Abstract

The seral phases of decay for carcases of the African elephant are described in detail. Rapid decomposition of soft tissue and skin is reported but the breakdown and/or incorporation of bone into the lithosphere is greatly delayed. In the absence of vertebrate scavengers, dipterous larvae consume up to 5 per cent of the soft tissues, the remainder being utilized by microorganisms. The importance of the calcium immobilized in large mammal bones in processes of mineral cycling is discussed.

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