Takeuchi Takeshi, Yamada Lixy, Shinzato Chuya, Sawada Hitoshi, Satoh Noriyuki
Marine Genomics Unit, Okinawa Institute of Science and Technology Graduate University, Onna, Okinawa, 904-0495, Japan.
Sugashima Marine Biological Laboratory, Graduate School of Science, Nagoya University, Sugashima, Toba, 517-0004, Japan.
PLoS One. 2016 Jun 2;11(6):e0156424. doi: 10.1371/journal.pone.0156424. eCollection 2016.
Despite the importance of stony corals in many research fields related to global issues, such as marine ecology, climate change, paleoclimatogy, and metazoan evolution, very little is known about the evolutionary origin of coral skeleton formation. In order to investigate the evolution of coral biomineralization, we have identified skeletal organic matrix proteins (SOMPs) in the skeletal proteome of the scleractinian coral, Acropora digitifera, for which large genomic and transcriptomic datasets are available. Scrupulous gene annotation was conducted based on comparisons of functional domain structures among metazoans. We found that SOMPs include not only coral-specific proteins, but also protein families that are widely conserved among cnidarians and other metazoans. We also identified several conserved transmembrane proteins in the skeletal proteome. Gene expression analysis revealed that expression of these conserved genes continues throughout development. Therefore, these genes are involved not only skeleton formation, but also in basic cellular functions, such as cell-cell interaction and signaling. On the other hand, genes encoding coral-specific proteins, including extracellular matrix domain-containing proteins, galaxins, and acidic proteins, were prominently expressed in post-settlement stages, indicating their role in skeleton formation. Taken together, the process of coral skeleton formation is hypothesized as: 1) formation of initial extracellular matrix between epithelial cells and substrate, employing pre-existing transmembrane proteins; 2) additional extracellular matrix formation using novel proteins that have emerged by domain shuffling and rapid molecular evolution and; 3) calcification controlled by coral-specific SOMPs.
尽管石珊瑚在许多与全球问题相关的研究领域中都很重要,如海洋生态学、气候变化、古气候学和后生动物进化,但对于珊瑚骨骼形成的进化起源却知之甚少。为了研究珊瑚生物矿化的进化,我们在鹿角珊瑚(Acropora digitifera)的骨骼蛋白质组中鉴定出了骨骼有机基质蛋白(SOMPs),该珊瑚拥有大量的基因组和转录组数据集。基于后生动物之间功能域结构的比较进行了细致的基因注释。我们发现SOMPs不仅包括珊瑚特有的蛋白质,还包括在刺胞动物和其他后生动物中广泛保守的蛋白质家族。我们还在骨骼蛋白质组中鉴定出了几种保守的跨膜蛋白。基因表达分析表明,这些保守基因在整个发育过程中持续表达。因此,这些基因不仅参与骨骼形成,还参与基本的细胞功能,如细胞间相互作用和信号传导。另一方面,编码珊瑚特有的蛋白质的基因,包括含细胞外基质结构域的蛋白质、 galaxins和酸性蛋白质,在变态后阶段显著表达,表明它们在骨骼形成中的作用。综上所述,珊瑚骨骼形成的过程被假设为:1)利用预先存在的跨膜蛋白在上皮细胞和基质之间形成初始细胞外基质;2)利用通过结构域改组和快速分子进化产生的新蛋白质形成额外的细胞外基质;3)由珊瑚特有的SOMPs控制钙化。