The distribution of nitrogen forms and the relationship with the total phytoplankon in the Huanghai Sea and the East China Sea continental shelf

ZHANG Xiaoyong; SUN Yao; SHI Xiaoyong; YANG Qian; HUANG Jiansheng; WANG Didi

doi:10.3969/j.issn.0253-4193.2013.01.013

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ZHANG Xiaoyong, SUN Yao, SHI Xiaoyong, YANG Qian, HUANG Jiansheng, WANG Didi. The distribution of nitrogen forms and the relationship with the total phytoplankon in the Huanghai Sea and the East China Sea continental shelf[J]. Haiyang Xuebao, 2013, 35(1): 111-120. doi: 10.3969/j.issn.0253-4193.2013.01.013

Citation:

ZHANG Xiaoyong, SUN Yao, SHI Xiaoyong, YANG Qian, HUANG Jiansheng, WANG Didi. The distribution of nitrogen forms and the relationship with the total phytoplankon in the Huanghai Sea and the East China Sea continental shelf[J]. Haiyang Xuebao, 2013, 35(1): 111-120. doi: 10.3969/j.issn.0253-4193.2013.01.013

Citation:

ZHANG Xiaoyong, SUN Yao, SHI Xiaoyong, YANG Qian, HUANG Jiansheng, WANG Didi. The distribution of nitrogen forms and the relationship with the total phytoplankon in the Huanghai Sea and the East China Sea continental shelf[J]. Haiyang Xuebao, 2013, 35(1): 111-120. doi: 10.3969/j.issn.0253-4193.2013.01.013

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The distribution of nitrogen forms and the relationship with the total phytoplankon in the Huanghai Sea and the East China Sea continental shelf

doi: 10.3969/j.issn.0253-4193.2013.01.013

1.
Laboratory of Marine Pollution Ecological Chemistry, Ocean University of China, Qingdao 266003, China;Yellow Sea Fisheries Research Institute, Chinese Fishery Science Academy, Qingdao 266071, China
2.
Yellow Sea Fisheries Research Institute, Chinese Fishery Science Academy, Qingdao 266071, China
3.
Laboratory of Marine Pollution Ecological Chemistry, Ocean University of China, Qingdao 266003, China

Received Date: 2012-01-12
Rev Recd Date: 2012-09-26

Abstract

Abstract

Nitrogen in marine sediment of Huanghai Sea and East China Sea continental shelf area was defined as transferable part and non-transferable part,with a sequential extraction separation method. Four forms of transferable part in marine sediment were ion-exchange form(IEF-N),carbonate form(CF-N), iron-manganese oxides form(IMOF-N),and organic matter-sulfide form (OSF-N),respectively.The horizontal,vertical distribution,and the age of the deposition profiles of the four forms were given.The correlation among different forms of nitrogen and biogenic silica (BSi)-the alternative indicators of paleoproductivity were further explored,revealing the geochemistry of the forms of nitrogen and relations with the total phytoplankton.The results showed that transferable nitrogen accounted for 16.81% of total nitrogen (TN) and the average content of four different transferable forms nitrogen in the surface area were IMOF-N(66.65 μg/g)>IEF-N(22.96 μg/g)>OSF-N(17.40 μg/g)>CF-N(11.26 μg/g),respectively. IMOF-N was the advantage form of transferable nitrogen in the surface area; various forms of nitrogen in each station were different,and there's a wide variation in different nitrogen forms of the Changjiang Estuary,compared with the central southern Huanghai Sea; BSi, IEF-N and IMOF-N in the southern Huanghai Sea surface sediments and columnar were correlated significantly,and the relevance of BSi and various forms of nitrogen were not obvious in the Changjiang Estuary and along the coast of Fujian and Zhejiang Province. IEF-N and IMOF-N had a greater contribution to the total phytoplankton.
- Huanghai Sea and East China Sea continental shelf,
- sediment,
- nirogen forms,
- total phytoplankton,
- biogenic silica

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References(30)

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