190
O. Sidoti et al
dominant that it characterizes the zooplankton
community. In winter, a persistent unstable
frontal system, caused by wide fluctuations of
meteo-marine conditions, prevents a clear differentiation of the mean percentage species composition between the two sub-systems.
From our analysis of the spatial distribution
of the most representative zooplankton groups,
we formulated a preliminary trophic model concerning the association of ecologically similar
species occupying the same habitat. In the
coastal zone of the neritic system. the zooplankton biocoenosis is characterized by the dominance of the fine mter feeders. e.g. tunicates
(Oikapleura, Salpa and Dolialum) and cladocerans (P. avirostris, E. spinifera and E. tergestina)
which feed on nanoplankton (Fonda Umani et
al. 1992), and mixtivorous copepods (A. clausi
and P. parvus) able to feed on nano-, microzooplankton and particulate organic matter. In the
offshore zone, in addition to the above-mentioned species but with less abundance, we
found both herbivorous copepods, e.g.
Ctenocalanus vanus and Clausocalanus Jurcatus
which mainly feed on diatoms, and carnivorous
species, e.g. Oithona similis, O. plumifera and
Centro pages typicus (Fonda Umani et al. 1992).
Close to the bottom, the zooplankton population
is characterized by herbivorous species andlor
omnivorous ones, e.g. Pseudocalanus elongatus,
Temora langicornis and Calanus helgolandicus
which generally feed on diatoms, together with
typical carnivorous species of the genera
Corycaeus, Oncaea and Podan. The predator
group, formed by chaetognaths. siphonophores
and medusas, occurs all along the water column,
but is more abundant in the layer under the pycnocline.
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