Biostratigraphically-controlled Darriwilian (Middle Ordovician) d(13)C excursions in North China: Implications for correlation and climate change
文献类型：期刊论文
| 作者 | Jing, Xiuchun1,5,6; Zhao, Zhenyu4; Fu, Ling4; Zhang, Caili3; Fan, Ru4; Shen, Yang5,6; Yang, Biao2 |
| 刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
 |
| 出版日期 | 2022-09-01 |
| 卷号 | 601页码:20 |
| 关键词 | Conodont biostratigraphy d(13)C chemostratigraphy The LDNICE The MDICE Carbon cycle |
| ISSN号 | 0031-0182 |
| DOI | 10.1016/j.palaeo.2022.111149 |
| 通讯作者 | Jing, Xiuchun(jxch@cugb.edu.cn) |
| 英文摘要 | A continuous, 545 m thick carbonate succession through the Darriwilian Bei'anzhuang and Machiakou (Majiagou) formations in the Tao-112 drillcore in the Ordos Basin, North China was sampled for an integrated study of conodont biostratigraphy (48 samples) and carbon isotope chemostratigraphy (510 samples). Two internationally correlatable conodont biozones were recognized in the drillcore, namely the Histiodella holodentata-Tangshanodus tangshanensis Biozone and the Plectodina onychodonta Biozone in stratigraphically ascending order. Constrained by the conodont biostratigraphy, two carbon isotopic anomalies can be distinguished, including the short-term LDNICE (Lower Darriwilian Negative Isotopic Carbon Excursion) in the lower part of the Bei'anzhuang Formation, and the long-lasting MDICE (Middle Darriwilian Isotopic Carbon Excursion) spanning the upper part of the Bei'anzhuang Formation and much of the Machiakou Formation. Moreover, the present high-resolution carbon isotope record allows the recognition of two peaks of the MDICE, the stratigraphically lower, small peak MDICE-1 and the follow-up, long-lived peak MDICE-2. The Darriwilian carbon isotope excursions in North China can be comparable to the delta C-13(carb) trends described in coeval successions in Baltoscandia, North America, South Korea, and other regions of China, suggesting their significance for global correlations and providing an integrated and high-resolution chemo-biostratigraphic framework for sedimentary records of Darriwilian age in North China. Based on widely accepted driving mechanisms of global carbon-cycle perturbations, here we put forth an inference on the climatic pattern of the Darriwilian that a short warm period causing the LDNICE in the early Darriwilian was followed in turn by a moderate global cooling event resulting in the MDICE during the middle and late Darriwilian. Carbon cycle processes of the Middle and Late Ordovician indicate that there was a clear pre-Hirnantian cooling step, with gradually enlarged alternating relative warmer and rather cooler interludes, culminating in the "Hirnantian' ice age. |
| WOS关键词 | CARBON-ISOTOPE CHEMOSTRATIGRAPHY ; DELTA-C-13 CHEMOSTRATIGRAPHY ; TARIM BASIN ; CONODONT BIOSTRATIGRAPHY ; GLOBAL CORRELATION ; YANGTZE PLATFORM ; SOUTHERN SWEDEN ; STRATIGRAPHY ; RECORD ; BIODIVERSIFICATION |
| 资助项目 | State Key Laboratory of Palae-obiology and Stratigraphy, China (Nanjing Institute of Geology and Palaeontology, CAS)[213107] ; National Natural Science Foundation of China[4152026] ; National Natural Science Foundation of China[42172037] ; International Geoscience Programme (IGCP) Project 735 Rocks ; Rise of Ordovician Life: Filling knowledge gaps in the Early Palaeozoic Biodiversification' |
| WOS研究方向 | Physical Geography ; Geology ; Paleontology |
| 语种 | 英语 |
| WOS记录号 | WOS:000843319900002 |
| 出版者 | ELSEVIER |
| 资助机构 | State Key Laboratory of Palae-obiology and Stratigraphy, China (Nanjing Institute of Geology and Palaeontology, CAS) ; National Natural Science Foundation of China ; International Geoscience Programme (IGCP) Project 735 Rocks ; Rise of Ordovician Life: Filling knowledge gaps in the Early Palaeozoic Biodiversification' |
| 源URL | [http://ir.nigpas.ac.cn/handle/332004/41154]  |
| 专题 | 中国科学院南京地质古生物研究所 |
| 通讯作者 | Jing, Xiuchun |
| 作者单位 | 1.China Univ Geosci Beijing, Sch Earth Sci & Resources, Dept Stratig & Palaeontol, Beijing 100083, Peoples R China 2.Geol Geomat Inst Hebei, Langfang 065000, Peoples R China 3.PetroChina Changqing Oil Field Branch Co, Xian 710018, Peoples R China 4.PetroChina Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China 5.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China 6.China Univ Geosci Beijing, State Key Lab Geobiol & Environm Geol, Beijing 100083, Peoples R China |
| 推荐引用方式 GB/T 7714 | Jing, Xiuchun,Zhao, Zhenyu,Fu, Ling,et al. Biostratigraphically-controlled Darriwilian (Middle Ordovician) d(13)C excursions in North China: Implications for correlation and climate change[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2022,601:20. |
| APA | Jing, Xiuchun.,Zhao, Zhenyu.,Fu, Ling.,Zhang, Caili.,Fan, Ru.,...&Yang, Biao.(2022).Biostratigraphically-controlled Darriwilian (Middle Ordovician) d(13)C excursions in North China: Implications for correlation and climate change.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,601,20. |
| MLA | Jing, Xiuchun,et al."Biostratigraphically-controlled Darriwilian (Middle Ordovician) d(13)C excursions in North China: Implications for correlation and climate change".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 601(2022):20. |
入库方式： OAI收割
来源：南京地质古生物研究所
浏览0
下载0
收藏0
其他版本
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。