Consequently, the annual turnover ratio is

∼12:1, so that all of the water within the reservoir is exchanged every month. However, in spite of this high turnover rate, large blooms of cyanobacteria occur every year, with no viable prospects for improving water quality beyond ICG-001 concentration the introduction of seawater. Despite over 3 billion yen being invested every year to improve water quality in the reservoir, COD levels continue to rise, and remain far above the targeted value set by MAFF (5 mg/L; Fig. 8). Moreover, pH levels detected at station R1 and other locations range from 8 to 9, well above recommended levels for rice cultivation (pH 6.0–7.5, MAFF, 1971). The solubility of iron is significantly diminished under high pH conditions, resulting in iron deficiency

in rice crops grown under these conditions (Ponnameperuma, 1975). Furthermore, the salinity of the irrigation water drawn from the reservoir is also an obstacle to agriculture. As shown in Fig. 9, the salinity of the water at stations R2–R4 is too high for agricultural use, resulting in water from the reservoir being used only for rice cultivation on reclaimed land created before 1997. The salinity declines soon after the rainy season, but it gradually returns over time, likely due to the permeation of seawater. The only water used on the vegetable fields grown on land created by project is supplied from the mouth of the Honmyo River and by other nearby rivers. Water drained from the reservoir often contains large amounts of sediment, which carries with learn more it considerable amounts of MCs, which are exhausted into the surrounding bay. Even if the figures presented in Table 3 represent an overestimation due to variation in MC levels at different depths, the levels of MCs exhausted into the surrounding area have played a considerable part in the decline of the fishing industry throughout

the bay. It is possible that some MCs exhausted from the Isahaya Bay reservoir could be degraded by bacteria in the surrounding environment (Bourne et al., 1996, Ishii PIK-5 et al., 2004, Park et al., 2001, Chen et al., 2010 and Jiang et al., 2011). However, an additional report detailing the sedimentation of cyanotoxins (nodularin-R, and microcystin-LR) in the north Baltic Sea (Kankaanpää et al., 2009) supports the notion of MC accumulation in the local environment. In the present study, MCs were detected in the sediment throughout the year, indicating a clear limit to environmental degradation. Preliminary data from our laboratory suggest that the degradation rate of MCs in sediment is temperature-dependent, with almost no degradation seen at temperatures below 20 °C. This allows for MC levels to persist throughout the year, as the activity of MC-degrading enzymes is lost at temperatures where cyanobacteria are unable to multiply.