Stable isotope characterization of pedogenic and lacustrine carbonates from the Chinese Tian Shan: Constraints on the Mesozoic-Lower Cenozoic palaeoenvironmental evolution
文献类型：期刊论文
| 作者 | Heilbronn, G.1; Boulvais, P.1; Marchand, E.1; Robin, C.1; Bourquin, S.1; Barrier, L.1; Jia, Y.1; Fu, B.1; Jolivet, M.1 |
| 刊名 | CHEMIE DER ERDE-GEOCHEMISTRY
 |
| 出版日期 | 2015 |
| 卷号 | 75期号:1页码:4279-4295 |
| 关键词 | Pedogenic carbonates Stable isotopes Mesozoic palaeoenvironment Tian Shan |
| 通讯作者 | Heilbronn, G (reprint author), CASP, West Bldg,181A Huntingdon Rd, Cambridge CB3 0DH, England. |
| 英文摘要 | In the Mesozoic-Cenozoic continental deposits of the Tian Shan area, two main levels containing pedogenic carbonates have been identified on both the southern and northern foothills of the range: one in the Upper Jurassic series and one in the Upper Cretaceous-Lower Palaeocene series. In order to reconstruct the palaeoenvironmental and palaeotopographic characteristics of the Tian Shan area during these two periods, we measured the oxygen and carbon isotope composition of these pedogenic carbonates (calcrete and nodules). The stable isotope compositions are homogeneous: most 8180 values are between 21 and 25% and most delta C-13 values are between -4 and -6%.. No distinction can be made between the calcrete and nodule isotopic compositions. The constancy of isotopic values across the Tian Shan is evidence of a development of these calcification features in similar palaeoenvironmental conditions. The main inference is that no significant relief existed in that area at the Cretaceous-Palaeogene boundary, implying that most of the present relief developed later, during the Cenozoic. In addition to the pedogenic carbonates, few beds of limestones interstratified in the Jurassic series of the southern foothills display oxygen and carbon isotope compositions typical of lacustrine carbonates, ruling out brackish water incursion at that period in the region. (C) 2014 Elsevier GmbH. All rights reserved. |
| 研究领域[WOS] | Geochemistry & Geophysics |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000355366000011 |
| 源URL | [http://ir.ceode.ac.cn/handle/183411/38512]  |
| 专题 | 遥感与数字地球研究所_SCI/EI期刊论文_期刊论文 |
| 作者单位 | 1.[Heilbronn, G. 2.Boulvais, P. 3.Marchand, E. 4.Robin, C. 5.Bourquin, S. 6.Jolivet, M.] Univ Rennes 1, Observ Sci Universe Rennes, Geosci Rennes, UMR 6118, Rennes, France 7.[Barrier, L.] Univ Paris Diderot, Sorbonne Paris Cite, Inst Phys Globe Paris, UMR CNRS 7154, F-75005 Paris, France 8.[Jia, Y. 9.Fu, B.] Chinese Acad Sci, Ctr Earth Observat & Digital Earth, Beijing, Peoples R China |
| 推荐引用方式 GB/T 7714 | Heilbronn, G.,Boulvais, P.,Marchand, E.,et al. Stable isotope characterization of pedogenic and lacustrine carbonates from the Chinese Tian Shan: Constraints on the Mesozoic-Lower Cenozoic palaeoenvironmental evolution[J]. CHEMIE DER ERDE-GEOCHEMISTRY,2015,75(1):4279-4295. |
| APA | Heilbronn, G..,Boulvais, P..,Marchand, E..,Robin, C..,Bourquin, S..,...&Jolivet, M..(2015).Stable isotope characterization of pedogenic and lacustrine carbonates from the Chinese Tian Shan: Constraints on the Mesozoic-Lower Cenozoic palaeoenvironmental evolution.CHEMIE DER ERDE-GEOCHEMISTRY,75(1),4279-4295. |
| MLA | Heilbronn, G.,et al."Stable isotope characterization of pedogenic and lacustrine carbonates from the Chinese Tian Shan: Constraints on the Mesozoic-Lower Cenozoic palaeoenvironmental evolution".CHEMIE DER ERDE-GEOCHEMISTRY 75.1(2015):4279-4295. |
入库方式： OAI收割
来源：遥感与数字地球研究所
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