Cited by 202Paleontology and Stratigraphy of FossilsGeological and Geochemical AnalysisEvolution and Paleontology Studies

The tempo of Ediacaran evolution

Open access
Yang, Chuan, Rooney, Alan D., Condon, Daniel J., Li, Xian-Hua, Grazhdankin, Dmitriy V., Bowyer, Fred T., Hu, Chunlin, Macdonald, Francis A. +1 more·2021·Science Advances

Abstract

New radio-isotopic data bracket the age of late Ediacaran fossil assemblages and two negative carbon isotope excursions.

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Crossref · 10.1126/sciadv.abi9643

Cites

20 of 20 references verified0 citation errors · 0 not checkable

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  • Both the Avalon and White Sea paleocommunities largely disappeared by ~550.5 Ma.

    “Both the Avalon and White Sea paleocommunities largely disappeared by ~550.5 Ma (25, 27, 28)”

    From Sea level controls on Ediacaran-Cambrian animal radiations (2024) · cites this paper as [28]

    The Discussion (‘A refined record of Ediacaran biotic evolution’; page unavailable) places a postulated first extinction pulse of Ediacaran taxa at the White Sea–Nama transition after the ~550 Ma carbon-isotope excursion. That broadly supports a decline around the claimed date, but the paper does not say that both the Avalon and White Sea paleocommunities largely disappeared by ~550.5 Ma; it also presents the extinction as postulated, not established. (LLM, conf=0.82)

    Experimental — accuracy not yet measured
  • This age model is currently permissible as radiometric data that could constrain global δ13Ccarb are conspicuously absent between approximately 555 and 550 Ma from all carbonate-dominated successions, and major sequence boundaries or erosional surfaces are ubiquitous from <555 Ma to approximately >550.5 Ma in radiometrically dated carbonate-dominated successions.

    “This age model is currently permissible as radiometric data that could constrain global δ13Ccarb are conspicuously absent between approximately 555 and 550 Ma from all carbonate-dominated successions, and major sequence boundaries or erosional surfaces are ubiquitous from <555 Ma [e.g., (68)] to approximately >550.5 Ma (28) in radiometrically dated carbonate-dominated successions”

    From Sea level controls on Ediacaran-Cambrian animal radiations (2024) · cites this paper as [28]

    Split into 2 atoms — 0 confirmed, 2 partially supported, 0 disputed, 0 misattributed, 0 unverifiable. Expand the claim to see per-atom verdicts.

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Cites

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Research works printed but not linked: 17

  1. [1]S. H. Xiao, G. M. Narbonne, The Ediacaran Period (Elsevier B.V., 2020).
  2. [2]P. F. Hoffman, D. S. Abbot, Y. Ashkenazy, D. I. Benn, J. J. Brocks, P. A. Cohen, G. M. Cox, J. R. Creveling, Y. Donnadieu, D. H. Erwin, I. J. Fairchild, D. Ferreira, J. C. Goodman, G. P. Halverson, M. F. Jansen, G. Le Hir, G. D. Love, F. A. Macdonald, A. C. Maloof, C. A. Partin, G. Ramstein, B. E. J. Rose, C. V. Rose, P. M. Sadler, E. Tziperman, A. Voigt, S. G. Warren, Snowball Earth climate dynamics and Cryogenian geology-geobiology. Sci. Adv. 3, e1600983 (2017). 29134193 PMC5677351
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  4. [17]P. Liu, M. Moczydłowska, Ediacaran Microfossils from the Doushantuo Formation Chert Nodules in the Yangtze Gorges Area, South China, and New Biozones (John Wiley & Sons Ltd., 2019).
  5. [28]M. Zhou, T. Luo, W. D. Huff, Z. Yang, G. Zhou, T. Gan, H. Yang, D. Zhang, Timing the termination of the Doushantuo negative carbon isotope excursion: Evidence from U-Pb ages from the Dengying and Liuchapo formations, South China. Sci. Bull. 63, 1431– 1438 (2018). 36658983
  6. [34]E. Hodgin, thesis, Harvard University (2020).
  7. [36]Z. Li, M. Cao, S. J. Loyd, T. J. Algeo, H. Zhao, X. Wang, L. Zhao, Z.-Q. Q. Chen, Transient and stepwise ocean oxygenation during the late Ediacaran Shuram Excursion: Insights from carbonate δ238U of northwestern Mexico. Precambrian Res. 344, 105741 (2020).
  8. [42]E. C. Geyman, A. C. Maloof, A diurnal carbon engine explains 13C-enriched carbonates without increasing the global production of oxygen. Proc. Natl. Acad. Sci. U.S.A. 116, 24433– 24439 (2019). 31704769 PMC6900632
  9. [46]S. A. F. Darroch, E. F. Smith, M. Laflamme, D. H. Erwin, Ediacaran extinction and cambrian explosion. Trends Ecol. Evol. 33, 653– 663 (2018). 30007844
  10. [49]J. Hiess, D. J. Condon, N. McLean, S. R. Noble, 238U/235U systematics in terrestrial uranium-bearing minerals. Science 335, 1610– 1614 (2012). 22461608
  11. [60]K. A. McFadden, J. Huang, X. Chu, G. Jiang, A. J. Kaufman, C. Zhou, X. Yuan, S. Xiao, Pulsed oxidation and biological evolution in the Ediacaran Doushantuo Formation. Proc. Natl. Acad. Sci. U.S.A. 105, 3197– 3202 (2008). 18299566 PMC2265117
  12. [62]Y. Sui, C. Huang, R. Zhang, Z. Wang, J. Ogg, D. B. Kemp, Astronomical time scale for the lower Doushantuo Formation of early Ediacaran, South China. Sci. Bull. 63, 1485– 1494 (2018). 36658830
  13. [65]W. Wang, C. Guan, C. Zhou, Y. Peng, L. M. Pratt, X. Chen, L. Chen, Z. Chen, X. Yuan, S. Xiao, Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy of the Ediacaran Lantian Formation in South China: Spatial gradient, ocean redox oscillation, and fossil distribution. Geobiology 15, 552– 571 (2017). 28063179
  14. [86]Y. Soldatenko, A. El Albani, M. Ruzina, C. Fontaine, V. Nesterovsky, J. L. Paquette, A. Meunier, M. Ovtcharova, Precise U-Pb age constrains on the Ediacaran biota in Podolia, East European Platform, Ukraine. Sci. Rep. 9, 1675 (2019). 30737449 PMC6368556
  15. [88]S. A. Bowring, J. P. Grotzinger, C. E. Isachsen, A. H. Knoll, S. M. Pelechaty, P. Kolosov, Calibrating rates of early Cambrian evolution. Science 261, 1293– 1298 (1993). 11539488
  16. [97]B. Z. Saylor, thesis, Massachusetts Institute of Technology (1996).
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Authors
Yang, C., Rooney, A. D., Condon, D. J., Li, X.-H., Grazhdankin, D. V., Bowyer, F. T., Hu, C., Macdonald, F. A., & Zhu, M.
Affiliations
  • British Geological Survey (GB)
  • Yale University (US)
  • Chinese Academy of Sciences (CN)
  • Novosibirsk State University (RU)
  • University of Leeds (GB)
  • University of California, Santa Barbara (US)
Corresponding author
  • Yang, Chuan
  • Rooney, Alan D.
  • Zhu, Maoyan
Venue
Science Advances
Published
2021-11-05
Volume
7
Issue
45
Pages
eabi9643-eabi9643
ISSN
2375-2548 (ISSN-L)
OpenAlex
W3208430661
Cited by
202
References
20
Citations by year
2026: 38 · 2025: 43 · 2024: 44 · 2023: 48 · 2022: 27 · 2021: 2
FWCI
22.72
Type
journal article
Language
en
Open access
Licence
cc-by-nc
Locations
  • Science Advances (publishedVersion, cc-by-nc)
  • PubMed Central (publishedVersion, cc-by-nc)
  • PubMed (publishedVersion)
  • White Rose Research Online (University of Leeds, The University of Sheffield, University of York) (acceptedVersion)
  • NERC Open Research Archive (Natural Environment Research Council) (acceptedVersion)
  • eScholarship (California Digital Library) (submittedVersion, cc-by-nc)
Funders
  • National Science Foundation (2021319)
  • National Natural Science Foundation of China (41921002, 41802029)
  • Chinese Academy of Sciences (26000000, XDB18030300, 2021319)
  • Russian Science Foundation (20‐67‐46028)
  • Natural Environment Research Council (bgs06001, NE/P013775/1)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
Keywords
origin of complex life, carbon isotope excursion, Shuram excursion, carbon cycle perturbation, biostratigraphic correlation, chronostratigraphy

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