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Gisbornian (Caradoc) graptolites from New South Wales, Australia: systematics, biostratigraphy and evolution

✍ Scribed by Barrie Rickards; Lawrence Sherwin; Penelope Williamson


Publisher
John Wiley and Sons
Year
2001
Tongue
English
Weight
692 KB
Volume
36
Category
Article
ISSN
0072-1050

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✦ Synopsis


Abstract

The biodiversity record of graptolites from the Cheeseman's Creek Formation, considered herein as late Gisbornian (Caradoc) in age, has been substantially increased to fifteen taxa, including the new species Dicellograptus praemorrisi sp. nov. and Climacograptus vandenbergi sp. nov. Some of the records have global correlative significance enabling us to identify the wilsoni Biozone ( = calcaratus Biozone of eastern Australia). Several evolutionary lineages have been recognized:

Dicellograptus moffatensis (Carruthers, 1858) →  D. praemorrisi sp. nov → D. morrisi Hopkinson, 1871

Glossograptus hincksi Hopkinson, 1872 → Glossograptus? sp.

Climacograptus bicornis (J. Hall, 1847) → C. vandenbergi sp. nov. → C. lanceolatus VandenBerg, 1990.

Copyright © 2001 John Wiley & Sons, Ltd.


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Discussion of ‘Gisbornian (Caradoc) grap
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Rickards, Sherwin and Williamson (2001) have described a small graptolite fauna from New South Wales which they interpret to be Gisbornian (Caradoc), and provide evolutionary schemes for several lineages (see also Sherwin and Rickards 2000) in which the precise age is crucial. My study of more diver

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VandenBerg (2002) and in his Discussion paper (2003, this issue of Geological Journal) raises doubts on our attribution of the Keenan's Bridge (near Cheeseman's Creek, NSW) graptolite fauna to the Late Gisbornian (Rickards et al. 2001), preferring to refer the assemblage to the Bolindian, and at