The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850Various
Science
The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850
Various
Science -- Periodicals
"Besides the different members of the Eocene formation, properly so
called, of the Paris basin, I comprehend in this Flora the fossils of
the same formation in England, at the Isle of Wight, and Isle of
Sheppey in the London basin. These latter fossils, consisting almost
solely of fruits transformed into pyrites, constitute a whole which
has no analogue in any other of the Tertiary basins of Europe; not
only in the number and diversity of these fruits, but in their
peculiar characters, which remove them widely from the plants whose
leaves occur in the other beds of the same geological epoch.
Everything, therefore, would lead us to suppose that these fruits,
although belonging to plants cotemporaneous with the Eocene deposits
of Europe, have been brought from distant countries by marine
currents, just as fruits are still brought from the equatorial regions
of America to the coasts of Ireland or Norway by the great current of
the Atlantic. The deposit in the Isle of Sheppey appears therefore to
be an accidental case in the Eocene deposits, and the Paris basin
presents none of these fossils.
"The Tertiary basin of Belgium, which follows that of London, has
yielded, near Brussels, some fossil fruits in very small numbers, but
which appear identical with one of the genera most abundant at
Sheppey. This is the _Nipadites_, considered at first as a species of
Coco, under the name of _Cocus burtini_.
"Lastly, following the advice of my learned associate, M. Elie de
Beaumont, I have included in the same Flora the plants contained in
the Lignites of the shores of the Baltic and Pomerania, so rich in
amber, in which these vegetables have often been preserved. It is to
the labours of M. Goeppert that we are indebted for a knowledge of
these vegetables, most frequently represented by very small fragments,
the relations of which he has determined with much skill and
accuracy."
With materials collected in these various localities, but of which the
greater part are still unpublished, we may construct the Flora of the
Eocene epoch; but the list, comprehending only the species described,
or at least determined, is only a mere sketch.
M. Brongniart then gives the names of the vegetables belonging to the
Eocene epoch; these are, for the Amphigenous cryptogams, algæ, and
mushrooms; for the Acrogenous cryptogams, hepatici, mosses, ferns,
equisetaceæ, and characeæ. The Monocotyledons present Naiades,
Nipaceæ, and palms. The Gymnospermous dicotyledons are represented by
Coniferæ (Cupressinæ, Abietineæ, Taxineæ, and Gnetaceæ.) Lastly, among
the Angiospermous dicotyledons, we find examples of Betulaceæ,
Cupuliferæ, Juglandeæ, Ulmaceæ, Proteaceæ, Leguminosæ, OEnothereæ,
Cucurbitaceæ, Sapindaceæ, Malvaceæ, Ericaceæ, and three doubtful
families (Phyllites, Antholithes, and Carpolithes.)
"The most remarkable characters of this Flora are,--
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