“…Two relevant such sources are the microbial biofilms that develop on the surface of bones from shallow and deep water marine environments, and the symbionts of bone-dwelling worms, e.g., Osedax mucofloris . These bio-resources have been shown to have a wide microbial diversity, whose compositions and involvement in the various and successive events involved in the degradation of mature bone, have been investigated to some detail [14] , [15] , [16] , [17] , [18] , [19] , [20] , [21] , [22] , [23] , [24] , [25] , [26] , [27] . In this process, recent metagenome sequence analyses suggested that, as mentioned above, the acidification by some organisms is key before the hydrolysis of bone matrix is initiated by other community members [27] .…”