Stratigraphy of Antarctic late Cenozoic pectinid-bearing deposits
Antarctic late Cenozoic pectinid-bearing sedimentary strata are chiefly confined to localities in the northern part of the Antarctic Peninsula, in the McMurdo Sound area, and Marine Plain, East Antarctica. Ages of these deposits range from Oligocene to Holocene. Chlamys -like scallops, which are abs...
Published in: | Antarctic Science |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1998
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Online Access: | http://dx.doi.org/10.1017/s0954102098000212 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102098000212 |