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He then describes the actual stone which passes as the toad-stone, or "Bufonius lapis," and says that it is also called batrachite, or brontia, or ombria. His description exactly corresponds with the "toad-stones" which are well known at the present day in collections of old rings. The palate of the fossil fish Lepidotus, showing the stud-like teeth in position.

Lepidopters as butterflies, etc. 5. Hemipters as cicada, plant-lice, fleas, etc. 6. Coleopters as cockchafers, fire-flies, etc. 7. Dipters as gnats, musquitoes, flies. 8. Rhipipters as stylops. 9. Parasites as acara, etc. 10. Thysanurans as lepidotus, flying-lice, etc.

In all the essentials of its very peculiar structure, the 'Macropoma' of the Chalk is identical with the 'Coelacanthus' of the Coal. Look at the genus 'Lepidotus', again, persisting without a modification of importance from the Liassic to the Eocene formations inclusive.

It is represented in the present seas by the delicate and rare Pentacrinus caput-medusae of the Antilles, which, with Comatula, is one of the few surviving members of the ancient family of the Crinoids, represented by so many extinct genera in the older formations. Scales of Lepidotus gigas. Agass. a. Aechmodus Leachii and Dapedius monilifer. a. Aechmodus. Restored outline. b.

The Nile had some curious fish peculiar to itself, as the oxyrinchus, the lepidotus, the Perca Nilotica, the Silurus Schilbe Niloticus, the Silurus carmuth and others. Great numbers of fish, mostly of the same species with those of the Nile, were also furnished by the Lake Moeris; and from these a considerable revenue was derived by the Great Kings.

These are based on a purely marine deposit, with Pecten, Modiola, Avicula, and Thracia. Below this, again, come limestones and shales, partly of brackish and partly of fresh-water origin, in which many fish, especially species of Lepidotus and Microdon radiatus, are found, and a crocodilian reptile named Macrorhynchus.

I recognised them at once as the palatal teeth of a fossil fish called "Lepidotus," common in our own oolitic and wealden strata, and in rocks of that age all over the world. They were white and colourless in life, but are stained of various colours according to the nature of the rock in which they were embedded.

In all the essentials of its very peculiar structure, the 'Macropoma' of the Chalk is identical with the 'Coelacanthus' of the Coal. Look at the genus 'Lepidotus', again, persisting without a modification of importance from the Liassic to the Eocene formations inclusive.

In the daytime, the Motuca, a much larger and more formidable fly than the mosquito, insisted upon levying his tax of blood. We had been tormented by it for many days past, but this place seemed to be its metropolis. The species has been described by Perty, the author of the Entomological portion of Spix, and Martius' travels, under the name of Hadrus lepidotus.

In all the essentials of its very peculiar structure, the Macropoma of the Chalk is identical with the Coelacanthus of the Coal. Look at the genus Lepidotus, again, persisting without a modification of importance from the Liassic to the Eocene formations inclusively.