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Geological formation in South Australia

Emu Bay Shale

Emu Bay Shale

Key facts

instance ofgeological formation
countryAustralia
located in the administrative territorial entitySouth Australia
All data from the card 12
Type
Geological formation
Unit of
Kangaroo Island Group
Underlies
Boxing Bay Formation
Overlies
Marsden Sandstone (unconformity)
Thickness
78 m (256 ft), of which the lowest 10 m are fossiliferous
Primary
Shale
Other
Sandstone
Coordinates
35°35′S 137°30′E / 35.583°S 137.500°E
Approximate paleocoordinates
12°30′N 161°12′W / 12.5°N 161.2°W
Region
The north coast of Kangaroo Island, around Emu Bay and Cape D'Estaing, South Australia
Country
Australia
Named for
Emu Bay

The Emu Bay Shale is a geological formation in Emu Bay, South Australia, containing a major Konservat-Lagerstätte (fossil beds with soft tissue preservation). It is one of two in the world containing Redlichiidan trilobites. The Emu Bay Shale is dated as Cambrian Series 2, Stage 4, correlated with the upper Botomian Stage of the Lower Cambrian.

Its mode of preservation is the similar to the Burgess Shale, but the larger grain size of the Emu Bay rock means that the quality of preservation is lower. More than 50 species of trilobites, non-biomineralized arthropods (including megacheirans, nektaspids, and hymenocarines), radiodonts, palaeoscolecids, a lobopodian, a polychaete, vetulicolians, nectocaridids, hyoliths, brachiopods, sponges, chancelloriids, several problematica and a chelicerate are known from the Emu Bay Shale.

Description

The Emu Bay Shale of Kangaroo Island, South Australia, is Australia's only known Burgess-Shale-type Konservat-Lagerstätte, and includes faunal elements such as Anomalocaris, Tuzoia, Isoxys, and Wronascolex, in common with other Burgess-Shale-type assemblages, notably the Chengjiang Biota in China, the closest palaeogeographically, although somewhat older. A few genera of non-biomineralized arthropods, among them Squamacula, Kangacaris, and the megacheiran Tanglangia, are known only from the Emu Bay Shale and Chengjiang. The site is also the source of high-quality specimens of trilobites such as Redlichia takooensis, Emuella polymera, Balcoracania dailyi, Megapharanaspis nedini, Holyoakia simpsoni, and Estaingia (=Hsuaspis) bilobata. Balcoracania and Emuella are the only known genera of the distinctive Redlichiina family Emuellidae, known for possessing the greatest number of thoracic segments known for Trilobita as a whole (a record of 103 in one Balcoracania specimen), and so far entirely restricted to Australia and Antarctica.

The sedimentary depositional environment of the majority of Burgess-Shale-type assemblages is outer shelf, deeper water. The Emu Bay Shale in contrast, appears to represent deposition in restricted basins on the inner shelf, indicating that soft tissue preservation occurred in a range of environmental settings during the Cambrian. Various organisms inhabited the varying depths of the area, for example, the Estaingia and the "petalloids" from the site typically inhabited the deeper areas of the depositional environment, while in contrast, the Balcoracania found at the site typically lived within intertidal areas, such as tide pools. Some Emu Bay fossils display extensive mineralization of soft tissues, most often of blocky apatite or fibrous calcium carbonate, including the oldest phosphatized muscle tissue – along with records from Sirius Passet in Greenland, the first thus far reported from the Cambrian. Mid-gut glands are preserved three-dimensionally in calcium phosphate in the arthropods Isoxys and Oestokerkus, as in related species from the Burgess Shale.

The type section of the Emu Bay Shale crops out on the east side of Emu Bay where it conformably overlies the White Point Conglomerate. Here it yields a rich assemblage of Estaingia, Redlichia, hyolithids, brachiopods, and the scleritome-bearing Chancelloria. At the Big Gully locality (8 km east of White Point), its presumed correlative is unconformable on the White Point Conglomerate and yields soft-bodied fossils in addition to the trilobites, including Anomalocaris, Echidnacaris, Isoxys, Tuzoia, two species of the nektaspid arthropod family Emucarididae (Emucaris fava and Kangacaris zhangi), the palaeoscolecid worm Wronascolex, the problematic Myoscolex, "petalloids" and Vetustovermis, and a number of rarer elements. The Big Gully trilobites rarely preserve any trace of non-biomineralized tissue; a small number of specimens of Redlichia have been reported with antennae. Taxa documented from a quarry located inland of the shoreline exposure at Big Gully include Oestokerkus, a genus of leanchoiliid closely related to the well-known Leanchoilia, the early chelicerate Wisangocaris and the type species of a monotypic genus of artiopodan arthropod, Australimicola. An armoured lobopodian of the Family Luolishaniidae is known from a single specimen that closely resembles the species Collinsovermis monstruosus from the Burgess Shale.

In 2011, seven fossils of large, isolated compound eyes were described from the inland quarry site at Emu Bay, as well as the first well-preserved visual surfaces of the eyes of Anomalocaris. The latter specimens are consistent with anomalocaridids being closely related to arthropods as had been suspected. The find also indicated that advanced arthropod eyes had evolved very early, before the evolution of jointed legs or hardened exoskeletons. The eyes were 30 times more powerful than those of trilobites, long thought to have had the most advanced eyes of any species contemporary with Anomalocaris and which were only able to sense night or day. With more than 24,000 lenses, the resolution of the 3 centimetres (1.2 in) wide eyes would have been rivaled only by that of the modern dragonfly, which has 28,000 lenses in each eye.

Paleobiota

Restoration of the related species T. burgessensis
Restoration of the related species T. burgessensis
Life restoration of the related Isoxys curvirostratus
Life restoration of the related Isoxys curvirostratus
A reconstruction of the closely related T. longicaudata
A reconstruction of the closely related T. longicaudata
A drawing of the closely related S. clypeata
A drawing of the closely related S. clypeata
Kangacaris (left) and Emucaris (right)
Kangacaris (left) and Emucaris (right)
12 images

After Paterson et al.(2015).

Arthropods

Arthropods
Genus Species Notes Images
Anomalocaris A. daleyae A predatory anomalocaridid radiodont closely related to the type species.
Echidnacaris E. briggsi A filter feeding tamisiocaridid radiodont, formerly known as "Anomalocaris" briggsi
Wisangocaris W. barbarahardyae A stem-chelicerate belonging to the Habeliida, and a durophagous predator, with evidence of trilobite predation.
Tuzoia T. australis, unnamed larger species A large bivalved hymemocarine, with a nearly cosmopolitan distribution.
Isoxys I. communis, I. glaessneri An extremely common bivalved arthropod, and a key component of most Cambrian faunas.
Oestokerkus O. megacholix A megacheiran belonging to the family Leanchoiliidae
Tanglangia T. rangatanga A megacheiran, a second species, T. longicaudata, is known from the earlier Chengjiang biota in China.
Squamacula S. buckorum A basal artiopod, often classified as one of the most basal members of the group.
Australimicola A. spriggi A basal artiopod
Eozetetes E. gemmelli A vicissicaudatan artiopod, and is often considered to be a close relative of Aglaspidida.
Kangacaris K. zhangi A nektaspid artiopod belonging to the family Emucarididae. A second species of Kangacaris, K. shui, is known from earlier deposits from China.
Emucaris Emucaris fava
Redlichia R. takooensis, R. rex A trilobite belonging to the order Redlichiida. One species from the area, R. rex, was carnivorous, and potentially cannibalistic.
Holyoakia H. simpsoni A trilobite belonging to the order Corynexochida
Megapharanaspis M. nedini A trilobite belonging to the order Redlichiida
Balcoracania B. dailyi A trilobite belonging to the order Redlichiida
Emuella E. polymera A trilobite belonging to the order Redlichiida
Estaingia E. bilobata A trilobite belonging to the order Redlichiida

Other animals

Non-arthropod animals
Genus Species Notes Images
Nesonektris N. aldridgei A member of Vetulicolia, a group of basal chordates often considered to be close relatives of tunicates.
Vetustovermis A possible member of Nectocarididae, a controversial family of nektonic invertebrates.
Myoscolex M. ateles An enigmatic animal of unknown affinity, has been suggested to represent an annelid worm, or as a close relative of Opabinia regalis.
"Petalloid" Indeterminate An enigmatic, unnamed animal of unknown affinity that represents one of the most common benthic organisms from the biota.
Wronascolex W. antiquus, W. iacoborum Palaeoscolecid worm
Luolishaniidae Indeterminate An armoured lobopodian, referred to as the "EBS Collin's Monster", and bears a similar appearance to the Burgess Shale species Collinsovermis monstruosus.
Chancelloria C. australilonga A member of Chancelloriidae, a group of spiny sponge-like animals.
Demospongiae Spp. Sponges, predominantly Leptomitidae, with minor Hamptoniidae and Choiidae
"Eldonioid" Indeterminate Related to Eldonia
Brachiopoda Includes members of the families Eoobolidae and Botsfordiidae
Hyolitha
Polychaeta Has possible affinities to Burgessochaeta.

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Text from Wikipedia, CC BY-SA 4.0 · Source article