Comparisons of surface Chl a and primary productivity along three transects of the southern South China Sea, northern Java Sea and eastern Indian Ocean in April 2011*

Yimeng Rong, Ke Zhixin, Song Xing-yu, Shen Pingping, Wang Sheng-fu, Fan Yan-zhi, Huang Liang-min, Tan Yehui, L. Gang
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引用次数: 3

Abstract

Results are presented about the changes in chlorophyll a density, carbon fixation and nutrient levels in the surfacewaters of three transects of the southern South China Sea (SCS), northern Java Sea (JS) and eastern Indian Ocean (IO) duringApril 5-16 of 2011. The in situ Chl a concentration and carbon fixation showed decreasing trends from high to low latitudealong the three transects, while the photosynthetic rate of phytoplankton estimated from 14C incorporation displayed no simplevariation with latitude. Chl a concentration and carbon fixation in the IO water was lower than that in the JS water. Highersalinity and lower contents of dissolved inorganic nitrogen (DIN) and silicate (SiO3^2-) characterized the IO water as comparedto the SCS or JS water, and the PO4^3- content was lower in the IO water than in the SCS or JS water in most cases. Our resultsalso indicate the importance of DIN and SiO3^2- concentrations for the geographical changes in phytoplankton biomass andprimary productivity among the three regions.
2011年4月南海南部、爪哇海北部和印度洋东部3个样带地表Chl a和初级生产力的比较*
研究了2011年4月5日至16日南海南部、爪哇海北部和印度洋东部3个样带表层水体叶绿素a密度、固碳和养分水平的变化。3个样带的原位Chl - a浓度和固碳量均呈现由高纬向低纬递减的趋势,而浮游植物的光合速率则随纬度变化不大。IO水体的Chl a浓度和固碳量均低于JS水体。与SCS或JS相比,IO水具有较高的盐度和较低的溶解无机氮(DIN)和硅酸盐(SiO3^2-)含量,并且在大多数情况下IO水的PO4^3-含量低于SCS或JS水。研究结果还表明,DIN和SiO3^2-浓度对三个区域浮游植物生物量和初级生产力的地理变化具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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