Tufa stromatolite ecosystems on the South African south coast

Following the first description of living marine stromatolites along the South African east coast, new investigations along the south coast have revealed the occurrence of extensive fields of actively calcifying stromatolites. These stromatolites have been recorded at regular distances along a 200-k...

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Published inSouth African Journal of Science Vol. 110; no. 9-10; p. 1
Main Authors Perissinotto, Renzo, Bornman, Tommy G, Steyn, Paul-Pierre, Miranda, Nelson A F, Dorrington, Rosemary A, Matcher, Gwynneth F, Strydom, Nadine, Peer, Nasreen
Format Journal Article
LanguageEnglish
Published Pretoria African Online Scientific Information Systems (Pty) Ltd t/a AOSIS 01.09.2014
Academy of Science of South Africa
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Summary:Following the first description of living marine stromatolites along the South African east coast, new investigations along the south coast have revealed the occurrence of extensive fields of actively calcifying stromatolites. These stromatolites have been recorded at regular distances along a 200-km stretch of coastline, from Cape Recife in the east to the Storms River mouth in the west, with the highest density found between Schoenmakerskop and the Maitland River mouth. All active stromatolites are associated with freshwater seepage streams flowing from the dune cordon, which form rimstone dams and other accretions capable of retaining water in the supratidal platform. Resulting pools can reach a maximum depth of about 1 m and constitute a unique ecosystem in which freshwater and marine organisms alternate their dominance in response to vertical mixing and the balance between freshwater versus marine inflow. Although, the factors controlling stromatolite growth are yet to be determined, nitrogen appears to be supplied mainly via the dune seeps.
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ISSN:0038-2353
1996-7489
DOI:10.1590/sajs.2014/20140011