Seasonal and vertical distribution of planktonic bacteria and heterotrophic nanoflagellates in the middle Adriatic Sea
© Springer-Verlag and AWI 2004
Received: 17 July 2003
Accepted: 21 January 2004
Published: 27 February 2004
Temporal and spatial patterns of bacteria and heterotrophic nanoflagellates (HNF) were studied monthly from January 1997 to December 1998 in the middle Adriatic Sea. Bacterial and HNF relationships with phytoplankton biomass and temperature were analyzed to examine how the relative importance of bottom-up and top-down factors may shift over seasons and locations. For the coastal area, an inconsistent relationship between bacterial abundance and chlorophyll a and a stronger relationship between bacterial abundance and bacterial production suggest that other substrates than those of phytoplankton origin are important for bacteria. The analysis of simultaneous effects of temperature and bacterial production on bacterial abundance showed that the effect of temperature obscured the effects of bacterial production, suggesting that bacterial growth itself is highly temperature-dependent. The relationship between HNF abundance and bacterial abundance was slightly improved by the inclusion of in situ temperature, bacterial production or both parameters, as additional independent variables. About 60% of the variability in HNF abundance can be explained by bacterial abundance, bacterial production and temperature. In the open sea, tight coupling of bacterial abundance with chlorophyll a concentrations implied that phytoplankton-derived substrates have a dominant role in controlling bacterial abundance. During the colder months, bacterial abundance was high enough to support higher HNF abundance than observed, suggesting that predation exerted a minor depressing influence on bacterial abundance during that period. During the spring-summer period, HNF controlled bacterial standing stocks by direct cropping of bacterial production.
KeywordsBacteria Heterotrophic nanoflagellates Seasonal distribution Temperature Adriatic Sea
The distribution and dynamics of microbial organisms are the result of complex interactions between environmental variables and interspecific relationships. Previous studies have provided considerable empirical evidence that resource availability, predation, viral lysis and temperature affect the components of the microbial food web (Cole et al. 1988; Currie 1990; Sanders et al. 1992; Shiah and Ducklow 1994; Azam 1998; Ducklow 1999). Bacterioplankton growth is positively correlated with temperature up to a certain threshold (Hoch and Kirchman 1993; Shiah et al. 1999, 2003), above which other controlling processes occur (Ducklow 1992; Shiah et al. 1999, 2000, 2003). The relative importance of resources derived from phytoplankton was shown to be higher in the oligotrophic open sea than in coastal and estuarine areas, where allochtonous inputs of organic matter present the dominant source of substrates for microorganisms. Heterotrophic nanoflagellates (HNF) have been identified as a major source of bacterial mortality in aquatic ecosystems (Sherr and Sherr 1994, 2001; Šolić and Krstulović 1994; Christaki et al. 2001), but predation pressure was found to be dependent on temperature and the trophic state of the studied area (Shiah and Ducklow 1994; Vaque et al. 1994; Krstulović et al. 1997; Šolić et al. 1998, 2001; Gurung et al. 2000). The effects of these factors are not always clear, as they can act simultaneously, changing their relative importance over space and time.
The aim of this study was to gain a better understanding of temporal (seasonal) and spatial (vertical; coastal sea vs. open sea) patterns of bacterial and HNF abundances. Bacterial and HNF distribution were analyzed in relation to phytoplankton biomass and temperature in order to examine how the relative importance of bottom-up and top-down factors may shift over seasons and locations.
This study was conducted at one coastal station (Kaštela Bay) and one station located in the open sea of the middle Adriatic (Island of Vis).
The coastal station (Station A) was located in an enclosed, shallow basin, Kaštela Bay (43°31′N; 16°22′E). The bay, with a surface area of 61 km2 and an average depth of 23 m, communicates with the adjacent channel through an inlet that is 1.8 km wide and 40 m deep. The river Jadro, which discharges into the eastern part of the Bay, is the most important freshwater source (average annual inflow of 10 m3 s−1). Its waters are characterized by a very high nitrogen to phosphorus (N/P) ratio. This part of the Bay also receives domestic and industrial sewage. Water circulation and exchange with the open sea is generated mostly by the local wind, which is related to the passage of mid-latitude cyclones over the area (Gačić 1989). Cyclones are more frequent during the winter, and therefore water circulation and exchange with the open sea are more intense during that period of the year. The strong terrestrial influence results in wide oscillations of chemical and physical parameters (Zore-Armanda 1980).
The open sea station (Station B) was located 4 km southeast of Cape Stončica on Vis Island (43°00′N; 16°20′E) where water depth is about 100 m. Because of its distance from the mainland (50 km), oscillations of all hydrographic parameters are smaller than in the coastal waters (Buljan and Zore-Armanda 1979). Fluctuations of thermohaline properties of the surface layers are subject to direct atmospheric conditions, while the fluctuations in deeper layers are more influenced by advection and diffusion (Grbec and Morović 1997). This station is also exposed to advection of Mediterranean waters (Grbec et al. 1998).
Sampling was conducted monthly, from January 1997 to December 1998 at depths of 0, 5, 10, 20 and 35 m at Station A, and 0, 5, 10, 20, 30, 50, 75 and 100 m at Station B. Samples for chlorophyll a (chl a), bacterial and HNF counts were collected using 5 l Niskin bottles, while an STD system was used for the measurement of temperature, salinity and depth.
Phytoplankton biomass was estimated from chl a concentrations using fluorimetric methods (Strickland and Parsons 1972). Bacterial abundance was determined in fixed samples (2% formalin, final concentration) using acridine orange direct counts (Hobbie et al. 1977). At least 300 bacteria per filter were counted under 1,000× magnification using an Olympus epifluorescence microscope. For HNF counts, preserved samples (2% formalin, final concentration) were filtered at low pressure through a 0.8-μm pore size black-stained Millipore filter. The preparations were stained with proflavine (Haas 1982) and phototrophic organisms differentiated by chlorophyll autofluorescence. The samples were counted the same day after preparation, and at least 100 fields per filter were counted.
Bacterial cell production was inferred from DNA synthesis measured as incorporation rate of 3H-thymidine (Fuhrman and Azam 1982). (Methyl-3H)-thymidine was added to 10 ml seawater to a final concentration of 10 nM (specific activity 86 Ci mmol−1, Amersham Ltd, UK). Incubations were run in triplicate, plus a formalin-killed control (final concentration 0.5%), in the dark for 1 h at in situ temperature. Formalin addition (final concentration 0.5%) stopped the incorporation. The fixed samples and the control were passed through a 0.2-μm pore size cellulose nitrate filter and rinsed seven times with 1 ml ice-cold TCA (5% weight/volume). The filters were dried, dissolved in 10 ml Filter-Count (Packard scintillation cocktail) and counted, after 24 h storage, in a scintillation counter (Packard Tricarb 2500). The conversion factors for estimating bacterial cell production were calculated from bacterial cell abundances and 3H-thymidine incorporations in the <1-μm fractions (Riemann et al. 1987) as: CF=(N2−N1)/3Hinc, where N1 and N2 are the abundances at the beginning and at the end of the experiment; 3Hinc is the integrated 3H-thymidine incorporation rate during the experiment.
At Station B, temperature ranged from 13.0°C to 26.1°C. A thermocline developed in July between 20 and 30 m depth, attaining its maximum in August. The stratified conditions remained until September, when a strong mixing occurred. The whole period from November until April was characterized by homothermy. Salinity values fluctuated between 37.60 and 38.78 psu. During the winter months, the water column was characterized by almost uniform salinity values. With the beginning of the spring heating, a halocline started to develop. The highest salinity gradient was recorded during the summer months.
Bacteria and heterotrophic nanoflagellates
At Station A, bacterial abundance varied from 0.44×106 to 2.50×106 cells ml−1, with a mean value of 1.13×106 cells ml−1. During the whole study period, bacteria were most abundant in the surface layers above 20 m depth, and their abundance peaked during summer at 0 and 5 m depth. The greatest variations of bacterial abundances with depth were observed during thermal stratification of the water column.
Bacterial production varied from 2.25 to 45.34 μg C l−1 day−1 (mean value=28.23 μg C l−1 day−1), with maximum values in the surface layers. Below 10 m depth, bacterial production showed little variation, with no clear seasonal patterns.
Simultaneous effects of temperature, chl a and bacterial production on bacterial abundance in the surface layers (0–5 m) of Kaštela Bay. R coefficient of correlation;r p coefficient of partial correlation;a,b coefficients of multiple linear regression (a intercept; b slope;n=24);β (beta coefficient) regression coefficient b stated in terms of its standard deviation;R coefficient of multiple regression; R 2 (%) coefficient of multiple determination, i.e. measure of the proportion (percentage) of variance explained; ** P<0.01; * P<0.05
Simultaneous effects of bacterial abundance, bacterial production and temperature on HNF abundance in the surface layers (0–10 m) of Kaštela Bay. R coefficient of correlation,r p coefficient of partial correlation;a,b coefficients of multiple linear regression (a intercept;b slope;n=36);β (beta coefficient) regression coefficient b stated in terms of its standard deviation;R coefficient of multiple regression; R 2 (%) coefficient of multiple determination, i.e. measure of the proportion (percentage) of variance explained; ** P<0.01; * P<0.05
At Station B (open sea station), bacterial abundance varied from 0.18×106 to 1.04×106 cells ml−1 with a mean value of 0.56×106 cells ml−1. In both years of study, higher bacterial abundances were observed during winter and spring months. The winter peak in 1997 was present above 50 m depth, while the spring maximum was found near the bottom. In 1998, both winter and spring peaks of bacterial abundance were found throughout the water column.
Simultaneous effects of chla and temperature on bacterial abundance in the surface layers (0–20 m), and bacterial production and temperature on heterotrophic nanoflagellates (HNF) in the layers between 20 and 30 m depth at station Stončica.R coefficient of correlation; r p coefficient of partial correlation;a,b coefficients of multiple linear regression (a intercept; b slope; n=36 for bacteria andn=24 for HNF);β (beta coefficient) regression coefficient b stated in terms of its standard deviation;R coefficient of multiple regression; R 2 (%) coefficient of multiple determination, i.e. measure of the proportion (percentage) of variance explained; ** P<0.01; * P<0.05
The observed relationship between bacterial abundance and bacterial production, and a lack of correlation with chl a in the coastal area (Station A), suggest that the input from land is a more important source of substrate than phytoplankton. An uncoupling between bacteria and phytoplankton in coastal areas has been reported to be due to a response to alochtonous inputs at specific times of the year (Kepkay et al. 1993), seasonal changes (Pomeroy et al. 1991), and variations in hydrodynamic conditions (Cho et al. 1994). Since Kaštela Bay receives large quantities of nutrients throughout the year (Barić et al. 1996; Bogner et al. 1998), this location shows conditions in which substrate concentrations are almost always above the saturation level. Therefore, variation in bacterial abundance cannot be explained by variation in substrate concentrations, especially not by variation in substrate of phytoplankton origin.
The analysis of the simultaneous effects of temperature and bacterial production on bacterial abundance (Table 1) showed that the effect of temperature masked the effect of bacterial production. That is, the effect of bacterial production on bacterial abundance failed to occur when temperature stayed constant, suggesting that in Kaštela Bay bacterial growth itself is a highly temperature-dependent seasonal phenomenon (Šolić and Krstulović 1994).
The inconsistent relationship between bacterial abundance and productivity could also suggest a strong influence of mortality factors such as bacteriovory and viral lysis. It seems that, in Kaštela Bay, temperature controlled not only bacterial abundance but also the abundance of bacteriovorous protozoa, which in turn limited bacterial abundance by high grazing pressure. In these conditions, grazing was a factor controlling bacterial abundance, particularly during summer. This is consistent with the results of several other studies which showed that bacteriovory is highly dependent on water temperature, with a maximum in summer (Marrase et al. 1992; Shiah and Ducklow 1994; Vaque et al. 1994; Gurung et al. 2000). A marked increase in bacterial abundance during the warm months, when temperature exceeded 20°C, resulted in an increase of HNF abundance. The weak relationship between bacteria and HNF during colder months could be a result of low grazing pressure on bacteria by HNF as found by Šolić and Krstulović (1994) and Šolić et al. (2001), as well as of high grazing pressure on HNF by ciliates (Weisse et al. 1990) or zooplankton (Jürgens and Güde 1994; Sanders et al. 1994). Šolić et al. (1998) found very high abundances of ciliates in that same period and reported the importance of ciliates as HNF predators during winter. In addition, Bojanić (2001) reported that the low levels of ciliates found during the summer cannot have much effect on HNF at this time of year.
Contrary to the coastal area, at the open sea (Station B) bacterial abundance was closely related to chl a concentrations, suggesting that bacterial abundance was strongly controlled by substrate supply, and that phytoplankton was the most important source of substrate. Other studies also showed that, in systems that do not receive alochtonous inputs of substrates, bacteria are supported by the supply of organic carbon derived from phytoplankton (Carlson et al. 1996; Kirchman and Rich 1997). Previous investigations at this station have shown the presence of high concentrations of nutrients in the deep layers of chl a (from 30 to 100 m depth), which presumably stimulated the beginning of the phytoplankton bloom and bacterial activity (Ninčević et al. 2002). The dominant role of substrate supply in controlling bacterial abundance during the winter-spring period is supported by the fact that the coupling between bacteria and their predators (HNF) was very weak in that period. Bacterial abundance was high enough to support higher HNF abundance than was realized, suggesting that predation exerted a minor depressing influence on bacterial abundance during this period. Very low grazing on bacteria during the colder part of the year has been reported for the open middle Adriatic in several other studies as well (Šolić and Krstulović 1994; Šolić et al. 1998, 2001).
Bacterial production at Station B followed the distribution of chl a and was lagging 2 months behind the peaks of algal biomass. This lag between algal and bacterial seasonal development has also been observed by other authors (Coffin and Sharp 1987; Vaque 1996). Billen et al. (1990) suggested that the delayed development of bacterioplankton bloom with respect to phytoplankton might be explained by the fact that decaying phytoplankton release more dissolved organic matter, favoring the activity of bacteria.
HNF abundance at the open sea station (Station B) showed a stronger relationship with bacterial production than with bacterial abundance. This suggests that, at the open sea station, HNF controlled bacterial standing stocks by direct cropping of bacterial production, and that such control occurred only during the warmer spring-summer period. This finding is supported by the results of Gonzalez et al. (1993) and Sherr et al. (1992) who suggested that, because of a higher grazing pressure on more actively growing and dividing cells, bacterivores crop the production rather than simply the standing stocks of bacteria. Although HNF abundance was not correlated with temperature, temperature may explain a small part of HNF abundance variance because its inclusion as an additional independent variable slightly improved the regression model (coefficient of multiple correlation R=0.565; Table 3).
This work was supported by the Ministry of Science and Technology of Croatia under the project “The role of bacteria in the pelagic food web”; grant No. 000 10 103.
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