Distribution of dimethylsulfide and dimethylsulfoniopropionate in the Yellow Sea and the East China Sea during spring: Spatio-temporal variability and controlling factors

被引:54
作者
Yang, Gui-Peng [1 ]
Zhuang, Guang-Chao [1 ]
Zhang, Hong-Hai [1 ]
Dong, Yuan [1 ]
Yang, Jian [1 ]
机构
[1] Ocean Univ China, Coll Chem & Chem Engn, Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao 266100, Peoples R China
基金
中国国家自然科学基金;
关键词
Dimethylsulfide (DMS); Dimethylsulfoniopropionate (DMSP); Distribution; Sea-to-air flux; Yellow Sea; East China Sea; DIMETHYLATED SULFUR-COMPOUNDS; CHANGJIANG YANGTZE-RIVER; SURFACE MICROLAYER; OCEANIC PHYTOPLANKTON; ATMOSPHERIC SULFUR; SEASONAL-VARIATION; GAS-EXCHANGE; DMSP; SULFIDE; DYNAMICS;
D O I
10.1016/j.marchem.2012.05.003
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Spatial distributions of dimethylsulfide (DMS) and total dimethylsulfoniopropionate (DMSP) were determined in the Yellow Sea (YS) and the East China Sea (ECS) during April-May, 2009. The average concentrations of DMS and DMSP in surface water in the study area were 4.91 (1.18-12.6) and 25.2 (5.47-73.7) nmol L-1, respectively. Significant relationships were observed between the sulfur compounds and chlorophyll a concentrations, suggesting that phytoplankton biomass might play an important role in controlling DMS and DMSP distributions in the YS and the ECS. Zooplankton community and complex hydrographic conditions including the Yangtze River effluent and the Kuroshio water might also influence DMS and DMSP spatial variability. The interannual and seasonal variations of DMS distribution were investigated in the study area by comparing the present results with previous data from the past two decades. Collectively these data suggest that more DMS was released after the 2000s likely because of shifts of phytoplankton population caused by the anthropogenic eutrophication in the YS and the ECS. The average flux of DMS from the YS and the ECS to the atmosphere was estimated to be 13.7 mu mol m(-2) d(-1), implying a significant relative contribution of continental shelf sea areas to global oceanic DMS emissions. (c) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:21 / 31
页数:11
相关论文
共 67 条
  • [1] OCEAN-ATMOSPHERE INTERACTIONS IN THE GLOBAL BIOGEOCHEMICAL SULFUR CYCLE
    ANDREAE, MO
    [J]. MARINE CHEMISTRY, 1990, 30 (1-3) : 1 - 29
  • [2] Production and turnover of particulate dimethylsulphoniopropionate during a coccolithophore bloom in the northern North Sea
    Archer, SD
    Widdicombe, CE
    Tarran, GA
    Rees, AP
    Burkill, PH
    [J]. AQUATIC MICROBIAL ECOLOGY, 2001, 24 (03) : 225 - 241
  • [3] DISCHARGE OF THE CHANGJIANG (YANGTZE RIVER) INTO THE EAST CHINA SEA
    BEARDSLEY, RC
    LIMEBURNER, R
    YU, H
    CANNON, GA
    [J]. CONTINENTAL SHELF RESEARCH, 1985, 4 (1-2) : 57 - &
  • [4] PRODUCTION OF DIMETHYLSULFONIUM PROPIONATE (DMSP) AND DIMETHYLSULFIDE (DMS) BY A MICROBIAL FOOD WEB
    BELVISO, S
    KIM, SK
    RASSOULZADEGAN, F
    KRAJKA, B
    NGUYEN, BC
    MIHALOPOULOS, N
    BUATMENARD, P
    [J]. LIMNOLOGY AND OCEANOGRAPHY, 1990, 35 (08) : 1810 - 1821
  • [5] Cao J., 2011, THESIS OCEAN U CHINA
  • [6] OCEANIC PHYTOPLANKTON, ATMOSPHERIC SULFUR, CLOUD ALBEDO AND CLIMATE
    CHARLSON, RJ
    LOVELOCK, JE
    ANDREAE, MO
    WARREN, SG
    [J]. NATURE, 1987, 326 (6114) : 655 - 661
  • [7] Chen H.-J., 2010, THESIS OCEAN U CHINA
  • [8] HYDROXIDE DECOMPOSITION OF DIMETHYLSULFONIOPROPIONATE TO FORM DIMETHYLSULFIDE
    DACEY, JWH
    BLOUGH, NV
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1987, 14 (12) : 1246 - 1249
  • [9] OCEANIC DIMETHYLSULFIDE - PRODUCTION DURING ZOOPLANKTON GRAZING ON PHYTOPLANKTON
    DACEY, JWH
    WAKEHAM, SG
    [J]. SCIENCE, 1986, 233 (4770) : 1314 - 1316
  • [10] Factors determining the vertical profile of dimethylsulfide in the Sargasso Sea during summer
    Gabric, A. J.
    Matrai, P. A.
    Kiene, R. P.
    Cropp, R.
    Dacey, J. W. H.
    DiTullio, G. R.
    Najjar, R. G.
    Simo, R.
    Toole, D. A.
    delValle, D. A.
    Slezak, D.
    [J]. DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2008, 55 (10-13) : 1505 - 1518