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Exact(1)
Rbc L sequences between these two specimens differed by about 2.6%.
Similar(59)
Between these six specimens, the majority of the cranial and postcranial osteology of G. stipanicicorum is known.
Similar FTIR spectra were obtained from calcified nodules present in the five different specimens that were subjected to FTIR-RM and Ca/P ratios obtained with SEM/SDD-EDS from two of these five specimens were very similar between the two specimens and between the two large calcified regions in the same specimen (Calc1).
Important differences between the two specimens are observed owing to the different size and amount of reinforcing steel.
X-ray diffraction analyses performed on material from the failed 25 and 950 °C specimens highlights a distinct difference in mineralogy between the two specimens that has been related to mineralogical changes in the sandstone cement with heating.
The inclination of the planum alveolare is similar between the two specimens.
The divergence between the two specimens of Barbourula busuangensis appears to have occurred during the Pleistocene.
Comparisons between the two specimens suggest that the complete sacral configuration of Melanosaurus readi includes two dorsosacrals, followed by the two primordial sacrals, and a single caudosacral (A. Yates, pers. com).
Although there are some variations between the two specimens, the results show two common features.
FMRFamide-like-IR was not consistent between the two specimens investigated.
Similar staining between the two specimens is shown for CK 7 and CK 5/6.
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