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

被引:21
作者
Yang Jian [1 ,2 ]
Yang Guipeng [1 ]
Zhang Honghai [1 ]
Zhang Shenghui [1 ]
机构
[1] Ocean Univ China, Coll Chem & Chem Engn, Key Lab Marine Chem Theory & Technol, Minist Educ, Qingdao 266100, Peoples R China
[2] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Coastal Environm Engn Technol Res Ctr Shandong Pr, Yantai 264003, Peoples R China
基金
高等学校博士学科点专项科研基金; 中国国家自然科学基金;
关键词
dimethylsulfide (DMS); dimethylsulfoniopropionate (DMSP); sea-to-air flux; Yellow Sea; Bohai Sea; DIMETHYLATED SULFUR-COMPOUNDS; EAST CHINA SEA; SURFACE MICROLAYER; GAS-EXCHANGE; SPATIOTEMPORAL VARIABILITY; TEMPORAL VARIABILITY; OXIDATION-PRODUCTS; BIOLOGICAL REMOVAL; SUBSURFACE WATER; NORTH-ATLANTIC;
D O I
10.1007/s00343-015-4188-5
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
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 mu m), 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 mu mol/(m(2)center dot d) during the summer.
引用
收藏
页码:1020 / 1038
页数:19
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