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
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
- DOI
- 10.1002/gj.876
No coin nor oath required. For personal study only.
✦ 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.
📜 SIMILAR VOLUMES
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