Spatial distribution of dimethylsulfide and dimethylsulfoniopropionate in the Yellow Sea and Bohai Sea during summer

被引:0
作者
Jian Yang
Guipeng Yang
Honghai Zhang
Shenghui Zhang
机构
[1] Ocean University of China,Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering
[2] Chinese Academy of Sciences,Coastal Environment Engineering Technology Research Center of Shandong Province, Yantai Institute of Coastal Zone Research
来源
Chinese Journal of Oceanology and Limnology | 2015年 / 33卷
关键词
dimethylsulfide (DMS); dimethylsulfoniopropionate (DMSP); sea-to-air flux; Yellow Sea; Bohai Sea;
D O I
暂无
中图分类号
学科分类号
摘要
The distributions of dimethylsulfide (DMS) and its precursor dimethylsulfoniopropionate (DMSP) in surface water of the Yellow Sea and the Bohai Sea were studied during June 2011. The mean concentrations and ranges of DMS, dissolved DMSP (DMSPd), and particulate DMSP (DMSPp) in surface waters were 6.85 (1.60–12.36), 7.25 (2.28–19.05) and 61.87 (6.28–224.01) nmol/L, respectively. There were strong correlations between DMSPp and chlorophyll a in the Bohai Sea and the North Yellow Sea, respectively, and concentrations of DMS and DMSP were high, with a relatively high proportion of dinoflagellates, in the region of the South Yellow Sea Cold Water Mass. Results show that phytoplankton biomass and species composition were important factors that controlled the distribution of DMS and DMSP. Complex environmental factors, including nutrients, transparency, and terrestrial runoff, might also influence the variability in DMS and DMSP. Biological production and consumption rates of DMS in the Bohai Sea were higher than those in the Yellow Sea. DMS production rates were closely correlated with DMSPd concentrations. DMS and DMSP exhibited obvious diel variations, with high concentrations occurring in the late afternoon (16:00–19:00) and low concentrations occurring during the night, implying that the intensity of solar radiation had a significant influence on these variations. Size distributions of chlorophyll a and DMSPp were also investigated and large nanoplankton (5–20 μm), mainly diatoms, contributed significantly to chlorophyll a and DMSPp at most stations. The average sea-to-air flux of DMS in the study area was estimated to be 11.07 μmol/(m2·d) during the summer.
引用
收藏
页码:1020 / 1038
页数:18
相关论文
共 300 条
[1]  
Andreae M O(1984)The marine chemistry of dimethylsulfide Marine Chemistry 14 267-279
[2]  
Barnard W R(1990)Ocean-atmosphere interactions in the global biogeochemical sulfur cycle Marine Chemistry 30 1-29
[3]  
Andreae M O(2001)Biogeochemical variation in dimethylsulfide, phytoplankton pigments and heterotrophic bacterial production in the subarctic North Pacific during summer Journal of Oceanography 57 315-322
[4]  
Aranami K(2011)Grazing suppression of dimethylsulphoniopropionate (DMSP) accumulation in iron-fertilised, sub-Antarctic waters Deep Sea Research Part II: Topical Studies in Oceanography 58 839-850
[5]  
Watanabe S(2005)Spatio-temporal variability of size fractionated phytoplankton on the shelf adjacent to the Ebro river (NW Mediterranean) Continental Shelf Research 25 1 081-1 095
[6]  
Tsunogai S(2000)DMS and its oxidation products in the remote marine atmosphere: implications for climate and atmospheric chemistry Journal of Sea Research 43 275-286
[7]  
Hayashi M(1994)The cycling of sulfur in surface seawater of the Northeast Pacific Journal of Geophysical Research 99 7 835-7 843
[8]  
Furuya K(2000)Diel variations of the DMSP-to-chlorophyll Journal of Marine Systems 25 119-128
[9]  
Nagata T(2004) ratio in northwestern Mediterranean surface waters Deep Sea Research I: Oceanographic Research Papers 51 1 179-1 197
[10]  
Archer S D(1987)Dimethylated sulfur compounds in seawater, seston and mesozooplankton in the seas around Turkey Nature 326 655-661