The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic RemainsMantell, Gideon Algernon
Science
The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic Remains
Mantell, Gideon Algernon
Geology -- England -- Guidebooks; Paleontology
Fossil Palm-leaves.--The pinnated and fan-shaped leaves of the Palms
are so peculiar as to be easily recognized in a fossil state. Though
many specimens have been found in the tertiary strata of the Continent,
but two or three examples have been met with in England. The first
discovered British specimen is in my cabinet, and was obtained by
Mr. Fowlstone, of Ryde, from the fresh-water limestone of Whitecliff
Bay, in the Isle of Wight. It is thirteen inches in length, and
eleven in width: fresh-water shells and plants are imbedded with it.
It is figured in Geol. I. of Wight, _2d edit._ p. 431. This species
(_Palmacites Lamanonis_) occurs also at Aix in Provence, in great
perfection, associated with Insects, Fishes, fresh-water shells, &c.
(_Wond._ p. 260. _Petrif._ p. 62).
Twelve species of palm-leaves are enumerated by M. Unger, from the
Tertiary deposits of the Continent. One species has been found in
the Chalk formation of Silesia; the most ancient strata in which the
remains of undoubted palms have as yet been observed.
The fossil palm-leaves of the pinnated form are named _Phœnicites_,[FF]
and examples occur in the Tertiary grits of Puy en Velais, I am not
aware that leaves of this type have been found in England: diligent
research in our tertiary leaf-beds (at Whitecliff Bay, Alum Bay,
Bournemouth, Wareham) will probably sooner or later discover them. The
leaflets have a well-marked median nerve, with fine nervures running
parallel with it; a character by which the foliage of _Phœnicites_ may
be distinguished from that of the Cycadeæ.
[162] From _Phœnix dactylifera_: the Date-Palm.
Fossil Fruits of Palms.--Although certain fruits found in the
coal-measures have been referred to the palm-tribe by M. Unger, Dr.
Lindley, and other botanists, M. Brongniart is of opinion that no such
identification can be established; the same remark applies to the
Carpolithes from the Oolite; in fine, the Tertiary deposits have alone
yielded fruits that can be unquestionably referred to plants of this
order. The most productive British locality of fossil fruits of Palms,
and of many other vegetables, is the Island of Sheppey; and I purpose
describing in this place, not only the remains of this family, but also
of the other plants associated with them.
[Sidenote: FOSSIL FRUITS OF THE ISLE OF SHEPPEY.]
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