract":"Geologic mapping and analysis of ASTER remote sensing data were used to define the effects of a large hydrothermal system in the 12–18 by 22 km Caetano caldera. The caldera formed at ~33.8Ma during eruption of >1100km3 of the rhyolitic Caetano Tuff that left a 1 km deep basin which was partly filled by a lake. Magma resurgence resulted in shallow(<1 km) emplacement of the Redrock Canyon granite porphyry intrusion into caldera fill in the southwestern part of the caldera. Field and petrographic studies indicate that heat from the pluton or from deeper residual Caetano magma caused a large hydrothermal system to form that altered both the pluton and intracaldera Caetano Tuff throughout the western half of the caldera. ASTER-based mineral mapping shows that the most intense alteration, including local alunite, developed primarily along the southwestern and western caldera margins. Alteration was most intense in the Redrock Canyon intrusion itself and in the upper unit of the Caetano Tuff, which is a sequence of thin ash flows interlayered with finely bedded sedimentary rocks and mesobreccia. Hydrothermally altered intracaldera tuff was domed and crosscut by the unaltered 33.78 ± 0.05 Ma Carico Lake pluton, indicating that caldera formation, magma resurgence, pluton emplacement, and hydrothermal activity all occurred in less than about 100 ka.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Geological Society of Nevada 2010 symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Geological Society of Nevada 2010 Symposium","conferenceDate":"May 14–22, 2010","conferenceLocation":"Reno, NV","language":"English","publisher":"Geological Society of Nevada","usgsCitation":"John, D.A., Rockwell, B.W., Henry, C., and Colgan, J.P., 2010, Hydrothermal alteration of the Late Eocene Caetano ash-flow caldera, north-central Nevada: A field and ASTER remote sensing study, in Proceedings of the Geological Society of Nevada 2010 symposium, Reno, NV, May 14–22, 2010, p. 1055-1083.","productDescription":"29 p.","startPage":"1055","endPage":"1083","ipdsId":"IP-021425","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":406687,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Caetano caldera","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.29827880859375,\n 39.90025505675715\n ],\n [\n -116.50726318359375,\n 39.90025505675715\n ],\n [\n -116.50726318359375,\n 40.29733393213022\n ],\n [\n -117.29827880859375,\n 40.29733393213022\n ],\n [\n -117.29827880859375,\n 39.90025505675715\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"John, David A. 0000-0001-7977-9106 djohn@usgs.gov","orcid":"https://orcid.org/0000-0001-7977-9106","contributorId":1748,"corporation":false,"usgs":true,"family":"John","given":"David","email":"djohn@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":851766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rockwell, Barnaby W. 0000-0002-9549-0617 barnabyr@usgs.gov","orcid":"https://orcid.org/0000-0002-9549-0617","contributorId":2195,"corporation":false,"usgs":true,"family":"Rockwell","given":"Barnaby","email":"barnabyr@usgs.gov","middleInitial":"W.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":851767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henry, Christopher D.","contributorId":36556,"corporation":false,"usgs":true,"family":"Henry","given":"Christopher D.","affiliations":[],"preferred":false,"id":851768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Colgan, Joseph P. 0000-0001-6671-1436 jcolgan@usgs.gov","orcid":"https://orcid.org/0000-0001-6671-1436","contributorId":1649,"corporation":false,"usgs":true,"family":"Colgan","given":"Joseph","email":"jcolgan@usgs.gov","middleInitial":"P.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":851769,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70207644,"text":"70207644 - 2010 - Microbial community shifts influence patterns in tropical forest nitrogen fixation","interactions":[],"lastModifiedDate":"2020-01-02T10:37:19","indexId":"70207644","displayToPublicDate":"2010-12-31T10:33:05","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2932,"text":"Oecologia","active":true,"publicationSubtype":{"id":10}},"title":"Microbial community shifts influence patterns in tropical forest nitrogen fixation","docAbstract":"The role of biodiversity in ecosystem function receives substantial attention, yet despite the diversity and functional relevance of microorganisms, relationships between microbial community structure and ecosystem processes remain largely unknown. We used tropical rain forest fertilization plots to directly compare the relative abundance, composition and diversity of free-living nitrogen (N)-fixer communities to in situ leaf litter N fixation rates. N fixation rates varied greatly within the landscape, and 'hotspots' of high N fixation activity were observed in both control and phosphorus (P)-fertilized plots. Compared with zones of average activity, the N fixation 'hotspots' in unfertilized plots were characterized by marked differences in N-fixer community composition and had substantially higher overall diversity. P additions increased the efficiency of N-fixer communities, resulting in elevated rates of fixation per nifH gene. Furthermore, P fertilization increased N fixation rates and N-fixer abundance, eliminated a highly novel group of N-fixers, and increased N-fixer diversity. Yet the relationships between diversity and function were not simple, and coupling rate measurements to indicators of community structure revealed a biological dynamism not apparent from process measurements alone. Taken together, these data suggest that the rain forest litter layer maintains high N fixation rates and unique N-fixing organisms and that, as observed in plant community ecology, structural shifts in N-fixing communities may partially explain significant differences in system-scale N fixation rates.
","language":"English","publisher":"U.S. Geological Survey ","doi":"10.1007/s00442-010-1649-6","issn":"00298549","usgsCitation":"Reed, S., Townsend, A., Cleveland, C., and Nemergut, D., 2010, Microbial community shifts influence patterns in tropical forest nitrogen fixation: Oecologia, v. 164, no. 2, p. 521-531, https://doi.org/10.1007/s00442-010-1649-6.","productDescription":"11 p. ","startPage":"521","endPage":"531","costCenters":[],"links":[{"id":370928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"164","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-05-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Reed, Sasha C. 0000-0002-8597-8619","orcid":"https://orcid.org/0000-0002-8597-8619","contributorId":207498,"corporation":false,"usgs":true,"family":"Reed","given":"Sasha C.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":778726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Townsend, A.R.","contributorId":16631,"corporation":false,"usgs":true,"family":"Townsend","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":778727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cleveland, C.C.","contributorId":62387,"corporation":false,"usgs":true,"family":"Cleveland","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":778728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nemergut, D.R.","contributorId":68998,"corporation":false,"usgs":true,"family":"Nemergut","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":778729,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":98785,"text":"ofr20101194 - 2010 - USGS-NPS Servicewide Benthic Mapping Program (SBMP) workshop report","interactions":[],"lastModifiedDate":"2023-12-07T15:21:27.24094","indexId":"ofr20101194","displayToPublicDate":"2010-12-31T10:15:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2010-1194","displayTitle":"USGS-NPS Servicewide Benthic Mapping Program (SBMP) Workshop Report","title":"USGS-NPS Servicewide Benthic Mapping Program (SBMP) workshop report","docAbstract":"The National Park Service (NPS) Inventory and Monitoring (I&M) Program recently allocated funds to initiate a benthic mapping program in ocean and Great Lakes parks in alignment with the NPS Ocean Park Stewardship 2007-2008 Action Plan. Seventy-four (ocean and Great Lakes) parks, spanning more than 5,000 miles of coastline, many affected by increasing coastal storms and other natural and anthropogenic processes, make the development of a Servicewide Benthic Mapping Program (SBMP) timely. The resulting maps and associated reports will be provided to NPS managers in a consistent servicewide format to help park managers protect and manage the 3 million acres of submerged National Park System natural and cultural resources. Of the 74 ocean and Great Lakes park units, the 40 parks with submerged acreage will be the focus in the early years of the SBMP.
The NPS and U.S. Geological Survey (USGS) convened a workshop (June 3-5, 2008) in Lakewood, CO. The assembly of experts from the NPS and other Federal and non-Federal agencies clarified the needs and goals of the NPS SBMP and was one of the key first steps in designing the benthic mapping program. The central needs for individual parks, park networks, and regions identified by workshop participants were maps including bathymetry, bottom type, geology, and biology. This workshop, although not an exhaustive survey of data-acquisition technologies, highlighted the more promising technologies being used, existing sources of data, and the need for partnerships to leverage resources. Workshop products include recommended classification schemes and management approaches for consistent application and products similar to other long-term NPS benthic mapping efforts. As part of the SBMP, recommendations from this workshop, including application of an improved version of the Coastal and Marine Ecological Classification Standard (CMECS), will be tested in several pilot parks. In 2008, in conjunction with the findings of this workshop, the NPS funded benthic mapping projects in Glacier Bay National Park and Preserve, Golden Gate National Recreational Area, Sleeping Bear Dunes National Lakeshore, Gulf Islands National Seashore, Virgin Islands National Park, and Virgin Islands Coral Reef National Monument. Full design and protocols of the SBMP based on the findings of this workshop are detailed in a second document dedicated to the subject.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101194","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Moses, C.S., Nayagandhi, A., Brock, J., and Beavers, R., 2010, USGS-NPS Servicewide Benthic Mapping Program (SBMP) workshop report: U.S. Geological Survey Open-File Report 2010-1194, vi, 32 p., https://doi.org/10.3133/ofr20101194.","productDescription":"vi, 32 p.","numberOfPages":"32","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":384764,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1194/ofr20101194.pdf","text":"Report","size":"1.27 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2010-1194"},{"id":126100,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2010/1194/coverthb.jpg"},{"id":14195,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1194/","linkFileType":{"id":5,"text":"html"}}],"contact":"Director, Woods Hole Coastal and Marine Science Center
U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
The following reply to the comments by Nolan and Cook makes the following points. The Palmer Drought Severity Index (PDSI) is not a measure of summer rainfall. Cahokia's \"Big Bang\" dates to the end of the Edelhardt phase and continued through the Lohmann phase. The \"American Bottom\" refers only to the Mississippi River floodplain in the vicinity of East St. Louis, and the exact nature of human response to climate change cannot be predicted from PDSI data alone.
","language":"English","publisher":"Cambridge University Press","doi":"10.7183/0002-7316.75.4.984","usgsCitation":"Benson, L.V., Pauketat, T.R., and Cook, E.R., 2010, Reply to comments of Nolan and Cook: American Antiquity, v. 75, no. 4, p. 984-985, https://doi.org/10.7183/0002-7316.75.4.984.","productDescription":"2 p.","startPage":"984","endPage":"985","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":394108,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"4","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Benson, Larry V. lbenson@usgs.gov","contributorId":1655,"corporation":false,"usgs":true,"family":"Benson","given":"Larry","email":"lbenson@usgs.gov","middleInitial":"V.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":830510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pauketat, T. R.","contributorId":40830,"corporation":false,"usgs":true,"family":"Pauketat","given":"T.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":830511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cook, Edward R","contributorId":218752,"corporation":false,"usgs":false,"family":"Cook","given":"Edward","email":"","middleInitial":"R","affiliations":[{"id":17701,"text":"Lamont-Doherty Earth Observatory","active":true,"usgs":false}],"preferred":false,"id":830512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70231171,"text":"70231171 - 2010 - Delaware Water Gap; a geology classroom","interactions":[],"lastModifiedDate":"2022-05-02T15:12:29.603406","indexId":"70231171","displayToPublicDate":"2010-12-31T10:04:22","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Delaware Water Gap; a geology classroom","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"New York State Geological Association 82nd annual meeting; field trip guidebook","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"New York State Geological Association","usgsCitation":"Epstein, J.B., 2010, Delaware Water Gap; a geology classroom, in New York State Geological Association 82nd annual meeting; field trip guidebook, v. 82, p. 1-46.","productDescription":"46 p.","startPage":"1","endPage":"46","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":399966,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":399965,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.nysga-online.org/guidebooks/by-year/"}],"country":"United States","state":"New Jersey, Pennsylvania","otherGeospatial":"Delaware Water Gap National Recreation Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.11489868164062,\n 40.9353026724978\n ],\n [\n -74.79766845703125,\n 41.156944322795525\n ],\n [\n -74.8443603515625,\n 41.19105625669688\n ],\n [\n -74.78118896484375,\n 41.31082388091818\n ],\n [\n -74.81964111328125,\n 41.304634388885916\n ],\n [\n -74.88143920898438,\n 41.22411753058293\n ],\n [\n -74.98306274414062,\n 41.11660732012896\n ],\n [\n -75.04898071289062,\n 41.04207384890103\n ],\n [\n -75.13687133789061,\n 40.994410999439516\n ],\n [\n -75.11489868164062,\n 40.9353026724978\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"82","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Epstein, Jack B. jepstein@usgs.gov","contributorId":1412,"corporation":false,"usgs":true,"family":"Epstein","given":"Jack","email":"jepstein@usgs.gov","middleInitial":"B.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":841851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70230545,"text":"70230545 - 2010 - Population demographics and breeding ecology of the Long-tailed Duck (Clangula hyemalis) in the Churchill, Manitoba area","interactions":[],"lastModifiedDate":"2022-04-15T15:05:36.935938","indexId":"70230545","displayToPublicDate":"2010-12-31T10:00:15","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Population demographics and breeding ecology of the Long-tailed Duck (Clangula hyemalis) in the Churchill, Manitoba area","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hudson Bay region research","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Aboriginal Issues Press","usgsCitation":"Perry, M., and Alison, R.M., 2010, Population demographics and breeding ecology of the Long-tailed Duck (Clangula hyemalis) in the Churchill, Manitoba area, chap. of Hudson Bay region research, p. 88-91.","productDescription":"4 p.","startPage":"88","endPage":"91","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":398824,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"Manitoba","city":"Churchill","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.30615234375,\n 57.27310364731209\n ],\n [\n -92.274169921875,\n 57.27310364731209\n ],\n [\n -92.274169921875,\n 59.689926220143356\n ],\n [\n -96.30615234375,\n 59.689926220143356\n ],\n [\n -96.30615234375,\n 57.27310364731209\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Perry, Matthew C. 0000-0001-6452-9534","orcid":"https://orcid.org/0000-0001-6452-9534","contributorId":91601,"corporation":false,"usgs":true,"family":"Perry","given":"Matthew C.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":840705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alison, Robert M.","contributorId":290288,"corporation":false,"usgs":false,"family":"Alison","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":840706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}