Access the full text.
Sign up today, get DeepDyve free for 14 days.
L. Labeyrie, W. Berger (1987)
Abrupt climatic change - Evidence and implications
Xiaohong Liu, D. Qin, X. Shao, Tuo Chen, Jiawen Ren (2005)
Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millenniumScience in China Series D: Earth Sciences, 48
Hai Xu, Yetang Hong, Q. Lin, B. Hong, Hongbo Jiang, Yongxuan Zhu (2002)
Temperature variations in the past 6000 years inferred from δ18O of peat cellulose from Hongyuan, ChinaChinese Science Bulletin, 47
Qin Yunshan, Li Fan, Xu Shanmin, J. Milliman, R. Limeburner (1988)
Study on suspended matter in seawater in the Southern Yellow SeaChinese Journal of Oceanology and Limnology, 6
R. Souchez (1993)
Climate instability during the last interglacial period recorded in the GRIP ice coreNature, 364
Tandong Yao, L. Thompson, Q. Dahe, Tian Lide, Ke-qin Jiao, Zhihong Yang, Xie Chao (1996)
Variations in temperature and precipitation in the past 2000 a on the Xizang (Tibet) Plateau——Guliya ice core recordScience China-earth Sciences, 39
J. Stuut, M. Prins, R. Schneider, G. Weltje, J. Jansen, G. Postma (2002)
A 300-kyr record of aridity and wind strength in southwestern Africa: inferences from grain-size distributions of sediments on Walvis Ridge, SE AtlanticMarine Geology, 180
D. DeMaster, B. McKee, C. Nittrouer, Q. Jiangchu, C. Guodong (1985)
Rates of sediment accumulation and particle reworking based on radiochemical measurements from continental shelf deposits in the East China SeaContinental Shelf Research, 4
M. Tan, Tung-sheng Liu, J. Hou, X. Qin, Hucai Zhang, Tieying Li (2003)
Cyclic rapid warming on centennial‐scale revealed by a 2650‐year stalagmite record of warm season temperatureGeophysical Research Letters, 30
Donghuai Sun, J. Bloemendal, D. Rea, J. Vandenberghe, F. Jiang, Z. An, R. Su (2002)
Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments, and numerical partitioning of the sedimentary componentsSedimentary Geology, 152
P. Grootes, M. Stuiver, J. White, S. Johnsen, S. Johnsen, J. Jouzel (1993)
Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice coresNature, 366
Yang Bao (2003)
CLIMATE HISTORY OF THE TIBETAN PLATEAU DURING THE LAST TWO MILLENNIAAdvance in Earth Sciences
K. Laird, S. Fritz, K. Maasch, B. Cumming (1996)
Greater drought intensity and frequency before AD 1200 in the Northern Great Plains, USANature, 384
J. Milliman, R. Beardsley, Yang Zuo-sheng, R. Limeburner (1985)
Modern Huanghe-derived muds on the outer shelf of the East China Sea: identification and potential transport mechanismsContinental Shelf Research, 4
Pleistocene Sediment, S. Boulay, C. Colin, A. Trentesaux, F. Pluquet, J. Bertaux, D. Blamart, C. Buehring, Pinxian Wang (2002)
MINERALOGY AND SEDIMENTOLOGY OF PLEISTOCENE SEDIMENT IN THE SOUTH CHINA SEA (ODP SITE 1144)
Zhibang Ma, Hongchun Li, M. Xia, T. Ku, Zi-cheng Peng, Yu-Song Chen, Zhaofeng Zhang (2003)
Paleotemperature changes over the past 3000 years in eastern Beijing, China: A reconstraction based on Mg/Sr records in a stalagmiteChinese Science Bulletin, 48
X. Tu, F. Zheng, Jiliang Wang, H. Cai, Pinxian Wang, C. Bühring, M. Sarnthein (2001)
An abrupt cooling event early in the last interglacial in the northern South China SeaScience in China Series D: Earth Sciences, 44
Dr. Jäger (2023)
Editor-in-ChiefAdvances in Ophthalmology and Optometry
X. Shao, H. Lei, Hongbin Liu, E. Liang, Fang Xiu-qi, W. Lili (2005)
Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, QinghaiScience China-earth Sciences, 48
Xingcheng Kang, L. Graumlich, P. Sheppard (1997)
A 1 835 A TREE-RING CHRONOLOGY AND ITS PRELIMINARY ANALYSES IN DULAN REGION, QINGHAIChinese Science Bulletin, 42
Youbin Sun, S. Gao, Jun Li (2003)
Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea settingChinese Science Bulletin, 48
Youbin Sun, Z. An (2002)
History and variability of Asian interior aridity recorded by eolian flux in the Chinese Loess Plateau during the past 7 MaScience in China Series D: Earth Sciences, 45
M. Prins, G. Postma, G. Weltje (2000)
Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Makran continental slopeMarine Geology, 169
M. Stuiver, P. Reimer, E. Bard, J. Beck, G. Burr, K. Hughen, B. Kromer, G. McCormac, J. Plicht, Marco Spurk (1998)
INTCAL98 Radiocarbon Age Calibration, 24,000–0 cal BPRadiocarbon, 40
S. Porter, Z. An (1995)
Correlation between climate events in the North Atlantic and China during the last glaciationNature, 375
M. Stuiver, P. Grootes, T. Braziunas (1995)
The GISP2 δ18O Climate Record of the Past 16,500 Years and the Role of the Sun, Ocean, and VolcanoesQuaternary Research, 44
Luejiang Wang, M. Sarnthein, H. Erlenkeuser, J. Grimalt, P. Grootes, S. Heilig, E. Ivanova, M. Kienast, C. Pelejero, U. Pflaumann (1999)
East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the south China SeaMarine Geology, 156
Environmentally sensitive grain-size component (ESGSC) extracted from grain-size data of a sediment core B2, which were retrieved from mud area southwest off Cheju Island (MACI), East China Sea (ECS), can be used to indicate the variations of East Asia Winter Monsoon (EAWM), with high (low) content/mean-size of ESGCS denote to strong (weak) EAWM. Combined with AMS 14 C datings core B2 provides a continuous high-resolution record of EAWM changes over the past 2300 years, with an average resolution of 13 years. The results show that the variations of EAWM are consistent with temperature changes inferred from historical documents in eastern China over the past 2300 years, from which four climate stages may be identified. In stages before 1900 aBP (50 AD) and 1450–780 aBP (50–1170 AD) the EAWM were comparatively weak, corresponding to warm climate periods in eastern China, respectively. And in stages of 1900–1450 aBP (50–500 AD) and 780–219 aBP (1170–1731 AD) the EAWM were strongly developed, which correspond well to climate changes of two cold periods in eastern China. It is also shown from this study that the stage at 780–219 aBP (1170–1731 AD) was the coldest climate period during the last 2300 years and could be, therefore, related to the Little Ice Age (LIA). Climatic fluctuations appeared obviously in all the four stages, and two climate events of abrupt changes from warm to cold occurred at around 1900 aBP (50 AD) and 780 aBP (1170 AD), of which the latter is probably related to globe-scale changes of atmospheric circulation at that time.
Science in China Series D: Earth Sciences – Springer Journals
Published: Jun 1, 2006
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.