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Applied and Environmental Microbiology, June 2005, p. 3379-3383, Vol. 71, No. 6
0099-2240/05/$08.00+0 doi:10.1128/AEM.71.6.3379-3383.2005
Copyright © 2005, American Society for Microbiology. All Rights Reserved.
Nitrate and Phosphate Affect Cultivability of Cyanobacteria from Environments with Low Nutrient Levels
Anneliese Ernst,1*
Manfred Deicher,2
Peter M. J. Herman,1 and
Ute I. A. Wollenzien1
Centre for Estuarine and Marine Ecology, Netherlands Institute of Ecology (NIOO-KNAW), 4400 AC Yerseke, The Netherlands,1
Fachbereich Physik, Universität Konstanz, 78457 Konstanz, Germany2
Received 16 August 2004/
Accepted 15 December 2004

ABSTRACT
Nitrate and phosphate concentrations higher than those found
in the natural environment slowed down growth of two strains
of non-bloom-forming, phycoerythrin-rich
Synechococcus spp.
isolated from mesotrophic subalpine lakes. The results make
clear why isolation of these picocyanobacteria in standard cultivation
media was difficult. At low concentrations, closely related
strains exhibited distinct growth characteristics with respect
to these two nutrients, possibly explaining differences in their
seasonal appearance in the natural environment.

INTRODUCTION
At low levels of nutrient loading, small red-pigmented phycoerythrin
(PE)-rich cyanobacteria of the
Synechococcus type dominate the
autotrophic picoplankton in freshwater ecosystems (
10,
12,
16,
21). These non-bloom-forming
Synechococcus spp. (
19) belong
to the same phylogenetic clade as marine
Synechococcus spp.
and
Prochlorococcus spp. (
7,
8,
20). Despite their ubiquity,
they were discovered in the late 1970s only, when epifluorescence
microscopy and flow cytometry were introduced as counting techniques
(see references in reference
18) and the first isolates from
marine and freshwater ecosystems became available (
6,
23). The
difficulty in cultivating red-pigmented freshwater
Synechococcus spp. contrasts with the easy accessibility of blue-green, phycocyanin-rich
species, particularly those of the closely related genus
Cyanobium (
8,
22; for strain histories, see reference
14).
Recently, Becker et al. (3) reported that PE-rich picocyanobacteria from a biofilm of tiles deposited for 6 weeks in Lake Constance formed small colonies on agar plates amended with a mineral medium lacking nitrate, BG110, although none of them was capable of nitrogen fixation. A similar inoculum spread on plates with nitrate (BG11) produced blue-green colonies only. The mineral medium BG11 was introduced by Stanier et al. (17) for the cultivation of coccoid cyanobacteria. In its original description, it is particularly rich in nitrate (1.5 g/liter NaNO3, equivalent to 247 mg/liter NO3-N) and exhibits an N:P molar ratio of 100:1, which is far above the molar ratio of these elements in biomass (Redfield ratio, 16:1). Nevertheless, phosphate also is plentiful in BG11 compared to the environmental concentrations often limiting the growth of photoautotrophs in meso- and oligotrophic lakes.
Cyanobacteria have developed highly efficient uptake and retention mechanisms for three nutrient anions: bicarbonate, nitrate, and phosphate (1, 11, 15). The apparent competitive disadvantage of PE-rich Synechococcus spp. on a cultivation medium rich in nitrate prompted us to examine the effect of high nutrient concentrations on the growth of two strains, Synechococcus rubescens strain SAG 3.81 and Synechococcus sp. strain BO 8807, isolated from Lake Zürich and Lake Constance, respectively.

Growth inhibition by phosphate and nitrate.
The two red-pigmented
Synechococcus strains BO 8807 and SAG
3.81 of subalpine cluster I (
8) were raised in 96-well microtiter
plates. Before growth experiments were conducted, aliquots of
batch cultures were diluted into fresh growth medium (BG11 amended
with sterile solutions of sodium bicarbonate [0.168 g/liter]
and vitamin B12 [0.02 mg/liter]) and maintained at least 20
h under continuous light (10 ± 1 µmol quanta m
2 s
1) at 19 ± 1°C, the conditions used during
growth experiments. After this preadaptation, cells were collected
by centrifugation (10 min; 10,000
x g), washed, and resuspended
in this medium lacking nitrate and phosphate. Sterile dilutions
of NaNO
3 and K
2HPO
4 were added, in a volume of 10 µl each,
to the 96 wells of flat-bottom microtiter plates (Greiner).
Finally, the resuspended cells were added in a volume of 130
µl. The microtiter plates were taped at the long sides
and then placed on a microtiter plate vortexer (Applied Quality
Services, United Kingdom) that was set to 2 min of vigorous
shaking per h to counteract sedimentation of cells.
The 96-well format allowed not only the application of a wide range of nutrient loadings and N:P ratios but also monitoring of growth with a microplate reader (ELx808; Bio-Tek, Germany), a convenient and nonintrusive detection method. Growth was followed by measuring the optical density at 750 nm (OD750). At this wavelength, the pigments of cyanobacteria exhibit negligible absorbance and, hence, turbidity can be used as a measure for biomass.
At low initial nutrient concentrations (0.3 mg/liter K2HPO4 and 15 mg/liter NaNO3), biomass did not increase significantly. Both concentrations were higher than those measured in Lake Constance, which exhibited a total P concentration of 40 µg/liter and 4.3 mg/liter NO3 in 1988, when a maximum of 7.7 x 105 cells/ml of autotrophic picoplankton was reported (9). The initial cell density of (2 to 4) x 107 cells/ml in our experiments may have already exceeded the carrying capacity. Also, at an initial NaNO3 concentration of 9.9 g/liter, the highest nitrate concentration used, biomass of both strains did not increase during the duration of the experiments (10 to 14 days in different series). At intermediate concentrations, growth strongly depended on the initial phosphate and nitrate concentrations (Fig. 1). The total biomass formation was limited by nitrate if the molar N:P ratio was
33 and was limited by phosphate at higher N:P ratios, a factor two higher than that expected from the Redfield ratio. For both strains, high initial nitrate and phosphate concentrations delayed growth. The initial phosphate concentration used in BG11 (0.03 g/liter K2HPO4) inhibited growth of both strains even at low nitrate concentrations (Fig. 1c and f). In combination with the high nitrate concentration of BG11 (1.5 g/liter; Fig. 1c and f), both strains did not reach stationary phase within 2 weeks. Similar growth characteristics were reported earlier for two other strains of the subalpine cluster I (13).
In batch cultures, growth rates are not constant because the
concentration of the limiting nutrient decreases during growth.
Growth limited by a vanishing resource is described by logistic
growth models. For the logistic fit of the growth measured at
OD
750, we applied the equation
 | (1) |
The
sigmoid shape of the growth curve is characterized by four parameters:
the upper asymptote,
a, represented by the absorbance reached
in the stationary phase, a rate parameter,
k, describing the
rate at which growth initially accelerates, and a time constant,
c, that describes the time elapsing between the beginning of
the growth experiment and the point of maximum increase in biomass
(turning point). To fit the data of our experiments, an offset
in the absorbance (
a0), which remained constant throughout the
experiment, was added. In Fig.
1, the fits of individual growth
curves are depicted as continuous lines. The model fitted growth
of the two PE-rich
Synechococcus strains well except at high
nutrient concentrations at which growth was inhibited and cultures
did not reach stationary phase before termination of the experiments.
From the parameters we calculated the biomass-specific initial growth rate at t = 0 (see Appendix). These calculations showed that k is an excellent approximation of the initial, biomass-specific growth rate. Hence, we used k as an approximation for the maximum growth rate at the indicated nutrient concentration.
For both Synechococcus strains, we conducted two series of growth experiments, both with an internal replicate for every concentration used. To calculate the growth parameters a, a0, c, and k for multiple experiments, the OD750 values were imported into the program Origin (version 7.5; OriginLab Corp.). A script for data management and analysis was written in LabTalk, a C-based scripting language provided by this program. The script was structured in four subroutines: first, the extinction values (triplicates) were averaged and the intrinsic absorption of each well filled with 150 µl H2O was subtracted. Next, time series were constructed with the net extinction values. Third, the time series were fitted assuming a logistic growth function (equation 1). Finally, the growth parameters of experiments with identical initial nutrient concentrations were averaged, and standard deviations were calculated (the peripheral wells of the 96-well plates were not considered). The results (Fig. 2) show that carrying capacity (a) was similar for both strains. Growth rate constants k and time constants c (not shown) were almost identical in multiple experiments conducted with the same starting material (internal replicates) but differed between experimental series. This variation is reflected in the error bars of the growth rate constant (Fig. 2). However, this variation did not obscure the effects of nutrient concentrations on growth outlined above. The generation time of both strains was about six times longer for BG11 than that in media with lower, optimal nutrient concentrations.
With these results in mind, we prepared agarose plates with
BG11 (plus vitamin B12) and four versions of the bicarbonate-enriched
medium, one with original concentrations of nutrients and three
in which phosphate was reduced to 30% and nitrate to either
10%, 3%, or 1%. These plates were inoculated with serial dilutions
of the two red-pigmented
Synechococcus strains used in this
study and a blue-green isolate, strain BO 8806, which is closely
related to
Cyanobium gracile PCC 6307 (
8). The blue-green strain
was able to form colonies with high plating efficiency (>90%)
on all variants of the medium (in Table
1, only colony numbers
of a 10
4-fold dilution of the preadapted cultures are shown).
In contrast, dilutions of the red-pigmented strains failed to
form colonies in full-strength BG11 with or without bicarbonate.
However, both strains grew with only slightly lower plating
efficiency on all plates with lowered nutrient concentrations
(Table
1). Apparently, on the surfaces of agarose plates, the
inhibitory effect of high nutrient concentrations on the growth
of the red-pigmented strains was enhanced by evaporation, resulting
in a very strong, negative isolation bias. The results are in
full agreement with the observations of Becker et al. (
3) reporting
a selective suppression of colony formation of red-pigmented
picoplankton by BG11.
View this table:
[in this window]
[in a new window]
|
TABLE 1. Number of colonies of Synechococcus sp. strains BO 8806 and BO 8807 and Synechococcus rubescens strain SAG 3.81 on agarose plates amended with variations of the mineral medium BG11
|

Clonal effects of nitrate and phosphate.
Figures
1 and
2 indicate that nitrate and phosphate affected
growth of the two
Synechococcus strains differently. Increasing
nitrate concentrations delayed growth of strain BO 8807 (Fig.
1a to c and
3a) even at low initial phosphate levels, while
growth of strain SAG 3.81 was affected by high nitrate only.
On the other hand, growth of strain SAG. 3.81 was delayed and
inhibited by increasing phosphate (Fig.
1d to f and
3b), while
strain BO 8807 not only needed higher initial phosphate concentrations
to obtain highest growth rates but also tolerated high phosphate
concentrations for cultivation, provided nitrate was low. Thus,
in strain BO 8807 the tolerance towards phosphate seemed to
be paired with a high sensitivity towards nitrate, while in
strain SAG 3.81 tolerance of nitrate is paired with high sensitivity
towards phosphate. Contour plots summarize the combined effect
of nitrate and phosphate on carrying capacity and growth rate
constants of the two strains (Fig.
3).
The observation that strain BO 8807 tolerates high concentrations
of phosphate but is highly sensitive towards nitrate, while
strain SAG 3.81 can tolerate high nitrate if phosphate is low,
indicates that uptake and assimilation of these two anions is
endogenously limited by a common resource. Thus, the question
remains why non-bloom-forming
Synechococcus spp. cannot cope
with high nutrient levels or what is the limiting endogenous
resource. Most studies of the regulation of N, P, and C assimilation
were conducted with blue-green freshwater cyanobacteria growing
well in presence of high concentrations of nitrate and phosphate.
Presumably, all these strains are capable of efficiently limiting
uptake and assimilation of N (via NtrA [
11]) and P (via the
P-regulon [
4]) when high concentrations (at low light intensity)
threaten to impair photosynthetic assimilation of CO
2. Such
a control may be missing not only in the oceanic
Synechococcus sp. strain WH 8103 (
5) but also in non-bloom-forming freshwater
Synechococcus spp., with the reported effects with cultivation
in the presence of high nutrient levels. However, at ambient
nutrient levels, the particular growth characteristics of the
two strains may be of relevance. In summer picoplankton, when
phosphate reaches a minimum in the euphotic zone of Lake Constance
(
9), genotypes closely related to that of strain SAG 3.81 are
abundant, while the genotype of isolate BO 8807 reaches a relative
and absolute minimum (
2; S. Becker, P. Richl, P. Boger, and
A. Ernst, unpublished data). As growth of this genotype is more
constrained by low levels of phosphate, this may reflect its
particular growth characteristics.

APPENDIX
The growth rate of a logistic model can be calculated from the
equation
From this equation, the initial
biomass-specific growth rate (IGR) at
t = 0 and
y = y0 can be
calculated as
For
c >>
k, the biomass-specific
IGR approaches the value of the growth rate constant
k, and
the biomass-specific growth rate at the turning point is half
that of the initial growth rate. In all our experiments,
k provided
an excellent approximation of IGR.

ACKNOWLEDGMENTS
This work was partly financed by the Commission of the European
Community through RTD project MIRACLE (contract: EVK3-CT-2002-00087).
The comments of L. Stal during preparation of the manuscript were greatly appreciated.

FOOTNOTES
* Corresponding author. Mailing address: NIOO-CEME, P.O. Box 140, NL-4400 AC Yerseke, The Netherlands. Phone: 31 (0) 113 577300. Fax: 31 (0) 113 573616. E-mail:
a.ernst{at}nioo.knaw.nl.

This is publication 3506 NIOO-KNAW of the Netherlands Institute of Ecology. 

REFERENCES
1 - Badger, M. R., and G. D. Price. 2003. CO2 concentrating mechanisms in cyanobacteria: molecular components, their diversity and evolution. J. Exp. Bot. 54:609-622.[Abstract/Free Full Text]
2 - Becker, S., M. Fahrbach, P. Böger, and A. Ernst. 2002. Quantitative tracing, by Taq nuclease assays, of a Synechococcus ecotype in a highly diversified natural population. Appl. Environ. Microbiol. 68:4486-4494.[Abstract/Free Full Text]
3 - Becker, S., A. K. Singh, C. Postius, P. Böger, and A. Ernst. 2004. Genetic diversity and distribution of periphytic Synechococcus spp. in biofilms and picoplankton of Lake Constance. FEMS Microbiol. Ecol. 49:181-190.[CrossRef]
4 - Bhaya, D., D. Vaulot, P. Amin, A. W. Takahashi, and A. R. Grossman. 2000. Isolation of regulated genes of the cyanobacterium Synechocystis sp. strain PCC 6803 by differential display. J. Bacteriol. 182:5692-5699.[Abstract/Free Full Text]
5 - Bird, C., and M. Wyman. 2003. Nitrate/nitrite assimilation of the marine picoplanktonic cyanobacterium Synechococcus sp. strain WH 8103: effect of nitrogen source and availability on gene expression. Appl. Environ. Microbiol. 69:7009-7018.[Abstract/Free Full Text]
6 - Chang, T.-P. 1980. Zwei neue Synechococcus-Arten aus dem Zurichsee. Schweiz. Z. Hydrobiol. 42:247-254.
7 - Crosbie, N. D., M. Pöckl, and T. Weisse. 2003. Dispersal and phylogenetic diversity of nonmarine picocyanobacteria, inferred from 16S rRNA gene and cpcBA-intergenic spacer sequence analysis. Appl. Environ. Microbiol. 69:5716-5721.[Abstract/Free Full Text]
8 - Ernst, A., S. Becker, U. I. A. Wollenzien, and C. Postius. 2003. Ecosystem-dependent adaptive radiations of picocyanobacteria inferred from 16S rRNA and ITS-1 sequence analysis. Microbiology (United Kingdom) 149:217-228.
9 - Gaedke, U., and T. Weisse. 1998. Seasonal and interannual variability of picocyanobacteria in Lake Constance (1987-1997). Arch. Hydrobiol. Spec. Issues Adv. Limnol. 53:143-158.
10 - Hawley, G. R. W., and B. A. Whitton. 1991. Seasonal changes in chlorophyll-containing picoplankton populations of ten lakes in Northern England. Int. Rev. Gesamten Hydrobiol. 76:545-554.
11 - Herrero, A., A. M. Muro-Pastor, and E. Flores. 2001. Nitrogen control in cyanobacteria. J. Bacteriol. 183:411-425.[Free Full Text]
12 - Pick, F. R. 1991. The abundance and composition of freshwater picocyanobacteria in relation to light penetration. Limnol. Oceanogr. 36:1457-1462.
13 - Postius, C., U. Kenter, A. Wacker, A. Ernst, and P. Böger. 1998. Light causes selection among two phycoerythrin-rich Synechococcus isolates from Lake Constance. FEMS Microbiol. Ecol. 25:171-178.[CrossRef]
14 - Rippka, R., J. Deruelles, J. B. Waterbeury, M. Herdman, and R. Y. Stanier. 1979. Generic assignments, strain histories and properties of pure cultures of cyanobacteria. J. Gen. Microbiol. 111:1-61.
15 - Ritchie, R. J., D. A. Trautman, and A. W. D. Larkum. 2001. Phosphate uptake in the cyanobacterium Synechococcus R-2 PCC 7942. Plant Cell Physiol. 38:1232-1241.
16 - Søndergaard, M. 1991. Phototrophic picoplankton in temperate lakes: seasonal abundance and importance along a trophic gradient. Int. Rev. Gesamten Hydrobiol. 76:505-522.
17 - Stanier, R. Y., R. Kunisawa, M. Mandel, and G. Cohen-Baziere. 1971. Purification and properties of unicellular blue-green algae (order Chroococcales). Bacteriol. Rev. 35:171-205.[Free Full Text]
18 - Stockner, J. G. 1988. Phototrophic picoplankton: an overview from marine and freshwater ecosystems. Limnol. Oceanogr. 33:765-775.
19 - Stockner, J. G., C. Callieri, and C. Cronberg. 2000. Picoplankton and other non-bloom-forming cyanobacteria in lakes, p. 195-231. In B. A Whitton and M. Potts (ed.), The ecology of cyanobacteria. Kluwer Academic Publishers, Dordrecht, The Netherlands.
20 - Urbach, E., D. J. Scanlan, D. L. Distel, J. B. Waterbury, and S. W. Chisholm. 1998. Rapid diversification of marine picoplankton with dissimilar light harvesting structures inferred from sequences of Prochlorococcus and Synechococcus (cyanobacteria). J. Mol. Evol. 46:188-201.[CrossRef][Medline]
21 - Vörös, L., C. Callieri, K. V. Balogh, and R. Bertoni. 1998. Freshwater picocyanobacteria along trophic gradient and light quality range. Hydrobiologia 369/370:117-125.[CrossRef]
22 - Waterbury, J. B., and R. Rippka. 1989. Subsection I, order Chroococcales Wettstein 1924, emend. Rippka et al., 1979, p. 1728-1746. In S. T. Williams, M. E. Sharpe and J. G. Holt (ed.), Bergey's manual of systematic bacteriology. Lippincott Williams and Wilkins, Philadelphia, Pa.
23 - Waterbury, J. B., S. W. Watson, R. R. Guillard, and L. E. Brand. 1979. Widespread occurrence of a unicellular, marine planktonic cyanobacterium. Nature 277:293-294.[CrossRef]
Applied and Environmental Microbiology, June 2005, p. 3379-3383, Vol. 71, No. 6
0099-2240/05/$08.00+0 doi:10.1128/AEM.71.6.3379-3383.2005
Copyright © 2005, American Society for Microbiology. All Rights Reserved.