The Holocene climatic evolution in Eastern China and its bearing on climatic events
-
摘要: 在格陵兰GISP2冰芯气候演化曲线及北半球30°～90°N全新世气候演化综合曲线的基础上，统合了中国东部地区近年获得的全新世洞穴石笋、黄土沉积、湖泊沉积等典型气候演化曲线，建立了全新世气候节律分期，划分了11个暖期（编号W1—W11），10个冷期（编号C1—C10）。以此为基础，首次将中国东部全新世发生的洪水、海进、海退、冰川、冰冻等各类气候事件进行对应性分析，确认了中国在全新世存在一个千年尺度的节律性气候演化特征。综合各类气候事件后显示，编号为C2、C4、C6的冷期降温幅度较大，分别对应于10、8.2、5.3 kaBP的强冷事件。编号为W5的暖期时段，对应于7.2 kaBP的大暖期。研究发现，全新世气候变化在中国东部产生了同步的陆海联动效应。Abstract: Based on the Holocene climate evolution curve constructed with the Greenland ice core GISP2 and the integrated climate curves at the latitude of 30°～90°N, as well as the climate evolutionary curves recently acquired from the Holocene cave stalagmites, loess and lake sediments, the Holocene climatic rhythm stages has been established by this paper for Eastern China, which consists of 11 warm periods (numbered W1-W11) and 10 cold periods (numbered C1-C10). Correspondingly, the analysis of Holocene climatic events, such as floods, transgressions, regressions, glaciers, freezing and other climate events in the eastern China is conducted. Evidence confirms that there is a millennium scale rhythmical climate evolution in China during the Holocene. The cooling periods numbered C2, C4 and C6 have showed the considerable cooling and may correspond to the cooling events in 10, 8.2 and 5.3 kaBP, respectively. The warming period numbered W5 is corresponding to the Megathermal around 7 kaBP. It indicates that the Holocene climate change in eastern China is obviously influenced by land-sea interactions.
-
-
![]()
图 1 中国东部全新世重要气候数据研究点分布位置
Figure 1. The distribution of research sites which recorded important Holocene climatic fluctuations in eastern China
![]()
图 2 中国东部全新世气候演化曲线
图中竖虚线代表降温期峰值，C1-C10为冷期编号。a. 格陵兰GISP2冰芯气候演化曲线[12]，曲线旁数字为Bond确定的降温期次；b. 北纬30°～90°N综合气候演化曲线[16]；c. 贵州省董哥洞石笋气候演化曲线[18]；d. 四川省红原泥炭腐殖质含量变化曲线[23]；e. 湖北省神农架大九湖泥炭沉积反映的温度变化曲线[24]；f. 陕西省岐山全新世黄土剖面磁化率曲线图[28]；g. 大兴安岭中段月亮湖沉积物反映的气候演化曲线[27]。
Figure 2. The Holocene climatic evolution curve of Eastern China
The horizontal dotted lines represent the mid-value of cooling periods, C1-C10 are the numbers of the cold periods.
表 1 全新世气候演化分期与洪水、海侵、海退、冰川、冰冻等气候事件年龄数据对应表
Table 1 The division of Holocene climatic evolution stages and their correlation with the dating data of flood events, transgression events, glaciation events and freezing events
事件类型 W1 C1 W2 C2 W3 C3 W4 C4 W5 C5 W6 C6 W7 C7 W8 C8 W9 C9 W10 C11 W11 参考文献 格陵兰GISP2冰芯降温事件 11.1 10.3 9.4 8.6 7.4 5.2 4.0 2.7 1.6 0.5 Bond等[12] 陕西岐山黄土剖面 10.8 7.5 5.0 4.0 3.0 张宗祜[28] 洪水事件 沂河、沭河流域 0.8，1.2 王江月[30] 汉江上游晏家棚 2.8～3.2 1.6～1.8 0.9～1.0 吉琳等[31] 河南安阳三杨庄 7.2～7.0 6.0～6.7 4.5 3.5 2.2～2.1 刘耀亮[32] 河南北洛河宜君段 7.4～7.6 5.0～5.8 4.0～4.2 Zhang Y Z[33] 二里头遗址 5.5～6.0 3.8～4.0 1.7～1.8 Zhang Y Z[33] 渭河支流石川 8.9～9.2 6.2～6.6 4.1～4.7 3.7～3.9 2.3～2.6 He Z等[34] 漆水河杨凌 4.0～4.3 3.0～3.1 黄春长等[35] 渭河天水 3.0～3.2 1.6～1.8 石彬楠等[36] 泾河高陵 4.0～4.2 2.8～3.2 顾洪亮等[37] 晋陕峡谷吉县 8.5～9.0 3.0～3.2 郝高建等[38] 晋陕峡谷马头关 3.0～3.4 1.7～1.9 刘雯瑾等[39] 晋陕峡谷柳林滩 10.2～10.8 9.6～10.6 刘雯瑾等[40] 晋陕峡谷龙门 2.9～3.2 1.7～1.8 0.61～0.77 石彬楠等[41] 菏泽 3.5～4.0 Yu S Y等[42] 平邑万寿湖 6.0 1.9 1.1，1.2 本文 海侵事件 贝壳沉积 5.4 3.0 2.5 周廷儒等[43] 大连地区 >7.0 3.4 1.5～2.0 刘国海等[44] 渤海湾BXZK13 8.7 雷雁翔等[45] 海退事件 东海QC2孔 8.2 5.3 韩喜彬等[46] 冰川
冰冻事件山东蒙山 10.0 8.2 5.3 王照波[8-10] 内蒙凉城 8.0 6.0 周廷儒等[43] 峰值年龄 11.3 10.9 10.5 10.0 9.6 9.1 8.5 8.2 7.2 6.2 5.8 5.3 4.5 4.2 3.5 2.8 2.1 1.5 1.0 0.5 气候事件 鳄鱼冰期 拦马冰期 湖沼沉积 万寿湖 清荣冰期 万寿湖 沙窝洪水 注：W编号为升温期，C编号为降温期；表中数据为年龄值，单位为ka。 
下载: 导出CSV
表 2 蒙山及周边全新世洪水事件光释光年龄
Table 2 OSLdating data of Holocene flood events in Mengshan and surrounding areas
采样位置 样品编号 岩性 U/(μg/g) Th/(μg/g) K/% 含水量/% 等效剂量/Gy 年龄/ka 误差/ka 平邑万寿湖畔
（35°31′31.28″N、117°40′09.47″E）WS01 粉细砂 1.83 10.93 1.88 22.81 7.2 1.9 ±0.2 WS02 中粗砂 2.14 10.73 1.91 19.14 23.4 6.0 ±0.6 兰溪峡谷上游
（35°33′37.25″N、117°49′48.33″E）QR01 中细砂 1.03 9.51 1.44 8.62 3.5 1.2 ±0.1 QR02 中细砂 1.21 9.38 1.61 2.83 3.6 1.1 ±0.1 注：中全新世大暖期（W5时段）之前的洪水沉积，极有可能由于大暖期的重大洪水事件的冲刷而不易保存，相应数据极为稀少。
下载: 导出CSV
-
[1] 徐馨. 全新世气候期划分初步综合[J]. 贵州地质, 1989(1):39-48 XU Xin. The preliminary study on division of Holocene climatic age [J]. Guizhou Geology, 1989(1): 39-48.
[2] 吕雁斌. 新疆东部巴里坤湖记录的全新世气候变化研究[D]. 兰州大学博士学位论文, 2011: 1-145 LV Yanbin. Holocene climate change recorded by Lake Balikun, eastern Xinjiang[D]. Doctor Dissertation of Lanzhou University, 2011: 1-145.
[3] Cohen K M, Finney D A, Glbbard P L, et al. The ICS international chronostratigraphic chart [J]. Episodes, 2013, 36(3): 199-204. doi: 10.18814/epiiugs/2013/v36i3/002
[4] 安芷生, 波特 S, 吴锡豪, 等. 中国中、东部全新世气候适宜期与东亚夏季风变迁[J]. 科学通报, 1993, 38(14):1302-1305 doi: 10.1360/csb1993-38-14-1302 AN Zhisheng, Peter S, WU Xihao, et al. Holocene climatic Optimum and East Asian Summer monsoon change in central and eastern China [J]. Chinese Science Bulletin, 1993, 38(14): 1302-1305. doi: 10.1360/csb1993-38-14-1302
[5] 杨仲康. 南北极与中国近海典型地区全新世气候变化与环境事件研究[D]. 中国科学技术大学博士学位论文, 2019: 11-13 YANG Zhongkang. Holocene climatic changes and environmental events in typical areas of Arctic, Antarctic and coastal China regions[D]. Doctor Dissertation of University of Science and Technology of China, 2019: 11-13.
[6] 王照波, 卞青, 李大鹏, 等. 山东蒙山第四纪冰川组合遗迹的发现及初步研究[J]. 地质论评, 2017, 63(1):134-142 WANG Zhaobo, BIAN Qing, LI Dapeng, et al. Discovery of the quaternary glacial relics in mount Mengshan, Shandong province [J]. Geological Review, 2017, 63(1): 134-142.
[7] 王照波, 张剑, 王江月, 等. 山东蒙山第四纪冰川遗迹光释光测年研究及冰期划分与对比[J]. 地质论评, 2017, 63(3):694-702 WANG Zhaobo, ZHANG Jian, WANG Jiangyue, et al. A study on Quaternary glaciation moraines in Mount Mengshan, Shandong province with Optically Stimulated Luminescence (OSL) and comparison of glacial period division [J]. Geological Review, 2017, 63(3): 694-702.
[8] 王照波, 王江月, 冯金华, 等. 山东蒙山全新世冰川遗迹的发现及确认: 来自宇生核素年龄证据[J]. 山东国土资源, 2018, 34(6):1-7 doi: 10.3969/j.issn.1672-6979.2018.06.001 WANG Zhaobo, WANG Jiangyue, FENG Jinhua, et al. Discovery and recognition of Holocene glacial remains in Mengshan mountain in Shandong province: evidences from cosmogenic isotopes dating Age [J]. Shandong Land and Resources, 2018, 34(6): 1-7. doi: 10.3969/j.issn.1672-6979.2018.06.001
[9] Wang Z B, Wang J Y, He L L, et al. Glacier relics of the last glacial and Holocene periods discovered in the middle-low mountains of Eastern China: sedimentary sequences and environmental evolution of Mengshan mountain in Shandong province since 80 ka [J]. Acta Geologica Sinica(English Edition), 2020, 94(1): 141-151.
[10] 王照波. 中国新生代冰川与环境演化[M]. 北京: 地质出版社, 2021: 105-113 WANG Zhaobo. Cenozoic Glaciers and Environmental Evolution in China[M]. Beijing: Geological Publishing House, 2021: 105-113.
[11] Bond G, Kromer B, Beer J, et al. Persistent solar influence on North Atlantic climate during the Holocene [J]. Science, 2001, 294(5549): 2130-2136. doi: 10.1126/science.1065680
[12] Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in north Atlantic Holocene and glacial climates [J]. Science, 1997, 278(5341): 1257-1266. doi: 10.1126/science.278.5341.1257
[13] Wanner H, Mercolli L, Grosjean M, et al. Holocene climate variability and change; a data-based review [J]. Journal of the Geological Society, 2015, 172(2): 254-263. doi: 10.1144/jgs2013-101
[14] An Z S. The history and variability of the East Asian paleomonsoon climate [J]. Quaternary Science Reviews, 2000, 19(1-5): 171-187. doi: 10.1016/S0277-3791(99)00060-8
[15] 王绍武, 谢志辉. 千年尺度气候变率的研究[J]. 地学前缘, 2002, 9(1):143-153 doi: 10.3321/j.issn:1005-2321.2002.01.018 WANG Shaowu, XIE Zhiping. climate variability at millennial time scales [J]. Earth Science Frontiers, 2002, 9(1): 143-153. doi: 10.3321/j.issn:1005-2321.2002.01.018
[16] Marcott S A, Shakun J D, Clark P U, et al. A reconstruction of regional and global temperature for the past 11, 300 years [J]. Science, 2013, 339(6124): 1198-1201. doi: 10.1126/science.1228026
[17] 施雅风, 崔之久, 李吉均, 等. 中国东部第四纪冰川与环境问题[M]. 北京: 科学出版社, 1989: 1-5 SHI Yafeng, CUI Zhijiu, LI Jijun, et al. Quaternary Glacial and Environmental Issues in Eastern China[M]. Beijing: Science Press, 1989: 1-5.
[18] 赵侃. 贵州董哥洞近1000年石笋纹层年代学与同位素气候重建[D]. 南京师范大学博士学位论文, 2011: 13-15 ZHAO Kan. Annually-counting chronology and isotopic climate reconstruction over the past millennia from stalagmites in Dongge cave[D]. Doctor Dissertation of Nanjing Normal University, 2011: 13-15.
[19] 黄俊华, 胡超涌, 周群峰, 等. 长江中游和尚洞石笋的高分辨率同位素、微量元素记录及古气候研究[J]. 沉积学报, 2002, 20(3):442-446 doi: 10.3969/j.issn.1000-0550.2002.03.013 HUANG Junhua, HU Chaoyong, ZHOU Qunfeng, et al. Study on high-resolution carbon, oxygen isotope and trace element record sand paleoclimate from Heshang Cave, the middle reach of the Yangtse river [J]. ActaSedimentologicaSinica, 2002, 20(3): 442-446. doi: 10.3969/j.issn.1000-0550.2002.03.013
[20] 董进国, 刁伟, 孔兴功. 湖北三宝洞石笋238U值变化的古气候意义[J]. 海洋地质与第四纪地质, 2013, 33(1):129-135 DONG Jinguo, DIAO Wei, KONG Xinggong. Variation in Uranium Isotopes of stalagmites from Sanbao Cave, Hubei province: implications for palaeoclimate [J]. Marine Geology & Quaternary Geology, 2013, 33(1): 129-135.
[21] 程海, 艾思本, 王先锋, 等. 中国南方石笋氧同位素记录的重要意义[J]. 第四纪研究, 2005, 25(2):157-163 doi: 10.3321/j.issn:1001-7410.2005.02.004 CHENG Hai, AI Siben, WANG Xianfeng, et al. Oxygen isotope records of stalagmites from Southern China [J]. Quaternary Sciences, 2005, 25(2): 157-163. doi: 10.3321/j.issn:1001-7410.2005.02.004
[22] 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. doi: 10.1016/j.jpgl.2005.01.036
[23] Yu X F, Zhou W J, Franzen L G, et al. High-resolution peat records for Holocene monsoon history in the eastern Tibetan Plateau [J]. Science in China:Series D, 2006, 49(6): 615-621. doi: 10.1007/s11430-006-0615-y
[24] Zhang W C, Yan H, Dodson J, et al. The 9.2 ka event in Asian summer monsoon area: the strongest millennial scale collapse of the monsoon during the Holocene [J]. Climate Dynamics, 2018, 50(7): 2767-2782.
[25] 宁凯. 巴丹吉林沙漠湖泊沉积孢粉和正构烷烃记录的全新世环境变化[D]. 兰州大学博士学位论文, 2018: 1-22 NING Kai. Holocene environmental evolution implied by pollen and N-alkanes in groundwater recharge lake, Badain Jaran desert, Northwestern China[D]. Doctor Dissertation of Lanzhou University, 2018: 1-22.
[26] 赵艳, 刘耀亮, 郭正堂, 等. 全新世气候渐变导致中亚地区植被突变[J]. 中国科学:地球科学, 2017, 60(7):1317-1327 doi: 10.1007/s11430-017-9047-7 ZHAO Yan, LIU Yaoliang, GUO Zhengtang, et al. Abrupt vegetation shifts caused by gradual climate changes in central Asia during the Holocene [J]. Science China Earth Sciences, 2017, 60(7): 1317-1327. doi: 10.1007/s11430-017-9047-7
[27] 李倩. 大兴安岭中段月亮湖记录的21kaBP以来高分辨率古气候变化: 来自TOC、TN及δ13Corg的证据[D]. 中国地质大学(北京)硕士学位论文, 2011: 1-66 LI Qian. A high resolution climate record of Moon Lake in the middle part of Daxing’an mountain range in Northwest China during the last 21ka: from evidence of TOC, TN and δ13Corg[D]. Master Dissertation of China University of Geoscience(Beijing), 2011: 1-66.
[28] 张宗祜. 中国北方晚更新世以来地质环境及未来生存环境变化趋势[J]. 第四纪研究, 2011, 21(3):208-217 ZHANG Zonghu. Geological environment since the late Pleistocene and the future environment evolution trend for existence in northern China [J]. Quaternary Science, 2011, 21(3): 208-217.
[29] 王艳娟. 关中西部地区全新世的气候环境演变[D]. 长安大学硕士学位论文, 2010: 38-40 WANG Yanjuan. The climatic evolution during the Holocene in the western of Guanzhong Region[D]. Master Dissertation of Chang’an University, 2010: 38-40.
[30] 王江月. “寒亭组”是山东唐宋时期两期洪水的产物: 基于沭河沙带调查及光释光测年研究[J]. 山东国土资源, 2019, 35(7):46-50 WANG Jiangyue. "Hanting Formation" is the product of two periods of Flood in Tang and Song dynasties in Shandong province: based on investigation and optical luminescence dating of Shuhe sand belt [J]. Shandong Land and Resources, 2019, 35(7): 46-50.
[31] 吉琳, 庞奖励, 黄春长, 等. 汉江上游晏家棚段全新世古洪水研究[J]. 地球科学进展, 2015, 30(4):487-494 JI Lin, PANG Jiangli, HUANG Chunchang, et al. Holocene palaeoflood studies of the Yanjiapeng reach in the upper Hanjiang River, China [J]. Advances in Earth Science, 2015, 30(4): 487-494.
[32] 刘耀亮. 河南三杨庄全新世以来的气候变化与洪水事件的沉积记录[D]. 河北师范大学硕士学位论文, 2013: 1-58 LIU Yaoliang. Holocene climate change and flood events documented by sedimentary record in Sanyangzhuang Site, Henan province, China[D]. Master Dissertation of Hebei Normal University, 2013: 1-58.
[33] Zhang Y Z, Huang C C, Tan Z H, et al. Prehistoric and historic overbank floods in the Luoyang Basin along the Luohe River, middle Yellow River basin, China [J]. Quaternary International, 2019, 521: 118-128. doi: 10.1016/j.quaint.2019.06.023
[34] He Z, Long H, Yang L H, et al. Luminescence dating of a fluvial sequence using different grain size fractions and implications on Holocene flooding activities in Weihe Basin, central China [J]. Quaternary Geochronology, 2019, 49: 123-130. doi: 10.1016/j.quageo.2018.05.007
[35] 黄春长, 庞奖励, 查小春, 等. 黄河流域关中盆地史前大洪水研究: 以周原漆水河谷地为例[J]. 中国科学:地球科学, 2011, 41(11):1658-1669 HUANG Chunchang, PANG Jiangli, ZHA Xiaochun, et al. Prehistorical floods in the Guanzhong basin in the Yellow River drainage area: a case study along the Qishuihe River valley over the Zhouyuan loess tableland [J]. Science Sinica(Terrae), 2011, 41(11): 1658-1669.
[36] 石彬楠, 黄春长, 庞奖励, 等. 渭河上游天水东段全新世古洪水水文学恢复研究[J]. 干旱区地理, 2016, 39(3):573-581 SHI Binnan, HUANG Chunchang, PANG Jiangli, et al. Hydrological reconstructions of the Holocene Palaeoflood in the Tianshui East Reach of the upper Weihe River [J]. Arid Land Geography, 2016, 39(3): 573-581.
[37] 顾洪亮, 黄春长, 周亚利, 等. 关中盆地杨官寨遗址古洪水事件释光测年[J]. 地理研究, 2012, 31(10):1837-1848 GU Hongliang, HUANG Chunchang, ZHOU Yali, et al. OSL dating study on the Palaeoflood events recorded in the Yangguanzhai Neolithic ruins in the Guanzhong basin [J]. Geographical Research, 2012, 31(10): 1837-1848.
[38] 郝高建, 黄春长, 刑莹莹, 等. 黄河晋陕峡谷吉县段全新世古洪水平流沉积特征研究[J]. 干旱区资源与环境, 2011, 25(3):106-112 HAO Gaojian, HUANG Chunchang, XING Yingying, et al. Sedimentary characteristics of the slackwater deposits of Holocene extreme floods in the FJJ section in the Yellow River valley, Ji County [J]. Journal of Arid Land Resources and Environment, 2011, 25(3): 106-112.
[39] 刘雯瑾, 黄春长, 庞奖励, 等. 黄河马头关段全新世古洪水水文恢复及气候背景研究[J]. 干旱区地理, 2017, 40(1):85-93 LIU Wenjin, HUANG Chunchang, PANG Jiangli, et al. Holocene Palaeoflood and climatic changes at the Matouguan Reach of the Yellow River [J]. Arid Land Geography, 2017, 40(1): 85-93.
[40] 刘雯瑾, 黄春长, 庞奖励, 等. 黄河柳林滩段全新世古洪水滞流沉积物物源研究[J]. 水土保持学报, 2016, 30(2):136-142 LIU Wenjin, HUANG Chunchang, PANG Jiangli, et al. Study on provenance of Holocene flood slackwater deposits in the Liulintan reach of the Yellow River [J]. Journal of Soil and Water Conservation, 2016, 30(2): 136-142.
[41] 石彬楠, 黄春长, 庞奖励, 等. 黄河龙门段商周转折时期的古洪水事件及气候背景[J]. 湖泊科学, 2017, 29(1):234-245 doi: 10.18307/2017.0125 SHI Binnan, HUANG Chunchang, PANG Jiangli, et al. Palaeoflood events and climate change at the turning time from the Shang to Zhou dynasty in the Longmen reach of the Yellow River [J]. Journal of Lake Sciences, 2017, 29(1): 234-245. doi: 10.18307/2017.0125
[42] Yu S Y, Hou Z F, Chen X X, et al. Extreme flooding of the lower Yellow River near the North grippian-Meghalayan boundary: evidence from the Shilipu archaeological site in southwestern Shandong Province, China [J]. Geomorphology, 2020, 350: 106878. doi: 10.1016/j.geomorph.2019.106878
[43] 周廷儒, 张兰生, 李华章. 华北更新世最后冰期以来的气候变迁[J]. 北京师范大学学报(自然科学版), 1982(1):77-88 ZHOU Yanru, ZHANG Lansheng, LI Huazhuang. The changes of climate in north China since the late glacial age of Pleistocene [J]. Journal of Beijing Normal University(Natural Science), 1982(1): 77-88.
[44] 刘国海, 高善明, 李元芳, 等. 大连地区全新世泥炭沉积环境及海面波动[J]. 地理研究, 1992, 11(4):38-46 LIU Guohai, GAO Shanming, LI Yuanfang, et al. Sea-level fluctuation and deposit environment of the Holocene peat in Dalian region [J]. Geographical Research, 1992, 11(4): 38-46.
[45] 雷雁翔, 何磊, 王玉敏, 等. 渤海湾西岸晚更新世以来的沉积环境演化及碳埋藏评价[J]. 海洋地质与第四纪地质, 2021, 41(6):194-205 LEI Yanxiang, HE Lei, WANG Yumin, et al. Environmental evolution and carbon burial assessment of the west coast of Bohai Bay since Late Pleistocene [J]. Marine Geology & Quaternary Geology, 2021, 41(6): 194-205.
[46] 韩喜彬, 李广雪, 杨子赓, 等. 中国东部陆架海对“新仙女木”事件的响应[J]. 海洋地质动态, 2005, 21(12):1-5 doi: 10.3969/j.issn.1009-2722.2005.12.001 HAN Xibin, LI Guangxue, YANG Zigeng, et al. The response of the continental shelf seas in eastern China to the “Younger Dryas” Event [J]. Marine Geology Letters, 2005, 21(12): 1-5. doi: 10.3969/j.issn.1009-2722.2005.12.001
[47] 张鹏, 杨劲松, 赵华, 等. 黄河流域全新世古洪水研究进展及展望[J]. 海洋地质与第四纪地质, 2020, 40(6):178-188 ZHANG Peng, YANG Jinsong, ZHAO Hua, et al. Research progress of the Holocene paleoflood in the Yellow River basin and a future prospect [J]. Marine Geology & Quaternary Geology, 2020, 40(6): 178-188.
[48] 顾家裕, 严钦尚, 虞志英. 苏北中部滨海平原贝壳砂堤[J]. 沉积学报, 1983, 1(2):47-59 GU Jiayu, YAN Qinshang, YU Zhiying. The cheniers of the northern coastal plain of Jiangsu province [J]. ActaSedimentologicaSinica, 1983, 1(2): 47-59.
[49] 姚菁. 渤海南岸LZ908孔海陆交互相地层气候代用指标及沉积环境研究[D]. 中国科学院研究生院(海洋研究所)博士学位论文, 2014: 30-32 YAO Jing. Climatic indicators and sedimentary environment studies inferred from transgressive and regressive sediments of core LZ908, south Bohai Sea[D]. Master Dissertation of Chinese Academy of Sciences (Institute of Oceanology), 2014: 30-32.
[50] 李凤林, 阎玉忠, 商志文, 等. 渤海西岸全新世气候演化与海陆变迁[J]. 地质学刊, 2014, 38(2):173-186 doi: 10.3969/j.issn.1674-3636.2014.02.173 LI Fenglin, YAN Yuzhong, SHANG Zhiwen, et al. Holocene climate evolution and land-sea changes on west Bohai Sea [J]. Journal of Geology, 2014, 38(2): 173-186. doi: 10.3969/j.issn.1674-3636.2014.02.173
[51] [52] 王可, 郑洪波, Prins M, 等. 东海内陆架泥质沉积反映的古环境演化[J]. 海洋地质与第四纪地质, 2008, 28(4):1-10 WANG Ke, ZHENG Hongbo, Prins M, et al. High-resolution paleoenvironmental record of the mud sediments of the East China Sea inner shelf [J]. Marine Geology & Quaternary Geology, 2008, 28(4): 1-10.
[53] 丁敏. 关中盆地东部与西部全新世成壤强度演变与气候变化高分辨率对比研究[D]. 陕西师范大学博士学位论文, 2015: 1-38 DING Min. The comparative study of Holocene pedogenic intensity evolution and High-resolution climate change in the eastern and western Guanzhong Basin[D]. Doctor Dissertation of Shanxi Normal University, 2015: 1-38.
[54] 陶士臣, 安成邦, 陈发虎, 等. 新疆托勒库勒湖孢粉记录的4.2 kaBP气候事件[J]. 古生物学报, 2013, 52(2):234-242 TAO Shichen, AN Chengbang, CHEN Fahu, et al. An abrupt climatic event around 4.2cal kaBP documented by fossil pollen of Tuolekule lake in the eastern Xinjiang Uyghur autonomous region [J]. ActaPalaeontologicaSinica, 2013, 52(2): 234-242.
[55] 吴文祥, 郑洪波, 侯梅, 等. 5.5cal.kaBP气候事件、人口增长、条件限制与中国史前复杂社会产生[J]. 中国科学:地球科学, 2018, 61(2):134-148 doi: 10.1007/s11430-017-9157-1 WU Wenxiang, ZHENG Hongbo, HOU Mei, et al. The 5.5cal kaBP climate event, population growth, circumscription and the emergence of the earliest complex societies in China [J]. Science China Earth Sciences, 2018, 61(2): 134-148. doi: 10.1007/s11430-017-9157-1
[56] 刘浴辉. 东亚季风区8.2kaBP气候突变记录及其精细解剖[D]. 中国地质大学博士学位论文, 2012: 1-66 LIU Yuhui. The abrupt climate change record of 8.2kaBP event from east Asian monsoon area with its characteristics analysis[D]. Doctor Dissertation of China University of Geoscience, 2012: 1-66.
[57] 崔英方, 董进国, 赵侃. 基于石笋记录的小冰期与“8.2 kaBP”事件的对比研究[J]. 中国岩溶, 2019, 38(1):40-49 CUI Yingfa, DONG Jin’guo, ZHAO Kan. A comparative study on the little ice age and the ‘8.2 kaBP’ event based on two stalagmite records from the Dongge cave, southwest China [J]. CarsologicaSinica, 2019, 38(1): 40-49.
[58] 王绍武. 8.2 kaBP冷事件[J]. 气候变化研究进展, 2008, 4(3):193-194 WANG Shaowu. 8.2 kaBP cold event [J]. Advances in Climate Change Research, 2008, 4(3): 193-194.
[59] Alley R B, Mayewski P A, Sowers T, et al. Holocene climatic instability: a prominent, widespread event 8200yr ago [J]. Geology, 1997, 25(6): 482-486.
[60] Dansgaard W, Johnsen S, Clausen H, et al. Evidence for general instability of past climate from a 250-kyrice-core record [J]. Nature, 1993, 364(6434): 281-220.
[61] 王绍武. 全新世大暖期[J]. 气候变化研究进展, 2011, 7(5):383-384 WANG Shaowu. Megathermal [J]. Advance in Climate Change Research, 2011, 7(5): 383-384.
[62] Renssen H, Seppä H, Heiri O, et al. The spatial and temporal complexity of the Holocene thermal maximum [J]. Nature Geoscience, 2009, 2(6): 411-414. doi: 10.1038/ngeo513
[63] 张风菊, 薛滨, 姚书春, 等. 全新世大暖期中国湖泊碳埋藏速率初步研究[J]. 第四纪研究, 2013, 33(2):401-402 doi: 10.3969/j.issn.1001-7410.2013.02.23 ZHANG Fengju, XUE Bin, YAO Shuchun, et al. The organic carbon burial rates in Chinese Lake sediments during Holocene megathermal [J]. Quaternary Sciences, 2013, 33(2): 401-402. doi: 10.3969/j.issn.1001-7410.2013.02.23
[64] 朱彤. 全新世大暖期7-5Ka. BP中国农业土地利用空间格局研究[D]. 甘肃农业大学硕士学位论文, 2019: 1-22 ZHU Tong. Study of the spatial pattern of agricultural land use of China in the Holocene Megathermal[D]. Master Dissertation of Gansu Agriculture University, 2019: 1-22.
[65] 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), 1994, 37(3):353-365 SHI Yafeng, KONG Zhaochen, WANG Sumin, et al. The climatic fluctuation and important events of Holocene Megathermal in China [J]. Science in China (Series B), 1994, 37(3): 353-365.
[66] 计宏祥. 中国全新世大暖期哺乳动物与气候波动[J]. 海洋地质与第四纪地质, 1996(1):5-16 JI Hongxiang. Paleoclimatic fluctuations and mammals in Holocene megathermal in China [J]. Marine Geology & Quaternary Geology, 1996(1): 5-16.
[67] 张振克, 吴瑞金, 王苏民, 等. 全新世大暖期云南洱海环境演化的湖泊沉积记录[J]. 海洋与湖沼, 2000, 31(2):210-214 doi: 10.3321/j.issn:0029-814X.2000.02.014 ZHANG Zhenke, WU Ruijin, WANG Sumin, et al. Environmental evolution recorded by lake sediments from Erhai Lake, Yunnan province in Holocene megathermal [J]. Oceanologia et LimnologiaSinica, 2000, 31(2): 210-214. doi: 10.3321/j.issn:0029-814X.2000.02.014
[68] 胡玉蓉, 颜家安. 海南岛全新世大暖期后的古气候波动分析[J]. 气象研究与应用, 2009, 30(4):42-44, 55 doi: 10.3969/j.issn.1673-8411.2009.04.012 HU Yurong, YAN Jiaan. Paleoclimate fluctuations analysis of Hainan islands after Holocene warm period [J]. Journal of Meteorological Research and Application, 2009, 30(4): 42-44, 55. doi: 10.3969/j.issn.1673-8411.2009.04.012
[69] 俞凯峰. 末次盛冰期和全新世大暖期中国北方沙地古气候定量重建探索[D]. 南京大学硕士学位论文, 2013:1-43. YU Kaifeng. A tentatively quantitative paleoclimate reconstruction of the dune fields of northern China during the Last Glacial Maximum and Holocene Optimum[D]. Master Dissertation of Nanjing University, 2013: 1-43.
[70] 王世进, 张富中, 孙天柱. 山东省平原地区第四纪全新世地层划分研究新进展[C]//地质与可持续发展: 华东六省一市地学科技论坛文集. 济南: 山东省科学技术协会, 2003: 26-28 .WANG Shijin, ZHANG Fuzhong, SUN Tianzhu. Study development on strata division of Quaternary Holocene in plain area, Shandong province[C]//Geology and Sustainable Development: Technology Forum Collection of Six Provinces and One City in East China. Ji’nan: Shandong Science and Technology Association, 2003: 26-28.
计量
- 文章访问数: 3432
- HTML全文浏览量: 1054
- PDF下载量: 110
