Climate Change Data Portal
DOI | 10.1016/j.palaeo.2019.05.003 |
Conodont biostratigraphy and astronomical tuning of the Lower–Middle Ordovician Liangjiashan (North China) and Huanghuachang (South China) marine sections | |
Ma K.; Li R.; Hinnov L.A.; Gong Y. | |
发表日期 | 2019 |
ISSN | 0031-0182 |
起始页码 | 272 |
结束页码 | 287 |
卷号 | 528 |
英文摘要 | In this study, systematic conodont biostratigraphy and cyclostratigraphy are carried out on Ordovician sections from the North China and South China blocks. The Liangjiashan section, situated on the North China Block margin, accumulated shallow marine carbonate during the Early Ordovician. The Huanghuachang section (GSSP for the Dapingian Stage), situated on the South China Block margin, accumulated thinly bedded carbonates and minor clastics in a deep shelf environment. Conodont biostratigraphy and 405-kyr long-eccentricity cycles interpreted from the Liangjiashan and Huanghuachang sections are used to establish an Astronomical Time Scale (ATS) for the Early–Middle Ordovician period. The ATS indicates that the duration of the Floian Stage is 7.08 ± 0.405 Myr. The temporal ranges of Lower–Middle Ordovician conodont biozones are also estimated: the durations of the Serratognathus bilobatus, Serratognathus extensus, Oepikodus communis, Oepikodus evae, and Baltoniodus triangularis zones are 1.0 Myr, 5.1 Myr, 0.2 Myr, 0.8 Myr, and 0.2 Myr, respectively. The evolution of the ratio of obliquity to total power and short-eccentricity power to total power depicts periodicities of 1 Myr for the s4–s3 term, and 1.9 Myr shifting to 1 Myr for the g4–g3 term. The shift in the g4–g3 term may indicate a chaotic transition in the Mars and Earth orbital motions from a (s4–s3)–2(g4–g3) to (s4–s3)–(g4–g3) resonance state during the Early Ordovician. © 2019 Elsevier B.V. |
英文关键词 | Astronomical time scale; Conodont biozones; Cyclostratigraphy; Earth-Mars chaotic transition; Floian |
语种 | 英语 |
scopus关键词 | astronomy; biostratigraphy; biozonation; conodont; cyclostratigraphy; eccentricity; Ordovician; periodicity; timescale; China; North China Block; South China Block |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/150918 |
作者单位 | State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China; Department of Atmospheric, Oceanic, and Earth Sciences, George Mason University, Fairfax, VA 22030, United States |
推荐引用方式 GB/T 7714 | Ma K.,Li R.,Hinnov L.A.,等. Conodont biostratigraphy and astronomical tuning of the Lower–Middle Ordovician Liangjiashan (North China) and Huanghuachang (South China) marine sections[J],2019,528. |
APA | Ma K.,Li R.,Hinnov L.A.,&Gong Y..(2019).Conodont biostratigraphy and astronomical tuning of the Lower–Middle Ordovician Liangjiashan (North China) and Huanghuachang (South China) marine sections.Palaeogeography, Palaeoclimatology, Palaeoecology,528. |
MLA | Ma K.,et al."Conodont biostratigraphy and astronomical tuning of the Lower–Middle Ordovician Liangjiashan (North China) and Huanghuachang (South China) marine sections".Palaeogeography, Palaeoclimatology, Palaeoecology 528(2019). |
条目包含的文件 | 条目无相关文件。 |
个性服务 |
推荐该条目 |
保存到收藏夹 |
导出为Endnote文件 |
谷歌学术 |
谷歌学术中相似的文章 |
[Ma K.]的文章 |
[Li R.]的文章 |
[Hinnov L.A.]的文章 |
百度学术 |
百度学术中相似的文章 |
[Ma K.]的文章 |
[Li R.]的文章 |
[Hinnov L.A.]的文章 |
必应学术 |
必应学术中相似的文章 |
[Ma K.]的文章 |
[Li R.]的文章 |
[Hinnov L.A.]的文章 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。