TABLE 1. The latent roots and vectors of the stratigraphically lower (i.e., older, 1810 m) sample of Brizalina.
|
Percentages of the latent roots |
|||
|
1 |
2 |
3 |
4 |
|
59.127 |
37.825 |
2.051 |
0.997 |
|
Latent vectors by columns |
|||
|
1 |
2 |
3 |
4 |
|
0.628 |
0.000 |
0.499 |
0.598 |
|
0.182 |
0.738 |
-0.580 |
0.293 |
|
0.096 |
0.623 |
0.544 |
-0.554 |
|
0.751 |
-0.259 |
-0.345 |
-0.500 |
TABLE 2. The latent roots and vectors of the stratigraphically younger core-sample of Brizalina (i.e., 1718 m)
|
Percentages of the latent roots |
|||
|
1 |
2 |
3 |
4 |
|
61.441 |
29.275 |
6.181 |
3.102 |
|
Latent vectors by columns |
|||
|
1 |
2 |
3 |
4 |
|
0.387 |
0.651 |
0.139 |
-0.638 |
|
0.367 |
-0.134 |
0.878 |
0.276 |
|
0.764 |
-0.521 |
-0.353 |
-0.145 |
|
0.365 |
0.535 |
-0.291 |
0.704 |
TABLE 3. Latent roots and vectors for five taxonomic distance traits (N = 18) for the species of ostracods Neobuntonia airella, Oligocene, Bells Headland, Victoria, Australia ( McKenzie et al., 1991).
|
Latent roots |
Latent vectors by rows |
|||||
|
Root No. |
Percent |
1 |
2 |
3 |
4 |
5 |
|
1. |
0.01306 (81.48%) |
0.1627 |
0.2506 |
0.9270 |
0.1609 |
0.1596 |
|
2. |
0.00244 (15.20%) |
0.4782 |
0.5868 |
-0.3690 |
0.4752 |
0.2549 |
|
3. |
0.00031 (1.94%) |
0.0558 |
-0.6911 |
0.0012 |
0.5456 |
0.4708 |
|
4. |
0.00015 (0.95%) |
0.0480 |
0.0677 |
-0.0585 |
-0.6022 |
0.7919 |
|
5. |
0.00007 (0.43%) |
-0.8600 |
0.3327 |
-0.0330 |
0.2965 |
0.2467 |
TABLE 4. The "Peronian" components of the first latent vector for Brizalina for sampling levels of the Ikang borehole cores.
|
Depth of Sample |
Components of the first latent vector |
|||
|
(in metres) |
1 |
2 |
3 |
4 |
|
1718 |
0.387 |
0.367 |
0.764 |
0.365 |
|
1740 |
0.621 |
0.146 |
0.200 |
0.744 |
|
1763 |
0.621 |
0.383 |
0.307 |
0.611 |
|
1787 |
0.558 |
0.456 |
0.284 |
0.633 |
|
1810 |
0.628 |
0.182 |
0.096 |
0.751 |
