{"pageNumber":"227","pageRowStart":"5650","pageSize":"25","recordCount":10956,"records":[{"id":70028358,"text":"70028358 - 2006 - Genetic variation among subspecies of Least Tern (Sterna antillarum): Implications for conservation","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028358","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"Genetic variation among subspecies of Least Tern (Sterna antillarum): Implications for conservation","docAbstract":"DNA sequence variation from two nuclear introns and part of the mitochondrial cytochrome-b gene were used to Evaluate population structure among three subspecies of Least Term that nest in the United States (California [Sterna antillarum browni], Interior [S. a. athalassos], Eastern [S. a. antillarum]). Sequence variation was highest for nuclear intron XI (Gadp) within the glyceraldehyde-3-phosphate dehydrogenase gene. The second nuclear intron was fixed for the same allele in all subspecies. Fixation indices, FST and MST, for Gadp indicated genetic divergence between California and Interior subspecies. Estimates of nuclear gene flow were <4 individuals/generation, except between the Interior and Eastern subspecies (4 individuals/generation). Genetic indices for mitochondrial DNA did not differ among subspecies, and gene flows (reflecting female dispersal) ranged from 10 to 83 individuals/generation. Reservations are expressed about the validity of the current subspecific divisions and further research is required, including their taxonomic relationship to the Little Tern (Sterna albifrons).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Waterbirds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1675/1524-4695(2006)29[176:GVASOL]2.0.CO;2","issn":"15244695","usgsCitation":"Whittier, J.B., Leslie, D., and Van Den Bussche, R.A., 2006, Genetic variation among subspecies of Least Tern (Sterna antillarum): Implications for conservation: Waterbirds, v. 29, no. 2, p. 176-184, https://doi.org/10.1675/1524-4695(2006)29[176:GVASOL]2.0.CO;2.","startPage":"176","endPage":"184","numberOfPages":"9","costCenters":[],"links":[{"id":210188,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1675/1524-4695(2006)29[176:GVASOL]2.0.CO;2"},{"id":237032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a158be4b0c8380cd54e78","contributors":{"authors":[{"text":"Whittier, Joanna B.","contributorId":53151,"corporation":false,"usgs":false,"family":"Whittier","given":"Joanna","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":417692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leslie, David M. Jr.","contributorId":52514,"corporation":false,"usgs":true,"family":"Leslie","given":"David M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":417691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Den Bussche, Ronald A.","contributorId":41121,"corporation":false,"usgs":true,"family":"Van Den Bussche","given":"Ronald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":417690,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028389,"text":"70028389 - 2006 - Leaf breakdown in streams differing in catchment land use","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028389","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1696,"text":"Freshwater Biology","active":true,"publicationSubtype":{"id":10}},"title":"Leaf breakdown in streams differing in catchment land use","docAbstract":"1. The impact of changes in land use on stream ecosystem function is poorly understood. We studied leaf breakdown, a fundamental process of stream ecosystems, in streams that represent a range of catchment land use in the Piedmont physiographic province of the south-eastern United States. 2. We placed bags of chalk maple (Acer barbatum) leaves in similar-sized streams in 12 catchments of differing dominant land use: four forested, three agricultural, two suburban and three urban catchments. We measured leaf mass, invertebrate abundance and fungal biomass in leaf bags over time. 3. Leaves decayed significantly faster in agricultural (0.0465 day-1) and urban (0.0474 day-1) streams than in suburban (0.0173 day-1) and forested (0.0100 day-1) streams. Additionally, breakdown rates in the agricultural and urban streams were among the fastest reported for deciduous leaves in any stream. Nutrient concentrations in agricultural streams were significantly higher than in any other land-use type. Fungal biomass associated with leaves was significantly lower in urban streams; while shredder abundance in leaf bags was significantly higher in forested and agricultural streams than in suburban and urban streams. Storm runoff was significantly higher in urban and suburban catchments that had higher impervious surface cover than forested or agricultural catchments. 4. We propose that processes accelerating leaf breakdown in agricultural and urban streams were not the same: faster breakdown in agricultural streams was due to increased biological activity as a result of nutrient enrichment, whereas faster breakdown in urban streams was a result of physical fragmentation resulting from higher storm runoff. ?? 2006 The Authors.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Freshwater Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-2427.2006.01612.x","issn":"00465070","usgsCitation":"Paul, M., Meyer, J., and Couch, C.A., 2006, Leaf breakdown in streams differing in catchment land use: Freshwater Biology, v. 51, no. 9, p. 1684-1695, https://doi.org/10.1111/j.1365-2427.2006.01612.x.","startPage":"1684","endPage":"1695","numberOfPages":"12","costCenters":[],"links":[{"id":210134,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2427.2006.01612.x"},{"id":236963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"9","noUsgsAuthors":false,"publicationDate":"2006-08-02","publicationStatus":"PW","scienceBaseUri":"505a45e9e4b0c8380cd6751b","contributors":{"authors":[{"text":"Paul, M.J.","contributorId":71300,"corporation":false,"usgs":true,"family":"Paul","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":417848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, J.L.","contributorId":73316,"corporation":false,"usgs":true,"family":"Meyer","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":417849,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Couch, C. A.","contributorId":36972,"corporation":false,"usgs":true,"family":"Couch","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":417847,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70030456,"text":"70030456 - 2006 - State summaries: Kentucky","interactions":[],"lastModifiedDate":"2012-03-12T17:21:04","indexId":"70030456","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"State summaries: Kentucky","docAbstract":"Kentucky mines coal, limestone, clay, sand and gravel. Coal mining operations are carried out mainly in the Western Kentucky Coal Field and the Eastern Kentucky Coal field. As to nonfuel minerals, Mississippian limestones are mined in the Mississippian Plateaus Region and along Pine Mountain in southeastern Kentucky. Ordovician and Silurian limestones are mined from the central part of the state. Clay minerals that are mined in the state include common clay, ceramic and ball clays, refractory clay and shale. Just like in 2004, mining activities in the state remain significant.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00265187","usgsCitation":"Greb, S., and Anderson, W., 2006, State summaries: Kentucky: Mining Engineering, v. 58, no. 5, p. 92-95.","startPage":"92","endPage":"95","numberOfPages":"4","costCenters":[],"links":[{"id":239306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b96d6e4b08c986b31b73d","contributors":{"authors":[{"text":"Greb, S.F.","contributorId":48294,"corporation":false,"usgs":true,"family":"Greb","given":"S.F.","email":"","affiliations":[],"preferred":false,"id":427223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, W.H.","contributorId":93420,"corporation":false,"usgs":true,"family":"Anderson","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":427224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70030309,"text":"70030309 - 2006 - Character and distribution of exposed glaciodeltaic deposits off outer Cape Cod, Massachusetts, and their effects on hydrogeology and benthic habitats","interactions":[],"lastModifiedDate":"2017-08-23T11:11:06","indexId":"70030309","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Character and distribution of exposed glaciodeltaic deposits off outer Cape Cod, Massachusetts, and their effects on hydrogeology and benthic habitats","docAbstract":"Seabed outcrops of glaciodeltaic sediments were identified in four places east of Cape Cod, Massachusetts, during seismic-reflection, multibeam bathymetric and backscatter, bottom photographic, and sediment sampling surveys. These strata record coarser-grained ice-proximal glaciofluvial topset to finer-grained distal glaciolacustrine bottomset deposition within deltaic systems that prograded southwestward into glacial lakes from the South Channel lobe about 18 ka B.P. These beds are important because they (1) influence the outer Cape's hydrogeologic framework, and (2) constitute relatively stable, locally rough habitats within an area of seafloor dominated by mobile sand and gravelly sediment, and benefit the benthic fauna by providing shelter and a substrate amenable to burrow construction. ?? Springer-Verlag 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s00367-005-0015-x","issn":"02760460","usgsCitation":"Poppe, L., Foster, D., and Danforth, W.W., 2006, Character and distribution of exposed glaciodeltaic deposits off outer Cape Cod, Massachusetts, and their effects on hydrogeology and benthic habitats: Geo-Marine Letters, v. 26, no. 1, p. 51-57, https://doi.org/10.1007/s00367-005-0015-x.","productDescription":"7 p.","startPage":"51","endPage":"57","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":477520,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1912/1707","text":"External Repository"},{"id":239198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.3067626953125,\n 41.126952506008436\n ],\n [\n -69.71099853515624,\n 41.126952506008436\n ],\n [\n -69.71099853515624,\n 42.332153998913704\n ],\n [\n -71.3067626953125,\n 42.332153998913704\n ],\n [\n -71.3067626953125,\n 41.126952506008436\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"26","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-01-05","publicationStatus":"PW","scienceBaseUri":"5059f484e4b0c8380cd4bd7a","contributors":{"authors":[{"text":"Poppe, L.J.","contributorId":72782,"corporation":false,"usgs":true,"family":"Poppe","given":"L.J.","affiliations":[],"preferred":false,"id":426612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, D.S.","contributorId":30641,"corporation":false,"usgs":true,"family":"Foster","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":426611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Danforth, W. W.","contributorId":16386,"corporation":false,"usgs":true,"family":"Danforth","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":426610,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70030306,"text":"70030306 - 2006 - Status of soil acidification in North America","interactions":[],"lastModifiedDate":"2015-04-27T10:05:37","indexId":"70030306","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2296,"text":"Journal of Forest Science","active":true,"publicationSubtype":{"id":10}},"title":"Status of soil acidification in North America","docAbstract":"Forest soil acidification and depletion of nutrient cations have been reported for several forested regions in North America, predominantly in the eastern United States, including the northeast and in the central Appalachians, but also in parts of southeastern Canada and the southern U.S. Continuing regional inputs of nitrogen and sulfur are of concern because of leaching of base cations, increased availability of soil Al, and the accumulation and ultimate transmission of acidity from forest soils to streams. Losses of calcium from forest soils and forested watersheds have now been documented as a sensitive early indicator and a functionally significant response to acid deposition for a wide range of forest soils in North America. For red spruce, a clear link has been established between acidic deposition, alterations in calcium and aluminum supplies and increased sensitivity to winter injury. Cation depletion appears to contribute to sugar maple decline on some soils, specifically the high mortality rates observed in northern Pennsylvania over the last decade. While responses to liming have not been systematically examined in North America, in a study in Pennsylvania, restoring basic cations through liming increased basal area growth of sugar maple and levels of calcium and magnesium in soil and foliage. In the San Bernardino Mountains in southern California near the west coast, the pH of the A horizon has declined by at least 2 pH units (to pH 4.0-4.3) over the past 30 years, with no detrimental effects on bole growth; presumably, because of the Mediterranean climate, base cation pools are still high and not limiting for plant growth.
","language":"English, Slovak","issn":"12124834","usgsCitation":"Fenn, M., Huntington, T., Mclaughlin, S., Eagar, C., Gomez, A., and Cook, R., 2006, Status of soil acidification in North America: Journal of Forest Science, v. 52, no. Special Issue, p. 3-13.","productDescription":"11 p.","startPage":"3","endPage":"13","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":239164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"North America","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -125.859375,\n 15.453680224345835\n ],\n [\n -125.859375,\n 49.26780455063753\n ],\n [\n -66.62109375,\n 49.26780455063753\n ],\n [\n -66.62109375,\n 15.453680224345835\n ],\n [\n -125.859375,\n 15.453680224345835\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"52","issue":"Special Issue","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b97e5e4b08c986b31bcfd","contributors":{"authors":[{"text":"Fenn, M.E.","contributorId":68686,"corporation":false,"usgs":true,"family":"Fenn","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":426598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huntington, T.G. 0000-0002-9427-3530","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":64675,"corporation":false,"usgs":true,"family":"Huntington","given":"T.G.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":426597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mclaughlin, S.B.","contributorId":92051,"corporation":false,"usgs":true,"family":"Mclaughlin","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":426599,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eagar, C.","contributorId":99493,"corporation":false,"usgs":false,"family":"Eagar","given":"C.","affiliations":[],"preferred":false,"id":426600,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gomez, A.","contributorId":62017,"corporation":false,"usgs":true,"family":"Gomez","given":"A.","email":"","affiliations":[],"preferred":false,"id":426596,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cook, R.B.","contributorId":8480,"corporation":false,"usgs":true,"family":"Cook","given":"R.B.","affiliations":[],"preferred":false,"id":426595,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70030288,"text":"70030288 - 2006 - Distribution, 14C chronology, and paleomagnetism of latest Pleistocene and Holocene lava flows at Haleakala volcano, Island of Maui, Hawai'i: A revision of lava flow hazard zones","interactions":[],"lastModifiedDate":"2020-09-27T19:35:44.560922","indexId":"70030288","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Distribution, 14C chronology, and paleomagnetism of latest Pleistocene and Holocene lava flows at Haleakala volcano, Island of Maui, Hawai'i: A revision of lava flow hazard zones","docAbstract":"New mapping and 60 new radiocarbon ages define the age and distribution of latest Pleistocene and Holocene (past 13,000 years) lava flows at Haleakalā volcano, Island of Maui. Paleomagnetic directions were determined for 118 sites, of which 89 are in lava flows younger than 13,000 years. The paleomagnetic data, in conjunction with a reference paleosecular variation (PSV) curve for the Hawaiian Islands, are combined with our knowledge of age limitations based on stratigraphic control to refine age estimates for some of the undated lava flows. The resulting volumetric rate calculations indicate that within analytical error, the extrusion rate has remained nearly constant during the past 13,000 years, in the range 0.05–0.15 km3/kyr, only about half the long-term rate required to produce the postshield strata emplaced in the past ∼1 Myr. Haleakalā's eruptive frequency is similar to that of Hualālai volcano on the Island of Hawai‘i, but its lava flows cover substantially less area per unit time. The reduced rates of lava coverage indicate a lower volcanic hazard than in similar zones at Hualālai.
","language":"English","publisher":"Wiley","doi":"10.1029/2005JB003876","issn":"01480227","usgsCitation":"Sherrod, D.R., Hagstrum, J.T., McGeehin, J., Champion, D.E., and Trusdell, F., 2006, Distribution, 14C chronology, and paleomagnetism of latest Pleistocene and Holocene lava flows at Haleakala volcano, Island of Maui, Hawai'i: A revision of lava flow hazard zones: Journal of Geophysical Research B: Solid Earth, v. 111, no. 5, B0525, 24 p., https://doi.org/10.1029/2005JB003876.","productDescription":"B0525, 24 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":477577,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jb003876","text":"Publisher Index Page"},{"id":239438,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Haleakala volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.45355224609375,\n 20.576224710301645\n ],\n [\n -156.45355224609375,\n 20.870360925364178\n ],\n [\n -155.97564697265625,\n 20.870360925364178\n ],\n [\n -155.97564697265625,\n 20.576224710301645\n ],\n [\n -156.45355224609375,\n 20.576224710301645\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"111","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-05-31","publicationStatus":"PW","scienceBaseUri":"505a0318e4b0c8380cd50332","contributors":{"authors":[{"text":"Sherrod, David R. 0000-0001-9460-0434 dsherrod@usgs.gov","orcid":"https://orcid.org/0000-0001-9460-0434","contributorId":527,"corporation":false,"usgs":true,"family":"Sherrod","given":"David","email":"dsherrod@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":426527,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hagstrum, Jonathan T. 0000-0002-0689-280X jhag@usgs.gov","orcid":"https://orcid.org/0000-0002-0689-280X","contributorId":3474,"corporation":false,"usgs":true,"family":"Hagstrum","given":"Jonathan","email":"jhag@usgs.gov","middleInitial":"T.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":426531,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGeehin, John P. 0000-0002-5320-6091 mcgeehin@usgs.gov","orcid":"https://orcid.org/0000-0002-5320-6091","contributorId":3444,"corporation":false,"usgs":true,"family":"McGeehin","given":"John P.","email":"mcgeehin@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":426528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Champion, Duane E. 0000-0001-7854-9034 dchamp@usgs.gov","orcid":"https://orcid.org/0000-0001-7854-9034","contributorId":2912,"corporation":false,"usgs":true,"family":"Champion","given":"Duane","email":"dchamp@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":426530,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Trusdell, Frank A. 0000-0002-0681-0528 trusdell@usgs.gov","orcid":"https://orcid.org/0000-0002-0681-0528","contributorId":754,"corporation":false,"usgs":true,"family":"Trusdell","given":"Frank A.","email":"trusdell@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":426529,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70030283,"text":"70030283 - 2006 - Reversing storm hotspots on sandy beaches: Spatial and temporal characteristics","interactions":[],"lastModifiedDate":"2017-09-19T10:17:58","indexId":"70030283","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Reversing storm hotspots on sandy beaches: Spatial and temporal characteristics","docAbstract":"Coastal erosion hotspots are defined as sections of coast that exhibit significantly higher rates of erosion than adjacent areas. This paper describes the spatial and temporal characteristics of a recently identified type of coastal erosion hotspot, which forms in response to storms on uninterrupted sandy coasts largely free from human intervention. These are referred to here as reversing storm hotspots because the erosion is reversed by accretion of a similar magnitude to the storm-induced erosion. The accretion occurs within a few days or weeks of fair weather after the storm. Reversing storm hotspots observed here, on two US east coast beaches, have a longshore length averaging 3.86 km, a cross-shore excursion (magnitude of erosion or accretion) averaging 15.4 m, and a time scale of days to weeks associated with individual storm events. These spatial and temporal scales clearly distinguish reversing storm hotspots from previously described forms of longshore variability in erosion, including those attributed to several types of shoreline undulations and hotspots associated with long-term shoreline change.
","language":"English","publisher":"Elsevier","doi":"10.1016/j.margeo.2005.10.003","issn":"00253227","usgsCitation":"List, J.H., Farris, A., and Sullivan, C., 2006, Reversing storm hotspots on sandy beaches: Spatial and temporal characteristics: Marine Geology, v. 226, no. 3-4, p. 261-279, https://doi.org/10.1016/j.margeo.2005.10.003.","productDescription":"19 p.","startPage":"261","endPage":"279","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":239332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.5322265625,\n 41.46742831254425\n ],\n [\n -69.78515625,\n 41.46742831254425\n ],\n [\n -69.78515625,\n 42.220381783720605\n ],\n [\n -70.5322265625,\n 42.220381783720605\n ],\n [\n -70.5322265625,\n 41.46742831254425\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"226","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aac3be4b0c8380cd86c17","contributors":{"authors":[{"text":"List, J. H.","contributorId":70406,"corporation":false,"usgs":true,"family":"List","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":426474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farris, A.S.","contributorId":98477,"corporation":false,"usgs":true,"family":"Farris","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":426476,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sullivan, C.","contributorId":75959,"corporation":false,"usgs":true,"family":"Sullivan","given":"C.","affiliations":[],"preferred":false,"id":426475,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70030250,"text":"70030250 - 2006 - Carbon dioxide emissions from vegetation-kill zones around the resurgent dome of Long Valley caldera, eastern California, USA","interactions":[],"lastModifiedDate":"2019-03-25T10:27:06","indexId":"70030250","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Carbon dioxide emissions from vegetation-kill zones around the resurgent dome of Long Valley caldera, eastern California, USA","docAbstract":"A survey of diffuse CO2 efflux, soil temperature and soil-gas chemistry over areas of localized vegetation-kill on and around the resurgent dome of Long Valley caldera California was performed to evaluate the premise that gaseous and thermal anomalies are related to renewed intrusion of magma. Some kill sites are long-lived features and others have developed in the past few years. Total anomalous CO2 emissions from the thirteen areas average around 8.7 t per day; but the majority of the emissions come from four sites west of the Casa Diablo geothermal power plant. Geochemical analyses of the soil-gases from locations west and east of the plant revealed the presence of isobutane related to plant operations. The δ13C values of diffuse CO2 range from − 5.7‰ to − 3.4‰, similar to values previously reported for CO2 from hot springs and thermal wells around Long Valley.
At many of the vegetation-kill sites soil temperatures reach boiling at depths ≤ 20 cm. Soil temperature/depth profiles at two of the high-emissions areas indicate that the conductive thermal gradient in the center of the areas is around 320 °C m− 1. We estimate total heat loss from the two areas to be about 6.1 and 2.3 MW. Given current thinking on the rate of hydrothermal fluid flow across the caldera and using the CO2 concentration in the thermal fluids, the heat and CO2 loss from the kill areas is easily provided by the shallow hydrothermal system, which is sourced to the west of the resurgent dome. We find no evidence that the development of new areas of vegetation kill across the resurgent dome are related to new input of magma or magmatic fluids from beneath the resurgent dome. Our findings indicate that the areas have developed as a response to changes in the shallow hydrologic system. Some of the changes are likely related to fluid production at the power plant, but at distal sites the changes are more likely related to seismicity and uplift of the dome.
The Yellowstone caldera, in the western United States, formed ![\"approx\"](\"http://www.nature.com/__chars/math/special/sim/black/med/base/glyph.gif\")
640,000 years ago when an explosive eruption ejected 1,000 km3 of material1. It is the youngest of a series of large calderas that formed during sequential cataclysmic eruptions that began 16 million years ago in eastern Oregon and northern Nevada. The Yellowstone caldera was largely buried by rhyolite lava flows during eruptions that occurred from 150,000 to 70,000 years ago1. Since the last eruption, Yellowstone has remained restless, with high seismicity, continuing uplift/subsidence episodes with movements of 70 cm historically2 to several metres since the Pleistocene epoch3, and intense hydrothermal activity. Here we present observations of a new mode of surface deformation in Yellowstone, based on radar interferometry observations from the European Space Agency ERS-2 satellite. We infer that the observed pattern of uplift and subsidence results from variations in the movement of molten basalt into and out of the Yellowstone volcanic system.
","language":"English","publisher":"Macmillan Journals Ltd.","doi":"10.1038/nature04507","issn":"00280836","usgsCitation":"Wicks, C., Thatcher, W., Dzurisin, D., and Svarc, J., 2006, Uplift, thermal unrest and magma intrusion at Yellowstone caldera: Nature, v. 440, no. 7080, p. 72-75, https://doi.org/10.1038/nature04507.","productDescription":"4 p.","startPage":"72","endPage":"75","numberOfPages":"4","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":239435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.0882568359375,\n 44.25110134697976\n ],\n [\n -111.0882568359375,\n 45.01141864227728\n ],\n [\n -110.0775146484375,\n 45.01141864227728\n ],\n [\n -110.0775146484375,\n 44.25110134697976\n ],\n [\n -111.0882568359375,\n 44.25110134697976\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"440","issue":"7080","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbd2ae4b08c986b328ef9","contributors":{"authors":[{"text":"Wicks, Charles W.","contributorId":52048,"corporation":false,"usgs":true,"family":"Wicks","given":"Charles W.","affiliations":[],"preferred":false,"id":426189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thatcher, Wayne","contributorId":35325,"corporation":false,"usgs":true,"family":"Thatcher","given":"Wayne","affiliations":[],"preferred":false,"id":426190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":426191,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Svarc, Jerry","contributorId":82012,"corporation":false,"usgs":true,"family":"Svarc","given":"Jerry","affiliations":[],"preferred":false,"id":426192,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70035497,"text":"70035497 - 2006 - Application of carbonate cyclostratigraphy and borehole geophysics to delineate porosity and preferential flow in the karst limestone of the Biscayne aquifer, SE Florida","interactions":[],"lastModifiedDate":"2020-03-27T06:47:37","indexId":"70035497","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Application of carbonate cyclostratigraphy and borehole geophysics to delineate porosity and preferential flow in the karst limestone of the Biscayne aquifer, SE Florida","docAbstract":"Combined analyses of cores, borehole geophysical logs, and cyclostratigraphy produced a new conceptual hydrogeologic framework for the triple-porosity (matrix, touching-vug, and conduit porosity) karst limestone of the Biscayne aquifer in a 0.65 km2 study area, SE Florida. Vertical lithofacies successions, which have recurrent stacking patterns, fit within high-frequency cycles. We define three ideal high-frequency cycles as: (1) upward-shallowing subtidal cycles, (2) upward-shallowing paralic cycles, and (3) aggradational subtidal cycles. Digital optical borehole images, tracers, and flow meters indicate that there is a predictable vertical pattern of porosity and permeability within the three ideal cycles, because the distribution of porosity and permeability is related to lithofacies. Stratiform zones of high permeability commonly occur just above flooding surfaces in the lower part of upward-shallowing subtidal and paralic cycles, forming preferential groundwater flow zones. Aggradational subtidal cycles are either mostly high-permeability zones or leaky, low-permeability units. In the study area, groundwater flow within stratiform high-permeability zones is through a secondary pore system of touching-vug porosity principally related to molds of burrows and pelecypods and to interburrow vugs. Movement of a dye-tracer pulse observed using a borehole fluid-temperature tool during a conservative tracer test indicates heterogeneous permeability. Advective movement of the tracer appears to be most concentrated within a thin stratiform flow zone contained within the lower part of a high-frequency cycle, indicating a distinctly high relative permeability for this zone. Borehole flow-meter measurements corroborate the relatively high permeability of the flow zone. Identification and mapping of such high-permeability flow zones is crucial to conceptualization of karst groundwater flow within a cyclostratigraphic framework. Many karst aquifers are included in cyclic platform carbonates. Clearly, a cyclostratigraphic approach that translates carbonate aquifer heterogeneity into a consistent framework of correlative units will improve simulation of karst groundwater flow. ?? 2006 Geological Society of America.","language":"English","publisher":"Geological Society of America","doi":"10.1130/2006.2404(16)","issn":"00721077","usgsCitation":"Cunningham, K.J., Renken, R.A., Wacker, M.A., Zygnerski, M., Robinson, E., Shapiro, A.M., and Wingard, G.L., 2006, Application of carbonate cyclostratigraphy and borehole geophysics to delineate porosity and preferential flow in the karst limestone of the Biscayne aquifer, SE Florida: Special Paper of the Geological Society of America, no. 404, p. 191-208, https://doi.org/10.1130/2006.2404(16).","productDescription":"18 p.","startPage":"191","endPage":"208","numberOfPages":"18","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":244062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Southern Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.529296875,\n 24.84656534821976\n ],\n [\n -79.8046875,\n 24.84656534821976\n ],\n [\n -79.8046875,\n 27.254629577800063\n ],\n [\n -82.529296875,\n 27.254629577800063\n ],\n [\n -82.529296875,\n 24.84656534821976\n ]\n ]\n ]\n }\n }\n ]\n}","issue":"404","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec98e4b0c8380cd49380","contributors":{"authors":[{"text":"Cunningham, Kevin J. 0000-0002-2179-8686 kcunning@usgs.gov","orcid":"https://orcid.org/0000-0002-2179-8686","contributorId":1689,"corporation":false,"usgs":true,"family":"Cunningham","given":"Kevin","email":"kcunning@usgs.gov","middleInitial":"J.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":450932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Renken, Robert A. rarenken@usgs.gov","contributorId":269,"corporation":false,"usgs":true,"family":"Renken","given":"Robert","email":"rarenken@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":450938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wacker, Michael A. mwacker@usgs.gov","contributorId":2162,"corporation":false,"usgs":true,"family":"Wacker","given":"Michael","email":"mwacker@usgs.gov","middleInitial":"A.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":450937,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zygnerski, M.R.","contributorId":45109,"corporation":false,"usgs":true,"family":"Zygnerski","given":"M.R.","affiliations":[],"preferred":false,"id":450933,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Robinson, E.","contributorId":73847,"corporation":false,"usgs":true,"family":"Robinson","given":"E.","email":"","affiliations":[],"preferred":false,"id":450934,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shapiro, Allen M. 0000-0002-6425-9607 ashapiro@usgs.gov","orcid":"https://orcid.org/0000-0002-6425-9607","contributorId":2164,"corporation":false,"usgs":true,"family":"Shapiro","given":"Allen","email":"ashapiro@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":450936,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wingard, G. Lynn 0000-0002-3833-5207 lwingard@usgs.gov","orcid":"https://orcid.org/0000-0002-3833-5207","contributorId":605,"corporation":false,"usgs":true,"family":"Wingard","given":"G.","email":"lwingard@usgs.gov","middleInitial":"Lynn","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":450935,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70033635,"text":"70033635 - 2006 - Containing arsenic-enriched groundwater tracing lead isotopic compositions of common arsenical pesticides in a coastal Maine watershed","interactions":[],"lastModifiedDate":"2018-10-18T12:23:03","indexId":"70033635","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Containing arsenic-enriched groundwater tracing lead isotopic compositions of common arsenical pesticides in a coastal Maine watershed","docAbstract":"Arsenical pesticides and herbicides were extensively used on apple, blueberry, and potato crops in New England during the first half of the twentieth century. Lead arsenate was the most heavily used arsenical pesticide until it was officially banned. Lead arsenate, calcium arsenate, and sodium arsenate have similar Pb isotope compositions: 208Pb207Pb = 2.3839-2.4722, and 206Pb207Pb = 1.1035-1.2010. Other arsenical pesticides such as copper acetoarsenite (Paris green), methyl arsonic acid and methane arsonic acid, as well as arsanilic acid are widely variable in isotope composition. Although a complete understanding of the effects of historical use of arsenical pesticides is not available, initial studies indicate that arsenic and lead concentrations in stream sediments in New England are higher in agricultural areas that intensely used arsenical pesticides than in other areas. The Pb isotope compositions of pesticides partially overlap values of stream sediments from areas with the most extensive agricultural use. The lingering effects of arsenical pesticide use were tested in a detailed geochemical and isotopic study of soil profiles from a watershed containing arsenic-enriched ground water in coastal Maine. Acid-leach compositions of the soils represent lead adsorbed to mineral surfaces or held in soluble minerals (Fe- and Mn-hydroxides, carbonate, and some micaceous minerals), whereas residue compositions likely reflect bedrock compositions. The soil profiles contain labile Pb (acid-leach) showing a moderate range in 206Pb 207Pb (1.1870-1.2069), and 208Pb207Pb (2.4519-2.4876). Isotope values vary as a function of depth: the lowest Pb isotope ratios (e.g.,208Pb206Pb) representing labile lead are in the uppermost soil horizons. Lead contents decrease with depth in the soil profiles. Arsenic contents show no clear trend with depth. A multi-component mixing scheme that included lead from the local parent rock (Penobscot Formation), lead derived from combustion of fossil fuels, and possibly lead from other anthropogenic sources (e.g., pesticides), could account for Pb isotope variations in the soil profiles. In agricultural regions, our preliminary data show that the extensive use of arsenical pesticides and herbicides can be a significant anthropogenic source of arsenic and lead to stream sediments and soils.
","largerWorkTitle":"Association for Environmental Health and Sciences - 21st Annual International Conference on Contaminated Soils, Sediments and Water ","conferenceTitle":"21st Annual International Conference on Contaminated Soils, Sediments and Water 2005","conferenceDate":"17 October 2005 through 20 October 2005","conferenceLocation":"Amherst, MA","language":"English","isbn":"9781604239522","usgsCitation":"Ayuso, R.A., Foley, N.K., Robinson, G.R., Colvin, A., Lipfert, G., and Reeve, A., 2006, Containing arsenic-enriched groundwater tracing lead isotopic compositions of common arsenical pesticides in a coastal Maine watershed, in Association for Environmental Health and Sciences - 21st Annual International Conference on Contaminated Soils, Sediments and Water , v. 11, Amherst, MA, 17 October 2005 through 20 October 2005, p. 64-92.","productDescription":"29 p.","startPage":"64","endPage":"92","numberOfPages":"29","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":242025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.69775390625,\n 45.72152152227954\n ],\n [\n -66.7529296875,\n 44.86365630540611\n ],\n [\n -70.697021484375,\n 43.004647127794435\n ],\n [\n -71.3671875,\n 43.83452678223684\n ],\n [\n -67.69775390625,\n 45.72152152227954\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fa2de4b0c8380cd4d986","contributors":{"authors":[{"text":"Ayuso, Robert A. 0000-0002-8496-9534 rayuso@usgs.gov","orcid":"https://orcid.org/0000-0002-8496-9534","contributorId":2654,"corporation":false,"usgs":true,"family":"Ayuso","given":"Robert","email":"rayuso@usgs.gov","middleInitial":"A.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":441783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foley, Nora K. 0000-0003-0124-3509 nfoley@usgs.gov","orcid":"https://orcid.org/0000-0003-0124-3509","contributorId":4010,"corporation":false,"usgs":true,"family":"Foley","given":"Nora","email":"nfoley@usgs.gov","middleInitial":"K.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":441781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, Glipin R. Jr.","contributorId":59336,"corporation":false,"usgs":true,"family":"Robinson","given":"Glipin","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":441780,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Colvin, A.S.","contributorId":11426,"corporation":false,"usgs":true,"family":"Colvin","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":441782,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lipfert, G.","contributorId":53135,"corporation":false,"usgs":true,"family":"Lipfert","given":"G.","email":"","affiliations":[],"preferred":false,"id":441784,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Reeve, A.S.","contributorId":64446,"corporation":false,"usgs":true,"family":"Reeve","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":441785,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70028069,"text":"70028069 - 2006 - A search for scale in sea-level studies","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70028069","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"A search for scale in sea-level studies","docAbstract":"Many researchers assume a proportional relationship among the atmospheric CO2 concentration, temperature, and sea level. Thus, the rate of sea-level rise should increase in concert with the documented exponential increase in CO2. Although sea surface temperature has increased in places over the past century and short-term sea level rose abruptly during the 1990s, it is difficult to demonstrate a proportional relationship using existing geologic or historic records. Tide gauge records in the United States cover too short a time interval to verify acceleration in the rate of sea-level rise, although multicentury tide gauge and staff records from the Netherlands and Sweden suggest a mid-19th-century acceleration in sea-level rise. Reconstructions of sea-level changes for the past 1000 years derived using benthic foraminifer data from salt marshes along the East Coast of the United States suggest an increased rate of relative sea-level rise beginning in the 1600s. Geologic records of relative sea-level rise for the past 6000 years are available for several sites along the US East Coast from 14C-dated basal peat below salt marshes and estuarine sediments. When these three scales of sea-level variation are integrated, adjusted for postglacial isostatic movement, and replotted, the range of variation in sea level suggested by basal peat ages is within ??1 meter of the long-term trend. The reconstruction from Long Island Sound data shows a linear rise in sea level beginning in the mid-1600s at a rate consistent with the historic record of mean high water. Long-term tide gauge records from Europe and North America show similar trends since the mid-19th century. There is no clear proportional exponential increase in the rate of sea-level rise. If proportionality exists among sea level, atmospheric CO2, and temperature, there may be a significant time lag before an anthropogenic increase in the rate of sea-level rise occurs.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Coastal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2112/03-0123.1","issn":"07490208","usgsCitation":"Larsen, C., and Clark, I., 2006, A search for scale in sea-level studies: Journal of Coastal Research, v. 22, no. 4, p. 788-800, https://doi.org/10.2112/03-0123.1.","startPage":"788","endPage":"800","numberOfPages":"13","costCenters":[],"links":[{"id":477363,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2112/03-0123.1","text":"Publisher Index Page"},{"id":210362,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2112/03-0123.1"},{"id":237258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e57be4b0c8380cd46d71","contributors":{"authors":[{"text":"Larsen, C.E.","contributorId":84518,"corporation":false,"usgs":true,"family":"Larsen","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":416401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, I.","contributorId":38766,"corporation":false,"usgs":true,"family":"Clark","given":"I.","email":"","affiliations":[],"preferred":false,"id":416400,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028102,"text":"70028102 - 2006 - Can hunting of translocated nuisance Canada geese reduce local conflicts?","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70028102","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Can hunting of translocated nuisance Canada geese reduce local conflicts?","docAbstract":"Resident Canada geese (Branta canadensis) nest or reside in the temperate latitudes of North America. In past years, translocation-the capture and subsequent release of geese at distant locations-has been used to establish resident goose populations and to reduce nuisance problems. However, with new special hunting seasons designed to target resident Canada geese, we can now evaluate translocation as a management tool when hunting is allowed at release sites. We selected 2 study sites, representative of urban and suburban locations with nuisance resident geese, in central and western New York, USA. In June 2003, we translocated 80 neck-banded adult geese, 14 radiomarked adult females, and 83 juveniles 150 km east and southwest from urban and suburban problem sites in western New York to state-owned Wildlife Management Areas. At these same capture sites, we used 151 neck-banded adult geese, 12 radiomarked females, and 100 juveniles as controls to compare dispersal movements and harvest vulnerability to translocated geese. All observations (n = 45) of translocated radiomarked geese were <20 km from release sites, in areas where hunting was permitted. Only 25 of 538 observations (4.6%) of radiomarked geese at control sites were in areas open to hunting. The remainder of observations occurred at nonhunting locations within 10 km of control sites. More translocated adult geese (23.8%) were harvested than control geese (6.6%; ??2 = 72.98, P = 0.0009). More translocated juvenile geese were harvested (22.9%) than juvenile controls (5.0%; ??2 = 72.30, P = 0.0005). Only 7 (8.8%) translocated adult geese returned to the original capture sites during Canada goose hunting seasons. Translocation of adult and juvenile geese in family groups may alleviate nuisance problems at conflict sites through increased harvest, reducing the number of birds returning in subsequent years.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/0091-7648(2006)34[845:CHOTNC]2.0.CO;2","issn":"00917648","usgsCitation":"Holevinski, R., Malecki, R., and Curtis, P.D., 2006, Can hunting of translocated nuisance Canada geese reduce local conflicts?: Wildlife Society Bulletin, v. 34, no. 3, p. 845-849, https://doi.org/10.2193/0091-7648(2006)34[845:CHOTNC]2.0.CO;2.","startPage":"845","endPage":"849","numberOfPages":"5","costCenters":[],"links":[{"id":210334,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0091-7648(2006)34[845:CHOTNC]2.0.CO;2"},{"id":237225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f334e4b0c8380cd4b66e","contributors":{"authors":[{"text":"Holevinski, R.A.","contributorId":62399,"corporation":false,"usgs":true,"family":"Holevinski","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":416545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malecki, R.A.","contributorId":70498,"corporation":false,"usgs":true,"family":"Malecki","given":"R.A.","affiliations":[],"preferred":false,"id":416546,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtis, Paul D.","contributorId":83633,"corporation":false,"usgs":true,"family":"Curtis","given":"Paul","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":416547,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031176,"text":"70031176 - 2006 - Lake Sturgeon, Acipenser fulvescens, movements in Rainy Lake, Minnesota and Ontario","interactions":[],"lastModifiedDate":"2021-05-06T21:45:01.845269","indexId":"70031176","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1163,"text":"Canadian Field-Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Lake Sturgeon, Acipenser fulvescens, movements in Rainy Lake, Minnesota and Ontario","docAbstract":"Rainy Lake, Minnesota-Ontario, contains a native population of Lake Sturgeon (Acipenser fulvescens) that has gone largely unstudied. The objective of this descriptive study was to summarize generalized Lake Sturgeon movement patterns through the use of biotelemetry. Telemetry data reinforced the high utilization of the Squirrel Falls geographic location by Lake Sturgeon, with 37% of the re-locations occurring in that area. Other spring aggregations occurred in areas associated with Kettle Falls, the Pipestone River, and the Rat River, which could indicate spawning activity. Movement of Lake Sturgeon between the Seine River and the South Arm of Rainy Lake indicates the likelihood of one integrated population on the east end of the South Arm. The lack of re-locations in the Seine River during the months of September and October may have been due to Lake Sturgeon moving into deeper water areas of the Seine River and out of the range of radio telemetry gear or simply moving back into the South Arm. Due to the movements between Minnesota and Ontario, coordination of management efforts among provincial, state, and federal agencies will be important.
","language":"English","publisher":"Canadian Field-Naturalist","doi":"10.22621/cfn.v120i1.249","issn":"00083550","usgsCitation":"Adams, W., Kallemeyn, L., and Willis, D., 2006, Lake Sturgeon, Acipenser fulvescens, movements in Rainy Lake, Minnesota and Ontario: Canadian Field-Naturalist, v. 120, no. 1, p. 71-82, https://doi.org/10.22621/cfn.v120i1.249.","productDescription":"12 p.","startPage":"71","endPage":"82","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":486990,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.22621/cfn.v120i1.249","text":"Publisher Index Page"},{"id":385519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Rainy Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.7957763671875,\n 48.17707562779612\n ],\n [\n -93.40576171875,\n 48.17707562779612\n ],\n [\n -93.40576171875,\n 48.50204750525715\n ],\n [\n -93.7957763671875,\n 48.50204750525715\n ],\n [\n -93.7957763671875,\n 48.17707562779612\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"120","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-01-01","publicationStatus":"PW","scienceBaseUri":"505a4154e4b0c8380cd65495","contributors":{"authors":[{"text":"Adams, W.E. Jr.","contributorId":23489,"corporation":false,"usgs":true,"family":"Adams","given":"W.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":430370,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kallemeyn, L.W.","contributorId":44864,"corporation":false,"usgs":true,"family":"Kallemeyn","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":430371,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willis, D.W.","contributorId":56179,"corporation":false,"usgs":true,"family":"Willis","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":430372,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031149,"text":"70031149 - 2006 - Variability in supply and cross-shelf transport of pink shrimp (Farfantepenaeus duorarum) postlarvae into western Florida Bay","interactions":[],"lastModifiedDate":"2016-03-30T13:48:43","indexId":"70031149","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Variability in supply and cross-shelf transport of pink shrimp (Farfantepenaeus duorarum) postlarvae into western Florida Bay","docAbstract":"The variability in the supply of pink shrimp (Farfantepenaeus duorarum) postlarvae and the transport mechanisms of planktonic stages were investigated with field data and simulations of transport. Postlarvae entering the nursery grounds of Florida Bay were collected for three consecutive years at channels that connect the Bay with the Gulf of Mexico, and in channels of the Middle Florida Keys that connect the southeastern margin of the Bay with the Atlantic Ocean. The influx of postlarvae in the Middle Florida Keys was low in magnitude and varied seasonally and among years. In contrast, the greater postlarval influx occurred at the northwestern border of the Bay, where there was a strong seasonal pattern with peaks in influx from July through September each year. Planktonic stages need to travel up to 150 km eastward between spawning grounds (northeast of Dry Tortugas) and nursery grounds (western Florida Bay) in about 30 days, the estimated time of planktonic development for this species. A Lagrangian trajectory model was developed to estimate the drift of planktonic stages across the SW Florida shelf. The model simulated the maximal distance traveled by planktonic stages under various assumptions of behavior. Simulation results indicated that larvae traveling with the instantaneous current and exhibiting a diel behavior travel up to 65 km and 75% of the larvae travel only 30 km. However, the eastward distance traveled increased substantially when a larval response to tides was added to the behavioral variable (distance increased to 200 km and 85% of larvae traveled 150 km). The question is, when during larval development, and where on the shallow SW Florida shelf, does the tidal response become incorporated into the behavior of pink shrimp.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","issn":"00900656","usgsCitation":"Criales, M.M., Wang, J.D., Browder, J.A., Robblee, M.B., Jackson, T.L., and Hittle, C.D., 2006, Variability in supply and cross-shelf transport of pink shrimp (Farfantepenaeus duorarum) postlarvae into western Florida Bay: Fishery Bulletin, v. 104, no. 1, p. 60-74.","productDescription":"15 p.","startPage":"60","endPage":"74","numberOfPages":"15","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":238947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":319626,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://fishbull.noaa.gov/1041/1041toc.htm"}],"country":"United States","state":"Florida","otherGeospatial":"Dry Tortugas, Florida Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.91455078125,\n 25.94816628853973\n ],\n [\n -79.9200439453125,\n 25.54244147012483\n ],\n [\n -80.2166748046875,\n 25.04081549894912\n ],\n [\n -80.8648681640625,\n 24.56211235799689\n ],\n [\n -81.5789794921875,\n 24.412140070651528\n ],\n [\n -82.6336669921875,\n 24.382124181118236\n ],\n [\n -83.07861328125,\n 24.45215015618098\n ],\n [\n -83.1060791015625,\n 24.696934226366672\n ],\n [\n -82.5787353515625,\n 24.806681353851964\n ],\n [\n -81.3262939453125,\n 24.926294766395593\n ],\n [\n -80.760498046875,\n 25.224820176765036\n ],\n [\n -80.4364013671875,\n 25.606855993715016\n ],\n [\n -80.343017578125,\n 25.849336891707605\n ],\n [\n -80.2056884765625,\n 25.93828707492375\n ],\n [\n -80.04638671875,\n 25.96792222903405\n ],\n [\n -79.91455078125,\n 25.94816628853973\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"104","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc12fe4b08c986b32a492","contributors":{"authors":[{"text":"Criales, Maria M.","contributorId":69330,"corporation":false,"usgs":false,"family":"Criales","given":"Maria","email":"","middleInitial":"M.","affiliations":[{"id":12565,"text":"Rosenstiel School of Atomospheric Science, University of Miami","active":true,"usgs":false}],"preferred":false,"id":430260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wang, John D.","contributorId":75224,"corporation":false,"usgs":true,"family":"Wang","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":430261,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Browder, Joan A.","contributorId":7439,"corporation":false,"usgs":true,"family":"Browder","given":"Joan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":430257,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robblee, Michael B. mike_robblee@usgs.gov","contributorId":3865,"corporation":false,"usgs":true,"family":"Robblee","given":"Michael","email":"mike_robblee@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":430258,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jackson, Thomas L.","contributorId":93667,"corporation":false,"usgs":true,"family":"Jackson","given":"Thomas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":430262,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hittle, Clinton D. cdhittle@usgs.gov","contributorId":2436,"corporation":false,"usgs":true,"family":"Hittle","given":"Clinton","email":"cdhittle@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":430259,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70028320,"text":"70028320 - 2006 - Flow-specific trends in river-water quality resulting from the effects of the clean air act in three mesoscale, forested river basins in the northeastern United States through 2002","interactions":[],"lastModifiedDate":"2012-03-12T17:20:44","indexId":"70028320","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"Flow-specific trends in river-water quality resulting from the effects of the clean air act in three mesoscale, forested river basins in the northeastern United States through 2002","docAbstract":"Two new methods for assessing temporal trends in stream-solute concentrations at specific streamflow ranges were applied to long (40 to 50-year) but sparse (bi-weekly to quarterly sampling) stream-water quality data collected at three forested mesoscale basins along an atmospheric deposition gradient in the northeastern United States (one in north-central Pennsylvania, one in southeastern New York, and one in eastern Maine). The three data sets span the period since the implementation of the Clean Air Act in 1970 and its subsequent amendments. Declining sulfate (SO2-4) trends since the mid 1960s were identified for all 3 rivers by one or more of the 4 methods of trend detection used. Flow-specific trends were assessed by segmenting the data sets into 3-year and 6-year blocks, then determining concentration-discharge relationships for each block. Declining sulfate (SO2-4) trends at median flow were similar to trends determined using a Seasonal Kendall Tau test and Sen slope estimator. The trend of declining SO2-4 concentrations differed at high, median and low flow since the mid 1980s at YWC and NR, and at high and low flow at WR, but the trends leveled or reversed at high flow from 1999 through 2002. Trends for the period of record at high flows were similar to medium- and low-flow trends for Ca2+ + Mg2+ concentrations at WR, non-significant at YWC, and were more negative at low flow than at high flow at NR; trends in nitrate (NO-3), and alkalinity (ALK) concentrations were different at different flow conditions, and in ways that are consistent with the hydrology and deposition history at each watershed. Quarterly sampling is adequate for assessing average-flow trends in the chemical parameters assessed over long time periods (???decades). However, with even a modest effort at sampling a range of flow conditions within each year, trends at specified flows for constituents with strong concentration-discharge relationships can be evaluated and may allow early detection of ecosystem response to climate change and pollution management strategies. ?? Springer Science+Business Media, B.V. 2006.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Monitoring and Assessment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10661-005-9028-1","issn":"01676369","usgsCitation":"Murdoch, P., and Shanley, J.B., 2006, Flow-specific trends in river-water quality resulting from the effects of the clean air act in three mesoscale, forested river basins in the northeastern United States through 2002: Environmental Monitoring and Assessment, v. 120, no. 1-3, p. 1-25, https://doi.org/10.1007/s10661-005-9028-1.","startPage":"1","endPage":"25","numberOfPages":"25","costCenters":[],"links":[{"id":236922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210103,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10661-005-9028-1"}],"volume":"120","issue":"1-3","noUsgsAuthors":false,"publicationDate":"2006-08-01","publicationStatus":"PW","scienceBaseUri":"505a125de4b0c8380cd5429a","contributors":{"authors":[{"text":"Murdoch, Peter S.","contributorId":73547,"corporation":false,"usgs":true,"family":"Murdoch","given":"Peter S.","affiliations":[],"preferred":false,"id":417520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":417519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175210,"text":"wdrNY053 - 2006 - Water resources data New York water year 2005, volume 3: Western New York","interactions":[],"lastModifiedDate":"2017-04-06T11:03:56","indexId":"wdrNY053","displayToPublicDate":"2005-11-06T09:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-05-3","title":"Water resources data New York water year 2005, volume 3: Western New York","docAbstract":"Water resources data for the 2005 water year for Western New York consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; ground-water levels and water quality; and quantity and chemical quality of precipitation. This volume contains records for water discharge at 71 gaging stations; stage only at 15 gaging stations; stage and contents at 6 gaging stations; water quality at 12 gaging stations, 29 wells, and 22 partial-record stations; water levels at 29 observation wells; daily precipitation totals at 1 site, and chemical quality of precipitation at 1 site. Also included are data for 38 crest-stage partial-record stations. Locations of these sites are shown on figure 1. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as measurements made at miscellaneous sites. Surface-water, ground-water, and water-quality data at all sites are listed in Eastern Standard Time (EST), unless otherwise noted. These data together with the data in Volumes 1 and 2 represent that part of the National Water Information System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in New York.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY053","collaboration":"Prepared in cooperation with the State of New York and other agencies","usgsCitation":"Szabo, C.O., Grover, J.S., and McInnes, S., 2006, Water resources data New York water year 2005, volume 3: Western New York: U.S. Geological Survey Water Data Report NY-05-3, Summary: 12 p.; Data: v, 454 p.; Discontinued Sites: 9 p., https://doi.org/10.3133/wdrNY053.","productDescription":"Summary: 12 p.; Data: v, 454 p.; Discontinued Sites: 9 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":325988,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":325990,"rank":3,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ny-05-3/ithaca_annualrpt2005.pdf","text":"Surface-water, Water-quality, and Ground-water Data","size":"13.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WDR NY-05-3"},{"id":325989,"rank":2,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ny-05-3/ithaca_rept.sum05.pdf","text":"Summary of Hydrologic Conditions","size":"309 KB","linkFileType":{"id":1,"text":"pdf"},"description":"WDR NY-05-3"},{"id":325991,"rank":4,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ny-05-3/ithaca_disc05.pdf","text":"Discontinued Sites","size":"32.6 KB","linkFileType":{"id":1,"text":"pdf"},"description":"WDR NY-05-3"}],"country":"United States","state":"New York","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.11328125,\n 43.929549935614595\n ],\n [\n -76.31103515625,\n 43.866218006556394\n ],\n [\n -76.234130859375,\n 43.77109381775651\n ],\n [\n -76.212158203125,\n 43.628123412124616\n ],\n [\n -76.2451171875,\n 43.55651037504758\n ],\n [\n -76.37695312499999,\n 43.54854811091288\n ],\n [\n -76.552734375,\n 43.476840397778915\n ],\n [\n -76.739501953125,\n 43.36512572875844\n ],\n [\n -76.937255859375,\n 43.30119623257966\n ],\n [\n -77.135009765625,\n 43.28520334369384\n ],\n [\n -77.49755859375,\n 43.26120612479979\n ],\n [\n -77.640380859375,\n 43.30919109985686\n ],\n [\n -77.838134765625,\n 43.33316939281735\n ],\n [\n -78.0908203125,\n 43.381097587278596\n ],\n [\n -78.431396484375,\n 43.381097587278596\n ],\n [\n -78.64013671875,\n 43.35713822211053\n ],\n [\n -78.98071289062499,\n 43.32517767999296\n ],\n [\n -79.068603515625,\n 43.25320494908846\n ],\n [\n -79.07958984375,\n 43.141078106345844\n ],\n [\n -79.03564453124999,\n 43.04480541304369\n ],\n [\n -79.013671875,\n 42.956422511073335\n ],\n [\n -78.958740234375,\n 42.91620643817353\n ],\n [\n -78.92578124999999,\n 42.85985981506279\n ],\n [\n -79.03564453124999,\n 42.73894375124379\n ],\n [\n -79.244384765625,\n 42.5611728553181\n ],\n [\n -79.4970703125,\n 42.407234661551875\n ],\n [\n -79.62890625,\n 42.342305278572816\n ],\n [\n -79.8046875,\n 42.261049162113856\n ],\n [\n -79.73876953125,\n 42.00848901572399\n ],\n [\n -75.35522460937499,\n 42.032974332441405\n ],\n [\n -75.4541015625,\n 42.13896840458089\n ],\n [\n -75.43212890625,\n 42.36666166373274\n ],\n [\n -75.333251953125,\n 42.65820178455667\n ],\n [\n -75.2783203125,\n 42.83569550641454\n ],\n [\n -75.223388671875,\n 43.13306116240612\n ],\n [\n -75.465087890625,\n 43.42898792344157\n ],\n [\n -75.750732421875,\n 43.691707903073805\n ],\n [\n -76.00341796875,\n 43.84245116699036\n ],\n [\n -76.11328125,\n 43.929549935614595\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Director, New York Water Science Center
U.S. Geological Survey
425 Jordan Rd
Troy, NY 12180
(518) 285-5695
http://ny.water.usgs.gov/
","tableOfContents":"- Summary of Hydrologic Conditions
- Surface-water, Water-quality, and Ground-water Data
- Discontinued Sites
","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b71e4b03bcb0104bcb3","contributors":{"authors":[{"text":"Szabo, Carolyn O. cszabo@usgs.gov","contributorId":2840,"corporation":false,"usgs":true,"family":"Szabo","given":"Carolyn","email":"cszabo@usgs.gov","middleInitial":"O.","affiliations":[],"preferred":true,"id":644485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grover, Jason S.","contributorId":112193,"corporation":false,"usgs":true,"family":"Grover","given":"Jason","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":644486,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McInnes, S.K.","contributorId":10093,"corporation":false,"usgs":true,"family":"McInnes","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":644487,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70440,"text":"sir20045143 - 2006 - Evaluation of metal loading to streams near Creede, Colorado, August and September 2000","interactions":[],"lastModifiedDate":"2020-01-26T11:13:33","indexId":"sir20045143","displayToPublicDate":"2005-04-22T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5143","title":"Evaluation of metal loading to streams near Creede, Colorado, August and September 2000","docAbstract":"Decisions about remediation of mine drainage on the watershed scale require an understanding of metal contributions from all sources to be able to choose the best sites for remediation. A hydrologic framework to study metal loading in the Willow Creek watershed, a tributary to the Rio Grande River, was established by conducting a series of tracer-injection studies. Each study used the tracer-dilution method in conjunction with synoptic sampling to determine the spatial distribution of discharge and concentration. Discharge and concentration data were then used to develop mass-loading curves for the metals of interest. The discharge and load profiles (1) identify the principal sources of load to the streams; (2) demonstrate the scale of unsampled, dispersed subsurface inflows; and (3) estimate the amount of natural attenuation. The greatest source of metal loads was from the Nelson Tunnel on West Willow Creek, which contributed 158 kilograms per day of zinc to the stream. Additional loading from other dispersed, subsurface inflows along West Willow Creek added substantial loads, but these were small in comparison to the loads from the Nelson Tunnel. No significant contributions of metal load from potential sources occurred along East Willow Creek. The lack of measurable loading may be a result of previous remedial actions along that stream. The lower Willow Creek section had relatively small contributions of load compared to what had been contributed upstream. This watershed approach provides a detailed snapshot of metal load for the watershed to support remediation decisions and quantifies processes that affect metal transport.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20045143","collaboration":"Prepared in cooperation with the City of Creede, Colorado and the U.S. Forest Service","usgsCitation":"Kimball, B.A., Runkel, R., Walton-Day, K., and Stover, B., 2006, Evaluation of metal loading to streams near Creede, Colorado, August and September 2000 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5143, viii, 64 p., https://doi.org/10.3133/sir20045143.","productDescription":"viii, 64 p.","numberOfPages":"75","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2000-08-01","temporalEnd":"2000-09-30","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":185498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334251,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2004/5143/PDF/SIR2004_5143.pdf"},{"id":6989,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5143/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Creede","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.95,37.81666666666667 ], [ -106.95,37.916666666666664 ], [ -106.9,37.916666666666664 ], [ -106.9,37.81666666666667 ], [ -106.95,37.81666666666667 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafd5","contributors":{"authors":[{"text":"Kimball, B. A.","contributorId":87583,"corporation":false,"usgs":false,"family":"Kimball","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runkel, R.L.","contributorId":97529,"corporation":false,"usgs":true,"family":"Runkel","given":"R.L.","affiliations":[],"preferred":false,"id":282438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walton-Day, K.","contributorId":14054,"corporation":false,"usgs":true,"family":"Walton-Day","given":"K.","affiliations":[],"preferred":false,"id":282435,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stover, B.K.","contributorId":67975,"corporation":false,"usgs":true,"family":"Stover","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":282436,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":77495,"text":"i2614 - 2006 - Geologic map of the middle east rift geothermal subzone, Kīlauea Volcano, Hawaiʻi","interactions":[],"lastModifiedDate":"2021-09-01T21:34:34.293919","indexId":"i2614","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2614","title":"Geologic map of the middle east rift geothermal subzone, Kīlauea Volcano, Hawaiʻi","docAbstract":"Kīlauea is an active shield volcano in the southeastern part of the Island of Hawai'i. The middle east rift zone (MERZ) map includes about 27 square kilometers of the MERZ and shows the distribution of the products of 37 separate eruptions during late Holocene time. Lava flows erupted during 1983-96 have reached the mapped area. The subaerial part of the MERZ is 3-4 km wide and about 18 km long. It is a constructional ridge, 50-150 m above the adjoining terrain, marked by low spatter ramparts and cones as high as 60 m. Lava typically flowed either northeast or southeast, depending on vent location relative to the topographic crest of the rift zone. The MERZ receives more than 100 in. of rainfall annually and is covered by tropical rain forest. Vegetation begins to grow on lava a few months after its eruption. Relative heights of trees can be a guide to relative ages of underlying lava flows, but proximity to faults, presence of easily weathered cinders, and human activity also affect the rate of growth. The rocks have been grouped into five basic age groups. The framework for the ages assigned is provided by eight radiocarbon ages from previous mapping by the authors and a single date from the current mapping effort. The numerical ages are supplemented by observations of stratigraphic relations, degree of weathering, soil development, and vegetative cover.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2614","isbn":"9781411306592","usgsCitation":"Trusdell, F., and Moore, R.B., 2006, Geologic map of the middle east rift geothermal subzone, Kīlauea Volcano, Hawaiʻi (Version 1.0): U.S. Geological Survey IMAP 2614, 1 Map, 34.17 × 26.40 inches, https://doi.org/10.3133/i2614.","productDescription":"1 Map, 34.17 × 26.40 inches","additionalOnlineFiles":"Y","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":110687,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78353.htm","linkFileType":{"id":5,"text":"html"},"description":"78353"},{"id":8825,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/2614/","linkFileType":{"id":5,"text":"html"}},{"id":191248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i2614.PNG"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.0670,19.4071 ], [ -155.0670,19.4634 ], [ -154.9965,19.4634 ], [ -154.9965,19.4071 ], [ -155.0670,19.4071 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a84b5","contributors":{"authors":[{"text":"Trusdell, Frank A. 0000-0002-0681-0528 trusdell@usgs.gov","orcid":"https://orcid.org/0000-0002-0681-0528","contributorId":754,"corporation":false,"usgs":true,"family":"Trusdell","given":"Frank A.","email":"trusdell@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":288609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Richard B. rmoore@usgs.gov","contributorId":1464,"corporation":false,"usgs":true,"family":"Moore","given":"Richard","email":"rmoore@usgs.gov","middleInitial":"B.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288610,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":75383,"text":"ofr20051381 - 2005 - Pilot inventory of mammals, reptiles, and amphibians, Golden Gate National Recreation Area, California, 1990-1997","interactions":[],"lastModifiedDate":"2021-08-20T14:54:19.615992","indexId":"ofr20051381","displayToPublicDate":"2021-08-20T09:35:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1381","displayTitle":"Pilot Inventory of Mammals, Reptiles, and Amphibians, Golden Gate National Recreation Area, California, 1990-1997","title":"Pilot inventory of mammals, reptiles, and amphibians, Golden Gate National Recreation Area, California, 1990-1997","docAbstract":"The United States Geological Survey Golden Gate Field Station conducted a baseline inventory of terrestrial vertebrates within the Golden Gate National Recreation Area (GGNRA), Marin, San Francisco, and San Mateo Counties, California between 1990 and 1997. We established 456 permanent study plots in 6 major park habitats, including grassland, coastal scrub, riparian woodland, coastal wetland, broad-leaved evergreen forest, and needle-leaved evergreen forest.\r\n\r\nWe tested multiple inventory methods, including live traps, track plate stations, and artificial cover boards, across all years and habitats. In most years, sampling occurred in 3-4 primary sampling sessions between July and September. In 1994, additional sampling occurred in February and May in conjunction with an assessment of Hantavirus exposure in deer mice (Peromyscus maniculatus).\r\n\r\nOverall, we detected 32 mammal, 14 reptile, and 6 amphibian species during 25,222 trap-nights of effort. The deer mouse-the most abundant species detected--accounted for 67% of total captures. We detected the Federal Endangered salt marsh harvest mouse (Reithrodontomys raviventris) at one coastal wetland plot in 1992.\r\n\r\nThis project represents the first phase in the development of a comprehensive terrestrial vertebrate inventory and monitoring program for GGNRA. This report summarizes data on relative abundance, frequency of occurrence, distribution across habitat types, and trap success for terrestrial vertebrates detected during this 7-year effort. It includes comprehensive descriptions of the inventory methods and sampling strategies employed during this survey and is intended to help guide the park in the implementation of future longterm ecological monitoring programs.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051381","collaboration":"Prepared in cooperation with the National Park Service, Golden Gate National Parks Association, and Earthwatch","usgsCitation":"Semenoff-Irving, M., and Howell, J.A., 2005, Pilot inventory of mammals, reptiles, and amphibians, Golden Gate National Recreation Area, California, 1990-1997: U.S. Geological Survey Open-File Report 2005-1381, vi, 107 p., https://doi.org/10.3133/ofr20051381.","productDescription":"vi, 107 p.","numberOfPages":"107","costCenters":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":191771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2005/1381/coverthb.jpg"},{"id":9839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1381/ofr20051381.pdf","text":"Report","size":"7.28 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":12535,"rank":9999,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2005/1381/ofr20051381.zip","size":"1.51 MB","linkFileType":{"id":6,"text":"zip"}}],"country":"United States","state":"California","otherGeospatial":"Golden Gate National Recreation Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.37258911132812,\n 37.260938147754544\n ],\n [\n -122.11990356445312,\n 37.45959832290546\n ],\n [\n -122.39456176757811,\n 37.79350762410675\n ],\n [\n -122.6513671875,\n 38.136716904135376\n ],\n [\n -122.89718627929688,\n 38.07620357665235\n ],\n [\n -122.79006958007812,\n 37.96260604160774\n ],\n [\n -122.54013061523438,\n 37.78482544885859\n ],\n [\n -122.52914428710938,\n 37.54893261064111\n ],\n [\n -122.37258911132812,\n 37.260938147754544\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"Original contributing office: Patuxent Wildlife Research Center","contact":"Contact Pubs Warehouse
","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc87","contributors":{"authors":[{"text":"Semenoff-Irving, Marcia","contributorId":9338,"corporation":false,"usgs":true,"family":"Semenoff-Irving","given":"Marcia","email":"","affiliations":[],"preferred":false,"id":286866,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, Judd A. jhowell@usgs.gov","contributorId":5728,"corporation":false,"usgs":true,"family":"Howell","given":"Judd","email":"jhowell@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":286865,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003996,"text":"70003996 - 2005 - A 40,000-year woodrat-midden record of vegetational and biogeographical dynamics in north-eastern Utah","interactions":[],"lastModifiedDate":"2017-05-10T16:08:07","indexId":"70003996","displayToPublicDate":"2011-05-31T12:59:01","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2193,"text":"Journal of Biogeography","active":true,"publicationSubtype":{"id":10}},"title":"A 40,000-year woodrat-midden record of vegetational and biogeographical dynamics in north-eastern Utah","docAbstract":"Aim A conspicuous climatic and biogeographical transition occurs at 40-45° N in western North America. This pivot point marks a north–south opposition of wet and dry conditions at interannual and decadal time-scales, as well as the northern and southern limits of many dominant western plant species. Palaeoecologists have yet to focus on past climatic and biotic shifts along this transition, in part because it requires comparisons across dissimilar records [i.e. pollen from lacustrine sediments to the north and plant macrofossils from woodrat (Neotoma) middens to the south]. To overcome these limitations, we are extending the woodrat-midden record northward into the lowlands of the central Rocky Mountains.
Location Woodrat middens were collected from crevices and rock shelters on south-facing slopes of Dutch John Mountain (2000-2200 m, 40°57′ N, 109°25′ W), situated on the eastern flanks of the Uinta Mountains in north-eastern Utah. The site is near the regional limits for Pinus ponderosa, P. edulis, P. contorta, Cercocarpus ledifolius var. intricatus, Abies concolor, Ephedra viridis and other important western species.
Methods We analysed pollen and plant macrofossils from the 40,000-year midden sequence. The middens represent brief, depositional episodes (mostly years to decades). Four middens represent the early to full-glacial period (40,000–18,000 cal-yr bp), eight middens are from the late-glacial/early Holocene transition (13,500–9000 cal yr bp), and 33 middens span the mid-to-late Holocene (last 7500 years). Temporal density of our Holocene middens (one every c. 210 years) is comparable with typical Holocene pollen sequences from lake sediments.
Results Early to full-glacial assemblages are characterized by low diversity and occurrence of montane conifers (Picea pungens, Pseudotsuga menziesii, P. flexilis, Juniperus communis) absent from the site today. Diversity increases in the late-glacial samples with the addition of J. scopulorum, J. horizontalis, C. montanus, C. ledifolius var. intricatus and mesic understory species. The coniferous trees and J. communis declined and J. osteosperma appeared during the late-glacial/Holocene transition. Juniperus osteosperma populations have occupied the site throughout the Holocene. Pinus ponderosa was established by 7500 cal-yr bp, and has occurred at least locally ever since. Montane conifers and J. horizontalis persisted until c. 5500 cal-yr bp. The signature events of the late Holocene were the invasions of P. edulis and Ephedra viridis and establishment of pinyon–juniper woodland in the last 800 years.
Main conclusions The Dutch John Mountain midden record adds to an emerging picture in which mid-elevation conifers (P. flexilis, Pseudotsuga menziesii, Picea pungens, J. scopulorum, J. communis) dominated vegetation over a wide area of the Colorado Plateau and adjacent Rocky Mountains. Rather than being fragmented, as often assumed in phylogeographical studies, these species had broader and more-connected distributions than they do in the region today. Paradoxically, subalpine conifers (Picea engelmannii, A. lasiocarpa) occurred at higher elevations to the south, possibly representing declining precipitation from south to north owing to southward displacement of the polar jet stream. The Dutch John Mountain record displays a series of extinction and invasion events. Most of the extinctions were local in scale; nearly all constituents of fossil midden assemblages occur within a few kilometres of Dutch John Mountain, and some occur at least locally on its slopes. The sole exception is J. horizontalis, which is regionally extinct. In contrast to extinctions, Holocene invasions were regional in scale; J. osteosperma, P. ponderosa, P. edulis and Ephedra viridis immigrated from glacial-age source populations far to the south.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2699.2005.01251.x","usgsCitation":"Jackson, S.T., Betancourt, J.L., Lyford, M.E., Gray, S., and Rylander, K.A., 2005, A 40,000-year woodrat-midden record of vegetational and biogeographical dynamics in north-eastern Utah: Journal of Biogeography, v. 32, no. 6, p. 1085-1106, https://doi.org/10.1111/j.1365-2699.2005.01251.x.","productDescription":"22 p.","startPage":"1085","endPage":"1106","costCenters":[{"id":148,"text":"Branch of Regional Research-Western Region","active":false,"usgs":true}],"links":[{"id":203837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","volume":"32","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-05-18","publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b428e","contributors":{"authors":[{"text":"Jackson, Stephen T. 0000-0002-1487-4652 stjackson@usgs.gov","orcid":"https://orcid.org/0000-0002-1487-4652","contributorId":344,"corporation":false,"usgs":true,"family":"Jackson","given":"Stephen","email":"stjackson@usgs.gov","middleInitial":"T.","affiliations":[{"id":569,"text":"Southwest Climate Science Center","active":true,"usgs":true},{"id":560,"text":"South Central Climate Science Center","active":true,"usgs":true}],"preferred":true,"id":350073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Betancourt, Julio L. 0000-0002-7165-0743 jlbetanc@usgs.gov","orcid":"https://orcid.org/0000-0002-7165-0743","contributorId":3376,"corporation":false,"usgs":true,"family":"Betancourt","given":"Julio","email":"jlbetanc@usgs.gov","middleInitial":"L.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":554,"text":"Science and Decisions Center","active":true,"usgs":true}],"preferred":true,"id":350074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lyford, Mark E.","contributorId":45815,"corporation":false,"usgs":true,"family":"Lyford","given":"Mark","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":350075,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gray, Stephen T. sgray@usgs.gov","contributorId":221,"corporation":false,"usgs":true,"family":"Gray","given":"Stephen T.","email":"sgray@usgs.gov","affiliations":[{"id":107,"text":"Alaska Climate Science Center","active":true,"usgs":true}],"preferred":true,"id":350072,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rylander, Kate Aasen","contributorId":76447,"corporation":false,"usgs":true,"family":"Rylander","given":"Kate","email":"","middleInitial":"Aasen","affiliations":[{"id":219,"text":"Desert Laboratory","active":false,"usgs":true}],"preferred":false,"id":350076,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":5224635,"text":"5224635 - 2005 - Effects of hunting on survival of American woodcock in the Northeast","interactions":[],"lastModifiedDate":"2022-05-26T15:12:46.986909","indexId":"5224635","displayToPublicDate":"2010-06-16T12:18:53","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Effects of hunting on survival of American woodcock in the Northeast","docAbstract":"Numbers of American woodcock (Scolopax minor) males counted on the annual singing ground survey (SGS) have declined over the last 35 years at an average rate of 2.3% per year in the Eastern Region and 1.8% per year in the Central Region. Although hunting was not thought to be a cause of these declines, mortality caused by hunters can be controlled. Furthermore, there has been no research on effects of hunting mortality on woodcock populations at local and regional levels on the breeding grounds. We used radiotelemetry to determine survival rates and causes of mortality for 913 woodcock captured during fall 1997–2000 on 7 areas in Maine, New Hampshire, Pennsylvania, and Vermont, USA. Three of 7 sites were closed to hunting. For all sites and all years combined, 176 woodcock died, and 130 were censored, of which 39 were censored mortalities. Predation was the major (n = 134, 76%) cause of mortality. Mammals accounted for 56% of the predation, raptors accounted for 25%, and 19% was attributed to unknown predators. On hunted sites, 36% of the total mortality (n = 102) was caused by hunting, 63% by predation, and 1 bird starved. Kaplan-Meier survival curves did not differ between hunted and non-hunted sites among years (P = 0.46). Overall, point estimates of survival did not differ (P = 0.217) between hunted (SR = 0.636, SE = 0.04) and nonhunted sites (SR = 0.661, SE = 0.08). We modeled hazard rates from hunting and natural mortality events using program MARK. Akaike's Information Criterion supported using a model with common constant hazards from both hunting and natural causes for groups of sites. Groupings of sites for hazard rates from natural causes were not influenced by whether a site was hunted or not. Models detected no effects of woodcock age and sex (P = 0.52) on survival. Proportional hazards models comparing hunted and nonhunted sites found no effects of age and sex (P = 0.45), interactions of age, sex, capture weight, and bill length (P ≥ 0.269). Our data suggest that current hunting regulations are not causing lower survival of woodcock.
","language":"English","publisher":"Wildlife Society","doi":"10.2193/0022-541X(2005)69[1565:EOHOSO]2.0.CO;2","usgsCitation":"McAuley, D.G., Longcore, J.R., Clugston, D.A., Allen, R.B., Weik, A., Williams, S., Dunn, J., Palmer, B., Evans, K., Staats, W., Sepik, G.F., and Halteman, W., 2005, Effects of hunting on survival of American woodcock in the Northeast: Journal of Wildlife Management, v. 69, no. 4, p. 1565-1577, https://doi.org/10.2193/0022-541X(2005)69[1565:EOHOSO]2.0.CO;2.","productDescription":"13 p.","startPage":"1565","endPage":"1577","numberOfPages":"13","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine, New Hampshire, Pennsylvania, 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,{"id":5224634,"text":"5224634 - 2005 - Population size and winter distribution of eastern American oystercatchers","interactions":[],"lastModifiedDate":"2022-05-26T14:49:29.023309","indexId":"5224634","displayToPublicDate":"2010-06-16T12:18:53","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Population size and winter distribution of eastern American oystercatchers","docAbstract":"Conservation of the eastern subspecies of the American oystercatcher (Haematopus palliatus palliatus) is a high priority in the U.S. Shorebird Conservation Plan, but previous population estimates were unreliable, information on distribution and habitat associations during winter was incomplete, and methods for long-term monitoring had not been developed prior to this survey. We completed the aerial survey proposed in the U.S. Shorebird Conservation Plan to determine population size, winter distribution, and habitat associations. We conducted coastal aerial surveys from New Jersey to Texas during November 2002 to February 2003. This area comprised the entire wintering range of the eastern American oystercatcher within the United States. Surveys covered all suitable habitat in the United States for the subspecies, partitioned into 3 survey strata: known roost sites, high-use habitat, and inter-coastal tidal habitat. We determined known roost sites from extensive consultation with biologists and local experts in each state. High-use habitat included sand islands, sand spits at inlets, shell rakes, and oyster reefs. Partner organizations conducted ground counts in most states. We used high resolution still photography to determine detection rates for estimates of the number of birds in particular flocks, and we used ground counts to determine detection rates of flocks. Using a combination of ground and aerial counts, we estimated the population of eastern American oystercatchers to be 10,971 /− 298. Aerial surveys can serve an important management function for shorebirds and possibly other coastal waterbirds by providing population status and trend information across a wide geographic scale.
","language":"English","publisher":"Wildlife Society","doi":"10.2193/0022-541X(2005)69[1538:PSAWDO]2.0.CO;2","usgsCitation":"Brown, S.C., Schulte, S., Harrington, B., Winn, B., Bart, J., and Howe, M., 2005, Population size and winter distribution of eastern American oystercatchers: Journal of Wildlife Management, v. 69, no. 4, p. 1538-1545, https://doi.org/10.2193/0022-541X(2005)69[1538:PSAWDO]2.0.CO;2.","productDescription":"8 p.","startPage":"1538","endPage":"1545","numberOfPages":"8","costCenters":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636a7b","contributors":{"authors":[{"text":"Brown, Stephen C.","contributorId":38457,"corporation":false,"usgs":false,"family":"Brown","given":"Stephen","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":342173,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schulte, Shiloh A.","contributorId":39911,"corporation":false,"usgs":true,"family":"Schulte","given":"Shiloh A.","affiliations":[],"preferred":false,"id":342171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harrington, B.","contributorId":17947,"corporation":false,"usgs":false,"family":"Harrington","given":"B.","affiliations":[],"preferred":false,"id":342170,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winn, Brad","contributorId":90852,"corporation":false,"usgs":true,"family":"Winn","given":"Brad","email":"","affiliations":[],"preferred":false,"id":342175,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bart, Jonathan jon_bart@usgs.gov","contributorId":57025,"corporation":false,"usgs":true,"family":"Bart","given":"Jonathan","email":"jon_bart@usgs.gov","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":false,"id":342174,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Howe, Marshall","contributorId":146168,"corporation":false,"usgs":false,"family":"Howe","given":"Marshall","email":"","affiliations":[],"preferred":false,"id":342172,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":5224605,"text":"5224605 - 2005 - Modeling anuran detection and site occupancy on North American Amphibian Monitoring Program (NAAMP) routes in Maryland","interactions":[],"lastModifiedDate":"2022-05-24T14:52:15.18942","indexId":"5224605","displayToPublicDate":"2010-06-16T12:18:51","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":"Modeling anuran detection and site occupancy on North American Amphibian Monitoring Program (NAAMP) routes in Maryland","docAbstract":"One of the most fundamental problems in monitoring animal populations is that of imperfect detection. Although imperfect detection can be modeled, studies examining patterns in occurrence often ignore detection and thus fail to properly partition variation in detection from that of occurrence. In this study, we used anuran calling survey data collected on North American Amphibian Monitoring Program routes in eastern Maryland to investigate factors that influence detection probability and site occupancy for 10 anuran species. In 2002, 17 calling survey routes in eastern Maryland were surveyed to collect environmental and species data nine or more times. To analyze these data, we developed models incorporating detection probability and site occupancy. The results suggest that, for more than half of the 10 species, detection probabilities vary most with season (i.e., day-of-year), air temperature, time, and moon illumination, whereas site occupancy may vary by the amount of palustrine forested wetland habitat. Our results suggest anuran calling surveys should document air temperature, time of night, moon illumination, observer skill, and habitat change over time, as these factors can be important to model-adjusted estimates of site occupancy. Our study represents the first formal modeling effort aimed at developing an analytic assessment framework for NAAMP calling survey data.
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\"}}]}","volume":"39","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6999cc","contributors":{"authors":[{"text":"Weir, Linda lweir@usgs.gov","contributorId":174278,"corporation":false,"usgs":true,"family":"Weir","given":"Linda","email":"lweir@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":342052,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Royle, J. Andrew 0000-0003-3135-2167","orcid":"https://orcid.org/0000-0003-3135-2167","contributorId":96221,"corporation":false,"usgs":true,"family":"Royle","given":"J. Andrew","affiliations":[],"preferred":false,"id":342055,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nanjappa, Priya","contributorId":84272,"corporation":false,"usgs":true,"family":"Nanjappa","given":"Priya","email":"","affiliations":[],"preferred":false,"id":342054,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jung, Robin E.","contributorId":22434,"corporation":false,"usgs":true,"family":"Jung","given":"Robin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":342053,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5224632,"text":"5224632 - 2005 - Impact of special early harvest seasons on subarctic-nesting and temperate-nesting Canada geese","interactions":[],"lastModifiedDate":"2022-05-26T14:37:14.938181","indexId":"5224632","displayToPublicDate":"2010-06-16T12:18:51","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Impact of special early harvest seasons on subarctic-nesting and temperate-nesting Canada geese","docAbstract":"Dramatic changes in wintering distributions of Canada geese (Branta canadensis) have occurred over the past 50 years in eastern North America. Declines in numbers of subarctic-nesting geese wintering in southern states, and increases in numbers wintering in northern regions, have resulted in a northern shift in winter distributions. In contrast, numbers of temperate-nesting geese have increased throughout eastern North America. Management efforts to control overabundant temperate-nesting flocks have included the establishment of special early harvest seasons in September. However, the effect of early seasons on survival and harvest of subarctic-nesting populations has not been documented. Understanding the timing of migration movements and the fidelity of subarctic-nesting flocks to terminal winter refuges in the Southeast also is necessary to design early harvest seasons that target temperate-nesting flocks and protect subarctic-nesting populations. We used recoveries of marked geese to estimate survival and harvest rates before and after implementation of early harvest seasons within the Mississippi Flyway during 1976–1999. In addition, we used observations of neck-banded geese from the Southern James Bay Population (SJBP) to evaluate the hypothesis that subarctic-nesting geese arriving prior to mid-December on several key terminal winter refuges in the Southeast (early arriving migrants) were more likely to return to those refuges in subsequent years than were migrants arriving after mid-December (late arriving migrants). September seasons during 1987–1994 were a minor source of mortality for subarctic-nesting populations and accounted for <10% of their annual harvest mortality. The effectiveness of early seasons for increasing mortality of temperate-nesting flocks varied among the states we examined and was tempered by concurrent changes in state-specific harvest regulations during the regular harvest season. For SJBP Canada geese, annual fidelity to southeastern refuges was 10% higher for early arrivers than for late arriving geese. However, in any given year only 47–57% of the surviving geese were expected to return to the refuges the following year. Although early arriving migrants had higher survival and higher return probabilities than did late arriving migrants or geese that failed to return, numbers of geese wintering on southeastern refuges likely declined because <60% of the surviving geese affiliated with the refuges would return in a given year and because of lower survival for geese that did not return to the refuges.
","language":"English","publisher":"Wildlife Society","doi":"10.2193/0022-541X(2005)69[1494:IOSEHS]2.0.CO;2","usgsCitation":"Sheaffer, S.E., Kendall, W.L., and Bowers, E.F., 2005, Impact of special early harvest seasons on subarctic-nesting and temperate-nesting Canada geese: Journal of Wildlife Management, v. 69, no. 4, p. 1494-1507, https://doi.org/10.2193/0022-541X(2005)69[1494:IOSEHS]2.0.CO;2.","productDescription":"14 p.","startPage":"1494","endPage":"1507","numberOfPages":"14","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db6592d7","contributors":{"authors":[{"text":"Sheaffer, S. E.","contributorId":54325,"corporation":false,"usgs":false,"family":"Sheaffer","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":342163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kendall, William L. 0000-0003-0084-9891","orcid":"https://orcid.org/0000-0003-0084-9891","contributorId":204844,"corporation":false,"usgs":true,"family":"Kendall","given":"William","email":"","middleInitial":"L.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":342162,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowers, E. Frank","contributorId":106833,"corporation":false,"usgs":true,"family":"Bowers","given":"E.","email":"","middleInitial":"Frank","affiliations":[],"preferred":false,"id":342164,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}