MARINE EUTROPHICATION My studies on fluctuations of population size of shellfish resources began in Canada, and were seen to reflect long-term natural fluctuations in tidal regimes and temperature. When beginning work as technical secretary to the Mediterranean Commission (GFCM), it became evident that the productivity of some Northern Mediterranean sub-areas was not only affected by natural environmental fluctuations, but also by a trend in runoff of nutrients from land of anthropogenic origins in recent decades. A negative factor in the Mediterranean trawl fishery, according to classical fisheries theory, is the very low size at first exploitation of cohorts (Ages 0+ to 1+, with few adult fishes present in the catches for some key species, and the lack of quota and effort control. These features all suggest serious overexploitation. This was confirmed by the few estimates of exploitation rate then available. However, landings, while not high, were not declining as would have been predicted from experience elsewhere, but in many cases were increasing during the 1970’s and 80’s. A review of landing trends in the late 1970’s-80’s also suggested this for many species. Extensive experience by UNEP and other environmental agencies, which were alarmed by rising nutrient inputs, had documented progressive eutrophication of many semi-enclosed seas, especially in the Mediterranean basins. This suggested, with rising landings of small fishes, that the lower levels of the food web were receiving greater nutrient inputs than formerly. The Mediterranean for example, was once an oligotrophic water body outside of estuarine areas in the early 20C, but by the 1980’s from satellite imagery, it was clear that areas such as the Gulf of Lions and Adriatic, were receiving heavy river inputs of nutrients due to human activities on land. In the case of the Black Sea, eutrophication of an almost-enclosed sea body was fed by a large catchment area subject to heavy nutrient supplements. This led in the 1980-90’s to what can be called a ‘toxic nutrient shock’ of excess nutrients due to runoff of large rivers such as the Danube and Dnieper. This has led to a collapse of the biological system, well documented by scientists of coastal countries, which affects almost all fishery resources. Supplemented by over-exploitation, migratory pelagic fish ceased to arrive seasonally from the Mediterranean to the eutrophic northern basin, reducing their top-down predatory control on small pelagic stocks. Key effects arose from the elimination of benthic algae which formerly oxygenated shelf waters, now hypoxic. This in turn, eliminated benthic filter feeders such as mussels which previously had removed suspended material. The arrival of an exotic ctenophore (Mnemiopsis) from the West Atlantic in ship ballast water, led to its explosion in numbers, causing a collapse of small pelagic stocks in the late 1970’s-80’s. A steady-state’ ECOPATH modeling exercise considered the possibilities for control of the outbreak, and suggested that a predator might help control Mnemiopsis populations. This option remained open, given that the only natural Mnemiopsis predator in its ‘home habitat’ in the West Atlantic was Beroe, another ctenophore. The subsequent appearance of this predator in the Black Sea ecosystem remains unexplained, but seems a likely cause for a subsequent reduction in Mnemiopsis stocks. A later modeling exercise with Russian colleagues provided a more detailed explanation of these ecosystem changes in the pelagic food web. What seems evident in retrospect is that overfishing and eutrophication led to a complex sequence of ecosystem impacts. 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