南海西北部陆架区沿岸流和上升流对中华哲水蚤分布的影响

尹健强; 黄良民; 李开枝; 练树民; 李超伦; 张建林

doi:10.3969/j.issn.0253 4193.2013.02.015

南海西北部陆架区沿岸流和上升流对中华哲水蚤分布的影响

doi: 10.3969/j.issn.0253 4193.2013.02.015

1.
中国科学院南海海洋研究所海洋生物资源可持续利用重点实验室, 广东广州 510301
2.
热带海洋环境国家重点实验室, 广东广州 510301
3.
中国科学院海洋研究所海洋生态与环境科学重点实验室, 山东青岛 266071

基金项目: 中科院知识创新工程项目(KZCX2-YW-Q07-02);中国近海海洋综合调查与评价专项(908-01-ST08);中国科学院战略先导专项(XDA05030403);国家基金重点项目(41130855)。

计量
- 文章访问数: 1999
- HTML全文浏览量: 2
- PDF下载量: 1458
- 被引次数: 0
出版历程
- 收稿日期: 2012-03-29
- 修回日期: 2012-08-13

Effects of coastal current and upwelling on the distributions of Calanus sinicus on the northwest continental shelf of the South China Sea

1.
Key Laboratory of Marine Bio-resources Sustainable Utilization, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
2.
State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
3.
Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

摘要

摘要: 中华哲水蚤(Calanus sinicus)是广泛分布于西北太平洋大陆架水域的浮游桡足类,在海洋生态系统的物质循环和能量流动中具有重要作用。根据2006年7月至2007年10月4个季节使用网目孔径为0.505 mm的浮游生物网采集的样品,分析了南海西北部陆架区中华哲水蚤的水平、季节和昼夜垂直分布以及与季风、海流和温度的关系。中华哲水蚤丰度季节变化显著,整个调查海域春季的平均达(22.30±77.78)个/m³,夏季的降低,平均为(13.74±45.10)个/m³,秋季消失,冬季调查期间仍未出现。中华哲水蚤的区域分布差异十分显著,将调查海域划分为粤西近海、琼东近海、粤西-琼东外海三个亚区,在粤西近海亚区春、夏季中华哲水蚤的平均丰度分别为(115.63±145.93),(68.12±84.00)个/m³,远高于另外两个亚区。夏季琼东沿岸上升流区的中华哲水蚤没有昼夜垂直移动行为,呈底层分布,以躲避表层高温的伤害。南海西北部陆架区是中华哲水蚤的季节分布区,冬春季东北季风期间由广东沿岸流从东海沿岸携带而来,出现的时间从北往南逐渐推迟;夏季西南季风期间雷州半岛东部近海的冷涡和琼东沿岸上升流区成为中华哲水蚤度夏的避难所;秋季季风转换时期上升流减弱或消失,中华哲水蚤因耐受不了高温(>27℃)死亡而消失。因此,中华哲水蚤对东北季风时期的沿岸流和西南季风时期的上升流均具有良好的指示作用。
- 中华哲水蚤 /
- 南海北部 /
- 分布 /
- 季风 /
- 海流 /
- 指示种
Abstract: Calanus sinicus is a planktonic copepod with wide geographical distribution on the continental shelf of the northwest Pacific.It plays an important role in marine system.Four cruises were conducted from July 2006 to October 2007 in order to understand the seasonal and horizontal variations with the influences of monsoon, ocean current and temperature on its distributions on the northwest continental shelf of the South China Sea.The diel vertical migration (DVM) of C.sinicus was studied at one station located in the southeast of Hainan Island during summer.The results showed that the distribution of C.sinicus abundance varied seasonally and regionally.The mean of C.sinicus abundance was high with 23.30±77.78 ind./m³ in spring, and decreased to 13.74±45.10 ind./m³ in summer.It disappeared in autumn and did not enter into the study area during the investigated period in winter.The surveyed area was divided into three sub-regions in order to further analyze the regional difference, including the east inshore waters of Leizhou Peninsula, the east inshore waters of Hainan Island and and the offshore waters from Leizhou Peninsula to Hainan Island.The average abundance of C.sinicus within the inshore waters of Leizhou Peninsula was reached to be 115.63 (±145.93) and 68.12 (±84.00) ind/m³ in spring and summer, respectively, which was higher than those of the inshore Hainan Island and the offshore from Leizhou Peninsula to Hainan Island.The behavior of C.sinicus DVM was not found in the upwelling area in summer. C.sinicus seemed to be mostly habited in the bottom layer in order to avoid the damage of high temperature in the surface layer.The study area is the seasonal distribution zone of C.sinicus.Our findings suggested that C.sinicus was transported from the East China Sea to the northwest continental shelf of South China Sea by the Guangdong Coastal Current, which was driven by the northeast monsoon in winter and spring.The presence of a cold eddy, in addition to coastal upwelling driven by the southwest monsoon, provided suitable survival conditions for C.sinicus in summer.This species disappeared in autumn due to high temperatures (>27℃) and did not begin to enter into the northwest continental shelf of South China Sea from the East China Sea during the period of investigation in winter.C.sinicus could be considered as an indicator species for China Coastal Current driven by the northeasterly monsoon, and coastal upwelling by the southwesterly monsoon in the northern South China Sea.
- Calanus sinicus /
- northern South China Sea /
- distribution /
- monsoon /
- ocean current /
- indicator species

HTML全文

参考文献(46)

陈清潮, 章淑珍.黄海和东海的浮游桡足类:Ⅰ.哲水蚤目[J].海洋科学集刊, 1965, 7: 20—137.

Hulsennann K.Calanus sinicus Brodsky and C.jashnivi, nom.nov.(Copepoda:Calanoida) of the North-west Pacific Ocean: a comparison, with notes on the integumental pore pattern in Clanus s.str.[J].Invertebrate Taxonomy, 1994, 8: 1461—1482.

Uye S.Why does Calanus sinicus prosper in the shelf ecosystem of the Northwest Pacific Ocean？ [J].ICES Journal of Marine Science, 2000, 57: 1850—1855.

Hwang J S, Wong C K.The China Coast Current as a driving force for transporting Calanus sinicus(Copepoda:Calanoida) from its population centers to waters off Taiwan and Hong Kong during the winter northeast monsoon period[J].Journal of Plankton Research, 2005, 27: 205—210.

Wang R, Zuo T, Wang K.The Yellow Sea Cold Bottom Water-an oversummering site for Calanus sinicus(Copepoda, Crustacea) [J].Journal of Plankton Research, 2003, 25(2): 169—183.

Pu X M, Sun S, Yang B, et al.The combined effects of temperature and food supply on Calanus sinicus in the southern Yellow Sea in summer[J].Journal of Plankton Research, 2004, 26(9): 1049—1057.

Huang C, Uye S, Onbe T.Geographic distribution, seasonal life cycle, biomass and production of a planktonic copepod Calanus sinicus in the Inland Sea of Japan and its neighboring Pacific Ocean[J].Journal of Plankton Research, 1993, 15(11): 1229—1246.

毕洪生,孙松,高尚武,等.渤海浮游动物群落生态特点:Ⅱ.桡足类数量分布及变动[J].生态学报, 2001, 21(2): 177—185.

李超伦,王荣,孙松.南黄海鳀产卵场中华哲水蚤的数量分布及其摄食研究[J].水产学报, 2003, 27(Suppl.): 55—63.

Xu Z L, Chen B J.Seasonal distribution of Calanus sinicus (Copepoda, Crustacea) in the East China Sea[J].Acta Oceanologica Sinica, 2007, 26(3): 150—159.

黄加祺, 李少菁, 陈刚.台湾海峡及其邻近海域中华哲水蚤的分布和繁殖[J].海洋科学集刊, 2002, 44: 95—100.

Tam P F, Wong C K, Chen Q C, et al.Planktonic copepods of the Zhujiang estuary, 1991-1996[J].National Taiwan Museum Special Publication Series 2000, 10: 87—100.

Li K Z, Yin J Q, Huang L M, et al.Spatial and temporal variations of mesozooplankton in the Pearl River estuary, China[J].Estuarine, Coastal and Shelf Science, 2006, 67: 543—552.

张武昌, 高尚武, 孙军, 等.南海北部冬季和夏季浮游哲水蚤类群落[J].海洋与湖沼, 2010, 41(3): 448—458.

黄企洲, 王文质, 李毓湘, 等.南海海流和涡旋概况[J].地球科学进展, 1992, 7(5):1—9.

杨仕瑛, 鲍献文, 陈长胜, 等.夏季粤西沿岸流特征及其产生机制[J], 海洋学报, 2003, 25(6): 1—8.

管秉贤.南海暖流—广东外海一支冬季逆风流动的海流[J].海洋与湖沼, 1978, 9(2): 117—127.

管秉贤.南海暖流研究回顾[J].海洋与湖沼, 1998, 29(3): 322—329.

李立.南海上层环流观测研究进展[J].台湾海峡, 2002, 21(1): 114—125.

Wang D X, Hong B, Gan J P, et al.Numerical investigation on propulsion of the counter-wind current in the northern South China Sea in winter[J].Deep-Sea Research I, 57:1206—1221.

管秉贤, 袁耀初.中国近海及其附近海域若干涡旋研究综述:Ⅰ.南海和台湾以东海域[J].海洋学报, 2006, 28(3):1—16.

韩舞鹰,王明彪,马克美.我国夏季最低表层水温海区——琼东沿岸上升流区的研究[J].海洋与湖沼, 1990, 21(3): 267—275.

吴日升, 李立.南海上升流研究概述[J].台湾海峡, 2003, 22(2): 269—277.

Jing Z Y, Qi Y Q, Hua Z L, et al.Numerical study on the summer upwelling system in the northern continental shelf of the South China Sea[J].Continental Shelf Research, 2009, 29:467—478.

Su J, Pohlmann T.Wind and topography influence on an upwelling system at the eastern Hainan coast[J].Journal of Geophysical Research, 2009, 114, C06017, doi: 10.1029/2008JC005018.

Li F Q, Li L, Wang X Q, et al.Water masses in the South China Sea and water exchange between the Pacific and the South China Sea[J].Journal of Ocean University of Qingdao, 2002, 1(1): 19—24.

曹文清,林元烧,杨青,等.我国中华哲水蚤生物学研究进展[J].厦门大学学报(自然科学版),2006,45(Sup.2): 54—61.

Chen Q C.Zooplankton of China Seas (1) [M].Beijing: Science Press, 1992.

Li C, Sun S, Wang R, et al.Feeding and respiration rates of a planktonic copepod (Calanus sinicus) oversummering in Yellow Sea Cold Bottom Waters[J].Marine Biology, 2004, 145:149—157.

李少菁.福建沿海太平洋哲镖溞(Calanus pacificus Brodsky)的比较形态研究[J].厦门大学学报(自然科学版), 1963, 10(1): 57—81.

陈清潮.中华哲水蚤的繁殖、性比率和个体大小的形态研究[J].海洋与湖沼, 1964, 6(3): 272—288.

Zhang G T, Sun S, Zhang F.Seasonal variation of reproduction rates and body size of Calanus sinicus in the Southern Yellow Sea, China[J].Journal of Plankton Research, 2005, 27(2): 135—143.

林元烧, 李松.厦门港中华哲水蚤生活周期的初步研究[J].厦门大学学报(自然科学版), 1984, 23(1): 111—117.

林景宏, 陈瑞祥.东山湾浮游桡足类的分布[J].海洋通报, 1992,11(4):41—46.

Uye S.Temperature dependent development and growth of Calanus sinicus (Copepoda: Calanoida) in the Laboratory[J].Hydrobiologia, 1988, 167/168: 285—293.

黄加祺, 郑重.温度和盐度对厦门港几种桡足类存活率的影响[J].海洋与湖沼, 1986, 17(2): 161—167.

Zhang G T, Sun S, Yang B.Summer reproduction of the planktonic copepod Calanus sinicus in the Yellow Sea: influences of high surface temperature and cold bottom water[J].Journal of Plankton Research, 2007, 29(2):179-186.

孙松, 王荣, 张光涛, 等.黄海中华哲水蚤度夏机制初探[J].海洋与湖沼, 2002,33(浮游动物研究专辑):92—99.

Nonomura T, Machida R J, Nishida S.Stage-V copepodites of Calanus sinicus and Calanus jashnovi(Copepoda: Calanoida) in mesopelagic zone of Sagami Bay as identified with genetic markers, with special reference to their vertical distribution[J].Progress in Oceanography, 2008, 77,45—55.

He D H, Yang G M, Shen W L,et al.Study of zooplankton ecology in Zhejiang coastal upwelling system—Species distribution and diversity of zooplankton[J].Acta Oceanologic Sinica, 1988, 7(2): 304—313.

Guo D H,Huang J Q,Li S J.Planktonic copepod compositions and their relationships with water masses in the southern Taiwan Strait during the summer upwelling period[J].Continental Shelf Research, 2011, 31: S67—S76.

Hwang J S, Dahms H U, Tseng L C, et al.Intrusions of the Kuroshio Current in the northern South China Sea affect copepod assemblages of the Luzon Strait[J].Journal of Experimental Marine Biology and Ecology, 2007, 352: 12—27.

Hsiao S H, Fang T H, Shih C T, et al.Effects of the Kuroshio Current on copepod assemblages in Taiwan[J].Zoological Studies, 2011, 50(4): 475—490.

李开枝, 尹健强, 黄良民, 等.粤西—琼东海域住筒虫属(Fritillaria)的种类描述及其数量分布[J].海洋学报, 2010, 32(5):76—85.

Uye S, Huang C, Onbe T.Ontogenetic diel vertical migration of the planktonic copepod Calanus sinicus in the Inland Sea of Japan[J].Marine Biology, 1990,104: 389—396.

Huang C, Uye S, Onbe T.Ontogenetic diel vertical migration of the planktonic copepod Calanus sinicus in the Inland Sea of Japan:Ⅲ.Early summer and overall seasonal pattern[J].Marine Biology, 1993, 117: 289—299.

施引文献

资源附件(0)

访问统计