Shell thickening and chambering in the oyster Crassostrea gigas: natural and anthropogenic influence of tributyltin contamination.

Abnormal thickening and chambering in Crassostrea gigas oysters have been adopted for many years as bioindicators of available tributyltin (TBT) in coastal waters. Nevertheless, since natural causes can also induce the formation of multiple chambers, a field study and laboratory experimentation has been conducted with 72 examples of C. gigas in successive culture media. This work has enabled differences to be established between natural fine sediment-induced characteristics and the influence of TBT on the shells. External shell deformities have been assessed using three biometric indices, shell thickness index, weight index and volume index. Internal differences have been observed in longitudinal sections of the shell: retraction of growth, stagnation of the adductor muscle scar and thinning of the chambers in the TBT-polluted shell secretion. A new index, the opening chambers index, has been proposed, with a value of less than 1 in the TBT-polluted environment and greater than 1 in shells secreted in an unpolluted production site. These conclusions should be borne in mind when C. gigas is used in biomonitoring programmes.

Distribution of butyltin and derivatives in oyster shells and trapped sediments of two estuaries in Cantabria (Northern Spain).

Distribution of butyltin compounds (BTs) and derivatives (monobutyltin, MBT; dibutyltin, DBT and tributyltin, TBT) was analysed in Crassostrea gigas oyster shells and the sediments trapped in the shell chambers, from two different estuaries in Cantabria (Northern Spain), with very different environmental conditions, where previous data have not been reported. Inorganic tin analysis in oyster shells was performed in order to study the degradation of BTs. Shell thickening and losses in biological growth are related with the presence of TBT, and were determined using three morphological indexes. Total BTs concentrations, expressed as Sn, ranged from 18.0 ng g(-1) to 176.7 ng g(-1) in sediments, and from 2.4 ng g(-1) to 11.1 ng g(-1) in oyster shells. Total inorganic tin concentrations ranged from 1775.0 ng g(-1) to 4781.3 ng g(-1) in oyster shells. The amount of BTs in oyster shells has been associated with the concentrations in the sediments trapped in the shell chambers. Partition coefficients between oyster sediments and oyster shells show the affinity of BTs by the sediments and the higher inorganic tin in oyster shells does not seem to be related to the BTs pollution.