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ZHANG Cheng jun, CHEN Fa hu, WANG Qi, SHI Qi, SUN Wei zhen. Unstability Record of Late Glacial Later Period in the Shiyang River Basin of Arid Northwestern China[J]. Acta Sedimentologica Sinica, 2000, 18(4): 646-650.
Citation: ZHANG Cheng jun, CHEN Fa hu, WANG Qi, SHI Qi, SUN Wei zhen. Unstability Record of Late Glacial Later Period in the Shiyang River Basin of Arid Northwestern China[J]. Acta Sedimentologica Sinica, 2000, 18(4): 646-650.

Unstability Record of Late Glacial Later Period in the Shiyang River Basin of Arid Northwestern China

  • Received Date: 2000-06-07
  • Publish Date: 2000-08-10
  • Carbon isotopic compositions of organic matters in the sediments during late Glacial Maximum and Late Glacial Period have been analyzed in arid semiarid areas of northwestern China. It shows that the sediment have recorded in detail the process of climatic oscillation that changed from dry and cool to warm and wet in thousand or hundred years scale during this period in the transition of monsoon edge belts. High resolution record of organic carbon isotopic compositions is the same as that of GRIP oxygen isotopic composition. It also indicates that there is a relative climatic changes between the globe and arid China. The climate was warm and wet in the transition period of late Glacial Maximum to Late Glacial, and terrestrial plants grew briskly. And the monsoon had taken an important action in the climatic oscillation in Shiyang river basin. The proxy of δ 13 C is the effective indicator of reconstructing the palaeoclimatic variation in the arid China because of its sensitivity to the climatic changes.
  • [1] Heinrich H. Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130000 years[J]. Quaternary Research, 1988,29:142 ~ 152
    [2] Bond G, Heinrich H, Broecker W, et al. Evidence for massive discharges of icebergs into the north Atlantic Ocean during the last glacial period[J]. Nature, 1992,360: 245~ 249
    [3] 张志强编译.地球气候将平衡于又一次跳跃[J].地球科学进展,1995,10(3):296~298
    [4] Grirnan E G, Jacobson G L, Watts W A, et al. A 50000 record of elimatic oscillations from Florida and its temporal correlation with the Heinrich events[J]. Science, 1993,261:198~200
    [5] Grafenstein U yon, Erlenkeuser H, Brauer A, et al. A mid - European decadal isotope-climate record from 15500 to 5000 years B. P. [J]. Science, 1999, 284:1 654~1 657
    [6] 杨志红,姚檀栋,黄翠兰等.古里雅冰芯中的新仙女木期事件记录[J].科学通报,1997,42(18):1975~1978
    [7] 安芷生,波特S C,夏佩尔J等.最近15万年洛川黄土堆积序列与格陵兰冰芯记录[J].科学通报,1994,39:2254~2256
    [8] Smith B N,Epstein S.Two categories of 13C/12C ratio for higher plants [J].Plant Physiology,1971,47:380~384
    [9] 张平中,王先彬,陈践发,王苏民.湖相有机质的氢指数及碳同位素组成——湖面波动评价的指标——以RH孔为例[J].科学通报,1995,40(18):1682~1685
    [10] 刘宝珺.沉积岩石学[M].北京:地质出版社,1980,307~315
    [11] An Z S, Porter S C, Zhou W J, et al. Episode of strengthened summer monsoon climate of younger dryas age on the loess plateau of central China[J]. Quaternary Research, 1993,39:4554
    [12] 周卫建,李小强,董光荣等.新仙女木期沙漠/黄土过渡带高分辨率泥炭记录——东亚季风气候颤动的实例[J].中国科学(D辑),1996,26(2):118~124
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  • Received:  2000-06-07
  • Published:  2000-08-10

Unstability Record of Late Glacial Later Period in the Shiyang River Basin of Arid Northwestern China

Abstract: Carbon isotopic compositions of organic matters in the sediments during late Glacial Maximum and Late Glacial Period have been analyzed in arid semiarid areas of northwestern China. It shows that the sediment have recorded in detail the process of climatic oscillation that changed from dry and cool to warm and wet in thousand or hundred years scale during this period in the transition of monsoon edge belts. High resolution record of organic carbon isotopic compositions is the same as that of GRIP oxygen isotopic composition. It also indicates that there is a relative climatic changes between the globe and arid China. The climate was warm and wet in the transition period of late Glacial Maximum to Late Glacial, and terrestrial plants grew briskly. And the monsoon had taken an important action in the climatic oscillation in Shiyang river basin. The proxy of δ 13 C is the effective indicator of reconstructing the palaeoclimatic variation in the arid China because of its sensitivity to the climatic changes.

ZHANG Cheng jun, CHEN Fa hu, WANG Qi, SHI Qi, SUN Wei zhen. Unstability Record of Late Glacial Later Period in the Shiyang River Basin of Arid Northwestern China[J]. Acta Sedimentologica Sinica, 2000, 18(4): 646-650.
Citation: ZHANG Cheng jun, CHEN Fa hu, WANG Qi, SHI Qi, SUN Wei zhen. Unstability Record of Late Glacial Later Period in the Shiyang River Basin of Arid Northwestern China[J]. Acta Sedimentologica Sinica, 2000, 18(4): 646-650.
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