Abstract
Buried nodules have been found at two positions in the central Pacific at 25, 33, and 40 cm beneath the sediment surface in a depth, which, from Io-dating, is younger than 75,000 years. These nodules differ from surface nodules in that they have an unusual additional outer zone of material of high porosity containing sediment inclusions. The material in this additional zone has a high α activity. Beneath this zone, a normal α decrease was measured. The outer zone has a higher Cu/Mn ratio and lower Ni/Mn, Fe/Mn, and Co/Fe ratios than the inner zones. Element mobilization within the sediment is assumed to supply the buried nodules during their additional growth. A higher sedimentation rate and an atypical distribution of organic matter with depth at these two stations point up the exceptional environment of the buried nodules. Therefore, only a small number of nodules are assumed to grow further after being buried.
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More From: Deep Sea Research Part A. Oceanographic Research Papers
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