{"pageNumber":"6904","pageRowStart":"172575","pageSize":"25","recordCount":184776,"records":[{"id":70219992,"text":"70219992 - 1957 - Physical and ecologic features of the Sagadahoc Bay Tidal Flat, Georgetown, Maine","interactions":[],"lastModifiedDate":"2021-04-16T17:03:54.075817","indexId":"70219992","displayToPublicDate":"1957-03-01T11:53:52","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1726,"text":"GSA Memoirs","active":true,"publicationSubtype":{"id":10}},"title":"Physical and ecologic features of the Sagadahoc Bay Tidal Flat, Georgetown, Maine","docAbstract":"

Sagadahoc Bay is open to the ocean at the south and has no significant fresh-water stream entering it. The intertidal zone is roughly a mile long by half a mile wide; most of it is made up of medium to fine sand, but organic-rich mud characterizes the head of the flat and the protected coves. Refraction-seismograph surveys showed that the bedrock surface lies 30 to 200 feet below the surface of the tidal flat and that it is irregular and fluted longitudinally. Repeated surveys indicate that the intertidal flat builds up and cuts down but is apparently in equilibrium with the present sea level. The sediment that fills the bay came from the sea. Waves and tidal currents tend to move it landward; storms accelerate this, or reverse the direction of movement, depending on the characteristics of the storm.

Tidal- and wave-generated currents 0.1 foot above the bottom range in velocity from 0.35 to 0.82 foot per second on incoming tides and from 0.20 to 0.58 foot per second on ebbing tides. Incoming tides float large quantities of sand landward; ebbing tides never carry floating sand.

Two distinctive and extensive Mya shell-pavement layers were found at depths of roughly 2 and 3 feet below the present surface of the tidal flat. The lower layer is approximately 1,000 years old according to a radiocarbon age determination of its Mya shells. It is suggested that these shell layers formed by sluicing away of a layer of sand about 2 feet thick, which had been thrown into loose packing by an earthquake at high tide. The earth shock induced a submarine slide of the sand in the outer part of the bay, which oversteepened the profile of the sand headward nearly to the head of the bay. Mya and other shells settled through the layer of quicksand while the sand was running out seaward.

Living in the intertidal zone is the usual assemblage of clams, gastropods, crustaceans, worms, and seaweeds found on most northern New England tidal flats. The Mya arenaria population is decreasing, but in general myas are more numerous in the muddy areas than in the sandy areas. They grow more rapidly in the sand, though in the past decade there has been no significant renewal of the Mya population in the sandy part of the flat. Macoma balthica inhabits the muddy areas, whereas Ensis, Spisula, and Arctica are restricted to the low-tide zone and the shallow water below. Gemma gemma grows in great abundance in the sandy part of the flat but is rare in the muddy parts. Small shrimp and green crabs are common.

The calcareous shells of these animals are all potential fossils, but the shrimp and crab exoskeletons are not, for their tests are rapidly decomposed in this environment. Other potential fossils are wood and bark, acorn caps, conifer cones, leaves of deciduous trees, seeds, and occasionally even grass stems and pieces of eel grass. All these are reasonably well preserved in the constant reducing environment that prevails an inch or two below the surface.

An inverse relationship exists between the abundances of Mya arenaria and Gemma gemma. Cores and test pits show that gemmas are more numerous on the Sagadahoc flat now than they have been in the recent past (estimated 10–100 years). Gemmas are the dominant mollusk in the sandy part of the flat now that the myas are so extremely rare. The speculation is that gemmas became dominant largely because the Mya population was greatly reduced by intensive digging during and just after the last war and through depredations by green crabs. Possibly the warming climate has favored the gemmas selectively.

The writer infers that the gemmas are a serious competitor of the myas and that the gemmas now starve out Mya spat, which is known to be carried into the bay each spring and fall. Two recommendations are made: (1) determining under controlled laboratory conditions the food requirements of Gemma and the density of Gemma population that will permit survival of Mya larvae from set through a stage that will assure maturation; and (2) killing off a large percentage of the Gemma population and observing whether or not a natural set of Mya occurs. Gemmas can be killed quickly under a flame shield such as is used to soften asphalt-sand mixtures in street paving. Inasmuch as gemmas are ovoviviparous they should not repopulate the flat rapidly.

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No abstract available. 

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Treatise on marine ecology and paleoecology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM67V2-p67","usgsCitation":"Ladd, H.S., and Gunter, G., 1957, Development of marine paleoecology, chap. 3 of Treatise on marine ecology and paleoecology, v. 67, no. 2, p. 67-74, https://doi.org/10.1130/MEM67V2-p67.","productDescription":"8 p.","startPage":"67","endPage":"74","costCenters":[],"links":[{"id":369522,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"2","noUsgsAuthors":false,"publicationDate":"1957-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ladd, Harry Stephen","contributorId":61811,"corporation":false,"usgs":true,"family":"Ladd","given":"Harry","email":"","middleInitial":"Stephen","affiliations":[],"preferred":false,"id":776007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gunter, G.","contributorId":220859,"corporation":false,"usgs":false,"family":"Gunter","given":"G.","email":"","affiliations":[],"preferred":false,"id":776008,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70219988,"text":"70219988 - 1957 - Radiocarbon age of the damariscotta shell heaps","interactions":[],"lastModifiedDate":"2021-04-16T16:46:38.39069","indexId":"70219988","displayToPublicDate":"1957-01-31T11:37:52","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":700,"text":"American Antiquity","active":true,"publicationSubtype":{"id":10}},"title":"Radiocarbon age of the damariscotta shell heaps","docAbstract":"

The large oyster shell heaps on both sides of the Damariscotta River, just north of the towns of Damariscotta and Newcastle, Maine, have been known for many years and both geologists and archaeologists have speculated about their age. During the summer of 1955 I made 2 collections of Mya shells from the largest shell heap on the west side of the river (Glidden estate) for radiocarbon age determinations.

","language":"English","publisher":"Society for American Archaeology","doi":"10.2307/276571","usgsCitation":"Bradley, W., 1957, Radiocarbon age of the damariscotta shell heaps: American Antiquity, v. 22, no. 3, p. 296-296, https://doi.org/10.2307/276571.","productDescription":"1 p.","startPage":"296","endPage":"296","costCenters":[],"links":[{"id":385160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","city":"Newcastle and Damariscotta","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -69.66430664062499,\n 43.96119063892024\n ],\n [\n -69.42535400390625,\n 43.96119063892024\n ],\n [\n -69.42535400390625,\n 44.10139306449849\n ],\n [\n -69.66430664062499,\n 44.10139306449849\n ],\n [\n -69.66430664062499,\n 43.96119063892024\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, W.H.","contributorId":220222,"corporation":false,"usgs":false,"family":"Bradley","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":814406,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048784,"text":"tem1026 - 1957 - Preliminary geologic map of the Paria Plateau SE Quadrangle, Coconino County, Arizona","interactions":[],"lastModifiedDate":"2014-03-25T09:58:29","indexId":"tem1026","displayToPublicDate":"1957-01-22T08:45:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1026","title":"Preliminary geologic map of the Paria Plateau SE Quadrangle, Coconino County, Arizona","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem1026","usgsCitation":"Petersen, R., 1957, Preliminary geologic map of the Paria Plateau SE Quadrangle, Coconino County, Arizona: U.S. Geological Survey Trace Elements Memorandum 1026, Report: 2 p.; 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No abstract available.

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Turkey is in a state of transition from an agricultural and pastoral economy to an economy that combines agriculture and industry. Such a transition includes use of water resources for water power, irrigation, manufacturing, and domestic uses. The control of streams for multiple purposes invariably leads to conflicts of interest. Several Turkish streams rise in or flow into other countries. For these reasons, data on the flow of streams over a fairly long period of time are needed in order to plan the most beneficial use and control of the streams of Turkey.

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1957 - Preliminary geologic map of the Clay Hills 2 NW quadrangle, San Juan County, Utah","interactions":[],"lastModifiedDate":"2014-03-04T13:49:37","indexId":"tem1001","displayToPublicDate":"1957-01-01T10:16:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1001","title":"Preliminary geologic map of the Clay Hills 2 NW quadrangle, San Juan County, Utah","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem1001","usgsCitation":"Mullens, T.E., 1957, Preliminary geologic map of the Clay Hills 2 NW quadrangle, San Juan County, Utah: U.S. Geological Survey Trace Elements Memorandum 1001, Report: 8.37 inches x 11.08 inches; Plate 1: 27.73 inches x 33.01 inches, https://doi.org/10.3133/tem1001.","productDescription":"Report: 8.37 inches x 11.08 inches; Plate 1: 27.73 inches x 33.01 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278220,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/1001/report-thumb.jpg"},{"id":283272,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1001/report.pdf"},{"id":283271,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1001/plate-1.pdf"}],"country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.375,37.375 ], [ -110.375,37.500 ], [ -110.250,37.500 ], [ -110.250,37.375 ], [ -110.375,37.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"524a9d64e4b017cb43afb11f","contributors":{"authors":[{"text":"Mullens, Thomas E.","contributorId":14817,"corporation":false,"usgs":true,"family":"Mullens","given":"Thomas","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":484812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37808,"text":"37808 - 1957 - Pesticides and wildlife","interactions":[],"lastModifiedDate":"2020-02-21T15:05:03","indexId":"37808","displayToPublicDate":"1957-01-01T09:52:03","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"392","title":"Pesticides and wildlife","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Stickel, L.F., and Springer, P.F., 1957, Pesticides and wildlife: Wildlife Leaflet 392, 12 p.","productDescription":"12 p.","numberOfPages":"12","costCenters":[],"links":[{"id":290861,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f4e4b0824b2d177094","contributors":{"authors":[{"text":"Stickel, Lucille F.","contributorId":76598,"corporation":false,"usgs":true,"family":"Stickel","given":"Lucille","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":218576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Springer, Paul F.","contributorId":70445,"corporation":false,"usgs":true,"family":"Springer","given":"Paul","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":218575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":81375,"text":"81375 - 1957 - The lake trout (Salvelinus namaycush)","interactions":[],"lastModifiedDate":"2023-04-05T16:38:47.474026","indexId":"81375","displayToPublicDate":"1957-01-01T01:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"441","title":"The lake trout (Salvelinus namaycush)","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Eschmeyer, P.H., 1957, The lake trout (Salvelinus namaycush): Fishery Leaflet 441, 11 p.","productDescription":"11 p.","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":415250,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nmfs.noaa.gov/content/lake-trout-salvelinus-namaycush","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d218","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":295305,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35846,"text":"b1045A - 1957 - Core logs from Owens, China, Searles, and Panamint basins, California","interactions":[],"lastModifiedDate":"2022-11-07T15:18:00.263617","indexId":"b1045A","displayToPublicDate":"1957-01-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1045","chapter":"A","title":"Core logs from Owens, China, Searles, and Panamint basins, California","docAbstract":"

Detailed logs of drill cores are presented in this report. The drill cores are of sediments from four basins that were occupied during the Pleistocene by a continuous chain of lakes. Owens Lake basin (one hole, 920 feet) contains fine-grained sediments and includes locally many diatoms and ostracodes. China Lake basin (one hole, 700 feet) contains silt- to sand-sized clastic sediments and some calcite and gaylussite; a few diatoms, ostracodes, and mollusks are present. Searles Lake basin (one hole, 875 feet) contains many layers of gaylussite- or pirssonite-bearing sediments intercalated with beds of halite, trona, and lesser amounts of other minerals peculiar to Searles Lake; the top 120 feet consists of thicker evaporite bodies with a more complex mineralogy. Panamint basin (three holes, 500, 375, and 995 feet) contains clastic deposits ranging from clay to gravel, a small amount of gypsum, anhydrite, a trace of bassanite, and thick bodies of halite in the basin center; a few diatoms and ostracodes are present.

","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1045A","usgsCitation":"Smith, G.I., and Pratt, W.P., 1957, Core logs from Owens, China, Searles, and Panamint basins, California: U.S. Geological Survey Bulletin 1045, 70 p.; 1 Plate, https://doi.org/10.3133/b1045A.","productDescription":"70 p.; 1 Plate","startPage":"1","endPage":"62","costCenters":[],"links":[{"id":164745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1045a/report-thumb.jpg"},{"id":93597,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1045a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93587,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1045a/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025aa","contributors":{"authors":[{"text":"Smith, George I.","contributorId":92637,"corporation":false,"usgs":true,"family":"Smith","given":"George","email":"","middleInitial":"I.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":215324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pratt, Walden P.","contributorId":68296,"corporation":false,"usgs":true,"family":"Pratt","given":"Walden","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":215323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}