Abstract
In an effort to explain the rarity of fish bones in the Great Lakes sediments, the degradation of ground fresh fish bones in microcosms containing Lake Erie sediments has been studied. The rapid build-up of phosphorus in the aqueous phase points to the great instability of the bone mineral in these sediments, while the actual analysis of the sediments shows that 10–50% of the added bone was degraded in three weeks. The decomposition rate was independent of the redox conditions of the microcosm, and was biologically mediated. Also, the incongruent dissolution of the bone apatite entailed the secondary formation of vivianite (ferrous phosphate) and other calcium and aluminocalcium phosphates. Calculations suggest that fish debris account for well over 10–20% of the P flux to the sediments in some nearshore areas. Since most of this P is quickly remineralized, the contribution of carrion to the differences in the quality of nearshore and offshore waters of the Lower Great Lakes must remain an intriguing question.
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Nriagu, J.O. Rapid decomposition of fish bones in Lake Erie sediments. Hydrobiologia 106, 217–222 (1983). https://doi.org/10.1007/BF00008119
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DOI: https://doi.org/10.1007/BF00008119