Harmful and parasitic unicellular eukaryotes persist in a shallow lake under reconstruction (L....
Transcript of Harmful and parasitic unicellular eukaryotes persist in a shallow lake under reconstruction (L....
PRIMARY RESEARCH PAPER
Harmful and parasitic unicellular eukaryotes persistin a shallow lake under reconstruction (L. Karla, Greece)
Eleni Nikouli • Konstantinos Ar. Kormas •
Panagiotis Berillis • Hera Karayanni •
Maria Moustaka-Gouni
Received: 11 February 2013 / Revised: 8 June 2013 / Accepted: 15 June 2013 / Published online: 29 June 2013
� Springer Science+Business Media Dordrecht 2013
Abstract The reconstructed Lake Karla, Greece, has
been undergoing its water-filling period since Novem-
ber 2009. In this paper, we aimed at investigating
whether the unicellular eukaryotes, including the
toxic/parasitic ones, that have been found during mass
fish kills in the lake (March–April 2010), persist
during the first warm period of the lake (May, August,
November 2010). Given that microscopic character-
ization of some of these eukaryotes is not adequate for
their identification, we analysed the 18S rRNA gene
diversity of plankton samples. All the found phylo-
types belonged to the phyla of Mesomycetazoa,
Chlorophyta, Fungi, Alveolata, Cercozoa, Crypto-
phyta and Stramenopiles. Some members of these
groups seem to persist in Lake Karla as they have been
found in early spring as well. These microscopic
eukaryotes are either ichthyotoxic/parasitic (e.g.
Pfiesteria sp./Pseudopfiesteria shumwayae, some
Fungi, Mesomycetazoa, Lagenidium sp., Cercozoa)
or indicative of hyper-eutrophic conditions (e.g.
Oocystis sp., Scenedesmus spp.) and were rather
abundant during the first spring–autumn period of
the lake’s refilling process. These complex micro-
scopic communities are expected to shape highly
dynamic and variable food webs with the risk of
repeated fish kills.
Keywords 18S rDNA � Plankton � Unicellular
eukaryotes � Shallow � Lake � Karla � Greece
Introduction
Practically all known biota of shallow lakes has been
the focus of numerous studies, starting from the old-
known strong relationship between the nutrient regime
and the lakes’ primary producers to conceptual and
mathematical models describing seasonal succession
of phytoplankton (Lampert & Sommer, 2007). The
latter, not just has a pivotal role in the shallow lake
ecosystem structure and function, but its community
composition, abundance and biomass are now recog-
nized as universal tools for assessing the ecological
quality of these systems (WFD, 2000). However,
ongoing research on these systems is still vivid and
Handling editor: Stefano Amalfitano
Electronic supplementary material The online version ofthis article (doi:10.1007/s10750-013-1604-8) containssupplementary material, which is available to authorized users.
E. Nikouli � K. Ar. Kormas (&) � P. Berillis
Department of Ichthyology and Aquatic Environment,
School of Agricultural Sciences, University of Thessaly,
384 46 Volos, Greece
e-mail: [email protected]
H. Karayanni
Department of Biological Applications and Technology,
University of Ioannina, 451 10 Ioannina, Greece
M. Moustaka-Gouni
School of Biology, Department of Botany, Aristotle
University of Thessaloniki, 541 24 Thessaloniki, Greece
123
Hydrobiologia (2013) 718:73–83
DOI 10.1007/s10750-013-1604-8
rewarding, mostly due to its often unpredictable
temporal and spatial changes. Due to their small water
volume and their frequently unstable hydrological
budget, they are influenced by variable environmental
parameters more pronounced than other lake ecosys-
tems (Padisak & Reynolds, 2003). These changes are
usually more pronounced in eutrophic shallow lakes
(e.g. Fernandez et al., 2012). Such great variance is
very difficult to incorporate in realistic experiments
which in most cases do not last long enough to
enlighten us with their result on the lakes’ microalgal
community succession (Waters et al., 2012). Shallow
lakes are of great interest to humans, as it is shown by
the large number of constructed ones. Their usage
includes mostly reservoirs for drinking water or
irrigation purposes and recreation sites (Padisak &
Reynolds, 2003). Worldwide, a majority of lakes are
categorized as shallow ones, whilst 70% of the lakes in
Greece are shallow (Coops et al., 2003).
In the study of shallow lakes, phytoplankton is
traditionally studied as it is highly responsive to
environmental changes and several phytoplankton
species serve as indicators for, e.g. eutrophication,
ecological water quality (Padisak et al., 2006). More-
over, we now know that some unicellular eukaryotes,
like nanoflagellates, dinoflagellates and ciliates, are
key players in the transfer of energy in aquatic food
webs (Sherr & Sherr, 2002). However, their precise
identification and enumeration can be a dubious task at
least in some cases (Caron et al., 2009; Christaki et al.,
2011). Nowadays, it is well accepted that the identi-
fication of unicellular eukaryotic species should
integrate both morphological traits and molecular
markers. This approach circumvents identification
problems of ecological importance, such as the cryptic
species of several morphospecies that exist in eukary-
otic lineages (Weisse, 2008) or the small (B5 lm)
freshwater eukaryotes which remain highly under-
investigated and are best studied only with molecular
tools (Sime-Ngando et al., 2011). In addition, in cases
of microorganisms with complex but unknown or
inefficiently described life cycles, the phylotype
approach assists in clarification of unknown cell
morphologies, thus rendering the trophic relationships
and ecophysiological traits more explicable.
Undesired blooms of harmful cyanobacteria and
algae, which are common in shallow eutrophic lakes,
pose the question of safety for these habitats, not only
for human, animal and ecosystem health but also for
economic growth and development of the areas where
they are found (Bakker, 2012). In a previous study,
provoked by fish kills in the recently reconstructed
L. Karla, Greece, associated with the occurrence of
toxic/parasitic unicellular eukaryotes and/or cyano-
bacteria, we had identified a high diversity of unicel-
lular eukaryotes and some of them could be related to
the fish kills (Oikonomou et al., 2012). In this study, we
aimed at (a) investigating whether these eukaryotes
persist during cyanobacterial blooms and (b) extending
our knowledge in planktic single-celled eukaryotes
biodiversity. For this, we investigated the unicellular
eukaryotes’ diversity in May (following the reported
blooms of Prymesium parvum and Pfiesteria piscicida
and the start of cyanobacteria blooms), August (peak of
cyanobacterial blooms) and November (end of cyano-
bacterial blooms) 2010, the lake’s first year of water
filling. Identifying the common, if any, 18S rDNA
phylotypes between different periods will permit us to
detect whether the lake’s planktic life kicks off with
opportunistic or typical shallow lake species.
Materials and methods
The water filling of Lake Karla, central Greece
(Fig. 1), which started in 2009, is the last major phase
of its reconstruction. With a 288-km perimeter. It
occupies ca. 1/4 of the old Lake Karla which covered
180 km2 and which was dried up in 1962 for
reclaiming agricultural land. The hydrological basin
of Lake Karla covers 1,171 km2 of which more than
600 km2 make up a southern flat plain, whilst the east
part is surrounded by mountains and hills with a
perimeter of 228 km. Elevation ranges from 50 m to
more than 2,000 m, and the mean elevation of the
region is about 230 m. It is a shallow lake with a
current maximum water depth of 2.5 m.
Sampling took place at the end of spring, summer
and autumn, spanning the lake’s pre-warm, warm and
late-warm phase (Table 1). Water samples of 1–2 l
were collected in 4-L collapsible plastic bottles
(Nalgene, USA) from ca. 0.5 m depth at the water-
level pier at the southeast end of the lake (Fig. 1).
Water temperature, dissolved oxygen, salinity and
pH were measured in situ using a WTW sensor
(Weilheim, Germany).
Water samples for DNA extraction were transferred
to the laboratory and processed\2 h after collection.
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After a 180-lm mesh net pre-screening to exclude
larger organisms and particles, a volume of
250–400 ml of water was filtered through a 0.2-lm
pore size Polycarbonate Isopore filter (Sartorius,
Germany). The filtration was conducted under reduced
pressure (B100 mmHg) to prevent cell damage and
before filters were clogged. Filters were stored imme-
diately at -80 �C until further analysis.
Bulk DNA was extracted using the UltraClean Soil
DNA isolation kit (MoBio Laboratories, USA) accord-
ing to the manufacturer’s protocol after aseptically
slicing the filters. Concentration of bulk DNA, as
estimated in a NanoDrop ND-1000 spectrophotometer
(NanoDrop Technologies, USA), was 10.2, 5.7 and
2.6 ng ll-1 for the May, August and November 2010
samples, respectively. For the May and August sam-
ples, the 18S rRNA gene was amplified using the
eukaryote-specific primers EukA (50-AACCTGGTTG
ATCCTGCCAGT-30; Medlin et al., 1988) and
Euk1633r (50-GGGCGGTGTGTACAARGRG-30;Dawson & Pace, 2002). Each PCR mix of the 50-ll
final volume contained ca. 10 ng of environmental
DNA, 10 ll of 59 Green GoTaq Flexi buffer
(Promega, USA), 5 ll of 2 mM dNTPs, 3 ll of
25 mM MgCl2, 0.25 ll of 100 pmol/ll of each primer
and 0.25 ll of 5 U of GoTaq DNA polymerase
Fig. 1 Map of Lake Karla, Greece, and sampling point (black dot). Black squares show points of inflowing water for reconstruction
purposes
Table 1 Basic
environmental parameters
in Lake Karla, Greece
Sampling date pH Temperature (�C) Salinity (PSU) Dissolved oxygen
(mg ml-1)
28–05–2010 8.0 19.7 9.1 5.6
28–08–2010 8.5 31.7 13.2 4.8
25–11–2010 8.8 12.2 2.9 6.9
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(Promega, USA). PCR reactions for the May and
August samples included an initial denaturation step at
95�C for 2 min followed by 40 cycles of denaturing at
95�C for 40 s, annealing at 50�C for 40 s, and
elongation at 72�C for 2 min and 15 s, with an
additional step of final elongation at 72�C for 7 min.
For the November samples, nested PCR was used, with
the first primers being EukA and EukB (50-GATCCT
TCTGCAGGTTCACCTAC-30; Medlin et al., 1988),
whilst in the second PCR, EukB was replaced by
Euk1633r. The latter included an initial denaturation
step at 95�C for 15 min, which was followed by 40
cycles consisting of denaturation at 95�C for 45 s,
annealing at 55�C for 1 min, and elongation at 72�C for
2 min and 30 s; a final 7-min elongation step at 72�C
was included.
PCR for each sample was repeated with different
cycle numbers (between 18 and 39). The lowest
number of cycles with a positive signal, i.e. 28, 31 and
20 cycles for the May, August and November samples,
respectively, was used for cloning in order to eliminate
some of the major PCR innate limitations (Wintzin-
gerode et al., 1997; Spiegelman et al., 2005) and to
avoid differential representation of low and high 18S
rRNA gene copy numbers.
PCR products were visualized on 1% agarose gel
under UV light, purified by the Montage purification kit
(Millipore Inc., Molsheim, France). The purified PCR
products were ligated into the PCR XL TOPO Vector
(Invitrogen-Life Technologies, USA) and transformed
in electrocompetent Escherichia coli cells according to
the manufacturer’s specifications. For each clone
library, a maximum of 72 clones were sequenced, each
containing an insert of ca. 1,600 bp. These clones were
grown in liquid Luria–Bertani medium with kanamycin
and their plasmids were purified using the Nucleospin
Plasmid Quick-Pure kit (Macherey-Nagel GmbH and
Co. KG, Duren, Germany) for DNA sequencing.
Capillary electrophoresis sequencing (Macrogen Inc.,
Seoul, Korea) was performed using the BigDye Termi-
nator kit (Applied Biosystems-Life Technologies, USA)
with the M13F (50-GTAAAACGACGGCCAG-30) and
M13R (50-CAGGAAACAGCTATGAC-30) primers.
Each sequence read was ca. 950–1,000 bp. For each
individual clone, forward and reverse reads were
assembled, and then the assembled sequences were
checked for chimeras. The Pintail program (http://
www.bioinformatics-toolkit.org/Web-Pintail/) was
used for the detection of putative chimeric sequences.
Chimeras were discarded from the dataset. Using the
multiple alignment program CLUSTALW2 (http://www.
ebi.ac.uk/Tools/clustalw2/index.html/) and based on
98% gene similarity as a phylotype cutoff (Caron et al.,
2009; Nebel et al., 2011), clones were grouped together
and considered members of the same phylotype. All
sequences were compared with the BLAST function
(http://www.ncbi.nlm.nih.gov/BLAST/) for the detec-
tion of closest relatives. Sequence data were compiled
using the MEGA5 software (Tamura et al., 2011) and
aligned with sequences obtained from the GenBank
(http://www.ncbi.nlm.nih.gov/) database, using the
ClustalX aligning utility. Phylogenetic analyses were
performed using the MEGA 5 software (Tamura et al.,
2011) and the topology of the tree was based on
neighbour joining according to Jukes-Cantor. Boot-
strapping under parsimony criteria was performed with
1,000 replicates. Sequences of unique phylotypes found
in this study have GenBank accession numbers
KC315804–KC315844.
Library clone coverage was calculated by the
formula of the Good’s C estimator [1 - (ni/N)] [Good,
1954], where ni is the number of phylotypes repre-
sented by only one clone and N is the total number of
clones examined in each library. The number of
predicted phylotypes for each clone library was
estimated after the abundance-based richness formula
SChao1 (Chao, 1984, 1987).
Results
pH (Table 1) showed little variation and always
remained above 8.0. Temperature (Table 1) showed
the expected seasonal pattern for Mediterranean shal-
low lakes, with its highest value in August (31.7�C) and
a lower value in November (12.2�C). Conductivity
(Table 1) showed high values in May and especially in
August (23.01 mS cm-1), but it decreased down to
5.51 mS cm-1 in November. Salinity values (in PSU)
were proportional to conductivity (Table 1). Dissolved
oxygen (Table 1), although minimum in August
(4.8 mg ml-1), never reached hypoxic values.
A total of 72, six and 54 sequences were analysed
for the May, August and November samples, respec-
tively, corresponding to 24, five and 12 phylotypes,
based on a C98% similarity cutoff limit. All phylo-
types but one, i.e. Copepoda, represented unicellular
eukaryotes of the following taxa: Mesomycetazoa,
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Chlorophyta, Fungi, Alveolata, Cercozoa, Crypto-
phyta and Stramenopiles (Fig. 2). The ratio of
observed to predicted phylotypes according to the
SChao1 index ranged between 35.4% (November) and
77.4% (May), whilst clone coverage based on the
Good’s C estimator was considered satisfactory for
May and November clone libraries (Fig. S1).
In May, the most abundant taxa were Fungi (Fig.
S1a, b) and Chlorophyta (Fig. S5). The August clone
library consisted only of five phylotypes belonging to
the Cryptophyta (Fig. S4), Fungi (Fig. S1a, b),
Mesomycetazoa (Fig. S2) and Stramenopiles (Fig.
S7), none of which dominated. In November, the
dominant phylum was the Stramenopiles (Fig. S7). The
vast majority of the remaining phylotypes belonged to
the Alveolata (Fig. S8) and Cercozoa (Fig. S6).
No phylotype was found to occur in all three
samplings, but there were some shared between
different samplings (Fig. 3). Two unknown Fungi-
related phylotypes (Fig. S1a, b; KRL03E17,
KRL03E21) and one from Mesomycetazoa (Fig. S2;
KRL03E02) related to Ichthyophonida sp., which were
detected in May were also found in August. Between
August and November, there were no common phyl-
otypes. The highest number of common phylotypes
occurred between May and November. These included
three Alveolata (Fig. S8; the unknown KRL03E03,
KRL03E57 and the Pseudopfiesteria shumwayae-like
KRL03E38), three Stramenopiles (Fig. S7, S9; the
Cyclotella sp.-like KRL03E08, the Goniochloris sp.-
like KRL03E85 and the Lagenidium sp.-like
KRL03E75) and the Scenedesmus subspicatus-related
KRL03E40 from the Chorophyta (Fig. S5).
Discussion
We investigated the existing 18S rRNA gene diversity
during the first warm period, after the water-filling
process started in the shallow, reconstructed Mediter-
ranean Lake Karla, in May, August and November
2010. These periods coincided with the start (May),
peak (August) and end (November) of the lake’s
cyanobacterial blooms (Papadimitriou et al., 2013).
Apart from adding to the very limited knowledge of
the unicellular eukaryotes’ diversity in reconstructed
lakes, and especially the small (B5 lm) eukaryotes in
freshwater, we also aimed at investigating whether the
microorganisms following the fish kills which
occurred in March/April 2010 (Oikonomou et al.,
2012) were the same with the ones recorded during
these fish kills.
Chlorophyta (Fig. S5, S9) were found in May and
November. Phylotype KRL03E07 dominated in May
and is practically identical to Scenedesmus pectinatus.
Another three phylotypes (KRL09E46, KRL03E19
and KRL03E40) were related to Scenedesmus spp.,
rendering this genus an important component of the
autotrophic community. Members of the Scenedesm-
aceae prefer lotic (Bellinger & Sigee, 2010) and
hypertrophic (Tavera & Dıez 2009) waters. The
family Oocystaceae was represented by phylotypes
Fig. 2 Collapsed
phylogenetic tree of the 18S
rDNA relationships (ca.
1600 bp) of the
representative unique for
each sample (grouped on
C98% similarity) phylotype
found in the Lake Karla
water column in May,
August and November 2010.
The tree is based on the
neighbour-joining method
as determined by distance
Jukes–Cantor analysis. One
thousand bootstrap analyses
(distance) were conducted.
Scale bar represents 2%
estimated distance. For
detailed sub-trees per
phylum, see Supplementary
Material
Hydrobiologia (2013) 718:73–83 77
123
KRL03E42 and KRL03E76. Oocystis sp. are fre-
quently found in freshwaters (Hepperle et al., 2000),
whilst dominant in heavily polluted water bodies like
the shallow brackish lake Koronia (Michaloudi et al.,
2012).
A total of 10 Stramenopiles phylotypes (Fig. S7)
were found. In August and November, they were most
abundant and closely related to the marine diatom
Chaetoceros gracilis. This could be due to the
increased salinity in summer. Similarly, KRL09E17
was related to marine phytoplankton centric diatoms,
whereas phylotypes KRL09E05 and KRL03E08 were
related to the frequently occurring freshwater genus
Cyclotella (Fig. S9; Hasle & Syvertsen, 1997; Stoer-
mer & Julius, 2003). Phylotype KRL03E60 repre-
sented Pseudotetraedriella kamillae which has been
found in the oligotrophic Lake Stechlin, Germany, and
is considered a low abundance species during spring
and autumn (Hegewald et al., 2007). The two Oomy-
cetes phylotypes (KRL03E75 and KRL09E14) repre-
sent Lagenidium caudatum, which has been isolated
from a nematode host originating from rabbit and cow
faecal material (Beakes et al., 2006).
Six phylotypes were found in the Alveolata (Fig.
S8), all in May and November. Four of them
(KRL03E03, -57, KRL09E06, -21) were not close to
any cultivated members of the phylum. Their closest
(93.7–94.1%) known relative is the predatory flagellate
Colpodela edax (Leander et al., 2003), which can be
found both in freshwaters and marine habitats
(Myl’nikov, 1991). It consumes smaller protists (Arndt
et al., 2000) by sucking the attacked cells (Brugerolle,
2002). Phylotypes KRL03E38 and KRL09E10 are
closely related to the heterotrophic dinoflagellates
Pseudopfiesteria shumwayae and Pfiesteria piscicida.
Pfiesteria piscicida has been associated with mass fish
kills (Burkholder et al., 1992; Noga et al., 1996;
Oikonomou et al., 2012), caused by the release of
potent ichthyotoxins (Smith et al., 1988; Burkholder &
Glasgow, 1995). It is also considered responsible for
cases of human diseases through the consumption of P.
piscicida-toxicated fish (Burkholder & Glasgow,
1997; Steidinger et al., 2006). Pseudopfiesteria shu-
mwayae is similar to P. piscicida, although its patho-
genicity, growth characteristics and food preference
are not completely known. In general, this and related
species become abundant after increased nutrient
loadings due to the increase of their prey, i.e. phyto-
plankton (Burkholder & Glasgow, 1997).
The Cryptophyta include both auto- and heterotro-
phic species (Mignot, 1965; McFadden et al., 1994).
Phylotype KRL06E73 is distantly (94.2%) related to
the heterotrophic Chilomonas paramecium (Cavalier-
Smith et al., 1994) and KRL09E02 was highly similar
to the photosynthetic Cryptomonas curvata (Marin
et al., 1998). The ecological importance of the
Cryptophyta lies in their potential as prey for fresh-
water plankton (Chen & Folt, 1993) and some inver-
tebrates like Dreissena polymorphya (Vanderploeg
et al., 1996). In a study that included 11 mountain lakes,
Fig. 3 Venn diagram
showing the common
unicellular eukaryotes
occurring during the first
year of Lake Karla’s,
Greece, water refilling
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Cryptophyta phylotypes were most abundant in the
most eutrophic lake (Triado-Margarit & Casamayor,
2012), indicating the preference of this group for
eutrophic systems, such as L. Karla.
In total, nine Fungi phylotypes (Fig. S1a, b) were
found, and all were related to yet uncultivated
members of the phylum with their closest relatives
originating from marine and freshwater sediments.
Two identical phylotypes from May (KRL03E21) and
August (KREL06E206) were related to Fungi found in
the water column of the severely degraded, hypertro-
phic L. Koronia, Greece (Genitsaris et al., 2009). Four
phylotypes (KRL03E17, -32, -80, KRL06E139),
along with similar phylotypes from the deep, oligo-
to mesotrophic L. Pavin, France (Lefevre et al., 2007)
and Ketelmeer, The Netherlands (Van Hannen et al.,
1999) with heavy metals polluted sediments (Hulscher
et al., 2002), form a discrete novel clade. The Fungi-
like phylotypes found in May belong most likely to a
novel clade. Whether these new Fungi are actual
parasites or not is not clarified from this study,
although their ecological role might be important
since the Fungi are considered to alter the prevailing
food web structure and function through the consump-
tion of zoospores by mesozooplankton and micro-
plankton (Niquil et al., 2011), especially in eutrophic
ecosystems (Miki et al., 2011).
All members of the Mesomycetazoa are considered
parasites of fish, crustaceans and amphibians (Van
Hannen et al., 1999). In L. Karla, such phylotypes
were found in May and August (Fig. S2), belonging to
the Ichthyophonida order and are related to Sphaero-
forma arctica, Ichthyophonida fragrantissima, iso-
lated from the digestive tract of marine invertebrates
(Marshall et al., 2008) and Anurofeca richardsi, a
known parasite of Anura (Baker et al., 1999).
Cercozoa (Fig. S6) where found only in May and
probably their occurrence is limited to spring, as they
were also found in March and April (Oikonomou et al.,
2012). Phylotype KRL03E11 is a yet uncultivated
taxon, but it belongs to a clade that includes Platyreta
germanica and Arachnula impatiens which are para-
sites of fungi, algae nematodes and possible bacteria
(Bass et al., 2009). Phylotype KRL03E39 was close to
the Cryothecomonas longipes and Protaspis grandis,
isolated from the marine environment, implying the
association of this phylotype with increased salinities
as is the case with other Cercozoa found in L. Karla
previously (Oikonomou et al., 2012). C. longipes is a
selective parasitic flagellate, infecting members of the
Stramenopiles (Kuhn et al., 2000) and can cause mass
death of phytoplankton (Drebes et al., 1996; Tillmann
et al., 1999).
The Copepoda phylotype found was closely related
to the predatory genus Cyclops. The genetic material
might have come from eggs, nauplii or body fragments
which occurred in the May sample. Members of the
genus Cyclops are widespread in freshwaters (Box-
shall & Defage, 2008). In L. Karla, in particular,
Cyclops sp. is the one and only—but highly abun-
dant—copepod species that has been observed to date
(Kagalou, unpublished data). Such metazoan
sequences have also been found before in similar
studies targeting unicellular eukaryotes (Luo et al.,
2011).
The major taxa found in our study were also found
in a parallel study which focused on the microscopic-
based analysis of phytoplankton between April and
October 2010 (Papadimitriou et al., 2013). However,
our study revealed the existence of some unicellular
eukaryotes that were not identified by microscopy, like
the phylotypes associated with the Mesomycetazoa
(Fig. S2), the Fungi (Fig. S1b) and the novel clades
within the Cercozoa (Fig. S6) and the Alveolata (Fig.
S8). The structure of unicellular eukaryotic commu-
nities in L. Karla, as revealed by their 18S rDNA
analysis, was found to vary from spring to autumn. At
the end of spring, Fungi (25/72 sequences, 6/24
phylotypes) and Chlorophyta (24/72 sequences, 6/24
unique phylotypes) dominated. On the contrary, at the
end of summer, only five low abundance eukaryotic
phylotypes were retrieved, indicating that unicellular
eukaryotes were not abundant, as was also reported by
microscopic analysis of phytoplankton during the
warm period in L. Karla in 2010 (Papadimitriou et al.,
2013). In addition, the relationship of the initial
extracted bulk DNA concentration with the DNA
concentration after the 18S rDNA-specific PCR indi-
cated that only a small fraction of the bulk DNA was of
eukaryotic origin, with its major part being prokary-
otic (data not shown). During the warm period in 2010,
i.e. April–October, Cyanobacteria dominated on aver-
age 75% in the phytoplankton community, and in
August this dominance was [90% (Papadimitriou
et al., 2013), as is the case in several other eutrophic
shallow lakes (Oliver & Ganf, 2000; Steven et al.,
2012). This could explain the low amount of eukary-
otic DNA and low number of eukaryotic phylotypes
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123
retrieved, especially the autotrophic ones through light
and nutrient limitation. Such a seasonal decline in
unicellular eukaryotic species richness has been
reported for the oligotrophic L. Stechlin as well (Luo
et al., 2011), implying that the increased trophic state
of a lake brings reduction in the prevailing phylotype
number. Moreover, another likely reason for the low
number of both autotrophic and hetero-/mixotrophic
microscopic eukaryotes is allelopathy. Allelopathy
contributes to promoting, maintaining and succeeding
cyanobacterial and microalgal blooms in freshwater
and marine environments (Gross, 2003; Legrand et al.,
2003). For example, Microcystis (Singh et al., 2001;
Sukenik et al., 2002), Anabaena species (Graneli et al.,
2008), Nodularia spumigena (Zak et al., 2012),
Planktothrix and Aphanizomenon species (Keating,
1987) are known to inhibit growth of microalgae and
other cyanobacteria as well.
A substantial part of the found phylotypes is related
to parasitic/saprophytic and not to bacterivorous
species, as is often revealed by similar studies
(Sime-Ngando et al., 2011 and references therein).
This is also indicated by the exceptionally high
prokaryotic cell counts measured during the first year
of the L. Karla’s refilling (Fig. S10) with its second
highest value (79.6 9 106 cells ml-1) in August,
when the lowest number of unicellular eukaryotic
phylotypes occurred.
Based on microscopy in freshwater lake ecosys-
tems, the Heterokonta, the kathablepharids and the
Choanozoa contribute in excess of 90% of the
flagellate protozoa diversity observed (Arndt et al.,
2000). However, microscopy with molecular studies
do not always corroborate (e.g. Luo et al., 2011), but
are rather complementary, especially for the smaller
protists and some specific groups like the cryptomo-
nads (e.g. Richards et al., 2005; del Campo &
Massana, 2011). In our study, we used a 0.2-lm filter
in order to include picoplanktic forms, whilst detailed
microscopic investigations of L. Karla’s first year are
reported elsewhere (Papadimitriou et al., 2013).
Previously, in L. Karla in March and April 2010
(Oikonomou et al., 2012; Papadimitriou et al., 2013),
we identified some ecologically important microor-
ganisms not found in the present study. For example,
Prymnesium parvum, a potentially toxic haptophyte,
reached 99 9 106 individuals ml-1 and represented
44.6% of all phytoplankton species abundance. In the
present study, P. parvum was not detected, probably
due to its low growth rate when nutrient concentra-
tions are high (Guo et al., 1996). In addition, in most
cases, its blooms occur at the beginning of spring,
suggesting its preference for lower temperature
regimes (Baker et al., 2007). Still, L. Karla seems to
be plagued by microscopic eukaryotes that are either
ichthyotoxic/parasitic (e.g. Pfiesteria sp./Pseudopfies-
teria shumwayae, some Fungi, Mesomycetazoa, La-
genidium sp., Cercozoa) or indicative of hyper-
eutrophic conditions (e.g. Oocystis sp., Scenedesmus
spp.), at least during its first spring–autumn period.
These complex communities are likely to be interact-
ing mostly by allelopathic or harshly competitive
trophic relationships. The question that remains is
whether these microorganisms are ‘vagabonds’ (sensu
Newton et al. (2011) and will persist and plague the
lake’s future or whether their occurrence is simply
opportunistic, ‘tourists’ (sensu Newton et al., 2011),
and the ongoing succession will result in typical lake
microorganisms, ‘natives’ (sensu Newton et al., 2011).
Ongoing, targeted and multiphasic monitoring of the
lake’s plankton as in every continuously changing
system is required, especially since several of these
microorganisms cannot be identified/quantified by a
single approach.
Acknowledgments This part of this work was supported by
the John S. Latsis Public Benefit Foundation, Research
Programs 2011. Part of the laboratory work was financed by
the MSc programme ‘‘Sustainable Management of Aquatic
Environment’’ by the Department of Ichthyology and Aquatic
Environment, University of Thessaly. Peter McGee http://
anglais.webs.com/englishotherversions.htm provided editorial
and linguistic assistance. We thank the two anonymous reviewers
for their comments on the originally submitted manuscript.
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