Abstract

10Be concentrations of six soils on the raised coral reef terraces of Kikai Island, southwest Japan range from 0.80 to 7.17×10 9 atoms g −1. The annual deposition rate of 10Be from the atmosphere to Kikai Island from 2000 to 2002 ranges from 2.0 to 3.5×10 6 atoms cm −2 year −1, with a mean of 2.8±0.7×10 6 atoms cm −2 year −1. Minimum absolute ages, calculated from the inventory of meteoric 10Be in the soils and the annual deposition rate of 10Be, are: Initial Rendzina-like soil, ≥8 ka; Rendzina-like soil, ≥18 ka; Brown Rendzina-like soil, ≥56 ka; Terra fusca-like soil, ≥127 ka; Terra rossa-like soil, ≥136 ka; and Intergrade between Terra rossa-like and Red-Yellow soil, ≥102 ka. Therefore, it was concluded that soil formation during the first ∼60,000 years would be as Rendzina-like soils and more than ∼100,000 years would be required for Red-Yellow soils to develop on raised coral reef terraces under subtropical humid climatic conditions.

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