{"pageNumber":"4495","pageRowStart":"112350","pageSize":"25","recordCount":184769,"records":[{"id":70162019,"text":"70162019 - 1989 - Construction and emplacement of a large enclosure for rearing fish off-station","interactions":[],"lastModifiedDate":"2016-01-12T09:01:41","indexId":"70162019","displayToPublicDate":"2015-09-16T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Construction and emplacement of a large enclosure for rearing fish off-station","docAbstract":"

A 1.5-acre barrier net, used to enclose large numbers of juvenile Pacific salmon (Oncorhynchus spp.) for rearing in backwaters along the Columbia River, USA, is described. This type of enclosure may provide additional rearing options to fishery managers.

","language":"English","publisher":"Bureau of Fisheries, U.S. Department of Commerce","doi":"10.1577/1548-8640(1989)051<0052:CAEOAL>2.3.CO;2","usgsCitation":"Novotny, J., and Macy, T., 1989, Construction and emplacement of a large enclosure for rearing fish off-station: Progressive Fish-Culturist, v. 51, no. 1, p. 52-54, https://doi.org/10.1577/1548-8640(1989)051<0052:CAEOAL>2.3.CO;2.","productDescription":"3 p.","startPage":"52","endPage":"54","numberOfPages":"3","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631bee4b039675d00a3c9","contributors":{"authors":[{"text":"Novotny, J.F.","contributorId":95856,"corporation":false,"usgs":true,"family":"Novotny","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":588342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macy, T.L","contributorId":152168,"corporation":false,"usgs":false,"family":"Macy","given":"T.L","email":"","affiliations":[],"preferred":false,"id":588343,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161975,"text":"70161975 - 1989 - Animal population dynamics: Identification of critical components","interactions":[],"lastModifiedDate":"2016-01-11T12:39:56","indexId":"70161975","displayToPublicDate":"2015-09-16T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1458,"text":"Ecological Modelling","active":true,"publicationSubtype":{"id":10}},"title":"Animal population dynamics: Identification of critical components","docAbstract":"

There is a growing interest in the use of population dynamics models in environmental risk assessment and the promulgation of environmental regulatory policies. Unfortunately, because of species and areal differences in the physical and biotic influences on population dynamics, such models must almost inevitably be both complex and species- or site-specific. Given the emormous variety of species and sites of potential concern, this fact presents a problem; it simply is not possible to construct models for all species and circumstances. Therefore, it is useful, before building predictive population models, to discover what input parameters are of critical importance to the desired output. This information should enable the construction of simpler and more generalizable models. As a first step, it is useful to consider population models as composed to two, partly separable classes, one comprising the purely mechanical descriptors of dynamics from given demographic parameter values, and the other describing the modulation of the demographic parameters by environmental factors (changes in physical environment, species interactions, pathogens, xenobiotic chemicals). This division permits sensitivity analyses to be run on the first of these classes, providing guidance for subsequent model simplification. We here apply such a sensitivity analysis to network models of mammalian and avian population dynamics.

","language":"English","publisher":"Elselvier ","doi":"10.1016/0304-3800(89)90033-1","usgsCitation":"Emlen, J., and Pikitch, E., 1989, Animal population dynamics: Identification of critical components: Ecological Modelling, v. 44, no. 3-4, p. 253-273, https://doi.org/10.1016/0304-3800(89)90033-1.","productDescription":"21 p.","startPage":"253","endPage":"273","numberOfPages":"21","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314134,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e03be4b039675d005de5","contributors":{"authors":[{"text":"Emlen, J.M.","contributorId":63979,"corporation":false,"usgs":true,"family":"Emlen","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":588232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pikitch, E.K.","contributorId":152152,"corporation":false,"usgs":false,"family":"Pikitch","given":"E.K.","email":"","affiliations":[],"preferred":false,"id":588233,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70162016,"text":"70162016 - 1989 - Methods for developing new stocks of Atlantic salmon","interactions":[],"lastModifiedDate":"2016-01-11T15:25:30","indexId":"70162016","displayToPublicDate":"2015-09-15T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":8,"text":"Biological Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"89(12)","title":"Methods for developing new stocks of Atlantic salmon","docAbstract":"

The productivity of many streams in NewEngland for Atlantic salmon is being restored through abatement of water pollution and removal of barriers to migrating fish. As a result, interest is increasing in reestablishment of natural spawning runs of Atlantic salmon in some of these streams. I describe methods intended to help develop and maintain \"new\" stocks of these fish.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Atlantic Salmon Brood Stock Management and Breeding Handbook","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"U.S. Fish and Wildlife Service, 1989, Methods for developing new stocks of Atlantic salmon: Biological Report 89(12), 3 p.","productDescription":"3 p.","startPage":"19","endPage":"21","numberOfPages":"3","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314190,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e049e4b039675d005e37"} ,{"id":70161970,"text":"70161970 - 1989 - Terrestrial population models for ecological risk assessment: A state-of-the-art review","interactions":[],"lastModifiedDate":"2016-01-11T12:28:55","indexId":"70161970","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Terrestrial population models for ecological risk assessment: A state-of-the-art review","docAbstract":"

Few attempts have been made to formulate models for predicting impacts of xenobiotic chemicals on wildlife populations. However, considerable effort has been invested in wildlife optimal exploitation models. Because death from intoxication has a similar effect on population dynamics as death by harvesting, these management models are applicable to ecological risk assessment. An underlying Leslie-matrix bookkeeping formulation is widely applicable to vertebrate wildlife populations. Unfortunately, however, the various submodels that track birth, death, and dispersal rates as functions of the physical, chemical, and biotic environment are by their nature almost inevitably highly species- and locale-specific. Short-term prediction of one-time chemical applications requires only information on mortality before and after contamination. In such cases a simple matrix formulation may be adequate for risk assessment. But generally, risk must be projected over periods of a generation or more. This precludes generic protocols for risk assessment and also the ready and inexpensive predictions of a chemical's influence on a given population. When designing and applying models for ecological risk assessment at the population level, the endpoints (output) of concern must be carefully and rigorously defined. The most easily accessible and appropriate endpoints are (1) pseudoextinction (the frequency or probability of a population falling below a prespecified density), and (2) temporal mean population density. Spatial and temporal extent of predicted changes must be clearly specified a priori to avoid apparent contradictions and confusion.

","language":"English","publisher":"Wiley","doi":"10.1002/etc.5620080912","usgsCitation":"Emlen, J., 1989, Terrestrial population models for ecological risk assessment: A state-of-the-art review: Environmental Toxicology and Chemistry, v. 8, no. 9, p. 831-842, https://doi.org/10.1002/etc.5620080912.","productDescription":"12","startPage":"831","endPage":"842","numberOfPages":"12","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":479861,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/etc.5620080912","text":"Publisher Index Page"},{"id":314129,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314128,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://onlinelibrary.wiley.com/doi/10.1002/etc.5620080912/abstract"}],"volume":"8","issue":"9","noUsgsAuthors":false,"publicationDate":"1989-09-01","publicationStatus":"PW","scienceBaseUri":"5694e065e4b039675d005e96","contributors":{"authors":[{"text":"Emlen, J.M.","contributorId":63979,"corporation":false,"usgs":true,"family":"Emlen","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":588225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162286,"text":"70162286 - 1989 - Assessment of smolt condition for travel time analysis","interactions":[],"lastModifiedDate":"2016-01-20T11:46:21","indexId":"70162286","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":396,"text":"Annual Report","active":false,"publicationSubtype":{"id":9}},"title":" Assessment of smolt condition for travel time analysis","language":"English","publisher":"U.S. Fish and Wildlife Service, National Fishery Research Station","usgsCitation":"Rondorf, D., Beeman, J., Faler, J., Free, M., and Wagner, E., 1989, Assessment of smolt condition for travel time analysis: Annual Report, xvii, 120 p.","productDescription":"xvii, 120 p.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314518,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pisces.bpa.gov/release/documents/DocumentViewer.aspx?doc=35245-3","text":"pdf"}],"country":"United States","state":"Idaho, 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 -126.32080078124999,\n 42.114523952464246\n ],\n [\n -126.32080078124999,\n 49.36806633482156\n ],\n [\n -113.70849609375,\n 49.36806633482156\n ],\n [\n -113.70849609375,\n 42.114523952464246\n ],\n [\n -126.32080078124999,\n 42.114523952464246\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"Contract No. DE-A179-87BP35245\nProject No. 87-401","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a0bdb8e4b0961cf280dc06","contributors":{"authors":[{"text":"Rondorf, D.W.","contributorId":80789,"corporation":false,"usgs":true,"family":"Rondorf","given":"D.W.","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":589108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beeman, J.W.","contributorId":32646,"corporation":false,"usgs":true,"family":"Beeman","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":589109,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Faler, J.C.","contributorId":152382,"corporation":false,"usgs":false,"family":"Faler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":589110,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Free, M.E.","contributorId":152383,"corporation":false,"usgs":false,"family":"Free","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":589111,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wagner, E.J.","contributorId":152384,"corporation":false,"usgs":false,"family":"Wagner","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":589112,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70161953,"text":"70161953 - 1989 - Concentration of infectious hematopoietic necrosis virus from water samples by tangential flow filtration and polyethylene glycol precipitation","interactions":[],"lastModifiedDate":"2016-01-11T10:44:32","indexId":"70161953","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1989","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":"Concentration of infectious hematopoietic necrosis virus from water samples by tangential flow filtration and polyethylene glycol precipitation","docAbstract":"

Infectious hematopoietic necrosis virus (IHNV) was concentrated from water samples by polyethylene glycol (PEG) precipitation, tangential flow filtration (TFF), and by a combination of TFF followed by PEG precipitation of the retentate. Used alone, PEG increased virus titers more than 200-fold, and the efficiency of recovery was as great as 100%. Used alone, TFF concentrated IHNV more than 20-fold, and average recovery was 70%. When the two techniques were combined, 10-L water samples were reduced to about 300 mL by TFF and the virus was precipitated with PEG into a 1 to 2 g pellet; total recovery was as great as 100%. The combined techniques were used to isolate IHNV from water samples taken from a river containing adult sockeye salmon (Oncorhynchus nerka) and from a hatchery pond containing adult spring chinook salmon (O. tshawytscha). The combination of these methods was effective in concentrating and detecting IHNV from water containing only three infectious particles per 10-L sample.

","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f89-125","usgsCitation":"Batts, W., and Winton, J., 1989, Concentration of infectious hematopoietic necrosis virus from water samples by tangential flow filtration and polyethylene glycol precipitation: Canadian Journal of Fisheries and Aquatic Sciences, v. 46 , no. 6, p. 964-968, https://doi.org/10.1139/f89-125.","productDescription":"5 p.","startPage":"964","endPage":"968","numberOfPages":"5","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314106,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46 ","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e03fe4b039675d005e02","contributors":{"authors":[{"text":"Batts, W.N. 0000-0002-6469-9004","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":51043,"corporation":false,"usgs":true,"family":"Batts","given":"W.N.","affiliations":[],"preferred":false,"id":588184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":588185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161952,"text":"70161952 - 1989 - Development, characterization, and use of monoclonal and polyclonal antibodies against the myxosporean, Ceratomyxa shasta","interactions":[],"lastModifiedDate":"2016-01-11T10:41:13","indexId":"70161952","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2272,"text":"Journal of Eukaryotic Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Development, characterization, and use of monoclonal and polyclonal antibodies against the myxosporean, Ceratomyxa shasta","docAbstract":"

Both monoclonal and polyclonal antisera were produced against Ceratomyxa shasta. Ascites containing trophozoites of the parasite was collected from infected fish and used as antigen for immunization of mice. The resulting monoclonal antibodies reacted specifically with trophozoite and sporoblast stages but did not react with C. shasta spores by either indirect fluorescent antibody techniques or in Western blots. This indicates that some C. shasta antigens are specific to certain life stages of the parasite. Polyclonal antiserum was produced in a rabbit by injecting a spore protein electro-eluted from an SDS-polyacrylamide gel. This antiserum reacted with both trophozoites and spores by indirect fluorescent antibody techniques and in Western blots. All antisera were tested for cross-reactivity to trout white blood cells, a contaminant of the ascites, and to other myxosporea. Two monoclonal antibodies reacted with white blood cells and myxosporea of the genera Sphaerospora and Myxobilatus. One hybridoma produced antibodies of high specificity for C. shasta pre-spore stages. This is the first report of a monoclonal antibody produced against a myxosporean parasite.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1550-7408.1989.tb05534.x","usgsCitation":"Bartholomew, J.L., Rohovec, J., and Fryer, J.L., 1989, Development, characterization, and use of monoclonal and polyclonal antibodies against the myxosporean, Ceratomyxa shasta: Journal of Eukaryotic Microbiology, v. 36, no. 4, p. 397-401, https://doi.org/10.1111/j.1550-7408.1989.tb05534.x.","productDescription":"5 p.","startPage":"397","endPage":"401","numberOfPages":"5","costCenters":[],"links":[{"id":314105,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e040e4b039675d005e0b","contributors":{"authors":[{"text":"Bartholomew, J. L.","contributorId":91661,"corporation":false,"usgs":true,"family":"Bartholomew","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rohovec, J. S.","contributorId":95979,"corporation":false,"usgs":true,"family":"Rohovec","given":"J. S.","affiliations":[],"preferred":false,"id":588182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fryer, J. L.","contributorId":21900,"corporation":false,"usgs":true,"family":"Fryer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588183,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162284,"text":"70162284 - 1989 - Utility of spawner-recruit relations for evaluating the effect of degraded environment on the abundance of Chinook salmon, Oncorhynchus tshawytscha","interactions":[],"lastModifiedDate":"2016-01-20T11:31:04","indexId":"70162284","displayToPublicDate":"2015-08-11T00:00:00","publicationYear":"1989","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}},"subseriesTitle":"Canadian Special Publication of Fisheries and Aquatic Sciences Symposium 105","title":"Utility of spawner-recruit relations for evaluating the effect of degraded environment on the abundance of Chinook salmon, Oncorhynchus tshawytscha","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceeding of the National Workshop on Effects on Habitat Alterations on Salmonid Stocks","largerWorkSubtype":{"id":10,"text":"Journal Article"},"conferenceTitle":"National Workshop on Effects on Habitat Alterations on Salmonid Stocks","language":"English","publisher":"Department of Fisheries and Oceans","publisherLocation":"Ottawa, Canada","usgsCitation":"Reisenbichler, R., 1989, Utility of spawner-recruit relations for evaluating the effect of degraded environment on the abundance of Chinook salmon, Oncorhynchus tshawytscha: Canadian Journal of Fisheries and Aquatic Sciences, p. 21-32.","productDescription":"12 p.","startPage":"21","endPage":"32","numberOfPages":"12","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314515,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314514,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://recherche-search.gc.ca/rGs/s_r?st=s&s5bm3ts21rch=x&num=10&st1rt=0&langs=eng&cdn=dfo&q=+Proceeding+of+the+National+Workshop+on+Effects+on+Habitat+Alterations+on+Salmonid+Stocks"}],"edition":"Canadian Special Publication of Fisheries and Aquatic Sciences Symposium 105","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a0bddae4b0961cf280dc36","contributors":{"editors":[{"text":"Levings, C.D.","contributorId":152379,"corporation":false,"usgs":false,"family":"Levings","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":589100,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Holtby, L.B.","contributorId":152380,"corporation":false,"usgs":false,"family":"Holtby","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":589101,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Henderson, M.A.","contributorId":152381,"corporation":false,"usgs":false,"family":"Henderson","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":589102,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Reisenbichler, R.R.","contributorId":77356,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":589099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162024,"text":"70162024 - 1989 - Isolation of a reovirus from coho salmon (Oncorhynchus kisutch) in Oregon, USA","interactions":[],"lastModifiedDate":"2016-01-12T09:37:56","indexId":"70162024","displayToPublicDate":"2015-08-11T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Isolation of a reovirus from coho salmon (Oncorhynchus kisutch) in Oregon, USA","docAbstract":"

Reoviruses isolated from aquatic animals share certain common characteristics: (1) a typical reovirus-like morphology which shows an icosahedral particle with a double capsid that is approximately 75 nm in diameter; (2) a genome with eleven segments of double-stranded RNA (dsRNA) distributed as three large, three medium and five small segments with a total molecular weight of approximately 15 x 106; (3) a virion composed of five major and several minor structural proteins that range in molecular weight from 32,000 to 137,000; and (4) form plaque-like syncytia in monolayer cultures of fish cells. Intact virus particles have buoyant densities in CsCl of 1.34 to 1.36 g/ml. The viruses have been isolated from fish and shellfish collected in both the marine and freshwater environments and will replicate in several fish cell lines (Plumb et al., 1979; Meyers and Hirai, 1980; Winton et al., 1981; Nagabayashi and Mori, 1983; Hedrick et al., 1984; Chen and Jiang, 1984). The original four aquatic reovirus isolates have been compared by Winton et al., 1987.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","usgsCitation":"Winton, J., Arakawa, C., Lannan, C., and Fryer, J.L., 1989, Isolation of a reovirus from coho salmon (Oncorhynchus kisutch) in Oregon, USA, p. 257-269.","productDescription":"13 p.","startPage":"257","endPage":"269","numberOfPages":"13","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314204,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314203,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.springer.com/us/book/9783642837296"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569631c9e4b039675d00a3e1","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":588356,"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":588357,"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":588358,"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":588359,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70161969,"text":"70161969 - 1989 - A method to directly measure maximum volume of fish stomachs or digestive tracts","interactions":[],"lastModifiedDate":"2016-01-11T12:16:28","indexId":"70161969","displayToPublicDate":"2015-08-04T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":" A method to directly measure maximum volume of fish stomachs or digestive tracts","docAbstract":"

A new method for measuring maximum stomach or digestive tract volume of fish incorporates air injection at constant pressure with water displacement to measure directly the internal volume of a stomach or analogous structure. The method was tested with coho salmon, Oncorhynchus kisutch (Walbaum), which has a true stomach, and northern squawfish, Ptychocheilus oregonensis(Richardson), which has a modified foregut as a functional analogue. Both species were collected during July-October 1987 from the Columbia River, U.S.A. Relationships between fish weight (= volume) and maximum volume of the digestive organ were best fitted for coho salmon by an allometric model and for northern squawfish by an exponential model. Least squares regression analysis of individual measurements showed less variability in the volume of coho salmon stomachs (R2= 0.85) than in the total digestive tracts (R2= 0.55) and foreguts (R2= 0.61) of northern squawfish, relative to fish size. Compared to previous methods, the new technique has the advantage of accurately measuring the internal volume of a wide range of digestive organ shapes and sizes.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1095-8649.1989.tb03351.x","usgsCitation":"Burley, C., and Vigg, S., 1989, A method to directly measure maximum volume of fish stomachs or digestive tracts: Journal of Fish Biology, v. 34, no. 5, p. 707-714, https://doi.org/10.1111/j.1095-8649.1989.tb03351.x.","productDescription":"8 p.","startPage":"707","endPage":"714","numberOfPages":"8","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-01-24","publicationStatus":"PW","scienceBaseUri":"5694e038e4b039675d005dce","contributors":{"authors":[{"text":"Burley, C.C.","contributorId":152149,"corporation":false,"usgs":false,"family":"Burley","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":588223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vigg, S.","contributorId":152150,"corporation":false,"usgs":false,"family":"Vigg","given":"S.","affiliations":[],"preferred":false,"id":588224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70159101,"text":"70159101 - 1989 - Water-quality data for the Potomac-Raritan-Magothy aquifer system in the northern coast plain of New Jersey, 1923-86","interactions":[],"lastModifiedDate":"2015-10-22T09:24:42","indexId":"70159101","displayToPublicDate":"2015-06-02T05:15:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesNumber":"19","title":"Water-quality data for the Potomac-Raritan-Magothy aquifer system in the northern coast plain of New Jersey, 1923-86","docAbstract":"

Ground-water-quality data for the upper and middle aquifers of the Potomac-Raritan-Magothy aquifer system in Middlesex and Monmouth Counties are compiled for the period 1923-86. A total of 330 wells were sampled: 192 wells in the upper aquifer and 138 wells in the middle aquifer. Most of the complete water-quality analyses were collected after September 1984, as part of a regional ground-water assessment. Well-construction data for the sampled wells also are presented. Public-supply, domestic-supply, industrial, commercial, irrigation, and observation wells were sampled for the study. Field measurements made at the time of sample collection include water temperature, specific conductance , dissolved oxygen, pH, alkalinity, and bicarbonate concentration. Laboratory determinations include common ions, silica, dissolved solids, trace metals, volatile organic compounds, and pesticides. A quality-assurance program was followed to evaluate and assure the quality of the data.

\n

The report also contains a table of lithologic and hydrologic characteristics of the geologic units in the study area, a table of chloride concentrations and field measurements from 1923-86, and statistical summaries of selected water-quality data for the upper and middle aquifers. Many constituents were found in a wide range of concentrations.

\n

Water from more than 25 percent of the wells sampled contained lead concentrations above the detection limit of 10 ug/L (micrograms per liter). Included in this number are some wells that had lead concentrations greater than the U.S. Environmental Protection Agency (USEPA) primary drinking-water regulation of 50 ug/L. Cadmium concentrations, although lower than lead concentrations, followed a similar pattern. Water from approximately 25 percent of the wells in the upper aquifer, contain cadmium concentrations equal to or greater than the detection limit of 1 ug/L.

\n

Dissolved iron concentrations ranged from 5 ug/L to 480,000 ug/L. Water from more than 50 percent of the wells sampled contained iron concentrations in excess of the USEPA secondary drinking-water recommended limit of 300 ug/L.

\n

Chloride concentrations greater than the USEPA secondary drinking-water recommended limit of 250 milligrams per liter were found in samples from wells located in the cities of Perth Amboy and South Amboy; in the boroughs of Keansburg, Sayreville, Keyport, and Union Beach; and in the townships of Old Bridge and Woodbridge.

\n

Of 21 samples collected from wells screened in the upper aquifer and analyzed for 30 volatile organic compounds (VOCs), 5 samples contained at least 1 VOC at or above the detection limit. In the middle aquifer, 12 of the 21 samples collected and analyzed for VOCs contained at least 1 VOC greater than the detection limit.

\n

Concentrations of pesticides generally were low. Of the 43 samples collected from wells screened in the upper aquifer and analyzed for pesticides, 4 samples contained concentrations of pesticides at or greater than the detection limit. In the middle aquifer, 6 of 38 samples collected and analyzed for 32 pesticides had at least 1 pesticide with a concentration greater than the detection limit.

\n

 

","language":"English","publisher":"U.S. Geological Survey","collaboration":"Prepared by the United States Geological Survey in cooperation with the New Jersey Department of Environmental Protection Division of Water Resources","usgsCitation":"Harriman, D.A., Pope, D.A., and Gordon, A.D., 1989, Water-quality data for the Potomac-Raritan-Magothy aquifer system in the northern coast plain of New Jersey, 1923-86, Report: iv, 94 p.; 2 Plates: 23.97 x 22.00 inches, 23.70 x 21.93 inches.","productDescription":"Report: iv, 94 p.; 2 Plates: 23.97 x 22.00 inches, 23.70 x 21.93 inches","numberOfPages":"100","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":309926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159101.jpg"},{"id":310333,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159101/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310334,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159101/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310335,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159101/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","county":"Middlesex County, Monmouth County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.6630859375,\n 40.1452892956766\n ],\n [\n -74.6630859375,\n 40.66813955408042\n ],\n [\n -73.94210815429688,\n 40.66813955408042\n ],\n [\n -73.94210815429688,\n 40.1452892956766\n ],\n [\n -74.6630859375,\n 40.1452892956766\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620cedde4b06217fc478b48","contributors":{"authors":[{"text":"Harriman, Douglas A.","contributorId":70544,"corporation":false,"usgs":true,"family":"Harriman","given":"Douglas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":577598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pope, Daryll A. dpope@usgs.gov","contributorId":3796,"corporation":false,"usgs":true,"family":"Pope","given":"Daryll","email":"dpope@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":577599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, Alison D. 0000-0002-9502-8633 agordon@usgs.gov","orcid":"https://orcid.org/0000-0002-9502-8633","contributorId":890,"corporation":false,"usgs":true,"family":"Gordon","given":"Alison","email":"agordon@usgs.gov","middleInitial":"D.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":577600,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70157488,"text":"70157488 - 1989 - A positive relationship between groundwater velocity and submersed macrophyte biomass in Sparkling Lake, Wisconsin","interactions":[],"lastModifiedDate":"2017-12-15T14:43:49","indexId":"70157488","displayToPublicDate":"2015-04-05T04:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"A positive relationship between groundwater velocity and submersed macrophyte biomass in Sparkling Lake, Wisconsin","docAbstract":"

We measured groundwater velocity and submersed macrophyte biomass at 52 shal- low (0.4-6.6 m) sites in mesotrophic Sparkling Lake, Vilas County, Wisconsin, during May-Au- gust 1985. Seventeen percent of variation in macrophyte biomass was explained by a signifi- cant (P < 0.005) relation with depth [log(biomass + 1) = 0.49 depth - 0.08 (depth)2 + 0.121. Some of the remaining variation in macrophyte bio- mass was explained by a significant rank corre- lation of biomass-on-depth residuals with groundwater velocity (rs = 0.46, P < 0.0 1). These results suggest that water movement through the sediment-water interface may be a determinant of macrophyte abundance and distribution. 

","language":"English","publisher":"American Society of Limnology and Oceanography, Inc.","doi":"10.4319/lo.1989.34.1.0235","usgsCitation":"Lodge, D.M., Krabbenhoft, D.P., and Striegl, R.G., 1989, A positive relationship between groundwater velocity and submersed macrophyte biomass in Sparkling Lake, Wisconsin: Limnology and Oceanography, v. 34, no. 1, p. 235-239, https://doi.org/10.4319/lo.1989.34.1.0235.","productDescription":"5 p.","startPage":"235","endPage":"239","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308537,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Vilas","otherGeospatial":"Sparkling Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.71040725708008,\n 45.99857150435143\n ],\n [\n -89.71040725708008,\n 46.01723083989765\n ],\n [\n -89.69023704528809,\n 46.01723083989765\n ],\n [\n -89.69023704528809,\n 45.99857150435143\n ],\n [\n -89.71040725708008,\n 45.99857150435143\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"34","issue":"1","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"56051eace4b058f706e512a4","contributors":{"authors":[{"text":"Lodge, David M.","contributorId":76622,"corporation":false,"usgs":false,"family":"Lodge","given":"David","email":"","middleInitial":"M.","affiliations":[{"id":16905,"text":"University of Notre Dame, Dept. of Biological Sciences, Notre Dame, IN, 46556, USA","active":true,"usgs":false}],"preferred":false,"id":573302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":573303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":573304,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70157480,"text":"70157480 - 1989 - Water resources of Vilas County, WI","interactions":[],"lastModifiedDate":"2015-09-24T11:56:31","indexId":"70157480","displayToPublicDate":"2015-02-16T13:15:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":406,"text":"Miscellaneous Public","active":false,"publicationSubtype":{"id":9}},"seriesNumber":"89-1","title":"Water resources of Vilas County, WI","language":"English","publisher":"Geological and Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by the United States Department of Interior Geological Survey in cooperation with the University of Wisconsin-Extension Wisconsin, Geological and Natural History Survey","usgsCitation":"Patterson, G.L., 1989, Water resources of Vilas County, WI: Miscellaneous Public 89-1, v, 46.","productDescription":"v, 46","numberOfPages":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308508,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Vilas","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.9879,46.0971],[-88.9329,46.0746],[-88.9332,45.9822],[-89.0478,45.9822],[-89.0477,45.8953],[-89.1091,45.8973],[-89.1752,45.8993],[-89.1754,45.859],[-89.3008,45.8606],[-89.3007,45.9014],[-89.3628,45.8987],[-89.4256,45.8987],[-89.5498,45.8988],[-89.6741,45.8987],[-89.7571,45.8985],[-89.797,45.898],[-89.8199,45.8984],[-89.9212,45.8981],[-89.9846,45.8974],[-90.0428,45.8972],[-90.0442,45.9823],[-90.0134,45.9824],[-89.9853,45.9821],[-89.9289,45.9818],[-89.9282,46.0693],[-89.9288,46.1558],[-89.9287,46.2428],[-89.929,46.3],[-89.7599,46.268],[-89.7368,46.2636],[-89.5829,46.2347],[-89.5331,46.2252],[-89.5133,46.2215],[-89.4272,46.2048],[-89.3759,46.1949],[-89.2666,46.1737],[-89.2302,46.1662],[-89.0854,46.1365],[-88.9879,46.0971]]]},\"properties\":{\"name\":\"Vilas\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051eece4b058f706e5132c","contributors":{"authors":[{"text":"Patterson, G. L.","contributorId":35356,"corporation":false,"usgs":true,"family":"Patterson","given":"G.","email":"","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70157443,"text":"70157443 - 1989 - Hydrogeology of Wood County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:23:20","indexId":"70157443","displayToPublicDate":"2014-11-03T04:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"60","title":"Hydrogeology of Wood County, Wisconsin","docAbstract":"

The presence of low-permeability Precambrian rocks near land surface limits ground-water availability in the northern two-thirds of Wood County. Sand and gravel deposits provide large amounts of water (more than 500 gallons per minute) to some wells in the southeastern part of the county. Fine-grained unconsolidated deposits generally are less than 20 feet thick in the northern two-thirds of the county, but sand and gravel deposits 40- to 100-feet thick underlie the extreme southeastern part of the county. Horizontal hydraulic conductivity of the sand and gravel deposits ranges from about 155 to about 280 feet per day. The horizontal hydraulic conductivity of fine-grained unconsolidated deposits in the northern part of the county ranges from about 0.02 to 2 feet per day. Where unconsolidated deposits do not yield dependable water supplies, wells are finished in Precambrian rocks. Fractures occurring at shallow depths are the primary source of water for wells finished in Precambrian rocks. Because the number of fractures tends to decrease with depth, the horizontal hydraulic conductivity of these rocks generally decreases from about 11 feet per day in wells less than 50-feet deep to about 0.02 foot per day in wells greater than 160 feet deep.

\n

Estimates of ground-water recharge to sand and gravel deposits in the southeastern part of the county range from about 7 to 12 inches per year. Recharge estimates for the central and northern parts of the county range from about 1 to 4 inches per year.

\n

The total dissolved-solids concentration in ground water in Wood County is relatively low. Concentrations in water samples from 124 wells ranged from 21 to 578 milligrams per liter, with a median concentration of about 190 milligrams per liter. Major dissolved constituents are calcium, magnesium, and bicarbonate; sodium, potassium, chloride, and sulfate are present in low concentrations. The most common water-quality problem in Wood County is elevated iron concentrations. Iron concentrations greater than 300 micrograms per liter were found in 54 of 124 samples, and 15 samples contained iron concentrations greater than 5,000 micrograms per liter.

\n

Nitrate as nitrogen concentrations exceeded Wisconsin's drinking-water standard (10 milligrams per liter) in water from just 4 of 124 wells. The pesticide aldicarb was detected in 7 of 36 samples, and various volatile organic compounds were detected in 24 of 102 ground-water samples collected by the Wisconsin Department of Natural Resources since 1980. Wells in which these chemicals were detected are near irrigated agricultural fields and in commercially developed areas where buried gasoline-storage tanks and chemical spills are more likely to occur.

\n

A reconnaissance approach combining electromagnetic surveys and sampling for water-quality indicators was used to assess effects of leachate on ground water near seven landfills. Results of the electromagnetic surveys were used to site water-quality observation wells. Total dissolved-solids concentrations and concentrations of volatile organic compounds, chloride, sulfate, iron, chemical oxygen demand, and organic carbon are some of the chemical constituents analyzed in samples collected from these wells.

\n

The average rate of ground·water pumpage in Wood County in 1985 was 9.7 million gallons per day. Of this rate, about 6 million gallons per day is pumped from municipal-supply wells in seven communities.An additional 1.08 million gallons per day is pumped for agricultural irrigation.

","language":"English","publisher":"Wisconsin Geological & Natural History Survey","collaboration":"Prepared in cooperation with the University of Wisconsin-Extension, Geological and Natural History Survey, and Wood County","usgsCitation":"Batten, W.G., 1989, Hydrogeology of Wood County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 60, vi, 27 p.","productDescription":"vi, 27 p.","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350382,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic60/"}],"country":"United States","state":"Wisconsin","county":"Wood County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.8449,44.6849],[-89.8451,44.5983],[-89.8447,44.5116],[-89.7268,44.5114],[-89.7259,44.4239],[-89.7243,44.3372],[-89.7247,44.2479],[-89.8376,44.249],[-89.8982,44.2493],[-89.9557,44.2491],[-89.9908,44.249],[-90.073,44.2491],[-90.0807,44.2491],[-90.1675,44.2491],[-90.1924,44.249],[-90.1975,44.249],[-90.1994,44.249],[-90.3123,44.2497],[-90.3161,44.2497],[-90.3172,44.3377],[-90.3163,44.4247],[-90.3161,44.5127],[-90.3165,44.5989],[-90.3163,44.6852],[-90.1981,44.6854],[-90.0793,44.685],[-89.9644,44.685],[-89.8449,44.6849]]]},\"properties\":{\"name\":\"Wood\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5603cd44e4b03bc34f544b10","contributors":{"authors":[{"text":"Batten, W. G.","contributorId":89504,"corporation":false,"usgs":true,"family":"Batten","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015452,"text":"70015452 - 1989 - Recent activities of the Priroda State Remote Sensing Center","interactions":[],"lastModifiedDate":"2025-05-09T16:25:48.124072","indexId":"70015452","displayToPublicDate":"2013-05-15T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2659,"text":"Mapping Sciences and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Recent activities of the Priroda State Remote Sensing Center","docAbstract":"

No abstract availalbe. 

","language":"English","publisher":"Taylor & Francis","doi":"10.1080/07493878.1989.10641782","usgsCitation":"Morrison, J.L., and Bond, A., 1989, Recent activities of the Priroda State Remote Sensing Center: Mapping Sciences and Remote Sensing, v. 26, no. 4, p. 334-340, https://doi.org/10.1080/07493878.1989.10641782.","productDescription":"7 p.","startPage":"334","endPage":"340","costCenters":[],"links":[{"id":224259,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"4","noUsgsAuthors":false,"publicationDate":"2013-05-15","publicationStatus":"PW","scienceBaseUri":"505a95d8e4b0c8380cd81c7a","contributors":{"authors":[{"text":"Morrison, J. L.","contributorId":28012,"corporation":false,"usgs":true,"family":"Morrison","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":370978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bond, A.R.","contributorId":20910,"corporation":false,"usgs":true,"family":"Bond","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":370977,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015026,"text":"70015026 - 1989 - A parabolic function to modify Thornthwaite estimates of potential evapotranspiration for the eastern United States","interactions":[],"lastModifiedDate":"2025-06-17T16:59:45.299851","indexId":"70015026","displayToPublicDate":"2013-05-15T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3059,"text":"Physical Geography","active":true,"publicationSubtype":{"id":10}},"title":"A parabolic function to modify Thornthwaite estimates of potential evapotranspiration for the eastern United States","docAbstract":"

The Thornthwaite potential evapotranspiration model is well known and widely used, but has received some criticism as it is primarily based on air temperature to estimate potential evapotranspiration. Errors of the Thornthwaite model can be analyzed using adjusted pan evaporation as an index of potential evapotranspiration. An examination of ratios of adjusted pan evaporation to Thornthwaite potential evapotranspiration indicates that the ratios are highest in the winter and lowest during summer months. This trend suggests a parabolic pattern. In this study a parabolic function is used to adjust Thornthwaite estimates of potential evapotranspiration. Forty locations east of the Rocky Mountains are analyzed and indicate that a parabolic adjustment of Thornthwaite potential evapotranspiration estimates generally increases correlation with adjusted pan evaporation and decreases error by 20 to 70 percent. 

","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02723646.1989.10642376","issn":"02723646","usgsCitation":"McCabe, G.J., 1989, A parabolic function to modify Thornthwaite estimates of potential evapotranspiration for the eastern United States: Physical Geography, v. 10, no. 2, p. 176-189, https://doi.org/10.1080/02723646.1989.10642376.","productDescription":"14 p.","startPage":"176","endPage":"189","costCenters":[],"links":[{"id":223743,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationDate":"2013-05-15","publicationStatus":"PW","scienceBaseUri":"5059e4d1e4b0c8380cd46951","contributors":{"authors":[{"text":"McCabe, G. J. Jr.","contributorId":77551,"corporation":false,"usgs":true,"family":"McCabe","given":"G.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":369886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044325,"text":"70044325 - 1989 - Thermal maturity of the Anadarko Basin","interactions":[],"lastModifiedDate":"2013-03-03T09:35:17","indexId":"70044325","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Thermal maturity of the Anadarko Basin","docAbstract":"Levels of thermal maturity are estimated for Paleozoic strata in five areas of the central Anadarko basin for times between the Paleozoic and the present, and depths of the oil window are plotted as a function of geologic time. Mean surface temperature assumed here for calculating Lopatin's time-temperature index of thermal maturity (TTl) in the central Anadarko basin declines from 80°F (27°C) to 60°F (16°C) from early Paleozoic time to the present. Shallow-water carbonates and lower paleolatitudes suggest warmer climates in the Paleozoic for this area. The geothermal gradient is assumed to equal 4.0°F/100 ft (7.3°C/100 m) in the Late Cambrian and to decay over a 100-m.y. period to the present regional gradient of 1.3°F/100 ft (2.4°C/100 m). Initial\nbasin formation was caused by crustal thinning. Accumulation of thick Pennsylvanian sediments in a foreland-style basin dominated by vertical lithospheric flexure represents a second major period of subsidence. An elevated geothermal gradient during this time is not assumed for TTl calculations, because mathematical models suggest time-invariant heat flows in such basins. TTl computations based on these assumptions indicate that oil could have been generated in the ancestral Anadarko basin >350 m.y. ago. By the end of the Pennsylvanian, significant volumes of kerogen were in the oil window (and perhaps beyond), and significant volumes have remained in the oil window up to the present day. These circumstances may partially explain the unusual richness of the Anadarko basin as a Paleozoic hydrocarbon province.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Schmoker, J.W., 1989, Thermal maturity of the Anadarko Basin, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 25-31.","productDescription":"7 p.","startPage":"25","endPage":"31","costCenters":[],"links":[{"id":268665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268664,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0ee4b0e1603e4fec7a","contributors":{"authors":[{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":475293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044327,"text":"70044327 - 1989 - Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration","interactions":[],"lastModifiedDate":"2013-03-03T09:30:32","indexId":"70044327","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration","docAbstract":"Organic geochemical analyses of 104 crude oils and 190 core samples of dark-colored shales from the greater Anadarko basin show three major oil types which generally correlate with reservoir age and source-rock age. Analyses include C3-C30 whole-oil gas chromatography, C10+ saturated-hydrocarbon-fraction gas chromatography, and carbon stable isotopes (ppt relative to PDB) of saturated (sat) and aromatic (arom) hydrocarbon fractions. Three samples from Middle Ordovician Simpson Group reservoirs are \"typical\" Ordovician oils (type 1), having strong odd-carbon predominance in the C13 to C19 n-alkanes, containing little or no acyclic isoprenoids, an δ13C values of -33.9 ppt (sat) and -33.7 ppt (arom). Oils from Silurian to Devonian and Mississippian reservoirs (type 2) show little or no odd-carbon predominance in the n-alkanes, a regular decrease in abundance of n-alkanes with increasing carbon number, pristane/phytane ratios (pr/ph) of 1.1 to 1.5, and δ13C values of -30.6 ppt (sat) and -30.1 ppt (arom). Oils in Pennsylvanian reservoirs (type 3) have the greatest amounts of C15+ hydrocarbons, are isotopically heavy (-27.5 ppt [sat] and -26.4 ppt [arom]), have methyl-cyclohexane as the most abundant hydrocarbon, and have pr/ph values from 2.0 to 0.9. Oils from the Kansas shelf area of the Anadarko basin are similar to the Anadarko oil types except that they have only traces of toluene and no detectable benzene. The relative abundance of toluene in the C7 hydrocarbons systematically decreases with distance from the depocenter of the basin. The aromatic compounds are removed by water-washing, and hence could have been lost by contact with progressively greater amounts of formation water during long-distance migration. The lack of thermally mature source rocks in southern and central Kansas supports this hypothesis.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Burruss, R., and Hatch, J.R., 1989, Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 53-64.","productDescription":"12 p.","startPage":"53","endPage":"64","costCenters":[],"links":[{"id":268669,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268668,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f06e4b0e1603e4fec50","contributors":{"authors":[{"text":"Burruss, R.C. 0000-0001-6827-804X","orcid":"https://orcid.org/0000-0001-6827-804X","contributorId":99574,"corporation":false,"usgs":true,"family":"Burruss","given":"R.C.","affiliations":[],"preferred":false,"id":475298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, J. R.","contributorId":14775,"corporation":false,"usgs":true,"family":"Hatch","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":475297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70044341,"text":"70044341 - 1989 - Relationship of clay-mineral diagenesis to temperature, age, and hydrocarbon generation–an example from the Anadarko Basin, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T19:16:11","indexId":"70044341","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Relationship of clay-mineral diagenesis to temperature, age, and hydrocarbon generation–an example from the Anadarko Basin, Oklahoma","docAbstract":"Randomly interstratified illite/smectite (I/S) is present in Springeran and Morrowan rocks (Late Mississippian and Early Pennsylvanian) of the Anadarko basin, Oklahoma, at present-day depths <2,750 m, but disappears at depths of 2,750-3,050 m. Only ordered I/S is found in samples below 3,050 m. The work reported here relates the diagenesis of I/S to burial history and oil generation in the Anadarko basin and tests the dependence of the smectite-to-illite reaction on temperature and time. Published temperature models of clay diagenesis suggest that, for Tertiary and Cretaceous rocks, the transition from randomly interstratified I/S to ordered I/S occurs at 100-110°C. Burial reconstructions for the Anadarko basin indicate that maximum temperatures of 100-110°C correspond to present-day burial depths between 2,700 and 3,100 m. These independently calculated depths for the 100-110°C isotherm match the depths at which randomly interstratified I/S is observed to disappear in Morrowan-Springeran rocks. Thus, random I/S disappears at the same temperature in rocks that differ in age by some 300 m.y. Although the extent of the smectite-to-illite reaction is controlled by kinetics, and effects of time are apparent in laboratory experiments and short-lived geologic systems, the results of this study suggest that time plays a secondary role in long-term diagenetic settings.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Pollastro, R.M., and Schmoker, J.W., 1989, Relationship of clay-mineral diagenesis to temperature, age, and hydrocarbon generation–an example from the Anadarko Basin, Oklahoma, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 257-261.","productDescription":"4 p.","startPage":"257","endPage":"261","costCenters":[],"links":[{"id":268695,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268694,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0be4b0e1603e4fec6e","contributors":{"authors":[{"text":"Pollastro, Richard M.","contributorId":25100,"corporation":false,"usgs":true,"family":"Pollastro","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":475321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":475322,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70044340,"text":"70044340 - 1989 - Analysis of sedimentary facies and petrofacies of lower Morrowan-upper Chesterian sandstones, Anadarko Basin, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T18:47:28","indexId":"70044340","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Analysis of sedimentary facies and petrofacies of lower Morrowan-upper Chesterian sandstones, Anadarko Basin, Oklahoma","docAbstract":"Three major lithofacies have been identified within the Morrow (Pennsylvanian) and Springer (Pennsylvanian-Mississippian) units, in core from 30 drill holes ranging from the Oklahoma Panhandle to the southwestern portion of the Anadarko basin. The study included inspection of ~6,500 ft of core, examination of ~100 thin sections, and a scanning-electron-microscope study of butts of the material used for thin-section preparation. The lithofacies identified are (1) fluvial-influenced coastal, which includes the deltaic facies described by Swanson (1979), (2) tidal-influenced nearshore, and (3) mixed, which shows mixed tidal and nontidal marine influence. Our interpretation is supported by the investigations of Moore (1979), Haiduk (1987), and Swanson (1979). The fluvial-influenced coastal facies is restricted to the northwestern (Panhandle) portion of the Anadarko basin.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Keighin, C.W., and Flores, R.M., 1989, Analysis of sedimentary facies and petrofacies of lower Morrowan-upper Chesterian sandstones, Anadarko Basin, Oklahoma, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 236-238.","productDescription":"3 p.","startPage":"236","endPage":"238","costCenters":[],"links":[{"id":268692,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"},{"id":268693,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f02e4b0e1603e4fec38","contributors":{"authors":[{"text":"Keighin, C. William","contributorId":36804,"corporation":false,"usgs":true,"family":"Keighin","given":"C.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":475319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flores, Romeo M. rflores@usgs.gov","contributorId":71984,"corporation":false,"usgs":true,"family":"Flores","given":"Romeo","email":"rflores@usgs.gov","middleInitial":"M.","affiliations":[{"id":165,"text":"Central Energy Resources Team","active":false,"usgs":true}],"preferred":false,"id":475320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70044338,"text":"70044338 - 1989 - Regional gravity of the Anadarko Basin area and a more detailed look at the Wichita frontal fault zone","interactions":[],"lastModifiedDate":"2013-03-03T18:22:19","indexId":"70044338","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Regional gravity of the Anadarko Basin area and a more detailed look at the Wichita frontal fault zone","docAbstract":"We presented poster displays on gravity surveys in and around the Anadarko basin at the Anadarko Basin Workshop in Norman, Oklahoma, on April 5-6, 1988.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Robbins, S.L., Jones-Cecil, M., and Keller, G.R., 1989, Regional gravity of the Anadarko Basin area and a more detailed look at the Wichita frontal fault zone, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 225-227.","productDescription":"3 p.","startPage":"225","endPage":"227","costCenters":[],"links":[{"id":268688,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"},{"id":268689,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0be4b0e1603e4fec6a","contributors":{"authors":[{"text":"Robbins, S. L.","contributorId":49766,"corporation":false,"usgs":true,"family":"Robbins","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":475314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones-Cecil, Meridee","contributorId":68313,"corporation":false,"usgs":true,"family":"Jones-Cecil","given":"Meridee","email":"","affiliations":[],"preferred":false,"id":475315,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keller, G. R. Jr.","contributorId":85031,"corporation":false,"usgs":true,"family":"Keller","given":"G.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":475316,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70044337,"text":"70044337 - 1989 - Sulfide mineralization and magnetization, Cement oil field, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T18:12:37","indexId":"70044337","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Sulfide mineralization and magnetization, Cement oil field, Oklahoma","docAbstract":"Geochemical, petrographic, and rock-magnetic studies were undertaken to investigate possible sources for reported positive aeromagnetic anomalies over the Cement oil field, Oklahoma. Ferrimagnetic pyrrhotite (monoclinic, Fe7S8 ), intergrown with more-abundant, nonmagnetic pyrite (FeS2), is present in well-cutting, core, and quarry samples at Cement, and it is the only identified source of possible enhanced magnetization in rocks over the field. Magnetite, found only in well cuttings from Cement, is contamination from drilling. Magnetite was considered previously by others to be the source of magnetic anomalies at Cement.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Reynolds, R.L., Fishman, N.S., Webring, M.W., Wanty, R.B., and Goldhaber, M.B., 1989, Sulfide mineralization and magnetization, Cement oil field, Oklahoma, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 209-209.","productDescription":"1 p.","startPage":"209","endPage":"209","costCenters":[],"links":[{"id":268687,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268686,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0de4b0e1603e4fec76","contributors":{"authors":[{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":441,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":271,"text":"Federal Center","active":false,"usgs":true}],"preferred":true,"id":475309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":475313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webring, Michael W. mwebring@usgs.gov","contributorId":1221,"corporation":false,"usgs":true,"family":"Webring","given":"Michael","email":"mwebring@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":475311,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wanty, Richard B. 0000-0002-2063-6423 rwanty@usgs.gov","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":443,"corporation":false,"usgs":true,"family":"Wanty","given":"Richard","email":"rwanty@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":475310,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":475312,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70044329,"text":"70044329 - 1989 - Structural evolution of the southeastern portion of the Anadarko Basin region","interactions":[],"lastModifiedDate":"2013-03-03T09:45:50","indexId":"70044329","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Structural evolution of the southeastern portion of the Anadarko Basin region","docAbstract":"Field investigations in the Lake Classen-Turner Falls, Oklahoma, area of the northern Arbuckle anticline, on the southeastern margin of the Anadarko basin, indicate that transpressional (oblique compressional) deformation of Late Pennsylvanian age dominated the structural development of this area. The Arbuckle anticline is detached along the NW -trending, SW -dipping, left-reverse Arbuckle fault and is thrust obliquely onto the margin of the Tishomingo block to the east. Paleostress analysis of slip lines on mesoscopic faults along the northeastern limb of the Arbuckle anticline, associated in style and geometry with oblique Arbuckle thrusting, indicates compression directed N. 35-60° E.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Perry, W.J., 1989, Structural evolution of the southeastern portion of the Anadarko Basin region, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 77-77.","productDescription":"1 p.","startPage":"77","endPage":"77","costCenters":[],"links":[{"id":268671,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268670,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0ce4b0e1603e4fec72","contributors":{"authors":[{"text":"Perry, William J. Jr.","contributorId":32498,"corporation":false,"usgs":true,"family":"Perry","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":475299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044331,"text":"70044331 - 1989 - Anadarko Basin conodont studies","interactions":[],"lastModifiedDate":"2013-03-03T10:08:34","indexId":"70044331","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Anadarko Basin conodont studies","docAbstract":"Preliminary analysis of early Paleozoic conodonts from the subsurface within and adjacent to the Anadarko basin demonstrates their utility in stratigraphic and thermal evolution studies in the basin. More than 100 samples from 30 drill holes produced conodonts that can be correlated with faunas known from rock sequences exposed along the southern flanks of the basin. For the Middle Ordovician to Devonian, extant biozonations and/or recent published literature based on Oklahoma surface sections allow good biostratigraphic correlation into the subsurface and often allow testing of physical correlations. In contrast, conodonts from the Arbuckle Group (Lower to Middle Ordovician) are less well known. Faunas from the upper half of the group are documented only in unpublished theses, and published faunas are in need of restudy and revision. However, this limited information, along with work in progress in Oklahoma and data from carbonate platform facies elsewhere in North America, still permit correlations into the subsurface with the promise of increasingly improved resolution.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Repetski, J.E., 1989, Anadarko Basin conodont studies, chap. of Anadarko Basin symposium, 1988 (Circular 90), p. 133-133.","productDescription":"1 p.","startPage":"133","endPage":"133","costCenters":[],"links":[{"id":268675,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268674,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347ef4e4b0e1603e4fec34","contributors":{"authors":[{"text":"Repetski, John E. 0000-0002-2298-7120 jrepetski@usgs.gov","orcid":"https://orcid.org/0000-0002-2298-7120","contributorId":2596,"corporation":false,"usgs":true,"family":"Repetski","given":"John","email":"jrepetski@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":475301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044336,"text":"70044336 - 1989 - Mineralogic and textural relations in deeply buried rocks of the Simpson Group (Middle Ordovician)--implications in diagenesis and petroleum geology","interactions":[],"lastModifiedDate":"2013-03-03T11:09:31","indexId":"70044336","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Mineralogic and textural relations in deeply buried rocks of the Simpson Group (Middle Ordovician)--implications in diagenesis and petroleum geology","docAbstract":"The mineral composition and petrography of sandstones, shales, carbonates, and intermediate lithologies were determined on 112 core samples of the Middle Ordovician Simpson Group in the Sunray DX Parker No. 1 Mazur well, Grady County, Oklahoma. Core was recovered from present depths of about 15,900-17,200 ft and included all or parts of the Bromide, Tulip Creek, McLish, Oil Creek, and Joins Formations. The bulk-rock mineral composition of Simpson Group rocks is diverse. The mean weighted composition of 50 sandstone samples is 66% quartz, 14% clay, and 18% carbonate, as determined by X-ray powder diffraction (XRD). Some sandstones from the Oil Creek and Tulip Creek Formations contain as much as 96% quartz. These quartz-rich sandstones were cemented early by silica. Feldspar averages 2%; some sandstones from the McLish Formation contain as much as 15% feldspar. Potassium feldspar is commonly more abundant than plagioclase; potassium feldspar overgrowths are found in some of the sandstones. Most of the shales are clay-rich and quartz-poor, averaging about 85% clay minerals, 7% quartz, and 3% feldspar, by weight, as determined by XRD. Carbonate, fluorapatite, and pyrite are present in variable amounts. Such high clay/quartz ratios are not characteristic of shales and suggest that silica has been expelled by diagenetic processes during burial. The main clay mineral in the Simpson Group at these depths is illite, although iron-rich chlorite is locally concentrated in sandstones. Illite typically makes up >90 wt. % of the clay minerals in sandstones and >95 wt. % of those in shale and carbonate. Total clay content, determined from XRD, correlates closely with total gamma-ray intensity from geophysical logs, because illite is the primary potassium-bearing phase in these deeply buried rocks. Therefore, the gamma-ray log is a good indicator of \"shaliness\" in potential Simpson reservoirs at similar depths. Much of the carbonate was introduced into the sandstones during burial as calcite, dolomite, or ankerite cement. Early iron-free calcite is commonly replaced by iron-bearing calcite, dolomite, or ankerite. Sandstones and carbonate rocks also contain rhombic dolomite. Many of the dolomite rhombs contain overgrowths of ferroan dolomite or ankerite, as evidenced by staining. Ankerite cementation is later and less selective than earlier dolomite and commonly replaces earlier carbonate or silica cements. Dolomite commonly replaces detrital clay and calcite. Spatial and textural relations suggest that the conversion of smectite to illite contributed, in part, to the formation of dolomite and ankerite cements. Scanning electron miscroscopy reveals that much of the diagenetic illite occurs as tabular fibers in pores or as pseudomorphic intergrowths after smectite. Most chlorite in sandstones is authigenic and occurs as a pore-lining cement or as a pseudomorphic replacement after kaolinite. Secondary porosity, formed mainly from the dissolution of intergranular carbonate cements, is best developed in sandstones from the Oil Creek and Tulip Creek Formations.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1998 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Pollastro, R.M., 1989, Mineralogic and textural relations in deeply buried rocks of the Simpson Group (Middle Ordovician)--implications in diagenesis and petroleum geology, chap. of Anadarko Basin symposium, 1998 (Circular 90), p. 194-208.","productDescription":"15 p.","startPage":"194","endPage":"208","costCenters":[],"links":[{"id":268685,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268684,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f09e4b0e1603e4fec5e","contributors":{"authors":[{"text":"Pollastro, Richard M.","contributorId":25100,"corporation":false,"usgs":true,"family":"Pollastro","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":475308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}