南海ODP1143站上新世至更新世天文年代标尺的建立

田军; 汪品先; 成鑫荣; 李前裕

Volume 30 Issue 1

Jan. 2005

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TIAN Jun, WANG Pin-xian, CHENG Xin-rong, LI Qian-yu, 2005. Establishment of the Plio-Pleistocene Astronomical Timescale of ODP Site 1143, Southern South China Sea. Earth Science, 30(1): 31-39.

Citation:

TIAN Jun, WANG Pin-xian, CHENG Xin-rong, LI Qian-yu, 2005. Establishment of the Plio-Pleistocene Astronomical Timescale of ODP Site 1143, Southern South China Sea. Earth Science, 30(1): 31-39.

TIAN Jun, WANG Pin-xian, CHENG Xin-rong, LI Qian-yu, 2005. Establishment of the Plio-Pleistocene Astronomical Timescale of ODP Site 1143, Southern South China Sea. Earth Science, 30(1): 31-39.

Citation:

TIAN Jun, WANG Pin-xian, CHENG Xin-rong, LI Qian-yu, 2005. Establishment of the Plio-Pleistocene Astronomical Timescale of ODP Site 1143, Southern South China Sea. Earth Science, 30(1): 31-39.

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Establishment of the Plio-Pleistocene Astronomical Timescale of ODP Site 1143, Southern South China Sea

Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

Received Date: 2004-11-26
Publish Date: 2005-01-25

Abstract

Abstract

An accurate timescale derived from benthic foraminiferal δ¹⁸O is crucial to paleoceanographic studies. In global oceans, there are few continuous δ¹⁸O records for the benthic foraminifers which span the past 5 Ma and have time resolution better than 5 ka. Such representative profiles have been established for ODP Site 659 in the Atlantic and ODP Site 846 in the east Pacific, but still have been absent in the"Western Pacific Warm Pool", an area playing an important role in global climate changes. Based on the benthic foraminiferal δ¹⁸O of ODP Site 1143 in the southern South China Sea, we establish a 5 Ma astronomical timescale for the west Pacific Plio-Pleistocene, with a time resolution of ~ 2-3 ka. The phases are fixed at 8 ka and 5 ka for the obliquity and precession bands respectively, and have been applied throughout the whole records. Obliquity and precession are calculated and treated as the tuning targets.An automatic orbital tuning method has been applied in this study, which is more efficient than those used at ODP Site 659 and 846. The results show that the 190.77 m long deep sea sediments in the South China Sea have recorded a paleoceanographic history of ~ 5.02 Ma, corresponding to 191 glacial/interglacial cycles. The tuned Brunhes/Matuyama paleomagnetic polarity reversal agrees well with an age of 0.78 Ma dated previously. The tuned ages for several planktonic foraminifer bio-events also agree well with published dates, and new ages for some other bio-events in the South China Sea are also estimated. The sedimentation rates calculated from this new timescale indicate that 2.9 Ma is a threshold for the sedimentation rate in the location of Site 1143. Before this time, the average sedimentation rate is ~ 39.5 m/Ma, with a small amplitude of ~ 50 m/Ma.After this time, the average sedimentation rate jumped to ~ 65.4 m/Ma, with an amplitude as large as 200 m/Ma. In addition, the sedimentation ratesin the southern South China Sea were higher during glacials or stadials but lower during interglacials orinterstadials, especially in the late Pleistocene period. This feature might be related to the global ice volume changes, which caused different erosion, denudation and transportation during glacials and interglacials.
- South China Sea,
- ODP Site 1143,
- Pliocene,
- Pleistocene,
- astronomical timescale

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References(26)

References

Berger, A., Loutre, M.F., 1991. Insolation values for the climate of the last 10 million years. Quat. Sci. Rev. , 10: 297-317. doi: 10.1016/0277-3791(91)90033-Q

Berggren, W.A., Kent, D.V., Swisher Ⅲ, C.C., et al., 1995a. A revised Cenozoic geochronology and chronostratigraphy. In: Berggren, W.A., Kent, D.V., Aubry, M.P., et al., eds., Geochronology, time scales and global stratigraphic correlation. Spec. Publ. SEPM, 54: 129-212.

Berggren, W.A., Hilgen, F. J., Langereis, C.G., et al., 1995b. Late Neogene chronology: New perspectives in high-resolution stratigraphy. Geol. Soc. Am. Bull. , 107: 1272-1287. doi: 10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2

Carter, R.M., McCave, I.N., Richter, C., et al., 1999. Proceedings of the Ocean Drilling Program. Initial Reports 181, Ocean Drilling Program, College Station, TX.

Chen, J., Farrel, J.W., Murray, D.W., et al., 1995. Timescale and paleoceanographic implications of a 3. 6 m. y. oxygen isotope record from the northeast Indian Ocean(Ocean Drilling Program Site 758). Paleoceanograpy, 10: 21-47. doi: 10.1029/94PA02290

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

Hall, C.M., Farrell, J.W., 1993. Laser ⁴⁰Ar/³⁹Ar age from ash D of ODP Site 758: Dating the Brunhes-Matuyama reversal and oxygen isotope stage 19.1. Eos Trans. AGU, 74(16): 110.

Hays, J.D., Imbrie, J., Shackleton, N.J., 1976. Variations in the earth's orbit: Pacemaker of the ice ages. Science, 194: 1121-1132. doi: 10.1126/science.194.4270.1121

Huang, W., Wang, P., 1998. A quantitative approach to deepwater sedimentation in the South China Sea. Sci. in China (Series D), 41: 195-201. http://www.cnki.com.cn/Article/CJFDTotal-JDXG199802011.htm

Imbrie J., Hays, J.D., Martinson, D.G., et al., 1984. The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ¹⁸O record. In: Berger, A., ed., Milankovitch and climate. D. Reidel, Norwell, Mass., 269-305.

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

Milankovitch, M., 1930. Mathematische Klimalehre und astronomishe Theorie der Klimasch-wankungen. In: Koppen, W., Geiger, R., eds., Handbuch der Klimatologie. Gebruder Borntraeger, Berlin, Ⅰ(A): 1-76.

Mix, A. C., Le, J., Shackleton, N. J., 1995a. Benthic foraminiferal stable isotope stratigraphy of site 846: 0-1. 8 Ma. In: Pisias, N.G., Mayer, L.A., Janecek, T.R., et al., eds., Proc. ODP Sci. Results, 138: 839-854.

Mix, A.C., Pisias, N.G., Rugh, W., et al., 1995b. Benthic foraminifer stable isotope record from site 849(0-5 Ma): Local and global climate changes. In: Pisias, N.G., Mayer, L.A., Janecek, T.R., et al., eds., Proc. ODP Sci. Results, 138: 371-412.

Raymo, M.E., Oppo, D.W., Curry, W., 1997. The mid-Pleistocene climate transition: A deep sea carbon isotopic perspective. Plaeoceanography, 12: 546-559. doi: 10.1029/97PA01019

Shackleton, N.J., Imbrie, J., Hall, M.A., 1983. Oxygen and carbon isotope record of East Pacific core V19-30: Implications for the formation of deep water in the late Pleistocene North Atlantic. Earth Planet. Sci. Lett. , 65: 233-244. doi: 10.1016/0012-821X(83)90162-0

Shackleton, N.J., Berger, A., Peltier, W.R., 1990. An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677. Trans. R. Soc. Edinburgh Earth Sci. , 81: 251-261. doi: 10.1017/S0263593300020782

Shackleton, N.J., Hall, N.J., Pate, D., 1995a. Pliocene stable isotope stratigraphy of site 846. In: Pisias, N.G., Mayer, L.A., Janecek, T.R. et al., eds., Proc. ODP Sci. Results, 138: 337-355.

Shackleton, N.J., Crowhurst, S., Hagelberg, T., et al., 1995b. A new late Neogene time scalel: Application to Leg 138 sites. In: Pisias, N.G., Mayer, L.A., Janecek, T.R., et al., eds., Proc. ODP Sci. Results, 138: 73-101.

Thompson, P.R., Bé, A., Duplessy, J.C., et al., 1979. Disappearance of pink-pigmented Globigerinoides ruber at 120, 000 yr BP in the Indian and Pacific oceans. Nature, 280: 554-558. doi: 10.1038/280554a0

Tian, J., Wang, P.X., Cheng, X.R., 2004. Stable isotope equilibrium test between benthic foraminifer Cibicidoides and Uvigerina at ODP Site 1143, southern South China Sea. Earth Sciences—Journal of China University of Geosciences, 29(1): 1-6(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200401000.htm

Tiedemann, R., Sarnthein, M., Shackleton, N.J., 1994. Astronomic timescale for the Pliocene Atlantic δ¹⁸O and dust flux records from Ocean Drilling Program Site 659. Paleoceanography, 9: 619-638. doi: 10.1029/94PA00208

Wang, P., Tian, J., Cheng, X., 2001. Transition of Quaternary glacial cyclicity in deep-sea records at Nansha, South China Sea. Sci. in China(Series D), 44: 926-933. doi: 10.1007/BF02907085

Wang, P.X., Prell, W.L., Blum, P., et al., 2000. Proceedings of the Ocean Drilling Program, Initial Reports 184, Ocean Drilling Program College Station.

Yu, Z., Ding, Z., 1998. An automatic orbital tuning method for paleoclimate records. Geophys. Res. Lett. , 25: 45254528.

田军, 汪品先, 成鑫荣, 2004. 南海ODP1143站底栖有孔虫Cibicidoides与Uvigerina稳定氧碳同位素值的均衡试验. 地球科学——中国地质大学学报, 29(1): 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200401000.htm

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