Vegetation and Climate Inferred from Pollen Record in East Asian Region During MIS 5: A Review
Received date: 2019-02-20
Revised date: 2019-04-10
Online published: 2019-07-04
Supported by
Project supported by the National Natural Science Foundation of China “Late Quaternary environmental change inferred from a high-resolution pollen record in the Mu Us Desert, China” (No.41571186) and “Research on extinction of rivers and lakes and aeolian landform evolution in Mu Us Desert since the Late Quaternary”(No.41330748)
The last interglacial, Marine Isotope Stage 5 (MIS 5, about 71~128 ka BP), is the closest to modern interglacial period, in which there are identifiable patterns that could give us clues into what will happen in the future. Pollen analysis, the study of fossil pollen and spores, is one of the key methods for the reconstruction of past vegetation and environment. Pollen data from 23 sites in eastern Asian region were reviewed to document regional patterns of vegetation and climate change during MIS 5 and to understand the large-scale controls on these changes. The regional patterns of vegetation during MIS 5 can be compared with the present-day vegetation. The climate, inferred from pollen record, was not stable during MIS 5. The substages (5a, 5b, 5c, 5d and 5e) of MIS 5 can be identi?ed by pollen assemblages in some areas, which describe the imprint of orbital-scale climate oscillations. East Asian monsoons have significantly contributed to the environment of modern eastern Asian monsoon region during MIS 5. However, the climate in Japan is also affected by the ocean currents and westerly circulation. The climate of the Tibetan Plateau is controlled by interactions of competing factors, including Indian monsoons, westerlies, and topography. In eastern Asian region, particularly in arid and semi-arid regions, the high-resolution pollen records need to be further studied for the better understanding of the climate change.
Key words: MIS 5; Pollen record; Vegetation and climate; Eastern Asia.
Congwen Luo , Yuzhen Ma , Kai Wang , Dandan Li . Vegetation and Climate Inferred from Pollen Record in East Asian Region During MIS 5: A Review[J]. Advances in Earth Science, 2019 , 34(5) : 540 -551 . DOI: 10.11867/j.issn.1001-8166.2019.05.0540
1 | Linsley B K . Oxygen-isotope record of sea level and climate variations in the Sulu Sea over the past 150, 000 years[J]. Nature, 1996, 380(6 571): 234-237. |
2 | Shen Caiming , Tang Lingyu , Wang Sumin , et al . Pollen records and time scale for the RM core of the Zoige Basin, northeastern Qinghai-Tibetan Plateau[J]. Chinese Science Bulletin, 2005, 50(6): 553-562. |
3 | Ge Yonggang , Wei Mingjian . Comparison of climate and environment change of the last interglacial period and Holocene in Beijing area, China[J]. International Journal of Geosciences, 2014, 5(8): 852-862. |
4 | Mu Huishuang , Xu Qinghai , Zhang Shengrui , et al . Pollen-based quantitative reconstruction of the paleoclimate during the formation process of Houjiayao Relic Site in Nihewan Basin of China[J]. Quaternary International, 2015, 374(3): 76-84. |
5 | Wang Zhaoduo , Huang Chunchang , Zhou Yali , et al . Characteristics of Holocene Loess-Palaeosol particle size composition and paleoclimatic significance in East Guanzhong,Shaanxi Province[J]. Advances in Earth Science, 2018, 33(3): 293-304. |
5 | 王兆夺, 黄春长, 周亚利, 等 . 关中东部全新世黄土—古土壤序列粒度组分变化特征及古气候意义[J]. 地球科学进展, 2018, 33(3): 293-304. |
6 | You Defang , Wang Rujian , Xiao Wenshen . Correlations between biogenic components and dust input and their change mechanism on Hess Rise, Central North Pacific, during the Late Quaternary[J]. Advances in Earth Science, 2018, 33(11): 1 203-1 214. |
6 | 由德方, 王汝建, 肖文申 . 北太平洋中部赫斯海隆(Hess Rise)晚第四纪以来生源组分与粉尘输入的关系及其变化机制[J]. 地球科学进展, 2018, 33(11): 1 203-1 214. |
7 | Imbrie J , Hays J D , Martinson D G , et al . The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ18O record[J]. Milankovitch and Climate, 1984, 126(1):269-305. |
8 | Hays J D , Imbrie J , Shackleton N J . Variations in the Earth's orbit: Pacemaker of the ice ages[J]. Science, 1976, 194(4 270): 1 121-1 132. |
9 | Kukla G J . Pleistocene land-sea correlations. I. Europe[J]. Earth Science Reviews, 1977, 13(4): 307-374. |
10 | Martinson D G , Pisias N G , Hays J D , et al . Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300, 000-year chronostratigraphy[J]. Quaternary Research, 1987, 27(1): 1-29. |
11 | Dansgaard W , Johnsen S J , Clausen H B , et al . Evidence for general instability of past climate from a 250-kyr ice-core record[J]. Nature, 1993, 364(6 434): 218-220. |
12 | Andersen K K , Azuma N , Barnola J M , et al . High-resolution record of Northern Hemisphere climate extending into the last interglacial period[J]. Nature, 2004, 431(7 005): 147-151. |
13 | Lu Huayu , Vandenberghe J , Miao Xiaodong , et al . Evidence for an abrupt climatic reversal during the Last Interglacial on the northeast Qinghai-Tibetan Plateau[J]. Quaternary International, 2006, 154: 136-140. |
14 | Pei Qiaomin , Ma Yuzhen , Hu Caili , et al . Climatic character of Marine Isotope Stage (MIS) 5e in the representative regions of the world: A review[J]. Advances in Earth Science, 2016, 31(11): 1 182-1 196. |
14 | 裴巧敏, 马玉贞, 胡彩莉, 等 .全球典型地区MIS 5e阶段气候特征研究进展[J]. 地球科学进展, 2016, 31(11): 1 182-1 196. |
15 | Johnsen S J , Clausen H B , Dansgaard W ,et al . The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability[J]. Journal of Geophysical Research Atmospheres, 1997, 1 022(C12):26 397-26 410. |
16 | An Zhisheng , Porter S C . Millennial-scale climatic oscillations during the last interglaciation in central China[J]. Geology, 1997, 25(7): 603-606. |
17 | Chen Fahu , Qiang Mingrui , Feng Zhaodong , et al . Stable East Asian monsoon climate during the Last Interglacial (Eemian) indicated by paleosol S1 in the western part of the Chinese Loess Plateau[J]. Global and Planetary Change, 2003, 36(3): 171-179. |
18 | Wang Yongjin , Cheng Hai , Edwards R L , et al . Millennial- and orbital-scale changes in the East Asian monsoon over the past 224, 000 years[J]. Nature, 2008, 451(7 182): 1 090-1 093. |
19 | Hayashi R , Takahara H , Tanida K , et al . Vegetation response to East Asian monsoon fluctuations from the penultimate to last glacial period based on a terrestrial pollen record from the inland Kamiyoshi Basin, western Japan[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2009, 284(3): 246-256. |
20 | Hayashi R , Takahara H , Inouchi Y , et al . Vegetation and endemic tree response to orbital-scale climate changes in the Japanese archipelago during the last glacial-interglacial cycle based on pollen records from Lake Biwa, western Japan[J]. Review of Palaeobotany and Palynology, 2017, 241: 85-97. |
21 | Takahara H , Kitagawa H . Vegetation and climate history since the last interglacial in Kurota Lowland, western Japan[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2000, 155(1): 123-134. |
22 | Heusser L E . Northeast Asian pollen records for the last 150, 000 years from deep-sea cores V28-304 and RC14-99 taken off the Pacific coast of Japan[J]. Review of Palaeobotany and Palynology, 1990, 65(1): 1-8. |
23 | Heusser L , Morley J . Monsoon fluctuations over the past 350 kyr: High-resolution evidence from Northeast Asia/Northwest Pacific climate proxies (marine pollen and radiolarians)[J]. Quaternary Science Reviews, 1997, 16(6): 565-581. |
24 | Igarashi Y , Oba T . Fluctuations in the East Asian monsoon over the last 144 ka in the northwest Pacific based on a high-resolution pollen analysis of IMAGES core MD01-2421[J]. Quaternary Science Reviews, 2006, 25:1 447-1 459. |
25 | Sugaya M , Okuda M , Okada M . Quantitative paleoclimate reconstruction based on a 130 ka pollen record from the C9001C core off NE Japan[J]. Quaternary International, 2016, 397: 404-416. |
26 | Sun Xiangjun , Luo Yunli . Pollen record of the last 280 ka from deep sea sediments of the Northern South China Sea[J]. Science in China (Series D), 2001, 44(10): 879-888. |
27 | Zheng Zhuo , Huang Kangyou , Deng Yun , et al . A~200 ka pollen record from Okinawa Trough: Paleoenvironment reconstruction of glacial-interglacial cycles[J]. Science in China (Series D), 2013, 56(10): 1 731-1 747. |
28 | Li Jie , Mei Xi , Li Rihui , et al . Environmental changes inferred from pollen records in the South Yellow Sea since late pleistocene[J]. Marine Geology & Quaternary Geology, 2014(4): 93-105. |
28 | 李杰, 梅西, 李日辉, 等 . 南黄海晚更新世以来孢粉记录的古环境变化[J]. 海洋地质与第四纪地质, 2014(4): 93-105. |
29 | Zheng Qiufeng , Zhang Maoheng , Li Jijun , et al . The climate and environment change of Shennongjia area recorded in the core of Dajiuhu Basin since the late Middle Pleistocene[J]. Geographical Research, 2014, 33(6): 1 167-1 177. |
29 | 郑秋凤, 张茂恒, 李吉均, 等 . 大九湖钻孔记录的神农架地区中更新世晚期以来的气候环境变化[J]. 地理研究, 2014, 33(6): 1 167-1 177. |
30 | Tang Zihua , Du Shusheng , Liu Fuliang . Late Pleistocene changes in vegetation and the associated human activity at Beiyao Site, Central China[J]. Review of Palaeobotany and Palynology, 2017, 244:107-112. |
31 | Cai Maotang , Wei Mingjian , Xu Dainan , et al . Vegetation and climate changes during three interglacial periods represented in the Luochuan loess-paleosol section, on the Chinese Loess Plateau[J]. Quaternary International, 2013, 296:131-140. |
32 | Xiao Jingyi , Chen Jianqiang , Xu Zheping ,et al . Characteristics of vegetation fluctuation as well as consequent impact on climate sicnce late Pleistocene in Handan area, Hebei[J]. Acta Sedimentologica Sinica, 2010, 28(6): 1 206-1 212. |
32 | 肖景义, 陈建强, 许哲平, 等 . 邯郸地区晚更新世以来植被波动特征及其对气候变化的响应[J]. 沉积学报, 2010, 28(6): 1 206-1 212. |
33 | Li Yusong , Chen Jianqiang , Zhao Shuo , et al . Spore-pollen assemblages in Tangshan area since late pleistocene with a correlation to those in adjacent areas[J]. Acta Geoscientica Sinica, 2011, 32(2): 178-188. |
33 | 李玉嵩, 陈建强, 赵硕, 等 . 唐山地区晚更新世以来的孢粉组合特征及其与邻区的对比[J]. 地球学报, 2011, 32(2): 178-188. |
34 | Yang Xiangdong , Wang Sumin , Tong Guobang , et al . The late Pleistocene pollen record in the lake sediments from ancient Heqing Lake and its significance for palaeoclimate[J]. Quaternary Sciences, 1998, 18(4): 335-343. |
34 | 羊向东, 王苏民, 童国榜, 等 . 云南鹤庆古湖晚更新世的孢粉记录及其古气候学意义[J]. 第四纪研究, 1998, 18(4): 335-343. |
35 | Bian Yanming , Yu Jia , Shao Zhaogang , et al . Palynological assemblages in the Paiku Co Basin of Tibet since Late Pleistocene and their paleoclimatic significance[J]. Acta Geoscientica Sinica, 2013, (1): 87-94. |
35 | 边彦明, 余佳, 邵兆刚, 等 . 西藏佩枯错盆地晚更新世以来的孢粉组合特征及其古气候意义[J]. 地球学报, 2013, (1): 87-94. |
36 | Yang Qinghua , Hou Xianhua , Yang Zhenjing , et al . Vegetation characteristics and environmental changes since the last interglacial period in Western Qaidam Basin[J]. Journal of Mountain Science, 2017, (5): 141-151. |
36 | 杨庆华, 侯献华, 杨振京, 等 . 柴达木盆地西部末次间冰期以来植被特征及其环境变化[J]. 山地学报, 2017, (5): 141-151. |
37 | Yang Jinsong . Records on Paleoenvironment in the Downstream of Salawusu River Valley Since 150 ka BP[D]. Beijing: Chinese Academy of Geologecal Sciences, 2013. |
37 | 杨劲松 . 萨拉乌苏河流域下游150 ka BP以来的古环境记录[D]. 北京:中国地质科学院, 2013. |
38 | Wang Liyuan , Xin Wei , Cheng Jie . Sporopollen assemblages and climate changes since the late quaternary at Qingtu Lake in northwestern margin of Tengger Desert [J]. Journal of Palaeogeography , 2014, 16(2): 239-248. |
38 | 王丽媛, 辛蔚, 程捷 . 腾格里沙漠西北缘青土湖晚第四纪孢粉组合特征与环境变迁[J]. 古地理学报, 2014, 16(2): 239-248. |
39 | Zheng Zhuo , Lei Zuoqi . Paleoflora and paleoecology during the last 400,000 years in the volcanic terrace of the Leizhou Peninsula[J]. Sun Yatsen University Forum, 1992,(1): 147-160. |
39 | 郑卓, 雷作淇 . 雷州半岛南部近40万年以来的古植被与古生态—田洋湖钻孔孢粉数值分析[J]. 中山大学学报论丛, 1992, (1): 147-160. |
40 | Wang Zhanghua , Zhao Baocheng , Chen Jing , et al . Chronostratigraphy and two transgressions during the Late Quaternary in Changjiang Delta area[J]. Journal of Palaeogeography, 2008, 10(1): 99-110. |
40 | 王张华, 赵宝成, 陈静, 等 . 长江三角洲地区晚第四纪年代地层框架及两次海侵问题的初步探讨[J]. 古地理学报, 2008, 10(1): 99-110. |
41 | Cheng Hai , Edwards R L , Sinha A , et al . The Asian monsoon over the past 640,000 years and ice age terminations[J]. Nature, 2016, 534(7 609): 640-646. |
42 | Chen Fahu , Wu Duo , Chen Jianhui , et al . Holocene moisture and East Asian summer monsoon evolution in the northeastern Tibetan Plateau recorded by Lake Qinghai and its environs: A review of conflicting proxies[J]. Quaternary Science Reviews, 2016, 154: 111-129. |
43 | Goldsmith Y , Broecker W S , Xu Hai , et al . Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales[J]. Proceedings of the National Academy of Sciences, 2017, 114(8): 1 817-1 821. |
44 | Liu Jianbao , Chen Shenqian , Chen Jianhui , et al . Chinese cave δ18O records do not represent northern East Asian summer monsoon rainfall[J]. Proceedings of the National Academy of Science, 2017, 114(15): 2 987-2 988. |
45 | Thompson L G , Yao Tandong , Davis M E , et al . Tropical climate instability: The last glacial cycle from a Qinghai-Tibetan Ice Core[J]. Science, 1997, 276(5 320):1 821-1 825. |
46 | Berger A L . Long-term variations of caloric insolation resulting from the earth’s orbital elements[J]. Quaternary Research, 1978, 9(2):139-167. |
47 | Yao Tandong , Shilong Piao , Shen Miaogen , et al . Chained impacts on modern environment of interaction between westerlies and Indian Monsoon on Tibeta Plateau[J]. Bulletin of Chinese Academy of Sciences,2017, 32(9): 976-984. |
47 | 姚檀栋, 朴世龙, 沈妙根, 等 . 印度季风与西风相互作用在现代青藏高原产生连锁式环境效应[J]. 中国科学院院刊, 2017, 32(9):976-984. |
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