{"pageNumber":"3215","pageRowStart":"80350","pageSize":"25","recordCount":184900,"records":[{"id":70126194,"text":"70126194 - 2000 - Benthic foraminifera and environmental changes in Long Island Sound","interactions":[],"lastModifiedDate":"2017-11-18T12:20:13","indexId":"70126194","displayToPublicDate":"2000-09-19T11:07:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Benthic foraminifera and environmental changes in Long Island Sound","docAbstract":"Benthic foraminiferal faunas in Long Island Sound (LIS) in the 1940s and 1960s were of low diversity, and dominated by species of the genus <i>Elphidium</i>, mainly <i>Elphidium excavatum clavatum</i>, with common <i>Buccella frigida</i> and <i>Eggerella advena</i>. The distribution of these species was dominantly correlated with depth, but it was not clear which depth-related environmental variable was most important. Differences between faunas collected in 1996 and 1997, and in the 1940s and 1960s include a strong decrease in relative abundance of <i>Eggerella advena</i> over all LIS, an increase in relative abundance of <i>Ammonia beccarii</i> in western LIS, and a decrease in species diversity. The decreased diversity suggests that environmental stress caused the faunal changes. Oxygen isotope data for <i>E. excavatum clavatum</i> indicate that a change in salinity is not a probable cause. Carbon isotope data suggest that the supply of organic matter to the benthos increased since the early 1960s, with a stronger increase in western LIS where algal blooms have occurred since the early 1970s, possibly as a result of nutrient input by waste water treatment plants. These blooms or the resulting episodes of anoxia/hypoxia may have played a role in the increased relative abundance of <i>A. beccarii</i>. There is no clear explanation for the decreased abundance of <i>E. advena</i>, but changes in the phytoplankton composition (thus food supply) are a possible cause. Benthic foraminiferal faunal and stable isotope data have excellent potential as indicators of physicochemical environmental changes and their effects on the biota in LIS.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Coastal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Coastal Education and Research Foundation","usgsCitation":"Thomas, E., Gapotchenko, T., Varekamp, J., Mecray, E., and Buchholtz ten Brink, M.R., 2000, Benthic foraminifera and environmental changes in Long Island Sound: Journal of Coastal Research, v. 16, no. 3, p. 641-655.","productDescription":"15 p.","startPage":"641","endPage":"655","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":294215,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294214,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/4300076"}],"country":"United States","state":"Connecticut, New York","otherGeospatial":"Long Island Sound","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.827,40.7578 ], [ -73.827,41.3293 ], [ -72.0244,41.3293 ], [ -72.0244,40.7578 ], [ -73.827,40.7578 ] ] ] } } ] }","volume":"16","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"541d459be4b0f68901ec30a3","contributors":{"authors":[{"text":"Thomas, E.","contributorId":64467,"corporation":false,"usgs":true,"family":"Thomas","given":"E.","email":"","affiliations":[],"preferred":false,"id":501903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gapotchenko, T.","contributorId":40528,"corporation":false,"usgs":true,"family":"Gapotchenko","given":"T.","email":"","affiliations":[],"preferred":false,"id":501901,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Varekamp, J.C.","contributorId":56006,"corporation":false,"usgs":true,"family":"Varekamp","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":501902,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mecray, E.I.","contributorId":81814,"corporation":false,"usgs":true,"family":"Mecray","given":"E.I.","email":"","affiliations":[],"preferred":false,"id":501904,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Buchholtz ten Brink, Marilyn R.","contributorId":88021,"corporation":false,"usgs":true,"family":"Buchholtz ten Brink","given":"Marilyn","email":"","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":501900,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70126186,"text":"70126186 - 2000 - Predicting coastal evolution at societally-relevant time and space scales","interactions":[],"lastModifiedDate":"2017-12-15T15:02:33","indexId":"70126186","displayToPublicDate":"2000-09-19T10:09:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"21","title":"Predicting coastal evolution at societally-relevant time and space scales","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The potential consequences of climate variability and change","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"National Oceanic and Atmospheric Administration","usgsCitation":"Thieler, E., 2000, Predicting coastal evolution at societally-relevant time and space scales, 3 p.","productDescription":"3 p.","startPage":"131","endPage":"133","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":294206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"541d45a1e4b0f68901ec30da","contributors":{"authors":[{"text":"Thieler, E.R. 0000-0003-4311-9717","orcid":"https://orcid.org/0000-0003-4311-9717","contributorId":93082,"corporation":false,"usgs":true,"family":"Thieler","given":"E.R.","affiliations":[],"preferred":false,"id":501881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70126185,"text":"70126185 - 2000 - Stratigraphic and structural evolution of the Selenga Delta Accommodation Zone, Lake Baikal Rift, Siberia","interactions":[],"lastModifiedDate":"2017-09-27T14:54:27","indexId":"70126185","displayToPublicDate":"2000-09-19T09:12:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2037,"text":"International Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphic and structural evolution of the Selenga Delta Accommodation Zone, Lake Baikal Rift, Siberia","docAbstract":"Seismic reflection profiles from the Lake Baikal Rift reveal extensive details about the sediment thickness, structural geometry and history of extensional deformation and syn-rift sedimentation in this classic continental rift. The Selenga River is the largest single source of terrigenous input into Lake Baikal, and its large delta sits astride the major accommodation zone between the Central and South basins of the lake. Incorporating one of the world's largest lacustrine deltas, this depositional system is a classic example of the influence of rift basin structural segmentation on a major continental drainage. More than 3700 km of deep basin-scale multi-channel seismic reflection (MCS) data were acquired during the 1989 Russian and the 1992 Russian–American field programs. The seismic data image most of the sedimentary section, including pre-rift basement in several localities. The MCS data reveal that the broad bathymetric saddle between these two major half-graben basins is underlain by a complex of severely deformed basement blocks, and is not simply a consequence of long-term deltaic deposition. Maximum sediment thickness is estimated to be more than 9 km in some areas around the Selenga Delta. Detailed stratigraphic analyses of the Selenga area MCS data suggest that modes of deposition have shifted markedly during the history of the delta. The present mode of gravity- and mass-flow sedimentation that dominates the northern and southern parts of the modern delta, as well as the pronounced bathymetric relief in the area, are relatively recent developments in the history of the Lake Baikal Rift. Several episodes of major delta progradation, each extending far across the modern rift, can be documented in the MCS data. The stratigraphic framework defined by these prograding deltaic sequences can be used to constrain the structural as well as depositional evolution of this part of the Baikal Rift. An age model has been established for this stratigraphy, by tying the delta sequences to the site of the Baikal Drilling Project 1993 Drill Hole. Although the drill hole is only 100 m deep, and the base of the cores is only ∼670 ka in age, ages were extrapolated to deeper stratigraphic intervals using the Reflection-Seismic-Radiocarbon method of Cohen et al. (1993). The deep prograding delta sequences now observed in the MCS data probably formed in response to major fluctuations in sediment supply, rather than in response to shifts in lake level. This stratigraphic framework and age model suggest that the deep delta packages developed at intervals of approximately 400 ka and may have formed as a consequence of climate changes affiliated with the northern hemisphere glaciations. The stratigraphic analysis also suggests that the Selenga Basin and Syncline developed as a distinct depocentre only during the past ∼2–3 Ma.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Earth Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s005310000095","usgsCitation":"Scholz, C., and Hutchinson, D.R., 2000, Stratigraphic and structural evolution of the Selenga Delta Accommodation Zone, Lake Baikal Rift, Siberia: International Journal of Earth Sciences, v. 89, no. 2, p. 212-228, https://doi.org/10.1007/s005310000095.","productDescription":"17 p.","startPage":"212","endPage":"228","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":294204,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia","otherGeospatial":"Lake Baikal Rift","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 104.9,52.29 ], [ 104.9,55.65 ], [ 113.1,55.65 ], [ 113.1,52.29 ], [ 104.9,52.29 ] ] ] } } ] }","volume":"89","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"541d45a7e4b0f68901ec310a","contributors":{"authors":[{"text":"Scholz, C.A.","contributorId":76810,"corporation":false,"usgs":true,"family":"Scholz","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":501880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, D. R.","contributorId":31770,"corporation":false,"usgs":true,"family":"Hutchinson","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":501879,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185741,"text":"70185741 - 2000 - The age of scarplike landforms from diffusion-equation analysis","interactions":[],"lastModifiedDate":"2021-03-25T16:09:33.969312","indexId":"70185741","displayToPublicDate":"2000-09-18T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"19","title":"The age of scarplike landforms from diffusion-equation analysis","docAbstract":"<p>The purpose of this paper is to review developments in the quantitative modeling of fault-scarp geomorphology, principally those since 1980. These developments utilize diffusionequation mathematics, in several different forms, as the basic model of fault-scarp evolution. Because solutions to the general diffusion equation evolve with time, as we expect faultscarp morphology to evolve with time, the model solutions carry information about the age of the structure and thus its time of formation; hence the inclusion of this paper in this volume. The evolution of fault-scarp morphology holds a small but special place in the much larger class of problems in landform evolution. In general, landform evolution means the evolution of topography as a function of both space and time. It is the outcome of the competition among those tectonic processes that make topography, erosive processes that destroy topography, and depositional processes that redistribute topography. Deposition and erosion can always be coupled through conservation-of-mass relations, but in general deposition occurs at great distance from the source region of detritus. Moreover, erosion is an inherently rough process whereas deposition is inherently smooth, as is evident from even casual inspection of shaded-relief, digital-elevation maps (e.g., Thelin and Pike, 1990; Simpson and Anders, 1992) and the current fascination with fractal representations oferoding terrains (e.g., Huang and Turcotte, 1989; Newman and Turcotte, 1990). Nevertheless, large-scale landform-evolution modeling, now a computationally intensive, advanced numerical exercise, is generating ever more realistic landforms (e.g., Willgoose and others, 1991a,b; Kooi and Beaumont, 1994; Tucker and Slingerland, 1994), although many of the rate coefficients remain poorly prescribed</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Quaternary geochronology: Methods and applications v. 4","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/RF004p0313","usgsCitation":"Hanks, T.C., 2000, The age of scarplike landforms from diffusion-equation analysis, chap. 19 <i>of</i> Quaternary geochronology: Methods and applications v. 4, v. 4, p. 313-338, https://doi.org/10.1029/RF004p0313.","productDescription":"26 p.","startPage":"313","endPage":"338","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":338486,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","noUsgsAuthors":false,"publicationDate":"2013-03-11","publicationStatus":"PW","scienceBaseUri":"58db7632e4b0ee37af29e4aa","contributors":{"authors":[{"text":"Hanks, Thomas C. 0000-0003-0928-0056 thanks@usgs.gov","orcid":"https://orcid.org/0000-0003-0928-0056","contributorId":3065,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","email":"thanks@usgs.gov","middleInitial":"C.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":686611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70125421,"text":"70125421 - 2000 - Comment [on “Sea level rise shown to drive coastal erosion”]","interactions":[],"lastModifiedDate":"2014-09-16T15:15:11","indexId":"70125421","displayToPublicDate":"2000-09-16T15:12:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Comment [on “Sea level rise shown to drive coastal erosion”]","docAbstract":"Leatherman et al. [2000] (Eos, Trans., AGU, February 8, 2000, p.55) affirm that global eustatic sea-level rise is driving coastal erosion. Furthermore, they argue that the long-term average rate of shoreline retreat is 150 times the rate of sea-level rise. This rate, they say, is more than a magnitude greater than would be expected from a simple response to sea-level rise through inundation of the shoreline. We agree that sea-level rise is the primary factor causing shoreline retreat in stable coastal areas.This is intuitive. We also believe, however, that the Leatherman et al. [2000] study has greatly underestimated the rate of coastal recession along most low slope shorelines. Slopes along the North Carolina continental shelf/coastal plain approach 10,000:1. To us, this suggests that we should expect rates of shoreline recession 10,000 times the rate of sea-level rise through simple inundation of the shoreline.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Eos, Transactions American Geophysical Union","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/00EO00034","usgsCitation":"Pilkey, O.H., Young, R.S., and Bush, D.M., 2000, Comment [on “Sea level rise shown to drive coastal erosion”]: Eos, Transactions, American Geophysical Union, v. 81, no. 38, https://doi.org/10.1029/00EO00034.","productDescription":"1 p.","startPage":"436","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293999,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293997,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/00EO00034"}],"volume":"81","issue":"38","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"54195129e4b091c7ffc8e60e","contributors":{"authors":[{"text":"Pilkey, Orrin H.","contributorId":11606,"corporation":false,"usgs":true,"family":"Pilkey","given":"Orrin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":501408,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, Robert S.","contributorId":94612,"corporation":false,"usgs":true,"family":"Young","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":501409,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bush, David M.","contributorId":98658,"corporation":false,"usgs":true,"family":"Bush","given":"David","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":501410,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70125401,"text":"70125401 - 2000 - Rapid movement of wastewater from on-site disposal systems into surface waters in the lower Florida Keys","interactions":[],"lastModifiedDate":"2022-09-29T13:12:09.798505","indexId":"70125401","displayToPublicDate":"2000-09-16T14:06:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Rapid movement of wastewater from on-site disposal systems into surface waters in the lower Florida Keys","docAbstract":"<p><span>Viral tracer studies have been used previously to study the potential for wastewater contamination of surface marine waters in the Upper and Middle Florida Keys. Two bacteriophages, the marine bacteriophage ϕHSIC and the </span><i>Salmonella</i><span>&nbsp;phage PRD1, were used as tracers in injection well and septic tank studies in Saddlebunch Keys of the Lower Florida Keys and in septic tank studies in Boot Key Harbor, Marathon, of the Middle Keys. In Boot Key Harbor, both phages were detected in a canal adjacent to the seeded septic tank within 3 h 15 min of the end of the seed period. The tracer was then detected at all sampling sites in Boot Key Harbor, including one on the opposite side of U.S. Highway 1 in Florida Bay, and at an Atlantic Ocean beach outside Boot Key Harbor. Rates of migration based on first appearance of the phage ranged from 1.7 to 57.5 m h</span><sup>−1</sup><span>. In Saddlebunch Keys, ϕHSIC and PRD1 were used to seed a residential septic tank and a commercial injection well. The septic tank tracer was not found in any surface water samples. The injection well tracer was first detected at a site most distant from the seed site, a channel that connected Sugarloaf Sound with the Atlantic Ocean. The, rate of tracer migration from the injection well to this channel ranged from 66.8 to 141 m h</span><sup>−1</sup><span>. Both tracer studies showed a rapid movement of wastewater from on-site sewage treatment and disposal systems in a southeasterly direction toward the reef tract and Atlantic Ocean, with preferential movement through tidal channels. These studies indicate that wastewater disposal systems currently in widespread use in the Florida Keys can rapidly contaminate the marine environment.</span></p>","language":"English","publisher":"Coastal and Estuarine Research Foundation","doi":"10.2307/1352892","usgsCitation":"Paul, J.H., McLaughlin, M.R., Griffin, D.W., Lipp, E.K., Stokes, R., and Rose, J.B., 2000, Rapid movement of wastewater from on-site disposal systems into surface waters in the lower Florida Keys: Estuaries, v. 23, no. 5, p. 662-668, https://doi.org/10.2307/1352892.","productDescription":"9 p.","startPage":"662","endPage":"668","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293988,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Keys","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.633824,24.580938 ], [ -81.633824,24.714542 ], [ -81.076819,24.714542 ], [ -81.076819,24.580938 ], [ -81.633824,24.580938 ] ] ] } } ] }","volume":"23","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5419514fe4b091c7ffc8e801","contributors":{"authors":[{"text":"Paul, John H.","contributorId":28183,"corporation":false,"usgs":true,"family":"Paul","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":501395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLaughlin, Molly R. 0000-0001-6962-6392 mmclaughlin@usgs.gov","orcid":"https://orcid.org/0000-0001-6962-6392","contributorId":4089,"corporation":false,"usgs":true,"family":"McLaughlin","given":"Molly","email":"mmclaughlin@usgs.gov","middleInitial":"R.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":501393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Griffin, Dale W. 0000-0003-1719-5812 dgriffin@usgs.gov","orcid":"https://orcid.org/0000-0003-1719-5812","contributorId":2178,"corporation":false,"usgs":true,"family":"Griffin","given":"Dale","email":"dgriffin@usgs.gov","middleInitial":"W.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":501392,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lipp, Erin K.","contributorId":73823,"corporation":false,"usgs":true,"family":"Lipp","given":"Erin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":501396,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stokes, Rodger","contributorId":6383,"corporation":false,"usgs":true,"family":"Stokes","given":"Rodger","email":"","affiliations":[],"preferred":false,"id":501394,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rose, Joan B.","contributorId":81791,"corporation":false,"usgs":true,"family":"Rose","given":"Joan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":501397,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70125394,"text":"70125394 - 2000 - Introduction to Quaternary geochronology","interactions":[],"lastModifiedDate":"2021-03-25T17:57:17.040535","indexId":"70125394","displayToPublicDate":"2000-09-16T13:54:00","publicationYear":"2000","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Introduction to Quaternary geochronology","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Quaternary geochronology: Methods and applications","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/RF004p0001","usgsCitation":"Noller, J.S., Sowers, J.M., Colman, S.M., and Pierce, K.L., 2000, Introduction to Quaternary geochronology, chap. <i>of</i> Quaternary geochronology: Methods and applications, v. 4, p. 1-10, https://doi.org/10.1029/RF004p0001.","productDescription":"10 p.","startPage":"1","endPage":"10","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":293981,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","noUsgsAuthors":false,"publicationDate":"2013-03-11","publicationStatus":"PW","scienceBaseUri":"54195141e4b091c7ffc8e72a","contributors":{"editors":[{"text":"Noller, Jay Stratton","contributorId":64166,"corporation":false,"usgs":true,"family":"Noller","given":"Jay","email":"","middleInitial":"Stratton","affiliations":[],"preferred":false,"id":509994,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Sowers, Janet M.","contributorId":51318,"corporation":false,"usgs":true,"family":"Sowers","given":"Janet","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":509993,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Lettis, William R.","contributorId":85970,"corporation":false,"usgs":true,"family":"Lettis","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509995,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Noller, Jay Stratton","contributorId":64166,"corporation":false,"usgs":true,"family":"Noller","given":"Jay","email":"","middleInitial":"Stratton","affiliations":[],"preferred":false,"id":501381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sowers, Janet M.","contributorId":51318,"corporation":false,"usgs":true,"family":"Sowers","given":"Janet","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":501380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Colman, Steven M.","contributorId":6439,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":501379,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":501378,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70125377,"text":"70125377 - 2000 - Hurricanes, coral reefs and rainforests: resistance, ruin and recovery in the Caribbean","interactions":[],"lastModifiedDate":"2017-12-15T14:30:00","indexId":"70125377","displayToPublicDate":"2000-09-16T13:23:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":698,"text":"Ambio","active":true,"publicationSubtype":{"id":10}},"title":"Hurricanes, coral reefs and rainforests: resistance, ruin and recovery in the Caribbean","docAbstract":"The coexistence of hurricanes, coral reefs, and rainforests in the Caribbean demonstrates that highly structured ecosystems with great diversity can flourish in spite of recurring exposure to intense destructive energy. Coral reefs develop in response to wave energy and resist hurricanes largely by virtue of their structural strength. Limited fetch also protects some reefs from fully developed hurricane waves. While storms may produce dramatic local reef damage, they appear to have little impact on the ability of coral reefs to provide food or habitat for fish and other animals. Rainforests experience an enormous increase in wind energy during hurricanes with dramatic structural changes in the vegetation. The resulting changes in forest microclimate are larger than those on reefs and the loss of fruit, leaves, cover, and microclimate has a great impact on animal populations. Recovery of many aspects of rainforest structure and function is rapid, though there may be long-term changes in species composition. While resistance and repair have maintained reefs and rainforests in the past, human impacts may threaten their ability to survive.","language":"English","publisher":"Royal Swedish Academy of Sciences","doi":"10.1579/0044-7447-29.2.106","usgsCitation":"Lugo, A.E., Rogers, C.S., and Nixon, S.W., 2000, Hurricanes, coral reefs and rainforests: resistance, ruin and recovery in the Caribbean: Ambio, v. 29, no. 2, p. 106-114, https://doi.org/10.1579/0044-7447-29.2.106.","productDescription":"9 p.","startPage":"106","endPage":"114","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293972,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293971,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1579/0044-7447-29.2.106"}],"otherGeospatial":"Caribbean","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.17,9.99 ], [ -85.17,27.26 ], [ -59.42,27.26 ], [ -59.42,9.99 ], [ -85.17,9.99 ] ] ] } } ] }","volume":"29","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5419513ee4b091c7ffc8e705","contributors":{"authors":[{"text":"Lugo, Ariel E.","contributorId":10111,"corporation":false,"usgs":true,"family":"Lugo","given":"Ariel","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":725152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, Caroline S. 0000-0001-9056-6961 caroline_rogers@usgs.gov","orcid":"https://orcid.org/0000-0001-9056-6961","contributorId":3126,"corporation":false,"usgs":true,"family":"Rogers","given":"Caroline","email":"caroline_rogers@usgs.gov","middleInitial":"S.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":725153,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nixon, Scott W.","contributorId":63676,"corporation":false,"usgs":true,"family":"Nixon","given":"Scott","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":725154,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70125358,"text":"70125358 - 2000 - A review of the geologic framework of the Long Island Sound Basin, with some observations relating to postglacial sedimentation","interactions":[],"lastModifiedDate":"2018-03-05T16:40:01","indexId":"70125358","displayToPublicDate":"2000-09-16T13:09:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"A review of the geologic framework of the Long Island Sound Basin, with some observations relating to postglacial sedimentation","docAbstract":"<p>Most of the papers in this thematic section present regional perspectives that build on more than 100 years of geologic investigation in Long Island Sound. When viewed collectively, a common theme emerges in these works. The major geologic components of the Long Island Sound basin (bedrock, buried coastal-plain strata, recessional moraines, glacial-lake deposits, and the remains of a large marine delta) interact with the water body to affect the way the modern sedimentary system functions.</p><p>Previous work, along with our present knowledge of the geologic framework of the Long Island Sound basin, is comprehensively reviewed with this theme in mind. Aspects of the crystalline bedrock, and the deltaic deposits associated with glacial Lake Connecticut, are examined with respect to their influence on sedimentation along the Connecticut coast and in the northern and western Sound. We also discuss the influence of the glacial drift that mantles the coastal-plain remnant along the north shore of Long Island and in the southern Sound.</p><p>A total of approximately 22.7 billion m<sup>3</sup> of marine sediment has accumulated in the Long Island Sound basin. A significant portion (44%) of the fine-grained marine section in the central and western basins was redistributed there from the eastern Sound, as tidal scour removed slightly over 5 billion m<sup>3</sup> (5.3 X 10<sup>12</sup> kg) of fine material from glacial lake and early-marine deposits east of the Connecticut River. The remainder of the estimated 1.2 X 10<sup>13</sup> kg of fine-grained marine sediment that now resides in the central and western Sound can be accounted for by riverine input over the past 13.5 ka.</p>","language":"English","publisher":"Coastal Education and Research Foundation","usgsCitation":"Lewis, R., and DiGiacomo-Cohen, M.L., 2000, A review of the geologic framework of the Long Island Sound Basin, with some observations relating to postglacial sedimentation: Journal of Coastal Research, v. 16, no. 3, p. 522-532.","productDescription":"11 p.","startPage":"522","endPage":"532","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":293966,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293965,"type":{"id":15,"text":"Index Page"},"url":"https://journals.fcla.edu/jcr/article/view/80857"}],"country":"United States","state":"Connecticut, New York","otherGeospatial":"Long Island Sound","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.826969,40.757828 ], [ -73.826969,41.329272 ], [ -72.024425,41.329272 ], [ -72.024425,40.757828 ], [ -73.826969,40.757828 ] ] ] } } ] }","volume":"16","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54195120e4b091c7ffc8e57b","contributors":{"authors":[{"text":"Lewis, Ralph S.","contributorId":9288,"corporation":false,"usgs":true,"family":"Lewis","given":"Ralph S.","affiliations":[],"preferred":false,"id":501328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DiGiacomo-Cohen, Mary L. 0000-0003-2384-8912 mdicohen@usgs.gov","orcid":"https://orcid.org/0000-0003-2384-8912","contributorId":2527,"corporation":false,"usgs":true,"family":"DiGiacomo-Cohen","given":"Mary","email":"mdicohen@usgs.gov","middleInitial":"L.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":501327,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70125356,"text":"70125356 - 2000 - Airborne laser mapping of Assateague National Seashore Beach","interactions":[],"lastModifiedDate":"2014-09-16T13:02:54","indexId":"70125356","displayToPublicDate":"2000-09-16T12:51:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Airborne laser mapping of Assateague National Seashore Beach","docAbstract":"Results are presented from topographic surveys of the Assateague Island National Seashore using an airborne scanning laser altimeter and kinematic Global Positioning System (GPS) technology.  The instrument used was the Airborne Topographic Mapper (ATM), developed by the NASA Arctic Ice Mapping (AIM) group from the Goddard Space Flight Center's Wallops Flight Facility.  In November, 1995, and again in May, 1996, these topographic surveys were flown as a functionality check prior to conducting missions to measure the elevation of extensive sections of the Greenland Ice Sheet as part of NASA's Global Climate Change program.  Differences between overlapping portions of both surveys are compared for quality control.  An independent assessment of the accuracy of the ATM survey is provided by comparison to surface surveys which were conducted using standard techniques.  The goal of these projects is to make these measurements to an accuracy of &plusmn; 10 cm.  Differences between the fall 1995 and 1996 surveys provides an assessment of net changes in the beach morphology over an annual cycle.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Krabill, W., Wright, C.W., Swift, R., Frederick, E., Manizade, S., Yungel, J., Martin, C., Sonntag, J., Duffy, M., Hulslander, W., and Brock, J., 2000, Airborne laser mapping of Assateague National Seashore Beach: Photogrammetric Engineering and Remote Sensing, v. 66, no. 1, p. 65-71.","productDescription":"7 p.","startPage":"65","endPage":"71","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293958,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryl","otherGeospatial":"Assateague Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.415522,37.845283 ], [ -75.415522,38.32727 ], [ -75.083727,38.32727 ], [ -75.083727,37.845283 ], [ -75.415522,37.845283 ] ] ] } } ] }","volume":"66","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54195123e4b091c7ffc8e5b3","contributors":{"authors":[{"text":"Krabill, W.B.","contributorId":22952,"corporation":false,"usgs":true,"family":"Krabill","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":501312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, C. W. wwright@usgs.gov","contributorId":49758,"corporation":false,"usgs":true,"family":"Wright","given":"C.","email":"wwright@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":false,"id":501315,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swift, R.N.","contributorId":67705,"corporation":false,"usgs":true,"family":"Swift","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":501318,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frederick, E.B.","contributorId":72994,"corporation":false,"usgs":true,"family":"Frederick","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":501319,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Manizade, S.S.","contributorId":53312,"corporation":false,"usgs":true,"family":"Manizade","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":501316,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Yungel, J.K.","contributorId":30160,"corporation":false,"usgs":true,"family":"Yungel","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":501313,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Martin, C.F.","contributorId":44846,"corporation":false,"usgs":true,"family":"Martin","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":501314,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sonntag, J.G.","contributorId":77065,"corporation":false,"usgs":true,"family":"Sonntag","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":501320,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Duffy, Mark","contributorId":54852,"corporation":false,"usgs":true,"family":"Duffy","given":"Mark","email":"","affiliations":[],"preferred":false,"id":501317,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Hulslander, William","contributorId":106030,"corporation":false,"usgs":true,"family":"Hulslander","given":"William","email":"","affiliations":[],"preferred":false,"id":501321,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Brock, John 0000-0002-5289-9332 jbrock@usgs.gov","orcid":"https://orcid.org/0000-0002-5289-9332","contributorId":2261,"corporation":false,"usgs":true,"family":"Brock","given":"John","email":"jbrock@usgs.gov","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":501311,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70125344,"text":"70125344 - 2000 - Protection of fish spawning habitat for the conservation of warm-temperature reef-fish fisheries of shelf-edge reefs of Florida","interactions":[],"lastModifiedDate":"2018-01-30T18:53:14","indexId":"70125344","displayToPublicDate":"2000-09-16T12:38:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Protection of fish spawning habitat for the conservation of warm-temperature reef-fish fisheries of shelf-edge reefs of Florida","docAbstract":"We mapped and briefly describe the surficial geology of selected examples of shelf-edge reefs (50–120 m deep) of the southeastern United States, which are apparently derived from ancient Pleistocene shorelines and are intermittently distributed throughout the region. These reefs are ecologically significant because they support a diverse array of fish and invertebrate species, and they are the only aggregation spawning sites of gag (<i>Mycteroperca microlepis</i>), scamp (<i>M. phenax</i>), and other economically important reef fish. Our studies on the east Florida shelf in the Experimental <i>Oculina</i> Research Reserve show that extensive damage to the habitat-structuring coral <i>Oculina varicosa</i> has occurred in the past, apparently from trawling and dredging activities of the 1970s and later. On damaged or destroyed <i>Oculina</i> habitat, reef-fish abundance and diversity are low, whereas on intact habitat, reef-fish diversity is relatively high compared to historical diversity on the same site. The abundance and biomass of the economically important reef fish was much higher in the past than it is now, and spawning aggregations of gag and scamp have been lost or greatly reduced in size. On the west Florida shelf, fishers have concentrated on shelf-edge habitats for over 100 yrs, but fishing intensity increased dramatically in the 1980s. Those reefs are characterized by low abundance of economically important species. The degree and extent of habitat damage there is unknown. We recommend marine fishery reserves to protect habitat and for use in experimentally examining the potential production of unfished communities.","language":"English","publisher":"University of Miami","usgsCitation":"Koenig, C., Coleman, F., Grimes, C.B., Fitzhugh, G.R., Scanlon, K.M., Gledhill, C.T., and Grace, M., 2000, Protection of fish spawning habitat for the conservation of warm-temperature reef-fish fisheries of shelf-edge reefs of Florida: Bulletin of Marine Science, v. 66, no. 3, p. 593-616.","productDescription":"24 p.","startPage":"593","endPage":"616","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293952,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293951,"type":{"id":15,"text":"Index Page"},"url":"https://www.ingentaconnect.com/content/umrsmas/bullmar/2000/00000066/00000003/art00008#expand/collapse"}],"country":"United 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R.","contributorId":70307,"corporation":false,"usgs":true,"family":"Fitzhugh","given":"Gary","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":501296,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scanlon, Kathryn M.","contributorId":6816,"corporation":false,"usgs":true,"family":"Scanlon","given":"Kathryn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":501294,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gledhill, Christopher T.","contributorId":61355,"corporation":false,"usgs":true,"family":"Gledhill","given":"Christopher","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":501295,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Grace, Mark","contributorId":18286,"corporation":false,"usgs":true,"family":"Grace","given":"Mark","email":"","affiliations":[],"preferred":false,"id":501292,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70125330,"text":"70125330 - 2000 - Sea-floor environments within Long Island Sound: A regional overview","interactions":[],"lastModifiedDate":"2017-09-19T11:10:22","indexId":"70125330","displayToPublicDate":"2000-09-16T11:44:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Sea-floor environments within Long Island Sound: A regional overview","docAbstract":"<p>Modern sea-floor sedimentary environments within the glaciated, topographically complex Long Island Sound estuary have been interpreted and mapped from an extensive collection of sidescan sonographs, bottom samples, and video-camera observations together with supplemental bathymetric, marine-geologic, and bottom-current data. Four categories of environments are present that reflect the dominant long-term processes of erosion or nondeposition; coarsegrained bedload transport; sediment sorting and reworking; and fine-grained deposition. (1) Environments of erosion or nondeposition contain exposures of glacial drift, coarse lag deposits, and possibly bedrock and include sediments which range from boulder fields to gravelly coarse-to-medium sands. (2) Environments of coarse-grained bedload transport are mantled by sand ribbons and sand waves and contain mostly coarse-to-fine sands with only small amounts of mud. (3) Environments of sediment sorting and reworking comprise both uniform and heterogeneous sediment types and contain variable amounts of fine sand and mud. (4) Environments of fine-grained deposition are blanketed by muds and sandy muds.</p>\n<br> \n<p>The patchy distribution of sedimentary environments within Long Island Sound reflects both regional and local changes in bottom processes. Regional changes are primarily the result of a strong, east-to-west decreasing gradient of bottom tidal-current speeds, coupled with the net (westward) estuarine bottom drift. The regional current regime has produced a westward succession of environments along the basin floor beginning with erosion or nondeposition at the narrow eastern entrance to the Sound, changing to an extensive area of coarse-grained bedload transport, passing into a contiguous band of sediment sorting, and ending with broad areas of fine-grained deposition in the central and western Sound. However, local changes in processes are superimposed on the regional conditions within the central and western parts of the basin and along the nearshore margins. Within the central and western basin, localized sedimentary environments are produced where the bottom flow is enhanced by, and interacts with, the bottom topography, whereas along the nearshore margins, they variously reflect wave-produced currents, the irregular bathymetry, the indented shoreline, and the proximal supply of sediments.</p>\n<br> \n<p>Results from this study (1) confirm the high trapping efficiency of fine-grained sediments in the Sound, (2) suggest that fine-grained sediments accumulate at an average (regional) rate of 0.08 g/cm<sup>2</sup>/y , and (3) indicate that the postglacial delta in the eastern Sound was a significant source of fine-grained sediments now buried beneath depositional areas.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Coastal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Coastal Education and Research Foundation","usgsCitation":"Knebel, H.J., and Poppe, L., 2000, Sea-floor environments within Long Island Sound: A regional overview: Journal of Coastal Research, v. 16, no. 3, p. 533-550.","productDescription":"18 p.","startPage":"533","endPage":"550","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":293943,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293942,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/view/4300069"}],"country":"United States","state":"Connecticut, New York","otherGeospatial":"Long Island Sound","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.827,40.7578 ], [ -73.827,41.3293 ], [ -72.0244,41.3293 ], [ -72.0244,40.7578 ], [ -73.827,40.7578 ] ] ] } } ] }","volume":"16","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54195153e4b091c7ffc8e832","contributors":{"authors":[{"text":"Knebel, Harley J.","contributorId":25930,"corporation":false,"usgs":true,"family":"Knebel","given":"Harley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":501291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poppe, Lawrence J. lpoppe@usgs.gov","contributorId":2149,"corporation":false,"usgs":true,"family":"Poppe","given":"Lawrence J.","email":"lpoppe@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":501290,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70125329,"text":"70125329 - 2000 - Regional processes, conditions, and characteristics of the Long Island Sound sea floor","interactions":[],"lastModifiedDate":"2017-09-19T10:08:14","indexId":"70125329","displayToPublicDate":"2000-09-16T11:35:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Regional processes, conditions, and characteristics of the Long Island Sound sea floor","docAbstract":"No abstract available.","language":"English","publisher":"Coastal Education and Research Foundation","usgsCitation":"Knebel, H.J., Lewis, R., and Varekamp, J.C., 2000, Regional processes, conditions, and characteristics of the Long Island Sound sea floor: Journal of Coastal Research, v. 16, no. 3, p. 519-521.","productDescription":"3 p.","startPage":"519","endPage":"521","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":293937,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293936,"type":{"id":15,"text":"Index Page"},"url":"https://journals.fcla.edu/jcr/article/view/80856"}],"country":"United States","state":"Connecticut, New York","otherGeospatial":"Long Island Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.90502929687499,\n              40.9218144123785\n            ],\n            [\n              -72.1142578125,\n              40.9218144123785\n            ],\n            [\n              -72.1142578125,\n              41.28606238749825\n            ],\n            [\n              -73.90502929687499,\n              41.28606238749825\n            ],\n            [\n              -73.90502929687499,\n              40.9218144123785\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"16","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54195150e4b091c7ffc8e80b","contributors":{"authors":[{"text":"Knebel, Harley J.","contributorId":25930,"corporation":false,"usgs":true,"family":"Knebel","given":"Harley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":501288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Ralph S.","contributorId":9288,"corporation":false,"usgs":true,"family":"Lewis","given":"Ralph S.","affiliations":[],"preferred":false,"id":501287,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Varekamp, Johan C. Johan C.","contributorId":87470,"corporation":false,"usgs":true,"family":"Varekamp","given":"Johan","suffix":"Johan C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":501289,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70125327,"text":"70125327 - 2000 - Barataria barrier-shoreline feasibility study","interactions":[],"lastModifiedDate":"2014-09-16T11:28:23","indexId":"70125327","displayToPublicDate":"2000-09-16T11:23:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3432,"text":"Soundwaves: coastal and marine research news from across the USGS","active":true,"publicationSubtype":{"id":10}},"title":"Barataria barrier-shoreline feasibility study","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Soundwaves: coastal and marine research news from across the USGS","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Kindinger, J., 2000, Barataria barrier-shoreline feasibility study: Soundwaves: coastal and marine research news from across the USGS, HTML document.","productDescription":"HTML document","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293931,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293930,"type":{"id":15,"text":"Index Page"},"url":"https://soundwaves.usgs.gov/2000/06/"}],"country":"United States","state":"Louisiana","otherGeospatial":"Barataria Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.98744,29.328828 ], [ -89.98744,29.427299 ], [ -89.847076,29.427299 ], [ -89.847076,29.328828 ], [ -89.98744,29.328828 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54195124e4b091c7ffc8e5ce","contributors":{"authors":[{"text":"Kindinger, Jack","contributorId":107338,"corporation":false,"usgs":true,"family":"Kindinger","given":"Jack","affiliations":[],"preferred":false,"id":501286,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70125322,"text":"70125322 - 2000 - Contrasting patterns of habitat use by prawns and crayfish in a headwater marsh of the St. Johns River, Florida","interactions":[],"lastModifiedDate":"2014-09-16T11:16:56","indexId":"70125322","displayToPublicDate":"2000-09-16T11:11:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2235,"text":"Journal of Crustacean Biology","active":true,"publicationSubtype":{"id":10}},"title":"Contrasting patterns of habitat use by prawns and crayfish in a headwater marsh of the St. Johns River, Florida","docAbstract":"We compared seasonal patterns of habitat use by the prawn <i>Palaemonetes paludosus</i> and the crayfish <i>Procambarus alleni</i> in Blue Cypress Marsh Conservation Area, Florida. Prawn densities were similar to those found in other oligotrophic wetlands of southern Florida, whereas crayfish densities were much greater than reported previously for other wetlands in the area. Prawns and crayfish had strikingly different patterns of habitat use. Prawn density and biomass were similar in wet prairies and sloughs, whereas crayfish density and biomass were significantly higher in wet prairies. Within habitats, the abundance of prawns and crayfish generally increased with increasing structural complexity and the abundance of crayfish generally decreased with increasing water depth. Differences in risk of predation, frequency of agonistic encounters, food availability, and other factors likely contributed to observed patterns of habitat use. Because of differences in their ability to burrow and avoid concentration into dry-season refugia, prawns and crayfish responded very differently to seasonal variation in hydrologic conditions. Prawn densities were initially low (following a severe drought) and then increased during much of the study period, whereas crayfish densities were relatively stable throughout the study period. Overall, it appears that prawns are more responsive to antecedent hydrologic conditions and crayfish are more responsive to the availability of suitable habitats such as wet prairies.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Crustacean Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Crustacean Society","doi":"10.1651/0278-0372(2000)020[0769:CPOHUB]2.0.CO;2","usgsCitation":"Jordan, F., Babbitt, K.J., McIvor, C.C., and Miller, S.J., 2000, Contrasting patterns of habitat use by prawns and crayfish in a headwater marsh of the St. Johns River, Florida: Journal of Crustacean Biology, v. 20, no. 4, p. 769-776, https://doi.org/10.1651/0278-0372(2000)020[0769:CPOHUB]2.0.CO;2.","productDescription":"8 p.","startPage":"769","endPage":"776","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293929,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293928,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1651/0278-0372(2000)020[0769:CPOHUB]2.0.CO;2"}],"country":"United States","state":"Florida","otherGeospatial":"St. Johns River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.947127,28.574612 ], [ -80.947127,28.593052 ], [ -80.939039,28.593052 ], [ -80.939039,28.574612 ], [ -80.947127,28.574612 ] ] ] } } ] }","volume":"20","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5419512ae4b091c7ffc8e623","contributors":{"authors":[{"text":"Jordan, Frank","contributorId":103405,"corporation":false,"usgs":true,"family":"Jordan","given":"Frank","affiliations":[],"preferred":false,"id":501268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Babbitt, Kimberly J.","contributorId":72316,"corporation":false,"usgs":true,"family":"Babbitt","given":"Kimberly","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":501265,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McIvor, Carole C.","contributorId":73254,"corporation":false,"usgs":true,"family":"McIvor","given":"Carole","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":501266,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Steven J.","contributorId":93836,"corporation":false,"usgs":true,"family":"Miller","given":"Steven","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":501267,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70125319,"text":"70125319 - 2000 - Evaluation of remote-sensing techniques to measure decadal-scale changes of Hofsjokull ice cap, Iceland","interactions":[],"lastModifiedDate":"2017-08-30T10:16:37","indexId":"70125319","displayToPublicDate":"2000-09-16T10:25:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2328,"text":"Journal of Glaciology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of remote-sensing techniques to measure decadal-scale changes of Hofsjokull ice cap, Iceland","docAbstract":"Dynamic surficial changes and changes in the position of the firn line and the areal extent of Hofsjökull ice cap, Iceland, were studied through analysis of a time series (1973–98) of synthetic-aperture radar (SAR) and Landsat data. A digital elevation model of Hofsjökull, which was constructed using SAR interferometry, was used to plot the SAR backscatter coefficient (\u0001\u0001σ°) vs elevation and air temperature along transects across the ice cap. Seasonal and daily σ° patterns are caused by freezing or thawing of the ice-cap surface, and abrupt changes in σ° are noted when the air temperature ranges from ∼−5° to 0°C. Late-summer 1997 σ° (SAR) and reflectance (Landsat) boundaries agree and appear to be coincident with the firn line and a SAR σ° boundary that can be seen in the January 1998 SAR image. In January 1994 through 1998, the elevation of this σ° boundary on the ice capwas quite stable, ranging from 1000 to 1300 m, while the equilibrium-line altitude, as measured on the ground, varied considerably. Thus the equilibrium line may be obscured by firn from previous years. Techniques are established to measure long-term changes in the elevation of the firn line and changes in the position of the ice margin.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3189/172756500781833061","usgsCitation":"Hall, D., Williams, R., Barton, J., Sigurdsson, O., Smith, L., and Garvin, J., 2000, Evaluation of remote-sensing techniques to measure decadal-scale changes of Hofsjokull ice cap, Iceland: Journal of Glaciology, v. 46, no. 154, p. 375-388, https://doi.org/10.3189/172756500781833061.","productDescription":"14 p.","startPage":"375","endPage":"388","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":479117,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3189/172756500781833061","text":"Publisher Index Page"},{"id":293913,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Iceland","otherGeospatial":"Hofsjokull ice cap","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -18.8487,64.8072 ], [ -18.8487,64.8262 ], [ -18.7847,64.8262 ], [ -18.7847,64.8072 ], [ -18.8487,64.8072 ] ] ] } } ] }","volume":"46","issue":"154","noUsgsAuthors":false,"publicationDate":"2017-09-08","publicationStatus":"PW","scienceBaseUri":"54195130e4b091c7ffc8e67d","contributors":{"authors":[{"text":"Hall, D.K.","contributorId":84506,"corporation":false,"usgs":true,"family":"Hall","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":501254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":501252,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barton, J.S.","contributorId":54905,"corporation":false,"usgs":true,"family":"Barton","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":501253,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sigurdsson, O.","contributorId":30156,"corporation":false,"usgs":true,"family":"Sigurdsson","given":"O.","email":"","affiliations":[],"preferred":false,"id":501250,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, L.C.","contributorId":88561,"corporation":false,"usgs":true,"family":"Smith","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":501255,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Garvin, J.B.","contributorId":37652,"corporation":false,"usgs":true,"family":"Garvin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":501251,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70125315,"text":"70125315 - 2000 - Last interglacial reef growth beneath Belize barrier and isolated platform reefs","interactions":[],"lastModifiedDate":"2022-09-21T16:51:08.205212","indexId":"70125315","displayToPublicDate":"2000-09-16T10:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Last interglacial reef growth beneath Belize barrier and isolated platform reefs","docAbstract":"We report the first radiometric dates (thermal-ionization mass spectrometry) from late Pleistocene reef deposits from offshore Belize, the location of the largest modern reef complex in the Atlantic Ocean. The results presented here can be used to explain significant differences in bathymetry, sedimentary facies, and reef development of this major reef area, and the results are significant because they contribute to the knowledge of the regional geology of the eastern Yucatán. The previously held concept of a neotectonically stable eastern Yucatán is challenged. The dates indicate that Pleistocene reefs and shallow-water limestones, which form the basement of modern reefs in the area, accumulated ca. 125–130 ka. Significant differences in elevation of the samples relative to present sea level (>10 m) have several possible causes. Differential subsidence along a series of continental margin fault blocks in combination with variation in karstification are probably the prime causes. Differential subsidence is presumably related to initial extension and later left-lateral movements along the adjacent active boundary between the North American and Caribbean plates. Increasing dissolution toward the south during Pleistocene sea-level lowstands is probably a consequence of higher precipitation rates in mountainous southern Belize.","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(2000)28<387:LIRGBB>2.0.CO;2","usgsCitation":"Gischler, E., Lomando, A.J., Hudson, J., and Holmes, C.W., 2000, Last interglacial reef growth beneath Belize barrier and isolated platform reefs: Geology, v. 28, no. 5, p. 387-390, https://doi.org/10.1130/0091-7613(2000)28<387:LIRGBB>2.0.CO;2.","productDescription":"4 p.","startPage":"387","endPage":"390","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":479119,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://doc.rero.ch/record/13985/files/PAL_E998.pdf","text":"External Repository"},{"id":293906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Belize","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.23,15.89 ], [ -89.23,18.5 ], [ -87.49,18.5 ], [ -87.49,15.89 ], [ -89.23,15.89 ] ] ] } } ] }","volume":"28","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54195144e4b091c7ffc8e752","contributors":{"authors":[{"text":"Gischler, Eberhard","contributorId":49285,"corporation":false,"usgs":true,"family":"Gischler","given":"Eberhard","email":"","affiliations":[],"preferred":false,"id":501237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lomando, Anthony J.","contributorId":79817,"corporation":false,"usgs":true,"family":"Lomando","given":"Anthony","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":501239,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hudson, J. Harold","contributorId":54897,"corporation":false,"usgs":true,"family":"Hudson","given":"J. Harold","affiliations":[],"preferred":false,"id":501238,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Holmes, Charles W.","contributorId":31071,"corporation":false,"usgs":true,"family":"Holmes","given":"Charles","email":"","middleInitial":"W.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":501236,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70125313,"text":"70125313 - 2000 - Portable coastal observatories","interactions":[],"lastModifiedDate":"2017-09-14T09:32:58","indexId":"70125313","displayToPublicDate":"2000-09-16T09:40:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2929,"text":"Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Portable coastal observatories","docAbstract":"Ocean observational science is in the midst of a paradigm shift from an expeditionary science centered on short research cruises and deployments of internally recording instruments to a sustained observational science where the ocean is monitored on a regular basis, much the way the atmosphere is monitored. While satellite remote sensing is one key way of meeting the challenge of real-time monitoring of large ocean regions, new technologies are required for in situ observations to measure conditions below the ocean surface and to measure ocean characteristics not observable from space. One method of making sustained observations in the coastal ocean is to install a fiber optic cable from shore to the area of interest. This approach has the advantage of providing power to offshore instruments and essentially unlimited bandwidth for data. The LEO-15 observatory offshore of New Jersey (yon Alt et al., 1997) and the planned Katama observatory offshore of Martha's Vineyard (Edson et al., 2000) use this approach. These sites, along with other cabled sites, will play an important role in coastal ocean science in the next decade. Cabled observatories, however, have two drawbacks that limit the number of sites that are likely to be installed. First, the cable and the cable installation are expensive and the shore station needed at the cable terminus is often in an environmentally sensitive area where competing interests must be resolved. Second, cabled sites are inherently limited geographically to sites within reach of the cable, so it is difficult to cover large areas of the coastal ocean.","language":"English","publisher":"Oceanography Society","doi":"10.5670/oceanog.2000.30","usgsCitation":"Frye, D., Butman, B., Johnson, M., von der Heydt, K., and Lerner, S., 2000, Portable coastal observatories: Oceanography, v. 13, no. 2, p. 24-31, https://doi.org/10.5670/oceanog.2000.30.","productDescription":"8 p.","startPage":"24","endPage":"31","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":479120,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5670/oceanog.2000.30","text":"Publisher Index Page"},{"id":293898,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Massachusetts Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.180419921875,\n              41.672911819602085\n            ],\n            [\n              -69.58740234375,\n              41.672911819602085\n            ],\n            [\n              -69.58740234375,\n              43.1090040242731\n            ],\n            [\n              -71.180419921875,\n              43.1090040242731\n            ],\n            [\n              -71.180419921875,\n              41.672911819602085\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5419514be4b091c7ffc8e7c8","contributors":{"authors":[{"text":"Frye, Daniel","contributorId":67021,"corporation":false,"usgs":true,"family":"Frye","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":501235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":501231,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Mark","contributorId":48272,"corporation":false,"usgs":true,"family":"Johnson","given":"Mark","email":"","affiliations":[],"preferred":false,"id":501233,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"von der Heydt, Keith","contributorId":21078,"corporation":false,"usgs":true,"family":"von der Heydt","given":"Keith","email":"","affiliations":[],"preferred":false,"id":501232,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lerner, Steven","contributorId":49282,"corporation":false,"usgs":true,"family":"Lerner","given":"Steven","email":"","affiliations":[],"preferred":false,"id":501234,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70124948,"text":"70124948 - 2000 - Holocene and recent sediment accumulation rates in southern Lake Michigan","interactions":[],"lastModifiedDate":"2017-11-05T10:20:43","indexId":"70124948","displayToPublicDate":"2000-09-12T12:03:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Holocene and recent sediment accumulation rates in southern Lake Michigan","docAbstract":"Rates of sediment accumulation in Lake Michigan are a key component of its geologic history and provide important data related to societal concerns such as shoreline erosion and the fate of anthropogenic pollutants. Previous attempts to reconstruct Holocene rates of sediment accumulation in Lake Michigan, as well as in the other Laurentian Great Lakes, have been bedeviled by the effect of refractory terrestrial material on radiocarbon ages from total organic carbon samples of lake sediments. AMS radiocarbon ages on small samples of biogenic carbonate (ostracodes and mollusks) in Lake Michigan provide accurate Holocene ages. The present bicarbonate reservoir effect is estimated from shells of mollusks collected live before atmospheric nuclear testing to be 250 yr. From paired samples of biogenic carbonate and terrestrial macrofossils, the past reservoir effect is thought to be less than 500 yr. The radiocarbon ages indicate a distinct decrease in sediment accumulation rates throughout the southern basin of Lake Michigan at about 5 ka, about the time when lake level stabilized at the Nipissing level after rising rapidly for several thousand years. Average rates of sediment accumulation for the historic period (the last 150 yr) can be estimated from radioisotopes (<sup>210</sup>Pb and <sup>137</sup>Cs), pollen stratigraphy, and changes in sediment properties associated with human activity. Multiple methods are necessary because at any given site, problems arise in the assumptions or applicability of one or more methods. In general, the mass accumulation calculations suggest that sediments were deposited 4 to 11 times faster in the historic period than before human settlement. The character of the sediment did not change in a dramatic way, but sediment magnetic properties suggest shifts in the sources of sediment. The data suggest that some of the changes in sources and (or) character of the sediment occurred just before human settlement and were probably related to climatic changes associated with the Little Ice Age.","language":"English","publisher":"Elsevier","doi":"10.1016/S0277-3791(00)00007-X","usgsCitation":"Colman, S.M., King, J., Jones, G.A., Reynolds, R.L., and Bothner, M., 2000, Holocene and recent sediment accumulation rates in southern Lake Michigan: Quaternary Science Reviews, v. 19, no. 6, p. 1563-1580, https://doi.org/10.1016/S0277-3791(00)00007-X.","productDescription":"18 p.","startPage":"1563","endPage":"1580","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488279,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.uri.edu/gsofacpubs/1749","text":"External Repository"},{"id":293828,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Lake Michigan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.04,41.61 ], [ -88.04,46.1 ], [ -84.74,46.1 ], [ -84.74,41.61 ], [ -88.04,41.61 ] ] ] } } ] }","volume":"19","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54140b20e4b082fed288b917","contributors":{"authors":[{"text":"Colman, Steven M. 0000-0002-0564-9576","orcid":"https://orcid.org/0000-0002-0564-9576","contributorId":77482,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":501048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, J.W.","contributorId":19265,"corporation":false,"usgs":true,"family":"King","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":501046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, Glenn A.","contributorId":17779,"corporation":false,"usgs":false,"family":"Jones","given":"Glenn","email":"","middleInitial":"A.","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":501045,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reynolds, R. 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,{"id":70124925,"text":"70124925 - 2000 - Local variability but landscape stability in coral reef communities following repeated hurricane impacts","interactions":[],"lastModifiedDate":"2014-09-12T10:50:24","indexId":"70124925","displayToPublicDate":"2000-09-12T10:43:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Local variability but landscape stability in coral reef communities following repeated hurricane impacts","docAbstract":"Coral reef community structure has remained remarkably stable over a 10 yr period within a small protected marine area despite repeated hurricane impacts. Local community dynamics have been highly variable, however. Sites that were destroyed by disease in the 1970s are showing little or no recovery, while sites less than a kilometre away that were devastated by Hurricane Hugo in 1989 are recovering well. Strong coral recruitment has occurred in shallow, exposed areas that showed the greatest hurricane impacts, and these areas are now more species rich than in 1988, although coral cover has not reached pre-hurricane levels. Coral colony survivorship has been high throughout most of the study area. Partial mortality rates were elevated for several years following Hurricane Hugo, but significant whole coral-head mortality only occurred during periods with hurricane impacts and only at the most exposed sites. Overall, the coral community has proved resilient to closely repeated major hurricane impacts. From a single case study we cannot attribute this resilience to the relatively low level of human impacts, but grazing fish populations have apparently remained high enough to keep macroalgae in check despite the mass mortality of the herbivore Diadema antillarum in the 1980s.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Ecology Progress Series","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Inter-Research Science Center","doi":"10.3354/meps204093","usgsCitation":"Bythell, J.C., Hillis-Star, Z.M., and Rogers, C.S., 2000, Local variability but landscape stability in coral reef communities following repeated hurricane impacts: Marine Ecology Progress Series, v. 204, p. 93-100, https://doi.org/10.3354/meps204093.","productDescription":"8 p.","startPage":"93","endPage":"100","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":479123,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/meps204093","text":"Publisher Index Page"},{"id":293811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293810,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3354/meps204093"}],"country":"U.S. Virgin Islands","otherGeospatial":"St. Croix","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -64.903334,17.673736 ], [ -64.903334,17.790137 ], [ -64.565193,17.790137 ], [ -64.565193,17.673736 ], [ -64.903334,17.673736 ] ] ] } } ] }","volume":"204","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54140b21e4b082fed288b920","contributors":{"authors":[{"text":"Bythell, John C.","contributorId":17544,"corporation":false,"usgs":true,"family":"Bythell","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":500968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hillis-Star, Zandy M","contributorId":106418,"corporation":false,"usgs":true,"family":"Hillis-Star","given":"Zandy","email":"","middleInitial":"M","affiliations":[],"preferred":false,"id":500969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rogers, Caroline S. 0000-0001-9056-6961 caroline_rogers@usgs.gov","orcid":"https://orcid.org/0000-0001-9056-6961","contributorId":3126,"corporation":false,"usgs":true,"family":"Rogers","given":"Caroline","email":"caroline_rogers@usgs.gov","middleInitial":"S.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":500967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70124921,"text":"70124921 - 2000 - Modern pollen deposition in Long Island Sound","interactions":[],"lastModifiedDate":"2017-11-18T12:30:05","indexId":"70124921","displayToPublicDate":"2000-09-12T10:16:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Modern pollen deposition in Long Island Sound","docAbstract":"Palynological analyses of 20 surface sediment samples collected from Long Island Sound show a pollen assemblage dominated by <i>Carya, Betula, Pinus, Quercus, Tsuga</i>, and <i>Ambrosia</i>, as is consistent with the regional vegetation. No trends in relative abundance of these pollen types occur either from west to east or associated with modern riverine inputs throughout the basin. Despite the large-scale, long-term removal of fine-grained sediment from winnowed portions of the eastern Sound, the composition of the pollen and spore component of the sedimentary matrix conforms to a basin-wide homogeneous signal. These results strongly support the use of select regional palynological boundaries as chronostratigraphic tools to provide a framework for interpretation of the late glacial and Holocene history of the Long Island Sound basin sediments.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Coastal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Coastal Education and Research Foundation","usgsCitation":"Beuning, K.R., Fransen, L., Nakityo, B., Mecray, E.L., and Buchholtz ten Brink, M.R., 2000, Modern pollen deposition in Long Island Sound: Journal of Coastal Research, v. 16, no. 3, p. 656-662.","productDescription":"7 p.","startPage":"656","endPage":"662","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":293807,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293806,"type":{"id":15,"text":"Index Page"},"url":"https://journals.fcla.edu/jcr/article/view/80870"}],"country":"United States","state":"Connecticut, New York","otherGeospatial":"Long Island Sound","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.827,40.7578 ], [ -73.827,41.3293 ], [ -72.0244,41.3293 ], [ -72.0244,40.7578 ], [ -73.827,40.7578 ] ] ] } } ] }","volume":"16","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54140b22e4b082fed288b929","contributors":{"authors":[{"text":"Beuning, Kristina R.M.","contributorId":70306,"corporation":false,"usgs":true,"family":"Beuning","given":"Kristina","email":"","middleInitial":"R.M.","affiliations":[],"preferred":false,"id":500956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fransen, Lindsey","contributorId":23081,"corporation":false,"usgs":true,"family":"Fransen","given":"Lindsey","email":"","affiliations":[],"preferred":false,"id":500953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nakityo, Berna","contributorId":89812,"corporation":false,"usgs":true,"family":"Nakityo","given":"Berna","email":"","affiliations":[],"preferred":false,"id":500957,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mecray, Ellen L.","contributorId":50887,"corporation":false,"usgs":true,"family":"Mecray","given":"Ellen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":500954,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Buchholtz ten Brink, Marilyn R.","contributorId":88021,"corporation":false,"usgs":true,"family":"Buchholtz ten Brink","given":"Marilyn","email":"","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":500955,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70205227,"text":"70205227 - 2000 - Land and water-resource development activities increase sinkhole frequency in the mantled karst region of Florida, USA","interactions":[],"lastModifiedDate":"2019-09-08T03:42:53","indexId":"70205227","displayToPublicDate":"2000-09-08T03:39:03","publicationYear":"2000","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Land and water-resource development activities increase sinkhole frequency in the mantled karst region of Florida, USA","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Sixth International Symposium on Land Subsidence","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Sixth International Symposium on Land Subsidence","conferenceDate":"September 24-29, 2000","conferenceLocation":"Ravenna, Italy","language":"English","publisher":"National Research Council of Italy","usgsCitation":"Tihansky, A.B., and Galloway, D.L., 2000, Land and water-resource development activities increase sinkhole frequency in the mantled karst region of Florida, USA, <i>in</i> Proceedings of the Sixth International Symposium on Land Subsidence, v. 1, Ravenna, Italy, September 24-29, 2000, p. 77-90.","productDescription":"14 p.","startPage":"77","endPage":"90","numberOfPages":"14","costCenters":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":367276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Tihansky, Ann B. tihansky@usgs.gov","contributorId":2477,"corporation":false,"usgs":true,"family":"Tihansky","given":"Ann","email":"tihansky@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":770454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":770455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70205226,"text":"70205226 - 2000 - Modeling residual aquifer-system compaction--Constraining the vertical hydraulic diffusivity of thick aquitards","interactions":[],"lastModifiedDate":"2019-09-10T09:27:55","indexId":"70205226","displayToPublicDate":"2000-09-08T03:33:06","publicationYear":"2000","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Modeling residual aquifer-system compaction--Constraining the vertical hydraulic diffusivity of thick aquitards","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Sixth International Symposium on Land Subsidence","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Sixth International Symposium on Land Subsidence","conferenceDate":"September 24-29, 2000","conferenceLocation":"Ravenna, Italy","language":"English","publisher":"National Research Council of Italy","usgsCitation":"Sneed, M., Pavelko, M.T., and Galloway, D.L., 2000, Modeling residual aquifer-system compaction--Constraining the vertical hydraulic diffusivity of thick aquitards, <i>in</i> Proceedings of the Sixth International Symposium on Land Subsidence, v. 2, Ravenna, Italy, September 24-29, 2000, p. 343-353.","productDescription":"11 p.","startPage":"343","endPage":"353","numberOfPages":"11","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":367275,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sneed, Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":770452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pavelko, Michael T. 0000-0002-8323-3998 mpavelko@usgs.gov","orcid":"https://orcid.org/0000-0002-8323-3998","contributorId":2321,"corporation":false,"usgs":true,"family":"Pavelko","given":"Michael","email":"mpavelko@usgs.gov","middleInitial":"T.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":770456,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":770453,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70205219,"text":"70205219 - 2000 - Mapping recoverable aquifer-system deformation and land subsidence in Santa Clara Valley, California, USA, using space-borne synthetic aperture radar","interactions":[],"lastModifiedDate":"2019-09-06T16:00:38","indexId":"70205219","displayToPublicDate":"2000-09-06T15:49:59","publicationYear":"2000","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"subseriesTitle":"Proceedings of the Sixth International Conference on Land Subsidence","title":"Mapping recoverable aquifer-system deformation and land subsidence in Santa Clara Valley, California, USA, using space-borne synthetic aperture radar","largerWorkTitle":"Proceedings of the Sixth International Conference on Land Subsidence","conferenceTitle":"Proceedings of the Sixth International Conference on Land Subsidence","conferenceDate":"September 25-29 2000","conferenceLocation":"Ravenna, Italy","language":"English","publisher":"International Association of Hydrological Sciences","usgsCitation":"Galloway, D.L., Burgmann, R., Fielding, E., Amelung, F., and Laczniak, R., 2000, Mapping recoverable aquifer-system deformation and land subsidence in Santa Clara Valley, California, USA, using space-borne synthetic aperture radar, <i>in</i> Proceedings of the Sixth International Conference on Land Subsidence, Ravenna, Italy, September 25-29 2000.","costCenters":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":367266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":770418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burgmann, R.","contributorId":10167,"corporation":false,"usgs":true,"family":"Burgmann","given":"R.","affiliations":[],"preferred":false,"id":770419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fielding, E.","contributorId":51057,"corporation":false,"usgs":true,"family":"Fielding","given":"E.","affiliations":[],"preferred":false,"id":770420,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Amelung, F.","contributorId":106268,"corporation":false,"usgs":true,"family":"Amelung","given":"F.","affiliations":[],"preferred":false,"id":770421,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Laczniak, R.L.","contributorId":218827,"corporation":false,"usgs":false,"family":"Laczniak","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":770422,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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