Byssally attached to lava around diffuse vents, with absence of massive hydrothermal deposits and vent fluid temperature not exceeding 8.5°C. Endemic to vents. Development not known but most probably with planktonic larval phase.
- COSEL R. VON, METIVIER B. & J. HASHIMOTO (1994) Veliger 37(4): 374-392 [380-386].
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