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  • 10-86; 10-94; 10-95; Acarinina collactea, δ13C; Acarinina collactea, δ18O; Acarinina mckannai, δ13C; Acarinina mckannai, δ18O; Acarinina nitida, δ13C; Acarinina nitida, δ18O; Chiloguembelina midwayensis, δ13C; Chiloguembelina midwayensis, δ18O; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Gavelinella spp., δ13C; Gavelinella spp., δ18O; Glomar Challenger; Gulf of Mexico/BENCH; Gulf of Mexico/SCARP; Leg10; Morozovella subbotinae, δ13C; Morozovella subbotinae, δ18O; Morozovella uncinata, δ13C; Morozovella uncinata, δ18O; Morozovella velascoensis, δ13C; Morozovella velascoensis, δ18O; Nuttallides spp., δ13C; Nuttallides spp., δ18O; Planktic foraminifera zone; Planorotalites compressus, δ13C; Planorotalites compressus, δ18O; Planorotalites pseudomenardii, δ13C; Planorotalites pseudomenardii, δ18O; Robulus spp., δ13C; Robulus spp., δ18O; Sample code/label; Subbotina trilocularis, δ13C; Subbotina trilocularis, δ18O; Subbotina triloculinoides, δ13C; Subbotina triloculinoides, δ18O
  • Dredge; DRG; Marara; NIXO10; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NX10-CL; Pacific Ocean; TECHNO 07
  • 1975-1979  (1)
  • 1978  (1)
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  • Data  (1)
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  • 1975-1979  (1)
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    PANGAEA
    In:  Supplement to: Guichard, Francois; Reyss, Jean-Louis; Yokoyama, Y (1978): Growth rate of manganese nodule measured with 10Be and 26Al. Nature, 272(5649), 155-156, https://doi.org/10.1038/272155a0
    Publication Date: 2023-08-28
    Description: Manganese nodules are considered to have accumulated in general very slowly: surface layers of nodules contain a large excess of 230Th, more than would be produced by uranium decay. The decrease of excess 230Th with depth within a nodule is generally interpreted to be due to the radioactive decay, and nodule accumulation rates were then estimated from this to be a few mm/Myr. How then do these nodules escape from burial by associated marine sediments which accumulate 3 orders of magnitude faster than the nodules? One possible explanation is that the radionuclides of interest were not incorporated in the nodule matrix during its growth but were adsorbed later. Subsequent inward diffusion of the radionuclides might result in an apparent radioactive decay. We have tested this hypothesis by measuring simultaneously two radionuclides of different half lives. If the gradients of the radionuclides are really due to the radioactive decay, then, assuming a constant growth rate for a nodule, we expect the profile of the shortlived nuclide to be steeper (because of its faster decay) than that of the longlived nuclide.
    Keywords: Dredge; DRG; Marara; NIXO10; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NX10-CL; Pacific Ocean; TECHNO 07
    Type: Dataset
    Format: application/zip, 2 datasets
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