中亚干旱区第四系黄土和干旱环境研究进展

doi:10.11867/j.issn.1001-8166.2019.01.0034

地球科学进展 ›› 2019, Vol. 34 ›› Issue (1): 34 -47. doi: 10.11867/j.issn.1001-8166.2019.01.0034

中亚干旱区第四系黄土和干旱环境研究进展

王鑫 ¹(

),张金辉 ¹,贾佳 ^1, ²,王蜜 ¹,王强 ¹,陈建徽 ¹,王飞 ¹,李再军 ¹,陈发虎 ^1, ^3, ^*(

)

1. 兰州大学资源环境学院西部环境教育部重点实验室，甘肃兰州 730000
2. 浙江师范大学地理与环境科学学院，浙江金华 321004
3. 中国科学院青藏高原研究所，北京 100101

收稿日期:2018-11-27 修回日期:2018-12-28 出版日期:2019-01-10
通讯作者: 陈发虎 E-mail:xinw@lzu.edu.cn;fhchen@itpcas.ac.cn
基金资助:
国家自然科学基金项目“塔吉克盆地晚始新统—中新统风成沉积序列的年代学和古环境记录研究”(编号：41672158);国家重点研发计划项目“亚洲中部干旱区气候变化影响与丝路文明变迁研究”(编号：2018YFA0606404)

Pleistocene Loess-Paleosol Sequences in Arid Central Asia State of Art

Xin Wang ¹( ),Jinhui Zhang ¹,Jia Jia ^1, ²,Mi Wang ¹,Qiang Wang ¹,Jianhui Chen ¹,Fei Wang ¹,Zaijun Li ¹,Fahu Chen ^1, ^3, ^*( )

1. Key Laboratory of Western China's Environmental Systems, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
2. College of Geography and Environmental Sciences, Zhejiang Normal University, Zhejiang 321004, China
3. Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China

Received:2018-11-27 Revised:2018-12-28 Online:2019-01-10 Published:2019-03-05
Contact: Fahu Chen E-mail:xinw@lzu.edu.cn;fhchen@itpcas.ac.cn
About author:Wang Xin (1983-), male, Wuzhi County, He'nan Province, Associate professor. Research areas include quaternary geology and global change. E-mail: xinw@lzu.edu.cn |Chen Fahu (1962-), male, Danfeng County, Shaanxi Province, Professor, Academician of Chinese Academy of Sciences. Research areas include environmental change and the evolution of human civilization．E-mail: fhchen@itpcas.ac.cn
Supported by:
National Natural Science Foundation of China “Chronological and paleoenvironmental study on the late Eocene to Miocene aeoilan sequences in the Tajik Basin”(No. 41672158);The National Key R&D Program of China “Research on the impact of environmental changes in central Asia and the change of the Silk Road civilization”(No. 2018YFA0606404)

全文 ( 16 ) 下载PDF ( 1063 )

中亚黄土位于连接欧洲黄土和中国黄土的咽喉地带，黄土地层的古气候记录研究对完整认识地质时期欧亚大陆古气候的演化历史、空间差异和不同时间尺度上的主控因素，深入理解欧亚大陆西风—季风系统的相互作用机制有重要意义。然而，中亚黄土的研究程度与欧洲和中国黄土相比明显偏弱，尤其与中国黄土的对比研究亟待加强。综述了近些年中亚第四系黄土研究的主要进展，基于代表性剖面和中国黄土古气候记录粗框架的对比，讨论了中亚干旱区第四纪以来构造尺度上的干旱化过程，轨道尺度上的干湿变化历史和亚轨道尺度上的干湿变化及其与东亚季风区古气候变化的相位关系。

关键词: 黄土—古土壤, 古气候, 中亚干旱区, 第四纪

Loess of central Asia is located in a linkage zone between the European and Chinese loess depositional belts. Paleoclimate signatures from loess-paleosol sequences here is a key for completely understanding the spatial-tempo paleoclimate changes of Euro-Asia and for understanding the interactions between westerlies and Asia monsoon system during geological time. However, paleoclimate investigations of loess-paleosol sequences in arid central Asia is relatively weak than those from Europe and Chinese Loess Plateau. Specific, correlations of paleoclimate records with Chinese loess is required for better understanding “westerly regimes” in central Asia and its phase relationship with monsoon Asia on various time scale. In this work, we reviewed new advantages of loess study in central Asia during the last decades. Based on the stratigraphic and paleoclimatic correlations of loess-paleosol sequences between central Asia and the Chinese Loess Plateau, we discussed aridification history of Asia on tectonic time scale, the hydroclimate changes in arid central Asia and its phase relationship with Monsoonal Asia on orbital and millennial time scale during the Pleistocene.

Key words: Loess-Paleosol, Paleoclimate, Arid Central Asia, Pleistocene.

中图分类号:

P532

图1 亚洲内陆气候格局和本文涉及的黄土剖面位置

Fig. 1 Major climate regimes over Central Asia and locations of typical loess sections

图2 中亚干旱区典型黄土—古土壤剖面照片

Fig. 2 Photograph showing lithology of representative loess-paleosol sequences from Central Asia

图3 中亚黄土释放—搬运—沉积过程示意图^{[

58
]}

Fig. 3 Schematic map showing emission, transportation, and deposition processes of loess deposits in Central Asia ^{[

58
]}

图4 伊朗北部晚第四系黄土粒度组成及组分分离结果^{[

64
]}

Fig. 4 Grain-size distribution of upper Pleistocene loess in north Iran ^{[

64
]}

图5 中亚第四系黄土—古土壤序列及其与中国黄土高原的对比框架^{[

27
,

35
,

42
,

43
]}

Fig. 5 Pleistocene loess-paleosol sequences in Central Asia and its correlation with the Chinese Loess Plateau ^{[

27
,

35
,

42
,

43
]}

图6 末次间冰期以来中亚代表性黄土—古土壤剖面的红度记录及其与中国黄土高原的对比^{[

41
,

43
,

86
,

88
,

89
]}

Fig. 6 Correlations of redness records from loess-paleosol sequences in Central Asia and the Chinese Loess Plateau since last inter-glacial period ^{[

41
,

43
,

86
,

88
,

89
]}

图7 中亚干旱区第四系黄土剖面的红度记录及其与中国黄土高原、深海氧同位素记录的对比框架^{[

42
,

43
,

88
,

89
]}

Fig. 7 Correlations of redness records from loess-paleosol sequences in Central Asia and the Chinese Loess Plateau since Pleistocene ^{[

42
,

43
,

88
,

89
]}

图8 中亚干旱区冰期(a)和间冰期(b)大气环流示意图^{[

46
,

90
]}

Fig. 8 Schematic map showing major circulation patterns in central Asia during glacial (a) and interglacial (b) periods ^{[

46
,

90
]}

图9 鹿角湾剖面的湿度记录^{[

8
]}及其与中国黄土^{[

94
]}和公海湖泊记录^{[

93
]}的对比

Fig. 9 Proxy indices of moisture changes from the Lujiaowan Section ^{[

8
]} and its correlation with those from the Chinese Loess ^{[

94
]} and Gonghai Lake ^{[

93
]}

1	Uematsu M , Duce R A , Prospero J M , et al . Transport of mineral aerosol from Asia over the North Pacific-Ocean[J]. Journal of Geophysical Research-Oceans, 1983, 88(C9): 5 343-5 352.
2	Rea D K , Leinen M , Janecek T R . Geologic approach to the long-term history of atmospheric circulation[J]. Science, 1985, 227(4 688): 721-725.
3	Zhang X Y , Gong S L , Zhao T L , et al . Sources of Asian dust and role of climate change versus desertification in Asian dust emission[J]. Geophysical Research Letters, 2003, 30(24):1-4.
4	Zheng H B . Asia dust production ramped up since latest Oligocene driven by Tibetan Plateau uplift[J]. National Science Review, 2016, 3(3): 271-274.
5	Arimoto R . Eolian dust and climate: Relationships to sources, tropospheric chemistry, transport and deposition[J]. Earth-Science Reviews, 2001, 54(1/3): 29-42.
6	Harrison S P , Kohfeld K E , Roelandt C , et al . The role of dust in climate changes today, at the last glacial maximum and in the future[J]. Earth-Science Reviews, 2001, 54(1/3): 43-80.
7	Jickells T D , An Z S , Andersen K K , et al . Global iron connections between desert dust, ocean biogeochemistry, and climate[J]. Science, 2005, 308(5 718): 67-71.
8	Chen F H , Yu Z C , Yang M L , et al . Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history[J]. Quaternary Science Reviews, 2008, 27(3/4): 351-364.
9	Chen F H , Chen J H , Holmes J , et al . Moisture changes over the last millennium in arid central Asia: A review, synthesis and comparison with monsoon region[J]. Quaternary Science Reviews, 2010, 29(7/8): 1 055-1 068.
10	Huang W , Chen J H , Zhang X J , et al . Definition of the core zone of the “westerlies-dominated climatic regime”, and its controlling factors during the instrumental period[J]. Science in China (Series D), 2015, 58(5): 676-684.
11	Ballato P , Mulch A , Landgraf A , et al . Middle to late Miocene Middle Eastern climate from stable oxygen and carbon isotope data, southern Alborz mountains, N Iran[J]. Earth and Planetary Science Letters, 2010, 300(1/2): 125-138.
12	Guan Xiaodan , Shi Rui , Kong Xiangning , et al . An overview of researches on land-atmosphere interaction over semi-arid region under global changes[J]. Advances in Earth Science, 2018, 33(10): 995-1 004.
	管晓丹，石瑞，孔祥宁，等．全球变化背景下半干旱区陆气机制研究综述[J]．地球科学进展，2018，33(10): 995-1 004.
13	Machalett B , Oches E A , Frechen M , et al . Aeolian dust dynamics in central Asia during the Pleistocene: Driven by the long-term migration, seasonality, and permanency of the Asiatic polar front[J]. Geochemistry Geophysics Geosystems, 2008, 9(8): 1-22.
14	Dettman D L , Kohn M J , Quade J , et al . Seasonal stable isotope evidence for a strong Asian monsoon throughout the past 10.7 m.y.[J]. Geology, 2001, 29(1): 31-34.
15	An Z S . Late Cenozoic Climate Change in Asia[M]. New York: Springer, 2014.
16	Chen J H , Chen F H , Feng S , et al . Hydroclimatic changes in China and surroundings during the Medieval Climate Anomaly and Little Ice Age: Spatial patterns and possible mechanisms[J]. Quaternary Science Reviews, 2015, 107: 98-111.
17	Haase D , Fink J , Haase G , et al . Loess in Europe—Its spatial distribution based on a European Loess map, scale 1 ∶ 2,500,000[J]. Quaternary Science Reviews, 2007, 26(9/10): 1 301-1 312.
18	Fitzsimmons K E , Markovic S B , Hambach U . Pleistocene environmental dynamics recorded in the loess of the middle and lower Danube basin[J]. Quaternary Science Reviews, 2012, 41: 104-118.
19	Markovi? S B , Stevens T , Kukla G J , et al . Danube loess stratigraphy-Towards a pan-European loess stratigraphic model[J]. Earth-Science Reviews, 2015, 148: 228-258.
20	Markovic S B , Fitzsimmons K E , Sprafke T , et al . The history of Danube loess research[J]. Quaternary International, 2016, 399: 86-99.
21	Liu Dongsheng . Loess and Invironment[M]. Beijing: Science Press, 1985.
	[ 刘东生 .黄土与环境[M].北京: 科学出版杜,1985.
22	Heller F , Liu T S . Magnetostratigraphical dating of Loess Deposits in China[J]. Nature, 1982, 300(5 891): 431-433.
23	Kukla G , An Z S . Loess stratigraphy in central China[J]. Palaeogeography Palaeoclimatology Palaeoecology, 1989, 72(1/2): 203-225.
24	An Z H , Kukla G J , Porter S C , et al . Magnetic-susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130,000 years[J]. Quaternary Research, 1991, 36(1): 29-36.
25	Liu T S , Ding Z L . Chinese loess and the paleomonsoon[J]. Annual Review of Earth And Planetary Sciences, 1998, 26: 111-145.
26	Chen F H , Bloemendal J , Wang J M , et al . High-resolution multi-proxy climate records from Chinese loess, evidence for rapid climatic changes over the last 75 kyr[J]. Palaeogeography Palaeoclimatology Palaeoecology, 1997, 130(1/4): 323-335.
27	Sun D H , Shaw J , An Z S , et al . Magnetostratigraphy and paleoclimatic interpretation of a continuous 7.2 Ma Late Cenozoic eolian sediments from the Chinese Loess Plateau[J]. Geophysical Research Letters, 1998, 25(1): 85-88.
28	Sun D H , An Z S , Shaw J , et al . Magnetostratigraphy and palaeoclimatic significance of late tertiary aeolian sequences in the Chinese Loess Plateau[J]. Geophysical Journal International, 1998, 134(1): 207-212.
29	An Z S , Kutzbach J E , Prell W L , et al . Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since Late Miocene times[J]. Nature, 2001, 411(6 833): 62-66.
30	Guo Z T , Ruddiman W F , Hao Q Z , et al . Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J]. Nature, 2002, 416(6 877): 159-163.
31	Sun Y B , An Z S . Late Pliocene-Pleistocene changes in mass accumulation rates of eolian deposits on the central Chinese Loess Plateau[J]. Journal of Geophysical Research—Atmospheres, 2005, 110(D23): 1-8.
32	Ding Z L , Liu T S , Rutter N W , et al . Ice-volume forcing of East-Asian winter monsoon variations in the past 800,000 Years[J]. Quaternary Research, 1995, 44(2): 149-159.
33	Ding Z L , Xiong S F , Sun J M , et al . Pedostratigraphy and paleomagnetism of a similar to 7.0 Ma eolian loess-red clay sequence at Lingtai, Loess Plateau, north-central China and the implications for paleomonsoon evolution[J]. Palaeogeography Palaeoclimatology Palaeoecology, 1999, 152(1/2): 49-66.
34	Dodonov A E , Zhou L P . Loess deposition in Asia: Its initiation and development before and during the Quaternary[J]. Episodes, 2008, 31(2): 222-225.
35	Dodonov A E . Loess of central Asia[J]. GeoJournal, 1991, 24(2): 185-194.
36	Dodonov A E , Baiguzina L L . Loess stratigraphy of Central Asia: Palaeoclimatic and palaeoenvironmental aspects[J]. Quaternary Science Reviews, 1995, 14(7/8): 707-720.
37	Kehl M . Quaternary climate change in Iran—The state of Knowledge[J]. Erdkunde, 2009, 62(1): 1-17.
38	Lauer T , Frechen M , Vlaminck S , et al . Luminescence-chronology of the loess palaeosol sequence Toshan, Northern Iran—A highly resolved climate archive for the last glacial-interglacial cycle[J]. Quaternary International, 2017, 429(B): 3-12.
39	Lu Y C , Wang X L , Wintle A G . A new OSL chronology for dust accumulation in the last 130,000 yr for the Chinese Loess Plateau[J]. Quaternary Research, 2007, 67(1): 152-160.
40	Frechen M , Kehl M , Rolf C , et al . Loess chronology of the Caspian lowland in northern Iran[J]. Quaternary International, 2009, 198(1/2): 220-233.
41	Lauer T , Vlaminck S , Frechen M , et al . The Agh Band loess-palaeosol sequence—A terrestrial archive for climatic shifts during the last and penultimate glacial-interglacial cycles in a semiarid region in northern Iran[J]. Quaternary International, 2016, 429(B): 13-30.
42	Wang X , Wei H T , Taheri M , et al . Early Pleistocene climate in western arid central Asia inferred from loess-palaeosol sequences[J]. Scientific Reports, 2016, 6: 1-9.
43	Ding Z L , Ranov V , Yang S L ,et al . The loess record in southern Tajikistan and correlation with Chinese loess[J]. Earth and Planetary Science Letters, 2002, 200(3/4): 387-400.
44	Dodonov A . Anthropogene of South Tadjikistan[M]. Moscow: Nauka, 1986.
45	Zhou L P , Dodonov A E , Shackleton N J . Thermoluminescence dating of the orkutsay loess section in Tashkent region, Uzbekistan, Central Asia[J]. Quaternary Science Reviews, 1995, 14(7): 721-730.
46	Machalett B , Frechen M , Hambach U , et al . The loess sequence from Remisowka (northern boundary of the Tien Shan Mountains, Kazakhstan)—Part I: Luminescence dating[J]. Quaternary International, 2006, 152: 192-201.
47	Feng Z D , Ran M , Yang Q L , et al . Stratigraphies and chronologies of late Quaternary loess-paleosol sequences in the core area of the central Asian arid zone[J]. Quaternary International, 2010, 240(1): 156-166.
48	Fitzsimmons K E , Sprafke T , Zielhofer C , et al . Loess accumulation in the Tian Shan piedmont: Implications for palaeoenvironmental change in arid Central Asia[J]. Quaternary International, 2018, 469(A): 30-43.
49	Youn J H , Seong Y B , Choi J H , et al . Loess deposits in the northern Kyrgyz Tien Shan: Implications for the paleoclimate reconstruction during the Late Quaternary[J]. Catena, 2014, 117: 81-93.
50	Fang Xiaomin , Shi Zhengtao , Yang Shengli , et al . Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of Northern Xinjiang[J]. Chinese Science Bulletin, 2002, 47(7): 540-545.
	方小敏，史正涛，杨胜利，等 . 天山黄土和古尔班通古特沙漠发育及北疆干旱化[J]. 科学通报，2002, 47(7): 540-545.
51	Li Chuanxiang , Song Yougui , Wang Lemin . Distribution, age and dust sources of Loess in the Ili Basin[J]. Earth and environment, 2012, 40(3):314-320.
	李传想，宋友桂，王乐民 . 伊犁盆地黄土分布、年代及粉尘来源分析[J]. 地球与环境，2012，40(3): 314-320.
52	Honghua Lü , Li Youli , Nan Feng, et al . Characteristics and age of loess along north piedmont of Tianshan Mountains[J] Geographical Science, 2008,28(3): 375-379.
	吕红华，李有利，南峰，等 . 天山北麓黄土发育特征及形成年代[J]. 地理科学，2008，28(3)：375-379.
53	Ye Wei . Characteristics and Paleoclimate of Loess Deposits in Westerly Area of Xinjiang[M]. Beijing: Ocean Press, 2001.
	叶玮 . 新疆西风区黄土沉积特征与古气候[M]. 北京: 海洋出版社，2001.
54	Wang Leibin , Wei Haitao , Jia Jia , et al . Advances and issues in luminescene dating of loess deposits in arid Central Asia [J]. Advances in Earth Science, 2018, 33 (1): 93-102.
	王蕾彬，魏海涛，贾佳，等 . 亚洲中部干旱区黄土释光测年研究进展及其问题[J]. 地球科学进展，2018, 33(1): 93-102.
55	Song Y G , Li C X , Zhao J D , et al . A combined luminescence and radiocarbon dating study of the Ili Loess, Central Asia[J]. Quaternary Geochronology, 2012, 10: 2-7.
56	Li G Q , Rao Z G , Duan Y W , et al . Paleoenvironmental changes recorded in a luminescence dated loess/paleosol sequence from the Tianshan Mountains, arid Central Asia, since the Penultimate Glaciation[J]. Earth and Planetary Science Letters, 2016, 448:1-12.
57	Zan J B , Fang X M , Yang S L , et al . A rock magnetic study of loess from the West Kunlun Mountains[J]. Journal of Geophysical Research, 2010, 115(1): 1-9.
58	Smalley I J , Mavlyanova N G , Rakhmatullaev K L , et al . The formation of loess deposits in the Tashkent region and parts of Central Asia; and problems with irrigation, hydrocollapse and soil erosion[J]. Quaternary International, 2006, 152: 59-69.
59	Smalley I . Making the material: The formation of silt-sized primary mineral particles for loess deposits[J]. Quaternary Science Reviews, 1995, 14(7/8): 645-651.
60	Smalley I , Derbyshire E . The Definition of 'Ice-Sheet' and 'Mountain' Loess[J]. Area, 1990, 22(3): 300-301.
61	Smalley I , Krinsley D H . Loess deposits associated with deserts[J]. catena, 1978, 5(1): 53-66.
62	Stuut J B , Smalley I , O'Hara-Dhand K . Aeolian dust in Europe: African sources and European deposits[J]. Quaternary International, 2009, 198: 234-245.
63	Wang X , Wei H T , Khormali F , et al . Grain-size distribution of Pleistocene loess deposits in northernIran and its palaeoclimatic implications[J]. Quaternary International, 2017, 429(B):41-51.
64	Wang X , Kraatz B , Meng J , et al . Central Asian aridification during the late Eocene to early Miocene inferred from preliminary study of shallow marine-eolian sedimentary rocks from northeastern Tajik Basin[J]. Science in China (Series D), 2016, 59(6): 1 242-1 257.
65	Pye K . The nature, origin and accumulation of loess[J]. Quaternary Science Reviews, 1995, 14(7/8): 653-667.
66	Pye K . Aeolian Dust and Dust Deposits[M]. New York: Academic Press Londres, 1987.
67	Okhravi R , Amini A . Characteristics and provenance of the loess deposits of the Gharatikan watershed in Northeast Iran[J]. Global And Planetary Change, 2001, 28(1/4): 11-22.
68	Dercourt J , Ricou L E , Vrielynck B . Atlas Tethys, Paleoenvironmental Maps: Explanatory Notes[M].Paris: Gauthier-Villars, 1993.
69	Rogl F . Mediterranean and Paratethys. Facts and hypotheses of an Oligocene to Miocene paleogeography (short overview) [J]. Geologica Carpathica, 1999, 50(4): 339-349.
70	Popov S V , R?gl F , Rozanov A Y , et al . Lithological-Paleogeographic maps of Parathys, 10 Maps Late Eocene to Pliocene[M]. Senckenberg: Courier Forschungsinstitut, 2004.
71	Bosboom R E , Dupont-Nivet G , Houben A J P , et al . Late Eocene sea retreat from the Tarim Basin (west China) and concomitant Asian paleoenvironmental change[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2011, 299(3/4): 385-398.
72	Bosboom R , Dupont-Nivet G , Grothe A , et al . Linking Tarim Basin sea retreat (west China) and Asian aridification in the late Eocene[J]. Basin Research, 2014, 26(5): 621-640.
73	Sun J M , Jiang M S . Eocene seawater retreat from the southwest Tarim Basin andimplications for early Cenozoic tectonic evolution in the Pamir Plateau[J]. Tectonophysics, 2013, 588: 27-38.
74	Wang X , Sun D H , Chen F H , et al . Cenozoic paleo-environmental evolution of the Pamir-Tien Shan convergence zone[J]. Journal of Asian Earth Sciences, 2014, 80: 84-100.
75	Carrapa B , DeCelles P G , Wang X , et al . Tectono-climatic implications of Eocene Paratethys regression in the Tajik Basin of Central Asia[J]. Earth and Planetary Science Letters, 2015, 424:168-178.
76	Muhs D R . Encyclopedia of Quaternary Science[M]. London: Elsevier, Oxford, 2007: 1 405-1 418.
77	Song Y G , Fang X M , Masayuki T , et al . Magnetostratigraphy of Late Tertiary sediments from the Chinese Loess Plateau and its paleoclimatic significance[J]. Chinese Science Bulletin, 2001, 46(Suppl.1):16-22.
78	Hao Q Z , Guo Z T . Magnetostratigraphy of an early-middle Miocene loess-soil sequence in the western Loess Plateau of China[J]. Geophysical Research Letters, 2007, 34(18): 1-6.
79	Qiang X K , An Z S , Song Y G , et al . New eolian red clay sequence on the western Chinese Loess Plateau linked to onset of Asian desertification about 25 Ma ago[J]. Science in China (Series D), 2011, 54(1): 136-144.
80	Zhang Y B , Sun D H , Li Z J , et al . Cenozoic record of aeolian sediment accumulation and aridification from Lanzhou, China, driven by Tibetan Plateau uplift and global climate[J]. Global And Planetary Change, 2014, 120: 1-15.
81	Yang S L , Ding F , Ding Z L . Pleistocene chemical weathering history of Asian arid and semi-arid regions recorded in loess deposits of China and Tajikistan[J]. Geochimica et Cosmochimica Acta, 2006, 70(7): 1 695-1 709.
82	Sun D H , Bloemendal J , Yi Z Y , et al . Palaeomagnetic and palaeoenvironmental study of two parallel sections of late Cenozoic strata in the central Taklimakan Desert: Implications for the desertification of the Tarim Basin[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2011, 300(1/4): 1-10.
83	Wang X , Sun D H , Wang F , et al . A high-resolution multi-proxy record of late Cenozoic environment change from central Taklimakan Desert, China[J]. Climate of the Past, 2013, 9(6): 2 731-2 739.
84	Pakhomov M M . New Data on Palaeogeography of Loess-Palaeosol Series in Middle Asia[M]. Moscow: Doclady Academii Nauk SSSR, 1983.
85	Deviatkin E A . A Capacitive Velocity Sensor[J]. Instruments And Experimental Techniques, 1993, 36(2): 300-302.
86	Vlaminck S , Kehl M , Lauer T , et al . Loess-soil sequence at Toshan (Northern Iran): Insights into late Pleistocene climate change[J]. Quaternary International, 2016, 399(1 571): 122-135.
87	Yang S L , Fang X M , Li J J , et al . Transformation functions of soil color and climate[J]. Science in China (Series D), 2001, 44(1):218-226.
88	Sun Y B , He L , Liang L J , et al . Changing color of Chinese loess: Geochemical constraint and paleoclimatic significance[J]. Journal of Asian Earth Sciences, 2011, 40(6): 1 131-1 138.
89	Lisiecki L E , Raymo M E . A Plio-Pleistocene stack of 57 globally distributed benthic δ¹⁸O records[J]. Paleoceanography and Paleoclimatology, 2005, 20(1): 522-533.
90	Yang S L , Ding Z L , Li Y Y , et al . Warming-induced northwestward migration of the East Asian monsoon rain belt from the Last Glacial Maximum to the mid-Holocene[J]. Proceedings of the National Academy of Sciences of the United States of America, 2015, 112(43): 13 178-13 183.
91	Chen F H , Jia J , Chen J H , et al . A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in Xinjiang, China[J]. Quaternary Science Reviews, 2016, 146: 134-146.
92	Jin L Y , Chen F H , Morrill C , et al . Causes of early Holocene desertification in arid Central Asia[J]. Climate Dynamics, 2012, 38(7/8): 1 577-1 591.
93	Chen F H , Xu Q , Chen J , et al . East Asian summer monsoon precipitation variability since the last deglaciation[J]. Scientific Reports, 2015, 5(11 186): 1-11.
94	Wang H P , Chen J H , Zhang X J , et al . Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: Evidence for a mid-Holocene maximum [J]. Quaternary International, 2014, 334/335: 155-164.
95	Wang W , Feng Z D . Holocene moisture evolution across the Mongolian Plateau and its surrounding areas: A synthesis of climatic records [J]. Earth-Science Reviews, 2013, 122: 38-57.
96	Leroy S A G , López-Merino L , Tudryn A , et al . Late Pleistocene and Holocene palaeoenvironments in and around the middle Caspian basin as reconstructed from a deep-sea core[J]. Quaternary Science Reviews, 2014, 101: 91-110.
97	Cheng H , Zhang P Z , Sp?tl C , et al . The climatic cyclicity in semiarid-arid central Asia over the past 500,000 years[J]. Geophysical Research Letters, 2012, 39: 1-5.
98	Li X Q , Zhao K L , Dodson J , et al . Moisture dynamics in central Asia for the last 15 kyr: New evidence from Yili Valley, Xinjiang, NW China[J]. Quaternary Science Reviews, 2011, 30: 3 457-3 644.
99	Liu X K , Rao Z G , Zhang X J , et al . Variations in the oxygen isotopic composition of precipitation in the Tianshan Mountains region and their significance for the Westerly circulation[J]. Journal of Geographical Sciences, 2015, 25(7): 801-816.

[1]	杨军怀,夏敦胜,高福元,王树源,陈梓炫,贾佳,杨胜利,凌智永. 雅鲁藏布江流域风成沉积研究进展[J]. 地球科学进展, 2020, 35(8): 863-877.
[2]	武雪超, 郝青振, Marković Slobodan B, 付玉, 娜米尔, 宋扬, 郭正堂. 多瑙河黄土与古环境研究进展[J]. 地球科学进展, 2020, 35(4): 363-377.
[3]	陈立雷,李凤,刘健. 海洋沉积物中 GDGTs和长链二醇的古气候—环境指示意义研究进展[J]. 地球科学进展, 2019, 34(8): 855-867.
[4]	宗秀兰, 宋友桂, 李越. 蚯蚓方解石颗粒——一种新的古气候信息记录载体[J]. 地球科学进展, 2018, 33(9): 983-993.
[5]	顾家伟. 长江河口区晚新生代以来沉积化学元素分布及物源指示意义[J]. 地球科学进展, 2018, 33(5): 506-516.
[6]	王兆夺, 黄春长, 周亚利, 庞奖励, 查小春. 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.
[7]	王蕾彬, 魏海涛, 贾佳, 李国强, 陈发虎. 亚洲中部干旱区黄土释光测年研究进展及其问题[J]. 地球科学进展, 2018, 33(1): 93-102.
[8]	李兴文, 张鹏, 强小科, 敖红. 三门峡会兴沟剖面黄土—古土壤序列的岩石磁学研究[J]. 地球科学进展, 2017, 32(5): 513-523.
[9]	王瑞, 余克服, 王英辉, 边立曾. 珊瑚礁的成岩作用[J]. 地球科学进展, 2017, 32(3): 221-233.
[10]	吕璇, 刘志飞. 大洋红层的分布、组成及其科学研究意义综述[J]. 地球科学进展, 2017, 32(12): 1307-1318.
[11]	李丽, 徐沁. 上新世以来巽他陆架海平面变化研究[J]. 地球科学进展, 2017, 32(11): 1126-1136.
[12]	黄伟, 刘殿兵, 王璐瑶, 张振球. 洞穴石笋δ ¹³C在古气候重建研究中的现状与进展[J]. 地球科学进展, 2016, 31(9): 968-983.
[13]	胡玉, 陈建徽, 王海鹏, 吕飞亚, 魏国英. 基于摇蚊的古环境和古气候国内外研究进展与展望[J]. 地球科学进展, 2016, 31(8): 870-884.
[14]	刘华华, 蒋富清, 周烨, 李安春. 晚更新世以来奄美三角盆地黏土矿物的来源及其对古气候的指示[J]. 地球科学进展, 2016, 31(3): 286-297.
[15]	周烨, 蒋富清, 南青云, 刘华华, 李安春. 奄美三角盆地晚更新世以来碎屑沉积物粒度特征及其物源和古气候意义[J]. 地球科学进展, 2016, 31(3): 298-309.

阅读次数

全文

摘要