10Be and Th isotopes in manganese nodules and adjacent sediments: Nodule growth histories and nuclide behavior

The concentration profiles of ⁹Be, ¹⁰Be, ²³⁰Th, ²³²Th, ²³¹Pa (via ²²⁷Th) and ²³⁸U have been measured in three manganese nodules, one each from the North Pacific (A47-16(4)), the South Pacific (TF-5) and the Indian Ocean (R/V Vitiaz). In addition the ¹⁰Be concentration in deep water from the GEOSECS reoccupation station 500 of the North Pacific, and in ? cores raised from the manganese nodule field in the North Pacific have been measured. The ¹⁰Be concentration in nodule and seawater samples was measured by the accelerator masss spectrometric technique employing the Yale Tandem Van de Graaff accelerator.The concentrations of ¹⁰Be, ²³⁰Th_exc and ²³¹Pa_exc and ratios of ¹⁰Be/⁹Be and ²³⁰Th_exc/²³²Th all decrease with depth in the nodules. This decrease, interpreted in terms of nodule growth, yields “average” growth rates of a few millimeters per million years for the nodules. The growth rates of the nodules exhibit temporal variations, both on short time (～ 50,000 years) and long time (several million years) scales. Of the three nodules studied, only in TF-5 is the short-term average growth rate based on ²³⁰Th_exc in the top 0–0.5 mm the same as the long-term average rate based on Be isotope data for the 0.5–17 mm interval. For the other two nodules, the recent average growth rates based on²³⁰Th_exc data differ significantly from the long-term average growth rates based on Be isotopes. In A47-16(4) the ¹⁰Be based rate is less than the ²³⁰Th_exc rate and in R/V Vitiaz the ¹⁰Be based rate is greater than the ²³⁰Th_exc rate. This observation, coupled with measurable changes in growth rates even during the past few hundred thousand years, suggests, but does not prove, that the discordant growth rates deduced from ²³⁰Th_exc and ¹⁰Be profiles document changes in nodule growth rate with time rather than mixing effects on ²³⁰Th_exc profiles.The ¹⁰Be concentration in the GEOSECS North Pacific deep water is 6100±1200 atoms/g. This value coupled with the average surface ¹⁰Be/⁹Be ratio of North Pacific nodules predicts a ⁹Be concentration within the limits of measured values. The inventory of ¹⁰Be and ²³⁰Th_exc in the nodules is only ～ 10% of the total, the remaining being in sediments. The ¹⁰Be concentrations in the upper portions of two adjacent cores studied are nearly the same, but the deposition fluxes of both ¹⁰Be and ²³⁰Th based on ²³⁰Th dating vary by a factor of two. This difference is attributable to local redistribution of sediment at the time of deposition prior to accumulation.