Cited by 189Paleontology and Stratigraphy of FossilsGeological and Geochemical AnalysisGeochemistry and Elemental Analysis

Earth'S Oldest Reported Glaciation: Physical and Chemical Evidence From the Archean Mozaan Group (∼2.9 Ga) of South Africa

Young, Grant M., Brunn, Victor von, Gold, Digby J. C., Minter, W. E. L.·1998·The Journal of Geology

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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Crossref · 10.1086/516039

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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)
Venue
The Journal of Geology
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

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