图2 显示了1987— 1988 年南海北部(SCS-N)浅层(1000m)及深层 (3350m)水域硅藻通量变化情况,及其与同时段南 海北部颗粒物总通量及生物蛋白石通量的对比情 况[1.
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南海北部陆架陆坡区 Continental shelf and slope of the northern South China Sea
南海北部大陆架 the Northern continental shelf of South China Sea
南海北部陆缘盆地 continental margin basins of the northern South China Sea
南海北部陆坡深水区 deep-water continental slope area in the northern South China Sea
南海北部表层沉积物 Surface sediment in the Northern South China Sea
南美洲北部海岸 North Coast of South America
海南岛西北部 northwest hainan island
南黄海和东海北部陆架 shelf of the southern yellow sea and the northern east china sea
南海西北部 northwestern south china sea
We investigated the abundance and species composition of phytoplankton community in the northern South China Sea(110°-120°E,18°-23°N) from 10th to 29th August 2007,using 208 samples taken from 41 sampling stations.
2007年8月10—29日对南海北部41个站位进行了浮游植物群落结构的调查。
参考来源 - 2007年夏季南海北部浮游植物的物种组成及丰度分布·2,447,543篇论文数据，部分数据来源于NoteExpress
南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。
There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.
断裂和断块构造是南海北部陆缘新生代构造作用的基本特征。
Structures of faults and fault-blocks are the basic characteristics of tectonism in the north continental margin of South China Sea in the Cenozoic.
这些气候变化与日本琵琶湖、 加勒比海和南海北部具有较好的可比性。
These climate changes are well comparable to the Pipa Lake, Caribbean Sea and the northern South China Sea.
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