泥河湾盆地基于粒度气候指标的轨道调谐时间标尺

韩志勇; 李徐生

Volume 31 Issue 6

Jun. 2006

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2006 > 31(6): 773-779

HAN Zhi-yong, LI Xu-sheng, 2006. Orbitally Tuned Time Scale Based on Climate Proxy Indicator of Grain Size Distribution in Nihewan Basin. Earth Science, 31(6): 773-779.

Citation:

HAN Zhi-yong, LI Xu-sheng, 2006. Orbitally Tuned Time Scale Based on Climate Proxy Indicator of Grain Size Distribution in Nihewan Basin. Earth Science, 31(6): 773-779.

HAN Zhi-yong, LI Xu-sheng, 2006. Orbitally Tuned Time Scale Based on Climate Proxy Indicator of Grain Size Distribution in Nihewan Basin. Earth Science, 31(6): 773-779.

Citation:

HAN Zhi-yong, LI Xu-sheng, 2006. Orbitally Tuned Time Scale Based on Climate Proxy Indicator of Grain Size Distribution in Nihewan Basin. Earth Science, 31(6): 773-779.

PDF( 547 KB)

Orbitally Tuned Time Scale Based on Climate Proxy Indicator of Grain Size Distribution in Nihewan Basin

HAN Zhi-yong^{1, 2
,},
LI Xu-sheng¹

1.
Department of Urban and Resources Sciences, Nanjing University, Nanjing 210093, China
2.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, Cbina

Received Date: 2006-05-12
Publish Date: 2006-11-25

Abstract

Abstract

The Donggou Section located in the east of Nihewan basin contains a suite of strata consisted mainly of lacustrine sediments approximate to 100 m thick. Both grain size distribution and magnetic susceptibility are measured in successive samples collected from this section. A preliminary time scale can be derived, based on the comparison between records of magnetic susceptibility, from the geomagnetic polarity reversals determined by previous studies. In this study, the grain (20-50 μm) content record of Donggou Section can be correlated to the ETP curve. The low value of the former is compared with the high value of the latter. This negative correlation implies that the dust inputs into sediments in the Nihewan basin decreases while the solar radiation on the north hemisphere increases. This scenario is compatible with the known evolution of the aeolian activity in North China. Therefore, the grain (20-50 μm) content is a reliable proxy indicator of the paleoclimate change. Orbital tuning method is performed and a time scale of high resolution is obtained for the strata older than > 780 ka since the sedimentation rate here is relatively high. The 20 ka and 41 ka periodic components filtered from the obtained grain (20-50 μm) content time series are consistent with the theoretic cycles of the precession and the tilt, respectively, indicating that the grain (20-50 μm) content record of Donggou Section can be used as the climatic curve for orbital tuning.
- Nihewan,
- Donggou Section,
- grain size,
- time series,
- orbital tuning.

FullText(HTML)

References(36)

References

An, Z. S., Liu, T. S., Lou, Y. C., et al., 1990. The long-termpalaeomonsoon variation recorded by the loess-paleosolsequence in central China. Quat. Int., 7 (8): 91-95.

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

Chen, F. H., Bloemendal, J., Zhang, P. Z., et al., 1999. An800ka proxy record of climate fromlake sediments of the Zoige basin, eastern Tibetan plateau. Palaeogeogr. Palaeocli matol. Palaeoecol., 151: 307-320. doi: 10.1016/S0031-0182(99)00032-2

Chi, Z. Q., Min, L. R., Zhu, G. X., et al., 2002. Paleocli maticperiodicities recorded in Nihewan lacustrine deposits, Hebei Province, North China. Earth Science Frontiers, 9 (1): 182-186 (in Chinese with English abstract).

Clemens, S. C., Tiedemann, R., 1997. Eccentricity forcing ofPliocene-Early Pleistocene climate revealed in a marineoxygen-isotope record. Nature, 385: 801-804. doi: 10.1038/385801a0

Ding, Z. L., Liu, T. S., Rutter, N. W., et al., 1995. Ice-volume forcing of east Asian winter monsoon variations in the past 800000 years. Quat. Res., 44: 149-159. doi: 10.1006/qres.1995.1059

Ding, Z. L., Yu, Z. W., Liu, D. S., 1991. Process in loess re-search (Part3): Time scale. Quaternary Sciences, (4): 336-348 (in Chinese with English abstract).

Ding, Z. L., Yu, Z. W., Rutter, N. W., et al., 1994. Towardsan orbital time scale for Chinese loess deposits. Quat. Sci. Rev., 13: 39-70. doi: 10.1016/0277-3791(94)90124-4

Guo, Z. T., Biscaye, P., Wei, L. Y., et al., 2000. Summermonsoon variations over the last 1.2 Ma from theweathering of loess-soil sequences in China. Geophys. Res. Lett., 27 (12): 1751-1754. doi: 10.1029/1999GL008419

Han, Z. Y., Liu, D. Y., Hovan, S. A., 2002. Lightness timescale for terrestrial sediments in loess deposit area in the past500000years. Paleoceanography, 17: 1048, doi: 10.1029/2001PA000731.

Heslop, D., Langereis, C. G., Dekkers, M. J., 2000. A newastronomical timescale for the loess deposits of Northern China. Earth Planet. Sci. Lett., 184: 125-139. doi: 10.1016/S0012-821X(00)00324-1

Hovan, S. A., Rea, D. K., Pisias, N. G., et al., 1989. Adirectlink between the China loess and marine δ¹⁸O records: Aeolian flux to the north Pacific. Nature, 340: 296-298. doi: 10.1038/340296a0

Hu, S., Goddu, S. R., Appel, E., et al., 2005. Palaeocli maticchanges over the past 1million years derived fromla-custrine sediments of Heqing basin (Yunnan, China). Quat. Int., 136: 123-129. doi: 10.1016/j.quaint.2004.11.013

Johnson, T. C., Brown, E. T., Mc Manus, J., 2002. A high-resolution paleoclimate record spanning the past 25000 years in southern East Africa. Science, 296: 113-132. doi: 10.1126/science.1070057

King, T., 1996. Quantifying non-linearity and geometry intime series of climate. Quat. Sci. Rev., 15: 247-266. doi: 10.1016/0277-3791(95)00060-7

Kohfeld, K. E., Harrison, S. P., 2003. Glacial-interglacialchanges in dust deposition on the Chinese Loess plat-eau. Quat. Sci. Rev., 22: 1859-1878. doi: 10.1016/S0277-3791(03)00166-5

Kravchinsky, V. A., Krainov, M. A., Evans, M. E., et al., 2003. Magnetic record of Lake Baikal sediments: Chron-ological and paleocli matic implication for the last 6.7 Myr. Palaeogeogr. Palaeocli matol. Palaeoecol., 195: 281-298. doi: 10.1016/S0031-0182(03)00362-6

Liu, Z. C., Chen, Y., Yuan, L. W., et al., 2000. Deducingthe pa-leoclimate change during the past2.85Ma by using thenatural gamma-ray hole logging curve. Science in China (Series D), 30 (6): 509-618 (in Chinese).

Lu, H. Y., Liu, X. D., Zhang, F. Q., et al., 1999. Astronomi-cal calibration of loess-paleosol deposits at Luochuan, central Chinese Loess plateau. Palaeogeogr. Palaeoclimatol. Palaeoecol., 154: 237-246. doi: 10.1016/S0031-0182(99)00113-3

Lu, H. Y., Van Huissteden, K., An, Z. S., et al., 1999. East Asia winter monsoon variations on a millennial time-scale before the last glacial-interglacial cycle. J. Quater-nary Sciences, 14: 101-110. doi: 10.1002/(SICI)1099-1417(199903)14:2<101::AID-JQS433>3.0.CO;2-M

Min, L. R., Chi, Z. Q., Zhu, G. X., 2000. Division of Quater-nary lacustrine beds in Jingerwa bolehole of the Yangyuan basin. Acta Geologica Sinica, 74 (2): 108-115 (in Chinese with English abstract).

Paillard, D., Labeyrie, L., Yiou, P., 1996. Macintosh program performs time-series analysis. EOS Trans. AGU, 77: 379.

Pye, K., Zhou, L., 1989. Late Pleistocene and Holocene aeo-lian dust deposition in north China and the northwestPacific Ocean. Palaeogeogr. Palaeocli matol. Palaeoecol., 73: 11-23. doi: 10.1016/0031-0182(89)90041-2

Rial, J., 1999. Pacemaking the ice ages by frequency modula-tion of earth sorbital eccentricity. Science, 285: 564-568. doi: 10.1126/science.285.5427.564

Shackleton, N. J., Berger, A., Peltier, W. R., 1990. An alterna-tive astronomical calibration of thelower Pleistocene times-cale based on ODP Site 677. Transactions of the Royal Society of Edinburgh: Earth Sciences, 81: 251-261. doi: 10.1017/S0263593300020782

Sun, D., Bloemendal, J., Rea, D. K., et al., 2002. Grain-sizedistribution function of polymodal sediments in hydrau-lic and aeolian environments, and numerical partitioningof the sedimentary components. Sedi ment. Geol., 152: 263-277. doi: 10.1016/S0037-0738(02)00082-9

Xiong, S. F., Ding, Z. L., Liu, D. S., 1999. Loess deposits inBeijing region since last 1.2 Ma and desert expansionover northern China. Marine Geology & Quaternary Geology, 19 (3): 68-73 (in Chinese with English abstract).

Yang, X. Q., Li, H. M., 1999. The sediment susceptibility andgrain-size profile respondto change of depositional environment in Nihewan basin. Acta Sedimentologica Sinica, 17 (Suppl. ): 763-768 (in Chinese with English abstract).

Zhu, R. X., Hoff man, K. A., Potts, R., et al., 2001. Earliestpresence of humans in northeast Asia. Nature, 413: 413-417. doi: 10.1038/35096551

Zhu, R. X., Potts, R., Xie F., et al., 2004. New evidence onthe earliest human presence at high northernlatitudes innortheast Asian. Nature, 431: 559-562. doi: 10.1038/nature02829

迟振卿, 闵隆瑞, 朱关祥, 等, 2002. 泥河湾湖相沉积层记录的古气候周期性. 地学前缘, 9 (1): 182-186. doi: 10.3321/j.issn:1005-2321.2002.01.022

丁仲礼, 余志伟, 刘东生, 1991. 中国黄土研究新进展(三): 时间标尺. 第四纪研究, (4): 336-348.

刘泽纯, 陈晔, 袁林旺, 等, 2000. 应用自然伽玛测井曲线反演2.85 MaBP. 来的古气候变化. 中国科学(D辑), 30 (6): 509-618. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199802014.htm

闵隆瑞, 迟振卿, 朱关祥, 2000. 从井儿洼孔岩心看阳原盆地第四纪湖相层的划分. 地质学报, 74 (2): 108-115. doi: 10.3321/j.issn:0001-5717.2000.02.002

熊尚发, 丁仲礼, 刘东生, 1999. 北京邻区1.2 Ma以来黄土沉积及其对东部沙漠扩张的指示. 海洋地质与第四纪地质, 19 (3): 68-73. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ903.010.htm

杨晓强, 李华梅, 1999. 泥河湾盆地沉积物磁化率及粒度参数对沉积环境的响应. 沉积学报, 17 (增刊): 763-768. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB1999S1017.htm

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(6)

Get Citation

PDF

XML

Article views (3994) PDF downloads(15)

Orbitally Tuned Time Scale Based on Climate Proxy Indicator of Grain Size Distribution in Nihewan Basin

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content