Features of the Comacchio ecosystem transformed during persistent bloom of picocyanobacteria |
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| Authors: | Yuri I Sorokin Olga Yu Zakuskina |
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| Institution: | (1) National Institute for Minamata Disease, Minamata Kumamoto, 867–0008, Japan;(2) Faculty of Engineering, Nagasaki University, Bunkyo-machi 1–14, Nagasaki 852–8521, Japan;(3) Faculty of Engineering, Kyusyu University, Nishiku Motooka 744, Fukuokashi 819–0395, Japan;(4) Faculty of Science, Kagoshima University, Korimoto Kagoshima, 890–0065, Japan;(5) International Mercury Laboratory Inc, Minamata Kumamoto, 867–0034, Japan |
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| Abstract: | The big Comacchio lagoons (NW Adriatic coast) have been experiencing a super-dense, long-term bloom of picocyanobacteria (PCB)
since 1985. This bloom has caused profound transformations in their ecosystem and has resulted in the loss of valuable fish
and clam resources. The composition, density and seasonal dynamics of this bloom and its impact on the ecosystem were studied
between spring and autumn 1995 and in the summer of 2001. The density of the blooming phytoplankton assemblages varied from
8 to 35 × 106 cells ml−1, and biomass from 20 to 40 g m−3, thus demonstrating a quasi-stable status since 1993. The share of pico + nanocyanobacterial fraction of the total phytoplankton
biomass was 98% in spring to early summer, and 92% in autumn. The remaining 0.2–5% comprised eukaryotic nano-algae. All components
of the animal food web were found to be drastically depleted in the lagoons. Their biomass range in the open lagoons areas
were: 2 to 20 mg m−3 of microzooplankton, 10 to 40 mg m−3 mesozooplankton, and 5 to 12 g m−2 macrozoobenthos. The share of filtering fauna in the whole ecosystem metabolism was less than 2%. The malfunction of the
deteriorated animal food web resulted in the hyper-accumulation of non-grazed microplankton biomass and detritus in the water
column and in bottom sediments. The sequence brought the acceleration of sulfide production and the accumulation of acid soluble
sulfides in the upper sediment layer of up to 700–800 mg S dm−3 of wet silt. The results of this study provide evidence that the state of ecological collapse continues in the lagoons since
1993. |
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