Serpulid tubes are composed of aragonite, calcite or mixture of both polymorphs.
In addition to the tubes, some serpulid species secrete calcareous opercula.
There are thin organic sheets in serpulid tube mineral structures.
These sheets have evolved as an adaptation to strengthen the mechanical properties of the tubes.
[1][2][3][4][5] Fossil and present-day cirratulid bioconstructors have been confirmed to be the only known occurrence of double-phased biomineralization processes in the animal kingdom.