The Pleistocene of North America: and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95°Hay, Oliver Perry
Science
The Pleistocene of North America: and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95°
Hay, Oliver Perry
Paleontology -- North America; Paleontology -- Pleistocene; Vertebrates, Fossil
In the eighth volume of the Geological Survey of Illinois, on page 23,
Worthen wrote that some of the smaller bones of the mastodon and those
of the other animals, except the antlers of the elk, were preserved in
the State Museum of Natural History, at Springfield.
In the museum of the Chicago Academy of Science are, as reported by the
curator, Frank C. Baker, to Netta C. Anderson (Augustana Lib. Pubs. No.
5, p. 14), two rami of the lower jaw and several molars of a mastodon,
all well preserved. They are labeled as having been found in Macon
County, “6 miles from Abraham Lincoln’s first home” and as having been
presented by C. F. Günther. With these is an upper tooth which probably
belonged with the same lot as the lower jaw. There can hardly be a doubt
that this jaw and these teeth are those described by Worthen. The finder
had probably sold them to Mr. Günther, of Chicago, who had a private
collection.
The region about Niantic is within the area of the Illinoian drift, so
that the bones must have been deposited in the pond after the passing
away of the Illinoian ice-sheet.
Dr. F. C. Baker (Bull. Univ. Illinois, vol. XVII, p. 300), in speaking
of this case, says that the deposit rests on Illinoian drift and hence
it appears referable to the Sangamon interval. It seems to the present
writer that these animals belong to a later time, possibly the Late
Wisconsin. The locality is about 5 miles from Sangamon River. One might
suppose that time enough had elapsed after the Illinoian for the
drainage of the pond that must once have been there. Also, Worthen in
his account states the uplands are covered by loess from 6 to 20 feet in
thickness. One might expect that the pond would have been filled up with
the loess which had blown into it and which had been washed into it from
the surrounding higher land. These considerations are of course not
final. The Wisconsin moraine is not far away, and it is possible that
outwash from this was responsible for the pond and that the animals
lived after the glacier had passed away.
8. _Warsaw, Hancock County._—In Netta C. Anderson’s “Preliminary List of
Fossil Mastodon and Mammoth Remains in Illinois and Iowa” (Augustana
Lib. Pubs. No. 5) it was reported by Mr. C. K. Worthen, of Warsaw, that
a part of a mastodon tooth had been found sticking out of a bank of a
creek 5 miles below the town mentioned.
The writer has seen in the collection of the Philadelphia Academy, from
near Warsaw, a part of a lower second molar, labeled as having been
found at a depth of 10 feet, 3 miles east of the Mississippi River. It
was presented by G. W. Hall.
Public-domain text, read in full here on John Shaqi.
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