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 Fruits of Chara. (_Gyrogonites._) _Lign. 66._--The Chara is a
well-known inhabitant of almost every stream and rivulet. The stems
are hollow, and composed of tubes filled with a fluid in which green
globules circulate; they form beautiful microscopic objects for
exhibiting the circulation in vegetables. The fruit consists of very
small nuclei, contained in a calcareous pericarp, composed of five
spirally twisted plates, that unite at the summit. These seed-vessels,
when first discovered in a fossil state, were supposed to be the shells
of mollusks, and a genus was formed for their reception with the name
of _Gyrogonites_ (_twisted-stones_); a term still employed, though the
vegetable nature of these bodies is well known. In _Plate III. fig. 5_,
a branch of the common Chara with seeds is represented: and figures
of the seed-vessels, of two fossil species are given in _Lign. 66,
figs. 1, 2_.
Specimens of the fossil fruits and stems of Charæ, may be collected
in abundance in the fresh-water limestone at East Cliff Bay, Isle of
Wight.[171]
[171] See my Geology of the Isle of Wight, _Lign. 5_, p. 109.
[Illustration: Lign. 66. Fossil Fresh-water Plants.
_Eocene, Paris._
Fig. 1.--Seed-vessel of _Chara helicteres_ × 10; side view.
1_a_.--View of the base of the same.
1_b_.--One of the spiral valves separated.
1_c_.--View from above.
2.--Seed-vessel of _Chara medicaginula_ × 10. The upper
figure is a side view: the lower, a view of the base.
3.--_Carpolithes ovulum_, magnified side view.
3_a_.--The same, natural size.
3_b_.--Magnified view of the base of the same.
4.--A piece of fresh-water limestone, with impressions
of two stems of _Nymphea arethusa_ ×.
]
The _Purbeck beds_ at Durlstone Bay, near Swanage, also contain
numerous Gyrogonites associated with fresh-water shells. The bands of
siliceous sinter, which occur in the lowermost deposits, are especially
rich in these remains.[172]
[172] I am indebted to the Rev. Osmond Fisher, of Dorchester, for a fine
suite of these and other interesting fossils from the Purbeck beds of
Ridgway and Osmington, near Weymouth; and to William Shipp, Esq., of
Blandford, and Edward Woodhouse, Esq., of Ansty, for many specimens
from Durlstone Bay, and Ridgway.
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