COMPARISON BETWEEN CARBONATE RECORD OF HEQING CORE, δ18O RECORD OF THE DEEP SEA AND GRAIN SIZE RECORD OF THE CONTINENTAL LOESS

XIAO Hai-feng; SHEN Ji; XIAO Xia-yun

2006 Vol. 26, No. 2

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Article navigation > Marine Geology & Quaternary Geology > 2006 > 26(2): 41-47

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XIAO Hai-feng, SHEN Ji, XIAO Xia-yun. COMPARISON BETWEEN CARBONATE RECORD OF HEQING CORE, δ18O RECORD OF THE DEEP SEA AND GRAIN SIZE RECORD OF THE CONTINENTAL LOESS[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 41-47.

Citation:

XIAO Hai-feng, SHEN Ji, XIAO Xia-yun. COMPARISON BETWEEN CARBONATE RECORD OF HEQING CORE, δ18O RECORD OF THE DEEP SEA AND GRAIN SIZE RECORD OF THE CONTINENTAL LOESS[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 41-47.

COMPARISON BETWEEN CARBONATE RECORD OF HEQING CORE, δ18O RECORD OF THE DEEP SEA AND GRAIN SIZE RECORD OF THE CONTINENTAL LOESS

1 Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Naning 210008, China;
2 Graduate School of the Chinese Academy of Sciences, Beijing 100039, China

Received Date: 12 August 2005

Revised Date: 27 November 2005

Abstract

Abstract

Based on the scale of time of Heqing core confirmed by astronomical tune, this paper compares the curve of carbonate content of Heqing core with that of the deep sea δ18O and the loess grain size. The results show that the carbonate record of Heqing core is earlier than deep sea δ18O record and the grain size record of the continental loess during the mid-Pleistocene revolution, meaning that the uplift of Tibet Plateau plays an important role among the mid-Pleistocene revolution. Further, the curve of the carbonate content of Heqing core corresponds well with that of the deep sea δ18O, reflecting that the change of the global ice volume plays an important role in the evolution of southwest monsoon.
- southwest monsoon /
- curve of the deep sea δ¹⁸O /
- curve of the loess grain /

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References

[1]	徐道一,杨正宗,张勤文,等. 天文地质学概论[M]. 北京:地质出版社,1983:158-174.[XU Dao-yi,YANG Zheng-zong,ZHANG Qin-wen,et al. An introduction to astrogeology[M]. Beijing:Geological Publishing House,1983:158 Google Scholar -174.] Google Scholar
[2]	汪品先,田军,成鑫荣. 第四纪冰期旋回转型在南沙深海的记录[J]. 中国科学D辑,2001,31(10):793-799. Google Scholar [WANG Pin-xian,TIAN Jun,CHENG Xin-rong. Transition of Quaternary glacial cyclicity in deep-sea records at Nansha, the South China Sea[J]. Science in China (Series D), 2001,31(10):793-799.] Google Scholar
[3]	Liu D S, Ding Z L, Rutter N. Comparison of Milankovitch periods between continental loess and deep sea records over the last 2.5 Ma[J]. Quaternary Science Reviews, 1999, 17(3):1205-1212. Google Scholar
[4]	Kravchinsky V A, Krainov M A, Evans M E. Magnetic record of Lake Baikal sediments:chronological and paleoclimatic implication for the last 6.7 Myr[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 195(6):281-298. Google Scholar
[5]	Shackleton N J. The 100000-year Ice-Age Cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity[J]. Science, 2000, 289:1897-1901. Google Scholar
[6]	Clemens S C, Murray D W, Prell W L. Nonstationary phase of the Plio-Pleistocene Asian monsoon[J]. Science, 1996, 274:943-947. Google Scholar
[7]	Ding Z L, Derbyshire E, Yu Z W, et al. Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ¹⁸O record[J]. Paleoceanography, 2002, 17(3):1-21. Google Scholar
[8]	李峰,薛传东. 滇西北新生代以来地球动力学背景及其环境影响[J]. 大地构造与成矿学,1999,23(2):115-122. Google Scholar [LI Feng, XUE Chuan-dong. Geodynamic setting since the Cenozoic and its environmental effects in northwest Yunnan China[J]. Geotectonica et Metallogenia,1999,23(2):115-122.] Google Scholar
[9]	张荣祖,郑度,杨勤业,等. 横断山区自然地理[M]. 北京:科学出版社,1997:90-97.[ZHANG Rong-zu, ZHENG Du, YANG Qin-ye, et al. Physical geography of Hengduan mountains[M]. Beijing:Science Press, 1997:90 Google Scholar -97.] Google Scholar
[10]	Yu Z W, Ding Z L. An automatic orbital tuning method for paleoclimate records[J]. Geophysical Research Letters, 1998, 25:4525-4528. Google Scholar
[11]	Berger A, Loutre M F. Insolation values for the climate of the last 10 million years[J]. Quaternary Science Reviews 1991, 10:297-317. Google Scholar
[12]	Imbrie J, Hays J D, Martinson D G, et a1. The orbital theory of Pleistocene climate:Support from a revised chronology of the marine δ¹⁸O record[C]//Berger A, ed. Milankovich and Climate. Norwell MA:Reidel Press, 1984:269-305. Google Scholar
[13]	陈敬安,万国江,汪福顺,等.湖泊现代沉积物碳环境记录研究[J].中国科学D辑,2002, 32(1):73-80. Google Scholar [CHEN Jing-an, WAN Guo-jiang, WANG Fu-shun, et al. Environmental records of carbon in recent lake sediments[J]. Science in China (Series D), 2002, 32(1):73-80.] Google Scholar
[14]	Shackleton N J, Crowhurst T, Hagelbera N G, et al. A new late Neogene time scale:Application to Leg 138 site, Proc[J]. Ocean Drill. Program Sci. Results, 1995, 138:73-101. Google Scholar
[15]	Raymo M E, Oppo D W, Curru W. The mid-Pleistocene climate transition:A deep sea carbon isotopic perspective[J]. Paleoceanography, 1997, 12(4):546-559. Google Scholar
[16]	施雅风,李吉均,李炳元. 青藏高原晚新生代隆起与环境变化[M]. 广州:广东科技出版社,1998:399-401.[SHI Ya-feng, LI Ji-jun, LI Bing-yuan. Uplift and Environmental Changes of Qinghai-Xizang Plateau in the Late Cenozoic[M]. Guangzhou:Guangdong Science and Technology Press, 1998:399 Google Scholar -401.] Google Scholar
[17]	Clemens S, Prell W, Murray, et al. Forcing mechanisms of the Indian Ocean monsoon[J]. Nature, 1991, 353(24):720-725. Google Scholar
[18]	李吉均. 青藏高原的地貌演化与亚洲季风[J]. 海洋地质与第四纪地质,1999,19(1):1-11. Google Scholar [LI Ji-jun. Studies on the geomorphological evolution of the Qinghai-Xizang (Tibetan) plateau and Asian monsoon[J]. Marine Geology and Quaternary Geology, 1999, 19(1):1-11.] Google Scholar
[19]	汤懋苍,刘晓东. 一个新的划分第四纪的标志——高原季风演变的地质环境结果[J].第四纪研究,1995,2(1):82-88. Google Scholar [TANG Mao-cang, LIU Xiao-dong. A new mark for delimitation of Quaternary:stable appearance of plateau monsoon and its environmental effects[J]. Quaternary Sciences, 1995, 2(1):82-88.] Google Scholar