Permian palynostratigraphy of the Collie Basin, Western Australia

Backhouse, John

doi:10.1016/0034-6667(91)90046-6

Cited by 144 publications

(84 citation statements)

References 11 publications

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“…There are however some difficulties in correlating the zonation scheme established here with that of Backhouse (1991) for the Collie Basin. The most important limitation is due to the fact that between the two areas certain key species reveal variable ranges and abundances, an observation also recognized by Backhouse (1991) when comparing the assemblages from the Collie Basin with other Australian basins. Due to the difficulties outlined above, only a broad correlation (Fig.…”

Section: Australiamentioning

confidence: 96%

“…Correlation with the zonation scheme of Backhouse (1991). -Backhouse (1991) established the most widely compared palynostratigraphic scheme from the Gondwana Permian sequences of the Collie Basin of Australia.…”

Section: Australiamentioning

confidence: 99%

Section: Australiamentioning

confidence: 99%

“…-Backhouse (1991) established the most widely compared palynostratigraphic scheme from the Gondwana Permian sequences of the Collie Basin of Australia. There are however some difficulties in correlating the zonation scheme established here with that of Backhouse (1991) for the Collie Basin. The most important limitation is due to the fact that between the two areas certain key species reveal variable ranges and abundances, an observation also recognized by Backhouse (1991) when comparing the assemblages from the Collie Basin with other Australian basins.…”

Section: Australiamentioning

confidence: 99%

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Late Palaeozoic palynomorph assemblages from the Karoo Supergroup and their potential for biostratigraphic correlation, Kalahari Karoo Basin, Botswana

Modie¹,

Hérissé²

2009

Bull. Geosci.

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Late Carbonifeous to Permian core samples from two borehole sections, STRAT 1 and CKP 6, that penetrate the glacial to postglacial and coal-bearing Lower Karoo sequence, Kalahari Karoo Basin, Botswana, contain well preserved pollen and spore palynomorphs. The palynomorph assemblages comprise 165 species of spores and pollen, and few acritarchs and chlorophycean algae. This paper presents a local biozonation of three succeeding assemblage zones, recognisable in each borehole section. The assemblage zones are named: the Hamiapollenites bullaeformis Biozone, the Cyclogranisporites gondwanensis Biozone and the Platysaccus papilionis-Striatopodocarpites fusus Biozone, in ascending order of stratigraphy. Assemblages are compared and correlated with assemblages described from other Gondwana areas of Africa, Australia, Arabia, South America and Antarctica. A general analysis of taxa from the Kalahari Karoo Basin indicates a distinct similarity with assemblages from the Paraná Basin of South America. The Hamiapollenites bullaeformis Biozone is comparable with the Vittatina costabilis Interval Zone of the Paraná Basin. Assemblages from the Cyclogranisporites gondwanensis and the Platysaccus papilionis-Striatopodocarpites fusus zones are comparable with the Lueckisporites virkkiae Interval Zone. Age determination for the assemblages in the Kalahari Karoo Basin is inferred from comparison with similar assemblages from previous Gondwana studies, and ranges from the Late Carboniferous (Kasimovian-Gzhelian) to latest Early or possibly earliest Middle Permian (Late Cisularian to Early Guadalupian)

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Section: Australiamentioning

confidence: 96%

Section: Australiamentioning

confidence: 99%

Section: Australiamentioning

confidence: 99%

Section: Australiamentioning

confidence: 99%

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Late Palaeozoic palynomorph assemblages from the Karoo Supergroup and their potential for biostratigraphic correlation, Kalahari Karoo Basin, Botswana

Modie¹,

Hérissé²

2009

Bull. Geosci.

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“…4) no presentan elementos diagnósticos que permitan referirlas a algunas de la biozonas conocidas para el centro-oeste de Argentina (Césari y Gutiérrez, 2001;Gutiérrez et al, 2003). Entre sus componentes se destaca la asociación de Barakarites rotatus, Protohaploxypinus bharadwaji, Anapiculatisporites teretangulus, Horriditriletes ramosus y Converrucosisporites confluens, cuyos registros se encuentran hasta el momento entre el Pennsylvaniano y el Guadalupiano (Tabla 5), siendo comunes en el Pérmico de Australia, India, Antártica, África (véase Foster, 1979;Playford, 1990;Backhouse, 1991), Brasil, Uruguay y Argentina (véase Césari et al, 1995;Quadros et al, 1996;Playford y Dino, 2000Souza y Calegari, 2004;Beri et al, 2006;Gutiérrez et al, 2006;Smaniotto et al, 2006;Vergel, 2008;di Pasquo et al, 2010 (Césari y Gutiérrez, 2001;Césari, 2007;Gutiérrez et al, 2008 (Césari, 2007;Gutiérrez et al, 2008), siendo parcialmente equivalente a las biozonas Striatites (Cuenca Chacoparaná en Argentina; Russo et al, 1980) y Lueckisporites virkkiae (Cuenca Paraná en Brasil; Souza y Marques Toigo, 2005).…”

Section: Edadunclassified

Paleoenvironment and paleontology of the Andapaico Formation (upper Paleozoic, central Precordillera, Argentina)

Correa¹,

Carrevedo²,

Gutiérrez³

2012

Andgeo

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Recognition of southern Gondwanan palynomorphs at Gondwana's northern margin—and biostratigraphic correlation of Permian strata from SE Turkey and Australia

Stolle¹

2010

Geological Journal

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This study focuses on the palynology of Guadalupian (Middle Permian) strata of SE Turkey, especially on late Wordian and earliest Capitanian deposits, which are dated by foraminifers and can be chronostratigraphically related to the geological timescale. Herein, palynological species, such as Altitriletes densus, Cymatiosphaera gondwanensis and Praecolpatites sinuosus, previously characteristic for Pakistan, Australia and Antarctica are recorded. Therefore, the Permian biozones of marine fauna and the palynology of SE Turkey and the rest of the Arabian area and Australia are compared and correlated. This long-distance, eastern Gondwana-wide biostratigraphical correlation, conducted for the first time in the Guadalupian epoch in this study, showed that Corisaccites alutas has a similar Last Occurrence Datum in SE Turkey and in Australia. The correlation also showed that in the late Wordian a number of species were present throughout eastern Gondwana, whereas the distribution of other certain species was influenced by provincialism. Hence, it may be concluded that certain species of parent plants probably co-occurred Gondwana-wide, while the distribution of others was dependant on climate.

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Permian palynostratigraphy of the Collie Basin, Western Australia

Cited by 144 publications

References 11 publications

Late Palaeozoic palynomorph assemblages from the Karoo Supergroup and their potential for biostratigraphic correlation, Kalahari Karoo Basin, Botswana

Late Palaeozoic palynomorph assemblages from the Karoo Supergroup and their potential for biostratigraphic correlation, Kalahari Karoo Basin, Botswana

Paleoenvironment and paleontology of the Andapaico Formation (upper Paleozoic, central Precordillera, Argentina)

Recognition of southern Gondwanan palynomorphs at Gondwana's northern margin—and biostratigraphic correlation of Permian strata from SE Turkey and Australia

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