These findings indicate that dead assemblages preserved in shallow, fully carbonate environments primarily reflect the composition of the original source communities, making them useful to identify recent changes in coral reef areas where anthropogenic impacts are present. Given that time averaging is approximately 19 years in the OTR lagoon, we conclude that the composition of the living assemblage has remained largely unchanged for the last 30 years. The live molluscan assemblage sampled was similar to the live assemblage sampled 30 years ago. Taphonomic factors were responsible for less than 20% of the differences in species composition between live and dead shell assemblages. Differences in composition were largely due to sample size, the low probability of sampling rare species and to a lesser degree differences in skeletal durability.
Diversity and evenness metrics indicated no significant difference between the live and dead assemblages, and dead assemblage rank order abundance explains 82% of that of the live assemblage. Live (n = 1335) and dead (n = 6919) molluscan assemblages were collected from three shallow (6 m) carbonate soft-sediment lagoons. One Tree Reef (OTR) (southern Great Barrier Reef, Australia) has had very little direct anthropogenic influence over the past four decades, making it a good system for focusing on taphonomic patterns. Given the potential of sedimentary assemblages to provide temporal perspectives on the history of modern communities, assessments of live-dead agreement in reef mollusk assemblage composition are necessary and timely for understanding rapid environmental change.
The agreement between live and dead assemblages has been extensively studied, because discrepancies between the two can reveal taphonomic bias, anthropogenic impact, and/or a decrease in temporal resolution of dead assemblages to centennial scales (i.e., time averaging). Reef-associated sediments accumulate over time recording the history of biological communities.
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