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Coalsack Bluff exposes a paleontologically important, fossiliferous sequence of sedimentary rocks containing the
Permian–Triassic boundary. This bluff is a fossil location that has yielded well preserved
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were first discovered in
Antarctica. The vertebrate fossils found at this location are important in understanding the
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Retallack, G.J., Jahren, A.H., Sheldon, N.D., Chakrabarti, R., Metzger, C.A. and Smith, R.M.H., 2005.
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Tetrapod turnover during the Permo-Triassic transition explained by temperature change.
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Permian – Triassic boundary in the central
Transantarctic Mountains, Antarctica.
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that reveal the paleoclimatic and paleontologic changes associated with the
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and vertebrate paleontology of
Permian and Triassic strata in Antarctica.
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Collinson, J. C., Hammer, W. R., Askin, R. A. & Elliot, D. H. 2006.
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65:(1961–62) because of the coal seams found running through the bluff.
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101:. It is the location where abundant fossils of Early Triassic
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Liu, J., Abdala, F., Angielczyk, K.D. and Sidor, C.A., 2022.
53:) is a small rock bluff standing at the northern limits of
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63:New Zealand Geological Survey Antarctic Expedition
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193:The Permian–Triassic boundary in Antarctica
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173:United States Department of the Interior
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305:Paleontological sites of Antarctica
164:Geographic Names Information System
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99:Permian–Triassic extinction event
320:Shackleton Coast geography stubs
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169:United States Geological Survey
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310:Cliffs of the Ross Dependency
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61:. It was so named by the
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16:Rock bluff in Antarctica
254:location article is a
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41:84.233°S 162.417°E
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176:. Retrieved
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84:invertebrate
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82:and plant,
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299:Categories
178:2011-11-16
145:References
88:vertebrate
103:tetrapods
95:paleosols
113:See also
80:Triassic
32:162°25′E
91:fossils
76:Permian
29:84°14′S
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