Not established in North America, including the Great Lakes region.
Monodacna colorata has a moderate probability of establishment if introduced to the Great Lakes (Confidence level: Moderate).
Specimens from the Caspian Sea are known to tolerate salinities of 1-10 ppt (Karpevich 1960), while those from the Azov die in salinities greater than 5 ppt (Zenkevich 1963).
This is well within the range of the Great Lakes; however, Shokhin et al. (2006) reported that juveniles best develop at a salinity of 5 ppt. This is higher than the typical range within the Great Lakes and may be a physiological factor that restricts establishment. Establishment may be further restricted by the inability of juveniles to overwinter; when shallow water regions become chilled, sexually immature individuals die out. Older (2-3 year old) individuals have adapted behaviorally to avoid these conditions by migrating to deeper waters of 4-5 m (Shokhin et al. 2006), but populations are still negatively affected. In 2003, severe winter conditions caused average biomass densities of M. colorata in areas of the Azov Sea to drop to 3.2 g/m2, down from usual densities of up to 600 g/m2 (Shokhin et al. 2006).
Hypanis colorata requires a sandy bottom environment with high oxygen content (Shokhin et al. 2006) and is reported to co-occur with the invasive Dreissena polymorpha in substrate at depths of 20-50 m (Kosova 1963). This habitat type is readily abundant in the Great Lakes, with possibly the exception of Lake Erie’s periodic anoxic conditions (Summers 2001). It feeds upon planktonic green algae, diatoms, and detritus (Zaitsev and Ozturk 2001), none of which are limiting within the Great Lakes. Hypanis colorata is likely to benefit from the predicted effects of climate change, including reduced ice-cover duration and warmer temperatures. This is evidenced by the massive reduction in biomass density in areas of the Azov Sea following harsh winter conditions in 2003 (Shokhin et al. 2006). Increased salinization, as predicted in the Great Lakes (Rahel and Olden 2008) is also likely to benefit this species, as juveniles best develop in salinity of 5 ppt and adults survive and reproduce in 8-9 ppt (Shokhin et al. 2006). This effect may also benefit H. colorata in terms of reduced competition with native bivalves (more than 40 species) that may not tolerate salinity increases.
There are no reported occurrences of M. colorata outcompeting another species within its native or introduced ranges throughout Europe. This species shows relatively low biomass densities in comparison to other species within benthic communities of Taganrog Bay in the Azov Sea (Shokhin et al. 2006) after once being reported as the dominant species there (Karatayev et al. 1997, Vorobiev 1949, Nekrasova 1971). In recent years, it has experienced native population reductions in areas of the Black Sea and is under strict protection in Romania (Popa et al. 2011).
Monodacna colorata is preyed upon by bottom-dwelling fish (Zaitsev and Ozturk 2001); however, the extent to which this predation will prevent the establishment of populations in the Great Lakes is unknown. It was intentionally stocked into the Veselovsky Reservoir, Russia from 1951-1956 for the purpose of enhancing fish diet (Grigorovich et al. 2002, Kruglova 1961, Zhuravel 1969, Zhuravel 1975). From there, it spread relatively quickly to other canals and reservoirs and reached the Caspian Sea and Volga delta—probably as a result of shipping traffic with the opening of the Volga-Don Canal (Grigorovich et al. 2002). Within 7 years of the opening of the canal in 1952, this species had spread from the Black-Azov Sea basin into the Caspian Sea (Saenkova 1956). In 1960, one year after appearing in the Caspian, this species was observed in the lower Volga River (Kosova 1963). Panov et al. (2009) classify this species as having a high probability of dispersal as well as a high probability of establishment once introduced to a new inland waterway based on information from Son (2007).