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Applied and Environmental Microbiology, August 2006, p. 5626-5630, Vol. 72, No. 8
0099-2240/06/$08.00+0 doi:10.1128/AEM.00586-06
Copyright © 2006, American Society for Microbiology. All Rights Reserved.
Development of a Dinoflagellate-Oriented PCR Primer Set Leads to Detection of Picoplanktonic Dinoflagellates from Long Island Sound
Senjie Lin,1*
Huan Zhang,1
Yubo Hou,1
Lilibeth Miranda,1 and
Debashish Bhattacharya2
Department of Marine Sciences, University of Connecticut, Groton, Connecticut 06340,1
Department of Biological Sciences and Roy J. Carver Center for Comparative Genomics, University of Iowa, 446 Biology Building, Iowa City, Iowa 52242-13242
Received 12 March 2006/
Accepted 18 May 2006

ABSTRACT
We developed dinoflagellate-specific 18S rRNA gene primers.
PCR amplification using these oligonucleotides for a picoplanktonic
DNA sample from Long Island Sound yielded 24 clones, and all
but one of these clones were dinoflagellates primarily belonging
to undescribed and
Amoebophrya-like lineages. These results
highlight the need for a systematic investigation of picodinoflagellate
diversity in both coastal and oceanic ecosystems.

INTRODUCTION
Dinoflagellates have received considerable attention due to
their ecological and economical significance and their remarkable
cytological and genetic features (
6,
7,
20). However, our knowledge
of the species diversity of these organisms remains limited
even though novel living (
2,
3,
10,
14) and fossil lineages
(
4,
19) have been discovered. Knowledge of the diversity of
"small" dinoflagellates is particularly deficient. The recent
discovery of ultraplanktonic (<5-µm) and picoplanktonic
(<3-µm) dinoflagellates in Antarctica and the Pacific
Ocean (
13,
15), respectively, is the first demonstration of
a rich biodiversity of small dinoflagellates that have escaped
routine microscopic detection. A better understanding of dinoflagellate
biodiversity requires targeted approaches, particularly for
picoplanktonic species.

Development of dinoflagellate-oriented primers.
Based on a large database of nuclear small-subunit (18S) rRNA
genes, we designed PCR primers that target dinoflagellates.
A total of 140 18S rRNA gene sequences, including sequences
from dinoflagellates, diatoms, chlorophytes, haptophytes, cryptophytes,
and other algae, were obtained from GenBank and were aligned
using ClustalW1.8; 11 of the dinoflagellate species were sequenced
in this study (GenBank accession no. DQ388456 to DQ388466).
Regions unique to dinoflagellates were used to design three
forward and two reverse PCR primers (Table
1), which were paired
with previously described eukaryotic 18S rRNA gene universal
primers (
22) for DNA amplification.
The primers were tested with 33 genera of cultured dinoflagellates
(35 species, including
Oxyrrhis marina), as well as nine other
taxa (Table
2). Algal cultures were grown in f/2 medium (28
or 15

salinity), cells were harvested, and DNA was purified
as previously described (
23). Briefly, after cell lysis in 1
ml DNA buffer (100 mM EDTA [pH 8.0], 0.5% sodium dodecyl sulfate,
200 µg ml
1 proteinase K), DNA was purified using
DNA Clean and Concentrator columns (Zymo Research, Orange, CA).
With these DNA samples as templates, PCR was performed using
five combinations of the primers, as follows: primers 18ScomF1
and Dino18SR1 (expected product size, 0.65 kb), primers 18ScomF1
and Dino18SR2 (0.92 kb), primers Dino18F1 and 18Scom R1 (1.60
kb), primers Dino18F2 and 18Scom R1 (0.92 kb), and primers Dino18F3
and 18S com R1 (0.90 kb). All primer sets except the Dino18SF2-18ScomR1
set exhibited specificity for dinoflagellate 18S rRNA genes,
which allowed amplification from most taxa examined (Table
2).
The only exceptions were
O. marina (often referred to as an
ancestral dinoflagellate [
17] or a predinoflagellate [
18]) and
Exuviaella cassubica, for which all primers failed, likely because
their 18S rRNA gene sequences are significantly divergent. Of
the four pairs of dinoflagellate-specific primers, 18ScomF1-Dino18SR1
and Dino18F1-18ScomR1 showed superior sensitivity and were able
to detect 1 to 10 cells/reaction mixture for most of the dinoflagellates
tested. Primers Dino18F1 and 18Scom R1 was chosen for further
study because they spanned a larger 18S rRNA gene region (1.6
kb).

Detection of picodinoflagellates in Long Island Sound.
Three water samples collected on 8 September 2005 along the
boat dock of the University of Connecticut Avery Point campus
(Long Island Sound) were combined and mixed. Microscopic examination
of a subsample revealed that phytoplankton lineages such as
Nitzschia,
Navicula,
Chaetoceros, and
Eucampia were dominant.
A 2-liter subsample was prescreened (100-µm mesh), and
this was followed by passage through a 3-µm polycarbonate
membrane (Nuclepore, Pleasanton, CA) under a low vacuum pressure
(<10 lb/in
2). One liter of the filtrate was collected and
filtered onto a 0.2-µm-pore-size, 47-mm-diameter polycarbonate
membrane (Nuclepore). The filter membrane was cut into small
pieces using sterile scissors, placed in a 1.5-ml microcentrifuge
tube, and stored at 80°C until DNA extraction. To
examine whether any large plankton were present in the sample,
100 ml of the 3-µm filtrate was filtered onto a 0.2-µm-pore
size, 25-mm-diameter black Poretics polycarbonate membrane (Osmonics
Inc., Minnetonka, MN), fixed with 1% paraformaldehyde, and stained
with 0.005% acridine orange. Observation with an epifluorescence
microscope (Olympus BX51) revealed only small organisms except
for one large cell (length,

12 µm) that appeared to be
a
Heterocapsa cell.
DNA extracted from the <3-µm plankton sample as described above was used for PCR amplification with primers Dino18F1 and 18Scom R1. The PCR was performed using Takara ExTaq DNA polymerase (Takara Mirus Bio, Madison, WI) following the manufacturer's instructions, with an annealing temperature of 58°C. The amplicon was cloned into a TA vector, and 24 of the clones were randomly selected and sequenced (GenBank accession no. DQ386737 to DQ386760). A BLAST search showed that all 24 clones were related to dinoflagellates. These sequences were aligned using CLUSTAL W (1.8) with a Kimura two-parameter model (11). A maximum likelihood tree was inferred using PHYML (5) based on the GTR + I +
model of nucleotide substitution, which was identified as the best-fit model by Modeltest3.7 (16). Species of chlorophytes (as an outgroup), cryptophytes, diatoms, ciliates, apicomplexa, and dinoflagellates (a total of 101 taxa) were initially included in the analysis to obtain a global view of the distribution of the dinoflagellate-like clones. One (clone 12) clustered with the recently recognized parasitic ciliate Cryptocaryon irritans (21) with robust bootstrap support, whereas the other 23 clones clustered with dinoflagellates. In further analyses we focused on dinoflagellates with Toxoplasma gondii (apicomplexa) as the outgroup. The results indicated that 12 of the 23 dinoflagellate-like clones (clones 3, 5 to 7, 9 to 11, 16, 18, 19, 23, and 24) were members of a clade of undescribed eukaryotes comprising previously isolated picoeukaryotes from the Pacific Ocean (Fig. 1). This clade received strong bootstrap support and diverged before all known dinoflagellates (Fig. 1), suggesting that it could be an ancestral clade of dinoflagellates or a lineage that is intermediate between dinoflagellates and apicomplexa. Of the remaining 11 clones, 7 formed a clade with the parasitic dinoflagellate Amoebophrya. Four of these seven clones (clones 4, 8, 17, and 21) clustered tightly with Amoebophrya sp., which infects various dinoflagellate species, and the other three (clones 13, 15, and 20) appeared to be more ancestral. These assignments had moderate to strong support. One of the four other clones (clone 1) was related to a Gymnodiniales-dominated clade and clustered tightly with Gymnodinium simplex and Symbiodinium microadriaticum, and two clones (clones 12 and 14) clustered with Gymnodinium catenatum/Lepidodinium viride. The last clone (clone 2) appeared to be a Heterocapsa species, likely related to the large cell observed under the microscope (see above). To our knowledge, this is the first documentation of the presence of picodinoflagellates in coastal waters.
An increasing number of studies have indicated that field DNA
samples derived from mixed microbial assemblages are prone to
formation of PCR chimeras by cDNA strands from different species,
thus creating artificial, novel genes (
1,
9). To examine whether
any of the sequences obtained in this study was a chimera of
different species in the water sample, sequences of the field-derived
clones, as well as previously reported dinoflagellate sequences
used in this study, were analyzed using the program Bellerophon
(
8). The details of the analysis are shown in Table S1 and Fig.
S1 in the supplemental material. The results indicated that
most clones appeared to be nonchimeric sequences; the only exception
was one clone (clone 20) that was ambiguous.

Wide distribution of diverse and predominantly unknown picodinoflagellates.
Strikingly, one-half of the 24 clones identified in this study
were closely related to undescribed picodinoflagellate lineages
from the Pacific Ocean. Furthermore, the seven clones that clustered
with the parasitic dinoflagellate
Amoebophrya were allied with
lineages from the Pacific Ocean. Separate analyses that included
the shorter sequences from Antarctic deep water (
13) revealed
that these sequences also were closely related to the
Amoebophrya-like
lineages detected in the Pacific Ocean and Long Island Sound
(results not shown). In addition, lineages close to
Gymnodinium/
Symbiodinium have also been found in the Pacific Ocean. Therefore, the distribution
of picodinoflagellates extends from the open ocean to coastal
waters, suggesting that small dinoflagellates are cosmopolitan.
Moreover, the similarity between the dinoflagellate species
composition in Long Island Sound surface water and the dinoflagellate
species composition in the aphotic zone of Antarctica and the
Pacific Ocean (
13,
15), especially the presence of
Amoebophrya,
suggests that heterotrophic and parasitic dinoflagellates may
be more common than currently thought. The ease with which novel
lineages were isolated also suggests that dinoflagellate diversity
has been underestimated. However, this observation should not
be surprising given that even in the larger cell size range
new species have frequently been discovered (e.g.,
Stoeckeria,
Takayama,
Polarella, and
Pfiesteria [
2,
3,
10,
14]). The dearth
of information regarding the lineages of small dinoflagellates
is a result of a lack of targeted analyses.
Interestingly, dinoflagellates have normally been categorized as larger phytoplankton. Recently, LaJeunesse et al. (12) suggested that Symbiodinium (4 to 13 µm) is the lineage containing the smallest dinoflagellates. It is clear now that smaller dinoflagellates are present in both oceanic and neritic waters and that the smallest organism is likely yet to be described. Once the widespread distribution of these picodinoflagellates is verified by culture and morphological analyses, their role in the microbial loop in the world's ocean can begin to be assessed. In addition, given the pressing need for a complete dinoflagellate genome sequence, free-living picodinoflagellates like those described here are likely to be the best candidates for such an attempt. The "normal-size" taxa have human-size (or much larger) genomes (12), which makes the use of current sequencing approaches with these organisms infeasible.

Concluding remarks.
This is the first report of dinoflagellate-oriented primers
and the first documentation of the presence of picodinoflagellates
in coastal waters. Although the number of clones sequenced was
limited, our findings nevertheless revealed the high level of
diversity and the dominance of novel lineages of picodinoflagellates.
Therefore, larger-scale targeted analyses of different oceanic
regions are essential for determining the true biodiversity
of these taxa.

Nucleotide sequence accession numbers.
The nucleotide sequences of the 24 field-retrieved picoplankton
clones have been deposited in the GenBank database under accession
numbers DQ386737 to DQ386760, and the nucleotide sequences of
the 11 dinoflagellate cultures have been deposited in the GenBank
database under accession numbers DQ388456 to DQ388466.
.

ACKNOWLEDGMENTS
We are grateful to Terry Gaasterland of Scripps Genome Center
for access to her computing facility for the phylogenetic analysis
and to Christopher Dungan of the Maryland DNR Cooperative Oxford
Laboratory for kindly providing
Perkinsus species.
This work was supported by National Science Foundation grants DEB-0344186 (to S.L. and H.Z.) and DEB-0107754 and EF-0431117 (to D.B.).

FOOTNOTES
* Corresponding author. Mailing address: Department of Marine Sciences, University of Connecticut, Groton, CT 06340. Phone: (860) 405-9168. Fax: (860) 405-9153. E-mail:
senjie.lin{at}uconn.edu.

Supplemental material for this article may be found at http://aem.asm.org/. 

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Applied and Environmental Microbiology, August 2006, p. 5626-5630, Vol. 72, No. 8
0099-2240/06/$08.00+0 doi:10.1128/AEM.00586-06
Copyright © 2006, American Society for Microbiology. All Rights Reserved.
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