Within the Permian Word Formation, Glass Mountains. Texas, five ecological associations based on fusulinid species Intertongue complexly. The lateral ranges of species apparently relate to lateral changes of the dominant rock type in the formation and the vertical ranges reflect the expansion of newly evolved species and the gradual extinction of old species. Of the ten species described, the following four are new: Parafusulina wildei, P. sullivanensis, P. ironensis, and Parafusulina sp. A. The geographic ranges of P. lineata, P. deliclasensis, and P. aiitimonioensis are extended to include the Word Formation in the Glass Mountains
Ammonoids are among the best of index fossils and are particularly useful for intercontinental corre...
Embedded within the gray Permian limestones of the Finlay Mountains, trans-Pecos, Texas, are abundan...
Fusulinid faunas from various locations spread throughout the Cantabrian mountains are described as ...
Five fusulinid zones are recognizable in the Hess member of the Leonard formation in the eastern Gla...
From the Leonard Formation in the western part of the Glass Mountains, eleven species of fusulinids ...
Six collections from the lower part of the Lower Permian Bone Spring Formation (Leonardian) were obt...
Fusulinids from the Howe Limestone Member (upper part of the Red Eagle Limestone, lower part of the ...
The Hueco Mountains are a north-trending range which occupy an area of about 584 square miles in El ...
An endemic fusulinid assemblage is herein first described from Sakmarian rocks of the Central Pamir....
Fusulinids identified from the Macal Shale Group, Macal Series, south central British Honduras and S...
Triticites patulus Dunbar and Newell and Schwagerina adamsi sp. nov. from the early Wolfcampian (Per...
Thirty-nine samples (three of which were unproductive) from three different sections of the Pinery L...
Fusulinaceans consisting of 56 species belonging to 30 genera are distinguished from the Surmaq Form...
The tendency toward fine discrimination in fusulinid species has made necessary standardization in t...
The lower Leonardian (Lower Permian) Hess Limestone in the eastern part of the Glass Mountains, West...
Ammonoids are among the best of index fossils and are particularly useful for intercontinental corre...
Embedded within the gray Permian limestones of the Finlay Mountains, trans-Pecos, Texas, are abundan...
Fusulinid faunas from various locations spread throughout the Cantabrian mountains are described as ...
Five fusulinid zones are recognizable in the Hess member of the Leonard formation in the eastern Gla...
From the Leonard Formation in the western part of the Glass Mountains, eleven species of fusulinids ...
Six collections from the lower part of the Lower Permian Bone Spring Formation (Leonardian) were obt...
Fusulinids from the Howe Limestone Member (upper part of the Red Eagle Limestone, lower part of the ...
The Hueco Mountains are a north-trending range which occupy an area of about 584 square miles in El ...
An endemic fusulinid assemblage is herein first described from Sakmarian rocks of the Central Pamir....
Fusulinids identified from the Macal Shale Group, Macal Series, south central British Honduras and S...
Triticites patulus Dunbar and Newell and Schwagerina adamsi sp. nov. from the early Wolfcampian (Per...
Thirty-nine samples (three of which were unproductive) from three different sections of the Pinery L...
Fusulinaceans consisting of 56 species belonging to 30 genera are distinguished from the Surmaq Form...
The tendency toward fine discrimination in fusulinid species has made necessary standardization in t...
The lower Leonardian (Lower Permian) Hess Limestone in the eastern part of the Glass Mountains, West...
Ammonoids are among the best of index fossils and are particularly useful for intercontinental corre...
Embedded within the gray Permian limestones of the Finlay Mountains, trans-Pecos, Texas, are abundan...
Fusulinid faunas from various locations spread throughout the Cantabrian mountains are described as ...