Carapace Nunatak
Carapace Nunatak (76°53′S 159°24′E / 76.883°S 159.400°E) is a prominent isolated
Geology
The Carapace Nunatak is an erosional
At the base of Carapace Nunatak, about 130 m (430 ft) of cross-bedded sandstones and fine lithic
Conformably overlying the Carapace Sandstone is 300 m (980 ft) of Kirkpatrick Basalt. The basalt
Fossils
The fossiliferous horizons of the Ferrar Group at Carapace Nunatak contain one of the richest and most diverse
In the laminated, and silicified, fine-grained lake deposits of Carapace Sandstone, fossil conchostracans (clam shrimp) are the most important in terms of number of individuals and distribution.[6][7] They consist of small, 1 to 2 cm (0.39 to 0.79 in), bivalved spinicaudatan arthropods. They are most typical of ephemeral, alkaline ponds. Associated macrofossils include notostracan branchiopods, ostracodes, insect nymphs and wings, and plant leaves. Macroscopic trace fossils are extremely rare.[5]
The lake cherts from the upper part of Carapace Sandstone contain an abundance of fusainized plant material and animal remains. This fine-grained Magadi-type chert preserves abundant plant fossils. These plant fossils include at least three conifer taxa represented by vegetative and reproductive structures, isolated ovules, a diversity of taxa of fern pinnules, rachides and rhizomes, and cycadophyte foliage. Intermixed with the plant fossils are numerous of shallow-water conchostracans and other ephemeral freshwater crustaceans.[5][8]
References
- ISBN 978-0-7864-3590-6
- ^ "Carapace Nunatak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 17 October 2023.
- ^ a b c Ballance, P.F. and Watters, W.A., 1971. The Mawson Diamictite and the Carapace Sandstone, formations of the Ferrar Group at Allan Hills and Carapace Nunatak, Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, 14(3), pp.512-527.
- ^ a b c Bradshaw, M.A., 1987. Additional field interpretation of the Jurassic sequence at Carapace Nunatak and Coombs Hills, south Victoria Land Antarctica. New Zealand Journal of Geology and Geophysics, 30(1), pp.37-49.
- ^ a b c Babcock, L.E., Leslie, S.A., Elliot, D.H., Stigall, A.L., Ford, L.A. and Briggs, D.E., 2006. The “Preservation Paradox”: microbes as a key to exceptional fossil preservation in the Kirkpatrick Basalt (Jurassic), Antarctica. The Sedimentary Record, 4(4), pp.4-8.
- ^ a b Ribecai, C., 2007. Early jurassic miospores from ferrar group of carapace nunatak, south victoria Land, Antarctica. Review of Palaeobotany and Palynology, 144(1-2), pp.3-12.
- ^ Yabin, Shen, 1994. Jurassic conchostracans from Carapace Nunatak, southern Victoria Land, Antarctica. Antarctic Science, 6, pp.105–113.
- ^ Hieger, T.J., Serbet, R., Harper, C.J., Taylor, T.N., Taylor, E.L. and Gulbranson, E.L., 2015. Cheirolepidiaceous diversity: an anatomically preserved pollen cone from the Lower Jurassic of southern Victoria Land, Antarctica. Review of Palaeobotany and Palynology, 220, pp.78-87.