Characterization of the chalky layer-derived EGF-like domain-containing protein (CgELC) in the pacific oyster, Crassostrea gigas

• Published in: Journal of structural biology Vol. 212; no. 1; p. 107594
• Main Authors: Iwamoto, Shihori, Shimizu, Keisuke, Negishi, Lumi, Suzuki, Nobuo, Nagata, Koji, Suzuki, Michio
• Format: Journal Article
• Language: English
• Published: United States Elsevier Inc 01.10.2020
• Subjects: Biomineralization; Calcite; Chalky layer; EGF-like domain; Mollusca; Biomineralization; Chalky layer; Mollusca; Calcite; EGF-like domain
• ISSN: 1047-8477; 1095-8657
• DOI: 10.1016/j.jsb.2020.107594

[Display omitted] •The EGF-like protein (CgELC) was found from the chalky layer in Crassostrea gigas.•Only the N-terminus of CGI_10017544 may be present inside the chalky layer (CgELC).•Aggregations of polycrystalline calcite were observed in the presence of CgELC. The shells of the Pacific oyster Crassostrea gigas contain calcite crystals with three types of microstructures: prismatic, chalky, and foliated layers. Many shell matrix proteins were annotated from the shells of C. gigas; however, it is unclear which SMPs play important roles in their shell mineralization. The matrix proteins have never been reported from the chalky layer. In this study, we identified a chalky layer-derived EGF-like domain-containing protein (CgELC) from the chalky layer of C. gigas shells. The gene sequence of the CgELC was encoded under CGI_ 10,017,544 of the C. gigas genome database. Only peptide fragments in the N-terminal region of CGI_ 10,017,544 were detected by LC-MS/MS analyses, suggesting that CGI_ 10,017,544 was digested at the predicted protease digestion dibasic site by post-translational modification to become a mature CgELC protein. We produced three types of CgELC recombinant proteins, namely, the full length CgELC, as well as the N-terminal and C-terminal parts of CgELC (CgELC-N or -C, respectively), for in vitro crystallization experiments. In the presence of these recombinant proteins, the aggregation of polycrystalline calcite was observed. Some fibrous organic components seemed to be incorporated into the calcite crystals in the presence of the r-CgELC protein. We also noted different features in the crystallization between CgELC-N and CgELC-C; some crystals were inhibited crystal plane formation and contained many columnar prisms inside the crystals (CgELC-N) and formed numerous holes on their surfaces (CgELC-C). These results suggest that CgELC is involved in crystal aggregation and incorporated into calcite crystals.