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Palmatolepis
Frasnian-Famennian transition in western Thailand: conodonts, biofacies, eustatic changes, extinction
Palmatolepis spallettae , new name for a Frasnian conodont species
Conodonts across the Devonian/Carboniferous boundary: a review and implication for the redefinition of the boundary and a proposal for an updated conodont zonation
Record of climate-driven morphological changes in 376 Ma Devonian fossils
CONODONT BIOSTRATIGRAPHY OF THE CHATTANOOGA SHALE, MIDDLE AND UPPER DEVONIAN, SOUTHERN APPALACHIAN BASIN, EASTERN UNITED STATES
FRASNIAN (UPPER DEVONIAN) CONODONT SUCCESSION AT HORSE SPRING AND CORRELATIVE SECTIONS, CANNING BASIN, WESTERN AUSTRALIA
Morphometrics of the Late Devonian conodont genus Palmatolepis : phylogenetic, geographical and ecological contributions of a generic approach
CONODONTS OF THE WILLIAMS ISLAND AND LONG RAPIDS FORMATIONS (UPPER DEVONIAN, FRASNIAN-FAMENNIAN) OF THE ONAKAWANA B DRILLHOLE, MOOSE RIVER BASIN, NORTHERN ONTARIO, WITH A REVISION OF LOWER FAMENNIAN SPECIES
Novel paleoecology of a postextinction reef: Famennian (Late Devonian) of the Canning basin, northwestern Australia: Comment and Reply: COMMENT
Upper Devonian conodonts from the Timan-Pechora region, Russia, and correlation with a Frasnian composite standard
Late Devonian conodonts define the precise horizon of the Frasnian–Famennian boundary at Cinquefoil Mountain, Jasper, Alberta
Multielement reconstructions of Palmatolepis and Polygnathus (Upper Devonian, Famennian) from the Canning Basin, Australia, and Bactrian Mountain, Nevada
Late Devonian (Frasnian and Famennian) conodonts from the Wadleigh Limestone, southeastern Alaska
Quantification of outlines in Frasnian (Upper Devonian) platform conodonts
The standard Late Devonian conodont zonation between the top of the Upper marginifera Zone and the earliest Carboniferous Siphonodella sulcata Zone is revised to replace the former velifer , styriacus , and costatus zonal groups, which were based primarily on genera other than Palmatolepis , and to eliminate a hiatus above the Upper costatus Zone. The changes were enabled by a new phylogenetic model of Palmatolepis , by range extensions that bridge former gaps between the records of some Palmatolepis taxa, and by further taxonomic revisions of some double-rowed Bispathodus taxa. Basing the standard zonation on conodonts of primarily pelagic biofacies permits construction of parallel, alternative zonations for shallower water biofacies and estimation of phylogenetically more precise zonal timespans.