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Zooplankton of the open Baltic: Extended Atlas - IOW

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2. GENERAL CHARACTERISTICS OF ZOOPLANKTON OF<br />

THE BALTIC SEA<br />

<strong>Zooplankton</strong> organisms range in size from few micrometers to meters.<br />

Mesozooplankton (0.2 – 20 mm) is <strong>the</strong> dominating group in <strong>the</strong> <strong>Baltic</strong> Sea in<br />

terms <strong>of</strong> biomass. It may constitute 76% (i.e. >1000 kg C/m²) <strong>of</strong> <strong>the</strong> average<br />

annual carbon mass, as it was measured in <strong>the</strong> western Gdańsk Bay during <strong>the</strong><br />

1980-s (Witek, 1995). The remaining 18 and 6% were contributions <strong>of</strong><br />

protozoans and macrozooplankton, respectively. The percentage <strong>of</strong> <strong>the</strong><br />

average annual production <strong>of</strong> mesozooplankton was 39%. Within <strong>the</strong><br />

mesozooplankton fraction, copepods Pseudocalanus spp., Temora<br />

longicornis 1 , Acartia spp., rotifers Synchaeta spp., and cladoceran Evadne<br />

nordmanni are <strong>the</strong> most important taxa in both, biomass and production. The<br />

ctenophore Pleurobrachia pileus, <strong>the</strong> copepod Eurytemora affinis and rotifers<br />

Keratella spp. played a minor role, while <strong>the</strong> appendicularian Fritillaria<br />

borealis, Polychaeta larvae, <strong>the</strong> cladocerans Bosmina spp., Podon spp., <strong>the</strong><br />

copepod Centropages hamatus, and Bivalvia larvae ranged in between (Fig.<br />

2.1).<br />

There are about forty mesozooplankton species that are regularly<br />

occurring in <strong>the</strong> <strong>Baltic</strong> Sea in significantly high abundances (Ackefors, 1981).<br />

Ten to twelve <strong>of</strong> <strong>the</strong>m are dominating taxa. Their spatial occurrence is mainly<br />

explained by <strong>the</strong> salinity patterns. According to hydrographic regime with<br />

prevailing outflow <strong>of</strong> low saline water in <strong>the</strong> upper layer and temporary<br />

inflow <strong>of</strong> higher saline water below <strong>the</strong> halocline, species <strong>of</strong> relevant salinity<br />

preferences inhabit <strong>the</strong> western and <strong>the</strong> eastern parts and <strong>the</strong> <strong>open</strong> <strong>Baltic</strong> Sea,<br />

respectively.<br />

Behrends et al. (1990) described presence <strong>of</strong> <strong>the</strong> dominant taxa in <strong>the</strong><br />

<strong>Baltic</strong> Sea regions from Kattegat to <strong>the</strong> Gulf <strong>of</strong> Finland and <strong>the</strong> Bay <strong>of</strong><br />

Bothnia, accordingly, in a semi-quantitative way. After conversion <strong>of</strong> this<br />

information into numbers, <strong>the</strong> changing occurrence, amount and rank <strong>of</strong><br />

various taxa from west to nor<strong>the</strong>ast became visible (Table 2.1). Generally, <strong>the</strong><br />

amount <strong>of</strong> species is larger in <strong>the</strong> transition to <strong>the</strong> marine or <strong>the</strong> limnetic<br />

environment than in <strong>the</strong> <strong>Baltic</strong> Proper (Remane & Schlieper, 1971).<br />

1 Authors <strong>of</strong> <strong>the</strong> Latin species names are mentioned in <strong>the</strong> zooplankton checklists (Tables<br />

4.2.1 and 5.2.1).<br />

15

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