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113:, that occurs on Fremouw Peak. This unique chert deposit contains anatomically preserved plant fossils. These fossils can be used to reconstructing complex three-dimensional plant structures and understand reproductive biology and development.
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Stratigraphy and petrology of the mainly fluviatile
Permian and Triassic Beacon rocks, Beardmore Glacier area, Antarctica.
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Fossil sites in the continental
Victoria and Ferrar groups (Triassic-Jurassic) of north Victoria Land, Antarctica.
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The Beacon
Supergroup (Devonian–Triassic) and Ferrar Group (Jurassic) in the Beardmore Glacier area, Antarctica.
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Carolina and London, McFarland & Company, Inc. 1771 pp.
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Bomfleur, B., Schneider, J.W., Schöner, R., Viereck-Götte, L. and Kerp, H., 2011.
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have been found in these sedimentary rocks. Of more significance is an
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Structurally
Preserved Permian and Triassic Floras from Antarctica.
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Antarctic
Paleobiology, its Role in the Reconstruction of Gondwana
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exposed on the slopes of
Fremouw Peak. This peak serves as the
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is named for a 614-metre (2,014 ft) thick interval of
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Ohio State
University Institute of Polar Studies Report
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In: Taylor, T.N., and Taylor, E.L., eds, pp. 149-164,
216:Barrett, P.J., Elliot, D.H., Lindsay, J.F., 1986.
222:Geology of the central Transantarctic Mountains.
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162:United States Department of the Interior
67:United States Antarctic Research Program
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91:for the Fremouw Formation. Fragmentary
16:Mountain in Ross Dependency, Antarctica
243:Taylor, E.L., and Taylor, T.N., 1990.
63:Advisory Committee on Antarctic Names
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348:Paleontological sites of Antarctica
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353:Mountains of the Ross Dependency
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301:. You can help Knowledge by
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65:for Edward J. Fremouw, a
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134:References
93:vertebrate
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104:Triassic
78:Triassic
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32:164°20′E
100:outcrop
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