STRONTIUM AND CARBON-ISOTOPE TRACERS AND THE ORIGINS OF SOIL CARBONATE IN SOUTH-AUSTRALIA AND VICTORIA

Calcium carbonate occurs in soils in association with a variety of roc k types in coastal and inland South Australia and Victoria. The Sr-87/ Sr-86 ratios of the coastal soil carbonates fall between 0.7094 and 0. 7098, showing that the ocean is the principal source of calcium to nea rly all soils near the coast, and that contributions from bedrock are generally small. An exception is the soil formed on the young volcano at Mt. Gambler in which the average ratio for carbonate is about 0.707 0 compared to 0.7041 for the volcanic ash. The basaltic ash of the vol cano is readily weathered and rich in calcium: roughly 40% of strontiu m and 10 to 20% of the calcium in the soil carbonate derives from the ash, and the balance from marine sources. The Sr-87/Sr-86 ratios from soil carbonate gradually increase inland, reaching values of 0.7152. T hese higher ratios reflect, at least in part, the increasing Sr-87/Sr- 86 ratio of inland dust. In contrast, the ocean does not contribute si gnificantly to the carbon pool of the soils we studied. The delta(13)C (PDB) values of soil carbonates on Kangaroo Island and the higher rai nfall areas of eastern Victoria fall between -11.0 and -8.7 parts per thousand, indicating that the carbonate formed in equilibrium with the C-3-dominated vegetation typical of the region. In the warmer inland areas to the north such as the Eyre Peninsula, the delta(13)C value of soil carbonate averages -5.3 parts per thousand, reflecting the highe r proportion of C-4 plants in the local biomass. Mixing with marine so urces of carbonate cannot account for the observed carbon isotopic pat terns. The flux of carbon into soils from the ocean therefore must be small compared to that derived from plant respiration and decay.