必须声明标量变量 "@Script_ID"。 福建仙云洞石笋记录的Termination I事件缓变特征-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]马乐,肖海燕,张鑫,等.福建仙云洞石笋记录的Termination I事件缓变特征[J].地球科学与环境学报,2019,41(05):604-612.
 MA Le,XIAO Hai-yan,ZHANG Xin,et al.Gradual Changes of the Termination I Inferred from Stalagmite Records in Xianyun Cave of Fujian, China[J].Journal of Earth Sciences and Environment,2019,41(05):604-612.
点击复制

福建仙云洞石笋记录的Termination I事件缓变特征(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第05期
页码:
604-612
栏目:
水资源与环境
出版日期:
2019-09-15

文章信息/Info

Title:
Gradual Changes of the Termination I Inferred from Stalagmite Records in Xianyun Cave of Fujian, China
文章编号:
1672-6561(2019)05-0604-09
作者:
马乐1肖海燕1张鑫1姜修洋123*蔡炳贵123
(1. 福建师范大学 地理科学学院,福建 福州 350007; 2. 福建师范大学 湿润亚热带生态地理过程 教育部重点实验室,福建 福州 350007; 3. 福建师范大学 地理研究所,福建 福州 350007)
Author(s):
MA Le1 XIAO Hai-yan1 ZHANG Xin1 JIANG Xiu-yang123* CAI Bing-gui123
(1. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, Fujian, China; 2. Key Laboratory of Humid Subtropical Eco-geographical Processes of Ministry of Education, Fujian Normal University, Fuzhou 350007, Fujian, China; 3. Institute of Geography, Fujian Normal University, Fuzhou 350007, Fujian, China)
关键词:
Termination I事件 东亚季风 石笋 转型特征 区域差异 驱动机制 仙云洞 福建
Keywords:
Termination I East Asian monsoon stalagmite transitional characteristic regional difference driving mechanism Xianyun cave Fujian
分类号:
P532
DOI:
-
文献标志码:
A
摘要:
末次冰期终止事件(Termination I,简称TI)是发生在末次冰消期约14.7 ka B.P.北半球最显著的一次快速升温事件,其气候突变的全球响应及转型特征是末次冰消期研究的重点。基于中国东南地区福建西部仙云洞两支石笋(样品编号为XY11和XYⅢ-21)17个高精度230Th年龄和567个氧同位素数据,建立了12.67~16.10 ka B.P.时段内平均分辨率达十年际的东亚夏季风强度演变序列,捕捉到了Termination I转型缓变特征。仙云洞石笋记录揭示Termination I事件缓变特征持续时间达800 a,明显比也门(约13 a)以及中国西南地区(约35 a)和长江中下游地区(约200 a)石笋记录的转型时间长很多,存在显著的区域差异。仙云洞石笋记录的Termination I转型时段季风开始增强响应于北高纬气候,但仙云洞石笋记录的Termination I缓变特征指示其可能受到热带低纬西太平洋暖池水文循环过程的影响。
Abstract:
The Termination I(TI)is the most significant abrupt warming event in the northern hemisphere during the last deglaciation of about 14.7 ka B.P., and its transitional characteristics and global response to climate change are the focus of the research. Based on 17 high-resolution 230Th ages and 567 oxygen isotope data from two stalagmites(XY11 and XYⅢ-21)in Xianyun cave of western Fujian, southeastern China, the East Asian summer monsoon intensity evolution sequence with an average resolution of ten years covering the period of 12.67-16.10 ka B.P. was established. It is characterized by slow transitional process over 800 a, which is much longer than that in Yemen(~13 a), the southwestern China(~35 a)and the middle-lower reaches of Yangtze River, China(~200 a), showing obvious regional differences. The onset of intensified monsoon mainly responses to the north high latitude climate during the Termination I inferred from stalagmite records in Xianyun cave. The slow transitional characteristic implies that the hydrology processes over the tropical low latitude West Pacific warm pool may exert significant impact on the monsoon climate.

参考文献/References:

[1] BLUNIER T,BROOK E J.Timing of Millennial-scale Climate Change in Antarctica and Greenland During the Last Glacial Period[J].Science,2001,291:109-112.
[2] LEMIEUX-DUDON B,BLAYO E,PETIT J R,et al.Consistent Dating for Antarctic and Greenland Ice Cores[J].Quaternary Science Reviews,2010,29(1):8-20.
[3] PELTIER W R,FAIRBANKS R G.Global Glacial Ice Volume and Last Glacial Maximum Duration from an Extended Barbados Sea Level Record[J].Quaternary Science Reviews,2006,25(23/24):3322-3337.
[4] MACMANUS J F,FRANCOIS R,GHERARDI J M,et al.Collapse and Rapid Resumption of Atlantic Meridional Circulation Linked to Deglacial Climate Changes[J].Nature,2004,428:834-837.
[5] GRACHEV A M,SEVERINGHAUS J P.Determining the Thermal Diffusion Factor for 40Ar/36Ar in Air to Aid Paleoreconstruction of Abrupt Climate Change[J].The Journal of Physical Chemistry A,2003,107(23):4636-4642.
[6] LOWE J J,RASMUSSEN S O,BJORCK S,et al.Synchronisation of Palaeoenvironmental Events in the North Atlantic Region During the Last Termination:A Revised Protocol Recommended by the INTIMATE Group[J].Quaternary Science Reviews,2008,27(1/2):6-17.
[7] BROCCOLI A J,DAHL K A,STOUFFER R J.Res-ponse of the ITCZ to Northern Hemisphere Cooling[J].Geophysical Research Letters,2006,33(1):1010-1029.
[8] DEPLAZES G,LUCKGE A,PETERSON L C,et al.Links Between Tropical Rainfall and North Atlantic Climate During the Last Glacial Period[J].Nature Geoscience,2013,6(3):213-217.
[9] 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.
[10] STRIKIS N M,CHIESSI C M,CRUZ F W,et al.Timing and Structure of Mega-SACZ Events During Heinrich Stadial 1[J].Geophysical Research Letters,2015,42(13):5477-5484.
[11] STEFFENSEN J P,ANDERSEN K K,BIGLER M,et al.High-resolution Greenland Ice Core Data Show Abrupt Climate Change Happens in Few Years[J].Science,2008,321:680-684.
[12] SHAKUN J D,BURNS S J,FLEITMANN D,et al.A High-resolution,Absolute-dated Deglacial Speleothem Record of Indian Ocean Climate from Socotra Island,Yemen[J].Earth and Planetary Science Letters,2007,259(3/4):442-456.
[13] 杨 琰,袁道先,程 海,等.末次冰消期亚洲季风突变事件的精确定年:以贵州衙门洞石笋为例[J].中国科学:地球科学,2010,40(2):199-210. YANG Yan,YUAN Dao-xian,CHENG Hai,et al.Precise Dating of Abrupt Shifts in the Asian Monsoon During the Last Deglaciation Based on Stalagmite Data from Yamen Cave,Guizhou Province,China[J].Science China:Earth Sciences,2010,40(2):199-210.
[14] YUAN D X,CHENG H,EDWARDS R L,et al.Timing,Duration and Transitions of the Last Interglacial Asian Monsoon[J].Science,2004,304:575-578.
[15] LI T Y,SHEN C C,LI H C,et al.Oxygen and Carbon Isotopic Systematics of Aragonite Speleothems and Water in Furong Cave,Chongqing,China[J].Geochimica et Cosmochimica Acta,2011,75(15):4140-4156.
[16] ZHANG H,GRIFFITHS M L,HUANG J,et al.An-tarctic Link with East Asian Summer Monsoon Variability During the Heinrich Stadial-Bolling Interstadial Transition[J].Earth and Planetary Science Letters,2016,453:243-251.
[17] PARTIN J W,COBB K M,ADKINS J F,et al.Millennial-scale Trends in West Pacific Warm Pool Hydrology Since the Last Glacial Maximum[J].Nature,2007,449:452-456.
[18] SHEN C C,CHENG H,EDWARDS R L,et al.Measu-rement of Attogram Quantities of 231Pa in Dissolved and Particulate Fractions of Seawater by Isotope Dilution Thermal Ionization Mass Spectroscopy[J].Analytical Chemistry,2003,75(5):1075-1079.
[19] ZHANG P,CHENG H,EDWARDS R L,et al.A Test of Climate,Sun,and Culture Relationships from an 1 810-year Chinese Cave Record[J].Science,2008,322:940-942.
[20] JIANG X Y,WANG X Y,HE Y Q,et al.Precisely Dated Multidecadally Resolved Asian Summer Monsoon Dynamics 113.5-86.6 Thousand Years Ago[J].Quaternary Science Reviews,2016,143:1-12.
[21] DUAN F C,WANG Y J,LIAO Z B,et al.Divergent Influences of the Greenland and Antarctica Climates on the Asian Monsoon During a Stadial to Interstadial Cycle[J].Journal of Asian Earth Sciences,2018,159:69-73.
[22] 孙喜利,杨勋林,史志超,等.石笋记录的西南地区MIS4阶段夏季风的演化[J].第四纪研究,2017,37(6):1370-1380. SUN Xi-li,YANG Xun-Lin,SHI Zhi-chao,et al.The Evolution of Summer Monsoon in Southwest China During MIS4 as Revealed by Stalagmite δ18O Record[J].Quaternary Sciences,2017,37(6):1370-1380.
[23] CHENG H,SINHA A,WANG X,et al.The Global Pa-leomonsoon as Seen Through Speleothem Records from Asia and the Americas[J].Climate Dynamics,2012,39(5):1045-1062.
[24] CHENG H,EDWARDS R L,SINHA A,et al.The Asian Monsoon over the Past 640 000 Years and Ice Age Terminations[J].Nature,2016,534:640-646.
[25] 崔梦月,肖海燕,孙晓双,等.福建仙云洞石笋记录的Heinrich 1事件突变特征[J].科学通报,2017,62(26):3078-3088. CUI Meng-yue,XIAO Hai-yan,SUN Xiao-shuang,et al.Characteristics of the Heinrich 1 Abrupt Climate Event Inferred from a Speleothem Record from Xianyun Cave,Fujian Province[J].Chinese Science Bulletin,2017,62(26):3078-3088.
[26] 崔梦月,洪 晖,孙晓双,等.福建仙云洞石笋记录的新仙女木突变事件结束时的缓变特征[J].第四纪研究,2018,38(3):711-719 CUI Meng-yue,HONG Hui,SUN Xiao-shuang,et al.The Gradual Change Characteristics at the End of the Younger Dryas Event Inferred from a Speleothem Record from Xianyun Cave,Fujian Province[J].Quaternary Sciences,2018,38(3):711-719.
[27] 车印平,肖海燕,崔梦月,等.闽西仙云洞石笋记录的Heinrich 2事件年龄及亚旋回特征[J].沉积学报,2018,36(6):1139-1147. CHE Yin-ping,XIAO Hai-yan,CUI Meng-yue,et al.Timing and Structure of the Heinrich 2 Abrupt Event Inferred from a Speleothem Record from Xianyun Cave,Western Fujian Province[J].Acta Sedimentologica Sinica,2018,36(6):1139-1147.
[28] 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.
[29] LIU D P,WANG Y J,CHENG H,et al.A Detailed Comparison of Asian Monsoon Intensity and Greenland Temperature During the Allerod and Younger Dryas Events[J].Earth and Planetary Science Letters,2008,272(3/4):691-697.
[30] DUTT S,GUPTA A K,CLEMENS S C,et al.Abrupt Changes in Indian Summer Monsoon Strength During 33 800 to 5 500 Years B.P.[J].Geophysical Research Letters,2015,42(13):5526-5532.
[31] KATHAYAT G,CHENG H,SINHA A,et al.Indian Monsoon Variability on Millennial-orbital Time Scales[J].Scientific Reports,2016,DOI:10.1038/srep24374.
[32] SUN Y B,CLEMENS S C,MORRILL C,et al.Influence of Atlantic Meridional Overturning Circulation on the East Asian Winter Monsoon[J].Nature Geoscience,2012,5(1):46-49.
[33] WURTZEL J B,ABRAM N J,LEWIS S C,et al.Tropical Indo-Pacific Hydro Climate Response to North Atlantic Forcing During the Last Deglaciation as Recorded by a Speleothem from Sumatra,Indonesia[J].Earth and Planetary Science Letters,2018,492:264-278.
[34] PARTIN J W,QUINN T M,SHEN C C,et al.Gra-dual Onset and Recovery of the Younger Dryas Abrupt Climate Event in the Tropics[J].Nature Communications,2015,DOI:10.1038/ncomms9061.
[35] CAROLIN S A,COBB K M,ADKINS J F,et al.Varied Response of Western Pacific Hydrology to Climate Forcings over the Last Glacial Period[J].Science,2013,340:1564-1566.
[36] STOTT L,TIMMERMANN A,THUNELL R.Southern Hemisphere and Deep-sea Warming Led Deglacial Atmospheric CO2 Rise and Tropical Warming[J].Science,2007,318:435-438.
[37] ROSENTHAL Y,OPPO D W,LINSLEY B K.The Amplitude and Phasing of Climate Change During the Last Deglaciation in the Sulu Sea,Western Equatorial Pacific[J].Geophysical Research Letters,2003,30(8):1-4.
[38] GRIFFITHS M L,KIMBROUGH A K,GAGAN M K,et al.Western Pacific Hydroclimate Linked to Global Climate Variability over the Past Two Millennia[J].Nature Communications,2016,DOI:10.1038/ncomms11719.
[39] DING X,ZHENG L,LI D,et al.Lacustrine Record of Centennial- and Millennial-scale Rainfall Variability of the East Asian Summer Monsoon During the Last Deglaciation:Multi-proxy Evidence from Taiwan[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2016,450:38-49.
[40] HUANG R H,HUANG G,WEI Z G.Climate Variations of the Summer Monsoon over China[M]∥CHANG C P.East Asian Monsoon.Singapore:World Scientific Publishing Co. Ltd.,2004:213-270.

相似文献/References:

备注/Memo

备注/Memo:
收稿日期:2019-04-25; 修回日期:2019-05-28投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41672170); 福建省自然科学基金项目(2017J01654); 福建省高校新世纪优秀人才支持计划项目
作者简介:马 乐(1995-),男,山西孝义人,理学硕士研究生,E-mail:1372350526@qq.com。
*通讯作者:姜修洋(1981-),男,山东临沂人,教授,博士研究生导师,理学博士,E-mail:xyjiang@fjnu.edu.cn。
更新日期/Last Update: 2019-09-19