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  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
  4. 中国科学院新生代地质与环境重点实验室
Climatic quantification and seasonality of the late MIS 3 in North China: A perspective from carbon and oxygen isotopes of fossil mammal teeth

文献类型：期刊论文

作者Wang, Xu1,2; Sun, Jing3; Longstaffe, Fred J.4; Gu, Xuejun5; Du, Shuisheng6; Cui, Linlin1,2; Huang, Xiaozhong7; Ding, Zhongli1,2
刊名QUATERNARY SCIENCE REVIEWS
出版日期2021-11-15
卷号272页码:16
ISSN号0277-3791
关键词Marine isotope stage 3 North China Stable isotopes Fossil mammal tooth Climate Seasonality
DOI10.1016/j.quascirev.2021.107222
英文摘要Marine Isotope Stage 3 (MIS 3, at 60-25 ka B.P.) was a short interstadial within the Last Glacial period. A generally warm and wet climatic condition during the MIS 3 period has been suggested by many previous studies. Quantitative climatic reconstruction and studies of seasonality, however, have been seldom attempted given the scarcity of useful proxy indicators. A full understanding the climatic characteristics during this period is hampered by their absence. This is especially the case in the East Asian monsoon region in North China, which is very sensitive to climatic change. To help fill this knowledge gap, we have determined the stable carbon (delta C-13) and oxygen isotope (delta O-13) compositions of tooth enamel from fossil mammals (Bubalus sp [buffalo] and Cervus elaphus [red deer], dated at similar to 33-31 ka B.P.) recovered from Longquan Cave in North China. We use these data to constrain ecology, local air temperature and precipitation amounts during the late MIS 3. The average delta C-13 (VPDB) of tooth enamel (-14.4 parts per thousand and -8.8 parts per thousand, respectively for buffalo and red deer) indicate that C3 plants comprised the main diet of animals living in this area. Pollen assemblages demonstrated that vegetation mainly consisted of grasses and herbs (similar to 64%) with trees only accounting for about 26%. These results indicate a landscape of open steppe with sparsely distributed trees. The reconstructed climate derived from tooth enamel delta O-13 was relatively colder and drier than present-day condition, with mean annual air temperature ranging from 4 to 13 degrees C and mean annual precipitation ranging from 360 to 670 mm. Moreover, the inferred summer and winter half-year temperatures were respectively 8-24 degrees C and -2 to 5 degrees C, which represents either similar or weaker seasonality than at the present time. The inferred cold and dry climate suggested by our study contrasts with the warm and wet conditions previously reconstructed using proxy indicators from bulk soil samples in North China. In comparison to the long-term, time-averaged climatic condition reflected by those soil proxies, the stable isotope compositions of fossil more likely recorded climatic conditions at annual or seasonal time-scale. The inferred annual cold/dry climate at Luanchuan Cave suggested by our data may indicate a short climatic cooling event from Greenland Interstadial (GIS) 5 to its following stadial. Mean annual temperature fluctuated by similar to 8 degrees C during this interstadial-stadial cycle. (C) 2021 Elsevier Ltd. All rights reserved.
WOS关键词PROGRESSIVE MINERALIZATION PATTERN ; TOOTH ENAMEL MINERALIZATION ; EAST-ASIAN DINOSAURS ; LAST GLACIAL CYCLE ; STABLE-ISOTOPE ; BONE PHOSPHATE ; LOESS PLATEAU ; DELTA-O-18 RECORD ; ORGANIC-CARBON ; BIOAPATITE
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA19050104] ; Key Research Program of the Institute of Geology and Geophysics[IGGCAS201905] ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program[05904-2019 RGPIN]
WOS研究方向Physical Geography ; Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000723151100002
资助机构Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Key Research Program of the Institute of Geology and Geophysics ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program ; Natural Sciences and Engineering Research Council of Canada Discovery Grant program
源URL[http://ir.iggcas.ac.cn/handle/132A11/103860]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Du, Shuisheng
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, POB 9825, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
3.Palace Museum, 4 Jingshan Qianjie, Beijing 100009, Peoples R China
4.Univ Western Ontario, Dept Earth Sci, London, ON N6A 5B7, Canada
5.Luoyang City Cultural Rel & Archaeol Res Inst, Luoyang 471000, Peoples R China
6.Beijing Normal Univ, Sch Hist, 19 Xinjiekouwai St, Beijing 100875, Peoples R China
7.Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Xu,Sun, Jing,Longstaffe, Fred J.,et al. Climatic quantification and seasonality of the late MIS 3 in North China: A perspective from carbon and oxygen isotopes of fossil mammal teeth[J]. QUATERNARY SCIENCE REVIEWS,2021,272:16.
APA Wang, Xu.,Sun, Jing.,Longstaffe, Fred J..,Gu, Xuejun.,Du, Shuisheng.,...&Ding, Zhongli.(2021).Climatic quantification and seasonality of the late MIS 3 in North China: A perspective from carbon and oxygen isotopes of fossil mammal teeth.QUATERNARY SCIENCE REVIEWS,272,16.
MLA Wang, Xu,et al."Climatic quantification and seasonality of the late MIS 3 in North China: A perspective from carbon and oxygen isotopes of fossil mammal teeth".QUATERNARY SCIENCE REVIEWS 272(2021):16.

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来源：地质与地球物理研究所

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