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Asynchronous Holocene climatic change across China

Published online by Cambridge University Press:  20 January 2017

Y. He ,
Wilfred H. Theakstone ,
Zhang Zhonglin ,
Zhang Dian ,
Yao Tandong ,
Chen Tuo ,
Shen Yongping  and
Pang Hongxi
Y. He*
Affiliation:
Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 73000, China
Wilfred H. Theakstone
Affiliation:
Department of Geography, University of Manchester, Manchester M13 9PL, UK
Zhang Zhonglin
Affiliation:
Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 73000, China
Zhang Dian
Affiliation:
Department of Geography, Hong Kong University, Hong Kong, China
Yao Tandong
Affiliation:
Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 73000, China
Chen Tuo
Affiliation:
Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 73000, China
Shen Yongping
Affiliation:
Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 73000, China
Pang Hongxi
Affiliation:
Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 73000, China
*
*Corresponding author. Fax: +86-931-8276345.E-mail address:yqhe@ns.lzb.ac.cn (Y. He).
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Abstract

A review of Holocene climatic variations in different parts of China shows that they were asynchronous. Proxy data from ice cores, pollen, loess, lacustrine sediments, and changes of sea and lake levels demonstrate that many warm and cold oscillations have occurred in China during the Holocene, including a most important climatic event known as the “Holocene optimum,” a milder and wetter period, and that the duration and amplitude of the optimum period, as well as its start and end times, differed in different parts of China. Uplift of the Tibetan plateau over the past millions of years led to the development of the monsoon climate and to complex atmospheric circulation over continental China during the Holocene. As a result, the Holocene optimum began and terminated earlier in high-altitude regions of western China than at lower elevations in eastern China, and the amplitude of the variations was lower in the east. This suggests that the western higher-altitude areas were more sensitive to climatic change than were the eastern lower-altitude areas. Holocene climatic records in the Dunde and Guliya ice cores do not correspond. Inverse δ18O variations between the two cores indicate that the effects of climate and atmospheric processes on the stable isotopes at the two sites differed. The correlation between the isotopic composition of carbonates in lake deposits in western China and climatic variations is similar to that in the ice cores. The climatic resolution in ice cores and lake sediments is higher than that in other media. The lack of precise correspondence of climatic records constructed on the basis of proxy data from different parts of China is a result of the different locations and elevations of the sampling sites, the different resolutions of the source material, and the varied climatic conditions within China. Further work is needed to confirm both the conclusions and the inferences presented here.

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Type
Research Article
Information
Quaternary Research , Volume 61 , Issue 1 , January 2004 , pp. 52 - 63
Copyright
University of Washington

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References

Ammann, B., Birks, H.J.B., Birks, , Brooks, S.J., Eicher, U., Grafenstein, U., Hofmann, W., Lemdahl, G., Schwander, J., Tobolski, K., Wick, L., (2000). Quantification of biotic responses to rapid climatic changes around the Younger Dryas—A synthesis. Paleogeography, Paleoclimatology, Paleoecology. 159, 313–347.CrossRefGoogle Scholar
An, Z., (2000). The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews. 19, 171–187.CrossRefGoogle Scholar
An, Z., Wu, X., Lu, Y., Zhang, D., Sun, X., Dong, G., (1990). A preliminary study on the paleoenvironment change of China during the past 20,000 years. Liu, D., Loess, Quaternary Geology, Global Change. Science Press, Beijing., 1–26., In Chinese.Google Scholar
An, Z., Kutzbach, J.E., Warren, L.P., Porter, S.C., (2001). Evolution of Asian monsoon and phased uplift of the Himalaya–Tibetan plateau since late Miocene times. Nature. 411, 62–66.Google Scholar
Andrews, J.T., Mode, W.N., Davis, P.T., (1980). Holocene climate based on pollen transfer functions, eastern Canadian arctic. Arctic and Alpine Research. 12, 41–64.CrossRefGoogle Scholar
Bartlein, P.J., Webb, T., Fleri, E., (1984). Holocene climatic changes in the northern Mideast: pollen-derived estimates. Quaternary Research. 22, 361–374.Google Scholar
Chen, F., Zhang, W., (1993). Loess Stratigraphy and Quaternary Glacial Problems in Gansu and Qinghai Provinces. Science Press, Beijing., 159In Chinese with English abstract.Google Scholar
Chen, C., Lu, Y., Shen, C., (1977). Evolution of the natural environment in southern Liaoning province since 10 ka. Science in China. 6, 603–614., (In Chinese with English abstract).Google Scholar
Chen, F., Bloemendal, J., Wang, J.M., Li, J., Oldfield, F., (1997). High-resolution multi-proxy climate records from Chinese loess: Evidence for rapid climatic changes over the last 75 kyr B.P. Paleogeography, Paleoclimatology, Paleoecology. 130, 323–335.Google Scholar
Colinvaux, P.A., De Oliveira, P.E., Moreno, J.E., (1996). A long pollen record from lowland Amazon: forest and cooling in glacial times. Science. 274, 85–88.CrossRefGoogle Scholar
Cui, H., Kong, Z., (1992). Preliminary analysis of climatic change in the central part of Inner Mongolia during the Holocene optimum. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 72–79., In Chinese with English abstract.Google Scholar
Dansgaard, W., (1964). Stable isotope in precipitation. Tellus. 14, 4 436–468.Google Scholar
Davis, M.B., Botkin, D.B., (1985). Sensitivity of cool-temperature forestes and their fossil pollen record to rapid temperature change. Quaternary Research. 23, 327–340.Google Scholar
Fang, G., Li, P., Huang, G., (1992). Sea level changes of Holocene along the coast in Guangdong and Guangxi, China. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 131–137., In Chinese with English abstract.Google Scholar
Flohn, H., (1981). The elevated heat sources of the Tibetan highlands and its role for the large scale atmospheric circulation. Geological and Ecological Studies of the Qinghai–Xizang Plateau 2. Science Press, Beijing., 1463–1469.Google Scholar
Fontes, J.C., Gasse, F., Gibert, E., (1996). Holocene environmental changes in Bangong Co basin (western Tibet). 1. Chronology and stable isotopes of carbonates of a Holocene lacustrine core. Paleogeography, Paleoclimatology, Paleoecology. 120, 25–47.Google Scholar
Gasse, F., Fontes, J.C., Van Campo, E., Wei, K., (1996). Holocene environmental changes in Bangong Co basin (western Tibet). 4. Discussion and conclusions. Paleogeography, Paleoclimatology, Paleoecology. 120, 79–92.Google Scholar
Han, Y., Meng, G., (1987). On the sea level changes along the eastern coast of China during 12,000 years. Qin, Y., Zhoo, S., Late Quaternary Sea-Level Changes. Ocean Press, Beijing., 119–136., In Chinese with English abstract.Google Scholar
Han, Y., Meng, G., Wang, S., Zhuang, Z., Xu, W., Xu, , (1992). The megathermal and high sea level of mid-Holocene along the coast in northern part of China. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 121–130., In Chinese with English abstract.Google Scholar
He, Y., Theakstone, W.H., Yao, T., Zhang, D., Yang, M., (2002). The irregular pattern of isotopic and ionic signals in a typical monsoon temperate–glacier area, Mt. Yulong, China. Annals of Glaciology. 35, 167–174.Google Scholar
He, Y., Zhang, Z., Theakstone, W.H., Chen, T., Yao, T., Pang, H., (2003). Changing features of the climate and glaciers in China's monsoonal temperate–glacier region. Journal of Geophysical Research(In press).Google Scholar
Heusser, C.G., Streeter, S.S., (1980). A temperature and precipitation record of the past 16,000 years in southern Chile. Science. 210, 1345–1347.CrossRefGoogle Scholar
Kang, X., Xie, Y., (1989). The character of the weather and climate in west Kunlun mountainous area in summer 1987. Bulletin of Glacier Research. 7, 77–82.Google Scholar
Kong, Z., Du, N., Zhang, Z., (1982). Development of the plant community and climatic change in Beijing region since 10 ka. Acta Botanica Sinica. 24, 2 172–181., (In Chinese with English abstract).Google Scholar
Kong, Z., Du, N., Shan, F., (1990). Vegetation evolution and the climatic analysis in Qinghai Lake during the Holocene—analytical micro-values of pollen in the QH85-14C core. Oceanic Geology and Quaternary Geology. 10, 3 79–96., (In Chinese with English abstract).Google Scholar
Kukla, G., Heller, F., Liu, X., Xu, T., Liu, T., An, Z., (1988). Pleistocene climates in China dated by magnetic susceptibility. Geology. 16, 811–814.Google Scholar
Kutzbach, J.E., Liu, Z., (1997). Response of the African monsoon to orbital forcing and ocean feedbacks in the middle Holocene. Science. 278, 440–443.CrossRefGoogle Scholar
Kutzbach, J.E., Guetter, P.J., (2002). The influence of changing orbital parameters and surface boundary conditions on climate simulations for the past 18,000 years. Journal of the Atmospheric Sciences. 43, 16 1726–1759.Google Scholar
Li, W., Liang, Y., (1985). Vegetation and environment in eastern Hebei province during the Holocene Megathermal. Acta Botanica Sinica. 27, 6 640–651., (In Chinese with English abstract).Google Scholar
Liu, D., (1985). Loess and Environment. Science Press, Beijing., In Chinese with English abstract.Google Scholar
Liu, J., (1989). Vegetational and climatic changes at Gushanntun bog in Jilin, NE China since 13,000 y. BP. Acta Palaeontologica Sinica. 28, 4 495–511., (In Chinese with English abstract).Google Scholar
Liu, X., Shaw, J., Liu, T., Heller, F., Yuan, B., (1992). Magnetic mineralology of Chinese loess and its significance. Geophysics Journal International. 108, 301–308.Google Scholar
Liu, X., An, Z., Wu, X., (1997). East Asian paleoclimates of the last glacial maximum in an atmospheric general circulation model and from geological records. Proceeding of the 3rd International Geology Conference. vol. 21, 156–171.Google Scholar
Liu, K., Yao, Z., Thompson, L.G., (1998). A pollen record of Holocene climatic changes from the Dunde ice cap, Qinghai–Tibetan Plateau. Geology. 26, 2 135–138.2.3.CO;2>CrossRefGoogle Scholar
Lu, H., An, Z., (1998). Paleoclimatic significance of loess's grain sizes in loess plateau. Science in China (D). 28, 3 278–283., (In Chinese with English abstract).Google Scholar
Maher, B.A., Thompson, R., (1991). Mineral magnetic record of the Chinese loess and paleosols. Geology. 19, 3–6.Google Scholar
Maher, B.A., Thompson, R., (1992). Paleoclimatic significance of the mineral magnetic record of the Chinese loess and paleosols. Quaternary Research. 37, 155–170.CrossRefGoogle Scholar
Shen, C., Tang, L., (1992). The Holocene climate in the regions of Mts. Changbai and Little Xinganling – a preliminary study on pollen/climate transfer function. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 33–39., In Chinese with English abstract.Google Scholar
Shi, Y., Kong, Z., Wang, S., Tang, L., Wang, F., Yao, T., Zhao, X., Zhang, P., Shi, S., (1993). Mid-Holocene climates and environments in China. Global and Planetary Change. 7, 219–233.Google Scholar
Shi, Y., Kong, Z., Wang, S., Tang, L., Wang, F., Yao, T., Zhao, X., Zhang, P., Shi, S., (1994). The climatic fluctuations and important events of Holocene Megathermal in China. Science in China. 37, 3 289–301.Google Scholar
Song, C., Sun, X., (1997). Establishment of transfer functions of the pollen—climatic factors in northern China and the quantitative climatic reconstruction at DJ core. Acta Botanica Sinica. 39, 6 554–560., (In Chinese with English abstract).Google Scholar
Stuijts, I., Newsome, J.C., Flenley, J.R., (1988). Evidence for the late Quaternary vegetational change in the Sumatran and Javan highlands. Review of Paleobotany and Palynology. 55, 207–216.Google Scholar
Sun, J., Zhao, J., (1991). Quaternary Environment in the Loess Plateau. Science Press, Beijing., 1–240., In Chinese with English abstract.Google Scholar
Tang, L., Shen, C., (1992). The vegetation and climate in northern Jiangsu province during the Holocene Megathermal. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 80–93., In Chinese with English abstract.Google Scholar
Tang, L., Li, C., (2001). Temporal–spatial distribution of the Holocene vegetation in the Tibetan plateau. Journal of Glaciology and Geocryology. 23, 4 367–374., (In Chinese with English abstract).Google Scholar
Thompson, L.G., Thompson, E.M., Davis, M.E., (1989). Holocene-late Pleistocene climatic ice core records from Qinghai–Tibetan plateau. Science. 246, 474–477.CrossRefGoogle ScholarPubMed
Thompson, L.G., Thompson, E.M., Davis, M.E., (1990). Glacial stage ice-core records from the subtropical Dunde ice cap, China. Annals of Glaciology. 14, 288–297.CrossRefGoogle Scholar
Thompson, L.G., Thompson, M.E., Davis, M., Lin, P.N., Yao, T., Dyurgerov, M., Dai, J., (1993). “Recent warming,” ice core evidence from tropical ice cores with emphasis on central Asia. Global and Planetary Change. 7, 145–156.CrossRefGoogle Scholar
Thompson, L.G., Yao, T., Davis, M.E., (1997). Tropical climatic instability: the Last Glacial Cycle from a Qinghai-Tibetan ice core. Science. 276, 1821–1825.Google Scholar
Tian, L., Masson-Delmotte, V., Stievenard, M., Yao, T., Jouzel, J., (2001). Tibetan plateau summer monsoon northward extent revealed by measurements of water stable isotopes. Journal of Geophysical Research. 106, D22 28081–28088.CrossRefGoogle Scholar
Tinner, W., Lotter, A.F., (2001). Central European vegetation response to abrupt climate change at 8.2 ka. Geology. 29, 551–554.2.0.CO;2>CrossRefGoogle Scholar
Van Campo, E., Gasse, F., (1993). Pollen and diatom-inferred hydrological and climatic changes in Sumxi–Longmu basin (western Tibet) from 13,000 yr BP. Quaternary Research. 39, 300–313.Google Scholar
Van Campo, E., Cour, P., Huang, S., (1996). Holocene environmental changes in Bangong Co basin (Western Tibet). 2. The pollen record. Palaeogeography, Palaeoclimatology, Palaeoecology. 120, 49–63.Google Scholar
Wang, S., (1990). Environment evolution and paleoclimate of Daihai lake, inner Mongolia since the Last Glaciation. Quaternary Sciences. 3, 223–232., (In Chinese with English abstract).Google Scholar
Wang, S., Feng, M., (1991). The relation between the environmental change at Lake Daihai in Inner Mongolia and the strength of the southeastern monsoon. Science in China (B). 7, 759–768., (In Chinese with English abstract).Google Scholar
Wang, S., Wang, F., (1992). The liminogic record of Holocene climatic fluctuation. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 146–152., In Chinese with English abstract.Google Scholar
Wang, J., Lu, H., Shen, C., (1990). Factor interpretation method and quantitative analysis of climatic changes over the last 12,000 years in China. Lu, C., Global Changes and Environmental Evolution in China. Science Press, Beijing., 63–68., In Chinese with English abstract.Google Scholar
Wang, R.L., Scarpitta, S.C., Zhang, S.C., Zheng, M.P., (2002). Later Pleistocene/Holocene climate conditions of Qinghai–Xizang plateau (Tibet) based on carbon and oxygen stable isotopes of Zabuye lake sediments. Earth and Planetary Letters. 302, 461–477.Google Scholar
Webb, T., Bryson, R.A., (1972). Late and post-glacial climatic change in the northern Midwest, USA: quantitative estimates derived from fossil pollen spectra by multivariate statistical analysis. Quaternary Research. 2, 70–115.Google Scholar
Wei, K., Gasse, F., (1999). Oxygen isotopes in lacustrine carbonates of west China revisited: implications for past glacial changes in summer monsoon circulation. Quaternary Science Reviews. 18, 1315–1334.Google Scholar
Wei, K., Lin, R., (1994a). The influence of the monsoon climate on the isotopic composition of precipitation in China. Geochimica. 23, 33–41., (In Chinese with English abstract).Google Scholar
Wei, K., Lin, R., (1994b). An enquiry into palaeoclimatic information from oxygen isotopic profile of Dunde ice core in Qilianshan. Geochimica. 23, 311–320., (In Chinese with English abstract).Google Scholar
Williams, J.W., Post, D.M., Cwynar, L.C., Lotter, A.F., Levesque, A.J., (2002). Rapid and widespread vegetation responses to past climate change in the North Atlantic Region. Geology. 29, 551–554.Google Scholar
Yang, H., Chen, X., (1985). Sea-level change, transgression range and coastal evolution in eastern China during the Quaternary. Oceanic Geology and Quaternary Geology. 5, 4 59–80., (In Chinese with English abstract).Google Scholar
Yao, T., Thompson, L.G., (1992a). Trends and features of climatic changes in the past 5000 years recorded by the Dunde ice core. Annals of Glaciology. 16, 21–24.Google Scholar
Yao, T., Thompson, L.G., (1992b). Climatic records in Dunde ice core and the temperature changes since 5 ka. Science in China (B). 22, 10 1089–1093.Google Scholar
Yao, T., Shi, Y., Thompson, L.G., (1992). The Holocene climatic changes in Mt. Qilian as recorded in Dunde ice core. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 206–211., In Chinese with English abstract.Google Scholar
Yao, T., Jiao, K., Tian, L., (1995). Climatic and environmental records in Guliya ice cap. Science in China (B). 38, 2 228–237., (In Chinese with English abstract.Google Scholar
Yao, T., Liu, X., Wang, N., (2000). A study on the amplitude of climatic variation in Tibetan plateau. Chinese Science Bulletin. 45, 1 98–105.Google Scholar
Yie, D.Z., (1990). Study on Global Changes of China in Advance. Meteorological Press, Beijing., 252in Chinese with English abstract.Google Scholar
Zhang ggnn, J., (2001). High-Resolution Holocene Paleoenvironmental Reconstruction through Lake Sediments and Loess–Paleosol Sequences in Monsoonal Boundary area in Central China. Ph.D. thesis. The University of Lanzhou, . In Chinese with English abstract.Google Scholar
Zhang, Z., Wang, D., Ding, J., (1981). Environmental evolution in Beijing region since 13,000 years. Geological Science. 3, 259–268., (In Chinese with English abstract).Google Scholar
Zhao, X., Wang, S., (1992). Holocene sea level variation in China and the correlation between the changes of shoreline and climate. Shi, Y., Kong, Z., The Climate and Environment in China during the Holocene Megathermal. Ocean Press, Beijing., 111–120., In Chinese with English abstract.Google Scholar
Zhao, X., Lu, G., Wang, S., (1991). The changes of environment and sea level as reflected by the Holocene stratigraphy in Qingfeng profile in Jiangsu province. Science in China (B). 21, 9 992–999.Google Scholar
Zheng, S., Hou, F., Ni, B., (1983). Study on the hydrogen and oxygen stable isotopes in precipitation in China. Chinese Science Bulletin. 13, 39–41., (In Chinese).Google Scholar
Zhou, L., Oldfield, F., Wintle, A.G., Robinson, S.G., Wang, J., (1990). Partly pedogenic origion of magnetic variations in Chinese loess. Nature. 346, 737–739.Google Scholar
Zhu, K., (1972). A preliminary study of the climatic changes in China since recent 5000 years. Acta Archaeological Sinica. 1, 15–38., (In Chinese with English abstract).Google Scholar