Rawnsley Quartzite

Geologic formation in South Australia From Wikipedia, the free encyclopedia

The Rawnsley Quartzite is an Ediacaran geologic formation in South Australia. It is most well known for its preservation of organisms of the Ediacaran Biota.

Unit ofPound Subgroup
Sub-unitsSee: Members
UnderliesUratanna Formation
Quick facts Type, Unit of ...
Rawnsley Quartzite
Stratigraphic range: Late Ediacaran 555 Ma [1]
Exposed rocks of the Rawnsley Quartzite
TypeFormation
Unit ofPound Subgroup
Sub-unitsSee: Members
UnderliesUratanna Formation
OverliesBonney Sandstone
Area20,000 km2 (7,700 sq mi)[2]
Location
RegionSouth Australia
CountryAustralia
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Geology

Contrary to what the name suggests, the Rawnsley Quartzite is dominated by sandstone rocks. The formation is found entirely within the Nilpena Ediacara National Park, in the Flinders Ranges of Southern Australia.[3]

Members

The Rawnsley Quartzite is composed of two formal members, and one currently informal member, which are as follows, in ascending stratigraphic order (lowest to highest):

  • Chace Quartzite Member: This member is primarily composed of white, fine to coarse-grained sandstone, which is petee-bedded and feldspathic.[3]
  • Ediacara Member: Getting up to 300 m (980 ft) thick, member is composed of various sandstones and quartzites. At the base of the member, there are predominately flat-laminated to rippled sandstone. This sandstone is khaki colored, weathers to a red color when exposed, and is fine to coarse-grained. Within these layers there can also be found white to brown feldspathic sandstone, which is medium to coarse-grained. In the middle of the member can be found gray-white, fine to coarse-grained sandstone, which is thin to medium-bedded and features wave ripples. Further towards the top of the member there are white, medium to coarse-grained arenite, which contains quartz and is feldspathic. It is also the fossil bearing member of the formation.[3]
  • Nilpena Sandstone/Upper Rawnsley Quartzite Member: This member is the informal one of the three, being at the very top of the formation, and contains very few fossils, mostly discoidal in appearance. It is primarily composed of fine-grained sandstones.[4] It is also sometimes simply referred to as the Upper Rawnsley Quartzite Member.[2]

Dating

The dating of the formation, and primarily the Ediacara Member, has been hindered due to the coarse-grained siliciclastic sedimentology of it. Despite this, there have been two grains dated through U-Pb dating that get close to a probable depositional age of the aforementioned member. The first grain yielded an age of 561.9±15.1 Ma, whilst the second one yields an age of 596±10 Ma. Meanwhile, another single grain from the underlying Bonney Sandstone yielded an age of 566±24 Ma.[1]

Due to these very few dates, a date of 555±0 Ma has been used as the Ediacara Member is known to correlate with the Zimnygory section in the Ustʹ Pinega Formation, Russia.[1]

Paleoenvironment

The environment at the time of the Ediacara Member's deposition was that of a shallow marine one, ranging from an estuarine, shoreface, and coastal environments.[2] Previous studies had a slightly wider range, with the environment going from the fair-weather wave base to a sub-storm wave base, as well as a delta-front, which ranged from a near to below the wave base.[3] The shallow marine environment was also inferred from the relatively thick matgrounds commonly found in most fossil beds of the member, which would have also helped to support the community of organisms within the general area.[3]

One researcher, Gregory Retallack, has regarded the member as being that of a terrestrial environment based on iron oxide coatings found within it,[5] although further studies done after have discounted these findings suggesting a terrestrial deposition for the member, as the compounds had been precipitated from groundwater beneath the member in the last ~2 million years.[6] Despite this piece of evidence, alongside a growing collection of other studies done before and after,[7] Retallack still supports a terrestrial environment for the Rawnsley Quartzite.[8]

Paleobiota

The beds at Nilpena Ediacara National Park contains a diverse, and complex system of Ediacaran organisms, from bilateral forms such as Parvancorina and Kimberella,[9] to the classic Ediacaran forms such as Dickinsonia and Arborea.[9] Due to its notable shallow environment, there is also a wide collection of algae forms, such as Flabellophyton and Longifuniculum, which are commonly referred to as "Bundles of Filaments" (BOF) in literature.[10][9]

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Bilaterian

More information Genus, Species ...
Genus Species Locality Notes Images
Ikaria[9]
  • I. wariootia
1T-F Surface Worm-like organism.
Kimberella[11][4][9]
  • K. quadrata
NECP Bed-1 Mollusc-like organism.
Uncus[9]
  • U. dzaugisi
1T-F Surface Worm-like organism.
Velocephalina[12]
  • V. greenwoodensis
NECP Bed-1 Surface Mollusc-like organism. Due to being named exclusively in a PhD thesis, it is considered a nomen ineditum, meaning it was not properly published.
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Cnidarian

More information Genus, Species ...
Genus Species Locality Notes Images
Ediacaria[13]
  • E. flindersi
Discoidal organism.
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Porifera

More information Genus, Species ...
Genus Species Locality Notes Images
Palaeophragmodictya[10]
  • P. reticulata
TC-MM3 Surface
Funisia[9]
  • F. dorothea
1T-F, TC-MM3, and TR-ARB Surfaces Olgunid tubular organism.
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Petalonamae

More information Genus, Species ...
Genus Species Locality Notes Images
Arborea[11][9]
  • A. arborea
NECP Bed-1 Surface Frondose organism.
Akrophyllas[14]
  • A. longa
Frondose organism.
Charniodiscus[11]
  • Charniodiscus sp.
NECP Bed-1 Surface Frondose organism.
Pteridinium[4]
  • Pteridinium sp.
  • P. simplex
Recumbent frondose organism
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Proarticulata

More information Genus, Species ...
Genus Species Locality Notes Images
Andiva[10][9]
  • A. ivantsovi
1T-F and TR-ARB Surfaces Elongated motile organism, with glided reflection.
Archaeaspinus[15]
  • A. fedonkini
Rounded motile organism, with glided reflection.
Dickinsonia[11][4][10][9]
  • D. costata
  • D. tenuis
NECP Bed-1, 1T-F, TC-MM3, and TR-ARB Surfaces Oval motile organism, with glided reflection.
Marywadea[16]
  • M. ovata
Elongated motile organism, with glided reflection.
Ovatoscutum[13]
  • O. concentricum
Rounded motile organism, with glided reflection. Previously described as a porpitid.
Praecambridium[17][11]
  • P. sigillum
NECP Bed-1 Surface Rounded motile organism.
Spriggina[11][4][10][9]
  • S. floundersi
NECP Bed-1 and 1T-F Surfaces Elongated motile organism, with glided reflection.
Yorgia[11][10]
  • Y. waggoneri
NECP Bed-1 and TC-MM3 Surfaces Rounded motile organism, with glided reflection.
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Trilobozoa

More information Genus, Species ...
Genus Species Locality Notes Images
Albumares (?)[18]
  • Albumares sp. (?)
Triradial organism. No proper description or image has been published of its record here, as such it remains uncertain if Albumares can also be found here.
Rugoconites[10][11][9]
  • R. enigmaticus
NECP Bed-1, 1T-F, and TC-MM3 Surfaces Triradial organism.
Tribrachidium[11][4][9]
  • T. heraldicum
  • T. gehlingi
NECP Bed-1 and 1T-F Surfaces Triradial organism.
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incertae sedis

More information Genus, Species ...
Genus Species Locality Notes Images
Aspidella[10][9]
  • A. terranovica
1T-F and TC-MM3 Surface Disoidal organism.
Attenborites[19][10][9]
  • A. janae
1T-F and TR-ARB Surfaces Pelagic oval organism.
Aulozoon[10][20][9]
  • A. soliorum
1T-F, TC-MM3, and TR-ARB Surfaces Sessile, tubular organism.
Conomedusites[10]
  • C. lobatus
TC-MM3 Surface Tetraradial organism, probable cnidarian.
Coronacollina[10][9]
  • C. acula
1T-F and TR-ARB Surfaces Triradial sponge-like organism, with four spicule-like structures.
Cyclomedusa[21]
  • Cyclomedusa sp.
Discoidal organism.
Eoandromeda[4]
  • E. octobrachiata
Eight-armed radial organism.
Eoporpita[9]
  • E. medusa
1T-F Surface Discoidal organism, probable cnidarian.
Harlaniella (?)[22]
  • Harlaniella (?) sp.
Ribbon-like organism.
Mawsonites[10][9]
  • M. spriggi
1T-F Surface Discoidal organism.
Nilpenia[23]
  • N. rossi
Branching, tubular and sediment-dwelling organism.
Obamus[24][10][9]
  • O. coronatus
1T-F and TB-ARB Surfaces Torus-shaped organism.
Parvancorina[11][4][10][9]
  • P. minchami
NECP Bed-1, 1T-F, TC-MM3, and TB-ARB Surfaces Anchor-shaped organism.
Phyllozoon[4]
  • P. hanseni
Interpreted as either an erniettomorph or a feeding trace.
Plexus[25][10]
  • P. ricei
TB-ARB Surface Worm-like organism, affinities unknown.
Pseudorhizostomites[11][10]
  • P. howchini
NECP Bed-1 Surface
Quaestio[9]
  • Q. simpsonorum
1T-F Surface Asymmetrical, rounded organism.
Somatohelix[10]
  • S. sinuosus
Tubular organism.
Palaeopascichnus[10][9]
  • Palaeopascichnus sp.
1T-F and TB-ARB Surfaces Palaeopascichnid organism
Intrites[10]
  • Intrites sp.
TC-MM3 and TR-ARB Surfaces Palaeopascichnid organism.
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Flora

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Genus Species Locality Notes Images
Flabellophyton[10]
  • F. stupendum
  • F. typicum
Filamentous macroalgae.
Liulingitaenia[10]
  • L. irregularis
Filamentous macroalgae.
Longifuniculum[10]
  • L. dissolutum
Whip-like macroalgae.
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Ichnogenera

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Genus Species Locality Notes Images
Helminthoidichnites[4][10]
  • Helminthoidichnites sp.
Burrows.
Epibaion[11]
  • E. costatus
NECP Bed-1 Surface Feeding traces of Dickinonsia.
Kimberichnus[26][11]
  • K. terruzi
NECP Bed-1 Surface Feeding traces of Kimberella.
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Undescribed

More information Genus, Species ...
Genus Species Locality Notes Images
Form 1[11]
  • ???
NECP Bed-1 Surface Bilterial organism, bears similarities with Kimberella, although features a prominent "head" region at the front, and a "flange" at the rear.
Form 2[11]
  • ???
NECP Bed-1 Surface Rounded organism, with a notable "head" shield.
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See also

References

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