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,{"id":70036279,"text":"70036279 - 2010 - Southern high latitude dune fields on Mars: Morphology, aeolian inactivity, and climate change","interactions":[],"lastModifiedDate":"2012-03-12T17:22:03","indexId":"70036279","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Southern high latitude dune fields on Mars: Morphology, aeolian inactivity, and climate change","docAbstract":"In a study area spanning the martian surface poleward of 50?? S., 1190 dune fields have been identified, mapped, and categorized based on dune field morphology. Dune fields in the study area span ??? 116400km2, leading to a global dune field coverage estimate of ???904000km2, far less than that found on Earth. Based on distinct morphological features, the dune fields were grouped into six different classes that vary in interpreted aeolian activity level from potentially active to relatively inactive and eroding. The six dune field classes occur in specific latitude zones, with a sequence of reduced activity and degradation progressing poleward. In particular, the first signs of stabilization appear at ???60?? S., which broadly corresponds to the edge of high concentrations of water-equivalent hydrogen content (observed by the Neutron Spectrometer) that have been interpreted as ground ice. This near-surface ground ice likely acts to reduce sand availability in the present climate state on Mars, stabilizing high latitude dunes and allowing erosional processes to change their morphology. As a result, climatic changes in the content of near-surface ground ice are likely to influence the level of dune activity. Spatial variation of dune field classes with longitude is significant, suggesting that local conditions play a major role in determining dune field activity level. Dune fields on the south polar layered terrain, for example, appear either potentially active or inactive, indicating that at least two generations of dune building have occurred on this surface. Many dune fields show signs of degradation mixed with crisp-brinked dunes, also suggesting that more than one generation of dune building has occurred since they originally formed. Dune fields superposed on early and late Amazonian surfaces provide potential upper age limits of ???100My on the south polar layered deposits and ???3Ga elsewhere at high latitudes. No craters are present on any identifiable dune fields, which can provide a lower age limit through crater counting: assuming all relatively stabilized dune fields represent a single noncontiguous surface of uniform age, their estimated crater retention age is &lt;???10000years. An average-sized uncratered dune field (94km2) has a crater retention age &lt;???8My. This apparent youth suggests that present-day climate conditions are responsible for the observed degradation and reduced level of aeolian activity. A lack of observed transport pathways and the absence of large dune fields in the largest basins (Hellas and Argyre Planitiae) are consistent with the previously proposed idea that dune sands are not typically transported far from their source regions on Mars. ?? 2009 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.geomorph.2009.11.006","issn":"0169555X","usgsCitation":"Fenton, L., and Hayward, R., 2010, Southern high latitude dune fields on Mars: Morphology, aeolian inactivity, and climate change: Geomorphology, v. 121, no. 1-2, p. 98-121, https://doi.org/10.1016/j.geomorph.2009.11.006.","startPage":"98","endPage":"121","numberOfPages":"24","costCenters":[],"links":[{"id":218197,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geomorph.2009.11.006"},{"id":246183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"121","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b93f1e4b08c986b31a78d","contributors":{"authors":[{"text":"Fenton, L.K.","contributorId":102189,"corporation":false,"usgs":true,"family":"Fenton","given":"L.K.","affiliations":[],"preferred":false,"id":455237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayward, R.K.","contributorId":31885,"corporation":false,"usgs":true,"family":"Hayward","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":455236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037674,"text":"70037674 - 2010 - Summary of the Second International Planetary Dunes Workshop: Planetary Analogs - Integrating Models, Remote Sensing, and Field Data, Alamosa, Colorado, USA, May 18-21, 2010","interactions":[],"lastModifiedDate":"2012-04-30T16:43:35","indexId":"70037674","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Summary of the Second International Planetary Dunes Workshop: Planetary Analogs - Integrating Models, Remote Sensing, and Field Data, Alamosa, Colorado, USA, May 18-21, 2010","docAbstract":"The Second International Planetary Dunes Workshop took place in Alamosa, Colorado, USA from May 18-21, 2010. The workshop brought together researchers from diverse backgrounds to foster discussion and collaboration regarding terrestrial and extra-terrestrial dunes and dune systems. Two and a half days were spent on five oral sessions and one poster session, a full-day field trip to Great Sand Dunes National Park, with a great deal of time purposefully left open for discussion. On the last day of the workshop, participants assembled a list of thirteen priorities for future research on planetary dune systems. ?? 2010.","largerWorkTitle":"Aeolian Research","language":"English","doi":"10.1016/j.aeolia.2010.09.001","issn":"18759637","usgsCitation":"Fenton, L., Bishop, M., Bourke, M., Bristow, C., Hayward, R., Horgan, B., Lancaster, N., Michaels, T., Tirsch, D., Titus, T., and Valdez, A., 2010, Summary of the Second International Planetary Dunes Workshop: Planetary Analogs - Integrating Models, Remote Sensing, and Field Data, Alamosa, Colorado, USA, May 18-21, 2010, <i>in</i> Aeolian Research, v. 2, no. 2-3, p. 173-178, https://doi.org/10.1016/j.aeolia.2010.09.001.","startPage":"173","endPage":"178","numberOfPages":"6","costCenters":[],"links":[{"id":487886,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1016/j.aeolia.2010.09.001>.","text":"External Repository"},{"id":218080,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.aeolia.2010.09.001"},{"id":246061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ef2e4b08c986b31e236","contributors":{"authors":[{"text":"Fenton, L.K.","contributorId":102189,"corporation":false,"usgs":true,"family":"Fenton","given":"L.K.","affiliations":[],"preferred":false,"id":462229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bishop, M.A.","contributorId":95426,"corporation":false,"usgs":true,"family":"Bishop","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":462226,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bourke, M.C.","contributorId":59165,"corporation":false,"usgs":true,"family":"Bourke","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":462223,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bristow, C.S.","contributorId":41684,"corporation":false,"usgs":true,"family":"Bristow","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":462222,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hayward, R.K.","contributorId":31885,"corporation":false,"usgs":true,"family":"Hayward","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":462220,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Horgan, B.H.","contributorId":99409,"corporation":false,"usgs":true,"family":"Horgan","given":"B.H.","email":"","affiliations":[],"preferred":false,"id":462227,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lancaster, N.","contributorId":36330,"corporation":false,"usgs":true,"family":"Lancaster","given":"N.","email":"","affiliations":[],"preferred":false,"id":462221,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Michaels, T.I.","contributorId":100632,"corporation":false,"usgs":true,"family":"Michaels","given":"T.I.","email":"","affiliations":[],"preferred":false,"id":462228,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Tirsch, D.","contributorId":68997,"corporation":false,"usgs":true,"family":"Tirsch","given":"D.","affiliations":[],"preferred":false,"id":462224,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Titus, T.N.","contributorId":102615,"corporation":false,"usgs":true,"family":"Titus","given":"T.N.","email":"","affiliations":[],"preferred":false,"id":462230,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Valdez, A.","contributorId":80127,"corporation":false,"usgs":true,"family":"Valdez","given":"A.","email":"","affiliations":[],"preferred":false,"id":462225,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70193281,"text":"70193281 - 2010 - Maintenance of Eastern hemlock forests:  Factors associated with hemlock vulnerability to hemlock woolly adelgid","interactions":[],"lastModifiedDate":"2017-11-15T14:27:03","indexId":"70193281","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Maintenance of Eastern hemlock forests:  Factors associated with hemlock vulnerability to hemlock woolly adelgid","docAbstract":"<p>Eastern hemlock (Tsuga canadensis [L.]) is the most shade-tolerant and long-lived tree species in eastern North America. The hemlock woolly adelgid (Adelges tsugae) (HWA), is a nonnative invasive insect that feeds on eastern hemlock and Carolina hemlock (Tsuga caroliniana Engelm.). HWA currently is established in 17 eastern states and is causing tree decline and wide-ranging tree mortality. Our data from West Virginia and Pennsylvania suggest that hemlock crown vigor (a ranking of amount of live crown) relates to a predictable pattern of hemlock vulnerability at light and moderate levels of HWA infestation. We found that crown variables, such as live crown ratio and crown density and transparency, are accurate predictors of hemlock decline; more vigorous trees appear to be less vulnerable to HWA. Thus, silvicultural thinning treatments may be a means for reducing stand densities and increasing crown vigor in colder areas where climate may slow HWA spread. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Proceedings from the Conference on the Ecology and Management of High-Elevation Forests in the Central and Southern Appalachian Mountains","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"USDA Forest Service","usgsCitation":"Fajvan, M.A., and Wood, P.B., 2010, Maintenance of Eastern hemlock forests:  Factors associated with hemlock vulnerability to hemlock woolly adelgid, <i>in</i> Proceedings from the Conference on the Ecology and Management of High-Elevation Forests in the Central and Southern Appalachian Mountains, p. 31-38.","productDescription":"8 p.","startPage":"31","endPage":"38","ipdsId":"IP-014482","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":348907,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":348906,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.nrs.fs.fed.us/pubs/gtr/gtr_nrs-p-64.pdf"}],"publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a610acee4b06e28e9c256ed","contributors":{"authors":[{"text":"Fajvan, Mary Ann","contributorId":200418,"corporation":false,"usgs":false,"family":"Fajvan","given":"Mary","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":722255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Petra Bohall pbwood@usgs.gov","contributorId":1791,"corporation":false,"usgs":true,"family":"Wood","given":"Petra","email":"pbwood@usgs.gov","middleInitial":"Bohall","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":false,"id":718524,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70005020,"text":"70005020 - 2010 - C is for cactolith","interactions":[],"lastModifiedDate":"2013-06-05T09:33:51","indexId":"70005020","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":674,"text":"Aggregates Manager","active":true,"publicationSubtype":{"id":10}},"title":"C is for cactolith","docAbstract":"Geologic jargon - though handy for triple-word scores - should be used in moderation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aggregates Manager","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Randall Reilly Publishing","usgsCitation":"Langer, W.H., 2010, C is for cactolith: Aggregates Manager, v. 15, no. 3, p. 44-44.","productDescription":"1 p.","startPage":"44","endPage":"44","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":204081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":24493,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.aggman.com/carved-in-stone-2/","linkFileType":{"id":5,"text":"html"}}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f98d5","contributors":{"authors":[{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":351829,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70005021,"text":"70005021 - 2010 - D is for diamond","interactions":[],"lastModifiedDate":"2013-06-05T09:35:11","indexId":"70005021","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":674,"text":"Aggregates Manager","active":true,"publicationSubtype":{"id":10}},"title":"D is for diamond","docAbstract":"Real diamonds are a girl's best friend, but synthetic ones opened up a whole new world for granite.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aggregates Manager","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Randall Reilly Publishing","usgsCitation":"Langer, W.H., 2010, D is for diamond: Aggregates Manager, v. 15, no. 4, p. 40-40.","productDescription":"1 p.","startPage":"40","endPage":"40","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":204082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":24492,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.aggman.com/carved-in-stone-3/","linkFileType":{"id":5,"text":"html"}}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eb60","contributors":{"authors":[{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":351830,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70037225,"text":"70037225 - 2010 - Breeding biology and natural history of the Slate-throated Whitestart in Venezuela","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037225","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3784,"text":"Wilson Journal of Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"Breeding biology and natural history of the Slate-throated Whitestart in Venezuela","docAbstract":"We provide details on the breeding biology of the Slate-throated Whitestart (Myioborus miniatus) from 126 nests found during seven breeding seasons, 2002-2008, at Yacamb?? National Park, Venezuela. Nesting activity peaked in late April and May. Only the female built the nest and incubated the eggs. Males rarely visited the nest during these stages. Mean clutch size (2.1 ?? 0.04 eggs, n = 93) was the smallest recorded for the Slate-throated Whitestart. Incubation and nestling period lengths were 15.3 ?? 0.31 (n = 21) and 10.8 ?? 0.24 (n = 7) days, respectively. Attentiveness (% of time on the nest) during incubation (59 ?? 1.6%, n = 52) was similar to other tropical warblers and much lower than northern relatives. This caused a relatively low egg temperature (34.40 ?? 0.33u C, n = ?? nests, 20 days) compared with north temperate birds. Both parents fed nestlings and increased their provisioning rates with nestling age. Growth rate based on nestling mass (k = 0.521 ?? 0.015) was faster than for other tropical passerines but slower than northern relatives. Predation was the main cause of nesting failure and rate of predation increased with age of the nest. An estimated 15% of nests were successful based on an overall Mayfield daily predation rate of 0.053 ?? 0.007. This study confirms a strong latitudinal variation in life history traits of warblers. ?? 2010 by the Wilson Ornithological Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Journal of Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1676/09-151.1","issn":"15594491","usgsCitation":"Ruggera, R., and Martin, T.E., 2010, Breeding biology and natural history of the Slate-throated Whitestart in Venezuela: Wilson Journal of Ornithology, v. 122, no. 3, p. 447-454, https://doi.org/10.1676/09-151.1.","startPage":"447","endPage":"454","numberOfPages":"8","costCenters":[],"links":[{"id":475899,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1676/09-151.1","text":"Publisher Index Page"},{"id":217315,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1676/09-151.1"},{"id":245252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"122","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f25ce4b0c8380cd4b12c","contributors":{"authors":[{"text":"Ruggera, R.A.","contributorId":54798,"corporation":false,"usgs":true,"family":"Ruggera","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":459972,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, T. E.","contributorId":10911,"corporation":false,"usgs":true,"family":"Martin","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":459971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70005022,"text":"70005022 - 2010 - E is for earth","interactions":[],"lastModifiedDate":"2013-06-05T10:01:01","indexId":"70005022","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":674,"text":"Aggregates Manager","active":true,"publicationSubtype":{"id":10}},"title":"E is for earth","docAbstract":"The planet's layers - particularly the earth's crust - provide many of life's essential building blocks.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aggregates Manager","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Randall Reilly Publishing","usgsCitation":"Langer, W.H., 2010, E is for earth: Aggregates Manager, v. 15, no. 5, p. 40-40.","productDescription":"1 p.","startPage":"40","endPage":"40","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":204083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":24496,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.aggman.com/carved-in-stone-4/","linkFileType":{"id":5,"text":"html"}}],"volume":"15","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fd52","contributors":{"authors":[{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":351831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70037320,"text":"70037320 - 2010 - Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037320","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2545,"text":"Journal of the Geological Society","active":true,"publicationSubtype":{"id":10}},"title":"Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary","docAbstract":"Mineralogy and chemical composition are presented for a chert-ironstone bed that overlies the ??rk??t Mn deposit. This bed is mottled green-brown in its lower and upper parts, which are composed of quartz, goethite and celadonite. These parts of the bed are interpreted to be strongly altered tuffs, reflecting oxidic, low-temperature alteration of a hydrated, Fe-rich, Al-poor tuff, and K and Mg uptake from seawater. The middle part of the bed is a mineralized bacterial mat (quartz, goethite). Textures resembling bacterial cells and colonies are common, with wavy, bulbous laminations composed of mounds overlying a mesh-work stromatolite-like texture constructed of micrometre-size Fe oxides. This bed is concordant with the underlying Mn deposit and marks the termination of Mn accumulation. Although no genetic connection exists between the two, the rocks adjacent to the contact record the oceanographic and bottom-water conditions extant when accumulation of one of the major Mn deposits of Europe ended, when the Transdanubian Range was located in the middle of the Adria-Apulian microcontinent between the Neotethys and Atlantic-Ligurian seaways. A pyroclastic origin for part of the bed has significance for the Toarcian of Central Europe because evidence of volcanism occurring at that time is otherwise sparse. ?? 2010 Geological Society of London.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Geological Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1144/0016-76492008-132","issn":"00167649","usgsCitation":"Polgari, M., Hein, J., Toth, M., Brukner-Wein, A., Vigh, T., Biro, L., and Cserhati, C., 2010, Genesis of a regionally widespread celadonitic chert ironstone bed overlying upper Lias manganese deposits, Hungary: Journal of the Geological Society, v. 167, no. 2, p. 313-328, https://doi.org/10.1144/0016-76492008-132.","startPage":"313","endPage":"328","numberOfPages":"16","costCenters":[],"links":[{"id":217376,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1144/0016-76492008-132"},{"id":245321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"167","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1558e4b0c8380cd54d84","contributors":{"authors":[{"text":"Polgari, Marta","contributorId":75750,"corporation":false,"usgs":true,"family":"Polgari","given":"Marta","email":"","affiliations":[],"preferred":false,"id":460459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hein, J.R. 0000-0002-5321-899X","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":61429,"corporation":false,"usgs":true,"family":"Hein","given":"J.R.","affiliations":[],"preferred":false,"id":460458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toth, M.","contributorId":85442,"corporation":false,"usgs":true,"family":"Toth","given":"M.","affiliations":[],"preferred":false,"id":460460,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brukner-Wein, A.","contributorId":98568,"corporation":false,"usgs":true,"family":"Brukner-Wein","given":"A.","email":"","affiliations":[],"preferred":false,"id":460461,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vigh, T.","contributorId":47613,"corporation":false,"usgs":true,"family":"Vigh","given":"T.","email":"","affiliations":[],"preferred":false,"id":460456,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Biro, L.","contributorId":47207,"corporation":false,"usgs":true,"family":"Biro","given":"L.","email":"","affiliations":[],"preferred":false,"id":460455,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cserhati, C.","contributorId":53633,"corporation":false,"usgs":true,"family":"Cserhati","given":"C.","email":"","affiliations":[],"preferred":false,"id":460457,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70043836,"text":"70043836 - 2010 - Emerging viral diseases of fish and shrimp","interactions":[],"lastModifiedDate":"2013-03-10T12:17:34","indexId":"70043836","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3689,"text":"Veterinary Research","active":true,"publicationSubtype":{"id":10}},"title":"Emerging viral diseases of fish and shrimp","docAbstract":"The rise of aquaculture has been one of the most profound changes in global food production of the past 100 years. Driven by population growth, rising demand for seafood and a levelling of production from capture fisheries, the practice of farming aquatic animals has expanded rapidly to become a major global industry. Aquaculture is now integral to the economies of many countries. It has provided employment and been a major driver of socio-economic development in poor rural and coastal communities, particularly in Asia, and has relieved pressure on the sustainability of the natural harvest from our rivers, lakes and oceans. However, the rapid growth of aquaculture has also been the source of anthropogenic change on a massive scale. Aquatic animals have been displaced from their natural environment, cultured in high density, exposed to environmental stress, provided artificial or unnatural feeds, and a prolific global trade has developed in both live aquatic animals and their products. At the same time, over-exploitation of fisheries and anthropogenic stress on aquatic ecosystems has placed pressure on wild fish populations. Not surprisingly, the consequence has been the emergence and spread of an increasing array of new diseases. This review examines the rise and characteristics of aquaculture, the major viral pathogens of fish and shrimp and their impacts, and the particular characteristics of disease emergence in an aquatic, rather than terrestrial, context. It also considers the potential for future disease emergence in aquatic animals as aquaculture continues to expand and faces the challenges presented by climate change.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Veterinary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"EDP Sciences","publisherLocation":"France","doi":"10.1051/vetres/2010022","usgsCitation":"Winton, J.R., and Walker, P.J., 2010, Emerging viral diseases of fish and shrimp: Veterinary Research, v. 41, no. 6, p. 51-75, https://doi.org/10.1051/vetres/2010022.","startPage":"51","endPage":"75","numberOfPages":"24","ipdsId":"IP-019740","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":475823,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1051/vetres/2010022","text":"Publisher Index Page"},{"id":269024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269023,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1051/vetres/2010022"}],"country":"United States","volume":"41","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-04-23","publicationStatus":"PW","scienceBaseUri":"53cd576ce4b0b290850f776d","contributors":{"authors":[{"text":"Winton, James R. 0000-0002-3505-5509 jwinton@usgs.gov","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":1944,"corporation":false,"usgs":true,"family":"Winton","given":"James","email":"jwinton@usgs.gov","middleInitial":"R.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":474287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, Peter J.","contributorId":24658,"corporation":false,"usgs":true,"family":"Walker","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":474288,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70005023,"text":"70005023 - 2010 - F is for fuller's earth","interactions":[],"lastModifiedDate":"2013-06-05T10:04:46","indexId":"70005023","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":674,"text":"Aggregates Manager","active":true,"publicationSubtype":{"id":10}},"title":"F is for fuller's earth","docAbstract":"Before putting on a wool cardigan, make sure you know how the wool was cleaned.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aggregates Manager","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Randall Reilly Publishing","usgsCitation":"Langer, W.H., 2010, F is for fuller's earth: Aggregates Manager, v. 15, no. 6, p. 40-40.","productDescription":"1 p.","startPage":"40","endPage":"40","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":203907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":24497,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.aggman.com/carved-in-stone-f-is-for-fullers-earth/","linkFileType":{"id":5,"text":"html"}}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8981","contributors":{"authors":[{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":351832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70036228,"text":"70036228 - 2010 - The Lake Ontario zooplankton community before (1987-1991) and after (2001-2005) invasion-induced ecosystem change","interactions":[],"lastModifiedDate":"2012-12-31T12:00:58","indexId":"70036228","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"The Lake Ontario zooplankton community before (1987-1991) and after (2001-2005) invasion-induced ecosystem change","docAbstract":"We assessed changes in Lake Ontario zooplankton biomass, production, and community composition before (1987–1991) and after (2001–2005) invasion-induced ecosystem changes. The ecosystem changes were associated with establishment of invasive dreissenid mussels and invasive predatory cladocerans (<i>Bythotrephes</i> and <i>Cercopagis</i>). Whole-lake total epilimnetic plus metalimnetic zooplankton production declined by approximately half from 42.45 (g dry wt∙m<sup>−2</sup>∙ year<sup>−1</sup>) during 1987–1991 to 21.91 (g dry wt∙m<sup>−2</sup>∙ year<sup>−1</sup>) in 2003 and averaged 21.01 (g dry wt∙m<sup>−2</sup>∙ year<sup>−1</sup>) during 2001–2005. Analysis of two independent data sets indicates that the mean biomass and biomass proportion of cyclopoid copepods declined while the same measures increased for the invasive predatory cladocerans. Changes in means and proportions of all other zooplankton groups were not consistent between the data sets. Cyclopoid copepod biomass and production declined by factors ranging from 3.6 to 5.7. Invasive predatory cladoceran biomass averaged from 5.0% to 8.0% of the total zooplankton biomass. The zooplankton community was otherwise resilient to the invasion-induced disruption as zooplankton species richness and diversity were unaffected. Zooplankton production was likely reduced by declines in primary productivity but may have declined further due to increased predation by alewives and invasive predatory cladocerans. Shifts in zooplankton community structure were consistent with increased predation pressure on cyclopoid copepods by alewives and invasive predatory cladocerans. Predicted declines in the proportion of small cladocerans were not evident. This study represents the first direct comparison of changes in Lake Ontario zooplankton production before and after the invasion-induced disruption and will be important to food web-scale investigations of invasion effects.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Great Lakes Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.jglr.2010.07.010","issn":"03801330","usgsCitation":"Stewart, T., Johannsson, O., Holeck, K., Sprules, W., and O'Gorman, R., 2010, The Lake Ontario zooplankton community before (1987-1991) and after (2001-2005) invasion-induced ecosystem change: Journal of Great Lakes Research, v. 36, no. 4, p. 596-605, https://doi.org/10.1016/j.jglr.2010.07.010.","productDescription":"10 p.","startPage":"596","endPage":"605","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":246366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218365,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jglr.2010.07.010"}],"otherGeospatial":"Lake Ontario","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.9363,43.1696 ], [ -79.9363,44.3608 ], [ -76.0002,44.3608 ], [ -76.0002,43.1696 ], [ -79.9363,43.1696 ] ] ] } } ] }","volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba7a3e4b08c986b3216d4","contributors":{"authors":[{"text":"Stewart, T.J.","contributorId":17198,"corporation":false,"usgs":true,"family":"Stewart","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":454991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johannsson, O. E.","contributorId":40948,"corporation":false,"usgs":true,"family":"Johannsson","given":"O. E.","affiliations":[],"preferred":false,"id":454992,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holeck, K.","contributorId":79340,"corporation":false,"usgs":true,"family":"Holeck","given":"K.","affiliations":[],"preferred":false,"id":454994,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sprules, W.G.","contributorId":85790,"corporation":false,"usgs":true,"family":"Sprules","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":454995,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O'Gorman, R.","contributorId":48896,"corporation":false,"usgs":true,"family":"O'Gorman","given":"R.","affiliations":[],"preferred":false,"id":454993,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70037544,"text":"70037544 - 2010 - The Reimer Diatom Herbarium: An important resource for teaching and research","interactions":[],"lastModifiedDate":"2012-03-12T17:22:04","indexId":"70037544","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The Reimer Diatom Herbarium: An important resource for teaching and research","docAbstract":"The Reimer Diatom Herbarium (ILH) at Iowa Lakeside Laboratory (ILL), a field station of Iowa's state universities, contains 3,280 permanent diatom slides of collections made from prairie potholes, alkaline fens, acid bogs, eutrophic lakes, saline lakes, Pleistocene paleolakes, and Miocene fossil deposits near ILL. The herbarium has a focus on collections made within Dickinson County, a region with an important legacy of study by students and visiting researchers from the US, Canada, and international institutions. The herbarium is well documented by taxon and location catalogues. The taxon card catalogue contains over 2,800 records referencing 67 genera, and the location card catalogue references collection sites from 51 counties in 16 North American states. Curated slides include over 300 species identifications made, or verified, by C.W. Reimer. Most curated slides have diatom specimens identified to species, circled with a diamond objective marker, and indicated on the slide label Six holotypes are included in the herbarium and we present the first light micrograph images of these type specimens. We present documentation of the contents and current condition of the herbarium and report that it is now available to researchers for scientific study. Many of the sites represented in the Reimer Diatom Herbarium are the same locations visited each year by students and visiting researchers at ILL, resulting in an important resource for monitoring environmental change, resolving taxonomic issues, and understanding species distributions in unique habitats.","largerWorkTitle":"Proceedings of the Academy of Natural Sciences of Philadelphia","language":"English","doi":"10.1635/053.160.0103","issn":"00973157","usgsCitation":"Rushforth, S., Edlund, M., Spaulding, S., and Stoermer, E.F., 2010, The Reimer Diatom Herbarium: An important resource for teaching and research, <i>in</i> Proceedings of the Academy of Natural Sciences of Philadelphia, v. 160, p. 13-20, https://doi.org/10.1635/053.160.0103.","startPage":"13","endPage":"20","numberOfPages":"8","costCenters":[],"links":[{"id":246067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218086,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1635/053.160.0103"}],"volume":"160","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba8b2e4b08c986b321dba","contributors":{"authors":[{"text":"Rushforth, S.J.","contributorId":20193,"corporation":false,"usgs":true,"family":"Rushforth","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":461537,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edlund, M.B.","contributorId":63644,"corporation":false,"usgs":true,"family":"Edlund","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":461538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spaulding, S. A. 0000-0002-9787-7743","orcid":"https://orcid.org/0000-0002-9787-7743","contributorId":74390,"corporation":false,"usgs":true,"family":"Spaulding","given":"S. A.","affiliations":[],"preferred":false,"id":461539,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stoermer, E. F.","contributorId":17773,"corporation":false,"usgs":false,"family":"Stoermer","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":461536,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70046694,"text":"dds49102 - 2010 - Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Average Atmospheric (Wet) Deposition of Inorganic Nitrogen, 2002","interactions":[],"lastModifiedDate":"2013-11-25T16:05:46","indexId":"dds49102","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"491-02","title":"Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Average Atmospheric (Wet) Deposition of Inorganic Nitrogen, 2002","docAbstract":"This tabular data set represents the average atmospheric (wet) deposition, in kilograms per square kilometer, of inorganic nitrogen for the year 2002 compiled for every catchment for MRB_E2RF1 of Major River Basins (MRBs, Crawford and others, 2006). The source data set for wet deposition was from the USGS's raster data set atmospheric (wet) deposition of inorganic nitrogen for 2002 (Gronberg, 2005). The MRB_E2RF1 catchments are based on a modified version of the U.S. Environmental Protection Agency's (USEPA) ERF1_2 and include enhancements to support national and regional-scale surface-water quality modeling (Nolan and others, 2002; Brakebill and others, 2011). Data were compiled for every catchment of MRB_E2RF1 catchments for the conterminous United States covering New England and Mid-Atlantic (MRB1), South Atlantic-Gulf and Tennessee (MRB2), the Great Lakes, Ohio, Upper Mississippi, and Souris-Red-Rainy (MRB3), the Missouri (MRB4), the Lower Mississippi, Arkansas-White-Red, and Texas-Gulf (MRB5), the Rio Grande, Colorado, and the Great basin (MRB6), the Pacific Northwest (MRB7) river basins, and California (MRB8).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/dds49102","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Average Atmospheric (Wet) Deposition of Inorganic Nitrogen, 2002: U.S. Geological Survey Data Series 491-02, Dataset, https://doi.org/10.3133/dds49102.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274190,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/mrb_e2rf1_atdep.xml"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.910792,23.243486 ], [ -127.910792,51.657387 ], [ -65.327751,51.657387 ], [ -65.327751,23.243486 ], [ -127.910792,23.243486 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51cabbe0e4b0d298e5434c28","contributors":{"authors":[{"text":"Wieczorek, Michael mewieczo@usgs.gov","contributorId":2309,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Michael","email":"mewieczo@usgs.gov","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":480026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":480027,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70005024,"text":"70005024 - 2010 - G is for gnome","interactions":[],"lastModifiedDate":"2013-06-05T10:06:08","indexId":"70005024","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":674,"text":"Aggregates Manager","active":true,"publicationSubtype":{"id":10}},"title":"G is for gnome","docAbstract":"Possibly based on miners from Southeast Germany, ceramic gnomes feature the pointed red hat often worn by these miners.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aggregates Manager","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Randall Reilly Publishing","usgsCitation":"Langer, W.H., 2010, G is for gnome: Aggregates Manager, v. 15, no. 7, p. 146-146.","productDescription":"1 p.","startPage":"146","endPage":"146","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":204073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":24498,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.aggman.com/carved-in-stone-5/","linkFileType":{"id":5,"text":"html"}}],"volume":"15","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4200","contributors":{"authors":[{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":351833,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046695,"text":"dds49103 - 2010 - Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Basin Characteristics, 2002  Geospatial_Data_Presentation_Form: tabular digital data","interactions":[],"lastModifiedDate":"2013-11-25T16:07:26","indexId":"dds49103","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"491-03","title":"Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Basin Characteristics, 2002  Geospatial_Data_Presentation_Form: tabular digital data","docAbstract":"This tabular data set represents basin characteristics for the year 2002 compiled for every MRB_E2RF1 catchment of selected Major River Basins (MRBs, Crawford and others, 2006).   These characteristics are reach catchment shape index, stream density, sinuosity, mean elevation, mean slope and number of road-stream crossings. The source data sets are based on a modified version of the U.S. Environmental Protection Agency's (USEPA) RF1_2 and include enhancements to support national and regional-scale surface-water quality modeling (Nolan and others, 2002; Brakebill and others, 2011) and the U.S. Census Bureau's TIGER/Line Files (U.S. Census Bureau,2006). The MRB_E2RF1 catchments are based on a modified version of the U.S. Environmental Protection Agency's (USEPA) ERF1_2 and include enhancements to support national and regional-scale surface-water quality modeling (Nolan and others, 2002; Brakebill and others, 2011). Data were compiled for every MRB_E2RF1 catchment for the conterminous United States covering New England and Mid-Atlantic (MRB1), South Atlantic-Gulf and Tennessee (MRB2), the Great Lakes, Ohio, Upper Mississippi, and Souris-Red-Rainy (MRB3), the Missouri (MRB4), the Lower Mississippi, Arkansas-White-Red, and Texas-Gulf (MRB5), the Rio Grande, Colorado, and the Great basin (MRB6), the Pacific Northwest (MRB7) river basins, and California (MRB8).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/dds49103","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Basin Characteristics, 2002  Geospatial_Data_Presentation_Form: tabular digital data: U.S. Geological Survey Data Series 491-03, Dataset, https://doi.org/10.3133/dds49103.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274193,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274192,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/mrb_e2rf1_bchar.xml"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.910792,23.243486 ], [ -127.910792,51.657387 ], [ -65.327751,51.657387 ], [ -65.327751,23.243486 ], [ -127.910792,23.243486 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51cabbe0e4b0d298e5434c30","contributors":{"authors":[{"text":"Wieczorek, Michael mewieczo@usgs.gov","contributorId":2309,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Michael","email":"mewieczo@usgs.gov","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":480028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":480029,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70036512,"text":"70036512 - 2010 - Self-noise models of seismic instruments","interactions":[],"lastModifiedDate":"2012-03-12T17:22:04","indexId":"70036512","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Self-noise models of seismic instruments","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Seismological Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/gssrl.81.6.972","issn":"08950695","usgsCitation":"Ringler, A., and Hutt, C., 2010, Self-noise models of seismic instruments: Seismological Research Letters, v. 81, no. 6, p. 972-983, https://doi.org/10.1785/gssrl.81.6.972.","startPage":"972","endPage":"983","numberOfPages":"12","costCenters":[],"links":[{"id":218267,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/gssrl.81.6.972"},{"id":246263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-11-15","publicationStatus":"PW","scienceBaseUri":"505b8d01e4b08c986b31821a","contributors":{"authors":[{"text":"Ringler, A. T. 0000-0002-9839-4188","orcid":"https://orcid.org/0000-0002-9839-4188","contributorId":99282,"corporation":false,"usgs":true,"family":"Ringler","given":"A. T.","affiliations":[],"preferred":false,"id":456492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutt, C. R. 0000-0001-9033-9195","orcid":"https://orcid.org/0000-0001-9033-9195","contributorId":61910,"corporation":false,"usgs":true,"family":"Hutt","given":"C. R.","affiliations":[],"preferred":false,"id":456491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70036131,"text":"70036131 - 2010 - Impacts of hikers on aquatic invertebrates in the North Fork of the Virgin River, Utah","interactions":[],"lastModifiedDate":"2012-03-12T17:22:06","indexId":"70036131","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3451,"text":"Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Impacts of hikers on aquatic invertebrates in the North Fork of the Virgin River, Utah","docAbstract":"Effects of in-stream hiking on benthic standing stocks and drifting aquatic invertebrates and on organic matter were examined in the North Fork of the Virgin River, Zion National Park, Washington County, Utah. Densities of drifting aquatic invertebrates and organic matter increased with increasing numbers of hikers and reached a threshold level at high numbers of hikers. However, there was no apparent longer-term effect on standing stocks of benthic invertebrates or on organic matter. Densities of benthic invertebrates and organic matter did not differ among sites. Results suggest that in-stream hiking in the North Fork of the Virgin River increases drifting by invertebrates, but invertebrates from nearby undisturbed patches readily colonize impacted reaches.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Southwestern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1894/JS-33.1","issn":"00384909","usgsCitation":"Caires, A., Vinson, M., and Brasher, A., 2010, Impacts of hikers on aquatic invertebrates in the North Fork of the Virgin River, Utah: Southwestern Naturalist, v. 55, no. 4, p. 551-557, https://doi.org/10.1894/JS-33.1.","startPage":"551","endPage":"557","numberOfPages":"7","costCenters":[],"links":[{"id":218245,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1894/JS-33.1"},{"id":246238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a38ede4b0c8380cd61733","contributors":{"authors":[{"text":"Caires, A.M.","contributorId":107542,"corporation":false,"usgs":true,"family":"Caires","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":454380,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vinson, M.R.","contributorId":44755,"corporation":false,"usgs":true,"family":"Vinson","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":454379,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brasher, A.M.D.","contributorId":8213,"corporation":false,"usgs":true,"family":"Brasher","given":"A.M.D.","email":"","affiliations":[],"preferred":false,"id":454378,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037543,"text":"70037543 - 2010 - Seismic performance assessment of base-isolated safety-related nuclear structures","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037543","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1434,"text":"Earthquake Engineering and Structural Dynamics","active":true,"publicationSubtype":{"id":10}},"title":"Seismic performance assessment of base-isolated safety-related nuclear structures","docAbstract":"Seismic or base isolation is a proven technology for reducing the effects of earthquake shaking on buildings, bridges and infrastructure. The benefit of base isolation has been presented in terms of reduced accelerations and drifts on superstructure components but never quantified in terms of either a percentage reduction in seismic loss (or percentage increase in safety) or the probability of an unacceptable performance. Herein, we quantify the benefits of base isolation in terms of increased safety (or smaller loss) by comparing the safety of a sample conventional and base-isolated nuclear power plant (NPP) located in the Eastern U.S. Scenario- and time-based assessments are performed using a new methodology. Three base isolation systems are considered, namely, (1) Friction Pendulum??? bearings, (2) lead-rubber bearings and (3) low-damping rubber bearings together with linear viscous dampers. Unacceptable performance is defined by the failure of key secondary systems because these systems represent much of the investment in a new build power plant and ensure the safe operation of the plant. For the scenario-based assessments, the probability of unacceptable performance is computed for an earthquake with a magnitude of 5.3 at a distance 7.5 km from the plant. For the time-based assessments, the annual frequency of unacceptable performance is computed considering all potential earthquakes that may occur. For both assessments, the implementation of base isolation reduces the probability of unacceptable performance by approximately four orders of magnitude for the same NPP superstructure and secondary systems. The increase in NPP construction cost associated with the installation of seismic isolators can be offset by substantially reducing the required seismic strength of secondary components and systems and potentially eliminating the need to seismically qualify many secondary components and systems. ?? 2010 John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Engineering and Structural Dynamics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/eqe.1038","issn":"00988847","usgsCitation":"Huang, Y., Whittaker, A., and Luco, N., 2010, Seismic performance assessment of base-isolated safety-related nuclear structures: Earthquake Engineering and Structural Dynamics, v. 39, no. 13, p. 1421-1442, https://doi.org/10.1002/eqe.1038.","startPage":"1421","endPage":"1442","numberOfPages":"22","costCenters":[],"links":[{"id":218073,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/eqe.1038"},{"id":246053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"13","noUsgsAuthors":false,"publicationDate":"2010-09-20","publicationStatus":"PW","scienceBaseUri":"505b8b34e4b08c986b317682","contributors":{"authors":[{"text":"Huang, Y.-N.","contributorId":98860,"corporation":false,"usgs":true,"family":"Huang","given":"Y.-N.","email":"","affiliations":[],"preferred":false,"id":461535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whittaker, A.S.","contributorId":8596,"corporation":false,"usgs":true,"family":"Whittaker","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":461533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luco, N.","contributorId":34240,"corporation":false,"usgs":true,"family":"Luco","given":"N.","email":"","affiliations":[],"preferred":false,"id":461534,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70044510,"text":"70044510 - 2010 - Novel silver tubing method for quantitative introduction of water into high temperature conversion systems for stable hydrogen and oxygen isotopic measurements","interactions":[],"lastModifiedDate":"2018-10-10T09:58:07","indexId":"70044510","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3233,"text":"Rapid Communications in Mass Spectrometry","active":true,"publicationSubtype":{"id":10}},"title":"Novel silver tubing method for quantitative introduction of water into high temperature conversion systems for stable hydrogen and oxygen isotopic measurements","docAbstract":"A new method to seal water in silver tubes for use in a TC/EA reduction unit using a semi-automated sealing apparatus can yield reproducibilities (1 standard deviation) of &delta;<sup>2</sup>H and &delta<sup>18</sup>O measurements of 1.0 ‰ and 0.06 ‰, respectively. These silver tubes containing reference waters may be preferred for calibration of H- and O-bearing materials analyzed with a TC/EA reduction unit. The new sealing apparatus employs a computer controlled stepping motor to produce silver tubes identical in length. The reproducibility of mass of water sealed in tubes (in a range of 200 to 400 µg) can be as good as 1 percent. Although silver tubes sealed with reference waters are robust and can be shaken or heated to 110 °C with no loss of integrity, they should not be frozen because the expansion during the phase transition of water to ice will break the cold seals and all water will be lost. They should be shipped in insulated containers. This new method eliminates air inclusions and isotopic fractionation of water associated with the loading of water into capsules using a syringe. The method is also more than an order of magnitude faster than preparing water samples in ordinary Ag capsules. Nevertheless, some laboratories may prefer loading water into silver capsules because expensive equipment is not needed, but they are cautioned to apply the necessary corrections for evaporation, back exchange with laboratory atmospheric moisture, and blank.","language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1002/rcm.4559","usgsCitation":"Qi, H., Groning, M., Coplen, T.B., Buck, B., Mroczkowski, S.J., Brand, W., Geilmann, H., and Gehre, M., 2010, Novel silver tubing method for quantitative introduction of water into high temperature conversion systems for stable hydrogen and oxygen isotopic measurements: Rapid Communications in Mass Spectrometry, v. 24, no. 13, p. 1821-1827, https://doi.org/10.1002/rcm.4559.","productDescription":"7 p.","startPage":"1821","endPage":"1827","numberOfPages":"7","additionalOnlineFiles":"N","ipdsId":"IP-020156","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":588,"text":"Toxic Hydrology Program","active":false,"usgs":true}],"links":[{"id":269701,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269698,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/rcm.4559"}],"volume":"24","issue":"13","noUsgsAuthors":false,"publicationDate":"2010-06-02","publicationStatus":"PW","scienceBaseUri":"514988f2e4b0971933f6369f","contributors":{"authors":[{"text":"Qi, Haiping 0000-0002-8339-744X haipingq@usgs.gov","orcid":"https://orcid.org/0000-0002-8339-744X","contributorId":507,"corporation":false,"usgs":true,"family":"Qi","given":"Haiping","email":"haipingq@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":475775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Groning, Manfred","contributorId":47659,"corporation":false,"usgs":true,"family":"Groning","given":"Manfred","affiliations":[],"preferred":false,"id":475782,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coplen, Tyler B. 0000-0003-4884-6008 tbcoplen@usgs.gov","orcid":"https://orcid.org/0000-0003-4884-6008","contributorId":508,"corporation":false,"usgs":true,"family":"Coplen","given":"Tyler","email":"tbcoplen@usgs.gov","middleInitial":"B.","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":475776,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buck, Bryan bbuck@usgs.gov","contributorId":2326,"corporation":false,"usgs":true,"family":"Buck","given":"Bryan","email":"bbuck@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":475777,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mroczkowski, Stanley J. 0000-0001-8026-6025 smroczko@usgs.gov","orcid":"https://orcid.org/0000-0001-8026-6025","contributorId":2628,"corporation":false,"usgs":true,"family":"Mroczkowski","given":"Stanley","email":"smroczko@usgs.gov","middleInitial":"J.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":475778,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brand, Willi A.","contributorId":38866,"corporation":false,"usgs":true,"family":"Brand","given":"Willi A.","affiliations":[],"preferred":false,"id":475780,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Geilmann, Heike","contributorId":41303,"corporation":false,"usgs":false,"family":"Geilmann","given":"Heike","email":"","affiliations":[{"id":13365,"text":"Max-Planck Institute for Biogeochemistry, Jena, Germany","active":true,"usgs":false}],"preferred":false,"id":475781,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gehre, Matthias","contributorId":34004,"corporation":false,"usgs":false,"family":"Gehre","given":"Matthias","email":"","affiliations":[],"preferred":false,"id":475779,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70037541,"text":"70037541 - 2010 - Rehabilitation for bilateral amputation of fingers","interactions":[],"lastModifiedDate":"2012-12-28T15:29:52","indexId":"70037541","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":728,"text":"American Journal of Occupational Therapy","active":true,"publicationSubtype":{"id":10}},"title":"Rehabilitation for bilateral amputation of fingers","docAbstract":"We describe reconstructive surgeries, therapy, prostheses, and adaptations for a patient who experienced bilateral amputation of all five fingers of both hands through the proximal phalanges in January 1992. The patient made considerable progress in the use of his hands in the 10 mo after amputation, including nearly a 120% increase in the active range of flexion of metacarpophalangeal joints. In late 1992 and early 1993, the patient had \"on-top plasty\" surgeries, in which the index finger remnants were transferred onto the thumb stumps, performed on both hands. The increased web space and functional pinch resulting from these procedures made many tasks much easier. The patient and occupational therapists set challenging goals at all times. Moreover, the patient was actively involved in the design and fabrication of all prostheses and adaptations or he developed them himself. Although he was discharged from occupational therapy in 1997, the patient continues to actively find new solutions for prehension and grip strength 18 yr after amputation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Journal of Occupational Therapy","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Occupational Therapy Association Press","publisherLocation":"Bethesda, MD","doi":"10.5014/ajot.2010.09153","issn":"02729490","usgsCitation":"Stapanian, M.A., Stapanian, A., and Staley, K.E., 2010, Rehabilitation for bilateral amputation of fingers: American Journal of Occupational Therapy, v. 64, no. 6, p. 923-928, https://doi.org/10.5014/ajot.2010.09153.","productDescription":"6 p.","startPage":"923","endPage":"928","costCenters":[],"links":[{"id":246041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218061,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.5014/ajot.2010.09153"}],"volume":"64","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-11-01","publicationStatus":"PW","scienceBaseUri":"50e4a5fbe4b0e8fec6cdc04a","contributors":{"authors":[{"text":"Stapanian, Martin A. 0000-0001-8173-4273 mstapanian@usgs.gov","orcid":"https://orcid.org/0000-0001-8173-4273","contributorId":3425,"corporation":false,"usgs":true,"family":"Stapanian","given":"Martin","email":"mstapanian@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":461522,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stapanian, Adrienne","contributorId":101125,"corporation":false,"usgs":true,"family":"Stapanian","given":"Adrienne","email":"","affiliations":[],"preferred":false,"id":461524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staley, Keith E.","contributorId":42819,"corporation":false,"usgs":true,"family":"Staley","given":"Keith","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":461523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037539,"text":"70037539 - 2010 - Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties","interactions":[],"lastModifiedDate":"2012-03-12T17:22:05","indexId":"70037539","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2468,"text":"Journal of Structural Geology","active":true,"publicationSubtype":{"id":10}},"title":"Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties","docAbstract":"The presence of clays in fault rocks influences both the mechanical and hydrologic properties of clay-bearing faults, and therefore it is critical to understand the origin of clays in fault rocks and their distributions is of great importance for defining fundamental properties of faults in the shallow crust. Field mapping shows that layers of clay gouge and shale smear are common along the Moab Fault, from exposures with throws ranging from 10 to ???1000 m. Elemental analyses of four locations along the Moab Fault show that fault rocks are enriched in clays at R191 and Bartlett Wash, but that this clay enrichment occurred at different times and was associated with different fluids. Fault rocks at Corral and Courthouse Canyons show little difference in elemental composition from adjacent protolith, suggesting that formation of fault rocks at those locations is governed by mechanical processes. Friction tests show that these authigenic clays result in fault zone weakening, and potentially influence the style of failure along the fault (seismogenic vs. aseismic) and potentially influence the amount of fluid loss associated with coseismic dilation. Scanning electron microscopy shows that authigenesis promotes that continuity of slip surfaces, thereby enhancing seal capacity. The occurrence of the authigenesis, and its influence on the sealing properties of faults, highlights the importance of determining the processes that control this phenomenon. ?? 2010 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Structural Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jsg.2010.07.009","issn":"01918141","usgsCitation":"Solum, J., Davatzes, N., and Lockner, D., 2010, Fault-related clay authigenesis along the Moab Fault: Implications for calculations of fault rock composition and mechanical and hydrologic fault zone properties: Journal of Structural Geology, v. 32, no. 12, p. 1899-1911, https://doi.org/10.1016/j.jsg.2010.07.009.","startPage":"1899","endPage":"1911","numberOfPages":"13","costCenters":[],"links":[{"id":218059,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jsg.2010.07.009"},{"id":246039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0f20e4b0c8380cd537a5","contributors":{"authors":[{"text":"Solum, J.G.","contributorId":79280,"corporation":false,"usgs":true,"family":"Solum","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":461508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davatzes, N.C.","contributorId":59219,"corporation":false,"usgs":true,"family":"Davatzes","given":"N.C.","email":"","affiliations":[],"preferred":false,"id":461507,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":461509,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70044496,"text":"70044496 - 2010 - Mid-Piacenzian sea surface temperature record from ODP Site 1115 in the western equatorial Pacific","interactions":[],"lastModifiedDate":"2013-03-18T09:05:49","indexId":"70044496","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3481,"text":"Stratigraphy","active":true,"publicationSubtype":{"id":10}},"title":"Mid-Piacenzian sea surface temperature record from ODP Site 1115 in the western equatorial Pacific","docAbstract":"Planktic foraminifer assemblages and alkenone unsaturation ratios have been analyzed for the mid-Piacen-zian (3.3 to 2.9 Ma) section of Ocean Drilling Program (ODP) Site 1115B, located in the western equatorial Pacific off the coast of New Guinea. Cold and warm season sea surface temperature (SST) estimates were determined using a modern analog technique. ODP Site 1115 is located just south of the transition between the planktic foraminifer tropical and subtropical faunal provinces and approximates the southern boundary of the western equatorial Pacific (WEP) warm pool. Comparison of the faunal and alkenone SST estimates (presented here) with an existing nannofossil climate proxy shows similar trends. Results of this analysis show increased seasonal variability during the middle of the sampled section (3.22 to 3.10 Ma), suggesting a possible northward migration of both the subtropical faunal province and the southern boundary of the WEP warm pool.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Stratigraphy","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Micropaleontology Press","publisherLocation":"Flushing, NY","usgsCitation":"Stoll, D., 2010, Mid-Piacenzian sea surface temperature record from ODP Site 1115 in the western equatorial Pacific: Stratigraphy, v. 7, no. 1, p. 1-6.","productDescription":"6 p.","startPage":"1","endPage":"6","additionalOnlineFiles":"N","ipdsId":"IP-017982","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":269646,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269645,"type":{"id":15,"text":"Index Page"},"url":"https://www.micropress.org/stratigraphy/"}],"volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51483796e4b022dd171afea2","contributors":{"authors":[{"text":"Stoll, Danielle","contributorId":34005,"corporation":false,"usgs":true,"family":"Stoll","given":"Danielle","affiliations":[],"preferred":false,"id":475728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70037535,"text":"70037535 - 2010 - Numerical simulation of a low-lying barrier island's morphological response to Hurricane Katrina","interactions":[],"lastModifiedDate":"2012-03-12T17:22:05","indexId":"70037535","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1262,"text":"Coastal Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Numerical simulation of a low-lying barrier island's morphological response to Hurricane Katrina","docAbstract":"Tropical cyclones that enter or form in the Gulf of Mexico generate storm surge and large waves that impact low-lying coastlines along the Gulf Coast. The Chandeleur Islands, located 161. km east of New Orleans, Louisiana, have endured numerous hurricanes that have passed nearby. Hurricane Katrina (landfall near Waveland MS, 29 Aug 2005) caused dramatic changes to the island elevation and shape. In this paper the predictability of hurricane-induced barrier island erosion and accretion is evaluated using a coupled hydrodynamic and morphodynamic model known as XBeach. Pre- and post-storm island topography was surveyed with an airborne lidar system. Numerical simulations utilized realistic surge and wave conditions determined from larger-scale hydrodynamic models. Simulations included model sensitivity tests with varying grid size and temporal resolutions. Model-predicted bathymetry/topography and post-storm survey data both showed similar patterns of island erosion, such as increased dissection by channels. However, the model under predicted the magnitude of erosion. Potential causes for under prediction include (1) errors in the initial conditions (the initial bathymetry/topography was measured three years prior to Katrina), (2) errors in the forcing conditions (a result of our omission of storms prior to Katrina and/or errors in Katrina storm conditions), and/or (3) physical processes that were omitted from the model (e.g., inclusion of sediment variations and bio-physical processes). ?? 2010.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Coastal Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coastaleng.2010.06.004","issn":"03783839","usgsCitation":"Lindemer, C., Plant, N., Puleo, J., Thompson, D., and Wamsley, T., 2010, Numerical simulation of a low-lying barrier island's morphological response to Hurricane Katrina: Coastal Engineering, v. 57, no. 11-12, p. 985-995, https://doi.org/10.1016/j.coastaleng.2010.06.004.","startPage":"985","endPage":"995","numberOfPages":"11","costCenters":[],"links":[{"id":246008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":218031,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coastaleng.2010.06.004"}],"volume":"57","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6906e4b0c8380cd73b1f","contributors":{"authors":[{"text":"Lindemer, C.A.","contributorId":11862,"corporation":false,"usgs":true,"family":"Lindemer","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":461492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plant, N.G.","contributorId":94023,"corporation":false,"usgs":true,"family":"Plant","given":"N.G.","email":"","affiliations":[],"preferred":false,"id":461495,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Puleo, Jack A.","contributorId":108287,"corporation":false,"usgs":true,"family":"Puleo","given":"Jack A.","affiliations":[],"preferred":false,"id":461496,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, D.M.","contributorId":16570,"corporation":false,"usgs":true,"family":"Thompson","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":461493,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wamsley, T.V.","contributorId":60477,"corporation":false,"usgs":true,"family":"Wamsley","given":"T.V.","email":"","affiliations":[],"preferred":false,"id":461494,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70043784,"text":"70043784 - 2010 - Analyzing debris flows with the statistically calibrated empirical model LAHARZ in southeastern Arizona, USA","interactions":[],"lastModifiedDate":"2020-12-02T15:03:26.875496","indexId":"70043784","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Analyzing debris flows with the statistically calibrated empirical model LAHARZ in southeastern Arizona, USA","docAbstract":"<p><span>Hazard-zone delineation for extreme events is essential for floodplain management near mountain fronts in arid and semiarid regions. On 31 July 2006, unprecedented debris flows occurred in the Santa Catalina Mountains of southeastern Arizona following extreme multiday precipitation (recurrence interval &gt;</span><span>&nbsp;</span><span>1000</span><span>&nbsp;</span><span>years for 4-day precipitation). Most mobilized sediment contributing to debris flows was derived from shallow-seated failures of colluvium on steep slopes. A total of 435 slope failures in the southern Santa Catalina Mountains released 1.34</span><span>&nbsp;</span><span>million</span><span>&nbsp;</span><span>Mg of sediment into the channels of 10 drainage basins. Five drainages produced debris flows that moved to the apices of alluvial fans on the southern edge of the mountain front, damaging infrastructure and aggrading channels to reduce future flood conveyance. Using the statistically calibrated, empirical debris-flow model LAHARZ and modified model coefficients developed to better match conditions in southeastern Arizona, we predicted the approximate area of deposition and travel distance in comparison to observed depositional areas and travel distance for seven debris flows. Two of the modeled debris flows represented single slope failures that terminated downslope with no additive influence of other debris flows or streamflow flooding. Five of the simulated debris flows represented the aggregation of multiple slope failures and streamflow flooding into multiple debris-flow pulses. Because LAHARZ is a debris-flow hazard-zone delineation tool, the complexity of alternating transport and deposition zones in channels with abrupt expansions and contractions reduces the applicability of the model in some drainage basins.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.geomorph.2010.02.022","usgsCitation":"Magirl, C.S., Griffiths, P.G., and Webb, R., 2010, Analyzing debris flows with the statistically calibrated empirical model LAHARZ in southeastern Arizona, USA: Geomorphology, v. 119, no. 1-2, p. 111-124, https://doi.org/10.1016/j.geomorph.2010.02.022.","productDescription":"14 p.","startPage":"111","endPage":"124","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-011799","costCenters":[{"id":148,"text":"Branch of Regional Research-Western Region","active":false,"usgs":true},{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true},{"id":49157,"text":"Rocky Mountain Regional Office","active":true,"usgs":true}],"links":[{"id":274285,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.82,31.33 ], [ -114.82,37.0 ], [ -109.05,37.0 ], [ -109.05,31.33 ], [ -114.82,31.33 ] ] ] } } ] }","volume":"119","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51ceb05fe4b044272b8e8914","contributors":{"authors":[{"text":"Magirl, Christopher S. 0000-0002-9922-6549 magirl@usgs.gov","orcid":"https://orcid.org/0000-0002-9922-6549","contributorId":1822,"corporation":false,"usgs":true,"family":"Magirl","given":"Christopher","email":"magirl@usgs.gov","middleInitial":"S.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true},{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":474238,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffiths, Peter G. 0000-0002-8663-8907 pggriffi@usgs.gov","orcid":"https://orcid.org/0000-0002-8663-8907","contributorId":187,"corporation":false,"usgs":true,"family":"Griffiths","given":"Peter","email":"pggriffi@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":474236,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webb, Robert H. rhwebb@usgs.gov","contributorId":1573,"corporation":false,"usgs":false,"family":"Webb","given":"Robert H.","email":"rhwebb@usgs.gov","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":474237,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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