THE ENVIRONMENTAL CHANGE RECORDED IN JIANGXIGOU LOESS SECTIONS IN QINGHAI LAKE REGION
-
摘要: 青海湖地区是全球变化研究的热点区域,对全球气候环境变化极其敏感。末次冰消期是青海湖地区风成沉积物发生广泛堆积的时期,也是青海湖地区气候环境发生重要变革时期。通过对青海湖江西沟JXG1和JXG2黄土剖面的研究,重建了末次冰消期以来的环境演变记录。结果指示:(1)13~11.5 kaBP,剖面主要发育砂质黄土,青海湖区总体环境从冷干向相对温暖湿润的凉干环境过渡;(2)11.5~5 kaBP左右,剖面主要发育古土壤层,特别是9~5 kaBP时期,水热组合匹配达到最佳,气候呈现暖湿状态;(3)5 kaBP以来,干湿冷暖交替,尘暴频繁,植被盖度降低,气候进入相对不稳定状态。江西沟黄土剖面记录与青海湖湖泊钻孔和黑马河黄土剖面记录的气候变化过程具有一致性,红度指标是记录环境演变的敏感指标。末次冰消期以来该区黄土沉积主要受控于北半球高纬度夏季太阳辐射驱动的冰量变化,西风带扮演了北大西洋和青藏高原东北部"冷空气传输机"的角色。Abstract: The Qinghai Lake area is a hot spot in global change studies, due to its sensitivity to global warming. During the last deglaciation, aeolian deposits were widely distributed in the region, with drastic environmental and climatic changes. In this paper, we studied two loess sections (JXG1 and JXG2) near the Jiangxigou town to the south of Qinghai Lake, upon which we reconstructed the regional environmental changes since the last deglaciation. The results show that:(1) During 13~11.5 kaBP, the paleolclimate was cold and dry there. Aeolian deposition prevailed and sandy loess formed. In general, the region was changing from a cold and dry to a cool and humid environment; (2) During 11.5~5 kaBP, pedogenesis was relatively strong. Maximum moisture levels occurred during the period of 9~5 kaBP, and in general, the paleoclimate was warm and wet; (3) After 5 kaBP, climate often alternated, dust storm occurred frequently, vegetation coverage decreased, and the climate entered a relatively unstable stage. The environmental changes of the Jiangxigou Loess section are comparable with those revealed by the boreholes in the Qinghai Lake and the Heimahe loess section. The redness of the Jiangxigou loess section is a sensitive index to environmental change. The loess deposition since the last deglaciation in Qinghai Lake area was mainly controlled by the ice volume of the northern hemisphere, which was driven by the summer solar irradiation at the high latitude. The Westerlies played the role as a cold-air conveyer between the North Atlantic and the northeastern Tibetan Plateau.
-
Key words:
- environment change /
- Jiangxigou loess sections /
- Qinghai Lake
-
-
[1] [2] 陈克造, Bowler J M, Kelts K. 四万年来青藏高原的气候变迁[J].第四纪研究,1990,10(1):21-32.
[CHEN Kezao, Bowler J M, Kelts K. Palaeoclimatic evolution within the Qinghai-Xizang (Tibet) Plateau in the last 40000 years.[J]. Quaternary Sciences, 1990, 10, (1):21-32.]
[3] Porter S C, Singhvi A, An Z S, et al. Luminescence age and palaeoenvironmental implication of a late Pleistocene ground wedge on the northeastern Tibetan Plateau[J]. Permafrost and Periglacial Processes, 2001, 12:203-210.
[4] Rhode D, Ma H Z, Madsen D B, et al. Paleoenvironmental and archaeological investigation at Qinghai Lake, western China:Geomorphic and chronometric evidence of lake level history[J]. Quaternary International, 2010, 218:29-44.
[5] Lu H Y, Zhao C F, Mason J, et al. Holocene climatic changes revealed by aeolian deposits from the Qinghai Lakearea (northeastern Qinghai-Tibetan Plateau) and possible forcing mechanisms[J]. Holocence, 2011, 21(2) 297-304.
[6] Liu X J, Lai Z P, Yu L P, et al. Luminescence chronology of aeolian deposits from the Qinghai Lake area in the Northeastern Qinghai-Tibetan Plateau and its palaeoenvironmental implications[J]. Quaternary Geochronology, 2012, 10:37-43.
[7] Ji J F, Shen J, William B, et al. Asian monsoon oscillations in the northeastern Qinghai-Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments[J].Earth and Planetary Science Letters, 2005,233:61-70.
[8] Shen J, Liu X Q, Wang S M, et al. Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years[J]. Quaternary International, 2005,163:131-140.
[9] An Z S, Colman S M, Zhou W J, et al. Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka[J]. Scientific Report, 2012, 2, 619, DOI:10.1038/srep00619.
[10] 赵存法, 鹿化煜, 周亚利,等. 青海湖地区冰消期以来气候变化的黄土记录[J]. 高校地质学报. 2009, 15(1):135-140.
[ZHAO Cunfa, LU Huayu, ZHOU Yali, et al. Palaeoclimate changes recorded by loess deposit around Qinghai Lake (Northeastern Qinghai-Tibetan Plateau) since last deglaciation[J]. Geological Journal of China Universities, 2009, 15:135-140.]
[11] 徐叔鹰. 青藏高原东北部的古土壤及其对环境变迁的反映. 地理科学. 1994, 14(3):225-232.
[XU Shuying. The paleosols and their reflection of the environmental change in the northeast region of the Qinghai-Xizang Plateau[J] Scientia Geographica Sinica, 1994, 14(3):225-232.]
[12] 陈发虎,汪世兰,张维信,等. 青海湖南岸全新世黄土剖面、气候信息及湖面升降探讨[J]. 地理科学, 1991,11(1):76-85.
[CHEN Fahu, WANG Shilan, ZHANG Weixin, et al. The loess profile at south bank, climatic information and lake-level fluctuations of Qinghai lake during the Holocene[J]. Scientia Geographica Sinica, 1991, 11:76-85.]
[13] Madsen D B, Ma H Z,Brantingham P J, et al. The late upper Paleolithic occupation of the northern Tibetan plateau margin[J]. Journal of Archaeological Science, 2006, 33, 1433-1444.
[14] Rhode D, Zhang H Y, Madsen D B, et al. Epipaleolithic/early Neolithic settlements at Qinghai Lake, western China[J]. Archaeological Science, 2007, 34:600-612
[15] 侯光良,魏海成,鄂崇毅,等. 青藏高原东北缘全新世人类活动与环境变化——以青海湖江西沟2号遗迹为例[J]. 地理学报, 2013, 68(3):380-388.
[HOU Guangliang,WEI Haicheng,E Cheongyi,et al. Human activities and environmental change in Holocene in the northeastern margin of Qinghai-Tibet Plateau:A case study of JXG2 relic site in Qinghai Lake[J]. Acta Geographica Sinica, 2013, 68(3):380-388.]
[16] 鹿化煜, 安芷生. 前处理方法对黄土古土壤粒度测量的影响[J].科学通报, 1997,42:2535-2538.[LU Huayu, AN Zhisheng. The influence of the pretreatment to grain-size analysis results of loess[J]. Chinese Science Bulletin, 1997
, 42:2535-2538.]
[17] 邓成龙, 刘青松, 潘永信, 等. 中国黄土环境磁学[J].第四纪研究, 2007, 27(2):193-209.
[DENG Chenglong, LIU Qingsong, PAN Yongxin,et al. Environmental magnetism of Chinese loess-paleosol sequences[J]. Quternary Science, 2007, 27(2):193-209.]
[18] 丁仲礼, 孙继敏, 刘东生. 联系沙漠-黄土演变过程中耦合关系的沉积学指标[J]. 中国科学D辑:地球科学,1999, 29(1):82-87.
[DING Zhongli, SUN Jimin, LIU Tongsheng. A sedimentological proxy indicator linking changes in loess and deserts in the Quaternary[J]. Science in China (Series D):Earth Sciences, 1999, 42(2):146-152.]
[19] 杨胜利, 方小敏,李吉均,等.表土颜色和气候定性至半定量关系研究[J].中国科学D辑:地球科学,2001,31(B12):175-181.
[YANG Shengli, FANG Xiaomin, LI Jijun, et al. Transformation functions of soil color and climate[J].Science in China Series D:Earth Sciences, 2001, 44,218-226.]
[20] Buylaert J P, Murray A S, Vandenberghe D, et al. Optical dating of Chinese loess using sand-sized quartz:Establishing a time frame for Late Pleistocene climate changes in the western part of the Chinese Loess Plateau[J]. Quaternary Geochronology, 2008, 3, 1:99-113.
[21] Laskar J, Robutel P, Joutel F, et al. A long-term numerical solution for the insolation quantities of the Earth[J]. Astronomy and Astrophysics, 2004, 428(1):261-285, doi:10.1051/0004-6361:20041335.
-
计量
- 文章访问数: 1252
- PDF下载数: 3
- 施引文献: 0