A long term (1988-2018) data set of phytoplankton and physico-chemical parameters was analyzed for the firsttime in an offshore station of the LTER Senigallia-Susak transect (northern Adriatic Sea) not directly affected bythe coastal nutrient input. The mean annual cycle of phytoplankton markedly differed from that observed in thecoastal areas, showing the maximum in June and the minimum in November. The main component of phytoplanktoncommunity was represented by phytoflagellates, whose trend paralleled that of total phytoplankton.On average, diatoms peaked in July, dinoflagellates in June and coccolithophores in April. The phytoplanktonmaximum in summer is explained mainly by the allochthonous input of DIN and PO4 carried by the low salinitywaters expanding eastward, during the stratification of water column. Resuspension processes seem to be less effectivefor PO4 than for DIN. The most representative phytoplankton taxa for each season as indicated by the Ind-Val analysis were identified and were only in part similar to those observed in the coastal area. The interannualanomaly trend showed a significant increase of temperature, DIN and phosphates. Although no significantchanges were found for the total phytoplankton, a reduction of winter dinoflagellate and coccolithophore abundanceswas observed.

Phytoplankton and environmental drivers at a long-term offshore station in the northern Adriatic Sea (1988-2018)

Alessandra Campanelli;Mauro Marini;Federica Grilli;
2022

Abstract

A long term (1988-2018) data set of phytoplankton and physico-chemical parameters was analyzed for the firsttime in an offshore station of the LTER Senigallia-Susak transect (northern Adriatic Sea) not directly affected bythe coastal nutrient input. The mean annual cycle of phytoplankton markedly differed from that observed in thecoastal areas, showing the maximum in June and the minimum in November. The main component of phytoplanktoncommunity was represented by phytoflagellates, whose trend paralleled that of total phytoplankton.On average, diatoms peaked in July, dinoflagellates in June and coccolithophores in April. The phytoplanktonmaximum in summer is explained mainly by the allochthonous input of DIN and PO4 carried by the low salinitywaters expanding eastward, during the stratification of water column. Resuspension processes seem to be less effectivefor PO4 than for DIN. The most representative phytoplankton taxa for each season as indicated by the Ind-Val analysis were identified and were only in part similar to those observed in the coastal area. The interannualanomaly trend showed a significant increase of temperature, DIN and phosphates. Although no significantchanges were found for the total phytoplankton, a reduction of winter dinoflagellate and coccolithophore abundanceswas observed.
2022
Istituto per le Risorse Biologiche e le Biotecnologie Marine - IRBIM
PhytoplanktonInterannual variability
LTER-Long-term ecosystem research
Biological oceanography
Biodiversity
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/444474
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