中天山山间盆地中晚全新世植被与气候变化

苏展艺; 姚付龙; 夏倩倩; 胡晓峰; 苏展艺; 姚付龙; 夏倩倩; 胡晓峰

doi:10.14027/j.issn.1000-0550.2024.058

[1]

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Fan Bin, Xu Shiyuan, Yu Lizhong, et al. 2006. Phytolith in the sediment of the Lake Chaohu since Middle Holocene and its paleoenvironmental implications[J]. Journal of Lake Sciences, 18(3): 273-279.

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Fan Yijiao, Tian Weidong, Yang Junhuai, et al. 2021. Environmental changes since last deglaciation recorded in loess at different altitude in Tianshan Mountains, Xinjiang[J]. Quaternary Sciences, 41(5): 1244-1253.

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Guo Chao, Ma Yuzhen, Li Jinfeng. 2022. Mid-to Late Holocene moisture evolution in China and surroundings: Spatial patterns and possible mechanisms[J]. Quaternary Sciences, 42(4): 1058-1077.

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何鹏，刘健，刘斌，等. 2019. 全新世两次典型突变事件下北半球季风降水的变化对比[J]. 第四纪研究，39（6）：1372-1383.

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Huang Changqing, Ran Min, Sang Yanli. 2017. Palaeoclimate history recorded by pollen of Valikhanov section during the last 28000 years in Kazakhstan[J]. Bulletin of Science and Technology, 33(9): 54-58, 167.

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Jiang Qingfeng, Ji Junfeng, Shen Ji, et al. 2013. Holocene vegetational and climatic variation in westerly-dominated areas of Central Asia inferred from the Sayram Lake in northern Xinjiang, China[J]. Science China Earth Sciences, 43(2): 243-255.

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[1]	陈发虎，黄小忠，杨美临，等. 2006. 亚洲中部干旱区全新世气候变化的西风模式：以新疆博斯腾湖记录为例[J]. 第四纪研究，26（6）：881-887. Chen Fahu, Huang Xiaozhong, Yang Meilin, et al. 2006. Westerly dominated Holocene climate model in arid Central Asia: Case study on Bosten Lake, Xinjiang, China[J]. Quaternary Sciences, 26(6): 881-887.
[2]	陈发虎，吴薇，朱艳，等. 2004. 阿拉善高原中全新世干旱事件的湖泊记录研究[J]. 科学通报，49（1）：1-9. Chen Fahu, Wu Wei, Zhu Yan, et al. 2004. A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China[J]. Chinese Science Bulletin, 49(1): 1-9.
[3]	陈曦. 2010. 中国干旱区自然地理[M]. 北京：科学出版社：1-801. Chen Xi. 2010. Physical geography of arid land in China[M]. Beijing: Science Press: 1-801.
[4]	丁一汇. 2013. 中国自然地理系列专著：中国气候[M]. 北京：科学出版社：1-557. Ding Yihui. 2013. Series of monographs on the physical geography of China: China's climate.[M]. Beijing: Science Press: 1-557.
[5]	段晓红，张芸，杨振京，等. 2018. 新疆石河子蘑菇湖湿地4800年以来的环境演变[J]. 海洋地质与第四纪地质，38（4）：203-211. Duan Xiaohong, Zhang Yun, Yang Zhenjing, et al. 2018. Environmental evolution of the Moguhu wetland of Shihezi city in Xinjiang since 4800 cal. a BP[J]. Marine Geology & Quaternary Geo-logy, 38(4): 203-211.
[6]	范斌，许世远，俞立中，等. 2006. 巢湖沉积植硅体组合及中全新世以来的环境演变[J]. 湖泊科学，18（3）：273-279. Fan Bin, Xu Shiyuan, Yu Lizhong, et al. 2006. Phytolith in the sediment of the Lake Chaohu since Middle Holocene and its paleoenvironmental implications[J]. Journal of Lake Sciences, 18(3): 273-279.
[7]	范义姣，田伟东，杨军怀，等. 2021. 新疆天山地区不同海拔黄土记录的末次冰消期以来的环境演变[J]. 第四纪研究，41（5）：1244-1253. Fan Yijiao, Tian Weidong, Yang Junhuai, et al. 2021. Environmental changes since last deglaciation recorded in loess at different altitude in Tianshan Mountains, Xinjiang[J]. Quaternary Sciences, 41(5): 1244-1253.
[8]	冯兆东，张同文，冉敏. 2017. 新疆北部及周边地区过去一万年的气候与水文变化[M]. 兰州：兰州大学出版社：1-238. Feng Zhaodong, Zhang Tongwen, Ran Min. 2017. Climatic and hydrological changes in northern Xinjiang and neighboring areas over the past 10, 000 years[M]. Lanzhou: Lanzhou University Press: 1-238.
[9]	郭超，马玉贞，李金凤. 2022. 中国及周边地区中晚全新世湿度演化及其可能机制[J]. 第四纪研究，42（4）：1058-1077. Guo Chao, Ma Yuzhen, Li Jinfeng. 2022. Mid-to Late Holocene moisture evolution in China and surroundings: Spatial patterns and possible mechanisms[J]. Quaternary Sciences, 42(4): 1058-1077.
[10]	何鹏，刘健，刘斌，等. 2019. 全新世两次典型突变事件下北半球季风降水的变化对比[J]. 第四纪研究，39（6）：1372-1383. He Peng, Liu Jian, Liu Bin, et al. 2019. Comparison of changes of northern hemisphere monsoon precipitation between two typical abrupt climate events in Holocene[J]. Quaternary Sciences, 39(6): 1372-1383.
[11]	胡汝骥. 2004. 中国天山自然地理[M]. 北京：中国环境科学出版社：1-443. Hu Ruji. 2004. Physical geography of the Tianshan Mountains in China[M]. Beijing: China Environmental Science Press: 1-443.
[12]	黄昌庆，冉敏，桑艳礼. 2017. 哈萨克斯坦Valikhanov剖面孢粉记录的28000年气候变化[J]. 科技通报，33（9）：54-58，167. Huang Changqing, Ran Min, Sang Yanli. 2017. Palaeoclimate history recorded by pollen of Valikhanov section during the last 28000 years in Kazakhstan[J]. Bulletin of Science and Technology, 33(9): 54-58, 167.
[13]	黄小忠. 2006. 新疆博斯腾湖记录的亚洲中部干旱区全新世气候变化研究[D]. 兰州：兰州大学：1-193. Huang Xiaozhong. 2006. Holocene climate variability of arid Central Asia documented by Bosten Lake, Xinjiang, China[D]. Lanzhou: Lanzhou University: 1-193.
[14]	蒋庆丰，季峻峰，沈吉，等. 2013. 赛里木湖孢粉记录的亚洲内陆西风区全新世植被与气候变化[J]. 中国科学：地球科学，43（2）：243-255. Jiang Qingfeng, Ji Junfeng, Shen Ji, et al. 2013. Holocene vegetational and climatic variation in westerly-dominated areas of Central Asia inferred from the Sayram Lake in northern Xinjiang, China[J]. Science China Earth Sciences, 43(2): 243-255.
[15]	刘浴辉，孙霞，郭彩青. 2013. 中国全新世4.2 ka BP气候事件及其对古文明的影响[J]. 地质科技情报，32（1）：99-106. Liu Yuhui, Sun Xia, Guo Caiqing. 2013. Records of 4.2 ka BP Holocene event from China and its impact on ancient civilizations[J]. Geological Science and Technology Information, 32(1): 99-106.
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