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Dimethylsulfoniopropionate Uptake by Marine Phytoplankton

Science, 2006
Dimethylsulfoniopropionate (DMSP) accounts for most of the organic sulfur fluxes from primary to secondary producers in marine microbial food webs. Incubations of natural communities and axenic cultures with radio-labeled DMSP showed that dominant phytoplankton groups of the ocean, the unicellular cyanobacteria Prochlorococcus
Vila-Costa, Maria   +5 more
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Cadmium in Marine Phytoplankton

2012
The distribution of cadmium in the ocean is very similar to that of major nutrients suggesting that it may be taken up by marine phytoplankton at the surface and remineralized at depth. This interpretation is supported by recent data on Cd isotope distribution showing an increase in the (112)Cd/(110)Cd ratio in Cd-depleted surface water.
Yan, Xu, François M M, Morel
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Is there a decline in marine phytoplankton?

Nature, 2011
Phytoplankton account for approximately 50% of global primary production, form the trophic base of nearly all marine ecosystems, are fundamental in trophic energy transfer and have key roles in climate regulation, carbon sequestration and oxygen production.
McQuatters-Gollop, A.   +13 more
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Hydrocarbons of marine phytoplankton

Marine Biology, 1971
The hydrocarbon contents of 23 species of algae (22 marine planktonic), belonging to 9 algal classes, were analyzed. The highly unsaturated 3,6,9,12,15,18-heneicosalhexaene predominates in the Bacillariophyceae, Dinophyceae, Cryptophyceae, Haptophyceae and Euglenophyceae.
M. Blumer, R. R. L. Guillard, T. Chase
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Ecology of Marine Phytoplankton

2014
Marine phytoplankton account for about 45 % of global net primary production (NPP). In addition, they perform other important biogeochemical functions including nitrogen fixation, calcium carbonate precipitation, and the production of climatically active gases such as dimethyl sulfide.
Geider, RJ, Moore, CM, Suggett, DJ
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Bioaccumulation of technetium by marine phytoplankton

Environmental Science & Technology, 1982
/sup 95m/Tc, in the IV and VII oxidation states, was added in picomolar quantities to monocultures of seven species of marine phytoplankton, including a green algae (Dunaliella tertiolecta), a diatom (Thalassiosira pseudonana), a blue-green alga (Oscillatoria woronichinii), a prasinophyte (Testraselmis chuii), two haptophytes (Emiliania huxleyi and ...
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Comment on “Patterns of Diversity in Marine Phytoplankton”

Science, 2010
Barton et al . (Reports, 19 March 2010, p. 1509) argued that stable conditions enable neutral coexistence of many phytoplankton species in the tropical oceans, whereas seasonal variation causes low biodiversity in subpolar oceans. However, their model prediction is not robust.
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