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The Ediacaran frondose fossilArboreafrom the Shibantan limestone of South China
Wang, Xiaopeng1,2,4; Pang, Ke (庞科)1,2,5; Chen, Zhe (陈哲)1,2,5; Wan, Bin (万斌)1,2,5; Xiao, Shuhai3; Zhou, Chuanming (周传明)1,2,5; Yuan, Xunlai (袁训来)1,2,5,6
2020-11-01
Source PublicationJOURNAL OF PALEONTOLOGY
ISSN0022-3360
Volume94Issue:6Pages:1034-1050
Abstract

Bituminous limestone of the Ediacaran Shibantan Member of the Dengying Formation (551-539 Ma) in the Yangtze Gorges area contains a rare carbonate-hosted Ediacara-type macrofossil assemblage. This assemblage is dominated by the tubular fossilWutubusChen et al., 2014 and discoidal fossils, e.g.,HiemaloraFedonkin, 1982 andAspidellaBillings, 1872, but frondose organisms such asCharniaFord, 1958,RangeaGurich, 1929, andArboreaGlaessner and Wade, 1966 are also present. Herein, we report four species ofArboreafrom the Shibantan assemblage, including the type speciesArborea arborea(Glaessner in Glaessner and Daily, 1959) Glaessner and Wade, 1966,Arborea denticulatanew species, and two unnamed species,Arboreasp. A andArboreasp. B.Arborea arboreais the most abundant frond in the Shibantan assemblage.Arborea denticulatan. sp. resemblesArborea arboreain general morphology but differs in its fewer primary branches and lower length/width ratio of primary branches.Arboreasp. A andArboreasp. B are fronds with aHiemalora-type basal attachment. Sealing by microbial mats and authigenic cementation may have played an important role in the preservation ofArboreain the Shibantan assemblage. The Shibantan material ofArboreaextends the stratigraphic, ecological, and taphonomic ranges of this genus. UUID:http://zoobank.org/554f21da-5f09-4891-9deb-cbc00c41e5f1

DOI10.1017/jpa.2020.43
Indexed BySCI
Language英语
WOS KeywordYANGTZE GORGES AREA ; DEATH MASK MODEL ; DENGYING FORMATION ; MICROBIAL MATS ; MISTAKEN POINT ; TRACE FOSSIL ; PRESERVATION ; BIOTA ; ANIMALS ; ORGANISMS
Funding ProjectChinese Academy of Sciences[QYZDJ-SSW-DQC009] ; Chinese Academy of Sciences[XDB26000000] ; Chinese Academy of Sciences[XDB18000000] ; National Natural Science Foundation of China[41921002] ; National Natural Science Foundation of China[41602007] ; Chinese Ministry of Science and Technology[2017YFC0603100] ; Science Foundation of Jiangsu Province of China[BK20161090] ; State Key Laboratory of Palaeobiology and Stratigraphy[20201102] ; U.S. National Science Foundation[EAR-2021207]
WOS Research AreaPaleontology
WOS SubjectPaleontology
WOS IDWOS:000574601900002
Funding OrganizationChinese Academy of Sciences ; National Natural Science Foundation of China ; Chinese Ministry of Science and Technology ; Science Foundation of Jiangsu Province of China ; State Key Laboratory of Palaeobiology and Stratigraphy ; U.S. National Science Foundation
PublisherCAMBRIDGE UNIV PRESS
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/32592
Collection中国科学院南京地质古生物研究所
Corresponding AuthorPang, Ke (庞科); Chen, Zhe (陈哲)
Affiliation1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Life & Palaeoenvironm, Nanjing 210008, Peoples R China
3.Virginia Tech, Dept Geosci, Blacksburg, VA 24061 USA
4.Univ Sci & Technol China, Hefei 230026, Peoples R China
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
6.Nanjing Univ, Ctr Res & Educ Biol Evolut & Environm, Nanjing 210023, Peoples R China
First Author AffilicationNanjing Institute of Geology and Palaeonotology,CAS
Corresponding Author AffilicationNanjing Institute of Geology and Palaeonotology,CAS
Recommended Citation
GB/T 7714
Wang, Xiaopeng,Pang, Ke ,Chen, Zhe ,et al. The Ediacaran frondose fossilArboreafrom the Shibantan limestone of South China[J]. JOURNAL OF PALEONTOLOGY,2020,94(6):1034-1050.
APA Wang, Xiaopeng.,Pang, Ke .,Chen, Zhe .,Wan, Bin .,Xiao, Shuhai.,...&Yuan, Xunlai .(2020).The Ediacaran frondose fossilArboreafrom the Shibantan limestone of South China.JOURNAL OF PALEONTOLOGY,94(6),1034-1050.
MLA Wang, Xiaopeng,et al."The Ediacaran frondose fossilArboreafrom the Shibantan limestone of South China".JOURNAL OF PALEONTOLOGY 94.6(2020):1034-1050.
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