Family
Cricetidae FISCHER
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[DE WALDHEIM], 1817
The
Cricetidae
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are a very successful and widespread clade of mammals, with a good fossil record, and they are widely recognized as the rodents that evolved into the clade
Muridae in
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the Miocene Epoch and the clade
Arvicolidae
in the Pliocene Epoch. Much of the terminology and knowledge of fossil cricetids was described by the German palaeontologist Samuel Schaub (1925), who called these rodents “
Cricetodontidae
”. A later German palaeontologist, Volker Fahlbusch (1964) collected much more abundant material from southern Germany, and assigned much of Schaub’s “
Cricetodontidae
” into two large subgroups he called the genera
Democricetodon
and
Megacricetodon
. Fahlbusch’s subgroups can be easily recognized dentally by
Democricetodon
having a single cusped anterocone on M1 and
Megacricetodon
having a bicusped anterocone on M1. Actually, Fahlbusch had identified a third group among the cricetids from Germany that he called
Cotimus
, a genus described from North America. Fahlbusch later decided that
Megacricetodon
and
Cotimus
are the same genus, so we now recognize two major groups among the Miocene
Cricetidae
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,
Democricetodon
and
Megacricetodon
. Another feature of
Democricetodon
is that it sometimes has what can be called two mesolophs, thin ridges of enamel that are directed labially between the two main labial cusps (paracone and metacone) in upper teeth, or two mesolophids, similar thin ridges that are directed lingually in the middle of lower teeth.
Democricetodon
from Pakistan may have two mesolophs (upper teeth) or mesolophids (lower teeth) in its dentition in which case the anterior loph is derived from the protocone (id) posterior spur and the posterior loph is derived from the mure. This (along with other features) is how we recognize
Democricetodon
in Miocene deposits of Pakistan.