Cited by 231Paleontology and Stratigraphy of FossilsPaleontology and Evolutionary BiologyEvolution and Paleontology Studies

Fossil preservation in the Neoproterozoic Doushantuo phosphorite Lagerstätte, South China

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Xiao, Shuhai, Knoll, Andrew H.·1999·Lethaia

Abstract

Phosphorites of the late Neoproterozoic Doushantuo Formation exposed in the vicinity of Weng'an, Guizhou Province, and Chadian, Shaanxi Province, South China, contain exceptionally well-preserved algal thalli, acritarchs, and globular microfossils interpreted as animal embryos. Combined optical microscopic and SEM observations provide insights into the taphonomy of phosphatized fossils. Algal cells and tissues are variably resistant to decay, and within preserved populations permineralization began at varying stages of degradation. In consequence, there is a spectrum of quality in cellular preservation. Algal cell walls, acritarch vesicles, and embryo envelopes are commonly encrusted by an isopachous rim of apatite, with cell interiors filled by collophane and later diagenetic dolomite. In contrast, blastomere surfaces of animal embryos are encrusted primarily by minute phosphatic spherules and filaments, possibly reflecting an immediately postmortem infestation of bacteria that provided nucleation sites for phosphate crystal growth. Thus, the same processes that gave rise to Phanerozoic phosphatized Lagerstatten--phosphatic encrustation, and impregnation, probably mediated by microbial activity--effected soft-tissue preservation in the Doushantuo Lagerstatte. It remains unclear how phosphatic ions and organic macromolecules interact at the molecular level and to what extent specific microbial metabolisms or microenvironmental conditions control the phosphatization of soft ti…

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Crossref · 10.1111/j.1502-3931.1999.tb00541.x

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  • Phosphatic preservation like that in the Doushantuo appears restricted to a relatively narrow Neoproterozoic interval, and similar preservation opportunities may not occur in older rocks.

    “Such unusual phosphatic preservation has been described from elsewhere in the Phanerozoic, but this complex preservational environment (Xiao and Knoll, 1999) appears restricted to a relatively narrow interval of the Neoproterozoic (Cook and Shergold, 1984).”

    From The last common bilaterian ancestor (2002) · cites this paper as Xiao and Knoll, 1999

  • Acritarchs are the most diverse and heterogeneous fossils from the 1200-740 Mya interval and increased greatly in diversity during the Neoproterozoic.

    “The most diverse and heterogeneous fossils from this interval are resistant, organic-walled microfossils known as acritarchs, which increased greatly in diversity during the Neoproterozoic (Knoll, 1996; Vidal and Moczydl ⁄ owska-Vidal, 1997; Xiao and Knoll, 1999; Zhou et al., 2001).”

    From The last common bilaterian ancestor (2002) · cites this paper as Xiao and Knoll, 1999

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Authors
Xiao, S., & Knoll, A. H.
Affiliations
Harvard University (US)
Venue
Lethaia
Published
1999-09
Volume
32
Issue
3
Pages
219-240
ISSN
  • 0024-1164 (ISSN-L)
  • 1502-3931
OpenAlex
W2114329528
Cited by
231
References
4
Citations by year
2026: 12 · 2025: 7 · 2024: 4 · 2023: 5 · 2022: 13 · 2021: 9 · 2020: 3 · 2019: 9 · 2018: 7 · 2017: 9 · 2016: 8 · 2015: 12 · 2014: 10 · 2013: 6 · 2012: 13
FWCI
4.00
Type
journal article
Language
en
Open access
Locations
  • Lethaia (publishedVersion)
  • PubMed (publishedVersion)
  • Digital Access to Scholarship at Harvard (DASH) (Harvard University) (submittedVersion, cc-by)
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, Neoproterozoic, phosphatization, taphonomy, soft tissue preservation, acritarchs, animal embryos, collophane, diagenesis, new taxa
MeSH terms
Animals, China, Embryo, Nonmammalian, Fossils, Invertebrates, Microscopy, Electron, Scanning, Minerals, Paleontology, Phosphates, Geologic Sediments, Eukaryota

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