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
A lobed zoophyte, resembling the above in its general form, and
long rootlets, is distinguished by a large central cavity, which is
continued above the body in the form of a cylinder.[203]
[203] Beautiful figures of these and other chalk zoophytes are given
by Mr. Toulmin Smith in his elegant memoir "On the Ventriculidæ."
The specimens above described are named _Bracholites_ by Mr. Smith.
The plan of the present work forbids the discussion of that author's
opinions and inferences.
Spongites (?) flexuosus. _Lign. 80, fig. 10._--Among the
cyathiform flints that abound in the chalk, a very elegant species
is distinguished by a flexuous band that runs round the margin, and
indicates the lobed structure of the original.
In the chalk of Flamborough Head, Yorkshire, many beautiful cyathiform
sponges are preserved, in which the outer surface is thickly covered
with projecting hollow papillæ; these fossils are generally silicified,
the surface and pores being frosted over with minute quartz crystals.
The museum of the York Institution contains a splendid series of these
spongites.[204]
[204] The silicified state of these zoophytes was first detected by Mr.
Charlesworth, who by immersing specimens in dilate hydrochloric acid,
obtained admirable examples of the delicate structure of the original.
[Sidenote: FOSSIL ZOOPHYTES OF FARINGDON.]
Fossil Zoophytes of Faringdon. _Lign. 70, 71, 72._--The richest
locality for fossil sponges in England is in the immediate
neighbourhood of the little town of Faringdon, in Berkshire.[205] The
Greensand beds that overlie the Oolite in that district, consist of
a coarse friable aggregation of sand, comminuted shells, corals,
amorphozoa, and echinoderms, more or less consolidated by a ferruginous
cement. The gravel-pits, as the quarries are locally termed, expose
what evidently were banks of detritus thrown up on the strand of a
sea-margin; among the water-worn and fragmentary relics of oolitic as
well as cretaceous forms, many perfect sponges of various kinds may be
collected in the course of a few hours. Figures of some of the common
species are subjoined.
[205] See Excursions, in vol. ii.
[Illustration: Lign. 70. Fossil Zoophytes.
Fig. 1.--Lunulites radiatus. _Preston Chalk-pits_; view of the convex
side. (_Mr. Walter Mantell._)
1_a_.--Front view; _nat._
1_b_.--Portion of the surface of fig. 1, magnified.
2.--Scyphia intermedia; 1/2 _nat._ _Faringdon._
3.--Lithododendron sociale: the left-hand branch shows a vertical
section at the upper part, displaying the internal structure;
1/2 _nat._ _Mountain Limestone, Yorkshire._
4.--Verticillipora anastomosans. _Faringdon._
5.--Scyphia ramosa; 1/2 _nat._ _Faringdon._
6.--Scyphia foraminosa; 1/2 _nat._ _Faringdon._
7.--Cnemidium astrophorum; 1/3 _nat._ _Faringdon._
]
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