Studies on Phytoplankton and Particulate Organic Carbon in the Southern Ocean

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Abstract:

Using China Southern Ocean’s study data collected from 1989 to 2009 year, this paper analyzed the related characteristics between phytoplankton abundance, Ch1 a concentrations and particulate organic carbon. The average cell abundance of Southern Ocean phytoplankton was 7.38×104 cells/dm3. The dominant species of Southern Ocean phytoplankton were Fragilariopsis kerguelensis, Fragilariopsis curta, Pseudo-nitzschia lineola, Eucampia antarctica, Thalassiosira antarctica and Corethron criophilum and son on. In Prydz Bay of the Southern Ocean, the contribution of phytoplankton cell abundance and phytoplankton carbon toward particulate organic carbon were higher than that in the Northern Gulf Ocean Area. In the upper layer of euphotic zone, the contribution of phytoplankton abundance and phytoplankton carbon toward particulate organic carbon were higher than that in the deep water district. Through analysis of regressive statistics, phytoplankton cell abundance (y) and particulate organic carbon (POC) and chlorophyll a (Chl a) were a remarkable positive correlation.

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344-352

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October 2011

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© 2012 Trans Tech Publications Ltd. All Rights Reserved

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[1] Zhu Gen-hai, Ning Xiu-ren, Liu Zi-lin(1998a): A study on distribution feature of nano- and micro- phytoplankton in Prydz Bay and its adjacent sea area, Antarctica during 1989/1990. Oceanog. in China,1998a,9:31-41. (in Chinese with English abstract)

Google Scholar

[2] Zhu Gen-hai, Ning Xiu-ren, Cai Yu-ming, Liu Zi-lin(2003): Phytoplankton in Prydz Bay and its adjacent sea area of Antarctica during the austral summer (1998/1999). Acta Botanica Sinica, 45(4): 390-398.

Google Scholar

[3] Zhu Gen-hai, Chen Li-hong, Jin Mao, Liu Zi-lin(2011): Studies on the Community Structure of Phytoplankton and its Environmental Restriction in the Water Encircling the Antarctica. Prog. Environm. Sci. & Tech., III: 60–65.

Google Scholar

[4] Sun Zuo-qing, Yang He-ming, Ji Ming-hou(1983):Seawater particulate organic carbon determination. Oceanol. & Limnol., 15(1):39~43.

Google Scholar

[5] Liu Wen-chen, Wang Rong(1996): Seawater particulate organic carbon research brief. Marine Science, 5, 21-23.

Google Scholar

[6] Hedges, J. I. (1992): Global biogeochemical cycles: progress and problem. Mar. Chem.,39:67-93.

Google Scholar

[7] Rainer M. W. Amon & R. Benner (1994): Rapid cycling of high-molecular-weight dissolved organic matter in the ocean. Nature, 369, 16.

DOI: 10.1038/369549a0

Google Scholar

[8] Longhurst, A. R. and Harrison, W. G. (1989): The biological pump: Profiles of plankton production and consumption in the upper ocean. Prog. Oceanog. 22, 47-123.

DOI: 10.1016/0079-6611(89)90010-4

Google Scholar

[9] Wang Rong,(1992): Global Change and Marine pump. Marine Science, 1, 18-21.

Google Scholar

[10] Parsons T. R. ,1975, Particulate organic carbon in the sea. In "Chemical Oceanography" (Riley J.P. and Skirrow G. eds), Academic Press, London, 2:365~383.

Google Scholar

[11] Steele J. H. and I. E. Baird, (1962): Further relations between primary production, chlorophyll, and particulate carbon. Limnol. Oceanogr., 7(1): 42~44.

DOI: 10.4319/lo.1962.7.1.0042

Google Scholar

[12] Ning Xiu-ren, Liu Zi-lin, Zhu Gen-hai, et al, (1998): 1992/1993, Prydz Bay, Antarctica and its adjacent waters the amount of phytoplankton, primary productivity and the distribution of particulate organic carbon . China Oceanographic Collection (9), 67-79. Ocean Press.

Google Scholar