Zooplankton of the open Baltic: Extended Atlas - IOW

Zooplankton of the open Baltic: Extended Atlas - IOW Zooplankton of the open Baltic: Extended Atlas - IOW

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Several investigators observed that ciliate abundance in the water column was positively correlated with the chlorophyll a concentration that increased with productivity and eutrophication (Arndt, 1991; Garstecki et al., 2000; Samuelsson et al., 2006). As it was shown for different parts of the Baltic Sea, large ciliates would increased in numbers with increasing primary production, while the bacterial production would govern the dynamics of small ciliates (Witek, 1998; Johansson et al., 2004; Samuelsson et al., 2006). Seasonal succession of ciliate community from large predatory ciliates in spring to small microphagous and epibiotic ciliates in summer is typical and was revealed for the northern (Johansson et al., 2004; Samuelsson et al., 2006), southern (Witek, 1998) and western Baltic Sea (Smetacek, 1981). Even though the growth rate of ciliates in summer seemed to be mainly limited by the amount of the resources in a coastal area, the biomass of ciliates in the northern Baltic Sea was found to be strongly affected by predation of mesozooplankton. Studies in the Baltic Proper suggest that the ciliate biomass is top-down predation-controlled, while the production may be bottom-up limited by the resources (Samuelsson et al., 2006). Role in zooplankton communities Analyses of the results of various recent studies in the pelagic regions of the Baltic Sea revealed that the protozoan biomass had been in the same range or even higher than mesozooplankton biomass (Arndt, 1991). For example, in the south-western Gdańsk Basin the heterotrophic ciliate community contributed 10 to 13% to the mean annual zooplankton biomass (Witek, 1998). In the Neva Bay, nearly 16% of the total destruction of organic matter accounted for planktonic ciliates (Khlebovich, 1987). Interestingly, it exceeded the joint decomposition of organic substances by rotifers, cladocerans and copepods (10%). Daily average ciliate production was 0.25 mg/l or 50 mg C/m 2 per day. It formed nearly 19% of primary production of phytoplankton and about 30% of bacterial production (Khlebovich, 1987). In the Gdańsk Basin, carbon demand of non-predatory ciliates calculated according to their potential production was estimated to be equivalent to 12- 15% of the gross primary production (Witek, 1998). Some unresolved research problems in ecology of Baltic ciliates During the last decades many researches have been involved in the study of functions and role of ciliates in the Baltic pelagic ecosystems. Thus, major interest has been centered around the structure of microbial loop. Several studies were devoted to experimental investigation of nutrition of Baltic ciliates and mainly concerned with their role as predators (Kivi & Setala, 1995; Aberle et al., 2007; Moorthi et al., 2008). In particular, these investigations deal with food spectrum, herbivore selectivity and grazing 40

impact of some common Baltic planktonic ciliates. In addition, there are some studies of trophic interactions between different levels of the Baltic Sea ecosystems which provide information about abundance and productivity of phytoplankton, microzooplankton including ciliates, and mesozooplankton (Uitto et al., 1997; Johansson et al., 2004). This ecosystem approach presents a picture of complex relationships within microbial community and opens wide range of unresolved research problems in ecology of ciliates. For example, our knowledge about functioning of microbial loop is rather schematic yet, and it is not clear enough how it changes spatially and temporally. Several other investigations provide information on the role of ciliates in food webs within poorly-studied anoxic enviroments of the Baltic Sea, with emphasis on microbial loop structure (Setala, 1991; Detmer et al., 1993). One more widely discussed question of ecology of Baltic ciliates is their contribution to the diet of different mesozooplankton species (Tiselius, 1989; Schmidt et al., 2002). It is necessary to mention that our knowledge concerning the diversity, abundance and distribution of larger ciliates is more complete than that of smaller species, whereas particularly nanociliates (

impact <strong>of</strong> some common <strong>Baltic</strong> planktonic ciliates. In addition, <strong>the</strong>re are some<br />

studies <strong>of</strong> trophic interactions between different levels <strong>of</strong> <strong>the</strong> <strong>Baltic</strong> Sea<br />

ecosystems which provide information about abundance and productivity <strong>of</strong><br />

phytoplankton, microzooplankton including ciliates, and mesozooplankton<br />

(Uitto et al., 1997; Johansson et al., 2004). This ecosystem approach presents<br />

a picture <strong>of</strong> complex relationships within microbial community and <strong>open</strong>s<br />

wide range <strong>of</strong> unresolved research problems in ecology <strong>of</strong> ciliates. For<br />

example, our knowledge about functioning <strong>of</strong> microbial loop is ra<strong>the</strong>r<br />

schematic yet, and it is not clear enough how it changes spatially and<br />

temporally. Several o<strong>the</strong>r investigations provide information on <strong>the</strong> role <strong>of</strong><br />

ciliates in food webs within poorly-studied anoxic enviroments <strong>of</strong> <strong>the</strong> <strong>Baltic</strong><br />

Sea, with emphasis on microbial loop structure (Setala, 1991; Detmer et al.,<br />

1993). One more widely discussed question <strong>of</strong> ecology <strong>of</strong> <strong>Baltic</strong> ciliates is<br />

<strong>the</strong>ir contribution to <strong>the</strong> diet <strong>of</strong> different mesozooplankton species (Tiselius,<br />

1989; Schmidt et al., 2002).<br />

It is necessary to mention that our knowledge concerning <strong>the</strong> diversity,<br />

abundance and distribution <strong>of</strong> larger ciliates is more complete than that <strong>of</strong><br />

smaller species, whereas particularly nanociliates (

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