{"pageNumber":"2580","pageRowStart":"64475","pageSize":"25","recordCount":184617,"records":[{"id":70028197,"text":"70028197 - 2005 - Modern pollen data from North America and Greenland for multi-scale paleoenvironmental applications","interactions":[],"lastModifiedDate":"2012-03-12T17:20:42","indexId":"70028197","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Modern pollen data from North America and Greenland for multi-scale paleoenvironmental applications","docAbstract":"The modern pollen network in North America and Greenland is presented as a database for use in quantitative calibration studies and paleoenvironmental reconstructions. The georeferenced database includes 4634 samples from all regions of the continent and 134 pollen taxa that range from ubiquitous to regionally diagnostic taxa. Climate data and vegetation characteristics were assigned to every site. Automated and manual procedures were used to verify the accuracy of geographic coordinates and identify duplicate records among datasets, incomplete pollen sums, and other potential errors. Data are currently available for almost all of North America, with variable density. Pollen taxonomic diversity, as measured by the Shannon-Weiner coefficient, varies as a function of location, as some vegetation regions are dominated by one or two major pollen producers, while other regions have a more even composition of pollen taxa. Squared-chord distances computed between samples show that most modern pollen samples find analogues within their own vegetation zone. Both temperature and precipitation inferred from best analogues are highly correlated with observed values but temperature exhibits the strongest relation. Maps of the contemporary distribution of several pollen types in relation to the range of the plant taxon illustrate the correspondence between plant and pollen ranges. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Science Reviews","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.quascirev.2005.03.005","issn":"02773791","usgsCitation":"Whitmore, J., Gajewski, K., Sawada, M., Williams, J., Shuman, B., Bartlein, P., Minckley, T., Viau, A., Webb, T., Shafer, S., Anderson, P., and Brubaker, L., 2005, Modern pollen data from North America and Greenland for multi-scale paleoenvironmental applications: Quaternary Science Reviews, v. 24, no. 16-17, p. 1828-1848, https://doi.org/10.1016/j.quascirev.2005.03.005.","startPage":"1828","endPage":"1848","numberOfPages":"21","costCenters":[],"links":[{"id":210286,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.quascirev.2005.03.005"},{"id":237162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"16-17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5c9de4b0c8380cd6fe0d","contributors":{"authors":[{"text":"Whitmore, J.","contributorId":53587,"corporation":false,"usgs":true,"family":"Whitmore","given":"J.","email":"","affiliations":[],"preferred":false,"id":417007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gajewski, K.","contributorId":73389,"corporation":false,"usgs":true,"family":"Gajewski","given":"K.","email":"","affiliations":[],"preferred":false,"id":417009,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sawada, M.","contributorId":21342,"corporation":false,"usgs":true,"family":"Sawada","given":"M.","email":"","affiliations":[],"preferred":false,"id":417002,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, J.W.","contributorId":53553,"corporation":false,"usgs":true,"family":"Williams","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":417006,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shuman, B.","contributorId":85386,"corporation":false,"usgs":true,"family":"Shuman","given":"B.","affiliations":[],"preferred":false,"id":417010,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bartlein, P. J.","contributorId":54566,"corporation":false,"usgs":false,"family":"Bartlein","given":"P. J.","affiliations":[],"preferred":false,"id":417008,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Minckley, T.","contributorId":94845,"corporation":false,"usgs":true,"family":"Minckley","given":"T.","email":"","affiliations":[],"preferred":false,"id":417011,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Viau, A.E.","contributorId":20138,"corporation":false,"usgs":true,"family":"Viau","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":417001,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Webb, T. III","contributorId":38297,"corporation":false,"usgs":true,"family":"Webb","given":"T.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":417004,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Shafer, S.","contributorId":47963,"corporation":false,"usgs":true,"family":"Shafer","given":"S.","email":"","affiliations":[],"preferred":false,"id":417005,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Anderson, P.","contributorId":102682,"corporation":false,"usgs":true,"family":"Anderson","given":"P.","affiliations":[],"preferred":false,"id":417012,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Brubaker, L.","contributorId":22564,"corporation":false,"usgs":true,"family":"Brubaker","given":"L.","affiliations":[],"preferred":false,"id":417003,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}} ,{"id":70027561,"text":"70027561 - 2005 - Large-volume, low-δ18O rhyolites of the central Snake River Plain, Idaho, USA","interactions":[],"lastModifiedDate":"2015-05-04T11:48:29","indexId":"70027561","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Large-volume, low-δ18O rhyolites of the central Snake River Plain, Idaho, USA","docAbstract":"

The Miocene Bruneau-Jarbidge and adjacent volcanic fields of the central Snake River Plain, southwest Idaho, are dominated by high-temperature rhyolitic tuffs and lavas having an aggregate volume estimated as 7000 km3. Samples from units representing at least 50% of this volume are strongly depleted in 18O, with magmatic feldspar δ18OVSMOW (Vienna standard mean ocean water) values between −1.4‰ and 3.8‰. The magnitude of the 18O depletion and the complete lack of any rhyolites with normal values (7‰–10‰) combine to suggest that assimilation or melting of a caldera block altered by near- contemporaneous hydrothermal activity is unlikely. Instead, we envisage generation of the high-temperature rhyolites by shallow melting of Idaho Batholith rocks, under the influence of the Yellowstone hotspot, affected by Eocene meteoric-hydrothermal events. The seeming worldwide scarcity of strongly 18O-depleted rhyolites may simply reflect a similar scarcity of suitable crustal protoliths.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/G21723.1","issn":"00917613","usgsCitation":"Boroughs, S., Wolff, J., Bonnichsen, B., Godchaux, M., and Larson, P., 2005, Large-volume, low-δ18O rhyolites of the central Snake River Plain, Idaho, USA: Geology, v. 33, no. 10, p. 821-824, https://doi.org/10.1130/G21723.1.","productDescription":"4 p.","startPage":"821","endPage":"824","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":238418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211192,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/G21723.1"}],"volume":"33","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a44a2e4b0c8380cd66c83","contributors":{"authors":[{"text":"Boroughs, Scott","contributorId":88946,"corporation":false,"usgs":true,"family":"Boroughs","given":"Scott","email":"","affiliations":[],"preferred":false,"id":414156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolff, John","contributorId":33117,"corporation":false,"usgs":true,"family":"Wolff","given":"John","affiliations":[],"preferred":false,"id":414154,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonnichsen, Bill","contributorId":94358,"corporation":false,"usgs":true,"family":"Bonnichsen","given":"Bill","email":"","affiliations":[],"preferred":false,"id":414153,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Godchaux, Martha","contributorId":18936,"corporation":false,"usgs":true,"family":"Godchaux","given":"Martha","email":"","affiliations":[],"preferred":false,"id":414152,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Larson, Peter","contributorId":57265,"corporation":false,"usgs":true,"family":"Larson","given":"Peter","affiliations":[],"preferred":false,"id":414155,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":1008464,"text":"1008464 - 2005 - Southern marl prairies conceptual ecological model","interactions":[],"lastModifiedDate":"2019-06-03T10:18:05","indexId":"1008464","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Southern marl prairies conceptual ecological model","docAbstract":"

About 190,000 ha of higher-elevation marl prairies flank either side of Shark River Slough in the southern Everglades. Water levels typically drop below the ground surface each year in this landscape. Consequently, peat soil accretion is inhibited, and substrates consist either of calcitic marl produced by algal periphyton mats or exposed limestone bedrock. The southern marl prairies support complex mosaics of wet prairie, sawgrass sawgrass (Cladium jamaicense), tree islands, and tropical hammock communities and a high diversity of plant species. However, relatively short hydroperiods and annual dry downs provide stressful conditions for aquatic fauna, affecting survival in the dry season when surface water is absent. Here, we present a conceptual ecological model developed for this landscape through scientific consensus, use of empirical data, and modeling. The two major societal drivers affecting the southern marl prairies are water management practices and agricultural and urban development. These drivers lead to five groups of ecosystem stressors: loss of spatial extent and connectivity, shortened hydroperiod and increased drought severity, extended hydroperiod and drying pattern reversals, introduction and spread of non-native trees, and introduction and spread of non-native fishes. Major ecological attributes include periphyton mats, plant species diversity and community mosaic, Cape Sable seaside sparrow (Ammodramus maritimus mirabilis), marsh fishes and associated aquatic fauna prey base, American alligator (Alligator mississippiensis), and wading bird early dry season foraging. Water management and development are hypothesized to have a negative effect on the ecological attributes of the southern marl prairies in the following ways. Periphyton mats have decreased in cover in areas where hydroperiod has been significantly reduced and changed in community composition due to inverse responses to increased nutrient availability. Plant species diversity and community mosaics have changed due to shifting gradients to more terrestrial or more aquatic communities, displacement of native communities by non-natives, expansion of woody plants, high-intensity dry season fires, tree-island burnout, and reduced microtopography resulting from alligator population decline. Cape Sable seaside sparrow populations are threatened by nest destruction resulting from extended hydroperiods, drying pattern reversals, and high intensity dry season fires, as well as by the expansion of woody plants into graminoid wetland habitats. Populations of marsh fishes and associated aquatic fauna that constitute the aquatic prey base for higher vertebrates have decreased in density and changed in species composition and size structure due to loss of wetland spatial extent, shortened hydroperiod, increased drought severity, loss of aquatic drought refugia in solution holes and alligator holes, and spread of exotic fishes. American alligator populations have declined in the Rocky Glades, and alligator holes have filled with sediment, as a result of shortened hydroperiod and increased drought severity. Habitat options for wading birds to forage during the early dry season and during unusually wet years have been reduced due to loss of spatial extent and shortened hydroperiod.

","language":"English","publisher":"Springer","doi":"10.1672/0277-5212(2005)025[0821:SMPCEM]2.0.CO;2","usgsCitation":"Davis, S., Loftus, W., Gaiser, E., and Huffman, A., 2005, Southern marl prairies conceptual ecological model: Wetlands, v. 25, p. 821-831, https://doi.org/10.1672/0277-5212(2005)025[0821:SMPCEM]2.0.CO;2.","productDescription":"11 p.","startPage":"821","endPage":"831","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":131020,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e71c2","contributors":{"authors":[{"text":"Davis, S.M.","contributorId":91057,"corporation":false,"usgs":true,"family":"Davis","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":317869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loftus, W.F.","contributorId":29363,"corporation":false,"usgs":true,"family":"Loftus","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":317867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaiser, E.E.","contributorId":67461,"corporation":false,"usgs":true,"family":"Gaiser","given":"E.E.","affiliations":[],"preferred":false,"id":317868,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Huffman, A.E.","contributorId":103223,"corporation":false,"usgs":true,"family":"Huffman","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":317870,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70029073,"text":"70029073 - 2005 - Short human occupations in the Middle Palaeolithic level i of the Abric Romani rock-shelter (Capellades, Barcelona, Spain)","interactions":[],"lastModifiedDate":"2015-05-04T13:22:47","indexId":"70029073","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2337,"text":"Journal of Human Evolution","active":true,"publicationSubtype":{"id":10}},"title":"Short human occupations in the Middle Palaeolithic level i of the Abric Romani rock-shelter (Capellades, Barcelona, Spain)","docAbstract":"

This paper presents a multidisciplinary study on the size of the occupied surfaces, provisioning strategies and behaviour planning at the Romani rock-shelter, using the Middle Palaeolithic record of the level i. This level is dated around 46.000 BP through U/Th ages. A behavioural interpretation is proposed, which emphasises the activities and the systemic value of the archaeological artefacts and structures.

\n

Occupation patterns are identified on the basis of the accumulations formed by human activities. These archaeological accumulations, consisting of artefacts and hearths, are easily defined visually as spatial units. The relationships between these accumulations, established by means of refitted remains, indicate that differences can be established between: 1) small and medium-sized occupation surfaces; 2) restricted and diversified provisioning strategies. This variability suggests that different modes of occupation are represented in the same archaeological level.

\n

The human activities reveal the generalization of fire technology. In almost all sizes of the occupation surfaces, the exploitation of vegetal resources near the Abric Romani marks the threshold of the restricted provisioning strategy. Limited use and fragmented knapping activities are recorded in the lithic assemblage. Faunal remains show differential transport. The exploitation of lithic, faunal and vegetal resources characterizes the diversified provisioning strategy.

\n

The small occupation surfaces and restricted provisioning strategies suggest short settlements in the Abric Romani. This shorter occupation model complements the longer diversified provisioning strategy recorded in both small and medium-sized occupied surfaces. The selection of precise elements for transport and the possible deferred consumption in the diversified provision strategy suggest an individual supply. In this respect, Neanderthal occupations in the Romani rock-shelter show a direct relation to: 1) hunting strategic resources; 2) high, linear mobility.

","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhevol.2004.10.004","issn":"00472484","usgsCitation":"Vallerdu, J., Allue, E., Bischoff, J.L., Caceres, I., Carbonell, E., Cebria, A., Garcia-Anton, D., Huguet, R., Ibanez, N., Martinez, K., Pasto, I., Rosell, J., Saladie, P., and Vaquero, M., 2005, Short human occupations in the Middle Palaeolithic level i of the Abric Romani rock-shelter (Capellades, Barcelona, Spain): Journal of Human Evolution, v. 48, no. 2, p. 157-174, https://doi.org/10.1016/j.jhevol.2004.10.004.","productDescription":"18 p.","startPage":"157","endPage":"174","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":237899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210853,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhevol.2004.10.004"}],"volume":"48","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8e9ae4b08c986b318a32","contributors":{"authors":[{"text":"Vallerdu, J.","contributorId":56847,"corporation":false,"usgs":true,"family":"Vallerdu","given":"J.","email":"","affiliations":[],"preferred":false,"id":421228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allue, E.","contributorId":20116,"corporation":false,"usgs":true,"family":"Allue","given":"E.","affiliations":[],"preferred":false,"id":421225,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, J. L.","contributorId":28969,"corporation":false,"usgs":true,"family":"Bischoff","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":421226,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Caceres, I.","contributorId":58082,"corporation":false,"usgs":true,"family":"Caceres","given":"I.","email":"","affiliations":[],"preferred":false,"id":421229,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carbonell, E.","contributorId":88107,"corporation":false,"usgs":true,"family":"Carbonell","given":"E.","affiliations":[],"preferred":false,"id":421232,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cebria, A.","contributorId":52392,"corporation":false,"usgs":true,"family":"Cebria","given":"A.","email":"","affiliations":[],"preferred":false,"id":421227,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Garcia-Anton, D.","contributorId":94088,"corporation":false,"usgs":true,"family":"Garcia-Anton","given":"D.","email":"","affiliations":[],"preferred":false,"id":421234,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Huguet, R.","contributorId":102686,"corporation":false,"usgs":true,"family":"Huguet","given":"R.","email":"","affiliations":[],"preferred":false,"id":421236,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ibanez, N.","contributorId":92041,"corporation":false,"usgs":true,"family":"Ibanez","given":"N.","email":"","affiliations":[],"preferred":false,"id":421233,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Martinez, K.","contributorId":18568,"corporation":false,"usgs":true,"family":"Martinez","given":"K.","email":"","affiliations":[],"preferred":false,"id":421224,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Pasto, I.","contributorId":101443,"corporation":false,"usgs":true,"family":"Pasto","given":"I.","email":"","affiliations":[],"preferred":false,"id":421235,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Rosell, J.","contributorId":86163,"corporation":false,"usgs":true,"family":"Rosell","given":"J.","email":"","affiliations":[],"preferred":false,"id":421231,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Saladie, P.","contributorId":104696,"corporation":false,"usgs":true,"family":"Saladie","given":"P.","affiliations":[],"preferred":false,"id":421237,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Vaquero, Manola","contributorId":86131,"corporation":false,"usgs":true,"family":"Vaquero","given":"Manola","email":"","affiliations":[],"preferred":false,"id":421230,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}} ,{"id":70029068,"text":"70029068 - 2005 - Long-term effects of precommercial thinning on small mammals in northern Maine","interactions":[],"lastModifiedDate":"2012-03-12T17:20:47","indexId":"70029068","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1687,"text":"Forest Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Long-term effects of precommercial thinning on small mammals in northern Maine","docAbstract":"Precommercial thinning (PCT) is being practiced increasingly throughout the Acadian forest of eastern North America to meet silvicultural objectives; however, effects of this practice on wildlife, both immediately and several years post-treatment are not well understood. Forest dependent small mammals have ecological roles as prey for numerous avian and mammalian predators, dispersers of seeds, fruit, and spores, and contribute to nutrient cycling. Researchers in the northwestern USA have suggested that thinning of young, regenerating clearcuts may increase the abundance and diversity of some forest-dependent small mammals by increasing rates of forest development and enhancing the ecological representation of mid-successional stands across managed landscapes. We examined the effects of PCT within conifer-dominated forest stands 1-, 6-, 11-, and 16-years post-treatment, on abundances of mice, voles, and shrews, and on within-stand structure in the commercially managed, Acadian forests of northern Maine. We live-trapped small mammals on 24 herbicide-treated clearcuts treated with PCT and on 13 similar, unthinned stands during summers of 2000 and 2001. Thinning of mid-successional conifer stands resulted in increased abundances, (red-backed voles, Clethrionomys gapperi, P = 0.008; masked shrews, Sorex cinereus, P < 0.001) or had no detectable effect on (deer mice, Peromyscus maniculatus, P = 0.544; short-tailed shrews, Blarina brevicauda, P = 0.517) the 4 most common species of Muridae and Soricidae in northern Maine. In general, abundance of deer mice responded more positively to increasing development class and to the number of years since thinning than other species of small mammals. Several within-stand habitat characteristics associated with stand maturity, such as larger stem diameters and a partially open canopy, occurred in thinned stands. Thus, PCT may accelerate the development of habitat attributes typical of mid-successional conifer stands in intensively managed stands within the Acadian Forest. PCT may increase abundances of small mammal species associated with mid-seral forest conditions at the scale of the forest stand. ?? 2004 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Forest Ecology and Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.foreco.2004.10.005","issn":"03781127","usgsCitation":"Homyack, J., Harrison, D., and Krohn, W., 2005, Long-term effects of precommercial thinning on small mammals in northern Maine: Forest Ecology and Management, v. 205, no. 1-3, p. 43-57, https://doi.org/10.1016/j.foreco.2004.10.005.","startPage":"43","endPage":"57","numberOfPages":"15","costCenters":[],"links":[{"id":210801,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.foreco.2004.10.005"},{"id":237827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"205","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a498be4b0c8380cd686d8","contributors":{"authors":[{"text":"Homyack, J.A.","contributorId":51530,"corporation":false,"usgs":true,"family":"Homyack","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":421206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, D.J.","contributorId":82022,"corporation":false,"usgs":true,"family":"Harrison","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":421208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krohn, W.B.","contributorId":64355,"corporation":false,"usgs":true,"family":"Krohn","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":421207,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1008125,"text":"1008125 - 2005 - Change in area of winter-flooded and dry rice in the northern Central Valley of California determined by satellite imagery","interactions":[],"lastModifiedDate":"2012-02-02T00:04:37","indexId":"1008125","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1153,"text":"California Fish and Game","active":true,"publicationSubtype":{"id":10}},"title":"Change in area of winter-flooded and dry rice in the northern Central Valley of California determined by satellite imagery","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"California Fish and Game","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Fleskes, J., Perry, W., Petrik, K., Spell, R., and Reid, F., 2005, Change in area of winter-flooded and dry rice in the northern Central Valley of California determined by satellite imagery: California Fish and Game, v. 91, no. 3, p. 207-215.","productDescription":"p. 207-215","startPage":"207","endPage":"215","numberOfPages":"9","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":132382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6db5","contributors":{"authors":[{"text":"Fleskes, J. P.","contributorId":98661,"corporation":false,"usgs":true,"family":"Fleskes","given":"J. P.","affiliations":[],"preferred":false,"id":316824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perry, W.M.","contributorId":15949,"corporation":false,"usgs":true,"family":"Perry","given":"W.M.","affiliations":[],"preferred":false,"id":316820,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petrik, K.L.","contributorId":21916,"corporation":false,"usgs":true,"family":"Petrik","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":316821,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Spell, R.","contributorId":90259,"corporation":false,"usgs":true,"family":"Spell","given":"R.","email":"","affiliations":[],"preferred":false,"id":316823,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reid, F.","contributorId":47740,"corporation":false,"usgs":true,"family":"Reid","given":"F.","affiliations":[],"preferred":false,"id":316822,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70029120,"text":"70029120 - 2005 - Disturbance of eelgrass Zostera marina by commercial mussel Mytilus edulis harvesting in Maine: Dragging impacts and habitat recovery","interactions":[],"lastModifiedDate":"2022-05-26T16:49:06.736759","indexId":"70029120","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Disturbance of eelgrass Zostera marina by commercial mussel Mytilus edulis harvesting in Maine: Dragging impacts and habitat recovery","title":"Disturbance of eelgrass Zostera marina by commercial mussel Mytilus edulis harvesting in Maine: Dragging impacts and habitat recovery","docAbstract":"

We studied the effects of commercial harvest of blue mussels Mytilus edulis on eelgrass Zostera marina L. in Maquoit Bay, Maine, USA, at a hierarchy of scales. We used aerial photography, underwater video, and eelgrass population- and shoot-based measurements to quantify dragging impacts within 4 sites that had been disturbed at different times over an approximate 7 yr interval, and to project eelgrass meadow recovery rates. Dragging had disturbed 10% of the eelgrass cover in Maquoit Bay, with dragged sites ranging from 3.4 to 31.8 ha in size. Dragging removed above- and belowground plant material from the majority of the bottom in the disturbed sites. One year following dragging, eelgrass shoot density, shoot height and total biomass of disturbed sites averaged respectively 2 to 3%, 46 to 61% and <1% that of the reference sites. Substantial differences in eelgrass biomass persisted between disturbed and reference sites up to 7 yr after dragging. Dragging did not affect physical characteristics of the sediment. The pattern and rate of eelgrass bed recovery depended strongly on initial dragging intensity; areas of relatively light dragging with many remnant eelgrass patches (i.e. patches that were missed by the mussel dredge) showed considerable revegetation in 1 yr. However, by developing recovery trajectories from measurements at sites disturbed in different years, we projected that it would require a mean of 10.6 yr for recovery of eelgrass shoot density within the areas of intense dragging characterizing most of the disturbed sites. A spatial simulation model based on measured rates of lateral patch-expansion (mean 12.5 cm yr-1) and new-patch recruitment (mean 0.19 patches m-2 yr-1) yielded a mean bed recovery time of 9 to 11 yr following dragging, depending on initial degree of plant removal. Model simulations suggested that with favorable environmental conditions, eelgrass beds might recover from dragging disturbance in 6 yr; conversely, recovery under conditions less conducive to eelgrass growth could require 20 yr or longer. This study shows that mussel dragging poses a severe threat to eelgrass in this region and that regulations to protect eelgrass from dragging impacts would maintain the integrity of a substantial amount of habitat.

","language":"English","publisher":"Inter-Research Science Publisher","doi":"10.3354/meps285057","usgsCitation":"Neckles, H.A., Short, F.T., Barker, S., and Kopp, B.S., 2005, Disturbance of eelgrass Zostera marina by commercial mussel Mytilus edulis harvesting in Maine: Dragging impacts and habitat recovery: Marine Ecology Progress Series, v. 285, p. 57-73, https://doi.org/10.3354/meps285057.","productDescription":"17 p.","startPage":"57","endPage":"73","numberOfPages":"17","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":477889,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/meps285057","text":"Publisher Index Page"},{"id":237504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","otherGeospatial":"Maquoit Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.05260467529297,\n 43.79042818348387\n ],\n [\n -70.01346588134766,\n 43.837498549851624\n ],\n [\n -69.98634338378906,\n 43.866713048323184\n ],\n [\n -69.99698638916016,\n 43.86696056766485\n ],\n [\n -70.00865936279297,\n 43.85978208946686\n ],\n [\n -70.01930236816406,\n 43.859039438939455\n ],\n [\n -70.04505157470703,\n 43.841955923776396\n ],\n [\n -70.05706787109375,\n 43.82412443010574\n ],\n [\n -70.07080078125,\n 43.80727868289013\n ],\n [\n -70.07354736328125,\n 43.793402146335886\n ],\n [\n -70.05260467529297,\n 43.79042818348387\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"285","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a032ee4b0c8380cd5039b","contributors":{"authors":[{"text":"Neckles, Hilary A. 0000-0002-5662-2314 hneckles@usgs.gov","orcid":"https://orcid.org/0000-0002-5662-2314","contributorId":3821,"corporation":false,"usgs":true,"family":"Neckles","given":"Hilary","email":"hneckles@usgs.gov","middleInitial":"A.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":421396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Short, Frederick T.","contributorId":72078,"corporation":false,"usgs":true,"family":"Short","given":"Frederick","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":421393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barker, Seth","contributorId":41536,"corporation":false,"usgs":true,"family":"Barker","given":"Seth","email":"","affiliations":[],"preferred":false,"id":421395,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kopp, Blaine S.","contributorId":99648,"corporation":false,"usgs":true,"family":"Kopp","given":"Blaine","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":421394,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70028024,"text":"70028024 - 2005 - From the Field: Capturing beavers in box traps","interactions":[],"lastModifiedDate":"2012-03-12T17:20:41","indexId":"70028024","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"From the Field: Capturing beavers in box traps","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/0091-7648(2005)33[1153:FTFCBI]2.0.CO;2","issn":"00917648","usgsCitation":"Koenen, K., DeStefano, S., Henner, C., and Beroldi, T., 2005, From the Field: Capturing beavers in box traps: Wildlife Society Bulletin, v. 33, no. 3, p. 1153-1159, https://doi.org/10.2193/0091-7648(2005)33[1153:FTFCBI]2.0.CO;2.","startPage":"1153","endPage":"1159","numberOfPages":"7","costCenters":[],"links":[{"id":210225,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0091-7648(2005)33[1153:FTFCBI]2.0.CO;2"},{"id":237082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a13fce4b0c8380cd54867","contributors":{"authors":[{"text":"Koenen, K.","contributorId":84964,"corporation":false,"usgs":true,"family":"Koenen","given":"K.","affiliations":[],"preferred":false,"id":416199,"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":416198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henner, C.","contributorId":69771,"corporation":false,"usgs":true,"family":"Henner","given":"C.","affiliations":[],"preferred":false,"id":416197,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beroldi, T.","contributorId":43962,"corporation":false,"usgs":true,"family":"Beroldi","given":"T.","email":"","affiliations":[],"preferred":false,"id":416196,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1008480,"text":"1008480 - 2005 - Improving removal-based estimates of abundance by sampling a population of spatially distinct subpopulations","interactions":[],"lastModifiedDate":"2015-12-11T10:52:06","indexId":"1008480","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1039,"text":"Biometrics","active":true,"publicationSubtype":{"id":10}},"title":"Improving removal-based estimates of abundance by sampling a population of spatially distinct subpopulations","docAbstract":"

 A statistical modeling framework is described for estimating the abundances of spatially distinct subpopulations of animals surveyed using removal sampling. To illustrate this framework, hierarchical models are developed using the Poisson and negative-binomial distributions to model variation in abundance among subpopulations and using the beta distribution to model variation in capture probabilities. These models are fitted to the removal counts observed in a survey of a federally endangered fish species. The resulting estimates of abundance have similar or better precision than those computed using the conventional approach of analyzing the removal counts of each subpopulation separately. Extension of the hierarchical models to include spatial covariates of abundance is straightforward and may be used to identify important features of an animal's habitat or to predict the abundance of animals at unsampled locations.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1541-0420.2005.00360.x","usgsCitation":"Dorazio, R., Jelks, H., and Jordan, F., 2005, Improving removal-based estimates of abundance by sampling a population of spatially distinct subpopulations: Biometrics, v. 61, p. 1093-1101, https://doi.org/10.1111/j.1541-0420.2005.00360.x.","productDescription":"9 p.","startPage":"1093","endPage":"1101","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":132196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","noUsgsAuthors":false,"publicationDate":"2005-12-02","publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5bf3","contributors":{"authors":[{"text":"Dorazio, R.M. 0000-0003-2663-0468","orcid":"https://orcid.org/0000-0003-2663-0468","contributorId":23475,"corporation":false,"usgs":true,"family":"Dorazio","given":"R.M.","affiliations":[],"preferred":false,"id":317900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jelks, H.L. 0000-0002-0672-6297","orcid":"https://orcid.org/0000-0002-0672-6297","contributorId":12000,"corporation":false,"usgs":true,"family":"Jelks","given":"H.L.","affiliations":[],"preferred":false,"id":317899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jordan, F.","contributorId":80622,"corporation":false,"usgs":true,"family":"Jordan","given":"F.","affiliations":[],"preferred":false,"id":317901,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70028767,"text":"70028767 - 2005 - The inverse problem of refraction travel times, part I: Types of Geophysical Nonuniqueness through Minimization","interactions":[],"lastModifiedDate":"2012-03-12T17:20:57","indexId":"70028767","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3208,"text":"Pure and Applied Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"The inverse problem of refraction travel times, part I: Types of Geophysical Nonuniqueness through Minimization","docAbstract":"In a set of two papers we study the inverse problem of refraction travel times. The purpose of this work is to use the study as a basis for development of more sophisticated methods for finding more reliable solutions to the inverse problem of refraction travel times, which is known to be nonunique. The first paper, \"Types of Geophysical Nonuniqueness through Minimization,\" emphasizes the existence of different forms of nonuniqueness in the realm of inverse geophysical problems. Each type of nonuniqueness requires a different type and amount of a priori information to acquire a reliable solution. Based on such coupling, a nonuniqueness classification is designed. Therefore, since most inverse geophysical problems are nonunique, each inverse problem must be studied to define what type of nonuniqueness it belongs to and thus determine what type of a priori information is necessary to find a realistic solution. The second paper, \"Quantifying Refraction Nonuniqueness Using a Three-layer Model,\" serves as an example of such an approach. However, its main purpose is to provide a better understanding of the inverse refraction problem by studying the type of nonuniqueness it possesses. An approach for obtaining a realistic solution to the inverse refraction problem is planned to be offered in a third paper that is in preparation. The main goal of this paper is to redefine the existing generalized notion of nonuniqueness and a priori information by offering a classified, discriminate structure. Nonuniqueness is often encountered when trying to solve inverse problems. However, possible nonuniqueness diversity is typically neglected and nonuniqueness is regarded as a whole, as an unpleasant \"black box\" and is approached in the same manner by applying smoothing constraints, damping constraints with respect to the solution increment and, rarely, damping constraints with respect to some sparse reference information about the true parameters. In practice, when solving geophysical problems different types of nonuniqueness exist, and thus there are different ways to solve the problems. Nonuniqueness is usually regarded as due to data error, assuming the true geology is acceptably approximated by simple mathematical models. Compounding the nonlinear problems, geophysical applications routinely exhibit exact-data nonuniqueness even for models with very few parameters adding to the nonuniqueness due to data error. While nonuniqueness variations have been defined earlier, they have not been linked to specific use of a priori information necessary to resolve each case. Four types of nonuniqueness, typical for minimization problems are defined with the corresponding methods for inclusion of a priori information to find a realistic solution without resorting to a non-discriminative approach. The above-developed stand-alone classification is expected to be helpful when solving any geophysical inverse problems. ?? Birkha??user Verlag, Basel, 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00024-004-2615-1","issn":"00334553","usgsCitation":"Ivanov, J., Miller, R., Xia, J., Steeples, D., and Park, C., 2005, The inverse problem of refraction travel times, part I: Types of Geophysical Nonuniqueness through Minimization: Pure and Applied Geophysics, v. 162, no. 3, p. 447-459, https://doi.org/10.1007/s00024-004-2615-1.","startPage":"447","endPage":"459","numberOfPages":"13","costCenters":[],"links":[{"id":209639,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00024-004-2615-1"},{"id":236302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"162","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bad5fe4b08c986b323b8f","contributors":{"authors":[{"text":"Ivanov, J.","contributorId":107068,"corporation":false,"usgs":true,"family":"Ivanov","given":"J.","email":"","affiliations":[],"preferred":false,"id":419672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, R. D.","contributorId":92693,"corporation":false,"usgs":true,"family":"Miller","given":"R. D.","affiliations":[],"preferred":false,"id":419671,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Xia, J.","contributorId":63513,"corporation":false,"usgs":true,"family":"Xia","given":"J.","email":"","affiliations":[],"preferred":false,"id":419670,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steeples, D.","contributorId":30422,"corporation":false,"usgs":true,"family":"Steeples","given":"D.","email":"","affiliations":[],"preferred":false,"id":419669,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Park, C.B.","contributorId":21714,"corporation":false,"usgs":true,"family":"Park","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":419668,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":1008483,"text":"1008483 - 2005 - Critical literature review of the evidence for unpalatability of amphibian eggs and larvae","interactions":[],"lastModifiedDate":"2022-05-24T14:42:53.657428","indexId":"1008483","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Critical literature review of the evidence for unpalatability of amphibian eggs and larvae","docAbstract":"

We examined 142 papers, which contained 603 separate predator-prey trials, to investigate whether unpalatability is an important defense against predation for amphibian eggs and larvae. Although unpalatability is often cited as an antipredator defense, it was rarely demonstrated that 89% of the trials that we reviewed found prey to be palatable. The most extensively studied taxa, the genera Bufo and Rana, were diagnosed unpalatable at rates comparable to all other taxa. Diagnoses of unpalatability were not always consistent for a prey species across different predators and were influenced by experimental method. Despite these limitations and our conservative definition of unpalatability, several patterns emerged. First, across all taxonomic groups, eggs and hatchlings were unpalatable more often than mobile larval stages. Second, species that breed in temporary ponds were more likely to be palatable to fish predators than those that breed in permanent habitats. Third, fish and caudates were more likely to find amphibian prey unpalatable than insect predators. We conclude that unpalatability is rare, but when it occurs, it is a property of an ensemble (predator, prey, and alternative prey) and a life-history stage in a particular circumstance but is not a species-specific attribute. We suggest methods of experimentation that could strengthen future research on the palatability of amphibian eggs and larvae.

","language":"English","publisher":"Society for the Study of Amphibians and Reptiles","doi":"10.1670/1-05A.1","usgsCitation":"Gunzburger, M.S., and Travis, J., 2005, Critical literature review of the evidence for unpalatability of amphibian eggs and larvae: Journal of Herpetology, v. 39, p. 547-571, https://doi.org/10.1670/1-05A.1.","productDescription":"25 p.","startPage":"547","endPage":"571","numberOfPages":"25","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":132223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6833a3","contributors":{"authors":[{"text":"Gunzburger, Margaret S.","contributorId":43449,"corporation":false,"usgs":true,"family":"Gunzburger","given":"Margaret","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":317909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Travis, Joseph","contributorId":196667,"corporation":false,"usgs":false,"family":"Travis","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":317910,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029196,"text":"70029196 - 2005 - Direct observation of heavy metal-mineral association from the Clark Fork River Superfund Complex: Implications for metal transport and bioavailability","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029196","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Direct observation of heavy metal-mineral association from the Clark Fork River Superfund Complex: Implications for metal transport and bioavailability","docAbstract":"Two sets of samples from riverbeds and adjacent floodplains, separated by 80 river kilometers, were collected from the Clark Fork River Superfund Complex, Montana, (the largest Superfund site in the United States), and studied primarily with transmission electron microscopy (TEM) with several supporting techniques to determine heavy metal-mineral association. Seven of the eight samples studied were strongly influenced by material that once resided in mining and smelting dumps and impoundments; this material was transported downstream sometime during the last century and a half from the Butte/Anaconda areas. The eighth sample was from a deeper floodplain level and dates to premining days. The TEM observations afford a direct look, down to the nanometer level, at secondary mineral formation as a result of the breakdown of sulfides and silicates in the acid environment of this massive mine-drainage system. In the shallow, oxic floodplain sediments, heavy metals of concern in this system (As, Cu, Pb, and Zn) are taken up by the formation of sulfates (particularly Pb in jarosite), as well as hydrous metal oxides (As, Cu, Pb, and Zn in and on ferrihydrite, and a possibly new vernadite-like mineral). The oxides are long-lived in these systems, as they were also found in the anoxic riverbeds. Metals are also taken up by the formation of sulfides in sulfate-reducing environments as observed in the formation of nanoclusters of chalcopyrite and sphalerite. In all samples, clays make up between 5 and 20% of the sediment and carry significant amounts of Cu and Zn. The hydrous oxides, secondary sulfides, and clays provide several routes for metal transport downstream over long distances. Besides the potential bioavailability of heavy metals exchanged on and off the hydrous metal oxides and clays, nanometer-sized sulfides may also be highly reactive in the presence of biologic systems. Copyright ?? 2005 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.gca.2004.07.038","issn":"00167037","usgsCitation":"Hochella, M., Moore, J., Putnis, C., Putnis, A., Kasama, T., and Eberl, D.D., 2005, Direct observation of heavy metal-mineral association from the Clark Fork River Superfund Complex: Implications for metal transport and bioavailability: Geochimica et Cosmochimica Acta, v. 69, no. 7, p. 1651-1663, https://doi.org/10.1016/j.gca.2004.07.038.","startPage":"1651","endPage":"1663","numberOfPages":"13","costCenters":[],"links":[{"id":210580,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gca.2004.07.038"},{"id":237548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a01b1e4b0c8380cd4fcfd","contributors":{"authors":[{"text":"Hochella, M.F. Jr.","contributorId":30765,"corporation":false,"usgs":true,"family":"Hochella","given":"M.F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":421707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, J.N.","contributorId":22795,"corporation":false,"usgs":true,"family":"Moore","given":"J.N.","affiliations":[],"preferred":false,"id":421706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Putnis, C.V.","contributorId":61235,"corporation":false,"usgs":true,"family":"Putnis","given":"C.V.","email":"","affiliations":[],"preferred":false,"id":421708,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Putnis, A.","contributorId":20965,"corporation":false,"usgs":true,"family":"Putnis","given":"A.","email":"","affiliations":[],"preferred":false,"id":421705,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kasama, T.","contributorId":20143,"corporation":false,"usgs":true,"family":"Kasama","given":"T.","email":"","affiliations":[],"preferred":false,"id":421704,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Eberl, D. D.","contributorId":66282,"corporation":false,"usgs":true,"family":"Eberl","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":421709,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70027933,"text":"70027933 - 2005 - A magnetotelluric study of the sensitivity of an area to seismoelectric signals","interactions":[],"lastModifiedDate":"2013-02-21T20:46:12","indexId":"70027933","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2824,"text":"Natural Hazards and Earth System Sciences","active":true,"publicationSubtype":{"id":10}},"title":"A magnetotelluric study of the sensitivity of an area to seismoelectric signals","docAbstract":"During recent years, efforts at better understanding the physical properties of precursory ultra-low frequency pre-seismic electric signals (SES) have been intensified. Experiments show that SES cannot be observed at all points of the Earth's surface but only at certain so-called sensitive sites. Moreover, a sensitive site is capable of collecting SES from only a restricted number of seismic areas (selectivity effect). Tberefore the installation of a permanent station appropriate for SES collection should necessarily be preceded by a pilot study over a broad area and for a long duration. In short, a number of temporary stations are installed and, after the occurrence of several significant earthquakes (EQs) from a given seismic area, the most appropriate (if any) of these temporary stations, in the sense that they happen to collect SES, can be selected as permanent. Such a long experiment constitutes a serious disadvantage in identifying a site as SES sensitive. However, the SES sensitivity of a site should be related to the geoelectric structure of the area that hosts the site as well as the regional geoelectric structure between the station and the seismic focal area. Thus, knowledge of the local and regional geoelectric structure can dramatically reduce the time involved in identifying SES sites. hi this paper the magnetotelluric method is used to investigate the conductivity structure of an area where a permanent SES station is in operation. Although general conclusions cannot be drawn, the area surrounding an SES site near Ioannina, Greece is characterized by: (1) major faults in the vicinity; (2) highly resistive structure flanked by abrupt conductivity contrasts associated with large-scale geologic contacts, and (3) local inhomogeneities in conductivity structure. The above results are consistent with the fact that electric field amplitudes from remotely-generated signals should be appreciably stronger at such sites when compared to neighboring sites. European Geosciences Union ?? 2005 Author(s). This work is licensed under a Creative Commons License.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Hazards and Earth System Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"European Geosciences Union","doi":"10.5194/nhess-5-931-2005","issn":"15618633","usgsCitation":"Balasis, G., Bedrosian, P.A., and Eftaxias, K., 2005, A magnetotelluric study of the sensitivity of an area to seismoelectric signals: Natural Hazards and Earth System Sciences, v. 5, no. 6, p. 931-946, https://doi.org/10.5194/nhess-5-931-2005.","startPage":"931","endPage":"946","numberOfPages":"16","costCenters":[],"links":[{"id":477929,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/nhess-5-931-2005","text":"Publisher Index Page"},{"id":238043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267920,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.5194/nhess-5-931-2005"}],"volume":"5","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-11-23","publicationStatus":"PW","scienceBaseUri":"5059e446e4b0c8380cd46542","contributors":{"authors":[{"text":"Balasis, G.","contributorId":67718,"corporation":false,"usgs":true,"family":"Balasis","given":"G.","email":"","affiliations":[],"preferred":false,"id":415830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedrosian, P. A.","contributorId":100109,"corporation":false,"usgs":true,"family":"Bedrosian","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":415832,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eftaxias, K.","contributorId":91292,"corporation":false,"usgs":true,"family":"Eftaxias","given":"K.","email":"","affiliations":[],"preferred":false,"id":415831,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70027325,"text":"70027325 - 2005 - An exploratory assessment of Cuban Treefrog (Osteopilus septentrionalis) tadpoles as predators of native and nonindigenous tadpoles in Florida","interactions":[],"lastModifiedDate":"2015-12-14T11:04:10","indexId":"70027325","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":751,"text":"Amphibia-Reptilia","active":true,"publicationSubtype":{"id":10}},"title":"An exploratory assessment of Cuban Treefrog (Osteopilus septentrionalis) tadpoles as predators of native and nonindigenous tadpoles in Florida","docAbstract":"

[No abstract available]

","language":"English","doi":"10.1163/156853805774806313","issn":"01735373","usgsCitation":"Smith, K.G., 2005, An exploratory assessment of Cuban Treefrog (Osteopilus septentrionalis) tadpoles as predators of native and nonindigenous tadpoles in Florida: Amphibia-Reptilia, v. 26, no. 4, p. 571-575, https://doi.org/10.1163/156853805774806313.","productDescription":"5 p.","startPage":"571","endPage":"575","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":477697,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1163/156853805774806313","text":"Publisher Index Page"},{"id":235385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209156,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1163/156853805774806313"}],"volume":"26","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea6ae4b0c8380cd48848","contributors":{"authors":[{"text":"Smith, Kimberly G.","contributorId":47720,"corporation":false,"usgs":true,"family":"Smith","given":"Kimberly","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":413183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70027868,"text":"70027868 - 2005 - Matthevia (Polyplacophora) invades the Ordovician: The first reported post-Cambrian occurrence","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70027868","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2412,"text":"Journal of Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"Matthevia (Polyplacophora) invades the Ordovician: The first reported post-Cambrian occurrence","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Paleontology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1666/0022-3360(2005)079[1021:MPITOT]2.0.CO;2","issn":"00223360","usgsCitation":"Pojeta, J., Taylor, J.F., and Darrough, G., 2005, Matthevia (Polyplacophora) invades the Ordovician: The first reported post-Cambrian occurrence: Journal of Paleontology, v. 79, no. 5, p. 1021-1027, https://doi.org/10.1666/0022-3360(2005)079[1021:MPITOT]2.0.CO;2.","startPage":"1021","endPage":"1027","numberOfPages":"7","costCenters":[],"links":[{"id":211013,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1666/0022-3360(2005)079[1021:MPITOT]2.0.CO;2"},{"id":238148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5292e4b0c8380cd6c502","contributors":{"authors":[{"text":"Pojeta, J. Jr.","contributorId":55150,"corporation":false,"usgs":true,"family":"Pojeta","given":"J.","suffix":"Jr.","affiliations":[],"preferred":false,"id":415611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, John F.","contributorId":80890,"corporation":false,"usgs":false,"family":"Taylor","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":415612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darrough, G.","contributorId":101074,"corporation":false,"usgs":true,"family":"Darrough","given":"G.","email":"","affiliations":[],"preferred":false,"id":415613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70028031,"text":"70028031 - 2005 - Historical record of Yersinia ruckeri and Aeromonas salmonicida among sea-run Atlantic salmon (Salmo salar) in the Penobscot River","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70028031","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1123,"text":"Bulletin of the European Association of Fish Pathologists","active":true,"publicationSubtype":{"id":10}},"title":"Historical record of Yersinia ruckeri and Aeromonas salmonicida among sea-run Atlantic salmon (Salmo salar) in the Penobscot River","docAbstract":"Despite restoration efforts, only about 2,000 Atlantic salmon (Salmo salar) salmon have annually returned to New England Rivers and more than 71% of these fish migrate to the Penobscot River alone. This report provides a historical compilation on the prevalence's of both Yersinia ruckeri, cause of enteric redmouth disease, and Aeromonas salmonicida, cause of furunculosis, among mature sea-run Atlantic salmon that returned to the Penobscot River from 1976 to 2003. Aeromonas salmonicida was detected in 28.6% and Yersinia ruckeri was detected among 50% of the yearly returns. Consequently, Atlantic salmon that return to the river are potential reservoirs of infection.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the European Association of Fish Pathologists","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"01080288","usgsCitation":"Cipriano, R.C., and Coll, J., 2005, Historical record of Yersinia ruckeri and Aeromonas salmonicida among sea-run Atlantic salmon (Salmo salar) in the Penobscot River: Bulletin of the European Association of Fish Pathologists, v. 25, no. 6, p. 280-283.","startPage":"280","endPage":"283","numberOfPages":"4","costCenters":[],"links":[{"id":237187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a319ae4b0c8380cd5e079","contributors":{"authors":[{"text":"Cipriano, R. C.","contributorId":12400,"corporation":false,"usgs":true,"family":"Cipriano","given":"R.","middleInitial":"C.","affiliations":[],"preferred":false,"id":416219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coll, J.","contributorId":11392,"corporation":false,"usgs":true,"family":"Coll","given":"J.","email":"","affiliations":[],"preferred":false,"id":416218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029104,"text":"70029104 - 2005 - A comparative analysis of the Global Land Cover 2000 and MODIS land cover data sets","interactions":[],"lastModifiedDate":"2017-04-10T13:04:38","indexId":"70029104","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"A comparative analysis of the Global Land Cover 2000 and MODIS land cover data sets","docAbstract":"

Accurate and up-to-date global land cover data sets are necessary for various global change research studies including climate change, biodiversity conservation, ecosystem assessment, and environmental modeling. In recent years, substantial advancement has been achieved in generating such data products. Yet, we are far from producing geospatially consistent high-quality data at an operational level. We compared the recently available Global Land Cover 2000 (GLC-2000) and MODerate resolution Imaging Spectrometer (MODIS) global land cover data to evaluate the similarities and differences in methodologies and results, and to identify areas of spatial agreement and disagreement. These two global land cover data sets were prepared using different data sources, classification systems, and methodologies, but using the same spatial resolution (i.e., 1 km) satellite data. Our analysis shows a general agreement at the class aggregate level except for savannas/shrublands, and wetlands. The disagreement, however, increases when comparing detailed land cover classes. Similarly, percent agreement between the two data sets was found to be highly variable among biomes. The identified areas of spatial agreement and disagreement will be useful for both data producers and users. Data producers may use the areas of spatial agreement for training area selection and pay special attention to areas of disagreement for further improvement in future land cover characterization and mapping. Users can conveniently use the findings in the areas of agreement, whereas users might need to verify the informaiton in the areas of disagreement with the help of secondary information. Learning from past experience and building on the existing infrastructure (e.g., regional networks), further research is necessary to (1) reduce ambiguity in land cover definitions, (2) increase availability of improved spatial, spectral, radiometric, and geometric resolution satellite data, and (3) develop advanced classification algorithms.

","language":"English","publisher":"Elsevier","doi":"10.1016/j.rse.2004.09.005","issn":"00344257","usgsCitation":"Giri, S., Zhu, Z., and Reed, B., 2005, A comparative analysis of the Global Land Cover 2000 and MODIS land cover data sets: Remote Sensing of Environment, v. 94, no. 1, p. 123-132, https://doi.org/10.1016/j.rse.2004.09.005.","productDescription":"10 p.","startPage":"123","endPage":"132","numberOfPages":"10","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":237829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210803,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.rse.2004.09.005"}],"volume":"94","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e34fe4b0c8380cd45f69","contributors":{"authors":[{"text":"Giri, S.","contributorId":102621,"corporation":false,"usgs":true,"family":"Giri","given":"S.","email":"","affiliations":[],"preferred":false,"id":421341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zhu, Z.","contributorId":10898,"corporation":false,"usgs":true,"family":"Zhu","given":"Z.","email":"","affiliations":[],"preferred":false,"id":421339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, B.","contributorId":62352,"corporation":false,"usgs":true,"family":"Reed","given":"B.","email":"","affiliations":[],"preferred":false,"id":421340,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1012930,"text":"1012930 - 2005 - Discovery of 100-160-year-old iceberg gouges and their relation to halibut habitat in Glacier Bay, Alaska","interactions":[],"lastModifiedDate":"2016-06-20T15:05:46","indexId":"1012930","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Discovery of 100-160-year-old iceberg gouges and their relation to halibut habitat in Glacier Bay, Alaska","docAbstract":"

Side-scan sonar and multibeam imagery of Glacier Bay, Alaska, revealed complex iceberg gouge patterns at water depths to 135 m on the floor of Whidbey Passage and south to the bay entrance. These previously undiscovered gouges likely formed more than 100 years ago as the glacier retreated rapidly up Glacier Bay. Gouged areas free of fine sediment supported greater biodiversity of Pacific halibut Hippoglossus stenolepsis than nearby sediment-filled gouges, probably due to increased habitat complexity. Small Pacific halibut were forund more frequently in sediment-free gouged areas, presumably due to higher prey abundance. In contrast, large Pacific halibut were found more frequently on soft substrates such as sediment-filled gouges, where they could bury themselves and ambush prey.

","language":"English","publisher":"American Fisheries Society","usgsCitation":"Carlson, P., Hooge, P., and Cochrane, G., 2005, Discovery of 100-160-year-old iceberg gouges and their relation to halibut habitat in Glacier Bay, Alaska: American Fisheries Society Symposium, v. 41, p. 235-243.","productDescription":"9 p.","startPage":"235","endPage":"243","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":133044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269654,"type":{"id":11,"text":"Document"},"url":"https://walrus.wr.usgs.gov/nearshorehab/Carlson_Hooge_Cochrane.pdf"}],"volume":"41","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae88d","contributors":{"authors":[{"text":"Carlson, P.R.","contributorId":97055,"corporation":false,"usgs":true,"family":"Carlson","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":318440,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hooge, P.N.","contributorId":36515,"corporation":false,"usgs":true,"family":"Hooge","given":"P.N.","email":"","affiliations":[],"preferred":false,"id":318439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cochrane, G.R.","contributorId":104002,"corporation":false,"usgs":true,"family":"Cochrane","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":318441,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70027426,"text":"70027426 - 2005 - Occurrence of antibiotics in water from 13 fish hatcheries, 2001-2003","interactions":[],"lastModifiedDate":"2018-10-31T09:54:23","indexId":"70027426","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2040,"text":"International Journal of Environmental Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of antibiotics in water from 13 fish hatcheries, 2001-2003","docAbstract":"

A 2-year study of extensive and intensive fish hatcheries was conducted to assess the general temporal occurrence of antibiotics in aquaculture. Antibiotics were detected in 15% of the water samples collected during the 2001-2002 collection period and in 31% of the samples during the 2003 collection period. Antibiotics were detected more frequently in samples from the intensive hatcheries (17 and 39%) than in samples from the extensive hatcheries (14 and 4%) during the 2001-2002 and 2003 collection periods, respectively. The maximum ormetoprim, oxytetracycline, and sulphadimethoxine concentrations were higher in samples from the intensive hatcheries (12, 10, and 36 µg L-1), respectively, than in samples from the extensive hatcheries (<0.05, 0.31, and 1.2 µg L-1), respectively. Sulphadimethoxine persisted for a longer period of time (up to 48 days) than ormetoprim (up to 28 days) and oxytetracycline (less than 20 days).

","language":"English","publisher":"Gordon and Breach","doi":"10.1080/03067310500273682","issn":"03067319","usgsCitation":"Dietze, J., Scribner, E., Meyer, M.T., and Kolpin, D., 2005, Occurrence of antibiotics in water from 13 fish hatcheries, 2001-2003: International Journal of Environmental Analytical Chemistry, v. 85, no. 15, p. 1141-1152, https://doi.org/10.1080/03067310500273682.","productDescription":"12 p.","startPage":"1141","endPage":"1152","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210900,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/03067310500273682"}],"volume":"85","issue":"15","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6bcfe4b0c8380cd748d2","contributors":{"authors":[{"text":"Dietze, J.E.","contributorId":11404,"corporation":false,"usgs":true,"family":"Dietze","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":413579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scribner, E.A.","contributorId":50925,"corporation":false,"usgs":true,"family":"Scribner","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":413580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, M. T.","contributorId":92279,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":413582,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kolpin, D.W.","contributorId":87565,"corporation":false,"usgs":true,"family":"Kolpin","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":413581,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70028250,"text":"70028250 - 2005 - The apparatus composition and architecture of Cordylodus pander - Concepts of homology in primitive conodonts","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028250","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1142,"text":"Bulletins of American Paleontology","active":true,"publicationSubtype":{"id":10}},"title":"The apparatus composition and architecture of Cordylodus pander - Concepts of homology in primitive conodonts","docAbstract":"A clear distinction may be drawn between the perpendicular architecture of the feeding apparatus of ozarkodinid, prioniodontid and prioniodinid conodonts, in which the P elements are situated at a high angle to the M and S elements, and the parallel architecture of panderodontid and other coniform apparatuses, where two suites of coniform elements lie parallel to each other and oppose across the midline. The quest for homologies between the two architectures has been fraught with difficulty, at least in part because of the paucity of natural assemblages of coniform taxa. A diagenetically fused apparatus of Cordylodns lindstroini elements is here described which is made up of one rounded and two compressed element morphotypes. One of the compressed elements is bowed and asymmetrical and the other is unbowed and more symmetrical. These compressed elements are considered to be homologous with those of panderodontid apparatuses and would have lain at the caudal end of the parallel arrays, with the more symmetrical morphotypes located rostrally to the asymmetrical ones. The bowed and unbowed compressed elements of Cordylodns thus correspond, respectively, to the pt and pf positions of panderodontid apparatuses. In addition, the presence of symmetry transition within the rounded elements of Cordylodns, but not the compressed morphotypes, enables correlation of these with the S and M element locations of ozarkodinid apparatuses. By extension, the compressed elements must be homologues of the P elements. Specifically, the asymmetrical pt morphotype is homologous with the P1 of ozarkodinids and the more symmetrical and rostral pf morphotype is homologous with the P2 position. However, because of uncertainties over the nature of topological transformation of the rostral element array (the \"rounded\" or \"costate\" suites), it is not possible to recognize specific homologies between these elements and the M and S elements of ozarkodinids. Morphologic differentiation of P from M and S element suites thus preceded the topological transformation from parallel to perpendicular apparatus architectures.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletins of American Paleontology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00075779","usgsCitation":"Smith, M., Donoghue, P., and Repetski, J., 2005, The apparatus composition and architecture of Cordylodus pander - Concepts of homology in primitive conodonts: Bulletins of American Paleontology, v. 2005, no. 369, p. 19-33.","startPage":"19","endPage":"33","numberOfPages":"15","costCenters":[],"links":[{"id":236918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2005","issue":"369","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba9c2e4b08c986b3224c6","contributors":{"authors":[{"text":"Smith, M.P.","contributorId":19720,"corporation":false,"usgs":true,"family":"Smith","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":417230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donoghue, P.C.J.","contributorId":56018,"corporation":false,"usgs":true,"family":"Donoghue","given":"P.C.J.","email":"","affiliations":[],"preferred":false,"id":417232,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Repetski, J.E.","contributorId":38579,"corporation":false,"usgs":true,"family":"Repetski","given":"J.E.","affiliations":[],"preferred":false,"id":417231,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70027806,"text":"70027806 - 2005 - Aquatic chytrid pathogen detected in terrestrial plethodontid salamander","interactions":[],"lastModifiedDate":"2012-03-12T17:20:50","indexId":"70027806","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"title":"Aquatic chytrid pathogen detected in terrestrial plethodontid salamander","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetological Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0018084X","usgsCitation":"Cummer, M., Green, D.E., and O’Neill, E.M., 2005, Aquatic chytrid pathogen detected in terrestrial plethodontid salamander: Herpetological Review, v. 36, no. 3, p. 248-249.","startPage":"248","endPage":"249","numberOfPages":"2","costCenters":[],"links":[{"id":238214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ed0ce4b0c8380cd495b9","contributors":{"authors":[{"text":"Cummer, M.R.","contributorId":61238,"corporation":false,"usgs":true,"family":"Cummer","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":415302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, D. E. 0000-0002-7663-1832","orcid":"https://orcid.org/0000-0002-7663-1832","contributorId":58971,"corporation":false,"usgs":true,"family":"Green","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":415301,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Neill, E. M.","contributorId":42023,"corporation":false,"usgs":true,"family":"O’Neill","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":415300,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70027424,"text":"70027424 - 2005 - Taxonomic status and biology of the Cuban blackhawk, Buteogallus anthracinus gundlachii (AVES: Accipitridae)","interactions":[],"lastModifiedDate":"2012-03-12T17:20:47","indexId":"70027424","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2442,"text":"Journal of Raptor Research","active":true,"publicationSubtype":{"id":10}},"title":"Taxonomic status and biology of the Cuban blackhawk, Buteogallus anthracinus gundlachii (AVES: Accipitridae)","docAbstract":"We reevaluate the taxonomic status of the Cuban population of the Common Black-Hawk (Buteogallus anthracinus) based on our examination of additional specimens, nests, eggs, and voice data. Buteogallus a. gundlachii is smaller than mainland populations of anthracinus and differs from mainland birds in plumage coloration and pattern. The common (alarm) call of gundlachii is a series of three or four notes, differing from that of mainland anthracinus, whose call consists of 9-24 notes. In the Isla de Pinos, Cuba, we observed gundlachii eating two species of land crabs (71.4%), centipedes (7.1%), lizards (10.7%), mammals (7.1%), and a bird (3.6%). We consider Buteogallus gundlachii Cabanis 1854 (1855), the Cuban Black-Hawk, to be a full species, endemic to Cuba, Isla de Pinos, and many of the cays of the Cuban Archipelago. ?? 2005 The Raptor Research Foundation, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Raptor Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08921016","usgsCitation":"Wiley, J.W., and Garrido, O., 2005, Taxonomic status and biology of the Cuban blackhawk, Buteogallus anthracinus gundlachii (AVES: Accipitridae): Journal of Raptor Research, v. 39, no. 4, p. 351-364.","startPage":"351","endPage":"364","numberOfPages":"14","costCenters":[],"links":[{"id":237940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba3eee4b08c986b31ffbd","contributors":{"authors":[{"text":"Wiley, J. W.","contributorId":51399,"corporation":false,"usgs":false,"family":"Wiley","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":413573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrido, O.H.","contributorId":105905,"corporation":false,"usgs":true,"family":"Garrido","given":"O.H.","email":"","affiliations":[],"preferred":false,"id":413574,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1008110,"text":"1008110 - 2005 - Spring migration of northern pintails from California's Central Valley wintering area tracked by satellite telemetry: Routes, timing, and destinations","interactions":[],"lastModifiedDate":"2021-06-10T21:17:24.610305","indexId":"1008110","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Spring migration of northern pintails from California's Central Valley wintering area tracked by satellite telemetry: Routes, timing, and destinations","docAbstract":"

We used satellite transmitters to track the 2000–2003 spring migrations of adult female Northern Pintails (Anas acuta L., 1758) from California's Central Valley, USA. PTT-tagged Pintails departed during late February to mid-March, and 77%–87% stopped first in the region of south-central Oregon, extreme northwestern Nevada, and northeastern California (SONEC). Subsequently, most Pintails used migration strategies characterized by the length of stay in SONEC and subsequent destinations: (i) extended stay in SONEC, migrated late April to early May directly to Alaska over the Pacific Ocean (7%–23% annually); (ii) same timing as in i, but flew to Alaska along the Pacific Coast using stopovers (0%–28% annually); (iii) moderate period in SONEC, migrated late March to mid-April directly primarily to southern Alberta in Prairie Canada (17%–39% annually), with many moving to northern Canada or Alaska; or (iv) short period in SONEC, migrated early to late March to Prairie Canada via stopovers primarily in southern Idaho and western Montana (32%–50% annually), with some moving to northern Canada or Alaska. Pintails that bypassed SONEC used these same strategies or moved easterly. Pintails modified migration strategies relative to record cold temperatures and wetland abundance in the mid-continent prairie region.

","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/z05-125","usgsCitation":"Miller, M.R., Takekawa, J.Y., Fleskes, J., Orthmeyer, D., Casazza, M.L., and Perry, W., 2005, Spring migration of northern pintails from California's Central Valley wintering area tracked by satellite telemetry: Routes, timing, and destinations: Canadian Journal of Zoology, v. 83, no. 10, p. 1314-1332, https://doi.org/10.1139/z05-125.","productDescription":"19 p.","startPage":"1314","endPage":"1332","numberOfPages":"19","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":132679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"83","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49e4","contributors":{"authors":[{"text":"Miller, M. R.","contributorId":19104,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":316772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":316774,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleskes, J. P.","contributorId":98661,"corporation":false,"usgs":true,"family":"Fleskes","given":"J. P.","affiliations":[],"preferred":false,"id":316776,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Orthmeyer, D.L.","contributorId":84684,"corporation":false,"usgs":true,"family":"Orthmeyer","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":316775,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Casazza, Michael L. 0000-0002-5636-735X mike_casazza@usgs.gov","orcid":"https://orcid.org/0000-0002-5636-735X","contributorId":2091,"corporation":false,"usgs":true,"family":"Casazza","given":"Michael","email":"mike_casazza@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":316773,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Perry, W.M.","contributorId":15949,"corporation":false,"usgs":true,"family":"Perry","given":"W.M.","affiliations":[],"preferred":false,"id":316771,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70029395,"text":"70029395 - 2005 - Characterization of waste rock associated with acid drainage at the Penn Mine, California, by ground-based visible to short-wave infrared reflectance spectroscopy assisted by digital mapping","interactions":[],"lastModifiedDate":"2018-09-25T10:15:15","indexId":"70029395","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of waste rock associated with acid drainage at the Penn Mine, California, by ground-based visible to short-wave infrared reflectance spectroscopy assisted by digital mapping","docAbstract":"Prior to remediation at the abandoned Cu-Zn Penn Mine in the Foothills massive sulfide belt of the Sierra Nevada, CA, acid mine drainage (AMD) was created, in part, by the subaerial oxidation of sulfides exposed on several waste piles. To support remediation efforts, a mineralogical study of the waste piles was undertaken by acquiring reflectance spectra (measured in the visible to short-wave infrared range of light (0.35-2.5 ??m) using a portable, digitally integrated pen tablet PC mapping system with differential global positioning system and laser rangefinder support. Analysis of the spectral data made use of a continuum removal and band-shape comparison method, and of reference spectral libraries of end-member minerals and mineral mixtures. Identification of secondary Fe-bearing minerals focused on band matching in the region between 0.43 and 1.3 ??m. Identification of sheet and other silicates was based on band-shape analysis in the region between 1.9 and 2.4 ??m. Analysis of reflectance spectra of characterized rock samples from the mine helped in gauging the spectral response to particle size and mixtures. The resulting mineral maps delineated a pattern of accumulation of secondary Fe minerals, wherein centers of copiapite and jarosite that formed at low pH (<3) were surrounded successively by goethite and hematite, which mark progressive increases in pH. This pattern represents the evolution of acid solutions discharged from the pyritic waste piles and the subsequent accumulation of secondary precipitates by hydrolysis reactions. The results highlight the high capacity of the pyritic waste to release further acid mine drainage into the environment, as well as the effectiveness of the mapping method to detect subtle changes in surface mineralogy and to produce maps useful to agencies responsible for remediating the site. ?? 2004 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.06.045","issn":"00092541","usgsCitation":"Montero, S., Brimhall, G., Alpers, C.N., and Swayze, G., 2005, Characterization of waste rock associated with acid drainage at the Penn Mine, California, by ground-based visible to short-wave infrared reflectance spectroscopy assisted by digital mapping: Chemical Geology, v. 215, no. 1-4 SPEC. ISS., p. 453-472, https://doi.org/10.1016/j.chemgeo.2004.06.045.","startPage":"453","endPage":"472","numberOfPages":"20","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":237812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210786,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.06.045"}],"volume":"215","issue":"1-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f4e9e4b0c8380cd4bfd2","contributors":{"authors":[{"text":"Montero, S.I.C.","contributorId":87744,"corporation":false,"usgs":true,"family":"Montero","given":"S.I.C.","email":"","affiliations":[],"preferred":false,"id":422553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brimhall, G.H.","contributorId":91992,"corporation":false,"usgs":true,"family":"Brimhall","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":422554,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":422555,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swayze, G.A. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":21570,"corporation":false,"usgs":true,"family":"Swayze","given":"G.A.","affiliations":[],"preferred":false,"id":422552,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70027407,"text":"70027407 - 2005 - Outgassing models for Landsat-4 thematic mapper short wave infrared bands","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70027407","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Outgassing models for Landsat-4 thematic mapper short wave infrared bands","docAbstract":"Detector responses to the Internal Calibrator (IC) pulses in the Landsat-4 Thematic Mapper (TM) have been observed to follow an oscillatory behavior. This phenomenon is present only in the Short Wave Infrared (SWIR) bands and has been observed throughout the lifetime of the instrument, which was launched in July 1982 and imaged the Earth's surface until late 1993. These periodic changes in amplitude, which can be as large as 7.5 percent, are known as outgassing effects and are believed to be due to optical interference caused by a gradual buildup of an ice-like material on the window of the cryogenically cooled dewar containing the SWIR detectors. Similar outgassing effects in the Landsat-5 TM have been characterized using an optical thin-film model that relates detector behavior to the ice film growth rate, which was found to gradually decrease with time. A similar approach, which takes into consideration the different operational history of the instrument, has been applied in this study to three closely sampled data sets acquired throughout the lifetime of the Landsat-4 TM. Although Landsat-4 and Landsat-5 Thematic Mappers are essentially identical instruments, data generated from analyses of outgassing effects indicate subtle, but important, differences between the two. The estimated lifetime model could improve radiometric accuracy by as much as five percent.","largerWorkTitle":"Proceedings of SPIE - The International Society for Optical Engineering","conferenceTitle":"Earth Observing Systems X","conferenceDate":"31 July 2005 through 2 August 2005","conferenceLocation":"San Diego, CA","language":"English","doi":"10.1117/12.620160","issn":"0277786X","usgsCitation":"Micijevic, E., and Helder, D., 2005, Outgassing models for Landsat-4 thematic mapper short wave infrared bands, in Proceedings of SPIE - The International Society for Optical Engineering, v. 5882, San Diego, CA, 31 July 2005 through 2 August 2005, p. 1-11, https://doi.org/10.1117/12.620160.","startPage":"1","endPage":"11","numberOfPages":"11","costCenters":[],"links":[{"id":211130,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1117/12.620160"},{"id":238328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5882","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a71bce4b0c8380cd7672e","contributors":{"editors":[{"text":"Butler J.J.","contributorId":128408,"corporation":true,"usgs":false,"organization":"Butler J.J.","id":536614,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Micijevic, E. 0000-0002-3828-9239","orcid":"https://orcid.org/0000-0002-3828-9239","contributorId":59939,"corporation":false,"usgs":true,"family":"Micijevic","given":"E.","affiliations":[],"preferred":false,"id":413528,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helder, D. L. 0000-0002-7379-4679","orcid":"https://orcid.org/0000-0002-7379-4679","contributorId":51496,"corporation":false,"usgs":true,"family":"Helder","given":"D. L.","affiliations":[],"preferred":false,"id":413527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}