黄、东海陆架2011年秋季活体浮游有孔虫生态分布

吕红红; 向荣

doi:10.3969/j.issn.0253-4193.2016.02.009

黄、东海陆架2011年秋季活体浮游有孔虫生态分布

doi: 10.3969/j.issn.0253-4193.2016.02.009

吕红红^1,,
向荣²

1.
中国科学院南海海洋研究所中国科学院边缘海地质重点实验室, 广东广州 510301;中国科学院大学地球科学学院, 北京 100049
2.
中国科学院南海海洋研究所中国科学院边缘海地质重点实验室, 广东广州 510301

基金项目: 国家重点基础研究发展计划973项目(2010CB428901);国家自然科学基金项目(41476040, 91228207)。

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出版历程
- 收稿日期: 2015-09-22
- 修回日期: 2015-11-16

Distribution of living planktonic foraminifera on the shelf of the Yellow Sea and the East China Sea in autumn,2011

Lyu Honghong^1
,,
Xiang Rong²

1.
Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
2.
Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

摘要

摘要: 现代活体浮游有孔虫的生态研究是其古环境重建应用的重要基础。根据黄、东海陆架2011年秋季采集的20个垂直浮游拖网样品,分析了该海域浮游有孔虫的秋季生态分布特征。结果表明,黄海秋季基本上没有浮游有孔虫的出现。东海共发现13种活体浮游有孔虫,主要优势属种依次为Globigerinoides sacculifer、Pulleniatina obliquiloculata、Globigerina bulloides、Neogloboquadrina dutertrei和Globigerinoides ruber。浮游有孔虫丰度整体上呈现东南高,西北低的分布格局,这种分布格局反映了浮游有孔虫在黄、东海陆架区的分布主要受外海水影响强弱控制。浮游有孔虫主要属种在东海陆架呈现明显的区域分布差异:暖水种G. sacculifer是秋季陆架海区的主要优势种,其分布格局与总丰度基本一致,相对含量从南至北、从东至西逐渐降低,主要受区域表层海水温度变化的控制。G. bulloides与G. sacculifer呈相反的含量分布变化,其高含量主要出现在东海中陆架,从北往南逐渐降低,此外,在闽浙沿岸也有较高含量,表明了温度和生产力是影响G. bulloides在黄、东海陆架分布的主要因素。秋季P. obliquiloculata和N. dutertrei的高含量主要出现在东海南部中陆架区和济州岛西南黄海暖流影响区,可能受暖水与生产力的共同制约。
- 黄海 /
- 东海 /
- 浮游拖网 /
- 浮游有孔虫 /
- 区域分布 /
- 海洋环境
Abstract: The knowledge of ecology of modern living planktonic foraminifera is very important for their application in paleoenvironmental reconstruction. The distribution of living planktonic foraminifers has been analyzed on 20 plankton tow samples collected from the shelf of the Yellow Sea and the East China Sea in Autumn, 2011. The results indicate that planktonic foraminifera is almost absent in autumn in the Yellow Sea. Thirteen planktonic foraminiferal species occurred in the East China Sea, dominated by Globigerinoides sacculifer, Pulleniatina obliquiloculata, Globigerina bulloides, Neogloboquadrina dutertrei and Globigerinoides ruber. The abundance of planktonic foraminifera shows a general pattern, with high abundance in the southeast and low values in the northwest of the study area, which may indicate that the distribution of foraminifers in the study area is mainly controlled by the influence of the open ocean water. The major species of planktonic foraminifera shows apparent different distribution in the East China shelf seas. G. sacculifer, the preponderant species of the shelf seas in autumn, shows a similar distribution pattern with the total abundance. Its relative percentage gradually decreased from south to north, and from east to west, suggesting the control of the variation by regional surface sea temperature. In contrast to the distribution of G. sacculifer, high percentage of G. bulloides mainly occurred in the middle shelf of the East China Sea, and its relative abundance gradually decreased from north to south, and high percentage also occurred in the inner shelf off Min-Zhe coast, suggesting that both temperature and productivity are principal factors controlling the distribution of G. bulloides in the study area. High abundance of P. obliquiloculata and N. dutertrei mainly appeared in the middle shelf of the southern East China Sea and southwest off Cheju Island, possibly modulated by the joint influence of warm water and productivity.
- the Yellow Sea /
- the East China Sea /
- plankton tow /
- planktonic foraminifera /
- spatial distribution /
- marine environment

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参考文献(35)

刘芳,向荣. 现代浮游有孔虫生态研究进展[J]. 微体古生物学,2010,27(4): 366-375. Liu Fang,Xiang Rong. Advances in the study of modern planktonic foraminifera[J]. Acta Micropalaeontologica Sinica,2010,27(4): 366-375.

Oda M,Yamasaki M. Sediment trap results from the Japan trench in the Kuroshio domain: Seasonal variations in the planktonic foraminifera flux[J]. The Journal of Foraminiferal Research,2005,35(4): 315.

Wilke I,Meggers H,Bickert T. Depth habitats and seasonal distributions of recent planktonic foraminifers in the Canary Islands region(29°N)based on oxygen isotopes[J]. Deep-Sea Research Ⅰ,2009,10: 1-18.

Eguchi N O,Ujiie H,Kawahata H,et al. Seasonal variations in planktonic foraminifera at three sediment traps in the subarctic,transition and subtropical zones of the central north Pacific Ocean[J]. Marine Micropaleontology,2003,48(1/2): 149-163.

丁旋,王汝建,张海峰,等. 北冰洋马克洛夫海盆现代浮游有孔虫深度分布及其生态与碳氧同位素特征[J]. 科学通报. 2014,59(13): 1230-1241. Ding Xuan,Wang Rujian,Zhang Haifeng, et al. Distribution,ecology,and oxygen and carbon isotope characteristics of modern planktonic foraminifers in the Makarov Basin of the Arctic Ocean[J]. Chinese Science Bulletin, 2014,59(13): 1230-1241.

Yamasaki M,Oda M. Sedimentation of planktonic foraminifera in the East China Sea: evidence from a sediment trap experiment[J]. Micropaleontology,2003,49: 3-20.

郑执中,郑守仪. 黄海和东海浮游有孔虫[J].海洋与湖沼,1960,3: 125-164. Cheng Tsi-chung,Cheng Sau-yee. The planktonic foraminifera of the Yellow Sea and the East China Sea[J]. Oceanologia et Limnologia Sinica,1960,3: 125-164.

郑执中,郑守仪. 黄海和东海浮游有孔虫生态的研究[J].海洋与湖沼,1962,4: 60-86. Cheng Tsi-chung,Cheng Sau-yee. On the ecology of the planktonic foraminifera of the Yellow Sea and the East China Sea[J]. Oceanologia et Limnologia Sinica,1962,4: 60-86.

汪品先,张纪军,赵泉鸿,等. 东海低质中的有孔虫和介形虫[M].北京:海洋出版社,1988: 1-438. Wang Pinxian,Zhang Jijun,Zhao Quanhong, et al.Foraminifera and Ostracoda in Bottom Sediments of the East China Sea[M]. Beijing:China Ocean Press,1988: 1-438.

Xu X D,Yamasaki M,Oda M,et al. Comparison of seasonal flux variations of planktonic foraminifera in sediment traps on both sides of the Ryukyu Islands,Japan[J]. Marine Micropaleontology,2005,58: 45-55.

王利波,杨作升,张荣平,等. 南黄海中部泥质区ZY2孔6200年以来的海表温度记录及黄海暖流变化的影响[J]. 科学通报,2011,56(15): 1213-1220. Wang Libo,Yang Zuosheng,Zhang Rongping, et al. Sea surface temperature records of core ZY2 from the central mud area in the South Yellow Sea during last 6200 years and related effect of the Yellow Sea Warm Current[J]. Chinese Science Bulletin,2011,56(15): 1213-1220.

Zhou C Y,Dong P,Li G X. Hydrodynamic processes and their impacts on the mud deposit in the Southern Yellow Sea[J]. Marine Geology,2015,360: 1-16.

Li G,Han X,Yue S,et al. Monthly variations of water masses in the East China Seas[J]. Continental Shelf Research,2006,26: 1954-1970.

Qi J F,Yin B S,Zhang Q L, et al. Analysis of seasonal variation of water masses in East China Sea[J]. Chinese Journal of Oceanology and Limnology,2014,32(4): 958-971.

Xu L,Wu D,Lin X,et al. The study of the Yellow Sea warm current and its seasonal variability[J]. J Hydrodyn Ser B,2009,21: 159-165.

宁修仁,刘子琳,史君贤. 渤、黄、东海初级生产力和潜在渔业生产量的评估[J].海洋学报,1995,17(3): 73-84. Ning Xiuren,Liu Zilin,Shi Junxian. Estimation of ocean primary productivity and the potential fisheries production of the Bohai Sea,the Yellow Sea and the East China Sea[J]. Haiyang Xuebao,1995,17(3): 73-84.

李国胜,王芳,梁强,等. 东海初级生产力遥感反演及其时空演化机制[J].地理学报,2003,58(4): 483-493. Li Guosheng,Wang Fang, Liang Qiang, et al. Estimation of ocean primary productivity by remote sensing and introduction to spacialtemperal variation mechenism for the East China Sea[J]. Journal of Geographical Sciences,2003,58(4): 483-493.

Quan Q,Mao X Y,Yang X D, et al. Seasonal variations of several main water masses in the southern Yellow Sea and East China Sea in 2011[J]. Oceanic and Coastal Sea Research,2013,12(4): 524-536.

Bé A W H. An ecological,zoogeographic and taxonomic review of recent planktonic foraminifera[G]//Ramsay A T S. Oceanic Micropaleontology. Academic press,London,1977: 1-100.

向荣,陈木宏,张兰兰,等. 南海北部秋季活体浮游有孔虫的组成与分布[J]. 中国地质大学学报,2010,35(1): 1-10. Xiang Rong,Chen Muhong,Zhang Lanlan, et al. Compositions and distribution of living planktonic foraminifera in autumn waters of the northern South China Sea[J]. Earth Science,Journal of China University of Geosciences,2010,35(1): 1-10.

Fabien L,Laurent L,Elisabeth M, et al. Modelling the temperature dependent growth rates of planktonic foraminifera[J]. Marine Micropaleontology,2009,70: 1-7.

BéHutson. Ecology of planktonic foraminifera and biogeographic patterns of life and fossil assemblages in the Indian Ocean[J]. Micropaleontology,1977,23: 369-414.

Kuroyanagi A,Kawahata H,Nishi H, et al. Seasonal changes in planktonic foraminifera in the northwestern North Pacific Ocean: sediment trap experiments from subarctic and subtropical gyres[J]. Deep-sea Research Ⅱ,2002,49: 5627-5645.

Gupta A K,Anderson D M,Overpeck J T. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean[J]. Nature,2003: 354-357.

Watkins J M,Mix A C,Wilson J. Living planktic foraminifera in the central tropical Pacific Ocean: articulating the equatorial ‘cold tongue’ during La Nifia,1992[J]. Marine Micropaleontology,1998,33:157-174.

张在秀,赵泉鸿,陈荣华,等. 东海泥质沉积区8千年来的有孔虫Mg/Ca和δ¹⁸O记录及其古环境意义[J]. 海洋地质与第四纪地质,2010,30(3): 79-86. Zhang Zaixiu,Zhao Quanhong,Cheng Ronghua, et al. Foraminiferal Mg/Ca and δ¹⁸O records in the mud aera of the East China Sea during the last 8000 years and their palaeoenvironmental implications[J].Marine Geology & Quaternary Geology,2010,30(3): 79-86.

赵泉鸿,翦知湣,张在秀,等. 东海陆架泥质沉积区全新世有孔虫和介形虫及其古环境应用[J]. 微体古生物学报,2009,26(2): 117-128. Zhao Quanhong,Jian Zhimin,Zhang Zaixiu, et al. Holocene Benthic Foraminifera and Ostracoda from the shelf mud aera of the East China Sea and their palaeoenvironmental implications[J]. Acta Micropalaeontologica Sinica,2009,26(2): 117-128.

经志友,齐义泉,华祖林. 闽浙沿岸上升流及其季节变化的数值研究[J]. 河海大学学报,2007,35(4): 464-470. Jing Zhiyou,Qi Yiquang,Hua Zulin. Numerical study on upwelling and its seasonal variation along Fujian and Zhejiang coast[J]. Journal o f Hohai University,2007,35(4): 464-470.

Xu X D,Oda M. Surface-water evolution of the eastern East China Sea during the last 36,000 years[J].Marine Micropaleontology,1999,156: 285-304.

Jian Z,Wang P,Saito Y, et al. Holocene variability of Kuroshio Current in the Okinawa Trough,northwestern Pacific Ocean[J]. Earth and Planetary Science Letters,2000,184: 305-319.

Fairbanks R G,Sverdlove M,Free R,et al.Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin[J]. Nature,1982,298: 841-844.

万随,翦知湣,成鑫荣,等. 南沙海区浮游有孔虫通量及其壳体化学性质的季节变化[J]. 中国科学: 地球科学,2010,40(7): 881-892. Wan Sui,Jian Zhimin,Cheng Xinrong, et al. Seasonal variations in planktonic foraminiferal flux and the chemical properties of their shells in the southern South China Sea[J]. Science China:Earth Science,2010,40(7): 881-892.

Li G S,Gao P,Wang F et al. Estimation of ocean primary productivity and its spatio-temporal variation mechanism for East China Sea based on VGPM model[J]. Journal of Geographical Sciences,2004,14(1): 32-40.

Lin H L,Hsieh H Y. Seasonal variations of modern planktonic foraminifera in the South China Sea[J]. Deep-Sea Research Part Ⅱ,2007,54: 1634-1644.

Kuroyanagi A,Kawahata H. Vertical distribution of living planktonic foraminifera in the seas around Japan[J]. Marine Micropaleontology,2004,53: 173-196.

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