Skip to main content

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