KMS Nanjing Institute of Geology and Palaeonotology,CAS
Astronomically forced dynamics of Late Devonian (Famennian) sea level and biotic recovery in western Junggar, Northwest China | |
通讯作者 | Ma, Kunyuan([email protected]) ; Gong, Yiming([email protected]) |
Ma, Kunyuan1,2,3; Hinnov, Linda3; Wang, Zhihong4; Wang, Kai2; Zong, Ruiwen2; Zhang, Xinsong5; Song, Junjun6; Bai, Yang1; Gong, Yiming2 | |
2025-02-01 | |
发表期刊 | GLOBAL AND PLANETARY CHANGE
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ISSN | 0921-8181 |
卷号 | 245页码:18 |
摘要 | The Hongguleleng Formation in western Junggar, northwest China preserves a rich variety of fossils and was previously regarded as a "refugium" during the Late Devonian biotic crisis. Uncertainty in the age of the Hongguleleng Formation has persisted for a considerable time. In this study, cyclostratigraphic analysis was carried out on the Upper Devonian Bulongguoer and Wulankeshun sections from western Junggar, northwest China. Time series analysis and modeling of iron (Fe) concentration proxy data reveal variations with frequencies comparable to those of the Earth's long and short orbital eccentricity, obliquity, and precession index in both successions. Interpreted 405-kyr long orbital eccentricity cycles were used to establish floating astronomical time scales (FATs) for the two successions. From these FATs the depositional duration of the Hongguleleng Formation is calculated as 11.5 +/- 0.58 Myr. The Devonian-Carboniferous boundary age of 359.3 +/- 0.3 Ma was chosen as a time "anchor", resulting in an astronomically determined age of 370.2 +/- 0.66 Ma for the base of the Hongguleleng Formation. Combined with conodont biostratigraphy, this age indicates that the Hongguleleng Formation in western Junggar does not reach down to the Frasnian-Famennian boundary. Sedimentary noise modeling of the reconstructed Fe concentration time series provides an interpretation of sea-level variations in the PaleoAsian Ocean controlled by astronomical forcing from very long orbital eccentricity cycles (g4-g3) throughout the Late Devonian period. Intensified monsoonal climates during these orbital eccentricity cycle maxima led to elevated terrigenous input and strengthened upwelling, which enhanced primary productivity in the western Junggar. We propose an "astronomical climate change" model as a driving mechanism that led to biotic recovery in the Famennian Hongguleleng Formation. |
关键词 | Cyclostratigraphy Astronomical time scale Devonian Sea-level change Hongguleleng Formation |
DOI | 10.1016/j.gloplacha.2024.104677 |
收录类别 | SCI |
语种 | 英语 |
关键词[WOS] | NW CHINA ; CYCLOSTRATIGRAPHIC CALIBRATION ; ORBITAL CYCLOSTRATIGRAPHY ; HONGGULELENG FORMATION ; KELLWASSER ANOXIA ; MASS EXTINCTION ; MARINE ANOXIA ; SOUTH CHINA ; CLIMATE ; XINJIANG |
资助项目 | National Natural Science Foundation of China[42202030] ; National Natural Science Foundation of China[42272014] ; National Natural Science Foundation of China[42072041] ; National Natural Science Foundation of China[41872034] ; National Natural Science Foundation of China[41802018] ; National Natural Science Foundation of China[41290260] ; Fundamental Research Program of Shanxi Province[202103021223037] ; Fundamental Research Program of Shanxi Province[202303021212041] ; State Key Laboratory of Ore Deposit Geochemistry open found[202208] ; Heising-Simons Foundation[2021-2796] |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:001389773700001 |
项目资助者 | National Natural Science Foundation of China ; Fundamental Research Program of Shanxi Province ; State Key Laboratory of Ore Deposit Geochemistry open found ; Heising-Simons Foundation |
出版者 | ELSEVIER |
文献类型 | 期刊论文 |
条目标识符 | http://ir.nigpas.ac.cn/handle/332004/44758 |
专题 | 中国科学院南京地质古生物研究所 |
通讯作者 | Ma, Kunyuan; Gong, Yiming |
作者单位 | 1.Taiyuan Univ Technol, Coll Geol & Surveying Engn, Taiyuan 030024, Peoples R China 2.China Univ Geosci, Sch Earth Sci, State Key Lab Biogeol & Environm Geol, Wuhan 430205, Peoples R China 3.George Mason Univ, Dept Atmospher Ocean & Earth Sci, Fairfax, VA 22030 USA 4.China Geol Survey, Wuhan Ctr, Geosci Innovat Ctr Cent South China, Wuhan 430074, Peoples R China 5.Fuzhou Univ, Zijin Min Coll, Fuzhou 350108, Peoples R China 6.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China |
推荐引用方式 GB/T 7714 | Ma, Kunyuan,Hinnov, Linda,Wang, Zhihong,et al. Astronomically forced dynamics of Late Devonian (Famennian) sea level and biotic recovery in western Junggar, Northwest China[J]. GLOBAL AND PLANETARY CHANGE,2025,245:18. |
APA | Ma, Kunyuan.,Hinnov, Linda.,Wang, Zhihong.,Wang, Kai.,Zong, Ruiwen.,...&Gong, Yiming.(2025).Astronomically forced dynamics of Late Devonian (Famennian) sea level and biotic recovery in western Junggar, Northwest China.GLOBAL AND PLANETARY CHANGE,245,18. |
MLA | Ma, Kunyuan,et al."Astronomically forced dynamics of Late Devonian (Famennian) sea level and biotic recovery in western Junggar, Northwest China".GLOBAL AND PLANETARY CHANGE 245(2025):18. |
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