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  • PANGAEA
  • 1965-1969  (267)
Collection
Keywords
Publisher
Years
Year
  • 11
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    Unknown
    Annotated record of the detailed examination of Mn deposits from R/V Eltanin Cruise 17 stations (1968)
    PANGAEA
    In:  Antarctic Research Facility, Florida State University
    Details
    Publication Date: 2024-04-07
    Description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 17 in 1965 by the Department of Geology, Florida State University. Cores and dredges were recovered for 49 stations along with bottom photography and are available at the Antarctic Research Facility, Florida State University for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; ELT17; ELT17.001-PC; ELT17.001-RD; ELT17.003-PC; ELT17.003-PH; ELT17.004-PH; ELT17.005A-PH; ELT17.006-PC; ELT17.007-PC; ELT17.007-PH; ELT17.008-PC; ELT17.008-PH; ELT17.009-RD; ELT17.013-RS; ELT17.015-PC; ELT17.018-PC; ELT17.022-PC; ELT17.023-PC; ELT17.027-PC; ELT17.027-PH; ELT17.029-BT; ELT17.029-PC; ELT17.029-PH; ELT17.030A-PH; ELT17.030-PC; ELT17.031-PC; ELT17.031-PH; ELT17.032A-PH; ELT17.032-PC; ELT17.032-PH; ELT17.032-TC; ELT17.035-BT; ELT17.036-BT; ELT17.036-PH; ELT17.10C; ELT17.18C; ELT17.19C; ELT17.20C; ELT17.29C; ELT17.2C; ELT17.30C; ELT17.32C; ELT17.33C; ELT17.34C; ELT17.4C; ELT17.5C; ELT17.9C; Eltanin; Event label; File name; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; TC; TRAWL; Trawl net; Trigger corer; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 745 data points
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  • 12
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    Annotated record of the detailed examination of Mn deposits from R/V Eltanin Cruise 15 stations (1965)
    PANGAEA
    In:  Antarctic Research Facility, Florida State University
    Details
    Publication Date: 2024-04-07
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; ELT15; ELT15.001-PC; ELT15.003-MT; ELT15.003-PC; ELT15.004-BT; ELT15.004-PC; ELT15.005-BT; ELT15.006-PC; ELT15.006-RD; ELT15.007-MT; ELT15.007-PC; ELT15.008-BT; ELT15.008-PC; ELT15.009-PC; ELT15.011-PC; ELT15.012-PC; ELT15.013-PC; ELT15.013-RD; ELT15.015-PC; ELT15.016-BT; ELT15.016-PC; ELT15.018-PC; ELT15.019-PC; ELT15.021-PC; ELT15.023-TC; ELT15.025-PC; ELT15.026-PC; ELT15.027-PC; ELT15.028-PC; ELT15-10C; ELT15-12C; ELT15-14C; ELT15-17C; ELT15-18C; ELT15-19C; ELT15-21C; ELT15-22C; ELT15-24C; ELT15-25C; ELT15-26C; ELT15-28C; ELT15-2C; ELT15-3C; ELT15-4C; ELT15-5C; ELT15-7C; ELT15-8C; ELT15-9C; Eltanin; Event label; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; TC; TRAWL; Trawl net; Trigger corer; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1015 data points
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  • 13
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    Seawater carbonate chemistry and calcification in the Bahama Bank, 1964-1965 (1967)
    PANGAEA
    In:  Supplement to: Traganza, Eugene D (1967): Dynamics of the carbon dioxide system on the Great Bahama Bank. Bulletin of Marine Science, 17(2), 348-366, https://www.ingentaconnect.com/content/umrsmas/bullmar/1967/00000017/00000002/art00010
    Details
    Publication Date: 2024-03-15
    Description: Carbon dioxide is lost from the ocean by calcium carbonate precipitation (-p), photosynthesis (-b) and gas evasion at the sea surface (-g). Among the most active sites are warm shallow seas. In this paper seasonal studies on the Great Bahama Bank relate these processes in an equation which takes into account the indirect effects of advection (a), evaporation (e), and eddy diffusion (d). Calcium carbonate precipitation is very seasonal and accounts for about half of the total losses. The delta sum CO2/deltaCa ratio is always about 1.87 on the bank. A high summer carbonate loss is inversely correlated with summer increases of chlorinity and temperature suggesting that CaCO3 is precipitated inorganically or biogenic production of CaCO3 is regulated by these parameters or both.
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate; Bicarbonate ion; Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, total; Chloride; Coast and continental shelf; Date; Entire community; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); North Atlantic; OA-ICC; OCE; Ocean Acidification International Coordination Centre; Oceanography; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Salinity; Temperate; Temperature, water; Traganza_Great_Bahama_Bank
    Type: Dataset
    Format: text/tab-separated-values, 279 data points
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  • 14
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    Macroremains from sediment core Elm B (1967)
    PANGAEA
    Details
    Publication Date: 2024-03-06
    Keywords: Betula sp., fruits; Betula sp., fruit scales; Calluna vulgaris; Carex sect. Eucarex; Carex sect. Vignea; Caryophyllaceae; Ceratophyllum demersum; Chara, oogonia; Counting, palynology; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EDEA; Edelman auger; Elm_B; Juncus; Lower Saxony, Northern Germany; Menyanthes; Najas minor; Nuphar; Nymphaea; Pinus, seeds; Pollen zone; Polygonum lapathifolium; Potamogeton cf. lucens; Potamogeton fluitans; Potamogeton friesii; Potamogeton natans; Potamogeton perfoliatus; Potamogeton praelongus; Potamogeton pusillus; Potamogeton sp.; Potamogeton trichoides; Ranunculus sceleratus; Rubus idaeus; Rumex maritimus; Rumex sp.; Umbelliferae
    Type: Dataset
    Format: text/tab-separated-values, 798 data points
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  • 15
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    Macroremains from sediment core Elm K (1967)
    PANGAEA
    Details
    Publication Date: 2024-03-06
    Keywords: 1b; Betula nana, fruits; Betula nana, fruit scales; Betula sp., fruits; Betula sp., fruit scales; Brasenia; Calluna vulgaris; Carex sect. Eucarex; Carex sect. Vignea; Caryophyllaceae; Ceratophyllum demersum; Chara, oogonia; Counting, palynology; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EDEA; Edelman auger; Elm_K; Juncus; Lower Saxony, Northern Germany; Menyanthes; Najas minor; Nuphar; Nymphaea; Nymphaea: hairs; Pinus, seeds; Pollen zone; Polygonum lapathifolium; Polygonum sp.; Potamogeton cf. lucens; Potamogeton natans; Potamogeton praelongus; Potamogeton sp.; Potamogeton trichoides; Ranunculus sceleratus; Rubus idaeus; Rumex maritimus; Rumex sp.; Sagittaria sagittifolia; Umbelliferae
    Type: Dataset
    Format: text/tab-separated-values, 1773 data points
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  • 16
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    (Table 1, page 376), Composition of manganese deposits from the Gulf of Aden and the Carlsberg Ridge (1969)
    PANGAEA
    In:  Supplement to: Johnson, C E; Glasby, Geoffrey P (1969): Mössbauer Effect determination of particle size in microcrystalline iron-manganese nodules. Nature, 222(5191), 376-377, https://doi.org/10.1038/222376a0
    Details
    Publication Date: 2024-03-01
    Description: Iron-manganese nodules from the ocean floor have been extensively studied. But, because of the fine grain size of the particles of the nodules, structural identification by X-ray and electron diffraction techniques is difficult and the mineralogy of the iron oxide phase has not been well characterized. The observation of the Mössbauer spectrum-in which each nucleus absorbs gamma-rays independently-is not limited by particle size in the same way as is the observation of Bragg peaks in diffraction measurements, in which radiation must be scattered coherently from a large number of atoms. The magnetic hyperfine splitting in the Mössbauer spectrum of magnetic materials is affected, however, when the particles are so small that they become superparamagnetic. We describe here an investigation using the 57Fe Mössbauer effect of two iron-manganese nodules in which the iron oxide phase could not be detected by X-ray or electron diffraction.
    Keywords: Chromium; Cobalt; Copper; D16; D6243; D6273; Description; Discovery (1962); Dredge, rock; DRG_R; Event label; Gulf of Aden; Indian Ocean, Carlsberg Ridge; Iron; Lead; Manganese; Minerals, surface area; Molybdenum; Mössbauer spectroscopy; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Silicon dioxide; Titanium; Vanadium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 17
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    (Table 2, page 17-18), Elemental composition of ferromanganese crust in lakes Windermere and Ullswater, United Kingdom (1965)
    PANGAEA
    In:  Supplement to: Gorham, Eville; Swaine, Dalway J (1965): The influence of oxidizing and reducing conditions upon the distribution of some elements in lake sediments. Limnology and Oceanography, 10(2), 268-279, https://doi.org/10.4319/lo.1965.10.2.0268
    Details
    Publication Date: 2024-02-26
    Description: Analyses for Fe, Mn, Pb, Zn, Co, P, Mo, Ba, Sr, Ti, Li, Rb, Na, K, Be, Cr, V, Y, Ag, Cu, C, S, Sn, Ni, Ga, Zr, and La have been carried out on some oxidate crusts, oxidized surface muds, reduced subsurface muds, and glacial clays collected in Windermere and Esthwaite Water in the English Lake District. The relatively organic lake muds exhibit the highest concentrations of C, S, Cu, Sn, and Ni. Many of the oxidate crusts exhibit strong enrichment in Mn, Fe, Ba, Sr, Pb, and Zn. Ti, Li, Rb, Co, P, and Mo are also enriched in some crusts. S, Sn, and Ni reach their highest levels in the reducing subsurface muds, but Mn, and to a lesser extent Fe and Mo, are higher in the oxidized than in the reduced muds. Relations between the elements in the various sediments are examined, and the English oxidate crusts are compared with lake and stream ores in Sweden and Finland, and with marine manganese nodules. These marine nodules are frequently enriched in Cu, Ni, Co, Mo, V, Ag, and Sn to a far higher degree than the freshwater ferromanganese concretions. Some freshwater crusts exhibit enrichments in Pb, Zn, and Ba of the same order as those observed in marine manganese nodules.
    Keywords: Barium; Boron; Carbon, organic, total; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Flame photometry; Gallium; Identification; Iron; Lake Ullswater, United Kingdom; Lake Windermere, United Kingdom; Lanthanum; Lead; Lithium; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; Rubidium; Silver; Sodium; Spectrophotometer (Unicam SP500); Spectroscopy, cathode layer arc; Strontium; Sulfur, total; Tin; Titanium; Ullswater_G; Vanadium; Wet chemistry; Windermere_G; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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  • 18
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    Chemical analysis of water samples of station M1_1207, Red Sea (Table 1-3) (1968)
    PANGAEA
    In:  Supplement to: Hartmann, Martin; Lohmann, Ludwig (1968): Untersuchungen an der heißen Salzlauge und am Sediment des Atlantis II-Tiefs in Roten Meer. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C1, 13-20
    Details
    Publication Date: 2024-02-03
    Description: Two water samples and two sediment samples taken in 1965 by the R. V. "Meteor" in the area of the hot salt brine of the Atlantis II-Deep were chemically investigated, and in addition the sediment samples were subjected to X-ray and optical analysis. The investigation of the sulfur-isotope-ratios showed the same values for all water samples. This information combined with the Ca-sulfate solubility data leads us to conclude that, for the most part, the sulfate content of the salt brine resulted from mixing along the boundary with the normal seawater. In this boundary area gypsum or anhydrite is formed which sinks down to the deeper layers of the salt brine where it is redisolved when the water becomes undersaturated. In the laboratory, formation of CaS04 precipitate resulted from both the reheating of the water sample from the uppermost zone of the salt brine to the in-situ-temperature as well as by the mixing of the water sample with normal Red Sea water. The iron and manganese delivered by the hot spring is separated within the area of the salt brine by their different redox-potentials. Iron is sedimented to a high amount within the salt brine, while, as evidenced by its small amounts in all sediment samples, the more easily reducible manganese is apparently carried out of the area before sedimentation can take place. The very good layering of the salt brine may be the result of the rough bottom topography with its several progressively higher levels allowing step-like enlargements of the surface areas of each successive layer. Each enlargement results in larger boundary areas along which more effective heat transfer and mixing with the next layer is possible. In the sediment samples up to 37.18% Fe is found, mostly bound as very poorly crystallized iron hydroxide. Pyrite is present in only very small amounts. We assume that the copper is bound mostly as sulfide, while the zinc is most likely present in an other form. The sulfur-isotope-investigations indicate that the sulfur in the sediment, bound as pyrite and sulfides, is not a result of bacterical sulfate-reduction in the iron-rich mud of the Atlantis II-Deep, but must have been brought up with the hot brine.
    Keywords: Alkalinity, total; Atlantis II Deep; BC; Box corer; Calcium; Calcium carbonate; Carbon, organic, total; Chloride; Comment; Copper; Description; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Iron; Loss on ignition; M1; M1_1207; Magnesium; Manganese; Meteor (1964); ORDINAL NUMBER; Oxygen; pH; Sample code/label; Sulfate; Sulfur, total; Zinc; δ34S, sulfate
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 19
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    Hydrochemistry measured on water bottle samples during the METEOR International Indian Ocean Expedition 1964/65 (1966)
    PANGAEA
    In:  Supplement to: Dietrich, Günter; Düing, Walter; Grasshoff, Klaus; Koske, Peter H (1966): Physikalische und chemische Daten nach Beobachtungen des Forschungsschiffes Meteor im Indischen Ozean 1964/65. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A2, 1-155
    Details
    Publication Date: 2024-02-03
    Description: The present volume gives the observed physical and chemical data obtained by R.V. "Meteor" in the Indian Ocean during cruise 1964/65. The tables are based on the computations made by the National Oceanographic Data Center (NODC) in Washington. In addition to the normally communicated data, the tables contain four chemical parameters: alkalinity, ammonia, fluoride, and calcium.
    Keywords: Biscaya; CTD/Rosette; CTD-RO; Eastern Arabian Sea; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_001; M1_005; M1_006; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD001; M1_CTD005; M1_CTD006; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Mediterranean Sea; Meteor (1964); Red Sea; Western Arabian Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 20
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    Hydrochemistry measured on water bottle samples from the Mediterranen Sea during the International Indian Ocean Expedition 1964/65 (1966)
    PANGAEA
    Details
    Publication Date: 2024-02-03
    Keywords: Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_005; M1_006; M1_CTD005; M1_CTD006; Mediterranean Sea; Meteor (1964); Nitrate; Oxygen; Oxygen, microelectrode, ex-situ; Phosphate; Salinity; Silicate; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 450 data points
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