Cited by 72Paleontology and Stratigraphy of FossilsPaleontology and Evolutionary BiologyEvolution and Paleontology Studies

The DOI matches its Crossref record; 54 of the 56 references it cites were found in a registry or an index; none of the 70 sources its claims cite is checked for support yet.

Tubular compression fossils from the Ediacaran Nama group, Namibia

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Abstract

Abundant tubular macrofossils occur in finely laminated siltstones and shales of the 548–542 Ma Schwarzrand Subgroup, Nama Group, Namibia. The Nama tubes occur in both the Vingerbreek and Feldschuhhorn members commonly in dense populations and always in fine-grained, lower shore-face lithologies deposited below fair-weather wave base. The tubes are preserved mostly as compressed casts and molds that range in width from 0.6 to 2.1 mm; apparently incomplete specimens reach lengths up to 10 cm. All specimens show sinuous bending and occasional brittle fracture, indicating an original construction of strong but flexible organic matter. Feldschuhhorn specimens preserve fine longitudinal pleats or folds that record pliant organic walls, but the older Vingerbreek populations do not. Similarly, some specimens in the Feldschuhhorn Member display branching, while Vingerbreek tubes do not. The abundant Feldschuhhorn tubes are assigned to the widespread Ediacaran problematicum Vendotaenia antiqua; however, the distinctive Vingerbreek population remains in open nomenclature. The most abundant fossils in Nama rocks, these tubes resemble populations in Ediacaran successions from Russia, China, Spain, and elsewhere. Beyond their local importance, then, such tubes may turn out to be the most abundant record of Ediacaran life.

Overview

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Written from the paper’s full text.

TL;DR

Abundant tubular compression fossils occur in the 548–542 Ma Schwarzrand Subgroup, Nama Group, Namibia, preserved as casts and molds in fine-grained lower shore-face deposits. The Feldschuhhorn population is assigned to *Vendotaenia antiqua*, while the older Vingerbreek population remains in open nomenclature; such tubes may be among the most abundant Ediacaran macrofossils.

Key findings

  • Tubes range from 0.6 to 2.1 mm in width; incomplete specimens reach lengths up to 10 cm, and both Vingerbreek and Feldschuhhorn populations show a bimodal width distribution. Sinuous bending and occasional brittle fracture indicate strong but flexible organic matter.
  • Feldschuhhorn specimens preserve fine longitudinal pleats or folds and rare branching (pseudomonopodial and dichotomous); Vingerbreek tubes lack folds and branching. The Feldschuhhorn tubes are assigned to *Vendotaenia antiqua*, while the Vingerbreek population is left in open nomenclature.
  • Feldschuhhorn internal molds consist primarily of iron-rich phyllosilicates, including chlorite; SEM shows a honeycombed wall pattern consistent with pyrite crystals later weathered out. Vingerbreek tubes and matrix differ in composition, and some Vingerbreek specimens are preserved as raised ridges, a style unique to that member.
  • The Nama tubes resemble Ediacaran populations from Russia, China, Spain, and elsewhere; the paper suggests they may be the most abundant record of Ediacaran life and a significant component of Ediacaran biomass.

Methods

  • Fossils were collected from the Vingerbreek Member at Kliphoek farm and the Feldschuhhorn Member at Sonntagsbrunn farm, southern Witputs sub-basin; fossils occur through approximately 50 m and 70 m of section, respectively, in fine-grained, parallel-laminated rocks.
  • Morphology was analyzed using light microscopy and SEM with EDAX; length and width of individual tubes were measured on approximately 75% of collected hand samples to generate size distributions. Specimens were deposited under accession numbers F608–F620.
  • Geochronologic context comes from U/Pb zircon dates: 548.8 ±1 Ma (Hoogland Member), 545.1 ±1 Ma, and 543 ±1 Ma (Spitskop Member), which bracket the fossils.

Limitations

  • The paper states that morphological simplicity and a general lack of distinguishing features make definitive taxonomic categorization difficult; the Vingerbreek population is left in open nomenclature. No definitively complete fossils were found, so original lengths were presumably longer, and terminal swellings were not confidently interpreted because they could be taphonomic artifacts.
  • The paper states that Vingerbreek material can be difficult to distinguish from simple trace fossils, and some raised-ridge specimens might be interpreted as trace fossils if found in isolation. It also notes that a *Thioploca*-like interpretation breaks down on size and lack of branching, and that absent reproductive structures make it challenging to differentiate cylindrical fossils of macroscopic green, red, or brown algae.
  • Evident from the text: the study is based on two localities/members in the southern Nama sub-basin, and most tube walls have low or no preserved organic content (hydrofluoric acid maceration of Vingerbreek samples failed to reveal preserved organic matter), limiting direct biological characterization.

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Integrity signals

Registry

Crossref · 10.1666/09-040r.1

Cites

54 of 54 references verified0 citation errors · 0 not checkable

Statistics

Nothing to recompute.

Verification

Claims the paper makes

46 Not checked yet · 44 Own interpretation · 37 No basis given · 33 Own result

Verify all 70 references — free account

Show all 86 claims

  • It may state two separate claims as one. 61
  • Probably not a substantial claim. 26
74 of 74
  • The authors state this as an assumption.

    Width is a proxy for age in Nama tube populations.

    “Assuming width is a proxy for age”
  • The paper relies on this without support.

    Thioploca is not known to display branching.

    “Moreover, Thioploca is not known to display branching.”
  • The paper relies on this without support.

    High-density populations of macroscopic tubes such as those preserved in Nama shales have not been reported from pre-Ediacaran successions and are not much in evidence after the Cambrian Period.

    “-While carbonaceous macrofossils are known throughout the Proterozoic record, high-density populations of macroscopic tubes such as those preserved in Nama shales have not been reported from pre-Ediacaran successions; nor are they much in evidence after the Cambrian Period.”
  • The paper relies on this without support.

    The global distribution of tubular compression fossils reflects original widespread expansion of macroscopic organisms in Ediacaran oceans rather than taphonomic or sampling bias.

    “Regardless of taxonomic affinity, the global distribution and sudden appearance of such tubes signal a widespread expansion of macroscopic organisms in basinal environments of Ediacaran oceans.”
  • The paper relies on this without support.

    Modern macroalgal primary production rates are applicable to Ediacaran tubular macroorganisms.

    “In modern marine systems, primary production rates in macroalgal communities range from 1.75 to 14.6 kg/m 2 /yr (Graham and Wilcox, 1999), rates equal to or greater than those in the most productive terrestrial plant communities.”
  • The paper relies on this without support.

    The morphological features used to distinguish body fossils from trace fossils (folds, elevated carbon) are reliable indicators of body fossil affinity.

    “Feldschuhhorn tubes show several morphological features that immediately distinguish them from trace fossils, including the presence of folds and elevated levels of carbon (Figures 3.5, 7.2).”
  • The paper relies on this without support.

    The absence of annulations in examined specimens indicates a true absence of annulations in the organisms, not a preservational artifact.

    “Additionally, the lack of annulations in dozens of specimens examined from each locality and the faint and superficial quality of those observed emphasizes the possibility that those seen in isolated specimens could be preservational artifacts.”
  • The paper relies on this without support.

    The Nama tube fossils are representative of Ediacaran tubular macrofossils globally.

    “The consistent presence of tubular compression fossils in tens of meters of section in the Nama Group and in numerous other globally distributed localities indicates that these organisms were a significant component of Ediacaran biomass and may prove to be the most abundant macrofossils in the Ediacaran system as a whole.”
  • The paper relies on this without support.

    The oxygen gradient and nitrogen cycle reconstructions from cited works apply to the Ediacaran Nama Group settings.

    “Thus, the global expansion of tube fossil populations in Ediacaran oceans is consistent with our understanding of Neoproterozoic environments and evolution.”
9 of 9

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Citations

Cites

Show all 56 references

Research works printed but not linked: 17

  1. Graham, 1999, Algae, 604
  2. Gnilovskaya, 1971, The oldest aquatic plants of the Vendian of the Russian Platform (late Precambrian), Paleontological Journal, 5, 372
  3. Hofmann, 1994, Early Life on Earth, 342
  4. Grotzinger, 2008, The Geology of Namibia, Volume 2, 13.229
  5. Bradley, 1998, A New Vendian Body Fossil from the Nama Group of Namibia: Evolutionary and Biostratigraphic Implications, 60
  6. 10.1017/s0022336000041743 · DOI
  7. Gnilovskaya, 1988, Vendotaenids of the East European Platform, 143
  8. Gnilovskaya, 1983, Upper Precambrian and Cambrian Paleontology of the East European Platform, 46
  9. Gnilovskaya, 1990, The Vendian System. Volume 1. Paleontology, 138
  10. Ivantsov, 1990, New data on the ultrastructure of sabellidites (Pogonophora?), Paleontologicheskii Zhurnal, 24, 125
  11. Jensen, 2005b, Megascopic filamentous organisms preserved as grooves and ridges in Ediacaran siliciclastics, Paleobios, 25, 65
  12. Sokolov, B. S. 1968. Vendian and Early Cambrian Sabelliditida (Pogonophora) of the USSR. Proceedings, 23rd International Geological Congress, Prague, pp. 79–96.
  13. Sokolov, B. S. 1972. Vendian and Early Cambrian Sabellidita (Pogonophora) of the USSR. Proceedings of the 23rd International Geological Congress, Proceedings of the International Palaeontological Union, 79–86.
  14. Sokolov, 1967, The oldest Pogonophora, Doklady Akademia Nauk SSSR, 177, 201
  15. Contreras Sánchez, 2007, Filamentous carbonaceous compressions from the terminal Ediacaran–Cambrian of central Spain, Palaeontological Association Newsletter, 66, 68
  16. 10.1666/0094-8373(2000)026 · DOI
  17. Herman, 2005, On the animal nature of the late Riphean Rugosoopsis., Paleontological Journal, 39, 582

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Metadata

Authors
Cohen, P. A., Bradley, A., Knoll, A. H., Grotzinger, J. P., Jensen, S., Abelson, J., Hand, K., Love, G., Metz, J., McLoughlin, N., Meister, P., Shepard, R., Tice, M., & Wilson, J. P.
Affiliations
  • Harvard University (US)
  • California Institute of Technology (US)
  • Universidad de Extremadura (ES)
  • University of California, Riverside (US)
  • University of Bergen (NO)
  • Max Planck Institute for Marine Microbiology (DE)
  • University of California, Davis (US)
  • Texas A&M University (US)
Venue
Journal of Paleontology
Published
2009-01
Volume
83
Issue
1
Pages
110-122
ISSN
  • 0022-3360 (ISSN-L)
  • 1937-2337
OpenAlex
W2105328483
Cited by
71
References
56
Citations by year
2026: 4 · 2025: 3 · 2024: 5 · 2023: 3 · 2022: 4 · 2021: 7 · 2020: 8 · 2019: 1 · 2018: 7 · 2017: 4 · 2016: 4 · 2015: 2 · 2014: 5 · 2012: 6
FWCI
2.02
Type
journal article
Language
en
Open access
Locations
  • Journal of Paleontology (publishedVersion)
  • Digital Access to Scholarship at Harvard (DASH) (Harvard University) (submittedVersion, cc-by)
  • CaltechAUTHORS (California Institute of Technology) (submittedVersion)
  • BioOne Complete (BioOne) (submittedVersion)
  • Max Planck Digital Library (submittedVersion)
  • MPG.PuRe (Max Planck Society) (submittedVersion)
Funders
  • National Science Foundation (ECS- 03-35765, 0335765)
  • Agouron Institute
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
Ediacaran, Nama Group, soft-bodied fossils, early animal evolution, Namibia

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