LC3: Neocomian, Australia
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Rintoulia variabilis leaf, cuticle
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Otwayia hermata leaf
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Plantae informal Long shoots bearing spur shoots sterile axis
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Equisetopsida
- Araucariaceae
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Araucariaceae informal Araucariacean cone scales
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Brachyphyllum tyersensis leaf
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Sphenopteridae
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Sphenopteris informal sp. B leaf
Sternberg 1825
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Lycopodiopsida
- Isoetales
- Isoetaceae
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Isoetites abundans leaf
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Polypodiopsida
- Cyatheales
- Cyatheaceae
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Coniopteris fruitiformis leaf
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Coniopteris victoriensis leaf
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Cycadopsida
- Cycadales
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Taeniopteris daintreei leaf
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Coniferales
- Podocarpaceae
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Bellarinea richardsii leaf
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Bennettitales
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Otozamites douglasii leaf
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Pinopsida
- Pinales
- Taxaceae
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Palissya elegans non-seed repro
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Hepaticae
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Hepaticites informal sp. A
Walton 1925
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>1 specimen | |||||||||
thallus | ||||||||||
see common names |
Geography
Country: | Australia | State/province: | Victoria |
Coordinates: | 38.1° South, 146.5° East (view map) | ||
Paleocoordinates: | 80.1° South, 75.2° East | ||
Basis of coordinate: | estimated from map |
Time
Period: | Cretaceous | Epoch: | Early/Lower Cretaceous |
Key time interval: | Neocomian | ||
Age range of interval: | 145.00000 - 130.00000 m.y. ago |
Stratigraphy
Geological group: | Strzelecki | Formation: | Rintoul Creek | Member: | Locmany |
Regional section: | Gippsland Basin | ||||
Stratigraphy comments: In the Tyers River Subgroup. |
Lithology and environment
Lithology description: The Locmany Member of the Rintoul Creek Formation consists of interbedded quartzose sandstones and fossiliferous siltstones. The lower portion of the Locmany Member contains a few thin, discontinuous, conglomerates and bituminous coal seams. The Locmany Member is the source of the majority of the fossils examined in this study. | |||
Environment: | terrestrial indet. | Tectonic setting: | rift |
Geology comments: The Gippsland Basin is a roughly east-west orientated rift and epicratonic sag basin located along the southeastern margin of Victoria, Australia. The basin was initiated in the latest Jurassic or Early Cretaceous as rifting propagated along a roughly west-east axis between Austrailia and Antarctica. |
Taphonomy
Modes of preservation: | adpression |
Size of fossils: | macrofossils |
Collection methods and comments
Collection methods: | surface (in situ),chemical,field collection |
Reason for describing collection: | biostratigraphic analysis |
Metadata
Also known as: | Gippsland Basin, Locmany Creek 3 | ||
Database number: | 33945 | ||
Authorizer: | R. Lupia | Enterer: | B. Wilborn |
Modifier: | B. Wilborn | Research group: | paleobotany |
Created: | 2003-08-10 12:18:13 | Last modified: | 2003-08-10 15:18:13 |
Access level: | the public | Released: | 2003-08-10 12:18:13 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
8849. | S. McLoughlin, A.-M.P. Tosolini, N.S. Nagalingum and A.N. Drinnan. 2002. Early Cretaceous (Neocomian) flora and fauna of the Lower Strzelecki Group, Gippsland Basin, Victoria. Memoirs of the Association of Australasian Palaeontologists 26:1-144 [R. Lupia/B. Wilborn/B. Wilborn] |