PLANKTONIC FORAMINIFERA IN THE XISHA TROUGH OF THE SOUTH CHINA SEA DURING THE LAST 120 KA AND THEIR PALEOCLIMATIC IMPLICATIONS

ZHUANG Chang; CHEN Fang; ZHANG Jinpeng; ZHOU Yang; CHENG Sihai

doi:10.3724/SP.J.1140.2013.05089

Marine Geology & Quaternary Geology > 2013 > 33(5): 89-96. > DOI: 10.3724/SP.J.1140.2013.05089

ZHUANG Chang, CHEN Fang, ZHANG Jinpeng, ZHOU Yang, CHENG Sihai. PLANKTONIC FORAMINIFERA IN THE XISHA TROUGH OF THE SOUTH CHINA SEA DURING THE LAST 120 KA AND THEIR PALEOCLIMATIC IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2013, 33(5): 89-96. DOI: 10.3724/SP.J.1140.2013.05089

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PLANKTONIC FORAMINIFERA IN THE XISHA TROUGH OF THE SOUTH CHINA SEA DURING THE LAST 120 KA AND THEIR PALEOCLIMATIC IMPLICATIONS

1. Key Laboratory of Subseafloor Mineral Resources, Ministry of Land and Resources, Guangzhou 510760;
2. Guangzhou Marine Geological Survey, Guangzhou 510760

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Received Date: March 10, 2013
Revised Date: June 11, 2013

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Abstract

Abstract

Planktonic foraminifera from the core 83PC in the Xisha Trough of the northern South China Sea (SCS) have been quantitatively analyzed. The microfaunal analytical results, combined with oxygen and carbon isotopes, carbonate content and AMS¹⁴C dating data, are used in this paper to reveal paleoceanographic characteristics of the study area during the last~120 ka. The distribution of planktonic foraminifera shows that the abundance decreased in glacial periods, warm water species were sensitive to temperature changes, and the percentages of cool water species have decreased gradually since MIS5. Sea surface paleotemperature (SST) was estimated via transfer function FP-12E. The calculation results suggest that the winter SST ranged from 21.3 to 26.4℃, the summer SST from 28.2 to 29.5℃, and the SST seasonality from 2.7 to 6.9℃. By comparison with the results from the southern SCS, the SST differences were evident from MIS2 to MIS5, which probably resulted from the growth of the Northern Hemisphere ice sheet and the strong East Asian Monsoon, the higher SST differences in glacial periods indicated enhanced winter monsoon. Several obvious short-term SST descending events, including the Younger Dryas and Heinrich events, have been recognized since the last glaciation, suggesting the sedimentary records in response to the global climatic changes in the SCS.
- planktonic foraminifera,
- sea surface temperature,
- climatic changes,
- Late Quaternary,
- South China Sea

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References

[1]	李学杰, 江茂生. 南海西沙海槽末次冰期以来浮游有孔虫与表层水温[J]. 中国科学D辑, 2002, 32(5):423-429. [LI Xuejie, JIANG Maosheng. Planktonic foraminifera and sea surface temperature from the western South China Sea since the last glaciations[J]. Science in China (Series D), 2002, 32(5):423-429.]
[2]	汪品先, 赵泉鸿, 成鑫荣, 等. 十五万年来的南海[M]. 上海:同济大学出版社, 1995.[WANG Pinxian, ZHAO Quanhong, CHENG Xinrong, et al. South China Sea since 150000 Years[M]. Shanghai:Tongji University Press, 1995.]
[3]	汪品先, 翦知湣, 刘志伟. 南沙海区盛冰期的气候问题[J]. 第四纪研究, 1996, 16(3):193-201. [WANG Pinxian, JIAN Zhimin, LIU Zhiwei. The last glacial maximum climate problem in the sea area of the Nansha islands, South China Sea[J]. Quaternary Sciences, 1996, 16(3):193-201.]
[4]	汪品先, 翦知湣, 赵泉鸿, 等. 南海演变与季风历史的深海证据[J]. 科学通报, 2003, 48(21):2228-2239. [WANG Pinxian, JIAN Zhimin, ZHAO Quanhong, et al. Evolution of the South China Sea and monsoon history revealed in deep sea records[J]. Chinese Science Bulletin, 2003, 48(21):2228-2239.]
[5]	赵泉鸿, 汪品先. 南海晚第四纪古海洋学研究进展[J]. 第四纪研究, 1999, 19(6):481-501. [ZHAO Quanhong, WANG Pinxian. Progress in Quaternary paleoceanography of the South China Sea:a review[J]. Quaternary Sciences, 1999, 19(6):481-501.]
[6]	赵泉鸿, 翦知湣, 王吉良, 等. 南海北部晚新生代氧同位素地层学[J]. 中国科学D辑, 2001, 31(10):800-807. [ZHAO Quanhong, JIAN Zhimin, WANG Jiliang, et al. Late Cenozoic oxygen isotope stratigraphy in the north of South China Sea[J]. Science in China (Series D), 2001, 31(10):800-807.]
[7]	王律江, Sarnthein M. 南海北部陆坡近四万年的高分辨率古海洋学记录[J]. 第四纪研究, 1999, 19(1):27-31. [WANG Lüjiang, Sarnthein M. High-resolution paleoceanographic records during the last 40000 years from the northern slope of the South China Sea[J]. Quaternary Sciences, 1999, 19(1):27-31.]
[8]	Wang L J, Sarnthein M, Erlenkeuser H, et al. East Asia monsoon climate during the Late Pleistocene:High-resolution sediment records from the South China Sea[J]. Marine Geology, 1999, 156(1):245-284.
[9]	翦知湣, 王博士, 乔培军. 南海南部晚第四纪表层海水温度的变化及其与极地冰芯古气候记录的比较[J]. 第四纪研究, 2008, 28(3):391-397. [JIAN Zhimin, WANG Boshi, QIAO Peijun. Late Quaternary changes of surface temperature in the southern South China Sea and the comparison with the paleoclimatic records of polar ice cores[J]. Quaternary Sciences, 2008, 28(3):391-397.]
[10]	李丽, 王慧, 李建如, 等. 南海西部45万年来的表层水温变化[J]. 科学通报, 2009, 54(9):1269-1277. [LI Li, WANG Hui, LI Jianru, et al. Ghanges in sea surface temperature in western South China Sea over the past 450 ka[J]. Chinese Science Bulletin, 2009, 54(9):1269-1277.]
[11]	李保华, 赵泉鸿, 陈民本, 等. 南沙海区晚第四纪浮游有孔虫演化及其古海洋学意义[J]. 微体古生物学报, 2001, 18(1):1-9. [LI Baohua, ZHAO Quanhong, CHEN Minben, et al. Late Quaternary evolution of planktonic foraminifera in the southern South China Sea and their paleoceanographic significance[J]. Acta Micropalaeontologica Sinica, 2001, 18(1):1-9.]
[12]	Li B H, Jian Z M, Li Q, et al. Paleoceanography of the South China Sea since the Middle Miocene:Evidence from planktonic foraminifera[J]. Marine Micropaleontology, 2005, 54:49-62.
[13]	涂霞, 郑范, 陈木宏, 等. 南海南部陆坡区的浮游有孔虫及其所表征的表层古水温[J]. 热带海洋, 2000, 19(3):40-49. [TU Xia, ZHENG Fan, CHEN Muhong, et al. Planktonic foraminifera and paleo-SST of southern slope of South China Sea since 200 kaBP[J]. Tropic Oceanology, 2000, 19(3):40-49.]
[14]	郑范, 李前裕,陈木宏, 等. 南海西南部晚更新世500 ka以来的古海洋学特征[J]. 地球科学-中国地质大学学报, 2005, 30(5):534-549. [ZHENG Fan, LI Qianyu, CHEN Muhong, et al. Late Pleistocene paleoceanographic characteristics of the southwestern South China Sea since 500 ka[J]. Earth Science-Journal of China University of Geosciences, 2005, 30(5):534-549.]
[15]	陈木宏, 涂霞, 郑范, 等. 南海南部近20万年沉积序列与古气候变化关系[J]. 科学通报, 2000, 45(5):542-548. [CHEN Muhong, TU Xia, ZHENG Fan, et al. Relations between sedimentary sequence and paleoclimatic changes during last 200 ka in the southern South China Sea[J]. Chinese Science Bulletin, 2000, 45(5):542-548.]
[16]	向荣, 刘芳, 孙有斌, 等. 冲绳海槽末次冰消期以来的浮游有孔虫群落变化及5种古温度转换函数对比[J]. 地球科学-中国地质大学学报, 2011, 36(4):599-609. [XIANG Rong, LIU Fang, SUN Youbin, et al. Changes of planktonic foraminiferal assemblages in the Okinawa Trough since the Last Deglaciation and comparisons of sea-surface temperature estimated from five foraminiferal transfer functions[J]. Earth Science-Journal of China University of Geosciences, 2011, 36(4):599-609.]
[17]	Thompson P R. Planktonic foraminifera in the western North Pacific during the past 150000 years:Comparison of modern and fossil assemblages[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1981, 35:241-279.
[18]	Yang X Q, Friedrich H, Wu N Y, et al. Geomagnetic paleointensity dating of South China Sea sediments for the last 130 kyr[J]. Earth and Planetary Science Letters, 2009, 284:258-266.
[19]	钱建兴. 晚第四纪以来南海古海洋学研究[M]. 北京:科学出版社, 1999.[QIAN Jianxin. A Study of Paleoceanography in the South China Sea During the Last Quaternary[M]. Beijing:Science Press, 1999.]
[20]	Bühring C, Sarnthein M, Erlenkeuser H. Toward a high-resolution stable isotope stratigraphy of the last 1.1 million years:Site 1144, South China Sea[R]. Proc. ODP, Sci. Results, 2004, 184:1-29.
[21]	蔡观强, 彭学超, 陈泓君, 等. 南海西沙海槽83PC柱状沉积物组成特征及其古环境意义[J]. 海洋地质与第四纪地质, 2012, 32(1):77-84. [CAI Guanqiang, PENG Xuechao, CHEN Hongjun, et al. The component characteristics and paleoenvironmental significances for sediments in core 83PC from the Xisha Trough, South China Sea[J]. Marine Geology and Quaternary Geology, 2012, 32(1):77-84.]
[22]	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 area of the East China Sea and their paleoenvironmental implications[J]. Acta Micropalaeontologica Sinica, 2009, 26(2):117-128.]
[23]	向荣, 陈木宏, 张兰兰, 等. 南海北部秋季浮游有孔虫的组成与分布[J]. 地球科学-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.]
[24]	黄宝琦, 翦知湣, 成鑫荣, 等. 南海晚第四纪上升流区海水上层水体结构的变化[J]. 科学通报, 2001, 46(11):948-952. [HUANG Baoqi, JIAN Zhimin, CHENG Xinrong, et al. Late Quaternary upper-water column structure in upwelling areas of the South China Sea[J]. Chinese Science Bulletin, 2001, 46(11):948-952.]
[25]	Jian Z M, Huang B Q, Kuhnt W, et al. Late Quaternary upwelling intensity and East Asia monsoon forcing in the South China Sea[J]. Quaternary Research, 2001, 55:363-370.
[26]	李小艳, 翦知湣, 石学法, 等. 南海西北部89PC柱样沉积物中浮游有孔虫特征及其古环境意义[J]. 海洋地质与第四纪地质, 2009, 29(3):85-92. [LI Xiaoyan, JIAN Zhimin, SHI Xuefa, et al. Planktonic foraminifera in core 89PC from the northwestern South China Sea and their paleoenvironment significance[J]. Marine Geology and Quaternary Geology, 2009, 29(3):85-92.]
[27]	汪品先, 卞云华, 李保华, 等. 西太平洋边缘海的"新仙女木"事件[J]. 中国科学D辑, 1996, 26(5):452-460. [WANG Pinxian, BIAN Yunhua, LI Baohua, et al. The Younger Dryas in the West Pacific marginal seas[J]. Science in China (Series D), 1996, 26(5):452-460.]
[28]	刘嘉麒, 倪云燕, 储国强. 第四纪主要气候事件[J]. 第四纪研究, 2001, 21(3):239-245. [LIU Jiaqi, NI Yunyan, CHU Guoqiang. Main palaeoclimatic events in the Quaternary[J]. Quaternary Sciences, 2001, 21(3):239-245.]
[29]	Dansgaard W, White J W C, Johnson S J. The abrupt termination of the Younger Dryas climate event[J]. Nature, 1989, 339:532-534.
[30]	Mayewski P A. The Younger Dryas as viewed through the Summit Greenland ice cores[J]. PAGES, 1995, 3:5-6.
[31]	王律江, 卞云华, 汪品先. 南海北部末次冰消期及快速气候回返事件[J]. 第四纪研究, 1994, 14(1):1-12. [WANG Lüjiang, BIAN Yunhua, WANG Pinxian. The last deglaciation in the South China Sea and the rapid climate return event[J]. Quaternary Sciences, 1994, 14(1):1-12.]
[32]	李丽, 王慧, 汪品先. 南海北部17937岩心四万年来古环境变化的分子有机地球化学记录[J]. 地球科学-中国地质大学学报, 2008, 33(6):793-799. [LI Li, WANG Hui, WANG Pinxian. Molecular organic geochemical record of paleoenvironmental changes of core 17937 in Northern South China Sea since 40 ka[J]. Earth Science-Journal of China University of Geosciences, 2008, 33(6):793-799.]
[33]	Andrews J T. Abrupt changes (Heinrich event) in late Quaternary North Atlantic marine environments[J]. Journal of Quaternary Science, 1997, 278:1257-1265.
[34]	Bond G, Broecker W, Johnson S, et al. Correlations between climate records from North Atlantic sediments and Greenland ice[J]. Nature, 1993, 365:143-147.
[35]	Yu P S, Huang C C, Chin Y, et al. Late Quaternary East Asian Monsoon variability in the South China Sea:Evidence from planktonic foraminifera faunal and hydrographic gradient records[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2006, 236:74-90.

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PLANKTONIC FORAMINIFERA IN THE XISHA TROUGH OF THE SOUTH CHINA SEA DURING THE LAST 120 KA AND THEIR PALEOCLIMATIC IMPLICATIONS