Abstract
The microspore content of samples from a bore at Comaum, S.A., has been
determined. Evidence is brought forward which suggests that the passage
from Tertiary to Mesozoic strata occurred between 620-ft and 650-ft levels.
Several new sporomorphs have been described; their affinities with living and
fossil types have been considered.
Subject
Plant Science,Ecology, Evolution, Behavior and Systematics
Cited by
52 articles.
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