LOCALITY:
Khermin Tsav, Gobi Desert, Mongolia
AGE:
Late Cretaceous, Barun Goyot Formation, 75 million years
ago.
SIZE:
About the size of a large rat
PRONUNCIATION:
Ka-TOP-sa-lis
CLASSIFICATION:
MULTITUBERCULATA: Taeniolabididae
The mammals, those descendants of the
mammal-like reptiles, which thrived in the Permian and
Triassic only to disappear in the Jurassic, survived as
small animals during the time when dinosaurs were
supreme.
One of the most extensive records of
mammals of the Mesozoic Era in earth's history (the Age
of Reptiles or Dinosaurs) is to be found in the
Cretaceous rocks of the Peoples' Republic of Mongolia.
Catopsalis is one of the small
mammals known from Mongolia. It had a set of teeth very
similar to those of rodents and yet Catopsalis was
only distantly related to rats and mice. Catopsalis
belonged to a group of mammals now completely extinct
that arose about the time the dinosaurs did and persisted
until 40 million years ago.
This group, the multituberculates (in
reference to the many cusps on their molar teeth), was
one of the most diverse mammalian groups that lived
alongside (rather, underneath!) the dinosaurs.
When dinosaurs died out, the
multituberculates went into a marked decline, while other
groups of mammals diversified rapidly. Multituberulates
may have been the Cretaceous and early Cainozoic ('Age of
Mammals') counterpart of the rodents, which didn't appear
until about 50 million years ago. Interchange of animals
between North America and eastern Asia occurred
frequently in the Late Cretaceous. Presumably they moved
along a landbridge in the Bering Straits region.
Catopsalis is just one of the
many mammals that crossed this route as did several
dinosaurs such as Saurolophus and Corythrosaurus.Catopsalis,
a primitive mammal (multituberculate) skeleton and
restoration.(From The Fossil Book, courtesy of
Doubleday, New York)
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