Where: Antarctica (84.7° S, 176.2° W: paleocoordinates 2.0° S, 155.2° W)
• outcrop-level geographic resolution
When: Taylor Formation, Floran (504.5 - 503.0 Ma)
• The Taylor Formation has been correlated to the archaeocyathid-rich Skackleton Limestone, located several hundred miles to the northwest. The age/stage determiantions are based on work done by Encarnacion et. al PMPD# Reference 579
• formation-level stratigraphic resolution
Environment/lithology: lithified, conglomeratic limestone and chert
Collection methods: bulk,
• Majority of the collection consists of oblique, longitudinal and transverse sections of tubes all attributed to one organism (Cloudina?). An additional trilobite fragment was found but not identified. It should be noted that the trilobite fragment precludes a PreCambrian age.
Primary reference: E. L. Yochelson and E. Stump. 1977. Discovery of Early Cambrian fossils at Taylor Nunatak, Antarctica. Journal of Paleontology 51(4):872-875 [M. Patzkowsky/P. Borkow/J. Alroy]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 7820: authorized by Mark Patzkowsky, entered by Zack Krug on 03.06.2000, edited by Phil Borkow and Pete Wagner
Creative Commons license: CC BY (attribution)
Taxonomic list
Acuticloudina | |
Acuticloudina borreloi "The Taylor Nunatak specimens do not closely resemble either of Germ's species, but they are quite similar to C. ? borrelloi."
| |
Trilobita | |
Trilobita indet. Walch 1771 trilobite |