• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    Volume 36 Issue 2
    Mar.  2011
    Turn off MathJax
    Article Contents
    Abstract
    References
    Article Navigation >  Earth Science  > 2011  >  36(2): 386-392
    QIN Xiao-guang, NING Bo, YIN Zhi-qiang, MU Yan, 2011. Evolution of Soil Organic Carbon Pool in Weinan Loess Region Since the Last Interglacial Period. Earth Science, 36(2): 386-392. doi: 10.3799/dqkx.2011.043
    Citation: QIN Xiao-guang, NING Bo, YIN Zhi-qiang, MU Yan, 2011. Evolution of Soil Organic Carbon Pool in Weinan Loess Region Since the Last Interglacial Period. Earth Science, 36(2): 386-392. doi: 10.3799/dqkx.2011.043
    shu

    Evolution of Soil Organic Carbon Pool in Weinan Loess Region Since the Last Interglacial Period

    doi: 10.3799/dqkx.2011.043
    • 1.

      Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

    • 2.

      National Library of China, Beijing 100081, China

    • 3.

      China Institute of Geo-Environment Monitoring, Beijing 100081, China

    • Received Date: 2010-09-11
      Available Online: 2021-11-10
    • Publish Date: 2011-03-01
      Abstract
    • Glacial-interglacial change in terrestrial carbon pools is an unknown issue in paleo-carbon cycle research. Carbon flux between carbon pools in different time scales has been studied from marine isotope, model simulating and paleo-environmental evidence by many scientists. Any tiny fluctuation of soil carbon pool with vast carbon reserves would affect ecosystem more easily than other terrestrial carbon pools and atmospheric CO2 concentration, and in turn impacted global climate finally. In this paper, the evolution of carbon density of soil organic matter (SOCD) in south of Chinese loess plateau over the past 40 ka was studied. It was found that SOCD in MIS-3 was more intensive than magnetic susceptibility in the details to explain tiny fluctuations. SOCD increased rapidly and fluctuated several times in high level in MIS-3. It may be because climate in this period was more suitable for soil organic carbon's accumulation and preservation in loess and paleosoil. In the last glacial maximum (LGM), SOCD decreased sharply as climate rapidly fluctuated. During the period, there was a climatic and SOCD rebounding event that lasted for about 2 ka and the minimum SOCD value occurred at ~14 ka BP and ~19 ka BP. Compared with the marine oxygen isotope, the trends of soil organic carbon pool in LGM and Holocene were similar. The magnetic susceptibility began to increase at 15 ka, and the increase seemed to be prior to SOCD and marine oxygen isotope. At the early time of Holocene, SOCD increased gradually and then decreased, and the maximum was at about 7-5 ka BP.

       

      • FullText(HTML)
      • References(46)
    • Batjes, N.H., 1996. Total carbon and nitrogen in the soils of the world. European Journal of Soil Science, 47: 151-163. doi: 10.1111/j.1365-2389.1996.tb01386.x
      Dean, W.E., 1999. The carbon cycle and biogeochemical dynamics in lake sediments. Journal of Paleolimnology, 21(4): 375-393. doi: 10.1023/A:1008066118210
      Ding, Z.L., Derbyshire, E., Yang, S.L., et al., 2002. Stacked 2.6 Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18O record. Paleoceanography, 17(3): 1033. doi: 10.1029/2001PA000725
      Fang, J.Y., Liu, G.H., Xu, S.L., 1996. Biomass and net production of forest vegetation in China. Acta Ecologica Sinica, 16(5): 497-508 (in China with English abstract). http://www.researchgate.net/publication/284688688_Biomass_and_net_production_of_forest_vegetation_in_China
      Feely, R.A., Sabine, C.L., Key, R.M., et al., 1999. CO2 survey synthesis results: estimating the anthropogenic carbon dioxide sink in the Pacific Ocean. U.S. JGOFS News, 9: 1-16.
      Guo, Z.T., Liu, D.S., An, Z.S., 1994. Paleosols of the last 0.15 Ma in the Weinan loess section and their paleoclimatic significance. Quaternary Sciences, (3): 256-269 (in China with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ199403006.htm
      Han, J.M., Jiang, W.Y., Liu, D.S., et al., 1996. The isotopic records in loess calcate of paleoclimate change. Science in China (Ser. D), 26: 399-404 (in Chinese).
      Hansen, J., Sato, M., Ruedy, R., et al., 2006. Global temperature change. Proceedings of the National Academy of Sciences of the United States of America, 103(39): 14288-14293. doi: 10.1073/pnas.0606291103
      Imbrie, J., Boyle, E.A., Clemens, S.C., et al., 1992. On the structure and origin of major glaciation cycles 1: linear responses to Milankovitch forcing. Paleoceanography, 7(6): 701-738. doi: 10.1029/92PA02253
      IPCC, 2001. Climate change 2001: the science of climate change. Cambridge University Press, Cambridge, UK.
      Jin, F., Yang, H., Cai, Z.C., et al., 2001. Calculation of density and reserve of organic carbon in soils. Acta Pedologica Sinica, 38(4): 522-528 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TRXB200104009.htm
      King, A.W., Emanuel, W.R., Wullschleger, S.D., et al., 1995. A search of the missing carbon sink: a model of terrestrial biospheric response to land-use change and atmospheric CO2. Tellus, 47(4): 501-519. doi: 10.1034/j.1600-0889.47.issue4.9.x
      Kukla, G., Heller, F., Liu, X.M., et al., 1988. Pleistocene climates in China dated by magnetic susceptibility. Geology, 16(9): 811-814. doi: 10.1130/0091-7613(1988)016<0811:PCICDB>2.3.CO;2
      Li, T.J., Zheng, Y.S., Wang, Y., 1983. Soil geography. Higher Education Press, Beijing, 59-95 (in Chinese).
      Liu, D.S., 1985. Loess and environment. Science Press, Beijing, 29-296 (in Chinese).
      Liu, J.Q., Chen, T.M., Nie, G.Z., et al., 1994. Datings and reconstruction of the high resolution time series in the Weinan loess section of the last 150 000 years. Quaternary Sciences, (3): 193-202 (in Chinese with English abstract). http://www.researchgate.net/publication/312662945_Dating_and_reconstruction_of_the_high_resolution_time_series_in_the_Weinan_loess_section_of_the_last_150000_years
      Liu, Z.W., Pan, K.W., 2005. Problems in Olson's litter decomposition model and its revision. Journal of Northwest Sci-Tech University of Agriculture and Forestry, 33(1): 69-70 (in Chinese with English abstract). http://europepmc.org/abstract/CBA/575422
      Lü, H.Y., Liu, D.S., Wu, N.Q., et al., 1999. Phytolith record of vegetation succession in the southern loess plateau since Late Pleistocene. Quaternary Sciences, (4): 336-349 (in Chinese with English abstract). http://www.researchgate.net/publication/284987929_Phytolith_record_of_vegetation_succession_in_the_southern_Loess_Plateau_since_Late_Pleistocene
      Morozova, T.D., Velichko, A.A., Dlussky, K.G., 1998. Organic carbon content in the Late Pleistocene and Holocene fossil soils (reconstruction for eastern Europe). Global and Planetary Change, 16-17: 131-151. doi: 10.1016/S0921-8181(98)00027-7
      Post, W.M., Emanuel, W.R., Zinke, P.J., et al., 1982. Soil carbon pools and world life zones. Nature, 298: 156-159. doi: 10.1038/298156a0
      Post, W.M., Peng, T.H., Emanuel, W.R., et al., 1990. The global carbon cycle. American Scientist, 78: 310-326.
      Qin, X.G., Cai, B.G., Liu, T.S., 2005. Loess record of the aerodynamic environment in the East Asia monsoon area since 60 000 years before present. Journal of Geophysical Research-Solid Earth, 110(B01204): 16. doi: 10.1029/2004JB003131
      Qin, X.G., Li, C.S., Cai, B.G., 2001. The sensitivity simulation of climate impact on C pools of loess. Quaternary Sciences, 21(2): 153-161 (in Chinese with English abstract). http://www.researchgate.net/publication/284048269_The_sensitivity_simulation_of_climate_impact_on_C_pools_of_loess
      Schimel, D.S., House, J.I., Hibbard, K.A., et al., 2001. Recent patterns and mechanisms of carbon exchange by terrestrial ecosystems. Nature, 414(6860): 169-172. doi: 10.1038/35102500
      Shi, P.L., Yu, G.R., Wang, S.Q., et al., 2003. Research of carbon cycle and carbon storage in Chinese terrestrial ecosystem. In: Yu, G.R., et al., eds., Global change, carbon cycle and storage in terrestrial system. Meteorological Press, Beijing, 396-442 (in Chinese).
      Starkel, L., 1998. Continental water cycle and carbon reservoirs and their relationships in the past. Global and Planetary Change, 16-17: 153-158. doi: 10.1016/S0921-8181(98)00028-9
      Sun, X.J., Song, C.Q., Wang, B.Y., et al., 1995. The vegetation at south of Loess plateau at last 100 ka—the pollen records of Weinan section in Shaanxi. Science Bulletin, 40(13): 1222-1224 (in Chinese).
      Velichko, A.A., Zelikson, E.M., Borisova, O.K., 1999. Vegetation, phytomass and carbon storage in northern Eurasia during the last glacial-interglacial cycle and the Holocene. Chemical Geology, 159(1-4): 191-204. doi: 10.1016/S0009-2541(99)00029-7
      Wang, S.Q., Zhou, C.H., 1999. Estimating soil carbon reservior of terrestrial ecosystem in China. Geographical Research, 18(4): 349-356 (in Chinese with English abstract). http://www.researchgate.net/publication/284651662_Estimating_soil_carbon_reservoir_of_terrestrial_ecosystem_in_China
      Wen, Q.Z., Diao, G.Y., Jia, R.F., et al., 1996. Geochemical indicators and their significance in paleoclimatic changes in Weinan loess section since the last interglacial. Geochimica, 25(6): 529-535 (in Chinese with English abstract). http://www.researchgate.net/publication/292016762_Geochemical_indicators_and_their_significance_in_paleoclimatic_changes_in_Weinan_loess_section_since_the_last_interglacial
      Wu, N.Q., Lü, H.Y., Sun, X.J., 1994. Climate transfer function from opal phytolith and its application in paleoclimate reconstruction of China loesspaleosol sequence. Quaternary Sciences, 3: 270-279 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ199403007.htm
      方精云, 刘国华, 徐嵩龄, 1996. 我国森林植被的生物量和净生产量. 生态学报, 16(5): 497-508. https://www.cnki.com.cn/Article/CJFDTOTAL-STXB605.006.htm
      郭正堂, 刘东生, 安芷生, 1994. 渭南黄土沉积中十五万年来的古土壤及其形成时的古环境. 第四纪研究, (3): 256-269. doi: 10.3321/j.issn:1001-7410.1994.03.007
      韩家懋, 姜文英, 刘东生, 等, 1996. 黄土碳酸盐中古气候变化的同位素记录. 中国科学(D辑), 26(5): 399-404. doi: 10.3321/j.issn:1006-9267.1996.05.001
      金峰, 杨浩, 蔡祖聪, 等, 2001. 土壤有机碳密度及储量的统计研究. 土壤学报, 38(4): 522-528. doi: 10.3321/j.issn:0564-3929.2001.04.010
      李天杰, 郑应顺, 王云, 1983. 土壤地理学. 北京: 高等教育出版社, 59-95.
      刘东生, 1985. 黄土与环境. 北京: 科学出版社, 29-296.
      刘嘉麒, 陈铁梅, 聂高众, 等, 1994. 渭南黄土剖面的年龄测定及十五万年来高分辨时间序列的建立. 第四纪研究, (3): 193-202. doi: 10.3321/j.issn:1001-7410.1994.03.001
      刘增文, 潘开文, 2005. Olson枯落物分解模型存在的问题与修正. 西北农林科技大学学报(自然科学版), 33(1): 69-70. doi: 10.3321/j.issn:1671-9387.2005.01.016
      吕厚远, 刘东生, 吴乃琴, 等, 1999. 末次间冰期以来黄土高原南部植被演替的植物硅酸体记录. 第四纪研究, (4): 336-349. doi: 10.3321/j.issn:1001-7410.1999.04.006
      秦小光, 李长生, 蔡炳贵, 2001. 气候变化对黄土碳库效应影响的敏感性研究. 第四纪研究, 21(2): 153-161. doi: 10.3321/j.issn:1001-7410.2001.02.008
      石培礼, 于贵瑞, 王绍强, 等, 2003. 中国陆地生态系统碳循环与碳储量研究进展. 见: 于贵瑞, 等主编, 全球变化与陆地生态系统碳循环与碳蓄积. 北京: 气象出版社, 396-442.
      孙湘君, 宋长青, 王琫瑜, 等, 1995. 黄土高原南缘10万年以来的植被——陕西渭南黄土剖面的花粉记录. 科学通报, 40(13): 1222-1224. doi: 10.3321/j.issn:0023-074X.1995.13.020
      王绍强, 周成虎, 1999. 中国陆地土壤有机碳库的估算. 地理研究, 18(4): 349-356. doi: 10.3321/j.issn:1000-0585.1999.04.003
      文启忠, 刁桂仪, 贾蓉芬, 等, 1996. 末次间冰期以来渭南黄土剖面地球化学指标所反映的古气候变化. 地球化学, 25(6): 529-535. doi: 10.3321/j.issn:0379-1726.1996.06.001
      吴乃琴, 吕厚远, 孙湘君, 等, 1994. 植物硅酸体-气候因子转换函数及其在渭南晚冰期以来古环境研究中的应用. 第四纪研究, 3: 270-279. doi: 10.3321/j.issn:1001-7410.1994.03.008
      • Relative Articles

    • Relative Articles

      • Supplements(0)
      • Cited By
    • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-072024-082024-092024-102024-112024-122025-012025-022025-032025-042025-052025-06010203040
      Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 49.2 %FULLTEXT: 49.2 %META: 49.8 %META: 49.8 %PDF: 0.9 %PDF: 0.9 %FULLTEXTMETAPDF
      Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 5.4 %其他: 5.4 %其他: 0.4 %其他: 0.4 %China: 0.2 %China: 0.2 %Russian Federation: 0.1 %Russian Federation: 0.1 %上海: 0.9 %上海: 0.9 %丽水: 0.1 %丽水: 0.1 %信阳: 0.1 %信阳: 0.1 %兰州: 0.1 %兰州: 0.1 %北京: 15.8 %北京: 15.8 %十堰: 0.1 %十堰: 0.1 %南京: 0.6 %南京: 0.6 %南昌: 0.5 %南昌: 0.5 %哥伦布: 0.1 %哥伦布: 0.1 %唐山: 0.4 %唐山: 0.4 %嘉兴: 0.1 %嘉兴: 0.1 %天津: 0.2 %天津: 0.2 %宣城: 0.4 %宣城: 0.4 %常州: 0.1 %常州: 0.1 %库比蒂诺: 0.1 %库比蒂诺: 0.1 %张家口: 0.6 %张家口: 0.6 %成都: 0.1 %成都: 0.1 %扬州: 0.1 %扬州: 0.1 %杭州: 1.1 %杭州: 1.1 %武汉: 1.4 %武汉: 1.4 %海口: 0.1 %海口: 0.1 %温州: 0.1 %温州: 0.1 %湖州: 0.1 %湖州: 0.1 %漯河: 0.3 %漯河: 0.3 %烟台: 0.2 %烟台: 0.2 %石家庄: 0.3 %石家庄: 0.3 %芒廷维尤: 16.8 %芒廷维尤: 16.8 %芝加哥: 0.1 %芝加哥: 0.1 %苏州: 0.2 %苏州: 0.2 %莫斯科: 0.1 %莫斯科: 0.1 %衡阳: 0.1 %衡阳: 0.1 %衢州: 0.1 %衢州: 0.1 %西宁: 50.2 %西宁: 50.2 %西安: 1.5 %西安: 1.5 %达尔斯: 0.2 %达尔斯: 0.2 %邯郸: 0.1 %邯郸: 0.1 %长沙: 0.4 %长沙: 0.4 %其他其他ChinaRussian Federation上海丽水信阳兰州北京十堰南京南昌哥伦布唐山嘉兴天津宣城常州库比蒂诺张家口成都扬州杭州武汉海口温州湖州漯河烟台石家庄芒廷维尤芝加哥苏州莫斯科衡阳衢州西宁西安达尔斯邯郸长沙

    Catalog

      通讯作者: 陈斌, bchen63@163.com
      • 1. 

        沈阳化工大学材料科学与工程学院 沈阳 110142

      1. 本站搜索
      2. 百度学术搜索
      3. 万方数据库搜索
      4. CNKI搜索

      Figures(4)

      Get Citation
      PDF
      XML
      Article views (689) PDF downloads(14) Cited by()
      Proportional views

      Address：湖北省武汉市洪山区鲁磨路388号《地球科学》编辑部 China Pos：430074

      Tel：027-67885075 Fax：027-67885075

      Copyright ©2020 鄂ICP备15021562号-2

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

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return