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Table 1 Typicality and posterior probabilities of Holocene subfossil specimens belonging to extant genera, calculated using Mahalanobis distances

From: Skeletal variation in extant species enables systematic identification of New Zealand’s large, subfossil diplodactylids

   Typicality probabilities Posterior probabilities
D H M N W D H M N W
A AU7700 0.026 0.215 0.020 0.018 0.033  < 0.001 1  < 0.001  < 0.001  < 0.001
B S.33703.2 0.013 0.030 0.021 0.013 0.041  < 0.001  < 0.001  < 0.001  < 0.001 0.999
C S.33703.3 0.031 0.110 0.046 0.026 0.070  < 0.001 0.999  < 0.001  < 0.001  < 0.001
D S.33703.4 0.257 0.688 0.096 0.046 0.122  < 0.001 1  < 0.001  < 0.001  < 0.001
E S.33703.7 0.570 0.819 0.133 0.072 0.120  < 0.001 0.999  < 0.001  < 0.001  < 0.001
F S.33703.8 0.157 0.557 0.125 0.060 0.286  < 0.001 0.999  < 0.001  < 0.001  < 0.001
G S.38813.2 0.031 0.060 0.054 0.024 0.061  < 0.001 0.019 0.004  < 0.001 0.809
H S.39086 0.041 0.167 0.043 0.020 0.114  < 0.001 0.999  < 0.001  < 0.001  < 0.001
I S.46528.1 0.028 0.091 0.044 0.016 0.090  < 0.001 0.049  < 0.001  < 0.001 0.512
J VT791a 0.078 0.205 0.027 0.022 0.038  < 0.001 1  < 0.001  < 0.001  < 0.001
K WO333 0.177 0.742 0.088 0.050 0.105  < 0.001 1  < 0.001  < 0.001  < 0.001
  1. Highest typicality (p > 0.20) and posterior probabilities for each Holocene subfossil specimen are indicated in bold