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,{"id":70122713,"text":"70122713 - 2003 - La mondialisation des poussieres, les vents transportent, d'un continent a l'autre, des poussieres, mai aussi des micro-organismes et des substances toxiques. Ces \"passagers clandestins\" pourraient transporter des maladies et modifier les ecosystems","interactions":[],"lastModifiedDate":"2022-06-03T15:21:48.776191","indexId":"70122713","displayToPublicDate":"2003-08-27T13:56:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":9946,"text":"Pour la Science","onlineIssn":"2267-490X","printIssn":"0153-4092","active":true,"publicationSubtype":{"id":10}},"title":"La mondialisation des poussieres, les vents transportent, d'un continent a l'autre, des poussieres, mai aussi des micro-organismes et des substances toxiques. Ces \"passagers clandestins\" pourraient transporter des maladies et modifier les ecosystems","docAbstract":"<p>Un tour d'horizon de la littérature scientifique révèle que de nombreux champs d'investigation sont jugés dignes d'intérêt de façon périodique : certaines idées sont à la mode pour un temps, puis sombrent dans l'oubli, avant de refaire surface comme si elles n'avaient jamais été émises. L'aérobiologie, c'est-à-dire l'étude des micro-organismes, tels des bactéries et des pollens transportés par les airs, est l'un de ces domaines.</p>","language":"French","publisher":"Pour la Science","usgsCitation":"Griffin, D., Kellogg, C., Garrison, V., and Shinn, E., 2003, La mondialisation des poussieres, les vents transportent, d'un continent a l'autre, des poussieres, mai aussi des micro-organismes et des substances toxiques. Ces \"passagers clandestins\" pourraient transporter des maladies et modifier les ecosystems: Pour la Science, v. 309, p. 79-85.","productDescription":"7 p.","startPage":"79","endPage":"85","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293133,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293132,"type":{"id":15,"text":"Index Page"},"url":"https://www.pourlascience.fr/sd/climatologie/la-mondialisation-des-poussieres-7418.php"}],"volume":"309","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0dfe4b01f35f8fd69de","contributors":{"authors":[{"text":"Griffin, D.","contributorId":86290,"corporation":false,"usgs":true,"family":"Griffin","given":"D.","email":"","affiliations":[],"preferred":false,"id":499659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kellogg, C.","contributorId":27802,"corporation":false,"usgs":true,"family":"Kellogg","given":"C.","email":"","affiliations":[],"preferred":false,"id":499657,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garrison, V.","contributorId":18300,"corporation":false,"usgs":true,"family":"Garrison","given":"V.","email":"","affiliations":[],"preferred":false,"id":499656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shinn, E.","contributorId":56824,"corporation":false,"usgs":true,"family":"Shinn","given":"E.","email":"","affiliations":[],"preferred":false,"id":499658,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70122709,"text":"70122709 - 2003 - Pathogenic human viruses in coastal waters","interactions":[],"lastModifiedDate":"2014-08-27T13:40:52","indexId":"70122709","displayToPublicDate":"2003-08-27T13:34:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1255,"text":"Clinical Microbiology Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Pathogenic human viruses in coastal waters","docAbstract":"This review addresses both historical and recent investigations into viral contamination of marine waters. With the relatively recent emergence of molecular biology-based assays, a number of investigations have shown that pathogenic viruses are prevalent in marine waters being impacted by sewage. Research has shown that this group of fecal-oral viral pathogens (enteroviruses, hepatitis A viruses, Norwalk viruses, reoviruses, adenoviruses, rotaviruses, etc.) can cause a broad range of asymptomatic to severe gastrointestinal, respiratory, and eye, nose, ear, and skin infections in people exposed through recreational use of the water. The viruses and the nucleic acid signature survive for an extended period in the marine environment. One of the primary concerns of public health officials is the relationship between the presence of pathogens and the recreational risk to human health in polluted marine environments. While a number of studies have attempted to address this issue, the relationship is still poorly understood. A contributing factor to our lack of progress in the field has been the lack of sensitive methods to detect the broad range of both bacterial and viral pathogens. The application of new and advanced molecular methods will continue to contribute to our current state of knowledge in this emerging and","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Clinical Microbiology Reviews","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society for Microbiology","doi":"10.1128/CMR.16.1.129-143.2003","usgsCitation":"Griffin, D.W., Donaldson, K.A., Paul, J., and Rose, J.B., 2003, Pathogenic human viruses in coastal waters: Clinical Microbiology Reviews, v. 16, no. 1, p. 129-143, https://doi.org/10.1128/CMR.16.1.129-143.2003.","productDescription":"15 p.","startPage":"129","endPage":"143","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":478348,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/145303","text":"External Repository"},{"id":293131,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293130,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1128/CMR.16.1.129-143.2003"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0e6e4b01f35f8fd6a0b","contributors":{"authors":[{"text":"Griffin, Dale W. 0000-0003-1719-5812 dgriffin@usgs.gov","orcid":"https://orcid.org/0000-0003-1719-5812","contributorId":2178,"corporation":false,"usgs":true,"family":"Griffin","given":"Dale","email":"dgriffin@usgs.gov","middleInitial":"W.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":499652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donaldson, Kim A.","contributorId":89810,"corporation":false,"usgs":true,"family":"Donaldson","given":"Kim","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":499655,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paul, J.H.","contributorId":62798,"corporation":false,"usgs":true,"family":"Paul","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":499653,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rose, Joan B.","contributorId":81791,"corporation":false,"usgs":true,"family":"Rose","given":"Joan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":499654,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70122706,"text":"70122706 - 2003 - Supraglacial sulfur springs and associated biological activity in the Canadian high arctic - signs of life beneath the ice","interactions":[],"lastModifiedDate":"2014-08-27T13:24:30","indexId":"70122706","displayToPublicDate":"2003-08-27T13:20:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":912,"text":"Astrobiology","active":true,"publicationSubtype":{"id":10}},"title":"Supraglacial sulfur springs and associated biological activity in the Canadian high arctic - signs of life beneath the ice","docAbstract":"Unique springs, discharging from the surface of an arctic glacier, release H2S and deposit native sulfur, gypsum, and calcite. The presence of sulfur in three oxidation states indicates a complex series of redox reactions. Physical and chemical conditions of the spring water and surrounding environment, as well as mineralogical and isotopic signatures, suggest biologically mediated reactions. Cell counts and DNA analyses confirm bacteria are present in the spring system, and a limited number of sequenced isolates suggests that complex communities of bacteria live within the glacial system.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Astrobiology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mary Ann Liebert, Inc.","doi":"10.1089/153110703322610672","usgsCitation":"Grasby, S.E., Allen, C.C., Longazo, T.G., Lisle, J.T., Griffin, D.W., and Beauchamp, B., 2003, Supraglacial sulfur springs and associated biological activity in the Canadian high arctic - signs of life beneath the ice: Astrobiology, v. 3, no. 3, p. 583-596, https://doi.org/10.1089/153110703322610672.","productDescription":"14 p.","startPage":"583","endPage":"596","costCenters":[{"id":185,"text":"Coastal and Marine Geology Progam","active":false,"usgs":true}],"links":[{"id":293128,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293127,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1089/153110703322610672"}],"country":"Canada","volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0eee4b01f35f8fd6a4e","contributors":{"authors":[{"text":"Grasby, Stephen E.","contributorId":15939,"corporation":false,"usgs":true,"family":"Grasby","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":499641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Carlton C.","contributorId":75451,"corporation":false,"usgs":true,"family":"Allen","given":"Carlton","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":499643,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Longazo, Teresa G.","contributorId":76661,"corporation":false,"usgs":true,"family":"Longazo","given":"Teresa","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":499644,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lisle, John T. 0000-0002-5447-2092 jlisle@usgs.gov","orcid":"https://orcid.org/0000-0002-5447-2092","contributorId":2944,"corporation":false,"usgs":true,"family":"Lisle","given":"John","email":"jlisle@usgs.gov","middleInitial":"T.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":499640,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Griffin, Dale W. 0000-0003-1719-5812 dgriffin@usgs.gov","orcid":"https://orcid.org/0000-0003-1719-5812","contributorId":2178,"corporation":false,"usgs":true,"family":"Griffin","given":"Dale","email":"dgriffin@usgs.gov","middleInitial":"W.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":499639,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Beauchamp, Benoit","contributorId":61349,"corporation":false,"usgs":true,"family":"Beauchamp","given":"Benoit","email":"","affiliations":[],"preferred":false,"id":499642,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70122690,"text":"70122690 - 2003 - Sediment dispersal pathways and conceptual sediment budget for a sediment starved embayment: Long Bay, South Carolina","interactions":[],"lastModifiedDate":"2017-09-20T09:35:00","indexId":"70122690","displayToPublicDate":"2003-08-27T12:19:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Sediment dispersal pathways and conceptual sediment budget for a sediment starved embayment: Long Bay, South Carolina","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal sediments '03: \"Crossing disciplinary boundaries\": the Fifth International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Coastal sediments '03: \"Crossing disciplinary boundaries\": the Fifth 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,{"id":70122685,"text":"70122685 - 2003 - African and Asian dust: from desert soils to coral reefs","interactions":[],"lastModifiedDate":"2014-08-27T12:07:14","indexId":"70122685","displayToPublicDate":"2003-08-27T12:02:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":997,"text":"BioScience","active":true,"publicationSubtype":{"id":10}},"title":"African and Asian dust: from desert soils to coral reefs","docAbstract":"Many hypotheses have been proposed to explain the decline of coral reefs throughout the world, but none adequately accounts for the lack of recovery of reefs or the wide geographical distribution of coral diseases. The processes driving the decline remain elusive. Hundreds of millions of tons of dust transported annually from Africa and Asia to the Americas may be adversely affecting coral reefs and other downwind ecosystems. Viable microorganisms, macro- and micronutrients, trace metals, and an array of organic contaminants carried in the dust air masses and deposited in the oceans and on land may play important roles in the complex changes occurring on coral reefs worldwide.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"BioScience","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Oxford Journals","doi":"10.1641/0006-3568(2003)053[0469:AAADFD]2.0.CO;2","usgsCitation":"Garrison, V.H., Shinn, E., Foreman, W., Griffin, D.W., Holmes, C.W., Kellogg, C.A., Majewski, M.S., Richardson, L.L., Ritchie, K.B., and Smith, G.W., 2003, African and Asian dust: from desert soils to coral reefs: BioScience, v. 53, no. 5, p. 469-480, https://doi.org/10.1641/0006-3568(2003)053[0469:AAADFD]2.0.CO;2.","productDescription":"12 p.","startPage":"469","endPage":"480","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":478349,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1641/0006-3568(2003)053[0469:aaadfd]2.0.co;2","text":"Publisher Index Page"},{"id":293115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293114,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1641/0006-3568(2003)053[0469:AAADFD]2.0.CO;2"}],"volume":"53","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0c6e4b01f35f8fd6911","contributors":{"authors":[{"text":"Garrison, Virginia H. ginger_garrison@usgs.gov","contributorId":2386,"corporation":false,"usgs":true,"family":"Garrison","given":"Virginia","email":"ginger_garrison@usgs.gov","middleInitial":"H.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":499605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shinn, Eugene A.","contributorId":6883,"corporation":false,"usgs":true,"family":"Shinn","given":"Eugene A.","affiliations":[],"preferred":false,"id":499606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foreman, William T. wforeman@usgs.gov","contributorId":1473,"corporation":false,"usgs":true,"family":"Foreman","given":"William T.","email":"wforeman@usgs.gov","affiliations":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"preferred":false,"id":499603,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Griffin, Dale W. 0000-0003-1719-5812 dgriffin@usgs.gov","orcid":"https://orcid.org/0000-0003-1719-5812","contributorId":2178,"corporation":false,"usgs":true,"family":"Griffin","given":"Dale","email":"dgriffin@usgs.gov","middleInitial":"W.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":499604,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Holmes, Charles W.","contributorId":31071,"corporation":false,"usgs":true,"family":"Holmes","given":"Charles","email":"","middleInitial":"W.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":499608,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kellogg, Christina A. 0000-0002-6492-9455 ckellogg@usgs.gov","orcid":"https://orcid.org/0000-0002-6492-9455","contributorId":391,"corporation":false,"usgs":true,"family":"Kellogg","given":"Christina","email":"ckellogg@usgs.gov","middleInitial":"A.","affiliations":[{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":499601,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Majewski, Michael S. majewski@usgs.gov","contributorId":440,"corporation":false,"usgs":true,"family":"Majewski","given":"Michael","email":"majewski@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":499602,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Richardson, Laurie L.","contributorId":29322,"corporation":false,"usgs":true,"family":"Richardson","given":"Laurie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":499607,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ritchie, Kim B.","contributorId":85515,"corporation":false,"usgs":true,"family":"Ritchie","given":"Kim","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":499610,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Smith, Garriet W.","contributorId":49715,"corporation":false,"usgs":true,"family":"Smith","given":"Garriet","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":499609,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70122660,"text":"70122660 - 2003 - Influence of climate on deep-water clastic sedimentation: application of a modern model, Peru-Chile Trough, to an ancient system, Ouachita Trough","interactions":[],"lastModifiedDate":"2014-08-27T10:55:57","indexId":"70122660","displayToPublicDate":"2003-08-27T10:49:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1247,"text":"Climate Controls on Stratigraphy: SEPM Special Publication","active":true,"publicationSubtype":{"id":10}},"title":"Influence of climate on deep-water clastic sedimentation: application of a modern model, Peru-Chile Trough, to an ancient system, Ouachita Trough","docAbstract":"<p>Traditionally, an abrupt and massive influx of siliciclastic sediments into an area of deposition has been attributed to tectonic uplift without consideration of the influence of climate or climatic change on rates of weathering, erosion, transportation, and deposition. With few exceptions, fluvial sediment transport is minimal in both extremely arid climates and in perhumid (everwet) climates. Maximum sediment transport occurs in climates characterized by strongly seasonal rainfall, where the effect of vegetation on erosion is minimal.</p>\n<br>\n<p>The Peru–Chile trench and Andes Mountain system (P–CT/AMS) of the eastern Pacific Ocean clearly illustrates the effects of climate on rates of weathering, erosion, transport, and deep-sea sedimentation. Terrigenous sediment is virtually absent in the arid belt north of lat. 30° S in the P–CT, but in the belt of seasonal rainfall south of lat. 30° S terrigenous sediment is abundant. Spatial variations in the amount and seasonality of annual precipitation are now generally accepted as the cause for this difference. The spatial variation in sediment supply to the P–CT appears to be an excellent modern analogue for the temporal variation in sediment supply to certain ancient systems, such as the Ouachita Trough in the southern United States.</p>\n<br>\n<p>By comparison, during the Ordovician through the early Mississippian, sediment was deposited at very slow rates as the Ouachita Trough moved northward through the southern hemisphere dry belt (lat. 10° S to lat. 30° S). The deposystem approached the tropical humid zone during the Mississippian, coincident with increased coarse clastic sedimentation. By the Middle Pennsylvanian (Atokan), the provenance area and the deposystem moved well into the tropical humid zone, and as much as 8,500 m of mineralogically mature (but texturally immature) quartz sand was introduced and deposited. This increase in clastic sediment deposition traditionally has been attributed solely to tectonic activity. However, we contend that the principal control on the introduction of abundant terrigenous sediment was the movement of the deposystem from an arid or semiarid climate into a seasonally wetter climatic regime. The physical and mineralogical maturity of the quartz sand is the result of tropical weathering in provenance areas.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Climate Controls on Stratigraphy: SEPM Special Publication","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Sedimentary Geology","doi":"10.2110/pec.03.77.0185","usgsCitation":"Edgar, N.T., and Cecil, C.B., 2003, Influence of climate on deep-water clastic sedimentation: application of a modern model, Peru-Chile Trough, to an ancient system, Ouachita Trough: Climate Controls on Stratigraphy: SEPM Special Publication, v. 77, p. 185-191, https://doi.org/10.2110/pec.03.77.0185.","productDescription":"7","startPage":"185","endPage":"191","costCenters":[{"id":183,"text":"Coastal and Marine Geology","active":false,"usgs":true}],"links":[{"id":293088,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293087,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2110/pec.03.77.0185"}],"country":"Chile;Peru;United States","volume":"77","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0dee4b01f35f8fd69cc","contributors":{"authors":[{"text":"Edgar, N. Terence","contributorId":14388,"corporation":false,"usgs":true,"family":"Edgar","given":"N.","email":"","middleInitial":"Terence","affiliations":[],"preferred":false,"id":499565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cecil, C. Blaine 0000-0002-9032-1689","orcid":"https://orcid.org/0000-0002-9032-1689","contributorId":22797,"corporation":false,"usgs":true,"family":"Cecil","given":"C.","email":"","middleInitial":"Blaine","affiliations":[],"preferred":false,"id":499566,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70122652,"text":"70122652 - 2003 - A modern analogue for tectonic, eustatic, and climatic processes in cratonic basins: Gulf of Carpentaria, northern Australia","interactions":[],"lastModifiedDate":"2014-08-27T10:43:43","indexId":"70122652","displayToPublicDate":"2003-08-27T10:28:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1247,"text":"Climate Controls on Stratigraphy: SEPM Special Publication","active":true,"publicationSubtype":{"id":10}},"title":"A modern analogue for tectonic, eustatic, and climatic processes in cratonic basins: Gulf of Carpentaria, northern Australia","docAbstract":"The Gulf of Carpentaria is a tropical, silled epicontinental sea and may be a modern analogue for ancient cratonic basins. For the purpose of this study, the Gulf of Carpentaria is compared to Pennsylvanian cratonic basins of the United States. During the Pennsylvanian, the North American continent moved from the Southern Hemisphere, through the Equator, into the Northern Hemisphere. Today, the Gulf of Carpentaria–New Guinea region is a few degrees south of the Equator and is moving towards it. During the Pennsylvanian, the world was subjected to major glaciations and associated sea-level changes. The island of New Guinea and the Gulf of Carpentaria have undergone similar processes during the Quaternary. A reconnaissance seismic survey of the gulf conducted by the USGS and the Australian National University (ANU), combined with oil-exploration well data, provided the first step in a systematic evaluation of a modern tropical epicontinental system. During the Cenozoic, the region was dominated by terrestrial sedimentation in a temperate climate. At the same time, carbonates were being deposited on the northern shelf edge of the Australian Plate. During the Miocene, carbonate deposition expanded southward into the gulf region. Then in the Late Miocene, carbonate sedimentation was replaced by terrigenous clastics derived from the developing Central Range of the island of New Guinea, which developed a wetter climate while moving northwards into the tropics. At least 14 basin-wide transgressive–regressive cycles are identified by channels that were eroded under subaerial conditions since about the Miocene. Comparison of the modern Gulf of Carpentaria sequences with those of the Pennsylvanian reveals many similarities.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Climate Controls on Stratigraphy: SEPM Special Publication","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Sedimentary Geology","doi":"10.2110/pec.03.77.0193","usgsCitation":"Edgar, N.T., Cecil, C.B., Mattick, R., de Deckker, P., and Djajadihardja, Y.S., 2003, A modern analogue for tectonic, eustatic, and climatic processes in cratonic basins: Gulf of Carpentaria, northern Australia: Climate Controls on Stratigraphy: SEPM Special Publication, v. 77, p. 193-205, https://doi.org/10.2110/pec.03.77.0193.","productDescription":"13 p.","startPage":"193","endPage":"205","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293084,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293085,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2110/pec.03.77.0193"}],"country":"Australia","otherGeospatial":"Gulf Of Carpentaria","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 137.03,-16.62 ], [ 137.03,-10.61 ], [ 141.69,-10.61 ], [ 141.69,-16.62 ], [ 137.03,-16.62 ] ] ] } } ] }","volume":"77","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0c4e4b01f35f8fd6903","contributors":{"authors":[{"text":"Edgar, N. Terence","contributorId":14388,"corporation":false,"usgs":true,"family":"Edgar","given":"N.","email":"","middleInitial":"Terence","affiliations":[],"preferred":false,"id":499552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cecil, C. Blaine 0000-0002-9032-1689","orcid":"https://orcid.org/0000-0002-9032-1689","contributorId":22797,"corporation":false,"usgs":true,"family":"Cecil","given":"C.","email":"","middleInitial":"Blaine","affiliations":[],"preferred":false,"id":499553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mattick, R.E.","contributorId":85162,"corporation":false,"usgs":true,"family":"Mattick","given":"R.E.","affiliations":[],"preferred":false,"id":499556,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"de Deckker, Patrick","contributorId":69070,"corporation":false,"usgs":true,"family":"de Deckker","given":"Patrick","email":"","affiliations":[],"preferred":false,"id":499555,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Djajadihardja, Yusuf S.","contributorId":29324,"corporation":false,"usgs":true,"family":"Djajadihardja","given":"Yusuf","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":499554,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70122646,"text":"70122646 - 2003 - Unique and exceptionally long interglacial marine isotope stage 11: window into Earth warm future climate","interactions":[],"lastModifiedDate":"2014-08-27T10:09:15","indexId":"70122646","displayToPublicDate":"2003-08-27T10:05:00","publicationYear":"2003","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"137","title":"Unique and exceptionally long interglacial marine isotope stage 11: window into Earth warm future climate","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Earth's climate and eccentricity: the marine isotope stage 11 question","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/137GM01","usgsCitation":"Droxler, A., Alley, R.B., Howard, W.R., Poore, R.Z., and Burckle, L.H., 2003, Unique and exceptionally long interglacial marine isotope stage 11: window into Earth warm future climate, chap. <i>of</i> Earth's climate and eccentricity: the marine isotope stage 11 question, p. 1-14, https://doi.org/10.1029/137GM01.","productDescription":"14 p.","startPage":"1","endPage":"14","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":502564,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://figshare.com/articles/chapter/Unique_and_Exceptionally_Long_Interglacial_Marine_Isotope_Stage_11_Window_into_Earth_Warm_Future_Climate/23053550","text":"External Repository"},{"id":293075,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293074,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/137GM01"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0f1e4b01f35f8fd6a6b","contributors":{"editors":[{"text":"Droxler, Andre","contributorId":25875,"corporation":false,"usgs":true,"family":"Droxler","given":"Andre","email":"","affiliations":[],"preferred":false,"id":509967,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Poore, Richard Z. rpoore@usgs.gov","contributorId":345,"corporation":false,"usgs":true,"family":"Poore","given":"Richard","email":"rpoore@usgs.gov","middleInitial":"Z.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":509966,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Burckle, Lloyd H.","contributorId":44475,"corporation":false,"usgs":true,"family":"Burckle","given":"Lloyd","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":509968,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Droxler, Andre","contributorId":25875,"corporation":false,"usgs":true,"family":"Droxler","given":"Andre","email":"","affiliations":[],"preferred":false,"id":499544,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alley, Richard B.","contributorId":34365,"corporation":false,"usgs":false,"family":"Alley","given":"Richard","email":"","middleInitial":"B.","affiliations":[{"id":13035,"text":"Department of Geosciences, Pennsylvania State University","active":true,"usgs":false}],"preferred":false,"id":499545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howard, William R.","contributorId":102808,"corporation":false,"usgs":true,"family":"Howard","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":499547,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Poore, Richard Z. rpoore@usgs.gov","contributorId":345,"corporation":false,"usgs":true,"family":"Poore","given":"Richard","email":"rpoore@usgs.gov","middleInitial":"Z.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":499543,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burckle, Lloyd H.","contributorId":44475,"corporation":false,"usgs":true,"family":"Burckle","given":"Lloyd","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":499546,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70122643,"text":"70122643 - 2003 - Mobility of authigenic rhenium, silver, and selenium during postdepositional oxidation in marine sediments","interactions":[],"lastModifiedDate":"2017-09-13T13:48:43","indexId":"70122643","displayToPublicDate":"2003-08-27T09:34:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Mobility of authigenic rhenium, silver, and selenium during postdepositional oxidation in marine sediments","docAbstract":"<p><span>Sedimentary records of redox-sensitive trace elements hold significant potential as indicators of paleoceanographic environmental conditions. Records of Re can reveal the intensity of past reducing conditions in sediments at the time of deposition, whereas records of Ag may record the magnitude of past diatom fluxes to the seafloor. Confidence in paleoenvironmental reconstruction from records of either metal, however, requires it to have experienced negligible redistribution since deposition. This study examines diagenetic rearrangements of Re and Ag that occur in response to exposure to bottom-water O</span><sub>2</sub><span><span>&nbsp;</span>in environments of low sedimentation rate, including Madeira Abyssal Plain turbidites and eastern Mediterranean basin sapropels. Authigenic Re was remobilized quantitatively by oxidation but poorly retained by the underlying sediments. All records are consistent with previous work demonstrating that only a limited reimmobilization of Re occurs preferentially in C</span><sub>org</sub><span>-rich, reducing sediments. Silver was also mobilized quantitatively by oxidation, but it was subsequently immobilized more efficiently in all cases as sharp peaks immediately into anoxic conditions below active oxidation fronts, and these peaks remain immobile in anoxic conditions during long-term burial. Comparison of Ag, S, and Se records from various cores suggests that Ag is likely to have been immobilized as a selenide, a mechanism previously proposed for Hg in similar situations<span>&nbsp;</span></span><a class=\"workspace-trigger\" name=\"bBIB32\" href=\"http://www.sciencedirect.com/science/article/pii/S001670370201075X?via%3Dihub#BIB32\" data-mce-href=\"http://www.sciencedirect.com/science/article/pii/S001670370201075X?via%3Dihub#BIB32\">(Mercone et al., 1999)</a><span>. Coexisting narrow peaks of Ag and Hg with Se offer a means of assessing whether oxidative burndown has ever occurred at the top of C</span><sub>org</sub><span>- and sulfide-rich sedimentary units. Although these results suggest that caution must be used when inferring paleoenvironmental information from records of Ag and Re in cores with low sediment accumulation rates (&lt;5 cm ka</span><sup>−1</sup><span>), they should not affect the promise that authigenic Ag and Re records hold for paleoenvironmental reconstruction in sediments with higher accumulation rates and where anoxic conditions have been maintained continuously.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(02)01075-X","usgsCitation":"Crusius, J., and Thomson, J., 2003, Mobility of authigenic rhenium, silver, and selenium during postdepositional oxidation in marine sediments: Geochimica et Cosmochimica Acta, v. 67, no. 2, p. 265-273, https://doi.org/10.1016/S0016-7037(02)01075-X.","productDescription":"9 p.","startPage":"265","endPage":"273","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":478350,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1912/1607","text":"External Repository"},{"id":293066,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0e2e4b01f35f8fd69fc","contributors":{"authors":[{"text":"Crusius, John 0000-0003-2554-0831 jcrusius@usgs.gov","orcid":"https://orcid.org/0000-0003-2554-0831","contributorId":2155,"corporation":false,"usgs":true,"family":"Crusius","given":"John","email":"jcrusius@usgs.gov","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":499531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomson, John","contributorId":31685,"corporation":false,"usgs":true,"family":"Thomson","given":"John","affiliations":[],"preferred":false,"id":499532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70122640,"text":"70122640 - 2003 - Tale of two pit lakes: initial results of a three-year study of the Main Zone and Waterline pit lakes near Houston, British Columbia, Canada","interactions":[],"lastModifiedDate":"2018-05-02T21:28:16","indexId":"70122640","displayToPublicDate":"2003-08-27T09:07:00","publicationYear":"2003","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":"Tale of two pit lakes: initial results of a three-year study of the Main Zone and Waterline pit lakes near Houston, British Columbia, Canada","docAbstract":"Pit lakes are becoming increasingly common in North America as well as in the rest of the world. They are created as openpit mines fill passively with ground water and surface inflows on cessation of mining activity. In many instances, the water quality in these pit lakes does not meet regulatory requirements due to a number of influences. The most important are the oxidation of sulfide minerals and the associated release of acid and metals and the flushing of soluble metals during pit filling. Examples of pit lakes with severe water-quality problems include the Berkeley Pit lake (Butte, MT) and the Liberty Pit lake (Nevada), whose waters are characterized by a pH near 3 and Cu concentrations as high as ~150 mg/L (Miller et al., 1996; Davis and Eary, 1997). The importance of the problem can be seen in the fact that some of these sites in the United States are Superfund sites.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Mining, Metallurgy, and Exploration, Inc.","usgsCitation":"Crusius, J., Pieters, R., Leung, A., Whittle, P., Pedersen, T., Lawrence, G., and McNee, J., 2003, Tale of two pit lakes: initial results of a three-year study of the Main Zone and Waterline pit lakes near Houston, British Columbia, Canada: Mining Engineering, v. 55, no. 2, p. 25-30.","productDescription":"6 p.","startPage":"25","endPage":"30","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":293061,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293060,"type":{"id":15,"text":"Index Page"},"url":"https://me.smenet.org/abstract.cfm?articleID=3958&page=25"}],"country":"Canada;United States","state":"British Columbia;Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -139.06,29.5236 ], [ -139.06,60.0 ], [ -95.0145,60.0 ], [ -95.0145,29.5236 ], [ -139.06,29.5236 ] ] ] } } ] }","volume":"55","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0eee4b01f35f8fd6a51","contributors":{"authors":[{"text":"Crusius, John 0000-0003-2554-0831 jcrusius@usgs.gov","orcid":"https://orcid.org/0000-0003-2554-0831","contributorId":2155,"corporation":false,"usgs":true,"family":"Crusius","given":"John","email":"jcrusius@usgs.gov","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":499525,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pieters, R.","contributorId":32094,"corporation":false,"usgs":true,"family":"Pieters","given":"R.","email":"","affiliations":[],"preferred":false,"id":499523,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leung, A.","contributorId":66180,"corporation":false,"usgs":true,"family":"Leung","given":"A.","email":"","affiliations":[],"preferred":false,"id":499526,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whittle, P.","contributorId":93831,"corporation":false,"usgs":true,"family":"Whittle","given":"P.","email":"","affiliations":[],"preferred":false,"id":499527,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pedersen, T.","contributorId":21872,"corporation":false,"usgs":true,"family":"Pedersen","given":"T.","email":"","affiliations":[],"preferred":false,"id":499521,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lawrence, G.","contributorId":37541,"corporation":false,"usgs":true,"family":"Lawrence","given":"G.","email":"","affiliations":[],"preferred":false,"id":499524,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McNee, J.J.","contributorId":23453,"corporation":false,"usgs":true,"family":"McNee","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":499522,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70121966,"text":"70121966 - 2003 - Quaternary sedimentation and subsidence history of Lake Baikal, Siberia, based on seismic stratigraphy and coring","interactions":[],"lastModifiedDate":"2017-09-14T15:04:16","indexId":"70121966","displayToPublicDate":"2003-08-25T16:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2451,"text":"Journal of Sedimentary Research","onlineIssn":"1938-3681","printIssn":"1527-1404","active":true,"publicationSubtype":{"id":10}},"title":"Quaternary sedimentation and subsidence history of Lake Baikal, Siberia, based on seismic stratigraphy and coring","docAbstract":"<p>The long, continuous, high-latitude, stratigraphic record of Lake Baikal was deposited in three broad sedimentary environments, defined by high-resolution seismic-reflection and coring methods: (1) turbidite depositional systems, by far the most widespread, characterizing most of the margins and floors of the main basins of the lake, (2) large deltas of major drainages, and (3) tectonically or topographically isolated ridges and banks. Holocene sedimentation rates based on radiocarbon ages vary by more than an order of magnitude among these environments, from less than about 0.03 mm/yr on ridges and banks to more than about 0.3 mm/yr on basin floors. Extrapolating these rates, with a correction for compaction, yields tentative estimates of about 25 and 11 Ma for the inception of rifting in the Central and North basins, respectively, and less than 6 Ma for the 200-m sediment depth on Academician Ridge.</p>\n<br>\n<p>The Selenga Delta has the distinctive form of a classic prograding Gilbert-type delta, but its history appears to represent a complex combination of tectonism and sedimentation. The central part of the delta is underlain by prograding, shallow-water sequences, now several hundred meters below the lake surface. These deposits and much of the delta slope are mantled by fine-grained, deep-water, hemipelagic deposits whose base is estimated to be about 650,000 years old. Modern coarse-grained sediment bypasses the delta slope through fault-controlled canyons that feed large, subaqueous fans at the ends of the South and Central basins. These relations, along with abundant other evidence of recent faulting and the great depths of the Central and South basins, suggest that these two rift basins have experienced a period of unusually rapid subsidence over the last 650,000 years, during at least part of which sedimentation has failed to keep pace.</p>","language":"English","publisher":"Society for Sedimentary Geology","doi":"10.1306/041703730941","usgsCitation":"Colman, S.M., Karabanov, E., and Nelson, C.H., 2003, Quaternary sedimentation and subsidence history of Lake Baikal, Siberia, based on seismic stratigraphy and coring: Journal of Sedimentary Research, v. 73, no. 6, p. 941-956, https://doi.org/10.1306/041703730941.","productDescription":"16 p.","startPage":"941","endPage":"956","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":293004,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia","otherGeospatial":"Lake Baikal","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 103.7,51.46 ], [ 103.7,55.93 ], [ 110.1,55.93 ], [ 110.1,51.46 ], [ 103.7,51.46 ] ] ] } } ] }","volume":"73","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fc4ddfe4b0413fd75d6b2b","contributors":{"authors":[{"text":"Colman, Steven M. 0000-0002-0564-9576","orcid":"https://orcid.org/0000-0002-0564-9576","contributorId":77482,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":499426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karabanov, E.B.","contributorId":37084,"corporation":false,"usgs":true,"family":"Karabanov","given":"E.B.","affiliations":[],"preferred":false,"id":499425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, C. H. III","contributorId":103589,"corporation":false,"usgs":true,"family":"Nelson","given":"C.","suffix":"III","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":499427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70121951,"text":"70121951 - 2003 - Optimizing the quality of sediment samples collected for geochemical measurement in coastal marine environments","interactions":[],"lastModifiedDate":"2017-11-05T12:21:43","indexId":"70121951","displayToPublicDate":"2003-08-25T14:54:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Optimizing the quality of sediment samples collected for geochemical measurement in coastal marine environments","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Collection and preparation of bottom sediment samples for analysis of radionuclides and trace elements","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"International Atomic Energy Agency","usgsCitation":"Bothner, M., 2003, Optimizing the quality of sediment samples collected for geochemical measurement in coastal marine environments, 11 p.","productDescription":"11 p.","startPage":"83","endPage":"93","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":292998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345753,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www-pub.iaea.org/books/IAEABooks/6674/Collection-and-Preparation-of-Bottom-Sediment-Samples-for-Analysis-of-Radionuclides-and-Trace-Elements"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fc4ddce4b0413fd75d6b0c","contributors":{"authors":[{"text":"Bothner, Michael H. mbothner@usgs.gov","contributorId":139855,"corporation":false,"usgs":true,"family":"Bothner","given":"Michael H.","email":"mbothner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":499416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121946,"text":"70121946 - 2003 - Complexity analysis of the change in shoreline position at Duck, NC","interactions":[],"lastModifiedDate":"2014-08-25T14:40:44","indexId":"70121946","displayToPublicDate":"2003-08-25T14:38:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Complexity analysis of the change in shoreline position at Duck, NC","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal sediments '03: \"crossing disciplinary boundaries\": the Fifth International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: proceedings: May 18-23, 2003, Sheraton Sand Key Resort, Clearwater Beach, Florida, USA","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"East Meets West Productions","usgsCitation":"Barton, C., Dismukes, J.S., and Morton, R., 2003, Complexity analysis of the change in shoreline position at Duck, NC, <i>in</i> Coastal sediments '03: \"crossing disciplinary boundaries\": the Fifth International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: proceedings: May 18-23, 2003, Sheraton Sand Key Resort, Clearwater Beach, Florida, USA, CD-ROM.","productDescription":"CD-ROM","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292997,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fc4dc7e4b0413fd75d6a70","contributors":{"authors":[{"text":"Barton, Christopher","contributorId":89453,"corporation":false,"usgs":true,"family":"Barton","given":"Christopher","affiliations":[],"preferred":false,"id":499415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dismukes, Jeffrey S.","contributorId":10727,"corporation":false,"usgs":true,"family":"Dismukes","given":"Jeffrey","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":499413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morton, R.A.","contributorId":53849,"corporation":false,"usgs":true,"family":"Morton","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":499414,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70121944,"text":"70121944 - 2003 - Links between erosional hotspots and alongshore sediment transport","interactions":[],"lastModifiedDate":"2017-08-24T10:19:30","indexId":"70121944","displayToPublicDate":"2003-08-25T14:25:00","publicationYear":"2003","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Links between erosional hotspots and alongshore sediment transport","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal sediments '03: \"crossing disciplinary boundaries\": the Fifth International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: proceedings: May 18-23, 2003, Sheraton Sand Key Resort, Clearwater Beach, Florida, USA","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"East Meets West Productions","usgsCitation":"Ashton, A., List, J., Murray, A.B., and Farris, A., 2003, Links between erosional hotspots and alongshore sediment transport, <i>in</i> Coastal sediments '03: \"crossing disciplinary boundaries\": the Fifth International Symposium on Coastal Engineering and Science of Coastal Sediment Processes: proceedings: May 18-23, 2003, Sheraton Sand Key Resort, Clearwater Beach, Florida, USA, 13 p.","productDescription":"13 p.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":292996,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fc4dd2e4b0413fd75d6ac0","contributors":{"authors":[{"text":"Ashton, Andrew","contributorId":63327,"corporation":false,"usgs":true,"family":"Ashton","given":"Andrew","affiliations":[],"preferred":false,"id":499409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"List, Jeffrey H. jlist@usgs.gov","contributorId":2416,"corporation":false,"usgs":true,"family":"List","given":"Jeffrey H.","email":"jlist@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":false,"id":499406,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murray, A. Brad","contributorId":57585,"corporation":false,"usgs":true,"family":"Murray","given":"A.","email":"","middleInitial":"Brad","affiliations":[],"preferred":false,"id":499408,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farris, Amy S.","contributorId":28075,"corporation":false,"usgs":true,"family":"Farris","given":"Amy S.","affiliations":[],"preferred":false,"id":499407,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179885,"text":"70179885 - 2003 - Conditions for growth and survival of bull trout in Beulah Reservoir, Oregon. Annual report 2002","interactions":[],"lastModifiedDate":"2017-01-19T14:32:31","indexId":"70179885","displayToPublicDate":"2003-08-25T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Conditions for growth and survival of bull trout in Beulah Reservoir, Oregon. Annual report 2002","docAbstract":"<p>The Bureau of Reclamation (BOR) constructed Agency Valley Dam on the North Fork of the Malheur River in 1934-35, creating Beulah Reservoir. The project is operated and maintained by the Vale Irrigation District for irrigation and downstream flood control. There is currently no formal agreement for a minimum pool level at Beulah Reservoir, but project operators of Agency Valley Dam and BOR are considering management alternatives. Although the project is not operated for fish and wildlife values, the reservoir supports a rainbow trout Oncorhynchus mykiss fishery and also seasonally harbors an adfluvial population of bull trout Salvelinus confluentus (Oregon Department of Fish and Wildlife [ODFW], unpublished data). Bull trout were listed by the USFWS as a threatened species throughout the Columbia and Klamath river basins in 1998, and Oregon has listed the North Fork Malheur River population “Of Special Concern”. </p>","language":"English","publisher":"U.S. Bureau of Reclamation","usgsCitation":"Petersen, J., Kofoot, E., and Rose, B., 2003, Conditions for growth and survival of bull trout in Beulah Reservoir, Oregon. Annual report 2002, 45 p. .","productDescription":"45 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333477,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.16328048706055,\n              43.94704092173972\n            ],\n            [\n              -118.1714344024658,\n              43.941169962996725\n            ],\n            [\n              -118.170747756958,\n              43.929302676319814\n            ],\n            [\n              -118.16834449768068,\n              43.91650560484078\n            ],\n            [\n              -118.16473960876465,\n              43.909333095564016\n            ],\n            [\n              -118.15632820129393,\n              43.90766350817876\n            ],\n            [\n              -118.1439685821533,\n              43.91477438864446\n            ],\n            [\n              -118.13332557678221,\n              43.932949646682616\n            ],\n            [\n              -118.13538551330565,\n              43.940860949106984\n            ],\n            [\n              -118.13607215881346,\n              43.944569009780324\n            ],\n            [\n              -118.15032005310059,\n              43.94580497860898\n            ],\n            [\n              -118.15993309020996,\n              43.94796786222348\n            ],\n            [\n              -118.16328048706055,\n              43.94704092173972\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881dedde4b01192927d9f97","contributors":{"authors":[{"text":"Petersen, J.H.","contributorId":72154,"corporation":false,"usgs":true,"family":"Petersen","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":659095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kofoot, E.E.","contributorId":89349,"corporation":false,"usgs":true,"family":"Kofoot","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":659096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rose, B.","contributorId":68500,"corporation":false,"usgs":true,"family":"Rose","given":"B.","email":"","affiliations":[],"preferred":false,"id":659097,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70121635,"text":"70121635 - 2003 - Atmospheric transport of mold spores in clouds of desert dust","interactions":[],"lastModifiedDate":"2014-08-22T16:17:58","indexId":"70121635","displayToPublicDate":"2003-08-22T16:13:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":888,"text":"Archives of Environmental Health","active":true,"publicationSubtype":{"id":10}},"title":"Atmospheric transport of mold spores in clouds of desert dust","docAbstract":"Fungal spores can be transported globally in clouds of desert dust. Many species of fungi (commonly known as molds) and bacteria--including some that are human pathogens--have characteristics suited to long-range atmospheric transport. Dust from the African desert can affect air quality in Africa, Europe, the Middle East, and the Americas. Asian desert dust can affect air quality in Asia, the Arctic, North America, and Europe. Atmospheric exposure to mold-carrying desert dust may affect human health directly through allergic induction of respiratory stress. In addition, mold spores within these dust clouds may seed downwind ecosystems in both outdoor and indoor environments.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Archives of Environmental Health","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Heldref Publications","usgsCitation":"Shinn, E., Griffin, D., and Seba, D., 2003, Atmospheric transport of mold spores in clouds of desert dust: Archives of Environmental Health, v. 58, no. 8, p. 498-504.","productDescription":"7 p.","startPage":"498","endPage":"504","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292917,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292916,"type":{"id":15,"text":"Index Page"},"url":"https://www.ncbi.nlm.nih.gov/pubmed/15259429"}],"volume":"58","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f85946e4b03f038c5c1756","contributors":{"authors":[{"text":"Shinn, E.A.","contributorId":38610,"corporation":false,"usgs":true,"family":"Shinn","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":499244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffin, Dale W.","contributorId":23668,"corporation":false,"usgs":true,"family":"Griffin","given":"Dale W.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":499243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seba, D.B.","contributorId":8393,"corporation":false,"usgs":true,"family":"Seba","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":499242,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70200802,"text":"70200802 - 2003 - Orogenic tectonism on Io","interactions":[],"lastModifiedDate":"2018-11-01T16:28:43","indexId":"70200802","displayToPublicDate":"2003-08-19T16:27:44","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Orogenic tectonism on Io","docAbstract":"<p><span>We catalog 143 Ionian mountains (montes) and mountain‐like features (mensae, tholi, plana, and small peaks) in order to investigate orogenic tectonism on Io. From this comprehensive list, we select 96 mountains for which there are sufficient coverage and resolution to discern spatial relationships with surrounding geologic features. Three of the 96 mountains are probably volcanoes, 92 appear to be tectonic massifs, and 1 is ambiguous. Of the 92 tectonic mountains, 38 abut paterae (volcanic or volcano‐tectonic craters with irregular or scalloped margins). This juxtaposition is unlikely to be a coincidence as the probability of it occurring by chance is ∼0.1%. We propose instead that orogenic faults may act as conduits for magma ascent, thus fueling patera formation near mountains. As resurfacing buries a shell of material from Io's surface to the base of the lithosphere, its effective radius is reduced and it heats up. We calculate the lithospheric volume change due to subsidence and thermal expansion as a function of lithospheric thickness. Conservation of volume dictates that this material must be uplifted at Io's surface. By estimating the total volume of the mountains, we are able to place a lower limit of 12 km on Io's lithospheric thickness. We hypothesize that, in some cases, mountain formation may be facilitated by asthenospheric diapirs impinging on the base of the lithosphere. The resulting lithospheric swell could focus the compressive stresses that drive orogenic tectonism. This model is one of several possible mechanisms for uplifting isolated mountains such as are observed on Io.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2002JE001946","usgsCitation":"Jaeger, W.L., Turtle, E.P., Keszthelyi, L., Radebaugh, J., McEwen, A., and Pappalardo, R.T., 2003, Orogenic tectonism on Io: Journal of Geophysical Research E: Planets, v. 108, no. E8, 18 p., https://doi.org/10.1029/2002JE001946.","productDescription":"18 p.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":478351,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2002je001946","text":"Publisher Index Page"},{"id":359090,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"E8","noUsgsAuthors":false,"publicationDate":"2003-08-19","publicationStatus":"PW","scienceBaseUri":"5c10ec84e4b034bf6a803753","contributors":{"authors":[{"text":"Jaeger, Windy L.","contributorId":61679,"corporation":false,"usgs":true,"family":"Jaeger","given":"Windy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":750585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turtle, Elizabeth P.","contributorId":45443,"corporation":false,"usgs":false,"family":"Turtle","given":"Elizabeth","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":750586,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keszthelyi, Laszlo P. 0000-0003-1879-4331 laz@usgs.gov","orcid":"https://orcid.org/0000-0003-1879-4331","contributorId":52802,"corporation":false,"usgs":true,"family":"Keszthelyi","given":"Laszlo P.","email":"laz@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":750587,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Radebaugh, Jani","contributorId":101792,"corporation":false,"usgs":true,"family":"Radebaugh","given":"Jani","email":"","affiliations":[],"preferred":false,"id":750588,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McEwen, A.S.","contributorId":202347,"corporation":false,"usgs":false,"family":"McEwen","given":"A.S.","email":"","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":750589,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pappalardo, Robert T.","contributorId":102380,"corporation":false,"usgs":true,"family":"Pappalardo","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":750590,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70217608,"text":"70217608 - 2003 - Clearing Toutle River sediment issue","interactions":[],"lastModifiedDate":"2021-01-22T18:36:57.288641","indexId":"70217608","displayToPublicDate":"2003-08-09T12:35:37","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":17,"text":"Newspaper Article"},"title":"Clearing Toutle River sediment issue","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"The Columbian","usgsCitation":"Major, J.J., and Spicer, K.R., 2003, Clearing Toutle River sediment issue.","costCenters":[],"links":[{"id":382509,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Major, Jon J. 0000-0003-2449-4466 jjmajor@usgs.gov","orcid":"https://orcid.org/0000-0003-2449-4466","contributorId":439,"corporation":false,"usgs":true,"family":"Major","given":"Jon","email":"jjmajor@usgs.gov","middleInitial":"J.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":808837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spicer, Kurt R. 0000-0001-5030-3198 krspicer@usgs.gov","orcid":"https://orcid.org/0000-0001-5030-3198","contributorId":2684,"corporation":false,"usgs":true,"family":"Spicer","given":"Kurt","email":"krspicer@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":808838,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70241068,"text":"70241068 - 2003 - Geomorphology, acoustic backscatter, and processes in Santa Monica Bay from multibeam mapping","interactions":[],"lastModifiedDate":"2023-03-08T17:37:00.842002","indexId":"70241068","displayToPublicDate":"2003-08-01T11:21:19","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2664,"text":"Marine Environmental Research","active":true,"publicationSubtype":{"id":10}},"title":"Geomorphology, acoustic backscatter, and processes in Santa Monica Bay from multibeam mapping","docAbstract":"<p><span>Santa Monica Bay was mapped in 1996 using a high-resolution multibeam system, providing the first substantial update of the submarine geomorphology since the initial compilation by Shepard and Emery [(1941) Geol. Soc. Amer. Spec. Paper 31]. The multibeam mapping generated not only high-resolution bathymetry, but also coregistered, calibrated acoustic backscatter at 95 kHz. The geomorphology has been subdivided into six provinces; shelf, marginal plateau, submarine canyon, basin slope, apron, and basin. The dimensions, gradients, and backscatter characteristics of each province is described and related to a combination of tectonics, climate, sea level, and sediment supply. Fluctuations of eustatic sea level have had a profound effect on the area; by periodically eroding the surface of Santa Monica plateau, extending the mouth of the Los Angeles River to various locations along the shelf break, and by connecting submarine canyons to rivers. A wetter glacial climate undoubtedly generated more sediment to the rivers that then transported the increased sediment load to the low-stand coastline and canyon heads. The trends of Santa Monica Canyon and several bathymetric highs suggest a complex tectonic stress field that has controlled the various segments. There is no geomorphic evidence to suggest Redondo Canyon is fault controlled. The San Pedro fault can be extended more than 30 km to the northwest by the alignment of a series of bathymetric highs and abrupt changes in direction of channel thalwegs.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0141-1136(02)00323-9","usgsCitation":"Gardner, J., Dartnell, P., Mayer, L.A., and Clarke, J.E., 2003, Geomorphology, acoustic backscatter, and processes in Santa Monica Bay from multibeam mapping: Marine Environmental Research, v. 56, no. 1-2, p. 15-46, https://doi.org/10.1016/S0141-1136(02)00323-9.","productDescription":"32 p.","startPage":"15","endPage":"46","costCenters":[],"links":[{"id":413866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Santa Monica Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.81293071164076,\n              34.001765773903585\n            ],\n            [\n              -118.74758258339918,\n              33.84683933588596\n            ],\n            [\n              -118.48752370570243,\n              33.72990520667567\n            ],\n            [\n              -118.4021710484071,\n              33.78368148613396\n            ],\n            [\n              -118.3828333369886,\n              33.8158202546048\n            ],\n            [\n              -118.38416697225858,\n              33.85680736423771\n            ],\n            [\n              -118.46551872374349,\n              33.99070894674546\n            ],\n            [\n              -118.55220501630879,\n              34.052056163386396\n            ],\n            [\n              -118.6355572206989,\n              34.048741231390935\n            ],\n            [\n              -118.68756899623844,\n              34.047636225257065\n            ],\n            [\n              -118.75491757738521,\n              34.03990077911911\n            ],\n            [\n              -118.79092572968185,\n              34.02884891788558\n            ],\n            [\n              -118.81293071164076,\n              34.001765773903585\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"56","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gardner, James V.","contributorId":61769,"corporation":false,"usgs":true,"family":"Gardner","given":"James V.","affiliations":[],"preferred":false,"id":865946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dartnell, Peter 0000-0002-9554-729X pdartnell@usgs.gov","orcid":"https://orcid.org/0000-0002-9554-729X","contributorId":2688,"corporation":false,"usgs":true,"family":"Dartnell","given":"Peter","email":"pdartnell@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":865947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mayer, Larry A.","contributorId":69583,"corporation":false,"usgs":true,"family":"Mayer","given":"Larry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":865948,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clarke, John E. Hughes","contributorId":101179,"corporation":false,"usgs":true,"family":"Clarke","given":"John","email":"","middleInitial":"E. Hughes","affiliations":[],"preferred":false,"id":865949,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70047123,"text":"70047123 - 2003 - Quantifying migratory delay: A new application of survival analysis","interactions":[],"lastModifiedDate":"2023-06-30T13:27:20.524478","indexId":"70047123","displayToPublicDate":"2003-08-01T10:56:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Quantifying migratory delay: A new application of survival analysis","docAbstract":"<p><span>Statistical techniques commonly used in fish passage research fail to adequately quantify delays incurred at obstacles, or the effects of modifications to those obstacles on passage rates. Analyses of telemetry data describing these effects can be misleading, particularly when passage route of some individuals is not established (e.g., because of mortality, tag failure, passage through unmonitored or alternate routes, etc.). Here, we demonstrate how event-time analysis, better known as survival analysis, can be used to quantify passage rates for any study that allows tracking of individuals through time, even when some individuals fail to pass the route or obstacle in question. We review two of the primary methods of event-time analysis (parametric and Cox's proportional hazards regression analyses) and use them in combination with logistic regression to provide unbiased estimates of delay incurred at a hydroelectric facility, as well as insights on factors affecting both rates of passage and route selection. Passage rate increased with increased depth of a surface bypass sluice gate and, among fish that passed through the turbines, with turbine flow. The data further indicate that risk of turbine passage increased with both delay and turbine flow.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f03-086","usgsCitation":"Castro-Santos, T., and Haro, A., 2003, Quantifying migratory delay: A new application of survival analysis: Canadian Journal of Fisheries and Aquatic Sciences, v. 60, no. 8, p. 986-996, https://doi.org/10.1139/f03-086.","productDescription":"11 p.","startPage":"986","endPage":"996","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":275181,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51ea8705e4b03397884d39ac","contributors":{"authors":[{"text":"Castro-Santos, Theodore 0000-0003-2575-9120","orcid":"https://orcid.org/0000-0003-2575-9120","contributorId":32573,"corporation":false,"usgs":true,"family":"Castro-Santos","given":"Theodore","affiliations":[],"preferred":false,"id":481130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haro, Alex 0000-0002-7188-9172","orcid":"https://orcid.org/0000-0002-7188-9172","contributorId":37223,"corporation":false,"usgs":true,"family":"Haro","given":"Alex","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":481131,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50602,"text":"ofr0251 - 2003 - Biosolids, soils, ground-water, and streambed-sediment data for a biosolids-application area near Deer Trail, Colorado, 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:11:17","indexId":"ofr0251","displayToPublicDate":"2003-08-01T00:00:00","publicationYear":"2003","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":"2002-51","title":"Biosolids, soils, ground-water, and streambed-sediment data for a biosolids-application area near Deer Trail, Colorado, 1999","docAbstract":"In January 1999, the U.S. Geological Survey began an expanded monitoring program near Deer Trail, Colorado, in cooperation with the Metro Wastewater Reclamation District and the North Kiowa Bijou Groundwater Management District. Monitoring components were biosolids, soils, crops, ground water, and streambed sediments. The monitoring program addresses concerns from the public about chemical effects from applications of biosolids to farmland in the Deer Trail, Colorado, area. Constituents of primary concern to the public are arsenic, cadmium, chromium, copper, lead, mercury, molybdenum, nickel, selenium, zinc, plutonium, and gross alpha and beta activity and are included for all monitoring components. This report presents chemical data from the first year of the monitoring program, January?December 1999, for biosolids, soils, alluvial and bedrock ground water, and streambed sediments. The groundwater section of this report also includes climate data, lithologic descriptions, well-completion diagrams, water levels, summary statistics for the water-quality data, and results of statistical testing of selected data for trends and for exceedance of Colorado regulatory standards. Data in this report provide a geochemical baseline for each monitoring component prior to the planned water transfer in 2000 from the Lowry Landfill Superfund site to Metro Wastewater Reclamation District treatment facilities.","language":"ENGLISH","doi":"10.3133/ofr0251","usgsCitation":"Stevens, M.R., Yager, T., Smith, D.B., and Crock, J., 2003, Biosolids, soils, ground-water, and streambed-sediment data for a biosolids-application area near Deer Trail, Colorado, 1999: U.S. Geological Survey Open-File Report 2002-51, v, 118 p. : ill., maps ; 28 cm., https://doi.org/10.3133/ofr0251.","productDescription":"v, 118 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":176257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4397,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr02051/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611693","contributors":{"authors":[{"text":"Stevens, Michael R. 0000-0002-9476-6335 mrsteven@usgs.gov","orcid":"https://orcid.org/0000-0002-9476-6335","contributorId":769,"corporation":false,"usgs":true,"family":"Stevens","given":"Michael","email":"mrsteven@usgs.gov","middleInitial":"R.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yager, Tracy J.B.","contributorId":10861,"corporation":false,"usgs":true,"family":"Yager","given":"Tracy J.B.","affiliations":[],"preferred":false,"id":241920,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":241921,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crock, J.G.","contributorId":58236,"corporation":false,"usgs":true,"family":"Crock","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":241922,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":51405,"text":"ofr03238 - 2003 - Magnetotelluric data in the Delta River mining district, near the Tangle Lakes area of southcentral Alaska","interactions":[],"lastModifiedDate":"2021-09-14T19:34:03.993841","indexId":"ofr03238","displayToPublicDate":"2003-08-01T00:00:00","publicationYear":"2003","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":"2003-238","title":"Magnetotelluric data in the Delta River mining district, near the Tangle Lakes area of southcentral Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr03238","usgsCitation":"Pellerin, L., and Sampson, J., 2003, Magnetotelluric data in the Delta River mining district, near the Tangle Lakes area of southcentral Alaska (Version 1.0): U.S. Geological Survey Open-File Report 2003-238, 184 p., https://doi.org/10.3133/ofr03238.","productDescription":"184 p.","costCenters":[],"links":[{"id":178927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389230,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_55336.htm"},{"id":4412,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-238/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Delta River mining district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -145.5,\n              62.9167\n            ],\n            [\n              -146.1667,\n              62.9167\n            ],\n            [\n              -146.1667,\n              63.4\n            ],\n            [\n              -145.5,\n              63.4\n            ],\n            [\n              -145.5,\n              62.9167\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64943a","contributors":{"authors":[{"text":"Pellerin, Louise","contributorId":20824,"corporation":false,"usgs":true,"family":"Pellerin","given":"Louise","email":"","affiliations":[],"preferred":false,"id":243480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sampson, Jay","contributorId":65915,"corporation":false,"usgs":true,"family":"Sampson","given":"Jay","affiliations":[],"preferred":false,"id":243481,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51406,"text":"ofr03237 - 2003 - Tethered acoustic doppler current profiler platforms for measuring streamflow","interactions":[],"lastModifiedDate":"2019-04-15T08:27:15","indexId":"ofr03237","displayToPublicDate":"2003-08-01T00:00:00","publicationYear":"2003","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":"2003–0237","displayTitle":"Tethered acoustic doppler current profiler platforms for measuring streamflow","title":"Tethered acoustic doppler current profiler platforms for measuring streamflow","docAbstract":"<p>The U.S. Geological Survey tested and refined tethered-platform designs for measuring streamflow. Platform specifications were developed, radio-modem telemetry of acoustic Doppler current profiler (ADCP) data and potential platform-hull sources were investigated, and hulls were tested and evaluated.</p>\n<p>Different platforms, which included a variety of hull configurations, were tested for drag and stability at the U.S. Geological Survey tow tank and at a field site below a reservoir. The testing indicated that, although any of the designs could be used under certain conditions, trimaran designs provided the best all-around performance under a range of conditions. The trimaran designs housed the ADCP in the center hull; this resulted in lower drag than the catamaran designs and retained the stability advantage of catamarans over monohull designs. Waterproof radio modems that operate at 900 megahertz were used to communicate wirelessly with instruments at high baud rates.</p>\n<p>A tethered-platform design with a trimaran hull and 900-megahertz radio modems is now commercially available. Continued field use has resulted in U.S. Geological Survey procedures for making tethered-platform discharge measurements, including methods for tethered-boat deployment, moving-bed tests, and measurement of edge distances.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr03237","usgsCitation":"Rehmel, M.S., Stewart, J., and Morlock, S.E., 2003, Tethered acoustic doppler current profiler platforms for measuring streamflow: U.S. Geological Survey Open-File Report 2003–0237, iv, 15 p., https://doi.org/10.3133/ofr03237.","productDescription":"iv, 15 p.","numberOfPages":"20","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science 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States\"}}]}","contact":"<p><a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Director, Indiana Water Science Center</a><br>U.S. Geological Survey<br>5957 Lakeside Blvd.<br>Indianapolis, IN 46278</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Development of the Tethered Platform</li><li>Project to Refine the Tethered Platform</li><li>Tethered-Platform Discharge-Measurement Procedures</li><li>Summary and Conclusions</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684302","contributors":{"authors":[{"text":"Rehmel, Michael S. msrehmel@usgs.gov","contributorId":3723,"corporation":false,"usgs":true,"family":"Rehmel","given":"Michael","email":"msrehmel@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":243483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, James A.","contributorId":49824,"corporation":false,"usgs":true,"family":"Stewart","given":"James A.","affiliations":[],"preferred":false,"id":243484,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morlock, Scott E. smorlock@usgs.gov","contributorId":3212,"corporation":false,"usgs":true,"family":"Morlock","given":"Scott","email":"smorlock@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":243482,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51397,"text":"ofr03261 - 2003 - Results of the U.S. Geological Survey's analytical evaluation program for standard reference samples distributed in March 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:11:22","indexId":"ofr03261","displayToPublicDate":"2003-08-01T00:00:00","publicationYear":"2003","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":"2003-261","title":"Results of the U.S. Geological Survey's analytical evaluation program for standard reference samples distributed in March 2003","docAbstract":"This report presents the results of the U.S. Geological Survey's analytical evaluation program for six standard reference samples -- T-173 (trace constituents), M-166 (major constituents), N-77 (nutrient constituents), N-78 (nutrient constituents), P-40 (low ionic-strength constituents), and Hg-36 (mercury) -- that were distributed in March 2003 to laboratories enrolled in the U.S. Geological Survey sponsored interlaboratory testing program. Analytical data received from 110 laboratories were evaluated with respect to overall laboratory performance and relative laboratory performance for each analyte in the six reference samples. Results of these evaluations are presented in tabular form. Also presented are tables and graphs summarizing the analytical data provided by each laboratory for each analyte in the six standard reference samples. The most probable value for each analyte was determined using nonparametric statistics.","language":"ENGLISH","doi":"10.3133/ofr03261","usgsCitation":"Woodworth, M.T., and Connor, B.F., 2003, Results of the U.S. Geological Survey's analytical evaluation program for standard reference samples distributed in March 2003: U.S. Geological Survey Open-File Report 2003-261, iv, 109 p. : ill. ; 28 cm., https://doi.org/10.3133/ofr03261.","productDescription":"iv, 109 p. : ill. ; 28 cm.","temporalStart":"2003-03-01","temporalEnd":"2003-03-30","costCenters":[{"id":576,"text":"Standard Reference Sample Project- Branch of Quality Systems","active":false,"usgs":true}],"links":[{"id":179503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://bqs.usgs.gov/srs/Report_Spr03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":8430,"rank":9999,"type":{"id":18,"text":"Project Site"},"url":"https://bqs.usgs.gov/srs/index.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6055a3","contributors":{"authors":[{"text":"Woodworth, Mark T. woodwort@usgs.gov","contributorId":3452,"corporation":false,"usgs":true,"family":"Woodworth","given":"Mark","email":"woodwort@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":true,"id":243456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connor, Brooke F. bfconnor@usgs.gov","contributorId":3172,"corporation":false,"usgs":true,"family":"Connor","given":"Brooke","email":"bfconnor@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":243455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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