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The remains of six additional specimens were recovered from other Kayenta localities in Arizona in 1983 by American paleontologist James M. Clark.
Specimens were recovered from nasal, axillary and rectal swabs.
The specimens were recovered from a creek near San Rafael, Mendoza Province, western Argentina, in the lower section of the Puesto Viejo Group, the Quebrada de los Fósiles Formation, considered as Early Triassic in age.
Both specimens were recovered from the Oldman Formation in the Judith River Group of Alberta.
The three known Deinocheirus specimens were recovered from the Nemegt Formation in the Gobi Desert of southern Mongolia.
Two measurable proximal tibial specimens were recovered.
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Instead, specimens are recovered as close relatives of shallow-water species.
Most of the relationships are resolved with high confidence, and species that were represented by more than one specimen were recovered as monophyletic.
These clockwork fuzes were also used for long-range shrapnel firing; inevitably, an undamaged specimen was recovered by the British, and the secret was out.
The DNA extracted from the denatured specimen was recovered in 57/60 (95%) of the samples.
After hydrothermal crystallization at 453 K for 24 h, the ZnAlPO4 solid specimen was recovered by filtration, washed with deionized water until neutrality, and dried.
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