L. Ginsburg et al., THE RUMINANTS (ARTIODACTYLA, MAMMALIA) FROM THE LOWER MIOCENE OF CETINA-DE-ARAGON (PROVINCE OF ZARAGOZA, ARAGON, SPAIN), Proceedings of the Koninklijke Nederlandse Akademie van Wetenschappen, 97(2), 1994, pp. 141-181
The study of the lower Miocene ruminants from Cetina de Aragon has per
mitted the identification of five species. Three of these, Andegameryx
andegaviensis Ginsburg, Pomelomeryx gracilis (Pomel), and Oriomeryx m
ajor (Viret), were previously found in localities in France. The oldes
t known record of Andegameryx andegaviensis Ginsburg is from Cetina de
Aragon. The new material from Cetina de Aragon, determined as Oriomer
yx major proves the close affinities of this species with Amphitragulu
s elegans. The other two species, Dremotherium celinensis nov. sp. and
Bedenomeryx truyolsi nov. sp., are described for the first time from
this locality. Dremotherium cetinensis nov. sp. is differentiated from
D. feignouxi by its more hypsodont dentition. B. truyolsi nov. sp. is
a large-sized species which has its last known occurrence in Cetina d
e Aragon. The species described from Cetina de Aragon provide firm evi
dence of the existence of three well-defined ruminant lineages in the
early Miocene. The first lineage is formed by Pomelomeryx, Oriomeryx a
nd Bedenomeryx which, together with Amphitragulus, form a homogeneous
group of which the larger-sized species could be related to palaeomery
cids. The second lineage is represented by Dremotherium whose evolved
dental morphology is comparable to that found in the first cervids. Fo
r this reason we have related Dremotherium to this pecoran family. The
third lineage is formed by Andegameryx. The phylogenetic relationship
of Andegameryx with the two above-mentioned lineages and with the bov
ids and giraffids appears problematical because of its primitive denta
l morphology. This study includes an updated list of the mammal fauna
from Cetina de Aragon, with the exception of the Marsupialia, Insectiv
ora and Chiroptera. According to its composition the rodent assemblage
may be correlated to the lower part of early Miocene Standard zone MN
2.