Nearly full-length 16S rRNA gene sequences of strains RKSG066 T (=TSD-73 T =LMG 29870 T) and RKSG123 T were deposited GenBank/EMBL/DDBJ under the accession numbers KX896698 and KX896700, respectively. Whole genome shotgun sequences of strains RKSG066 T , RKSG123 T , JCM 16186 T and KCTC 42720 T were deposited in GenBank/EMBL/DDBJ under the accession numbers SMMD00000000, SMMB00000000, SMLW00000000 and SMLV00000000, respectively. Three supplementary tables and five supplementary figures are available with the online version of this article.
The Sargasso Sea is a dynamic physical environment in which strong seasonal variability combines with forcing by mesoscale (~ 100 km) eddies. These drivers determine nutrient, light, and temperature regimes and, ultimately, the composition and productivity of the phytoplankton community. On four cruises (2011 and 2012; one eddy per cruise), we investigated links between water column structure and phytoplankton community composition in the Sargasso at a range of time and space scales. On all cruises, cyanobacteria (Prochlorococcus and Synechococcus) dominated the phytoplankton numerically, while haptophytes were the dominant eukaryotes (up to 60% of total chl-a). There were substantial effects of mesoscale and sub-mesoscale forcing on phytoplankton community composition in both spring and summer. Downwelling (in anticyclones) resulted in Prochlorococcus abundances that were 22-66% higher than at ‗outside' stations. Upwelling (in cyclones) was associated with significantly higher abundances and POC biomass of nanoeukaryotes. In general, however, each eddy had its own unique characteristics. The center of anticyclone AC1 (spring 2011) had the lowest phytoplankton biomass (chl-a) of any eddy we studied and had lower nitrate + nitrite (N+N <5 mmol m-2) and eukaryote chl-a biomass as compared to its edge and to the Bermuda Atlantic Time-Series station (BATS). At the center of cyclone C1 (summer 2011), we observed uplift of the 26.5 kg m-3 isopycnal and high nutrient inventories (N+N = 74 ± 46 mmol m-2). We also observed significantly higher haptophyte chl-a (noncoccolithophores) and lower cyanobacterial chl-a at the center and edge of C1 as compared to outside the eddy at BATS. Cyclone C2 (spring 2012) exhibited a deep mixed layer, yet had relatively low nutrient concentrations. We observed a shift in the 2 taxonomic composition of haptophytes between a coccolithophore-dominated community in C2 (98% of total haptophyte chl-a) and a non-coccolithophore community at BATS. In summer 2012, downwelling associated with anticyclone AC2 occurred at the edge of the eddy (not at the center), where AC2 interacted with a nearby cyclone. At the edge, we found significantly lower Synechococcus abundances and higher eukaryote chl-a compared to the center of AC2 and BATS. These along-transect nuances demonstrate the significance of small-scale perturbations that substantially alter phytoplankton community structure. Therefore, while seasonality in the North Atlantic is the primary driver of broad-scale trends in phytoplankton community composition, the effects of transient events must be considered when studying planktonic food webs and biogeochemical cycling in the Sargasso Sea.
A Gram-stain-negative, strictly aerobic, motile, rod-shaped bacterium, designated strain RKSG058, was isolated from the marine sponge Verongula gigantea, collected off the west coast of San Salvador, The Bahamas. Phylogenetic analyses based on 16S rRNA gene sequences revealed that RKSG058 formed a distinct lineage within the family Hahellaceae (order Oceanospirillales, class Gammaproteobacteria), and was most closely related to the genus Endozoicomonas, with sequence similarities to members of this genus ranging from 92.0 to 93.7 %. Optimal growth occurred at 30 °C, at pH 7 and in the presence of 2-3 % (w/v) NaCl. The predominant cellular fatty acids were summed feature 3 (C16 : 1ω7c and/or C16 : 1ω6c), summed feature 8 (C18 : 1ω7c and/or C18 : 1ω6c) and C16 : 0. The major and minor respiratory quinones were Q-9 and Q-8, respectively. The polar lipids comprised diphosphatidylglycerol, phosphatidylglycerol, phosphatidylethanolamine, three unidentified aminolipids, an unidentified phospholipid and five unidentified lipids. The DNA G+C content was 42.3 mol%. Biochemical, chemotaxonomic and phylogenetic analyses indicated that strain RKSG058 represents the first cultured isolate of a novel bacterial genus and species within the family Hahellaceae, for which the name Sansalvadorimonas verongulae gen. nov., sp. nov. is proposed. The type strain of Sansalvadorimonas verongulae is RKSG058 (=TSD-72=LMG 29871). An emended description of the genus Kistimonas is provided.
A Gram-stain-negative, strictly aerobic, motile bacterium, designated strain RKSG073T, was isolated from the sea sponge Aplysina fistularis, collected off the west coast of San Salvador, The Bahamas. Cells were curved-to-spiral rods with single, bipolar (amphitrichous) flagella, oxidase- and catalase-positive, non-nitrate-reducing and required salt for growth. RKSG073T grew optimally at 30–37 °C, pH 6–7, and with 2–3 % (w/v) NaCl. The predominant fatty acids of RKSG073T were summed feature 8 (C18 : 1ω6c and/or C18 : 1ω7c) and C16 : 0. Major isoprenoid quinones were identified as Q-10 and Q-9. Phylogenetic analyses of nearly complete 16S rRNA genes and genome sequences positioned strain RKSG073T in a clade with its closest relative Aestuariispira insulae AH-MY2T (92.1 % 16S rRNA gene sequence similarity), which subsequently clustered with Hwanghaeella grinnelliae Gri0909T, Marivibrio halodurans ZC80T and type species of the genera Kiloniella , Thalassospira and Terasakiella . The DNA G+C content calculated from the genome of RKSG073T was 42.2 mol%. On the basis of phylogenetic distinctiveness and polyphasic analysis, here we propose that RKSG073T (culture deposit numbers: ATCC collection = TSD-74T, BCCM collection = LMG 29869T) represents the type strain of a novel genus and species within the family Kiloniellaceae , order Rhodospirillales and class Alphaproteobacteria , for which the name Curvivirga aplysinae gen. nov., sp. nov. is proposed.
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