Using the Stylophora pistillata genome and cell cultures to understand the mechanism of aragonite precipitation in corals

Atmospheric CO 2 levels are rising rapidly, resulting in a decrease in both oceanic pH, and the carbonate saturation state (Ω). It has been hypothesized that calcifying marine organisms, including reef-building corals, will be affected by the decline of the carbonate saturation state. However, it is still unclear how corals will respond to these changes, as their skeletal formation is biologically mediated and occurs in isolated space rather than directly from seawater. In corals new skeletal material is precipitated in the subcalicoblastic space between the skeleton and the calicoblastic epithelium which, does not exceed a few nanometers and contains the ''calcifying fluid''. The goal of our project is to understand how these fluids respond to changes in the surrounding seawater and in turn affects the biologically mediated calcification mechanisms at the molecular, cellular and tissue levels. While it is generally thought that an organic matrix, which contain a suite of proteins, lipids and poly-saccharides, take part in calcification process, the specific mechanism by which the mineral is precipitated is unknown. The organic matrix composed of two fractions: the soluble organic matrix (SOM) and the insoluble organic matrix (IOM). It is suggested that the IOM plays a role as structural proteins forming a framework for crystal growth whereas the SOM plays a role in nucleation and crystal growth. To address this question we have investigated both the structural framework proteins (Drake et al abstract submitted to the AGU fall meeting) the role of proteins in nucleation and crystal growth (this work). Here, we established cell cultures and sequenced the 458-megabase genome of the stony coral, Stylophora pistillata, using next-generation sequencing technology. This genome contains 21,678 predicted protein-coding genes. Many of the known protein components of invertebrate skeletal matrices are acidic and/or contain repeated sequences. We searched for genes encoding proteins with the following characteristics: (1) high content (>35%) of acidic amino acids (aspartate and glutamate), (2) at least 150 residues, and (3) a signal peptide. This approach revealed eight coral acidic proteins (CAPs). We confirmed the sequence of four candidates (CAP1-3 and 8). A search for similarity in the UniProt database and published coral's genomes and ESTs reveals high similarity of CAPs 2, 3, and 8 to both invertebrate and vertebrate acidic rich proteins. CAP1, however, has no significant matches in any of the databases. We expressed and purified these four proteins to examine their role in coral bio-mineralization. We show that the pure CAPs bind Ca+2, and furthermore, individual CAPs can precipitate calcium carbonate in vitro in artificial seawater. These results strongly suggest that aragonite precipitation in the calcifying region of corals is promoted by a highly conserved set of acidic proteins. Based purely on thermodynamic grounds, the predicted change in surface ocean pH should not affect the binding ability of these acidic proteins. To the extent these proteins are responsible for calcification in this and other corals, we suggest that corals will continue to calcify at pH changes predicted to occur in this century.