Earth'S Oldest Reported Glaciation: Physical and Chemical Evidence From the Archean Mozaan Group (∼2.9 Ga) of South Africa
Abstract
The Pongola Supergroup is a thick succession of Archean (∼2.9 Ga) supracrustal rocks in the eastern part of the Kaapvaal craton of southern Africa. Its upper part, the Mozaan Group (∼5000 m‐thick) includes diamictites with a highly varied suite of clasts, some of which are striated and faceted. Clasts in associated stratified siltstones are interpreted as ice‐rafted debris. A glacial origin is also supported by geochemical investigation of diamictite matrix materials and associated mudstones. Plots of SiO2:Al2O3 and TiO2:Al2O3 suggest that these rocks underwent little chemical weathering, an interpretation confirmed by calculation of a Chemical Index of Alteration with low values, typical of other glacial deposits. The analyzed rocks are rich in Fe (average Fe2O3(T) is ∼24% wt %), like rocks of many other glaciomarine successions. The diamictites and associated mudstones of the Mozaan Group have low Th/Sc ratios, suggesting preferential incorporation of mafic materials into the diamictite matrix material. Previous studies suggest that this part of the Kaapvaal craton underwent early cratonization, involving tectonic and plutonic events that may have contributed to the drawdown of atmospheric CO2 and eventually provided a suitable substrate for development of continental glaciers.
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Glacial rocks are reported from 3.5, 2.9, and 2.7 Ga ago.
“Glacial rocks are reported from 3.5, 2.9, and 2.7 Ga ago.”
From The Archean atmosphere (2020) · cites this paper as [54]
In the ~2.9-Ga-old Pongola in South Africa, which was 43° to 48° paleolatitude, diamictites contain striated clasts, while associated silty laminates have dropstones with splash-up of substrata.
“Later, in the ~2.9-Ga-old Pongola in South Africa, which was 43° to 48° paleolatitude (224), diamictites contain striated clasts, while associated silty laminates have dropstones with splash-up of substrata (54).”
From The Archean atmosphere (2020) · cites this paper as [54]
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- Authors
- Young, G. M., Brunn, V. V., Gold, D. J. C., & Minter, W. E. L.
- Affiliations
- University of KwaZulu-Natal (ZA)
- Western University (CA)
- ORCID
- Young, Grant M.
- Venue
- The Journal of Geology
- Publisher
- University of Chicago Press
- Published
- 1998-09
- Volume
- 106
- Issue
- 5
- Pages
- 523-538
- ISSN
- 0022-1376 (ISSN-L)
- 1537-5269
- OpenAlex
- W1992746976
- Cited by
- 189
- References
- 0
- Citations by year
- 2026: 3 · 2025: 9 · 2024: 7 · 2023: 10 · 2022: 5 · 2021: 10 · 2020: 9 · 2019: 9 · 2018: 11 · 2017: 11 · 2016: 6 · 2015: 13 · 2014: 6 · 2013: 15 · 2012: 13
- FWCI
- 0.00
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- The Journal of Geology (publishedVersion)
- 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 › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- Pongola Supergroup, Kaapvaal Craton, diamictite, ice-rafted debris, glacial deposits, chemical index of alteration, chemical weathering, atmospheric CO2 drawdown, ice sheets
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 ›
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