| Croudace Bay Formation | |
|---|---|
| Stratigraphic range: Lopingian (Wuchiapingian) ~ | |
| Type | Geological formation |
| Unit of | Newcastle Coal Measures |
| Sub-units | Belmont Conglomerate Member |
| Underlies | Upper Pilot Coal |
| Overlies | Fassifern Coal |
| Thickness | 20–32 cm (7.9–12.6 in) (Belmont insect bed) |
| Lithology | |
| Primary | Coal, conglomerate and sandstone |
| Other | Volcanic chert and shale |
| Location | |
| Coordinates | 32°58′48″S 151°38′42″E / 32.98°S 151.645°E (Warner's Bay) |
| Region | Hunter Region |
| Country | Australia |
The Croudace Bay Formation is a geological formation dating back to approximately ~255 Ma, during the Wuchiapingian age of the Lopingian (Late Permian). Its lithology comprises of coal, conglomerates, sandstones, and smaller amounts of volcanic chert and shales. It is best known for the Belmont insect bed, part of the Belmont Conglomerate Member in the upper strata of the formation.
The Belmont Conglomerate Member filled an engraved river valley and the stream, which transported the gravel that was deposited within this valley, flowed in a south-southwest direction at about 210°. The gravel which filled the valley originated from the New England Fold Belt to the north-east, a highland area during the Permian. This river flowed into the Hunter Trough, a part of the Sydney Basin, depositing gravel within the Belmont area, along with sand further downstream, west of Fennel Bay in the Lake Macquarie area. The Belmont Conglomerate is one of the several lenticular fluvial bodies deposited during the Late Permian in the Newcastle Coal Measures. The Awaba and Warner's Bay tuffs, overlaying and underlaying the Belmont Conglomerate respectively, become thinner from north to south.
The Belmont insect bed is comprised of lithified volcanic chert, represented by a fine groundmass of crystalized glass shards and fine, large crystals consisting primarily of feldspars, along with additional opaque material. In thin sections, the grains show linear alignment, and within sliced insect seam blocks, fine horizontal bedding planes are visible. Cross-lamination has not been observed. There is a slight upward fining within the insect seam, more noticeable in some specimens than others. The seam descends gently towards the west and weathers to generally rhomboidal blocks. In the majority of localities there are three distinct vertical zones. One section of insect bed from site 206 is typical of the sequence at all other sites sampled along the Violet Town Ridge. In other localities there are variations in the presence and thickness of a conchostracan layer, located in the zonation of the fossil insects and in the absence or presence of a basal layer known as the "chopped straw" zone.
Coleopterans represent all beetles.
| Coleopterans of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Permosyne | P. affinis | Permosynoidea, | |
| P. belmontensis | |||
| P. mitchelli | |||
| P. pincombeae | |||
Auchenorrhyncha includes cicadas, leafhoppers, treehoppers, planthoppers, and spittlebugs.
| Auchenorrhynchans of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Anomaloscytina | A. incompleta | Scytinopteroidea, | |
| A. metapteryx | |||
| Austroprosbole | A. maculata | Palaeontinoidea, | |
| Belmontocarta | B. perfecta | Cercopoidea, | |
| Elliptoscarta | E. ovalis | Scytinopteroidea, | |
| Eochiliocycla | E. angusta | Scytinopteroidea, | |
| Homaloscytina | H. plana | Prosboloidea, | |
| Mitchelloneura | M. permiana | Prosboloidea, | |
| Orthoscytina | O. belmontensis | Prosboloidea, | |
| O. indistincta | |||
| O. irregularis | |||
| O. mitchelli | |||
| O. obliqua | |||
| O. pincombei | |||
| O. quinquemedia | |||
| O. subcostalis | |||
| O. tetraneura | |||
| Palaeovicia | P. incerta | Scytinopteroidea, | |
| Paraknightia | P. magnifica | Scytinopteroidea, | |
| Permagra | P. distincta | Scytinopteroidea, | |
| Permocentrus | P. trivenulata
(Formerly Permoscarta trivenulata) |
Scytinopteroidea, | |
| Permobrachus | P. dubia
(Formerly Permodiphthera dubia) |
Prosboloidea, | |
| P. magnus | |||
| Permodiphthera | P. robusta | Prosboloidea, | |
| Permofulgor | P. belmontensis | Permofulgoridae | |
| P. indistinctus (Synonym of P. belmontensis; specimen is a counterpart) | |||
| Permoglyphis | P. belmontensis | Prosboloidea, | |
| Permojassus | P. australis | Scytinopteroidea, | |
| P. dubius | |||
| Permoscarta | P. mitchelli | Scytinopteroidea, | |
| Permovicia | P. obscura | Scytinopteroidea, | |
| Psocoscytina | P. bifida | Scytinopteroidea, | |
| Stanleyana | S. pulchra | Scytinopteroidea, | |
| Stenoscytina | S. australiensis | Scytinopteroidea, | |
| Stenovicia | S. angustata | Scytinopteroidea, | |
| Scytinopteridae indet. | sp. indet. | Scytinopteroidea, | |
Coleorrhyncha includes moss bugs and extinct relatives such as the Progonocimicidae.
| Coleorrhynchans of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Actinoscytina | A. belmontensis | Progonocimicoidea, | |
| Paleorrhynchans of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Austroscytina | A. imperfecta | Archescytinoidea, | |
| Bekkerscytina | B. primitiva | Archescytinoidea, | |
| Eoscytina | E. incompleta | Archescytinoidea, | |
| E. migdisovae | |||
Sternorrhynchans include aphids, whiteflies, and scale insects.
| Sternorrhynchans of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Belpsylla | B. reticulata | Protopsyllidioidea, | |
| Clavopsyllidium | C. minutum | Protopsyllidioidea, | |
| Eopsyllidium | E. delicatulum | Protopsyllidioidea, | |
| Eupincombea | E. postica | Pincombeoidea, | |
| Permocapitus | P. globulus | Pincombeoidea, | |
| Permocephalus | P. knighti | Pincombeoidea, | |
| Permopsyllidium | P. affine | Protopsyllidioidea, | |
| P. mitchelli | |||
| Permopsyllidops | P. stanleyi | Protopsyllidioidea, | |
| Permopsylloides | P. insolita | Protopsyllidioidea, | |
| Permothea | P. latipennis | Protopsyllidioidea, | |
| Permotheella | P. scytinopteroides | Protopsyllidioidea, | |
| Pincombea | P. mirabilis | Pincombeoidea, | |
| Protopincombea | P. obscura | Pincombeoidea, | |
| Protopsyllidium | P. australe | Protopsyllidioidea, | |
| P. sinuatum | |||
| Protopsyllops | P. minuta | Protopsyllidioidea, | |
| Psocopsyllidium | P. media | Protopsyllidioidea, | |
| Psyllidella | P. magna | Protopsyllidioidea, | |
| Psyllidiana | P. davisia | Protopsyllidioidea, | |
| Tripsyllidium | T. wadei | Protopsyllidioidea, | |
Mecopterans are known as scorpionflies.
| Mecopterans of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Belmontia | B. mitchelli | Belmontiidae | |
| Parabelmontia | P. permiana
(Synonym of Belmontia) |
Belmontiidae | |
| Mesochorista
(All listed species previously under Permochorista) |
M. affinis | Permochoristidae | |
| M. australica | |||
| M. mitchelli | |||
| M. sinuata | |||
The protelytropterans are considered a stem group of modern earwigs.
| Protelytroptera of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Permophilus | P. pincombei | Permophilidae | |
| Protocoleus | P. mitchelli | Protocoleidae | |
Thysanopterans are known as thunderbugs.
| Thysanopterans of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Austrocypha | A. abrupta | Lophioneurida, | |
| Lophioneura | L. angusta | Lophioneurida, | |
| L. conjuncta | |||
| L. ustulata | |||
| Lophiocypha | L. maxima | Lophioneurida, | |
| L. permiana | |||
| L. stanleyi | |||
| Zoropsocus | Z. delicatulus | Lophioneurida, | |
| Z. stanleyi | |||
| Other insects of the Croudace Bay Formation | |||
|---|---|---|---|
| Genus | Species | Clade | Image |
| Permithone | P. belmontensis | Neuropterida, | |
| Permosialis | P. belmontensis | Neoptera, | |
| Eumegasecoptera indet. | sp. indet. | Megasecoptera, | |
| Meganisoptera indet. | sp. indet. | Meganisoptera, | |
| Paraplecoptera indet. | sp. indet. | Paraplecoptera, | |
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