Two distinctive pattens of microbial destruction of mineral shell in m
ussels from the Florida Escarpment (3266 m water depth) are described.
One pattern follows a surfacial selective removal of intercrystalline
organic matrix creating caries-like pits. Pitting of the shell resemb
les spreading bacterial colonies and results in substantial thinning o
f the original shell. The second pattern consists of an extensive syst
em of sacs with branched and tapered extensions penetrating deep into
the shell. Both activities are carried out by unknown microbial agents
on live mussels, as evidenced by the presence of repair nacre, which
often underlies effected areas. Shell destruction is primarily biologi
cal, providing conditions for enhanced chemical dissolution of the min
eral shell.