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  • Data  (14)
  • 2000-2004
  • 1955-1959  (8)
  • 1950-1954  (6)
  • 1945-1949
  • 1959  (8)
  • 1953  (6)
Collection
Keywords
Publisher
Years
  • 2000-2004
  • 1955-1959  (8)
  • 1950-1954  (6)
  • 1945-1949
Year
  • 1
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    PANGAEA
    In:  Supplement to: Tatsumoto, M; Goldberg, Edward D (1959): Some aspects of the marine geochemistry of uranium. Geochimica et Cosmochimica Acta, 17(3-4), 201-208, https://doi.org/10.1016/0016-7037(59)90094-8
    Publication Date: 2024-07-01
    Description: The uranium concentrations in marine calcareous material of a biological origin varied between 0.0X and 0.X p.p.m. with the exception of corals which had concentrations of several p.p.m. The aragonitic oolites and aragonite precipitated from sea-water had values similar to those of the corals. A geochronology based on the growth of ionium (thorium-230) from uranium is applicable not only to corals, as previous investigators have pointed out, but also to oolites. Several examples of "oolite ages" are given. The uranium content of ferromanganese minerals from pelagic deposits is of the order of from 4 to 5 p.p.m.
    Keywords: Atlantic Ocean; DEPTH, sediment/rock; DNWB0BBD; DNWB0BBD-047G; DNWB0BBD-052G; DOWNWIND-B2; DOWNWIND-H; Dredge; DRG; DWBG47; DWBG52; DWHD55; Event label; GC; Gravity corer; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Spencer F. Baird; TH1; TH1-TR4; Theta; Uranium; Wired profile sonde; WP
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 2
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    PANGAEA
    In:  Supplement to: Kröll, Victor (1953): Vertical Distribution of Radium in Deep-Sea Sediments. Nature, 171(4356), 742-742, https://doi.org/10.1038/171742a0
    Publication Date: 2024-06-26
    Description: The surprisingly high content of radium in certain deep-sea sediments discovered nearly fifty years ago by J. Joly remained unexplained until 1937, when H. Pettersson suggested an ocean-wide precipitation of ionium from sea water on to the ocean bottom as its origin. Extensive radium measurements on deep-sea cores raised by the Swedish Deep-Sea Expedition carried out in this institute by Pettersson, T. Bernert and me did not confirm the regular vertical distribution of radium reported by other workers. An expected rise in radium content from moderate values in the uppermost surface layers to a maximum corresponding to a radioactive equilibrium between precipitated ionium and ionium-supported radium generally occurred; but the maximum was not followed by the theoretical exponential decline downwards governed by the rate of decay of ionium, to 50 per cent in 83,000 years, to 25 per cent in 166,000 years, etc. Instead, a number of secondary maxima of radium content separated by equally pronounced minima were observed (see graph), which could not well be explained as due to intervening changes in the rate of total sedimentation. Another explanation offered was that ionium and radium are not in radioactive equilibrium; that is, the assumption underlying the use of measurements of radium as indicating the concentration in the same layer of its mother element is unjustified.
    Keywords: Albatross IV (1963); Core; CORE; core_87; Deposit type; DEPTH, sediment/rock; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NODC-0418; North Pacific Ocean; Radium; SDSE_136-2; SwedishDeepSeaExpedition
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Ljunggren, P (1953): Some Data concerning the Formation of Manganiferous and Ferriferous Bog Ores. Geologiska Föreningens i Stockholm förhandlingar, GFF (The transactions of the Geological Society of Sweden), 75(2), 277-297, https://doi.org/10.1080/11035895309454173
    Publication Date: 2023-08-28
    Description: In connection with a discovery of oxidic manganiferous and ferriferous precipitations in northern Vermland and north-western Dalecarlia, pH measurements of different waters and chemical analyses of waters and bog ores were carried out. The origin of the different bog ores is dealt with in connection with a discussion of some problems of the geochemistry of manganese and iron.
    Keywords: Grycken_L; Lake Grycken, Sweden; Lake Tisjoen, Sweden; Lika_L; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; River Lika, Sweden; Tisjoen_L
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
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    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1953): R/V Atlantis Cruise 185 - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
    Publication Date: 2023-08-28
    Description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) operating as guests scientists during the R/V Atlantis Cruise 185 undertaken by the Woods Hole Oceanographic Institution from April until June 1953. A total of 65 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: AT185; AT185-12P; AT185-6P; AT185-7P; Atlantic Ocean; Atlantis (1931); Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to metadata file
    Type: Dataset
    Format: text/tab-separated-values, 43 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Bruun, Anton F (1959): General introduction to the reports and list of deep-sea stations. in: Galathea Report - Scientific Results of the Danish Deep Sea Expedition Round the World. 1950-1952, Danish Science Press, Copenhagen, Denmark, 7-48
    Publication Date: 2023-08-28
    Description: The Danish Expedition of the "Galathea II" around the world brought important results concerning the marine organisms in the deep sea. The "Galathea II" showed not only different organisms of the Abyssal but for the first time of the deepest trenches of the western Pacific. Anton Bruun coined the term Hadal for the region below the Abyssal under 6000 m. Although the "Galathea II" aimed to investigate new deep sea regions beside the routes of former expeditions and to widen the horizon of knowledge relating marine organisms the technical equipment and the methodological approach had partly been developed earlier. The expedition of the "Galathea II" is part of a long tradition of cruises such as that of the British "Challenger", the German "Valdivia" and the Swedish "Albatross" and especially the Danish cruises of the "Dana I" and "Dana II" which happened some years before.
    Keywords: Banda Sea; Comment; Core; CORE; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GAL_1950-1952_Denmark; Galathea; GALT-179; GALT-182; GALT-435; GALT-469; GALT-494; GALT-574; GALT-658; GALT-724; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Philippine Sea; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Tasman Sea
    Type: Dataset
    Format: text/tab-separated-values, 73 data points
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  • 6
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1959): FANFARE Expedition 1959, List of cores and dredge samples copied from shipboard logs (R/V H. M. Smith and R/V Spencer F. Baird). Scripps Institution of Oceanography, UC San Diego, unpublished, 6 pp, https://www.ngdc.noaa.gov/mgg/geology/data/1599/15995003/15995003.pdf
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken on the FANFARE Expedition in July 1959 by Scripps Institution of Oceanography from the R/V H. M. Smith and the R/V Spencer F. Baird. A total of 49 cores and dredges were recovered and are available at Scripps for sampling and study. The coring sites, all in the eastern tropical central Pacific.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge, chain bag; DRG_C; Elevation of event; Event label; FANB01BD; FANB01BD-024G; FANBD-20D; FANBD-24G; FANBD-25D; FANFARE-B; FANFARE-S; FANS01HMS; FANS01HMS-016G; FANS-16G; GC; Gravity corer; H.M. Smith; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Size; Spencer F. Baird; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Bramlette, M; Faughn, James L; Hurley, RJ (1959): Anomalous sediment deposition on the flank of Eniwetok Atoll. Geological Society of America Bulletin, 70(12), 1549-1552, https://doi.org/10.1130/0016-7606(1959)70%5B1549:ASDOTF%5D2.0.CO;2
    Publication Date: 2023-08-28
    Description: Some short cores from the shelf at about 800-1000 fathoms on the southwest flank of Eniwetok Atoll penetrated Pliocene deposits with little to no later sediment cover. The Quaternary deposits include much coarse reef debris, particularly the fragments of algae such as Halimeda and other shallow-water material up to several millimeters in grain size, mixed with varying amounts of pelagic Foraminifera. The Pliocene sediments (one may be upper Miocene) are pure pelagic deposits of much finer grain size, consisting of coccoliths and pelagic Foraminifera with no admixture of reef material. Bottom photographs show areas of well-developed ripple marks in coarse sediment (C. J. Shipek, manuscript) apparently formed only in the areas with the veneer of post-Tertiary coarse sediments. A brown impregnation at the top and extending down as mottling for a few centimeters is also usual in the Tertiary sediment of the cores. This seems to consist of iron and manganese oxides and adds somewhat to the induration.
    Keywords: 10-J1268; 10-J1269; 10-J1270; 10-J1271; 10-J1272; 10-J1273; 10-J1274; 10-J1275; 11-J1276; 3-J1225; 3-J1226; 3-J1227; 3-J1228; 4-J1230; 4-J1231; 4-J1232; 4-J1233; 4-J1234; 4-J1235; 6-J1237; 6-J1238; 6-J1239; 6-J1240; 6-J1241; 6-J1242; 6-J1243; 6-J1244; 8-J1260; 8-J1261; 8-J1262; 8-J1263; 8-J1264; 8-J1265; 8-J1266; Comment; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; ENIW10PH-1268; ENIW10PH-1269; ENIW10PH-1270; ENIW10PH-1271; ENIW10PH-1272; ENIW10PH-1273; ENIW10PH-1274; ENIW10PH-1275; ENIW11PH-1276; ENIW20C; ENIW27C; ENIW3PH-1225; ENIW3PH-1226; ENIW3PH-1227; ENIW3PH-1228; ENIW4C; ENIW4PH-1230; ENIW4PH-1231; ENIW4PH-1232; ENIW4PH-1233; ENIW4PH-1234; ENIW4PH-1235; ENIW6PH-1237; ENIW6PH-1238; ENIW6PH-1239; ENIW6PH-1240; ENIW6PH-1241; ENIW6PH-1242; ENIW6PH-1243; ENIW6PH-1244; ENIW8PH-1260; ENIW8PH-1261; ENIW8PH-1262; ENIW8PH-1263; ENIW8PH-1264; ENIW8PH-1265; ENIW8PH-1266; ENIWETOK_Operation; Eniwetok Atoll, Central Pacific; Event label; H.M. Smith; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 341 data points
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  • 8
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    In:  Supplement to: Lamont-Doherty Earth Observatory (1959): Expedition VEMA 15. Lamont Geological Observatory, Columbia University, New York, unpublished, 26 pp, https://www.ngdc.noaa.gov/mgg/curator/data/vema/vm15/vm15_summary.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the VEMA 15 Expedition from October 1958 until July 1959 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 410 cores and dredges were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; TRAWL; Trawl net; V15; V15-003PD; V15-101; V15-119SBT; V15-120SBT; V15-122SBT; V15-125SBT; V15-129; V15-130; V15-131; V15-135; V15-135SBT; V15-136; V15-138; V15-144; V15-151SBT; V15-160; V15-187; V15-188; V15-197; V15-202; V15-30; V15-40; V15-44A; V15-45; V15-47; V15-48; V15-61SBT; V15-66; V15-77SBT; V15-78SBT; V15-79SBT; V15-8; V15-80SBT; V15-81SBT; V15-82SBT; V15-95SBT; Vema
    Type: Dataset
    Format: text/tab-separated-values, 698 data points
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  • 9
    Publication Date: 2023-08-28
    Keywords: DEPTH, sediment/rock; Description; Event label; Fluorine; Grycken_L; Identification; Lake Grycken, Sweden; Lake Tisjoen, Sweden; Manganese; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Tisjoen_L; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 10
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Event label; Grycken_L; Identification; Lake Grycken, Sweden; Lake Tisjoen, Sweden; Lika_L; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; River Lika, Sweden; Size; Substrate type; Tisjoen_L; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 17 data points
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