Cited by 82Paleontology and Stratigraphy of FossilsProtist diversity and phylogenyPaleontology and Evolutionary Biology

Possible early foraminiferans in post-Sturtian (716−635 Ma) cap carbonates

Open access
Bosak, Tanja, Lahr, Daniel J.G., Pruss, Sara B., Macdonald, Francis A., Gooday, Andrew J., Dalton, Lilly, Matys, Emily D.·2012·Geology

Abstract

Foraminifera are an ecologically important group of modern heterotrophic amoeboid eukaryotes whose naked and testate ancestors are thought to have evolved ?1 Ga ago. However, the single-chambered agglutinated tests of these protists appear in the fossil record only after ca. 580 Ma, coinciding with the appearance of macroscopic and mineralized animals. Here we report the discovery of small, slender tubular microfossils in the Sturtian (ca. 716–635 Ma) cap carbonate of the Rasthof Formation in Namibia. The tubes are 200–1300 ?m long and 20–70 ?m wide, and preserve apertures and variably wide lumens, folds, constrictions, and ridges. Their sometimes flexible walls are composed of carbonaceous material and detrital minerals. This combination of morphologic and compositional characters is also present in some species of modern single-chambered agglutinated tubular foraminiferans, and is not found in other agglutinated eukaryotes. The preservation of possible early Foraminifera in the carbonate rocks deposited in the immediate aftermath of Sturtian low-latitude glaciation indicates that various morphologically modern protists thrived in microbially dominated ecosystems, and contributed to the cycling of carbon in Neoproterozoic oceans much before the rise of complex animals.

Integrity signals

Registry

Crossref · 10.1130/g32535.1

Cites

29 of 29 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • The geological record of multicellularity in the form of sponge biomarkers extends as far back as the Marinoan glaciation around 635 million years ago, with records of small tubular microfossils extending back to 716 Ma and controversial reports extending as far back as 1.8 Ga.

    “Regardless of how multicellularity arose, the geological record of multicellularity (in the form of sponge biomarkers) extends as far back as the Marinoan glaciation around 635 million years ago (Ma) (Love et al., 2009), with records of small tubular microfossils extending back to 716 Ma (Bosak et al., 2012) and controversial reports extending as far back as 1.8 Ga (Nichols and Wörheide, 2005).”

    From The Astrobiology Primer v2.0 (2016) · cites this paper as Bosak et al., 2012

Cites

Flagged first, then by citations

Cited by

Sorted by citations

Authors
Bosak, T., Lahr, D. J. G., Pruss, S. B., Macdonald, F. A., Gooday, A. J., Dalton, L., & Matys, E. D.
Affiliations
  • Massachusetts Institute of Technology (US)
  • Universidade de São Paulo (BR)
  • Smith College (US)
  • Harvard University (US)
  • National Oceanography Centre (GB)
Venue
Geology
Published
2012-01
Volume
40
Issue
1
Pages
67-70
ISSN
  • 0091-7613 (ISSN-L)
  • 1943-2682
OpenAlex
W2144409058
Cited by
82
References
29
Citations by year
2026: 2 · 2025: 5 · 2024: 6 · 2023: 5 · 2022: 2 · 2021: 4 · 2020: 6 · 2019: 5 · 2018: 8 · 2017: 7 · 2016: 11 · 2015: 5 · 2014: 3 · 2013: 8 · 2012: 5
FWCI
3.56
Type
journal article
Language
en
Open access
Licence
cc-by
Locations
  • Geology (publishedVersion)
  • Scientific Electronic Library Online (São Paulo Research Foundation, Latin American and Caribbean Center on Health Sciences Information, Conselho Nacional de Desenvolvimento Científico e Tecnológico) (publishedVersion)
  • Digital Access to Scholarship at Harvard (DASH) (Harvard University) (submittedVersion, cc-by)
  • Smith ScholarWorks (Smith College) (submittedVersion)
  • ePrints Soton (University of Southampton) (submittedVersion)
  • NERC Open Research Archive (Natural Environment Research Council) (submittedVersion)
  • Zenodo (CERN European Organization for Nuclear Research) (submittedVersion, other-oa)
Funders
Natural Environment Research Council (noc010004, noc010009)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Protist diversity and phylogeny
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
Keywords
Sturtian glaciation, agglutination test, Neoproterozoic, microbial ecosystems, carbon cycle, Ediacaran, protist evolution, Namibia

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review