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However, an indication of the threshold pore diameter, ideally not as an absolute value, but as a parameter to facilitate comparison between specimens, can be obtained from the differential pore volume-pore diameter relationships (Atahan et al. 2009).
Thus, there is little evidence that any chasmosaurine consistently added marginal ossifications during ontogeny, and any differences in count between specimens can be attributed to specific differences or individual variation (note that Godfrey and Holmes [36] suggested the number of undulations increased ontogenetically, an interpretation not supported here).
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Therefore, parameter transferability between different specimens can be investigated and comparative studies of predicted crack driving forces can be performed.
Between 16 and 384 specimens can be assayed in an experiment using procedures that can be automated and reagent costs much lower than a standard microarray [ 5].
Testing results of matched pairs of specimens can be considered comparable, better than specimens between different donors.
Hysteretic behaviors of the specimens can be effectively simulated, and differences of ultimate strengths between the experimental and numerical results are less than 9%.
Prized specimens can be several hundred years old.
Finally, self-healed specimens can be simply regarded as specimens characterized by a smaller crack.
But the largest specimens can be even more fertile.
The surviving rounded rim specimens can be readily distinguished from later 1907 strikes, as they have dots before, between, and after the words "Ten Dollars" on the reverse.
The mismatch between the species distribution data and the biome maps raised the question of whether georeferenced herbarium specimens can be validly used as surrogates for biome distribution.
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