中晚全新世湘西莲花洞石笋旋回沉积速率变化及其古气候意义

张会领; 余克服; 赵建新; 俸月星; 林玉石; 周 玮; 刘国辉

doi:10.11932/karst20170421

中晚全新世湘西莲花洞石笋旋回沉积速率变化及其古气候意义

doi: 10.11932/karst20170421

1.
广东海洋大学海洋工程学院海洋工程系/中国科学院南海海洋研究所边缘海地质重点实验室/中国地质科学院岩溶地质研究所岩溶动力学重点实验室
2.
中国科学院南海海洋研究所边缘海地质重点实验室/广西大学海洋学院
3.
Radiogenic Isotope Laboratory, Department of Geology, University of Queensland
4.
中国地质科学院岩溶地质研究所岩溶动力学重点实验室
5.
中国科学院南海海洋研究所边缘海地质重点实验室

基金项目: 国家重大科学研究计划（2013CB956102）;国家自然科学基金项目（41025007、41302281、41272199）；中国科学院边缘海地质重点实验室开放基金（MSGL15-09）；广东海洋大学博士科研启动项目（No:E13389）；中国地质科学院岩溶地质研究所岩溶动力学重点实验室开放基金（KDL201501）

计量
- 文章访问数: 1573
- HTML浏览量: 294
- PDF下载量: 975
- 被引次数: 0
出版历程
- 发布日期: 2017-08-25

Variations in deposition rate of sedimentary cycle from a stalagmite in Lianhua -Cave and its paleoclimatic implications during the mid-late Holocene

1.
Department of Ocean Engineering, College of Ocean Engineering, Guangdong Ocean University/South China Sea Institute of Oceanology,Key Laboratory of Marginal Sea Geology, CAS/Institute of Karst Geology, CAGS/ Key Laboratory of Karst Dynamics, MLR＆GZAR
2.
South China Sea Institute of Oceanology,Key Laboratory of Marginal Sea Geology, CAS/School of Marune Sciences, Guangxi University
3.
Radiogenic Isotope Laboratory, Department of Geology, University of Queensland
4.
Institute of Karst Geology, CAGS/ Key Laboratory of Karst Dynamics, MLR＆GZAR
5.
South China Sea Institute of Oceanology,Key Laboratory of Marginal Sea Geology, CAS

摘要

摘要: 石笋旋回沉积速率是按照石笋沉积旋回测年得到的沉积速率，是石笋沉积过程的重要参数和反演古气候变化的有效代用指标。旋回沉积速率的波动可能反应了地表温度和降雨量的变化，与夏季风强度存在关联。文章以湖南湘西莲花洞LH2石笋为材料，利用42个230Th年龄获得的石笋旋回沉积速率序列重建了8.6 ka BP以来湖南湘西地区温度和降雨雨量的变化历史: 8.6-4.2 ka BP期间，气候以高温多雨为特征，夏季风强，石笋生长率高，但气候并不稳定，存在一系列千年-百年尺度的波动；4.2-0.05 ka BP期间，气候整体偏冷干，旋回沉积速率偏低。总体上，在轨道尺度上，LH2石笋的旋回沉积速率与该石笋的δ18O值之间存在负相关关系。旋回沉积速率的重复性检验证明了旋回沉积速率古气候记录的有效性。石笋旋回沉积速率变化主要受北半球夏季太阳辐射量的控制和ITCZ的直接影响，在百年尺度上，旋回沉积速率的波动可能与中晚全新世的弱季风事件存在关联。
- 旋回沉积速率 /
- 古气候意义 /
- 石笋 /
- 莲花洞 /
- 湘西
Abstract: Deposition rate of sedimentary cycle of stalagmite，which is calculated based on 230Th age dating according to sedimentary cycle of stalagmite, is an important parameter of stalagmite formation and an effective paleoclimatic index to reconstruct paleoclimate. Variations in deposition rate of sedimentary cycle may reflect the change of surface temperature and rainfall, which immediately relates to intensity of summer monsoon. Making use of stalagmite LH2, collected from Lianhua Cave, Hunan Province , China, the paper reconstructs the history of surface temperature and rainfall since 8.6 ka BP based on 42 230Th ages. From 8.6 ka BP to 4.2 ka BP, the climate is characterized by high temperature and rainy, the summer monsoon is strong, deposition rate of sedimentary cycle is high. But the climate is not stable and there is a series of millennial to centennial fluctuations.From 4.2 ka BP to now, the climate is cool and dry, deposition rate of sedimentary cycle is low. Generally speaking, in orbital timescale, there is a negative correlation between deposition rate of sedimentary cycle andδ18O record from stalagmite LH2. The deposition rate of sedimentary cycle stalagmite D4 from Dongge Cave duplicates that of stalagmite LH2, which confirms the validity of deposition rate of sedimentary cycle to record climate changes. Basically, changes of deposition rate of stalagmite are controlled by the summer solar radiation in Northern Hemisphere and ITCZ exerts directly influence on it. In centenniarl timescale, deposition rate of sedimentary cycle of stalagmite LH2 may relate to weak monsoon events occuring in the mid-late Holocene.
- deposition rate of sedimentary cycle, paleoclimate implications, stalagmite,Lianhua Cave /
- western Hunan /

HTML

参考文献(56)

[1]	Behloul C, Guijarro D, Yus M Testing theoretically predicted stalagmite growth rate with recent annually laminated samples:Implications for past stalagmite deposition［J］. Geochimica et Cosmochimica Acta,1998, 62(3): 393-404.
[2]	Baker A, Smart P L, Edwards R L, et al. Annual growth banding in a cave stalagmite［J］. Nature, 1993,364(6437):518-520.
[3]	刘东生, 谭明, 秦小光, 等. 洞穴碳酸钙微层理在中国的首次发现及其对全球变化研究的意义［J］. 第四纪研究, 1997, 17(1): 41-51.
[4]	Tan M, Liu T S, Hou J Z, 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): 11-19.
[5]	王新忠,班凤梅,潘根兴.洞穴滴水地球化学的空间和时间变化及其控制因素：以北京石花洞为例［J］.第四纪研究, 2005, 25(2):258-264.
[6]	班凤梅, 潘根兴，王新中. 北京石花洞石笋微层层面有机质的形成时间和机理初探［J］, 第四纪研究,2005, 25(2), 265-268.
[7]	Frisia A, Borsato A, Preto N, et al. Late Holocene annual growth in three Alpine stalagmites records the influence of solar activity and the North Atlantic Oscillation on winter climate［J］. Earth and Planetary Science Letters,2003, 216(3), 411-424.
[8]	Baker A, Proctor C, Lauritzen S R. High-resolution stalagmite records of NE Atlantic climate in the last millennium.2000,8(2):14.
[9]	刘浴辉,胡超涌,黄俊华, 等.长江中游石笋年层厚度作为东亚季风强度代用指标的研究［J］. 第四纪研究, 2005.25(2): 228-234.
[10]	Bums S J, Fleitmann D, Mudelsee M, et al. A 780-year annually resolved record of Indian Ocean monsoon precipitation from a speleothem from south Oman［J］.Journal of Geophysical Atmospheres, 2002,107(D20), 4434-4442.
[11]	Fleitmann D, Stephen B J, Neff U,et al. Palaeoclimatic interpretation of high-resolution oxygen isotope profiles derived from annually laminated speleothems from Southern Oman［J］. Quaternary Science Reviews, 2004, 23(7-8), 935-945.
[12]	Brook G A, Rafter M A, Railsback L B, et al. A highresolution proxy record of rainfall and ENSO since AD 1550 from layering in stalagmites from Anjohibe Cave, Madagascar［J］. Holocene, 1999, 9(6), 695-706.
[13]	Holmgren K,Karlén W, Lauritzen S E,et al. A 3000year high-resolution stalagmite based record of palaeoclimate for northeastern South Africa［J］. Holocene, 1999,9(3), 295-309.
[14]	Polyak V J, Asmerom Y. Late holocene climate and cultural changes in the Southwestern United States［J］.Science, 2001,294(5540): 148-151.
[15]	Qin X G, Tan M, Liu T S, et al. Spectral analysis of a 1000year stalagmite lamina-thickness record from Shihua Cavern, Beijing, China, and its climatic significance［J］. Holocene,2011,9(6): 689-694.
[16]	Railsback L B, Brook G A, Chen J,et al. Environmental controls on the petrology of a Late Holocene speleothem from Botswana with annual layers of aragonite and calcite［J］. Journal of Sedimentary Research, 1994,64(1): 147-155.
[17]	Zhao K, Wang Y J, Edwards R L,et al. A high-resolved record of the Asian Summer Monsoon from Dongge Cave, China for the past 1200 years［J］. Quaternary Science Reviews, 2015, 122:250-257.
[18]	吴江滢,邵晓华,孔兴功,等.盛冰期太阳活动在南京石笋年层序列中的印迹［J］. 科学通报, 2006,51(4):431-435.
[19]	Proctor C,Baker A, Barnes W. A three thousand year record of North Atlantic climate［J］. Climate Dynamics, 2002,19(5-6):449-454.
[20]	林玉石，张美良，覃嘉铭.洞穴石笋沉积速率研究中值得注意的几个问题［J］.中国岩溶，2001,20（2）:131-136.
[21]	何潇,王建力,李清,等.重庆地区石笋沉积速率与古气候意义初探［J］. 中国岩溶,2007, 26(3): 196-201.
[22]	Buhmann D, Dreybrodt W. The kinetics of calcite dissolution and precipitation in geologically relevant situations of karst areas: 1. Open system［J］. Chemical Geology,1985, 48(1-4): 189-211.
[23]	Buhmann D, Dreybrodt, W. The kinetics of calcite dissolution and precipitation in geologically relevant situations of karst areas: 2. Closed system［J］. Chemical Geology, 1985,53(1-2):109-124.
[24]	Dreybrodt W. Chemical kinetics, speleothem growth and climate［J］. Boreas, 2010, 28(3): 347-356.
[25]	Dreybrodt W. 1988. Processes in karst system:physics, chemistry and geology［M］. Berlin, New York: Springer Verlag: 288.
[26]	Genty D, Quinif Y. Annually laminated sequences in the internal structure of some Belgian stalagmites  Importance for paleoclimatology［J］. Journal of Sedimentary Research, 1996,66(1): 275-288.
[27]	Zhang HL, Yu KF, Zhao JX, et al. East Asian Summer Monsson variaitons in the past 12.5 ka: highresolution δ18 O record from a precisely dated aragonite stalagmite in central China［J］. Journal of Asian Earth Science, 2013,73（8）：162-175.
[28]	韦刚健, 余克服, 赵建新. 雷州半岛中晚全新世造礁珊瑚 Sr/Ca值的表层海水温度记录［J］. 科学通报, 2004b ，49(17): 1770-1775.
[29]	黄镇国, 张伟强.中国热带珊瑚礁的第四纪气候记录［J］. 热带地理, 2008,28(1): 11-15.
[30]	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):300-301.
[31]	张兰生，方修琦. 中国古地理——中国自然环境的形成［M］.北京：科学出版社, 2011.
[32]	方修琦,章文波,张兰生.全新世暖期我国土地利用的格局及其意义［J］. 自然资源学报, 1998, 13(1):16-22.
[33]	葛全胜. 中国历朝气候变化［M］.北京：科学出版社，2010，1-708.
[34]	Wang Y, Cheng H, Edwards R L, et al. The Holocene Asian monsoon: links to solar changes and North Atlantic climate［J］. Science, 2005,308(5723): 854-857.
[35]	邵晓华, 汪永进, 程海, 等. 全新世季风气候演化与干旱时间的湖北神农架石笋记录［J］. 科学通报, 2006.51(1): 80-86.
[36]	Tan M, Cai B G, Preliminary calibration of stalagmite oxygen isotopes from eastern monsoon China with northern Hemisphere temperatures［N］. Pages News, 2005. 13(Aug.):16-17.
[37]	Yao T D, Thompson L G. Trends and features of climatic changes in the past 5000 years recorded by the Dunde ice core［J］. International Annals of Glaciology, 1992,16(4):21-24.
[38]	Hong Y, Wang ZG, Jiang H B, et al. A 6000-year record of changes in drought and precipitation in northeastern China based on a δ13C time series from peat cellulose［J］. Earth and Planetary Science Letters, 2001,185(s1-2): 111-119.
[39]	Schettler G, Liu Q, Mingram J, et al. East-Asian monsoon variability between 15 000 and 2000 cal. yr BP recorded in varved sediments of Lake Sihailongwan (northeastern China, Long Gang volcanic field)［J］. Holocene, 2006,16(8):1043-1057.
[40]	Wang L, Sarnthein M, Erlenkeuser H, et al. East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea［J］. Marine Geology, 1999,156(1-4):245-284.
[41]	Liu X, Ren J. Dendroclimatic temperature record derived from treering width and stable carbon isotope chronologies in the Middle Qilian Mountains, China［J］. Arctic Antarctic& Alpine Research,2002, 39(4): 651-657.
[42]	Thompson L G, Yao T, Davis M E, et al. Holocene climate variability archived in the Puruogangri ice cap on the central Tibetan Plateau［J］. Annals of Glaciology, 2006,43(1): 61-69.
[43]	竺可桢.中国近五千年来气候变迁的初步研究［J］. 考古学报, 1972,(1):168-189.
[44]	杨保,谭明.近千年东亚夏季风演变历史重建及与区域温湿变化关系的讨论［J］. 第四纪研究, 2009,29(5): 880-887.
[45]	Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution, absolutedated Holocene and deglacial Asian monsoon record from Dongge Cave, China［J］. Earth and Planetary Science Letters, 2005, 233(1-2):71-86.
[46]	Dayem K E, Molnar P, Battisti D S, et al. Lessons learned from oxygen isotopes in modern precipitation applied to interpretation of speleothem records of paleoclimate from eastern Asia［J］. Earth and Planetary Science Letters, 2010,295(1-2): 219-230.
[47]	丁一汇.中国气候变化科学概论［J］.北京：气象出版社, 2008:281.
[48]	Wright H E, Kutzbach J E, Webb T. Global climates since the last glacial maximum［M］. Minneapolis:University of Minnesota Press, 1993：468-513.
[49]	Hastenrath S, Greischar L. Circulation mechanisms related to northeast Brazil rainfall anomalies［J］. Journal of Geophysical Research Atmospheres,1993, 98(D3): 5093-5102.
[50]	Haug G H, Hughen K A, Sigman D M, et al. Southward migration of the Intertropical Convergence Zone through the Holocene［J］. Science, 2001,293(5533): 1304-1308.
[51]	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(5626):1737-1739.
[52]	王淑云, 吕厚远, 刘嘉麒. 湖光岩玛珥湖高分辨率孢粉记录揭示的早全新世适宜期环境特征［J］. 科学通报,2007, 52:1285-1291.
[53]	Berger A L.Long-term variations of daily insolation and Quaternary climatic changes［J］. Journal of Atmospheric Sciences,1978, 35(12):2362-2367.
[54]	金祖辉，陶诗言. ENSO循环与中国东部地区夏季和冬季降水关系的研究［J］.大气科学，1999,23（6）：663-672.
[55]	Rodbell D T, Seltzer G O, Anderson D M, et al. An 5,000-year record of El Nio-driven alluviation in southwestern Ecuador［J］. Science, 1999，283（5401）:516-520.
[56]	Moy C M, Seltzer G O, Rodbell D T, et al. Variability of El Nio/Southern Oscillation activity at millennial timescales during the Holocene epoch［J］. Nature, 2002，420（6912）: 162-165.