Cited by 187Paleontology and Stratigraphy of FossilsPaleontology and Evolutionary BiologyEvolution and Paleontology Studies

The DOI matches its Crossref record; 43 of the 44 references it cites were found in a registry or an index; none of the 29 sources its claims cite is checked for support yet.

Precambrian animal diversity: Putative phosphatized embryos from the Doushantuo Formation of China

Open access
Chen, Jun-Yuan, Oliveri, Paola, Li, Chia-Wei, Zhou, Gui-Qing, Gao, Feng, Hagadorn, James W., Peterson, Kevin J., Davidson, Eric H.·2000·Proceedings of the National Academy of Sciences

Abstract

Putative fossil embryos and larvae from the Precambrian phosphorite rocks of the Doushantuo Formation in Southwest China have been examined in thin section by bright field and polarized light microscopy. Although we cannot completely exclude a nonbiological or nonmetazoan origin, we identified what appear to be modern cnidarian developmental stages, including both anthozoan planula larvae and hydrozoan embryos. Most importantly, the sections contain a variety of small (≤200 μm) structures that greatly resemble gastrula stage embryos of modern bilaterian forms.

Overview

AI snapshot

Written from the paper’s full text.

TL;DR

Thin-section microscopy of phosphorites from the Doushantuo Formation revealed putative fossil embryos and larvae resembling modern cnidarian and bilaterian gastrulae, including small ≤200 μm forms. The authors argue these may extend cnidarian and bilaterian evolutionary history deeper into the Precambrian, while acknowledging that a nonbiological or nonmetazoan origin cannot be completely excluded.

Key findings

  • The sections contain what appear to be modern cnidarian developmental stages, including anthozoan planula larvae and hydrozoan embryos, plus small (≤200 μm) structures resembling gastrula-stage embryos of modern bilaterian forms.
  • Bilaterian-like gastrulae are typically 150–200 μm in diameter; in three deuterostome embryo-like specimens, the archenteron diameter was 27 ± 3% of the average external diameter, and cnidarian-like embryo wall thicknesses were consistently similar.
  • About 2,000 thin sections were examined and over 4,000 digital images of embryos and larvae were recorded; each reported morphotype was encountered multiple times.
  • The Doushantuo Formation could be as old as 580 Ma, pending direct measurement within 570 ± 20 Ma, and is likely to precede the lowest strata with which bilaterian remains have so far been associated.

Methods

  • Samples were collected from the Wusi and Baidoushan quarries of the Weng’an phosphate mine; thin sections were 30–50 μm thick and examined by transmitted light microscopy at ×100 or ×200 magnification, with selected samples viewed in cross-polarized light with a gypsum plate.
  • About 2,000 sections were examined, over 4,000 digital images of embryos and larvae were recorded, and morphometric measurements were taken from photographic representations and converted to μm by reference to size standards.

Limitations

  • Stated: the authors cannot completely exclude a nonbiological or nonmetazoan origin, and it remains formally possible that only some aspects of the fossils are biogenic—perhaps not even metazoan—while other features are nonbiogenic.
  • Stated: this is an initial analysis; the actual diversity of bilaterian forms can be established only by examination of later developmental stages, if they can be recovered, and taxonomic assignments are tentative; more extensive morphometric measurements are forthcoming.
  • Evident: the study is from one particular location/deposit and relies on morphological resemblance to modern embryos, with no direct molecular or adult-form evidence reported.

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Integrity signals

Registry

Crossref · 10.1073/pnas.97.9.4457

Cites

43 of 43 references verified0 citation errors · 0 not checkable

Statistics

Nothing to recompute.

Verification

Claims the paper makes

22 Own result · 11 Own interpretation · 10 Not checked yet · 2 No basis given · 1 Own method

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Show all 33 claims

  • It may state two separate claims as one. 9
  • Probably not a substantial claim. 3
  • The quote only partly states this claim. 1
13 of 13
  • The authors state this as an assumption.

    The fossil embryos in Fig. 3 are real (authentic fossils).

    “In any case, assuming that they are indeed real, the bilaterian nature of the fossil embryos in Fig. 3 is hard to doubt.”
  • The paper relies on this without support.

    Constant morphology and constant dimension are outputs of genetically controlled developmental systems and are a powerful index of biological origin.

    “Constant morphology and constant dimension are the outputs of genetically controlled developmental systems and are thus a powerful index of biological origin.”
  • The paper relies on this without support.

    Morphological resemblance between fossil structures and modern developmental stages is a reliable indicator of biological affinity.

    “The comparisons with modern forms in Fig. 3 are intended only to show that the morphological characters of the fossil gastrulae are paralleled in detail by those of modern bilaterian gastrulae.”
3 of 3

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Citations

Cites

Research works printed but not linked: 10

  1. J-Y Chen, G-Q Zhou The Cambrian Explosion and the Fossil Record (Bulletin of the National Museum of Natural Science), eds J-Y Chen, Y N Cheng, H V Iten (National Museum of Natural History, Taichung) 10, 11–105 (1997).
  2. S Bengtson, S Conway Morris, B J Cooper, P A Jell, B N Runnegar Mem Ass Australas Palaeontols 9, 1–364 (1990).
  3. M A Fedonkin Early Life on Earth: Nobel Symposium No. 84, ed S Bengtson (Columbia Univ. Press, New York), pp. 370–388 (1994).
  4. J G Gehling, G M Narbonne, S Jensen, M L Droser Geol Soc Am Abstr Prog 31, 362 (1999).
  5. Y Qian, M Chen, Y Chen Acta Paleont Sinica 18, 207–232 (1979).
  6. Y Xing, Q Ding, H Luo, T He, Y Wang Chin Acad Geol Sci 7, 1–262 (1984).
  7. Y Zhang, L Yin, S Xiao, A H Knoll Paleont Soc Mem 50, 1–52 (1998).
  8. G Shields Eclogae Geol Helv 92, 221–233 (1999).
  9. Z Zhao, Y Xing, G Ma, Y Chen Biostratigraphy of the Yangtze Gorge Area, (1) Sinian (Geological Publishing House, Beijing, 1985).
  10. J-P Chevalier Traité de Zoologie, ed P-P Grassé (Masson, Paris), pp. 403–764 (1987).

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Metadata

Authors
Chen, J.-Y., Oliveri, P., Li, C.-W., Zhou, G.-Q., Gao, F., Hagadorn, J. W., Peterson, K. J., & Davidson, E. H.
Affiliations
  • Nanjing Institute of Geology and Paleontology, Nanjing 210008, China; Divisions of Biology and Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125; and Department of Life Sciences, National Tsing Hua University, Hsinchu 300, Taiwan, China
  • California Institute of Technology (US)
Venue
Proceedings of the National Academy of Sciences
Published
2000-04-25
Volume
97
Issue
9
Pages
4457-4462
ISSN
  • 0027-8424 (ISSN-L)
  • 1091-6490
OpenAlex
W2165010994
Cited by
187
References
44
Citations by year
2026: 1 · 2025: 1 · 2024: 3 · 2023: 2 · 2022: 7 · 2021: 1 · 2020: 2 · 2019: 7 · 2018: 3 · 2017: 4 · 2016: 7 · 2015: 7 · 2014: 6 · 2013: 8 · 2012: 5
FWCI
9.01
Type
journal article
Language
en
Open access
Locations
  • Proceedings of the National Academy of Sciences (publishedVersion)
  • Europe PMC (PubMed Central) (publishedVersion)
  • PubMed Central (publishedVersion)
  • PubMed (publishedVersion)
  • CaltechAUTHORS (California Institute of Technology) (submittedVersion)
  • UCL Discovery (University College London) (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
Keywords
Doushantuo Formation, phosphate rock, fossil embryos, early animal evolution, Precambrian fossils
MeSH terms
Animals, China, Cnidaria, Embryo, Nonmammalian, Biological Evolution, Fossils, Gastrula, Paleontology, Genetic Variation, Body Patterning

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