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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Triticites
Quantifying Late Pennsylvanian Multivariate Morphological Change in the Fusulinid Genus Triticites from the Central and Southwestern United States Available to Purchase
Heterochronic origin of spherical fusulinid foraminifera in the late Paleozoic Open Access
CONVOLUTIONAL NEURAL NETWORKS AS AN AID TO BIOSTRATIGRAPHY AND MICROPALEONTOLOGY: A TEST ON LATE PALEOZOIC MICROFOSSILS Available to Purchase
A TEST FOR THE POSSIBILITY OF PHOTOSYMBIOSIS IN EXTINCT FUSULINE FORAMINIFERA: SIZE AND SHAPE RELATED TO DEPTH OF HABITAT Available to Purchase
STRATIGRAPHY AND FORAMINIFERS FROM THE UPPERMOST CARBONIFEROUS (KASIMOVIAN-GZHELIAN) OF THE JAMANTOO AND BAIBICHETOO RANGES (MIDDLE TIEN-SHAN, KYRGYZSTAN) Available to Purchase
Fusulinid Taphonomy: Encrustation, Corrasion, Compaction, and Dissolution Available to Purchase
CHARACTERISTICS AND PALEOGEOGRAPHIC AFFINITIES OF THE EARLY GZHELIAN FUSULINOIDEANS FROM THE CANTABRIAN ZONE (NW SPAIN) Available to Purchase
FUSULINIDS: PREDATION DAMAGE AND REPAIR OF TESTS FROM THE UPPER PENNSYLVANIAN OF KANSAS Available to Purchase
Late fusulinellid early schwagerinid Foraminifera; relationships and occurrences in the Las Llacerias Section (Moscovian/Kasimovian), Cantabrian Mountains, Spain Available to Purchase
Wall structure and growth of fusulinacean Foraminifera Free
Early Permian Fusulinids from the Owens Valley Group, east-central California Available to Purchase
Sixty fusulinid species, 17 of which are newly named, are herein described from the Lower Permian part of the Owens Valley Group in east-central California. These consist of 2 species of Triticites , 1 of Leptotriticites , 16 of Schwagerina , 1 of Pseudofusulina , 3 of Chusenella , 1 of Paraschwagerina , 9 of Stewartina , 6 of Pseudoschwagerina , 3 of Chalaroschwagerina , 6 of Cuniculinella , 3 of Eoparafusulina , and 6 of Parafusulina . In addition, a new genus, Reticulosepta (with three species), is described. The fusulinid fauna of the Owens Valley Group contains some elements of the Pseudoschwagerina association of the Texas-Cordilleran region and a few species similar to those of the Chalaroschwagerina association of the eastern Klamath Mountains. In addition, several species apparently are endemic. Most of the fusulinids are from sediment-gravity-flow deposits in which there was apparently a great deal of mixing of faunas from different coexistent environments. In general, however, there is little evidence of mixing through reworking of older faunas, which has allowed biostratigraphic subdivision of the Lower Permian part of the Owens Valley Group based on fusulinids. The subunits recognized—lower Wolfcampian, middle Wolfcampian, upper Wolfcampian, and Leonardian—are comparable to subunits of the Lower Permian based on fusulinids in other parts of North America.