Despite our growing knowledge of the relationships of Pliocene faunas of Asia and North America, relatively few cases are on record in which a given mammalian genus has been found to occur in both continental areas. It is a matter of considerable interest therefore, to discover in the collections of fossil mammals obtained by the California Institute in the Kern River Pliocene deposits of California, a mustelid that resembles closely Eomellivora wimani, described by Zdansky from the red clays of the provinces of Honan and Shansi, China. Indeed, so similar are these two forms that an examination of our specimen, in the light of Zdansky's description and good illustrations of the Chinese material, makes it difficult to establish any...
In 1920 Stock described the fragmentary remains of three mammalian types (Hypertragulus sp., Caenopu...
A newly discovered maxillary dentition from the Early Eocene rocks of the Bighorn Basin, Wyoming, is...
In several papers, published in the PROCEEDINGS,(1) I have described some of the very late Eocene ma...
Despite our growing knowledge of the relationships of Pliocene faunas of Asia and North America, re...
Of the several occurrences of Hyaenognathus in the Pliocene and Pleistocene of North America three a...
Systematic collecting over a number of years in the Thousand Creek beds of northwestern Nevada has ...
The artiodactyla found at the Kew Quarry site in the Sespe deposits of the Las Posas Hills, Ventura...
Rare fossil mammals from Hengdong in the Hengyang Basin of southern China have provided unusual oppo...
Rodents are of rather common occurrence in the later Tertiary of North America, yet voles have been ...
The concentration of fossil vertebrate remains at the Kew Quarry site in the Sespe deposits of the L...
Since publication of the description and discussion of the Thousand Creek fauna in 1911, further col...
From 1932 to 1950 vertebrate fossils were collected in the Hungry Valley area located in the north...
It becomes increasingly clear that the faunal stage represented at Locality 150 in the Sespe deposit...
Since the announcement(1) of the discovery of upper Eocene mammals in the Sespe deposits north of th...
In addition to three distinct types of hyaenodonts now known from the Sespe Upper Eocene(1) (Localit...
In 1920 Stock described the fragmentary remains of three mammalian types (Hypertragulus sp., Caenopu...
A newly discovered maxillary dentition from the Early Eocene rocks of the Bighorn Basin, Wyoming, is...
In several papers, published in the PROCEEDINGS,(1) I have described some of the very late Eocene ma...
Despite our growing knowledge of the relationships of Pliocene faunas of Asia and North America, re...
Of the several occurrences of Hyaenognathus in the Pliocene and Pleistocene of North America three a...
Systematic collecting over a number of years in the Thousand Creek beds of northwestern Nevada has ...
The artiodactyla found at the Kew Quarry site in the Sespe deposits of the Las Posas Hills, Ventura...
Rare fossil mammals from Hengdong in the Hengyang Basin of southern China have provided unusual oppo...
Rodents are of rather common occurrence in the later Tertiary of North America, yet voles have been ...
The concentration of fossil vertebrate remains at the Kew Quarry site in the Sespe deposits of the L...
Since publication of the description and discussion of the Thousand Creek fauna in 1911, further col...
From 1932 to 1950 vertebrate fossils were collected in the Hungry Valley area located in the north...
It becomes increasingly clear that the faunal stage represented at Locality 150 in the Sespe deposit...
Since the announcement(1) of the discovery of upper Eocene mammals in the Sespe deposits north of th...
In addition to three distinct types of hyaenodonts now known from the Sespe Upper Eocene(1) (Localit...
In 1920 Stock described the fragmentary remains of three mammalian types (Hypertragulus sp., Caenopu...
A newly discovered maxillary dentition from the Early Eocene rocks of the Bighorn Basin, Wyoming, is...
In several papers, published in the PROCEEDINGS,(1) I have described some of the very late Eocene ma...