Molecular record of the SPICE event in well YD2, Tarim Basin: Insights from catalytic hydropyrolysis of kerogens
文献类型：期刊论文
| 作者 | Wang, Haozhe1,3,4; Zhao, Guanyu1,3,4; Cheng, Bin1,3; Zhang, Haizu2; Liao, Zewen1,3 |
| 刊名 | MARINE AND PETROLEUM GEOLOGY
 |
| 出版日期 | 2023-02-01 |
| 卷号 | 148页码:13 |
| 关键词 | SPICE event Catalytic hydropyrolysis Plankton evolution Regression-transgression cycle Redox changes Late Cambrian Tarim Basin |
| ISSN号 | 0264-8172 |
| DOI | 10.1016/j.marpetgeo.2022.106038 |
| 英文摘要 | The Steptoean Positive Carbon Isotope Excursion (SPICE) event is extensively documented in globally distributed carbonate and organic-rich successions of slope and platform environments during the late Cambrian (ca. 497-494 Ma). Despite numerous studies, its regional manifestation remains controversial because of the major uncertainty of the redox conditions in sedimentary paleoenvironments and its effect on the changes in the biota. Biogeochemical processes that occurred during the SPICE event are important for assessing whether the excursion is associated with the co-evolution of organisms and environments. In this study, we investigated the changes in plankton and paleoenvironment at the molecular level by combining kerogen elemental analysis, catalytic hydropyrolysis (HyPy), and gas chromatography-mass spectrometry (GC-MS) analyses of saturates and aromatics with published carbon isotopic data. The three fluorene series, gammacerane/C30hopane (G/C30H) and pristine/phytane (Pr/Ph) ratios demonstrated that the shallow shelf seawater changed significantly from relatively reducing to oxidizing and back to reducing conditions during the SPICE interval coupled with a regression-transgression cycle. The phytoplankton during the rise of the SPICE were mainly organic-walled, such as cyanobacteria, various acritarchs, and algae, as evidenced by terpanes, hopanes, and steranes. Significant decreases in phytoplankton diversity and abundance coincided with the peak of the SPICE, corresponding to the most oxidized and hypersaline periods during the SPICE event in the eastern Tarim Basin. Plankton assemblages diversified significantly with increasing living space due to the rise of sea-level during the post-SPICE period. Therefore, this study supports the idea that plankton groups changed dramatically with the environment, and its revolution followed the SPICE into the Great Ordovician Biodiversification Event. |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000901541600002 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/71375]  |
| 专题 | 有机地球化学国家重点实验室 |
| 通讯作者 | Cheng, Bin; Liao, Zewen |
| 作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Peoples R China 2.PetroChina Tarim Oilfield Co, Res Inst Petr Explorat & Dev, Korla 841000, Peoples R China 3.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China 4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Haozhe,Zhao, Guanyu,Cheng, Bin,et al. Molecular record of the SPICE event in well YD2, Tarim Basin: Insights from catalytic hydropyrolysis of kerogens[J]. MARINE AND PETROLEUM GEOLOGY,2023,148:13. |
| APA | Wang, Haozhe,Zhao, Guanyu,Cheng, Bin,Zhang, Haizu,&Liao, Zewen.(2023).Molecular record of the SPICE event in well YD2, Tarim Basin: Insights from catalytic hydropyrolysis of kerogens.MARINE AND PETROLEUM GEOLOGY,148,13. |
| MLA | Wang, Haozhe,et al."Molecular record of the SPICE event in well YD2, Tarim Basin: Insights from catalytic hydropyrolysis of kerogens".MARINE AND PETROLEUM GEOLOGY 148(2023):13. |
入库方式： OAI收割
来源：广州地球化学研究所
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。