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
The bones mentioned by Harlan had belonged to a young animal and
consisted of 5 vertebræ, a few fore-limb bones, a few hinder-limb bones,
a scapula, a rib, and a part of a molar tooth. Some of the articulating
surfaces still retained their cartilage. In the same cave were found
bones of “_Bos_” (_Bison_), “_Cervus_” (_Odocoileus?_), _Ursus_, and a
human metacarpal. These were said to have been found on the surface,
while the megalonyx bones were buried at a depth of 2 or 3 feet. The
mandible of the bear (Harlan, op. cit., p. 283) was described as
displaying appearances of antiquity equal to that of the megalonyx
bones. The sloth bones were made the basis of the name _Megalonyx
laqueatus_. In 1855 (Smithson. Contrib. Knowl., vol. VII, art. 5, p. 4),
Leidy determined that these bones belonged to _M. jeffersonii_. He wrote
that the collection consisted of one molar tooth, four dorsal vertebræ,
one lumbar, a left humerus lacking the upper epiphysis, the proximal
two-thirds of the right ulna, the right radius, the left scapula, the
distal epiphysis of the right femur, the left tibia, and the distal
epiphysis of the right tibia, a right calcaneum, two claws of a hinder
foot, and some fragments of ribs. Leidy appears to have concluded that
these bones had been those of a young animal, but that other bones in
the collection had belonged to adult individuals. He stated that they
had come from Bigbone Cave, White County. This adjoins Van Buren on the
north and possibly at that time included the latter; or Leidy may have
been mistaken. Besides the bones above mentioned, Harlan described from
this cave an ilium of _Megalonyx_ (Med. and Phys. Res., p. 334).
In 1892 (Bull. Geol. Soc. Amer., vol. III, pp. 121–123), Professor J. M.
Safford reported the discovery of some bones of a megalonyx in Bigbone
Cave. They had been met with in the bat manure at a depth of about 3
feet. The parts received by Professor Safford, and which are all
probably in Vanderbilt University, were the skull, 17 vertebræ
(including 5 sacrals), a fragment of a rib, a right scapula, a right
humerus, the two ilia, a part of the right pubis, a part of the right
ischium, and a left tibia. Safford concluded that these bones formed a
part of the same young animal that Harlan had described.
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