Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China

Dickinsonia is an iconic fossil of the Ediacara biota (similar to 575-539 Ma). It was previously known from siliciclastic successions of the White Sea assemblage in Australia, Baltica, and possibly India. Here we describe Dickinsonia sp. from the terminal Ediacaran Shibantan Member limestone (ca. 55...

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Published in:Palaeoworld
Main Authors: Wang, Xiao-Peng, Chen, Zhe, Pang, Ke, Zhou, Chuan-Ming, Xiao, Shuhai, Wan, Bin, Yuan, Xun-Lai
Format: Report
Language:English
Published: ELSEVIER 2021
Subjects:
AGE
Online Access:http://ir.nigpas.ac.cn/handle/332004/40096
https://doi.org/10.1016/j.palwor.2021.01.002
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spelling ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/40096 2023-05-15T18:43:47+02:00 Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China Wang, Xiao-Peng Chen, Zhe Pang, Ke Zhou, Chuan-Ming Xiao, Shuhai Wan, Bin Yuan, Xun-Lai 2021-12-01 http://ir.nigpas.ac.cn/handle/332004/40096 https://doi.org/10.1016/j.palwor.2021.01.002 英语 eng ELSEVIER PALAEOWORLD http://ir.nigpas.ac.cn/handle/332004/40096 doi:10.1016/j.palwor.2021.01.002 Dickinsonia Shibantan biota Ediacaran Yangtze Gorges area South China MICROBIAL MATS TRACE FOSSIL EVOLUTION OXYGEN BIOTA AGE PRESERVATION COMPLEXITY AFFINITY ANIMALS Paleontology 期刊论文 2021 ftchinacscnigpas https://doi.org/10.1016/j.palwor.2021.01.002 2021-12-17T01:08:46Z Dickinsonia is an iconic fossil of the Ediacara biota (similar to 575-539 Ma). It was previously known from siliciclastic successions of the White Sea assemblage in Australia, Baltica, and possibly India. Here we describe Dickinsonia sp. from the terminal Ediacaran Shibantan Member limestone (ca. 551-543 Ma) of the Dengying Formation in the Yangtze Gorges area of South China. The stratigraphic distribution of Ediacara-type fossils in the Shibantan Member indicates that this biota uniquely preserves both the White Sea and Nama assemblages in stratigraphic succession. The new data presented here suggests that Dickinsonia had wider paleogeographic and paleoenvironmental distributions, implying its strong dispersal capability and environmental tolerance. (C) 2021 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved. Report White Sea Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) White Sea Palaeoworld 30 4 602 609
institution Open Polar
collection Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacscnigpas
language English
topic Dickinsonia
Shibantan biota
Ediacaran
Yangtze Gorges area
South China
MICROBIAL MATS
TRACE FOSSIL
EVOLUTION
OXYGEN
BIOTA
AGE
PRESERVATION
COMPLEXITY
AFFINITY
ANIMALS
Paleontology
spellingShingle Dickinsonia
Shibantan biota
Ediacaran
Yangtze Gorges area
South China
MICROBIAL MATS
TRACE FOSSIL
EVOLUTION
OXYGEN
BIOTA
AGE
PRESERVATION
COMPLEXITY
AFFINITY
ANIMALS
Paleontology
Wang, Xiao-Peng
Chen, Zhe
Pang, Ke
Zhou, Chuan-Ming
Xiao, Shuhai
Wan, Bin
Yuan, Xun-Lai
Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
topic_facet Dickinsonia
Shibantan biota
Ediacaran
Yangtze Gorges area
South China
MICROBIAL MATS
TRACE FOSSIL
EVOLUTION
OXYGEN
BIOTA
AGE
PRESERVATION
COMPLEXITY
AFFINITY
ANIMALS
Paleontology
description Dickinsonia is an iconic fossil of the Ediacara biota (similar to 575-539 Ma). It was previously known from siliciclastic successions of the White Sea assemblage in Australia, Baltica, and possibly India. Here we describe Dickinsonia sp. from the terminal Ediacaran Shibantan Member limestone (ca. 551-543 Ma) of the Dengying Formation in the Yangtze Gorges area of South China. The stratigraphic distribution of Ediacara-type fossils in the Shibantan Member indicates that this biota uniquely preserves both the White Sea and Nama assemblages in stratigraphic succession. The new data presented here suggests that Dickinsonia had wider paleogeographic and paleoenvironmental distributions, implying its strong dispersal capability and environmental tolerance. (C) 2021 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.
format Report
author Wang, Xiao-Peng
Chen, Zhe
Pang, Ke
Zhou, Chuan-Ming
Xiao, Shuhai
Wan, Bin
Yuan, Xun-Lai
author_facet Wang, Xiao-Peng
Chen, Zhe
Pang, Ke
Zhou, Chuan-Ming
Xiao, Shuhai
Wan, Bin
Yuan, Xun-Lai
author_sort Wang, Xiao-Peng
title Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
title_short Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
title_full Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
title_fullStr Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
title_full_unstemmed Dickinsonia from the Ediacaran Dengying Formation in the Yangtze Gorges area, South China
title_sort dickinsonia from the ediacaran dengying formation in the yangtze gorges area, south china
publisher ELSEVIER
publishDate 2021
url http://ir.nigpas.ac.cn/handle/332004/40096
https://doi.org/10.1016/j.palwor.2021.01.002
geographic White Sea
geographic_facet White Sea
genre White Sea
genre_facet White Sea
op_relation PALAEOWORLD
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doi:10.1016/j.palwor.2021.01.002
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