Thesis (Ph. D.)--Boston University, 1991. / Interest in deep sea microbiota was stimulated by recent discoveries of productive redox communities associated with hydrothermal vents and brine seeps, and based on bacterial chemolithotrophy. This study investigates microbial destruction of mussel shells from a redox community at the base of the Florida Escarpment (3360 m), in comparison with microbial boring in shells of typical, low productivity areas of the ocean floor. An assemblage of eukaryotic and prokaryotic periostracum borers and their boring traces were discovered in shells of Bathymodiolus mussels from the base of the Florida Escarpment, and characterized. Microbial destruction of this protective layer results in colonization of secondary microbial inhabitants inside boreholes, and exposes the underlying mineralized shell to colonization and destruction by microbial endoliths. Microbial consumption of periostracum often proceeds in successive waves. These organisms show different "foraging" behaviors and leave accordingly varied boring patterns. These activities create a labyrinth of pits, holes and tunnels which, in tum, provide sheltered microenvironments for secondary microbial settlers, including primary producers, which all constitute an abundant food source for numerous ciliates and gastropods observed on the shells. This concerted attack on the periostracum eventually leads to the exposure of the mineralized shell. Such exposed areas are characterized by [TRUNCATED]