IGGCAS OpenIR  > 油气资源研究院重点实验室
Palaeoenvironmental distribution of Ordovician dasycladaleans in the Tarim Basin, Xinjiang, China
Zhang, Yue-Yang1,2,3; Jiang, Hong-Xia4; Wu, Ya-Sheng1,2,3; Pan, Wen-Qing5; Liu, Li-Jing6; Zhang, Bao-Shou5; Zhang, Liu-Ping1,2,3
2020-05-18
Source PublicationGEOLOGICAL JOURNAL
ISSN0072-1050
Pages17
AbstractDasycladalean calcified green algae are common in the Phanerozoic, and have been reported from various lagoons and other environments of post-Ordovician periods. There is a paucity of studies exploring palaeoecology of Ordovician dasycladaleans. Based on examination of 1,089 large thin sections from the Upper Ordovician Lianglitag Formation in 12 drilling wells in the Tarim Basin, Xinjiang, China, dasycladaleans mainly occur in platform margins, less abundant in open platforms, and absent from restricted platform tidal-flats and lagoons. Lagoons used here are in a geological sense, referring to only water bodies enclosed by reefs and banks and featured by abnormal salinity and monotonous eurytopic animals. According to lithology and biota, the lagoons in previous studies are actually open platforms. Thus, this study shows that dasycladaleans are not adapted to lagoons, and this nature of them did not change with time. Statistical analysis shows that occurrence frequency of the Ordovician dasycladaleans is 52% in platform margin environments, 22% in open platform environments, and 0% in restricted platform environments.
Keyworddasycladaleans Ordovician palaeoecology palaeogeographic distribution Tarim Basin
DOI10.1002/gj.3857
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences
WOS KeywordCARBONATE PLATFORM ; CARNIC ALPS ; DEPOSITIONAL-ENVIRONMENTS ; ALGAL MOUNDS ; LIMESTONE ; FACIES ; MARGIN ; SOUTH ; MOUNTAINS ; ROMANIA
Language英语
Funding ProjectNational Natural Science Foundation of China[41972320] ; National Science and Technology Major Project[2016ZX05004-004] ; Chinese Academy of Sciences[XDB26000000]
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000533327700001
PublisherWILEY
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/96743
Collection油气资源研究院重点实验室
Corresponding AuthorWu, Ya-Sheng
Affiliation1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
3.Univ Chinese Acad Sci, Beijing, Peoples R China
4.Hebei Geo Univ, Inst Paleontol, Shijiazhuang, Hebei, Peoples R China
5.PetroChina, Res Inst Petr Explorat & Dev, Tarim Oilfield Co, Korla, Peoples R China
6.Northwest Univ, Geol Dept, Xian, Peoples R China
First Author AffilicationKey Laboratory of Petroleum Resource Research, Chinese Academy of Sciences
Corresponding Author AffilicationKey Laboratory of Petroleum Resource Research, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Zhang, Yue-Yang,Jiang, Hong-Xia,Wu, Ya-Sheng,et al. Palaeoenvironmental distribution of Ordovician dasycladaleans in the Tarim Basin, Xinjiang, China[J]. GEOLOGICAL JOURNAL,2020:17.
APA Zhang, Yue-Yang.,Jiang, Hong-Xia.,Wu, Ya-Sheng.,Pan, Wen-Qing.,Liu, Li-Jing.,...&Zhang, Liu-Ping.(2020).Palaeoenvironmental distribution of Ordovician dasycladaleans in the Tarim Basin, Xinjiang, China.GEOLOGICAL JOURNAL,17.
MLA Zhang, Yue-Yang,et al."Palaeoenvironmental distribution of Ordovician dasycladaleans in the Tarim Basin, Xinjiang, China".GEOLOGICAL JOURNAL (2020):17.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Zhang, Yue-Yang]'s Articles
[Jiang, Hong-Xia]'s Articles
[Wu, Ya-Sheng]'s Articles
Baidu academic
Similar articles in Baidu academic
[Zhang, Yue-Yang]'s Articles
[Jiang, Hong-Xia]'s Articles
[Wu, Ya-Sheng]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Zhang, Yue-Yang]'s Articles
[Jiang, Hong-Xia]'s Articles
[Wu, Ya-Sheng]'s Articles
Terms of Use
No data!
Social Bookmark/Share
Add to CiteULike Add to Connotea Add to Del.icio.us Add to Digg Add to Reddit Add to Technorati
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.