380 ANIMAL REMAINS FROM THE EXCAVATIONS AT ANAU. 
The latter alternative does not appear to me to be sufficiently justified, and 
I incline rather to the first idea, for the following reasons. 
We find in the layer at +30 feet the frontal piece of an adult animal with a 
little horn-core of 3.5 cm. length and a circumference of 7.3 cm. ‘This cranial 
piece must represent a transitional form to Ovis palustris, especially as no mistake 
as to the age of this animal is possible, because of the presence of a parietal piece 
which is connected with the frontal by the sutura coronalis. If this cranial piece 
had belonged to a young animal it would have broken open along the sutures 
when the skull was crushed, while in the old individual as a matter of fact the 
suture is still so firm that the bones would break before the sutures would open. 
Thus it seems that the long-tailed Ovis palustris form may have given rise 
to the long-tailed sheep (Maimene breed) which is still living in those regions, 
provided always that the formation of the fat tail, which was probably patholog- 
ical, did not originate until after the distribution of the turbary sheep to Europe, 
which possibly happened towards the end of the eneolithic period of Anau. The 
occurrence to-day of hornless female animals among the fat-tailed sheep and 
turbary sheep renders this explanation more probable. However, this view 
rests only upon speculation, for direct proofs are not to be had and probably 
never will be. 
In the tables on pp. 378-379, the extremity bones of the sheep of the Anau 
kurgan are brought together and compared with some accurately determined ex- 
tremity bones of subfossil or recent sheep. In these one can see that the larger 
wild sheep or its direct descendants occurred in the lower layers, while in the 
middle and upper layers the small palustris sheep predominated. 
Capra hircus rutimeyeri Duerst. (See plate 76, figs. 9 and 14.) 
The goat, of which we find the horn-cores and extremity bones among the 
bone remains from Anau, belongs, as already stated, in the uppermost layers 
of the North Kurgan. Really typical and well-preserved remains are very scarce. 
Of these there are some horn-core pieces and two perfectly preserved metacarpi, 
as well as the fragment of another. In these we can recognize a small short- 
horned goat, such as lives still, in a slightly differentiated form, in Central, Eastern, 
and Southern Asia, as well as in the Malayan Archipelago. One of the most primi- 
tive forms is without doubt the so-called wild goat of Crete, which is probably 
only a reversion from the domesticated to a wild state, very similar to Capra 
egagrus, and in which is embodied the exact type of the goat of the pile-dwellings. 
M. Evans has published from his excavations at Cnosse (Crete) of the second 
palace (about 1500 B. Cc.) a very perfectly preserved relief in faience representing 
a she-goat with her young.* The horns of this animal are much longer than those 
of the recent goat from Crete, figured in plate 78, fig. 5. 
The horn-cores differ from those of the sheep in the greater height to which 
the inner cavity extends, which leaves room for only a little dense substance at 
the point of the horn-core. 


* Salomon Reinach, La Créte avant |’Histoire, 1’ Anthropologie, 1904, p. 265, fig. 7. 
