The Student's Elements of GeologyLyell, Charles, Sir
Science
The Student's Elements of Geology
Lyell, Charles, Sir
Geology
Upper Miocene Beds of Œningen, in Switzerland.—The faluns of the Loire
first served, as already stated (p. 211), as the type of the Miocene
formations in Europe. They yielded a plentiful harvest of marine fossil
shells and corals, but were entirely barren of plants and insects. In
Switzerland, on the other hand, deposits of the same age have been
discovered, remarkable for their botanical and entomological treasures.
We are indebted to Professor Heer, of Zurich, for the description,
restoration, and classification of several hundred species and
varieties of these fossil plants, the whole of which he has illustrated
by excellent figures in his “Flora Tertiaria Helvetiæ.” This great
work, and those of Adolphe Brongniart, Unger, Goppert and others, show
that this class of fossils is beginning to play the same important part
in the classification of the tertiary strata containing lignite or
brown coal as an older flora has long played in enabling us to
understand the ancient coal or carboniferous formation. No small
skepticism has always prevailed among botanists as to whether the
leaves alone and the wood of plants could ever afford sufficient data
for determining even genera and families in the vegetable kingdom. In
truth, before such remains could be rendered available a new science
had to be created. It was necessary to study the outlines, nervation,
and microscopic structure of the leaves, with a degree of care which
had never been called for in the classification of living plants, where
the flower and fruit afforded characters so much more definite and
satisfactory. As geologists, we cannot be too grateful to those who,
instead of despairing when so difficult a task was presented to them,
or being discouraged when men of the highest scientific attainments
treated the fossil leaves as worthless, entered with full faith and
enthusiasm into this new and unexplored field. That they should
frequently have fallen into errors was unavoidable, but it is
remarkable, especially if we inquire into the history of Professor
Heer’s researches, how often early conjectures as to the genus and
family founded on the leaves alone were afterwards confirmed when
fuller information was obtained. As examples to be found on comparing
Heer’s earlier and later works, I may instance the chestnut, elm,
maple, cinnamon, magnolia, buckbean or Menyanthes, vine, buckthorn
(_Rhamnus_), _Andromeda_ and _Myrica,_ and among the conifers _Sequoia_
and _ Taxodium._ In all these cases the plants were first recognised by
their leaves, and the accuracy of the determination was afterwards
confirmed when the fruit, and in some instances both fruit and flower,
were found attached to the same stem as the leaves.
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