[1]侯晨阳a,b,靳建辉a,等.末次冰消期以来福建福宁湾钻孔的粒度特征及其环境指示意义[J].山地学报,2023,(5):621-633.[doi:10.16089/j.cnki.1008-2786.000775]
　HOU Chenyanga,b,JIN Jianhuia,et al.Grain Size Characteristics of Boreholes in Funing Bay, China and Their Environmental Indications since the Last Deglaciation Period[J].Mountain Research,2023,(5):621-633.[doi:10.16089/j.cnki.1008-2786.000775]
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末次冰消期以来福建福宁湾钻孔的粒度特征及其环境指示意义
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2023年第5期
页码:
621-633
栏目:
山地环境
出版日期:
2023-11-15

文章信息/Info

Title:
Grain Size Characteristics of Boreholes in Funing Bay, China and Their Environmental Indications since the Last Deglaciation Period
文章编号:
1008-2786-(2023)5-621-13
作者:
侯晨阳a;  b; 靳建辉a;  b*; 邱俊杰a;  b; 卫俊杰a;  b; 许岱玉a;  b
(福建师范大学 a.福建省亚热带资源与环境重点实验室,福州 350007; b.地理科学学院,福州 350108)
Author(s):
HOU Chenyanga; b; JIN Jianhuia; b*; QIU Junjiea; b; WEI Junjiea; b; XU Daiyua; b
(a. Key Laboratory for Subtropical Resources and Environment, Fuzhou 350007; b. School of Geographical Sciences, Fuzhou 350108, Fujian Normal University, China)
关键词:
粒度;  端元分析;  环境演变;  福建福宁湾
Keywords:
grain size;  end-member analysis(EMA);  environmental evolution;  Funing Bay
分类号:
K903
DOI:
10.16089/j.cnki.1008-2786.000775
文献标志码:
A
摘要:
海岸沉积物是记录海-陆-气相互作用下区域古环境变化的重要载体。因短历时古气候事件发生时间短、各物质载体和代用指标都存在一定不足,对华南海岸带沉积物研究多探讨其与海平面波动等长时间尺度上的关系,限制了对粒度信息中可能记录的短期气候事件的深入研究,不利于解译古气候与古人类历史。本研究选取福建霞浦福宁湾FN1钻孔0～8 m部分,以光释光年代标尺为基础,使用粒度作为主要环境代用指标,并通过端元分析、主成分和相关性分析方法,阐明福建东北沿海地区沉积物粒度特征; 再结合TOC/TN含量变化,探讨其环境指示意义。结果表明:(1)钻孔0～8 m沉积物以粉砂为主,不同沉积相中各粒级百分比含量波动较大,根据粒径变化趋势和各粒度参数变化曲线分为U1 、U2、U3三层。(2)根据BasEMMA方法选取3个端元进行分析。其中,EM1代表低能沉积条件,以粉砂为主,是受冬季风影响的敏感组分,可指示冬季风强度变化; EM2代表中能沉积条件,出现粒级、TOC/TN及沉积速率的突变。受东亚冬季风影响,陆源物质含量增加; EM3代表高能沉积条件,区域水动力增强,沉积物粗颗粒含量增加; 高能与低能条件的频繁变化使沉积过程变得复杂,形成海陆过渡相。(3)3.9 ka B.P.～3.7 ka B.P.、 1.4 ka B.P.～1.2 ka B.P. 以及距今约500 a以来,沉积物粒度与TOC/TN均出现明显变化。与前人对东亚季风与ENSO变化的研究对比发现,环境代用指标的突变与华南沿海在该时段发生的风暴潮频率密切相关,可能对该地区人类生活居住产生严重威胁,进而影响区域文化演替,这表明沉积物粒度特征和TOC/TN含量变化特征等具有指示区域人类活动和环境演变的潜力。本研究可以为古环境重建和人类文化研究提供支持。
Abstract:
As the key zone of sea-land-air interaction, the coastal zone of South China has developed coastal sediments with a scale of thousands of years in evolution history, which is an important carrier to accurately record the regional paleoenvironment changes under the sea-land-air interaction. There were lots of scientific discussion about coastal sediments of South China in association with sea level fluctuation on a long-term scale, but hardly involving with short-term paleoclimatic events which may be recorded by granularity information in the coastal sediments on a particle-size scale. Because short-duration paleoclimate events occurred in a short time and their occurrences were difficult to be accurately determined, and available material carriers and proxy indicators in sediments, all of which prevented scientists from comprehensively interpreting and understanding paleoclimate and paleoanthropology.
Sediment grain size is an effective index for paleoenvironment reconstruction. The granularity end-member analysis(EMA)method can isolate sensitive components from complex granularity data and is widely used in paleoclimate research.
In this study, the 0-8 m segment of samples at FN1 borehole in Funing Bay, Xiapu, Fujian was selected for test. Based on photoluminescence dating scale, and sediment granularity as main environmental proxy index, it elucidates the characteristics of sediment grain size by means of end-member analysis, principal component analysis and correlation analysis; then by combined with the change of TOC/TN content, it discussed the significance of environmental indication.
It found that(1)The sediments from 0-8 m in the borehole were dominated by silt, with widely fluctuated percentage content of each grain size in different sedimentary phases. And it can be divided into three sections(U1, U2 and U3)according to the grain size trend and the curve of grain size parameters.(2)Three end-members were selected for analysis by BasEMMA method. Among them, EM1 represented low-energy deposition conditions, dominated by fine silt, which was a sensitive to East Asia winter monsoon(EAWM), a indicative of intensity of EAWM. EM2 represented medium-energy deposition conditions, suggesting possible mutations in grain size, TOC/TN and deposition rate. Due to East Asian monsoon, it brought out an increase in terrigenous geomaterial. EM3 represented high-energy deposition conditions, manifested as enhanced regional hydrodynamics and increased sediment coarse-grained content. Frequent shifts in high-energy and low-energy conditions complicated sedimentary processes and formed sea-land transition phase.(3)From 3.9 ka B.P. to 3.7 ka B.P., from 1.4 ka B.P. to 1.2 ka B.P. and about 500 years ago, the grain size and TOC/TN of sediments changed significantly. By comparison with previous studies on East Asian monsoon and ENSO changes, it revealed that abrupt changes in environmental proxies was closely related to the frequency of storm surges occurring along the coast of South China in the same period, which might pose a serious threat to habitation in the region, and consequently affected the regional cultural succession, suggesting that characteristics such as sediment grain size characteristics and changes in the content of TOC/TN have the potential to be indicative of regional human activities and environmental evolution.
This study can support paleoenvironmental reconstruction and human cultural studies for the coastal zone of South China.

参考文献/References:

[1] 吴正, 吴克则, 黄山, 等. 华南沿海全新世海岸沙丘研究[J]. 中国科学(B辑: 化学, 生命科学, 地学), 1995(2): 211-218. [WU Zheng, WU Keze, HUANG Shan, et al. Study on Holocene coastal sand dunes off south China coast [J]. Science in China(Series B: Chemistry, Life, Sciences Geoscience), 1995(2): 211-218]
[2] 杨建明. 福建沿海晚第四纪泥炭形成的分期及其与气候、海面变化的关系[J]. 热带海洋, 1992, 11(1): 45-51. [YANG Jianming. The phases of peat formation and their relationships to climatic and sea-level changes in coastal area of Fujian during Late Quaternary [J]. Tropic Oceanology, 1992, 11(1): 45-51]
[3] 赵倩. 福建东部沿海流水剖面砂质沉积地球化学特征及其古环境意义[D]. 福州: 福建师范大学, 2013:7-18. [ZHAO Qian. Geochemical characteristics of the coastal sandy deposition and its paleoenvironment significance from liushui profile, eastern coast of Fujian province [D]. Fuzhou: Fujian Normal University, 2013: 7-18]
[4] 龚松柏, 李志忠, 苏晓玲, 等. 福建漳浦六鳌半岛海岸沙丘记录的风沙气候变化[J]. 华中师范大学学报(自然科学版), 2014, 48(3): 448-455. [GONG Songbai, LI Zhizhong, SU Xiaoling, et al. The sandstorm climate change indicated by coastal dune at Liuao peninsula of Zhangpu county in Fujian province [J]. Journal of Huazhong Normal University(Natural Science), 2014, 48(3): 448-455] DOI: 10.19603/j.cnki.1000-1190.2014.03.028
[5] 于俊杰, 彭博, 兰佑, 等. 孢粉证据揭示MIS5a以来福建东北沿海地区人类活动、海平面及气候变化[J]. 地球科学, 2021, 46(1): 281-292. [YU Junjie, PENG Bo, LAN You, et al. Palynological record revealed anthropogenic deforestation, sea level and climate changes since Marine Isotope Stage 5a in the northeastern coast of Fujian province [J]. Earth Science, 2021, 46(1): 281-292] DOI: 10.3799/dqkx.2019.264
[6]马明明, 刘秀铭, 周国华, 等. 福建沿海地区晚第四纪海侵研究进展及存在的问题[J]. 亚热带资源与环境学报, 2016, 11(3): 9-19. [MA Mingming, LIU Xiuming, ZHOU Guohua, et al. A review of late quaternary transgression studies and some basic questions in Fujian coastal area [J]. Journal of Subtropical Resources and Environment, 2016, 11(3): 9-19] DOI: 10.19687/j.cnki.1673-7105.2016.03.002
[7] ROLETT B V, ZHENG Z, YUE Y F. Holocene sea-level change and the emergence of Neolithic seafaring in the Fuzhou basin(Fujian, China)[J]. Quaternary Science Reviews, 2011, 30(7): 788-797. DOI: 10.1016/j.quascirev.2011.01.015
[8] WANG Z H, RYVES D B, SHAO L, et al. Middle Holocene marine flooding and human response in the south Yangtze coastal plain, east China [J]. Quaternary Science Reviews, 2018, 187: 80-93. DOI: 10.1016/j.quascirev.2018.03.001
[9] LI Pingyuan, LI Mingkun, GAN Huayang, et al. A preliminary study on sediment records of possible typhoon in the northern South. China Sea during the past 6500 yr [J]. The Holocene, 2021, 31(7): 1221-1228. DOI: 10.1177/09596836211003229
[10] 赵松, 常凤鸣, 李铁刚, 等. 粒度端元法在东海内陆架古环境重建中的应用[J]. 海洋地质与第四纪地质, 2017, 37(3): 187-196. [ZHAO Song, CHANG Fengming, LI Tiegang, et al. The application of grain-size end member algorithm to paleoenvironmental reconstruction on inner shelf of East China Sea [J]. Marine Geology and Quaternary Geology, 2017, 37(3): 187-196] DOI: 10.16562/j.cnki.0256-1492.2017.03.019
[11] 白雪, 杨振京, 毕志伟, 等. 银川盆地第四纪沉积物粒度特征及其沉积环境[J]. 山地学报, 2017, 35(6): 874-881. [BAI Xue, YANG Zhenjing, BI Zhiwei, et al. Grain size characteristics and its depositional environment of Quaternary sediments in Yinchuan Plain, northwest China [J]. Mountain Research, 2017, 35(6): 874-881] DOI: 10. 16089/j.cnki.1008-2786.000289
[12] LI Yunhai, LI Haidong, QIAO Lei, et al. Storm deposition layer on the Fujian coast generated by Typhoon Saola(2012)[J]. Scientific Reports, 2015, 5(1): 14904. DOI: 10.1038/srep14904
[13] HARRIS C K, WIBERG P. Across-shelf sediment transport: Interactions between suspended sediment and bed sediment [J]. Journal of Geophysical Research: Oceans, 2002, 107(C1): 3008. DOI: 10.1029/2000JC000634
[14] 高文婷, 王斌, 彭俊, 等. 腾格里沙漠南缘风积物粒度空间分布及物源指示[J]. 水土保持研究, 2022, 29(6): 129-137. [GAO Wenting, WANG Bin, PENG Jun, et al. Spatial distribution of granularity parameter and provenance indication of aeolian deposits on the southern margin of the Tengger Desert [J]. Research of Soil and Water Conservation, 2022, 29(6): 129-137] DOI: 10.13869/j.cnki.rswc.2022.06.029
[15] 肖春晖, 王永红, 林间. 近1 Ma以来帕里西维拉海盆沉积物物源和古气候: 粒度和黏土矿物特征的指示[J]. 沉积学报, 2022, 40(2): 508-524. [XIAO Chunhui, WANG Yonghong, LIN Jian. Provenance and paleoclimate of sediments in the Parece Vela Basin in past 1 Ma: Inferences from grain-size and clay mineral distribution [J]. Acta Sedimentologica Sinica, 2022, 40(2): 508-524] DOI: 10.14027/j.issn.1000-0550.2020.091
[16] 文星跃, 吴勇, 黄成敏, 等. 岷江上游晚更新世黄土粒度与元素组成特征及其物源指示意义[J]. 山地学报, 2019, 37(4): 488-498. [WEN Xingyue, WU Yong, HUANG Chengmin, et al. Grain size and elements composition characteristics and their implications for provenance of the Late Pleistocene Loess in the upper reaches of the Minjiang River, China [J]. Mountain Research, 2019, 37(4): 488-498] DOI: 10. 16089/j.cnki.1008-2786.000441
[17] 王斌, 曾琳, 赵万苍, 等. 对黄土高原风尘搬运动力与沉积控制因素的新认识[J]. 中国沙漠, 2017, 37(2): 237-246. [WANG Bin, ZENG Lin, ZHAO Wancang, et al. New research progress of the transport dynamics and the accumulation factor of the aeolian dust in Chinese Loess Plateau [J]. Journal of Desert Research, 2017, 37(2): 237-246] DOI: 10.7522/j.issn.1000-694X.2017.00035
[18] 何继山, 梁杏, 李静, 等. 天津滨海平原区深孔沉积物环境敏感粒度提取及其意义[J]. 地球科学(中国地质大学学报), 2015, 40(7): 1215-1225. [HE Jishan, LIANG Xing, LI Jing, et al. Environmentally sensitive grain-size extraction of deep hole sediment from Tianjin costal plain and its significance [J]. Earth Science-Journal of China University of Geosciences, 2015, 40(7): 1215-1225] DOI: 10.3799/dqkx.2015.101
[19] 张晓东, 季阳, 杨作升, 等. 南黄海表层沉积物粒度端元反演及其对沉积动力环境的指示意义[J]. 中国科学: 地球科学, 2015, 45(10): 1515-1523. [ZHANG Xiaodong, JI Yang, YANG Zuosheng, et al. End member inversion of surface sediment grain size in the South Yellow Sea and its implications for dynamic sedimentary environments [J]. Science China: Earth Sciences, 2015, 45(10): 1515-1523] DOI: 10.1007/s11430-015-5165-8
[20] DING Yihui, CHAN J C L. The East Asian summer monsoon: An overview [J]. Meteorology and Atmospheric Physics, 2005, 89(1-4): 117-142. DOI: 10.1007/s00703-005-0125-z
[21] 孙丹丹, 刘平, 张杰, 等. 基于沉积成因地化元素指标的闽北海湾晚更新世海侵地层辨识及其意义[J]. 古地理学报, 2022, 24(1): 139-151. [SUN Dandan, LIU Ping, ZHANG Jie, et al. Identification and significance of the Late Pleistocene Transgressive strata in the bays of northern Fujian province based on geochemical element indicators of sedimentary origin [J]. Journal of Palaeography(Chinese Edition), 2022, 24(1): 139-151] DOI: 10.7605 /gdlxb.2022.01.011
[22] 童永福. 福建省第四系沉积概况[J]. 第四纪研究, 1985(1): 99-106. [TONG Yongfu. An outline of the Quaternary deposits of Fujian province [J]. Quaternary Sciences, 1985(1): 99-106]
[23] YUE Yuanfu, ZHENG Zhuo, ROLETT B V, et al. Holocene vegetation, environment and anthropogenic influence in the Fuzhou Basin, southeast China [J]. Journal of Asian Earth Sciences, 2015, 99: 1-48. DOI: 10.1016/j.jseaes.2014.12.004
[24] 郑荣章, 陈桂华, 徐锡伟, 等. 福州盆地埋藏晚第四纪沉积地层划分[J]. 地震地质, 2005, 27(4): 556-565. [ZHENG Rongzhang, CHEN Guihua, XU Xiwei, et al. Strata division of bured Late Quaternary of Fuzhou Basin [J]. Seismology and Geology, 2005, 27(4): 556-565]
[25] 马明明, 葛伟亚, 李春海, 等. 福建霞浦钻孔沉积物记录的约 7800a BP 以来海平面波动的磁学响应[J]. 第四纪研究, 2016, 36(5): 1307-1318. [MA Mingming, GE Weiya, LI Chunhai, et al. Magnetic responses to sea-level fluctuations since about 7800a B.P. recorded by core sediments at Xiapu, Fujian [J]. Quaternary Sciences, 2016, 36(5): 1307-1318] DOI: 10.11928/j.issn.1001-7410.2016.05.24
[26] 王雨灼. 福建省第四纪地层的划分[J]. 福建地质, 1990(4): 289-306. [WANG Yuzhuo. The classification of Quaternary strata in Fujian province [J]. Geology of Fujian, 1990(4): 289-306]
[27] JIN Jianhui, HUANG Yunming, LI Zhizhong, et al. Optically stimulated luminescence dating of coastal sediments at Funing Bay, southeastern China [J]. Geochronometria, 2019, 46(1): 15-24. DOI: 10.1515/geochr-2015-0103
[28] REN Yongqing, JIN Jianhui, HUANG Yunming, et al. Chronology of Last Glacial Maximum sediments in the coast of Fujian, south China [J]. Marine Geology, 2022, 451: 106884. DOI: 10.1016/j.margeo.2022.106884
[29] MEYERS P A. Preservation of elemental and isotopic source identification of sedimentary organic matter [J]. Chemical Geology, 1994, 114(3-4): 289-302. DOI: 10.1016/0009-2541(94)90059-0
[30] MEYERS P A. Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes [J]. Organic Geochemistry, 1997, 27(5-6): 213-250. DOI: 10.1016/S0146-6380(97)00049-1
[31] MEYERS P A. Applications of organic geochemistry to paleolimnological reconstructions: A summary of examples from the Laurentian Great Lakes [J]. Organic Geochemistry, 2003, 34(2): 261-289. DOI: 10.1016/S0146-6380(02)00168-7
[32] 程良清, 宋友桂, 李越, 等. 粒度端元模型在新疆黄土粉尘来源与古气候研究中的初步应用[J]. 沉积学报, 2018, 36(6): 1148-1156. [CHENG Liangqing, SONG Yougui, LI Yue, et al. Preliminary application of grain size end member model for dust source tracing of Xinjiang Loess and Paleoclimate reconstruction [J]. Acta Sedimentologica Sinica, 2018, 36(6): 1148-1156] DOI: 10.14027 /j.issn.1000-0550.2018.087
[33] 王思齐, 魏东岚, 张威. 末次冰期以来辽东半岛风沙沉积的粒度端元特征与古气候演变研究[J]. 第四纪研究, 2022, 42(2): 338-349. [WANG Siqi, WEI Donglan, ZHANG Wei. The end-member characteristics of the grain size of the aeolian sand deposits in the Liaodong Peninsula since the last glacial period and the study on paleoclimate evolution [J]. Quaternary Sciences, 2022, 42(2): 338-349] DOI: 10.11928 /j.issn.1001-7410.2022.02.02
[34] 韩鹏, 刘兴起. 内蒙古中东部查干淖尔湖流域 7000 年以来的气候演变[J]. 第四纪研究, 2017, 37(6): 1381-1390. [HAN Peng, LIU Xingqi. The climate evolution inferred from Chagan-Nuur in middle-east part of Inner Mongolia since the last 7000 years [J]. Quaternary Sciences, 2017, 37(6): 1381-1390] DOI: 10.11928/j.issn.1001-7410.2017.06.20
[35] 聂军胜, 李曼. 柴达木盆地晚中新世河湖相沉积物粒度组成及其古环境意义[J]. 第四纪研究, 2017, 37(5): 1017-1026. [NIE Junsheng, LI Man. A grain size study on Late Miocene Huaitoutala section, Ne Qaidam Basin, and implications for Asian monsoon evolution [J]. Quaternary Sciences, 2017, 37(5): 1017-1026] DOI: 10.11928/ j.issn.1001-7410.2017.05.09
[36] 岳保静, 刘金庆, 刘健, 等. 渤海西缘YRD-1101孔晚更新世以来沉积物粒度特征及其环境变迁[J]. 中国地质, 2020, 47(3): 853-867. [YUE Baojing, LIU Jinqing, LIU Jian, et al. Grain size distribution of sediment of core YRD-1101 in the western margin of the modern Bohai Sea since the latest Pleistocene and its environmental change [J]. Geology in China, 2020, 47(3): 853-867] DOI: 10.12029/gc20200321
[37] ZHANG Xiaodong, WANG Hongmin, XU Shumei, et al. A basic end-member model algorithm for grain-size data of marine sediments [J]. Estuarine, Coastal and Shelf Science, 2020, 236: 106656. DOI: 10.1016/j.ecss.2020.106656
[38] PEARSON K. Notes on the History of Correlation [J]. Biometrika, 1920, 13(1): 25-45. DOI: 10.1130/GSAB-25-655
[39] UDDEN J A. Mechanical composition of clastic sediments [J]. Bulletin of the geological society of America, 1914, 25(1): 655-744.
[40] WENTWORTH C K. A scale of grade and class terms for clastic sediments [J]. The Journal of Geology, 1922, 30(5): 377-392. DOI: 10.1086/622910
[41] 皮仲, 李铁刚, 南青云. 中全新世以来南黄海岩心记录的沉积环境演变对东亚季风的响应[J]. 海洋地质前沿, 2016, 32(7): 1-10. [PI Zhong, LI Tiegang, NAN Qingyun. Environmental changes since Mid Holocene revealed by core Z1 in the South Yellow Sea and their response to East Asian monsoon [J]. Marine Geology Frontiers, 2016, 32(7): 1-10] DOI: 10.16028/j.1009-2722.2016.07001
[42] 曾从盛. 闽东北沿海晚第四纪海侵与海面变动[J]. 福建师范大学学报(自然科学版), 1997, 13(4): 94-101. [ZENG Congsheng. Transgressions and sea level changes along the northeast coast of Fujian during the Late Quaternary [J]. Journal of Fujian Teachers University(Natural Science), 1997, 13(4): 94-101]
[43] 王绍鸿, 杨建明, 曾从盛, 等. 福建沿海晚更新世以来的海平面变化[J]. 台湾海峡, 1994, 13(2): 166-175. [WANG Shaohong, YANG Jianming, ZENG Congsheng, et al. Sea level changes since Late Pleistocene along Fujian coast [J]. Jouranl of Oceanography in Taiwan Strait, 1994, 13(2): 166-175]
[44] 童永福, 徐书勇. 福建省沿海第四系与活动构造[J]. 福建地质, 1989(2): 81-99. [TONG Yongfu, XU Shuyong. The Quaternary and active fault in coastal area of Fujian [J]. Geology of Fujian, 1989(2): 81-99]
[45] VANDENBERGHE J. Grain size of fine-grained windblown sediment: A powerful proxy for process identification [J]. Earth-Science Reviews, 2013, 121: 18-30. DOI: 10.1016/j.earscirev.2013.03.001
[46] ZHANG Xilin, FAN Dejiang, TIAN Yuan, et al. Quantitative reconstruction of the East Asian Winter Monsoon evolution over the past 100 years: Evidence from high-resolution sedimentary records of the inner continental shelfof the East China Sea[J]. The Holocene, 2020, 30(7): 1-10. DOI: 10.1177/0959683620908661
[47] DONNELLY J P, WOODRUFF J D. Intense hurricane activity over the past 5,000 years controlled by El Nino and the West African monsoon [J]. Nature, 2007, 447(7143): 465-468. DOI: 10.1038/nature05834
[48] MOY C M, SELTZER G O, RODBELL D T, et al. Variability of El Nino/ Southern Oscillation activity at millennial timescales during the Holocene epoch [J]. Nature, 2002, 420(6912): 162-165. DOI: 10.1038/nature01194
[49] WANG Yongjin, CHENG Hai, EDWARDS R L, et al. The Holocene Asian monsoon: Links to solar changes and North Atlantic climate [J]. Science, 2005, 308(5723): 854-857. DOI: 10.1126/science.1106296
[50] YANCHEVA G, NOWACZYK N R, MINGRAM J, et al. Influence of the intertropical convergence zone on the East Asian monsoon [J]. Nature, 2007, 445(7123): 74-77. DOI: 10.1038/nature05431
[51] WANG Bin, WU Renguang, FU Xiouhua. Pacific-East Asian teleconnection: How does ENSO affect East Asian climate? [J]. American Meteorological Society, 2000, 13: 1517-1536. DOI: 10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO; 2
[52] WANG Bin, ZHANG Qin. Pacific-East Asian teleconnection. Part II: How the Philippine Sea anomalous anticyclone is established during El Ni?o development [J]. Journal of Climate, 2002, 15: 3252-3265. DOI: 10.1175/1520-0442(2002)015<3252:PEATPI>2.0.CO; 2
[53] 巢纪平, 张人禾. 热带海气相互作用波及其不稳定性[J]. 气象学报, 1990, 48(1): 46-54. [CHAO Jiping, ZHANG Renhe. The air-sea interaction waves in the tropics and their instabilities [J]. Acta Meteorologica Sinica, 1990, 48(1): 46-54]
[54] FENG Juan, CHEN Wen. Interference of the East Asian winter monsoon in the impact of ENSO on the East Asian summer monsoon in decaying phases [J]. Advances in Atmospheric Sciences, 2014, 31(2): 344-354. DOI: 10.1007/s00376-013-3118-8
[55] WANG Chunzai, WANG Xin. Classifying El Nino Modoki I and II by different impacts on rainfall in southern China and typhoon tracks [J]. Journal of Climate, 2013, 26(4): 1322-1338. DOI: 10.1175/JCLI-D-12-00107.1
[56] 潘爱军, 万小芳, 郭小钢, 等. 平潭岛外海浙闽沿岸流对2006年冬季风松弛的响应特征与机理[J]. 中国科学: 地球科学, 2012, 42(9): 1317-1328.[PAN Aijun, WAN Xiaofang, GUO Xiaogang, et al. Responses of the Zhe-Min coastal current adjacent to Pingtan Island to the wintertime monsoon relaxation in 2006 and its mechanism [J]. Science China: Earth Science, 2012, 42(9): 1317-1328] DOI: 10.1007/s11430-012-4429-9
[57] 王中波, 杨守业, 张志珣, 等. 东海陆架中北部沉积物粒度特征及其沉积环境[J]. 海洋与湖沼, 2012, 43(6): 1039-1049. [WANG Zhongbo, YANG Shouye, ZHANG Zhixun, et al. The grain size compositions of the surface sediments in the East China Sea: Indication for sedimentary environments [J]. Oceanologia et Limnologia Sinica, 2012, 43(6): 1039-1049]
[58] 管清玉, 潘保田, 邬光剑, 等. 末次冰期东亚季风快速波动的模式与成因[J]. 沉积学报, 2007, 25(3): 429-436. [GUAN Qingyu, PAN Baotian, WU Guangjian, et al. East Asian monsoon pattern and cause of rapid climate fluctuations during the last glacial [J]. Acta Sedimentologica Sinica, 2007, 25(3): 429-436] DOI: 10.14027/j.cnki.cjxb.2007.03.015
[59] 曾从盛. 福建沿海全新世海平面变化[J]. 台湾海峡, 1991, 10(1): 77-84. [ZENG Congsheng. Sea level variation along Fujian coast in Holocene [J]. Journal of Oceanography in Taiwan Strait, 1991, 10(1): 77-84]

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备注/Memo

备注/Memo:
收稿日期(Received date): 2023-01-27; 改回日期(Accepted date): 2023-10-16
基金项目(Foundation item): 国家自然科学基金(41301012); 福建省自然科学基金(2020J01185)[National Natural Science Foundation of China(41301012); Natural Science Foundation of Fujian Province(2020J01185)]
作者简介(Biography): 侯晨阳(2000-),女,山西运城人,硕士研究生,主要研究方向:释光测年与环境演变。[HOU Chenyang(2000-), female, born in Yuncheng,Shanxi province,M.Sc. candidate, research on luminescence dating and environmental change] E-mail:hcyang1116@163.com
*通讯作者(Corresponding author): 靳建辉(1981-),男,博士,副教授,主要研究方向:风沙地貌过程与环境演变,释光年代学方法与应用。[JIN Jianhui(1981-), male,Ph.D., associate professor, research on the process of aeolian geomorphology and environmental change, luminescence chronology] E-mail:geojjh@fjnu.edu.cn
更新日期/Last Update: 2023-09-30