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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Temporal and spatial variations of dimethylsulfide (DMS) and dimethylsulfoniopropionate (DMSP) in the East China Sea and the Yellow Sea
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Temporal and spatial variations of dimethylsulfide (DMS) and dimethylsulfoniopropionate (DMSP) in the East China Sea and the Yellow Sea

机译:东海和黄海中二甲基硫醚(DMS)和二甲基磺丙酸酯(DMSP)的时空变化

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摘要

Temporal and spatial distributions of dimethylsulfide (DMS) and its precursor dimethylsulfoniopropionate (DMSP) were determined in the East China Sea and the Yellow Sea during June-July, 2006 and January-February, 2007. The concentrations of DMS and total DMSP in surface water in the study area were 5.64 (1.79-12.24) and 28.25 (13.98-44.93)nmolL~(-1) in summer, and were 1.79 (1.02-3.51) and 11.01 (6.90-17.98)nmolL~(-1) in winter, respectively. The distributions of DMS and DMSP in the study area were obviously influenced by the Yangtze River effluent and the Kuroshio water. Even under highly variable hydrographic conditions, a significant relationship was observed between DMS and chlorophyll a concentrations in summer as well as in winter, suggesting that phytoplankton biomass might play an important role in controlling DMS distribution in the study area. The summer ratios of DMS/chlorophyll a and DMSP/chlorophyll a were approximately twofold higher than winter values, corresponding with the temporal variation in phytoplankton community structure between summer and winter. The sea-to-air fluxes of DMS were estimated to be 5.32 and 11.92μmolm~(-2)d~(-1) using the equations of Liss and Merlivat (1986) and Wanninkhof (1992), respectively.
机译:在2006年6月至7月和2007年1月至2月期间,在东海和黄海确定了二甲基硫醚(DMS)及其前体二甲基磺丙酸二甲酯(DMSP)的时空分布。地表水中DMS和总DMSP的浓度研究区的夏季分别为5.64(1.79-12.24)和28.25(13.98-44.93)nmolL〜(-1),冬季为1.79(1.02-3.51)和11.01(6.92-3.98)nmolL〜(-1) , 分别。研究区DMS和DMSP的分布明显受到长江污水和黑潮水的影响。即使在高度可变的水文条件下,在夏季和冬季也观察到DMS与叶绿素a浓度之间的显着关系,这表明浮游植物生物量可能在控制研究区域内DMS的分布中起重要作用。 DMS /叶绿素a和DMSP /叶绿素a的夏季比率比冬季高约两倍,与夏季和冬季之间浮游植物群落结构的时间变化相对应。利用Liss和Merlivat(1986)和Wanninkhof(1992)的方程,DMS的海气通量分别估计为5.32和11.92μmolm〜(-2)d〜(-1)。

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