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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 16
Biogeosciences, 13, 4767–4775, 2016
https://doi.org/10.5194/bg-13-4767-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 13, 4767–4775, 2016
https://doi.org/10.5194/bg-13-4767-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 23 Aug 2016

Research article | 23 Aug 2016

Effect of the silica content of diatom prey on the production, decomposition and sinking of fecal pellets of the copepod Calanus sinicus

Hongbin Liu and Chih-Jung Wu
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Cited articles  
Armstrong, R. A., Lee, C., Hedges, J. I., Honjo, S., and Wakeham, S. G.: A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals, Deep-Sea Res. Pt. II, 49, 219–236, 2002.
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Ayukai, T. and Nishizawa, S.: Defecation rate as a possible measure of ingestion rate of Calanus pacificus (Copepoda: Calanoida), Bull. Plankton Soc. Japan, 33, 3–10, 1986.
Båmstedt, U., Nejstgaard, J. C., and Solberg, P. T.: Utilisation of small-sized food algae by Calanus finmarchicus (Copepoda, Calanoida) and the significance of feeding history, Sarsia, 84, 19–38, 1999.
Bathmann, U. V., Noji, T. T., Voss, M., and Peinert, R.: Copepod fecal pellets: abundance, sedimentation and content at a permanent station in the Norwegian Sea in May/June 1986, Mar. Ecol.-Prog. Ser., 38, 45–51, 1987.
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The transport of organic C from the surface to the deep ocean by sinking particles composed of remains of dead cells and zooplankton fecal pellets can reduce the atmospheric CO2. Study of the effect of the silica content of diatoms, one of the most important primary products, on the production, degradation and sinking of its fecal pellets provides a better understanding of the complexity and variability of the planktonic food web and its implication on the vertical flux of C in the global ocean.
The transport of organic C from the surface to the deep ocean by sinking particles composed of...
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