南海南部50万年以来碳酸钙和有机碳记录及其揭示的东亚夏季风演化

梅西; 张训华; 郑洪波; 刘锐; 黄恩清

doi:10.3799/dqkx.2010.003

Volume 35 Issue 1

Jan. 2010

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MEI Xi, ZHANG Xun-hua, ZHENG Hong-bo, LIU Rui, HUANG En-qing, 2010. 500000-Year Records of Carbonate and Organic Carbon from the Southern South China Sea and Implication for East Asian Summer Monsoon Evolution. Earth Science, 35(1): 22-30. doi: 10.3799/dqkx.2010.003

Citation:

MEI Xi, ZHANG Xun-hua, ZHENG Hong-bo, LIU Rui, HUANG En-qing, 2010. 500000-Year Records of Carbonate and Organic Carbon from the Southern South China Sea and Implication for East Asian Summer Monsoon Evolution. Earth Science, 35(1): 22-30. doi: 10.3799/dqkx.2010.003

Citation:

MEI Xi, ZHANG Xun-hua, ZHENG Hong-bo, LIU Rui, HUANG En-qing, 2010. 500000-Year Records of Carbonate and Organic Carbon from the Southern South China Sea and Implication for East Asian Summer Monsoon Evolution. Earth Science, 35(1): 22-30. doi: 10.3799/dqkx.2010.003

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500000-Year Records of Carbonate and Organic Carbon from the Southern South China Sea and Implication for East Asian Summer Monsoon Evolution

doi: 10.3799/dqkx.2010.003

1.
Institute of Oceanology, Chinese Academy Sciences, Qingdao 266071, China
2.
Graduate University, Chinese Academy of Sciences, Beijing 100049, China
3.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China
4.
Institute of Surficial Geochemistry, State Key Laboratory of Mineral Deposit Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China
5.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

Received Date: 2009-06-13
Publish Date: 2010-01-01

Abstract

Abstract

In order to understand the relation between surface productivity changes and the evolution of the East Asian summer monsoon during the Quaternary glacial cycles in southern South China Sea, high-resolution study on content and accumulation rate of calcium carbonate and organic carbon of Core MD05-2897 were done to draw the conclusions as follows: the content and accumulation rate of calcium carbonate showed significant glacial-interglacial cycle change while organic carbon mainly showed a higher frequency of the periodic changes. Both of the content and the accumulation rate of calcium carbonate and organic carbon increased in the interglacial periods and decreased in the glacial periods, which reflects the enhancement of the summer monsoon in the interglacial periods caused the strengthening of the upwelling currents and the increase of nutrients, the surface productivity increased consequently. The most abundant spectrum periods of 100ka eccentricity, 40ka obliquity, 20ka precession and 10ka semi-precession indicate the characteristics of the low latitude sea areas responding to the orbital periods. The accumulation rate of calcium carbonate and organic carbon were in good agreement with summer insolation of low latitude in the Northern Hemisphere related to precession which may be the main controlling factor of East Asia summer monsoon changes, and climate changes related to the global ice volume is possibly the secondary controlling factor.
- southern South China Sea,
- Late Quaternary,
- East Asia summer monsoon,
- orbital drive,
- organic carbon,
- calcium carbonate,
- oceangraphy

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References(64)

References

An, Z.S., Kutzbach, J.E., Prell, W.L., et al., 2001. Evolution of Asian monsoons and phased uplift of the Himalaya Tibetan plateau since Late Miocene times. Nature, 411(6833): 62-66. doi: 10.1038/35075035

Chen, M.T., Huang, C.Y., Wei, K.Y., 1997.25, 000-year Late Quaternary records of carbonate preservation in the South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 129(1-2): 155-169. doi: 10.1016/S0031-0182(96)00063-6

Chen, M.T., Shiau, L.J., Yu, P.S., et al., 2003.500000-year records of carbonate, organic carbon, and foraminifera sea-surface temperature from the southeastern South China Sea (near Palawan Island). Palaeogeography, Palaeoclimatology, Palaeoecology, 197(1-2): 113-131. doi: 10.1016/S0031-0182(03)00389-4

Clemens, S., Prell, W.L., Murray, D., et al., 1991. Forcing mechanisms of the Indian Ocean monsoon. Nature, 353(6346): 720-725. doi: 10.1038/353720a0

Davies, T.A., Kidd, R.B., Ramsay, A.T., 1995. A time-slice approach to the history of Cenozoic sedimentation in the Indian Ocean. Sedimentary Geology, 96(1-2): 157-179. doi: 10.1016/0037-0738(94)00131-D

Ding, Z.L., Liu, T.S., Rutter, N.W., et al., 1995. Ice-volume forcing of East Asian Winter monsoon variations in the past 800, 000 years. Quaternary Research, 44(2): 149-159. doi: 10.1006/qres.1995.1059

Ding, Z.L., Yu, Z.W., 1995. Forcing mechanisms of paleomonsoons over east asia. Quaternary Sciences, 1: 63-74 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=1712337

Fang, D.Y., Jian, Z.M., Wang, P.X., 2000. Paleoproductivity records for the past 30ka in the southern Nansha area, the South China Sea. Chin. Sci. Bull., 45(13): 1227-1230. doi: 10.1007/BF02886085

Guo, Z.T., Ruddiman, W.F., Han, Q.Z., et al., 2002. Onset of Asian desertification by 22myr ago inferred from loess deposits in China. Nature, 416(6877): 159-163. doi: 10.1038/416159a

Higginson, M, J., Maxwell, J.R., Altabet, M.A., 2003. Nitrogen isotope and chlorin paleoproductivity records from the northern South China Sea: remote versus local forcing of millennial and orbital-scale variability. Mar. Geol., 201(1-3): 223-250. doi: 10.1016/S0025-3227(03)00218-4

Howard, W.R., Prell, W.L., 1994. Late Quaternary CaCO₃ production and preservation in the South China Sea and Sulu seas. Paleoceanograpy, 9: 453-482. doi: 10.1029/93PA03524

Huang, B.Q., Jian, Z.M., Lin, H.L., 2000. Late quaternary changes of paleoproductivity in the northeastern South China Sea. Marine Geology & Quaternary Geology, 20(2): 65-68 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200002013.htm

Huang, W., Wang, P.X., 2006. The statistics of sediment mass in the South China Sea: method and result. Advances in Earth Science, 21(5): 465-473 (in Chinese with English abstract). http://www.onacademic.com/detail/journal_1000034540330710_5737.html

Imbrie, J., Hays, J.D., Martinson, D.G., et al., 1984. The orbital theory of pleistocene climate: support from a revised cronology of the marine δ¹⁸O record. In: Berger, A., Imbrie, J., eds., Milankovitch and climate. Holland Reidel D., Holland, 269-307.

Jian, Z.M., Wang, L.J., Kienast, M., 1999. Late Quaternary surface paleoproductivity and variations of the East Asian monsoon in the South China Sea. Quaternary Sciences, 1: 32-40 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ199901003.htm

Jian, Z.M., Wang, P.X., Chen, M.P., et al., 2000. Foraminiferal responses to major Pleistocene paleoceanographic changes in the southern South China Sea. Paleoceanography, 15(2): 229-243. doi: 10.1029/1999PA000431

Kuhnt, W., Hess, S., Jian, Z.M., 1999. Quantitative composition of benthic foraminifera assemblages as a proxy indicator for organic carbon flux rates in the South China Sea. Mar. Geol., 156(1-4): 123-157. doi: 10.1016/S0025-3227(98)00176-5

Kukla, G., An, Z.S., Melice, J.L., et al., 1990. Magnetic susceptibility record of Chinese loess. Trans. R. Soc. Ed. Earth. Sci., 81(4): 263-288. doi: 10.1017/S0263593300020794

Laj, C., Wang, P.X., Balut, Y., et al., 2005. MD147-Marco Polo IMAGESⅫ cruise report. Institut Paul-Emile Victor (IPEV), France.

Laskar, J., 1990. The chaotic notion of the solar system: a numerical estimate of the size of the chaotic zoins. Icarus, 88: 266-291. doi: 10.1016/0019-1035(90)90084-M

Li, J.R., Wang, R.J., Li, B.H., 2002. Variations of opal accumulation rates and paleoproductivity over the past 12Ma at ODP site 1143, southern South China Sea. Chinese Science Bulletin, 47(7): 596-598. doi: 10.1360/02tb9137

Lin, H., Lai, C., Ting, H., et al., 1999. Late Pleistocene nutrients and sea surface productivity in the South China Sea: a record of teleconnections with northern hemisphere events. Mar. Geol., 156(1-4): 197-210. doi: 10.1016/S0025-3227(98)00179-0

Liu, C.L., Cheng, X.R., Zhu, Y.H., et al., 2002a. Oxygen and carbon isotope records of calcareous nannofossils for the past 1Ma in the southern South China Sea. Chinese Science Bulletin, 47(10): 798-803. doi: 10.1360/02tb9180

Liu, C.L., Wang, P, X., Tian, J., et al., 2008. Coccolith evidence for Quaternary nutricline variations in the southern South China Sea. Marine Micropaleontology, 691: 42-51. doi: 10.1016/j.marmicro.2007.11.008

Liu, C.L., Zhang, S.Y., Jin, H.Y., et al., 2005. Coccolith evidence of upper ocean water variations for past 1.53Ma in western Pacific warm pool. Journal of Tongji University (Natural Science), 33(9): 1172-1176 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TJDZ200509006.htm

Liu, C.L., Zhu, Y.H., Cheng, X.R., 2001. Calcareous nannofossil evidence for variations in Quaternary surface water paleoproductivity in the southern South China Sea. Marine Geology & Quaternary Geology, 21(4): 61-66 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HYDZ200104014.htm

Liu, K.K., Chao, S.Y., Shaw, P.T., et al., 2002b. Monsoon-forced chlorophyll distribution and primary production in the South China Sea: observations and a numerical study. Deep-Sea Research, 49(8): 1387-1412. doi: 10.1016/S0967-0637(02)00035-3

Liu, Z.F., Zhao, Y.L., Li, J.R., et al., 2007. Late Quaternary clay minerals of Middle Vietnam in the western South China Sea: implications for source analysis and East Asian monsoon evolution. Science in China (Ser. D), 50(11): 1674-1684. doi: 10.1007/s11430-007-0115-8

Lyle, M., 1988. Climatically forced organic carbon burial in the equatorial Atlantic and Pacific oceans. Nature, 335(6190): 529-532. doi: 10.1038/335529a0

Lemark, L., Steinke, S., Wang, C.H., et al., 2009. New evidence for a glacioeustatic influence on deep water circulation, bottom water ventilation and primary productivity. Dynamics of Atmospheres and Oceans, 47(1-3): 138-153. doi: 10.1016/j.dynatmoce.2008.08.004

Paillard, D., Labeyrie, L., Yiou, P., 1996. Analyseries 1.0: a Macintosh software for the analysis of geographical time-series. Eos, 77: 379. doi: 10.1029/96EO00259

Sarnthein, M., Pflaumann, U., Ross, R., et al., 1992. Transfer functions to reconstruct ocean palaeoproductivity: a comparison. In: Summerhayes, C.P., Prell, W.L., Emeis, K.C., eds., Upwelling systems: evolution since the Early Miocene. Geological Society Special Publication Geological Society, London, 411-427.

Tamburini, F., Adatte, T., Fllmi, K., et al., 2003. Investigating the history of East Asian monsoon and climate during the last glacial-interglacial period (0-140000 years): mineralogy and geochemistry of ODP sites 1143 and 1144, South China Sea. Mar. Geol., 201(1-3): 147-168. doi: 10.1016/S0025-3227(03)00214-7

Thunell, R.C., Miao, Q.M., Calvert, S.E., et al., 1992. Glacial-Holocene biogenic sedimentation patterns in the South China Sea: productivity variations and surface water pCO₂. Paleoceanography, 7(2): 143-162. doi: 10.1029/92PA00278

Tian, J., Wang, P.X., 2006. Tropical process and its periodicity in the deep sea records. Earth Science-Journal of China University of Geosciences, 31(6): 747-753 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200606001.htm

Tian, J., Wang, P.X., Cheng, X.R., 2004. Pleistocene precession forcing of the upper ocean structure variations of the southern South China Sea. Progress in Natural Science, 14(6): 683-688 (in Chinese with English abstract). http://www.nsfc.gov.cn/csc/20345/24371/pdf/2004/Pleistocene%20precession%20forcing%20of%20the%20upper%20ocean%20structure%20variations%20of%20the%20southern%20South%20China%20Sea.pdf

Tian, J., Wang, P.X., Cheng, X.R., et al., 2005. Forcing mechanism of the Pleistocene East Asian monsoon variations in a phase perspective. Science in China (Ser. D), 48(10): 1708-1717. doi: 10.1360/01YD0467

Wang, B., Clemens, S.C., Liu, P., 2003b. Contrasting the Indian and East Asian monsoons: implications on geological timescales. Mar. Geol., 201(1-3): 5-21. doi: 10.1016/S0025-3227(03)00196-8

Wang, L.J., Sarnthein, M., Pflaumann, U., et al., 1999. East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea. Mar. Geol., 156(1-4): 245-284. doi: 10.1016/S0025-3227(98)00182-0

Wang, P.X., 1999. Response of western Pacific marginal seas to glacial cycles: paleoceanographic and sedimentological features. Mar. Geol., 156(1-4): 5-39. doi: 10.1016/S0025-3227(98)00172-8

Wang, P.X., Jian, Z.M., Zhao, Q.H., et al., 2003a. Evolution of the South China Sea and monsoon history revealed in deep sea records. Chinese Science Bulletin, 48(23): 2549-2561. doi: 10.1360/03wd0156

Wang, P.X., Wang, L.J., Bian, Y.H., et al., 1995a. Late Quaternary paleoceanography of the South China Sea: surface circulation and carbonate cycles. Mar. Geol., 127(1): 145-165. doi: 10.1016/0025-3227(95)00008-M

Wang, P.X., Zhao, Q.H., Cheng, X.R., et al., 1995b. South China Sea since 150000 years. Publishing House of Tongji University, Shanghai (in Chinese).

Wang, R., Abelmann, A., 2002. Radiolarian responses to paleoceanographic events of the southern South China Sea during the Pleistocene. Mar. Micropaleontol., 461: 25-44. doi: 10.1016/S0377-8398(02)00048-8

Wang, R.J., Jian, Z.M., Xiao, W.S., et al., 2007. Quaternary biogenic opal records in the South China Sea: linkages to East Asian monsoon, global ice volume and orbital forcing. Science in China (Ser. D), 50(5): 710-724. doi: 10.1007/s11430-007-0041-9

Wang, R.J., Li, J., 2003. Quaternary high-resolution opal record and its paleoproductivity implication at ODP site 1143, southern South China Sea. Chinese Science Bulletin, 48(4): 363-367. doi: 10.1360/03tb9077

Wang, R.J., Lin, J., Zheng, L.F., 2000. Siliceous microplankton fluxes and seasonal variations in the Central South China Sea during 1993-1995: monsoon climate and El Nino responses. Chinese Science Bulletin, 45(23): 2168-2172. doi: 10.1007/BF02886323

Webster, P.J., 1994. The role of hydrological processes in ocean-atmosphere interactions. Review of Geophysics, 32(4): 427-476. doi: 10.1029/94RG01873

Wei, G.J., Huang, C.Y., Wang, C.C., et al., 2006. High-resolution benthic foraminifer δ¹³C records in the South China Sea during the last 150ka. Mar. Geol., 232: 227-235. doi: 10.1016/j.margeo.2006.08.005

Wiesner, M.G., Zheng, L., Wong, H.K., 1996. Fluxes of particulate matter in the South China Sea. In: Ittekkot, V., Schafer, P., Honjo, S., et al., eds., Par-ticle flux in the Ocean. John Wiley and Sons, New York, 91-154.

Xiang, F., Wang, R.J., Li, J.R., et al., 2006. High resolution records of biogenic components and their paleoceanographic implications in the upwelling area of the South China Sea of eastern Vietnam over past 480ka. Marine Geology & Quaternary Geology, 26(6): 81-89 (in Chinese with English abstract).

Zhao, M.X., Huang, C.Y., Wang, C.C., et al., 2006. Amillennial-scale U37Ksea-surface temperature record fromthe South China Sea (8°N) over the last 150 kyr: monsoon and sea-level influence. Palaeogeogr. Palaeoclimatol. Palaeoecol., 236(1-2): 39-55. doi: 10.1016/j.palaeo.2005.11.033

Zheng, H.B., Yang, W.G., He, J., et al., 2008. Marine isotope stage 3 (mis 3) of South China Sea. Quaternary Sciences, 28(1): 68-79 (in Chinese with English abstract). doi: 10.1029/2007RG000226/full

丁仲礼, 余志伟, 1995. 第四纪时期东亚季风变化的动力机制. 第四纪研究, 1: 63-74. doi: 10.3321/j.issn:1001-7410.1995.01.007

黄宝琦, 翦知湣, 林慧玲, 2000. 南海东北部晚第四纪古生产力变化. 海洋地质与第四纪地质, 20(2): 65-68. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200002013.htm

黄维, 汪品先, 2006. 南海沉积物总量的统计: 方法与结果. 地球科学进展, 21(5): 465-473. doi: 10.3321/j.issn:1001-8166.2006.05.004

翦知湣, 王律江, Kienast, M., 1999. 南海晚第四纪表层古生产力与东亚季风变迁. 第四纪研究, 1: 32-40. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199901003.htm

刘传联, 祝幼华, 成鑫荣, 2001. 南海南部第四纪表层海水古生产力变化的钙质超微化石证据. 海洋地质与第四纪地质, 21(4): 61-66. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200104014.htm

刘传联, 张拭颖, 金海燕, 等, 2005. 暖池区1.53Ma以来上层海水变化的颗石藻证据. 同济大学学报(自然科学版), 33(9): 1172-1176. https://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ200509006.htm

田军, 汪品先, 成鑫荣, 2004. 更新世南海南部上层海水结构变化的岁差驱动. 自然科学进展, 14(6): 683-688. doi: 10.3321/j.issn:1002-008X.2004.06.014

田军, 汪品先, 2006. 深海记录中的热带过程及其周期性. 地球科学——中国地质大学学报, 31(6): 747-753. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200606001.htm

汪品先, 赵泉鸿, 成鑫荣, 等, 1995b. 十五万年来的南海. 上海: 同济大学出版社.

向霏, 王汝建, 李建如, 等, 2006. 越南岸外上升流区48万年来高分辨率的生源组分记录及其古海洋学意义. 海洋地质与第四纪地质, 26(6): 81-89. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200606013.htm

郑洪波, 杨文光, 贺娟, 等, 2008. 南海的氧同位素3期. 第四纪研究, 28(1): 68-79. doi: 10.3321/j.issn:1001-7410.2008.01.008

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500000-Year Records of Carbonate and Organic Carbon from the Southern South China Sea and Implication for East Asian Summer Monsoon Evolution

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