Coccolith assemblages and their response to climate and surface hydrography in the Yellow Sea, Northwest Pacific, AD 1780–2011

YUAN Mingli; HUANG Jiansheng; SUN Jun; SUN Yao

doi:10.1007/s13131-016-0895-9

近200年黄海颗石藻群落结构及其对气候变化的响应

doi: 10.1007/s13131-016-0895-9

1.
天津科技大学, 海洋与环境学院, 天津 300222, 中国;中国水产科学研究院, 黄海水产研究所, 青岛 266071, 中国
2.
中国水产科学研究院, 黄海水产研究所, 青岛 266071, 中国;海洋与地球学院, 厦门大学, 厦门 361005, 中国
3.
天津科技大学, 海洋与环境学院, 天津 300222, 中国
4.
中国水产科学研究院, 黄海水产研究所, 青岛 266071, 中国

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- 收稿日期: 2015-09-23
- 修回日期: 2016-05-03

Coccolith assemblages and their response to climate and surface hydrography in the Yellow Sea, Northwest Pacific, AD 1780–2011

1.
College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300222, China;Yellow Sea Fisheries Research Institute, Chinese Fisheries Science Academy, Qingdao 266071, China
2.
Yellow Sea Fisheries Research Institute, Chinese Fisheries Science Academy, Qingdao 266071, China;College of Ocean and Earth Science, Xiamen University, Xiamen 361005, China
3.
College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300222, China
4.
Yellow Sea Fisheries Research Institute, Chinese Fisheries Science Academy, Qingdao 266071, China

摘要

摘要: 对取自黄海中部的箱式沉积柱样进行颗石粒群落的分析，其结果为：颗石粒总丰度范围为7.0-55.1×106个/g，虽然不同种类的颗石粒在整个柱子中的丰度变化很大，但总的来说在群落中占有主要优势的有7个物种。其中，大洋桥石藻（Gephyrocapsa oceanica）占有绝对的优势，颗石粒平均相对丰度为50.1%，并且其相对丰度分布规律与贝氏布拉藻（Braarudosphaera bigelowii）和希布格脐球藻（Umbilicosphaera sibogae）（均为寡营养种）的颗石粒相对丰度的总和成相反趋势，这表明，在黄海大洋桥石藻分布情况可能与该海域可利用的营养盐有关。大洋桥石藻的颗石粒相对丰度与西伯利亚高压指数相似的分布规律表明，东亚冬季风可能是黄海生态变化的重要驱动因素。当东亚冬季风盛行时，黄海沿岸流和黄海暖流都加强，由此所带来的营养盐浓度增加和暖水有利于像大洋桥石藻这样的富营养暖水种的生长，这一机制也证明了气候变化可以通过海流等影响生态系统。
- 颗石粒 /
- 黄海 /
- 古海洋学 /
- 东亚冬季风 /
- 海流
Abstract: A study of coccolith assemblages from a box core from the central South Yellow Sea (SYS) was performed revealing fluctuations on their relative abundance (%) that can be related to climatic and hydrographic changes over the last 230 years (1780-2011). Total coccolith abundances ranged from 7.0 to 55.1×106 coccoliths·g-1 sediment. Although the abundance of different species varied widely throughout the core, seven taxa dominated the assemblage. Among these species, Gephyrocapsa oceanica was the most dominant species, and it showed an average percentage of 50.1%. The pattern of G. oceanica (eutrophic species) was opposite to that of the combined percentage of Braarudosphaera bigelowii and Umbilicosphaera sibogae (both oligotrophic species), indicating that in the Yellow Sea (YS), the distribution pattern of G. oceanica might be characteristic of nutrient availability. Similar patterns between G. oceanica and the Siberian High were observed on an inter-decadal time scale, indicating that the East Asian Winter Monsoon (EAWM) may be an important driver of ecological changes in the YS. When the EAWM prevails, both the Yellow Sea Coastal Current (YSCC) and Yellow Sea Warm Current (YSWC) strengthen, and the increasing nutrient availability and warmer water brought by the strengthened YSWC favor eutrophic and warm-water coccolithophore species, such as G. oceanica. This likely mechanism demonstrates that coccolith assemblages can be used as benign and reliable proxy for climate change and surface oceanography.
- coccolith /
- Yellow Sea /
- paleooceanography /
- East Asian Winter Monsoon /
- current

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参考文献(46)

Andruleit H. 1996. A filtration technique for quantitative studies of coccoliths. Micropaleontology, 42(4):403-406

Andruleit H, Rogalla U. 2002. Coccolithophores in surface sediments of the Arabian Sea in relation to environmental gradients in surface waters. Marine Geology, 186(3-4):505-526

Appleby P G. 2001. Chronostratigraphic techniques in recent sedi-ments. In:Last W M, Smol J P, eds. Tracking Environmental Change using Lake Sediments:Basin Analysis, Coring, and Chronological Techniques. Dordrecht:Kluwer Academic, 171-203

Boeckel B, Baumann K H. 2004. Distribution of coccoliths in surface sediments of the south-eastern South Atlantic Ocean:ecology, preservation and carbonate contribution. Marine Micropaleon-tology, 51(3-4):301-320

Boeckel B, Baumann K H, Henrich R, et al. 2006. Coccolith distribu-tion patterns in South Atlantic and Southern Ocean surface sediments in relation to environmental gradients. Deep Sea Re-search Part I:Oceanographic Research Papers, 53(6):1073-1099

Bukry D. 1974. Coccoliths as paleosalinity indicators-evidence from Black Sea:biology. In:Degens E T, Ross D A, eds. The Black Sea-Geology, Chemistry, and Biology. Tulsa, Oklahoma:The American Association of Petroleum Geologists, 353-363

Cao Qiyuan. 2003. Techniques for quantitative nannofossil studies. Marine Sciences (in Chinese), 27(3):1-3

Cao Qiyuan, Cang Shuxi, Li Tiegang, et al. 2002. Distribution of cal-careous nannofossils in surface sediment of the northern Ok-inawa trough and their environmental characteristics. Oceano-logia et Limnologia Sinica (in Chinese), 33(6):600-607

Cheng Xinrong. 1991. Distribution of calcareous nannoplankton in surface sediments of the central and northern parts of the South China Sea. Oceanologia et Limnologia Sinica (in Chinese), 22(4):377-383

Cheng Zhenbo, Shi Xuefa, Chen Z H, et al. 1999. The analysis of the sedimentary character of the microfossils and the material re-source in the surface sediments from the South Yellow Sea. Acta Sedimentologica Sinica (in Chinese), 17(S):775-781

Cheng Zhenbo, Shi Xuefa, Ju Xiaofa. 2000. The general situation about the study of micropalaeontology in the Southern Yellow Sea. Journal of Oceanography of Huanghai & Bohai Seas (in Chinese), 18(1):84-88

D'Arrigo R, Jacoby G, Wilson R, et al. 2005. A reconstructed Siberian High index since A.D. 1599 from Eurasian and North American tree rings. Geophysical Research Letters, 32(5):doi: 10.1029/2004GL022271

De Bernardi B, Ziveri P, Erba E, et al. 2005. Coccolithophore export production during the 1997-1998 El Niño event in Santa Bar-bara basin (California). Marine Micropaleontology, 55(1-2):107-125

De Bernardi B, Ziveri P, Erba E, et al. 2008. Calcareous phytoplank-ton response to the half century of interannual climatic variab-ility in Santa Barbara Basin (California). Paleoceanography, 23(2):doi: 10.1029/2007PA001503

Dittert N, Baumann K H, Bickert T, et al. 1999. Carbonate dissolution in the deep-sea:methods, quantification and paleoceano-graphic application. In:Fischer G, Wefer G, eds. Use of Proxies in Paleoceanography. Berlin Heidelberg:Springer, 255-284

Fatela F, Taborda R. 2002. Confidence limits of species proportions in microfossil assemblages. Marine Micropaleontology, 45(2):169-174

Frada M, Young J, Cach.o M, et al. 2010. A guide to extant coccolitho-phores (Calcihaptophycidae, Haptophyta) using light micro-scopy. Journal of Nannoplankton Research, 31(2):58-112

Giraudeau J, Grelaud M, Solignac S, et al. 2010. Millennial-scale vari-ability in Atlantic water advection to the Nordic Seas derived from Holocene coccolith concentration records. Quaternary Science Reviews, 29(9-10):1276-1287

Grelaud M, Schimmelmann A, Beaufort L. 2009. Coccolithophore re-sponse to climate and surface hydrography in Santa Barbara Basin, California, AD 1917-2004. Biogeosciences, 6(10):2025-2039

Ichikawa H, Beardsley R C. 2002. The current system in the Yellow and East China Seas. Journal of Oceanography, 58(1):77-92

Kirchner G. 2011. 210Pb as a tool for establishing sediment chronolo-gies:examples of potentials and limitations of conventional dating models. Journal of Environmental Radioactivity, 102(5):490-494

Liu Xiqing. 1996. Sedimentary division in marginal seas of China. Marine Geology & Quaternary Geology (in Chinese), 16(3):1-11

Liu Chuanlian, Shao Lei, Chen Ronghua, et al. 2001. Distribution of calcareous nannoplankton in surface sediments of the north-eastern parts of the South China Sea. Marine Geology & Qua-ternary Geology (in Chinese), 21(3):23-28

Liu Yi, Zhou Xin, Huang Wen, et al. 2013. Responses of primary pro-ductivity to current and climate changes in the mud area to the southwest of Cheju Island during the past 800 years. Journal of Ocean University of China, 12(4):605-610

Okada H, Honjo S. 1975. Distribution of coccolithophores in the mar-ginal seas along the western Pacific Ocean and in the Red Sea. Marine Biology, 31(3):271-285

Okada H, McIntyre A. 1979. Seasonal distribution of modern cocco-lithophores in the western North Atlantic Ocean. Marine Bio-logy, 54(4):319-328

Rui Xiaoqing, Liu Chuanlian, Liang Dan, et al. 2011. Distribution of calcareous nannofossils in the surface sediments of the South-ern Yellow Sea. Marine Geology & Quaternary Geology (in Chinese), 31(5):89-93

Saavedra-Pellitero M, Flores J A, Baumann K H, et al. 2011a. Compar-ison of different preparation and analysis techniques for quant-itative coccolith studies focusing on biogeographic patterns of species. Micropaleontology, 57(2):139-161

Saavedra-Pellitero M, Flores J A, Lamy F, et al. 2011b. Coccolitho-phore estimates of paleotemperature and paleoproductivity changes in the southeast Pacific over the past~27 kyr. Pa-leoceanography, 26(1):doi: 10.1029/2009PA001824

Schwab C, Kinkel H, Weinelt M, et al. 2012. Coccolithophore paleo-productivity and ecology response to deglacial and Holocene changes in the Azores Current System. Paleoceanography, 27(3):doi: 10.1029/2012PA002281

Schwab C, Kinkel H, Weinelt M, et al. 2013. A coccolithophore based view on paleoenvironmental changes in the open ocean mid-latitude North Atlantic between 130 and 48 ka BP with special emphasis on MIS 5e. Quaternary Science Reviews, 81:35-47

Sun Jun. 2007. Organic carbon pump and carbonate counter pump of living coccolithophorid. Advances in Earth Science (in Chinese), 22(12):1231-1239

Sun Jun, Gu Xiaoyao, Feng Yuanyuan, et al. 2014. Summer and winter living coccolithophores in the Yellow Sea and the East China Sea. Biogeosciences, 11(3):779-806

Sun Jun, Jin Shaofei. 2011. Species diversity of living coccolitho-phores in Chinese sea waters. Biodiversity Science (in Chinese), 19(6):787-797

Tanaka Y. 2003. Coccolith fluxes and species assemblages at the shelf edge and in the Okinawa Trough of the East China Sea. Deep Sea Research Part Ⅱ:Topical Studies in Oceanography, 50(2):503-511

Wang Jun, Luan Qingshan, Zuo Tao, et al. 2012. Taxonomic composi-tion of marine-living coccolithophores in the Yellow Sea and East China Sea-new records and a species list. Marine Biod-iversity Records, 5:e114

Wang Pinxian, Min Qiubao. 1981. A preliminary study of calcareous nannoplankton in bottom sediments of the East China Sea. Haiyang Xuebao (in Chinese), 3(1):188-192

Winter A, Jordan R W, Roth P H. 1994. Biogeography of living cocco-lithophores in ocean waters. In:Winter A, Siesser W G, eds. Coccolithophores. Cambridge:Cambridge University Press, 161-177

Winter A, Reiss Z, Luz B. 1979. Distribution of living coccolithophore assemblages in the Gulf of Elat ('Aqaba). Marine Micropaleon-tology, 4:197-223

Xiang Rong, Yang Zuosheng, Saito Y, et al. 2006. East Asia Winter Monsoon changes inferred from environmentally sensitive grain-size component records during the last 2300 years in mud area southwest off Cheju Island, ECS. Science in China Series D Earth Sciences, 49(6):604-614

Xiao Shangbin, Li Anchun, Jiang Fuqiang, et al. 2005. Recent 2000-year geological records of mud in the inner shelf of the East China Sea and their climatic implications. Chinese Science Bul-letin, 50(5):466-471

Xing Lei, Zhao Meixun, Zhang Hailong, et al. 2009. Biomarker re-cords of phytoplankton community structure changes in the Yellow Sea over the Last 200 years. Periodical of Ocean Uni-versity of China (in Chinese), 39(2):317-322

Yuan Dongliang, Hsueh Y. 2010. Dynamics of the cross-shelf circula-tion in the Yellow and East China Seas in winter. Deep Sea Re-search Part Ⅱ:Topical Studies in Oceanography, 57(19-20):1745-1761

Zhang Jian. 2011. Study on summer and winter community and dis-tribution of living coccolithophores in the Yellow Sea and East China Sea (in Chinese)[dissertation]. Qingdao:Ocean Uni-versity of China

Ziveri P, Broerse A T C, van Hinte J E, et al. 2000. The fate of cocco-liths at 48°N 21°W, Northeastern Atlantic. Deep Sea Research Part Ⅱ:Topical Studies in Oceanography, 47(9-11):1853-1875

Ziveri P, Thunell R C. 2000. Coccolithophore export production in Guaymas Basin, Gulf of California:response to climate forcing. Deep Sea Research Part Ⅱ:Topical Studies in Oceanography, 47(9-11):2073-2100

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文章访问数: 944
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近200年黄海颗石藻群落结构及其对气候变化的响应

doi: 10.1007/s13131-016-0895-9

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出版历程

Coccolith assemblages and their response to climate and surface hydrography in the Yellow Sea, Northwest Pacific, AD 1780–2011

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出版历程

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