Annulus formation on opercula of the cui-ui Chasmistes cujus in Pyramid Lake, Nevada, was validated over an 8-year interval. Many fish were old, as old as 41 years of age, As many as three annuli were hidden (covered by supporting bone) in older fish. Growth was rapid during the first 10 years, slow from 10 to 20 years, and extremely slow or nil after 20 years. Age and growth were strongly correlated for about the first 10 years of life, but less so when fish became sexually mature. Examination of opercula of 15 additional species of large catostomids and cyprinids of western North America revealed that they were older than had previously been thought.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1988)117<0301:GALOTC>2.3.CO;2","usgsCitation":"Scoppettone, G., and Coleman, M., 1988, Growth and longevity of the cui-ui and longevity of other catostomids and cyprinids in western North America: Transactions of the American Fisheries Society, v. 117, no. 3, p. 301-307, https://doi.org/10.1577/1548-8659(1988)117<0301:GALOTC>2.3.CO;2.","productDescription":"7 p.","startPage":"301","endPage":"307","numberOfPages":"7","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5697833ce4b039675d00a6e3","contributors":{"authors":[{"text":"Scoppettone, G.G.","contributorId":22793,"corporation":false,"usgs":true,"family":"Scoppettone","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":588560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coleman, M.E.","contributorId":152230,"corporation":false,"usgs":false,"family":"Coleman","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":588561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70162288,"text":"70162288 - 1988 - Correlation of biological characteristics of smolts with survival and travel time. Annual report 1987","interactions":[],"lastModifiedDate":"2016-01-20T12:21:41","indexId":"70162288","displayToPublicDate":"2015-10-13T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":3,"text":"Annual Report","active":false,"publicationSubtype":{"id":1}},"title":"Correlation of biological characteristics of smolts with survival and travel time. Annual report 1987","language":"English","publisher":"U.S. Fish and Wildlife Service","doi":"10.2172/6654459","usgsCitation":"U.S. Fish and Wildlife Service, 1988, Correlation of biological characteristics of smolts with survival and travel time. Annual report 1987: Annual Report, xi, 109, https://doi.org/10.2172/6654459.","productDescription":"xi, 109","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":486855,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.osti.gov/biblio/6654459","text":"External Repository"},{"id":314523,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River, Snake River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -125.72753906249999,\n 42.09822241118974\n ],\n [\n -125.72753906249999,\n 49.28214015975995\n ],\n [\n -116.89453125,\n 49.28214015975995\n ],\n [\n -116.89453125,\n 42.09822241118974\n ],\n [\n -125.72753906249999,\n 42.09822241118974\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"Project No. 87-406\nContract No. DE-AI79-87BP35245","noUsgsAuthors":false,"publicationDate":"1988-06-01","publicationStatus":"PW","scienceBaseUri":"56a0bdc6e4b0961cf280dc15"} ,{"id":70162105,"text":"70162105 - 1988 - Relation between distance transferred from natal stream and recovery rate for hatchery coho salmon, Oncorhynchus kisutch","interactions":[],"lastModifiedDate":"2016-01-13T10:25:35","indexId":"70162105","displayToPublicDate":"2015-10-13T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Relation between distance transferred from natal stream and recovery rate for hatchery coho salmon, Oncorhynchus kisutch","docAbstract":"Distance transferred from the natal stream was negatively related to recovery rate (recruits per gram of juveniles released) for hatchery-reared coho salmon Oncorhynchus kisutch. This relation, which reflects the important influence of genetic adaptation and genetic differences among stocks on recovery rates and survival, should be useful in deciding whether or not to transfer fish.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8675(1988)008<0172:RBDTFN>2.3.CO;2","usgsCitation":"Reisenbichler, R., 1988, Relation between distance transferred from natal stream and recovery rate for hatchery coho salmon, Oncorhynchus kisutch: North American Journal of Fisheries Management, v. 8, no. 2, p. 172-174, https://doi.org/10.1577/1548-8675(1988)008<0172:RBDTFN>2.3.CO;2.","productDescription":"3 p.","startPage":"172","endPage":"174","numberOfPages":"3","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314265,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56978340e4b039675d00a6f6","contributors":{"authors":[{"text":"Reisenbichler, R.R.","contributorId":77356,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":588559,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162051,"text":"70162051 - 1988 - Radioimmunoassay of salmon growth hormone (GH) using recombinant chum salmon GH","interactions":[],"lastModifiedDate":"2016-01-12T14:19:58","indexId":"70162051","displayToPublicDate":"2015-10-05T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":749,"text":"American Zoologist","active":true,"publicationSubtype":{"id":10}},"title":"Radioimmunoassay of salmon growth hormone (GH) using recombinant chum salmon GH","docAbstract":"Abstract not available
","language":"English","publisher":"Society for Integrative and Comparative Biology","usgsCitation":"Palmisano, A., Swanson, P., Kawauchi, H., Moriyama, S., and Dickhoff, W.W., 1988, Radioimmunoassay of salmon growth hormone (GH) using recombinant chum salmon GH: American Zoologist, v. 28, no. 4.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314227,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631cbe4b039675d00a3ee","contributors":{"authors":[{"text":"Palmisano, A.N.","contributorId":152185,"corporation":false,"usgs":false,"family":"Palmisano","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":588404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, P.","contributorId":152188,"corporation":false,"usgs":false,"family":"Swanson","given":"P.","email":"","affiliations":[],"preferred":false,"id":588405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kawauchi, H.","contributorId":152187,"corporation":false,"usgs":false,"family":"Kawauchi","given":"H.","email":"","affiliations":[],"preferred":false,"id":588406,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moriyama, S.","contributorId":57408,"corporation":false,"usgs":true,"family":"Moriyama","given":"S.","email":"","affiliations":[],"preferred":false,"id":588407,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dickhoff, Walton W.","contributorId":85133,"corporation":false,"usgs":true,"family":"Dickhoff","given":"Walton","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":588408,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70162045,"text":"70162045 - 1988 - Predation of Karluk River sockeye salmon by coho salmon and char","interactions":[],"lastModifiedDate":"2018-02-27T18:09:01","indexId":"70162045","displayToPublicDate":"2015-10-05T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Predation of Karluk River sockeye salmon by coho salmon and char","docAbstract":"The number of sockeye salmon, Oncorhynchus nerka, in Alaska's Karluk River (Fig. 1) declined from millions to thousands during the early part of the present century. Rounsefell (1958) discussed alternative explanations for the decline including a general loss offertility ofthe system as the number of salmon carcasses declined, competition, overfishing, subtle changes in climate, and predation; he concluded that the combined effect of predation and fishing was the most probable explanation. Later, Van Cleave and Bevan (1973) suggested that the weir constructed in the river each year to facilitate counting the fish as they entered the system was the most probable cause ofthe decline. Itprevented free movement of both adults and juveniles in the river. All of these hypotheses remain as potential explanations for the decline
","language":"English","publisher":"National Marine Fisheries Service","usgsCitation":"McIntyre, J., Reisenbichler, R., Emlen, J., Wilmot, R., and Finn, J., 1988, Predation of Karluk River sockeye salmon by coho salmon and char: Fishery Bulletin, v. 86, no. 3, p. 611-616.","productDescription":"6 p.","startPage":"611","endPage":"616","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314223,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://fishbull.noaa.gov/863/mcintyre.pdf","text":"pdf"},{"id":314225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314224,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://fishbull.noaa.gov/863/863toc.htm"}],"country":"United States","state":"Alaska ","otherGeospatial":"Karluk Lake, Karluk River, Kodiak Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.423583984375,\n 56.87899917413543\n ],\n [\n -155.423583984375,\n 57.58066944459514\n ],\n [\n -153.12744140624997,\n 57.58066944459514\n ],\n [\n -153.12744140624997,\n 56.87899917413543\n ],\n [\n -155.423583984375,\n 56.87899917413543\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"86","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631c9e4b039675d00a3e8","contributors":{"authors":[{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":588396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reisenbichler, R.R.","contributorId":77356,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":588397,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Emlen, J.M.","contributorId":63979,"corporation":false,"usgs":true,"family":"Emlen","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":588398,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilmot, R.L.","contributorId":97662,"corporation":false,"usgs":true,"family":"Wilmot","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":588399,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Finn, J.E.","contributorId":8795,"corporation":false,"usgs":true,"family":"Finn","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":588400,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70162107,"text":"70162107 - 1988 - Neutralizing monoclonal antibodies recognize antigenic variants among isolates of infectious hematopoietic necrosis virus","interactions":[],"lastModifiedDate":"2023-12-08T01:37:04.467736","indexId":"70162107","displayToPublicDate":"2015-09-22T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1396,"text":"Diseases of Aquatic Organisms","active":true,"publicationSubtype":{"id":10}},"title":"Neutralizing monoclonal antibodies recognize antigenic variants among isolates of infectious hematopoietic necrosis virus","docAbstract":"eutralizing monoclonal antibodies were developed against strains of infectious hematopoietic necrosis virus (IHNV) from steelhead trout Salmo gairdneri in the Deschutes River of Oregon, chinook salmon Oncorhynchus tshawytscha in the Sacramento River of California, and rainbow trout Salmo gairdneri reared in the Hagerman Valley of Idaho, USA. These antibodies were tested for neutralization of 12 IHNV isolates obtained from salmonids in Japan, Alaska, Washington, Oregon, California, and Idaho. The antibodies recognized antigenic variants among the isolates and could be used to separate the viruses into 4 groups. The members of each group tended to be related by geographic area rather than by source host species, virulence, or date of isolation.
","language":"English","publisher":"Inter-Research","doi":"10.3354/DAO004199","usgsCitation":"Winton, J., Arakawa, C., Lannan, C., and Fryer, J.L., 1988, Neutralizing monoclonal antibodies recognize antigenic variants among isolates of infectious hematopoietic necrosis virus: Diseases of Aquatic Organisms, v. 4, p. 199-204, https://doi.org/10.3354/DAO004199.","productDescription":"6 p.","startPage":"199","endPage":"204","numberOfPages":"6","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314268,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5697833fe4b039675d00a6f3","contributors":{"authors":[{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":588562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arakawa, C.N.","contributorId":152171,"corporation":false,"usgs":false,"family":"Arakawa","given":"C.N.","email":"","affiliations":[],"preferred":false,"id":588563,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lannan, C.N.","contributorId":152142,"corporation":false,"usgs":false,"family":"Lannan","given":"C.N.","email":"","affiliations":[],"preferred":false,"id":588564,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fryer, J. L.","contributorId":21900,"corporation":false,"usgs":true,"family":"Fryer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588565,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70162043,"text":"70162043 - 1988 - Selection to increase survival of smolts in four successive broods of coho salmon","interactions":[],"lastModifiedDate":"2016-01-12T13:12:11","indexId":"70162043","displayToPublicDate":"2015-09-14T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Selection to increase survival of smolts in four successive broods of coho salmon","docAbstract":"Survival from smolt to adult for full and half-sib families of coho salmon Oncorhynchus kisutch was used to identify families with the highest survival rates at Big Creek Salmon Hatchery in Oregon. Adult fish from families with high survival were bred selectively for four consecutive generations in an attempt to increase smolt survival. A significant improvement in survival in the select line compared to the control after two generations of selection was not maintained in subsequent generations. We concluded that selection was not an effective method for increasing survival of smolts released at Big Creek Hatchery.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1988)117<0090:NSTISO>2.3.CO;2","usgsCitation":"McIntyre, J., Hemmingsen, A., and Simon, R., 1988, Selection to increase survival of smolts in four successive broods of coho salmon: Transactions of the American Fisheries Society, v. 117, no. 1, p. 90-92, https://doi.org/10.1577/1548-8659(1988)117<0090:NSTISO>2.3.CO;2.","productDescription":"3 p.","startPage":"90","endPage":"92","numberOfPages":"3","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314222,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631cce4b039675d00a3f4","contributors":{"authors":[{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":588393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hemmingsen, A.R.","contributorId":84313,"corporation":false,"usgs":true,"family":"Hemmingsen","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":588394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simon, R.C.","contributorId":34454,"corporation":false,"usgs":true,"family":"Simon","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":588395,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162028,"text":"70162028 - 1988 - Effects of variation in flow on distribution of northern squawfish (Ptychocheilus oregonensis) below McNary Dam on the Columbia River","interactions":[],"lastModifiedDate":"2016-01-12T10:24:57","indexId":"70162028","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Effects of variation in flow on distribution of northern squawfish (Ptychocheilus oregonensis) below McNary Dam on the Columbia River","docAbstract":"The movements of 23 northern Squawfish Ptychocheilus oregonensis were monitored by radiotelemetry below a Columbia River hydroelectric dam during the out-migration of juvenile anadromous salmonids in 1984 and 1985. The work was done as part of a study to relate predator abundances and distribution to juvenile salmonid mortalities associated with dams. Northern Squawfish remained in protected shoreline areas in spring and early summer, when discharge rates were high, but moved close to the dam and the juvenile bypass outflow area in mid to late summer, when discharge rates were low. Trends in northern Squawfish movements were similar during abrupt changes in discharge rate. During short-term closures of the spillway, when flow patterns were abruptly changed, four of five northern Squawfish moved out of protected areas and into the main river channel. Surface water velocities at 81 locations occupied by radio-tagged northern Squawfish in June to August 1985 ranged from 0 to 70 cm/s (mean, 24.5 cm/s). No preference within this range was evident, but the fish seemingly avoided areas of high current velocity, because they did not move into a substantial portion of the tailrace where water velocities exceeded 100 cm/s. Modification of structures to maintain high water velocities around bypass outflow areas should reduce potential predation on juvenile salmonids by northern squawfish.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8675(1988)008<0030:EOVIFO>2.3.CO;2","usgsCitation":"Faler, M., Miller, L., and Welke, K., 1988, Effects of variation in flow on distribution of northern squawfish (Ptychocheilus oregonensis) below McNary Dam on the Columbia River: North American Journal of Fisheries Management, v. 8, no. 1, p. 30-35, https://doi.org/10.1577/1548-8675(1988)008<0030:EOVIFO>2.3.CO;2.","productDescription":"6 p.","startPage":"30","endPage":"35","numberOfPages":"6","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314211,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River, Mcnary Dam","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.958740234375,\n 46.01985337287634\n ],\n [\n -123.519287109375,\n 45.867062714815475\n ],\n [\n -122.904052734375,\n 45.583289756006316\n ],\n [\n -122.178955078125,\n 45.32897866218559\n ],\n [\n -121.79443359375,\n 45.359865333959746\n ],\n [\n -119.86083984375,\n 45.55252525134013\n ],\n [\n -118.94897460937499,\n 45.87471224890479\n ],\n [\n -118.94897460937499,\n 46.027481852486645\n ],\n [\n -119.06982421874999,\n 46.20264638061019\n ],\n [\n -119.88281249999999,\n 46.00459325574482\n ],\n [\n -121.28906250000001,\n 45.82879925192134\n ],\n [\n -122.574462890625,\n 45.767522962149904\n ],\n [\n -122.794189453125,\n 46.24824991289166\n ],\n [\n -123.64013671874999,\n 46.437856895024225\n ],\n [\n -124.1455078125,\n 46.50595444552051\n ],\n [\n -123.958740234375,\n 46.01985337287634\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631c8e4b039675d00a3d7","contributors":{"authors":[{"text":"Faler, M.P.","contributorId":152178,"corporation":false,"usgs":false,"family":"Faler","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":588371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, L.M.","contributorId":16245,"corporation":false,"usgs":true,"family":"Miller","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":588372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welke, K.I.","contributorId":68496,"corporation":false,"usgs":true,"family":"Welke","given":"K.I.","email":"","affiliations":[],"preferred":false,"id":588373,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70159105,"text":"70159105 - 1988 - Land cover mapping of the upper Kuskokwim Resource Managment Area using LANDSAT and a digital data base approach","interactions":[],"lastModifiedDate":"2022-04-13T13:43:31.46543","indexId":"70159105","displayToPublicDate":"2015-07-20T12:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Land cover mapping of the upper Kuskokwim Resource Managment Area using LANDSAT and a digital data base approach","docAbstract":"Digital land cover and terrain data for the Upper Kuskokwim Resource Hanagement Area (UKRMA) were produced by the U.S. Geological Survey, Earth Resources Observation Systems Field Office, Anchorage, Alaska for the Bureau of Land Management. These and other environmental data, were incorporated into a digital data base to assist in the management and planning of the UKRMA. The digital data base includes land cover classifications, elevation, slope, and aspect data centering on the UKRMA boundaries. The data are stored on computer compatible tapes at a 50-m pixel size. Additional digital data in the data base include: (a) summer and winter Landsat multispectral scanner (MSS) data registered to a 50-m Universal Transverse Mercator grid; (b) elevation, slope, aspect, and solar illumination data; (c) soils and surficial geology; and (e) study area boundary. The classification of Landsat MSS data resulted in seven major classes and 24 subclasses. Major classes include: forest, shrubland, dwarf scrub, herbaceous, barren, water, and other. The final data base will be used by resource personnel for management and planning within the UKRMA.
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Robbins","contributorId":57497,"corporation":false,"usgs":true,"family":"Church","given":"M.","email":"","middleInitial":"Robbins","affiliations":[],"preferred":false,"id":573298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gebert, Warren A. wagebert@usgs.gov","contributorId":1546,"corporation":false,"usgs":true,"family":"Gebert","given":"Warren","email":"wagebert@usgs.gov","middleInitial":"A.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":573299,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Graczyk, David J.","contributorId":107265,"corporation":false,"usgs":true,"family":"Graczyk","given":"David J.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":573300,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Krug, William R.","contributorId":53381,"corporation":false,"usgs":true,"family":"Krug","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":573301,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70042384,"text":"pp1386 - 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Glaciers of Alaska"},"predicate":"IS_PART_OF","object":{"id":70042384,"text":"pp1386 - 1988 - Satellite image atlas of glaciers of the world","indexId":"pp1386","publicationYear":"1988","noYear":false,"title":"Satellite image atlas of glaciers of the world"},"id":8},{"subject":{"id":98690,"text":"pp1386F - 2010 - Glaciers of Asia","indexId":"pp1386F","publicationYear":"2010","noYear":false,"chapter":"F","title":"Glaciers of Asia"},"predicate":"IS_PART_OF","object":{"id":70042384,"text":"pp1386 - 1988 - Satellite image atlas of glaciers of the world","indexId":"pp1386","publicationYear":"1988","noYear":false,"title":"Satellite image atlas of glaciers of the world"},"id":9},{"subject":{"id":70043298,"text":"pp1386A - 2012 - State of the Earth’s cryosphere at the beginning of the 21st century: Glaciers, global snow cover, floating ice, and permafrost and periglacial environments","indexId":"pp1386A","publicationYear":"2012","noYear":false,"chapter":"A","title":"State of the Earth’s cryosphere at the beginning of the 21st century: Glaciers, global snow cover, floating ice, and permafrost and periglacial environments"},"predicate":"IS_PART_OF","object":{"id":70042384,"text":"pp1386 - 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Chapter A provides a comprehensive, yet concise, review of the \"State of the Earth's Cryosphere at the Beginning of the 21st Century: Glaciers, Global Snow Cover, Floating Ice, and Permafrost and Periglacial Environments,\" and a \"Map/Poster of the Earth's Dynamic Cryosphere,\" and a set of eight \"Supplemental Cryosphere Notes\" about the Earth's Dynamic Cryosphere and the Earth System. The next 10 chapters, B through K, are arranged geographically and present glaciological information from Landsat and other sources of historic and modern data on each of the geographic areas. Chapter B covers Antarctica; Chapter C, Greenland; Chapter D, Iceland; Chapter E, Continental Europe (except for the European part of the former Soviet Union), including the Alps, the Pyrenees, Norway, Sweden, Svalbard (Norway), and Jan Mayen (Norway); Chapter F, Asia, including the European part of the former Soviet Union, China, Afghanistan, Pakistan, India, Nepal, and Bhutan; Chapter G, Turkey, Iran, and Africa; Chapter H, Irian Jaya (Indonesia) and New Zealand; Chapter I, South America; Chapter J, North America (excluding Alaska); and Chapter K, Alaska. Chapters A–D each include map plates.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1386","usgsCitation":"1988, Satellite image atlas of glaciers of the world: U.S. Geological Survey Professional Paper 1386, Chapters A-K, https://doi.org/10.3133/pp1386.","productDescription":"Chapters A-K","additionalOnlineFiles":"Y","costCenters":[{"id":320,"text":"Glacier Studies Project","active":false,"usgs":true}],"links":[{"id":267198,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1386.png"},{"id":265317,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/p1386/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511a2115e4b084e2824d6997","contributors":{"editors":[{"text":"Williams, Richard S. Jr.","contributorId":17355,"corporation":false,"usgs":true,"family":"Williams","given":"Richard S.","suffix":"Jr.","affiliations":[],"preferred":false,"id":509152,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Ferrigno, Jane G. jferrign@usgs.gov","contributorId":39825,"corporation":false,"usgs":true,"family":"Ferrigno","given":"Jane","email":"jferrign@usgs.gov","middleInitial":"G.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":509151,"contributorType":{"id":2,"text":"Editors"},"rank":2}]}} ,{"id":70006540,"text":"70006540 - 1988 - Assessment of sea lamprey (Petromyzon marinus) predation by recovery of dead lake trout (Salvelinus namaycush) from Lake Ontario, 1982-85","interactions":[],"lastModifiedDate":"2016-03-21T14:00:13","indexId":"70006540","displayToPublicDate":"2012-07-06T13:36:00","publicationYear":"1988","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":"Assessment of sea lamprey (Petromyzon marinus) predation by recovery of dead lake trout (Salvelinus namaycush) from Lake Ontario, 1982-85","docAbstract":"During 1982-85, 89 dead lake trout (Salvelinus namaycush) were recovered with bottom trawls in U.S. waters of Lake Ontario: 28 incidentally during four annual fish-stock assessment surveys and 61 during fall surveys for dead fish. During the assessment surveys, no dead lake trout were recovered in April-June, one was recovered in August, and 27 were recovered in October or November, implying that most mortality from causes other than fishing occurred in the fall. The estimated numbers of dead lake trout between the 30- and 100-m depth contours in U.S. waters ranged from 16 000 (0.08 carcass/ha) in 1983 to 94 000 (0.46 carcass/ha) in 1982. Of 76 carcasses fresh enough to enable recognition of sea lamprey (Petromyzon marinus) wounds, 75 bore fresh wounds. Assuming that sea lamprey wounding rates on dead fish were the same as on live ones of the same length range (430-740 mm), the probability of 75 of the 76 dead lake trout bearing sea lamprey wounds was 3.5 x 10-63 if death was independent of sea lamprey attack, thus strongly implicating sea lampreys as the primary cause of death of fish in the sample. The recovery of only one unwounded dead lake trout also suggested that natural mortality from causes other than sea lamprey attactks is negligible.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f88-164","usgsCitation":"Bergstedt, R.A., and Schneider, C.P., 1988, Assessment of sea lamprey (Petromyzon marinus) predation by recovery of dead lake trout (Salvelinus namaycush) from Lake Ontario, 1982-85: Canadian Journal of Fisheries and Aquatic Sciences, v. 45, no. 8, p. 1406-1410, https://doi.org/10.1139/f88-164.","productDescription":"5 p.","startPage":"1406","endPage":"1410","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":259083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lake Ontario","volume":"45","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ee51e4b0c8380cd49cd1","contributors":{"authors":[{"text":"Bergstedt, Roger A. rbergstedt@usgs.gov","contributorId":4174,"corporation":false,"usgs":true,"family":"Bergstedt","given":"Roger","email":"rbergstedt@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, Clifford P.","contributorId":45251,"corporation":false,"usgs":true,"family":"Schneider","given":"Clifford","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":354714,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006741,"text":"70006741 - 1988 - Characterization of an avian cholera epizootic in wild birds in western Nebraska","interactions":[],"lastModifiedDate":"2023-01-12T12:17:53.852885","indexId":"70006741","displayToPublicDate":"2012-01-01T15:47:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":948,"text":"Avian Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of an avian cholera epizootic in wild birds in western Nebraska","docAbstract":"Avian cholera killed an estimated 2500 birds in western Nebraska and eastern Wyoming from 28 November 1985 to late January 1986. Wild mallards (Anas platyrhynchos) suffered the most losses. Other wild waterfowl, wild turkeys (Meleagris gallopavo), a few domestic fowl, and a bald eagle (Haliaeetus leucocephalus) also died. Pasteurella multocida serotype 1 was the predominant isolate from these carcasses. Cold, wet weather persisted throughout the outbreak, but daily losses in the flock of 50,000 mallards using the area were low. Pasteurella multocida was isolated from nasal swabs of 35 of 37 cattle from a feedlot in which many of these mallards were feeding. Eighty percent of the cattle isolates had antigenic characteristics of serotype 3 or serotype 3 with cross-reactivity. Isolates from wild mallards, wild turkeys, and the bald eagle were virulent to game-farm mallards when inoculated subcutaneously, but P. multocida isolates from cattle were not.
","language":"English","publisher":"American Association of Avian Pathologists","doi":"10.2307/1590960","usgsCitation":"Windingstad, R.M., Kerr, S., Duncan, R.M., and Brand, C.J., 1988, Characterization of an avian cholera epizootic in wild birds in western Nebraska: Avian Diseases, v. 32, no. 1, p. 124-131, https://doi.org/10.2307/1590960.","productDescription":"8 p.","startPage":"124","endPage":"131","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":259814,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska, 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","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","usgsCitation":"Starliper, C.E., and Schill, W.B., 1988, Uniformity of Edwardsiella ictaluri isolates is corroborated by genetic analysis: Research Information Bulletin 82, 2 p.","productDescription":"2 p.","startPage":"1","endPage":"2","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc81e4b08c986b328c7e","contributors":{"authors":[{"text":"Starliper, C. E.","contributorId":59739,"corporation":false,"usgs":true,"family":"Starliper","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":355189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schill, W. B.","contributorId":60146,"corporation":false,"usgs":true,"family":"Schill","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":355190,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006985,"text":"70006985 - 1988 - Current status of Rudd in the United States","interactions":[],"lastModifiedDate":"2012-07-14T01:01:39","indexId":"70006985","displayToPublicDate":"2012-01-01T13:05:01","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":284,"text":"Research Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"37","title":"Current status of Rudd in the United States","docAbstract":"No abstract available at this time.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","usgsCitation":"Williams, J., and Jennings, D., 1988, Current status of Rudd in the United States: Research Information Bulletin 37, 2 p.","productDescription":"2 p.","startPage":"1","endPage":"2","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd13e4b0c8380cd4e608","contributors":{"authors":[{"text":"Williams, J.","contributorId":76270,"corporation":false,"usgs":true,"family":"Williams","given":"J.","affiliations":[],"preferred":false,"id":355618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jennings, D.","contributorId":15054,"corporation":false,"usgs":true,"family":"Jennings","given":"D.","email":"","affiliations":[],"preferred":false,"id":355617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70039037,"text":"70039037 - 1988 - United States Geological Survey Yearbook, fiscal year 1987","interactions":[],"lastModifiedDate":"2017-03-08T16:13:58","indexId":"70039037","displayToPublicDate":"2012-01-01T12:16:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1987","docAbstract":"The fiscal year 1987 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039037","issn":"0892-3442","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, United States Geological Survey Yearbook, fiscal year 1987: Yearbook, x, 174 p., https://doi.org/10.3133/70039037.","productDescription":"x, 174 p.","costCenters":[],"links":[{"id":261279,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039037/report.pdf","text":"Report","size":"62.37 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":261280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039037/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc95e4b08c986b328d0d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70014102,"text":"70014102 - 1988 - The origin of summit basins on the Aleutian Ridge: Implications for block rotation of an arc massif","interactions":[],"lastModifiedDate":"2025-09-10T16:46:06.414234","indexId":"70014102","displayToPublicDate":"2010-07-26T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"The origin of summit basins on the Aleutian Ridge: Implications for block rotation of an arc massif","docAbstract":"It is proposed that many summit basins along the Aleutian Arc form from the clockwise rotation of blocks of the arc massif. Summit basins are arc-parallel grabens or half-grabens formed within the arc massif and are commonly located near or along the axis of late Cenozoic volcanism. Geomorphically, the Aleutian Arc appears to consist of contiguous rhombic blocks of varying size, tens to hundreds of kilometers in length. The boundaries between adjacent blocks are delineated by fault-controlled canyons that cut the southern slope of the arc transverse to its regional trend. Evidence that these blocks have rotated clockwise is provided by the triangular-shaped summit basins bordering the blocks to the north, oblique physiographic trends, offsets in the summit platform, and broad deflections in the southern slope of the arc. We present a model for block rotation that involves translation of blocks parallel to an arc. It is suggested that block rotation, which appears to have accelerated in late Cenozoic time, is linked to (1) a shift in the Euler pole for the Pacific plate, (2) the consequential start-up of late Cenozoic volcanism, (3) improved interplate coupling instigated by sediment flooding of the Aleutian Trench, and (4) westward subduction of northeast striking segments of the inactive Kula-Pacific Ridge.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TC007i002p00327","issn":"02787407","usgsCitation":"Geist, E., Childs, J., and Scholl, D., 1988, The origin of summit basins on the Aleutian Ridge: Implications for block rotation of an arc massif: Tectonics, v. 7, no. 2, p. 327-341, https://doi.org/10.1029/TC007i002p00327.","productDescription":"15 p.","startPage":"327","endPage":"341","costCenters":[],"links":[{"id":226066,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Ridge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -182.82659819331917,\n 56.878412454140914\n ],\n [\n -182.82659819331917,\n 50.315460649064136\n ],\n [\n -159.4163666014261,\n 50.315460649064136\n ],\n [\n -159.4163666014261,\n 56.878412454140914\n ],\n [\n -182.82659819331917,\n 56.878412454140914\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"7","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"505bae6ee4b08c986b3240c6","contributors":{"authors":[{"text":"Geist, E.L. 0000-0003-0611-1150","orcid":"https://orcid.org/0000-0003-0611-1150","contributorId":71993,"corporation":false,"usgs":true,"family":"Geist","given":"E.L.","affiliations":[],"preferred":false,"id":367577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Childs, J.R.","contributorId":63011,"corporation":false,"usgs":true,"family":"Childs","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":367576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scholl, D.W.","contributorId":106461,"corporation":false,"usgs":true,"family":"Scholl","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":367578,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70014392,"text":"70014392 - 1988 - Tectonics of formation, translation, and dispersal of the Coast Range ophiolite of California","interactions":[],"lastModifiedDate":"2025-09-09T17:03:23.83655","indexId":"70014392","displayToPublicDate":"2010-07-26T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Tectonics of formation, translation, and dispersal of the Coast Range ophiolite of California","docAbstract":"Data from the Coast Range ophiolite and its tectonic outliers in the northern California Coast Ranges suggest that the lower part of the ophiolite formed 169 to 163 Ma in a forearc or back arc setting at equatorial latitudes. Beginning about 156 Ma and continuing until 145 Ma, arc magmatism was superimposed on the ophiolite, and concurrently, a transform developed along the arc axis or in the back arc area. Rapid northward translation of this rifted active magmatic arc to middle latitudes culminated in its accretion to the California margin of North America at about 145 Ma. This Late Jurassic episode of translation, arc magmatism, and accretion coincided with the Nevadan orogeny and a proposed major plate reorganization in the eastern Pacific basin. The high rate of poleward motion necessary to translate the Coast Range ophiolite to middle latitudes during this time implies that the ophiolite traveled north on a fast-moving plate of the eastern Pacific basin, here termed plate X. Plate X probably was driven by a cryptic ridge east-northeast of the Pacific-Farallon-Izanagi ridge triple junction. Structural relations indicate that following Late Jurassic time, parts of the Coast Range ophiolite were displaced from the west side of the Great Valley province and incorporated into the Central belt of the Franciscan Complex along steep-dipping to low-angle reverse faults having dominant components of dextral shear. A northwest trending eastern zone of these right-laterally displaced outliers shows strong affinities to the main Coast Range ophiolite of the northwestern Sacramento Valley (the Elder Creek terrane), in that the outliers include ophiolitic breccias of Oxfordian to Kimmeridgian age. A southwestern zone of outliers lacks ophiolitic breccia and instead includes latest Oxfordian or Kimmeridgian to Tithonian, arc-derived volcanic rocks like those found in the Del Puerto and Stanley Mountain terranes of the main ophiolite. Whereas outliers of the northeastern outlier zone are right-laterally displaced no more than 260 km from the western side of the Sacramento Valley, outliers of the southwestern zone are displaced a minimum of 169 to 249 km. This displacement occurred between about 60 and 52 Ma. Ophiolitic rocks in the Decatur terrane of western Washington that have recently been correlated with the Coast Range ophiolite and the Great Valley sequence of California were apparently displaced at least 950 to 1200 km from the west side of the Great Valley between early Tertiary and Early Cretaceous time. Derived rates of northward translation for the ophiolite outliers in California are in the range of 1 to 4 cm/yr. Rates for the Decatur terrane are in the range of 2.5 to 4 cm/yr if translation was initiated 90 Ma, but as much as 11.9 to 15 cm/yr if it was not initiated until 60 Ma. The lower rates for the Decatur terrane are consistent with the rates derived for the California outliers and with the northward component of relative motion between the Farallon and North American plates from 90 to 50 Ma. The higher rates require northward transport on the Kula plate or on a fast-moving microplate. The higher translation rates derived for the Decatur terrane are also consistent with paleomagnetically determined rates for some limestones of the Central belt. This may indicate that outliers of the Coast Range ophiolite dispersed in the Central belt of the Franciscan Complex record only part of the total displacement which occurred along the Late Cretaceous to early Tertiary western margin of North America.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TC007i005p01033","issn":"02787407","usgsCitation":"McLaughlin, R.J., Blake, M., Griscom, A., Blome, C., and Murchey, B., 1988, Tectonics of formation, translation, and dispersal of the Coast Range ophiolite of California: Tectonics, v. 7, no. 5, p. 1033-1056, https://doi.org/10.1029/TC007i005p01033.","productDescription":"24 p.","startPage":"1033","endPage":"1056","costCenters":[],"links":[{"id":225705,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.45708685149472,\n 42.02344524262293\n ],\n [\n -124.45708685149472,\n 37.3366369809728\n ],\n [\n -121.5401474278405,\n 37.3366369809728\n ],\n [\n -121.5401474278405,\n 42.02344524262293\n ],\n [\n -124.45708685149472,\n 42.02344524262293\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"7","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"505ba48ae4b08c986b320403","contributors":{"authors":[{"text":"McLaughlin, R. J. 0000-0002-4390-2288","orcid":"https://orcid.org/0000-0002-4390-2288","contributorId":107271,"corporation":false,"usgs":true,"family":"McLaughlin","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":368295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blake, M.C. Jr.","contributorId":27094,"corporation":false,"usgs":true,"family":"Blake","given":"M.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":368292,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Griscom, A.","contributorId":80018,"corporation":false,"usgs":true,"family":"Griscom","given":"A.","email":"","affiliations":[],"preferred":false,"id":368294,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blome, C.D.","contributorId":60647,"corporation":false,"usgs":true,"family":"Blome","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":368293,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murchey, B.","contributorId":11772,"corporation":false,"usgs":true,"family":"Murchey","given":"B.","email":"","affiliations":[],"preferred":false,"id":368291,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70014173,"text":"70014173 - 1988 - The Goodman swell: A lithospheric flexure caused by crustal loading along the midcontinent rift system","interactions":[],"lastModifiedDate":"2025-09-10T15:40:44.542471","indexId":"70014173","displayToPublicDate":"2010-07-26T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"The Goodman swell: A lithospheric flexure caused by crustal loading along the midcontinent rift system","docAbstract":"Rb-Sr biotite ages of Archean and Early to Middle Proterozoic crystalline rocks in northern Wisconsin and adjacent Upper Peninsula of Michigan describe a regionally systematic pattern related to differential uplift. An “age low” occurs in northern Wisconsin where values range from 1070–1172 Ma for rocks with crystallization ages of 1760 to 1865 Ma. These values overlap with the main episode of mafic igneous activity (1090 to 1120 Ma) along the Midcontinent rift system (MRS). We interpret these low biotite ages as registering closure due to cooling below the 300°C isotherm as a consequence of uplift and rapid erosion of an area that we are informally naming the Goodman swell. The position of the Goodman swell is independent of the Archean and Early Proterozoic regional geologic framework but closely linked with the curvilinear (concave to the south) MRS. We interpret the swell to be a forebulge imposed on an elastic crust by loading of mafic igneous rocks along and within the axis of the MRS. The southward concavity of load axes resulted in flexural interaction that localized the swell. Because of rapid uplift the swell may have been a source area for clastic sediments in the rift sequence.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TC007i005p01077","issn":"02787407","usgsCitation":"Peterman, Z.E., and Sims, P., 1988, The Goodman swell: A lithospheric flexure caused by crustal loading along the midcontinent rift system: Tectonics, v. 7, no. 5, p. 1077-1090, https://doi.org/10.1029/TC007i005p01077.","productDescription":"14 p.","startPage":"1077","endPage":"1090","costCenters":[],"links":[{"id":225361,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Lake Superior","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -93.66942415908665,\n 48.81927797346091\n ],\n [\n -93.66942415908665,\n 46.19811413087436\n ],\n [\n -83.85490696495197,\n 46.19811413087436\n ],\n [\n -83.85490696495197,\n 48.81927797346091\n ],\n [\n -93.66942415908665,\n 48.81927797346091\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"7","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"505ba760e4b08c986b32151a","contributors":{"authors":[{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":367774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":367773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70014354,"text":"70014354 - 1988 - Geologic structure of the northern New Caledonia ridge, as inferred from magnetic and gravity anomalies","interactions":[],"lastModifiedDate":"2025-09-10T15:32:25.430354","indexId":"70014354","displayToPublicDate":"2010-07-26T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Geologic structure of the northern New Caledonia ridge, as inferred from magnetic and gravity anomalies","docAbstract":"Bathymetric, gravity, and magnetic data collected in the southwest Pacific Ocean over the northern New Caledonia ridge show that the main geological units known from the island of New Caledonia extend northward from this island, beneath the Grand Lagon Nord, the Grand Passage, and the d'Entrecasteaux reefs. These data support the model of tectonic evolution of the New Caledonia region proposed by Kroenke [1984]. We interpret a linear axial gravity low that extends from southern New Caledonia to the Grand Passage as evidence for the continuity of the thick pre-Permian to Jurassic core of the island. The Belep magnetic pattern, which covers the southwestern half of the Grand Lagon Nord, shows linear, high relief (1000–2000 nT) anomalies that are locally associated with a 120-mGal gravity high. These magnetic and gravity anomalies resemble anomalies measured over the west coast of New Caledonia, suggesting that the Cretaceous to Eocene basaltic complex of the coastal area is overlain by ophiolite remnants as far north as the western d'Entrecasteaux reefs. The similarity between the Belep magnetic pattern and a highly magnetic province evident 200 km southwest across the New Caledonia basin, along the Fairway ridge, indicates that volcanic rocks lie symmetrically on both sides of the New Caledonia basin. We suggest that part of these volcanic rocks were emplaced during the middle Cretaceous when the New Caledonia ridge rifted from the Australian margin. Simple gravity models of an elongated gravity high, having peak values in the range of +130 to +150 mGal, suggest that the ophiolite, which was thrust over New Caledonia during the Upper Eocene, extends along the east side of the Grand Lagon Nord and as far north as the d'Entrecasteaux reefs. Gravity and magnetic models suggest that in the area of the d'Entrecasteaux reefs, the ophiolite belt includes two subunits. The first subunit underlies the Huon-La Surprise platform and may include highly serpentinized ultramafic rocks without basaltic oceanic crust. The second subunit, which lies beneath the Guilbert ridge, may include ultramafic rocks as well as thin imbricate slices of oceanic crust. At the northern termination of the New Caledonia ridge, seismic and geopotential data evidence a major east-west trending tectonic zone that separates the basement of the New Caledonia ridge from the d'Entrecasteaux zone, an arcuate oceanic feature extending northward from the ridge. Differences in structure, geophysical signatures and morphology evident between areas north and those south of the Grand Passage, together with the nearness of the Le Noroit massif west of the Grand Passage, suggest that contemporaneously with Eocene to early Oligocene subduction along the western New Caledonia margin, an arc-ridge collision may have occurred near the northern termination of this subduction zone.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TC007i005p00991","issn":"02787407","usgsCitation":"Collot, J., Rigolot, P., and Missegue, F., 1988, Geologic structure of the northern New Caledonia ridge, as inferred from magnetic and gravity anomalies: Tectonics, v. 7, no. 5, p. 991-1013, https://doi.org/10.1029/TC007i005p00991.","productDescription":"23 p.","startPage":"991","endPage":"1013","costCenters":[],"links":[{"id":226083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"New Caledonia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 163.47203359037502,\n -19.65675118374793\n ],\n [\n 163.47203359037502,\n -23.02679639997224\n ],\n [\n 168.1838529120788,\n -23.02679639997224\n ],\n [\n 168.1838529120788,\n -19.65675118374793\n ],\n [\n 163.47203359037502,\n -19.65675118374793\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"7","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"505a21ebe4b0c8380cd56bd9","contributors":{"authors":[{"text":"Collot, J.-Y.","contributorId":39130,"corporation":false,"usgs":true,"family":"Collot","given":"J.-Y.","email":"","affiliations":[],"preferred":false,"id":368202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rigolot, P.","contributorId":98889,"corporation":false,"usgs":true,"family":"Rigolot","given":"P.","email":"","affiliations":[],"preferred":false,"id":368204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Missegue, F.","contributorId":75286,"corporation":false,"usgs":true,"family":"Missegue","given":"F.","email":"","affiliations":[],"preferred":false,"id":368203,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5224797,"text":"5224797 - 1988 - Population trends of the Purple Martin in North America, 1966-1986","interactions":[],"lastModifiedDate":"2012-02-02T00:15:06","indexId":"5224797","displayToPublicDate":"2010-06-16T12:19:06","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3211,"text":"Purple Martin Update","active":true,"publicationSubtype":{"id":10}},"title":"Population trends of the Purple Martin in North America, 1966-1986","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Purple Martin Update","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"6783_Sauer.pdf","usgsCitation":"Sauer, J., Klimkiewicz, M.K., and Droege, S., 1988, Population trends of the Purple Martin in North America, 1966-1986: Purple Martin Update, v. 1, no. 1, p. 4-6.","productDescription":"4-6","startPage":"4","endPage":"6","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683dd2","contributors":{"authors":[{"text":"Sauer, J.R. 0000-0002-4557-3019","orcid":"https://orcid.org/0000-0002-4557-3019","contributorId":66197,"corporation":false,"usgs":true,"family":"Sauer","given":"J.R.","affiliations":[],"preferred":false,"id":342709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klimkiewicz, M. K.","contributorId":53490,"corporation":false,"usgs":true,"family":"Klimkiewicz","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":342707,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Droege, Sam 0000-0003-4393-0403","orcid":"https://orcid.org/0000-0003-4393-0403","contributorId":64185,"corporation":false,"usgs":true,"family":"Droege","given":"Sam","affiliations":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":342708,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5224409,"text":"5224409 - 1988 - Effects of zinc smelter emissions on farms and gardens at Palmerton, PA","interactions":[],"lastModifiedDate":"2019-11-07T15:44:14","indexId":"5224409","displayToPublicDate":"2010-06-16T12:19:06","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3616,"text":"Trace Substances in Environmental Health","active":true,"publicationSubtype":{"id":10}},"title":"Effects of zinc smelter emissions on farms and gardens at Palmerton, PA","docAbstract":"In 1979, before the primary Zn smelter at Palmerton was closed due to excessive Zn and Cd emissions and change in the price of Zn, we were contacted by a local veterinarian regarding death of foals (young horses) on farms near the smelter. To examine whether Zn or Cd contamination of forage or soils could be providing potentially toxic levels of Zn or other elements in the diets of foals, we measured metals in forages, soils, and feces of grazing livestock on two farms near Palmerton. The farms were about 2.5 and about 10 km northeast of the East stack. Soils, forages, and feces were greatly increased in Zn and Cd. Soil, forage, and fecal Zn were near 1000 mg/kg and Cd, 10-20 mg/kg at farm A (2.5 km) compared to normal background levels of 43 mg Zn and 0.2 mg Cd/kg, respectively. Liver and kidney of cattle raised on Farm A were increased in Zn and Cd, indicating that at least part of the Zn and Cd in smelter contaminated forages was bioavailable. During the farm sampling, we obtained soil from one garden in Palmerton within 200 m of the primary (West) smelter. The Borough surrounds the smelter facility in a valley. Because soil Cd was near 100 mg/kg, we sampled garden soils and vegetables from over 40 gardens in 6 randomly selected blocks and in rural areas at different distances from the smelter during September, 1980. All homes were contacted on each sampled block. Nearly all homes had some garden, while at least 2 appeared to grow over 50% of their annual vegetable and potato consumption. Palmerton garden soils averaged 76 mg Cd/kg and 5830 mg Zn/kg. Gardeners had been taught to add limestone and organic fertilizers to counteract yield reduction and chlorosis due to the excessive soil Zn. Gardens with over 5000 mg Zn/kg were nearly allover pH 7, and many were calcareous. Because the smelter had not yet ceased operations in 1980, crops could have been polluted by aerosol Zn and Cd emitted by the smelter. Crop Zn and Cd were extremely high, about 100 times normal Cd levels. In more distant gardens, soil metals were not so high, and gardeners had not added as much limestone. Bean rotated with the potatoes and leafy vegetables often suffered chlorosis and visible yield reduction. Potatoes contained up to 6 mg Cd/kg dry wt. compared to backgrournd 0.20 mg/kg DW. An estimate of potential Zn and Cd intakes due to the contaminated crops was made using the teen-aged male diet model, and average Cd intakes would be 250 ug/day if diets contained 100% locally grown leafy and root vegetables and potatoes. Gardeners were warned to restrict consumption of garden grown leafy and root vegetables and potatoes, and to apply 22 T/A of limestone to restrict Cd uptake. Use of improved adult diet models, and increased understanding of the effect of Zn on Cd bioavailability indicate that little Cd risk may result from consuming garden vegetables grown at Palmerton. Individuals appear to be protected because Zn accompanied crop Cd, they grew only small amounts of vegetables in most cases, and aerosol pollution of crops has ceased. Reduced Zn emissions, and Cu supplementation have prevented further health effects on foals or cattle. Detailed examination of these risks is needed to develop remedial measures for both farms and gardens in the Zn + Cd polluted soils near Zn smelters at many locations in the United States and other countries. Remedial actions are necessarary to prevent chronic Zn toxicity to crops and livestock, and minimize the risk of chronic Cd toxicity to humans who consume locally grown garden crops.
","language":"English","usgsCitation":"Chaney, R.L., Beyer, W., Gifford, C., and Sileo, L., 1988, Effects of zinc smelter emissions on farms and gardens at Palmerton, PA: Trace Substances in Environmental Health, v. 22, p. 263-280.","productDescription":"18 p.","startPage":"263","endPage":"280","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":299697,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.researchgate.net/publication/236400202_Effects_of_zinc_smelter_emissions_on_farms_and_gardens_at_Palmerton_PA"}],"country":"United States","state":"Pennsylvania","city":"Palmerton","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.80703735351562,\n 40.725925340669626\n ],\n [\n -75.80909729003906,\n 40.72228267283148\n ],\n [\n -75.77407836914062,\n 40.686886382151116\n ],\n [\n -75.72807312011719,\n 40.72124187397379\n ],\n [\n -75.65322875976562,\n 40.74465591168391\n ],\n [\n -75.51864624023438,\n 40.7717018705776\n ],\n [\n -75.37513732910156,\n 40.80237530523985\n ],\n [\n -75.39985656738281,\n 40.83355409739852\n ],\n [\n -75.53924560546875,\n 40.842385424129375\n ],\n [\n -75.67176818847656,\n 40.80705305827059\n ],\n [\n -75.80703735351562,\n 40.725925340669626\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"22","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fb0c","contributors":{"authors":[{"text":"Chaney, R. L.","contributorId":81851,"corporation":false,"usgs":true,"family":"Chaney","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":341592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beyer, W. N. 0000-0002-8911-9141","orcid":"https://orcid.org/0000-0002-8911-9141","contributorId":55379,"corporation":false,"usgs":true,"family":"Beyer","given":"W. N.","affiliations":[],"preferred":false,"id":341591,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gifford, C.H.","contributorId":99934,"corporation":false,"usgs":true,"family":"Gifford","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":341593,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sileo, L.","contributorId":46895,"corporation":false,"usgs":true,"family":"Sileo","given":"L.","email":"","affiliations":[],"preferred":false,"id":341590,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5221948,"text":"5221948 - 1988 - MARKOV: A methodology for the solution of infinite time horizon MARKOV decision processes","interactions":[],"lastModifiedDate":"2012-02-02T00:14:36","indexId":"5221948","displayToPublicDate":"2010-06-16T12:19:06","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":848,"text":"Applied Stochastic Models and Data Analysis","active":true,"publicationSubtype":{"id":10}},"title":"MARKOV: A methodology for the solution of infinite time horizon MARKOV decision processes","docAbstract":"Algorithms are described for determining optimal policies for finite state, finite action, infinite discrete time horizon Markov decision processes. Both value-improvement and policy-improvement techniques are used in the algorithms. Computing procedures are also described. The algorithms are appropriate for processes that are either finite or infinite, deterministic or stochastic, discounted or undiscounted, in any meaningful combination of these features. Computing procedures are described in terms of initial data processing, bound improvements, process reduction, and testing and solution. Application of the methodology is illustrated with an example involving natural resource management. Management implications of certain hypothesized relationships between mallard survival and harvest rates are addressed by applying the optimality procedures to mallard population models.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Stochastic Models and Data Analysis","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/asm.3150040405","usgsCitation":"Williams, B.K., 1988, MARKOV: A methodology for the solution of infinite time horizon MARKOV decision processes: Applied Stochastic Models and Data Analysis, v. 4, no. 4, p. 253-271, https://doi.org/10.1002/asm.3150040405.","productDescription":"253-271","startPage":"253","endPage":"271","numberOfPages":"19","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":17888,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://dx.doi.org/10.1002/asm.3150040405","linkFileType":{"id":5,"text":"html"}},{"id":193793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-08-31","publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648b8e","contributors":{"authors":[{"text":"Williams, B. Kenneth","contributorId":107798,"corporation":false,"usgs":true,"family":"Williams","given":"B.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":335106,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220732,"text":"5220732 - 1988 - Organochlorine pesticides, polychlorinated biphenyls, and mercury in osprey eggs – 1970-79 – And their relationships to shell thinning and productivity","interactions":[],"lastModifiedDate":"2023-12-12T15:34:56.79531","indexId":"5220732","displayToPublicDate":"2010-06-16T12:19:06","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Organochlorine pesticides, polychlorinated biphenyls, and mercury in osprey eggs – 1970-79 – And their relationships to shell thinning and productivity","docAbstract":"Osprey (Pandion haliaetus) eggs were collected in 14 states in 1970–79 and analyzed for organochlorine pesticides, polychlorinated biphenyls (PCBs), and mercury. Moderate shell thinning occurred in eggs from several areas. DDE was detected in all eggs, PCBs in 99%, DDD in 96%, dieldrin in 52%, and other compounds less frequently. Concentrations of DDT and its metabolites declined in eggs from Cape May County, New Jersey between 1970–72 and 1978–79. Eggs from New Jersey in the early 1970s contained the highest concentrations of DDE. Dieldrin concentrations declined in eggs from the Potomac River, Maryland during 1971–77. Five different contaminants were significantly negatively correlated with shell thickness; DDE was most closely correlated. Ten percent shell thinning was associated with 2.0 ppm DDE, 15% with 4.2 ppm, and 20% with 8.7 ppm in eggs collected from randomly selected nests before egg loss. Shell thickness could not be accurately predicted from DDE concentrations in eggs collected after failure to hatch, presumably because the eggs with the thinnest shells had been broken and were unavailable for sampling. DDE was also significantly negatively correlated with brood size. Other contaminants did not appear to adversely affect shell thickness or reproductive success.
","language":"English","publisher":"Springer","doi":"10.1007/BF01061982","usgsCitation":"Wiemeyer, S.N., Bunck, C.M., and Krynitsky, A.J., 1988, Organochlorine pesticides, polychlorinated biphenyls, and mercury in osprey eggs – 1970-79 – And their relationships to shell thinning and productivity: Archives of Environmental Contamination and Toxicology, v. 17, no. 6, p. 767-787, https://doi.org/10.1007/BF01061982.","productDescription":"21 p.","startPage":"767","endPage":"787","numberOfPages":"21","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196454,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a825","contributors":{"authors":[{"text":"Wiemeyer, Stanley N.","contributorId":78279,"corporation":false,"usgs":true,"family":"Wiemeyer","given":"Stanley","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":332314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bunck, Christine M. cbunck@usgs.gov","contributorId":731,"corporation":false,"usgs":true,"family":"Bunck","given":"Christine","email":"cbunck@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":332312,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krynitsky, Alexander J.","contributorId":81542,"corporation":false,"usgs":true,"family":"Krynitsky","given":"Alexander","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":332313,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5220007,"text":"5220007 - 1988 - Host selection by the shiny cowbird","interactions":[],"lastModifiedDate":"2023-11-24T14:11:20.119884","indexId":"5220007","displayToPublicDate":"2010-06-16T12:19:06","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Host selection by the shiny cowbird","docAbstract":"Factors important in Shiny Cowbird (Molothrus bonariensis) host selection were examined within the mangrove community in Puerto Rico. Cowbirds did not parasitize birds in proportion to their abundance. The cowbird breeding season coincided with those of its major hosts, which were 'high-quality' foster species (i.e., species that fledge .gtoreq. 55% of cowbirds hatched: Yellow Warbler, Dendroica petechia; Yellow-shouldered Blackbird, Agelaius xanthomus; Black-whiskered Vireo, Vireo altiloquus; Black-cowled Oriole, Icterus dominicensis; Peurto Rican Flycatcher, Myiarchus antillarum; Troupial, Icterus icterus), and did not extend into other periods even though nests of 'low-quality: species (i.e., species that fledge < 55% of cowbird chicks that hatched: Bronze Mannikin, Lonchura cucullata; Greater Antillean Grackle, Quiscalus niger; Gray Kingbird, Tyrannus dominicensis; Northern Mockingbird, Mimus polyglottos; Red-legged Thrush, Turdus plumbeus) were available. Shiny Cowbird food habits and egg size were similar to those of their hosts, suggesting that cowbirds choose hosts partly on the basis of this combination. Cowbirds located host nests primarily by cryptically watching activities of birds in likely habitats. Other nest locating strategies were active searching of suitable habitat and 'flushing' of hosts by the cowbird's noisy approach. Cowbirds closely monitored nest status with frequent visits that peaked on the host's first day of egg laying. Hosts using covered nests (e.g., cavities, domed nests) were as vulnerable to cowbird parasitism as those building open nests.","language":"English","publisher":"Oxford Academic","doi":"10.2307/1368557","usgsCitation":"Wiley, J.W., 1988, Host selection by the shiny cowbird: Condor, v. 90, no. 2, p. 289-303, https://doi.org/10.2307/1368557.","productDescription":"15 p.","startPage":"289","endPage":"303","numberOfPages":"15","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":503141,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol90/iss2/1","text":"External Repository"},{"id":197781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"90","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880a1","contributors":{"authors":[{"text":"Wiley, J. W.","contributorId":51399,"corporation":false,"usgs":false,"family":"Wiley","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":331172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}