Andersen, M E (1978): Chemical composition of ferromanganese crusts and manganese nodules from the Indian and Southern Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.881835, Supplement to: Andersen, ME (1978): Accumulation rates of manganese nodules and sediments - An alpha track method. Master thesis, University of California, San Diego, USA, unpublished
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Abstract:
Excess 230Th dominates the alpha activity of the surface regions of manganese nodules and deep sea sediments. If uranium series eguilibrium is maintained, total alpha activity depth profiles should be as useful in determining sedimentation rates as are 230Th measurements. We have used cellulose nitrate alpha track recorders pressed against manganese nodule slabs to record high resolution alpha activity "maps' of a large number of nodules. Total alpha activity profiles have also been obtained for several sediment cores. From the approximately 90 nodule profiles measured to date, 73 show simple, approximately exponential depth dependence; about 2/3 of these have inferred deposition rates of 4-10 mm/10power6 yr. Ten profiles show statistically significant breaks in slope, suggesting growth rate changes. Within single dredge hauls there is little variation in growth rates, although different portions of the same nodule sometimes exhibit different growth rates. There is no correlation between depth and measured growth rate, except for a general tendency for the few Atlantic Ocean nodules we have measured to have slightly lower rates than Pacific or Indian Ocean samples. For a number of nodules and sediments the alpha track results have been compared with 230Th-based deposition rates measured by other workers. Two nodules have 230Th rates (W. S. Broecker et al., pers. comm.) identical within errors to the alpha track determinations. A third nodule (S. Krishnaswami, pers. comm. ) and two sediment cores previously measured by Goldberg and Koide (E. Sci. and Meteoritics, 1963, p. 90} all have much slower rates based on 230Th measurements compared with the alpha track results.
Related to:
Andersen, M E; MacDougall, J Douglas (1977): Accumulation rates of manganese nodules and sediments: An Alpha Track Method. Geophysical Research Letters, 4(9), 351-353, https://doi.org/10.1029/GL004i009p00351
Source:
Grant, John Bruce; Moore, Carla J; Alameddin, George; Chen, Kuiying; Barton, Mark (1992): The NOAA and MMS Marine Minerals Geochemical Database. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V52Z13FT
Further details:
Warnken, Robin R; Virden, William T; Moore, Carla J (1992): The NOAA and MMS Marine Minerals Bibliography. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V53X84KN
Project(s):
Coverage:
Median Latitude: -27.975308 * Median Longitude: 110.136714 * South-bound Latitude: -62.092000 * West-bound Longitude: 55.165000 * North-bound Latitude: 6.872333 * East-bound Longitude: -119.837000
Date/Time Start: 1968-01-01T00:00:00 * Date/Time End: 1975-06-19T00:00:00
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Event(s):
ELT33.017-PC * Latitude: -62.092000 * Longitude: -119.837000 * Date/Time: 1968-01-01T00:00:00 * Elevation: -5062.0 m * Recovery: 6.85 m * Campaign: ELT33 * Basis: Eltanin * Method/Device: Piston corer (PC)
ELT48.006-PC * Latitude: -34.005000 * Longitude: 97.543000 * Date/Time: 1971-01-01T00:00:00 * Elevation: -4343.0 m * Recovery: 10.78 m * Campaign: ELT48 * Basis: Eltanin * Method/Device: Piston corer (PC)
ELT50.036-PC * Latitude: -58.010000 * Longitude: 169.813000 * Date/Time: 1972-01-01T00:00:00 * Elevation: -5112.0 m * Recovery: 1.56 m * Campaign: ELT50 * Basis: Eltanin * Method/Device: Piston corer (PC)
Comment:
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
789 data points