
Twenty-Third Annual Meeting and Symposium of the
Desert Tortoise Council, April 3-5, 1998
Abstracts

POSTER PRESENTATION
Geo- Bio- Chemistry of the Desert Tortoise: Trace Element Composition
of Carapace and Scute by Neutron Activation Analysis
Roy J. Knight, *Gordon B. Haxel, Kristin H. Berry, and Joseph L. Wooden
U. S. Geological Survey
Geologic Division, Denver Federal Center, MS 424, 6th & Ripling,
Denver, CO 80225
Geologic Division, 2255 N. Gemini Drive, Flagstaff, AZ 86001
Biological Resources Division, 6221 Box Springs Blvd., Riverside,
CA 92507
Geologic Division, Menlo Park, CA

The desert tortoise (Gopherus agassizii) is a federally listed
threatened species in the Mojave and Colorado desert portions
of its range in the Southwest. Diseases contributing to accelerated
tortoise mortality include upper respiratory tract disease, cutaneous
dyskeratosis (lesions of the scutes, the horny plates covering
the shell), and degeneration of the liver and kidney. Necropsies
by B. L. Homer and colleagues indicate elevated concentrations
of several potentially toxic metals in the liver and kidney of
some animals. We are investigating the abundances and sources
of trace elements, including potentially toxic metals, in desert
tortoise shell and scute by instrumental neutron activation analysis
(INAA), and by lead isotopic analysis, which should enable us
to distinguish natural and anthropogenic sources of lead.
Our initial, reconnaissance INAA investigations have two purposes:
to learn which chemical elements can be measured in desert tortoise
bone and scute, and to determine overall abundance levels. Two
tortoises from the northern Colorado Desert were analyzed: a healthy
subadult male (killed on a highway) and a diseased subadult female.
Gamma ray counts were performed at <1 hour, and 5, 7, 14, and
60 days after irradiation. At least 33 elements, including many
of the potentially toxic metals, can be measured with acceptable
accuracy and precision in tortoise bone, scute, or both.
Provisional inferences from these initial analyses are: (1) The
more electropositive (lithophile) transition elements (Sc, Ti,
V, Zr, Hf, Ta, rare earth elements, Th, U) are more readily accommodated
in the apatite of bone than in the keratin of scute. (2) Although
desert tortoises spend much of their time underground in burrows,
the data tentatively suggest minimal elemental input to the scute
through contact with soil or bedrock. (3) Trace element abundances
in tortoise bone are generally similar to those in human bone;
tortoise scute is likewise fairly similar to human nail material.
(4) Scute from the diseased tortoise shows relative depletion
in most of the elements determined. Whether this apparent difference
is an effect or a cause of disease, or simply variation between
two individuals, remains to be determined.
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