@article {dulong_exopolysaccharide_2024,
	title = {Exopolysaccharide from marine microalgae belonging to the \textit{Glossomastix genus: fragile gel behavior and suspension stability},
	journal = {Bioengineered},
	volume = {15},
	number = {1},
	year = {2024},
	note = {Publisher: Taylor \& Francis _eprint: https://doi.org/10.1080/21655979.2023.2296257},
	month = {dec},
	pages = {2296257},
	abstract = {With the aim to find new polysaccharides of rheological interest with innovated properties, rhamnofucans produced as exopolysaccharides (EPS) in a photobioreactor (PBR) and an airlift bioreactor (ABR) by the marine microalgae Glossomastix sp. RCC3707 and RCC3688 were fully studied. Chemical characterizations have been conducted (UHPLC {\textendash} MS HR). Analyses by size-exclusion chromatography (SEC) coupled online with a multiangle light scattering detector (MALS) and a differential refractive index detector showed the presence of large structures with molar masses higher than 106 g.mol-1. The rheological studies of these EPS solutions, conducted at different concentrations and salinities, have evidenced interesting and rare behavior characteristic of weak and fragile hydrogels i.e. gel behavior with very low elastic moduli (between 10-2 and 10 Pa) and yield stresses (between 10-2 and 2 Pa) according to the EPS source, concentration, and salinity. These results were confirmed by diffusing wave spectroscopy. Finally, as one of potential application, solutions of EPS from Glossomastix sp. have evidenced very good properties as anti-settling stabilizers, using microcrystalline cellulose particles as model, studied by multiple light scattering (MLS) with utilization in cosmetic or food industry. Compared to alginate solution with same viscosity for which sedimentation is observed over few hours, microalgae EPS leads to a stable suspension over few days.},
	keywords = {fragile gel, Glossomastix, Microalgae, Polysaccharide, RCC3688, RCC3707, stabilizer},
	issn = {2165-5979},
	doi = {10.1080/21655979.2023.2296257},
	url = {https://doi.org/10.1080/21655979.2023.2296257},
	author = {Dulong, Virginie and Rihouey, Christophe and Gaignard, Cl{\'e}ment and Bridiau, Nicolas and Gourvil, Priscilla and Laroche, C{\'e}line and Pierre, Guillaume and Varacavoudin, Tony and Probert, Ian and Maugard, Thierry and Michaud, Philippe and Picton, Luc and Le Cerf, Didier}
}
@article {ben-joseph_crystallization_2023,
	title = {Crystallization of Coccolith Calcite at Different Life-Cycle Phases Exhibits Distinct Degrees of Cellular Confinement},
	journal = {Small Structures},
	volume = {n/a},
	number = {n/a},
	year = {2023},
	note = {_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/sstr.202200353},
	pages = {2200353},
	abstract = {Coccolithophores are a group of unicellular marine algae that shape global geochemical cycles via the production of calcium carbonate crystals. Interestingly, different life-cycle phases of the same coccolithophore species produce very different calcitic scales, called coccoliths. In the widely studied diploid phase, the crystals have anisotropic and complex morphologies, while haploid cells produce coccoliths consisting solely of calcite crystals with simple rhombohedral morphology. Understanding how these two life-cycle phases control crystallization is a highly sought-after goal, yet, haploid phase crystallization has rarely been studied, and the process by which they form is unknown. Herein, advanced electron microscopy is employed to elucidate the cellular architecture of the calcification process in haploid cells. The results show that in contrast to diploid-phase calcification, the coccolith-forming vesicle of haploid-phase cells is voluminous. In this solution-like environment, the crystals nucleate and grow asynchronously in a process that resembles calcite growth in bulk solution, leading to the simple morphologies of the crystals. The two distinct mineralization regimes of coccolithophore life-cycle phases suggest that cellular architecture, and specifically confinement of the crystallization process, is a pivotal determinant of biomineral morphology and assembly.},
	keywords = {biomineralization, calcites, Coccoliths, crystal growths, haploid{\textendash}diploid life cycles, RCC1181, RCC3777},
	issn = {2688-4062},
	doi = {10.1002/sstr.202200353},
	url = {https://onlinelibrary.wiley.com/doi/abs/10.1002/sstr.202200353},
	author = {Ben-Joseph, Oz and de Haan, Diede and Rechav, Katya and Shimoni, Eyal and Levin-Zaidman, Smadar and Langer, Gerald and Probert, Ian and Wheeler, Glen L. and Gal, Assaf}
}
@article {mertens_morpho-molecular_2023,
	title = {Morpho-molecular analysis of podolampadacean dinoflagellates (Dinophyceae), with the description of two new genera},
	journal = {Phycologia},
	year = {2023},
	note = {Publisher: Taylor \& Francis _eprint: https://doi.org/10.1080/00318884.2022.2158281},
	month = {feb},
	pages = {1{\textendash}19},
	abstract = {Sequences were obtained for 58 podolampadacean single cells from France, Reunion Island (French territories) and Japan (6 SSU rDNA only, 40 SSU+LSU and 12 LSU only). The sequenced taxa belong to five of the eight described genera: Podolampas, Blepharocysta, Lissodinium, Gaarderiella and Mysticella. Two new genera, Alatosphaera and Pseudalatosphaera, were erected to accommodate {\textquoteleft}Blepharocysta{\textquoteright} hermosillae and {\textquoteleft}Blepharocysta{\textquoteright} denticulata. Most genera are well supported by concatenated LSU{\textendash}SSU rDNA phylogenies, with the least support for Lissodinium. Metabarcoding of podolampadaceans using the V4 region of SSU rDNA showed a resolution too low to discriminate genera or species. Roscoffia and Cabra are here considered podolampadaceans, whilst Lessardia is considered to belong in a separate family. The relationship of Rhinodinium to the Podolampadaceae needs further study. Desmoschisis was recorded for the first time in Alatosphaera and Pseudalatosphaera. Several ribotypes need further study to attribute a species name to them.},
	keywords = {Alatosphaera, Blepharocysta, desmoschisis, Gaarderiella, Lissodinium, LSU rDNA, Mysticella, Podolampas, Pseudalatosphaera, SSU rDNA},
	issn = {0031-8884},
	doi = {10.1080/00318884.2022.2158281},
	url = {https://doi.org/10.1080/00318884.2022.2158281},
	author = {Mertens, Kenneth Neil and Carbonell-Moore, M. Consuelo and Chom{\'e}rat, Nicolas and Bilien, Gwenael and Boulben, Sylviane and Guillou, Laure and Romac, Sarah and Probert, Ian and Ishikawa, Akira and N{\'e}zan, Elisabeth}
}
@article {bendif_rapid_2023,
	title = {Rapid diversification underlying the global dominance of a cosmopolitan phytoplankton},
	journal = {The ISME Journal},
	year = {2023},
	note = {Publisher: Nature Publishing Group},
	pages = {1{\textendash}11},
	abstract = {Marine phytoplankton play important roles in the global ecosystem, with a limited number of cosmopolitan keystone species driving their biomass. Recent studies have revealed that many of these phytoplankton are complexes composed of sibling species, but little is known about the evolutionary processes underlying their formation. Gephyrocapsa huxleyi, a widely distributed and abundant unicellular marine planktonic algae, produces calcified scales (coccoliths), thereby significantly affects global biogeochemical cycles via sequestration of inorganic carbon. This species is composed of morphotypes defined by differing degrees of coccolith calcification, the evolutionary ecology of which remains unclear. Here, we report an integrated morphological, ecological and genomic survey across globally distributed G. huxleyi strains to reconstruct evolutionary relationships between morphotypes in relation to their habitats. While G. huxleyi has been considered a single cosmopolitan species, our analyses demonstrate that it has evolved to comprise at least three distinct species, which led us to formally revise the taxonomy of the G. huxleyi complex. Moreover, the first speciation event occurred before the onset of the last interglacial period (\textasciitilde140 ka), while the second followed during this interglacial. Then, further rapid diversifications occurred during the most recent ice-sheet expansion of the last glacial period and established morphotypes as dominant populations across environmental clines. These results suggest that glacial-cycle dynamics contributed to the isolation of ocean basins and the segregations of oceans fronts as extrinsic drivers of micro-evolutionary radiations in extant marine phytoplankton.},
	keywords = {Microbial biooceanography, phylogenomics, population genetics, rcc1212, RCC1216, rcc1220, RCC1239, RCC1240, RCC1242, RCC1245, rcc1252, RCC1253, RCC1266, RCC1304, rcc1731, RCC1754, RCC1813, RCC1823, rcc1824, RCC1830, RCC1838, RCC1840, RCC1853, RCC1856, RCC3746, RCC4027, RCC4028, RCC4030, RCC5134, RCC5137, RCC5141, RCC6381, RCC6421, RCC6427, RCC6566, RCC6660, RCC6666, RCC911, RCC963},
	issn = {1751-7370},
	doi = {10.1038/s41396-023-01365-5},
	url = {https://www.nature.com/articles/s41396-023-01365-5},
	author = {Bendif, El Mahdi and Probert, Ian and Archontikis, Odysseas A. and Young, Jeremy R. and Beaufort, Luc and Rickaby, Rosalind E. and Filatov, Dmitry}
}
@article {sucheras-marx_coccolith_2022,
	title = {Coccolith size rules {\textendash} What controls the size of coccoliths during coccolithogenesis?},
	journal = {Marine Micropaleontology},
	volume = {170},
	year = {2022},
	pages = {102080},
	abstract = {Heterococcoliths are calcite platelets produced inside diploid coccolithophore cells and extruded to form a covering on the cell surface called a coccosphere. The size of coccoliths is an important parameter sometimes used to identify species, and it is observed to be influenced in extant species by abiotic parameters (e.g., CO2, light). However, the variable distribution of coccolith sizes occurring within a single coccosphere questions the mechanisms controlling coccolith size. A relationship between cell/coccosphere size and mean coccolith size was previously identified, called the {\textquotedblleft}coccolithophore size rules{\textquotedblright}. In this study, we query the mechanisms controlling the size of a coccolith during coccolithogenesis. A culture experiment on Gephyrocapsa huxleyi strain RCC1216 shows that coccolithogenesis occurs during the cell growth G1 interphase and newly produced coccoliths get bigger as the cell grows. These observations provide parameters for the development of two numerical models used to simulate the coccolith size distribution within a coccolithophore population. Neither model can accurately reproduce an empirical monoclonal coccolith size distribution, indicating that additional factors influence coccolith size. According to our results, coccolith size is only clearly related to cell size at the time of its formation. We confirm that application of the coccolithophore size rules model should be limited to inferring average cell dimensions from (fossil) coccolith biometry, and that comparisons are valid only in multipopulational studies. The coccolith size rule model {\textendash} the constraining effect of coccolith production during G1 interphase cell growth on coccolith size {\textendash} proposed here is applicable only for some placolith-forming species.},
	keywords = {Biometry, coccolith, coccolithophore, life cycle, RCC1216, Size variation},
	issn = {0377-8398},
	doi = {10.1016/j.marmicro.2021.102080},
	url = {https://www.sciencedirect.com/science/article/pii/S0377839821001213},
	author = {Such{\'e}ras-Marx, Baptiste and Viseur, Sophie and Walker, Charlotte E. and Beaufort, Luc and Probert, Ian and Bolton, Clara}
}
@article {johnson_nutritional_2022,
	title = {Nutritional response of a coccolithophore to changing pH and temperature},
	journal = {Limnology and Oceanography},
	volume = {n/a},
	number = {n/a},
	year = {2022},
	note = {_eprint: https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.12204},
	abstract = {Coccolithophores are a calcifying unicellular phytoplankton group that are at the base of the marine food web, and their lipid content provides a source of energy to consumers. Coccolithophores are vulnerable to ocean acidification and warming, therefore it is critical to establish the effects of climate change on these significant marine primary producers, and determine potential consequences that these changes can have on their consumers. Here, we quantified the impact of changes in pH and temperature on the nutritional condition (lipid content, particulate organic carbon/nitrogen), growth rate, and morphology of the most abundant living coccolithophore species, Emiliania huxleyi. We used a regression type approach with nine pH levels (ranging from 7.66 to 8.44) and two temperatures (15{\textdegree}C and 20{\textdegree}C). Lipid production was greater under reduced pH, and growth rates were distinctly lower at 15{\textdegree}C than at 20{\textdegree}C. The production potential of lipids, which estimates the availability of lipids to consumers, increased under 20{\textdegree}C, but decreased under low pH. The results indicate that, while consumers will benefit energetically under ocean warming, this benefit will be mitigated by ocean acidification. The carbon to nitrogen ratio was higher at 20{\textdegree}C and low pH, indicating that the nutritional quality of coccolithophores for consumers will decline under climate change. The impact of low pH on the structural integrity of the coccosphere may also mean that coccolithophores are easier to digest for consumers. Many responses suggest cellular stress, indicating that increases in temperature and reductions in pH may have a negative impact on the ecophysiology of coccolithophores.},
	keywords = {RCC1832},
	issn = {1939-5590},
	doi = {10.1002/lno.12204},
	url = {http://onlinelibrary.wiley.com/doi/abs/10.1002/lno.12204},
	author = {Johnson, Roberta and Langer, Gerald and Rossi, Sergio and Probert, Ian and Mammone, Marta and Ziveri, Patrizia}
}
@inbook {Paredes2021,
	title = {Cryopreservation of algae},
	booktitle = {Cryopreservation and freeze-drying protocols},
	volume = {2180},
	year = {2021},
	pages = {607{\textendash}621},
	publisher = {Springer Science+Business Media, LLC},
	organization = {Springer Science+Business Media, LLC},
	keywords = {cryopreservation, macroalgae, Microalgae},
	isbn = {978-1-07-160783-1},
	doi = {10.1007/978-1-0716-0783-1_32},
	url = {http://link.springer.com/10.1007/978-1-0716-0783-1_32},
	author = {Paredes, Estefania and Ward, Angela and Probert, Ian and Gouhier, L{\'e}na and Campbell, Christine N.},
	editor = {Wolkers, Willem F. and Oldenhof, Harriette}
}
@article {kawachi_rappemonads_2021,
	title = {Rappemonads are haptophyte phytoplankton},
	journal = {Current Biology},
	year = {2021},
	month = {mar},
	abstract = {Rapidly accumulating genetic data from environmental sequencing approaches have revealed an extraordinary level of unsuspected diversity within marine phytoplankton,1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11 which is responsible for around 50\% of global net primary production.12,13 However, the phenotypic identity of many of the organisms distinguished by environmental DNA sequences remains unclear. The rappemonads represent a plastid-bearing protistan lineage that to date has only been identified by environmental plastid 16S rRNA sequences.14, 15, 16, 17 The phenotypic identity of this group, which does not confidently cluster in any known algal clades in 16S rRNA phylogenetic reconstructions,15 has remained unknown since the first report of environmental sequences over two decades ago. We show that rappemonads are closely related to a haptophyte microalga, Pavlomulina ranunculiformis gen. nov. et sp. nov., and belong to a new haptophyte class, the Rappephyceae. Organellar phylogenomic analyses provide strong evidence for the inclusion of this lineage within the Haptophyta as a sister group to the Prymnesiophyceae. Members of this new class have a cosmopolitan distribution in coastal and oceanic regions. The relative read abundance of Rappephyceae in a large environmental barcoding dataset was comparable to, or greater than, those of major haptophyte species, such as the bloom-forming Gephyrocapsa huxleyi and Prymnesium parvum, and this result indicates that they likely have a significant impact as primary producers. Detailed characterization of Pavlomulina allowed for reconstruction of the ancient evolutionary history of the Haptophyta, a group that is one of the most important components of extant marine phytoplankton communities.},
	keywords = {environmental DNA sequences, morphological evolution, organellar phylogenomics, phytoplankton diversity, RCC3430, transmission electron microscopy},
	issn = {0960-9822},
	doi = {10.1016/j.cub.2021.03.012},
	url = {https://www.sciencedirect.com/science/article/pii/S0960982221003511},
	author = {Kawachi, Masanobu and Nakayama, Takuro and Kayama, Motoki and Nomura, Mami and Miyashita, Hideaki and Bojo, Othman and Rhodes, Lesley and Sym, Stuart and Pienaar, Richard N. and Probert, Ian and Inouye, Isao and Kamikawa, Ryoma}
}
@article {langer_role_2021,
	title = {Role of silicon in the development of complex crystal shapes in coccolithophores},
	journal = {New Phytologist},
	volume = {231},
	number = {5},
	year = {2021},
	note = {_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1111/nph.17230},
	pages = {1845{\textendash}1857},
	abstract = {The development of calcification by the coccolithophores had a profound impact on ocean carbon cycling, but the evolutionary steps leading to the formation of these complex biomineralized structures are not clear. Heterococcoliths consisting of intricately shaped calcite crystals are formed intracellularly by the diploid life cycle phase. Holococcoliths consisting of simple rhombic crystals can be produced by the haploid life cycle stage but are thought to be formed extracellularly, representing an independent evolutionary origin of calcification. We use advanced microscopy techniques to determine the nature of coccolith formation and complex crystal formation in coccolithophore life cycle stages. We find that holococcoliths are formed in intracellular compartments in a similar manner to heterococcoliths. However, we show that silicon is not required for holococcolith formation and that the requirement for silicon in certain coccolithophore species relates specifically to the process of crystal morphogenesis in heterococcoliths. We therefore propose an evolutionary scheme in which the lower complexity holococcoliths represent an ancestral form of calcification in coccolithophores. The subsequent recruitment of a silicon-dependent mechanism for crystal morphogenesis in the diploid life cycle stage led to the emergence of the intricately shaped heterococcoliths, enabling the formation of the elaborate coccospheres that underpin the ecological success of coccolithophores.},
	keywords = {biomineralization, Calcification, coccolith, coccolithophore, evolution, rcc, RCC1178, RCC1181, RCC1456, RCC1460, RCC1461, RCC1477, RCC1800, RCC1801, RCC3777, RCC6506, silicon},
	issn = {1469-8137},
	doi = {10.1111/nph.17230},
	url = {https://onlinelibrary.wiley.com/doi/abs/10.1111/nph.17230},
	author = {Langer, Gerald and Taylor, Alison R. and Walker, Charlotte E. and Meyer, Erin M. and Ben Joseph, Oz and Gal, Assaf and Harper, Glenn M. and Probert, Ian and Brownlee, Colin and Wheeler, Glen L.}
}
@article {Nissimov2020,
	title = {Aquatic virus culture collection: an absent (but necessary) safety net for environmental microbiologists},
	journal = {Applied Phycology},
	volume = {00},
	number = {00},
	year = {2020},
	note = {Publisher: Taylor \& Francis},
	pages = {1{\textendash}15},
	keywords = {algae, Aquatic viruses, bacteria, biological preservation, community resource, culture collection, genetic and metabolic diversity},
	issn = {2638-8081},
	doi = {10.1080/26388081.2020.1770123},
	url = {https://doi.org/10.1080/26388081.2020.1770123 https://www.tandfonline.com/doi/full/10.1080/26388081.2020.1770123},
	author = {Nissimov, Jozef I and Campbell, Christine N and Probert, Ian and Wilson, William H}
}
@article {Ribeiro2020,
	title = {Culturable diversity of Arctic phytoplankton during pack ice melting},
	journal = {Elementa: Science of the Anthropocene},
	volume = {8},
	number = {1},
	year = {2020},
	note = {tex.mendeley-tags: RCC5197,RCC5198,RCC5199,RCC5200,RCC5201,RCC5202,RCC5203,RCC5204,RCC5205,RCC5206,RCC5207,RCC5208,RCC5209,RCC5210,RCC5211,RCC5212,RCC5213,RCC5214,RCC5215,RCC5216,RCC5217,RCC5218,RCC5219,RCC5220,RCC5221,RCC5222,RCC5223,RCC5224,RCC5225,RCC5226,RCC5227,RCC5228,RCC5229,RCC5230,RCC5231,RCC5232,RCC5233,RCC5234,RCC5235,RCC5236,RCC5237,RCC5238,RCC5239,RCC5240,RCC5241,RCC5242,RCC5243,RCC5244,RCC5245,RCC5246,RCC5247,RCC5248,RCC5249,RCC5250,RCC5251,RCC5252,RCC5253,RCC5254,RCC5255,RCC5256,RCC5257,RCC5258,RCC5259,RCC5260,RCC5261,RCC5262,RCC5263,RCC5264,RCC5265,RCC5266,RCC5267,RCC5268,RCC5269,RCC5270,RCC5271,RCC5272,RCC5273,RCC5274,RCC5275,RCC5276,RCC5277,RCC5278,RCC5279,RCC5280,RCC5281,RCC5282,RCC5283,RCC5284,RCC5285,RCC5286,RCC5287,RCC5288,RCC5289,RCC5290,RCC5291,RCC5292,RCC5293,RCC5294,RCC5295,RCC5296,RCC5297,RCC5298,RCC5299,RCC5300,RCC5301,RCC5302,RCC5303,RCC5304,RCC5305,RCC5306,RCC5307,RCC5308,RCC5309,RCC5310,RCC5311,RCC5312,RCC5313,RCC5314,RCC5315,RCC5316,RCC5317,RCC5318,RCC5319,RCC5320,RCC5321,RCC5322,RCC5323,RCC5324,RCC5325,RCC5326,RCC5327,RCC5328,RCC5329,RCC5330,RCC5331,RCC5332,RCC5333,RCC5334,RCC5335,RCC5336,RCC5337,RCC5338,RCC5339,RCC5340,RCC5341,RCC5342,RCC5343,RCC5344,RCC5345,RCC5346,RCC5347,RCC5348,RCC5349,RCC5350,RCC5351,RCC5352,RCC5353,RCC5354,RCC5355,RCC5356,RCC5357,RCC5358,RCC5359,RCC5360,RCC5361,RCC5362,RCC5363,RCC5364,RCC5365,RCC5366,RCC5367,RCC5368,RCC5369,RCC5370,RCC5371,RCC5372,RCC5373,RCC5374,RCC5375,RCC5376,RCC5377,RCC5378,RCC5379,RCC5380,RCC5381,RCC5382,RCC5383,RCC5384,RCC5385,RCC5386,RCC5387,RCC5388,RCC5389,RCC5390,RCC5391,RCC5392,RCC5393,RCC5394,RCC5395,RCC5396,RCC5397,RCC5398,RCC5399,RCC5400,RCC5401,RCC5402,RCC5403,RCC5404,RCC5405,RCC5406,RCC5407,RCC5408,RCC5409,RCC5410,RCC5411,RCC5412,RCC5413,RCC5414,RCC5415,RCC5416,RCC5417,RCC5418,RCC5419,RCC5420,RCC5421,RCC5422,RCC5423,RCC5424,RCC5425,RCC5426,RCC5427,RCC5428,RCC5429,RCC5430,RCC5431,RCC5432,RCC5433,RCC5434,RCC5435,RCC5436,RCC5437,RCC5438,RCC5439,RCC5440,RCC5441,RCC5442,RCC5443,RCC5444,RCC5445,RCC5446,RCC5447,RCC5448,RCC5449,RCC5450,RCC5451,RCC5452,RCC5453,RCC5454,RCC5455,RCC5456,RCC5457,RCC5458,RCC5459,RCC5460,RCC5461,RCC5462,RCC5463,RCC5464,RCC5465,RCC5466,RCC5467,RCC5468,RCC5469,RCC5470,RCC5471,RCC5472,RCC5473,RCC5474,RCC5475,RCC5476,RCC5477,RCC5478,RCC5479,RCC5480,RCC5481,RCC5482,RCC5483,RCC5484,RCC5485,RCC5486,RCC5487,RCC5488,RCC5489,RCC5490,RCC5491,RCC5492,RCC5493,RCC5494,RCC5495,RCC5496,RCC5497,RCC5498,RCC5499,RCC5500,RCC5501,RCC5502,RCC5503,RCC5504,RCC5505,RCC5506,RCC5507,RCC5508,RCC5509,RCC5510,RCC5511,RCC5512,RCC5513,RCC5514,RCC5515,RCC5516,RCC5517,RCC5518,RCC5519,RCC5520,RCC5521,RCC5522,RCC5523,RCC5524,RCC5525,RCC5526,RCC5527,RCC5528,RCC5529,RCC5530,RCC5531,RCC5532,RCC5533,RCC5534,RCC5535,RCC5536,RCC5537,RCC5538,RCC5539,RCC5540,RCC5541,RCC5542,RCC5543,RCC5544,RCC5545,RCC5546,RCC5547,RCC5548,RCC5549,RCC5550,RCC5551,RCC5552,RCC5553,RCC5554,RCC5555,RCC5556,RCC5557,RCC5558,RCC5559,RCC5560,RCC5561,RCC5562,RCC5563,RCC5564,RCC5565,RCC5566,RCC5567,RCC5568,RCC5569,RCC5570,RCC5571,RCC5572,RCC5573,RCC5574,RCC5575,RCC5576,RCC5577,RCC5578,RCC5579,RCC5580,RCC5581,RCC5582,RCC5583,RCC5584,RCC5585,RCC5586,RCC5587,RCC5588,RCC5589,RCC5590,RCC5591,RCC5592,RCC5593,RCC5594,RCC5595,RCC5596,RCC5597,RCC5598,RCC5599,RCC5600,RCC5601,RCC5602,RCC5603,RCC5604,RCC5605,RCC5606,RCC5607,RCC5608,RCC5609,RCC5610,RCC5611,RCC5612},
	month = {feb},
	pages = {6},
	abstract = {Massive phytoplankton blooms develop at the Arctic ice edge, sometimes extending far under the pack ice. An extensive culturing effort was conducted before and during a phytoplankton bloom in Baffin Bay between April and July 2016. Different isolation strategies were applied, including flow cytometry cell sorting, manual single cell pipetting and serial dilution. Although all three techniques yielded the most common organisms, each technique retrieved specific taxa, highlighting the importance of using several methods to maximize the number and diversity of isolated strains. More than 1,000 cultures were obtained, characterized by 18S rRNA sequencing and optical microscopy and de-replicated to a subset of 276 strains presented in this work. Strains grouped into 57 genotypes defined by 100\% 18S rRNA sequence similarity. These genotypes spread across five divisions: Heterokontophyta, Chlorophyta, Cryptophyta, Haptophyta and Dinophyta. Diatoms were the most abundant group (193 strains), mostly represented by the genera Chaetoceros and Attheya. The genera Rhodomonas and Pyramimonas were the most abundant non-diatom nanoplankton strains, while Micromonas polaris dominated the picoplankton. Diversity at the class level was higher during the peak of the bloom. Potentially new species were isolated, in particular within the genera Navicula, Nitzschia, Coscinodiscus, Thalassiosira, Pyramimonas, Mantoniella and Isochrysis.},
	keywords = {RCC5197, RCC5198, RCC5199, RCC5200, RCC5201, RCC5202, RCC5203, RCC5204, RCC5205, RCC5206, RCC5207, RCC5208, RCC5209, RCC5210, RCC5211, RCC5212, RCC5213, RCC5214, RCC5215, RCC5216, RCC5217, RCC5218, RCC5219, RCC5220, RCC5221, RCC5222, RCC5223, RCC5224, RCC5225, RCC5226, RCC5227, RCC5228, RCC5229, RCC5230, RCC5231, RCC5232, RCC5233, RCC5234, RCC5235, RCC5236, RCC5237, RCC5238, RCC5239, RCC5240, RCC5241, RCC5242, RCC5243, RCC5244, RCC5245, RCC5246, RCC5247, RCC5248, RCC5249, RCC5250, RCC5251, RCC5252, RCC5253, RCC5254, RCC5255, RCC5256, RCC5257, RCC5258, RCC5259, RCC5260, RCC5261, RCC5262, RCC5263, RCC5264, RCC5265, RCC5266, RCC5267, RCC5268, RCC5269, RCC5270, RCC5271, RCC5272, RCC5273, RCC5274, RCC5275, RCC5276, RCC5277, RCC5278, RCC5279, RCC5280, RCC5281, RCC5282, RCC5283, RCC5284, RCC5285, RCC5286, RCC5287, RCC5288, RCC5289, RCC5290, RCC5291, RCC5292, RCC5293, RCC5294, RCC5295, RCC5296, RCC5297, RCC5298, RCC5299, RCC5300, RCC5301, RCC5302, RCC5303, RCC5304, RCC5305, RCC5306, RCC5307, RCC5308, RCC5309, RCC5310, RCC5311, RCC5312, RCC5313, RCC5314, RCC5315, RCC5316, RCC5317, RCC5318, RCC5319, RCC5320, RCC5321, RCC5322, RCC5323, RCC5324, RCC5325, RCC5326, RCC5327, RCC5328, RCC5329, RCC5330, RCC5331, RCC5332, RCC5333, RCC5334, RCC5335, RCC5336, RCC5337, RCC5338, RCC5339, RCC5340, RCC5341, RCC5342, RCC5343, RCC5344, RCC5345, RCC5346, RCC5347, RCC5348, RCC5349, RCC5350, RCC5351, RCC5352, RCC5353, RCC5354, RCC5355, RCC5356, RCC5357, RCC5358, RCC5359, RCC5360, RCC5361, RCC5362, RCC5363, RCC5364, RCC5365, RCC5366, RCC5367, RCC5368, RCC5369, RCC5370, RCC5371, RCC5372, RCC5373, RCC5374, RCC5375, RCC5376, RCC5377, RCC5378, RCC5379, RCC5380, RCC5381, RCC5382, RCC5383, RCC5384, RCC5385, RCC5386, RCC5387, RCC5388, RCC5389, RCC5390, RCC5391, RCC5392, RCC5393, RCC5394, RCC5395, RCC5396, RCC5397, RCC5398, RCC5399, RCC5400, RCC5401, RCC5402, RCC5403, RCC5404, RCC5405, RCC5406, RCC5407, RCC5408, RCC5409, RCC5410, RCC5411, RCC5412, RCC5413, RCC5414, RCC5415, RCC5416, RCC5417, RCC5418, RCC5419, RCC5420, RCC5421, RCC5422, RCC5423, RCC5424, RCC5425, RCC5426, RCC5427, RCC5428, RCC5429, RCC5430, RCC5431, RCC5432, RCC5433, RCC5434, RCC5435, RCC5436, RCC5437, RCC5438, RCC5439, RCC5440, RCC5441, RCC5442, RCC5443, RCC5444, RCC5445, RCC5446, RCC5447, RCC5448, RCC5449, RCC5450, RCC5451, RCC5452, RCC5453, RCC5454, RCC5455, RCC5456, RCC5457, RCC5458, RCC5459, RCC5460, RCC5461, RCC5462, RCC5463, RCC5464, RCC5465, RCC5466, RCC5467, RCC5468, RCC5469, RCC5470, RCC5471, RCC5472, RCC5473, RCC5474, RCC5475, RCC5476, RCC5477, RCC5478, RCC5479, RCC5480, RCC5481, RCC5482, RCC5483, RCC5484, RCC5485, RCC5486, RCC5487, RCC5488, RCC5489, RCC5490, RCC5491, RCC5492, RCC5493, RCC5494, RCC5495, RCC5496, RCC5497, RCC5498, RCC5499, RCC5500, RCC5501, RCC5502, RCC5503, RCC5504, RCC5505, RCC5506, RCC5507, RCC5508, RCC5509, RCC5510, RCC5511, RCC5512, RCC5513, RCC5514, RCC5515, RCC5516, RCC5517, RCC5518, RCC5519, RCC5520, RCC5521, RCC5522, RCC5523, RCC5524, RCC5525, RCC5526, RCC5527, RCC5528, RCC5529, RCC5530, RCC5531, RCC5532, RCC5533, RCC5534, RCC5535, RCC5536, RCC5537, RCC5538, RCC5539, RCC5540, RCC5541, RCC5542, RCC5543, RCC5544, RCC5545, RCC5546, RCC5547, RCC5548, RCC5549, RCC5550, RCC5551, RCC5552, RCC5553, RCC5554, RCC5555, RCC5556, RCC5557, RCC5558, RCC5559, RCC5560, RCC5561, RCC5562, RCC5563, RCC5564, RCC5565, RCC5566, RCC5567, RCC5568, RCC5569, RCC5570, RCC5571, RCC5572, RCC5573, RCC5574, RCC5575, RCC5576, RCC5577, RCC5578, RCC5579, RCC5580, RCC5581, RCC5582, RCC5583, RCC5584, RCC5585, RCC5586, RCC5587, RCC5588, RCC5589, RCC5590, RCC5591, RCC5592, RCC5593, RCC5594, RCC5595, RCC5596, RCC5597, RCC5598, RCC5599, RCC5600, RCC5601, RCC5602, RCC5603, RCC5604, RCC5605, RCC5606, RCC5607, RCC5608, RCC5609, RCC5610, RCC5611, RCC5612},
	issn = {2325-1026},
	doi = {10.1525/elementa.401},
	url = {https://www.biorxiv.org/content/10.1101/642264v1 https://www.elementascience.org/article/10.1525/elementa.401/},
	author = {Ribeiro, Catherine G{\'e}rikas and dos Santos, Adriana Lopes and Gourvil, Priscillia and Le Gall, Florence and Marie, Dominique and Tragin, Margot and Probert, Ian and Vaulot, Daniel}
}
@article {Fitzsimons2020,
	title = {Dissolved organic phosphorus uptake by marine phytoplankton is enhanced by the presence of dissolved organic nitrogen},
	journal = {Journal of Experimental Marine Biology and Ecology},
	volume = {530-531},
	number = {July},
	year = {2020},
	note = {Publisher: Elsevier tex.mendeley-tags: RC2563,RCC2565},
	month = {sep},
	pages = {151434},
	abstract = {Organic nutrients can constitute the major fractions (up to 70\%) of aquatic nitrogen (N) and phosphorus (P), but their cycling is poorly understood relative to the inorganic pools. Some phytoplankton species access P from the dissolved organic phosphorus (DOP) pool through expression of alkaline phosphatase (AP), which hydrolyses orthophosphate from organic molecules, and is thought to occur either at low concentrations of dissolved inorganic P (DIP), or elevated ratios of dissolved inorganic N (DIN) to DIP. Three algal strains native to the North-East Atlantic Ocean (coccolithophore, dinoflagellate and diatom species) were grown under representative, temperate conditions, and the dissolved N and P components amended to include dissolved organic N (DON) and DOP. The activity of AP was measured to determine the rate of DOP uptake by each algal species. The addition of DON and DOP enhanced the growth of the algal species, regardless of DIN and DIP concentrations. In cultures where the total concentrations and absolute N: P ratio was unchanged but the N pool included both DON and DIN, an increase in alkaline phosphatase activity (APA) was measured. This suggested that the presence of DON triggered the selective uptake of DOP. The uptake of organic P was confirmed by detection of adenosine in DOP-amended culture media, indicating that P had been cleaved from ADP and ATP added to the media as DOP, and cellular P concentration in these cultures exceeded the calculated concentration based on uptake of DIP only. Our data demonstrates that organic nutrients can enhance and sustain marine algal productivity. The findings have implications for marine ecosystem function and health, since climate change scenarios predict variable riverine inputs to coastal areas, altered N: P ratios, and changes in the inorganic to organic balance of the nutrient pools.},
	keywords = {Alkaline phosphatase, COASTAL WATERS, Dissolved organic nitrogen, Dissolved organic phosphorus, Marine algae, P-limitation, RCC2563, RCC2565},
	issn = {00220981},
	doi = {10.1016/j.jembe.2020.151434},
	url = {https://doi.org/10.1016/j.jembe.2020.151434 https://linkinghub.elsevier.com/retrieve/pii/S0022098119304666},
	author = {Fitzsimons, Mark F. and Probert, Ian and Gaillard, Fanny and Rees, Andrew P.}
}
@article {Langer2020,
	title = {Li partitioning into coccoliths of Emiliania huxleyi : evaluating the general role of {\textquotedblleft}vital effects{\textquotedblright} in explaining element partitioning in biogenic carbonates},
	journal = {Geochemistry, Geophysics, Geosystems},
	year = {2020},
	note = {ISBN: 0000000272 tex.mendeley-tags: RCC3652},
	month = {jun},
	pages = {0{\textendash}2},
	abstract = {Abstract Emiliania huxleyi cells were grown in artificial seawater of different Li and Ca concentrations and coccolith Li/Ca ratios determined. Coccolith Li/Ca ratios were positively correlated to seawater Li/Ca ratios only if the seawater Li concentration was changed, not if the seawater Ca concentration was changed. This Li partitioning pattern of E. huxleyi was previously also observed in the benthic foraminifer Amphistegina lessonii and inorganically precipitated calcite. We argue that Li partitioning in both E. huxleyi and A. lessonii is dominated by a coupled transmembrane transport of Li and Ca from seawater to the site of calcification. We present a refined version of a recently proposed transmembrane transport model for Li and Ca. The model assumes that Li and Ca enter the cell via Ca channels, the Li flux being dependent on the Ca flux. While the original model features a linear function to describe the experimental data, our refined version uses a power function, changing the stoichiometry of Li and Ca. The version presented here accurately predicts the observed dependence of DLi on seawater Li/Ca ratios. Our data demonstrate that minor element partitioning in calcifying organisms is partly mediated by biological processes even if the partitioning behaviour of the calcifying organism is indistinguishable from that of inorganically precipitated calcium carbonate.},
	keywords = {RCC3652},
	issn = {1525-2027},
	doi = {10.1029/2020GC009129},
	url = {https://onlinelibrary.wiley.com/doi/abs/10.1029/2020GC009129},
	author = {Langer, Gerald and Sadekov, Aleksey and Greaves, Mervyn and Nehrke, Gernot and Probert, Ian and Misra, Sambuddha and Thoms, Silke}
}
@article {GerikasRibeiro2020,
	title = {Taxonomic reassignment of \textit{Pseudohaptolina birgeri comb. nov . (Haptophyta)},
	journal = {Phycologia},
	volume = {in press},
	year = {2020},
	note = {tex.mendeley-tags: RCC5268,RCC5270},
	month = {oct},
	pages = {1{\textendash}10},
	keywords = {RCC5268, RCC5270},
	issn = {0031-8884},
	doi = {10.1080/00318884.2020.1830255},
	url = {https://www.biorxiv.org/content/10.1101/2020.05.06.081489v1 https://www.tandfonline.com/doi/full/10.1080/00318884.2020.1830255},
	author = {G{\'e}rikas Ribeiro, Catherine and Lopes dos Santos, Adriana and Probert, Ian and Vaulot, Daniel and Edvardsen, Bente}
}
@article {Iglesias2019,
	title = {NMR characterization and evaluation of antibacterial and antiobiofilm activity of organic extracts from stationary phase batch cultures of five marine microalgae (Dunaliella sp., D. salina, Chaetoceros calcitrans, C. gracilis and Tisochrysis lutea)},
	journal = {Phytochemistry},
	volume = {164},
	number = {April},
	year = {2019},
	note = {Publisher: Elsevier tex.mendeley-tags: RCC1349,RCC1811,RCC3579,RCC5,RCC5953},
	month = {aug},
	pages = {192{\textendash}205},
	keywords = {Antibacterial, Antibiofilm, Chaetoceros, Dunaliella, Metabolite identification, NMR, RCC1349, RCC1811, RCC3579, RCC5, RCC5953, Tisochrysis},
	issn = {00319422},
	doi = {10.1016/j.phytochem.2019.05.001},
	url = {https://linkinghub.elsevier.com/retrieve/pii/S0031942219300184},
	author = {Iglesias, Ma Jos{\'e} and Soengas, Raquel and Probert, Ian and Guilloud, Emilie and Gourvil, Priscillia and Mehiri, Mohamed and L{\'o}pez, Yuly and Cepas, Virginio and Guti{\'e}rrez-del-R{\'\i}o, Ignacio and Redondo-Blanco, Sa{\'u}l and Villar, Claudio J. and Lomb{\'o}, Felipe and Soto, Sara and Ortiz, Fernando L{\'o}pez}
}
@article {bendif_repeated_2019,
	title = {Repeated species radiations in the recent evolution of the key marine phytoplankton lineage Gephyrocapsa},
	journal = {Nature Communications},
	volume = {10},
	number = {1},
	year = {2019},
	pages = {4234},
	abstract = {Abstract Phytoplankton account for nearly half of global primary productivity and strongly affect the global carbon cycle, yet little is known about the forces that drive the evolution of these keystone microscopic organisms. Here we combine morphometric data from the fossil record of the ubiquitous coccolithophore genus Gephyrocapsa with genomic analyses of extant species to assess the genetic processes underlying Pleistocene palaeontological patterns. We demonstrate that all modern diversity in Gephyrocapsa (including Emiliania huxleyi ) originated in a rapid species radiation during the last 0.6 Ma, coincident with the latest of the three pulses of Gephyrocapsa diversification and extinction documented in the fossil record. Our evolutionary genetic analyses indicate that new species in this genus have formed in sympatry or parapatry, with occasional hybridisation between species. This sheds light on the mode of speciation during evolutionary radiation of marine phytoplankton and provides a model of how new plankton species form.},
	keywords = {RCC1253, RCC1296, RCC3370, RCC3711, RCC4028, RCC4030, RCC4032, RCC4033, RCC4034},
	issn = {2041-1723},
	doi = {10.1038/s41467-019-12169-7},
	url = {https://www.nature.com/articles/s41467-019-12169-7},
	author = {Bendif, El Mahdi and Nevado, Bruno and Wong, Edgar L. Y. and Hagino, Kyoko and Probert, Ian and Young, Jeremy R. and Rickaby, Rosalind E. M. and Filatov, Dmitry A.}
}
@article {Pierre2019,
	title = {What is in store for EPS microalgae in the next decade?},
	journal = {Molecules},
	volume = {24},
	number = {23},
	year = {2019},
	month = {nov},
	pages = {4296},
	abstract = {Microalgae and their metabolites have been an El Dorado since the turn of the 21st century. Many scientific works and industrial exploitations have thus been set up. These developments have often highlighted the need to intensify the processes for biomass production in photo-autotrophy and exploit all the microalgae value including ExoPolySaccharides (EPS). Indeed, the bottlenecks limiting the development of low value products from microalgae are not only linked to biology but also to biological engineering problems including harvesting, recycling of culture media, photoproduction, and biorefinery. Even respecting the so-called {\textquotedblleft}Biorefinery Concept{\textquotedblright}, few applications had a chance to emerge and survive on the market. Thus, exploiting EPS from microalgae for industrial applications in some low-value markets such as food is probably not a mature proposition considering the competitiveness of polysaccharides from terrestrial plants, macroalgae, and bacteria. However, it does not imply drawing a line on their uses but rather {\textquotedblleft}thinking them{\textquotedblright} differently. This review provides insights into microalgae, EPS, and their exploitation. Perspectives on issues affecting the future of EPS microalgae are also addressed with a critical point of view.},
	keywords = {application, eps, exopolysaccharides, market, Microalgae},
	issn = {1420-3049},
	doi = {10.3390/molecules24234296},
	url = {https://www.mdpi.com/1420-3049/24/23/4296},
	author = {Pierre, Guillaume and Delattre, C{\'e}dric and Dubessay, Pascal and Jubeau, S{\'e}bastien and Vialleix, Carole and Cadoret, Jean-Paul and Probert, Ian and Michaud, Philippe}
}
@article {Meng2018,
	title = {Analysis of the genomic basis of functional diversity in dinoflagellates using a transcriptome-based sequence similarity network},
	journal = {Molecular Ecology},
	year = {2018},
	note = {tex.mendeley-tags: RCC1491,RCC1516,RCC3387,RCC3468,RCC3507},
	pages = {0{\textendash}2},
	abstract = {Dinoflagellates are one of the most abundant and functionally diverse groups of eukaryotes. Despite an overall scarcity of genomic information for dinoflagellates, constantly emerging high-throughput sequencing resources can be used to characterize and compare these organisms. We assembled de novo and processed 46 dinoflagellate transcriptomes and used a sequence similarity network (SSN) to compare the underlying genomic basis of functional features within the group. This approach constitutes the most comprehensive picture to date of the genomic potential of dinoflagellates. A core predicted proteome composed of 252 connected components (CCs) of putative conserved protein domains (pCDs) was identified. Of these, 206 were novel and 16 lacked any functional annotation in public databases. Integration of functional information in our network analyses allowed investigation of pCDs specifically associated to functional traits. With respect to toxicity, sequences homologous to those of proteins found in species with toxicity potential (e.g. sxtA4 and sxtG) were not specific to known toxin-producing species. Although not fully specific to symbiosis, the most represented functions associated with proteins involved in the symbiotic trait were related to membrane processes and ion transport. Overall, our SSN approach led to identification of 45,207 and 90,794 specific and constitutive pCDs of respectively the toxic and symbiotic species represented in our analyses. Of these, 56\% and 57\% respectively (i.e. 25,393 and 52,193 pCDs) completely lacked annotation in public databases. This stresses the extent of our lack of knowledge, while emphasizing the potential of SSNs to identify candidate pCDs for further functional genomic characterization. This article is protected by copyright. All rights reserved.},
	keywords = {Genomics/Proteomics, Microbial Biology, Molecular Evolution, Protists, rcc1491, RCC1516, RCC3387, rcc3468, rcc3507, transcriptomics},
	issn = {09621083},
	doi = {10.1111/mec.14579},
	url = {http://www.ncbi.nlm.nih.gov/pubmed/29624751\%0Ahttp://doi.wiley.com/10.1111/mec.14579},
	author = {Meng, Arnaud and Corre, Erwan and Probert, Ian and Gutierrez-Rodriguez, Andres and Siano, Raffaele and Annamale, Anita and Alberti, Adriana and Da Silva, Corinne and Wincker, Patrick and Le Crom, St{\'e}phane and Not, Fabrice and Bittner, Lucie}
}
@article {Partensky2018,
	title = {A novel species of the marine cyanobacterium Acaryochloris with a unique pigment content and lifestyle},
	journal = {Scientific Reports},
	volume = {8},
	number = {1},
	year = {2018},
	note = {tex.mendeley-tags: RCC1774},
	month = {dec},
	pages = {9142},
	keywords = {RCC1774},
	issn = {2045-2322},
	doi = {10.1038/s41598-018-27542-7},
	url = {http://www.nature.com/articles/s41598-018-27542-7},
	author = {Partensky, Fr{\'e}d{\'e}ric and Six, Christophe and Ratin, Morgane and Garczarek, Laurence and Vaulot, Daniel and Probert, Ian and Calteau, Alexandra and Gourvil, Priscillia and Marie, Dominique and Gr{\'e}bert, Th{\'e}ophile and Bouchier, Christiane and Le Panse, Sophie and Gachenot, Martin and Rodr{\'\i}guez, Francisco and Garrido, Jos{\'e} L.}
}
@article {Walker2018,
	title = {The requirement for calcification differs between ecologically important coccolithophore species},
	journal = {New Phytologist},
	volume = {in press},
	year = {2018},
	note = {tex.mendeley-tags: RCC1731},
	month = {jun},
	keywords = {Calcification, coccolithophore, Coccolithus braarudii, Emiliania huxleyi, phytoplankton, rcc1731},
	issn = {0028646X},
	doi = {10.1111/nph.15272},
	url = {http://doi.wiley.com/10.1111/nph.15272},
	author = {Walker, Charlotte E. and Taylor, Alison R. and Langer, Gerald and Durak, Gra{\.z}yna M. and Heath, Sarah and Probert, Ian and Tyrrell, Toby and Brownlee, Colin and Wheeler, Glen L.}
}
@article {Bolton2016,
	title = {Decrease in coccolithophore calcification and CO2 since the middle Miocene},
	journal = {Nature Communications},
	volume = {7},
	year = {2016},
	note = {tex.mendeley-tags: 2016,rcc},
	pages = {10284},
	abstract = {Marine algae are instrumental in carbon cycling and atmospheric carbon dioxide (CO2) regulation. One group, coccolithophores, uses carbon to photosynthesize and to calcify, covering their cells with chalk platelets (coccoliths). How ocean acidification influences coccolithophore calcification is strongly debated, and the effects of carbonate chemistry changes in the geological past are poorly understood. This paper relates degree of coccolith calcification to cellular calcification, and presents the first records of size-normalized coccolith thickness spanning the last 14 Myr from tropical oceans. Degree of calcification was highest in the low-pH, high-CO2 Miocene ocean, but decreased significantly between 6 and 4 Myr ago. Based on this and concurrent trends in a new alkenone ep record, we propose that decreasing CO2 partly drove the observed trend via reduced cellular bicarbonate allocation to calcification. This trend reversed in the late Pleistocene despite low CO2, suggesting an additional regulator of calcification such as alkalinity. 1},
	keywords = {2016, rcc},
	issn = {2041-1723},
	doi = {10.1038/ncomms10284},
	url = {http://www.nature.com/doifinder/10.1038/ncomms10284},
	author = {Bolton, Clara T. and Hern{\'a}ndez-S{\'a}nchez, Mar{\'\i}a T. and Fuertes, Miguel-{\'A}ngel and Gonz{\'a}lez-Lemos, Sa{\'u}l and Abrevaya, Lorena and M{\'e}ndez-Vicente, Ana and Flores, Jos{\'e}-Abel and Probert, Ian and Giosan, Liviu and Johnson, Joel and Stoll, Heather M.}
}
@article {Bendif2016,
	title = {Recent reticulate evolution in the ecologically dominant lineage of coccolithophores},
	journal = {Frontiers in Microbiology},
	volume = {7},
	number = {May},
	year = {2016},
	note = {tex.mendeley-tags: 2016,RCC4032,RCC4033,RCC4034,RCC4035,RCC4036,rcc,sbr?hyto},
	month = {may},
	keywords = {2016, coccolithophores, cyto-nuclear discordance, diversity, Emiliania, evolution, Gephyrocapsa, introgressive hybridization, rcc, RCC4032, RCC4033, RCC4034, RCC4035, RCC4036, Reticulofenestra, sbr?hyto},
	issn = {1664-302X},
	doi = {10.3389/fmicb.2016.00784},
	url = {http://journal.frontiersin.org/article/10.3389/fmicb.2016.00784 http://journal.frontiersin.org/Article/10.3389/fmicb.2016.00784/abstract},
	author = {Bendif, El Mahdi and Probert, Ian and D{\'\i}az-Rosas, Francisco and Thomas, Daniela and van den Engh, Ger and Young, Jeremy R. and von Dassow, Peter}
}
@article {Durak2016,
	title = {A role for diatom-like silicon transporters in calcifying coccolithophores},
	journal = {Nature Communications},
	volume = {7},
	number = {February},
	year = {2016},
	note = {tex.mendeley-tags: 2016,RCC1130,RCC1303,RCC1453,RCC1456,RCC3432},
	pages = {10543},
	abstract = {Biomineralisation by marine phytoplankton, such as the silicifying diatoms and calcifying coccolithophores, plays an important role in carbon and nutrient cycling in the oceans. Silicification and calcification are distinct cellular processes with no known common mechanisms. As a result, it is thought that coccolithophores are able to outcompete diatoms in Si-depleted waters, which can contribute to the formation of coccolithophore blooms. Here, we show that an expanded family of diatom-like silicon transporters (SITs) are present in both silicifying and calcifying haptophyte phytoplankton, including some coccolithophores of global ecological importance. We find an essential role for Si in calcification in these coccolithophores, indicating that Si uptake contributes to the very different forms of biomineralisation in diatoms and coccolithophores. However, SITs and the requirement for Si are significantly absent from the highly abundant bloom-forming coccolithophores, such as Emiliania huxleyi. These very different requirements for Si in coccolithophores are likely to have major influence on their competitive interactions with diatoms and other siliceous phytoplankton.},
	keywords = {(RCC1130, (RCC1456), 2016, biomineralisation, coccolithophores, Gephyrocapsa oceanica (RCC1303) and Scyphosphaera, haptophytes, RCC1130, RCC1303, RCC1453, RCC1456, RCC3432, silica, TMR5 (RCC3432{\textemdash}Sea of Japan) and PZ241 (RCC1453{\textemdash}Med},
	issn = {2041-1723},
	doi = {10.1038/ncomms10543},
	author = {Durak, Grazyna M and Taylor, Alison R and Probert, Ian and de Vargas, Colomban and Audic, St{\'e}phane and Schroeder, Declan C and Brownlee, Colin and Wheeler, Glen L}
}
@article {Supraha2015,
	title = {Eco-physiological adaptation shapes the response of calcifying algae to nutrient limitation},
	journal = {Scientific Reports},
	volume = {5},
	number = {November},
	year = {2015},
	note = {Publisher: Nature Publishing Group tex.mendeley-tags: 2015,RCC1323,RCC1334},
	pages = {16499},
	keywords = {2015, RCC1323, RCC1334},
	issn = {2045-2322},
	doi = {10.1038/srep16499},
	url = {http://www.nature.com/articles/srep16499},
	author = {{\v S}upraha, Luka and Gerecht, Andrea C. and Probert, Ian and Henderiks, Jorijntje}
}
@article {Bendif2015,
	title = {Morphological and phylogenetic characterization of new gephyrocapsa isolates suggests introgressive hybridization in the Emiliania/Gephyrocapsa complex (haptophyta)},
	journal = {Protist},
	volume = {166},
	number = {3},
	year = {2015},
	note = {tex.mendeley-tags: 2015,RCC1281,RCC1282,RCC1284,RCC1286,RCC1292,RCC1300,RCC1305,RCC1307,RCC1316,RCC1317,RCC1318,RCC1319,RCC1320,RCC1562,RCC1839,RCC3370,RCC3862,RCC3898,rcc},
	pages = {323{\textendash}336},
	abstract = {The coccolithophore genus Gephyrocapsa contains a cosmopolitan assemblage of pelagic species, including the bloom-forming Gephyrocapsa oceanica, and is closely related to the emblematic coccolithophore Emiliania huxleyi within the No{\"e}laerhabdaceae. These two species have been extensively studied and are well represented in culture collections, whereas cultures of other species of this family are lacking. We report on three new strains of Gephyrocapsa isolated into culture from samples from the Chilean coastal upwelling zone using a novel flow cytometric single-cell sorting technique. The strains were characterized by morphological analysis using scanning electron microscopy and phylogenetic analysis of 6 genes (nuclear 18S and 28S rDNA, plastidial 16S and tufA, and mitochondrial cox1 and cox3 genes). Morphometric features of the coccoliths indicate that these isolates are distinct from G. oceanica and best correspond to G. muellerae. Surprisingly, both plastidial and mitochondrial gene phylogenies placed these strains within the E. huxleyi clade and well separated from G. oceanica isolates, making Emiliania appear polyphyletic. The only nuclear sequence difference, 1bp in the 28S rDNA region, also grouped E. huxleyi with the new Gephyrocapsa isolates and apart from G. oceanica. Specifically, the G. muellerae morphotype strains clustered with the mitochondrial β clade of E. huxleyi, which, like G. muellerae, has been associated with cold (temperate and sub-polar) waters. Among putative evolutionary scenarios that could explain these results we discuss the possibility that E. huxleyi is not a valid taxonomic unit, or, alternatively the possibility of past hybridization and introgression between each E. huxleyi clade and older Gephyrocapsa clades. In either case, the results support the transfer of Emiliania to Gephyrocapsa. These results have important implications for relating morphological species concepts to ecological and evolutionary units of diversity.},
	keywords = {2015, coccolithophores, Emiliania huxleyi, Gephyrocapsa muellerae, Gephyrocapsa oceanica, hybridization, phylogeny., rcc, RCC1281, RCC1282, RCC1284, RCC1286, RCC1292, RCC1300, RCC1305, RCC1307, RCC1316, RCC1317, RCC1318, RCC1319, RCC1320, RCC1562, RCC1839, RCC3370, RCC3862, RCC3898, species concept},
	issn = {14344610},
	doi = {10.1016/j.protis.2015.05.003},
	url = {http://www.sciencedirect.com/science/article/pii/S1434461015000243},
	author = {Bendif, El Mahdi and Probert, Ian and Young, Jeremy R. and von Dassow, Peter}
}
@article {Andersen2015,
	title = {Phaeocystis rex sp. nov. (Phaeocystales, Prymnesiophyceae): a new solitary species that produces a multilayered scale cell covering},
	journal = {European Journal of Phycology},
	volume = {50},
	number = {2},
	year = {2015},
	note = {Publisher: Taylor \& Francis tex.mendeley-tags: 2015,RCC 4025,rcc},
	pages = {207{\textendash}222},
	abstract = {A morphologically distinct marine species, Phaeocystis rex sp. nov., was described on the basis of light microscopy, transmission electron microscopy and DNA sequence comparisons. Non-motile cells were solitary (non-colonial), 6{\textendash}10 {\textmu}m in diameter and 8{\textendash}15 {\textmu}m long, and possessed chloroplasts with distinctive finger-like lobes. TEM observations demonstrated the presence of two short flagella and a very short haptonema that arose from an invagination of the protoplast. Non-motile cells were surrounded by one to several dense layers composed of scales, presumably unmineralized, and an amorphous material. Phylogenetic analyses based upon combined partial nucleotide sequences for five nuclear-or plastid-encoded genes (18S rRNA, 28S rRNA, 16S rRNA, psbA and rbcL) from cultured strains and from uncharacterized acantharian symbionts confirmed that P. rex was a distinct species. These analyses implied that P. rex occupies an intermediate evolutionary position between solitary and colonial Phaeocystis species.},
	keywords = {2015, algae, organic scales, Phaeocystales, Phaeocystis rex, Prymnesiophyceae, rcc, RCC4025, RCC?o?dd, SBR$_\textrmP$hyto$_\textrmE$PPO, systematics, ultrastructure},
	issn = {0967-0262},
	doi = {10.1080/09670262.2015.1024287},
	url = {http://www.tandfonline.com/doi/full/10.1080/09670262.2015.1024287},
	author = {Andersen, Robert A. and Bailey, J. Craig and Decelle, Johan and Probert, Ian}
}
@article {Decelle2015,
	title = {PhytoREF: a reference database of the plastidial 16S rRNA gene of photosynthetic eukaryotes with curated taxonomy},
	journal = {Molecular Ecology Resources},
	volume = {15},
	number = {6},
	year = {2015},
	note = {tex.mendeley-tags: 2015,macumba,rcc,sbr?hyto$_\textrmd$ipo,sbr?hyto?ppo},
	pages = {1435{\textendash}1445},
	abstract = {Photosynthetic eukaryotes have a critical role as the main producers in most ecosystems of the biosphere. The ongo- ing environmental metabarcoding revolution opens the perspective for holistic ecosystems biological studies of these organisms, in particular the unicellular microalgae that often lack distinctive morphological characters and have complex life cycles. To interpret environmental sequences, metabarcoding necessarily relies on taxonomically curated databases containing reference sequences of the targeted gene (or barcode) from identified organisms. To date, no such reference framework exists for photosynthetic eukaryotes. In this study, we built the PhytoREF data- base that contains 6490 plastidial 16S rDNA reference sequences that originate from a large diversity of eukaryotes representing all known major photosynthetic lineages. We compiled 3333 amplicon sequences available from public databases and 879 sequences extracted from plastidial genomes, and generated 411 novel sequences from cultured marine microalgal strains belonging to different eukaryotic lineages. A total of 1867 environmental Sanger 16S rDNA sequences were also included in the database. Stringent quality filtering and a phylogeny-based taxonomic classifica- tion were applied for each 16S rDNA sequence. The database mainly focuses on marine microalgae, but sequences from land plants (representing half of the PhytoREF sequences) and freshwater taxa were also included to broaden the applicability of PhytoREF to different aquatic and terrestrial habitats. PhytoREF, accessible via a web interface (http://phytoref.fr), is a new resource in molecular ecology to foster the discovery, assessment and monitoring of the diversity of photosynthetic eukaryotes using high-throughput sequencing.},
	keywords = {2015, MACUMBA, rcc, RCC?o?dd, SBR$_\textrmP$hyto$_\textrmD$IPO, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto$_\textrmd$ipo, sbr?hyto?ppo},
	issn = {1755098X},
	doi = {10.1111/1755-0998.12401},
	url = {http://doi.wiley.com/10.1111/1755-0998.12401},
	author = {Decelle, Johan and Romac, Sarah and Stern, Rowena F. and Bendif, El Mahdi and Zingone, Adriana and Audic, St{\'e}phane and Guiry, Michael D. and Guillou, Laure and Tessier, D{\'e}sir{\'e} and Le Gall, Florence and Gourvil, Priscillia and dos Santos, Adriana Lopes and Probert, Ian and Vaulot, Daniel and de Vargas, Colomban and Christen, Richard}
}
@article {Probert2014a,
	title = {Brandtodinium gen. nov. and B. nutricula comb. Nov. (Dinophyceae), a dinoflagellate commonly found in symbiosis with polycystine radiolarians},
	journal = {Journal of Phycology},
	volume = {50},
	number = {2},
	year = {2014},
	note = {tex.mendeley-tags: RCC3378,RCC3379,RCC3380,RCC3381,RCC3382,RCC3383,RCC3384,RCC3385,RCC3386,RCC3387,RCC3388},
	pages = {388{\textendash}399},
	abstract = {Symbiotic interactions between pelagic hosts and microalgae have received little attention, although they are widespread in the photic layer of the world ocean, where they play a fundamental role in the ecology of the planktonic ecosystem. Polycystine radiolarians (including the orders Spumellaria, Collodaria and Nassellaria) are planktonic heterotrophic protists that are widely distributed and often abundant in the ocean. Many polycystines host symbiotic microalgae within their cytoplasm, mostly thought to be the dinoflagellate Scrippsiella nutricula, a species originally described by Karl Brandt in the late nineteenth century as Zooxanthella nutricula. The free-living stage of this dinoflagellate has never been characterized in terms of morphology and thecal plate tabulation. We examined morphological characters and sequenced conservative ribosomal markers of clonal cultures of the free-living stage of symbiotic dinoflagellates isolated from radiolarian hosts from the three polycystine orders. In addition, we sequenced symbiont genes directly from several polycystine-symbiont holobiont specimens from different oceanic regions. Thecal plate arrangement of the free-living stage does not match that of Scrippsiella or related genera, and LSU and SSU rDNA-based molecular phylogenies place these symbionts in a distinct clade within the Peridiniales. Both phylogenetic analyses and the comparison of morphological features of culture strains with those reported for other closely related species support the erection of a new genus that we name Brandtodinium gen. nov. and the recombination of S. nutricula as B. nutricula comb. nov.},
	keywords = {Dinoflagellate, MACUMBA, Peridiniales, polycystines, Radiolaria, rcc, RCC3378, RCC3379, RCC3380, RCC3381, RCC3382, RCC3383, RCC3384, RCC3385, RCC3386, RCC3387, RCC3388, SBR$_\textrmP$hyto$_\textrmD$PO, Scrippsiella, symbiosis, taxonomy, Zooxanthella},
	doi = {10.1111/jpy.12174},
	url = {http://dx.doi.org/10.1111/jpy.12174},
	author = {Probert, Ian and Siano, Raffaele and Poirier, Camille and Decelle, Johan and Biard, Tristan and Tuji, Akihiro and Suzuki, Noritoshi and Not, Fabrice}
}
@article {Bendif2014,
	title = {Genetic delineation between and within the widespread coccolithophore morpho-species Emiliania huxleyi and Gephyrocapsa oceanica (Haptophyta)},
	journal = {Journal of Phycology},
	volume = {50},
	year = {2014},
	note = {tex.mendeley-tags: 2014,cc3549,rcc,rcc1210,rcc1213,rcc1220,rcc1227,rcc1229,rcc1242,rcc1252,rcc1253,rcc1258,rcc1259,rcc1260,rcc1271,rcc1281,rcc1288,rcc1292,rcc1297,rcc1300,rcc1303,rcc1305,rcc1316,rcc1562,rcc174,rcc1839,rcc3545,rrcc1247,sbr?hyto?ppo},
	pages = {140{\textendash}148},
	keywords = {2014, cc3549, rcc, rcc1210, RCC1213, rcc1220, rcc1227, rcc1229, RCC1242, rcc1252, RCC1253, rcc1258, RCC1259, rcc1260, rcc1271, RCC1281, rcc1288, RCC1292, rcc1297, RCC1300, RCC1303, RCC1305, RCC1316, RCC1562, rcc174, RCC1839, rcc3545, rrcc1247, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto?ppo},
	doi = {10.1111/jpy.12147},
	author = {Bendif, El Mahdi and Probert, Ian and Carmichael, Margaux and Romac, Sarah and Hagino, Kyoko and de Vargas, Colomban}
}
@article {Abida2013,
	title = {Bioprospecting marine plankton},
	journal = {Marine Drugs},
	volume = {11},
	number = {11},
	year = {2013},
	note = {tex.mendeley-tags: 2013,rcc,sbr?hyto$_\textrmd$ipo,sbr?hyto?ppo},
	pages = {4594{\textendash}4611},
	keywords = {2013, MicroB3, rcc, SBR$_\textrmP$hyto$_\textrmD$PO, sbr?hyto$_\textrmd$ipo, sbr?hyto?ppo},
	doi = {10.3390/md11114594},
	url = {http://www.mdpi.com/1660-3397/11/11/4594},
	author = {Abida, Heni and Ruchaud, Sandrine and Rios, Laurent and Humeau, Anne and Probert, Ian and de Vargas, Colomban and Bach, St{\'e}phane and Bowler, Chris}
}
@article {Bendif2013,
	title = {On the description of Tisochrysis lutea gen . nov . sp . nov . and Isochrysis nuda sp. nov. in the Isochrysidales, and the transfer of Dicrateria to the Prymnesiales (Haptophyta)},
	journal = {Journal of Applied Phycology},
	volume = {25},
	year = {2013},
	note = {tex.mendeley-tags: 2013,RCC1195,RCC1207,RCC1281,RCC1286,RCC1344,RCC1346,RCC1347,RCC1348,RCC1349,RCC1350,RCC1353,RCC2477,RCC3681,RCC3684,RCC3686,RCC3687,RCC3690,RCC3691,RCC3692,RCC3693,RCC3694,RCC3695,RCC3696,RCC3699,RCC3701,RCC3707,rcc,sbr?hyto?ppo},
	pages = {1763{\textendash}1776},
	keywords = {2013, dicrateria, imantonia, isochrysidaceae, isochrysis galbana, phylogeny, rcc, RCC1195, RCC1207, RCC1281, RCC1286, RCC1344, RCC1346, RCC1347, RCC1348, RCC1349, RCC1350, RCC1353, RCC2477, RCC3681, RCC3684, RCC3686, RCC3687, RCC3690, RCC3691, RCC3692, RCC3693, RCC3694, RCC3695, RCC3696, RCC3699, RCC3701, RCC3707, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto?ppo, taxonomy, ultrastructure},
	doi = {10.1007/s10811-013-0037-0},
	author = {Bendif, El Mahdi and Probert, Ian and Schroeder, Declan C and de Vargas, Colomban}
}
@article {Guillou2013,
	title = {The protist ribosomal reference database (PR2): a catalog of unicellular eukaryote small SubUnit rRNA sequences with curated taxonomy},
	journal = {Nucleic Acids Research},
	volume = {41},
	year = {2013},
	note = {tex.mendeley-tags: 2013,rcc,sbr?hyto$_\textrmd$ipo,sbr?hyto?ppo},
	pages = {D597{\textendash}D604},
	keywords = {2013, rcc, SBR$_\textrmP$hyto$_\textrmD$PO, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto$_\textrmd$ipo, sbr?hyto?ppo},
	doi = {10.1093/nar/gks1160},
	author = {Guillou, Laure and Bachar, Dipankar and Audic, St{\'e}phane and Bass, David and Berney, Cedric and Bittner, Lucie and Boutte, Christophe and Burgaud, Gaetan and de Vargas, Colomban and Decelle, Johan and del Campo, Javier and Dolan, John and Dunthorn, Micah and Bente, Edvardsen and Holzmann, Maria and Kooistra, Wiebe H C F and Lara, Enrique and Lebescot, Noan and Logares, Ramiro and Mah{\'e}, Fr{\'e}d{\'e}ric and Massana, Ramon and Montresor, Marina and Morard, Raphael and Not, Fabrice and Pawlowski, Jan and Probert, Ian and Sauvadet, Anne-Laure and Siano, Raffaele and Stoeck, Thorsten and Vaulot, Daniel and Zimmermann, Pascal and Christen, Richard}
}
@article {Frada2012,
	title = {In situ survey of life cycle phases of the coccolithophore Emiliania huxleyi (Haptophyta)},
	journal = {Environmental Microbiology},
	volume = {14},
	number = {6},
	year = {2012},
	note = {Publisher: Blackwell Publishing Ltd tex.mendeley-tags: 2012,rcc,sbr?hyto?ppo},
	pages = {1558{\textendash}1569},
	abstract = {The cosmopolitan coccolithophore Emiliania huxleyi is characterized by a strongly differentiated haplodiplontic life cycle consisting of a diploid phase, generally bearing coccoliths (calcified) but that can be also non-calcified, and a non-calcified biflagellated haploid phase. Given most studies have focused on the bloom-producing calcified phase, there is little-to-no information about non-calcified cells in nature. Using field mesocoms as experimental platforms, we quantitatively surveyed calcified and non-calcified cells using the combined calcareous detection fluorescent in situ hybridization (COD-FISH) method and qualitatively screened for haploid specific transcripts using reverse transcription-PCR during E. huxleyi bloom successions. Diploid, calcified cells formed dense blooms that were followed by the massive proliferation of E. huxleyi viruses (EhVs), which caused bloom demise. Non-calcified cells were also detected throughout the experiment, accounting for a minor fraction of the population but becoming progressively more abundant during mid-late bloom periods concomitant with EhV burst. Non-calcified cell growth also paralleled a distinct window of haploid-specific transcripts and the appearance of autotrophic flagellates morphologically similar to haploid cells, both of which are suggestive of meiosis and sexual life cycling during natural blooms of this prominent marine phytoplankton species.},
	keywords = {2012, rcc, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto?ppo},
	doi = {10.1111/j.1462-2920.2012.02745.x},
	url = {http://dx.doi.org/10.1111/j.1462-2920.2012.02745.x},
	author = {Frada, Miguel J and Bidle, Kay D and Probert, Ian and de Vargas, Colomban}
}
@article {Reid2011,
	title = {Coccolithophores: Functional biodiversity, enzymes and bioprospecting},
	journal = {Marine Drugs},
	volume = {9},
	number = {4},
	year = {2011},
	note = {tex.mendeley-tags: 2011,rcc},
	pages = {586{\textendash}602},
	keywords = {2011, rcc, SBR$_\textrmP$hyto$_\textrmE$PPO},
	doi = {10.3390/md9040586},
	url = {http://www.mdpi.com/1660-3397/9/4/586/},
	author = {Reid, Emma L and Worthy, Charlotte A and Probert, Ian and Ali, Sohail T and Love, John and Napier, Johnathan and Littlechild, Jenny A and Somerfield, Paul J and Allen, Michael J}
}
@article {Frada2010,
	title = {A guide to extant coccolithophores (Calcihaptophycidae, Haptophyta) using light microscopy.},
	journal = {Journal of Nannoplankton Research},
	volume = {31},
	year = {2010},
	note = {tex.mendeley-tags: 2010,rcc,sbr?hyto?ppo},
	pages = {58{\textendash}112},
	keywords = {2010, ? No DOI found, rcc, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto?ppo},
	author = {Frada, Miguel and Young, Jeremy and Cach{\~a}o, M{\'a}rio and Lino, S{\'\i}lvia and Martins, Ana and Narciso, {\'A}urea and Probert, Ian and de Vargas, Colomban}
}
@article {Liu2010,
	title = {A timeline of the environmental genetics of the haptophytes},
	journal = {Molecular Biology and Evolution},
	volume = {27},
	year = {2010},
	note = {tex.mendeley-tags: 2010,rcc,sbr?hyto?ppo},
	pages = {171{\textendash}176},
	abstract = {The use of genomic data and the rise of phylogenomics have radically changed our view of the eukaryotic tree of life at a high taxonomic level by identifying four to six "supergroups". Yet our understanding of the evolution of key innovations within each of these supergroups is limited because of poor species sampling relative to the massive diversity encompassed by each supergroup. Here we apply a multigene approach that incorporates a wide taxonomic diversity to infer the timeline of the emergence of strategic evolutionary transitions in the haptophytes, a group of ecologically and biogeochemically significant marine protists that belong to the Chromalveolata supergroup. Four genes (SSU, LSU, tufA and rbcL) were extensively analyzed under several Bayesian models to assess the robustness of the phylogeny, particularly with respect to (i) data partitioning, (ii) the origin of the genes (host vs. endosymbiont), (iii) across-site rate variation and (iv) across-lineage rate variation. We show with a relaxed clock analysis that the origin of haptophytes dates back to 824 MYA (95\% highest probability density 1031-637 MYA). Our dating results show that the ability to calcify evolved earlier than previously thought, between 329-291 MYA, in the Carboniferous period, and that the transition from mixotrophy to autotrophy occurred during the same time period. Although these two transitions precede a habitat change of major diversities from coastal / neritic waters to the pelagic realm (291-243 MYA, around the P/Tr boundary event), the emergence of calcification, full autotrophy and oceanic lifestyle seem mutually independent.},
	keywords = {2010, rcc, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto?ppo},
	doi = {10.1093/molbev/msp222},
	url = {http://mbe.oxfordjournals.org/cgi/content/abstract/msp222v1},
	author = {Liu, Hui and Aris-Brosou, Stephane and Probert, Ian and de Vargas, Colomban}
}
@article {VonDassow2009,
	title = {Transcriptome analysis of functional differentiation between haploid and diploid cells of Emiliania huxleyi, a globally significant photosynthetic calcifying cell},
	journal = {Genome Biology},
	volume = {10},
	number = {10},
	year = {2009},
	note = {tex.mendeley-tags: 2009,rcc,rcc1216,rcc1217,sbr?hyto?ppo},
	pages = {R114},
	abstract = {BACKGROUND:Eukaryotes are classified as either haplontic, diplontic, or haplo-diplontic, depending on which ploidy levels undergo mitotic cell division in the life cycle. Emiliania huxleyi is one of the most abundant phytoplankton species in the ocean, playing an important role in global carbon fluxes, and represents haptophytes, an enigmatic group of unicellular organisms that diverged early in eukaryotic evolution. This species is haplo-diplontic. Little is known about the haploid cells, but they have been hypothesized to allow persistence of the species between the yearly blooms of diploid cells. We sequenced over 38000 Expressed Sequence Tags (ESTs) from haploid and diploid E. huxleyi normalized cDNA libraries to identify genes involved in important processes specific to each life phase (2N calcification or 1N motility), and to better understand the haploid phase of this prominent haplo-diplontic organism.RESULTS:The haploid and diploid transcriptomes showed a dramatic differentiation, with [almost equal to]20\% greater transcriptome richness in diploid cells than in haploid cells and only [less than or equal to]50\% of transcripts estimated to be common between the two phases. The major functional category of transcripts differentiating haploids included signal transduction and motility genes. Diploid-specific transcripts included Ca2+, H+, and HCO3- pumps. Potential factors differentiating the transcriptomes included haploid-specific Myb transcription factor homologs and an unusual diploid-specific histone H4 homolog.CONCLUSIONS:This study permitted the identification of genes likely involved in diploid-specific biomineralization, haploid-specific motility, and transcriptional control. Greater transcriptome richness in diploid cells suggests they may be more versatile for exploiting a diversity of rich environments whereas haploid cells are intrinsically more streamlined.},
	keywords = {2009, rcc, RCC1216, rcc1217, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto?ppo},
	doi = {10.1186/gb-2009-10-10-r114},
	url = {http://genomebiology.com/2009/10/10/R114},
	author = {von Dassow, Peter and Ogata, Hiroyuki and Probert, Ian and Wincker, Patrick and Da Silva, Corinne and Audic, St{\'e}phane and Claverie, Jean-Michel and de Vargas, Colomban}
}
@article {Frada2008,
	title = {The {\textquotedblleft}Cheshire Cat{\textquotedblright} escape strategy of the coccolithophore Emiliania huxleyi in response to viral infection},
	journal = {Proceedings of the National Academy of Sciences of the United States of America},
	volume = {105},
	year = {2008},
	note = {tex.mendeley-tags: 2008,rcc,sbr?hyto?ppo},
	pages = {15944{\textendash}15949},
	abstract = {The coccolithophore is one of the most successful eukaryotes in modern oceans. The two phases in its haplodiploid life cycle exhibit radically different phenotypes. The diploid calcified phase forms extensive blooms, which profoundly impact global biogeochemical equilibria. By contrast, the ecological role of the noncalcified haploid phase has been completely overlooked. Giant phycodnaviruses ( viruses, EhVs) have been shown to infect and lyse diploid-phase cells and to be heavily implicated in the regulation of populations and the termination of blooms. Here, we demonstrate that the haploid phase of is unrecognizable and therefore resistant to EhVs that kill the diploid phase. We further show that exposure of diploid to EhVs induces transition to the haploid phase. Thus we have clearly demonstrated a drastic difference in viral susceptibility between life cycle stages with different ploidy levels in a unicellular eukaryote. Resistance of the haploid phase of provides an escape mechanism that involves separation of meiosis from sexual fusion in time, thus ensuring that genes of dominant diploid clones are passed on to the next generation in a virus-free environment. These {\^a}{\texteuro}{\oe}Cheshire Cat{\^a}{\texteuro} ecological dynamics release host evolution from pathogen pressure and thus can be seen as an opposite force to a classic {\^a}{\texteuro}{\oe}Red Queen{\^a}{\texteuro} coevolutionary arms race. In , this phenomenon can account for the fact that the selective balance is tilted toward the boom-and-bust scenario of optimization of both growth rates of calcifying cells and infectivity of EhVs.},
	keywords = {2008, rcc, SBR$_\textrmP$hyto$_\textrmE$PPO, sbr?hyto?ppo},
	doi = {10.1073/pnas.0807707105},
	author = {Frada, Miguel and Probert, Ian and Allen, Michael J and Wilson, William H and de Vargas, Colomban}
}
@article {Claquin2008,
	title = {Effects of temperature on photosynthetic parameters and TEP production in eight species of marine microalgae},
	journal = {Aquatic Microbial Ecology},
	volume = {51},
	year = {2008},
	note = {tex.mendeley-tags: 2008,rcc},
	pages = {1{\textendash}11},
	keywords = {2008, rcc, SBR$_\textrmP$hyto},
	doi = {10.3354/ame01187},
	author = {Claquin, Pascal and Probert, Ian and Lefebvre, S{\'e}bastien and Veron, Benoit}
}
