Osteocalcin is a small (45 amino acids) secreted protein found to accumulate in bone and dentin of many organisms by interacting with calcium and hydroxyapatite, through the presence of three γ-carboxylated residues. In this work, we describe the first X-ray crystal structure for a nonmammalian osteocalcin, obtained at 1.4 Å resolution, purified from the marine teleost fish Argyrosomus regius. The three-dimensional fit between the A. regius structure and that of the only other known X-ray structure, the porcine osteocalcin, revealed a superposition of the CR atoms of their metal chelating residues, Gla and Asp, showing that their spatial distribution is consistent with the interatomic distances of calcium cations in the hydroxyapatite crystals. In both structures, the protein forms a tight globular arrangement of their three R-helices while the remaining residues, at N-and C-terminal regions, have essentially no secondary structure characteristics. This study revealed the presence of a fourth γ-carboxylation at Glu 25 , not previously detected in the structure of the porcine osteocalcin or in any other of the sequentially characterized mammalian osteocalcins (human, cow, and rat). A confirmation of the fourth Gla residue in A. regius osteocalcin was achieved via LC-MS analysis. These four doubly charged residues are, together with Asp 24 , concentrated in a common surface region located on the same side of the molecule. This further suggests that the known high affinity of osteocalcin for bone mineral may be derived from the clustering of calcium binding sites on this surface of the molecules.Osteocalcin, also called bone Gla protein or BGP, 1 was the first member of the calcium binding and vitamin K-dependent protein family not associated with blood coagulation to be described, sequenced, and characterized (2, 3). This small protein of 46-50 amino acid residues (depending on the species) (4, 5) is secreted mainly by osteoblasts. It is also one of the most abundant (10-20%) noncollagenous proteins in bones of most vertebrates examined to date, from bony fish to mammals (depending on species, age, and site) (4,(6)(7)(8)(9).Conserved elements in all osteocalcin sequences examined to date include a single disulfide bond (Cys 17 -Cys 23 ) using Argyrosomus regius amino acid sequence numbering, and three γ-carboxyglutamic acid residues (Gla) located at positions 11, 15, and 18 (4, 9-13). These Gla residues are thought to facilitate adsorption of osteocalcin to hydroxyapatite (10,14,15) and are located in the central, conserved portion of the molecule. In contrast, its N-terminal part exhibits considerable sequence variation (4,8,9,13).Initial studies showed that osteocalcin binds strongly to hydroxyapatite crystals (7) and affects mineral formation and mineral crystal growth in solution (16,17). Several studies also suggested a role for osteocalcin as a matrix signal for the recruitment and differentiation of osteoclasts (18-21). However, the understanding of the physiological function of osteocalcin was su...