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Bivalves with ‘concrete overcoats’: Granicorium and Samarangia
Author(s) -
Taylor J. D.,
Glover E. A.,
Braithwaite C. J. R.
Publication year - 1999
Publication title -
acta zoologica
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.414
H-Index - 37
eISSN - 1463-6395
pISSN - 0001-7272
DOI - 10.1046/j.1463-6395.1999.00019.x
Subject(s) - calcium carbonate , aragonite , biomineralization , cement , carbonate , nucleation , materials science , mineralogy , rosette (schizont appearance) , mucus , geology , biology , composite material , paleontology , chemistry , metallurgy , organic chemistry , immunology
Two veneroidean bivalves Granicorium indutum from Australia and Samarangia quadrangularis from the tropical Indo‐Pacific region, cement a thick, hard layer of sand over most of their shells. In Granicorium this layer forms low commarginal ribs while in Samarangia it forms more prominent radial features. Sand grains are cemented to the shell and to each other with growths of a crystalline aragonitic cement similar in morphology to inorganic marine cements. Both species secrete mucus layers at the growing shell margin which initially hold the sediment grains together and form a substrate for the nucleation and growth of calcium carbonate crystals. The ribs of Samarangia are formed by the accretion of successive sheets of spherulitic growths. In G. indutum , the middle and outermost of two inner mantle folds are large, glandular and capable of considerable extension beyond the shell margin. Mucus secreted by the folds contains abundant bacteria and small calcium carbonate crystals. It is proposed that initial nucleation of the calcium carbonate cement takes place within this biofilm possibly mediated by the bacteria. The function of the sand layers is unknown but predation resistance and protection of the shells from endobionts are the most likely possibilities.