A New Extinct Emydid Turtle from the Lower Pliocene of Oklahoma — John Shaqi
A New Extinct Emydid Turtle from the Lower Pliocene of OklahomaGalbreath, Edwin C. (Edwin Carter)
Science
A New Extinct Emydid Turtle from the Lower Pliocene of Oklahoma
Galbreath, Edwin C. (Edwin Carter)
Turtles, Fossil -- Oklahoma
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A New Extinct Emydid Turtle from the Lower
Pliocene of Oklahoma
BY
EDWIN C. GALBREATH
University of Kansas Publications
Museum of Natural History
Volume 1, No. 16, pp. 265-280, plate 1
August 16, 1948
University of Kansas
LAWRENCE
1948
UNIVERSITY OF KANSAS PUBLICATIONS, MUSEUM OF NATURAL HISTORY
Editors: E. Raymond Hall, Chairman; H. H. Lane, Edward H. Taylor
Volume 1, No. 16, pp. 265-280, plate 1
August 16, 1948
UNIVERSITY OF KANSAS
Lawrence, Kansas
PRINTED BY
FERD VOILAND, JR., STATE PRINTER
TOPEKA, KANSAS
1948
22-3340
[Illustration: PLATE 1. _Chrysemys limnodytes._ Univ. Kans.
Mus. Nat. Hist., Vert. Paleo. Coll. No. 7676. Fig. A, dorsal
view of carapace; fig. B, ventral view of plastron. Both views
approximately x .4.]
A New Extinct Emydid Turtle from the Lower Pliocene
of Oklahoma
By
EDWIN C. GALBREATH
In the summer of 1946 a party from the University of Kansas Museum of
Natural History visited exposures of the Laverne formation in Beaver
County, Oklahoma, at the invitation of Dr. Stuart Schoff of the United
States Geological Survey. When examining the marl beds an Emydid turtle
was discovered which appears to be an unnamed species of the genus
_Chrysemys_. A description of the new species follows.
Chrysemys limnodytes, new species
_Holotype._--University of Kansas Museum of Natural History No.
7676, vertebrate paleontological collection, a turtle consisting of
a fragmental anterior portion of a carapace, left part of the
plastron, and several marginals collected by the 1946
paleontological field party of the University of Kansas Museum of
Natural History.
_Geological Age and locality._--Marl beds of the Laverne formation,
early Pliocene age, in SW 1/4 Sec. 15, T. 4 N., R. 25 ECM, Beaver
County, Oklahoma. The specimen was removed from the marl
immediately below the fossil leaf zone (see Chaney and Elias, 1936;
Frye and Hibbard, 1940).
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