Pliocene Nothofagus Wood from the Transantarctic Mountains
Subfossil wood fragments up to 10 cm long and 2 cm in diameter recovered from a locality thought on the basis of diatom deposits to be upper Pliocene-lower Pleistocene (Oliver Bluffs, Sirius Formation, 85°10'S., between 1800 and 1900 m in the Transantarctic Mountains) were sectioned for identif...
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Scholarship @ Claremont
1987
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Online Access: | https://scholarship.claremont.edu/aliso/vol11/iss4/12 https://scholarship.claremont.edu/cgi/viewcontent.cgi?article=1512&context=aliso |