Annual variation in Calanus sinicus abundance and population structure in the northern boundary area of the Yellow Sea Cold Water Mass

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作者
Jiehui Yin
Guangtao Zhang
Zengxia Zhao
Shiwei Wang
Aiyong Wan
机构
[1] Chinese Academy of Sciences,Jiaozhou Bay Marine Ecosystem Research Station, Institute of Oceanology
[2] University of Chinese Academy of Sciences,undefined
关键词
Yellow Sea Cold Water Mass (YSCWM); over-summer strategy; boundary area; thermal stratification;
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摘要
The Yellow Sea Cold Water Mass (YSCWM) was suggested as an over-summering site of the dominant copepod species Calanus sinicus in coastal Chinese seas. Population abundance and structure were investigated by monthly sampling along three transects across the northern boundary of the YSCWM during 2009–2010. Results show that thermal stratification existed from June to October and that the vertical thermal difference increased with depth. Generally, total abundance was lowest in October and highest in June, and the female/male sex ratio was highest in February and lowest in August. Evident spatial differences in abundance were observed during the existence of the YSCWM. In June, total abundance averaged 158.8 ind/m3 at well-stratified stations, and 532.1 ind/m3 at other stations. Similarly, high abundances of 322.0 and 324.4 ind/m 3 were recorded from July to August inside the YSCWM, while the abundance decreased from 50.4 to 1.9 ind/m3 outside the water mass. C. sinicus distribution tended to even out over the study area in September when the YSCWM disappeared. We believe that the YSCWM may retard population recruitment in spring and preserve abundant cohorts in summer. The summer population was transported to neritic waters in autumn. In addition to low temperatures, stable vertical structure was also an essential condition for preservation of the summer population. C. sinicus can survive the summer in marginal areas in high abundance, but the population structure is completely different in terms of C5 proportion and sex ratio.
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页码:1284 / 1294
页数:10
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    [J]. Chinese Journal of Oceanology and Limnology, 2013, 31 (06) : 1284 - 1294
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