IntroductionPolychaeta is one of the most diverse and abundant benthic groups in marine ecosystems: 12,632 species of polychaetes are reported in the world's oceans (Appeltans et al., 2012), while 1122 species are reported in the Mediterranean Sea (Coll et al., 2010) and 238 species in the Black Sea to date (Kurt Şahin and Çınar, 2012). The polychaetes distributed among the Turkish coasts were recently reported by Çınar et al. (2014) with 459 species from the coast of the Levantine Sea, 547 species from the coast of the Aegean Sea, 390 species from the coast of the Sea of Marmara, and 136 species from the Black Sea coast of Turkey.The Black Sea is a semiclosed sea and it is the largest (547,000 km 3 ) permanently stratified marine basin in the world (Zaitsev et al., 2002). It is connected to the Aegean region of the Mediterranean Sea by the narrowest strait of Turkey, the Bosphorus, to the south, and the Sea of Azov by the Strait of Kerch to the north. Nearly 87% of the Black Sea is entirely anoxic (without oxygen) and it contains high levels of hydrogen sulfide. Anoxic conditions occurring below 70 to 200 m limit the vertical distribution of organisms. The hydrographic regime is characterized by low salinity surface water of river origin overlying high salinity of deep water of Mediterranean origin (Bakan and Büyükgüngör, 2000). The structure of its ecosystem differs from that of the neighboring Mediterranean Sea in that species diversity is lower and the dominant organism groups are different. However, the abundance, total biomass, and productivity of the Black Sea are much higher than those in the Mediterranean Sea (Zaitsev and Alexandrov, 1998).The first studies concerning polychaetes in the Black Sea date back to the late 1800s (