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  • 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  (1)
  • Aluminium; Calcium; Cobalt; Copper; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; DRG; DWHD16; Electron Probe Microanalysis (EPMA); Horizon; Iron; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Potassium; Sample ID; Silicon; Titanium; Zinc  (1)
  • Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; ELT13; ELT13.001-PC; ELT13.005-PC; ELT13.006-PC; ELT13.007-BT; ELT13.008-BT; ELT13.009-PC; ELT13.010-PC; ELT13.013-BT1; ELT13.013-BT2; ELT13.013-PC; ELT13.016-PC; ELT13.017-PC; ELT13.018-PC; ELT13.021-PC; ELT13.024-PC; ELT13-11C; ELT13-19C; ELT13-1C; ELT13-3C; ELT13-4C; ELT13-5C; ELT13-6C; ELT13-8C; 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; TRAWL; Trawl net; Uniform resource locator/link to image; Visual description  (1)
  • PANGAEA  (3)
  • Geological Society of America (GSA)
  • Nature Publishing Group
  • Springer Nature
  • 1965-1969  (3)
  • 1935-1939
  • 1930-1934
Collection
Keywords
Publisher
  • PANGAEA  (3)
  • Geological Society of America (GSA)
  • Nature Publishing Group
  • Springer Nature
Years
  • 1965-1969  (3)
  • 1935-1939
  • 1930-1934
Year
  • 1
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    Unknown
    PANGAEA
    In:  Antarctic Research Facility, Florida State University
    Publication Date: 2023-08-28
    Description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 13 in 1964 by the Department of Geology, Florida State University. Cores and dredges were recovered for 31 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; ELT13; ELT13.001-PC; ELT13.005-PC; ELT13.006-PC; ELT13.007-BT; ELT13.008-BT; ELT13.009-PC; ELT13.010-PC; ELT13.013-BT1; ELT13.013-BT2; ELT13.013-PC; ELT13.016-PC; ELT13.017-PC; ELT13.018-PC; ELT13.021-PC; ELT13.024-PC; ELT13-11C; ELT13-19C; ELT13-1C; ELT13-3C; ELT13-4C; ELT13-5C; ELT13-6C; ELT13-8C; 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; TRAWL; Trawl net; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 557 data points
    Location Call Number Expected Availability
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  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Burns, Roger G; Fuerstenau, D W (1966): Electron-probe determination of inter-element relationships in manganese nodules. American Mineralogist, 51, 895-902, http://www.minsocam.org/ammin/AM51/AM51_895.pdf
    Publication Date: 2023-08-28
    Description: Manganese nodules have attracted considerable attention in recent years as a potential source of Mn, Fe, Co, Ni, Cu and other minor elements. These elements are enriched in manganese nodules relative to igneous rocks, sea-water, and deep-sea clays. The present paper describes methods by which element correlations may be determined with the electron-probe, and summarizes the results obtained by electron-beam scanning and specimen traversing. The results obtained in the present electron-probe investigation of manganese nodules may be summarized as follows: (l) The iron concentration fluctuates whereas the manganese concentration is relatively uniform throughout a manganese nodule, hbing slightly higher where iron is low. (2) There is a distinct correlation between Fe, Co, Ti, and Ca. (3) There is pronounced element coherence between Xi, Cu, Zn, and Mg, and between K and Ba. These elements are enriched with Mn and Al in regions of a nodule where the iron concentration is low. (4) The pronounced inter element relationships suggest that isomorphic substitution is an important factor controlling minor element distribution in manganese nodules. The ions Ni2+. Cu2+, Zn2+, Mg2+, K+ and Ba2+ substitute for Mn2+ in the "manganite" phases, Co(III) occurs with Fe(III) in hydrated iron oxide phases and Ti(IV) in delta-MnO2.
    Keywords: Aluminium; Calcium; Cobalt; Copper; DEPTH, sediment/rock; Description; DOWNWIND-H; Dredge; DRG; DWHD16; Electron Probe Microanalysis (EPMA); Horizon; Iron; Magnesium; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Potassium; Sample ID; Silicon; Titanium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
    Location Call Number Expected Availability
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  • 3
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    Unknown
    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
    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
    Location Call Number Expected Availability
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