First report of acrotretoid brachiopod shell beds in the lower Cambrian (Stage 4) Guanshan Biota of eastern Yunnan, South China

Brachiopod shell accumulations are abundant and diverse in the lower Cambrian strata of Yunnan Province,South China, but most commonly they are composed of linguloid and acrotheloid brachiopods. Here, we describe the firstrecord of shell beds with high-density accumulations of microscopic acrotretoid brachiopods (usually <2 mm in width) inthe muddy deposits of the Wulongqing Formation (Guanshan Biota, Cambrian Stage 4) in the Wuding area of YunnanProvince. The acrotretoid shell beds from the Wulongqing Formation vary from thin mm-thick pavements to more well-developed beds, several centimeters thick. The occurrence of remarkably rich acrotretoid shell beds indicates that micro-scopic lingulates began to exert an important role in hardening and paving the soft-substrate seafloor during the earlyCambrian evolution of Phanerozoic “mixgrounds.” The new Guanshan material is referred to a new species, Linnarsso-nia sapushanensis n. sp., which differs from other species of Linnarssonia mainly in having a well-developed internalpedicle tube, as well as a relatively longer dorsal median septum. The occurrence of Linnarssonia sapushanensis n. sp. inthe Wulongqing Formation in eastern Yunnan extend the oldest record of the genus on the Yangtze Platform of SouthChina back to at least Cambrian Stage 4.