@article {Henry2021,
	title = {The influences of phytoplankton species, mineral particles and concentrations of dispersed oil on the formation and fate of marine oil-related aggregates},
	journal = {Science of the Total Environment},
	volume = {752},
	year = {2021},
	note = {Publisher: Elsevier B.V. tex.mendeley-tags: RCC1698,RCC1719,RCC290},
	month = {jan},
	pages = {141786},
	abstract = {The formation and fallout of oil-related marine snow have been associated with interactions between dispersed oil and small marine particles, like phytoplankton and mineral particles. In these studies, the influences of phytoplankton species, mineral particle concentration, and oil concentration on the aggregation of oil in seawater (SW) were investigated. The experiments were performed in a low-turbidity carousel incubation system, using natural SW at 13 {\textdegree}C. Aggregation was measured by silhouette camera analyses, and oil compound group distribution and depletion by gas chromatography (GC-FID or GC{\textendash}MS). Aggregates with median sizes larger than 500 ??m in diameter were measured in the presence of dispersed oil and the phytoplankton species Thalassiosira rotula, Phaeocystis globosa, Skeletonema pseudocostatum, but not with the microalgae Micromonas pusilla. When mineral particles (diatomaceous earth) were incubated at different concentrations (5{\textendash}30 mg/L) with dispersed oil and S. pseudocostatum, the largest aggregates were measured at the lower mineral particle concentration (5 mg/L). Since dispersed oil rapidly dilutes in the marine water column, experiments were performed with oil concentrations of from 10 mg/L to 0.01 mg/L in the presence of S. pseudocostatum and diatomaceous earth. Aggregates larger than 500 ??m was measured only at the highest oil concentrations (10 mg/L). However, oil attachment to the marine particles were also measured at low oil concentrations (<=1 mg/L). Depletion of oil compound groups (n-alkanes, naphthalenes, PAHs, decalins) were measured at all oil concentrations, both in aggregate and water phases, with biodegradation as the expected main depletion process. These results showed that oil concentration may be important for oil-related marine snow formation, but that even oil droplets at low concentrations may attach to the particles and be transported by prevailing currents.},
	keywords = {Aggregation, Dispersed oil, Marine snow, Mineral particles, phytoplankton, RCC1698, RCC1719, RCC290},
	issn = {18791026},
	doi = {10.1016/j.scitotenv.2020.141786},
	author = {Henry, Ingrid A. and Netzer, Roman and Davies, Emlyn and Brakstad, Odd Gunnar}
}
@article {royer_response_2021,
	title = {Response of dimethylsulfoniopropionate (DMSP) and dimethylsulfoxide (DMSO) cell quotas to oxidative stress in three phytoplankton species},
	journal = {Journal of Plankton Research},
	volume = {43},
	number = {5},
	year = {2021},
	month = {sep},
	pages = {673{\textendash}690},
	abstract = {Several phytoplankton species produce the metabolites dimethylsulfoniopropionate (DMSP) and dimethylsulfoxide (DMSO) but their intracellular roles need to be better understood. To improve the understanding of the DMSP antioxidant function suggested by Sunda et al. (2002), we exposed the diatom Skeletonema costatum, the Prymnesiophyceae Phaeocystis globosa and the dinoflagellate Heterocapsa triquetra to experimental treatments known to cause potential oxidative stress (high light intensities (HL); HL with 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU); menadione sodium bisulfite (MSB)). DMSP and DMSO concentrations decreased after 6 h in all treatments indicating an interaction with Reactive Oxygen Species (ROS) produced. DMSP and DMSO-to-cell ratios in control conditions were higher for H. triquetra, while being unable to grow under HL. DMSP and DMSO-to-cell carbon were the highest for P. globosa, while the other species had similar values. During long-term treatment, these ratios were not increased in high-light grown cells of P. globosa and S. costatum. Overall, this illustrates that (1) the DMSP- and DMSO-to-cell or carbon seems to be not indicative of the capability of the species to tolerate an oxidative stress, (2) these molecules could react with ROS and lower their cellular concentration, but no clues demonstrated that these molecules are part of the antioxidant response of the cell.},
	keywords = {rcc, RCC1719, RCC4800},
	issn = {0142-7873},
	doi = {10.1093/plankt/fbab052},
	url = {https://doi.org/10.1093/plankt/fbab052},
	author = {Royer, C and Gypens, N and Cardol, P and Borges, A V and Roberty, S}
}
@article {Decelle2019,
	title = {Algal remodeling in a ubiquitous planktonic photosymbiosis},
	journal = {Current Biology},
	volume = {29},
	number = {6},
	year = {2019},
	note = {Publisher: Cell Press tex.mendeley-tags: RCC1719},
	month = {mar},
	pages = {968{\textendash}978.e4},
	abstract = {Photosymbiosis between single-celled hosts and microalgae is common in oceanic plankton, especially in oligotrophic surface waters. However, the functioning of this ecologically important cell-cell interaction and the subcellular mechanisms allowing the host to accommodate and benefit from its microalgae remain enigmatic. Here, using a combination of quantitative single-cell structural and chemical imaging techniques (FIB-SEM, nanoSIMS, Synchrotron X-ray fluorescence), we show that the structural organization, physiology, and trophic status of the algal symbionts (the haptophyte Phaeocystis) significantly change within their acantharian hosts compared to their free-living phase in culture. In symbiosis, algal cell division is blocked, photosynthesis is enhanced, and cell volume is increased by up to 10-fold with a higher number of plastids (from 2 to up to 30) and thylakoid membranes. The multiplication of plastids can lead to a 38-fold increase of the total plastid volume in a cell. Subcellular mapping of nutrients (nitrogen and phosphorous) and their stoichiometric ratios shows that symbiotic algae are impoverished in phosphorous and suggests a higher investment in energy-acquisition machinery rather than in growth. Nanoscale imaging also showed that the host supplies a substantial amount of trace metals (e.g., iron and cobalt), which are stored in algal vacuoles at high concentrations (up to 660 ppm). Sulfur mapping reveals a high concentration in algal vacuoles that may be a source of antioxidant molecules. Overall, this study unveils an unprecedented morphological and metabolic transformation of microalgae following their integration into a host, and it suggests that this widespread symbiosis is a farming strategy wherein the host engulfs and exploits microalgae.},
	keywords = {RCC1719},
	issn = {0960-9822},
	doi = {10.1016/J.CUB.2019.01.073},
	url = {https://www.sciencedirect.com/science/article/abs/pii/S0960982219301320$\#$undfig1},
	author = {Decelle, Johan and Stryhanyuk, Hryhoriy and Gallet, Benoit and Veronesi, Giulia and Schmidt, Matthias and Balzano, Sergio and Marro, Sophie and Uwizeye, Clarisse and Jouneau, Pierre-Henri and Lupette, Josselin and Jouhet, Juliette and Mar{\'e}chal, {\'E}ric and Schwab, Yannick and Schieber, Nicole L. and Tucoulou, R{\'e}mi and Richnow, Hans and Finazzi, Giovanni and Musat, Niculina}
}
