8 刘现彬, 夏敦胜, 贾佳等.兰州九州台黄土磁性特征及其古气候意义研究. 第四纪研究, 2012, 32 (4): 761~770 Liu Xianbin, Xia Dunsheng, Jia Jia et al. Magnetic properties of Jiuzhoutai loess in Lanzhou and its significance of palaeoclimate. Quaternary Sciences, 2012, 32 (4): 761~770
[2]
11 梁莲姬, 孙有斌, Christiaan J B等. 黄土中的碳酸盐矿物特征与化学风化. 第四纪研究, 2014, 34 (3): 345~653 Liang Lianji, Sun Youbin, Christiaan J B et al. Characteristics of carbonate minerals in loess and its implication for chemical weathering. Quaternary Sciences, 2014, 34 (3): 345~653
[3]
12 饶志国, 陈发虎, 曹洁等. 黄土高原西部地区末次冰期和全新世有机碳同位素变化与C3/C4 植被类型转换研究. 第四纪研究, 2005, 25 (1):107~114 Rao Zhiguo, Chen Fahu, Cao Jie et al. Variation of soil organic carbon isotope and C3/C4 vegetation type transition in the western Loess Plateau during the Last Glacial and Holocene periods. Quaternary Sciences, 2005, 25 (1):107~114
[4]
13 Chen Fahu, Rao Zhiguo, Zhang Jiawu et al. Variations of organic carbon isotopic composition and its environmental significance during the Last Glacial on western Chinese Loess Plateau. Chinese Science Bulletin, 2006, 51 (13):1593~1602
[5]
14 何勇, 秦大河, 任贾文等. 临夏塬堡全新世黄土剖面古土壤有机质碳同位素的气候记录. 冰川冻土, 2002, 24 (5):512~516 He Yong, Qin Dahe, Ren Jiawen et al. The climatic record of organic matter in the paleosol from the Yuanbao Holocene profile. Journal of Glaciology and Geocryology, 2002, 24 (5):512~516
[6]
15 何 勇, 秦大河, 任贾文等. 塬堡黄土剖面末次间冰期古土壤有机质碳同位素记录的夏季风演化历史. 科学通报, 2002, 47 (12):943~945 He Yong, Qin Dahe, Ren Jiawen et al. The summer monsoon evolution recorded by carbon isotope of organic matter from the Yuanbao loess section during the Last Interglaciation. Chinese Science Bulletin, 2002, 47 (15):1289~1291
[7]
16 杨桂芳, 彭红霞, 黄长生等. 黄土高原西缘末次盛冰期以来古气候演化的有机碳同位素记录. 华中师范大学学报(自然科学版), 2005, 39 (1):126~130 Yang Guifang, Peng Hongxia, Huang Changsheng et al. Paleoclimatic evolution deduced from organic carbon isotope of western Loess Plateau sediments since Last Glacial Maximum. Journal of Central China Normal University(Natural Science Edition), 2005, 39 (1):126~130
[8]
17 An Z S, Stephen C P, Zhou W J et al. Episode of strengthened summer monsoon climate of Younger Dryas age on the Loess Plateau of Central China. Quaternary Research, 1993, 39 (1):45~54
[9]
18 Liu W G, Yang H, Sun Y B et al.δ 13 C values of loess total carbonate:A sensitive proxy for Asian summer monsoon in arid northwestern margin of the Chinese Loess Plateau. Chemical Geology, 2011, 284 (3):317~322
[10]
1 刘东生等. 黄土与环境. 北京: 科学出版社, 1985.1~412 Liu Tungsheng et al. Loess and Environmental. Beijing:Science Press, 1985. 1~412
3 Chen F H, Bloemendal J M, Wand J M et al. High resolution multi-proxy climate records from Chinese Loess Plateau:Evidence for rapid climatic changes over the last 75 kyr. Paleogeography, Paleoclimatology, Paleoecology, 1997, 130 (1):323~335
[13]
4 Ding Z L, Ren J Z, Yang S L et al. Climate instability during the penultimate glaciations:Evidence from two high-resolution loess records, China. Journal of Geophysical Research, 1999, 104 (B9):20123~20132
[14]
5 Sun Y B, Clemens S C, Morrill C et al. Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon. Nature Geoscience, 2012, 5 (1):46~49
[15]
6 Sun Y B, Wang X L, Liu Q S et al. Impacts of post-depositional processes on rapid monsoon signals recorded by the last glacial loess deposits of Northern China. Earth and Planetary Science Letters, 2010, 289 (1):171~179
[16]
7 Rao Z G, Chen F H, Cheng H et al. High-resolution summer precipitation variations in the western Chinese Loess Plateau during the last glacial. Scientific Reports, 2013, 3 :doi:10.1038/srep02785
[17]
19 张晓, 贾鑫, 饶志国等. 陇西黄土高原东南部地区末次冰期以来C3/C4植物相对丰度变化及其区域性剖面的对比研究. 第四纪研究, 2013, 33 (1):187~196 Zhang Xiao, Jia Xin, Rao Zhiguo et al. C3/C4 variation since the last glacial in the southeastern Longxi Loess Plateau and its comparison with other results. Quaternary Sciences, 2013, 33 (1):187~196
[18]
20 饶志国, 张晓, 薛骞等. 西峰红粘土/黄土剖面有机碳同位素研究的初步结果. 第四纪研究, 2012, 32 (4):825~827 Rao Zhiguo, Zhang Xiao, Xue Qian et al. Primary organic carbon isotopic study result of Xifeng loess/red clay profile. Quaternary Sciences, 2012, 32 (4):825~827
[19]
21 赵得爱, 吴海斌, 吴建育等. 过去典型增温期黄土高原东西部C3/C4植物组成变化特征. 第四纪研究, 2013, 33 (5):848~855 Zhao De''ai, Wu Haibin, Wu Jianyu et al. C3/C4 plants characteristics of the eastern and western parts of the Chinese Loess Plateau during Mid-Holocene and last interglacial. Quaternary Sciences, 2013, 33 (5):848~855
[20]
22 Xie S C, Guo J Q, Huang J H et al. Restricted utility of δ 13 C of bulk organic matter as a record of paleovegetation in some loess-paleosol sequences in the Chinese Loess Plateau. Quaternary Research, 2004, 62 (1):86~93
[21]
23 Liu W G, Yang H, Ning Y F et al. Contribution of inherent organic carbon to the bulk δ 13 C signal in loess deposits from the arid western Chinese Loess Plateau. Organic Geochemistry, 2007, 38 (9):1571~1579
[22]
24 Rao Z G, Zhu Z Y, Chen F H et al. Does δ 13 Ccarb of the Chinese loess indicate past C3/C4 abundance?A review of research on stable carbon isotopes of the Chinese loess. Quaternary Science Reviews, 2006, 25 (17):2251~2257
[23]
25 Liu W G, Huang Y S, An Z S et al. Summer monsoon intensity controls C4/C3 plants abundance during the last 35ka in the Chinese Loess Plateau:Carbon isotope evidence from bulk organic matter and individual leaf waxes. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 220 (3):243~254
[24]
26 顾兆炎, 刘强, 许冰等. 气候变化对黄土高原末次盛冰期以来的C4/C3植物相对丰度的控制. 科学通报, 2003, 48 (13):1458~1464 Gu Zhaoyan, Liu Qiang, Xu Bing et al. Climate as the dominant control on C3 and C4 plant abundance in the Loess Plateau:Organic carbon isotope evidence from the last glacial-interglacial loess-soil sequences. Chinese Science Bulletin, 2003, 48 (12):1271~1276
[25]
27 饶志国, 贾国东, 朱照宇等. 中国东部表土总有机质碳同位素和长链正构烷烃碳同位素对比研究及其意义. 科学通报, 2008, 53 (17):2077~2084 Rao Zhiguo, Jia Guodong, Zhu Zhaoyu et al. Comparison of the carbon isotope composition of total organic carbon and long-chain n-alkanes from surface soils in Eastern China and their significance. Chinese Science Bulletin, 2008, 53 (24):3921~3927
[26]
28 钟艳霞. 末次冰期以来黄土高原西部地区环境变化的黄土有机地球化学记录研究. 兰州: 兰州大学博士学位论文, 2008. 25~33 Zhong Yanxia. A Study on Palaeoenvironmental Changes Recorded by Organic Geochemistry Proxies of Loess in the Western Loess Plateau since the Last-glacial. Lanzhou:The Dissertation for the Doctoral Degree of Lanzhou University, 2008. 25~33
[27]
29 Chen F H, Li J J, Zhang W X. Loess stratigraphy of the Lanzhou profile and its comparison with deep-sea sediment and ice core record. GeoJournal, 1991, 24 (2):201~209
[28]
30 陈发虎, 张宇田, 张维信等. 兰州九洲台黄土沉积年代的综合研究. 沉积学报, 1989, 7 (3):105~112 Chen Fahu, Zhang Yutian, Zhang Weixin et al. The comprehensive study on depositional age of Jiuzhoutai loess, Lanzhou. Acta Sedimentologica Sinica, 1989, 7 (3):105~112
[29]
31 魏明建, 董军社, 张静等. 黄土高原现代表层黄土植物残体稳定同位素组成特征. 现代地质, 1998, 12 (14):582~585 Wei Mingjian, Dong Junshe, Zhang Jing et al. Isotope composition characteristics of vegetation residues in modern loess deposition on the Loess Plateau in China. Geoscience, 1998, 12 (14):582~585
[30]
32 Melillo J M, Aber J D, Linkins A E. Carbon and nitrogen dynamics along the decay continuum:Plant litter to soil organic matter. Plant and Soil, 1989, 115 :189~198
[31]
33 Wang G, Feng X, Han J et al. Paleovegetation reconstruction using δ 13 C of soil organic matter. Biogeosciences, 2008, 5 (2):1325~1337
[32]
34 Zhang Z H, Zhao M X, Lu H Y et al. Lower temperature as the main cause of C4 plant declines during the glacial periods on the Chinese Loess Plateau. Earth and Planetary Science Letters, 2003, 214 (3):467~481
[33]
35 Vidic N J, Monta?ez I P. Climatically driven glacial-interglacial variations in C3 and C4 plant proportions on the Chinese Loess Plateau. Geology, 2004, 32 (4):337~340
[34]
36 刘卫国, 宁有丰, 安芷生等. 黄土高原现代土壤和古土壤有机碳同位素对植被的响应. 中国科学(D辑), 2002, 32 (10):830~836 Liu Weiguo, Ning Youfeng, An Zhisheng et al. Modern soil and paleosol organic carbon isotope response to vegetation of Chinese Loess Plateau. Science in China(Series D), 2005, 48 (1):93~99