A Pictorial Atlas of Fossil Remains, consisting of coloured illustrations selected from Parkinson's "Organic remains of a former world," and Artis's "Antediluvian phytology."Mantell, Gideon Algernon
Science
A Pictorial Atlas of Fossil Remains, consisting of coloured illustrations selected from Parkinson's "Organic remains of a former world," and Artis's "Antediluvian phytology."
Mantell, Gideon Algernon
Paleontology
[Illustration: Plate LXII.]
PLATE LXII.
Fossil Foraminifera.
With the exception of figs. 23, 24, 29, 31 and 32, all the specimens
delineated in this Plate belong to the Foraminifera. The figures
represent magnified views; the natural size is indicated in some
instances by a minute outline. Under the article "Foraminifera,"
in the "_Supplementary Notes_," a general account is given of the
structure and economy of the living animalcules. A list of names is
subjoined.
Figs. 1, & 2. _Rotalia trochiliformis_, of Lamarck. Tertiary.
Fig. 3. _Rotalia Beccarii_, of Linnæus. Tertiary.
Fig. 4. _Cristellaria rotulata_, Lamarck. Chalk.
Figs. 5, 6, 7. _Lituola nautiloidea_, Lamarck. Chalk.
Fig. 8. _Spirolina depressa_, Lamarck. This and the specimens to
fig. 21 inclusive, are tertiary fossils.
Fig. 9. _Spirolina cylindracea_, Lamarck.
Fig. 10. _Orthocerina clavulus._
Fig. 11. _Biloculina ringens_, Lamarck.
Figs. 12, & 13. _Quinqueloculina cor anguinum_, Lamarck.
Figs. 14, 15, & 16. _Quinqueloculina._
Figs. 17, 18, 19. _Triloculina trigonula_, Lamarck.
Fig. 20. _Quinqueloculina opposita_, Lamarck.
Fig. 21. _Peneroloplis opercularis_.
Fig. 22. _Adelosina_, of D'Orbigny; a recent species.
Figs. 23, & 24. _Gyrogonites_. The fossils here figured on a
magnified scale as microscopic shells of the same family as
those above described, received the name of Gyrogonites,
or twisted stones. They prove to be the seed-vessels of a
species of the common fresh-water plant, the _Chara_. The
fruit of this genus consists of minute nuclei, with an
external calcareous covering, composed of five spirally
twisted plates, which unite at the summit. These fossils
occur by myriads in many of the fresh-water secondary and
tertiary limestones, as well as in the calcareous deposits
now in progress of formation in our lakes. In the lacustrine
limestones of the Isle of Wight (at Binstead, White Cliff,
&c.), beautiful specimens may be obtained.[60] Professor E.
Forbes has discovered Gyrogonites in the Wealden strata of
the Isle of Purbeck, associated with shells of the genera
_Planorbis_, _Physa_, _Paluolina_, &c.
[Footnote 60: See Geological Excursions round the Isle of Wight. 2d
Edit. 1850, p. 108.]
Fig. 25. _Polystomella crispa_, of Linnæus. From the tertiary
strata of the Apennines.
Fig. 26. _Cristellaria ?_
Figs. 27, & 28. _Rotalia Beccarii_. Apennines.
Fig. 30. _Cristellaria galea_, of Lamarck. Apennines.
Fig. 29. Cast of a species of Area; a bivalve shell, from
tertiary strata, Bordeaux.
Fig. 31. A curious pteropodous shell (_Vaginella depressa_), from
tertiary strata, Basterot.
Fig. 32. This appears to be an imperfect specimen of a bivalve
having a fibrous structure, like _Pinna_. It is probably a
fragment of an Inoceramus.
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