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TAG 166 - Geological Society of Australia

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Ediacaran Golden Spike localityVisitors to South <strong>Australia</strong>’s Flinders Ranges wishing to view the EdiacaranGlobal Stratotype Section and Point (GSSP), also known as ‘Golden Spike’,may benefit from an explanation to assist them find its location.Approach the site by turning left at the well-signposted, gravelBrachina Gorge <strong>Geological</strong> Trail intersection with the bitumen Hawker toBlinman Road. Time spent at the excellent information station, close tothe beginning <strong>of</strong> the trail, provides the visitor with comprehensive knowledge<strong>of</strong> the geology <strong>of</strong> the trail that they are about to drive along.Back on the trail, regular signage directs the traveller to self-guidedlocalities to view exposures <strong>of</strong> geological interest and to campinglocalities. Take the signposted Trezona Campsite turn<strong>of</strong>f, approximately6 km from the eastern end <strong>of</strong> the trail. Within the campsite on EnoramaCreek (not at the trail turn<strong>of</strong>f) is an information panel shown in a photographaccompanying this article. This panel gives both the background tothe Ediacaran time-slice and broad directions as to where the Ediacarangolden spike may be found by walking along the creek.Follow the yellow marker posts for about 500 m in an easterlydirection along the southern bank <strong>of</strong> Enorama Creek. The final marker,several metres from the golden spike, states:Golden Spike — Global Stratotype Section and Point. Geo site marks thestart <strong>of</strong> the Ediacaran Period <strong>of</strong> geological time, as Earth warmed followingglaciation. Multi-celled organisms became widespread in maritimeenvironments. The brass disc indicates its location, where pink ElatinaFormation glacial tillite is overlain by buff Nuccaleena Formation dolomite.The Ediacaran Period information panel in Trezona Campsite, Enorama Creek,Flinders Ranges. Image courtesy Roger Pierson.Ediacaran GSSP in the Nuccaleena Formation dolomite exposure on thesouthern bank <strong>of</strong> Enorama Creek at Lat 31.331°S, Long 138.633°E. Scale incentimetres.The tillite, with prominent erratic pebbles, is shown below. A photograph<strong>of</strong> the golden spike Lat 31.331°S, Long 138.633°E is shown above.On 19 March 2004 the IUGS approved the reference point indicatingthe beginning <strong>of</strong> the Ediacaran Period (about 620 Ma) in the FlindersRanges. The Ediacaran Period golden spike marks the first new geologicalperiod to be defined in 120 years and it is the only time-slice demarcatedby rocks in the Southern Hemisphere. On 16 April 2005, the then-premier<strong>of</strong> South <strong>Australia</strong>, Mike Rann, completed the formal defining <strong>of</strong> thisespecially significant <strong>Australia</strong>n geological site by driving in the brass‘Golden Spike’. No fossils are present in the dolomite near the golden spike.Ediacaran fossils are found further west along the geological trail inyounger sections <strong>of</strong> the Nuccaleena Formation.Useful resourcesUseful information resources for geological travellers in the FlindersRanges include:Commonwealth <strong>of</strong> <strong>Australia</strong> (1999) Parachilna South <strong>Australia</strong>, TopographicalMap 1:250 000 scale, SH54-13 Edition 2.Hema Maps <strong>Australia</strong>, Regional Map, Flinders Ranges Regional Map,4th Edition.Minerals and Energy, Primary Industries and Resources SA, Brachina Gorge<strong>Geological</strong> Trail.Primary Industries and Resources SA (1999) Parachilna South <strong>Australia</strong>,1:250 000 scale <strong>Geological</strong> Series, Sheet SH54-13 with explanatory notes.Primary Industries and Resources SA, Geology <strong>of</strong> the Flinders RangesNational Park.South <strong>Australia</strong>n Department <strong>of</strong> Lands (1994) Corridors Through Time —the Geology <strong>of</strong> the Flinders Ranges National Park.ROGER PIERSONSchool <strong>of</strong> Life and Environmental SciencesDeakin UniversityPink Elatina Formation, 620 Ma glacial tillite with erratics, which underliesEdiacaran Nuccaleena Formation dolomite. Images courtesy Roger Pierson.20 |<strong>TAG</strong> March 2013

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