Rock pool tufa stromatolites on a modern South African wave-cut platform: partial analogues for Archaean stromatolites?

Smith, Alan M., Andrews, Julian E., Uken, Ronald, Thackeray, Zane, Perissinotto, Renzo, Leuci, Rio and Marca, Alina (2011) Rock pool tufa stromatolites on a modern South African wave-cut platform: partial analogues for Archaean stromatolites? Terra Nova, 23 (6). pp. 375-381. ISSN 1365-3121

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Abstract

Calcifying tufa stromatolites are forming on a high energy coast of the South African Indian Ocean. The tufa stromatolites form in upper intertidal to supra tidal rock pools, encrust bedrock and are linked both laterally and vertically to physico-chemical properties of their pool water. Calcification only occurs in pools where dissolved carbonate-rich, spring-fed groundwater is routed, and d18O values are consistent with calcification in a mixture of freshwater and seawater. Increasing pH and less negative isotope values away from the spring are consistent with CO2 degassing and in-stream calcification, albeit with some in-mixing of seawater. The rocky shore setting of these active tufa stromatolites is new and invites serious comparison with some Archaean rocky substrate peritidal stromatolites (e.g. the c. 3.45 Ga Strelley Pool sequences, Pilbara Craton). This new association shows that initial encrustation of rocky intertidal substrates can begin with freshwater influence in the intertidal zone, a facies detail that should be sought in ancient peritidal stromatolites.

Item Type: Article
Uncontrolled Keywords: sdg 6 - clean water and sanitation ,/dk/atira/pure/sustainabledevelopmentgoals/clean_water_and_sanitation
Faculty \ School: Faculty of Science > School of Environmental Sciences
UEA Research Groups: Faculty of Science > Research Groups > Geosciences
Faculty of Science > Research Groups > Geosciences and Natural Hazards (former - to 2017)
Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences
Depositing User: Users 2731 not found.
Date Deposited: 12 Oct 2011 10:02
Last Modified: 23 Oct 2022 00:31
URI: https://ueaeprints.uea.ac.uk/id/eprint/34988
DOI: 10.1111/j.1365-3121.2011.01022.x

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