Rawnsley Quartzite
Geologic formation in South Australia
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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.
| Rawnsley Quartzite | |
|---|---|
| Stratigraphic range: Late Ediacaran [1] | |
Exposed rocks of the Rawnsley Quartzite | |
| Type | Formation |
| Unit of | Pound Subgroup |
| Sub-units | See: Members |
| Underlies | Uratanna Formation |
| Overlies | Bonney Sandstone |
| Area | 20,000 km2 (7,700 sq mi)[2] |
| Location | |
| Region | South Australia |
| Country | Australia |
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
|
Notes Uncertain or tentative taxa are in small text; |
Bilaterian
| Genus | Species | Locality | Notes | Images |
|---|---|---|---|---|
| Ikaria[9] |
|
1T-F Surface | Worm-like organism. | |
| Kimberella[11][4][9] |
|
NECP Bed-1 | Mollusc-like organism. | |
| Uncus[9] |
|
1T-F Surface | Worm-like organism. | |
|
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. | ||
Cnidarian
Porifera
| Genus | Species | Locality | Notes | Images |
|---|---|---|---|---|
| Palaeophragmodictya[10] |
|
TC-MM3 Surface | ||
| Funisia[9] |
|
1T-F, TC-MM3, and TR-ARB Surfaces | Olgunid tubular organism. | |
Petalonamae
| Genus | Species | Locality | Notes | Images |
|---|---|---|---|---|
| Arborea[11][9] |
|
NECP Bed-1 Surface | Frondose organism. | |
| Akrophyllas[14] |
|
Frondose organism. | ||
| Charniodiscus[11] |
|
NECP Bed-1 Surface | Frondose organism. | |
| Pteridinium[4] |
|
Recumbent frondose organism | ||
Proarticulata
| Genus | Species | Locality | Notes | Images |
|---|---|---|---|---|
| Andiva[10][9] |
|
1T-F and TR-ARB Surfaces | Elongated motile organism, with glided reflection. | |
| Archaeaspinus[15] |
|
Rounded motile organism, with glided reflection. | ||
| Dickinsonia[11][4][10][9] |
|
NECP Bed-1, 1T-F, TC-MM3, and TR-ARB Surfaces | Oval motile organism, with glided reflection. | |
| Marywadea[16] |
|
Elongated motile organism, with glided reflection. | ||
| Ovatoscutum[13] |
|
Rounded motile organism, with glided reflection. Previously described as a porpitid. | ||
| Praecambridium[17][11] |
|
NECP Bed-1 Surface | Rounded motile organism. | |
| Spriggina[11][4][10][9] |
|
NECP Bed-1 and 1T-F Surfaces | Elongated motile organism, with glided reflection. | |
| Yorgia[11][10] |
|
NECP Bed-1 and TC-MM3 Surfaces | Rounded motile organism, with glided reflection. |
Trilobozoa
| Genus | Species | Locality | Notes | Images |
|---|---|---|---|---|
| Albumares (?)[18] |
|
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] |
|
NECP Bed-1, 1T-F, and TC-MM3 Surfaces | Triradial organism. | |
| Tribrachidium[11][4][9] |
|
NECP Bed-1 and 1T-F Surfaces | Triradial organism. | |
incertae sedis
| Genus | Species | Locality | Notes | Images |
|---|---|---|---|---|
| Aspidella[10][9] |
|
1T-F and TC-MM3 Surface | Disoidal organism. | |
| Attenborites[19][10][9] |
|
1T-F and TR-ARB Surfaces | Pelagic oval organism. | |
| Aulozoon[10][20][9] |
|
1T-F, TC-MM3, and TR-ARB Surfaces | Sessile, tubular organism. | |
| Conomedusites[10] |
|
TC-MM3 Surface | Tetraradial organism, probable cnidarian. | ![]() |
| Coronacollina[10][9] |
|
1T-F and TR-ARB Surfaces | Triradial sponge-like organism, with four spicule-like structures. | |
| Cyclomedusa[21] |
|
Discoidal organism. | ||
| Eoandromeda[4] |
|
Eight-armed radial organism. | ||
| Eoporpita[9] |
|
1T-F Surface | Discoidal organism, probable cnidarian. | |
| Harlaniella (?)[22] |
|
Ribbon-like organism. | ||
| Mawsonites[10][9] |
|
1T-F Surface | Discoidal organism. | |
| Nilpenia[23] |
|
Branching, tubular and sediment-dwelling organism. | ||
| Obamus[24][10][9] |
|
1T-F and TB-ARB Surfaces | Torus-shaped organism. | |
| Parvancorina[11][4][10][9] |
|
NECP Bed-1, 1T-F, TC-MM3, and TB-ARB Surfaces | Anchor-shaped organism. | |
| Phyllozoon[4] |
|
Interpreted as either an erniettomorph or a feeding trace. | ||
| Plexus[25][10] |
|
TB-ARB Surface | Worm-like organism, affinities unknown. | |
| Pseudorhizostomites[11][10] |
|
NECP Bed-1 Surface | ||
| Quaestio[9] |
|
1T-F Surface | Asymmetrical, rounded organism. | |
| Somatohelix[10] |
|
Tubular organism. | ||
| Palaeopascichnus[10][9] |
|
1T-F and TB-ARB Surfaces | Palaeopascichnid organism | |
| Intrites[10] |
|
TC-MM3 and TR-ARB Surfaces | Palaeopascichnid organism. | |




































