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    SEASONAL AND INTER-ANNUAL VARIABILITY OF MESOZOOPLANKTON BIOMASS IN THE NORTHERN ADRIATIC SEA (GULF OF TRIESTE).

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    This paper reports the rate of change of mesozooplankton biomass on seasonal, inter-annual and decadal time scale in the Gulf of Trieste (NE Mediterranean, Northern Adriatic). We measured variability in mesozooplankton dry weight (mg DW m−3), organic carbon and nitrogen contents of the DW in relation to mesozooplankton taxonomic structure and some environmental parameters. The study is based on data obtained from mesozooplankton samples collected monthly by a vertical WP2 net (200 μm) from January 1986 to September 2005 at one monitoring station, a coastal site in the Gulf of Trieste. We considered mesozooplankton DW in relation to copepods, phytoplankton taxonomic structure, water temperature and North Atlantic Oscillation. For further analyses we counted also on data for DW for the period 1972–1980, monthly data for organic carbon (mg C m−3) and nitrogen contents (mg N m−3) of the DW for the period 1991–2005, determined by a CHN Elemental Analyzer.We explored statistically our high temporal resolution time series data picking out the main features: seasonal components and trends. Mesozooplankton DW ranged from only 1 mg m−3 (January 1977) to 95 mg m−3 (March 1990) in the coastal ecosystem of the Northern Adriatic during the period 1972–2005. The annual cycle of the DW was found to be bimodal with maximum in late winter–spring and a weaker one in late summer. Maximum DW were regularly recorded when Copepods prevailed the mesozooplankton community structure. Similarly, high organic carbon and nitrogen contents were detected when copepods dominated, although wide-ranging on a seasonal scale. Irregular intra- and inter-annual fluctuations were typical mostly during the 1990s. Mesozooplankton DW sharply shifted since 2001–2002 to the level exceeding the observed one during the regime of the 1980s. Our results indicate substantial changes in the seasonal timing of mesozooplankton DW, which together with decadal inter-annual fluctuations match significantly with shifts in copepods, phytoplankton taxonomic structure, temperature and NAO index. The discussed zooplankton descriptors (DW, C and N contents and C:N ratio) being to a certain degree predictive of phyto- and mesozooplankton composition, in essence might foretell the phenological response of plankton communities to environmental changes in the coastal ecosystem, including climate change

    Long-Term Copepod Dynamic in the Gulf of Trieste (Northern Adriatic Sea). Recent Changes and Trends

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    Cluster and time series analyses were applied to a 1970–1999 data set of zooplankton collected from the Gulf of Trieste (Northern Adriatic Sea). Two time periods were compared: 1970–1980 and 1986–1999. Associations of copepod species were identified and an attempt was made to reveal their long-term dynamics and significant patterns over the study period. Two main groups with 2 and 3 subgroups each were identified. We observed a seasonal alternation of the 2 main groups, albeit with remarkably different patterns during the 2 periods. Time-series analyses suggested recent changes in the periodicity of the associations. The long-term annual mean copepod abundance showed an increase in the late 1990s in comparison to the 1970s; however, this increase was not constant. Small-sized copepods increased in the second period, indicative of changes in the phytoplankton size spectrum. Shifts in the 1990s appeared to be related to climate change in the Northern Hemisphere that appeared abruptly after 1987. Climate change is thus recognized as the most important factor (more so than anthropogenic change) affecting inter-annual and inter-decadal variability of plankton dynamics. The strong signal recorded in the zooplankton community seems to reflect this, identifying the Gulf of Trieste as one of the most sensitive areas in the Mediterranean
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