XUE Ji-bin, ZHONG Wei, PENG Xiao-ying, ZHAO Yin-juan, ZHEN Zhi-guo, LIU Wei, ZHENG Yan-ming. PALEO-CLIMATE SIGNIFICANCE FOR THE PAST 12 kaBP REVEALED BY DAHU PEAT RECORD IN THE EASTERN SOUTH MOUNTAIN[J]. Marine Geology & Quaternary Geology, 2007, 27(5): 105-113.
Citation: XUE Ji-bin, ZHONG Wei, PENG Xiao-ying, ZHAO Yin-juan, ZHEN Zhi-guo, LIU Wei, ZHENG Yan-ming. PALEO-CLIMATE SIGNIFICANCE FOR THE PAST 12 kaBP REVEALED BY DAHU PEAT RECORD IN THE EASTERN SOUTH MOUNTAIN[J]. Marine Geology & Quaternary Geology, 2007, 27(5): 105-113.
shu

PALEO-CLIMATE SIGNIFICANCE FOR THE PAST 12 kaBP REVEALED BY DAHU PEAT RECORD IN THE EASTERN SOUTH MOUNTAIN

  • School of Geography Science, South China Normal University, Guangzhou 510631, China

More Information
  • Received Date: May 13, 2007
  • Revised Date: September 21, 2007
    Graphical Abstract
    • Abstract
  • Based on the synthesis analysis of the multiply indexes from the Dahu peat sequence obtained from the eastern South Mountain and the reliable testing of the radiocarbon ages, the variations of the paleo-climate in the eastern South Mountain during the past 12 ka were reconstructed. The results indicate that during about the 12~9 kaBP, the precipitation increased and the monsoon got stronger in this study region, and after 9 kaBP or so the precipitation decreased and the monsoon became weak. The results show that the general trend of the paleo-climate changes in the eastern South Mountain seems to follow the summer solar radiation variations at 33°N, which indicates to a certain extent that the climate responds to the variations of the solar radiation. The multiply indexes mainly reflect the variations of the climatic changes in the low-latitude regions while they also recorded some information from the high-latitude regions, which shows regional climatic characteristics as well as coherences to the global climatic variations.
    • FullText(HTML)
    • References (41)
  • [1]
    洪业汤,姜洪波,洪冰,等. 近5000年的气候波动与太阳变化[J]. 中国科学D辑, 1998, 28(6):491-497.

    [HONG Ye-tang, JIANG HONG-bo, HONG Bing, et al. Climate change and solar variability during the past 5000 years[J]. Science in China (Series D), 1998,28(6):491-497.]
    [2]
    洪业汤,刘东生,姜洪波,等. 太阳辐射驱动气候变化的泥炭氧同位素证据[J]. 中国科学D辑, 1999, 29(6):527-531.

    [HONG Ye-tang, LIU Tung-sheng, JIANG Hong-bo, et al. Evidence for solar forcing of climate variation from δ18O of peat cellulose[J]. Science in China (Series D), 1999, 29(6):527-531.]
    [3]
    Hong Y T, Hong B, Lin Q H, et al. Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene[J]. Earth and Planet Science Letters, 2003,211:371-380.
    [4]
    王华,洪业汤,朱咏煊,等. 红原泥炭腐殖化度记录的全新世气候变化[J]. 地质地球化学, 2003, 31(2):51-56.

    [WANG Hua, HONG Ye-tang, ZHU Yong-xuan, et al. The peat humification records of Holocene climate change in Hongyuan region[J]. Geology-Geochemistry, 2003, 31(2):51-56.]
    [5]
    王华,洪业汤,朱咏煊,等. 青藏高原泥炭腐殖化度的古气候意义[J]. 科学通报, 2004, 49(7):686-691.

    [WANG Hua, HONG Ye-tang, ZHU Yong-xuan, et al. The significance of the peat humification on paleoclimate in Tibetan Plateau[J]. Chinese Science Bulletin, 2004, 49(7):686-691.]
    [6]
    周卫建,卢雪峰,武振坤,等. 若尔盖高原全新世气候变化的泥炭记录与加速器放射性碳测年[J]. 科学通报, 2001, 46(12):1040-1044.

    [ZHOU Wei-jian, LU Xue-feng, WU Zhen-kun, et al. Peat record reflecting Holocene climate change in the Zoige Plateau and AMS radiocarbon dating[J]. Chinese Science Bulletin, 2002, 47(1):66-70.]
    [7]
    于学峰,周卫建,Lars G Franzen,等. 青藏高原东部全新世冬夏季风变化的高分辨率泥炭记录[J]. 中国科学D辑, 2006, 36(2):182-187.

    [YU Xue-feng, ZHOU Wei-jian, Franzen Lars G,et al. High resolution peat records for Holocene monsoon history in the eastern Tibetan Plateau[J]. Science in China (Series D), 2006, 49(6):615-621.]
    [8]
    何报寅,张穗,蔡述明. 近2600年神农架大九湖泥炭的气候变化记录[J]. 海洋地质与第四纪地质, 2003, 23(2):109-115.

    [HE Bao-yin, ZHANG Sui, CAI Shu-ming. Climatic changes records in peat from the Dajiu Lake Basin in Shennongjia since the last 2600 years[J]. Marine Geology and Quaternary Geology, 2003, 23(2):109-115.]
    [9]
    萧家仪,王建,安芷生,等. 南岭东部新仙女木事件的孢粉学证据[J]. 植物学报, 1998, 40(11):1079-1082.

    [XIAO Jia-yi, WANG Jian, AN Zhi-sheng,et al. Evidence for the Younger Dryas Event in the eastern part of Nanling region[J].Acta Phytologica Sinica,1998, 40(11):1079-1082.]
    [10]
    ZHOU Wei-jian, YU Xue-feng, Timothy A J,et al. High-resolution evidence from southern China of an early Holocene optimum and a mid-Holocene dry event during the past 18000 years[J]. Quaternary Research, 2004, 62:39-48.
    [11]
    ZHOU Wei-jian, XIE Shu-cheng, Meyers, Philip A,et al. Reconstruction of late glacial and Holocene climate evolution in southern China from geolipids and pollen in the Dingnan peat sequence[J]. Organic Geochemistry, 2005, 36:1272-1284.
    [12]
    Raphael A J. Late Pleistocene and Holocene development of the interior peat-accumulating basin of tropical Tasek Bera,Peninsular Malaysia[J]. Palaeogeography, Palaeoclimatology, Paleoecology, 2004, 211:241-270.
    [13]
    Taylor D. Late Quaternary peat formation and vegetation dynamics in a lowland tropic swamp, NeeSoon, Singapore[J]. Palaeogeography, Palaeoclimatology, Paleoecology, 2001, 171:269-287.
    [14]
    洪冰,林庆华,洪业汤. 全新世亚洲季风、ENSO及高北纬气候间的关联[J]. 科学通报, 2006, 51(17):1977-1984.

    [HONG Bing, LIN Qing-hua, HONG Ye-tang. Interconnections between the Asian monsoon, ENSO, and high northern latitude climate during the Holocene[J]. Chinese Science Bulletin, 2006, 51(18):2169-2177.]
    [15]
    Stuiver M, Reimer P J. Extended 14C Database and Revised 3.014C Calibration Program[J]. Radiocarbon, 1993, 35(1):215-230.
    [16]
    柴岫. 泥炭地学[M]. 北京:地质出版社,1990:32-42.[CHAI Xiu. Peatland[M]. Beijing:Geological Publishing House, 1990:32

    -42.]
    [17]
    马学慧,夏玉梅,王瑞山. 我国泥炭形成时期的探讨[J]. 地理研究, 1987, 6(1):31-42.

    [MA Xue-hui, XIA Yu-mei, WANG Rui-shan. A study of the peat-forming periods in China[J]. Geographical Research, 1987, 6(1):31-42.]
    [18]
    于学峰,周卫建. 全新世泥炭古气候记录研究进展[J]. 海洋地质与第四纪地质, 2004, 24(4):121-126.

    [YU Xue-feng, ZHOU Wei-jian. Advances of paleoclimatic researches of Holocene peat bogs[J]. Marine Geology and Quaternary Geology, 2004, 24(4):121-126.]
    [19]
    陈发虎,朱艳,李吉均,等. 民勤盆地湖泊沉积记录的全新世千百年尺度夏季风快速变化[J]. 科学通报, 2001, 46(17):1414-1419.

    [CHEN Fa-hu, ZHU Yan, LI Ji-jun, et al. Abrupt Holocene changes of the Asian monsoon at millennial-and centennial-scales:Evidence from lake sediment document in Minqin Basin, NW China[J]. Chinese Science Bulletin, 2001, 46(23):1942-1947.]
    [20]
    温孝胜,彭子成,赵焕庭. 中国全新世气候演变研究的进展[J]. 地球科学进展, 1999, 14(3):292-298.

    [WEN Xiao-sheng, PENG Zi-cheng, ZHAO Huan-ting. Advance in study on the Holocene climate evolution in China[J]. Advance in Earth Sciences, 1999, 14(3):292-298.]
    [21]
    Fairbanks R G. The age and origin of the "Younger Dryas climate event" in Greenland ice cores[J]. Paleoceanography, 1990, 5(6):937-948.
    [22]
    汪品先,卞云华,李保华,等. 西太平洋边缘海的"新仙女木"事件[J]. 中国科学D辑, 1996, 26(5):452-460.

    [WANG Pin-xian, BIAN Yun-hua, LI Bao-hua, et al. The "Younger Dryas climate event" in the west Pacific margin[J]. Science in China (Series D), 1996, 26(5):452-460.]
    [23] 施雅风,孔昭宸,王苏民,等. 中国全新世大暖期的气候波动与重要事件[J]. 中国科学(B辑), 1992, 22(12):1300-1308.[SHI Ya-feng, KONG Zhao-chen, WANG Su-min, et al. Climate variations and important events during the Holocene Epoch in China[J]. Science in China (Series B), 1992, 22(12):1300-1308.]
    [24]
    沈吉,杨丽原,羊向东,等. 全新世以来云南洱海流域气候变化与人类活动的湖泊沉积记录[J]. 中国科学D辑, 2004, 34(2):130-138.

    [SHEN Ji, YANG Li-yuan, YANG Xiang-dong, et al. Climate changes and human activities recorded by the lake sediment from Erhai lake, Yunnan Province during the Holocene[J]. Science in China (Series D), 2004, 34(2):130-138.]
    [25]
    邵晓华,汪永进,程海,等. 全新世季风气候演化与干旱事件的湖北神农架石笋记录[J]. 科学通报, 2006, 51(1):80-86.

    [SHAO Xiao-hua, WANG Yong-Jin,CHENG Hai, et al. Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in central China[J]. Chinese Science Bulletin, 2006, 51(2):221-228.]
    [26]
    Wang Y J, Cheng H, Edwards R L, et al. A high resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China[J]. Science, 2001, 294:2345-2348.
    [27]
    蔡演军,彭子成,安芷生,等. 贵州七星洞全新世石笋的氧同位素记录及其指示的季风气候变化[J]. 科学通报, 2001, 46(16):1398-1402.

    [CAI Yan-jun, PENG Zi-cheng, AN Zhi-sheng, et al. The δ18O variation of a stalagmite from Qixing Cave, Guizhou Province and indicated climate change during the Holocene[J]. Chinese Science Bulletin, 2001, 46(22):1904-1908.]
    [28]
    Tan M, Liu D S, Hou J, et al. Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature[J]. Geophysical Research Letters, 2003, 30(12):1617-1621.
    [29]
    钟巍,王立国,塔西甫拉提·特依甫,等. 太阳活动对塔里木盆地南缘近4 ka以来气候波动的可能影响[J]. 科学通报, 2004, 49(11):1079-1083.

    [ZHONG Wei, WANG Li-guo, Tyip Tashpolat, et al. Possible solar forcing of climate variability in the past 4000 years inferred from a proxy record at the southern margin of Tarim Basin[J].Chinese Science Bulletin,2004, 49(11):1079-1083.]
    [30]
    姚檀栋,Thompson L G, 施雅风,等. 古里雅冰芯中末次间冰期以来气候变化记录研究[J]. 中国科学D辑, 1997, 27(5):447-452.

    [YAO Tan-dong, Thompson L G, SHI Ya-feng, et al. Climate variation since the last interglacition recorded in the Guliya ice core[J]. Science in China (Series D), 1997, 27(15):447-452.]
    [31]
    姜修洋,汪永进,孔兴功,等. 神农架140~124 kaBP百年尺度东亚季风降水的石笋记录[J]. 海洋地质与第四纪地质, 2006, 26(3):39-44.

    [JIANG Xiu-yang, WANG Yong-jin, KONG Xing-gong, et al. Centennial-scale east Asian monsoon precipitation record over 140~124 kaBP from a stalagmite in Shennongjia[J]. Marine Geology and Quaternary Geology, 2006, 26(3):39-44.]
    [32]
    姜修洋,汪永进,孔兴功,等. 130 kaBP左右东亚季风突变过程的洞穴石笋记录[J]. 科学通报, 2005, 50(23):2644-2648.

    [JIANG Xiu-yang, WANG Yong-jin, KONG Xing-gong, et al. Abrupt climate change of East Asian monsoon at 130 kaBP inferred from a high resolution stalagmiteδ18O record[J]. Chinese Science Bulletin, 2005, 50(23):2765-2769.]
    [33]
    Schulza M, Mudelsee M. REDFIT:estimating red-noise spectra directly from unevenly spaced paleoclimatic time series[J]. Computers & Geosciences, 2002, 28:421-426.
    [34]
    汪品先. 低纬过程的轨道驱动[J]. 第四纪研究, 2006, 26(5):694-701.

    [WANG Pin-xian. Orbital forcing of the low-latitude processes[J]. Quaternary Sciences, 2006, 26(5):694-701.]
    [35]
    刘嘉麒,吕厚远,Negendank J,等. 湖光岩玛珥湖全新世气候波动的周期性[J]. 科学通报, 2000, 45(11):1190-1195.

    [LIU Jia-qi, LÜ Hou-yuan, Negendank J, et al. Periodicity of Holocene climatic variations in the Huguangyan Maar Lake[J]. Chinese Science Bulletin, 2000, 45(18):1712-1717.]
    [36]
    Bond G, Kromer B, Beer J, et al. Persistent solar influence on North Atlantic climate during the Holocene[J]. Science, 2001, 294:2130-2136.
    [37]
    Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in north Atlantic Holocene and glacial climates[J]. Science, 1997, 278:1257-1266.
    [38]
    Fleitmann D, Burns S J, Mudelsee M, et al. Holocene forcing of the Indian Monsoon recorded in a stalagmite from Southern Oman[J]. Science,2003,300:1737-1739.
    [39]
    于革,刘健. 全球12000 aBP以来火山爆发记录及对气候变化影响的评估[J]. 湖泊科学, 2003, 15(1):11-20.

    [YU Ge, LIU Jian. Geological records of volcanic explosions during the last 12000 years and the volcanic impacts on climate changes[J]. Journal of Lake Sciences, 2003, 15(1):11-20.]
    [40]
    王绍武. 2200-2000BC的气候突变与古文明的衰落[J]. 自然科学进展, 2005, 15(9):1094-1099.

    [WANG Shao-wu. Abrupt climate change and collapse of ancient civilizations at 2200-2000BC[J]. Progress in Natural Science, 2005, 15(9):1094-1099.]
    [41]
    An Z S, Porter S C, Kutzbach J E, et al. Asynchronous Holocene optimum of the East Asian Monsoon[J]. Quaternary Science Review, 2000, 19:743-762.
    • Related Articles

Catalog

    Get Citation
    PDF
    XML
    Article views (1494) PDF downloads (16) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return