The extant shore platform stromatolite (SPS) facies association: a glimpse into the Archean?

• Published in: Biogeosciences Vol. 15; no. 7; pp. 2189 - 2203
• Main Authors: Smith, Alan, Cooper, Andrew, Misra, Saumitra, Bharuth, Vishal, Guastella, Lisa, Botes, Riaan
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 13.04.2018; Copernicus Publications
• Subjects: Archean Eon; Bogs; Boulders; Causeway; Causeways; Cliffs; Coastal storms; Coasts; Dunes; Flooding; Fossils; Geology; Geomorphology; Headlands; Lithology; Mars; Mars (Planet); Peat; Peat bogs; Precambrian; Precipitation; Prokaryotes; Rainfall; Ridges; Slope; Storms; Stromatolites; Surf zone; Terraces; Tidal energy; Tidal power; Tidal regimes; Topography; Topography (geology); Wave energy; Wave power; Mozambique; United Kingdom > UK; Ireland; Africa; South Africa; Kuwait; Australia; Northern Ireland; Western Australia Australia
• ISSN: 1726-4189; 1726-4170; 1726-4189
• DOI: 10.5194/bg-15-2189-2018

Shore platform stromatolites (SPS) were first noted at Cape Morgan on the south-east African seaboard. Since then they have been found growing discontinuously in rocky peritidal zones along the entire southern African seaboard. They have also been found on the southwest Australian coast, at Giant's Causeway in Northern Ireland, and more recently at Harris on the Scottish Hebridean Atlantic coast. In this paper SPS occurrence and SPS potential as analogues for Precambrian fossil stromatolites, as well as potential stromatolite occurrences in shore platform regions on Mars, are assessed. Sub-horizontal surfaces promote stromatolite development, while tufa develops on cliffs and steep rocky surfaces. Tufa and stromatolites are end members of a spectrum dictated by coastal topography. Extant SPS occur on well indurated shore platforms in high wave energy settings, often around or near headlands. They can be associated with boulder beaches, boulder ridges, storm swash terraces, coastal dunes, and peat bogs. In contrast to other extant stromatolites, SPS are produced primarily by mineral precipitation, although minor trapping and binding stromatolites do occur. From a geological perspective, SPS develop in mildly transgressive siliciclastic settings in various climatic and tidal regimes. We suggest that SPS could be preserved in the geological record as micritic lenses on palaeo-shore platform surfaces. SPS share many features with Precambrian stromatolites and are a valid modern analogue despite the widely different atmospheric and oceanic conditions of the Archean. We suggest that terraces associated with former oceanic or lacustrine flooding surfaces on Mars are potential targets in the search for palaeo-SPS on Mars.