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If a larval fish hatches too early or too late relative to its food supply Lasker, , it will die. Additionally wind-induced turbulence dilution effect of prey organisms and temperature influence the capture efficiency, growth and develop- ment of fish larvae Conover et al.

In the Black Sea, sprat recruitment is related to the strength of western winds dur- ing November-December and January-March. Prodanov et al. The upwelled waters are rich in nutrients and organic matter, and contribute much to productivity in the Black Sea. The effects of this recent climate shift can be observed in marine populations. An increase in the biomass of jellyfish that may be related to climate changes has been reported for the western Bering Sea in the early s.

Since these jellyfish increased in the same period as the M. The continental shelf of the eastern Bering Sea is the second largest in the world, and provides rich stock of walleye pollock Gadidae. Since the beginning of the s it increased dramatically and averaged over The rapid increase in jellyfish biomass followed the decline of age 1 pollock and other forage fishes in each region of the SE Bering Sea after 3 to 7 yr Fig.

Figure 8. Bering Sea: Biomass metric tons of jellyfish collected in the total national marine fisheries service NMFS sampling area in and from to on the eastern Bering Sea shelf. Bering Sea: Forage fish and jellyfish biomass both 3 year running mean based on summer bottom trawl surveys on eastern Bering Sea shelf from to Brodeur et al.

Chrysaora melanaster can be an important consumer and may deplete the zooplankton standing stocks on a local scale. Therefore, an abundance of C. The inverse relationship between the biomass of forage fishes and jellyfishes suggests the possibility of a competitive interaction. Once established, jellyfishes can apparently outcompete fish populations because many jellyfish have higher consumption rates, respond more rapidly to pulses of food than their competitors, and have the potential to prey upon the early life stages of many fishes Purcell et al.

Brodeur, et al. Whether this increase in biomass of gelatinous zooplankton is a consequence of human intervention, perhaps related to overfishing or is a result of changes in the physi- cal regime, is unclear at this time.

The walleye pol- lock fishery removes millions of tonnes of production from the eastern Bering Sea each year and these removals have likely affected the pelagic ecosystem to some undeter- mined extent.

The increase in jellyfishes may have resulted from a release from competi- tion with Age 1 pollock, juvenile herring Clupea pallasi, and capelin Mallotus villosus for zooplankton resources.

Jellyfish, with their rapid growth rates and turnover times, are highly opportunistic and can easily become a dominant component of perturbed pelagic ecosystems Mills, The increased biomass of medusae in the Bering Sea coincides with changes in the general circulation of the atmosphere, which helps determine sea surface temperature SST and annual extent of sea ice. This index has a north-south dipole in pressure, with higher pressure over the Bering Sea and lower pressure south of the Aleutian Islands in its positive phase, and the opposite pattern i.

A shift toward more years with positive values of the NP red after the late s, implied reduced cloud cover and increased solar radiation at the sea surface. Years with positive values of the NP tend to correspond to years with positive summer SST anoma- lies, including longer ice coverage. Over the north-west Middle shelf, ice persisted from 0.

Figure A positive value corresponds to higher heights over the Bering Sea and lower heights for the region south of the Aleutian Islands Brodeur et al. Winds, mixing the water column, hamper stratification, and thus the phytoplankton sinks to a deeper, unproductive region. The greater ice extent over the SE Bering Sea persisting to April in the years may have led to a more stable and productive surface layer following the spring ice retreat Hunt et al.

Due to the melting ice, the salinity of the surface water decreases and the stratification of the water column increases, as more as the surface water becomes warmer do to the increas- ing air temperature. The stability of the surface water column inhibits the sinking of the phytoplankton below the unproductive layer, thus enhancing primary production.

The bloom associated with sea ice can account for a large fraction of the total annual phyto- plankton production. A good phytoplankton production enhances the mesozooplankton production, leading to a good food resource for the developing jellyfish. Alternation of the plankton composition by jellyfish blooms In the Bering Sea, another event was observed that may be put to a certain extent in relation to the jellyfish increase.

It was obvious as well in the Black Sea. Coccolithophores are a unicellular phytopankton that forms part of the nano- plankton. Characteristic is an external shell composed of calcareous plates. Blooms of coccolithophores Emiliana huxleyi , with a biomass 1. Whether these extraordinary coccolithophoride blooms can be put into relation to the increase of mesozooplanktivorous jelly organisms or to changes in the hydrological structure of the water column should be carefully investigated.

These authors studied the impacts of Aurelia aurita blooms to the mesozooplankton in the Baltic Sea in different years between Similarities in their seasonal and annual distribution, growth, food demand and effects to the mesozooplankton are obvious in both seas.

Like the Black Sea, the Baltic Sea is an enclosed sea with similar hydrography. In both seas the dominant mesozooplankton species are largely identical. Total zooplankton numbers, i. Copepod species, which are shared with the Black Sea, as the genus Pseudocalanus, Paracalanus and the species Oithona similis, and the appendicularian Oikopleura dioica were rather affected by increasing abundance of medusae, whereas the copepods Centropages hamatus and the Acartia spp.

Phytoplankton concentration in the photic zone of the western deep part of the Black Sea during The phytoplankton blooms consisted mainly of coccolithophorids. Years without bars: no measurements. Thus, in years with low abundance of A. The abundance of the highly productive Acartia. Species able to compensate for losses by reproduction, were not reduced by predation of medusae.

Pseudocalanus minutus elon- gatus develops and reproduces in late spring. This period coincides with the main season of A. Consequently, the spring peak of the copepod is suppressed in bloom years of the medusa.

The spawning of 0. Predation by abundant medusae on adults and developmental stages of this copepod can, therefore, hinder population build-up during summer. Both Acartia spp. Nevertheless, their reproduction will, perhaps, be slightly affected by Aurelia predation. The larval stages of bivalves did not show a trend with increasing population densities of A. The different response of mesozooplankton to varying abundances of medusae could have the following consequences for the zooplankton community: high abundance of medusae can modify zooplankton composition and lead finally to a modified trophic structure.

The dominant copepods mentioned above represent three different feeding types: Pseudocalanus minutus elongatus and Paracalanus parvus are fine-filter feeders, the Acartia species and Centropages hamatus are coarse-filter feeders or omnivores, whereas Oithona similis is a raptorial predator which also needs plant material.

An abun- dance of Aurelia caused reduced numbers of Pesudocalanus, Paracalanus, 0. These general findings in the Baltic Sea were observed as well in the Black Sea after the mass invasion of M. After the Mnemiopsis leidyi-invasion, a strong decline of mesozooplankton including Acartia clausi and the appendicularian Oikopleura was obvious all over the Black Sea Purcell et al.

Badly affected were the same spe- cies as in the Baltic Sea, namely Pesudocalanus, Paracalanus and 0ithona similis. Like in the Baltic Sea, Acartia clausi became the dominant species of the copepod community Shiganova et al. Thus, heavy blooms of gelatinous macrozooplankton have more far-reaching consequences than the simple reduction of zooplankton prey alone. Conclusion Around the end of the s - beginning of the s, the Black Sea ecosystem under- went major changes: a decrease in mesozooplankton stock, severe changes in zooplank- ton composition, an extraordinary bloom of the introduced ctenophore Mnemiopsis leidyi, and the collapse of its anchovy stock.

The root causes of these changes are not easy to identify. It seems that a combination of factors triggered them. Anthropogenic activities like pollution and eutrophication, overfishing and the accidental introduction of M. It is possible that the regime shift, of which effects on hydrology and organisms were documented for the North Atlantic and North Pacific region, affected the ecosystem of the Black Sea as well.

Hydrologic changes especially an increase in water temperature , which influenced the primary production, were registered in the Black Sea too. These changes should have an impact the secondary producers and on fish larvae, due to changes in the available food composition.

It may be assumed that M. In the Black Sea, the impact of the regime shift on the second trophic level is dif- ficult to prove, since overfishing and the voracious predation of Mnemiopsis leidyi had an impact on the mesozooplankton too. The removal of biomass of anchovy since mid s may have presented the developing ctenophore with a good food resource, and so it started to deplete the zooplankton.

Since , in line with the changing hydrology of the Black Sea, the situation improved: the M. Similar effects of extraordinary jellyfish and ctenophore blooms in the Baltic Sea and in the Black Sea were obvious: a high abundance of medusae caused a decrease in mesozooplankton and ichthyoplankton, coupled with major changes in the zooplankton community.

Opportunistic copepod species like Acartia spp. The changes of the dominant mesozooplankton species finally led to modified trophic struc- ture, resulting in blooms of nanoplankton coccolithophores Emiliana huxleyi. Blooms of this species where observed in the Black and Bering Seas together with large assem- blages of ctenophores and medusae, respectively.

This may implicate that the number of trophic levels increases due to the grazing of the gelatinous plankton. The sudden collapse of the anchovy fishery in the Black Sea during is in line with the life patterns of small pelagics, which display strong fluctuation in abundance as seen in the Mediterranean and in other regions of the world. A sudden collapse of a fish stock in a whole ecosystem as large as the Black Sea due to a bloom of ctenophores or jellyfish had to date not been reported from any other sea in the world except the Mnemiopsis invasion into the Caspian Sea which appeared to coincide with the collapse of the kilka fishery; Shiganova et al.

The impact of jellyfish and ctenophores on fin fish as previously documented was, as a rule, restricted to smaller areas. In conclu- sion, it is more likely that the collapse of the Black Sea anchovy, including the decrease of the zooplankton, was not a mere consequence of the Mnemiopsis invasion, but as well of overfishing and a shift in the oceanographic and meteorological regime at the end of the s.

References Behrends G. Schneider, Impact of Aurelia aurita medusae Cnidaria, Scyphozoa on the stand- ing stock and community composition of mesozooplankton in Kiel Bight western Baltic Sea. Marine Ecology Progress Series Bodeanu, N. Brodeur, R. Mills, J. Overland, G. Schumacher, Evidence for a substantial increase in gelatinous zooplankton in the Bering Sea, with possible links to climate change.

Fisheries and Oceanography 8: Hunt Jr, Increases in jellyfish biomass in the Bering Sea: implications for the ecosystem. Brusca, R. Sinauer Associates, USA: pp. Burrell, V. Van Engel, Predation by and distribution of a ctenophore, Mnemiopsis leidyi A. Agassiz, in the York River estuary. Estuarine and Coastal Marine Sciences 4: Caddy J. Griffiths Studies and reviews. General Fisheries Council for the Mediterranean No Rome, FAO, 71 pp. Conover, R.

Wilson, G. Vass, Climate, copepods and cods: some thought on the long-range prospects for a sustainable northern cod fishery. Climate Research 5: Corten, A. Variation in the abundance of the southern fish species in the southern North Sea in relation to hydrography and wind. Cowan, Jr. Houde, Relative predation potentials of scyphomedusae, ctenophores and planktivorous fish on ichthyoplankton in Chesapeake Bay.

Dickson, R. Turrel, The NAO: the dominant atmospheric process affecting oceanic variability in home, middle and distant waters of European Salmon. In Mills, D.

Dunn, M. Reid, in prep. Relationships between the environment and the fisheries for red mullet, Mullus surmuletus Linne , in the North Sea. Edwards, M. Planque, Fromentin, J. Calanus and environment in the eastern North Atlantic. Influence of the North Atlantic Oscillation on C. Gomoiu, M. Ecological observations on the jellyfish Aurelia aurita L. Gordina, A. Niermann, A. Kideys, A. Subbotin, Y. Artyomov, State of ichtyoplankton of the Black Sea and features of its distribution depending on dynamics of waters.

Ecosystem modeling as a management tool for the Black Sea, Vol. Goubanova, A. Prusova, U. Niermann, N. Polikarpov, Dramatic change in the copepod community in Sevastopol Bay Black Sea during two decades Senckenbergiana maritima Role of fishing in the Black Sea ecosystem, in: E. Ozsoy and A. Can overfishing be responsible for the successful establishment of Mnemiopsis leidyi in the Black Sea? Estuarine, Coastal and Shelf Science Oguz, Modeling trophic interrelationships in the Black Sea.

In: Ivanov L. Oguz eds , Ecosystem modelling as a management tool for the Black Sea. Kluwer Academic Publishers. Hare S. Mantua, Empirical indicators for North Pacific regime shifts in and Progress in Oceanography Hare, S. Wooster, The nature and impacts of North Pacific climate regime shifts. Hunt G. L Jr, P. Stabeno, G. Walters, E. Sinclair, R. Brodeur, J. Napp, N. Bond, Climate change and control of the southeastern Bering Sea pelagic ecosystem. Deep-Sea Research II in press.

Hunter, J. Alheit, Kamburska L. Moncheva, A. Konsulov, A. Prodanov, in press. The Invasion of Beroe ovata in the Black Sea. Why a Warning for Ecosystem Concern? Mediterranean Marine Science, Vol. Kideys, E. A, Fall and rise of the Black Sea ecosystem. Science Kideys A. Romanova, Distribution of gelatinous macrozooplankton in the southern Black Sea during Marine Biology Gordina, U. Bingel, The effect of environmental conditions on the distribution of eggs and larvae of anchovy Engraulis encrasicolus L.

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