Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, China

During the Late Neoproterozoic and Early Cambrian, a series of paleogeographic and paleoecological events occurred associated with deglaciations and the evolution of life. The appearance of fossils representing diverse phyla, novel body plans and complex ecologies in Ediacaran and Cambrian sedimenta...

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Main Authors: Feng Tang, Si-cun Song, Guang-xu Zhang, Ai-lin Chen, Jun-ping Liu
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2021-06-01
Series:China Geology
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2096519221000525
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author Feng Tang
Si-cun Song
Guang-xu Zhang
Ai-lin Chen
Jun-ping Liu
author_facet Feng Tang
Si-cun Song
Guang-xu Zhang
Ai-lin Chen
Jun-ping Liu
author_sort Feng Tang
collection DOAJ
description During the Late Neoproterozoic and Early Cambrian, a series of paleogeographic and paleoecological events occurred associated with deglaciations and the evolution of life. The appearance of fossils representing diverse phyla, novel body plans and complex ecologies in Ediacaran and Cambrian sedimentary successions has sparked diverse hypotheses about potential drivers for the radiation of early animals during this interval. Recently, new macroscopic fossils of carbonaceous compressions with unique features have been found in Anning, Yunnan, China. The fossils’ bodies are ribbon-shaped and bilaterally symmetric, with dense longitudinal features and transversal features. The fossils occur 0.68 m below a bentonite interlayer which has been dated 535.2 ± 1.7 Ma by Ri-xiang Zhu and his team in 2009. The relatively simply morphology of these fossils, coupled with a lack of preserved internal structures challenge efforts taxonomically identify the precursor organism and definitively ally it to a living group. However, the symmetry and unusual features of the body are analogous to members of Platyzoa. The presence of ribbon-shaped fossils in the Zhongyicun Member in Anning indicates that these organisms were at least a locally significant component of Cambrian seafloor ecosystems, and may hold important implications for our understanding of the early evolution of Bilateria.
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spelling doaj.art-2b931b3e7ea04279b2f61b9b9d36ad012023-02-07T04:22:31ZengKeAi Communications Co., Ltd.China Geology2096-51922021-06-0142205214Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, ChinaFeng Tang0Si-cun Song1Guang-xu Zhang2Ai-lin Chen3Jun-ping Liu4Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China; Corresponding author: E-mail address: tangfeng65@qq.com (Feng Tang); sicun.song.sicun.song19@ucl.ac.uk (Si-cun Song).Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China; Department of Earth Sciences, University College London, London WC1E6BT, United Kingdom; Corresponding author: E-mail address: tangfeng65@qq.com (Feng Tang); sicun.song.sicun.song19@ucl.ac.uk (Si-cun Song).Yunnan Key Laboratory For Palaeobiology, Kunming 650091, ChinaResearch Center of Paleobiology, Yuxi Normal University, Yuxi 653100, ChinaYunnan Institute of Geological Survey, Kunming 650216, ChinaDuring the Late Neoproterozoic and Early Cambrian, a series of paleogeographic and paleoecological events occurred associated with deglaciations and the evolution of life. The appearance of fossils representing diverse phyla, novel body plans and complex ecologies in Ediacaran and Cambrian sedimentary successions has sparked diverse hypotheses about potential drivers for the radiation of early animals during this interval. Recently, new macroscopic fossils of carbonaceous compressions with unique features have been found in Anning, Yunnan, China. The fossils’ bodies are ribbon-shaped and bilaterally symmetric, with dense longitudinal features and transversal features. The fossils occur 0.68 m below a bentonite interlayer which has been dated 535.2 ± 1.7 Ma by Ri-xiang Zhu and his team in 2009. The relatively simply morphology of these fossils, coupled with a lack of preserved internal structures challenge efforts taxonomically identify the precursor organism and definitively ally it to a living group. However, the symmetry and unusual features of the body are analogous to members of Platyzoa. The presence of ribbon-shaped fossils in the Zhongyicun Member in Anning indicates that these organisms were at least a locally significant component of Cambrian seafloor ecosystems, and may hold important implications for our understanding of the early evolution of Bilateria.http://www.sciencedirect.com/science/article/pii/S2096519221000525Early CambrianPlatyhelmintheBilateriaMacrofossilEastern YunnanGeological survey engineering
spellingShingle Feng Tang
Si-cun Song
Guang-xu Zhang
Ai-lin Chen
Jun-ping Liu
Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, China
China Geology
Early Cambrian
Platyhelminthe
Bilateria
Macrofossil
Eastern Yunnan
Geological survey engineering
title Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, China
title_full Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, China
title_fullStr Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, China
title_full_unstemmed Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, China
title_short Enigmatic ribbon-like fossil from Early Cambrian of Yunnan, China
title_sort enigmatic ribbon like fossil from early cambrian of yunnan china
topic Early Cambrian
Platyhelminthe
Bilateria
Macrofossil
Eastern Yunnan
Geological survey engineering
url http://www.sciencedirect.com/science/article/pii/S2096519221000525
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