Late Pennsylvanian-Early Triassic conchostracan biostratigraphy: A preliminary approach species and marine index fossils such as conodonts and
fusulinids, allow us to correlate our assemblage
A geomagnetic polarity timescale for the Permian, calibrated to stage boundaries succession of
fusulinid zones, the later Cisuralian and Guadalupian to a conodont and
fusulinid Late Paleozoic–early Mesozoic continental biostratigraphy — Links to the Standard Global Chronostratigraphic ScaleSchneider J.,
Lucas S.,
Scholze F.,
Voigt S.,
Marchetti L.,
Klein H.,
Opluštil S.,
Werneburg R.,
Golubev V.,
Barrick J.,
Nemyrovska T.,
Ronchi A.,
Day M.,
Silantiev V.,
Rößler R.,
Saber H.,
Linnemann U.,
Zharinova V.,
Shen S. , the nonmarine strata produce biochronologically significant fossils and the marine strata yield
fusulinids