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1

Tamminen, Timo, and H. Kuosa, eds. Eutrophication in Planktonic Ecosystems: Food Web Dynamics and Elemental Cycling. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-017-1493-8.

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2

Yool, Andrew. The dynamics of open-ocean plankton ecosystem models. [s.l.]: typescript, 1997.

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3

Gin, Karina Y. H. Microbial size spectra from diverse marine ecosystems. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1996.

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4

Heiskanen, Anna-Stiina. Sedimentation and recycling in aquatic ecosystems: The impact of pelagic processes and planktonic food web structure. Helsinki: Finnish Environment Institute, 1999.

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5

International PELAG Symposium (4th 1996 Helsinki, Finland). Eutrophication in planktonic ecosystems: Food web dynamics and elemental cycling : proceedings of the Fourth International PELAG Symposium, held in Helsinki, Finland, 26-30 August 1996. Dordrecht: Kluwer Academic Publishers, 1998.

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6

Dalziel, Robert Ian Ralph. The role of planktonic heterotrophic bacteria in lake ecosystem trophic dynamics. 1985.

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7

Sheppard, Charles. 5. Microbial and planktonic engines of the reef. Oxford University Press, 2014. http://dx.doi.org/10.1093/actrade/9780199682775.003.0005.

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Symbiotic algae are a crucial source of fuel for the reef, via corals and others, but how is the food and energy from the corals transferred to other parts of the ecosystem to support the huge abundance and diversity seen there? ‘Microbial and planktonic engines of the reef’ describes the filter feeding—extracting particles from the water—of the large proportion of reef animals. These particles consist of plankton, microbes, bacteria, viruses, and zooplankton. Sponges also display microbial symbiotic connections with algae and cyanobacteria that is a key component of material and energy transfer. The productivity from seaweeds on which numerous species of herbivorous fish and sea urchins graze is also important.
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8

Tamminen, T., and H. Kuosa. Eutrophication in Planktonic Ecosystems: Food Web Dynamics and Elemental Cycling. Springer London, Limited, 2013.

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9

Tamminen, T., and H. Kuosa. Eutrophication in Planktonic Ecosystems: Food Web Dynamics and Elemental Cycling. Springer, 2014.

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10

Tamminen, T., and H. Kuosa. Eutrophication in Planktonic Ecosystems: Food Web Dynamics and Elemental Cycling. Springer Netherlands, 2011.

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11

Eutrophication in Planktonic Ecosystems: Food Web Dynamics and (Developments in Hydrobiology). Springer, 2007.

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12

Antoine, David, and Oleg Dubovik, eds. From the Satellite to the Earth's Surface: Studies Relevant to NASA’s Plankton, Aerosol, Cloud, Ocean Ecosystems (PACE) Mission. Frontiers Media SA, 2020. http://dx.doi.org/10.3389/978-2-88963-500-9.

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13

Holliday, N. Penny, and Stephanie Henson. The Marine Environment. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199233267.003.0001.

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The growth, distribution, and variability of phytoplankton populations in the North Atlantic are primarily controlled by the physical environment. This chapter provides an overview of the regional circulation of the North Atlantic, and an introduction to the key physical features and processes that affect ecosystems, and especially plankton, via the availability of light and nutrients. There is a natural seasonal cycle in primary production driven by physical processes that determine the light and nutrient levels, but the pattern has strong regional variations. The variations are determined by persistent features on the basin scale (e.g. the main currents and mixed layer regimes of the subtropical and subpolar gyres), as well as transient mesoscale features such as eddies and meanders of fronts.
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14

Livingston, Robert J. Eutrophication Processes in Coastal Systems: Origin and Succession of Plankton Blooms and Effects on Secondary Production in Gulf Coast Estuaries. Taylor & Francis Group, 2000.

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15

Livingston, Robert J. Eutrophication Processes in Coastal Systems: Origin and Succession of Plankton Blooms and Effects on Secondary Production in Gulf Coast Estuaries. Taylor & Francis Group, 2000.

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