Sensitivity of lacustrine stromatolites to Cenozoic tectonic and climatic forcing in the southern Junggar Basin, NW China: New insights from mineralogical, stable and clumped isotope compositions
Yang, Wei1,2; Zuo, Rusi1,2; Wang, Xu3; Song, Yan1,2; Jiang, Zhenxue1,2; Luo, Qun1,2; Zhai, Jixuan3; Wang, Qianyou1,2; Zhang, Chen1,2; Zhang, Ziya4,5
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
2019-01-15
卷号514页码:109-123
关键词Mineralogical Palaeothermometer Aridification Lake level Palaeoenvironment Northern Tian Shan
ISSN号0031-0182
DOI10.1016/j.palaeo.2018.10.011
英文摘要Lacustrine stromatolites serve as high-resolution and sensitive archives of palaeoenvironmental settings and palaeoclimatic conditions. An exceptionally well-developed stromatolite bed was discovered within nearshore shallow lacustrine sediments of the Lower Miocene Taxihe Formation on the southern margin of the Junggar Basin, north of the Tian Shan Range. We investigated the morphology, mineralogy, clumped and traditional stable isotope geochemistry of the stromatolites by using a multi-method approach with the application of X-ray diffraction analysis, advanced mineral identification and characterization (AMICSCAN), a clumped isotope palaeothermometer and modelling. The overall positive excursions and covariance of delta O-18 (varying from +10.61 parts per thousand to -5.82 parts per thousand V-PDB) and delta C-13 (ranging between -1.27 parts per thousand and +2.08 parts per thousand V-PDB) values are interpreted as the result of deposition in a closed-basin system under local progressive evaporation conditions during an episode of aridification. Clumped isotope proxy records display a significant decrease in water delta O-18 values and a decline of lake water temperature from similar to 38 to similar to 32 degrees C, suggesting a shift towards more arid and relatively cooler conditions during the course of stromatolite accretion. This interpretation agrees with lake volume and water level decreases inferred from isotope modelling results. The Late Cenozoic aridification of the southern margin of the Junggar Basin is thus interpreted from a new and unique perspective to have prevailed since the Early Miocene, driven by renewed uplift of the northern Tian Shan Range. The investigated stromatolite records reflect a snapshot of the local palaeoclimatic and palaeoenvironmental evolution, and our work provides references for potential studies of future discoveries of lacustrine microbialites in northwestern China.
资助项目National Natural Science Foundation of China[41602233] ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing[2462017BJB07] ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing[PRP/indep-4-1406] ; Chinese State 973 Project[2015CB250901] ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology[2017ZX05008-001]
WOS关键词TIEN-SHAN ; TIAN-SHAN ; GEODYNAMIC EVOLUTION ; EASTERN TIANSHAN ; TIBETAN PLATEAU ; NORTHWEST CHINA ; CENTRAL-ASIA ; TARIM BASIN ; CARBON ; ARIDIFICATION
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000456355800009
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Chinese State 973 Project ; Chinese State 973 Project ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Chinese State 973 Project ; Chinese State 973 Project ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Chinese State 973 Project ; Chinese State 973 Project ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Science Foundation for topnotch innovative talents of China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Foundation of State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ; Chinese State 973 Project ; Chinese State 973 Project ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology ; State Science and Technology Major Project from the Chinese Ministry of Science and Technology
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/90187]  
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Yang, Wei; Wang, Xu
作者单位1.China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
2.China Univ Petr, Unconvent Nat Gas Inst, Beijing 102249, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing, Peoples R China
4.China Geol Survey, Oil & Gas Survey, Beijing 100029, Peoples R China
5.CGS, Key Lab Unconvent Petr Geol, Beijing 100029, Peoples R China
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Yang, Wei,Zuo, Rusi,Wang, Xu,et al. Sensitivity of lacustrine stromatolites to Cenozoic tectonic and climatic forcing in the southern Junggar Basin, NW China: New insights from mineralogical, stable and clumped isotope compositions[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2019,514:109-123.
APA Yang, Wei.,Zuo, Rusi.,Wang, Xu.,Song, Yan.,Jiang, Zhenxue.,...&Zhang, Ziya.(2019).Sensitivity of lacustrine stromatolites to Cenozoic tectonic and climatic forcing in the southern Junggar Basin, NW China: New insights from mineralogical, stable and clumped isotope compositions.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,514,109-123.
MLA Yang, Wei,et al."Sensitivity of lacustrine stromatolites to Cenozoic tectonic and climatic forcing in the southern Junggar Basin, NW China: New insights from mineralogical, stable and clumped isotope compositions".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 514(2019):109-123.
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