中国科学院南京地质古生物研究所机构知识库

Abundant well-preserved shelly fossils of Sinotubulites occur in the upper part of the late Neoproterozoic Dengying Formation in Ningqiang County, Shaanxi Province, China. Unlike 'funnel-in-funnel' structures of co-occurring Cloudina shells, the tube of Sinotubulites is nearly cylindrical, composed of several thin layers and characterized by 'tube-in-tube' structure. The tube bears prominent longitudinal sculptures and/or irregular annulations, which were formed by the wrinkles of tube layers, and weaken gradually towards the inner layers. The irregular wrinkle ornament of the outer layer shows plastic feature of the Sinotubulites tubes, which may further imply that the organisms secrete the elastic and flexible organic-dominated walls with mineralization, possibly aragonitic. Detailed thin section and SEM studies indicate that the silicification occurred earlier than phosphatation. Specimens preserved in situ from Hubei and surface ornamentation and polygonal shape of the cross-section suggest that Sinotubulites probably lived as an epibenthos lying on the sea floor.