中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Diversity and systematics of Middle-Late Ordovician calcified cyanobacteria and associated microfossils from Ordos Basin, North China

文献类型:期刊论文

作者Liu, Lijing3; Wu, Yasheng2; Bao, Hongping4; Jiang, Hongxia1; Zheng, Lijing2; Chen, Yanlong3
刊名JOURNAL OF PALEONTOLOGY
出版日期2021
卷号95期号:1页码:1-23
ISSN号0022-3360
DOI10.1017/jpa.2020.82
英文摘要Calcified cyanobacteria are of considerable research value for reconstructing the ecology of Paleozoic and Mesozoic benthic communities on carbonate platforms due to their ability to produce oxygen and fix nitrogen and CO2. The diversity and abundance of calcified cyanobacteria was initially suggested to have declined in the Middle and Late Ordovician, although more recent work suggests that complex and diverse assemblages persisted throughout the Ordovician. Here, calcified cyanobacteria and associated microfossil flora from the Middle and Late Ordovician of the Ordos Basin, North China Block, are systematically described for the first time based on 1330 thin sections from seven outcrop profiles and four drill cores. In total, there are 18 species belonging to 16 genera, including a new species, Proaulopora ordosia n. sp. Girvanella, Subtifloria, Acuasiphonoria, Xianella, and Oscillatoriaceae gen. indet. are assigned to Osillatoriales of cyanobacteria; Ortonella, Hedstroemia, Cayeuxia, Zonotrichites, Proaulopora, and Phacelophyton are assigned to Nostocales of cyanobacteria; and Garwoodia, Renalcis, Izhella, Rothpletzella, and Wetheredella are assigned to calcified Microproblematica. A literature survey of Ordovician microfloral assemblages shows that cyanobacteria and associated microfossils occur in reef, open platform, lagoon, and tidal facies. Most genera occur on at least two independent blocks, and many have a cosmopolitan distribution in similar sedimentary facies. Our research suggests that calcified cyanobacteria and associated microfossils formed complex ecosystems and played greater ecological roles on carbonate platforms during the late Middle and Late Ordovician than was previously thought. UUID: http://zoobank.org/1812ccf8-136c-4cff-92ba-faeaf06523ef
WOS关键词TARIM BASIN ; PINGLIANG FORMATION ; CARBONATE PLATFORM ; ALGAE ; CALCIFICATION ; REEFS ; STROMATOLITES ; WETHEREDELLA ; SUBSURFACE ; GIRVANELLA
资助项目National Natural Science Foundation of China[42072127] ; National Natural Science Foundation of China[41502004] ; National Natural Science Foundation of China[41972143] ; National Natural Science Foundation of China[41502148] ; National Natural Science Foundation of China[41720104002] ; National Natural Science Foundation of China[41890844] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000] ; Natural Science Foundation of Shaanxi Province[2018JM4037] ; National Science and Technology Major Project[2016ZX05004006]
WOS研究方向Paleontology
语种英语
出版者CAMBRIDGE UNIV PRESS
WOS记录号WOS:000601088700001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; Natural Science Foundation of Shaanxi Province ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project
源URL[http://ir.iggcas.ac.cn/handle/132A11/99945]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Liu, Lijing; Wu, Yasheng
作者单位1.Hebei GEO Univ, Shijiazhuang 050031, Hebei, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
3.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China
4.Changqing Oilfield, Res Inst Petr Explorat & Dev, Xian 710021, Peoples R China
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Liu, Lijing,Wu, Yasheng,Bao, Hongping,et al. Diversity and systematics of Middle-Late Ordovician calcified cyanobacteria and associated microfossils from Ordos Basin, North China[J]. JOURNAL OF PALEONTOLOGY,2021,95(1):1-23.
APA Liu, Lijing,Wu, Yasheng,Bao, Hongping,Jiang, Hongxia,Zheng, Lijing,&Chen, Yanlong.(2021).Diversity and systematics of Middle-Late Ordovician calcified cyanobacteria and associated microfossils from Ordos Basin, North China.JOURNAL OF PALEONTOLOGY,95(1),1-23.
MLA Liu, Lijing,et al."Diversity and systematics of Middle-Late Ordovician calcified cyanobacteria and associated microfossils from Ordos Basin, North China".JOURNAL OF PALEONTOLOGY 95.1(2021):1-23.

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来源:地质与地球物理研究所

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