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福建宁化上石炭统类生物地层自下而上划分为4带3亚带:1)Pseudoendothyraninghuaensis带,2)Fusulina-Fusulinella带,其中包括Fusulinellahelenae-Pseudostaffellapaxadoxa亚带、Beedeinamayiensis亚带和Fusulinaquasicylindrica亚带,3)Protriticitesobsoletus带和4)Montiparusmontiparus-Quasifusulinafusiformis带。该区生物地层可与我国华南、华北和西北沉积区以及俄罗斯地台同期地层进行对比,其年代地层归属于上石炭统达拉阶至逍遥阶下部,相当于国际地层表上石炭统(宾夕法尼亚亚系)的莫斯科阶和卡西莫夫阶。
The upper Carboniferous biogenic strata in Ninghua, Fujian Province are divided into four zones and three sub-zones from bottom to top: 1) Pseudoendothyraninghuaensis zone, 2) Fusulina-Fusulinella zone, including Fusulinella helenae-Pseudostaffellapaxadoxa zone, Beedeinamayiensis zone and Fusulinaquasicylindrica zone, 3) Protriticites obsoleteus and 4) Montiparus montiparus-Quasifusulinafusiformis bands. The biostratigraphy of this area can be compared with the contemporaneous stratigraphy of the sedimentary areas in South China, North China and Northwest China and the platform of Russia. The chronostratigraphic belonged to the lower part of the Upper Carboniferous from the Dalat to the Xiaoyao step, which is equivalent to the Carboniferous in the international stratigraphic table Department) of the Moscow and Kasimov order.