Nearly 50 sections through the Llandovery and Wenlock black shales of
the Barrandian area (Bohemia) have been examined bed by bed. This has
made possible the compilation of an improved and well defined graptoli
te zonal scheme with much new biostratigraphic data included. A total
of 268 graptolite species and subspecies have been found. Their strati
graphic distribution allows the recognition of 27 graptolite zones: as
census-acuminatus, vesiculosus, cyphus, triangulatus-pectinatus, simul
ans, convolutus, sedgwickii, linnaei, turriculatus, crispus, griestoni
ensis, tullbergi, spiralis, grandis, insectus, centrifugus, murchisoni
, riccartonensis, dubius, belophorus, rigidus, ramosus-perneri, lundgr
eni, parvus, nassa-frequens, praedeubeli-deubeli, ludensis, and severa
l subzones. The biozones are defined by the vertical ranges of their '
index' species and are characterized by rich accompanying associations
. The zonal scheme is correlated with graptolite sequences elsewhere.