Polar algal communities impact (Lutz et al., 2016) and are impacted by (Brown and Arrigo, 2013) ice melting cycles. The tight links between phytoplankton diversity/production and sea ice dynamics are beginning to be decoded and seem to be fairly complex (Arrigo et al., 2014; Olsen et al., 2017). Due to increased light availability and vertical mixing, the shrinking of pack ice and the shift from thick multi-year ice to thinner first-year ice has been linked to enhanced Arctic primary production (Arrigo et al., 2008; Brown and Arrigo, 2013). However, the salinity decrease in surface waters, resulting from higher ice melting rates and increased river run off, leads to an increase in water column stratification which in turn may impact nutrient availability and plankton diversity (Li et al., 2009). The presence of ice-associated algae may impact the quantity (Leu et al., 2011; Kohlbach et al., 2016) and quality (Duerksen et al., 2014; Schmidt et al., 2018) of secondary production at high latitudes, as well as the recruitment of ice-associated diatoms to the water column (Kauko et al., 2018). Climate-related changes can also increase Arctic vulnerability to invasive species (Vincent, 2010) as the intrusion of warmer waters “atlantifies” the Arctic Ocean (Årthun et al., 2012) and temperate phytoplankton move northwards, replacing Arctic communities (Neukermans et al., 2018).
Massive Arctic phytoplankton blooms have been detected not only along the ice edge (Perrette et al., 2011), but also extending large distances under the pack ice (Arrigo et al., 2012). The increasingly thin pack ice and the formation of melt ponds may favor areas experiencing sub-ice bloom formation that may reach almost one third of the ice-covered Arctic Ocean in the summer (Horvat et al., 2017).
The Arctic phytoplankton community exhibits strong seasonal variability (Sherr et al., 2003), with smaller organisms (picoplankton) dominating during winter and early summer, followed by diatoms during the spring bloom (Marquardt et al., 2016). The green alga Micromonas (Mamiellophyceae) is recognized as the dominant picophytoplankton (0.2–3.0 μm) genus during the Arctic summer (Lovejoy et al., 2007; Balzano et al., 2017). The genus Micromonas is widespread throughout the world oceans (Worden et al., 2009; Tragin and Vaulot, 2019) and genetically diversified (Simon et al., 2017) in relation to thermal niches (Demory et al., 2018), with one species, Micromonas polaris, restricted to polar regions. Another species of Mamiellophyceae, Bathycoccus prasinos, may replace M. polaris during polar winter (Joli et al., 2017).
Regarding the more diverse Arctic nano-phytoplankton, the genus Pyramimonas has often been reported (Lovejoy et al., 2002; Joli et al., 2017) displaying high intra-generic diversity (Daugbjerg and Moestrup, 1993; Balzano et al., 2012) and associated with sea ice (Harðardóttir et al., 2014; Kauko et al., 2018). The mamiellophyte Mantoniella is reported to a lesser extent in Arctic waters (Lovejoy et al., 2007; Terrado et al., 2013; Joli et al., 2017), although diversity within this genus seems to be higher than other polar Mamiellophyceae (Yau et al., 2019). Other commonly observed Arctic taxa include the bloom-forming genus Phaeocystis (Assmy et al., 2017), unidentified Pelagophyceae, the mixotrophic and cosmopolitan Dinobryon faculiferum, and the genus Chlamydomonas (Lovejoy et al., 2002; Balzano et al., 2012; Terrado et al., 2013; Crawford et al., 2018).
Large size classes of polar phytoplankton are dominated by diatoms and dinoflagellates (Crawford et al., 2018). Diatoms constitute a large fraction of polar phytoplankton communities, especially in coastal areas and during episodic upwelling (Sherr et al., 2003; Arrigo et al., 2014), impacting carbon flux to the benthic community (Booth et al., 2002). This group is particularly important during late spring/summer months in the pelagic environment (Lovejoy et al., 2002; Balzano et al., 2012), but also comprises a significant portion of protist biomass during young ice formation (Kauko et al., 2018) and of taxa diversity in first-year ice during the dark Arctic winter (Niemi et al., 2011). Successional patterns in diatom diversity are observed during Arctic spring bloom development, possibly linked with temperature optima or transportation from lower latitudes (Quillfeldt, 2000). The genera most often reported among Arctic centric diatoms are Chaetoceros and Thalassiosira (Lovejoy et al., 2002; Johnsen et al., 2018). Chaetoceros gelidus and Chaetoceros neogracilis often dominate Arctic phytoplankton assemblages (Katsuki et al., 2009; Crawford et al., 2018), although other species such as Chaetoceros decipiens or Chaetoceros furcellatus have also been reported (Joo et al., 2012; Johnsen et al., 2018). Thalassiosira is a diverse genus with both Arctic, ice-associated and subpolar/temperate water representatives (Luddington et al., 2016), in particular Thalassiosira nordenskioeldii and Thalassiosira antarctica var. borealis (Quillfeldt, 2000; Lovejoy et al., 2002; Johnsen et al., 2018). High abundances of pennate diatoms are linked to late autumn/winter sea ice (Niemi et al., 2011) and bottom communities (Kauko et al., 2018; Leeuwe et al., 2018). The most commonly reported genera include Cylindrotheca, Fragilariopsis, Navicula, Nitzschia and Pseudo-nitzschia (Katsuki et al., 2009; Poulin et al., 2011; Leeuwe et al., 2018). In contrast to diatoms and small flagellates that present a strong seasonal signal, dinoflagellates are prevalent throughout the year (Comeau et al., 2011; Marquardt et al., 2016), although some taxa vary seasonally (Onda et al., 2017).
Culturing efforts in the Arctic have been scarce, with one campaign in early spring in northern Baffin Bay in 1998 (Potvin and Lovejoy, 2009) and the MALINA cruise in summer 2009, which covered the Northeast Pacific Ocean, the Bering Strait, the Chukchi and Beaufort Seas (Balzano et al., 2012, 2017). As microbial communities respond to the rapid loss in Arctic ice cover and thickness (Vincent, 2010; Comeau et al., 2011), efforts to culture phytoplankton from the region are important in order to have at our disposal reference strains whose physiology and taxonomy can be studied in the laboratory under controlled conditions. In the present work, Baffin Bay samples from both an ice camp at a fixed station and an icebreaker cruise were obtained for phytoplankton isolation before, during and at the peak of the Arctic spring bloom. More than 1,000 cultures were obtained by serial dilution, single cell pipetting and flow cytometry (FCM) cell sorting, characterized by partial 18S rRNA sequencing and optical microscopy and de-replicated to a subset of 276 strains presented here.
The Green Edge project (http://www.greenedgeproject.info) aimed at investigating the dynamics of the Arctic spring bloom at the ice edge. Samples for phytoplankton isolation were obtained both at a fixed station (Ice Camp) and during a cruise onboard the Canadian icebreaker CCGS Amundsen.
The ice camp (IC) was set up near the Inuit village of Qikiqtarjuaq, Nunavut, on Baffin Island (67° 28’ N, 63° 47’ W), in a location identified to have little influence from continental drainage (Figure 1). To observe the changes in the phytoplankton community during the ice melting process, sampling was carried out between 4 May and 18 July 2016. Samples were collected in the water column under the ice at two depths three times a week and from melted ice cores once per week. The ice cores were melted at room temperature with the addition of 0.2 μm filtered sea water prior to isolation procedures.
The Amundsen cruise (AM) took place between 3 June and 14 July 2016 in Baffin Bay, Canada, between 60°N and 70°N. (Figure 1). Sampling transects were designed to cross the marginal ice zone perpendicularly in order to observe changes in the phytoplankton community from open water to solid sea ice (Figure 1). Seawater for isolation was sampled approximately every two days at two depths with Niskin bottles mounted on a CTD frame Sea-Bird SBE-911 plus.
The development of the spring phytoplankton bloom at the IC site was monitored by flow cytometry (Massicotte et al., 2020), and its phases were defined as follows: ‘pre-bloom’ from 4 May to 23 May; ‘bloom-development’ from 24 May to 22 June and ‘bloom-peak’ from 23 June to 18 July. AM strains were not related to bloom phases due to spatial variability across the marginal ice zone during sampling.
Several isolation strategies were employed in order to maximize the number and diversity of cultures retrieved. Different pre-isolation procedures were applied to different samples, which included filtration, concentration and enrichment. In order to target the smaller plankton size fractions, samples were gravity pre-filtered with 3 μm and 0.8 μm filters prior to enrichment or serial dilution, as described previously (Le Gall et al., 2008; Balzano et al., 2017). Some samples were concentrated with tangential flow filtration (Vivaflow Cartridge 200, Sartorius) with a 0.2 μm polyethersulfone membrane using 2 L of seawater or 0.5 L of ice core melted into filtered seawater (roughly 1 volume of ice for 5 volumes of sea water). Enrichment was performed by mixing 25 mL of pre-filtered seawater with 1 mL of L1 (Guillard and Hargraves, 1993) or PCR-S11 culture medium (Rippka et al., 2000) (media recipes at http://roscoff-culture-collection.org/protocols/media-recipes). Diatom proliferation was prevented in some cultures by the addition of GeO2 (Sigma-Aldrich, St-Quentin-Fallavier, France) at 9.6 μM.
Isolation from enriched samples was performed by single cell pipetting or by FCM cell sorting (Marie et al., 2017). A FACSAria® cytometer (Becton Dickinson, San José, CA, USA) equipped with a 488-nm laser was used for cell sorting. Acquisition was triggered on red fluorescence and sorting was performed in “single cell” mode using 20 PSI as sheath pressure. Filtered seawater (0.22 μm) was used as sheath fluid. Cells were sorted into 48-well plates containing 1 mL of L1 medium supplemented with 0.01% bovine serum albumin. Three days after sorting, a mixture of penicillin, neomycin, and streptomycin (PNS, Ref P4083; Sigma) was added to each well at a final concentration of 0.1%. Cell growth was monitored by flow cytometry and microscopy after 2 weeks.
For serial dilution either 500 or 50 μL of water sample was added to 15 mL of L1. Then, 24 wells of a Greiner Bio-One™ 96 Deep Well plate (Dominique Dustscher, Brumath, France) were filled with 0.5 mL of each dilution. Wells were later screened by optical microscopy and with a Guava® (Merck, Darmstadt, Germany) flow cytometer. Unialgal wells were transferred to ventilated T-25 CytoOne® flasks (Starlab, Orsay, France) with 15 mL of L1 media.
All cultures were incubated at 4°C with a 12:12 light–dark cycle and transferred to new medium once a month. Light intensity was approximately 100 μmole photons.m–2.s–1. The isolation method, culture medium and environmental conditions for each strain are reported in Supplementary Data S1.
Cultures were screened and de-replicated by optical microscopy and partial 18S rRNA sequences (see below). We aimed to keep, whenever possible, one strain of each taxon per sampling day and per depth. After de-replication, 416 strains were added to the Roscoff Culture Collection (http://www.roscoff-culture-collection.org) of which 276 were chosen to be described in this paper based on 18S rRNA sequence quality and reliability of culture growth.
Strains were identified using partial 18S rRNA sequences. DNA was extracted directly from the cultures by a simple heating cycle of 95°C for 5 min, prior to PCR. A DNA extraction with NucleoSpin Plant II kit (Macherey-Nagel) was performed following the manufacturer’s instructions for thick-walled or low concentration strains. For 18S rRNA amplification the primers 63F (5’-ACGC-TTGTCTCAAAGATTA-3’) and 1818R (5’-ACGGAAACCTTGTTACGA-3’) (Lepère et al., 2011) were used. PCR amplification was performed in a 10 μL mix containing 5 μL of Phusion High-Fidelity PCR Master Mix® 2×, 0.3 μM final concentration of primer 63F, 0.3 μM final concentration of primer 1818R, 1 μL of DNA and H2O. Thermal conditions were: 98°C for 5 min, followed by 35 cycles of 98°C for 20 s, 55°C for 30 s, 72°C for 90 s, and a final cycle of 72°C for 5 min. The PCR products were sent for sequencing at Macrogen Europe (https://dna.macrogen-europe.com) using the internal primer 528F (5’-CCGCGGTAATTCCAGCTC-3’) (Zhu et al., 2005).
Partial sequences were compared with those available in Genbank using the BLAST plugin in Geneious 10 (Kearse et al., 2012). Sequences were aligned using the ClustalW2 (Larkin et al., 2007) plugin in Geneious 10 and grouped into phylotypes with 100% sequence similarity. Phylotypes represented by more than one strain are listed in Supplementary Data S1. Depending on general sequence quality, partial 18S rRNA sequence alignments were built for each group, including: 49 sequences with 436 nucleotide positions for pennate diatoms, 36 sequences with 612 positions for centric diatoms, 27 sequences with 392 positions for other members of the Heterokontophyta, 52 sequences with 361 positions for Chlorophyta, 10 sequences with 638 positions for Cryptophyta, 11 sequences with 692 positions for Haptophyta, and 6 sequences with 372 positions for Alveolata (Dinophyta). Phylogenetic trees were built using FastTree v2.1.11 (Price et al., 2010) as implemented in Geneious 10. Alignments are available from https://github.com/vaulot/Paper-2019-Ribeiro-GE-cultures.
One strain per phylotype representative of the 18S rRNA genetic diversity was chosen for optical light microscopy (LM). Using a Nikon Eclipse 80i (Nikon) with a 100× objective and differential interference contrast, pictures of live cultures were captured with a SPOT digital camera (Diagnostics Instruments, Sterling Heights, MI, USA).
In the present study, partial 18S rRNA gene sequences and light microscopy were used to characterize 276 Arctic strains obtained during the Green Edge campaign (Supplementary Data S1), 77 and 199 isolated from ice and water samples, respectively (Figure 2). By combining different pre-isolation and isolation techniques we were able to retrieve 276 strains assigned to 57 phylotypes characterized by 100% similarity of partial 18S rRNA sequencing. A significant level of novelty exists within these strains, as almost 60% of the representative sequences of phylotypes did not match any sequence from previously cultured strains (Table 1) and more than 40% did not match any existing sequence from environmental datasets. The sequence of one strain (RCC5319) had only a 95.3% match to any existing sequence. Strains belonged to 5 divisions (Table 2): Heterokontophyta (208), Chlorophyta (44), Cryptophyta (16), Haptophyta (4), and Dinophyta (4). Diatoms were by far the most abundant group (193), with the genera Chaetoceros (42) and Attheya (40), followed by Synedra (23), Thalassiosira (18), Naviculales (18) and Fragilariopsis (17), being the most represented. The flagellates Baffinella (13) and Pyramimonas (24) were the most abundant non-diatom genera. With 10 strains, Micromonas polaris dominated picoplanktonic isolates, although one strain of Bathycoccus prasinos was also isolated. Four strains of dinoflagellates assigned to the genus Biecheleria were retrieved from samples from the Amundsen cruise. The level of novelty varied between the different taxonomic groups and, for some classes such as Chlorophyceae and Cryptophyceae, we did not recover any strains corresponding to novel 18S rRNA sequences (Figure S1).
|Phylotype novelty1||Number of phylotypes|
|previously observed but not cultured||9|
|not previously observed||24|
The Cylindrotheca sp. phylotype represented by RCC5303 contains two strains from ice core samples from the pre-bloom and bloom-development phases (Supplementary Data S1). Cells are solitary with two chloroplasts, a long apical (>35 μm) and short transapical axis (~3 μm) (Figure 3R). Cylindrotheca is a genus frequently observed in the Arctic, mainly represented by the cosmopolitan species complex C. closterium (Lovejoy et al., 2002; Li et al., 2007; Katsuki et al., 2009; Poulin et al., 2011). However, sequences from the strains obtained in this study branched apart from C. closterium (Figure 4), but grouped with 100% identity with an uncultured Cylindrotheca sequence from the Arctic (GenBank JF698839). The sequence of Cylindrotheca sp. RCC5216, also isolated from an IC ice core sample (Supplementary Data S1), differed from that of Cylindrotheca sp. RCC5303 by two base pairs. Cells of RCC5216 are curved to sigmoid, forming coarse aggregates, with 17–20 μm apical and ~4 μm transpical axes (Figure 3B).
The Fragilariopsis cylindrus phylotype represented by RCC5501 groups 17 strains originating from all main sampling sites, substrates and phases of the bloom (Supplementary Data S1). The 18S rRNA sequence matched with 100% similarity the Arctic F. cylindrus strain RCC4291 (Figure 4), a known cold-adapted diatom (Mock et al., 2017), used as an indicator of polar water and ice (Quillfeldt, 2004). Cells have a short apical axis (~4 μm), rounded ends, and a transapical axis of approximately 3 μm length (Figure 3U).
Navicula ramosissima strain RCC5373 was retrieved from an ice core sample from the pre-bloom period and shared 100% similarity with Navicula ramosissima strain TA439 from the Yellow Sea and Navicula sp. strain ECT3499 obtained from the skin of Florida manatees (Figure 4). Cells are solitary, lanceolate, with apical and transpical axes of ~25 μm and 7 μm, respectively, two elongated chloroplasts on each side of the girdle, and large lipid bodies (Figure 3I). Interestingly, none of the Navicula spp. strains recovered in this study were related to previous polar strains or environmental sequences, despite this genus being diverse (Katsuki et al., 2009) and abundant in the Arctic (Poulin et al., 2011; Kauko et al., 2018).
Navicula sp. strain RCC5374 was recovered from an ice core sample from the bloom-development phase. The sequence of this strain is not very closely related to those of previously reported polar Navicula, but is 99.2% similar to strain RCC5373 and 99.7% similar to strain KSA2015-19 from the Red Sea (Figure 4). Cells have a ~25 μm apical axis, slightly radiating valvar striae and rostrate ends (Figure 3J).
The Naviculales phylotype represented by RCC5564 contains 12 strains from all phases and sampling sites (Supplementary Data S1). Its sequence is 99.7% similar to Naviculales strain CCMP2297 from northern Baffin Bay and to uncultured sequences from the Arctic (Figure 4). Cells have ~3 μm apical and 5 μm pervalvar axes. They are solitary or form short chains (Figure 3AC).
The Naviculales phylotype represented by RCC5387 contains four strains from IC water and ice samples (Supplementary Data S1). Its sequence has low similarity to sequences from GenBank or to the phylotype represented by RCC5564, sharing only 96.9% similarity with strain CCMP2297 (Naviculales) (Figure 4). Cells are elongated, mainly solitary, with up to 6 μm apical and 3 μm pervalvar axes (Figure 3K).
The Naviculales phylotype represented by RCC5402 has two strains, both retrieved from IC ice cores during the pre-bloom period (Supplementary Data S1). Their sequence shares 99.2% identity with the Bacillariophyta MBIC10102 strain from the Pacific Ocean and groups with Naviculales sequences with strong bootstrap support (91%, Figure 4). Cells are small ~4 μm long and 2 μm wide, sometimes solitary, but mainly forming large aggregates (Figure 3O).
The Nitzschia sp. phylotype represented by RCC5489 contains three strains from both sampling sites and substrates (Supplementary Data S1). Its sequence has no close similarity to any GenBank sequence from strains besides RCC5390 (Figure 4). Cells are ~11 μm wide, mainly solitary or forming small aggregates (Figure 3L). Members of the genus Nitzschia are often reported to thrive in the Arctic (Johnsen et al., 2018; Kauko et al., 2018), with Nitzschia frigida, for example, being considered as the single most important diatom associated with sea ice (Rózanska et al., 2009; Leu et al., 2015). Surprisingly, none of the Nitzschia spp. strains isolated in this study had high 18S rRNA similarity to other known polar strains. They did, however, have high similarity with Arctic environmental sequences (Figure 4).
Nitzschia sp. RCC5390 was retrieved from an IC pre-bloom sample (Supplementary Data S1) and its sequence is the closest to RCC5489 (99.8% similarity, Figure 4). Cells have 7 μm apical axis and 5 μm pervalvar distance, forming ribbon-like colonies (Figure 3M).
Nitzschia sp. RCC5391 was isolated from an ice core sample during the pre-bloom period. Its sequence matches with only 97.8% similarity that of a strain TA394 (Nitzschia paleaeformis) from the Yellow Sea (Figure 4). Cells are solitary lanceolate with bluntly rounded apices, measuring ~10 μm and 2 μm for the apical and transapical axes, respectively (Figure 3N).
Nitzschia sp. RCC5458 was also retrieved from an ice sample from the pre-bloom period and its sequence is 98.1% similar to Nitzschia sp. strain KSA2015-49 from the Red Sea (Figure 4). Cells are linear to lanceolate and larger than other Nitzschia strains retrieved in this study, with an apical axis up to 15 μm (Figure 3P).
Nitzschia sp. RCC5510 was isolated from AM waters (Supplementary Data S1). Its sequence is 98.6% similar to Nitzschia sp. strain KSA2015-38 from the Red Sea (Figure 4). It is the only strain from this genus recovered only from AM. Its sequence branches apart from all other Nitzschia sp. (Figure 4). Cells are almost round in the valvar view and rather small (apical axis ~4 μm) compared to the other Nitzschia strains isolated here (Figure 3W).
The Pseudo-nitzschia arctica phylotype represented by RCC5469 contains nine strains of the recently described P. arctica (Percopo et al., 2016), all originating from IC (Supplementary Data S1). Their sequence is 100% similar to P. arctica RCC2004 (Figure 4), a potentially endemic species with a wide distribution in the Arctic (Percopo et al., 2016; Balzano et al., 2017). Only solitary cells were observed, with lanceolate shape in valvar view, measuring ~50 μm and 3 μm for the apical and transapical axes, respectively (Figure 3S).
Sellaphora sp. strain RCC5460 was retrieved during pre-bloom from an IC ice core sample. Its sequence matches with 99% similarity that of the freshwater Sellaphora pupula strain SM-BLCAP (Figure 4). Cells are small, with 5 μm apical and 4 μm pervalvar axes, solitary or forming aggregates (Figure 3Q). S. pupula is a species complex containing many pseudo- and semi-cryptic representatives capable of thriving in a wide range of environmental conditions (Poulíčková et al., 2008). Further molecular/morphological analyses are needed to properly assign this phylotype.
The Synedropsis hyperborea phylotype represented by RCC5291 contains only two strains, from both IC and AM (Supplementary Data S1). Its sequence shares 100% similarity with S. hyperborea strain CCMP1423 (Figure 4), although members of the Fragilariaceae are not well resolved by 18S rRNA (Balzano et al., 2017). Cells are solitary or in pairs, exhibiting great variability in shape, which is attributed to vegetative cell division (Hasle et al., 1994). The apical axis is ~14 μm (Figure 3D). S. hyperborea is an Arctic species with circumpolar distribution, often found in association with sea ice and as an epiphyte of Melosira arctica (Hasle et al., 1994; Assmy et al., 2013).
The Synedra sp. phylotype represented by RCC5535 comprises twenty-three strains of which fifteen were isolated from the AM and the other eight from within or under the IC ice (Figure 4). Its sequence shares 100% identity with other Arctic strains such as Fragilariales RCC2509. Cells vary considerably in shape, from almost linear to lanceolate and sometimes asymmetrical in the valvar central area. Apical and transapical axes are ~13 μm and 3 μm, respectively (Figure 3AA).
The Actinocyclus sp. phylotype represented by RCC5608 comprises two strains isolated from AM waters (Supplementary Data S1). Its sequence shares 100% similarity with a clone from the Arctic (EU371328), and 99.8% with the Actinocyclus sp. MPA-2013 isolate from the Pacific Ocean (Figure 5). Cells have a pervalvar axis (13–17 μm) longer than the valvar diameter (~5 μm) and discoid chloroplasts (Figure 3AG). Although sometimes spotted in low abundance (Katsuki et al., 2009; Crawford et al., 2018), this genus may dominate phytoplankton biomass in Arctic spring blooms (Lovejoy et al., 2002).
Coscinodiscus sp. strain RCC5319 was isolated from an IC under-ice sample at the peak of the bloom (Supplementary Data S1). The sequence is only 95% similar to that of C. jonesianus isolate 24VI12 (KJ577852) (Figure 5). Unfortunately, this strain was lost and no images are available. Coscinodiscus may be abundant under the ice pack (Duerksen et al., 2014) and is often reported in Arctic diversity studies (Booth et al., 2002; Lovejoy et al., 2002).
The Arcocellulus sp. phylotype represented by RCC5530 contains three strains isolated from 17-m depth from the AM (Supplementary Data S1). Their sequence is 100% similar to RCC2270 Arcocellulus cornucervis (Figure 5). However, 18S rRNA sequences do not have enough resolution to separate Arcocellulus sp. from closer groups such as Minutocellulus sp. (Balzano et al., 2017), requiring further analyses for proper assignation. Cells are small (~5 μm) and solitary (Figure 3X). The cold-adapted A. cornucervis has been reported to be part of the protist community in the Arctic (Blais et al., 2017), including in Baffin Bay in early summer (Lovejoy et al., 2002).
The Attheya septentrionalis phylotype represented by RCC5567 comprises 26 strains from all substrates and sampling sites, from bloom-development and bloom-peak phases (Supplementary Data S1). Their sequence shares 100% similarity with the Arctic strain RCC1988 (Figure 5). Cells are lightly silicified with ~6 μm pervalvar axis and horns up to two times the cell length. They are either solitary or form big aggregates (Figure 3AD). A. septentrionalis is often reported in abundance in Arctic waters and ice (Assmy et al., 2013; Balzano et al., 2017), outcompeting pennate diatoms in high-luminosity/low nutrient conditions (Campbell et al., 2017).
The Attheya longicornis phylotype represented by RCC5555 contains 14 strains, 11 of which were retrieved from AM water samples (Supplementary Data S1). Sequences are 100% identical to the Arctic A. longicornis strains RCC4284 and CCMP214 (Figure 5). Cells are often solitary or in short chains, with horns up to three times the length of the pervalvar axis (Figure 3AB). Together with A. septentrionalis, A. longicornis can comprise a significant portion of the diatom community in Arctic sea ice (Campbell et al., 2017).
Bacterosira bathyomphala strain RCC5328 was retrieved from an ice core sample and its sequence shares 99.8% identity with the Arctic Bacterosira sp. RCC4297 and with B. bathyomphala strain NB04-B6 from an estuary (Figure 5). Cells (~9 μm pervalvar axis) form short and tight chains with contiguous valves (Figure 3F). B. bathyomphala is often reported in northern and polar waters (Crawford et al., 2018; Johnsen et al., 2018), especially where silicate concentration is high (Luddington et al., 2016).
The Chaetoceros neogracilis phylotype represented by RCC5210 contains 33 strains retrieved from all sites, substrates and phases of the bloom (Supplementary Data S1). Its sequences share 100% similarity with polar C. neogracilis strains (e.g. RCC2506). The 18S rRNA gene does not, however, have enough resolution to differentiate within C. neogracilis clades (Balzano et al., 2017). Cells are small, solitary or forming aggregates, with the pervalvar axis slightly longer than the valvar diameter (4 μm) (Figure 3A). The genus Chaetoceros is abundant in temperate and polar waters (Lovejoy et al., 2002;, Malviya et al., 2016) and C. neogracilis dominates the nanophytoplankton community in surface waters in the Beaufort Sea in the summer (Balzano et al., 2012a).
The Chaetoceros gelidus phylotype represented by RCC5266 contains eight strains from all substrates and sampling sites, but only from the bloom-development and bloom-peak periods (Supplementary Data S1). Their sequences were 100% similar to those of the Arctic strains RCC4290 and RCC1992 (Figure 5). Cells are rectangular (~6 μm), forming small, tight chains with narrow apertures and long inner setae, up to 25 μm (Figure 3C). C. gelidus is a recently described species, previously considered as a Chaetoceros socialis ecotype, and is characteristic of northern temperate and polar waters (Chamnansinp et al., 2013). It is reported to form blooms (Booth et al., 2002) and can represent an important fraction of diatom abundance and biomass in Baffin Bay (Crawford et al., 2018).
Chaetoceros decipiens strain RCC5606 was isolated from 30-m depth in AM water (Supplementary Data S1). Its sequence is 99.8% similar to Arctic strain C. decipiens RCC1997 (Figure 5). Cells (~10–30 μm apical axis) have very long inner setae (>100 μm) and form short, semi-circular colonies (Figure 3AF), which contrasts with previous morphological descriptions of C. decipiens (Hasle and Syvertsen, 1997; Balzano et al., 2017), indicating that it might correspond to a new phylotype. This cosmopolitan species has frequently been reported in the Arctic, both in ice and open waters (Lovejoy et al., 2002; Joo et al., 2012; Johnsen et al., 2018).
Eucampia groenlandica RCC5531 strain was retrieved from 30 m depth during the Amundsen cruise. Its sequence shares 100% similarity with E. groenlandica Arctic strain RCC2038 (Figure 5). Cells are lightly silicified with varying sizes, forming straight or moderately curved colonies (Figure 3Y). E. groenlandica was first reported in Baffin Bay (Cleve, 1896) although its distribution is not constrained to the Arctic (Lee and Lee, 2012).
The Shionodiscus bioculatus phylotype represented by RCC5532 contains two strains isolated from the AM (Supplementary Data S1). Its sequence shares 99.8% similarity with S. bioculatus strain RCC1991 from the Beaufort Sea (Figure 5). The morphology of the two strains differs (Figure 3Z and AH): RCC5532 cells have a longer pervalvar axis (~32 μm), shorter valve diameter and fewer discoid chloroplasts in comparison to RCC5609. Isolates with identical 18S rRNA may present cryptic diversity based on ITS divergence (Luddington et al., 2016). S. bioculatus is reported as dominating the top portion of submerged sea-ice ridges (Fernández-méndez et al., 2018).
Skeletonema sp. RCC5502 strain was retrieved during the AM and its sequence shared 100% similarity with Skeletonema japonicum from Onagawa Bay and 99.7% with an Arctic environmental sequence (JF698855, Figure 5). Cells are small (5 μm diameter) with a very short pervalvar axis ~3 μm, being either solitary or in pairs (Figure 3V). The genus Skeletonema has been reported from high latitude, winter samples (Eilertsen and Degerlund, 2010) and S. aff. japonicum seems to thrive in polar environments with low silicate concentration (Luddington et al., 2016).
The Thalassiosira sp. phylotype represented by RCC5327 contains 12 strains from all sampling sites, substrates and phases of the bloom (Supplementary Data S1). The best match to its sequence is from an Arctic environmental sequence (99.5% similarity), branching apart from other Thalassiosira clades (Figure 5). It shares 99.2% identity with T. nordenskioeldii strain RCC2021. Cells are small (<8 μm diameter) with a long pervalvar dimension relative to valve size and long (>20 μm) marginal threads (Figure 3E).
The Thalassiosira sp. phylotype represented by RCC5348 contains three strains from IC water and ice. Its sequence is 99.8% similar with a T. antarctica var. borealis isolate from the Barents Sea (Figure 5). Cells are cylindrical with a short pervalvar axis, a 17–22 μm valvar diameter, and contain fine areolae radiating from the valve center (Figure 3G). T. antarctica is reported in coastal and ice-edge cold waters (Hasle and Heimdal, 1968) and associated with high-nutrient concentrations (Luddington et al., 2016).
The sequence of Thalassiosira nordenskioeldii strain RCC5350 isolated from an ice core sample is (100%) identical to that of T. nordenskioeldii Arctic strain RCC2021 (Figure 5). Cells are cylindrical, either solitary or forming colonies, with a ~6 μm valvar diameter and a 10 μm pervalvar axis, with long processes (Figure 3H). T. nordenskioeldii is widely distributed in North Atlantic cold, temperate and polar waters (Crawford et al., 2018; Johnsen et al., 2018), often associated with ice (Luddington et al., 2016).
The Thalassiosira rotula phylotype represented by RCC5605 contains two strains, one isolated during the Amundsen cruise and one from under-ice at the ice camp during the bloom peak (Supplementary Data S1). The sequence from this phylotype had 100% similarity with those of T. rotula strains from the Arctic and the English Channel, but also with that of Thalassiosira gravida (RCC1984) (Figure 5). 18S rRNA is not a good marker to discriminate between T. rotula, a known cosmopolitan species (Hasle and Syvertsen, 1997; Whittaker et al., 2012), and the bipolar T. gravida (Balzano et al., 2017). Cells are mainly solitary, with a ~6 μm valvar diameter and a 10–13 μm pervalvar axis with several long marginal threads (Figure 3AE).
Dinobryon faculiferum strain RCC5261 was isolated from 1.5 m depth in IC waters from the peak of the bloom (Supplementary Data S1). Its sequence shares 100% similarity to those of other Arctic strains, such as RCC2294 (Figure 6A). Cells are solitary with a ~4 μm diameter lorica and long spines (>25 μm) (Figure 7C). D. faculiferum is a frequently observed mixotroph in Arctic surface waters (Lovejoy et al., 2002; Balzano et al., 2012) that can be found encysted in the top section of ice cores (Kauko et al., 2018), although it is not restricted to polar environments (Unrein et al., 2010).
Spumella sp. RCC5513 strain isolated from an AM sample branches with D. faculiferum and its sequence is 99.8% similar to those of Spumella sp. strains from the Baltic Sea (isolate IOW91) and the Atlantic Ocean (RCC4558) (Figure 6A). Cells are colorless and solitary, round or slightly elongated with 4 μm diameter and 5 μm flagella (Figure 7N). Heterotrophic flagellates from the genus Spumella have been previously reported in the Arctic (Lovejoy et al., 2006) and are mostly cold-adapted and associated with lower salinities (Grossmann et al., 2015).
The Spumella sp. phylotype represented by RCC5412 contains two isolates from IC waters. Their sequence is 100% similar to those of Spumella sp. isolate CCAP 955/1 from a soil sample collected in China and Spumella elongata isolate JBC/S24 from the UK (Figure 6A). Interestingly, these sequences are part of a soil sub-cluster within Chrysophyceae clade C with few aquatic representatives (Boenigk et al., 2005). These strains were lost and no images are available.
Pedinellales strain RCC5264 was retrieved from an IC ice sample at the peak of the bloom (Supplementary Data S1), and its sequence matched with 100% similarity that of the undescribed Pedinellales Arctic strain RCC2301 and also with CCMP2098 isolated from Baffin Bay (GenBank EU247836). Cells are solitary, round in anterior view (6 μm diameter), apple-shaped to slightly elongated in side view, with six peripheral chloroplasts (Figure 7D). Further taxonomic analyses are needed to properly assign this strain at the genus level, although its sequence matches with with 98.6% similarity that of a Pseudopedinella sp. strain (CCMP1476) from the Sargasso Sea (Figure 6A).
The Pelagophyceae phylotype represented by RCC5450 groups five strains from IC, four from water samples and one from ice (Supplementary Data S1). Its sequence shares 100% similarity with other Arctic strains such as RCC2505 and RCC2515. Cells are round, ~4 μm in diameter, with two flagella of different sizes, ~2 μm and 7 μm, respectively (Figure 7J). Pelagophyceae may dominate surface waters during the Arctic summer (Balzano et al., 2012a) and yet undescribed strains have been recovered previously from northern waters (Balzano et al., 2012).
The Pelagophyceae phylotype represented by RCC5251 contains four strains from the peak of the bloom (Supplementary Data S1) and its representative sequence shares 100% similarity with that of the undescribed Arctic Pelagophyceae RCC2040 (Figure 6A). Cells are elongated with ~7 μm in side view (Figure 7B).
Pelagophyceae strain RCC5488, isolated from an ice sample during bloom-development phase (Supplementary Data S1), has a sequence that branches apart from the other Pelagophyceae phylotypes (Figure 6A), matching with 100% similarity another strain isolated from Baffin Bay, CCMP2097. Cells are solitary, ~4 μm in size (Figure 7M).
The Chlamydomonas sp. phylotype represented by RCC5305 contains 6 strains isolated from IC water and ice samples from the peak of the bloom and is the only representative of the Chlorophyceae in our set of culture isolates (Supplementary Data S1). Its sequence is 100% identical to sequences from the Chlamydomonas pulsatilla polar strain CCCryo 038–99, but also strains from Antarctic ice and Arctic fresh water (Figure 8), all belonging to the Polytoma clade (Pocock et al., 2004). Cells are round or elongated, ~7 μm in diameter or 10 μm long, respectively (Figure 7H). Chlamydomonas is a common genus found in the Arctic during the spring and summer months (Lovejoy et al., 2002; Balzano et al., 2012a), that can occur in association with sea-ice (Majaneva et al., 2017).
Bathycoccus prasinos RCC5417 strain was recovered from an IC ice core sample during bloom development (Supplementary Data S1). This genus has recently been observed in Arctic waters (Terrado et al., 2013; Kilias et al., 2014), including during winter (Joli et al., 2017) and has a highly conserved 18S rRNA. Its sequence shares 100% similarity with B. prasinos strain CCMP1898 from the Mediterranean Sea (Figure 8).
The Micromonas polaris phylotype represented by RCC5239 regroups 10 strains recovered from IC ice and water samples. Its sequence shares 100% similarity with those of the Arctic strains M. polaris CCMP2099 and RCC2308 (Figure 8). M. polaris often dominates the picoplanktonic community in the Arctic (Sherr et al., 2003; Not et al., 2005; Balzano et al., 2012a), and metagenomic data suggest its presence in Antarctic waters (Delmont et al., 2015; Simmons et al., 2015).
Mantoniella baffinensis RCC5418, recently described (Yau et al., 2019), was recovered from pre-bloom IC ice core samples. Its sequence branched apart from other known strains (Figure 8), matching with 98% similarity the Arctic strains RCC2497 and RCC2288, which were also recently described as Mantoniella beaufortii (Yau et al., 2019). Cells are round, ~4 μm in diameter bearing two unequal flagella with a visible red eyespot opposite to the flagella (Figure 7I).
Mantoniella sp. strain RCC5273 was isolated from a sample taken at 20-m depth during the peak of the bloom. Its sequence shared 99.8% similarity with that of Mantoniella squamata strain CCAP 1965/1, a cosmopolitan species (Hasle and Syvertsen, 1997) frequently observed in the Arctic (Lovejoy et al., 2007; Majaneva et al., 2017). This strain was lost and no images are available.
Mantoniella sp. strain RCC5301 was also isolated from 20-m depth during the peak of the bloom and its sequence is not closely related to any strain or environmental sequence. However, it clustered together with other Mantoniella sequences, sharing 98.3% identity with M. squamata CCAP 1965/1 (Figure 8). This strain was also lost and no images are available.
The Pyramimonas diskoicola/Pyramimonas gelidicola phylotype represented by RCC5525 contains 11 strains from all main sampling sites, substrates, and phases of the bloom (Supplementary Data S1). The sequence from RCC5525 is 100% similar to that of the Arctic P. diskoicola and the Antarctic P. gelidicola within the subgenus Vestigifera (Figure 8). Three types of cell morphology have been observed: pyramidal, elongated, and nearly round. A big starch grain with two lobes surrounds a pyrenoid located at the basal end; large lipid bodies are present near the apical end. Cells are ~7 μm in length and have four flagella with similar size (Figure 7Q).
The Pyramimonas sp. phylotype represented by RCC5284 contains 8 strains from the IC during the later phases of the bloom, 7 of which were isolated from water samples (Supplementary Data S1). The representative sequence shares 99.7% similarity with that of P. diskoicola RCC5525 (Figure 8). Cells are pyramidal to round, ~8 μm long with a pyrenoid and basally positioned starch grain, four flagella shorter than cell length, and a flagellar pit ~2 μm deep (Figure 7G).
The Pyramimonas sp. phylotype represented by RCC5281 is formed by two IC strains from samples taken at 20-m depth at the peak of the bloom on different sampling days (Supplemntary Data S1). The representative sequence is 100% similar to that of the Arctic strain Pyramimonas sp. RCC1987. These strains were lost and no images are available.
Pyramimonas australis RCC5269 strain from IC water has a sequence matching with 100% similarity that of P. australis (GenBank AJ404886) from the subgenus Trichocystis, an Antarctic species described based on light/electron microscopy, nuclear-encoded small-subunit ribosomal DNA and chloroplast-encoded rbcL gene sequences, but with no representative sequence from cultures until now (Moro et al., 2002). Cells are pear-like to almost oval, ~10 μm long and 6 μm wide with four flagella (Figure 7E).
Pyramimonas sp. RCC5483 strain was recovered from IC surface waters during the pre-bloom phase and its sequence shares 100% similarity with that of the Arctic strain RCC669 (Figure 8). This strain was lost and no images are available.
Pyramimonas sp. RCC5453 was isolated from an IC ice core sample during the pre-bloom phase and its sequence matches with 99.7% similarity that of the Arctic strain Pyramimonas sp. RCC1987. Cells are pear-like to round, from 4 to 7 μm long and with four flagella (Figure 7K).
The Baffinella frigidus phylotype represented by RCC5246 contains 13 strains collected from IC water and ice samples (Supplementary Data S1). Their representative sequence matches with 100% similarity those of the B. frigidus sp. strain CCMP2045 (Figure 6B). This genus was originally isolated from Baffin Bay and is the first Cryptophyta representative described from this region (Daugbjerg et al., 2018). Cells are ~10 μm long and 5 μm wide with a prominent pyrenoid (Figure 7A).
The Rhodomonas sp. phylotype represented by RCC5610 groups 3 strains, 2 of them isolated from IC and one from AM water samples (Supplementary Data S1). Its representative sequence has low similarity to that of RCC5246 (96.8%) and is 100% similar to other Arctic strains such as RCC2020 and Rhodomonas marina SCCAP K-0435 from Denmark (Figure 6B), a species associated with sea ice (Niemi et al., 2011). Cell length is ~18 μm with a ventral to dorsal width ~8 μm, two flagella, and a clearly visible furrow with rows of ejectisomes (Figure 7R). This genus is frequently observed in Arctic waters (Lovejoy et al., 2002), being abundant in the subsurface chlorophyll maximum (Joo et al., 2012) or associated with sea ice (Niemi et al., 2011).
Pseudohaptolina sorokinii strain (RCC5270) was retrieved from IC water during the peak of the bloom. Its sequence shares 100% similarity with that of the recently described P. sorokinii (Orlova et al., 2016) strain PsAB2015 collected from coastal, under-ice water and 99.7% with the strain P. arctica CCMP 1204 (Figure 6C). Cells are round to oblong, ~17 μm in length and 12 μm in width. The two flagella have almost the same length as the cell, with a shorter haptonema (Figure 7F).
The Isochrysis sp. phylotype represented by RCC5486 contains three strains, all retrieved from IC ice core samples. Their sequence shared low similarity to any other cultured strain in the GenBank database, matching with 99.2% identity the Isochrysis nuda strain RCC2477 and 99.1% Isochrysis galbana strain 24–25B5 (Figure 6C). Cells are solitary, round to oval, ~6 μm long and 5 μm wide. The nucleus, stigma and two 7 μm flagella can be observed (Figure 7L). Although mainly isolated from coastal and estuarine environments (Bendif et al., 2013), this genus has also been reported as characteristic of sea-ice environments (Majaneva et al., 2017).
The Biecheleria cincta phylotype represented by RCC5518 has three strains, all from AM water samples at 20-m depth during the bloom-development phase (Supplementary Data S1). Sequences from this phylotype are related with 100% identity to the Arctic isolate RCC2013 Biecheleria cincta (Figure 6D), a cosmopolitan species found also in polar waters (Balzano et al., 2012a), with reported mixotrophic behaviour (Kang et al., 2011). Cells are ~10 μm wide with irregular shaped chloroplasts (Figure 7O).
The sequence of Biecheleria sp. (RCC5522), collected in the same sample as the B. cincta RCC5518 phylotype, differed by only one base pair from the sequence of RCC5518, branching with B. brevisulcata strain trd276-kt from freshwater (Figure 6D). Cells are spherical to oval, ~8 μm long and 6 μm wide with irregularly shaped chloroplasts (Figure 7P).
A total of 187 strains were isolated from IC samples, 110 from the water and 77 from the ice (Supplementary Data S1). Diatoms dominated isolates from all phases of the bloom (pre-bloom, bloom-development and bloom-peak), although the diversity and number of strains varied (Figure 9). During the pre-bloom phase, 28 strains were recovered from the ice and 10 from the water, belonging to six classes (Figure 9). This phase was dominated by Bacillariophyceae, mainly Nitzschia and F. cylindrus (Figure 9, Supplementary Data S1). Eight out of the eleven Mediophyceae strains belonged to the genus Thalassiosira. Strains from Pyramimonadales, Prymnesiophyceae, Pelagophyceae and Mamiellophyceae were also retrieved during pre-bloom. The bloom-development phase yielded 50 strains from seven classes. New taxa not isolated during the first phase appeared in this second phase, including one strain of Pedinellales (Dictyochophyceae) from an ice sample, and 7 strains of Cryptophyceae assigned to Rhodomonas and Baffinella, all from water samples (Figure 9, Supplementary Data S1). More strains were retrieved during the bloom-peak phase than the other two phases combined (99), and 11 classes were isolated. In contrast to the previous two phases, strains retrieved from water were more diverse than from the ice (Figure 9). Chlorophyceae were represented by Chlamydomonas sp., from both water and ice samples. One strain of the Prymnesiophyceae P. sorokinii and the Chrysophyceae strains D. faculiferum and Spumella spp. were only retrieved during this phase (Supplementary Data S1). With respect to diatoms, this phase was marked by an increase in Mediophyceae, particularly from the genera Chaetoceros and Attheya (Supplementary Data S1).
A total of 89 strains were isolated from AM water samples, of which 81 were diatoms. Although some stations were dominated by Bacillariophyceae, such as station G102, the majority of the strains belonged to the Mediophyceae, particularly Attheya spp. and C. neogracilis (Supplementary Data S1). Only two strains of the Coscinodiscophyceae genus Actinocyclus sp. were recovered, both from surface waters at the same station (G713). Few non-diatom strains were isolated. The only station with Cryptophyceae representatives was AM1, from which one Rhodomonas strain was isolated (Figure S2). Four Dinophyceae strains (Biecheleria spp.) were retrieved from station G204. One strain of Spumella sp. was recovered from G110 and two Pyramimonas sp. strains from G512 and G707 (Supplementary Data S1).
Serial dilution yielded the most phylotypes (18), followed by FCM cell sorting (14) and single cell pipetting (7). Eighteen phylotypes had representatives isolated by more than one technique (Figure S3). Among diatoms, Bacillariophyceae and Mediophyceae were retrieved by the three isolation methods, but Coscinodiscophyceae were isolated only by single cell pipetting (Figure S4A to C). Specifically, Arcocellulus sp. and E. groenlandica were retrieved only by flow cytometry sorting, while B. bathyomphala, Coscinodiscus sp. and Actinocyclus sp. strains came only from single cell pipetting. The strains isolated only by serial dilution included Sellaphora sp., Skeletonema sp. and one Naviculales phylotype (Supplementary Data S1). For non-diatoms, FCM cell sorting was the technique which retrieved the highest diversity at the class level (Figure S4F). D. faculiferum, Biecheleria spp., P. sorokinii, and two phyloypes of Mantoniella sp., were only obtained by this technique. B. prasinos, M. baffinensis and Spumella spp. were recovered only by serial dilution, as well as 9 of 10 M. polaris strains.
Half of the strains in this study were retrieved using FCM cell sorting, reflecting previous reports on the efficiency of this isolation technique (Marie et al., 2017). The use of other techniques helped to increase the diversity of taxa successfully cultured, as 68% of phylotypes were obtained by a single isolation method, confirming previous work in the Arctic and other marine systems (Le Gall et al., 2008; Balzano et al., 2012). For instance, although only 12% of strains originated from single cell pipetting, Coscinodiscophyceae were only retrieved by this technique, as well as three of four Thalassiosira phylotypes. Serial dilution yielded 38% of the strains and was particularly successful for retrieving picoplanktonic Mamiellophyceae. In fact, at the early stages of isolate characterization (before screening and dereplication), 60 picoplankton strains were established by this technique, compared to only one by cell sorting and none by single cell pipetting. Among the phylotypes retrieved by more than one isolation method were some well known Arctic taxa such as A. septentrionalis, C. neogracilis and F. cylindrus.
Of the 57 retrieved phylotypes, 32 could not be assigned at the species level and 6, at the genus level. Some species cannot be reliably determined by 18S rRNA sequencing alone, like T. rotula, A. cornucervis or C. neogracilis that may display cryptic diversity. In such cases accurate determination would usually require the use of alternative gene markers such as 28S rRNA or ITS (Balzano et al., 2017), or there may be morphological characters that distinguish the species. For example, the closely related species A. septentrionalis and A. longicornis cannot be discriminated by 18S rRNA (Rampen et al., 2009), but the latter can be distinguished morphologically by its characteristic long horns.
Of the diversity cultured in this study, pennate diatoms contained the most candidates for novel taxa (i.e., similarity above 99% only to environmental sequences). The five phylotypes affiliated to Nitzschia spp. were not closely related to any existing sequenced strain. For example, the Nitzschia RCC5458 strain isolated from the ice branched apart from other Nitzschia phylotypes with high bootstrap support (95%), with only 98% similarity to a strain from the Red Sea. Also retrieved from the ice, Cylindrotheca RCC5303 grouped with C. closterium in a moderately supported clade (72%), apparently forming a new lineage within the C. closterium species complex (98% similarity). Other pennate diatoms with low sequence identity matches to existing strains included Naviculales sp. RCC5387 and Sellaphora sp. RCC5460. With respect to centric diatoms, Coscinodiscus RCC5319 had the greatest dissimilarity to any existing strain sequence (95% identity), grouping with moderate bootstrap support (80%) with C. radiatus from the North Pacific, a species previously reported from Baffin Bay (Lovejoy et al., 2002). Unfortunately, this strain was lost before morphological analysis was undertaken. C. decipiens RCC5606 is interesting in that it is clearly distinguishable from the closely related C. decipiens RCC1997 from the Beaufort Sea (99.8% similarity) (Balzano et al., 2017) and differs from the original description (Hasle and Syvertsen, 1997) by its prominently curved chains.
Among green algae, the newly described Arctic species M. baffinensis (from RCC5418) and M. beaufortii (Yau et al., 2019), as well as the other Mantoniella-related strains from this work that were lost (RCC5273 and RCC5301), suggest that this genus is more diverse than other Arctic Mamiellophyceae and hosts several rare species that are not often revealed in environmental sequencing data. The Mamiellophyceae B. prasinos (RCC5417) strain that was isolated from ice is, to the best of our knowledge, the only available Arctic isolate of this very ubiquitous species (Tragin and Vaulot, 2019). This will offer interesting perspectives in terms of genome sequencing and physiological experiments, as this strain might correspond to a new cold-adapted ecotype.
The Isochrysis sp. strains that originated from sea ice are not closely related to any polar strain or environmental sequence, potentially representing a new cold-adapted phylotype. The retrieval of only one dinoflagellate species, Biecheleria cincta, previously Woloszynskia (Balzano et al., 2012), is at odds with the known diversity of dinoflagellates in the Arctic (Bachy et al., 2011; Onda et al., 2017) and especially in Baffin Bay (Lovejoy et al., 2002). Another extensive Arctic culture isolation effort yielded a similar result (Balzano et al., 2012), indicating the need for alternative isolation methods to overcome this bias.
The strains recovered were more numerous and more diverse during the bloom itself when sea-ice melted. During the two preliminary phases of the bloom (pre-bloom and bloom-development) the highest strain diversity originated from sea ice samples. A shift occurred as the bloom became established and the water column samples yielded more strain diversity. The number of flagellate strains isolated from water during the bloom increased from 3 during the pre-bloom period to 33 at its peak. Flagellate-dominated communities have been reported in late summer in northern Baffin Bay and the Beaufort Sea (Tremblay et al., 2009). During pre-bloom, flagellates isolated from water samples belonged to only two classes (Pelagophyceae and Pyramimonadales), compared to seven classes during later phases. Chlamydomonas (Chlorophyceae), a genus usually associated with freshwater environments, was only isolated in July when ice melting accelerated, lowering the salinity of surface waters. All Micromonas and most Pyramimonas strains (20 out of 24) were also isolated from the two later phases of the bloom. Both genera have been documented in abundance in lower salinity, summer Arctic waters (Not et al., 2005; Balzano et al., 2012), although higher M. polaris abundance has been associated with both pre-bloom and post-bloom stages (Marquardt et al., 2016; Meshram et al., 2017), thriving in both nutrient-replete and nutrient-deplete conditions (Balzano et al., 2012a). Flow cytometry data showed a peak in picoplankton abundance preceding that of nanoplankton (Figure 9), a pattern that has been observed previously (Sherr et al., 2003). One M. polaris strain was retrieved from an ice core sample during bloom-development, confirming previous studies using high throughput sequencing that have shown that M. polaris is part of both Arctic (Comeau et al., 2013) and subarctic sympagic communities (Belevich et al., 2018). Pyramimonas cell abundance in the Baffin Bay region during summer is exceptionally high compared to other Arctic domains such as the Bering, Chukchi and Beaufort Seas (Crawford et al., 2018), where it seems to be also fairly diverse (Balzano et al., 2012). Pyramimonadales were indeed the third most represented class in the present study, from both water and ice samples. Ochrophyta strains associated with heterotrophic or mixotrophic behavior such as Spumella, Dinobryon (Unrein et al., 2010) and Pedinellales (Piwosz and Pernthaler, 2010) were only isolated during the bloom-peak, which might be related to a competitive advantage under nitrogen deprivation in surface waters as the spring bloom develops.
Diatoms play a major role in sympagic assemblages (Mundy et al., 2011), and a pennate dominated community (Comeau et al., 2013) is considered a mature state of the successional stages during sea ice formation (Niemi et al., 2011; Kauko et al., 2018), when centric diatoms are found in lower numbers (Olsen et al., 2017). Navicula and Nitzschia representatives thrive in high abundance in the high salinity brine channels (Rózanska et al., 2009; Johnsen et al., 2018). In the present study, eight out of the sixteen phylotypes retrieved solely from ice were pennate diatoms, including two Navicula and two Nitzschia species. As the ice melts and the bloom develops in the Arctic pelagic environment, bigger cells prosper, including centric diatoms such as T. nordenskioeldii, T. antarctica var. borealis and/or the smaller-sized C. gelidus (Booth et al., 2002; Horvat et al., 2017). The relevance of the pelagic environment to centric diatoms was demonstrated by the Bacillariophyceae/Coscinodiscophyceae genera recovered solely from the water column, including Skeletonema, Shionodiscus and Actinocyclus. Although Thalassiosira strains were isolated from the first phase of the bloom, including ice samples, C. gelidus was only retrieved from mid-June onwards. C. gelidus has been often reported in the Arctic (Ardyna et al., 2017; Johnsen et al., 2018), in particular following Thalassiosira blooms (Booth et al., 2002). C. neogracilis strains alone comprised 12% of all strains and were retrieved from all phases of the bloom, from ice and surface waters down to 35 meters. The wide spatial and temporal range from which this species was retrieved attests for its ubiquity and importance in this environment.
Sea ice, under-ice and open water Arctic phytoplankton communities differ in diversity, biomass, growth rate and tolerance of environmental conditions (Arrigo et al., 2012). Similarly, different types of sea ice provide different substrates, and therefore harbor different communities, as observed between fast, pack and drift ice (Comeau et al., 2013; Majaneva et al., 2017). The same is true for the stages of sea ice formation (Olsen et al., 2017; Kauko et al., 2018). Although many species recovered in this study have been isolated before, ice core samples yielded most of the novel taxa, for all groups from diatoms to green algae. It is important that culturing efforts continue in the Arctic, as ongoing and predicted loss in ice coverage and thickness (Perovich and Richter-Menge, 2009) will certainly impact plankton diversity, dynamics and community structure (Comeau et al., 2011; Blais et al., 2017; Horvat et al., 2017). As the diversity within culture collections improves to reflect the complexity of the environment, the increased amount of validated reference sequences will help scientists to better access eukaryotic plankton distribution patterns across the Arctic. In addition, the availability of polar strains will enable experimental studies to observe physiological and metabolic impacts of current changes such as global warming on polar phytoplankton communities.
Strains have been deposited to the Roscoff Culture Collection (http://www.roscoff-culture-collection.org) under numbers RCC5197 to RCC5612 and sequences to Genbank under accession numbers MH764681:765044.
The supplemental file for this article can be found as follows:
We thank the whole Green Edge team, as well as the Amundsen crew, for the help they provided at all stages of this project. Special thanks to Marie-Hélène Forget and Joannie Ferland for the ice camp logistics.
Financial support for this work was provided by the Green Edge project (ANR-14-CE01-0017, Fondation Total), the ANR PhytoPol (ANR-15-CE02-0007) and TaxMArc (Research Council of Norway, 268286/E40). M.T. was supported by a PhD fellowship from the Université Pierre et Marie Curie and the Région Bretagne (ARED GreenPhy). ALS was supported by FONDECYT grant PiSCOSouth (N1171802). CGR was supported by CONICYT project 3190827.
The authors have no competing interests to declare.
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