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The first molecular characterization of picocyanobacteria from the Argentine Sea.

1. Introduction

Oxygenic prokaryotic photoautotrophs (Cyanobacteria) were estimated to constitute about 10% of the total ocean marine picoplankton in the upper 200 m [1]. Strains of Synechococcus and Prochlorococcus genera dominate the marine picophytoplankton in the world's oceans and contribute significantly to C[O.sub.2] fixation and primary production [2, 3]. Although both genera often can coexist in tropical and temperate waters, their distribution patterns differ spatially and seasonally [4, 5]. Whereas Prochlorococcus are largely confined to a 40[degrees]N-40[degrees] Slatitudinal band andare mostly abundant in oligotrophic waters, Synechococcus are distributed ubiquitously throughout oceanic regions from polar to tropical waters [6-9].

The use of molecular markers based on PCR amplification of different conserved genes, molecular probes, pyrosequencing, and multilocus sequence analysis allowed defining several Synechococcus genetic lineages using cultured and natural samples from marine environments [7-14]. Marine Synechococcus have been classified into three major subclusters (5.1 to 5.3) [15, 16]. Most strains belong to subcluster 5.1, which contains at least 10 distinct phylogenetic clades according to 16S rRNA sequences [8]. Additional lineages have been proposed based on other sequences, such as 16S-23S rRNA ITS, the N-regulatory ntcA gene, and the encoding sequence of the cytochrome b6 subunit of the cytochrome b6f complex (petB) [9,11,14,17,18].

Analyses of Synechococcus and Prochlorococcus lineage Distribution at local and ocean basin scale were reported using data from cruises in the Pacific, Atlantic, Indian, and Arctic Oceans and in the RedSea [4, 5,13,18-20]. However, there are unexplored oceanic regions, such as the waters of the Southwest Atlantic Ocean [21], where the Argentine shelf and its shelf-break constitute one of the richest regions for marine life [22]. This was supported by global studies using ocean-color satellite images that revealed bright features denoting high chlorophyll concentrations [23, 24]. However, no molecular characterization of the ultraphytoplankton components has been still reported. Therefore, taking into account the importance of this oceanic region, we started the examination of the population diversity of picocyanobacteria, a crucial plankton component for primary productivity.

The aim of this study was to contribute to the knowledge of the global biogeography of prokaryotic components of the marine picophytoplankton. Thus we characterized picocyanobacteria in waters from the Argentine Sea, one of the richest biological areas of the world oceans and a still unexplored region. Our data constitute the beginning of more comprehensive studies in this region, and, importantly, it is a contribution to the knowledge of the Synechococcus diversity.

2. Materials and Methods

2.1. Sample Collection, Strain Isolation, and Characterization. Water samples were collected at 5 m depth in duplicate using Niskin bottles from (i) a permanent coastal station located off Mar del Plata (EPEA) by the cruises conducted monthly onboard the RV "Capitan Canepa" (INIDEP) and (ii) four stations in the Argentine Sea: two from the continental shelf (stations 66 and 27) and two from adjacent waters (oceanic stations 62 and 20), in March 2006 (RV ARA "Puerto Deseado" cruise GEFII, PNUD ARG 02/018 Project) (Figure 1). Temperature and salinity profiles of water column at each station were recorded by a Seabird SBE1901 CTD (Table 1). Samples of 50 mL were fixed with formaldehyde (0.4% final concentration) and filtered by a polycarbonate membrane of 0.2 [micro]m pore size. Synechococcus were characterized by epifluorescence microscopy and carbon biomass was calculated directly from cell number using a conversion factor of 0.21 pg C cell- [25]. Synechococcus isolates were obtained by the serial dilution culture method using f/10 medium without silicate [26].

2.2. DNA Extraction, PCR Amplification, Cloning, and Sequencing. For total DNA extraction from environmental samples, up to 5 L of sea water was collected in surface with a Niskin bottle and transferred through a 200 [micro]m nylon mesh to a black bottle. Samples were prefiltered through a 3 [micro]m Nuclepore membrane (Whatman International Ltd, Maidstone, England) to separate picoplankton and subsequently filtered through a Sterivex unit (Milli-pore, Billerica, MA, USA) with a peristaltic pump. The units were kept in liquid nitrogen on board until arrival to the laboratory and stored at -80[degrees]C before proceeding. The units were incubated at 37[degrees]C for 30 min with lysozyme (1 mg [mL.sup.-1]) and then with proteinase K (0.5 mg [mL.sup.-1]), followed by three freeze-thaw cycles. Finally, DNA was extracted with the DNeasy Plant Mini Kit (Qiagen). DNA from the isolates was extracted as previously described [27].

16S rRNA genes were amplified either from DNA of the isolates or from environmental samples, using primers SYN172F and OXY1313R. This primer pair amplifies all known sequences from Synechococcus subclusters 5.1 (clades I-X [8], some subclusters 5.2 strains, no fresh water Synechococcus strains, all low-light (LL) Prochlorococcus strains, some high light (HL), HLI Prochlorococcus strains, but no HLII Prochlorococcus strains [28]). Three environmental libraries from EPEA sampling during summer time were constructed by ligating PCR products to pGEM-T vectors and introduced into E. coli cells.

The amplification of the nitrogen regulatory gene ntcA (approach that specifically targets cyanobacteria) was used to identify novel Synechococcus clades with considerably higher resolution than the 16S rRNA sequences [11,13]. The primer pair 1F/4R [29] was used to amplify ntcA genes from the isolates. In Table S1 we summarize the oligonucleotide sequences of primer pairs used in this study (see Supplementary Material available online at PCR products were cloned using a pGEM-T Easy kit according to the manufacturer's instructions (Promega Corporation). To screen for Synechococcus 16S rRNA and ntcA clones, inserts were digested with the restriction endonucleases EcoRI and PstI (Promega Corporation), respectively. Plasmid DNA was isolated from three representatives of each restriction pattern, using a QIAprep Spin Miniprep Kit (QIAGEN), and inserts were sequenced (Macrogen, Korea).

2.3. Denaturing Gradient Gel Electrophoresis (DGGE). As a diversity study approach, the environmental samples were analyzed by DGGE. The amplification products of the 16S rRNA genes (either from the isolates or the environmental samples from Patagonian shelf and oceanic waters) were used as templates in a nested PCR with the primer pair 358fGC/907r [30] (Table S1). The amplification products of the 16S rRNA genes from the isolates Syn-EPEA.1 and Syn-GEF.1 were used as references. The products were subjected to DGGE (2001 system, CBS Scientific Company) [30]. A 6% polyacrylamide gel with a gradient of DNA-denaturant agent was casted by mixing solutions of 40 and 80% denaturant agent (100% denaturant agent was 7 M urea and 40% deionized formamide). Electrophoresis was performed at 100 V and 60[degrees]Cfor 18 hinTAE buffer(40 mM Tris-HCl, 20 mM sodium acetate, 1 mM EDTA, pH 7.4). DGGE gels were stained with 100 [micro]L [L.sup.-1] SybrGold (Molecular Probes Europe, Leiden, The Netherlands) in TAE buffer for 45 min, rinsed with the same buffer for 20 min, removed from the glass plate to a UV transparent gel scoop, visualized, and registered by using a Photodyne system apparatus (Photodyne Technologies, LA, USA) [31]. Prominent DNA bands were excised from the DGGE gels and eluted from the gel by sterile water at 4[degrees]Cover night. These eluted products were reamplified with primers 358fGC, without the GC-clamp, and 907r and the PCR products were sequenced.

2.4. Sequence and Phylogenetic Analyses. All 16S rRNA and ntcA gene sequences were first compared with those present in public databases using the basic local alignment search tool BLAST network service ( Phylogenetic trees were constructed with the neighbour-joining and maximum parsimony methods, and bootstrap analyses (1,000 replicates) were done with MEGA version 5 [32].

3. Results and Discussion

3.1. Isolation and Molecular Identification of Two Synechococcus Strains from Coastal and ShelfWaters. For further diversity studies, we initially isolated Synechococcus strains from different regions of the Argentine Sea. In EPEA station, the maximum phytoplankton biomass value was observed during summer (December-March), with being Synechococcus the major contributor [33]. Firstly, from surface waters at this station, we PCR amplified environmental DNA and obtained only three different partial 16S rRNA sequences (EMBL accession numbers HE600704, HE600705, and HE600706), which were 98.9 to 99.7% identical to the sequence of Synechococcus sp. Almo3. Then we isolated under microscope a strain (named Syn-EPEA.1), whose complete 16S rRNA sequence was amplified for molecular characterization (EMBL accession number HE600707), and being around 98.9% identical to sequences of members of the genus Synechococcus.

On the other hand, from shelf waters corresponding to the GEF-III cruise (at a location equivalent to station 27, 61[degrees]48'W47[degrees]22' S),we isolated a picophytoprokaryote strain (named Syn-GEF.1), whose complete 16S rRNA sequence (EMBL accession number HE601900) was 99.8% identical to marine Synechococcus sequences.

To better differentiate between genotypes, we amplified and sequenced ntcA gene fragments from the Syn-EPEA.1 and Syn-GEF.1 isolates (EMBL accession numbers HE601901 and HE601902, resp.). Syn-EPEA.1 and Syn-GEF.1 sequences were about 91.6, 90.6, and 70.2% identical to partial ntcA sequences of Synechococcus sp. WH 8020, CC9311, and RS9905, respectively and 97.9% identical among them.

3.2. Molecular Identification of Synechococcus Strains from Shelf and Adjacent Waters of the Argentine Sea. DGGE technique was used to analyze Synechococcus diversity in shelf and adjacent waters at the Patagonian region of the Argentine Sea. The amplification products of the 16S rRNA genes from the isolates Syn-EPEA.1 and Syn-GEF.1 (used as references) and amplicons from the environmental samples corresponding to stations 66 and 27 (shelf waters) and 62 and 20 (adjacent waters) were subjected to DGGE (Table S1 and Figure 1). Although some bands appeared dispersed across the gel gradient, obvious and representative bands (Figure 2) could be selected for DNA reamplification and further sequencing. All environmental sequences were about 93 to 100% identical to sequences of marine Synechococcus (Table 2). Although bands of samples corresponding to a shelf and adjacent waters migrate at similar positions on the gel (Table 2 and Figure 2), their sequences shown high degree of identity to sequences of different Synechococcus strains: 27.2 and 62.2 bands were 100% and 99.3 identical to CC 9902 and CC 9311, respectively.

3.3. Phylogenetic Analyses. Partial 16S rRNA sequences were aligned with representative sequences of Synechococcus belongingtoclades ItoIX[8] and to clades XV and XVI [9]. Neighbour-joining phylograms were constructed after sequence alignments (Figure 3). Similar tree topologies were observed by maximum parsimony analyses (not shown). The 16S rRNA sequences from the EPEA environmental samples and the two Synechococcus isolates grouped in clade I. For the analysis of ntcA sequences, we also included Synechococcus sequences of clades XI to XIV, which were identified in ntcA phylogenies [11]. The phylogenetic analysis using ntcA sequences showed similar results for the isolates to those obtained with the 16S rRNA sequences (Figure 4), which suggests a good congruence with the two genetic markers used. On the other hand, whereas most of the 16S rRNA sequences obtained from the DGGE bands produced significant alignments with Synechococcus sequences belonging to clade I, three sequences from shelf waters (66 and 27) grouped with those ofclade IV, and another one from station 62 clustered with sequences of subcluster 5.3 (Table 2 and Figure 3).

According to our results, clade I Synechococcus seems to be the most common group in the Southwest Atlantic from latitude 38[degrees]S to 48[degrees]S. Also, sequences from clade IV were found at 43[degrees]S and 47[degrees]S at the Patagonian shelf(stations 66 and 27) but not in oceanic waters. The coexistence of clades I and IV has been well-documented in other mesotrophic temperate regions (latitudes above 30[degrees]N/S), and the ratio of abundances of the two clades is likely to vary both spatially and temporally suggesting that both clades are adapted to high-nutrient/low-temperature waters [4, 5, 19, 34, 35]. Interestingly, comparative genome studies show that strains of those clades lack regulatory genes that are important for phosphate scavenging when this nutrient is under limiting conditions [16]. Yet, there is a glaring lack of understanding about the genetic and physiological features that allow clades I and IV to compete with other Synechococcus clades in mesotrophic regions. Strikingly, our data show an extraordinarily high level of biomass (287.7 [micro]gC [L.sup.-1])in station 27 (Table 1), which could be ascribed exclusively to picocyanobacteria (Silva, personal communication). A recent report, studying six Synechococcus strains isolated along a gradient of latitude in the North Atlantic Ocean, revealed the existence of lineages of marine Synechococcus physiologically specialized in different thermal niches, suggesting the existence of temperature ecotypes within the marine Synechococcus radiation [36]. Moreover, the authors suggest that clade I and probably clade IV Synechococcus have a physiology preferentially adapted to cold thermal niches. Our results are in line with those findings since the range of water temperatures at the sites of sampling was between 10.6 and 14.7[degrees]C (Table 1).

Finally, a sequence belonging to subcluster 5.3 (formerly included in clade X [8]) was detected in the oceanic station 62. Synechococcus subcluster 5.3 has been recently reestablished [15, 16] and includes Synechococcus RCC307 [9], KORDI-15, and KORDI-30 [17]. Much less is known about the biogeography of those Synechococcus strains compared with subcluster 5.1 [18]. Our results showed that members of the subcluster 5.3 are also present in oceanic waters.

4. Conclusions

This study is the first report on the molecular characterization of Synechococcus in the Southwest Atlantic Ocean, contributing to the knowledge of their global distribution. Synechococcus were identified not only in coastal waters, as reported in EPEA, a permanent coastal station located off Mar del Plata [37], but also in the shelf and oceanic waters.

While Synechococcus clade IV sequences could only be retrieved from Patagonian shelf waters (stations 66 and 27), Synechococcus clade I seems to be widespread in the Argentine Sea, from latitude 38[degrees]S to 48[degrees]S. Moreover, strains of clades I and IV, suggested as low temperature ecotypes [36], can coexist at the Patagonian shelf (stations 27). The cooccurrence of both ecotypes could be associated with the biomass increment in station 27; however, further studies are needed to support this speculation. Data presented are a starting point to evaluate the role of Synechococcus ecotypes, as powerful bioindicators to monitor the impact of possible climatic changes in the South Atlantic Ocean. However, a large-scale and a long-term effort will be needed to understand seasonality and population dynamic not only of picocyanobacteria but also of other ultraphytoplankton components.

Conflict of Interests

The authors declare that there is no conflict of interests regarding the publication of this paper.


This project was supported by CONICET (Project no. 134), INIDEP, PNUD ARG 02/018 Project, Universidad Nacional de Mar del Plata (EXA 644/645), and Fundacion para Investigaciones Biologicas Aplicadas (FIBA).


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Macarena Perez-Cenci, (1) Gonzalo F. Calo, (1) Ricardo I. Silva, (2) Ruben M. Negri, (2) and Graciela L. Salerno1

(1) Instituto de Investigaciones de Biodiversidad y Biotecnologia (INBIOTEC-CONICET), Centro de Investigaciones Biologicas (CIB-FIBA), Vieytes 3103, 7600 Mar del Plata, Argentina

(2) Instituto Nacional de Investigacion y Desarrollo Pesquero (INIDEP), Paseo Victoria Ocampo No. 1, 7600 Mar del Plata, Argentina

Correspondence should be addressed to Graciela L. Salerno;

Received 31 May 2014; Revised 2 October 2014; Accepted 3 October 2014; Published 20 November 2014

Academic Editor: Jakov DulCic

TABLE 1: Localization and environmental parameters of
Patagonian stations at the Argentine Sea. Data were registered
by the Instituto Nacional de InvestigaciOn y Desarrollo Pesquero
(INIDEP), Gabinete de Oceanografia Fisica, Base Regional de
Datos Oceanograficos (BaRDO).

Station     Date                 Location               Depth (m)

20        13-03-06   58[degrees]53'W 47[degrees]19'S       208
27        16-03-06   61[degrees]48'W 47[degrees]22'S       130
62        29-03-06   58[degrees]46'W 43[degrees]52'S       201
66        29-03-06   61[degrees]25'W 43[degrees]20'S      88.0

Station   Temperature    Salinity    Abundance cell
          ([degrees]C)                m[L.sup.-1]

20           10.945       34.061       10 (2.1) *
27           13.076       33.564    1,370 (287.7) *
62           10.631       33.952      65 (13.7) *
66           14.730       33.553       26 (5.5) *

Numbers in brackets indicate biomass expressed
in [micro]g [CL.sup.-1].

TABLE 2: Analysis of 16S rRNA sequences from the
DGGE excised bands (Figure 2) of environmental
samples from the Argentine Sea. The isolated
strains Syn-EPEA.1 and Syn-GEF.1 were used
as reference. E values of all sequences were 0.0.

Site    Sample           Bands     Closest relatives

GEF     Syn GEF.1        GEF.1     Synechococcus sp. Almo316S
                                   rRNA gene, partial sequence.

                         GEF.2     Synechococcus sp. Almo3 16S
                                   rRNA gene, partial sequence.

EPEA    Syn EPEA.1      EPEA.1     Synechococcus sp. Almo3 16S
                                   rRNA gene, partial sequence.

                         EPEA.2    Synechococcus sp. Almo3 16S
                                   rRNA gene, partial sequence.

27      Environmental     27.1     Synechococcus sp. CC9311 16S
                                   rRNA gene, partial sequence.

                          27.2     Synechococcus sp. CC 9902,
                                   complete genome.

20      Environmental     20.1     Synechococcus sp. Almo3 16S
                                   rRNA gene, partial sequence.

66      Environmental     66.1     Synechococcus sp. CC9902,
                                   complete genome.

                          66.2     Synechococcus sp. CC 9902,
                                   complete genome.

62      Environmental     62.1     Synechococcus sp. RCC307
                                   genomic DNA sequence.

                          62.2     Synechococcus sp. CC9311 16S
                                   rRNA gene, partial sequence.

Site    Identity (%)        Clade        Accession number

GEF         99.8              I             HE792894

            100               I             HE687328

EPEA        99.6              I             HE687320

            99.8              I             HE687321

27          100               I             HE687322

            100              IV             HE687323

20          99.6              I             HE687324

5           99.6             IV             HE792895

            100              IV             HE687325

62          93.5       subcluster 5.3       HE687326

            99.3              I             HE687327
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Title Annotation:Research Article
Author:Perez-Cenci, Macarena; Calo, Gonzalo F.; Silva, Ricardo I.; Negri, Ruben M.; Salerno, Graciela L.
Publication:Journal of Marine Biology
Article Type:Report
Date:Jan 1, 2014
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