Next Article in Journal
Estimations of Fracture Surface Area Using Tracer and Temperature Data in Geothermal Fields
Next Article in Special Issue
Geochemical Signatures of Paleoclimate Changes in the Sediment Cores from the Gloria and Snorri Drifts (Northwest Atlantic) over the Holocene-Mid Pleistocene
Previous Article in Journal
Early European Observations of Precipitation Partitioning by Vegetation: A Synthesis and Evaluation of 19th Century Findings
Previous Article in Special Issue
Copper and its Isotopes in Organic-Rich Sediments: From the Modern Peru Margin to Archean Shales
Open AccessArticle

The Sedimentary Origin of Black and White Banded Cherts of the Buck Reef, Barberton, South Africa

ISTerre, University Grenoble Alpes, 38400 Grenoble, France
Author to whom correspondence should be addressed.
Geosciences 2019, 9(10), 424;
Received: 28 July 2019 / Revised: 16 September 2019 / Accepted: 20 September 2019 / Published: 1 October 2019
The Buck Reef is a 250–400 m thick sequence of banded black and white (B&W) cherts deposited ca. 3416 Ma ago in a shallow basin. We provide field, petrological and geochemical constraints on the chert-forming process and the origin of the banding. White layers consist of nearly pure microquartz, while black layers are mixed with detrital carbonaceous matter, quartz grains and carbonaceous microlaminae, interpreted as remnants of microbial mats. The circulation of Si-rich fluid is recorded by abundant chert veins and pervasive silicification. However, the high purity of the white layers, their lack of internal structures and extremely low Al, Ti and high-field-strength elements preclude an origin by silicification of sedimentary or volcanic precursors. Moreover, their reworking at the surface into slab conglomerates, and sediment-like contacts with black layers rule out a diagenetic origin. We propose a new model whereby the white layers were periodically deposited as precipitates of pure silica; and the micro-layering within the black layers formed by annual temperature fluctuations, favouring microbial activity in summer and inorganic silica precipitation in winter. Outcrop-scale alternation of B&W layers was associated with major, thousand-year-long climate events: white cherts represent massive silica precipitation resulting from changes in ocean circulation and temperature during cold intervals. View Full-Text
Keywords: chert; Archean; Buck Reef; sediment; geochemistry; climate chert; Archean; Buck Reef; sediment; geochemistry; climate
Show Figures

Figure 1

MDPI and ACS Style

Ledevin, M.; Arndt, N.; Chauvel, C.; Jaillard, E.; Simionovici, A. The Sedimentary Origin of Black and White Banded Cherts of the Buck Reef, Barberton, South Africa. Geosciences 2019, 9, 424.

Show more citation formats Show less citations formats
Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Article Access Map by Country/Region

Back to TopTop