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Aim. For the first time, flow cytometry has been used to study the structure and functional characteristics of bacterio‐, pico‐ and nano‐ phytoplankton in the Middle Caspian during the bloom period in early September 2022.Water samples were taken at different horizons (from the surface to the bottom layer) at a series of stations along the western coast of the Caspian Sea on the border between its northern and central parts to quantitatively assess heterotrophic bacterioplankton, picophyto‐ and nanophy‐ toplankton. Sampling was undertaken in early September 2022 under summer hydrological conditions with water surface temperatures ranging from 24.7°C to 26.7°C. Sample analysis was performed using flow cytometry.Extremely high concentrations of picophytoplankton (up to 1.8×105 cells/mL), probably of Synechococcus picocyanobacteria, were detected off the northwestern coast of the Middle Caspian. Very high values of nanophytoplankton abundance (up to 1.6×105 cells/mL), dominated by small flagellates, were also found. A clear spatial uncoupling of pico‐ and nanophytoplankton was revealed. Maximum levels of nanophytoplankton were confined to the area of intensive phytoplankton blooming with high concentrations of chlorophyll a, while picophytoplankton reached peak abundance further south, outside this area. The influence of the thermocline on the vertical structure of microbial communities was detected. The concentrations of picophytoplankton and the proportion of physiologically active HNA‐bacteria decreased sharply under the thermocline.The results obtained indicate the leading role of the smallest phototrophs in the Caspian pelagial and emphasise the need for further comprehensive studies of Caspian microbial communities using modern methods.
Aim. For the first time, flow cytometry has been used to study the structure and functional characteristics of bacterio‐, pico‐ and nano‐ phytoplankton in the Middle Caspian during the bloom period in early September 2022.Water samples were taken at different horizons (from the surface to the bottom layer) at a series of stations along the western coast of the Caspian Sea on the border between its northern and central parts to quantitatively assess heterotrophic bacterioplankton, picophyto‐ and nanophy‐ toplankton. Sampling was undertaken in early September 2022 under summer hydrological conditions with water surface temperatures ranging from 24.7°C to 26.7°C. Sample analysis was performed using flow cytometry.Extremely high concentrations of picophytoplankton (up to 1.8×105 cells/mL), probably of Synechococcus picocyanobacteria, were detected off the northwestern coast of the Middle Caspian. Very high values of nanophytoplankton abundance (up to 1.6×105 cells/mL), dominated by small flagellates, were also found. A clear spatial uncoupling of pico‐ and nanophytoplankton was revealed. Maximum levels of nanophytoplankton were confined to the area of intensive phytoplankton blooming with high concentrations of chlorophyll a, while picophytoplankton reached peak abundance further south, outside this area. The influence of the thermocline on the vertical structure of microbial communities was detected. The concentrations of picophytoplankton and the proportion of physiologically active HNA‐bacteria decreased sharply under the thermocline.The results obtained indicate the leading role of the smallest phototrophs in the Caspian pelagial and emphasise the need for further comprehensive studies of Caspian microbial communities using modern methods.
Field sampling for this research was conducted in the Southern Caspian Sea with careful planning to ensure broad spatial coverage and high-quality data collection. Sampling stations along each transect were spaced 4 km apart, with adjacent transects separated by 10 km. Six research cruises in the summer of 2011 under varying environmental conditions provided a representative dataset of the marine ecosystem. Key bio-optical components, including Colored Dissolved Organic Matter (CDOM) absorption, Chlorophyll-a concentration (Chl-a), and turbidity, were analyzed. CTD sensors (Idronaut OCEAN SEVEN 316) were used to measure physico-chemical parameters such as salinity, temperature, and dissolved oxygen, while surface water samples were collected for laboratory analysis. CDOM absorption was measured using the PERKIN ELMER Lambda 25 spectrophotometer, and the data were fitted with an exponential function to calculate parameters like the spectral slope (S) and aCDOM(375). In situ Chl-a measurements were taken with the Seapoint Chlorophyll Fluorometer, and water turbidity was assessed with the Seapoint Turbidity Meter. Higher values of aCDOM(375) (ranging from 0.38–3.52 m⁻¹) were observed at nearshore stations, indicating significant freshwater influence. Linear regression analysis showed a weak inverse relationship between aCDOM(375) and salinity (r = -0.08; R² = 0.007), suggesting minimal salinity impact on CDOM variability. The match-up analysis revealed that turbidity and dissolved organic matter products tended to underestimate values, while chlorophyll was overestimated using satellite data. The lowest mean absolute error was found for CDOM (0.84). The spatial variability of bio-optical components highlights the influence of freshwater inputs and nearshore processes. The weak correlation with salinity suggests that other factors, such as terrestrial inputs and biological activity, may affect CDOM variations in the region.
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