New non-bilaterian transcriptomes provide novel insights into the evolution of coral skeletomes
AbstractA general feature of animal skeletomes is the co-presence of taxonomically widespread and lineage-specific proteins that actively regulate the biomineralization process. Among cnidarians, the skeletomes of scleractinian corals have been shown to follow this trend, however in this group distribution and phylogenetic analyses of biomineralization-related genes have been often based on limited numbers of species, with other anthozoan calcifiers such as octocorals, being overlooked. We de-novo sequenced the transcriptomes of four soft-coral species characterized by different calcification strategies (aragonite skeleton vs. calcitic sclerites) and data-mined published non-bilaterian transcriptomic resources to construct a taxonomically comprehensive sequence database to map the distribution of scleractinian and octocoral skeletome components. At the large scale, no protein showed a ‘Cnidaria+Placozoa’ or ‘Cnidaria+Ctenophora’ distribution, while some were found in cnidarians and Porifera. Within Scleractinia and Octocorallia, we expanded the distribution for several taxonomically restricted genes (TRGs) and propose an alternative evolutionary scenario, involving an early single biomineralization-recruitment event, for galaxin sensu stricto. Additionally, we show that the enrichment of acidic residues within skeletogenic proteins did not occur at the Corallimorpharia-Scleractinia transition, but appears to be associated with protein secretion in the organic matrix. Finally, the distribution of octocoral calcification-related proteins appears independent of skeleton mineralogy (i.e. aragonite/calcite) with no differences on the proportion of shared skeletogenic proteins between scleractinians and aragonitic or calcitic octocorals. This points to skeletome homogeneity within but not between groups of calcifying cnidarians, although some proteins like galaxins and SCRiP-3a could represent instances of commonality.