A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological MonumentsLyell, Charles, Sir
Science
A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological Monuments
Lyell, Charles, Sir
Geology
_Triassic Mammifer (Microlestes antiquus Plieninger.)_--In the year 1847,
Professor Plieninger, of Stuttgart, published a description of two fossil
molar teeth, referred by him to a warm-blooded quadruped[xiii-A], which he
obtained from a bone-breccia in Wuertemberg occurring between the lias and
the keuper. As the announcement of so novel a fact has never met with the
attention it deserved, we are indebted to Dr. Jaeger, of Stuttgart, for
having recently reminded us of it in his Memoir on the Fossil Mammalia of
Wuertemberg.[xiii-B]
Fig. 529. represents the tooth first found, taken from the plate published
in 1847, by Professor Plieninger; and fig. 530. is a drawing of the same
executed from the original by Mr. Hermann von Meyer, which he has been
kind enough to send me. Fig. 529. is a second and larger molar, copied from
Dr. Jaeger's plate lxxi., fig. 15.
[Illustration: Fig. 529. _Microlestes antiquus_, Plieninger. Molar tooth
magnified. Upper Trias, Diegerloch, near Stuttgart, Wuertemberg.
_a._ View of inner side?
_b._ same, outer side?
_c._ Same in profile.
_d._ Crown of same.]
[Illustration: Fig. 530. _Microlestes antiquus_, Plien.
View of same molar as No. 529. From a drawing by Herman von Meyer.
_a._ View of inner side?
_b._ Crown of same.]
[Illustration: Fig. 531. Molar of _Microlestes_? Plien. 4 times as large as
fig. 529. From the trias of Diegerloch, Stuttgart.]
Professor Plieninger inferred in 1847, from the double fangs of this tooth
and their unequal size, and from the form and number of the protuberances
or cusps on the flat crowns, that it was the molar of a Mammifer; and
considering it as predaceous, probably insectivorous, he called it
Microlestes, from +mikros+, little, and +lestes+, a beast of prey. Soon
afterwards, he found the second tooth also, at the same locality,
Diegerloch, about two miles to the south-east of Stuttgart. Some of its
cusps are broken, but there seem to have been six of them originally. From
its agreement in general characters, it is supposed by Professor Plieninger
to be referable to the same animal, but as it is four times as big, it may
perhaps have belonged to another allied species. This molar is attached to
the matrix consisting of sandstone, whereas the tooth, No. 529., is
isolated. Several fragments of bone, differing in structure from that of
the associated saurians and fish, and believed to be mammiferous, were
imbedded near them in the same rock.
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