Sabellariid polychaetes are well known as reef builders in shallow waters throughout temperate and tropical oceans (Kirtley 1994; Pandolfi et al. 1998). They often apply mucus to sorted particles and lay tubes as building blocks of reef structure (Kirtley 1994). They typically occur in dense aggregations and form mounds or reef-like structures in intertidal or subtidal areas off coasts of America and the Mediterranean Sea. In May 2008, we discovered well-developed sabellariid reefs on subtidal wavebreakers that extend for about 1 km near Hualien Port (23°58.155 N, 121°36.905 E) in eastern Taiwan. Densely aggregated tubes of Idanthyrsus cretus Chamberlin, 1919 piled up as reef masses and extend from 1 to 7 m in depth near the sandy bottom (Fig. 1). The density reaches 5,400 worm tubes/m2, with a gradual decrease as water depth increases. The average thickness of the worm reef is 10.1 ± 10.4 cm (mean ± SD) and the maximum is about 50 cm at depth between 3 and 5 m. Based on the installation date of wavebreakers in 1996–2003, the estimated growth rate of the worm reefs was about 4.2–10.0 cm/year, which is higher than the accretion rates of most coral reefs.

Fig. 1
figure 1

a Dense aggregation of Idanthyrsus cretus on a wavebreaker and b a portion of worm reef, scale = 1 cm

The sabellariid reefs provide substrata for a diverse community of epifauna and infauna, and their ecological roles are comparable to those of the tropical coral reefs. In addition, they form consolidated structures that offer protective cover to wavebreakers, which further help stabilizing the substrate. This is the first observation of I. cretus as a primary frame-builder forming subtidal reefs in the West Pacific, since it has not been recorded as fossils nor in the extant forms in this area (Pandolfi et al. 1998). The occurrence of I. cretus reefs along the Hualien coast is possibly due to a concurrence of various local environmental conditions, where there is an abundant supply of terrestrial organic particles and sand-size sediment, vigorous wave action, and strong currents. These unusual sabellarid reefs invite further ecological and biological studies.